MISSIONA RY R E •' E -\ R C H Uni O' 5041 Broadway , : ev> LIBRARY on ork City »• IS* _ THE HIMALAYAN DISTRICTS OF THE s NORTH-WESTERN PROVINCES OF INDIA, EDWIN T. ATKINSON, B.A., F.R.G.S. VOL. I. CF 0 R M ! N G VOLUME X. OF THE GAZETTEER, N.-W. P.) ALLAHABAD: SORT II- WESTERN TBOVINCES AND OUDH GOVERNMENT PRESS. 1 8 82. o o AZETT fra-m^unyl / \ S | ^Dpcrn&x* I ^\tyeangri* arty ! f\\ \ 188§3 a ^Chagycosicnu^ ^Zcumjja, ^T^Li'a-k / S * /> t? J 1 £^wnla,Kha*\ l t' ■ ■ -p)uru iun v. 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K: JflBr-vnqjLa, \\%> drri' ■ ' . 1 -j - \\,£’ i^cu-dh^.Feah 30 aiigyaim^ \ ^ .4*000 f,s Si3b' %i '&¥>“*' ' / » / / G J SHAHABAO (Burae^h 3XHYRABAD! JtdraJnpoc \ib$tu» Rjnmwghur » ^Adampoor LU K NOW (jBctUah 300GOWLEE 0 VTory* Sooji , Urny Sxy CAWNPOOf*^ 'DhanRsee Bengal t Sshar, prdtmvuvy Camp datum Map on. SJhrJKtht tothlneh. bateden&Jci.rfurvey, fim Auote to Tttalpa., 10 the Sou A JX Hookers Sikkim- Map. I Cip^' S. SKermOj Recenru. Sumy Mop cf J/asjeetaig jyu/reed , to the huh. to the Soft Kwnaoan.irOudH, CfHee. Compilation Maps _ m 8 MU*? lo th» Inch. - to the Vest. MK and S Mist-- - Jfipah proper, and, all to iha T/orth emrds . front/a, (fanptlatLn Map prepared ut the y,V General's Office, ibmo Stale. J, Milts to an Inch. Jung Rahadoars ThpaL Sketch Map. in leva, Mag ret character t received from Foreign PepaePnl sent cheerio by Resident oC Bfipal. (no Scale j ifrrvwsmith, Walker Major Cranford, Colt JOrkpairteh.. and a. Frvfnectlsm, by Major C remme/m of art Itinerary Root* of FT Campbell*, from. Chain, MmC.il to l.assa,. hair a/co been consulted The position, of Soomla. in/brrnatum. respeetau/ tie Military Rosts and the. Suhdunsvmt of the Country, mrp supplied by Mqpyr G. 'Ramsay. TUsiAend of Wiped A Miles Reg. No, MS, S. I. D.— Aug. 91.— ICC, COMPILED IN THE OFFICE Of THE SURVEYOR GENERAL OF INDIA, FROM ACTUAL SURVCYSJHE BEST AVAILABLE cl a, Sur '■dJuiru. Pass $£>11270 _ SjtShtUmg $sl^\ ^ 13000^^-] SP ( *7uutyma'''"?s% ^ Wooo | 'k %£$•*&. Shibuj ', C 1 *•••'/ IV PREFACE. the publication of the District Memoirs, but there are subjects of general importance which the publication of the local accounts does not subserve. One of these is the history, using this word in its widest sense, of the Himalaya-Tibetan region, and I offer the refer- ences as the nucleus of a complete index to our knowledge of its physiography, products, peoples, and institutions. As observed in the foot-note to Chapter I., much remains to be done, but at the same time very much more has been accomplished than is generally known. Scientific and economic botany have been carefully explored ; the chapter on economic mineralogy leaves little to be desired : those on meteorology and geology have been brought up to the level of our present scientific knowledge ; and the introduction to physical geography gives a popular and suggestive summary of the information that we possess, whilst the references afford a guide to materials for the study of details. All this is new, or embodies information buried, in correspondence and reports, and practically as inaccessible to the public as if it had never been com- mitted to writing. To General Diehard Strachey I am indebted for the use of an unpublished work of his own on the physical geography of the Himalaya, which has been specially made use of in the chapters on 1 Geology’ and 1 Meteorology.’ Mr. H. B. Med- licott, Superintendent of the Geological Survey of India, prepared the chapter on ‘ Geology,’ and Mr. S. A. Hill, Meteorological Re- porter to the Government of the Hortli- Western Provinces, contri- buted the valuable chapter on t Meteorology.’ Dr. King, Superin- tendent of the Royal Botanical Gardens, Calcutta, furnished the list of the flora of Western Garhwal, Dehra Dun, and Jaunsar- Bawar, and Dr. Watson, the list for Eastern Garhwal, Kumaon, and the Bhabar. To General Strachey I am further indebted for the list of plants collected by himself and Mr. W r interbottom in Ku- maon, Garhwal, and the neighbouring parts of Tibet, and which has never before been published. This list has been admirably edited by Mr. F. Duthie, Superintendent of the Botanical Gardens at Saharanpur, to whom also I am indebted for the sketch of the history of the Tea industry in th® Himalayan districts. The sheets of the portions relating to economic botany have had the criticism of Dr. Watson and Mr. Duthie; and for the forest history Mr. Greig and Major Garstinliave advised me in many matters of detail. PREFACE. V Of the maps, the map of Kumaon was prepared under the instruc- tions of Colonel Walker, R.E., Superintendent of the Great Trigono- metrical Survey, and is the result of great labour and care for detail : indeed, a less accurate map might possibly be more useful. The great 1 one-inch to one-mile’ sheets were photographed down to a smaller scale and sent to me. I then obtained the correct names in Hindi of all the villages, rivers, &c., in Kumaon and Garhwal (about 8,000) and entered against each the correct transliteration for use in a new edition of the large maps, and then drew up a draft list of names for the district map. I desired to enter the names of all halting-places on every ordinary route ; villages in which the patwari usually re- sides; places of note ; trade-centres; and all villages containing over one hundred inhabitants. After much trouble, correspondence, and inquiry, this was fairly accomplished. The villages retained were marked off on the photographic copies of the maps, and these were returned to the Surveyor-General with lists showing the actual and revised spelling for the further compilation. In addition, the prin- cipal lines of road have been laid down, and for the first time the pattis or subdivisions adopted at the recent settlement by Mr. J. Beckett have b een shown. In the trans-Himalayan portion to which the sur- vey had not extended I have added places from the village maps pre- pared by the patwaris, and in their selection was aided by Mr. Beckett. The map of the Iiimalaya-Tibetan region is taken from one prepared by Mr. Trelawny Saunders, omitting the eastern portion. The geolo- gical map is a revised copy of that which accompanied General Strachey’s paper ‘ On part of the Himalaya Mountains and Tibet’ read before the G-eological Society in 1851. It may be necessary to explain that these volumes are not intended to be solely a popular account of the districts which they describe, but to contain, first of all, a record of all facts of permanent scientific or economic value that have been gathered by me during my visits to Kumaon and the Dehra Dun or which have been contributed by others. This work has occupied my leisure time for several years, and I can only hope that the labour and care bestowed on it will be of some use to my successors, and enable them to produce a more worthy record for those who are truly interested in the moral and material pro- gress of the North-Western Provinces. Bombay, 1 E. T. ATKINSON. 17 if A December , 1881. J CONTENTS. CHAPTER I. Introductory. Limitation of this work— Systematic geography— Herbert ; Vigne, Jacque-^^* mont, &c. ; Hodgson ; R. Strachey ; Thompson ; Cunningham • II. Stra- chey; Rawlinson; Saunders; Markham; Calcutta Review, Blanford — Nomenclature— Ethnical sketch : Plains of Asam and Bengal ; Plains of Upper India; Clothing; Pood; Customs; Eastern Himalaya— Eastern tribes; Tribes of the Southern watershed; Bhutan, Sikkim; Nepal; Tribes of the Lower Himalaya— Karnali to Tons; Bisahr ; the Satlaj to the Indus Afghanistan; Galchha States; Kara-Tangutans ; Tibet — General distribution *" ••• (M References 1 42 CHAPTER II. Physical Geography of the Himalaya. The Himalayan river basins— The Indus basin — Subordinate systems of the Indus basin — The Ganges basin — Subordinate systems of the Ganges basin; The Brahmaputra basin— Subordinate systems of the Brahma- putra basin ; Systems of Tibet — Lob-Nor basin ; Oxus basin. Plains of Hindustan— Indus plain ; Indian desert ; Gangetic plain ; Asam val- ley ; Bhabar; Tarai ; Siwaliks; Duns. Extent of Bhabar — Cause of the deposit— Hodgson’s oceanic theory; Fluviatile theory; Tarai; Siwaliks ; Duns ; Ganges to Brahmaputra ; Lower Himalaya. Materials of the mountains — Eocene period ; Mode of mountain formation ; Moun- tain-sculpture ; Ice-wedges ; Avalanches ; Glaciers ; Rain; Rivers CHAPTER III. Geology. Position of the ground. Early observers : Herbert, Cautley, Falconer. The mountain system. The sub-Himalayan zone formed of tertiary rocks. Siwaliks. Post-tertiary deposits. Supposed glacial deposits. Lower Himalayan region. Simla region. Sirmur formation. Relation of Sir- mur and Siwalik series. The Satlaj valley. East of Simla. The Ku- maon section. The Nepal section. Sikkim section. Slight correspond- ence between the rocks of the Himalaya and of the Peninsula. Fre- quent occurrence of carbonaceous deposits throughout the Lower Hima- laya. Conjectural affiliation of the Lower Himalayan sections. The Central Himalaya. Strachey. Stolickza. Western Tibet. The principal crystalline areas. Nummulitic deposits. Post-eocene eruptive rocks. Central gneiss. Kashmir-Kishtwar region. Central Tibet. Its granites, schists, slates, conglomerates and iossilifeious rocks. Paleozoic strata. Vlll CONTENTS. Page. Silurian, Trias, Jurassic. Fossils Tertiary deposits. So-called Niti fossils. General Strachey’s conclusions. Stolickza’s views ... Ill CHAPTER IV. Tiie Him a' la ya. The outer Himalaya. Mountain systems ; Jumna; Ganges; Kali. Subordi- nate boundaries The Nayar. Western Ramganga ; Kali. The snowy range. Axis of highest elevation. The Tibetan plateau. Glaciers. Glacier of the Pindar ; feeder of the glacier ; moraines ; crevasses and ice tables. Glacier of the Kuphini. Motion of the Pindar glacier. Snow-line. Observations in the eastern Himalaya. Observations in Kumaon: Bisahr Across the snowy range. Kumacn; Garhwal; Kunaor ; Western Tibet. Lakes ... .. ... ••• ••• CHAPTER V. Meteorology. Preliminary sketch of climate. Contrast between the eastern and western parts of the plain and the Himalaya. Radiation, solar and nocturnal. Temperature: — Diurnal and annual ranges, — Vertical decrement, • Height of snow-line. Pressure and winds : — Barometric tides, Moun- tain winds,' — -Annual variation of pressure, — Monsoons. Humidity. ■ Vertical distribution of vapour, — Relative humidity,- 'Cloud. Rain- fall : — Distribution on plains anl on the Himalayan slope,' 'Annual variation,— The winter rains, — The monsoon rains ... 201 CHAPTER VI. Economic Mineralogy . Min’ng history : experiments in Garhwal. The Kumaon Iron Works Company. Causes of present poor returns — Mode of mining : excavation : removing the ore : crushing the ore : cleaning the ore : drainage. Smelting opera- tions : refining the ore. Division of profits. Improvement needed in appliances : Chili furnace : English system. Outturn. Financial results of the settlement of the revenue derived from minerals. Gold : Tibetan gold-fields : Thok Jalung mines. Silver. Copper mines : Bai mine and its ores: Sira mines : Gaul and Sor Gurang. Bournonite. Copper mines of Garhwal : Dhanpur : Dliobri : Pokhri : Chaumattiya mines : Raja’s mine: Notamine: Thalamine: Danda mine : Talapungla mine: Kharna mine : Agar Sera mine. Iron mines : Kumaon Iron mines : Giwar mines: Garhwal mines : Nagpur: Dasauli : Iriyakot. Lead Arsenic. Lignite. Graphite. Sulphur. Borax. Gypsum. Soap. Stone. As- bestos. Silajit. Limestone. Building stone. Roofing slate. Alum... 259 ... 297 IUJei ences ... ••• CHAPTER VII. Scientific Botany. A list of th e flora of Garhwal, Jaunsai-Bawar and the Dehra Dun, by Dr. King. Tract to_which the list refers : The Siwaliks. Sub Siwalik Tract. CONTENTS. IX Page. Dehra Dun. Himalayan tract. Characteristic vegetation from the plains to Mussooree. From Mussooree northwards. A list of the flora of Kumaon and the Kumaon Bhabar by Dr. Watson ... ... 299 CHAPTER VIII. Scientific Botany— { continued ). Plants found in Kumaon, Garhwal and the adjoining parts of Tibet by Captain (now General) Richard Strachey and Mr.. W interbottom ... 403 CHAPTER IX. Economic Botany. Arrangement of the subject. Food of the people. Analysis of the food- grains. Watson’s formula. Cultivated food-grains. Cereals. Pulses. Amaranths. Polygonacsse. Cultivated vegetables. Gourds. Vegeta- bles. Condiments and spices, greens. Fruits, cultivated and wild. Uncultivated products used as food. Drugs. Narcotics and spirits. Oil-seeds. Dyes and tans. Gums and gum-resins. Fibres. Woods ... 672 CHAPTER X. Economic BotanY' — ( continued ). Forest history. Grazing tax. Boundary disputes. Government forests. Ku- maon forest-division. Naini Tal forest-division. Ranikhet forest- division. Garhwal forest-division. Dehra Dun forest-division. Ganges (Bhagirathi) division. Forest at the head of theTons andtheJumna. Jaun- sar forest-division. Rheea cultivation. Cinchona. Tallow-tree. Ipeca* cuanha, Cork-oak, Sweet chestnut. Carob. Mezquit and others. Tea ... References ... ... ... ••• ••• ••* Appendix A. Forest Statistics ... General Index iti ••• ••• *** Botanical Index ... ... ... ••• ••• •** Vernacular Index ... ... ... ••• ••• ••• 845 909 915 925 930 936 MAPS AND ILLUSTRATIONS. 1. Map of Kumaon and the adjoining part of Tibet (in cover). 2. Map of the Himalaya-Tibetan region (in cover). 3. Geological map of the country between the Satlaj and the Sarda (page 115). 4. Front view of the Pindar glacier (page 182). 6. The Pindar and Kuphini glaciers (page 184). , I O : : . — __ THE HIMALAYAN DISTRICTS OF THE NORTH WESTERN PROVINCES. PART I CHAP T E R I , Introductory- Limitation of tins work — Systematic geography — Herbert", Vigne, Jacquemont, &c. ; Hodgson ; R. Strachey ; Thompson ; Cunningham ; H. Strachey ; Rawlinson ; Saunders; Markham; Calcutta Review ; Blanford — Nomenclature — Ethnical sketch ; Plains of As am and Bengal ; Plains of Upper India ; Clothing ; Food ; Customs ; Eastern Himalaya— Eastern tribes ; Tribes of the Southern Watershed ; Bhutan ; Sikkim ; Nepal ; Tribes of the Lower Himalaya — Karnali to Tons ; Bisahr ; the Satlaj to the Indus — Afghanistan, Galcha States ; Kara-Tangutans ; Tibet — General distribution — Appendix : list of authorities for this Chapter. Limitation of work. 1 Under the name Himalayan districts of the North-Western Provinces of India we include the British districts of Kumaon, Ghirhwal, Tarai, Dehra Dun and Jaunsar-Ba war, and the independent State of Tihri or foreign Garhwal, comprising the tract within the Himalaya bounded by the 1 The collection of materials for the ‘ Memoir on the Kumaon Himalaya’ has been in progress since 1872, but other and more pressing duties have hitherto pre- vented their arrangement for publication. It was tben intended to give as complete a description of the entire Himalaya as the means at our disposal would permit. There is little hope, however, that the leisure necessary for such an undertaking will occur within any reasonable time, and it therefore seems better to work up the materials already existing in their present form than to wait until opportunity is found for completing the original design. There are many and- great gaps in our informa- tion regarding Kumaon, but the first step towards remedying this defect will be this attempt to take stock of our present knowledge, which is far more complete than is supposed. Without the aid of the materials entrusted to me by General R. Strachey, Sir John Strachey, Mr. J. H. Batten, Rudradatta Pant, and others, whose assist- ance will be found acknowledged in the preface, as well as the co-operation of Mr. H. B. Medlicott, Mr. S. A. Hill, Mr. Duthie, Dr. King, Dr. Watson, Captain G. Marshall, and others, my own work would be very meagre and unsatisfactory, as well from the great range of subjects discussed as from their frequent special and technical character. 2 HIMALAYAN DTSTETCTS Tons on the west, and the Kali or Sarda on the east. The adjoining portion of Tibet, to which British subjects resort for the purposes of trade, or in order to visit the sacred lakes, also comes within the scope of our investigations. A glance at the accompanying map will show that both the Himalayan and Tibetan portions of the tract with which we are concerned form but a small slice or segment of a greater system, which must be studied as a whole before an adequate conception of the structure and relation of its parts can be arrived at. The Himalaya itself is but the southern belt of that great girdle of mountains which encloses within them the country of which the southern half is commonly called Eastern Turkistan. From or through the southern slope of the Himalaya flow the great rivers known as the Indus, Ganges, and Brahmaputra. To the east, the continuation of the Himalaya is traced in the mountain ranges; through which flow the Yang-tse-kiang and the Hoang-lio, and which are prolonged to the north in the Ala-shan, Inshan, and Khing-han mountains* The last of these ranges joins- the Yablonnoi Khrebet branch of the Altai system at right angles in about 55> Q north latitude. The Yablonnoi mountains are the north-eastern continuation of the Altai range and form the water-parting between the Lena and the Amour. The Altai rises, on the right bank of the Irtish river, at the north-western angle of the central plateau, and separates the Upper Gobi from the Siberian steppes. It consists of a belt of mountains varying in breadth from 400 to 1,000 miles, though in one place contracting to 150 miles, of no great elevation, and descending in a succession of broad terraces to the Siberian plains. It is pierced by the rivers draining into Lake Baikal, and, east of the 88th meridian, consists of three almost parallel ranges — - the Saiansk, Tangnou, and Ulangomula. From the sources of the Kara-Irtish the Barluk Orochuk and Zungarian Ala-tau connect with the Tian-shan, the Celestial mountains of the maps, in which are the sources of the Syr-Darya or Jaxartes. The Tian-shan to the north and north-east of Kashgar consists of a series of parallel ranges having a direction from the east to west and an increased elevation as they proceed northwards. They abut on the elevated mountainous region known as the Alai and Pamir plateau, the latter of which contains the source of the Oxus in the little lad or lake of the lesser Pamir. The eastern margin of the Pamir is OF THE NORTH-WESTERN PROVINCES. 3 Eastern T urldst an. described by M. Severtsof, who visited it in 1878, as neither a mountain chain nor the precipitous extremity of a table-land, but an extensive mountainous region filled with numerous ranges. The peak measured by Hayward (21,000 feet), and the Tagharma or Muztagh-Ata peak measured by Trotter (25,350 feet), and supposed to form a part of the Ivizil-Art range connecting the Tian-shan with the Himalayan system, are now reported to be only the culminating points of groups of snowy peaks separated from each other by a distance of over thirty miles. The intervening country contains the basin of the little Kara-kul lake surrounded by a complicated system of short and comparatively low mountain ranges having an altitude of from 14,000 to 15,000 feet. These ranges, however, connect with the Hindu Kush, Karakoram, and W estern Himalaya, and thus complete idle girdle of mountains from one or another side of which flow all the great rivers of Asia. The country thus defined forms a part of the great Empire of China. To the south lies the rugged, elevated plateau of Tibet, regarding which we shall have more to say hereafter. To the north of this comes the depression known as the Lob-nor basin, which receives the drainage ©f the northern slope of the Tibetan plateau called, in the 39th degree of north latitude, the Altyn-Tagli range, but more generally known as the Kuen-lun, a name given probably from some well- known pass. The drainage from the eastern slope of the Tian-shan flows in the same direction, as well as that from the south-eastern slopes of the Altai range ; but all is swallowed up in the great sandy desert of Gfobi, which at one time apparently formed the bed of an ancient sea some 300,000 square miles in extent. According to Prejevalsky this plateau varies in height from 6,000 feet on the margin to about 2,000 feet in the middle. It is intersected from west to east by a depressed valley called Shamo, or 1 sea of sand,’ contain- ing salt. West of this lies the Han-hai, or £ dry sea.’ Prejevalsky has crossed the desert between Kuldja and what may turn out to be Lob-nor, lying in east latitude 90° and north latitude 39° 30/ and found himself at only 2,500 feet above the level of the sea on the banks of the Tarim. To the west, the desert presented a thin loam impregnated with salt, and to the east a plain of drift-sand. Towards the Kurugh-tagh hills, from which he descended on the 4 hima'layan eistbigts desert ; lay a belt of pebble and gravel some 15 to 18 miles wicfe* He also crossed tbe desert to the north between the Ala-shan range and Urga, where he found it to vary in height between 3,000 and 5,500 feet, whilst it still preserved its sandy character. On the route between Urga and Kalgan explored by the same traveller, there is a great depression towards the middle, where the elevation is as low as 2,400 feet. Here the soil of the Gobi proper is composed of coarse reddish gravel and small pebbles interspersed with drifts of yellow shining sand. Leaving these regions, we shall in future restrict ourselves to the southern plateau, of which the Kuen- lun mountains are the northern boundary, and which is so intimately connected in its physical relations with the Himalaya. Herbert. Before proceeding with our examination of the structure of the Early attempts at gene- Himalaya-Tibetan legion, it will be conve- falisation. nient to pass in review the different theories 1 that have been advanced in regard to its systematic geography, since a complete understanding as to what has been done in this direction will enable us to arrive at some conclusion as to what remains to be done. Captain Herbert, who conducted the mineralo- gical survey of the Himalayan country between the Kali and the Satlaj in 1818, was the first who attempted to give a general account of its physical characteristics. His description 2 was intended to serve as an intro- duction to his geological account of the Himalaya, as well as to bo a distinct contribution to general geography ; the existing works on the subject “being singularly deficient in details, as well as errone- ous in the few that are given. ” His idea of the country north of India was apparently derived only from maps. He describes it as a large central space strongly marked by the feature that it was little intersected by rivers, whilst from its sides flowed the streams which united to form the greatest rivers in the world. As the source of every river must be higher than any other part of its course, he inferred that the zone in which those rivers originated must be higher than the plains through which they flowed to seek the ocean, and that the entire central tract itself was completely surrounded br- iefly mountains. He considered the upper beds of the Brahmaputra 1 For a brief summary of these theories sec Mr. C. E, Markham’s ‘ Memoir on the Indian Surreys,’ p. 341, 2 J, As, Boc, Ben., XI., Ft. I., p. x, OF THE NORTH-WESTERN PROVINCES, 5 and the Satlaj as forming part of the barrier zone which surrounds the central tract, and not as a part of the plateau itself. He further showed that the true u line of boundary is undoubtedly the chain of water-heads, and that this is by no means synonymous with the line of greatest elevation. ” At first view the arrangement of the mountain masses in the tract between the Kali and the Satlaj appeared to be irregular and confused, but by tracing the courses of the rivers and their tributary streams, a clue was found to lead the observer out of this labyrinth. “ By connecting their sources and by following out the devious windings of the several feeders, an idea is obtained of the extent, the direction, and the connection of the several ranges. * * * Instead of a succession of parallel and continu- ous ranges running south-east to north-west, and rising one behind the other in regular array and increasing elevation till the series is closed in the farthest distance by the line of snow-clad peaks, we see only one continuous range of any extent forming an irregularly curved line which bends round the tract, commencing on the north- east angle, and with a north-westerly direction, which it gradually alters to a south-easterly one on the south-west angle, and latterly due south just before it is lost in the plain country. This range forms one of the boundaries of the basin of the Satlaj which bends around the convex side, while within its concavity are contained the numerous sources of the Ganges. ” This he called the Indo-Gan- getic chain, “ a ramification of that more extensive line of water- heads which would exclude from the central plateau all the mountain tract watered by the Sanpu and the Indus as well as by the Ganges. Next in extent are the two principal ramifications separating the basin of the Jumna from that of the Ganges, and the basin of the latter from that of the Kali. From these two principal ramifica- tions proceed a number of minor ones which, but for the assistance derived from a study of the course of the rivers, would almost bid defiance to any analysis. Transverse ridges, several thousand feet higher in elevation, ramify from the Indo-Gangetic chain towards the Ganges basin, and a line or plane connecting their summits would be that of the greatest elevation, which, however, has no connection with the disposition of the water-heads. It is a fact that in a line of 500 miles two summits are found exceeding five miles in perpendicular height, not isolated, but connected to appearance by a 6 HIMALAYAN DISTRICTS regular series of peaks of very little inferior elevation. If we confined ourselves to heights of 21,000 feet, we should find a connected line of peaks extending over 1 5 000 miles ; that is, one apparently without breaks, hut in reality connected only through the line of water-heads from which they ramify. Whether the word ‘ line ’ or ‘ plane ’ is used, the idea of considerable breadth must be conceded, and in that case its surface would be very irregularly studded with peaks, and in this way it may be said to be parallel to the common boundary of mountain and plain land, and to intersect instead of bounding the river districts.” The above summary gives a resume of Herbert’s speculations on the physical structure of the Himalaya. His errors were those of his time, when the knowledge even of descriptive geography was in its infancy. He was unable to recognise the unity of the great central mass and its bulwarks, and was wrong in saying that the groups of snowy peaks intersected the river basins, when, in fact, they bound the drainage area, and are the determining causes of its existence. Still Herbert is to be remembered as the first who attempted to give a systematic account of the Himalaya as a whole, 1 and is therefore worthy of a prominent place in this brief notice of its geography. Next to Herbert comes Hodgson, who in an admirable article in the Asiatic Society’s Journal 2 also alludes to Hodgson. J the difficulty experienced by a traveller in the Himalaya in getting “ rid of that tyranny of the senses which so strongly impresses almost all beholders of this stupendous scenery with the conviction that it is a mighty maze without a plan.” His first step towards freedom was his grasping the fact “ that the vast volume of the Himalayan waters flows more or less at right angles to the general direction of the Himalaya, but so that the num- berless streams of the mountains are directed into a few grand rivers of the plains either at or near the confines of the two regions.” Secondly, a study of the river systems like the “Sapt Gandaki” and the “Sapt Kausiki” urged him “to discover, if possible, what cause operated this marked convergence of innumer- able transverse parallel streams, so as to bring them into a series of distinct main rivers.” Thirdly, he found that “the transcendant 1 Neither Moorcroft, Vigne, Jacqnemont, Hooker, Shaw, Iicnclcrson, nor Bellow attempt any description of the Himalaya as a whole. 2 J, As, Sac. Ben., XVIII.. Pt, II., p. 701. OF THE NORTH-WESTERN PROVINCES. 7 elevation and forward position, at right angles to the line of ghats of the great snowy peaks, presented that casual agency : the remotest radiating points of the feeders of each great river being coincident with the successive loftiest masses belonging to the entire extent of the Himalaya.” The great peaks bound and do not intersect the principal Alpine river basins, as Herbert had thought, and, by so bounding, create the basins, whereas their intersection would destroy them. Hodgson’s Himalaya proper is the ghat line or watershed between Tibet and India, and the watershed between the valleys of the Indus and Sanpu and the great plateau is called by him the Nyenchhen Thangla chain. The cause of the convergence of the various streams which form the great rivers upon or near the verge of the plains is shown by him to be “the superior elevation of the lateral barriers of these river basins, between which there are synclinal slopes of such decided preponderance that they overrule the effect of all other inequalities of surface, how vast soever the latter may sometimes be.” These lateral barriers are crowned by the great peaks which stand forth from the watershed and send forth south- ward ridges proportionally immense. Equally effective with the divergent power of these peaked ridges is the convergent power of two ridges upon the single contained river basin. “ The synclinal lines from the inner faces of the two adjacent ridges draw the waters together, and because these ridged peaks are the loftiest masses of the entire mountains, the effect of all other masses, even that of the spine of Himachal or the ghat line of the snows, is overruled or modified, so that in the most rugged region on earth a very limited series of distinct main rivers appear in the plains from innumerable independent Alpine feeders.” We may assume that where the loftiest peaks occur, there is a proportionate intumescence of the general mass, and therefore that these grand peak-crowned ridges determine the essential character of the aqueous distribution along the entire line. A further proof is adduced from the fact that the lower rivers, which take their rise in the middle region, do not show this unitizing principle, such as the Bagmati and Iiamganga. With regard to the mountain systems, Hodgson divides them into the lower, central, and upper ; sub-dividing the first into the sand- stone range with its contained Duns or Maris, the Bliabar or sal forest, and the Tarai. The lower region extends from the level of the 8 H I MA L AYA N D I STRICTS plains to 4,000 feet above the level of the sea ; the central region from 4,000 to 10,000 feet; and the upper region to the watershed or ghat line : divisions which fairly correspond with the distribution of both organic life and inorganic matter. Though unable to follow Mr. Hodgson in all his theories and the deductions that he draws from them, credit must be given for his recognition of the position of the great mountain masses in regard to the alpine river basins and for his appreciation of the intiuence of climatic conditions on the animal and vegetable world. Captain (now General) 14. Strachey, in his paper on the Physical Geography of the Provinces of Kumaon and Captain R. Jtiac he} . Garhwal, read before the Royal Geographical Society 1 in 1851, pointed out distinctly for the first time that the Himalaya was in truth the broad mountainous slope of the great Tibetan table-land descending to the plains of Northern India, while a slope of corresponding character descending to the north is known as the Kuen-lun. He remarks that the great peaks in Kumaon and Garhwal “ are not found on a continuous ridge, but are grouped together in masses that are separated one from the other by deep depressions, through which flow the streams that drain those parts of the mountains that are immediately contiguous to the north.” To the east the same sort of arrangement obtains, but to the west it is much less distinct. The river-beds to within a distance of ten miles in a direct line from the snowy peaks seldom exhibit a rise of more than four or five thousand feet ; but when we cross “the line on which the great peaks are situated, the ascent very rapidly increases, and a very few miles carries the river-bed up to an altitude of nine or ten thousand feet ; thus showing that the sudden increase of height of the mountains along this line is not confined to the peaks alone, but is a general elevation of the whole surface.” Hr. Thomson 3 substitutes the name cis-Satlaj Himalaya for Herbert’s Indo-Gangetic chain, and gives the name trans-Satlaj Himalaya to the chain which, commencing in Kailas, separates the waters of the Satlaj from those of the Indus. He refers to these two great chains the whole of the mountains between the Indus and the plains, and says : “ The northern boundary i ,/. 11. G. S., XXI., p. 57: adopted in Somerville’s Physical Geography, 7th edition ; London, 1877, p. 56, 2 Travels, p. 456. OE THE NORTH-WESTERN PROVINCES. 9 of Tibet is formed by the great chain north of the Indus, to which Humboldt gave the name Kouen-lun” : and again, that every part of Tibet is traversed by mountains having their origin either in the trans-Satlaj Himalaya or the Kouen-lun. So far the unity of the Himalaya-Tibetan region is acknowledged Major A. Cunningham. by this distinguished traveller. Major A. Cun- ningham 1 makes the Bara-lacha range, which forms the watershed between the Indus and its five affluents, the continuation of the main Himalaya or watershed between the Sanpu and the Ganges. To the south of this lies two distinct and independent ranges stretching in the same general direction from south-east to north-west, which he calls the mid- Himalaya, or Pir Panjal, and the outer or sub-Hima- laya, leaving the name Siwalik unchanged for the lowermost sand- stone ranges. Beyond the Himalaya the same system of parallel chains is observed, comprising at least three distinct ranges of moun- tains, which Cunningham proposes to call the trans-Himalayan, or that which divides the head waters of the Satlaj from those of th© Indus and extends to the western limits of Bongdo and Astor ; second, the Kailas or Gangri range which runs through the midst of Western Tibet along the right bank of the Indus to its confluence with the Shay ok; and third, the trans-Tibetan range, also called . „ , Bolor and Karakoram. These distinctions are Captain H. Stracney. however, purely local and geographical and are so far convenient and to be accepted. Captain H. Strachey, in his paper 2 on the Physical Geography of Western Tibet, shows us that the Indian watershed is not the Great Himalaya as seen by the Indian •observer, but is found in a succession of valley heads much depressed and penetrating that mass to such a depth that the passes from India to Tibet are never visible from any station fairly south of the perpe- tual snow. The Turkish watershed divides the waters of Tibet from those of Turkistan, including Khoten and Kashgar. “ The general plan of the mountain system of W estern Tibet appears to consist of a series of parallel ranges running right across the breadth of the table- land in a direction so extremely oblique to the general extension of the •whole as often to confound the one with the other, or to convert the transverse direction to a longitudinal one. Short transverse necks connecting the main ranges in some parts, and cross fissures cutting 1 Ladak, p, 41. 2 London, 1854. 2 10 HIMALAYAN DISTRICTS Sir H. Rawlinson, through them in others, together with projecting spurs of a secondary order, will suffice to convert the supposed primary arrangement into all the existing variety of valley and drainage.* *The great snowy peaks lying mostly on the terminal butt-ends of the primary ranges, sometimes widened by lateral spurs ; and the Tibetan passes ci ossing the low connecting links, whose alignment forms the main watei shed, but not the main mountain-crest.’' Sir H. Rawlinson 1 recognises the unity of the entire mass, and writes that the u whole country between India and Tartary may be considered as a broad mountain range, the Himalaya forming the southern crest, and the Kuen-lun the northern. The direction of this range is from east to west, trending to the north- ward, while the parallel chain which bounds Siberia to the south, and the outer crest of which is the Tian-shan, trends somewhat to the south; so that at a short distance to the west of Yarkand and Kashgar the great interior depression of Chinese Tartary terminates, and the bounding ranges coalesce in the elevated table-land of Pamir. We have now come to the theory set forth by Mr. Trelawny Saunders , 2 Geographer to the India Office, according to whom the summit of the Hima- laya consists of a double range of peaks enclosing a series of valleys running parallel to the axis of the mass, and which he would call the northern and southern Himalaya respectively. The first of the two forms the water-parting between the Ganges basin and that of the Sanpu. To the latter must be assigned nearly all the great snowy peaks which are seen from the plains of India, and which are separated from the former by the valleys already mentioned. These valleys are comparatively elevated, and at length burst through the southern range by intersecting gorges. Both Herbert and Hodgson are set aside, and the great peaks are described as forming a chain, broken at intervals by intersecting gorges. u The upper valleys of the Sanpu, the Satlaj, and the Indus appear to form a huge elevated trough separating the Himalaya from the northern part of the table-land of Tibet and from the snowy range into which the table-land contracts at its western end.” This range is crossed by the Muztagh, Karakoram, and * 1 England and Russia in the East : London, 1875, p. 236, 2 Sketch of the Mountains and River Basins of India : London, 1870, Mr. Saunders’ theory. OF THE NORTH-WESTERN PROVINCES. 11 Mr. Markham. and Changchemno passes, and is remarkable for the great length of its glaciers and the great height of its peaks. The Indus forms its southern base as well as the northern base of the Himalaya. The Indus, Satlaj, and Sanpu, u are the only rivers which, washing the northeni base of the Himalaya in channels parallel to the range, break through the entire breadth of the range and water the plains at its southern base.” The eastern base of the mountainous highland of Tibet is marked by the Min river, and on the north-east the slope is defined by the basin of the Hoang-ho. From the latter river west- ward to the Muztagh the Kuen-lun mountains descend to the plains of Gobi from the northern edge. These unite with the Himalaya, Pamir, and Hindu Kush in the lofty peak or knot called Pusht-khar or Taghdambash. The accompanying map, prepared by Mr. Saunders for Mr. C. It. Markham’s Memoir on the Indian Surveys, will illustrate better than any further quotations his views on the subject of the relations of the great mountain systems, as well as serve our own purpose. Mr. Markham 1 divides the Himalayan system into three great culminating chains, which he calls the inner, central, and outer, running more or less parallel to each other from the gorge of the Indus to that of the Dihong. “ The lofty region of Great Tibet lies mainly between the inner and outer range, with the central chain, whence most of the rivers of Northern India take their rise, running through its length.” The western extremity of his inner and most northern range is the Karakoram, which separates the Indus valley from the affluents of the Lob-nor system, and the eastern section is the Gangri mountains of the map, the Nyenchhen Thangla of Hodgson and Ninjinthangla or Nyenclihen-tang-la of Markham, which commences in peak or knot called Kailas. Parallel to the northern range runs the central range, the eastern section of which commences at the Mariam-la pass near the Kailas peak. “ Here a comparatively low saddle connects the northern and central ranges and separates the valley of the Satlaj from that of the Brahmaputra. To the east- ward the northern side of the central chain forms the southern watershed of the Brahmaputra, whilst on its southern slopes are the sources of many important rivers, which, forcing their way through the southern chain of the Himalaya, eventually join the Ganges or 1 Tibet, p. xxiii., 1876. 12 HIMALAYAN DISTRICTS the Brahmaputra.” The southern chain is made up of the series o! snowy peaks which, to the east, overhang Nepal, Sikkim, and Bhutan. Thus, Mr. Markham is at one with Mr. Saunders in his theory as to the Himalayan system, only substituting the terms “inner or northern, central and outer or southern,” for the terms Gangri, northern and southern Himalaya,” used by Mr. Saunders. A writer in the Calcutta Review 1 has taken objection to the creation of the southern chain, which, “being occasionally intersected by rivers of more Calcutta Review . remote origin, is not a chain at all, but a series of spurs running southwards from an extended line of elevation more to the north, in the neighbourhood of which the said rivers rise.” He also suggests for the whole system the name Indo-Tibetan, correctly urging that it is undesirable to give to the whole a name which belongs only to a part. He prefers simply to lay down two lines of watersheds, the northern corresponding for the most part with Mr. Markham s inner range, and the southern extending from Chilas by the Zoji-la, Baralacha, Niti, and No passes to the Laghalangla above Shikatse. He then examines the river basins and shows that Hodgson s tlieoiy regarding them is in accordance with tacts ; that these basins deiive much of their water from certain prominent peaks which, standing in advance — that is, southwards of the watershed — are connected with it, and from which ridges with dependent spurs project, that serve as lateral barriers to the basins. “ The preponderating synclinal slopes of the ridges and spurs which overrule the effect of all other intervening inequalities of surface, however vast, cause the several groups of mountain streams between them to converge till they unite and constitute a main river near the edge of the plains.” Tins is practically Hodgson’s law re-affirmed in the full light of all that modern research has shown us regarding the geography of Tibet, the Karakoram and Kashgar, a terra incognita to our early writers. Both Mr, Markham and Mr. Saunders have issued rejoinders Rejoinders of Mr. Mark- to the criticisms in the Calcutta Review in ham and Mr. Saunders. two articles in the Geographical Magazine . 2 1 January, 1877, p. 145. 2 By Mr. C. R. Markham in May, 1877, and Mr. Saunders in July, 1877, Geo. Mag. IV, 113, 173, London. The other matters in contro- versy between the reviewer and Mr« Markham are omitted as foreign to the subject of this notice, OF THE NORTH-WESTERN PROVINCES. 13 Mr. Markham chiefly confines himself to a defence of his use of the word ‘ chain’ as applied to a series of culminating ridges, whether rivers force their way through its gorges or not ; but Mr. Saunders goes more fully into the entire question at issue between him and the reviewer, and supports his arguments by a re-statement of his views on the physical geography of the entire Himalaya-Tibetan system. For this purpose he draws largely on his “ Sketch of the Mountains and Fiver Basins of India,” already noticed, in which the theory of the southern chain of snowy peaks was first developed; and whether we agree with his deductions or not, we must consider his summary as a valuable contribution to our knowledge of the subject. He recapitulates the arguments in favour of considering the line of snowy peaks a southern chain, and concludes that they are entitled to that name, u (1) as the culminating summit of the southern or Indian slope ; (2) as the common origin of a succession of rivers ; (3) as cut off from the northern range by a succession of remarkable valleys, sometimes very long, sometimes very deep, and sometimes very broad and flat, and all containing considerable rivers running parallel to the chains which they divide.” He objects to the inclusion of the mountain ranges on both sides of the troughs of the Indus and Sanpu under the term Himalaya, the northern watershed of those rivers composing the contreforts, buttresses and slopes or escarpments of the great central plateau which they uphold and from which they cannot be separated. The table- land is Tibetan ; therefore its southern slope cannot be called Himala- yan. The remaining portion of Mr. Saunders’ article will be noticed as we proceed. The latest contribution to the physical geography of the Himalaya is to be found in Mr. TI. Blanford’s Manual 1 Mr Blanford. n ^ and Mr. W. Blanford s introduction 4 to the “ Manual of the Geology of India.” In the latter work, which may presumably be taken as giving Mr. W. Blanford’s conclusions on the subject, he considers the Himalaya to form a curved belt of mountains with their convexity to the southward which mark the southern scarp of the Tibetan plateau as the 1 Physical Geography for the use of Indian Schools, Calcutta. 2 * Calcutta, 1879, I., ix. It should be remembered that the term, ‘range’, is used here for geological purposes which are not always the same as those intended by geographers. Its precise meaning depends on the context. 14 HIMALAYAS’ DISTEICTS Kuen-lun define the northern. The western terminal portion of the Himalayan chain comprises a number of great ranges variously named. It is doubtful whether any of these “should be considered the prolongation of the main Himalayan axis, although, if any be really a continuation of the Himalaya proper, it is either the Pir Panjal or the Zanskar range.” Geological considerations would lead him to suppose that “the main range commences on the west- ward in the Dhauradhar near Dalhousie, and extends to the east- south-east till it rises into the main snowy range of the north- west Himalaya. Many geographers distinguish two parallel ranges from the neighbourhood of Simla to the eastward; the snowy range proper, formed of the highest peaks (Saunders theory), and a more northern ridge, forming the watershed between the Tibetan plain and the rivers running to the plains of India. Others consider the latter to be the true Himalayan range, and look on the higher peaks as belonging to the spurs between the rivers flowing from that range. It is certain that the great peaks, such as Nandadevi, &c., are separated from each other by deep valleys, through which flow streams coming from the northern range, and that, although the peaks of the latter are inferior in elevation, the passes by which it is traversed are much higher ; but it has not yet been ascertained whether the great peaks are on the strike of any continuous band of rock, or whether they merely consist of hard nuclei left undenuded.” There is little doubt that, until the geologist is able to assist us, the question whether the line of snowy peaks should be considered a true chain or merely spurs from the main water-parting must be left undecided. Though year by year fresh materials are added to our stock of knowledge regarding the Himalaya, they are yet too imperfect for us to offer little more than a suggestion as to the views that should be adopted regarding its structure. A glance at Mr. Saunders’ map will show us the vastness of the subject, and that the Himalaya of Kumaon and Garhwal, with which we are more immediately concerned, is but a very small portion of the great girdle of snowy peaks that uphold between them the elevated plateau of Tibet. Herbert showed us that this girdle, as seen from the plains of India, is not a continuous line of parallel ranges rising one behind the other, and increasing in eleva- tion until the series is closed in the farthest distance by the line of OF THE NORTH-WESTERN PROVINCES. 15 snow-clad peaks ; but that these peaks or groups of peaks are ramifications from the line of water-parting which itself is lower than the line of greatest elevation. Hodgson subsequently explained the influence of these groups of peaks on the river-systems, and Captain Strachey showed us that the Himalaya was the southern slope of the Tibetan plateau as the Kuen-lun formed its northern slope. These are, broadly, the more important additions to our knowledge of the physical geography of the Himalaya that have been made of late years. To our mind the recognition of the unity of the entire Himalaya-Tibetan system is the most important of them all, and that alone which will lead to practical results. The division of the Himalaya into ranges may be allowed as a matter of convenience, but should not be permitted to cloud the great fact that all are but varia- tions in the southern slope of the great table-land due to the influ- ence of the elements on the materials of which they are composed, and to the disturbing action of subterranean forces. We can lay down the line of water-parting and the line of greatest elevation with some precision, but must call in the aid of the geologist and mineralogist to distinguish which amongst the ranges is entitled to be called the real main axis of the Himalaya; and, until their labours are communicated to the world, must rest content with the somewhat arbitrary distinctions afforded by the prominence or other- wise of existing physical features. Seeing the misunderstandings that have arisen from a too loose Nomenclature. USe ° f WOrds ™ d P hraSeS * !t w!U b « as well to state here that we adopt the word ( water- parting ’ to represent the ridge which separates the flow of water on either side of a range of hills . 1 The word ‘ range ’ will include a series of mountains or hills continuing in one direction alono- a common axis, whether broken by chasms or not ; and the word ‘spur’ will be used of a ramification from a range, whether connecting it with another range or sinking gradually into a plain. The great mountain chain lying between Tibet and the plains of India is generally known to the natives of India by the term pahdv (mountain), to which they prefix the local name where such exists. 1 The use of this word in this sense is one of the subjects of controversy between the Calcutta reviewer and Mr. Markham. The former (p. 147, note) objects that the old word ‘ water-shed ’ is sufficient. 16 HIMALAYAN DISTRICTS 'The more educated give the name Himachal 1 (snowy-range) or Himalaya (abode of snow) to the snow-covered ranges ; whilst Euro- peans popularly include under the name Himalaya the entire moun- tainous region lying between the gorge of the Brahmaputra on the east and that of the Indus on the west, and between the upper valleys of the same rivers on the north and the plains of India on the south. A first glance at any good map will convince us of the general unity of the physical relations of the range within the limits commonly assigned to the Himalaya, whilst a closer examina- tion will induce us to include much more. For our part we accept the popular definition of the Himalaya as extending from the gorge of the Indus on the west to that of the Brahmaputra on the east, and from the upper courses of the main branches of those rivers on the north to the plains of India on the south, speaking of its connections beyond those limits as the western and eastern extensions respectively. It will materially aid the reader if we further preface our remarks with a short description of the ethnical and Ethnical Sketch. political divisions of its surface, and of the regions in immediate contact with it. We have arrived at some idea of the physical relations of the tract itself, and shall now, at the risk of being thought diffuse, endeavour to trace the ethnical affinities of its inhabitants. Commencing, then, with the plain on the south, we find the provinces of British India flanking the foot of the Himalaya along its entire length from the 96th to the 72nd meridian of east longitude. Following the direction of the Himalaya from east to west, we find in Upper Asarn a number of tribes speaking different languages and dialects, and so intermixed and blending the one into i The word Himachal ( ) is derived from two Sanskrit words, 1 hii net? (snow) and ‘ achala’ (mountain), meaning ‘snowy-mountain’ or ‘snowy-range. Similarly the word Himalaya ^ ) is derived from ‘ lima ’ and ‘ alaya, (abode), meaning the ‘home ’or ‘abode of snow.’ The proper pronunciation is therefore Ilim-Alay-a, not Him-a-lay-a as commonly obtains. The plains-men speak of the Simla -pah&r, the Mansuri -pah&r, and sometimes of the snowy-range as the harf (ioeypah&r. “ The people south of the Himalaya in Nepal call all snowy mountains langar, by which they mean the highest points. They call the peaks that have no snow banjang, and the low ground under the said banjang they call rpheili. The term Himalaya is not used by uneducated people, who only talk of the snowy mountains as '■barf (mi langar,'— G, T, S, Rep., 1872, p, 46, OF THE NORTH-WESTERN PROVINCES. 17 tlie other that, beyond a mere cursory description, their classification cannot be attempted here. In the extreme north-east they are Plains of Asam and allied with or are members of the tribes inha- Bcngal. biting the neighbouring hills, of whom more will be said hereafter. They speak a language having an affinity with the great Barma-Tibetan group, and are mere pagan savages. Alon g either side of the Brahmaputra in its course through the valley we find the settled tribes of Asam speaking a language akin to Bengali. Though differences exist they so closely resemble in habits and character the people of the conterminous parts of Bengal that it is difficult to draw a strict line of severance between them without entering into long historical and ethnical discussions quite out of place here : many that are now Hindu or Musalman Bengalis in all outward appearance can be shown to be converts in recent times from the pagan tribes in their neighbourhood of unmistakably aboriginal origin. The people of Bengal, the flat alluvial plains of which lie along the lower courses of the Ganges and Brahmaputra, exhibit all the features characteristic of a race inhabiting a region of tropical heat and moisture. They are small in stature, of dark com- plexion, and effeminate in character, living chiefly on rice grown in the lowlands subject to annual inundation. Their dress is of the scantiest proportions, consisting chiefly of one or two pieces of cotton cloth simply wrapped around their waist and shoulders, and not wrought into any form of garment. Their heads and feet are usually left bare. Their houses, constructed of mats, lie scattered amongst the thick groves of bambus and palms that spring up in wild luxuriance on the uncultivated ground. As we ascend the Ganges, 1 we find a drier climate with greater contrasts between the summer and winter Plains of Upper India. temperature, and a taller, more manly, and more robust race, of whose food the millets and unleavened bread of wheat, barley, and other grains form the principal element. Their clothing is more elaborate and warmer than that of the Bengali. All wear turbans, and those who can afford it have short jackets fastening on the right breast in the case of Hindus, and on the left breast in the case of Musalmans. Their houses are built of mud and are either 1 This account of the Hindiis in the plains is partly based on Elphinstone and Notes by General R, Strachey. 3 18 HIM/LAY AN DISTRICTS tiled or tlmi died in tlie villages, but in many of tlie towns very small brides are used in the construction of the better class of dwellings. The country is open and unenclosed, and almost the only trees are groves planted near towns and villages, with occasional patches of dh ah ( Butea frondosa) and babul ( Acacia arcibica ) jungle. The peo- ple are mostly Hindu in religion and speak dialects of Hindi. On approaching the Satlaj the language passes into Panjabi, also Sans- luitic in its character, and we find the religion of the Sikhs the seal of the double dispensation of Brahma and Muhammad. 1 To the west of the Panjab, or country of the five rivers, the religion of Islam predominates amongst a motley group of tribes of very varied origin. The name Hindustan, which is more correctly applied to the north- ern Gan get ic districts alone, may without impropriety be used so as to include the entire tract below the Himalaya. Intersected by the innumerable streams that flow from the mountains above it, watered by the copious falls of periodical rains, and enjoying a semi-tropical climate, the great unbroken plain is thus supplied with the two great requisites, heat and moisture, that are the necessary and certain agents for the development of vegetable life. We naturally, therefore, find an agricultural population often in the older settled parts extremely dense, and attaining to no small degree of civilisation. Cities and large towns are common, many with a population of over 50,000 souls ; and the inhabitants, without coming up to a European standard, enjoy considerable wealth. Literature, both indigenous and of European origin, is cultivated ; schools are numerous, and the useful arts are highly advanced and eagerly followed. The hot climate which induces a love of repose and fertility of soil which renders severe labour unnecessary has, in some measure, modified the habits of patient industry which are usually character- istic of an agricultural population ; but the dislike to change which marks those communities in all parts of the civilised world is nowhere more strikingly exhibited than in Hindustan. The great wealth of the country and its open and easily accessible character, together with the insuperable obstacles to union presented by differences in race and caste, have, for many centuries, subjected it to the reiterated attacks of foreigners. With very few exceptions all truly national government has ceased to exist; and from what little 1 Cunningham, History of the Sikhs, p. 13, OF THE NORTH-WESTERN RRO VINCES. 19 we know regarding it, the people have small cause to regret the successive changes of masters. India has never had in the whole course of its history so strong, universal, and just a government as it has enjoyed under the British since the memorable mutiny of 1857. Englishmen may well point with just pride to the lengthy catalogue of measures attesting true moral and material progress that have been introduced during the last quarter of a century, and have been assimilated by the people to such a degree that the advance — political, moral, and social — made has eclipsed all that had been previously effected under British rule. Taking the people of the plains as a whole, their clothing is cotton and their food is vegetable, though Clothing, food, customs. n . ,, , , , IVlusahnans and some Hindus eat meat and a few eat fish. The dress of the men, as a rule, is white, though they often wear coloured jackets ; the women, who have no other covering for their heads than a corner of the cloth that they wrap round their bodies, frequently wear bright colours, usually indigo blue, Turkey red, or safflower yellow. The Hindus preserve their mous- tache, but shave their beards, and frequently their heads, except a small scalp-lock, whilst the Musalmans allow their beards to grow. The seclusion of women seems to be a custom introduced by the Muhammadans, but amongst all religions and races in Hindustan the position of females is essentially inferior to that of the other sex, with whom they do not mix in society. Marriages are almost always contracted in childhood, and the betrothed bride is always under the age of puberty. Amongst Hindus, a dowry is given with the daughter, though the practice of accepting a sum of money for a daughter is in many parts of the country gaining ground. Female infanticide has been rife in the Grangetic districts of Upper India, due to the disgrace supposed to be attached to the expression ‘ father-in-law,’ as well as to the great expenses ordinarily consequent on the marriage of a daughter. The education of women is absolutely neglected, and the efforts of Gfovernment in this direction have proved a total failure. The men, however, for the most part, amongst the classes above those actually engaged in the cultivation of the soil, can read and write, and even the men who have not acquired those attainments possess the power of mental calculation to a remarkable degree. The Brahmanical faith is with few exceptions 20 HIMALAYAN DISTRICTS dominant throughout Hindustan. The Musalmans arc, however, numerous everywhere, and in some districts are in the majority. They belong chiefly to the Suni sect, but Shiahs are also found in certain tracts where the influence of powerful families of their persuasion has been felt. The peculiar modification of Hinduism adopted by the Sikhs is chiefly confined to that portion of the Panjab which lies east of the Chinab. To the west of that river, the great mass of the population is Muhammadan. Taking the people of the Pan jab proper, excluding Peshawar and the trans-Indus distiicts attached to the Leia and Multan divisions, we have a population of ten millions, of whom seven-twelfths are Musalmans, four-twelfths are Hindus, and one-twelftli are Sikhs. Distributing them accord- ing to race, General Cunningham 1 makes o per cent, of so-called early Turanian origin, 27 per cent. Aryans, and 70 per cent, later Turanians. We shall now consider the ethnical and political divisions of the Himalaya itself, proceeding in the same Eastern Himalaya. direction from east to west. At the extreme east we have the same races speaking a Barma-Tibetan language that we found in the plains, but a line drawn north and south across the Brahmaputra, in the general direction of the Dhansiri river, and continued southwards so as to leave Kachar to the west of it, would, according to Hodgson, divide them from the Alpine laces of moic pronounced Tibetan stock, as well as from the so-called aboriginal tribes of the central Himalaya. These Barma-Tibetan tribes are known as Abors, Bor-Abors, Daphlas, Akas, Mishmis, Miris, &c., and their communities are reported to have a sort of rough republican constitution. This conjecture of Hodgson appears to be supported by the result of the most recent investigations. The country lying on the Tawang route by the Dhansiri river from Asam to Chetang in the valley of the Sanpu, in the 92nd meridian of east longitude, has been traversed by one of the Pandits of the Great Trigo- nometrical Survey, from whom we learn that to the east of that line the Himalaya is inhabited by Lhoba Daplila tribes. 2 These men are remarkable for the abnormal development of the muscles of the arms and calves of the legs. They wear cylindrical-shaped hats made of Eastern tribes. 1 Cunningham’s Arch. Rep., II., 2, H 2 See section A. of references attached to this chapter, OF THE NORTH-WESTERN PROVINCES. 21 bambus, and their only garment is a long blanket folded somewhat after the fashion of a plaid and fastened round the waist by a cloth girdle, which is used as a quiver for their arrows, which all carry, as well as a bow slung over their left shoulder. The greater part of their legs and arms is bare. They wear no boots, but ornamental rings made of rope, fastened very tightly both on the wrists and legs below the knee. They have a decided Tibetan caste of feature, high cheek-bones, and Chinese-looking eyes. They wear no hair on the face, but the hair of the head is allowed to grow to a great length, and is drawn together behind the head and then allowed to hang down . 1 They appear to be distributable into two groups — those living in the great rice country to the north on the banks of the Sanpu, called Lho-khals, and who are independent of the Lhasa authorities; and the Shiyar Lliobas, a wild race who inhabit the country through which the great river flows to Gaya, Asam, and who may be identified with the wilder tribes of Mishmis. The Mishmis are distributed into three great divisions com- prising numerous clans — the Chulikata or crop haired, the Midhu, and the Digaru, each of whom have a separate dialect, and the last reside within British territory along the hills as far west as the Digaru river. The Abors or Padams inhabit the country to the west of the Dibong river. They are described by their neighbours as exceed- ingly fierce and blood-thirsty : “ like tigers, two cannot dwell in the same den. Their houses are scattered singly or in groups of two and three over the immense extent of mountains inhabited by them.” They manufacture the weapon called clao, and weave coarse cloth, which with manjit , beads, bell-metal cooking vessels, female slaves or rather wives, and the breed of cattle called mithans, are exchanged for salt and coarse cloth imported by the Miris from the plains. The Miris are more civilised than the Abors, and dwell in villages both in the hills and plains. The Alias or Hrussos live between the Miris and the Daphlas on the upper waters of the Sundari, and call themselves Tenae. The women of the Akas wear blue or black petticoats and jackets of white cotton of their own manufacture. Their faces are tattooed, whence the name “Aka” given them by the people of Asam. The males wear a girdle of canework painted red, which hangs down behind in a long bushy tail. Their staple food is rice, but everything edible is made use of. The KG. T. S., 1878, p. 70. 22 HIMALAYAN DISTRICTS Daphlas belong to the same stock, and all are mere pagan savages, debased, cruel, and treacherous, though in the last respect the Akas have a somewhat favourable report. To complete our review, we shall diverge to the south of the Tribes Of the southern Brahmaputra and briefly notice the tribes water-shed. inhabiting its southern water-shed . 1 In the extreme east we find the Khamtis or Shans, a tribe linguistically allied to the Siamese and Buddhists in religion ; next we have the Singphos, or Kakhyens, and the Jilis, on the northern slopes of the Patkoi range, both of whom are pagans and speak a language intermediate between Barmese and Tibetan. Further west come the Nagas, who are distributed into three great classes — the Namsang, Khari, and Angami. They are the most numerous of all the pagan tribes to the south of the Brahmaputra, extending from the Kopili river in the meridian of Nowgong on the west to the meridian of Sadiya on the east. They bury their dead and appear to manage their affairs in a sort of republican assembly. The Kopili river separates the Nagas from the Kliasiyas of the Jaintiya and Khasiya hills around Shillong. The Kliasiyas appear to be an isolated group, speaking a monosyllabic language which cannot be classed with any other of the same family. The form of government is republican and the religion is mere paganism. To the west are the Garos, who also are pagans, though their language has affinities with the Aryan dialects spoken on the north, south, and west. The language, however, has a Tibetan basis, and Hodgson would include it in the Bodo group, of which more hereafter. South-west of the Nagas come the tribes of the Manipur, Lushai, Tipura (Tipperah), and Chitta- gong hills. From McCulloch and Damant we learn that there are numerous dialects in Manipur, and that the principal has a character of its own derived from the Nagari. The inhabitants have adopted the Brahmanieal faith. The people further west are known as Kukis, and appear to speak four dialects of a common stem-language : — the Lushai spoken by the I)zos of the Lushai highland, the Thadu in northern Kachar, the Kuki in the same district, and the Hallami in the Tipura hills. The Kukis are pagans, but are gradually yield- ing to the influence of their Brahmanieal neighbours, as indeed are all the pagan tribes similarly situated in the Asam valley. We shall 1 See section ]j. of references attached to this chapter. OF THE NORTH-WESTERN PROVINCES. 23 now return again to the tribes inhabiting the Himalaya to the west of the Dliansiri river. The whole country along the Tawang route from Asam to the , head of the valley leading down to Chetang on the banpu is under the rule of the Lhasan Jongpen of the Chona Jang. The Lamas of the great lamasery of Tawang, however, own the country to the south of the range of hills which form the water-parting between the Tawang and Dhirang valleys, and are entirely independent of Lhasa. They manage all public business in an assembly of the principal Lamas, called the Kato, ■which is also the supreme court of justice. To the north, near the Chetang valley, the elevated highlands are occupied by nomad tribes ; but to the south, in the Mon-yul or Sub-Himalaya, the country within which Tawang is situated, the people are called Monpas or Hill Indians, and differ materially in language, dress, and manners from the Bod- pas, or people of Bod-yul to the north of Chona. The Monpas resemble the inhabitants of Bhutan on the west. They wear their hair closely cut round the head, not in plaited tails as in Tibet, and as a covering have a small skull-cap of woollen cloth or felt. Instead of the long gown of Tibet a short coat is worn which reaches to the knee, and is fastened by a woollen girdle that invariably holds a long, straight knife. The people keep cattle, sheep, and pigs. Thus, the line drawn north and south by the Dliansiri river passes through this wedge of Tibetan territory, separating the Barma-Tibetan tribes on the east from those who have a more pronounced Tibetan origin in the central Himalaya and the so-called aboriginal tribes of the lower Himalaya on the west. Hodgson assigns to the latter the name Tamulian, but it cannot stand, involving as it does linguistic and ethnical associations which modern research has failed to establish. To the west of the Dliansiri river we have the countries of Bhu- tan, Sikkim, and Nepal, all of which possess Bhutan, Sikkim. / „ 1 a more or less established form of govern- ment . 1 Much has been written regarding the people inhabiting those countries which we can but very lightly touch upon here. The entire tract may be divided into three great belts, — the elevated region beyond the snowy range that is visible from the plains, varying 1 See section 0. of references attached to this chapter. 24 HIM/LAY AN DISTRICTS from 10,000 to 16,000 feet above the level of the sea ; the central region, varying from 4,000 to 10,000 feet ; and the lower region, extending from the plains to 4,000 feet. 1 To the central region are confined the Lhopas, Lepchas, Limbus, Kirantis, Mnrmis, Newars, Sunwars, Cliepangs, Gurungs, Magars, and Kliasiyas. To the lower regions belong the Kocli, Bodo, Dhimal, Kichak, Tharu, Denwar, and Pallah tribes. The inhabitants of the central region belong to a comparatively recent Tibetan immigration, whilst those of the lower region, the so-called Tamulian aborigines, are apparently to be ascribed partly to an early Tibetan immigration and partly to an Aryan source. To the north, along the entire line of ghats from the 92nd meridian to the Jumna, we find the Bhotiyas or Bod-pas of pure Tibetan origin and Buddhists in religion. Bhutan, the Lho-pato, Llio-duk, or Lho-mon of the Tibetans, is also a Buddhist country, as well as Sikkim, the Demojong of the Tibetans. Nepal, called Palbo by the Tibetans, is partly Buddhist and partly Brah- manical in religion. In the central Himalaya of Bhutan and Sikkim we find the Lhopas, Lepchas, and Limbus. The name ‘Lhopa’ seems to be a generic term signifying the people of Lho or Bhutan, as £ Bod-pa’ means a person of Bod or central Tibot, and £ Kham-pa,’ a person of Kham or eastern Tibet. So also the term £ Dok-pa’ is the religious equivalent of the territorial term £ Lho-pa.’ The Lepchas extend from Panakha in mid-Bhutan on the east into eastern Nepal on the west. They are divided into the Bong and Khamba tribes. The women of both divisions wear a loose coat of the fibre of the silk-worm that feeds on the castor plant, or of unbleached cotton with a wrapper of the same material around the waist to form a petticoat. The men wear a robe of striped red and white cotton cloth crossed over the breast and shoulders and descending to the calf of the leg, leaving the arms bare ; a loose jacket of red cotton cloth is worn over the robe by those who can afford it, and both are bound round the waist by a red girdle. Some strings of coloured beads round the neck, silver and coral earrings, a bambu bow with a quiver of iron-pointed arrows, and a long knife complete their costume. This knife, called £ ban by the Lepchas and £ chipsa by the Bhotiyas, is worn on the right side, suspended from the left shoulder, and serves as 1 Bettor known as Hodgson’s belts. OF THE NORTH-WESTERN PROVINCES. 25 an axe, hoe, spade, sword, and knife. The Lepchas eat any flesh of bird or beast, all cultivated and many wild grains, and drink beer and tea. They are Buddhists in religion. Their language, though allied to Tibetan, is not Tibetan, and has a character of its own. They bury their dead ; though the Murmis, a tribe of the same country, first burn their dead* and then bury the ashes. The Lepchas are short in stature, averaging about five feet, bulky for their height, and rather fleshy than sinewy. They have a fair complexion, pleasantly marked Tibetan features, and part their hair along the crown of the head. Both sexes allow it to grow long ; the younger males allow it to hang loose over the shoulders, whilst the elder males and women plait it into tails, and the latter tie the ends with braid and silken cords and tassels. Like all Buddhist hill-tribes they are very filthy in their habits, ablution being unknown. The Limbus are an important tribe of the central Himalaya, T . . found between the Tista on the east and the Dudh-Kosi on the west. The word ‘ Limbu,’ according to Dr. Campbell, is a corruption of the term ‘ Ekthumba,’ the correct name of this people, and used generally to designate the whole population of this portion of the Himalaya not included amongst the well-known divisions, such as Lepchas, Murmis, Bhotiyas, and Parbatiyas. Under the name Limbu are included the Kirantis or Kiratis, Ekas, and Pais, and their country is divided into Kirati-des from Dudh-Kosi to the Arun and Limbua from the Arun to the Ivonki river, which leaves the Nepal hills about twenty miles to the west of the Mechi river. Further east and west they occur only in small colonies. Hodgson records the vocabulary of seventeen dialects of the Kirati language, none of which are referable to the written Tibetan or Hindi. They are pagans in religion, though willing to pass themselves off as followers of Hinduism or Buddhists where those religions prevail. Their features, the absence of a beard, and the colour of their skin, all show them to be of Tibetan origin. The Limbu wears his hair long, but does not plait it ; he carries a hukhvi or curved knife instead of the ban, and has a wide trousers and jacket instead of the robe and long jacket of the Lepcha. Both tribes are found at elevations of from 2,000 to 4,000 feet above the level of the sea. 4 •26 HIMALAYAN DISTRICTS The Hayus or Yahus prefer the lowest elevations in the valleys, and occupy the central and lower ranges Ncpa1, of the mountains of eastern Nepal between the A run river and the Konki. They are found mixed with the Eka division of the Limbus, but possess clearances and villages of their own. They differ from all around in language, religion, and habits, and are esteemed an outcast race by the Gur- khalis. They do not intermarry or hold intercourse with other tribes. The Bramhus, similarly placed in the Noakot valley to the west, speak a Barma-Tibetan dialect and aie also pagans. The great bulk of the Murmis are found between the Nepal valley and the Dudh-Kosi, whence in smaller numbers they extend to the Tista on the east and as far as twenty miles west of Kath- mandu on the west. They are divided into two classes : one from the Ni district in Tibet, and the other from the Tsang dis- trict ; hence the generic name Nitsang or Nishang applied to the whole tribe. They prefer elevations of from 4,000 to 6,000 feet and engage in pastoral and agricultural operations, living 'in cottages built of stone and thatched with grass. They are Buddhists m religion and their language is akin to Tibetan. In their physical traits they resemble the Lepchas, though somewhat taller. The Newars compose the majority of the inhabitants of the Nepal valley, but are not numerous beyond its limits. They are a shortci race than the Gurkhalis, and their appearance betrays their transmontane origin. The greater number are Buddhists, and the remainder profess the Brahmanical faith. They possess a written character of their own and speak a distinct dialect, though the Buddhist portion also use Tibetan, in which their religious books are chiefly written. In the forests to the west of Nepal, close to the plains, we have the wild tribes known as Chepangs and Kusundas, the former clearly akin to the Raj is of Knmaon. They speak a language allied to that of the Lhopas of Bhutan. In the same direction are the TIinduised tribes of Khasiya, Magars and Guiungs, generically known as Parbatiyas. They speak a language having a Tibetan basis, and into which many Hindi and Urdu vocables have been introduced. The Gurungs, like the Murmis, prefer elevations of 6,000 feet, and are partly pagan and partly Hindu in religion. The Magars are entirely Hindu in religion, and to them OF THE NORTI-I-WESTERN PROVINCES. 27 belong the Thapa clan so famous in later Nepalese history. Both these tribes supply numerous recruits to the regiments in the British service, and to this is probably due the Indianised form of their speech. North of them we find the Sunwars, and on the west the Thaksyas (Thakuris ?), and on the east the Pahris. Vocabularies of the languages of these tribes have been preserved by Hodgson. The Gurkhalis speak the Hindi dialect called Nepalese Khas or Parbatiya. In summer they wear a sort of pantaloons called pdejdrnas and a jacket or coat of white or blue cotton, and in the winter the same padded with cotton or lined with fur and fastened by a cotton girdle, which invariably holds the heavy, crooked knife, called kukhri. Turbans of dark cloth or loosely-folded cotton are used as a head-dress, or small tinsel, embroidered skull-caps. The Newars wear a waist-cloth of cotton and a jacket of the same, or some woollen materials. Some adopt the Tibetan costume of full short trousers, a long tunic, and a fur-edged cap. The head-dress is a small skull-cap of black or white cloth thinly wadded with cotton and generally turned up an inch or so at the border. The dress of the other inhabitants of Nepal differ little from that already described. The women of the Newars wear their hair gathered into a short thick club at the crown of the head, whilst others have it plaited into a long tail. Flesh is much more commonly used by all classes than in the plains. The lower classes drink a coarse fermented stimulant called rakshi, and the higher classes, when they can afford it, consume large quantities of tea. Taking now the tribes inhabiting the lower Himalaya to the Tribes of tlie lower north of the Brahmaputra, we find on the Himalaya. extreme east the Deoriya Chutiya, the remnants of a powerful tribe, who though Hinduised in religion preserve their old language, which is affined to the Barma- Tibetan group. Next come the Dhimal, Kachari or Bodo, and the Koch. Hodgson tells us that in travelling between Gwalpara in Asam and Aliganj in the Morang Tarai of Nepal one has to pass through the country of the following tribes : — the Ivoch, Bodo, Dhimal, Rablia, Hajong, Kudi, Batar or Bor, Kebrat, Pallah, Gangai, Marahi, and Dhanuk. The Rablia, Kudi, Hajong, Mech, Garo, and Pani-koch, are all affined to the Kachari or Bodo type. The last six of Hodgson’s list are doubtful and undefined 2.8 HIMALAYAN DISTRICTS and require further investigation. The Dhimals are found hi the sal forest between the Ivonki and the Tarsa, mixed with the Bodos, but without intermarriage and living in separate villages. The Bodos extend from the Surma to the Dhansiri, and thence by Bijni and the Bhutan and Sikkim Tarai to the Konki ; besides occupying outside the forest limits a large proportion of central and lower Asam. 1 The Rabhas and Hajongs are found in the Gwalpara district and are Hindus, whilst the Pani-koch occupy the tract along the foot of the Garo hills and are still pagans. The Dhimals and some of the Bodos, Kochs, and Mecliis are still pagans. The last- mentioned tribe is found all along the Tarai with the Kochs and Dhimals. Their dialect and religion differ from those of the neigh- bouring tribes of the hills and plains. They are fairer than the Kochs and have strongly marked Mongolian features, but softer than those of the Lepcha or Limbu, resembling more the Newars than the other hill-tribes of Tibetan origin. They live at elevations between 800 and 1,000 feet, and almost always keep to the forest, where they make temporary clearances. Their religion is connected with the Bhairava form of Sivaism. The Koch tribe is now nearly completely converted to Islam or Brahmanism, and with their conversion have dropped their old name and language, speaking a corrupted form of Bengali, in which, however, many of the ancient vocables are retained. The Pani-koch, according to Hodgson, represents the unimproved primitive Koch stock ; but Dalton considers them a plains tribe driven upwards by the Aryan invader. Hodgson estimates the number of all religions at over a million souls. The settled Koch assimilate in their food and clothing with the Bengalis, and show no marked differences. The Bodo women wear garments of coarse silk, the produce of the worm that feeds on the castor-plant. The Bodo men and Dhimals of both sexes wear cotton clothes. The men wear one cloth thrown over the shoulders and another wrapped round the waist and drawn up between the legs. The female garment consists of a cloth wrapped around the body and enveloping it from the arm-pits to the centre of the calves. Wooden sandals are worn, but ornaments are rare, though the women sometimes wear small silver rings in their noses and ears and heavy bracelets of mixed metal. Meat, fish, and 1 See Hodgson’s Aborigines of India, p. 151. OF THE NORTH-WESTERN PROVINCES. 29 vegetables are eaten by all, ancl beer made of rice or millet is a favourite beverage. Tharus and Denwars are found westwards in Nepal mixed with the Mechis, and especially the former in the malarious tract in the Gorakhpur and Tirliut Tarais along the foot of the mountains where no other human being can live. They, however, seem to be healthy, robust races. The mass of the people of the Doti district of Nepal and the British district of Kumaon belong to the race Karnali to the Tons. . , genencally known as Khasas or Khasiyas. In Garhwal they are more mixed, though the difference is scarcely discoverable. The northern inter-Alpine valleys are, however, inhabited by Bhotiyas, who are decidedly of Tibetan origin. Amongst the Khasiyas there is a great admixture of immigrants from the plains, and most of the better classes look down with contempt on the purer members of the Khasiya class, who appear to represent the oldest inhabitants of these hills, though now much modified by centuries of close connection and intermarriage with the more civilized tribes of the plains. Throughout Kumaon, the Kyunam of the Tibetans, the inhabitants dress and eat like those of the plains, the only difference being that to the north woollen materials find more favour, and there is greater license in matters of food and drink. In Garhwal, which is known as Galdiya to the Tibetans and to the north as Chongsa, garments made of hempen fibre are common amongst the poorer classes. The language spoken throughout is pure Hindi, though for purposes of trade the Bhotiyas also use Tibetan, and amongst themselves speak a dialect of Tibetan origin. In the land of marsh and forests which borders the plains we find the Tharus in the eastern Tarai and the Bhuksas, a tribe of similar character, occupying the tract between Puranpur-Sabna in the Bareilly district and Chandpur in the Bijnor district. The Raj is in eastern Kumaon are akin to, the Chepangs of Nepal, and the Luis and Rawats of the same tract are now absorbed in the Hinduised population. To the west of the Tons we have a number of petty independent states known as the “ protected hill-states,” Bisahr. followed by British territory. Amongst the former the most important is Bisahr , 1 of which the northern part, 1 See section D. of references attached to this chapter. 30 HIM/LAY AN DISTRICTS- called Kunawar, or more correctly Knaor, the Kunu of the Tibetans, marches with Tibet. The people of upper Knaor are of Tibetan origin and Buddhists in religion, and correspond to the Bhotiyas further east. Buddhism extends down the valley of the Satlaj as far as Sarahan, between which and Pangi is a sort of debateable ground common to Hindus and Buddhists ; but north of Pangi Buddhism prevails, and south of Sarahan, Hinduism. With our approach to these Buddhist countries the curious custom of poly- andry appears. Commencing in north-western Tihri, we trace it through Bisahr and Lahul, but find it confined to the inhabitants of the valleys of the central and higher ranges professing both the Buddhist and Hindu religions. The central tract is inhabited by a fair, slight, and muscular race of mixed origin known as Kunets, and akin to the Khasiyas on the east. To the south, in the portion adjoining the plains, the people resemble the inhabitants of the lower country, and appear of every shade of colour from dark-brown to a tawny yellow or yellowisli-white. The hair is black and worn long at the sides and back of the head down about the ears, where it is cut short. The crown of the head is shaved bare, but moustache and beards are worn. The dress is a short coat of coarse cotton reaching to the knee, pleated in folds to give it fulness, and fastened round the waist by a girdle of the same material. A pair of cotton pdejdmas and a sheet of the same material complete the hot-weather costume. In winter these are exchanged for a pair of woollen drawers and a blanket, but the poorer classes remain content with a coarse waist-cloth and a blanket all the year round. The food of the people from the Kali to the Indus differs very little in each tract, or, indeed, from that of the people in the adjoining plains. Wheat, barley, rice, and various millets and pulses are grown in the lower hills, and to the north hardier varieties suited to a sub- arctic climate are cultivated. When the produce is insufficient for the wants of the inhabitants, a supply is imported from the lower districts. To the north, woollen home-spun replaces the cotton worn in the lower hills, and the girdle supports an axe. The women wear a similar dress, the coat reaching down to the ancles, and the hair, done up in long plaits, is twisted into rolls and covered with a piece of cloth wound like a turban round the head. OF THE NORTH-WESTERN PROVINCES. 31 To the west of the Satlaj we find the British territory of Knlu and Mandi, the independent state of Chamba, and the territories of Kashmir and Jamu. 1 Kulu, called in Tibetan Nyungti and Mandi, lies along the upper course of the Byas ; Chamba, known to Tibetans as Panga, along the Itavi ; and Laliul, the Tibetan Grarzha, on the Upper Chinab. To the north in Laliul and Ladak the people are Bhotiyas or Bodpas of Tibetan origin, professing tho Buddhist religion, and amongst them is a servile race known as Bern or ‘ low.’ Further east in Bcil- tistcin are Tibetan Musalmans who have adopted with their religion the Arabic alphabet. All these have decided Mongolian features, and are noted for their strength of body and power of enduring fatigue. In this respect the Baltis are somewhat inferior to their Buddhist brethren in race. The men wear a coat of woollen mate- rial reaching to the knees, fastened by a girdle, in which a knife is usually carried. Bound their legs, from knee to ancle, they have coarse woollen leggings secured by a tape of the same material wound spirally round the leg from the ancle upwards. The head-dress is either a quilted skull-cap or a fur cap with the hair or wool inside, and with a large flap behind which covers the neck and ears. They wear boots of felt with soles of sheep or goat-skin. The women wear a black woollen jacket with a striped parti-coloured petticoat and baggy trousers, and over all a skin coat with the fur turned inside. The hair is arranged in a number of small plaits, and is ornamented by a band of cloth, on which is sown a number of tur- quoises and beads. The food of the common people consists of thick barley cakes, though those who can afford it eat wheaten bread and drink tea and a fermented liquor called dicing. Tho name Kunet seems properly to designate only the mixed race in southern Ivnaor, but it is used for the population of the central tract in Bisahr, Kulu, Chamba, and Kashtwar, which borders on Ladak. In Chamba we find the Gaddis, who cross over into the neighbouring territory of Kashmir and meet the Thakars or Takkas, the chief cultivating class in those hills, and apparently in the same position with refer- ence to other Hindus as the Jats of the plains. In the valley of Kashmir we have the Kashmiris, and amongst them the servile class called Batal. To the south-west, along the left bank of the 1 See section E. of references attached to this chapter. 32 HIM A' LAY AN DISTRICTS J hoi am, we have the Musalman Dogras, called Chibhalis, and the Musalman Sadans of Punch. On the right bank of the same river we have Musalman Gakkars, Satis, and Dunds. To the east of the Chibhalis come the Hindu Dogras, and amongst them the servile tribes of the Meghs and Dums, who are scattered about everywhere and form a considerable part of the population. The Dogras have a light-brown complexion, clearly-cut features, and black hair, which is cut to form a fringe below the turban. The hair is worn on the face. The Thakars are a well-made race, somewhat more powerful in body than the Dogra Rajputs, whilst the Meghs and Dums are darker in colour, smaller in limb, shorter in stature, and less bearded. The food and clothing differ in no marked respect from that of the hill-tribes at a similar elevation to the east. Passing to the north-west of the Kashmir valley we come upon the Dards, an Aryan tribe called Brokpa by the Tibetans, and most of whom are Musalmans, though the Dab section have adopted the Buddhist religion, language, and customs. They occupy Astor and the trans-Indus Kashmiri district of Gilgit, as well as the neighbouring Kanjdd states of Nagar and Hanza, and the Kashkara states of Chitral, Yassan, and Mastuj. They are a strongly-built race, with decidedly Aryan features, wearing woollen garments, except among the higher classes, who wear cotton in summer. The ordinary costume consists of trousers, a coat reaching to the knees and confined by a girdle, and a cap of woollen cloth about half a yard long and turned up at the edges until it fits the head, the outward roll thus forming a protection against heat and cold. On their feet they have scraps of leather put under, over, and around the foot, and kept in their place by straps of the same material wound around them. A servile race is also found amongst them, known as Dums, and performing the same duties as the Dums of Kumaon. To the south-west of Kashmir, in the salt range, we find the Awans and Janjuhas, tribes of Aryan origin and of considerable antiquity. From the Kali to the Indus, dialects of Tibetan are spoken to the north. Mr. Drew tells 1 us that from near the Nunkun group of peaks which form the water- parting between the Maru-wadwan and Suru rivers, “and from no other spot in Asia, one may go westward through countries entirely 1 Northern Barrier of India, p. 20. OP THE NORTH-WESTERN PROVINCES. 33 Muhammadan as far as Constantinople ; eastward among none but Buddhists, to China ; and southward over lands where the Hindu religion prevails, to the extremity of the Indian peninsula.” Amongst the great mountain groups comprising the western or , „ , , . , , trans-Indus extension of the Himalaya, and Afghanistan, &c. , J including the ranges known as the Hindu Kush, Kara-koram, and those connecting them with the Tian-shan, are several petty states, regarding which much has been learned of late. 1 To the south lies the country called Afghanistan, the north- eastern portion of which is included in the western prolongation of the Himalaya, while the south-western part is a mountainous country confluent with the Himalaya on the one hand and extend- ing far in the opposite direction to the table-land of Persia. To the north the boundaries are ill-defined and vary almost from decade to decade. The authority of the ruler of Kabul, in many places, depends on the forces at his disposal to coerce his unwilling subjects; but in 1879, the Afghan province of Turkistan included the whole of the countries between the Hindu Kush and the Oxus, comprising Balkli, Kunduz, and Badakshan, with their dependent states. The seat of the government is Balkh, Avith cantonments at Faizabad. Karatigin, on the upper valley of the Surkhab, pays tribute to Bukhara ; also Darwaz, on the Panja branch of the same river, and Shignan-cwm-Iloshan, on the Ghund and Murghab rivers. Wakhan is tributary to Badakshan, and south of it lies Kashkara, also called Chitral. Northern Kashkara, including Yassan and Mastuj, is subordinate to the ruler of southern Kashkara, who resides at Chitral. North of Gilgit we have the robber states of Hanza and Nagar or Kanjud. South of Gilgit, in the A-alley of the Indus beloAV Banji or Bawanji, are a number of small republics, who manage their affairs in assemblies called sigas , with Avhich we may compare the similar institutions at the opposite extremity of the Himalaya. Some of these, such as Darel and Hodar, owe a nominal subjection to Kashmir. Further south Ave come to the independent tribes of Buner and Swat. West of the Indus, in the Kunar valley, are the Bajaur and Dir states, and betAveen them and the Hindu Kush range the country of Kafiristan. 2 It may Avell 1 See section F. of references attached to this chapter. 2 Lately partially explored by Major Tanner, R.E. 5 34 HIMALAYAN DISTRICTS be supposed that this rugged tract, the meeting-place of the Turanian, Iranian, and Aryan races, presents many points of interest to the ethnographer as well as to the geographer ; but here we can but very briefly refer to them, however important they may be. We have already noticed an Aryan race, the Dards, occupying Gilgit and forming a part of the population of the neighbouring states. Here they meet the great Iranian race, which, under the name Tajik or Galcha, form the bulk of the cultivating population of the Musalman states between the Indus and Jaxartes. History tells us that from the third century before Christ to the sixth century after Christ this tract was subject to the continued incursions of a Skythian race, traces of whom may be seen in the Brahuis of Biluchistan, the Hazaralis of the Hindu Kush, the Gujars there and in India, the Gakkars and Kohistanis of the Indus, and the Jats of India, and who have continued to influence the entire history of this tract to the present day. In the eleventh century the Afghans were a small tribe in the Sulaiman mountains, of no importance and but little known. Since then they have increased so much as to have been able to annex a considerable extent of country, and to impose their language, Pukhtu or Pushtu, on the populations which they have absorbed. Along the Indus, Afghans occupy the villages as far as Batera in 34° 53' north latitude, where the Kohistan commences. The Afghans themselves are tolerably fair, robust, and of moderate stature. They have long faces, high cheek-bones, and dark hair, which they wear unshaved. Their underclothing is of cotton, over which they throw a loose coat of woollen cloth, felt, or, more commonly, of sheepskin. They wear low caps on their heads, around which a cloth is twisted to form a turban. Boots are generally worn, and they cany a matchlock, scymitar, and shield. Leavened bread and meat are eaten by all classes. The women are rigorously secluded in the towns, but in the country, beyond the influence of the local maulvi or mullah, much more liberty is allowed. The use of wine is forbidden, but in the hills it is taken in secret, and that made in the Harel valley has more than a local reputation. Pushtu approaches the Pehlavi or Zendic form of old Persian on the one hand, and the Sindhi form of Prakrit on the other. It is spoken throughout Afghanistan, and, with dialectal variations, in OF THE NORTH-WESTERN PROVINCES. 35 Kohistan, Kaslikara. Bajaur, Panjkora, Dir, and Swat. Afghans are Sunni Muham- madans. The Kohistanis of the Indus claim an Arab descent and speak a language different from Pushtu and akin to Kashkari and Dardui. They are fair and have sandy hair, and are of a robust make. They wear a tight-fitting coat and trousers resembling somewhat those of the European, with a cap of brown woollen material in the form of a bag rolled up at the edges. Around the legs and the feet a goatskin is wound, kept in its place by a strap of leather, the great-toe and the heel being left bare. A matchlock and sword are always carried, and they are expert shots. The women wear a loose jacket and trousers, and a cap of cotton or wool, over which they throw a woollen or cotton sheet when proceeding far from their villages. Unleavened bread of wheat, barley or millet (liolcus sorghum ) is eaten with vegetables, milk, butter, or stewed meat. Further north the people are less prosperous and more regardless of cleanliness. In some of the villages there are colonies of pastoral Gfujars, and in the Yassan villages settlements of Duins, who supply the musicians and dancers of the country. Following next the Kunar valley, we have dialects of Pushtu spoken in Bajaur and Dfr as far as the Lahori pass leading into Chitral. Here it meets the Kaslikara, which is akin to the Dardui and is of Prakritic origin, though many Persian vocables have been added. The pagan inhabitants of Ivafiristan are of the same race as the Kashkaras and the Dards, and speak a language having an archaic Prakritic origin. Moving further westward into Badakshan, we come amongst a large Iranian population speaking Pushtu in the south and Persian in the north, and from Harm an Uzbeg population speaking Tiirki, and the nomad Hazarahs having a dialect of their own. On the invasion of the Turks the old inhabitants retreated into the more inaccessible valleys of the great ranges, and there founded the Galcha states of Darwaz, Karatigin, Shighnan, and Waklian. In Darwaz and the adjoining- parts of Badakshan pure Persian is spoken or understood. The vocables and grammar of the Galcha proper show a strong affinity to Dardui, and many conjecture that, in its pure state, it must have been the intermediate link between the Iranian and Indian branches Galcha states. 36 HIMALAYAN DISTRICTS of the great Aryan family ; that the dispersion took place from the ‘ bam-i-dunya , / £ the roof of the world/ the Indian branch proceeding southwards and along the Kabul river to India, whilst the Iranian branch crossed the Pamir to the plains of Turkistan. Towards the plains the Galchas are Sunnis, but in all the hill districts, except Darwaz, they are Shiahs. The Shiah is held in the same contempt as the infidel, and the Sunni esteems it a holy and righteous act to capture and sell his less orthodox fellow-believer into slavery. Amongst the tribute paid by the hill states to the Afghan governors of Badakshan and to the Wali of Bukhara, not the least important parts are the troops of fair- complexioned girls from the upper valleys of the Gbilclui states, and, when procurable, pagan boys from Ivafiristan. Uzbegs are chiefly found in the country, and Tajiks in the towns along the plains below Badakshan and in Turkistan ; the former invariably speak Turki and the latter Persian, or dialects with a number of Persian words in them. In IVakhan the men wear brown woollen coats and trousers, Ladaki boots, and a scanty cotton turban, either blue or white. The women here also dress much like the men, and, as in Chitral, wear their hair in long plaits. They have Jewish noses and are not very fair-looking. Kirghiz are found along the eastern slopes of the Tian-shan and the northern slopes of the Pamir and Kuen-lun ranges in Chinese Turkistan. The Alai Kii ghiz of the Pamir have a bad reputation as robbers. East of them lie the great uninhabited steppes until we come to the countiy neai Kanjud, which is rendered unsafe by the raids of the people of Hanza and Nagar. Further east we have the Chang-thang highlands, occupied by the robber Bhotiya tribes of Changpas, speaking a Tibetan dialect akin to Zanskari. The dress of the male Kirghiz inhabiting the pastoral slopes of the highlands south of Yarkand and Kashgai is not different in any material degree from that of the other inhabitants . 1 Their women wear as a head-dress a white cloth rolled evenly and regularly round a skull-cap ol red or other bright material, with lappets over the ears. The end of the turban is drawn down and passed over the lappets and under the chin, and the coat worn is a dressing-grown of wadded and cpulted cotton. In the plains the winter dress of the females comprises a fur cap of black lamb’s i Gordon : Roof of the World. OF THE NORTH-WESTERN PROVINCES. 37 wool with a trimming of the fur, and a crown of coloured silk or cloth worn over a square of muslin which forms a veil. The coat worn is full and long, and the boots are of embroidered leather with high heels. The hair is worn either in two long plaits or in ringlets. The men wear a close-fitting cap lined with fur and turned up at the bottom. The coat resembles that worn by the women, only it is fastened by a cotton girdle, and the boots are worn long and plain, with felt stockings. In winter, sheepskin with the wool attached is the universal material for clothing. To Prejevalsky we are indebted for an account of the people around the lake country of the Tarim near Kara-kurchins. m t Lob-nor, to the north of the Altyn-Tagh, and of those inhabiting the eastern extremity of the Kuen-lun near the sources of the Hoang-ho. The former 1 present “ a strange mixture of facial types, some of which call to mind a Mongolian race. The prevailing characteristics are, however, Aryan, though far from pure. * * In height they are rather below the average ; frame weak and hollow-chested ; cheek-bones prominent and chin pointed ; beard scanty and a V Espcignole ; whisker even smaller ; hair on the face generally of feeble growth ; lips often thick and protruding ; teeth white and regular and skin dark, whence their name Kara-kurchin may be derived.” Their language is said to resemble closely the dialect of Khoten. The clothing of the lake-dwellers is made from the fibres of a species of cisdepias, and consists of a loose coat and trousers with, in winter, a sheep- skin cap, and in summer one made of felt. In summer the feet are uncovered, and in winter shoes of untanned hide are worn. The coats in winter are lined with duckskins dressed in salt.. Fish, wild-fowl, and the tender shoots of reeds are their principal food. All profess the Muhammadan religion. The inhabitants of the country along the Tarim towards Korla appear to be also of the same race, though comparatively more civilised. To the north-east, towards the Yellow river, we have the Kara- Tangutans, a race apparently connected with the Tibetans proper. They are more robust in form, greater in stature, and darker in complexion, than 1 From Kulja across the Tian-shan to Lob-nor : London, 1879, pp. 44, 166, See, further, section G. of references attached to this chapter. Tara-Tangutans. 38 HIMALAYAN DISTRICTS the Tan gu tans of Kan-su. Their hair is black, hut the head is shaved clean and no pig-tails are worn. The eyes are dark and large, never narrow like the Mongols ; the nose straight and some- times aquiline and also sometimes retroussde; the lips thick and protruding ; the cheek-bones not so prominent as in the Mongol ; the face long and never flat, and the skin tawny coloured. The language is akin to Tibetan. The dress in summer comprises a long, grey, woollen coat reaching to the knees, boots, and a low- crowned, broad-brimmed, felt hat. In winter a sheepskin coat is put next the skin, and the upper part of the legs is usually left bare and also the right arm and part of the right breast, the right sleeve being allowed to hang down empty. The women dress like the men, and all live in tents made of black, coarse, woollen cloth, whence the name Kara (or black)-Tangutans. They are met as far as the Murui-ussu, the extreme point reached by Prejevalsky. 1 Of the people between the Hoang-ho and Brahmaputra very little is known beyond the fact that they are of Tibetan origin and chiefly Buddhists in religion. Pamutan near Bathang, which lies in about 99° east longitude and 28° 50' north latitude, is the most westerly point attained by Mr. Cooper 2 in his memorable journey from Han- kow towards the frontier of India in 1868 ; and Prun, in the Mishmi country, the most easterly point reached in his attempt to penetrate the intervening ranges to China in 1870, leaving a space of about 120 miles as the crow flies unexplored and unknown. W e have now briefly sketched the character of the countries ^ and peoples encircling the great elevated area which from Ladak on the west to the Chinese frontier is known as Tibet, and is entirely under Chinese influence. The true name of this tract is Bod-yul or Bod-land, and the people Bod-pas, corrupted by the Indians into Bhotiyas, a name now applied to the Tibetans living on the borders between India and Tibet, whilst the people of Tibet proper are called Huniyas and the country Hundes. The eastern division of Tibet is known as Kham or Kham-yul, sometimes called Bod-chon ; it extends from the frontiers of China to about 95° east longitude. Central Tibet or Tibet proper is called Bod at its eastern end, and 1 Mongolia, by Prejevalsky: London, 1876, II., pp. 109, 301. 2 Travels of a Pioneer of Commerce in Pig-tail and Petticoats : London, 1871. OF THE NORTH-WESTERN PROVINCES. 39 g-Ndri or Nari at its north-western end ; the former division being the shorter of the two, but perhaps broader and more civilised and populous. A line drawn from Darjiling northwards would apparently separate Bod from Nari. The central part is also called U-Tsang from the two provinces of U and Tsang in which Lhasa is situated. Nari is divided into the three great districts of Mang-yul, Khorsum, and Mar-yul. 1 The first marches with Nepal almost to its western boundary ; the second extends along the British frontier of Kumaun and Gfarhwal and that of the independent state of Bisahr ; and the last included western Tibet and the Kashmiri states of Balti and Ladak. The physical characteristics of this tract have had the effect of isolating its inhabitants, who are distinct in race . and language, from all the nations we have described, and find their affinities in the Tangutans of the north-eastern Kuen-lun already noticed. They are broadly built; have dark hair, scanty beards, high cheek-bones, oblique eyes, complexion fair amongst the better classes, dark amongst the lower, who are more exposed to the weather. To the east in the warmer valleys they are agriculturists, and to the west and north follow a pastoral life. The costume varies in the different provinces and with the means of the person, but as a rule the men in the wilder parts shave the head clean like the Kara-Tangutans, whilst the more settled allow it to grow long and plait it into a queue or tail like the Tangutans proper. To the east Chinese fashions are in vogue, and to the west the common dress is a coat and trousers of undyed woollen material with boots to the knee. The Lamas wear distinctive dresses, red or yellow according to the sect to which they belong, and the wealthier indulge in coloured broad-cloth garments of English or Russian manufacture. Barley porridge, tea and meat form the staple food of the people, and dicing or beer, a simple infusion of malted barley, is of universal use all over Tibet. Having completed our review of the nations inhabiting the Himalaya and the surrounding country, we General distribution. , . n .. ,. may now bnefiy notice the natural distribution of the several great races that have come under our consideration in 1 From Captain Henry Strachey’s paper on the physical geography of Western Tibet, London, 1854, still our best authority on the subject. A more detailed account will be given hereafter in tlie Gazetteer portion of this memoir ; see also section H, of references attached to this chapter. 40 HIMALAYAN DISTRICTS the special tracts that each now occupies. The extraordinary rigour of the climate and the physical barrier that exists between Tibet and India sufficiently explains the absence of ethnical or political relations between the two countries. Accident has (riven the Indian state of Kashmir political preponderance in western Tibet, but the ethnical distinction still remains, and will probably ever continue. The climatic condition of eastern and northern Tibet allows of a free migration of the inhabitants from one part to the other, which is shewn in the common origin of the people of those countries to the present day. Turks and Tartars occupy the country called Turkistan, similar in character to their original homes ; but in proportion as the climatal conditions become Indian, so does the population become Aryan. The Tartar is the child of the rugged bleak steppes ; and when we approach the cold and wooded mountains we come on the Hindu element at its maximum in the tract around the sacred sources of the Jumna and the Ganges, gradually diminishing as we move eastward towards the excessively moist though warmer valleys of the Nepal and Asam Himalaya, where they are replaced by races akin to the people of eastern Tibet and Siam, and on the west meeting the Iranian and the Tartar in the trans-Indus ranges. To the north of the Kuen-lun the Mongol and Chinese converts to Muhammadanism, called Tunganis, and in western Tibet the Muhammadan Baltis, divide the Buddhists from the followers of Islam. In the valleys of the affluents of the Oxus and the Kabul river we have an Iranian race of Galchas or Tajiks driven upwards by political disturbances and mixing with an indi- genous mountain race of Aryan extraction. The rigorous climate and scant}- cultivation which prevents the intrusion in any numbers of a southern race also debars the tribes inhabiting the higher hills from making any permanent occupation of the lowlands. Like their favourite domestic animal the yak, the Himalayan mountaineers do not thrive at low altitudes, nor can plains-bred men or animals with- stand for any time the arctic cold and rarefied air of the more elevated regions. Thus, there is a clear connection between the distribution of the nations that are found in the Himalaya and the physical characteristics of the regions that they occupy ; and if we had time to pursue the subject further, it might be shown that the orographical conditions of a tract have materially influenced its history, political OF THE NORTH-WESTERN PROVINCES. 41 Hnd religious, and tlie social and moral character of its inhabitants. The disposition of a people towards peace or war ; their migrations ; the diffusion of their language ; their habits, pastoral, agricultural, or commercial ; the extent of their influence — all depend more or less on the physical peculiarities of the country that they inhabit. And not only is man so affected, but the entire fauna and flora obey the same laws, so that the skilful naturalist can from a plant or even a butterfly describe the general character of the country of which it is a native, and with it the customs and manners of the inhabitants. For the nature of a country, whether mountainous or level, the direction of the great ranges, the length and line of coast, the position with regard to the equator, the relations of land and water, and the drainage systems, are all primary agents in the distribution of organic life and of the influences which govern all atmospheric and climatic phenomena. G 42 HIMALAYAN DISTRICTS REFERENCES. The following list of references to books bearing on the geographical and ethnological notices in the preceding chapter is not intended to bo exhaustive, but simply to furnish a guide to the bibliography of the countries within and adjoining the Himalaya, aud only includes such works as are ordinarily procurable. Section A.— Eastern Asam and Tibet. («) — Indo-Chinese Frontier. 1. La Mission du Thibet, by Fr. C. FI. DesGocIins. Verdun, 1872. 2. Pays frontieres du Thibet, de la Burmanie et de Yunnan, by the same. Bull, de la Soc. de Geogr. de Paris, Oct., 1876. 8. Territoire de Bathang, by the same. Ibid, Dec., 1876, and Dec., 1877. 4. Le cours superieur des fleuves de lTndo-Chine, by the same. Ibid, Aug., 1876, 5. Notes sur le Thibet, by the same. Ibid, Oct., 1877. 6. Mandalay to Momein, by J. Anderson. London, 1876. 7. Overland route to China via Asam, the Tenga Pani river, Khamti and Singpho country, across the Irrawaddy river into Yunnan, by PI. Cottam. P. R. G. S., XXI., 6. 8 Travels in Western China and on the Eastern borders of Tibet, by Capt. W. J. Gill. Ibid, XXII., 255, and see H., 26. 9. Across China from Chin-Eaing to Bhamo in 1877, by J. McCarthy. Ibid, I. N. S., 489. 10. Official narrative of the expedition to explore the trade routes to China via, Bhamo under Major Sladen. Calcutta, 18 lO. ^ j Travels of a Pioneer of Commerce in Pigtail and Petticoats ■ an overland jour- ney from China towards India, by T. T. Cooper. London, 1871. 12. Journal of an attempted ascent of the river Min to visit the tea-plantations of the Fukhien Province of China, by G. J. Gordon. J . A. S., Ben., IV ., 553. 13. Short survey of the country between Bengal and China, by Baron Otto des Granges. Ibid, XVII., i., 132. 14 Memorandum on the countries between Thibet, Yunnan, and Burmali, by Rev. T. D’Mazure. Ibid, XXX., 367. (See also the writings of Blakiston, Margary, Fytche, Poll ok, Phayre, &c.) (5) — Upper Asam. 15, Memoir of a survey of Asam and the neighbouring countries executed in 1825-28, by Lieut, R. Wilcox. As. Res., XVII., 436, and Sel. Rec., Bengal, XXIII., 1855, and Sel. papers, Hill tracts, 1S73, p. 1. 36. Account of Asam, the local geography, tea-plant, manners of the neighbour- ing tribes, by W. Robinson. Calcutta, 1841. 17. Report on the Eastern frontier of British India, by Capt. R. B. Pemberton, Calcutta, 1835. 18, Journals of travels in Asam, Burmah, Bootan, and Afghanistan, by W. Griffiths', Calcutta, 1847. 19. Memoir on Sylhet, Kachar, and the adjacent districts, by F. H. Fisher. J. A, S., Ben., IX., 808. 20, Notes on northern Cachar, by Lieut. R. Stewart, Ibid, XXIV., 582, OF THE NORTH-WESTERN PROVINCES. 43 21. Travels and adventures in the Province of Asam, by Major J. Butler. Lon- don, 1855. 22. Koch Bihar, Koch Ha jo, and Asam in the 16th and 17th centuries, by H. Blochmann. J. A. S., Ben., XLI., i., 49. 23. History of Asam, by Anundorum Boruah. Calcutta. 24. Memorandum on various phenomena in Asam, by the Rev. N. Brown, J. A. S., Ben., XIL, 909. 25. Notes on the Asam temple ruins, by Capt. E. T. Dalton. Ibid, XXIV., i. 26. Description of ancient temples and ruins at Chardwar in Asam, by G. E. Westmacott. Ibid, IV., 185. 27. Note on ancient temples and other remains in the vicinity of Suddyah in Upper Asam, by Major S. F. Hannay. Ibid, XVII., i., 459. 28. Ruins at Dimapur on the Dunsiri river, Asam, by Major Godwin-Austen. Ibid , XLIII., 1. 29. Temple at Jaysagar in Upper Asam, by J. M. Foster. Ibid, 311. 30. Contributions to the geography and history of Bengal, by PI. Blochmann. Ibid, XLII., 209 : XLIII., 280. 31. Report of a visit to the hills in the neighbourhood of the Soobansiri river, by Lieut. S. F. Hannay. Ibid, XIV., 250. 32. Account of a visit to the Jugloo and Seesee rivers in Upper Asam, by the same. Ibid, XXII., 511. 33. Report of an expedition into the Mishmee hill to the north-east of Sudyah, by Lieut. E. A. Rowlatt. Ibid, XIV., 477. 34. Journal of a visit to the Mishmee hills in Asam, by W. Griffith. Ibid, VI., 325, and Sel. papers, Hill tracts, 110. 35. Notes on the language spoken by the Mi-Shmis, by W. Robinson. Ibid, XXIV., 307. 36. Note on the Dophlas and the peculiarities of their language, by W. Robinson. Ibid, XX., 126. 37. Correspondence and journal of Capt. Dalton in a visit to a clan of Abors on the Dihing river. Sel. Res., Ben., XXIII., 139. 38. On the Meris and Abors of Asam, by the same. J. A. S., Ben., XIV., 426. 39. Account of the mountain tribes on the extreme north-eastern frontier of Ben- gal, by Capt. Jenkins, edited by J. McCosh : containing notices of the Miris, Abors, Mishmis, Kangtis, Singhphos, Muamarias, and Nagas. Ibid, V., 193. 40. Notes on the tribes of the eastern frontier, by J. H. 0’D.oneI. Ibid, XXXII., 400-404, and by PI. J. Reynolds. Ibid, 407. 41. Memorandum an the north-eastern tribes, by A. Mackenzie. Calcutta, 1869. (c) — E thnography. 42. Descriptive Ethnology of Bengal, by E„ T. Dalton : Calcutta, 1872. [Gives an account (with figures) of the Khamtis ; Singhphos, Mishmis, Cliulikata Mishmis ; Abor group', including Padams, Miris, Dophlas, and Akas ; Nagas of Upper Asam ; lower Nagas, including Kukis, Mainpuris, and Koupouis ; Mikirs ; Jaintiyas and Khasiyas ; Garos, Kacharies ; Mechs ; Kochs ; Bhotiyas ; Lepchas ; Murmis ; Limbus and Kirantis ; Hayas, and the Tipura (Tipperah) and Chittagong tribes]. 44 HIMALAYAN DISTRICTS (d)— Gabo Hills. 43. Observations on the inhabitants of the Garrow hills, by J. Eliot. As. Res., III., 17. 44. A narrative of our connection with the Dushani and Cliianni Garrows, with a short account of their country, by C. S. Reynolds. J. A. S., Ben., NYU!., 1, 45. 45. Some account of the Casiah hills. Gl. in sec. I., 252. 46. Notes on the Casiah hills, by H. Yule. J. A. S., Ben., XIII., 612. 47. A vocabulary of the Garo and Konch languages, by Lieut. W. J. Williamson. Ibid, XXXVIII.., 14. 48. Khasia grammar, selections and vocabulary, by W. Pryce. Calcutta, 1855. 49. English- Khasia vocabulary, by Kelsall. Calcutta, 1864. See also Hodgson’s papers. 50. Some account of the Palis of Dinajpur, by G. H„. Damant, Ind. Ant., I., 336, 371. 51. On the dialect of the Palis, by the same. Ibid, II., 101. 52. The Garos, by the Rev. I. J. Stoddard. Ibid, II., 336. 53. On the Khasia hill-tribes of north-eastern Bengal, by A. Morgan. P. Lit. and Phil. Soc., Liverpool, 30, 1875-76. Section B — Southern Asam. 1. Report on the wild tribes of the Chittagong frontier, by C. Ricketts. Cal- cutta, 1847. 2. Some account of the hill-tribes in tire interior of the district of Chittagong, by the Rev. M. Barbe, J, A. S., Ben., XIV., 380. 8. Selection of papers regarding the hill tracts between Asam and Burmah and on the Upper Brahmaputra. Calcutta, 1873. 4. The wild tribes of the south-east frontier, by Capt. T. H. Lewin. 5. The Chittagong hill tracts and the dwellers therein, with comparative voca- bularies of the hill dialects, by the same. Calcutta, 1869. 6. History of Arakan, by Col. J. P. Phayre. J. A, S., Ben., XV., 232. 7. Account of Arakan, by the same. Ibid, X., 679, 8. History of Pegu, by Sir A, Phayre. Ibid, XLII., 23, 120 : XLIIL, 6. 9. Notes on the Heuma or Shendoos, a tribe inhabiting the hills north of Arra- can, by Capt. Tickell. Ibid, XXL, 207. 10. History of the Burmah race, by Sir A, Phayre. Ibid, XXXVII., i. : XXXVIII., 29. 31. The hill tribes of the north-east frontier. Ind. Ant,, I., 62, 12. The Lushais, by Capt. Badgley, Ibid, II., 363. 13. Abstract of the journal of a route travelled by Capt. S. F. Hannay from the capital of Ava to the amber mines of the Hukong valley on the south- eastern frontier of Asam, by Capt. R. B. Pemberton. J. A. S., Ben., VI., 245, and No. 3 above, p. 83. 14. Journey from Upper Asa:m towards Hookhoom, Ava, and Rangoon, by W, Griffiths. No. 3 above, p. 125. Narrative of a journey from Ava to the frontier of Asam and back in 1836-31, by G. T. Bayfield. Ibid, 134, 15 . OF THE HORTI-I-WESTERN PROVINCES. 45 16. Notes on a trip across the Patkoi range from Asam to the Hukoong valley, by H. L. Jenkins in 1869-70. Ibid, 245. 17. Notes on the Burmese route from Asam to the Hukoong valley, by the same. Ibid, 250. 18. The Nagas of Asam, by Capt. Jenkins. J. A. S., Ben., V., 207. 19. Extract from the narrative of an expedition into the Naga territory of Asam in 1840, by Lieut, Grange. Ibid, VIII., 445 : IX., 947. 20. Extracts from a report on a journey into the Naga hills in 1844, by B. Wood. Ibid, IX., 947 : X., 126 : XIII., 771. 21. Extract from a memoir on some of the natural products of the Angami Naga Hills, by J. W. Masters. Ibid, XIII., 707 : XVII., i., 57. 22. Narrative of a tour over that part of the Naga hills lying between the Diko and Dyang rivers, by Capt. Brodie. Ibid, XIV., 828. 23. Report of Lieut. Brodie’s dealing with the Nagas on the Sibsagar frontier in 1841-46. Sel. papers, Hill tracts, p. 284. 24. Note on a visit to the tribes inhabiting the Hills to the south of Sibsagar in Asam, by S. E. Peal, J. A. S., Ben., XLI„ i., 9 : and Sel. papers, Hill Tracts, p. 316. (/)— Languages. 25. A rough comparative vocabulary of some of the dialects spoken in the Naga Hills, by Capt. J. Butler. J. A. S., Ben., XLII., i., App. i. Vocabulary of the Banpara Nagas, by S. E. Peal. Ibid, xxx. 26. Account of the valley of Munipur and of the Hill tribes, by Major McCulloch. (To which is added a comparative vocabulary of the Munniporee, Undro Sengmai, Chairel, Meeyang, Koupooee Poveeron, Koupooee Songboo, Qoireng, Khoonggoee, Pliudang, Koopome, Tukaimee, Muram, Murring Anal Namfau, Kookie, Burmese and Shan languages). Sel. Res., Government of India, For. Dept., XXVII., 1859. 27. Analysis of the Bengali poem ‘ Rajmala,’ or chronicles of Tripura, by the Rev. J. Long. J. A. S., Ben., XIX., 533. 28. Progressive colloquial exercises in the Lusliai dialect of the Dzo or Kuki language, by Capt. T. H. Lewin. Calcutta, 1874. 29. Hill Proverbs : a collection of wit and wisdom from the people of the Chitta- gong Hills, by the same. Calcutta, 1875. 30. Notes on the languages spoken by the various tribes inhabiting the valley of Asam and its mountain confines, by W. Robinson. J. A. S., Ben., XVIII., i., 183, 310. ' 81. A dictionary in Asamese and English, by M. Brouson, American Baptist Missionary. London, 1876. 32. Note on the Shans, by Col. S. F. Hannay. Calcutta, 1846. 83. A visit to Xiengmai, the principal city of the Shan State, by Sir R. H. Schomburgh. J. A. S., Ben., XXXII., 387 (1863). 84. Introductory sketch of the history of the Shans in Upper Burmah and Yunan, by N. Elias. Calcutta, 1876. 85. A grammar of the Shan languages, by J. Cushing. London, 1877. 86. Alphabets of the Tai languages, by Rev. Nathan Brown, with plates of those of the Ahom, Khamti, Shyan, Laos, and Burmese. J, A. S., Ben., VI., 17. 46 HIMALAYAN DISTRICTS 37. Interpretation of an Ahom inscription, by Capt. Jenkins. Ibid, 980, 38. Comparison of Indo-Chinese languages with comparative vocabularies of Bangali, Asamese, Khamti, Siamese, Aka, Abor, Mishimi, Barmese, Karen, Singpho, Jili, Garo, Manipuri, Songpu, Kapwi, Koreng, Maram, Champhung, Lahuppa, N. Tangkhul, C. Tangkhul, S. Tangkhul, Khoibu, May ing, Anamese, Japanese and Corean, by Rev. W. Brown. Ibid, 1,023. 39. Description of the tomb of an Ahom noble, by C. Clayton. Ibid, XVII., i., 473. 40. Note on Ghargaon in Asam, by J. M. Forster. Ibid, XLI., i., 32. 41. Note on the Singphos, by Col. S. F. Hannay. Calcutta, 1846. 42. Report of a visit by Capt. Vetch to the Singpho and Naga frontier of Lakim- pur in 1842. Sel. papers, Hill tracts, p. 255. 43. Remarks on the Indo-Chinese alphabets, by Dr. Bastian. J.R.A. S., III., ii. Section C.— Bhutan, Sikkim, Nepal. (&) — Bhutan. 1. Narratives of the Mission of George Bogle to Tibet (1774), and of the journey of Thomas Manningto Lhasa (1811-12), by C. R. Markham. London, 1870. 2. Notes on Dr. Hamilton’s Missions to Panakha in 1775 and 1777. 3. Account of an embassy to the court of the Teshoo Lama in Tibet and a journey through Bootan, by Capt. S. Turner. London, 1806. 4. Poorungeer Gosseyn’s residence at Lhasa in 1785. As. Res., I., 207. 5. Account of Bhutan, by Kishan Kant Bose. As. Res., XII., 128. 6. Report on Bootan, by Capt. R. B. Pemberton. Calcutta, 1839. Journal of the Mission to Bhutan, 1837-38, under Capt. R. B. Pemberton, by W. Griffiths, M.D. Calcutta, 1847, and J. A. S., Ben., VIII., 208, 251. 7. Report on the state of Bootan and on the progress of the Mission of 1863-64, by the Hon’ble Ashley Eden. Calcutta, 1864. 8. The last four are reprinted in ‘ Political Missions to Bootan.’ Calcutta, 1865. 9. Bootan, or the story of the Dooar war, by Surgeon Rennie, M.D. London, 1866. 10. Papers relating to Bootan presented to Parliament. No. 13 of 8th February, 1865. 11. Further papers relating to Bootan presented to Parliament. No. 47 of 15th February, 1865. 12. Visit to Dewangiri, by E. T. Dalton. J. A. S., Ben., XVIII., 66. 13. A Military report on the country of Bhutan, containing all the information of Military importance which has been collected up to 12tli July, 1866, by Lieut. C. M. Macgregor. Calcutta, 1873. (5)— Sikkim. 14. Himalayan Journals : notes of a naturalist in Bengal, the Sikkim and Nepal Himalayas, &c., by J. D. Hooker. London, 1855. 15. Notes, chiefly botanical, made on a journey from Darjeeling to Tonglo, by the same. J. A. S., Ben., XVIII., i., 419. 16. Notes on a tour in the Sikkim Himalayan mountains undertaken for the pur- pose of ascertaining the geological formation of Kinchinjanga. by W. S. Slierwill. Ibid, XXIL, 540, 611. OF THE NORTH-WESTERN PROVINCES. 47 17. Journal of a trip undertaken to explore the glaciers of the Kancliinjinga group, by Major J. L. Sherwill. Ibid, XXXI., 457. 18. Diary of a journey through Sikkim to the frontiers of Thibet, by A. Campbell. Ibid, XXL, 407, 477, 563. 19. A journal of a trip to the Sikkim, by the same. Ibid, XVIII., i , 482. 20. Routes from Darjiling to Tibet, by the same. Ibid, XVII., ii., 488. 21. Itinerary from Phari in Tibet to Lassa, with appended routes from Darjiling to Phari, by the same. Ibid, XVII., i., 257. 22. Notes on eastern Thibet, by the same. Ibid, XXIV., 252. 23. Report on a visit to Sikkim and the Tibetan frontier in 1873, by J. Ware- Edgar, C.S.l. Calcutta, 1874. 24. Sikkim, with hints on mountain and jungle warfare, exhibiting also the facili- ties for opening commercial relations through the hills of Sikkim with Central Asia, Tibet, and Western China, by Col. J. C. Gawler. London, 1873. 25. A short account of the Cooch Behar State, by Capt. T. H. Lewin. 26. The Indian Alps and how we crossed them. London, 1S76. 27. Note on the Mechis, together with a small vocabulary of the languarge, by Dr. A. Campbell. J. A. S., Ben., VIII., 623. 28. Note on the Lepchas of Sikkim, with a vocabulary of their language, by the same. Ibid, IX., 379. 29. A note on the Limboos and other hill tribes hitherto undescribed, by the same. Ibid, IX., 595. 30. On the literature and origin of certain hill tribes, by the same. Ibid, XI., 4. 31. Note on the Limboo alphabet of Sikkim, by the same. Ibid, XXIV., 202. 32. Ethnology of India, by Mr. Justice Campbell. Ibid, XXXV., 1. 33. Specimens of the languages of India, including tribes of Bengal, the Central Provinces, and the eastern frontier, by Sir G. Campbell. London, 1874. 34. A sketch of the modern languages of the East Indies, accompanied by two language maps, by R. N. Cust. London, 1878. 35. A comparative dictionary of the languages of India and High Asia, by W. W. Hunter. London, 1868. 36. A grammar of the Rong (Lepcha) language as it exists in the Dorjeling and Sikkim hills, by G. B. Mainwaring. Calcutta, 1876. (c) — N epal. 37. An account of the kingdom of Nepal, by Father Guiseppe. As. Res., II., 307. 38. An account of the kingdom of Nepal, being observations made during a mission to that country in the year 1793, by Colonel Kirkpatrick. London, 1811. 39. An account of the kingdom of Nepal and of the house of Gorklia, by Francis Hamilton (formerly Buchanan). Edinburgh, 1819. 40. Narrative of a five years’ residence at Nepal, from 1841 to 1845, by T. Smith. London, 1852. 41. A journal to Kathmandu with the camp of Jang Bahadoor, by Lawrence Oli pliant. London, 1852. 42. History of Nepal, translated from the Parbatiya by Munslii Shew Sliunker Singh and Pandit Sliri Gunanand and edited by D. Wright, M.D. Cam- bridge, 1877. 48 HIMALAYAN districts 43. Nepal : its people, religion, customs, zoology, botany, by Dr. Oldfield. London, 1879. 44. Memorandum relative to the seven Kosis of Nepal, by B. H. Hodgson. J. A. S., Ben., XVII., ii., 646. 45. Route from Kathmandu to Darjiling, by the same. Ibid, 634. 46. A cursory notice of Nayakot, by the same. Ibid, IX., 1114. 47. Selections from the records of the Government of Bengal, No. XXVIL 48. Quality of the Kosis of Nepal. J. A. S., Ben., V., 369. 49. Papers on the colonisation, commerce, geography, &c., of the Himalaya moun- tains and Nepal, by B, H. Hodgson. London, 1857. (/7) — Ethnology. 50. Notices of the languages, literature, and religion of Nepal and Thibet, by B. H. Hodgson. As. Res., XVI., 409. 51. On the aborigines of the Himalaya, by the same. J. A. S., Ben., XVI., 1235, and XVII., i., 73. 52. Origin and classification of the military tribes of Nepal, with a tabular view of the tribes, by the same. Ibid, II., 217* 53. On the Chepang and Kusunda tribes of Nepal, with a Chepang vocabulary, by the same. Ibid, XVII., ii, 650. 54. Cursory notice of Nayakot and the remarkable tribes inhabiting it, by the same. Ibid, IX., 1114. 55. On the tribes of northern Tibet, Horsok and Sifan, by the same. Ibid, XXIL, 121 . 56. On the colonisation of the Himalaya by Europeans. Sel. Rec. Ben., XXVII., p. 1. 57. On the commerce of Nepal. Ibid, p. ll. 58. The preceding seven papers have been reprinted in ‘ Essays on the languages, literature, and religion of Nepal and Tibet.’ London, 1874. 59. Classification of the Newars or aborigines of Nepal Proper, preceded by the most authoritative legend relative to the origin and early history of the race, by the same. J. A. S., Ben., III., 215. 60. Comparative vocabulary of the several languages and dialects of the eastern Sub-Himalaya from the Kali or Ghagra to the Dhansri, by the same, Ibid, XVI., 1244. 61. Ethnography and geography of the Sub-Himalayas, by the same, with a Khas vocabulary. Ibid, XVII., i., 544. 62. On the Tibetan type of mankind, by the same. Ibid, XVII., ii,, 222, 580. 63. A brief note on Indian Ethnology, by the same. Ibid, XVIII., 238, 64. On the aborigines of north-eastern India, by the same, with a comparative vocabulary of Tibetan written and spoken, Dhimal, Bodo and Garo. Ibid, 451. 65. On the origin, location, creed, customs, character and condition of the Kooch Bodo and Dhimal people, with a general description of the climate they dwell in, by the same. Ibid, 702. Reprinted with the preceding in the Aborigines of India. Calcutta, 1847. 66. On the aborigines of the eastern frontier with vocabularies of Burman written and spoken, Singpho, Naga, Abor-miri and Miri, by the same. J. A. S., Ben,, XVIII., 967. OF THE NORTH-WESTERN PROVINCES. 49 67. On the aborigines of southern India, by the same. Ibid, 350. 68. On the aborigines of Central India, by the same. Ibid, XVII., ii., 550. 69. On the aborigines of the north-eastern frontier, by the same. Ibid, XIX., 309. 70. Indo-Chinese bo-rderers and their connection with the Himalayans and Tibet- ans, by the same. Ibid, XXII., 1. 71. Caucasian and Mongolian affinities, by the same. Ibid, XXII,, 26. 72. Comparative vocabulary of the languages of the broken tribes of Nepal : [(1) Dahi or Darhai ; (2) Denwar; (3) Pahi or Pahari ; (4) Chepang ; {5) Bhramu ; (6) Vayu or Hayu ; (7) Kuswar ; (8) Kusunda ; (9) Pakhya (unbroken) ; (10) Thaksya (do.)'; (11) Tharu], and comparative vocabulary of the (seventeen) dialects of the Kiranti language, also a Vayu and a vocabulary and grammar, by the same. Ibid, XXVI., 317 '. XXVII., 393, 73. On the Vayu tribe, by the same. Ibid, XXVII., 443. 74. On the Kiranti tribe, by the same. Ibid, 446. 75. The Magar language of NepAl, by J. Beames. J. Ik A. S., IV., 1869. Note. — A rticles Nos. 44, 45, 62, 64 — 66, 68, 69, 70 — 74 above have been reprinted in Miscellaneous Essays relating to Indian subjects, by B. H. Hodgson, London, 1880. Section D. — Kali to the Satlaj, 1. Illustrations of the botany and other branches of the Natural History of the Himalayan mountains, by J. Forbes Royle. London, 1839. 2. Notes of an excursion to the Pindaree Glacier in 1846, by E. Madden. J. A. S., Ben., XVI., 226, 596 (chiefly botanical). -3. The Turaee and outer mountains of Kumaon, by the same. Ibid, XVII., 1., 349 : XVIII., i., 603 (chiefly botanical). 4. Description of the (so-called) mountain trout of Kumaun, by J. McClelland. Ibid, IV., 59. 5. Notes of observations on the Boksas, by Dr. J. L. Stewart. Ibid, XXXIV., 11., 147, 6. Ancient remains in the Garhwal Bhabar, by H. Pullan. Ibid, XXXVI., 155. 7. Narrative of a survey for the purpose of discovering the source of the Ganges, by Capt. F. V. Rapier. As. Res., XI., 446. 8. Pilgrim’s wanderings in the Himmala, by Barron. Agra, 1844. 9. Report on the Bhotia mahals of Kumaon, by G. Traill. J. A. S., Ben., II., 551. Reprinted in Kumaon Reports. 10. A. few notes on the subject of the „ Kumaon and Rohilkhand Tarai, by J. H. Batten. Ibid, XIII., 887. 11. Extract from the journal of J. Weller on a trip to the Bulcha and Oonta Dhoora passes, edited by the same. Ibid., XII., 78. 12. Journal of a visit to Melum and the Gonta Dhoora pass in Jawahir, by E. Masson, edited by the same. Ibid, XI., 1157. 13. Note of a visit to the Niti pass of the grand Himalayan chain, by the same. Ibid, VII., 310. 14. Notice of a trip to the Niti pass. Ibid, XIX., 79. 15. Account of a visit to the Bians pass. Gl. in Sci., I., 97. 7 50 HIMALAYAN DISTRICTS 16. Notes on a trip to the Kedamath and other parts of the snowy range of the Himalayas in 1853 (by J. M.) Edinburgh, 1856. 17. The Himalaya in Kumaon and Garhwal. Col. Rev., XVIII., 72. 18. Kumaon and its Hill stations. Ibid, XXVI., 373. 19. On the Physical geography of the Himalaya, by B. H. Hodgson. J. A. S., Ben., XVIII., ii., 761. 20. On the Physical geography of the provinces of Kumaon and Garhwal in the Himalaya mountains and of the adjoining parts of Tibet, by Capt. (now General) R. Strachey. J. E. G. S., XXI., 57 (1851). 21. Explanation of the elevation of places between Almora and Gangn, by Lieut. H. Strachey. J. A. S., Ben., XVII., ii., 527. 22. Narrative of a journey to Cho Lagan (Kakas Tal), Cho Mapan (Manasaro war) , and the valley of Pruang in Gnari Hundes, by the same. J. A. S., Ben., XVII., ii., 98, 127, 327. 23. A description of the glaciers of the Pindur and Kuphinee rivers in the Kumaon Himalaya, by the same. Ibid, XVI., 794, 1002. 24. Notice of Lieut. H. Strachey’ s scientific inquiries in Kumaon and Garhwal. Ibid, XIX,, 239. 25. Note' on the motion of the glacier of the Pindur in Kumaon, by Lieut. H, Strachey. Ibid, XVII., if., 203. 26. A Sketch of the mountains and river-basins of India, by Trelawny Saunders, India Office, London, 1870. 27. Trans-Himalayan missions- and their results. Cal. Rev., Jan, 1877, 115. 28. Geographical Magazine (London), IV., 113 (May, 1877), by C. R. Markham, on “ the Himalayan system,” and p. 173, by T. Saunders, on the same subject, being a reply to the preceding article in the Calcutta Review. 29. A memoir on the Indian Surveys, by C, R. Markham. London, 1878. 30. On the snow-line in the Himalaya, by Lieut. H. Strachey. J. A. S., Ben., XVIII., r., 287. 31. On the limits of perpetual snow, by Capt. J. D. Cunningham. Ibid, XVIII., ii., 694. 32. Remarks on the snow-line, by Capt. T. Hutton. Ibid, 954. 33. Reports on the trans-Himalayan explorations in connection with the Great Trigonometrical Survey of India, 1866-67, 1867, 1868, 1869, 1870, 1871, 1872, 1873-75, 1876, 1877, viz — (1.) Route-survey from Nepal to Lhasa, and thence to the sources of the Brahma- putra, made in 1865-66. As well as a route survey through western Nepal and from Niti to Gartokh and back. (2.) Route-survey from Manato Totling, thence to Demchok and along the northern branch of the Indus to Thok Jalung and back to Milam, in 1867. (3.) Surveys from Rudok by the gold fields to King-lo, and. thence to the Mana- sarowar lake ; from Manasarowar to Shigatze and from the Tadam Monas- tery to Muktinath in Nepal; also along the Tingri maidan in the eastern Himalaya, 1868. (4.) Smwey from Kabul to Badakshan and through the upper valley of the Oxus to Kashgar and back by the Karakoram, 1867-68. OF THE NORTH-WESTERN PROVINCES. 51 (5.) Survey from Peshawar to Fyzabad in Budakshna, 1870. (6.) Exploration of the Namcho or Tengri Nuf lake in Tibet, 1872, and Havildar’s journey from Kabul to Bukhara, 1872. (7.) Account of the survey operations in eastern Turkistan, 1873-74, in connection with the Yarkand Mission, by Oapt. H. Trotter, E.E. (8.) Survey from Badakshan to Kolab, Darwaz, and Kubadian to Balakli in 1873. (9.) Journey from Jalalabad to Sarhadd-i-Wakhan by the Baroghil pass in 1873. (10.) Journey from Leh in Ladakh to Lhasa, and thence by Chetang to Odalguri near Tezpur in Asam, July 1873 to March, 1875. (11.) Indus river from Amb to Bunji ; Yassin to Mastuj and thence toBarkulti ; Sar Laspur to Dodbah near Dir; Mianlcalai to Pachat near New Kunar by Nawagi and Nawagi to Abazai in 1876. (12.) Mr. E. C. Ryall’s exploration of Hundes to the north of Kumaon and Garhwal, 1877. Account of the operations of the G. T. S., India, Yol. I. (1870), II. to IV. (1879), Dehra Diin, 1879. Section E. — Satlaj to the Indus, 1 . Journal of a tour through part of the snowy range of the Himalaya mourn tains and to the sources of the rivers Jumna and Ganges, by J. B. Fraser, London, 1820. 2. Travels in the Himalayan provinces of Hindustan and the Panjab ; in Ladakh and Kashmir ; in Peshawar, Kabul Kunduz and Bokhara, by W, Moorcroft and G. Trebeck, from 1819 to 1825, edited by H. H. Wilson. London, 1841, 3. Account of Koonawar in the Himalayas, by Capt. A. Gerard. London. 1841. 4. Notes on Moorcroft’s travels in Ladakh and on Gerard’s account of Koonawur, by Capt. J. D. Cunningham. J. A, S., Ben., XIII., 172, 223. 5. Journal of a trip through Kulu and Lahul to the Chumureri lake in Ladakh in 1846, by Capt. A. Cunningham. Ibid, XVII., i., 201. 6. Kashmir and das Reich der Siek, by C, Von Hugel, translated into English by Major Jervis. London, 1845. 7. Notes of a visit to the valley of Kashmir in 1836, by Baron Hugel. J. A. S., Ben., V., 184, 303. 8. Travels in Kashmir, Ladakh, Iskardo, the countries adjoining the mountain course of the Indus, &c,, by G. J. Vigne. London, 1842, 9. Notice by Vigne of his travels in Kashmir. J. A. S., Ben,, V,, 56. Description of the valley of Kashmir, Ghazni and Kabul, by G. J. Vigne. Ibid , VI., 766. 10. Ladakh, physical, statistical, and historical, with notices of the surrounding countries, by Major A, Cunningham. London, 1854, 11. Abstract journal of the routes to the sources of the Panjab rivers, by the same and A. Broome. J. A. S, Ben., X,, 105, 12. Correspondence of the Commissioners deputed to the Tibetan frontier, by Captain A. Cunningham. Ibid, XVII., i., 89. 13. Memorandum on the boundary between the territories of Maharaja Gulab Singh and British India as determined by the Commissioners, by J. D, Cunningham. .Ibid, XVII,, i., 295. 52 HIMALAYAN districts 14. Memorandum on the district of Bussahir and the pacification of the disaffect- ed portion of the inhabitants, by G. C. Barnes. Lahore, 1859. 15. Journal of a tour through Hungrung, Kunawur and Spiti in 1838, by T. Hutton. Ibid, VIII., 901 : IX., 489, 555. 16. Journal of a trip to the Burenda pass, by the same. Ibid, VI., 901. 17. Diary of an excursion to the Boorun and Shatool passes over the Himalaya, by E. Madden. Ibid, XV., 79. 18. Journey from Soobathoo to Shipke in Chinese Tartary, by J. G. Gerard. Ibid, XL, 363. 19. Report on the valley of Spiti, by the same. Ibid, X., 198 ; and by W. C. Hay. Ibid, XIX., 429 ; see also As. Res., XVIII., 239. 20. Notes of a trip from Simla to the Spiti valley and Chomoriri lake in 1861, by W. Theobald. Ibid, XXXI., 480. 21. Illustrations of ancient buildings in Kashmir, by H. H. Cole. London, 1869. 22. Kashmir, the Western Himalaya, and the Afghan mountains, by Dr. A. M. Verchere. J. A. S., Ben., XXXV., ii., 89, 159. 23. Western Himalaya and Thibet : a narrative of a journey through the mountains of northern India during the years 1847-48, by T. Thomson, M.D. London, 1852. 24. Voyage dans l’lnde, by V. Jacquemont. Paris, 1841. 25. Letters from India, describing a journey in the British dominions of India, Tibet, Lahore, and Cashmere during 1828-31, by the same. London, 1834. 26. Notes taken in 1829 relative to the territory and the Government of Iskardo, by C. M. Wade. J. A. S., Ben., IV., 589. 27. Notes on Iskardo, by Vigne. Ibid, V., 56, 308 : VI., 773. 28. The abode of snow : observations on a journey from Chinese Tibet to the Indian Caucasus, through the upper valleys of the Himalaya, by A. Wilson, Edinburgh, 1876. 29. The Jummoo and Kashmir territories : a geographical account, by F. Drew. London, 1875. 30. The northern barrier of India, a popular account of the Jummoo and Kashmir territories, by F. Drew. London, 1877. 31. A Gazetteer of Kashmir and the adjacent districts of Kishtwar, Bhadrawar, Jamu, Naoshera, Ptlnch, and the valley of the Kishenganga, by Capt. E. Bates, B.S.C. Calcutta, 1873. 32. Handbook to Kashmir, by Dr. Ince. Calcutta, 1868. 33. Recollections of India, by the Hon. C. H. Hardinge. London, 1847. 34. Vazeeri Rupi, the silver country of the Vazeers in Kulu, by J. Calvert. London, 1873, 35. The Himalayan districts of Kooloo, Lahoul, and Spiti, by Capt. A. F. Har- court. Lahore, 1874, 36. Hunting in the Himalaya, by R, H. Dunlop. London, 1860. 37. Large game shooting, Thibet and the North-West, by A. Kinloch. London, 1876. 38. The large and small game of Bengal and the North-Western Provinces of India, by S. J, Baldwin. London, 1876. 39. From the Hebrides to the Himalayas, by 0. F. G. Cumming. London, 1876, OF THE NORTH-WESTERN PROVINCES. 53 40. A grammar and vocabulary of the Kashmiri language, by M. P. Edgworthj J. A. S., Ben., X., 1038 41. A grammar of the Kashmiri language, by R. Leach. Ibid , XIII., 397, 553. 42. Kashmiri vocabulary and grammatical forms, by L. Bowring. Ibid, XXXV., ii., 225. 43. A vocabulary of English, Balti and Kashmiri, by Capt. H. H. Godwin Austen. Ibid , XXXV., i., 223. 44. A vocabulary of the Kashmiri language, by Dr. W. J. Elmslie. London, 1872. 45. Kashmiri test-words, by the Same. J. A. S., Ben., XXXIX., 95. 46. A vocabulary of the Koonawar language, by A. Gerard. Ibid , XI., 479. 47. Manners and custom of the Dards, by G. W. Leitnef. Ind. Ant., I., 7, 84, 187. 48. The languages and races of Dardiston, by the same. Lahore, 1877. Section F.— Afghanistan, ( a ) — Baluchistan. 1. Notes taken on a tour through part of Baluchistan in 1838-39 by Haji Abdun Nabi of Kabul, edited by R. Leech. J. A. S,, Ben., XIII., 667, 786. 2. Some account of a journey from Kurrachee to Hinglaj in the Lus territory, descriptive of the intermediate country and of the port of Sonmeanee, by N. Hart. Ibid, IX., 134. 3. Map of the route to Hinglaj, by the same. Ibid, IX., 615. 4. Journeys in Balochistan, Afghanistan, the Panjab, and Kalat, by C. Masson. London, 1844. 5. Caravan journeys and wanderings in Persia, Afghanistan, Turkistan, and Baluchistan, by J. P. Ferrier. London, 1856. 6. Travels in Belochistan and Scinde, by H. Pottinger. London, 1816. 7. Central Asia, Part III., Balochistan, by Col. MacGregor. Calcutta, 1875. 8. The country of Balochistan, by A. W. Hughes. London, 1877, 9. Gazetteer of Sind, by the same. London, 1874. 10. Report on the country between Kurrachee, Tatta, and Sehwan Scinde, by E. P. de La Hoste. J. A. S., Ben., IX,, 907. 11. Brief history of Kalat, brought down to the deposition and death of Mehrab Khan Brahoee, by R, Leech. Ibid, XII., 473. 12. Memorandum on the Beloch tribes in the Dera Ghazi Khan district, by Capt. Minchin. Lahore, 1869. 13. Sindh and the races that inhabit the Indus valley, by R. Burton. London, 1851. Corespondence relative to Sinde, 1836-43, presented to both houses of Parliament by Her Majesty’s command. Calcutta, 1844. 14. Note on the Brahooes, by N. Hart. Ibid, X., 136. 15. General notice of the tribes of Kujjukzyes, by the same. Ibid, IX,, 1214. 16. Report on Upper Sindh and the eastern portion of Cutchee, with a memo- randum on the Beloochee and other tribes of Upper Sindh and Cutchee, by J. Postans. Ibid, XII., 123. 17. Vocabulary of the Scind language, by J. B. Eastwick. Bombay, 1843, and J. A. S,, Ben,, XII., 1. 54 HIMA'LAYAN DISTRICTS. 18. Sindlii and English dictionary, by G-. Stack. Bombay, 1855. 19. Sindlii reading-book, by Dr. E. Trumpp. London, 1858. 20. Grammar of the Sindlii language, by the same. London, 1872. 21 . Grammar of the Sindlii language, by W. H. Wathen. J . A. S., Ben., VI., 347. 22. Epitome of the grammars of the Brahnilty, the Balochky, and the Panjabi languages, with vocabularies of the Baraky, the Pashi, the Laghmani, the Cashgari, the Teerhoi, and the Deer dialects, by Lieut. R. Leech. Ibid, VII., 538, 608, 711, 780. 23. A Balochee grammar, by E. Mockler. London, 1877. (5) — Western frontier. 24 Narrative of a journey into Khorasan and the countries noith-east of Peisia in 1821-22, by J. B. Fraser. London, 1825. 25. Extracts from a demi-official report on a mission into Khorasan, by A. Conolly. J. A. S., Ben., X., 116, 718. 26. Ibn Haukul’s account of Khorasan, by W. Anderson. Ibid, XXII., 162. 27. A description of the country of Seistan, by R. Leech. Ibid, XIII., 115. 28. Sketch of the physical geography of Seistan, by A. Conolly. Ibid, IX., 710. 29. Journal kept whilst travelling in Seistan, by the same. Ibid, X., 319. 30. Narrative of a journey from Heraut to Khiva, by Capt. J. Abbot. London, 1843. 31. Central Asia, Part IV., Persia, by Col. MacGregor. Calcutta, 1871. 32. Narrative of a journey through the Province of Khorasan and on the north- western frontier of Afghanistan in 1875, by Col. C. M. MacGregor. London, 1879. 33. From the Indus to the Tigris : a narrative of a journey through the countries of Baluchistan, Afghanistan, Khorasan, and Iran in 1872 : together with a synoptical grammar and vocabulary of the Brahoe language, by H. W. Bellew. London, 1874. 34. Clouds in the east : travels and adventures on the Perso-Turkoman frontier, by V. Baker. London, 1876. 35. Journey on the Turkoman frontier of Persia, by G. Napier. P. R.G. S., XX., 3. 36. Eastern Persia : an account of the journeys of the Persian boundary com- mission, 1872. London, 1876. 37. The sixth great oriental monarchy, or the geography, history, and antiquities of Parthia, by Professor Rawlinson. London, 1876. 38. The seventh great oriental monarchy, or a history of the Sassanians or new Persian Empire, with notices, geographical and antiquarian, by the same. London, 1876. 39. Persia, from the earliest period to the Arab conquest, by W. S. W. Vaux. London, 1876. (c) — A fghanistan. 40. Journey from Bengal to England through Kashmir, Afghanistan, and Persia into Russia, by G. Forster. London, 1798. 41. Account of the kingdom of Cabul, comprising a history of the Afghan nation, by M. Elphinstone. London, 1818. 42. Account of the kingdom of Cabul and its dependencies in Persia, Tartary, and India: a view of the Afghan nation and history of the Dooraunee monarchy, by the same. London, 1842, OF THE NORTH-WESTERN PROVINCES. 55 43. Narrative of a visit to Ghazni, Kabul, and Afghanistan, by G. Vigne. Lon- don, 1840. 44. Journey to and residence in Cabul, by A. Barnes. London, 1842. 45. Journey to the north of India overland from England, by A. Conolly. London, 1834. 46. Ariana Antiqua : a descriptive account of the antiquities and coins of Afghanistan, with a memoir on the buildings called topes, by C. Masson, by H. H. Wilson. London, 1841. 47. Ancient geography of India : Buddhist period, by A. Cunningham. London, 1871. 48. Memoirs of Zehir-ed-in Muhammad Baber, written by himself in Jaghatai Turki, translated from the Persian version by Leyden and Erskine. Lon- don, 1826. 49. Geographical notice of the valley of Jalalabad, by G. H. MacGregor. J. A. S., Ben., XI., 117. 50. Notice of Jalalabad, by J. G. Gerard. Ibid, III., 325. 51. Journal of a political mission to Afghanistan in 1857, by Dr. Bellew. London, 1862. 52. On the highland region adjacent to the trans-Indus frontier of India, by Col. J. T. Walker. R. G. S. J., XXXII., 316. 53. Central Asia, Part II., Afghanistan, by Col. MacGregor. Calcutta, 1875. 54. Survey operations of the Afghanistan expedition, the Kurram valley, by Capt. G. Martin. P. R. G. S., I., 617, N. S. 55. Afghan geography, by C. R. Markham. P. R. G. S., XX., 4, 1876. 56. Mountain passes on the Afghan frontier, by the same. Ibid, I., 38, N. S. 57. The upper basin of the Cabul river, by the same. Ibid, 110. 58. The basin of the Helmund, by the same. Ibid, 191. 59. The mountain passes leading to the valley of Bamian, by Lieut.-Col. Kaye, Ibid, 244. 80. March and operations of the army of the Indus to Afghanistan in 1838-39, by Major W. Hough. London, 1841. 81. British operations at Kabul in 1841-42, by the same. London, 1849. 82. Campaign in Sinde and Afghanistan, by Col. Outram. London, 1840. 63. Narrative of the campaign of the army of the Indus, in Scind, and Cabul in 1838-39, by R. H. Kennedy. London, 1840. 64. Diary of a march through Sinde and Afghanistan, by Rev. J. N. Allen. London, 1843. 65. Sale’s brigade in Afghanistan, by Rev. G. R. Gleig. London, 1846. 66. The Sikhs and Afghans immediately before and after the death of Ranjit Singh, from the journal of an expedition to Cabul through the Pan jab and the Khaibar Pass, by Shahamat Ali. Calcutta, 1847. 67. History of the war in Afghanistan, by J. W. Kaye. London, 1851. 68. Reminiscences of forty-three years in India, by Lieut.-Genl. Sir. G. Law- rence. London 1874. 69. A retrospect of the Afghan war, with reference to passing events in Central Asia, by Sir V. Eyre. London, 1869. The Panjab and North-Western frontier of India, by Major-Genl. H, Coxe, London, 1878. 70 . 56 HIMALAYAN DISTRICTS 71. General Gilbert’s raid to the Khaibar, by R. W. Bingham. London, 1850, 72. History of Afghanistan from the earlier period to the outbreak of the war in 1878, by Col. Malleson. London, 1879. 73. Journal of a tour through part of the Panjab and Afghanistan in the year 1837, by Agha Abbass of Shiraz, edited by R. Leech. J. A. S., Ben., XII., 561. 71, Account of parts of the Cabul and Peshawar territories, by the same. Ibid, XIV., 660. 75. Reports by B times, Lord, and Wood, political, geographical, and commercial, on Scinde and Afghanistan. Calcutta, 1839. 76. Memoir on the climate, soil, produce, and husbandly of Afghanistan, by Lieut, Irwin. J. A. S. Ben., VIII., 715, 779, 869, 1005 : IX., 33, 189. 77. Extracts from a report on subjects connected with Afghanistan, by W, Griffiths. Ibid, X., 977. 78. Notes on the geography of Western Afghanistan, by W. Anderson. Ibid, XVIII., i., 553. 79. Verification of the itinerary of Hwen Thsang through Afghanistan and India, by Capt. A. Cunningham. Ibid, XVII., i., 176, and ii., 13. 80. Route from Dera Ghazi Khan through the Veziri country to Kabul, by M. Honigberger. Ibid, III., 175. 81 . Route from Dera Ghazi Khan to Kandahar through the Sakhi Sarwar and Bozdar passes, with other routes, by R. Leech. Ibid, XIII., 527. 82. Diary of a trip to Pind Dadan Khan, &c., by A. Fleming. Ibid, XVI., I., 661, 83. Account of Ghazni. Ibid, VI., 775. 81. Itinerary from Yezd to Herat (official). XIII,, 827. 85. Route from Kandahar to Herat (official). XIII., 121. 86. Report of a journey by Candahar, Kabul, and the Panjab from Herat to Simla, by Major Todd. XIII., 339. 87. Description of Herat, by Mohan Lai, III., 9. 88. Central Asia, Part I., our north-western frontier, by Col. MacGregor. Cal- cutta, 1871. 89. Bannu, or our Afghan frontier, by S. Thorbum. London, 1876. 90. Notes on the Bunnoo district, by Major H. B. Urmston. Lahore, 1869. {( I ) — Languages. 91. Dictionary of the Panjabi language, prepared by a Committee of the Lodiaaaa Mission. Lodiana, 1 851. 92. Pukhto-English dictionary, by H. G, Raverty. London, 1860. 93. Grammar of the Pukhto or Pushto language, by the same. London, 1869, 91. Grammar of the Pashto, or language of the Afghans, by Dr. E. Trumpp. London. 95. Dictionary of the Pukkhto or Pukshto language, by H. W. Bellew. London, 1867. 96. Grammar of the Pukkhto language, by the same. 97. Grammar of the Pushtoo or Afghani language, by R.. Leech. J. A S., Ben., VIII., i. : XXIII., 550. 98. Is the Pushto a Semitic language ? by Rev. I. Loewenthal. Ibid , XXIX., 323. 99. Some remarks on the origin of the Afghan people and dialect, by II, G, Raverty. Ibid, XXIII. 550, OF THE NORTH-WESTERN PROVINCES. 57 100. Translation of the Pukhto text-book, Kalid-i- Afghani, by T. C. Plowden. Lahore, 1875. 101. Notes on the Eusofzye tribes of Afghanistan, by E. Conolly. Ibid, IN., 924 : XVII., i., 624. 102. Report on the Yoosoofzaie district, by Lieut. H. P>. Lumsden. Sel. Rec. Panj., L, 5, 1853. And Covert, J. A. S., Ben., V., 481. 103. An account of the early Ghiljaees, by R. Leech. Ibid, XIV., 306. 104. An account of the early Abdalees, by the same. Ibid , XIV., 445. 105. An account of the Hazarehs, by the same. Ibid, XIV., 393. 106. Account of Roh in Derajat, by H. G-. Raverty. 7 bid, XXVI., 177. 107. The district of Dera Ismail Khan, by T. W. Tolbort. Ibid, XL., 1. 108. History of the Gakkhars, by J. G. Delmerick. Ibid, XL., 67. 109. Rough notes on the Khutuks of the Teree country and Khurali below Atok, by Lieut. F. H. Pollock. Lahore, 1850. 110. Report on the eastern Khutuks, by Lieut. H. Lumsden. Ibid, 1851. 111. The lower Derajat frontier, by Capt. G. 0. Jacob. Ibid, 1854. 112. Kohistan of the Jullundhur Doab, by Lieut. Parish. J. A. S., Ben., XVII., i., 281 : XVIII., !., 360. 1T3. The Syads of Tira and their quarrels with the Sunis, by Capt. P. Cavagnari of Kohat. Lahore, 1875. 114. Notes on the Dera Ghazi Khan district and its border tribes, by R. Bruce. Lahore, 1871. 115. Memorandum on the Dera Ghazi Khan district. Sel. Rec. Panj,, IV., 4, 1860. 0)— Kohistan. 116. An account of upper and lower Suwat. and the Kohistan to the source of the Suwat river and of the tribes inhabiting those valleys, by Capt. H. G. Raverty. J. A. S., Ben., XXXI., 227. 1 1 7. An account of upper Kashkar and Chitral or lower Kashkar, together with the independent Afghan State of Panjkorah, including Talash, by the same. Ibid, XXXIII., 125. 118. An account of the Panjkora valley and upper and lower Kaslikara, by Rajah Khan of Cabul, edited by R. Leech. Ibid, XIV., 812. 1 1 9. Some account of a visit to the plain of Koh-i-Daman, the district of Ghorband, and the pass of Hindu -kusli, by P. B. Lord. Ibid, VII., 521. 120. On the Siah-posh Kaffirs, with specimens of their language and costume, by Capt. A. Burnes. J. A. S., Ben., VII., 325. 121. Information regarding the Siah-posh --tribe, by A. Burnes Ibid II 305. ‘ ’ ■’ 122. Further information regarding the same, by Mohan Lall Ibid III 76. 123. On the language of the Siah-posh Kafirs, with -a short list of words, to which are aided specimens of Kohistani and other dialects spoken on the northern borders of Afghanistan, by H. G. Raverty. Ibid, XXIII, 267. 124. Notes on Kafiristan, by the same. Ibid, XXVIIL, 317. 125. On the language of the so-called Kafirs of the Indian Caucasus, by Dr. Trumpp. J, R, a. Soc., XIX. 8 58 HIMALAYAN districts 1 . 2 . 3. 4. 5. 6 . 7. 8 . 10 . 31. 12 . 13. 14. 15. 16. 17. 18 . 19. 20 . 21 . 22 . 23. 24. 25 26. 27 . Section Pamir and Turkistan, Memorandum on routes from the Punjab to eastern Turkistan, by T. D. Forsyth. Lahore, 1868. Report on the route to the Karakash valley and pass, by Dr. H. Caley. Ibid. Results of a scientific mission to India and High Asia, by H. A. and R. von Schlagentweit. Leipzig, 1861-66. Route-book of the western parts of the Himalaya, Tibet and Central Asia, by the same. Leipzig, 1863. Lahore to Yarkand, by G. Henderson and A. Hume London, 1872. Visits to High Tartary, Yarkand and Kasligarh, by R. Shaw. London, 18< ( . The Roof of the world, being the narrative of a journey over the high pla- teau of Tibet to the Russian frontier and the Oxus sources on Pamir, by Lieut. -Col. T. E. Gordon, C.S.I. Edinburgh, 1876. Kashmir and Kashgarh, a narrative of the journey of the embassy to Kasligarh in 1873-74, by H. W. Bellew, C.S.I. London, 1875. Report of the mission to Yarkand in 1873 under command of Sii 1. D. Forsyth. Calcutta, 1875. Account of the survey operations in E. Turkistan, 1873-74. by Capt. H, Trotter. Calcutta, 1875. A sketch of the Turki language as spoken in E. Turkistan, by R. B. Shaw. Lahore, 1875. Les confins Anglo-Russes dans l’Asie Centrale : Etude historique, geogra- phique, politique, et militaire Mr la Kacligarie (E. Turkistan), by Capt, Kouropatkine. Translated by G. LeMarchand. Paris, 1849. Benoit de Goes, missionaire voyageur, 1603-07 (in E. Turkistan), by J, Brucker. Lyons, 1879. Route from Peshawar to Bokhara, by Dr. Gerard and Lieut. A. Bumes. J. A, S., Ben., I., 139 : II., i., 143, 224. Memoir on the Usbelc State of Kokan, called Khokend (the ancient Ferghana), by W. H. Wathen. Ibid, III., 369. Memoir on Chinese Tartary and Khoten, by the same. Ibid, IV., 6:>3. Notes on the manners and habits of the Turkoman tribes, with some geogia- pliical notices, by E. Stirling. Ibid, X., 290. Russian geographical operations in Asia, by Col. J. T. Walker. Ibid , XXXI < 7, Note on Central Asia, lb'ul, XXXIV., 113. Central Asia, by T. Hutton. London, 1874. Central Asia and the Anglo-Russian frontier, by A. Vambery. London, 1874, History of Bokhara, by the same. London, 1873. Asie Centrale, recherches, by A. von Humboldt. Paris, 1843. Travels into Bokhara, journey from India to Kabul, Tartary, and Persia, and voyage on the Indus, by A. Burnes. London, 1834. Diplomatic transactions in Central Asia, 1834-38, by J. Urquhart. London, 1841. Journey to the source of the Oxus by the route of the Indus, Kabul and Badakshan, by J. Wood. London, 1841. New edition, London, 1872. Narrative of a mission to Bokhara in the years 1843-45 to ascertain the fate of Col. Stoddart and Capt. Conolly, by Dr. J. Wolff. London, 1846. OF THE NORTH-WESTERN PROVINCES. 59 28. Httaoire sur la partie mdridionale cle I Asie Centrale, by N. de Khanik of. Paris, 1861. 29. Notes of a journey in Russian Turkistan, Khokand, Bokhara and Kuldja, by E. Schuyler. London, 1876. 30. Campaigning on the Oxns and the fall of Khiva, by J. A. MacGahan. London, 1876. Section H. — Tibet. 1. Geographical notice of Tibet, by Csoma de Koros. J. A. S., Ben. I., 121. 2. The physical geography of Western Tibet, by Capt. H. Strachey. London, 1854, and J. R. G. S. XXIII., 2. 3. Thibet nacli den resultaten geographischer forschungen friilierer und neuester zeit, by K. Ganzenmuller. Stuttgart, 1877. 4. Tibet, Tartary and Mongolia, by H. T. Prinsep. London, 1851. 5. Explorations in Western Tibet by the Trans- Himalayan parties of the G. T. S. P. R. G. S., 444, 1879. 6. Historic generate des Huns, des Turcs, des Mongols et des autres Tartares occidentaux, by Des Guignes. Paris, 1756-58. ' 1 . History of the Mongols, by II. H. Howorth. London, 1876. 8*. History of tlie Genghizan, the Great, first Emperor of the ancient Moguls and Tartars, by Petis de la Croix, translated into English. Calcutta, 1819. 9. The book of Ser Marco Polo, concerning the kingdoms and marvels of the east, edited by Col. Yule. London, 1875. 10. Cathay and the way thither, by the same. London. 11. Recueil de Turkestan : comprenant des lives et des articles sur 1 Asie Cen- trale en general et la province du Turkistan en particulier, by V. J. Mejovv. St. Petersburg, 1878. 12. Notices of the mediaeval geography of Central and Western Asia, by E. 13. 14. 15. 16. 17 . 18. 19. 20 . 21 . Bretschneider. London. Notes on Chinese mediaeval travellers to- the west, by the same. Itineraire de Marco Polo a travel’s la region du Pamir au XIIIc siecle, by J. B. Paquier. Paris, 1876. Le Pamir : etude de geograpliie physique et historique sur l’Asic Centrale, by the same. Paris, 1876. The Russians in Central Asia, their relations with Khiva, Bokhara and Kokand, descriptions of Chinese Turkistan and Dzungaria from the Russian’ of Valikhanoff, &c-.,by Messrs. Michell. London, 1865. Lc Kohistan, le Ferghanah et Kouldja, avec an appendice sur la Kachgane, by C. E. de Ujfalvy de Meso-Kovesd. Paris, 1S78. Le Syr-Daria, Le Zerafchane, les pays des sept-rivieres et la Sibene-occiden- tale, by the same. Paris, 1879. Resultats anthropologies d’un voyage en Asie Centrale, communiques au Congres anthropologique de Moscou, by the same. Pans, 1880. Die Russen in Central Asien, by Fr. von Hellwald. Augsburg, 1877. Pevtsoli’s expedition in North-Western Mongolia, by E. D. Morgan. P. R. G. S. , 701, 1879. 60 HIMA'LAYAN DISTRICTS OF THE N.-W. PROVINCES. 22. The Russians on the Amur, by E. G. Ravenstein. London, 1861. 23. England and Russia in the East : a series of papers on the political and geo- graphical condition of Central Asia, by Major-General Sir Henry Rawlin- son. London, 1875. 24. Mongolia, the Tangut country and the solitudes of Northern Tibet ; being a narrative of three years’ travel in eastern High Asia, by Lieut.-Col. N. Prejevalsky. London, 1876. 25. From Kulja across the Tian-Shan to Lob Nor, by the same. London, 1871). 26. The river of Golden Sand, the narrative of a journey through China and eastern Tibet to Burmah, by Captain W. Gill, R. E. ; with an introductory essay by Colonel H Yule, R. E,, London, 1S80. Physical Geography of the Himalaya. CONTENTS. The Himalayan river basins— The Indus basin— Subordinate systems of the Indus basin ; The Ganges basin— Subordinate systems of the Ganges basin ; The Brahmaputra basin— Subordinate systems of the Brahmaputra basin ; Systems of Tibet— Lob-Nor basin ; Oxus basin. Plains of Hindustan— Indus plain ; Indian desert ; Gangetic plain ; Asam valley ; Bhabar ; Tarai ; Siw&liks ; Duns. Extent of Bhabar Cause of the deposit — Hodgson’s oceanic theory ; Fluviatile theory ; Tarai ; Siwaliks ; Duns ; Ganges to Brahmaputra ; Lower Himalaya. Materials of the mountains— Eocene period ; Mode of mountain formation ; Mountain- sculpture ; Ice-wedges ; Avalanches ; Glaciers ; Rain ; Rivers. The Himalaya. We have already decided to restrict our use of the word ‘ Himalaya ’ to that portion of the great mountain girdle which lies between the bend of the Indus on the west and the unexplored gorge of the Brahma- putra on the east. Hodgson, in 1849, estimated the length of this range at 1,800 miles with a mean breadth of about 90 miles, a maxi- mum breadth of 110 miles, and a minimum breadth of about 70 miles. In fixing the breadth of the Himalaya, however, as in determining its length, we have similar difficulties to contend with. For, as we have seen that the popular estimate as to the boundaries of the range may possibly be correctly extended both on the east and on the west, so on the north, the channels of the Indus and the Brahmaputra, which are commonly assigned as the northern limit, are found in a plateau, but little lower than the passes by which the traveller crosses the first line of snowy mountains into Tibet. • On the south, we have a well-marked descent to the plains of India, but on the north there is no immediate descent to a fevfer country beyond. On the contrary, range after range is met with to the north, many of which may compete in altitude with the snowy mountains seen from the plains of northern India. Before proceeding to a closer examination of the form of that River-basins. portion of the Himalaya lying within the province of Jvumaon, it will be convenient o ^ descube tlie river-basins throughout the Himalaya and 62 HIMALAYAN DISTRICTS endeavour to trace the general law underlying their arrangement. For as this depends in the main on the direction of the great ranges and the position of the great peaks, a consideration of it will conduce to a clearer apprehension of the entire mountain system itself as well as of the relations of its various parts. We find that from a water-parting about longitude 81° east and almost imme- diately due north of Kumaon, the drainage of the southern part of the Tibetan plateau flows north-west in the Indus and south-east in the Brahmaputra. These two rivers maintain a course along the length of the table-land, and receive as they proceed the drainage of a large part of its breadth ; the exceptions being, first, the eastern border, which apparently is drained by the Lu-tse, the Lan-tsang, and the Murui-ussu, one of the sources of the Yang-tse-kiang J second, an occasional strip along the southern edge from which the water passes. off 2 more or less directly to the south through the Himalaya ; and third, the north-western part from which the water has no escape, but is collected in lakes at the lowest level it can reach. 3 The waters thus accumulated in the two great streams are at length discharged by two openings in the Himalayan slope through the plains of India into the Indian Ocean. No great portion of the drainage of the table-land, so far as we know, passes in the opposite direction through the northern slope, and the area that dischaiges itself southward at points intermediate between the debouches of the Indus and the Brahmaputra is with one exception, that of the’ Satlaj, comparatively small. The waters of the northern slope with a small area of the table-land adjoining flow down to the plains of eastern Turkistan : while, in like manner, those of the southern slope -with the drainage of the exceptional area along the southern border of the table-land which passes through the line of water-parting from the north, give rise to such rivers as the Jhilam, Clnnab, Ravi, Jumna, •From Prejevalsky’s Mongolia (London, 1876) it would appear that his Burkhan Buddha range marks, in 96° longitude, the north-eastern termination of the Tibetan plateau. This range forms the southern boundary of the Isaidarn plain, which, according to native report, extends thence to Lob-Nor. The Nomokhun-gol, which rises on the southern face of the Burkhan Buddha range and joins the Baian- gol, does not appear to be a feeder of the Hoang-lio or Yellow River which has its origin outside the Tibetan plateau. To the south of the Burkhan Buddha range the elevation is from 13,000 to 15,000 as far as the Murui-ussu, the bed of which where seen by Preievalsky -was 13,000 feet above the level of sea with a channel 7o0 feet broad in January. The name ‘Murui-ussu’ signifies ‘ the tortuous river ’ and according to Yule, it is the Bri-chu of the Tibetans, the Bmis of Marco Polo, and the Yang-tse-kiang or Blue River of the Chinese. _ ~ By the Satlaj, Karnali, and A run. 3 Examples of river-systems without an outlet to the ocea^i are to be found in the basins of the Caspian, Aral, Balkhash, Lob-Noi, &c, OF THE NORTH-WESTERN PROVINCES. 03 Ganges, Kali, Gandak, Kosi, and Tista. We thus see that the northern crest of the table-land or the summit of its northern slope practically forms the water-parting between the rivers that flow southwards and those that lose themselves in the plain of Gobi, In the southern crest we have a subordinate water-parting separating the rivers that fall into the Indian Ocean into two classes ; first, those that rise on that slope and flow directly down it to the plains of Hindustan ; and secondly, those that are collected along the table-land and are finally discharged also through the southern slope, chiefly by two concentrated channels at distant points towards the ends of the range. Captain Henry Stracliey 1 has called the northern crest of the table-land the Turkish, and the southern the Indian water- parting. If we examine the river-systems having their source in the Himalaya, we find a regularity of plan and arrangement which at first sight would not be expected. Taking the Indus basin and its system, we see that the Satlaj and all the rivers that join the Indus on its left bank have a south-westerly direction towards the Arabian Sea. On the east this system is bounded by the small inland basin of the Kaggar, which receives the drainage from an inconsiderable portion of the outer hills between the Satlaj and the Jumna, and finally loses its waters in the Indian desert. The eastern water-parting of the Indus system is found in the elevated range extending from the main Himalayan mass along the left bank of the Satlaj to Rtipur, and is continued thence in the uplands hordering the khadir of that river until it meets the Arvali (Aravali) range which constitutes the north-western abutment of the table-land of Central India. The character of the slope towards the south-west will be best understood from the following table of heights taken along the course of the Satlaj to Ludhiana, and thence by The Grand Trunk Road to the Jumna : — Tara, about two miles below the junction of the Panjnad and Indus, 337 feet above the level of the sea ; Bahawalpur, 375 feet ; Nur Shah, 481 feet ; Pir Ivhalis, seven miles north-east of Bahawalgarli, 548 feet ; Fazilka, 588 feet ; Firozpur cantonment, 645 feet ; Jagraon, 765 feet ; Ludhiana, 806 feet ; Amballa Church, 899 feet; and Madalpur, on the banks of the Jumna khadir, 906 ij. R. Ct. S., XXIII., p. 7. htmXlayan districts G4 feet. From Sodiwala in the Firozpnr district southwards on the 75th meridian we have Sodiwala, 718 feet; Ahmad wala, 705 feet ; Sirsa, on a mound, 737 feet ; level of Sambhar lake, 1,184 feet. 1 These observations show a slight depression towards the south in addition to that towards the south-west, and would make us include the Kaggar inland basin in the Indus system. The Sotra or Hakra, the ancient river of the Indian desert, seems, however, to have once had its debouche in the Kan of Kachh, 2 and would therefore be still entitled to be considered separate. To the west the Ravi and the Chmab run in lines almost parallel to the Satlaj, as well as the Jhilam, from the town of that name, until it takes a bend to the south to its junction with the Chmab. To the west, the water-parting of the Indus commences at Cape Monze on the Arabian Sea, and advances nearly northwards along the Hala mountains to the east of Sohrab, Kalat, and Quettab (Kwatah). It thence continues in the same direction along the western Sulaiman range, also known as the Konak, and Kub Jadran range to the Safed-koh, at the head of the Kurram valley. Thence it follows the crest of the Safedkoh westwards to the hills north of Gfhazni, where it separates the southern affluents of the Kabul river from the waters of the small inland basin of lake Abistida. The direction is then continued north- westerly to the ridge separating the head-waters of the Argand-ab from those of the Kabul river, and again in the range that separates the waters of the Halmand basin from the most westerly affluents of the Kabul river, whence a transverse ridge near the pass to Bamian connects the line of water-parting with the Hindu-kush. For 300 miles the line follows the Hindu-kush to its junction with the great Taglidambash Pamir near the Baroghil pass. It then follows the Muztagk iange, 3 but cuts through it around by the Karakoram pass to the north, so as to include the tributaries of the Shayok, and proceeds in a south-easterly direction by the Aling Gfang-ri to its junction with the Grang-ri at Kailas, where a transverse ridge separates the head-waters of the Indus, the Brahmaputra, and the trans-Himalayan feeder of the Granges system. The Indus has a length of 1,800 miles, and, according to Mr. Saunders, its basin has an area of 372,000 square miles. r< l* ^ T ' 2 See Notes on the lost river of the Indian desert, Dai. Kev., July, 1874. 3 < Ice-mountain’ : a better name than Karakoram (, black-gravel), which should be restricted to the pass, OF THE NORTH-WESTERN PROVINCES. 65 The Hala mountains to the south of the Mula pass are better known Subordinate systems of the Khirthar lulls and as the Pubh hills, the Indus basm. and the drainage from them loses itself in the plains before it can reach the Indus. The same may be said of the drainage through the Mula and Bolan passes, and that by the Thai valley. To the north, the Luni, Gomal, Kurram, and Kabul rivers, each possessing a perennial stream, have an easterly course more or less parallel to each other, and break through the range bordering the right bank of the Indus by deep and narrow gorges which form the passes into the upper country. The Kabul river itself is the drainage channel for the very elevated country from the hills north of Ghazni to the Baroghil pass north of Chitral, and from Naushera to the pass leading to Bamian, and thus forms a compact subordinate system well deserving of separate study . 1 The upper waters of the Jhilam drain the Tile and Kashmir valleys, and have a general direction between west and north to Muzaffarabad, where they unite, and, meeting a meridional ridge, take a bend southwards to the plains. The Chi nab, in the upper portion of its course known as the Chan- dra, has a similar direction between west and north until it meets the spurs from the range which forms the water-parting between it and the Jhilam, whence it seeks an outlet southwards towards the plains. The Ravi runs in a valley parallel to that of the Chinab and south of it until it meets the outliers of the range that forms the water-parting between it and the Chinab, when it also turns suddenly southwards towards the plains. Next comes the Bias, which has also a westerly direction until it meets the ridge between it and the Ravi, when it takes a bend to the south through the outer hills. The upper course of the Satlaj has a similar westerly trend until it meets the great obstruction culminating in the Leo Porgyul peak, after which the direction is between west and south until it enters the plains. A range runs between the Satlaj and the southern branch of the Indus from the meridian of Tirthapuri by Gar, to where it is joined by the ridge connecting it with Leo Porgyul, and thence into Rupshu to the north of the Tso Moriri lake, and consti- tutes the subordinate water-parting between the Satlaj itself and the 1 For interesting articles on the tract between the Arabian sea and the Gilgit river, by Mr. C. R. Markham, see Proceedings R. G. S., 1879 : the mountain passes on the Afghan frontier of British India, p. 38 : the upper basin of the Kabul river p. 110 : the basin of the Helmund, p. 191. 9 hima'layan districts 66 Indus. Thus we see that the great feeders of the Indus system from the west have a similar character, and that those from the east, from the Himalaya proper, have a general westerly direction, in the upper portions of their courses in the hills, until they turn south- wards towards the plains, where the direction is south-west to th ex- junction with the Indus. Tlie Ganges basin. Next we have the Ganges basin with its subordinate systems. To the north, the water-parting, as a rule, follows the ghat-line of the Himalaya and on the extreme west separates the sources of the Jadh-Ganga, one of the head-waters of the Bhagiratlii, from the Hop-gadh, an affluent of the Satlaj. North of Kumaon, however, we have a phenomenon similar to that observed near the Karakoram 1 pass, where the waters of the Shay ok, Yarkand, and Karakash rivers have a common origin in that elevated plateau at no great distance from each other. We find that to the east of the Unta-dhura pass, north of Milam in Kumaon, the water-parting of the Ganges basin crosses to the north of the ghat-line to a place called Tara, where the sources of the Satlaj and the Karnali lie close together, “ divided by an almost level plain, across which a man might walk from one river to the other in an hour or two, without a vertical ascent or descent of 500 feet,” yet the waters of one stream seek the sea at Karachi, and of the other by Goalundo. Further east the water-parting is continued in the ghat-line to the Arun river, which has its sources to the north and forces for itself a way through the Himalaya to the plains. The water-parting then follows the eastern boundary of Nepal to the plains, where an intricate system of drainage is met with, throwing off feeders sometimes to the Brahmaputra and sometimes to the Ganges down to their junction at Goalundo. Following the line on the west from east longitude 79° 11' and north latitude 25°, we 1 Dr. Scully describes the appearance of the country between the top of one of the Shayok gorges and the Karakoram pass thus : — “ At the top of the ascents strange sight met our eyes, for we found ourselves on an immense undulating plain, the Dipsang, which looked like the top of the world. * * Northwards, in front of us, we saw a few irregular flat-topped hillocks, they looked like scattered about * * I had occasion to look back in the direction of the route by which we had come. A fine snowy range of mountains met my view and looked quite continuous ; but, of course, this was a deceptive appearance, as we had passed through this chain without crossing any pass.” This was the Muztagh range, whilst the Karakoram pass, dis- tant about 25 miles ahead and forming the water-parting, lay amongst the seeming hillocks, a fact which shows that though a range may form a water-parting, a water- S irting does not always form a part of a range , Colonel Gordon gives views of the arakoram pass in his 1 Roof of the World.”’ OF THE NORTH-WESTERN PROVINCES. 67 find in the extreme north-west that the water-parting keeps to the crest of the range running along the left bank of the Baspa, an affluent of the Satlaj, and is continued by Hattu to the ridge on which Simla is built. Thence it proceeds southward, and then eastward along the right bank of the Griri to the junction of that stream with the Jumna near Raj ghat. Here the water-parting turns southwards along the line separating the drainage area of the Kaggar system from that of the Jumna, and continuing along the Arvali range- and the edge of the Malwa plateau, passes through the Jabalpur and Mandla districts, separating the sources of the Nerbudda from those of the Son, and then along the range connecting the Satpuras with the Rajmahal hills to the plains, where it follows a course along the left bank of the S'abanreka to the sea. Mr. Saunders has given the length of the main stream of the Gan- ges as 1,514 miles, and the area of its basin at 391,000 square miles. The Ganges basin, like that of the Indus, possesses several subor- Subordinate systems of dinate systems that may be called in their the Ganges basin. order from west to east, the Jumna- Ganges,. Karnali, Gandak, and Kosi systems. The alpine basin of the J umna- Ganges system is bounded on the west by the well-defined range which descends from the Jamnotri group of peaks to the Satlaj river, and on the east by a similar ridge descending from the Nan da Devi group of peaks and separating the waters of the Pindar from those of the Himalayan Sarju. To the north, the ghat-line separates it from the source of the Karnali on the east, and the source of the Satlaj on the west. Although the upper waters of both the Jumna and the Alaknanda, or principal source of the Ganges, have at first a westerly direction, they soon take a bend to the south, and form the main channels to which are directed their affluents from either side. It is remarkable that, with the exception of the Ramganga, which unites with the Ganges in the Farukhabad district, neither the Jumna nor the Ganges before their junction receives any consider- able affluent of Himalayan origin during its course through the plains. The western boundary of the alpine basin of the Karnali is marked by the ridge extending from the Nanda Devi group between the Pindar and Sarju rivers, already noticed. The eastern boundary 68 HIMALAYAN DISTRICTS is formed by a similar ridge descending from the Dhaulagiri group of peaks. To the west the Sarju, eastern Ramganga, Gori, and Kali enter the plains in one stream as the Sarda. Then the Swetaganga Karnali, and Bheri form the Karnali, and further east we have the Jhingrak or Rapti and its affluents. All unite in the plains to form the Ghogra, which joins the Ganges to the south of the Ghazipur district. But this unitising law is better exemplified in the alpine basin of the Gandak, which reaches from the Dhaulagiri group to the Gosain-than group of peaks. We have here seven rivers named in order from west to east, the Barigar, Narayani, Sweti- gandaki, Marsyangdi, Daramdi, Burhiya-Gandaki, and Trisul- Gandaki. These are called the seven Gandaki by the Nepalese, and unite their waters at Tribeni within the hills to form the Gandak river of the plains. Here we have what Hodgson 1 terms an admi- rably defined natural division lying between two great groups of peaks. In the same manner as the Karnali basin is bounded on the west by the spur descending from the Nanda-Devi group of peaks, and on the east by the ridge from the Dhaulagiri group, so the Barigar of the Gandak system does not receive a single streamlet from the westward of the Dhaulagiri ridge, nor does the Trisul of the same system receive any .water from the east of the ridge descending from Gosain-than. The alpine basin of the Kosi lies between the Gosain-than group and the Kanchinjinga group of peaks, and, like the Gandak system, consists of seven rivers , 2 known as the seven Kosis. These, named in their order from west to east, are the Milamchi or Indrawati, the Bhotiya-Kosi, Tamba-Kosi, Likhu-Kosi, Dud-Kosi, Arun, and Tamra or Tamor. The Aran has one of its sources to the north of the line of snowy peaks seen from the plains, and the Tamor is also said to have trans-nivean affluents, but all the others rise on the southern slope of the Himalaya’ and unite within the hills at Varaha-Kshetra above Nathpur. The subordinate systems of the Ganges basin thus appear to be strongly characterised by a common origin within an area bounded on the north by the ghat-line, and on the west and east by well-marked groups of culminating peaks, whence ridges descend and form the water-parting between successive systems. xvn\ h %46 ticlc ° n the GangeS basin ’ J - A ’ s -’ Ben > XVIII., 761, * ibid, OF THE NORTH-WESTERN PROVINCES. The Brahmaputra basin in its full extent has not been explored, but sufficient evidence has been collected by recent travellers to show that from the water- Brahmaputra basin. parting between the sources of the Brahmaputra and the Indus, the northern water-parting of the former river continues in a range of lofty peaks on its left bank to the bend towards the south, by which it reaches the plains of India. This range has a direction south-east, and to the west of the 86th meridian is sufficiently distant from the Brahmaputra to allow of such affluents as the Chachu and the Charta rivers. About the 86th meridian, a line of peaks culminating in the Targot La stretch in a north-easterly direction to the Gfyakharma group of peaks, south-east of the Kyaring-cho or Kyaring lake, one of the sources of the Nak-chu-kha. The drainage of the southern slope of the range is sent by the Dumphu-chu into the Kyaring lake, so that the northern water-parting of the Brahmaputra must here approach much closer to the river and run in a south-easterly direc- tion. On the 89th meridian, it descends as low as the 30th parallel in the Shiang Lahu range, which appears to be connected with the great Ninjin-thangla range of snowy peaks to the south of the Jang Namcho or Tengri-Nor lake with a trend to the north-east, for it gives the head-waters of the Ki-chu or Lhasa river from its southern slope, as well as other important streams further east, regarding which our information is still very imperfect. To the north-east we find the Nak-chu-kha or Hota Sanpo, a large river that issues from the Chargut lake about north latitude 32° and east longitude 89° and flows eastward, having its drainage area on the south, bounded by the water-parting between it and the Brahmaputra basin. This great river takes a bend to the south, and according to one of the Pandit explorers/ flows by Tsiamdo on the road from Lhasa to Bathang, and thence through Amdu to China, under the names Machu and Konkong. These names would connect it with the Yang- tse, but if it flows by Tsiamdo it should_be one of the branches of the Lan-Tsang, the name of the upper portion of the Mekong or Kam- bodia river. Des Godins notes that the Nu-Tse or Lu-Tse is known as the Ngen-kio in Tibet, a name which may perhaps be referred to 1 Gr. T. S. Rep-, 1873-75, p. 63. The Atlienceuvi of the 17th April 1880 e arrival of Colons! Prp-ioTraioV-,. « + w/i, , , . w 11 ! • io80, announces marches north of oblenr connected with this river from this great traveller, 70 HIMALAYAN DISTEICTS the Nak-chu, and it would then be the head-waters of the Salween,, whilst others claim it as the source of the Ira wadi. All that can, therefore, be said is that there is a great river in eastern Tibet, between which and the Brahmaputra is an unexplored tract of country, and within it will be found the eastern water-parting of the Brahmaputra. So far as we may conjecture from the imperfect materials at our command, the range that forms the northern water- parting of the Brahmaputra takes a sudden bend southwards between the 96th and 97th meridians along the right bank of the Lu-Tse. Thence one branch proceeds westwards in the Patkoi rano-e, and another southwards, between the Irawadi and Salween. To the south, the water-parting follows the crest of the Patkoi range, and is continued westwards in the Manipur, Lusliai, and Chittagong hills, where it separates the southern affluents of the Brahmaputra from those of the Burmese systems. To the west, the water-parting is conterminous with that of the Ganges basin. Mr. Saunders estimates the course of the Brahmaputra at 1,800 miles, and the area of its basin at 361,000 square- miles. Following the systems that carry off the drainage from the south- - Subordinate systems of ™ dope* ° f the Himalaya and join tlie Brail- the Brahmaputra basin. maputra in its course through the plains, we trace much the same regularity found in the subordinate systems of the Ganges basin further west. The Tista system of Sikkim is bounded on the west by a ridge descending from the Kanchinjinga group of peaks, and on the east by a similar ridge from the Chumalari group that also forms the eastern boundary of Sikkim. The alpine rivers of this system in order from west to east are the Bari Ranjit, Baton g, Lachen, Lachung, and Rang-chu, and all unite within the hills above Kalingpong to the east of Darjiling. The alpine basin of the Tarsa-Gangadhar system extends from the Chumalari group on the west to the ridge descending some fifteen miles east of the 90th meridian in the 28th parallel, and which separates the waters of the affluents of the Tarsa from those of the Manas system. The rivers of this alpine basin from west to east are the Ammo, Dor, Par, Wang, Ma, Pachu, and Tanchu, which unite within the hills to form the Tarsa and the Gangadhar tributaries of the Brahmaputra. Further east comes the Manas system, of which the western water- OF THE NORTI-I-WESTEEN PROVINCES. 71 parting is conterminous with that of the Tarsa-Gangadhar system. On the east, it is bounded by a ridge descending from the group of snowy peaks to the west of the Karkang pass crossed by the Pandit on the Tawang route in 1873, and for its alpine feeders has the Mali, Manas, Kuril, Lhopra, and Tawang streams, which apparently also unite within the verge of the mountains to form the Manas. Eastwards lies the Subansiri system between the Manas and the Dihong. The Sikang-chu, which rises to the south of the Karkang pass, probably forms one of its sources, but the remainder lie within the wild country of the Abors and have not yet been explored. The southern affluents of the Brahmaputra during its course through the valley of Asam are not so important, and may be divided into two classes — ’those which carry the drainage of the northern slope of the hills inhabited by the Singpho, Aror, and Naga tribes, and fall directly into the Brahmaputra, and those which carry the drainage of the northern slope of the hills of the Lushai country and hill Tipura and of the southern slopes of the Jaintiya, Khasiya, and Garo hills to the Megna, which joins the Brahma- putra below Dakka. To the former class belong the Dihing, Disung, Southern Dhansiri, and Kopili, and to the latter the Barak, Surma, and Dhani. 1 To the extreme east of the Asam valley is a snowy range from which issues the Lohit or Brahmakund river that gives its name to the Brahmaputra ; but geographers have applied the same name to the great river flowing by Lhasa, and which the best authorities identify with the Dihong that joins the Lohit in the upper valley of Asam. The more general name of the Brahmaputra, in the upper portion of its course, seems to be ( Tsanpo ’ or c Sanpo,’ meaning 1 the river ’ or ‘ the great river,’ used like ‘ Ganga ’ in the plains and ‘ Iviang ’ in China. In Asam, the name varies with the tribe inhabiting its banks or those of its tributaries, so that the designation ‘ Brahma- putra,’ to express the entire course of the river from its source to the north of Kumaon to its junction* with the Ganges, must be considered a convenient device of geographers, and not a term based on received usage. We have seen that at its junction with 1 Any further discussion of the systems of the Asam valley would be out of place here; they are sufficiently described in the Asam Gazetteer, to which the reader in search of further information on this subject is referred. 72 htmXlayan districts: the Loli it, the Brahmaputra is called the Dihong. 1 East of this junction, the Lohit receives a tributary from the north, called the Dibong, and on the south another called the Dihing, and again one called the Disung. Much confusion has resulted in Asam geography from not remembering that all these names refer to different rivers. 2 We have already noticed the division of Tibet into the eastern, western, and central provinces. It is called Tibet. ’ . 1 Si-tsang by the Chinese, and is also known under the names Tu-pu and Mu-tu, or Upper and Lower Tibet. From the accounts of the eastern province in the writings of Klaproth, Hue, Blakeston, Cooper, Des Godins, and Gill, we may assume that the drainage to the east of the 96th meridian has a southerly direction, and that the general conditions resemble much those further west. Pengshan on the Yang-tse in western Sz-chuen is 1,500 feet above the level of the sea. At Ching-tu, some seventy miles due north of Pengshan, Cooper, in March, found the fields in the neighbourhood occupied by luxuriant crops of wheat, barley, sugarcane, and opium, the latter of which demands a climate similar to that of the plains below the Kumaon Himalaya. The same traveller crossed the Yalung and Kinsha branches of the Yang-tse between Chingtu and Bathang, and beyond Tatsien-lu entered Eastern Tibet, where yaks are used in the carrying trade and a more alpine climate is met with. Bathang on the west has much the same position with respect to the elevated highland to the north that Chingtu has on the east, but lies a degree of latitude more to the south than Chingtu ; so that from the meridian of Bathang, the range dividing the Tibetan plateau from the plains of China seems to take a north-easterly direction. The feeders of the Yang-tse and other rivers find their way through this range by a series of gorges similar to that of the Dihong further west. Between the Yang-tse and the Dihong, we have two 1 Klaproth suggested the Irawadi as the continuation of the Sanpo, and Colonel Godwin- Austen was the principal advocate for the Subansiri ; Progs. R. G. S., August, 1876 ; but the researches of the Pandit employed by Lieutenant Harman perhaps show that the Dihong is the real representative of the Sanpo, and that the bend it takes beyond Chetang is quite sufficient to leave a large water-shed for the Subansiri. The most recent advocate of the Irawadi as the true continuation of the Sanpo is Mr. R. Gordon, in his elaborate “ Report on the Irrawaddy River.” The first volume is illustrated with hydrographical hypsometrical and orographi- cal maps of Tibet and the neighbouring countries together with a hyetographical map of India. 2 See Peal’s observations on As&m nomenclature in J.A.S., Ben, OF THE NORTH-WESTERN PROVINCES. 73 great rivers, the Lan-tsang identified with the Mekong or river of Kambodia, and the Lu-tse or upper course of the Salween. Father Des Godins informs us that the Mekong has its origin in about 33° to 34° north latitude in the mountains south of Koko-Nor, and the Lu-tse further west is known as the Ngen-kio in Tibet ; but whether this name is to be regraded as one with the Nak-chu-kha of the Pandit explorer is left to future travellers to decide. Turning now to the upper portions of central and western Tibet, we find from the Pandit explorations that the drainage to the north of the northern water-parting of the upper portions of both the Indus and the Brahmaputra flows into a number of lakes. East of the 84th meridian, these lakes appear to be connected the one with the other, and eventually with the great river Nak-chu-kha, which has an easterly direction in the upper part of its course and finds a southern outlet in one of the great rivers to the east of the Dihone-. I rom the Pangong lake on the west to the Lonkor Clio between the 83rd and 84th meridians on the east, the drainage is collected in a series of depressions without any outlet, each of which is the centre of a subordinate minor system of its own. We do not know of any considerable stream proceeding northwards or westwards from this tract. This lake-system is a characteristic feature of the orography of north-western Tibet. The waters of these lakes are generally brackish and the margins exhibit expanses of salt-marsh. Streams of fresh water are found, but in their course towards the lakes these rapidly become brackish, and in the end little influence the quality of the lake-water itself. According to the Pandit, the country to the north of Garge and Garchethol is a great uninhabited plain. 1 It was formerly customary to travel in a north-north-westerly direction from Tliok Daurakpa 2 for some twenty days to the range overlooking the Gobi plain in which -'the commercial entrepot Nari Tharu lay. 3 A two months’ journey from Tliok Daurakpa to the 1 Called Jung Pliayil Puyil, meaning literally “ the desert country in which the father and son have wandered,” from a tradition that two men had entered it and died there from want of water. G. T. S. Eep., 1S73--75, p. 55. 2 In about 85° 8' east longitude, and 32° V north latitude. 3 Trotter suggests that N ari Tharu occupies a position at the foot of the northern boundary ridge of the Tibetan plateau, similar to that held by Polu and Sorghak, and that the stream passing Nari Tharu may be the same that passes by Charchand. Prejevalsky (p. 76) says that Charchen is situate about 200 miles to the south-west of Chargalilc on a river of the same name. Hence it is a ten days’ journey to the oasis of Nai (900 houses), and three days further to Kiria. The position and distance of Nai would suit the Pandit’s description of Nari Tharu. 10 •HIMALAYAN DISTRICTS 7 ^ Lob-Nor basin. north-east brought the traveller to Ajan, also a commercial centre. 1 This road lay throughout over an extensive plain ; no large moun- tains were seen and no streams were crossed. Drinking-water was obtained from a number of fresh-water lakes mostly dependent on the rainfall for their supply. From these reports we learn that northern Tibet is a plateau of great elevation without inhabitants and possessed of few streams. As we approach the west, the boundary ranges that support the Tibetan plateau between them on the north and south gradually incline towards each other, so that westwards of the Pangong lake they are little more than fifty miles apart. 2 Here we find the water-parting of the Indus and Lob-Nor systems in the elevated Dipsang plain, which attains a height of 18,000 feet above the level of the sea near the Karakoram pass (18,550 feet). From the Karakoram pass on the north flows a feeder of the Yarkand river, and from the east, an affluent of the Khrakash river, both of which belong to the Lob-Nor system. On the south-east, only eleven miles from the pass, the Daulat-beguldi encamping ground is close to one of the feeders of the Nubra branch of the Shayok river that belongs to the Indus system. In one case the waters lose themselves in the Gobi desert, and in the other they reach the Indian Ocean at Karachi. If the statements of Kostenko and Severtsof be accepted, we have here in the west an analogue of the arrangement that has been described as characteristic of all the river-systems along the southern face of the Himalaya between the Jumna and the Brahmaputra. The alpine basin of the Yamanyar lies between two great groups of peaks, some thirty miles apart. On the south-east of the Yamanyar is the Tagharma group, of which the Muztagh-Ata 3 peak attains an elevation of 25,350 feet above the level of the sea. On the north-west there is a similar group, of which the Tash-balik peak reaches an elevation of 22,500 feet. The Yamanyar collects its waters in an elevated valley 1 On approaching Ajan, a bare rocky range is passed and the town is occupied by Sokpas, who procure their corn and flour from Kokod and Karka, a large monastery some ten or twelve days’ journey beyond the borders of their country. Trotter suggests that Karka lies between Lob-Nor and Koko-Nor, and that Ajan is one with the Anj-si of Uspenski ; but both of these identifications require confirmation. 3 From the Khrakoram to Shahidullah (11,780 feet) on the verge of the plains of Yhrkand is a distance by road of 78 miles, and from the same to Changlung on the south is 83 miles, and to Leh on the Indus, 163 miles. 3 ‘ Father of ice-mountains,’ OF THE NORTH-WESTERN PROVINCES- 75 between these groups and the water-parting range on the west, which is known variously as the Tagharma plain or plain of the Kichik Kara-kul . 1 The groups themselves are in advance of the water-parting range and are connected with it by transverse ridges. That on the south connects the Muztagh-Ata group near the Kok Mainak pass with the water-parting range, west of the Neza-tash pass, while that on the north has not yet been accurately defined'. Spurs from the groups descend northwards towards the plains and effectually divide the waters of the Yamanyar from those of the Kashgar-darya on the west and from those of the Yarkand river on the east. It has generally been supposed 2 that these two groups of peaks belonged to a great meridional range ; but Severtsof, who has had recently exceptional means for obtaining an accurate estimate of its character, distinctly states that “ these two peaks were sup- posed to be connected by a continuous range, while the real fact is that each is respectively the highest point of separate small high mountain knots capped with eternal snow.” We have, therefore, in the west also an apparent snowy chain of mountains as seen from the plains, but which on closer examination resolves itself into groups of snowy peaks in advance of the water-parting range from which they are divided by an elevated valley. This valley gives rise to a river that makes a way for itself between the boundary groups to the plains below, while the groups themselves are con- nected by transverse ridges with the line of water-parting. A ridge from Muztagh-Ata to Yangi Hissar separates the drainage of the northern slope from that of the Kinkol river on the east, and' a second ridge follotvs at some distance the left bank of the Yamanyar which shortly after its issue from the mountains is ab- sorbed in artificial branches or canals for irrigation purposes. The whole system is a remarkable illustration of Hodgson’s formula for the river-systems of the eastern Himalaya. The alpine affluents of the Yarkand river known as the Sarikol and Zarafshan rivers also illustrate the unit- ising principle observed elsewhere. They Oxus basin. 1 Lesser Kara-kul or ‘ black lake.’ 2 The two groups form a part of Hayward’s meridional Kizil-Art range, the existence of which was supported by Shaw and Trotter and denied by Fedchenko, who considered the phenomenon described by Hayward as merely representing the terminal butt ends of parallel ranges belonging to the Pamir plateau. Kostenko, however, maintained it to be a great mountain range. Views of the Muztagh-Ata peak and the Karikol valley are given by Gordon in his ‘ Roof of the World-’ 76 iilma'layan districts are separated from eacli otlier by the Kandar range, which descends in a north-easterly direction from the water-parting range to the south, and terminates where the Sarikol and Zarafshan unite their waters within the outer range of hills to the north. The Oxus sys- tem further gives an example of another of the characteristic features of the Himalayan river-systems. The water-parting follows the line of the Hindu Kush from the pass near Bamian to the Baroghil pass, and thence follows the Pamir range to the greater Kara-kul. The height of the water-parting on the Baroghil plain has been estimated by Captain Biddulph at about 12,000 feet. The Mullah states that in traversing it for a distance of five miles there was no appreciable rise or fall, and further it is said that from a point one-and-a-half miles short of the crest, the difference in height did not appear to be more than two hundred feet. The Sarhad head of the Panjah branch of the Oxus is not more than two miles distant from the Gez-kul or Oi-kul, the longest source of the Aksu branch of the same river known as the Murghab. The principal source of the western head of the Panjah branch of the Oxus in Wood’s Victoria lake is but twelve miles distant from the water-parting between it and another branch of the Aksu. So little is his water-parting marked by any defined physical feature that it was only after some difficulty that Trotter discovered it at a height of 420 feet above the level of lake Victoria. There is also reason to believe that the greater Kara-kul once gave off at one end a feeder to the Kashgar-darya of the Lob-Nor system, and at the other a feeder to the Oxus. We have already seen that it is but a little difference in perpendicular height that determines the drainage between the Satlaj and Karnali and between the Nubra branch of the Shay ok and the Karakash, so that where rivers have their sources in these elevated areas it may be generally stated that a slight inequality in the surface, such as it is not possible to delineate on any ordinary map, is sufficient to determine the course of springs into channels that have a very remote debouche one from the other in the pla ns. The terms trough, channel, basin arc in such cases often misleading. Nor are the bounding ranges in these elevated regions marked with such well-defined characters as are met with elsewhere. The great Pamir is divided from the Alichur Pamir on the west by a range having an average elevation of only 3,000 feet above the level of the OF THE NORTH-WESTERN PROVINCES. 77 Victoria lake, and from the little Pamir by a similar range averag- ing about 2,000 feet above the same level. The direction of the rivers depends, therefore, on the influence of much less relatively important masses of matter than are to be found at lower levels. The slight difference in level that determines the course of the head-streams of the Karakash and Yarkand rivers on the Dip- sang plains, is sufficient to divert the former from their normal direction and drive them directly against the Kuen-lun range, where, finding a fault in the wall, they work their way through towards the plains. The influence of the law of gravity and the me- chanical and chemical changes wrought by water are the sufficient causes for every form of river channel that is met with, and it is to their ceaseless action that even the stupendous gorges of the Indus, the Satlaj, and the Brahmaputra, are due. Plains of Hindustan. Indus plain. Having concluded our review of the river-basins and their to relations to each other, we shall now pro- ceed to examine the different parts of the area under our consideration. The great plain of Hindustan which first claims our notice is a vast flat extending with an almost unbroken surface along the foot of the Himalayan slope from the upper Indus to the Bay of Bengal. Its direction is from north- west to south-east over a distance of nearly 1,500 miles, and having an area, including its western branch along the Indus and its eastern prolongation into Asam, of about 500,000 square miles. On the west it has its greatest development stretch- ing along the Indus from the foot of the mountains to the sea, from north-east to south-east for a length of 750 miles. Its breadth from the Arvali hills to those west of the Indus is about 400 miles. The Arvali hills run in a north-easterly direction from the peninsula of Kathiawar until they lose themselves in the plain near Delhi. From this v point they run in a south-east- erly direction connecting with the Vindhyas, and in both cases con- stitute the abutments of the elevated plateau of Central India. They thus form two sides of a triangle with its apex towards the north, where it separates the Indus plain from that of the Ganges. The general slope of the Indus plain is south-west, with, as we have seen, a slight depression towards the south, until the influence of the north- ern slope of the Arvalis is felt, when it gradually rises again. Taking 78 HIMALAYAN DISTRICTS a line along the Indus/ we have Sell wan, 117 feet above the level of the sea ; Shikarpur, 199 feet ; Dehra Grhazi Khan, 395 feet ; Segra, on the eastern bank of the Indus, opposite Dehra Ismail Khan, 606 feet ; and Khairabad, opposite Kalabagh, 750 feet. Following the 32nd parallel from west to east, we have Sandi on the left bank of the Indus, 629 feet above the level of the sea ; Lodri, on the left bank of the Chinab, 657 feet ; and Ramdas, on the left bank of the Ravi, 796 feet : further east, we enter the hills. Following the 30th parallel we find Mare on the 71st meridian, with an elevation of 386 feet ; Nur Shah on the 73rd meridian, 482 feet; and Pakka Sarawa, on the 75th meridian, 698 feet. The perfect uniformity of the surface is broken in the north-west by the small table-land be- tween the Indus and the Jhilam, of which the salt range 2 forms the abutment. These hills at the Sakesir station of the survey in the Jhilam district rise to a height of 4,994 feet above the level of the sea. They extend from Khairabad on the Indus to the Jhilam op- posite Chilianwala, and thence those forming the eastern flank of the table-land as well as a subsidiary range to the east of the Jhilam turn abruptly north-east and connect with the outer ranges of the Hima- laya near Bhimbar (1,200 feet). The table-land itself is seldom more than two or three hundred feet above the general level of the plain, and presents an undulating though tolerably even surface bro- ken occasionally by ridges which attain a height of from two to three thousand feet. The Indus plain along the foot of the hills is sufficiently watered, , , but to the east and south at any distance Indian desert. .... . from the rivers cultivation on an extended scale is only possible when the scanty rainfall can be aided by artificial irrigation. The latter tract known as the great Indian desert stretches through Bhatiana, Bikamr, and Bahawalpur into Sind. Tradition tells us that in former time it was a fertile and populous country studded with numerous cities and towns and inhabited by prosperous and civilised tribes. A recent writer 3 states that “there is nothing in history to show that the rivers (of this tract) ever contained much more water than they do now. Some diminution in their volume may have taken place during the 1 All these heights are taken from the records of the Great Trigonometrical Sur- vey. 2 Fleming on the salt range, J. As. Soc., Ben., XXII., 229. 3 Cal. Rev., July, 1874, p. 3. OF THE NORTH-WESTERN PROVINCES. 79 lapse of ages, from changes in the lower Himalayan range, as well as from the destruction of forests and increase of irrigation. There is no doubt also a tendency to the obliteration of the lower part of their course ; partly by the drift of sand and dust from the desert ; and partly by the deposit of the silt brought down by the streams themselves, owing to the absence of the great river by Avhich it would have been carried off to the sea.” Between the Sarasvati and the Satlaj are a series of broad channels, most of them a mile in width, of which those to the west appear to terminate in the valley of the Satlaj, while those to the east, which are also the more ancient, lead to the channel of the lost river Hakra or Sotra. 1 The Kaggar now runs in an old bed of the Satlaj and was formerly an affluent of that river. The change may have taken place owing to some great cataclysm 3 which formed a new bed for the river and left the old one for its tributaries on the east, and there is much to be said in favour of the identification of the Sotra channel with this old bed. At the present day the water-level in wells in this tract is excessively low, being often so deep as three hundred feet from the surface. As the water when procured is often brackish, it is a matter of wonder that people are found to inhabit this country which long ago receiv- ed the name of Marusthali, ‘ the region of death.’ The Gangetic plain extends from the debouche of the Jumna from the hills to the head of the delta of the Gangetic plain. Ganges, and lies between the great bend of the Himalaya and the north-eastern slope of the table-land of Central India, which here has a general elevation of about one thousand feet above the plain. The breadth of the plain varies from about two hundred miles at Agra to about one hundred miles at Bajmahal. The direction is to the south-east, but to the east of the Ganges the courses of the rivers exhibit more southing. A general idea of the fall in height along the course of the Ganges may be obtained from the following figures : Saharanpur, 903 feet above the level of the sea ; Meerut, 735 feet ; Aligarh, 610 feet ; Agra, 516 feet ; Cawn- pore, 517 feet; Allahabad, 315 feet ; Benares, 255 feet ; Patna, 174 feet ; Bhagalpur, 159 feet; and Bardwan, 97 feet. 3 Cross sections 1 Said to have dried up in the thirteenth century. * Like that of 1762, when, according to General Cunningham, the river was dammed up by a landslip in the hills and rose some four hundred feet before the barrier gave way. A similar cataclysm occurred on the Indus. 2 From G . T. S. tables. 80 HIMALAYAN DISTRICTS show little difference in height at any point. Bhatpura, below Mohan, at the entrance to the principal pass into the Dehra Dun, is 954 feet above the level of the sea. Following eastwards the line along the foot of the hills, we have Hard war, 1,016; Najfbabad 860; Barhapura, 910 ; Kashipur, 750; Bilahri, 760 ; Sigauli in Gorakhpur, 300 ; Madanpur in Tirhut, 230; and Amua, 248 feet. 1 Noting these figures on any good map and following the course of the rivers, a sufficiently correct idea of the general slope of the Gangetic plain will be obtained. At the termination of the hills near Rajmahal, the plain once more expands largely to the south and again presents an uninterrupted surface from the moun- tains to the sea. The length of this section is about 350 miles, and its breadth from Bajmahal to the Brahmaputra about 150 miles, but increasing to about 300 miles along the coast at the head of the Bay of Bengal. The height varies from 100 feet, the level of the river Mahanadi at Malda, 2 to 75 feet at Jelinghi, the head of the Hugh branch of the Ganges, 3 and 31 feet at Chinsurah. The Howrah station bench-mark is but 1 8 - 2 feet above the level of the sea. 4 These portions of the great plain, often though not very appropriately called the valley of the Ganges, are intersected by the countless tributaries of that river and are under the full influence of the periodical rains. They therefore, as might be expected, com- prise the richest, the most populous, and the most civilised districts of India, and in these respects form a striking contrast to the west- ern parts along the Indus which are doomed to perpetual sterility, not from any natural deficiency in the quality of the soil, but only from the great aridity of the climate. This barrenness is no doubt, in a great measure, due to the relative position of the Indus plain to the higher ground around it and to the prevailing winds ; matters which, at first sight, appear to be of little importance, but which are the efficient causes of the extremely dry climate that it possesses. Fluviatile action in erosion and deposition, productive of the allu- vion and diluvium, terms so well known in the settlement records of these provinces, has clearly directed the course of the rivers in the great Gangetic plain. Mr. Fergusson, in an article quoted by the authors 5 of the £ Manual of the Geology of India,’ shows that the 1 First five from Webb and Sigauli from Kirkpatrick. 2 Hooker. 3 Prinsep. 4 G. T. S., 52 : in sc, VIII., 1866. 5 Pp. 406, 4 12. OF THE NORTH-WESTERN PROVINCES. 81 rivers of the Granges delta oscillate in curves, the extent of which is directly proportional to the quantity of water flowing down their channels. Thus, the oscillations of the Granges between Mungir and Raj mall al average 9^ miles, and between Allahabad and Chunar, only 3‘7 miles in length. Further, when a great river runs through a low country, its course is considerably stayed by the sluggish expanses of stationary water generally termed jhils in Bengal, and it is thus compelled to deposit its silt along its banks. Hence arises the phenomenon of a river passing through a country between banks that are higher than the adjacent alluvial flats, and the gra- dual increase of the banks until the stream makes its way through them to some lower level. Mr. Fergusson estimates that when the slope of a river bed falls to less than six inches in a mile, a denuding river will be converted into a depositing river, and as the deposit commences at the bottom of the slope, the change proceeds up- stream. Moreover, since the Ganges receives its more consider- able affluents from the north, the left bank gradually increases and drives the main stream more and more towards the table-land of Central India, and makes the point of confluence of its affluents continually move upwards. This tendency is well marked in the Jumna in the Mainpuri district, where the old silted-up bed is locally known as the bhagna. 1 In the Tarai below Kumaon the same law prevails, and streams that in the upper portion of their course are denuding rivers in the lower portion where the check in slope occurs deposit their silt, form jhils, and continually change their courses like the rivers of the Gangetic delta. The Asam valley forms a narrow prolongation of the- eastern extremity of the plain, partaking more, however, of the nature of a simple river valley liable to annual floods. It has a length of about 300 miles with a breadth of thirty to forty miles, widening at its junction with the 1 Gaz. IV., 478. The old bed in Sahlranpur is called the Budhi Jumna. — Ibid, II., 140. Remains have been found in the Jumna alluvion near Allahabad. — J. A. S., Ben., III., 302, 529 : IV., 262, &c. Wilford also notices the discovery of bones of men and animals in the Ganges alluvion near Benares about a furlong from its present bed at ninety-five feet from the surface and' thirty feet below the level of the present bed. He says the human bones were entire, but those of quadrupeds were broken and bore evident marks of their having been cut with a sharp instru- ment He found no marine deposits at over 105 feet when the water-bearing strata was reached. — As. Res., VIII., 294. He has also noticed the fact that the point of junction of the Kosi with the Ganges had moved up from Nawabganj opposite Rilj- mahal some twenty-five miles. 11 82 HIMALAYAN DISTRICTS Gangetic delta. It is shut in on all sides, except the west, by mountains. The characteristic of a sudden and total change j^ong a definite line at the foot of the mountains from a broken hilly sur- face to an absolute flat, which holds good throughout the other parts of the plain, here no longer prevails. We frequently see small iso- lated hills standing out like islands from the general level surface, a, phenomenon observable on a smaller scale where the Yindhyan range mingles with the plain. From Sadiya, which is 440 feeF above the level of the sea,, the fall is gentle to Gauhati, which is placed at 163 feet, and Goalpara, Ay Inch is 150 feet. 1 Taking a line along the foot of the hills, we have Titaliya, 330 feet ; Raj hat at the footed the * hills near Buxa, 220 feet ; and the station at the foot of the hills ^ below Diwangiri, A70 feet : figure^ which show a more sudden descent than those at similar positions under the western Himalaya. We shall now return to the plain between the Jumna and the Sarda, and more particularly to that part Bhabai. which lies immediately below the foot of the Kumaon hills. We find there a narrow belt of country usually covered with forest and remarkable for the entire absence of water, a phenomenon eminently characteristic of this tract. The great rivers preserve their course with some diminution in their volume, but all the minor streams that have their origin in the lower hills on enter- in c- this belt soon lose themselves in the shingly deposit thatconsti- tutes the substratum. In time of flood, however, they often preserve a visible stream throughout their course, but this appearance lasts only so long as the cause exists. This belt of waterless forest land is called the Bliabar or ukhar bhumi (waterless forest) under Kumaon, and has a breadth of from five to fifteen miles. Though no stream or spring exists, the Bliabar is clothed with a magnificent forest finding its nourishment in the few feet of alluvial matter that rests on the boulder and shingle deposit below. 3 To the 1 These figures are from the Great Trigonometrical Survey records, which make Dibruo-arh, 3-18 feet above the level of the sea ; Sibsa gar, 319 feet ; and Baramak, near Tezpur, 256 feet. 2 First from Hooker, two last from Pemberton. 3 These descriptions are chiefly based on Herbert’s report ; and on an article entitled ‘The Himalaya in Kumaon and GarlrwaT by Mr. (now Sir John) Strachey, Cal Rev. No. 35. Stewart notes that he can find no definite statement as to the breadth of the tract known as Bhabar and Tarai to the east of Sikkim, but Hooker mentions expressly that there it ranges from 8 to 12 miles in width ; Kirkpatrick and Hoffmeister coincide in making its breadth opposite Nepal about 10 or 12 miles, and between the Sarda and Ramganga it ranges from 20 to 30 miles, falling to 6 or 7 miles abreast of Garhwal and disappearing to the west of the J umna. OF THE NORTH-WESTERN PROVINCES. 83 south of the Bhabar, the character of the country changes into a swamp devoid of trees and intersected by sluggish streams that rise from unhealth v morasses. This tract is Tar&i. included with the Bhabar between the Ganges and the Phika under the general term ban or jungle. East of the Phika under Kumaon, where it apparently attains its maximum breadth, it is known as the Tarai, and under Nepal as the Taryani, with some specific addition as Morang, &c. It lies between the forest belt and the cultivated plains, with an average breadth of about ten miles under Kumaon, though varying much in different parts. Thus wo have between the plains proper under Kumaon and the foot of the hills two distinct belts of country, each about ten to fifteen miles broad, known as the Tarai and the Bhabar. The Tarai is characterised by the presence of reeds and grasses showing the marshy nature of the ground. The streams carry off only a portion of the superfluous moisture and sluggishly run in tortuous channels, doubling back con- stantly in their course. The soil consists of moist alluvial mat- ter without a sign of rock either in fragments or in site. In the Bhabar, on the other hand, no water rises from the ground. Through- out its whole extent not a single spring nor any water can be seen, except occasionally where one of the larger rivers takes its course. In the rainy season alone torrents cut into the ground, and the chan- nels thus formed exhibit characteristic sections of this remarkable tract. We then find that there is but a thin covering of alluvial soil on a vast dry bed of boulders and of shingle, through which all rain that falls sinks rapidly, and which absorbs in the same way all the minor streams of the outer ranges. Instead of reeds and grasses, we have here all the magnificence usually attributed to oriental forest scenery. Gigantic haldus ( Adina cordifolia ) and /chairs ( Acacia catechu ) rear their heads above a tangled undergrowth of creepers and tliorn-buslies which present a barrier to progress that an elephant alone can surmount. Towards the hills we find the sal 1 ( Shorea robusta ), and in Kota great groves of mangoes, while patches of cultivation appear wherever irrigation is practicable. For this 1 The sal is the characteristic tree of the upper Bhabar wherever it is found. Hodgson notes that constant -observation has enabled the people of the Tarai to dis- tinguish the principal belts of the Bhabar from the trees that grow in each. The highest is the sal level, the next is the Jthair level, and the lowest is the sisu ( Dul- ler tji a sisu ) level. 84 HIMALAYAN DISTRICTS purpose, the streams of the lower hills are turned into artificial chan- nels before they reach the shingle deposit, and even the lakes in the lower hills are dammed up to retain a sufficient supply of water for the Bhabar. West of the Ivosi, however, there is little cultivation or irrigation, and the Bliabar there almost remains untouched by the plough. The actual slope of the ground between the Tarai and the foot of the hills is considerable, though not apparent to the tra- veller, except when he observes the rapidity of the current in the irri- gation channels that line the road by which the Bhabar is crossed. Siwaliks. Before entering into more detail regarding the Bhabar and Tarai, there is yet a third feature characteristic of the tract below the Himalaya that must be noticed here as intimately connected with the other two, and this is the line of hills called the Siwalik 1 or sub-Himalayan. These will be well known to palaeontologists in connection with the rich col- lection of fossil mammalian bones discovered in them by Dr. Fal- coner and Colonel Cautley. As a rule, they appear to rise abruptly and without any intermediate undulating slope from the apparently level surface of the flat country below to heights varying from a few hundred to three or four thousand feet. They are composed of sand- stones and conglomerates, and the dip of the strata is usually towards the general mass of the mountains at a low angle. The form of dis- turbance of the strata is very regular, producing broad normal anti- clinal flexures, the axis-plane sloping towards the mountains. To- wards the plains the slope has been weathered out, so that plains- wards the Siwaliks exhibit a steep face from which rise the highest summits of the range, while a long gentle declivity slopes inwards and forms a longitudinal shallow valley by meeting the foot of the next line of hills. The latter, as a rule, run on a line parallel to the Siwaliks, but at a distance of from five to ten miles from them. The bottom of this longitudinal depression is, as may be supposed, by no means continuous. In some places it is cut through by the passage of the streams that drain the interior of the mountains ; in others, it is quite obli- terated by the near approach to each other of the two ranges that flank it, and which usually form distinct lines. This is, moreover, a I) tins. 1 Sivawala, belonging to Siva ; for use of the term ‘ Siwaliks’ by Musalman historians, see ‘ History ’ posted. OF THE NORTH-WESTERN PROVINCES. 85 structural feature and not due simply to denudation. In the country between the Satlaj and the Kali, these valleys are called Duns and under Nepal, according to Hodgson, they are called Maris. They have been confounded by some writers 1 with the Tarai, which, as we have seen, is quite distinct. The lower part of the Duns generally appears to be covered with a deposit of boulders and gravel that slopes somewhat steeply from the Himalaya towards the Siwa- liks, so that the whole bottom of the valley is considerably raised above the level of the plain without. In consequence of this eleva- tion, the outer hills when viewed from the interior of the valley, as from Masuri, present a very insignificant outline. The drainage of these valleys usually collects along their longitudinal axis and either falls into some of the larger streams that cross them, or less frequently finds an independent exit for itself into the plains by a sudden bend to the south through a break in the outer range. Owing to the considerable elevation of the Duns above the plains down to the level of which the drainage finds its way in a very short distance, the unconsolidated strata that form the floor of these valleys are constantly cut through to a great depth by water-courses. Conse- quently, the surface, though often presenting an apparent flat for several miles together, is frequently broken up into steps which, on the whole, are tolerably level, but at different heights, the one above the other. This phenomenon is not uncommon, and is constantly observed along rivers that are eroding their banks. To the same causes also are to be attributed the practical impossibility of procuring water by means of wells in the Duns, a difficulty which mainly arises from the thorough dessication of the gravelly soil by the deep drainage. We have not sufficient information to state distinctly how far the Bhabar extends both east and west along Extent of the Bhabar. * the foot of the Himalaya, but the following indications would lead us to suppose that this phenomenon is inherent in the relations of such a mass as the Himalaya with the subjacent plains. Under Nepal it is called the Jhari or Bhavar, and, according to Hodgson , 2 extends from the Kali to the Mechi on the east with the same general characteristics as under Kumaon. 1 Somerville’s Physical Geography corrected in 7th edition, 1878. 2 Physical Geography of the Himalaya. — J. A. S., Ben., XVIII., 778. HIMALAYAN DISTRICTS 86 Eastward of the Tista, according to the same writer, the Bhabar and Tarai do not exhibit the same parallelism to the line of the Himalaya, but “show themselves plain wards, like an irregular series of salient and re-salient angles resting on the mountains. Or like small insulated plateaus or high undulated plains, surrounded in both the latter cases by low swampy land analogous to the Tarai.” An example of the former is found in the plateau called the Parbat Joar on the coniines of As am and Rangpur, which is considerably elevated, quite insulated, remote from the mountains and covered with scd , the characteristic tree of the upper Bhabar. Again, we have undulating plains, such as those that occur around Dinajpur and to the north-west and north-east of Siligori, all of which may be identified with the Bhabar. In all these cases where the detritus bed thins out, a moist tract is met with, though in no case so marked as to the westward. Herbert 1 affirms the general applica- bility of his remarks regarding the submontane tract below Kumaon to the entire country between the Ganges and the Satlaj and Parish 2 to the tract further west between the Satlaj and the Bias. There is no well-defined line dividing the area of swamp from the Bhabar proper between the Sarda and the Ramganga. To the east in the Tallades Bhabar, where the streams seek the Sarda directly, there is less Bhabar, and the swamps that exist are not so extensive, but at the same time are more formidable, being often surrounded by tangled masses of canebrake. The Dhyanirau Bhabar also is comparatively narrow, and it is not until we come to the Chhakhata Bhabar that we get a breadth of eight to twelve miles that lasts until the Phika river is reached. The Tarai exist all along the tract to the south of, and parallel to, the Bhabar from the Sarda to the Phika. But west of the Phika it loses its charac- teristics and can only be traced in the closeness to the surface of the water-level in wells. Westward of the Phika, the Bhabar or water- less tract also narrows and the scd forest does not descend more than six miles from the foot of the hills, and a few miles further west it has not a breadth of two miles. The Bhabar, however, exists, and is broader than the present sal forest, of which much has been cut down of late years. Its presence is shown by the absence 1 Report of the Mineralogical Survey of the Himalaya Mountains, 1 bid, extra No., Vol. XI. 2 Kohistan of the Jullundhur Doab, Ibid, XVII., p, 281 : XVIII., p. 360. OF THE NORTH-WESTERN PROVINCES. 87 of wells, and similarly the Tarai appears in a line of wells with water at from three to six feet from the surface, running parallel to and bordering on the Bhabar. This limitation of both the Bhabar and Tarai is conterminous with the commencement of the Path Dun, which has detained the greater part of the detritus that is elsewhere spread out below over the plains. From the Pliika eastwards to the Sarda, where these tracts attain their maximum importance, there are no Duns, properly speaking ; for the Kota Dun presents no great barrier to the south, and further east the Siwaliks are so blended with the outer range that a geologist alone can trace their sequence. In this fact, we have an illustration of that portion of Hodgson’s theory that gives a narrow extent to the Bhabar below the Duns and a broader range where there is no Dun to intercept the debris from the hills. The facts that we know regarding the Bhabar to the north of the Saharanpur district 1 further confirm this deduction. In Eastern Turkistan we find a similar phenomenon. Trotter The Bhabar in Turkis- us that the Sagon river, which has its tan - source at the eastern foot of the Terek pass, after it reaches the plains north of Kalti Ailak wastes away and leaks through crevices in the stony ground. The hakim of the latter place assured him that wells had been often sunk but proved of no use. Trotter writes : — “ This diminution in the size of rivers as they des- cend is one of the chief characteristics of the country, and occurs in all minor streams that have come under my notice. Of course much of this is due to irrigation, which necessarily carries off large quan- tities of water, but the stony soil has also much to answer for ; on the other hand, the frequent appearance of large springs giving con- siderable supplies of water and often issuing from the open plains at long distances from the mountains may account in a great measure, if not fully, for the water thus dost in its early infancy.” Here we have the existence of a Bhabar and Tarai vouched for by competent authority in the Yarkand and Kashgar country. The same pheno- menon, but on a larger scale, was found by Prejevalsky to charac- terise the tract between Korla and Lob-Nor. A belt of country about three to four miles wide, consisting of an undulating plain covered with a pebbly or gravelly soil and totally devoid of 1 Gazetteer, II., 110. 88 hima'layan districts vegetation, runs parallel to and at the foot of the Kurugh-tagh, a low waterless and barren range. Beyond this stony margin, which appears to define the shore-line of an ancient sea, lies the great desert of drift sand amid which salt marshes exist wherever the moisture comes to the surface. The same pebbly plain was found under the northern slope of the Altyn-tagh, the north-easterly continuation of the Kuen-lun mountains between the 90th and 92nd meridians, and north of and below the stony margin the usual salt marshes occurred. The latter are also found at the foot of the north-eastern portion of the Tibetan table-land in Tsaidam. It would, therefore, appear that tracts analogous to the Bhabar and Tarai of Kumaon surround the entire Himalaya-Tibetan mass, and that they vary in character accord- ing to local influences. Hodgson attributes the distinctive character of the Bhabar, as a © Cause Of the deposit : whole, “ to the vast mass of diluvial detritus Hodgson’s oceanic theory. w hicli was shot from the mountains upon the plains, like gravel from a cart, at some great geological epoch, and which has been, since its deposit, variously and often abraded both in degree and direction by oceanic and, in a far less degree, by ordinary floods.” Another writer considers that this theory of Hodgson’s appears to be a reasonable explanation of the existence of these great beds of shingle, sand, and boulder all along the foot of the mountains. It is argued that no rivers can have laid out such a vast deposit, and we can only conclude that we see here the limits of an ancient ocean that once washed the base of the Himalaya. The boulders and shingle are spread out only for a distance of ten or fifteen miles from the mountains from which they are derived, while- the finer particles of sand and clay are carried much further. Great variations in the depth and breadth of the deposit occur, due, in a great measure, to local causes. One which apparently has had a great influence is the existence or otherwise of the Siwalik range-. Where there was no sandstone range to intervene between the moun- tains and the plains and collect the detritus within their contained Duns, the deposit is broader and not so thick. Where there was such a barrier, it has been carried less southwards and exists in great accumulations between the barrier and the mountains. Again, where no range existed but only spurs sent forth, like bent arms, upon the plains from the mountains, Hodgson observes that the embayed OF THE NORTH-WESTERN PROVINCES. 89 detritus is simply deeply piled and lofty within such spurs, and thinly and unequally spread without them, by reason of the action of the spurs on the current. He notices, as an example of this form, the debris embayed by a spur on the road to Darjiling by Pankabari, where it is accumulated to several hundred feet, and where, moreover, there is outside the spur a succession of terraces, apparently due to oceanic forces . 1 Further, “ where, as from Gauhati to Sadiya, there was not room upon the plains for the free spread and deposit of the detritus owing to large and rapid rivers and to other chains both proximate and parallel to the Himalaya, the phenomena, created elsewhere by the more or less unrestricted spread of the Himalayan detritus over the plains, would necessarily be- faintly, if at all, trace- able. Lastly, if at the time of the descent of the debris, there existed a great dip in the Gangetic plain from north-west to south-east, the lithologic character, as well as the distribution, of the debris, would be materially affected thereby, for the subsiding oceanic current would have a set from the former to the latter quarter and would continue to lash the gravel into sand and here to deposit both in a series of terraces, there perhaps utterly to displace both in the latter quarter long after the former had emerged from the waves.” Fluviatile theory. The oceanic theory of Hodgson is not accepted by the majority of professed geologists. Mr. W. Blandford writes : 2 — u There is absolutely no proof of any sort or kind that the whole Indo-Gangetic plain has at any time been a marine area ; but there is equally no proof that it has not. It has been shown that in eocene times the sea occupied the Indus valley as far as the foot of the Himalaya, and extended along what is now the base of the mountains, as far east as Ku- maon ; and also that marine conditions prevailed to the north-west throughout a great part of the tract now occupied by the Asam range ; but it was also pointed out- that, in the area between Ivu- maon and the Garo hills, no trace of marine formations had been found. Yet it is difficult to understand, if the Gangetic plain was a; sea-basin, why no marine beds occur. It is true that the north- ern border of the plain, throughout the most important part of the 1 The oldest advocate of the oceanic theory is Wilford (in As. Res., VIII., 292). who thus accounts for several statements made by the Pauranik geographers,, and particulary the story of Sagara. He, however, acknowledges that the existing - soil of the Gangetic plain, so far as is known, was due to fluviatile. action. 2 Manual of Geology of India, p. lx., 393. 12 00 HIMALAYAN DISTRICTS intervening space in Nepal, is, unfortunately, inaccessible to Euro- peans ; but still, if the Gangetic plain in any way corresponds to an eocene sea, as the Indus plain doubtless does, why are no traces of marine beds found to the south of the valley on the margin of the peninsular area, as they are in the desert to the east of the Indus ? In the Brahmaputra plain, also, no marine deposits of tertiary age are found ; in the plain itself only fluviatile deposits have been detected and the marine, eocene, and miocene beds are confined to the southern slope of the range forming the southern watershed of the valley.” Mr. Blandford considers the post-tertiary formation of these proAnnces to be clearly river deposits. The latter tertiary formations belonging to the Siwalik series contain reptilia and mollusca, but not a single marine shell. “ It is impossible to tell what beds may be concealed below the Indo-Gangetic alluvium, and marine strata may exist to an enormous extent without appear- ing at the surface ; it is also unquestionable that the amount of information hitherto derived from borings is very small indeed, but so far as that information extends, and so far as the lower strata of the alluvial plain have been exposed in the beds of rivers, not a single occurrence of a marine shell has ever been observed, nor is there such a change in the deposits as would render it probable that the underlying stratra are marine * * . The only evidence known in favour of marine conditions having prevailed durino- the deposition of any portion of the Gangetic alluvium is the occur- rence of brine springs at considerable depths in a few localities. These springs, however, are not numferous, and, without additional evidence, it is impossible to look upon them as proofs of marine deposits. At the same time it is by no means impossible that the sea occupied portions of Sind and Bengal long after the plains of Upper India were dry land.” On the whole, Mr. Blandford thinks that the oceanic theory wants further support ; that the fluviatile theory is the only one that fits in with the present state of our knowledge, and that the depression of the Gangetic plain is of con- temporaneous origin with the disturbance and contortion of the Himalayan ranges, and that the physical features of the two areas are closely connected. No important borings have ever been made in these provinces, and nothing has ever been discovered so far as we are aware, to show that the older theory is the correct one. The OF THE NORTH-WESTERN PROVINCES. 91 newer theory is further supported by the discovery of the buried town of Behat in the Saharanpur district, some seventeen feet below the present level of the country and containing coins of the com- mencement of the Christian era, thus showing what can be effected by fluvial action in eighteen centuries. We have already seen that the distinctive features of the Tarai are not found west of the Phfka river, if we Tarai. except a small tract on the left bank of the Ramganga, the condition of which, however, is probably due to de- fective drainage in that particular part, and might occur in any other place. The existence, therefore, of the Tarai as a distinctive feature must be due to local causes capable of explanation, but the imperfect nature of our knowledge will only allow us to guess at them. Her- bert 1 described the Tarai as “ defined in its southern boundary by a rise or step which runs parallel to the common boundary of moun- tain and plain land.” He observes the height is variable, occasion- ally as much as thirty feet and sometimes sudden and steep. Modem research can discover no well-defined boundary beyond the chain of springs which sometimes approach within a couple of miles of the foot of the hills and sometimes are separated from them by a belt fifteen miles wide. In no case is there any such rise or step as des- cribed. Hodgson 2 also accepted the existence of a longitudinal trough running parallel to the Himalaya as a characteristic of the Tarai, which he held to be a natural depression in the plain, and thus accounted for its peculiarities. This theory, however, is opposed to the results obtained by levelling operations and appears to be based on an entirely erroneous idea, the fact being that the drainage of the higher country, beyond which has been lost in the absorbent strata of the Bhabar, here breaks out again in a line of copious springs which collect into swamps in the Tarai. This feature has also some- what plausibly been accounted for 3 by the existence of an impervi- ous stratum below the absorbent boulder detritus, and as the latter gradually thins out the finer and less permeable silt underlying it approaches nearer, and eventually reaches the surface, bringing with it the water that has been absorbed by the shingle talus and has been retained by the impervious silt. 1 l. c„ art. 73. 2 l. c., p. 788. p. 184. 3 Batten in Kuxnaun Reports, 9:2 HIMALAYAN DISTEICTS (a) Point of 7e-appearance of water. | (b) Point of disappearance of water. Although this explanation seems reasonable so far as it goes, it must be remembered that the swampy Tarai extends only from the Plhka to the Tista, and we must, therefore, look for some peculiarity in this part of the plain which does not exist elsewhere, by which we may account for the existence of swamps exclusively in this particular locality. In a recent note, Mr. Lawder gives the following section of the Bhabar and Tarai — His experience of this tract has led him to consider that, what- ever may be the nature of the underlying formation, the surface beds are solely due to fluvial action. The mountain torrents along the foot of the Kumaon hills bring down every year a vast amount of debris which is spread out over the surface now on one side of their previous course and again on the other. This irregular depo- sition itself compels the torrents to change their beds from place to place until, as now obtains, the points where they debouche from the hills are marked by more or less irregular, great, fan-shaped boulder and gravel deposits. The clayey or semi-soluble particles are necessarily carried farthest and are readily deposited not only where there is a check in the slope, but where the current is impeded OF THE NORTH-WESTERN PROVINCES. 93 by the tortuous nature of the channel which itself naturally assumes that form under these conditions. Here, during the rains, the streams saturated with clayey silt, overflow their banks, form new channels, fill up old ones, and create the Tarai. Above this deposit of clay we find one of clay combined with sand, in which, how- ever, the latter predominates. From this bed issues the line of Tarai springs that flow uninterruptedly throughout the year, and its margin marks the northern boundary of the Tarai. Above we meet beds of sand and gravel or gravel and boulders as we approach nearer to the hills. A longitudinal section taken at the top of the Bhabar (Fig. 2 B.) will show that the hill torrents in the upper portions of their course run along a ridge formed by the debris transported by themselves, whilst a similar section of the Tarai (Fig. 2 C.) would show that, as a rule, the river channels are found in depressions below the general level of the country. The geological section (Fig. 2 A.) shows the gradients of the present ground sur- face on the road between Bareilly and Ranibagh, and from them it will appear that in the boulder region deposition takes place at a slope of sixty-six feet to the mile, whilst the clay is not deposited until the descent falls to about eight feet in the mile. It may fairly be assumed that these are the usual angles of deposition of the ma- terials, and that they have obtained since the degradation of the lower hills and the resulting deposition below them commenced. If so, a series of proportionate curved lines running almost parallel to the present ground surface may be taken to represent the ground surface of succeeding periods, and such portions of these lines as may be similarly inclined with the present Tai’ai portion ( i.e ., at the same angle with the horizon) will evidently represent the Tarai or clay deposit as it then existed. A line intersecting all these beds at the several points of junction of the ‘ clay’ with the ‘ sand and clay’ will represent the present impermeable bottom of the Bhabar basin and account for the line of springs upon the surface where the stra- tum of sand and clay crops out. The upper boulder and gravel beds permit of the filtration of water freely through them to the clay, at the same time acting as a capillary reservoir to keep up the dry weather supply to the springs below. We have further evidence in support of this theory in the fact that the Tarai proper does not extend westwards of the Pliika river. 94 HIMALAYAN DISTRICTS Between the Phika and the Sarda there are no Duns, for the Kota Dun has its southern boundary broken through by rivers, and along the entire tract numerous torrents find their way directly to the fiat country below. The proximity of these torrents to each other causes the accumulation of debris to exhibit a continuous appear- ance which seems to have suggested the theory of a marine origin. To the west of the Phika river, the drainage of the lower hills is carried oft' mainly by streams which collect the drainage within the Sub-Himalayan range and seek the plains in one well-defined chan- nel. The Ramganga is the great arterial drainage channel fol- lower Garhwal, and between it and the Ganges, the only consider- able stream is the Ivhoh, which has a small strip of Bhabar below it. In eastern Kumaon the Ladhiya serves a similar purpose, and where in its course towards the Kali it approaches the plains and does not allow of any considerable stream from the southern face of the outer range, both Bhabar and Tarai are narrow, and as this influence of the Ladhiya on the east and the Ramganga on the west decreases the Bhabar and Tarai increase and eventually attain their maximum breadth where that influence is least felt. Where rivers discharge large volumes of water like the Ganges and the Sarda, and in a lesser degree the Ramganga and Kosi, the velocity at their debouches from the mountains is much less than that of the minor torrents, owing to their having cut back and more deeply their channels within the hills, so that only the lighter particles of eroded matter are carried onwards, whilst the boulders are left behind at their natural point of deposition. Hence, near these larger rivers it curiously happens that the width of the Bhabar and Tarai con- tracts in a certain ratio and in the case of the Ganges disap- pears. This explanation is supported by the results obtained during the contour survey of the Tarai. 1 The second diagram 2 (Fig. 3) shows a portion of the country between the Dhora river and the Bhuta stream, taken from the survey maps, and will illustrate the intricate nature of the levelling operations, and show why in some 1 See Proceedings, N.-W. P., P. W. Department, May 31, 1864; July, 1869; February, 1872. 2 From the Rohilkhand remodelled canals’ contour map of a portion of the Tar&i surveyed in 1865-67 by Captains Thomason and F. Brown and Lieutenant Bisset. An examination of the records of this survey shows that what is stated regarding the portion noticed here is true also of the entire tract between the Phika and the Sarda. OF THE NORTH-WESTERN PROVINCES. 95 places the streams double back on their original direction and exhibit the tortuous courses so characteristic of this tract : — 96 HIMALAYAN DISTRICT It will also be observed that there is a sudden check in the slope where the Tarai commences ; to the north in the Bhabar the slope is from sixty to a hundred feet in the mile, and in the Tarai it falls to about ten feet. These are the adequate causes of the existence of swamps, and though the neglect of artificial obstructions made for the purpose of utilising the water for irrigation may doubtless aggravate the natural defects of drainage, it would probably produce no effect whatever were it not for the peculiar physical conditions that exist here. To the west between the Indus and the Ganges, the great arterial drainage lines collect within the hills and run off directly from them, the general fall of the surface receiving no such check as is found under Kumaon. The same is true of the country to the east along the head of the Bay of Bengal, and in the narrow valley of Asam, the Brahmaputra runs in a deep bed at right angles to the natural course of the streams from the hills, and thus forms a perfect system of cross-drainage that dons not allow of the formation of swamps. The Siwaliks appear to have a more or less definite existence along the whole of the Himalaya from the Indus to the Brahmaputra, presenting modi- fications of the same general features along the entire line. To the eastward of the Tfsta they are wanting locally, a fact which it has- been suggested is due to denudation as in the case of the partially obliterated barrier to the south of the Kota Dun. As the Siwaliks will be noticed hereafter in the chapter on the geology of Kumaon, we need not describe them here . 1 Between the Jumna and the Sarda they are found as the southern boundaries of valleys as far eastwards as the Kiln'd river, and thence onwards they almost coalesce with the outer range of the lower Himalaya. Of the Duns or valleys, between the Siwaliks and the Himalaya, that known as ‘ the Dun ’ or Dehra Dun, from the town of Dehra, is not only the most remarkable but the best known. Since the physical geography of this tract will be considered in more detail hereafter, in the notice of the Dehra Dun district, it will be sufficient for our purpose here to note that the Dun, a little to the west of the town of Dehra, is 1 See also Chaps. XXII.-IV. of the ‘Manual of the Geology of India. ’ and Gaz., II., IG. Siwaliks. Duns. OF THE NORTH-WESTERN PROVINCES. 97 divided by a ridge that serves as a water-parting between the Asan, a tributary of the Jumna on the west, and the Suswa, a feeder of the Ganges on the east. The tracts drained by these rivers are known respectively as the western and eastern Duns. The two taken together have a length of about forty-five miles and an aver- age breadth of eleven miles. The east end of the Dehra base line of the Great Trigonometrical Survey on the extremity of one of the spurs of the Gliati range, about one mile west of Mahobawala, is 1,9 57-65 feet above the level of the sea : Mahobawala itself is 2,096-56 feet and Dehra is 2,323 feet. The junction of the Suswa and the Ganges is little more than 1,000 feet above the level of the sea, giving a considerable fall for that stream between Dehra and the Ganges. A well sunk by Mr. Shore, when Administrator of the Dun, attained a depth of 221 feet before a plentiful supply of water was met with, and even at that depth the nature of the deposit was the same as at the surface. 1 The greatest thickness of the deposit is observed near the central ridge. It thins out to the west and east along the course of the Asan and the Suswa, and, according to Herbert, may be observed in the beds of the Jumna and Ganges resting on sandstone. Next, on the west, comes the Kayarda Dun, 1 The following table shows the character of the stratum, and is reproduced here from Mr. Shore’s notes in the Dehra archives compared with Herbert’s record as one of the few notices of this character that we possess. Feet. Total. Soil. Feet. Co O H Soil. 5 5 Fine black mould, few stones. 9 158 Sand, larger pieces of conglom- 4 9 Reddish earth with gravel. erate. 9 18 Sand, gravel, large stones. 4 162 Do., enormous stones 2 20 Do., with reddish clay. 6 168 Conglomerate and gravel. 3 23 Stiff reddish clay. 3 171 Sand, gravel, and conglomerate. 8 31 Do., yellow clay. 3 174 Blocks of conglomerate. 3* 34i Sand, gravel, little red clay. 3| 177| Sand, gravel, conglomerate. 14 36 Stiff reddish clay. 4| 182 Do., gravel. 2 38 Sand and gravel. 1 3 1824 Conglomerate. 22 60 Stiff red clay. 2 3 185 Sand and clay. 2 62 Clay, sand and gravel. 13 i 2.94 Loose sand and gravel and large 16 78 Sand and gravel. blocks conglomerate. 12 90 Stiff yellow clay with little 5 209 Sand, gravel, very moist. sand. 1 3 2094 Conglomerate, over half. 35 125 Sand, gravel, few round stones. If 211 Red clay. 6 131 Sand, large conglomerate blocks. 7 218 Sand and gravel. 13 144 Do., gravel, stones, 34 2214 Brackish clay with angular frag- 5 149 Do., larger stones. ments of clay slate. Another well in Dehra gives water at a depth of 88 feet from the surface, and one at Sati-bagh at 75 feet. There are only twenty-nine wells in the whole valley, and many of these are at favourable places near rivers, so that the difficulty of procuring water by this means is common to the whole Dun. Herbert records the 13 98 hima'layan districts some six miles broad and twenty-five miles long, to the water-part- ing between the Jumna and the Kaggar systems. Beyond it w r e have the Pinjor Dun, which has in parts a breadth of six miles and a length of about thirty miles. The Siwaliks here are neither so broad nor so high as to the south of the Dehra Dun. The Pinjor Dun is divided into two parts, the eastern and western Duns, by a ridge similar to that observed in the Dehra Dun, and which attains an elevation of 2,402 feet 1 above the level of the sea. To the east, the drainage flows into the Kaggar, and to the "west into a tributary of the Satlaj. Mansi Devi, a temjfle in the plains just within the Dun, has an elevation of 1,263 feet,, 1 giving a fall to the rivers within this Dun similar to that found to exist within that of Dehra. East of the Dehra Dun we have the Patli Dun, also divided into Ganges to the Brahma- two parts, but by a depression, not a ridge, a l mtl ' a - fact possibly pointing to its being a valley of denudation. That to the west, which is drained by the Sona nadi, has a slope eastwards parallel to the Himalaya, and is known as the Ivotri Dun. That to the east, which is drained by the Bamganga and has a slope to the west in the same direction, is called the Path Dun. The two rivers meet just before their waters take a bend to the south at an elevation of about 950 feet 3 above the level of the sea. A few miles eastward of their confluence, the valley of the Path Dun shows an elevation of 1,200 feet on the right bank of the stream, and thus allows a considerable fall to the Ramganga in a comparatively short horizontal distance. The peaks of the Siwaliks to the south along this entire line seldom rise above 2,500 feet, whilst the plains at their southern base average between eight and nine hundred feet. Eurther east comes the small Kota Dun between result of borings made by Mm In various parts of the tract along the foot of the hills. At Kashipur, in a spot some twenty feet below the surface of the red clay, he obtained the following results — S>'3" superficial red clay : 1"3" green sandy clay, water : 4'6" black clay, extremely tenacious : T6" light blue sand and abundant water. At Haldua, seven miles north, nearly similar results were obtained : — S' 6" a ferruginous sandy clay or loam, latterly becoming more stiff : T6" a greenish clay, becoming blackish below : 2 ' a bluisli-grey clay, partially sandy, not so tenacious, and quite moist. At Jaspur, nine miles north-west of Kashipur, he found : — S’ surface sand, which gra- dually changed to a stiff red clay : 2' a red, loose sand, damp : 2' variegated sand and clay, spotted : 3' yellowish sand changing to light grey : twigs and roots were found at nine feet and water at twelve feet. At Afzalgarh 6' superficial loam with small nests of imperfectly formed lignite : 2'6" red sand and a quicksand : 4' blackish stiff clay, and 3'6" stiff clay, latterly sandy. Two other borings are recorded without mentioning the locality. 1 Herbert, l. c. art 63. 2 G. T. S. OF THE NORTH-WESTERN PROVINCES. 99 Dhikuli and Kali-dhungi, much broken up by torrents, and having its southern boundary cut through by the various hill streams that cross it at right angles. From Naim Tal to the Sarda the sandstone ridge that represents the Siwaliks is so close to the Himalaya that the geologist alone can discern the connection. The Duns are here reduced “ to deep longitudinal gorges and low gaps, corresponding with a leading geological boundary, that between the old slaty and schistose rocks of the mountains and the massive tertiary sandstones of the Siwaliks.” Further east, according to Hodgson, the Duns are represented by the Saliyan Mari, the Gfongtali Mari,, the Chit- wan Mari, the Makwanpur Mari, and the Bijayapur Mari, all under Nepal. With the exception, however, of the Dun lying on the road to Kathmandu, none of these have been subjected to scientific exami- nation. “ On this track,” writes Mr. Medlicott, 1 “ very complete representatives are found of the two sub-Himalayan ranges and their intervening dun or mart. The Churiaglniti range ' is -structurally a facsimile of the original Siwaliks. At the outer base at Bichiyakoh, there are some earthy rusty beds, all greatly crushed. The dip soon settles down to 30° to north-north-' west, maintaining the same angle steadily to> the top of the pass. This is the typical structure of these detached sub-Himalayan ranges, . the flat inner half of a normal anticlinal flexure. The range is about four miles wide.” Through- out the Sikkim and Bhutan cludrs there is no representative of the Siwalik hills' and therefore no (Vans, but in the Dikrang basin of the Daphla hills. Colonel Gfodwin-Austen discovered two well-marked ranges of sub-Himalayan hills with an intervening dun. We have now seen that the first characteristic features met with in advancing from the plains to the Himalaya are the Tarai, Bhabar, Siwalik range, and duns or valleys, and that though not continuous and indeed occa- sionally altogether absent, they are, taking the whole range, characte- ristic of the relations of the Himalayan mass with the subjacent plains. Lower Himalaya. Crossing tlie Duns northwards towards the snows, we meet the outer ranges of the lower Himalaya. They have a general elevation of about 7,000 feet above the level of the sea, while the highest summits along the line reach between 8,000 and 9,000 feet. This generalisation, though giving the nearest approach to accuracy that the state of our knovv- 1 Manual of Geology, p. 543, 100 HIMALAYAN DISTRICTS ledge permits, is only approximate, for we know very little regarding the outer range between the Sarda and the Brahmaputra. There is this peculiarity in Kumaon, that the outer range first crossed by the traveller is of considerably higher elevation than the intermediate ranges crossed between it and the outlying spurs of the great snowy range itself. We have said that we hold the entire Himalaya to be but the southern slope of the great Tibetan plateau ; that however rugged and furrowed this slope appears, it is homogeneous throughout. W e reserve for the district notices the purely geogra- phical description, and will here try to answer the questions that naturally arise regarding these mountains as a whole. What have geologists been able to discover regarding their history and the ma- terials of which they are composed, and are the causes at work sufficient to produce such very varied results as are here exhibited? In attempting 1 to answer these questions, we must refer to well- known principles, ^ which have been found true in Europe and apply with equal or even greater force to the phenomena observable in the Himalaya. Without trespassing on the domain of the professed geologist, we may briefly summarise the facts observed regarding the Himalaya as a whole. We have seen that the outer range forms a geological as well as a physical boundary under Kumaon. The whole mountain mass may be divided into three great belts ► First, the sub-Himalayan tertiary sandstones outside the Himalaya proper of geologists, and which have a considerable development west of the Jumna. To them belong the Siwaliks and the Sirmiir series on which the hill sanitaria of Kasauli, Dagshai, and Subathu are built. Secondly, a belt of limestone and slate forming the outer range of the lower Himalaya on which the hill sanitaria of Simla, Chakrata, Misuri, Landaur, and Naim Tal are situate. Thirdly, the crystalline rocks with granitic intrusions that form the remainder of the lower Himalayan region as well as the line of snowy peaks, and across the British frontier to the north of Ku- maon, the paleozoic and secondary rocks of Tibet. Thus we have as the materials of the Himalaya the two great classes of rock known as the stratified or bedded and the crystalline. To the 1 My acknowledgements are due to the works of Medlicott, Blandford, Tyndall, and Geikie, on which the following pages are based. 2 Though known to 1 every student, a re-statement of these principles seems necessary in a work intended for popular use in India. OF THE NORTH-WESTERN PROVINCES. 101 former belong the limestone, sandstones, and slates that have been derived from the waste of the older rocks ; and to the latter the gra- nite, Gneiss, and schists which occur in masses. The core or nucleus of all great mountain masses is formed of Materials of the Hima- crystalline rocks, while the stratified rocks la y a - enter largely into the composition of the lower subordinate ranges. This is true of the Himalaya, Alps, Pyrenees, Pocky Mountains, and indeed of all the great mountain sys- tems. A glance at the geological map given hereafter will show more clearly than any description the arrangement of these rocks in Kumaon. One of the fundamental principles of geology is that the sites of all the great mountain masses of the world at one time formed a part of the bottom of the sea. K2, Nanda Devi and Mount Everest, the last of which exceeds a height of 29,000 feet above the level of the sea, at one time apparently formed parts of the bed of an ancient ocean. For the crystalline rocks have arisen either from the gradual consolidation of materials which had been fused deep within the crust of the earth or from the influence of subterranean water combined with the earth’s internal heat, out of earlier sediments such as sea-mud and sea-sand, which in the course of time had sunk down and been covered by many thousands of feet of later deposits. 1 Geologists tell us 2 that while no important move- ments, except small and partial changes of elevation, can be traced in the peninsular formations of India, the whole of the gigantic forces, to which the contortion and folding of the Himalaya and the other extra-peninsular mountains are due, must have been exercised since eocene times. The sub-Himalayan beds were deposited upon uncontorted paleozoic rocks ; and although a part of the Himalayan area may have then been land, the direction of the ranges is clearly due to post-eocene disturbance. It has also been shown that the movement has been distributed over the tertiary, post-tertiary, and pleistocene periods. It has been suggested that upheaval still goes 1 on, as earthquakes are of common occurrence along the line of the Himalaya and as far westwards as Kabul. Three distinct shocks were felt at Kami Tal in April, 1880, and Srinagar in Garhwal was almost destroyed by a great earthquake in 1803. A recent traveller, 1 Professor Geikie on * Mountain architecture.’ 2 Manual of the Geology of India, Ivi. 102 HIMALAYAN DISTRICTS M. Severtsof, attributes the contraction of the great Kara-kul lake on the western Pamir to a similar cause, and says that the connection of the Tian-shan with the Pamir is due to an upheaval which geo- logically is of recent date and is still progressing. At the end of the cretaceous period and at the beginning of the tertiary period, the Tian-shan was separated from the Pamir by a strait with rocky islands, the marine deposits of which are found beyond the Tuz- Ashu pass. It is startling to the uninitiated to be told that the mighty mass of the Himalaya, as it now appears, is a forma- tion younger than the comparatively insignificant hills of the Dak- hin (Deccan) and Central India. The same, however, is said of the Alps, Pyrenees, Andes, and Rocky Mountains, all of which received their chief upheaval in tertiary times. According to Mr. Blandford it is probable that the crystalline „ . , axis of the western Himalaya which appa- Locene period. _ ^ 1 A rently terminates in the Dhauladhar peak, the western extremity of the snowy range seen from Simla, coin- cides with the shore of the ancient paleozoic continent of which the Indian peninsula formed a portion. If this be a correct view, the cis-Himalayan paleozoic rocks are in a great part of fresh water origin, whilst the marine paleozoic formations are found through- out the extreme north of the Panjab, Kashmir, and the neighbour- ing countries north of the Dhauladhar and crystalline axis. In eocene times, the peninsula of India was part of a great continent probably united with Africa. To the east was a great sea extend- ing up the Asam valley along the southern base of the (Taro hills and thence southward throughout a considerable area west of the Irawadi in Banna. There was another sea to the north-west cover- ing a great part, if not the whole, of Persia, Baluchistan, the Indus plain, and extending as far north-east as Grarhwal, and an arm of this sea extended up the Indus valley into Ladak. The Himalaya and perhaps Tibet, wholly or in part, were raised above the sea, but there is no evidence to show that they had then attained any un- usual elevation. In later eocene times, the Himalaya had risen sufficiently to send back the sea boundary to the north of the Panjab, and in miocene times, the marine area was still further contracted. The existence of a sea in these places is attested by the pre- sence of marine deposits and shells, and this discovery clearly shows OF THE NORTH-WESTERN PROVINCES. 103 that not only did the sites in which they occur once form the bot- tom of a sea but that the difference in height now observed between them and the level of the sea must be greatly added to in order to arrive at the true measure of the upheaval that has since occurred. The work of denudation that continually goes on shows us that the present summits of the mountains must in the course of time have lost a considerable portion of their substance, and in the next place we cannot suppose that the marine shells now found lay exactly at the sea level. The bed of the great sea may also have been subject to successive periods of depression and elevation before the eocene period without greatly altering its height. Professor Geikie 1 tells us what the forces are to which these marvellous results are due : — “The upheaval of the sea floor into land seems to have been due to a cause which has been going on from the earliest geological times and which is still in progress. It is believed that originally this planet possessed an enormously high temperature ; that, indeed, it was thrown off from its parent sun with a temperature probably even much fiercer than that of the sun at present ; and that it has since been gradually cooling and contracting. The external crust of the earth, varying greatly in structure and otherwise, has yielded unequally to the strain of contraction. One result of this process has been the elevation of portions here and there into long ridges, forming the continental masses and mountain chains. You may illustrate this production of lines of elevation along a generally subsiding surface by what takes place when an apple dries. Its surface contracts and wrinkles, most of the skin sinking inwards, but, at the same time, inequally and leaving intermediate ridges to stand up. So in the gradual contraction of our planet, wrinkles have arisen on its surface. It is these wrinkles which form our mountain chains. But such a subsidence of the crust could not have taken place without a very great deal of folding of the rocks. Descending nearer to the earth’s centre, the various layers of the crust had a less diameter to fill. They could only accommodate themselves to their new position by being crumpled up so as to occupy less space, or by being cracked across so as to allow some parts to be pushed above others.” We find that both these results have been produced, and the records of the Indian Geological Survey teem with illustrations of them. 104 HIMALAYAN DISTRICTS One other fact is noticed, by the same writer, in connection with Mode of mountain forma- the crumpling up of the mountains, and that tion - is that this process has been the means of bringing up the crystalline rocks. “ Before the time of the crump- ling, the whole future mountain area was covered with one continuous sheet of marine strata. But as the mountain chain began to form, the central portions came to be more and more compressed, puckered, and crystalline, some parts being squeezed up, whilst intrusive masses and veins of granite and other crystalline rocks were injected amongst the intensely altered strata along the central nucleus or core. It was during this process, doubtless, that the crystallisation of the gneisses and schists took place, w'hen they passed from their original character of fragmentary (bedded) rocks and assumed the peculiar crystalline texture which they now present.” We have already noticed that there have been successive upheavals of the Himalayan mass through the tertiary and post-tertiary and even the pleistocene periods, and the effect of these upheavals on the form of the mountain ranges must have been considerable. Supposing, with Professor Gfeikie, that a whole mass of sedimentary rocks has been upheaved into land as a mountain chain, we find that “on the outskirts of this elevated area, sedimentary deposits will continue to accumulate in the sea. If in the course of the slow secular contraction of the planet the upraised tract subsides, a new set of strata will be laid down upon the upturned edges of the older rocks. It is evident that in every junction of this kind, some considerable interval must have elapsed between the formation of the older series of rocks A (Fig* 4.) and the newer series B. Fig. 4. Section of a mountain chain showing three epochs of upheaval (Geikie). “In the course of time, the region having once yielded to the strain from terrestrial contraction will probably yield again, and a new upheaval will take place. The series B will now be raised up together with A, and another series C will be laid down in turn OF THE NORTH-WESTERN PROVINCES. 10& upon its edges. Subsequently, the same fate will befall the group C. These three sets of differently inclined strata would fix for us three successive periods of upheaval.” This simple explanation shows how very varying must be the results of successive periods of depression and upheaval, and especially when, as in the case of the Himalaya, such an immense area has been subject to disturbance. W e have now seen that the primary factor in mountain architecture are the great changes in the earth’s crust by which mountains have been formed, and the bedded deposits have become rocks, and eventually, as the process of upheaval went on, have been crumpled, folded, crystallised, and fractured. In this process, late- ral pressure has been the chief agent, and this has been exerted simultaneously from different sides in the case of the Himalaya, at least in the pleistocene period. No better examples can be given than those enumerated by Mr. Blandford as characteristic of the western area. Here we have amongst the mountain ridges that encircle the Indus plain and comprise pliocene beds, “ranges run- ning north and south such as the Khirthar and Sulaiman; east and west as the Mari and Bliugti and the Afridi hills ; north-west and south-east as the Pir Panjal ; north-east and south-west as the eastern Salt Range and Kharian hills ; and many intermediate directions may also be traced, independently of curved ridges.” Of the extent of these lateral thrusts an example will be found to the west of the Indus. Taking the Persian area and that of the Hima- laya and Tibet, “ the mountain ranges fall roughly into two great curves convex to the southward ; but the deeper western curve has produced the smaller mountain ranges. That a gigantic lateral movement has taken place in the apex of the western curve is, however, shown by the fact that for nearly 150 miles between Gwadar and Jalk in Baluchistan, the track traverses beds, all appa- rently of tertiary age, at right angles to their strike and that all these beds are vertical or nearly so. The contraction in breadth, or in other words, the lateral movement must have been great to have converted horizontal formations into a series of undulations, with dips so high as those seen in the Baluchistan ranges.” The terms at our disposal to denote the relations of magnitude and adequately to depict the changes that have been wrought during such a period are utterly insufficient to convey a correct idea of what has taken place. Perhaps 14 106 HIMALAYAN DISTRICTS Mountain sculpture. Ice-weclges. Professor Geikie’s simile of the dried apple is as far as we can go with- out entering into scientific details that belong to the professed geologist. Only second in importance to subterranean influence in the forma- tion of mountains are the sub-aerial tools of the great sculptor, the different forms of water, ice-wedges, glaciers, snow, rain, and rivers . 1 It is impossible to say what may have been the appearance of the mountain ranges when first formed, but we have every reason to believe that usually the process was gradual and that at once the denuding influence of the different forms of water came into play. Nature from the time the first atmosphere existed has ever been at work tracing lines which gradually work into gorges, ravines, and valleys, weathering- peaks and rounding ridges and producing those alterations in the general appearance of the mountains that on a very small scale are familiar to most of us in a neglected hill-station. Both crystalline and bedded rocks abound in joints or divisional planes by which they are separable into blocks and no small part of nature’s work in sculpturing moun- tains is thus rendered possible. Into these crevices runs the melted snow or rain, and there congeals and again expands, forcing the blocks asunder by slow degrees. The sun’s rays turn the ice into water during the day, to penetrate still further and again congeal during the night, and this ceaseless process continued for many centuries shows its effect in the form of the mountains composed of even the hardest rocks. These are covered with massive boulders quarried by nature’s ice-wedges in this simple fashion. Where the dislocation takes place near the edge of a weathered cliff, the mass of ruin caused by the toppling over of huge blocks is often gigantic. Gerard describes the upper portion of Purgial (Lio Porgyul) as the “wreck of some towering peak burst asunder by severe frost.” Fraser tells us that the summits near Gangotri and Jamnotri are a mere con- fused mass of huge crumbling boulders, and the same description applies to nearly all the peaks that have been visited by travellers. We have next to notice snow in the form of avalanches as one of the tools employed in mountain sculpture. The winter snow, when exposed to the summer Professor Tyndall's and Professor Avalanches. 1 Acknowledgment is due here to A.Gcikie's mountain architecture. OF THE NORTH-WESTERN PROVINCES. 107 sun and influenced also by the heat of the earth itself, is often de- tached in masses sufficient to cause great natural disturbances. It has been suggested that the change in the bed of the Satlaj in the plains to its present one has been produced by an avalanche in its upper course having dammed up the river. In time the barrier gave way and sent down an immense flood to the plains, sufficient to carve out a more direct course which the river itself has since continued to occupy. It is, however, to the action of snow in the form of glaciers that the more important results are due. These great engines of denudation have the form of a solid river ever progressing downwards through the valleys until the point is reached where the rate of motion is balanced by the melting of the ice. In the figure of the Pindari glacier, given hereafter, it will be seen that the glacier fills the bed of the upper valley and is fed by the drainage of the snow-covered slopes on either side. Its face is discoloured with mud and stones and is utterly unlike one’s preconceived idea of masses of ice. Along the sides and edges, too, are rows of earth, stones, and boulders trans- ported and deposited in order by the ice-stream. These deposits are called moraines. Much of the material transported falls down into the crevices and gets between the bottom of the glacier and the rocky bed along which it moves, and which is thus subjected to a grinding process that reduces even the hardest rocks to powder. This fact accounts for the turbid character of glacier streams, especially near their source. The influence of glaciers, therefore, is two-fold, firstly in transporting materials and secondly in reducing them to mud or sand. The combined result is often seen in the mass of detritus heaped up towards the end ot a glacier called a terminal moraine, and in the striated and smoothed appearance of the rocks that have been subjected to glacial action. As will be seen hereafter, there is sufficient evidence of a great extension of glacial action in former times that must have had a very important influence on the form of the mountains. Cunningham records three gieat inunda- tions of the Indus due to the bursting of glaciers in the upper por- tions of its course. These had dammed up the river bed and eventually gave way, sending a flood down the channel which in the cataclysm of June, 1841, appeared as a wall of water some 108 HIMALAYAN DISTRICTS thirty feet high, destroying every thing that came within its reach . 1 Rain has had even a more constant and penetrating influence on the mountain masses than any of the pre- Bain. J ceding forms, for it has furnished the ma- terials from which the ice has been formed and is more universal in its operations. The salts and acids contained in it have also had a peculiar action of their own. Rain while falling through the air takes up some portion of carbonic acid and when it reaches a rock dissolves and carries away certain portions of its texture. The result of this process is that not only is the rock reduced in bulk by chemical action but what remains also becomes more easily operated on by the mechanical action of falling water in the next shower. For illustrations of these processes take any line along the lime- stone ridges about the hill sanitaria already mentioned, and it will be seen how the outer crust where exposed is crumbly to the touch, and has a rough sandy appearance. For those who have seen the long gneissic range extending from Almora to Devi Dhura in Kumaon, there could not be a better example of the influence of rain or rock than is there exhibited. Along the road on each side where the rock has been exposed to the weather, the outer layer is removable by the hand, and at the base will be found a little heap of sand that has been weathered away in course of time. Many of the more loosely formed shales, especially those that contain alum, speedily decompose on exposure to the atmosphere and it is on this account that in the midst of rocky formations in the Himalaya it is so often very difficult to obtain good building stone. Another familiar example of the influence of the rain-fall on the rocks will be seen in the stones of old buildings throughout the hills. Where protected from the weather their surface exhibits the faintest trace of the graver s tool intact, but where exposed they are worn and eaten into and the outer skin appears granulated and rough. This waste of rock material has been in progress for centuries and has produced a soil in which trees have taken root and shed their leaves to pioduce by decomposition and mixture with the waste the rich vegetable mould that overlies our forest-clad hills. The presence of these tiees has had the further effect of retarding the removal of 1 Laclak, 104 : J. A. S. Ben. X. 017 : XII. 183 : XVII. 230. OF THE NORTH-WESTERN PROVINCES. 109 the newly formed soil not only by absorbing a portion of the chemi- cal elements carried down by the rain-water, but also by breaking the force with which the rain would otherwise fall on the soft soil. Thus we find that on well wooded hills the depth of useful soil is considerable and that springs are numerous and abundant. On the other hand where the hills have been cleared of forests, the finer soils are soon washed away by the almost tropical rain. The rocks from which the soil has been formed again appear at the surface and the rainfall rapidly drains off leaving no supply for springs, and if the process be continued over any considerable area, cultivation becomes impossible and the climate is essentially altered. What de- foresting has done for Almora can be seen in its scanty rain-fall, its barren slopes, and few springs, although the area affected is so small. The action of a river in the sculpture of mountains is three-fold. First, it has the chemical action of rain in dis- solving portions of rock constituents : again, it has in its mountain course the grinding power of the glacier in the force with which it drives the gravel, stones, and boulders along its rocky bed : and thirdly, it has the glacier function of transporting material and laying them down in deposits elsewhere. In the case of glaciers the denuding process is the more important, and in the case of rivers the transporting function has, perhaps, more influence in mould- in o- the features of the surrounding country. In the beds of many of our mountain streams we can detect the action of both glaciers and rivers in the striated and furrowed appearances produced by the former and the rounded forms of worn pebbles due to the influence of flowing water. The muddy colour of the water is due to mud or sand held in suspension, and it has been estimated that in this way one six- thousandth part of a foot is annually carried away from the water-shed of a great river. This waste is, however, very unequally distributed, being very much greater in slopes and valleys and less in plains. “We may be prepared, therefore,” with Professor Geikie, “ to find that solely by the continued erosion of running water, even the most recently up- lieaved mountain chains have had stupendous chasms carved out of their sides, and an almost incredible amount of material removed from their surface.” Such has been the origin of the Scottish valleys which, according to the same writer, “ have been cut out of the general mass of the upraised rock. The existing mountains are no HIMALAYAN DISTRICTS OF THE N.-W. PROVINCES. what we now find them to be, because they have been left standing while the valleys have been excavated among them.” Playfair in his “ Illustrations of the Huttonian Theory,” as quoted by the same author, writes : — u If indeed a river consisted of a single stream without branches, running in a straight valley, it might be supposed that some great concussion, or some powerful torrent, had opened at once the channel by which its waters are conducted to the ocean; but when the usual form of a river is considered, the trunk divided into many branches, and then again subdivided into an infinity of smaller ramifications, it becomes strongly impressed upon the mind that all these channels have been cut by the waters themselves ; that they have been slowly dug out by the washing and erosion of the land; and that it is by the repeated touches of the same instrument that this curious assemblage of lines has been engraved so deeply on the surface of the globe.” In major and minor river systems the same principle is observed ; the lines marking the tributaries of a stream appear like the veins of a leaf all converging on the mid-rib and each forming within its own area a separate main line of a smaller system until the differences are inappreciable. But it may be asked why, if these influences are uniform in their action, the results are so varied. The answer is not far to seek and is to be found in the varied character of the materials on which the aerial forces operate. The southern flank of the Siwaliks below Dehra, consisting of soft sandstones, are weathered by the heavy monsoon rains until they are almost perpendicular. The Krol limestones give their picturesque outline to the outer Himalaya, when compared with the other lower ranges. The shales and slates have a character of their own, and the great crystalline range itself owes its form to the rocks of which it is composed. Kamet has its peculiar pyramidal shape from its cap of granite, and Nanda Devi, Trisfd, and the Panch Chilli have had their peaks defined by simple aerial action on their materials. Thus, our mountain ranges are due in the first place to subterranean disturb- ances, and in the second place, to the action of the different forms of water, chemically and mechanically, on the varied materials of which the rocks are composed. It is the combination of these two forces that gives such varied results, and until more accurate and compre- hensive information is recorded regarding their operation, it is impos- sible to base our physical description on other than arbitrary grounds. ■ I CHAPTER III. Geology. 1 CONTENTS. Position of the ground. Early observers : Herbert, Cautley, Falconer. The mountain system. The sub-Himalayan zone formed of tertiary rocks. Siwaliks. Post-tertiary deposits. Supposed glacial deposits. Lower Himalayan region. Simla region. Sirmur formation, ltelation of Sirmur and Siwalik series, the Satlaj valley. East of Simla. The Kumaon section. The Nepal section. Sikkim section. Slight correspondence between the rocks of the Himalaya and of the Peninsula. Frequent occurrence of carbonaceous deposits throughout the Lower Himalaya. Conjectural affiliation of the Lower Himalayan sections, i he Cent] al Himalaya. Strachey. Stoliekza. Western Tibet. The principal crystalline areas. Nunimu- lilic deposits. Post-eocene eruptive rocks. Central gneiss. Kaslimir-Kishtwar region. Central Tibet, Its granites, schists, slates, conglomerates and fossiliferous fco- Position of the ground. rocks. Palaeozoic strata, Silurian, Trias, Jurassic. Fossils. Tertiary deposits, called Niti fossils. General Stracliey’s conclusions. Stolickza's views. The British Himalayan districts, which form the immediate subject of this sketch, are themselves such a small portion of the immense geological region to which they belong, that we shall have to wander consider- ably beyond their limits to attain some idea of their place in nature. Some of the ground forms part of one of the best known, and certainly the most widely known, ot our Indian rock-tor illations . the Dehra Dun is pre-eminently the Dun ; and the low hills sepa- ratum it from the wide Gangetic plains are the original Siwaliks, a name to be found in every geological text book. The rocks ot the higher hills to the north, below the snowy range, have as yet received only cursory attention, being chiefly non-lossi I iterous slates and crys- talline schists. On the snowy range and beyond it in Chinese territory we again come upon formations ot well-established position, but ot which we have little real knowledge, and are altogether dependent upon the occasional observations of a few adventurous explorers. In geology, no less than in other sciences, it is desirable to be able to trace the stages of knowledge. Even in descriptive geology this information is interesting ; and for the student such illustrations are almost essen- tial. Although the germinal idea of geology, that the aboriginal i This chapter has been written by Mr. H. B. Medlieott, Superintendent of the Geological Survey of India, for this volume. E. 1. A. Early observers. 112 HIMALAYAN DISTRICTS superposition of sedimentary deposits is a sure indication of succes- sion in time of formation, and hence that the structural relations of rocks are the ultimate criterion of age, had to be conceived before geology could have birth. The difficulty of applying this test, of observing obscure and scattered outcrops, and of putting together and discussing the features thus laboriously collected, is so great, that, from the beginning, geologists have sought for, and adopted more ready tests for the chronological classification of rocks. The history of progress in geology is in great measure made up of the failures of generalisations thus too hastily arrived at ; the total breakdown of false assumptions, and the correction of errors due to the forced application of partially understood principles ; to the neglect of the regulating laws of structure. The science is so young that its history in India affords examples of these errors. In some cases our admiration of the men and the work they accomplished is positively enhanced by our knowledge of the difficulties under which they laboured. The names Herbert, Falconer, Cautley, and Strachey call especially for mention in connection with the around under notice. Cautley and Falconer will be imperishably associated with the paleontological branch of geology, as having with great labour brought together the unrivalled collection of fossils, the description of which was partially published in the Fauna Antiqua Sivalensis. Work of this kind endures, in so far as it is to a great extent a record of hard facts, having each a permanent interest, such as the existence of a certain fossil within a fixed rano-e of o strata. It is not so with facts of the first order in geology proper i the announcement that such a kind of stone occurs in any particular place conveys no information that can be said to have scientific value ; it is only when accumulated and colligated under established principles of formation that such petrographical facts come to have any geological meaning. Herbert’s observations were of this order. He dealt entirely with unfossiliferous rocks, and the principles under which he had to arrange those observations were still to a great extent artificial ; his work has therefore only an historical interest. Captain G. H. Herbert, however, must rank in merit as well as Herbert. date amongst the foremost pioneers of geo- ffigy in India. As a man of great talent and of sound and extensive scientific culture, he may stand with Captain OF THE NORTH-WESTERN PROVINCES. 113 Newbold, who did so much for the geology of Southern India. The advantage of the latter lay in the greater simplicity of the ground he worked in and in his being even a few years later in the field. The mineralogical survey of the Himalayan districts was one of the earliest attempts at a geological map of a considerable area made officially in India. The work was entrusted to Captain Herbert by the Marquis of Hastings ; but it was left to private enterprise to make known the results. The publication was taken up by Mr. Henry Torrens, of the Bengal Civil Service, the accomplished editor and proprietor of the so-called Journal of the Asiatic Society of Bengal, which was then brought out at the personal risk and responsibility of the Society’s Secretary, and was really the continuation of the publication started by Captain Herbert himself in 1829 with the more appropriate title (under such conditions) of Gleanings in Science. The report appeared as an extra number of volume XI. of the Journal for 1842, nine years after the death of Captain Herbert, and seventeen years after the completion of the survey. The map to illustrate the report was issued with volume XIII. for 1844. It comprises the very large area lying between the river Kali and Satlaj, more than 200 miles in length, and from the plains to beyond the snowy peaks, a breadth of 90 miles. Captain Herbert does not assume any pretensions to authority. He tells us very plainly that he made up his geology for the occasion, but it is plain, too, from his obser- II is geological theories. . a , . ,, , , ,, - - vations and reflections, that fie thoroughly mastered his authors. His suggestions in correction of current views are often very judicious, and display a truly scientific turn of mind. His work, nevertheless, can only be noticed in illustration of the history of Indian geology. He divides all the rocks of the mountains into two great 1 primary ’ formations — one for the gneiss occupying the central region, and one for the micaceous, chloritic, hornblendic, and argillaceous schists, to which also hq, joins the limestones. He makes a third zone of the narrow strip of “ secondary rocks, mostly, if not entirely, the Newer Red, or Saliferous Sandstone.” On the strength of this purely imaginary identification borings were recom- mended, if not actually undertaken, along the margin of the plains, to find the carboniferous formation with its coal. This notion was not quite exploded by the discovery of the famous tertiary fauna in a part of the rocks designated by Herbert as New Red Sandstone ; 15 114 HIMALAYAN DISTRICTS and by the latest writers, prior to the Geological Survey, the sand- stone along the fringe of the Kumaon mountains, and now known as the Nahan or lower Siwalik group, are treated as secondary. The constant dip of the rocks of the southern Himalaya towards the central axis, so marked a feature in their structure, was treated by Herbert in a manner characteristic of the times. His three forma- tions being by assumption successive in order of time, the observed structure seemed to subvert this ordained relation, making the younger apparently pass beneath the older, the schists beneath the gneiss, and the sandstones beneath the schists. He attempted first to explain this anomalous feature by faulting ; but when his cal- culations seemed to demand a fault having a throw of eight miles, he gave up the idea in favour of a supposition infinitely more extravagant. He came to the conclusion that the apparent bed- dins in each of his three series is not true stratification, due to the process of deposition in water, but only pseudo-stratification, produced by some process of concretionary action ; thus, for the sake of a collateral issue, he cut away the very foundations of the science of geology. The work of Cautley and Falconer was the geological converse of that attempted by Herbert. They dealt Cautley and Falconer. . entirely with one series ot rocks, and treated them almost exclusively from the point of view of their fossil contents. The range of their operations was limited to the low fringing hills between the Ganges and the Satlaj. The structural features w r ere very slightly touched upon, the strata being taken to belong to one unbroken formation, which was recognised as of geologically recent date, and as being distinctly made up of the debris of the Himalaya. The following abstract list of fossils will give an idea of the extent of their labours, and of the richness of the fauna they discovered : — * SIWALIK FOSSIL VERTEBRATES. Quadrumana. Semnopithecus , Pithecus. Carnivora. Hycena, Amphicyon, Hyamarctos, Canis, Mellivora, Fells,, Drepanodon, Lutra , Enhydriodon, jpRGY fj [, S’ -- r / ) j/\ a 4SRMV&>.Oi€pi«J f *0« .jferv' ■ > ii r «.. ; 4»i: i*P- •,.^V^ "oSsh- 1 ^- ooKto/fi.oo^rj, / rom/ 16 . ■ ’•// V\V I A - .■>( \ . V ' oiinViq . \ V 'l PPM W/////////7/A ; .zUigclyepmj/,..^, \ ' / Mgy 7 ■ sfs StS®0®llSw .\ HU/w>iii(rn/ iSfeS?? t^ ; C ,W I ^JfflTspMapha ■s^jV jihlfancLsanotyt \ijti§/X 15,200 \mr« Bb^ ■ v.r,;A JL ;•%■• , . V- >/U/-/'' V ^ ’ v,,,;- 1 p—*, > ' 10MgR(fe3 / / r'J'FUWWWyfflw/ ■^w^G^scfSdm ms s&Y?. •fyih4.'6t°i mmmm Fatia. 1 ; ^taua# V J ' , ' : //f 9U^ I : / ' . «|| 1 fSlIgl Mar-tfvv’i opod>4 mTJo IOOO' Thaa\e s aa? Sililtf •■•‘i. - ■ - baruliX-n) "Roorkee. ft Hi a ;1,;^V^ §£<#xfa,ooo fr-Yfi'-'-v \ Kotdyvcuu fl.ZOO flslp S’XsSc^ £%%% : NA.JIBA BAD A) huiiajziiQt 1.800 sgasSft/l «§* B1JN OR CbaM cLyaS o~j \ Ka-shipiir' £/“> 730 Ewctr£i/| ^ <> ^JQxoT'Qo2i\ \s2j£WMi MERA NcuTwCkrruUhou lAmrohd ORABABAD 610 >RA mpu: 550 0 UL1BH1T 5 550 DELHI Six*itind REFERENCES. upper and middle Tertiary Lower Tertiary Mezozoic Talceozoic Azoic Slates Crystalline Schists Gneiss and Granite Greenstone X; OUTLINE GEOLOGICAL MAP of Part of the HIMALAYA MOUNTAINS English Miles 2.0 30 40 NOTE NOTE The Crystalline Schists of the outer hills have a fringing' zone of less al- tered rocks, some of which have been doubtfully recognised asTriassic. The Schists are in part formed of the same formations metamorphosed. Reproduced, with slight corrections from the map published by Captain R. Strachev. R. E., in 1851 in the Ii Joul-nal of the Geological Society of L London. O U D LITHOGRAPHED IN COLORS AT THE SURVEYOR GENERAL’S OFFICE, CALCUTTA, FEBRUARY 1876, For E. T. Atkinson Esq., in charge of the N. W. P. Gazetteer. OF THE WORTH-WESTERN PROVINCES.. 115 Proboscidia. Stegodon (4 sp.), Loxodon (1 sp.), Enelephas, Mastodon (2 sp.), Dinotherium (sp.). Artiodactyla. Hexaprotodon , Merycopotamus, Hippohyus, Sits, Chalicotherium , Sivatherium, Antilope , Cervus (sp.), Camelopardalis, Camelus , Bos (sp.), Hemibos, Amphibos. Perissodactyla. Rhinoceros (3 sp.), Antoletlierium, Equus, Hippotherium. Reptilia. Crocodilus, Leptorhynchus, Varanus , Colossockelys, Emys, Trionyx, Testudo. Undetermined species of Aves, Pisces, Mollusca and Crustacea. It is to Captain Richard Strachey, of the Bengal Engineers, now General Strachey, Member of the India Council, that we owe the first sound attempt at a sketch of Himalayan geology based upon extensive observation. An abstract of his results was published in the Quarterly Journal of the Geological Society of London for November, 1851, and the map accompanying his paper includes about the same ground as that of Herbert. A comparison of the two maps shows how great an advance had been made. It is greatly to be regretted that official and other business prevents General Strachey from making with his own hand the few corrections and additions necessary to bring his work up to date for the present publication. The annexed map is little more than a reproduction of General Strachey’s, and the description also of a large portion of the ground is a reprint of his paper. 1 Acknowledgment is made by him that a considerable portion of the observations recorded were contributed by his brother, now Sir John Strachey, late Lieutenant-Governor of these provinces. ' . v For the geographer a mountain chain is fixed by the conditions of continuity and direction. The geologist would fain make his mountain systems to 1 On the Geology of Part of the Himalaya Mountains and Tibet : Quar, Jour.,. Geol. Soc., London, for November, 1851, Vol. VII. — E. T. A. The mountain system. 116 HIMALAYAN DISTRICTS depend primarily upon contemporaneity of formation, as suggesting causal connection. From neither point of view can the Himalaya pretend to fixity of limits. On the south, indeed, no great physical boundary could be more marked than the base of the mountains between the Jhelum on the west and the Bramaputra on the east, a distance of about 1,500 miles. The line is remarkably unbroken, without projecting spurs or open re-entering valleys. It has a uniform curve, the bearing in Upper Asam being to east by north, while in the Panjab it is nearly to north-west. Throughout this entire length the hills rise abruptly from the alluvial plains. The terminations of this boundary are also very well marked. The Asam valley ends against the ranges of the Barma-Malayan mountains, which pass up from the south, at right angles to the Himalayan chain, to coalesce with it in the elevated regions of Eastern Tibet. Similarly on the north-west the ranges of the Suliman and Hindu Kush pass continuously into the mountain region of Little Tibet, nearly at right angles to the run of the north-west Himalaya. It is on the north that the question of a physical boundary is to a great extent arbitrary. The chain of mountains that, under the name of Himalaya, forms the northern boundary of Hindustan, is in reality the southern face of the great mass of elevated land extending through nearly 30 degrees of longitude, from the sources of the Oxus to those of the great rivers of China, while its northern face appears upon our maps as the range called Kuenluen. To the south lie the plains of India, whose greatest elevation is about 1,000 feet above the sea; while on the north is the Central Asiatic desert, which nowhere is at a less altitude than 3,000 feet. The loftiest summits known on the surface of the earth are to be found towards the southern edge of this elevated region, at least one peak having been measured whose height is upwards of 29,000 feet, while along the whole line peaks of 20,000 feet abound. So little is known of the interior and northern parts of this region that it is impossible to offer any general account of it based upon actual observation ; but as far as we may judge from those parts that h<.i\ e been exploied, it appears that the surface is, with few excep- Tibetan plateau. tions, broken up into a mass of mountains, the general elevation of which, valleys as well as ridges, is very great ; and there seems no reason for supposing OF THE NORTH-WESTERN PROVINCES. 117 that either the Himalayan or Kuenluen have any definite special existence as mountain ranges apart from the general elevated mass of which they appear to be the two opposite faces. The portion of the southern chain to which the following description more particu- larly refers, is somewhat to the west of a central line, on about the 80th degree of east longitude, which meridian passes through the island of Ceylon, and not far from Cape Comorin. The order of notice will be in successive zones from south to north — the plains, the Sub-Himalayan zone, the Outer or Lower Himalaya, and the Central Himalaya. While difference of opinion exists as to the formation of the most recent deposits, it is not to be wondered at The plains. that there is often much doubt as to the origin of ancient formations. The primitive idea that a water-basin is necessary to the accumulation of extensive sedimentary deposits is still widely held. To it is primarily due the not yet obsolete opinion that the plains of India are in great part of marine origin. The only direct evidence in support of this vieAv is the local occurrence of salt- wells, which also involves a popular error, for although the sea is the great receptacle of salt, it is chiefly by rock-decomposition on dry land that salts originate. This fact is likely to force itself disagree- ably upon future generations in India ; at present we have only to do. with it as at least weakening a mistaken geological position. The only fossil remains found in these plains-deposits are of land or fresh water oriffin, and these occur even in the delta below the present sea level. The surface-form, and the distribution of the materials of these deposits, is, moreover, just what is now understood to be due to the normal action of rivers above their final point of discharge. T orrents, streams and rain-scour from the precipitous slopes have accumulated a wide bank of coarse diluvial deposits along the base of the mountains which is known in these provinces as the bhd- bar or forest zone. In Rohilkhand it is about ten miles wide, and has a fall of from fifty to seventeen feet per mile, and, except in the rainy season, water is not procurable in it. Even considerable streams sink into the porous [L'a vd l gravel-beds. Outside the bheibar is the tarcii, also about ten miles wide, in which water is superabundant, 118 HIMALAYAN DISTRICTS producing swamps and excessive moisture. Formerly it was supposed that this was an area of actual depression ; it has, however, a very considerable fall, averaging (in Rohilkhand) more than ten feet in a mile. The moisture is due to the copious re-appearance of the water absorbed at the head of the bhdbar. From the tardi the plains gradually decrease in slope to three or four inches per mile in the deltaic regions. A belt of fringing ridges, varying in width and abruptly lower than the contiguous mass of the Himalaya, The Sub-Himalayan or ® J ’ Siwalik zone, formed of occurs throughout their entire length, with J perhaps two short interruptions m Lower Asam, which are doubtfully and in part attributed to denudation. The pure geographer might, in some places, ignore this feature, as perhaps below Nairn Tal and Darjeeling, choosing to regard its representative there as mere spurs of the mountains. Geological observation, however, draws attention to geographical features that might otherwise escape notice, and notes that these so-called spurs will always be found affecting the form, not of spurs proper, but of ridges parallel to the adjoining mountains, and in a more or less marked degree semi-detached from them by a chain of deep longitu- dinal gorges and low gaps, corresponding with a leading geological boundary, that between the old slaty and schistose rocks of the mountains and the massive tertiary sandstones of these fringing hills. From this double consideration the name Sub-Himalaya has Divisions of the terti- been g iven to these lower ranges and to ary senes. the rock-series forming them. For the most part these hills are apparent to the least observant traveller, their outer ranges being separated from the inner ones by broad flat valleys, or duns. These more detached ridges have long been familiarly called Siwaliks, a name extended by Cautley from the native name (Shib-wala) of the representative range separating the Dehra Dun from the plains. This name, too, has been hitherto currently applied to the hills and rocks here described as Sub- Himalayan, wherever distinctly recognised. The closer study of this zone has, however, brought to light distinctions involving some difficulties regarding the application of this familiar name. It has been found that there are recognisable divisions in this great series OF THE NORTH-WESTERN PROVINCES. 119 •of the tertiary deposits of the Sub-Himalayan hills, and that the younger of these groups contains by far the largest share (if not all) of the well known Siwalik fossils. On this account it was proposed to restrict the name Siwalik to the band in which those fossils occur ; but there are good reasons for preferring to con- tinue the extension of the old name, and to indicate the separable geological horizons as Upper, Middle, and Lower Siwaliks. On the small map annexed they are coloured together as upper tertiary. It was in the ground west of the Jumna, between the Kayarda Supposed key section of and Pinjor duns, where the outer and inner unconformable groups. bills are confluent for a length of about forty miles, that the separation of the original Siwalik series into distinct groups was first brought to notice. Throughout the whole cross-section the dip of the strata is inwards, towards the moun- tains ; but along a sharply marked line, continuous through the length of these hills, there is a junction of highly contrasting rocks : the brown and yellow clays, and conglomeratic gravels at the top of the series forming the outer zones of low hills, abut against harder red clays and sandstones forming an inner zone of somewhat higher hills. The feature is nowhere better seen than in the region of the Markanda, south of the town of Nahan, the capital of Sirmur. As is generally the case along the junction of rocks of very different textures, the actual surface of contact is concealed by debris ; and the appearance suggested by the conformable dips is that the outer rocks pass regularly beneath the inner ones. Such was the view tacitly adopted by the discoverers of the Overlooked by early Fauna Sivalensis. It was from the same observers. trans-Jumna region, south of ISTahan and of this rock-junction, that a very large proportion of the great Siwalik fossils were procured. No particular notice was taken of the striking feature just described ; and Cautley accounted for the absence to the east of the Jtunna of the highly fossilifer- ous beds known to the west, by supposing a lesser upheave- ment of the ground to have occurred in that direction ; thus dis- tinctly implying that those beds underlie and are older than the rocks of the cis- Jumna Siwalik range, which he had himself, 120 HIMA'LAYAN DISTRICTS from fossil and petrological evidence, identified with the rocks at Nahan. Herbert’s deliberate' rejection of the elementary fact of stratifi- Nature of the uncon- cation, to make way for a theoretical diffi- foimity. culty, is scarcely a less remarkable date- mark than the ignoring of so striking a stratigraphical feature by the original explorers of the Siwaliks. The facies of the two con- trasting groups, as seen along the boundary, at once suggest that the outer and apparently underlying rocks are really the younger, and this is immediately confirmed by finding that the conglome- rates of this group are principally made up of the debris of the contiguous inner strata. Although this latter fact would be some- what against the supposition, the steep abutting rock-junction would next suggest a fault, along which the lower strata were upheaved on the north, and thus brought into contact with younger beds of the same series. Patient search, however, revealed an exposed section of the actual contact showing the relation of the strata to be quite different from that implied by faulting. The con- glomerates were found to rest against a denuded surface of the older group of rocks ; the junction being in fact that of an original steep edge of deposition to which an actually overhanging, inverted pitch had been given at many points by subsequent lateral compres- sion. The feature, as thus described, involves much more than simple successive deposition of the groups. It ex- First inferences from it. ..... . „ .. . . „ mbits strong unconformity between them, requiring the older group to have been upraised and deeply denuded before and during the formation of the younger one. Such a relation generally implies a considerable break and lapse of time between the formations, with a corresponding change in their fossil fauna. It is precisely the history of such changes which it is the business of geology to unfold. But to the unfortunate neglect of the simplest stratigraphical observations, fossils from both groups were mixed together in the magnificent collection that lay ready to the hand of the early discoverers. On account of the character and extent of this stratigraphical feature, suggesting that an unconformity of such depth must have a very wide range, it was proposed by the first observer of it to restrict the name Siwalik to the younger formation, and to designate OF THE NORTH-WESTERN PROVINCES. 121 the older rocks, of the inner zone, as the Nahan group. It is the name by which Cautley identified a certain horizon in the series, although apparently assigning to it a position the reverse of the correct one. Corrected view. Large as is the gap absolutely required between the ages of the beds actually in contact along this boundary, it was matter of surprise from the first that no trace of so great an unconformity could be found in the immense thickness of deposits to the south of it. From the conglomerates at the junction, southwards to the plains, one crosses a descending section of several thousands of feet of strata without a trace of unconformity : showing either that even at the base of this section the beds of the Nahan group are not represented, or that the dis- turbance which produced the unconformity along this line of abrupt contact was of such a nature as to admit of continuous deposition within so very short a distance. Ruling ideas at the time were certainly against the latter supposition, that extended observation seems to confirm it. Going westwards along the Pinjor Dun, we find at the Satlaj, on the very strike and extension of the Nahan range, a continuous conformable sequence from the beds of the Nahan horizon into the softer sandstones, clays and conglomerates at the top of the series. The line of disturbance which in the Nahan region resulted in a denuded scarp against which the topmost beds were deposited by overlap, produced in the Satlaj region an anticlinal flexure which must have been so gradually evolved that the deposits accumulating along its southern base were sensibly conformable throughout, although now we find the uppermost conglomerates almost vertical, with a southerly underlie, at the edge of the Dun. Thus it is evident that a well-defined break is not a general feature in the Sub-Himalayan rock-series, and that it would be premature so far to sever such a portion of it by a separate name from the time- honoured Siwaliks. The name Nahan is already current in print and may at present be understood to indicate lower Siwalik rocks. It is important, however, to point out that the real inference from the unconformable junction is of more interest than the primd facie one ; without it we should not have had distinct proof that slow disturbance of great amount took place in the Sub-Himalayan zone during the formation of the Siwalik deposits. 10 122 HIMALAYAN DISTRICTS Although the marked separation of groups suggested by the peculiar feature of the hills between the Kayarda and Pinjor duns A division maintained is not maintainable westwards, there is a uni- the rocks and fossils : up- through the character of f orm jty 0 f change throughout the series from per Siwaliks. base to top whereby approximate horizons are assignable. Conglomerates and gravels prevail at the top, variably associated with brown sandy clays. In many clear sections the thickness is quite 4,000 to 5,000 feet. It is not, however, to be understood that the deposits were ever strictly superimposed to that depth vertically. The mode of deposition in successive banks, each trailing upon and thinning out beyond its predecessor, as pointed out above for the section on the Satlaj, must greatly modify the familiar meaning of the word thickness as regards space ; although where such deposits become tilted up by lateral pressure, and exposed along a comparatively shallow section, the appearance is quite the same as if vertical superposition of the whole series had obtained. Nevertheless, as regards time , the fullest thickness must be taken into account, for each bed is truly successive to that below it. Even when raised to the vertical, those upper Siwalik strata have so fresh an appearance as to be scarcely distinguishable from the most recent deposits — from the beds of the torrent shingle or of sandy alluvium now accumulating in the duns or on the plains. The complete justification for their distinction as an upper Siwalik group is found in the few fossils they have yielded, some of which, as Buhalus paloeindicus , would connect them with the pleistocene deposits of the Narbada valley rather than with the pliocene Siwaliks. The main fossiliferous zone of the Siwalik series constantly Middle Siwaliks. occurs beneath the thick mass of deposits noticed in the last paragraph, and it has a fairly characteristic rock-facies of its own. Massive, clear, gray; soft sandstone is decidedly the prevailing rock ; but brightly tinted clays are also often in great force. The large vertebrate remains, although mostly found in sandstone, are certainly more abundant where there are associated clays. Several thousand feet of thickness must also be assigned to this middle Siwalik group. Falconer con- sidered this Siwalik fauna to be miocene, but pakeontologists are now decidedly in favour of its pliocene affinities. OF THE NORTH-WESTERN PROVINCES. 123 In conformable sequence beneath the fossiliferous zone we find Nahan or lower Siwalik. rocks of the same type, but having a decid- edly different aspect — strong sandstones, but of a darker hue, and often highly indurated, with hard clays generally of a deep red or purple colour. Throughout the Himala- yan range, east of the Satlaj, they form the flanking ridges close under the higher mountains, and inside the duns ; or at least they mostly occupy that position, for it cannot be said that middle Siwa- lik beds do not occur there too, as will be seen from the remarks upon structure. No fossils can be quoted from those beds, but it is believed that some existed in the original Siwalik collections. They would probably be of miocene age. One of the most interesting features in these Siwalik deposits is Horizontal variations the variation they exhibit in relation to the in the Siwalik deposits. position of the great river-gorges. This is most marked in the case of the upper portion of the series. The accumulation of coarse conglomerates is immensely greater in the immediate vicinity of the large rivers of the Himalayan system, and, moreover, it is only within the range of those streams that we find the beds of large rounded blocks of quartzite and other hard locks such as are now brought down by those great torrents. In the intervals between the rivers such congl omerates as occur are formed almost exclusively of the debris of the adjoining hills, the same as are found in the minor streams now flowing from those hills; but in this position sandy clays often form the bulk of the formation. The same influence is observable in the middle group of the series, which is often conglomeratic and gravelly, or almost exclusively sandy, near the main rivers, while away from them the clays are often in great force. These facts are very observable at the Satlaj ; in the gorge above Bubhor the whole of the upper group is coarsely con- oiomeratic, and the middle one is more or less pebbly throughout, while at seven miles to the north-west the brown sandy clays, in which the fossil huhalus and camelus were found, form three-fourths of the entire thickness of the upper group. The apparent exception in the case of the Jumna is even a more marked illustration of the fact under notice. The river now flows through the Siwalik range at many miles to the west of the gorge, where it leaves the moun- tains; the fact being that in the elevation of the outer range the 124 HIMALAYAN DISTRICTS Jumna could not erode a passage through the great accumulation of conglomerates it had formerly discharged in front of that gorge, and which now form the highest summit of the outer range. It had to work round them not in the direction of its near neighbour the Granges, hut towards the region of lesser deposition. Thus the con- trast between the Siwalik strata to the east and west of the actual river-passage is so great that it has been questioned if the formations can really he the same. To the east the upper group is made of the hard shingle conglomerates, while on the same strike to the w r est the conglomerates are composed of local, principally lower Siwalik, debris. In the cis-Jumna Siwaliks the middle group is formed of thick masses of soft sandstones that have yielded very few fossils, while to the west clays occur largely on the same horizon, and fossils abound. The facts indicated in this paragraph are of great importance, as bearing upon the question of the mountain-formation ; showing, as they clearly do, that although these deposits, to a thickness of 8,000 to 10,000 feet, are now in many places turned up to ' the vertical, and even in- verted, yet the main features of the higher mountains must have been during the Siwalik period sensibly similar to what they are now. So far we have briefly considered the original characters of the structure of the Siwalik Siwalik strata : it is necessary now to notice rocks - the features induced by disturbance. This has taken place on the grandest scale. On the right bank of the Ganges above Hard war the gray sandstones of the middle group have a high southerly dip ; and this rises gradually, through an enormous thickness of strata, to a nearly vertical underlie in the conglomerates at the outer edge of the range. A section of the same type is splendidly exposed in the gorge of the Satlaj above Bubhor, in -the second range of the Sub-Himalayan hills. There is much method in the form of these flexures : they very generally affect the form known as normal , i. e., bends in which the dip is greater on one side of the axis, and so called because of more com- mon occurrence than the symmetrical flexure — when both dips are equal — or than the folded flexure, in which the strata on the side of the steeper dip have been pushed beyond the vertical, and so partially inverted. As an almost universal rule in this region, the OF THE NORTH-WESTERN PROVINCES. 125 steep side of these normal anticlinal flexures is turned from the mountains. From this there results the familar conformation of the Sub-Himalayan hills, presenting a scarped face to the plains and a long' slope towards the interior valley. These duns, or at least the flat longitudinal valleys which are the typical duns, are thus struc- tural features, not mere valleys of denudation ; they rest upon the comparatively little disturbed strata in the hollow of the synclinal flexure. The range separating the dun from the plains is formed by the anticlinal, the steep (outer) limb of which is generally broken up and denuded away, hence the south face of the range presents the scarped outcrop of the beds on the north side of the axis of flexure. In the inner ranges, where the disturbing action was greater, The Nun under Mus- the normal flexure often becomes folded, sooree - with, of course, inversion of the strata. There is an instance of this fairly seen in the Nun stream under Mussooree : below the narrow gorge, through massive sandstones having a steep northerly underlie, there is a continuous section in the low banks showing the sandstone becoming pebbly, then interbedded with thin conglomerates, then with thicker and coarser beds, all having the same high northerly dip. This is undoubtedly an ascending section though apparently, according to the dip, it is a descending one, i.e., the whole series is inverted. To any one who has understood these simple explanations, it will be apparent that if these conglomerates are upper Siwalik, and unless there is a fault somewhere about the mouth of the Nun gorge, the inner Sub-Himalayan range under Mussooree must be in great part made up of middle Siwalik, and not of Nahan beds ; and indeed their character would support that view. If these conglomerates of the Nun are not upper Siwalik they would form a new sub-division of the Nahan group, which could then hardly be classed as lower Siwalik. Similar conglomer- ates have lately been observed in this inner Sub-Himalayan zone east of Naini Tab It is however to be remarked that these folded flexures often are attended by great faulting, on such a scale that all appearance of flexure is lost and we only find a section of upper Siwaliks dipping against, and apparently passing under, beds of the Nahan type. There are several grand instances of such faults in the broad area of Sub-Himalayan rocks beyond the Satlaj in the Kangra 126 HIMALAYAN DISTRICTS region and on through the Jamu hills. They run quite straight or in very open curves for several scores of miles, and as the dislo- cation lessens, the unfaulted flexure is gradually disclosed. The section in the Nun shows us that to the east as well as to the west flexures may take the place of the peculiar unconformable overlap- ping boundary between the upper and lower Siwaliks described in the Nahan region, where there is no dun. The difference of struc- ture would be such as might result from the presence of some unyielding mass of rock underground in this latter position, prevent- ing the formation of flexures. This Nahan region is in other ways remarkable, as we shall see in following sections. The form of the structural features prevailing in the Sub-Hima- layan zone indicates plainly a thrust from the adjoining mountain mass ; and the magnitude of the total movement is astonishing in connection with the reflection made in a previous section, that it must in great part have occurred since the mountain mass had assumed somewhat of its present form ; or, at least, that the main drainage system had remained the same throughout. From what has already been said, a general idea might be formed Distribution of Siwalik of the distribution of the different groups of rocks. the Siwalik series ; but the effects of denu- dation and other influences remain to be indicated. The chief expanse of the Sub-Himalayan hills and rocks is beyond the Satlaj. From about Pinjor, the lower Himalayan ranges trend northwards towards the lofty gneissic ridge of the Dhauladhar, overlooking the Kangra Dun. The outer range of the Sub-Himalayan is not affected by this change of direction, so that the zone of tertiary rocks becomes permanently widened to about three times the breadth it exhibits along the whole mountain range to the east. In the Kangra region there is a succession of three duns occupied by conglomerates, separated by ridges of sandstone brought up along great faults. To as far as the Ganges the upper Siwaliks are still well represented in the outer hills ; but east of this river, along the whole of Rohilkhand, only remnants of these outer Siwaliks have been observed. They seem to have been mostly denuded away, and one conies at once upon the older sandstones of the ranges immediately flanking the high moun- tains. This is the case under Naini Tab The change, however, is not a permanent one ; for, again, far to the east, on the read- to OF THE NORTH-WESTERN PROVINCES. 127 Kathmandu, there is a broad outer Siwalik range, formed of soft sandstones and conglomerates, and separated by a dun from an inner zone of lower sandstones. But, again, along the Sikkim and Bhutan border, there is no sign of the outer Sub-Himalayan range. It has been said above that the uppermost Siwalik strata are considered to be of newer pliocene age, and Post-tertiary deposits. , , . we have seen modern deposits being laid down against them along the base of the hills in the bhdbar region. In these a fossil village was dug out by Colonel Cautley in the excavations for the Eastern Jumna Canal. They no doubt passed down into beds of the prehistorical or recent period. Still there would be a great gap left in the sequence of formations — the whole of the pleistocene period, represented in Europe by the drift, and the cave deposits, which for years past attracted so much attention in connection with the discovery of human remains. For some middle portion of that period representatives are found in the Sub- Himalayan zone. They are unmistakably exposed on the Satlaj, above Bubhor, where the hills on either side of the river, to a height of some 500 feet, are capped by clays and coarse conglomerates, resting quite undisturbed on the edges of vertical Siwalik strata, both of the middle and uppermost groups. It is clear that a long time of disturbance and denudation must have intervened between the deposition of those totally unconformable deposits ; also that those high-level conglomerates are separated from recent deposits by at least the time it has taken the Satlaj to excavate its gorge to its present depth. These two limiting tests of age are quite as co- gent as those applied to corresponding deposits in Europe. Beds of the same age are well exposed above the sanction already described in the Nun river under Mussooree. They are here quite on a level with the summits of the Siwalik hills to south of the Dehra Dun. The most interesting deposits of this age are those to which a glacial origin has been assigned. It was long Supposed glacial deposits. . , . f , , , since observed that the glaciers of the Himalaya had once extended to a much lower level than they do now. Unmistakable moraines are found-in Sikkim to within 8,000 feet of the sea level, the present limit of glaciers being about 14,000 128 him/layan districts feet. More recently a glacial deposit lias been described in the Kangra valley. Enormous blocks of gneiss are freely scattered in the low ground, at an elevation of 2,500 to 3,000 feet, along the whole base of the Dhauladhar range, resting on the Siwalik strata. One cannot well assign a limit to the mass that may be moved by a rush of water on a considerable slope ; but the distribution of these blocks makes it very difficult to account for them by any action of this kind through the existing gorges ; for they occur along the slope of the flanking ridges, seemingly quite out of reach of any possible sweep of the torrents. They are three possible assumptions to account for their position : by supposing the scarp of the gneiss now forming the mountain-ridge to have once extended a couple of miles in advance of where it is now, and so as to bring- those blocks within the range of its talus, but in this case the blocks should be found over the intermediate heights, which is not the case; or to admit that the blocks were ice-borne, and not by glaciers, for the blocks are not arranged in moraine fashion, but by floating ice in a lake of that period ; or to suppose that the whole valley and the main gorges were formerly choked up with detrital accumulations to such a level as may have brought these lateral positions within the range of the spill from the gorges, ever overtopping the lower flanking hills. This is by no means a gratuitous supposition, for we find those coarse superficial deposits capping the heights above Kangra fort, on the south of the valley, and not derivable from the Siwalik conglomerates on which they rest. The necessary slope of deposition for such materials, from this position to the mountain range, would give elevation enough there for any observed distribu- tion of the great blocks, by simple diluvial action. This is probably the real history of the case ; but the possible influence of ice action to aid the process is not to be lost sight of. When the Himalayan glaciers reached to 8,000 feet lower than at present, ice-work must have been very active in the Dhauladhar, and its effects very mark- ed in the deposits at the base of the range. All the facts suggest that those high-level gravels are of the same age throughout ^the Himalayan border, and probably of the same age as the former extension of glacial action ; and it is impossible not to notice the near coincidence of this age with that of the glacial period of Europe. There is no independent evidence of changes of level since the ao-e OF THE NORTH-WESTERN PROVINCES. 129 of these deposits ; and it is doubtful how far mere difference of rain- fall could count for the change ; we should thus he driven to enter- tain the idea of an ice-age. The confirmation of this physical evidence of a great phenome- non having affected synchronously so large Importance of the theory. ^ p 0r tion of the earth’s surface would be of the highest importance to geological science. Since the abandon- ment of the primitive idea that all similar rocks were of contem- poraneous origin, we have been at a loss for any test of absolute time-horizons. Within continuous land areas some approach to a judgment can he made by closely comparing series of adjoining sections, but for any distant or detached area we have to tiust to palaeontology for the homotaxis, or comparative classification, of formations. Palaeontological homotaxis, however, implies differ- ence as well as correspondence in actual time relations ; and the problem of settling, from fossil evidence only, in which direction the difference should be counted, is an exceedingly complex under- taking. Thus palaeontology itself was the chief sufferer by the natural limitation of age-tests for the stratigraphical foundation upon which it was based, and of which it is as yet far from being independent. And as the history of life upon the globe is the object of the highest interest in geology, the check to progress was a very serious one. The occurrence of even one semi-universal phenomenon, leaving such peculiar and well-marked stratigraphi- cal characters as those of an ice-period, would afford an invalu- able test whereby to check the direction of growth and distribution of organic forms in all the formations nearly connected therewith. The change from the Sub-Himalayan hills to the outer region of the mountains is always, as has been The lower Himalayan region. sliown^ a more marked feature than the mere difference of height would suggest. The hills of the Nahau zone ran«e from 3,000 to nearly 5,000 feet, while the summits of the adjoining mountain-ridge vary from 6,000 to 8,000. From this to the great snowy range there lies-, a tract more than fifty mi es wide, of deep valleys and narrow ridges, the average elevation of which would be scarcely over that of the border-zone of mountains. This is the region appropriately known as the lower or outer Himalaya. The main watershed of this broad tract ol mountains lies' 130 htmXlayan districts well to the north of the line of snowy peaks, and the great rivers traverse the lower hills in very tortuous courses. The configuration stamped npon the area by the denudation from rain and rivers gives very little clue to the rock-structure. Although the general strike of the formations is parallel to that of the range, the composition of the strata is too complex, and the cases of local distortion too frequent, to admit of anything like the regularity of feature that has been described in the Sub-Himalayan zone. One character may, how- ever, be noticed as constant throughout the western part of the lower Himalaya to as far east as the Nepal frontier : along the outermost zone there occurs a strong limestone formation, producing ridges of more rugged outline and having a greater elevation than the hills for some distance to the north of it. Our knowledge of this immense stretch of mountains is so fragmentary that no connected account can be given of it. We can only give a sketch of the four sections that have been even cursorily observed, and offer some conjectures as to their connection. The four sections occur in the Simla region, the Kuinaon region, Nepal and Sikkim. The first thing to note of the Simla region is that it constitutes the termination of the Lower Himalaya as The Simla region. Sub-Himalayan zone it was noted how from about Pinjor (on the main road to Simla) the boundary of the mountains trended round to the north for about eighty miles, up to the base of the Dhaula- dhar ridge, which is exactly on the line of the great snowy range, and is structurally its equivalent. Thus, of course, the continuous broad area of lower mountains is cut off. It is important to notice that this is not a freak of denudation, a great bay worn into the mountains by a tertiary sea : were this the case, we should find the successive formations of the area striking out along that curve and abruptly cut off there. The fact is not so. The strike of the rocks bends regularly with the direction of the boundary, thus showing that the entire feature is an original character of the mountain- structure. We have here, in the extinction of the Outer Hima- layan region, the beginning of the north-westerly decrease of the Himalayan elevation. The mountains beyond the Ravi, which, in a superficial sense — as being south of the range of maximum elevation — might be held to represent the Lower Himalaya, do not characterised above. In describing the OF THE NORTH-WESTERN PROVINCES. 131 reproduce its characters. Kashmir has structurally more relation to the Central Himalaya than to anything south of the snowy range. This fact of diminishing original elevation comes out very clearly in the peculiar distribution of some of the formations that occur in the Simla region. These have been roughly classified as below : — r Kasauli. Sirmur ... < Dagshai. v. Subathu (nummulitic). Krol (? triassic). Infra-Krol. Blaini. Infra-Blaini. Schists and gneiss. The marked change in the surface configuration from the Sub- Himalayan to the Lower Himalayan hills The Sirmur formation, j n j :roc [ uces for the most part a total change of rocks. Below Mussooree and Kami Tal, and throughout the whole range to eastward, one steps at once and for good fiom the upper tertiary sandstone to the much oldei slaty locks. It is not so, however, in the region between the Jumna and the Satlaj. The high ridge on which stand the stations of Kasauli and Dagshai is formed of rocks very similar in character to those of the Nahan zone close by ; but the marked boundary separating them is con- tinuous with that forming to the east the separation of the Nahan from the slates. Indeed even here, under Kasauli, the slates often appear along the boundary beneath the sandstones of the ridge, which have been upheaved upon a basement of their supporting- rock. Resting upon the slates in this position we find thick beds of dull brown, gray, and olive indurated clays with bands of lime- stone, in which there occur abundantly fossils characteristic of the nummulitic period. These beds are well seen about Subathu. They are overlaid conformably and with alternating transition by red clays with hard purple and gray sandstone, well seen about Dao-shai. In the ascending section sandstone prevails to the exclusion of the red clays, as is well seen on the ridge at Kasauli. In these top beds numerous leaves have been found indicating the proximity of an abundant sub-tropical vegetation. The ao-o-reo-ate thickness of this threefold formation (Subathu, Dagshai, 132 HIMALAYAN DISTRICTS Its distribution. and Kasauli) may be from 2,000 to 3,000 feet. Collectively it may be known as the Sirmur series, a considerable part of its area occurring within that State. Here, then, at last we have a formation the horizon of which is fixed by a well-marked marine fauna. The Subathu group at the base of this series is certainly eocene ; and considering the perfectly transitional charac- ter of the three groups, we may provisionally consider the whale series to be of this age. The study of its position and relations seems to throw much light upon the history of the mountain-system. It forms an almost isolated outlier, caught up on the edge of the moun- tain-area. Its greatest width, east of Dagshai, is about ten miles. In that direction it stops out along the crest of a ridge at about fifteen miles west of the Jumna ; the mode of termination show- ing that it was effected simply by greater elevation to the east, and consequent denudation. The only other known occurrence of these rocks within the south Himalayan boundary to eastwards is a small patch of Subathu beds on the top of the ridge east of the Ganges close to the village of Bon in Garhwal. In the far east, however, the nummulitic deposits at the south base of the Garo hills have a very striking resemblance to the Subathu beds ; but it is doubtful if they were ever connected. To the west, at the Satlaj, the outlier is attenuated to a band a few yards wide — a bottom remnant of the Subathu beds. These rocks again appear in some force in the ridge beyond, but become gradually depressed in that direction, so that before reaching the Bias the most characteristic bottom group has disappeared. The band as represented by the upper groups is well marked, though very narrow, at the Ravi. The hill station of Dharmsala stands upon it. Some points of interest have been made out regarding the rela- Its uncomformity to the tions between the Sirmur series and the Older rocks. contiguous older formations. There is very deep unconformity : the Subathu beds do not rest upon the next youngest rock, which is the great Krol limestone, but upon beds which underlie that limestone. This is fully made out. As a natural concomitant, we find that the surface of contact of the two contrasting foi mations is a very uneven one. On the ridge at Subathu there are not more than 50 feet of the typical Subathu OF THE NORTH-WESTERN PROVINCES. 183 beds below the red rocks ; while in the valley alongside there must be 600 to 800 feet of this bottom group. These facts suggest proximity to the edge of deposition of the nummulitic sea ; and the succeeding deposits, ending in the plant-beds of the Kasauli zone, tend to confirm the view. It seems, too, that little or none of the contortion which now Contortion of the slates affects a11 tlie rocks kad occured before the post-eocene. deposition of the Subathu beds ; for at Subathu itself a characteristic bottom layer is clearly seen, resting continuously throughout a considerable synclinal flexure upon approximately the same bed of the supporting slates. In agree- ment with this observation, we now find these rocks to have undergone equal contortion with the slates. The inner boundary of the eocene area is a very broken one ; and outlying shreds of the nummulitic clays are found caught up in folds of the slates, as may be seen on the road north of the Haripur rest- house. All these facts would tend to prove that although some general elevation of the mountain area, involving Inf ci cnees. deep denudation of the rocks, had occurred here prior to the tertiary period, none of the special disturbance characteristic of the existing mountain-system, and so specially marked in this fringing zone, took place till after the deposi- tion of the eocene rocks. The Sirmur series exhibits more intense and varied disturbance than is at all general in the Nahan group. The relation of the Sirmur to the Nahan group cannot be so Relation of Sirmur and definitely made out, as they are only seen Siwalik series. near eac h other along a single steep line of boundary ; and the question is, as to the nature of this boundary. The argument for the total separation of the groups in this region appears, however, to be pretty conclusive. Although, as has been said, the rocks of the upper Sirmur groups have a strong lithologi- cal resemblance to those of the Nahan .group — so much so that the type of the Sub-Himalayan deposits may be said to have set in with the eocenes — the facies of the Nahan and Sirmur groups are so distinct, in close proximity, that there is little ground for consider- ing any parts of them, as represented in this Jumna-Satlaj region, to be equivalent. It is only on the supposition of the boundary 134 HIMALAYAN DISTEICTS between the areas (which is also the chief boundary along the base of the mountains) being a great fault, that the question of correspondence can arise at all. But as this supposition is the prima facie one — the one that would be applied from the accepted interpretation of like boundaries in other mountain regions — it is necessary to state the evidence against it. Throughout the whole range of the Nahan zone in this region no trace of the very characteristic Subathn Probable unconformity. , . , , beds has been found, either at the apparent local base of the section, or as a remnant adhering along the sup- posed fault-ground. In the former position it might be said we should be more likely to find the top rocks of the older group ; but this too can be answered negatively r the lower we get in the Nahan group, we find clays to occur more frequently, whereas the Kasauli beds are almost exclusively sandstones. It is also to be noted that no remnant of the Nahan rocks has been recognised capping the Kasauli beds, or otherwise, within the eocene area. No conglome- rate has been observed in the Sirmur group. The only position from which the original continuity of the groups, with separation by faulting, could be maintained, would be to assert that, as the actual base of the Nahan group has never been seen in this region, the whole eocene group may be buried beneath it in conformable sequence, or otherwise ; and correspondingly, that any trace of the Nahan deposits had been washed away from the present eocene area. So much for the direct evidence. As to the indirect, there is really little, except the fact of abruptness, in the character of the boundary itself to countenance the supposition of a great fault. A straight line drawn from the west end of the eocene area in Sirmur to the small nummulitic outlier east of the Ganges would touch the Siwalik hills south of Dehra ; and along the great bay-like course of the boundary, north of that line, there are many sharp changes of direction, such as are not supposed to he compatible with dislocations of such dimensions as would be required in this case. The great faults in the Sub-Himalayan zone were seen to be remarkably straight. The alternative and most probable supposition is that the eocene area was upraised, and something approaching to the present steep edge of contact eroded out of it, before the deposition of the Nahan rocks. OF THE NORTH-WESTERN PROVINCES. 135 It is, however, to he mentioned that far to the north-west Change of character to there is complete transition throughout the the north-west. tertiary series, from the Subathu to the top Siwalik. The partial obliteration of the Sirmur series, as forming a sharply defined zone at the base of the mountains, commences at some fifty miles beyond the Ravi about Udampur. The zone is there more than twenty miles broad, and rocks of Siwalik aspect occur within it. Still as a zone of greater upheaval it is traceable to beyond the Punch ; but before reaching the Jhilam it is quite effaced, the whole tertiary series sweeping across it in an anticlinal flexure. These facts do not in the least disturb our conclusions regarding the relation of the lower and upper tertiary series in the Lower Himalayan region. They only form part of the concurrent evidence that towards the middle of the Himalayan system the elevation was greater, and commenced earlier than in the terminal region. The same fact is emphatically shown in the comparative relation of the Sirmurs to the older rocks in these two positions. In this case there can be no doubt of the deep unconformity in the Simla region — a relation of the same kind as that here adopted for the Sirmur-Nahan relation in the same area. But this feature too is quite changed to the north-west : in the great inkers of old limestone that occur within the tertiary area of the Jamu hills, the Subathu group, with the same characteristic bottom- bed as noticed at Subathu, is everywhere observed in parallel (con- formable) superposition with the old limestone. It is not in- deed proven that this rock represents the Ivrol formation ; never- theless, the contrast of the stratigraphical relation is most striking. We have again to refer to the Jumna-Satlaj ground for the Older rocks of the Simla best sections of the next older rocks to the region. eocene. The peculiarities of this region come out stronger as we recede in time. Its character in the plains, as the present main watershed of Hindustan, is really its least permanent feature : there is some reason to think that the Jumna once upon a time may have flowed towards the Indus through western Rajputana. It can certainly be affirmed that such a course was within the range of the diluvial conditions that formerly obtained in upper India. The peculiar unconformity found in this position between the upper tertiary rocks is not, hima'layan districts 136 like the plains’ watershed, accidental or temporary, but structural. In the well-preserved sections of the Sirmur group we found in this region the only representative of the eocene period within the Southern Himalaya ; and again here we find the best preserved remains of the older formations. This ground too has been examined in more detail, so it will serve as a standard of comparison. Standard section. The Solan rest-house on the new road to Simla stands between three picturesque mountains of limestone, more or less isolated in each case upon a base of supporting rock. It is a blue gray stone, several hundred feet in thickness. From its position here we are safe in taking it as the youngest group of the series with which it is connected. It has now for some years been spoken of as the Krol limestone. There is often a band of coarse sandstone at the base of it, which seems to vary a good deal in thickness, often at the expense of the limestone. Below this there is well exposed in this neighbourhood a thick band of black carbonaceous slaty shales, which pass down into similar non-carbonaceous flaggy beds, forming the whole base of the mountains in this zone, down to the lowest levels. At a thousand feet or more from the base of the Krol limestone there occurs in those slaty flags a thin band of compact limestone of clear pink, yellow, or gray tints, often accompanied by a bed of conglomerate, and a white quartzite. This band, though a thin one, seems to be very persistent to great distances ; it is therefore important as a well-marked horizon. It has been identified on the flanks of the hills under Simla; far up the valley of the Tons, at the crossing of the Simla-Mussooree road ; on the Ganges near Tapuban, and again on the hillside north of the Kota Dun in Kumaon. It is called the Blaini group. The Krol group is traceable eastwards almost continuously, and in about the same condition as at the Krol, through Deoban in Jaunsar to Mussooree and Naini Tab From certain lithological resemblances to the rocks in Spiti, which he had classified from fossil evidence, Conjectured affinities. Dr Stolickza fl as conjectured that the Blaini and infra - Blaini beds may correspond with members of his Maith and Bhabe series, of upper and lower silurian age ; that the Krol group represents his Lilang series, which is triassic ; and that the infra - Krol may correspond with his Kuling series of the OF THE NORTH-WESTERN PROVINCES. 137 carboniferous period, in the central Himalaya. But no recognizable fossil has yet been found in these rocks in the lower Himalayan region. The relation of this series, which forms so continuously the outermost zone of the lower Himalaya, to Extension to Simla. . . . . . , . . the metamorphic rocks on the north is very puzzling, yet essential to the explanation of the mountain structure. Some important hints towards it are found in the Simla region. Unless one chances to stumble upon an outcrop of the Blaini group, the flaggy slates of the infra- Krol and infra- Blaini horizons are indistinguishable. Immediately north of the Krol there is a com- pressed anticlinal flexure, with elevation to the north of it ; so that the slaty rocks occupy the whole ground till we reach the quartzites of Tara Devi and Boileauganj, which dip towards their common synclinal axis at the gap south of Simla : limestone occurs above them on Jatog. These may represent the Krol group. However this may be, there can be no doubt about the identification of the Blaini group on the spur under the Yarrows and under Chota Simla, on the opposite sides of Jako. The thickness of strata above these outcrops, to the top of Jako, would quite carry the section up to the base of the Krol group. An interesting feature of the section is that the rocks of the Jako and Boileauganj hills are highly Typical instance of over- ... • i • > l ±.*d lying metamorpliism at metamorphic — mica-schists and garnetiierous hornblende-schists with abundance of vein- quartz — while the flaggy slates above and below the Blaini group, all round the west, north and east base of the hill, are as little meta- morphic as on the base of the Krol. This is a crucial instance of a phenomenon that meets us far and wide throughout the Himalaya, the superposition of highly metamorphic upon non-metamorphic strata. The metamorphism is often apparently greater than here — we find gneiss instead of crystalline schists at top — while the case for superposition is less distinct ; so that it is possible to doubt the fact of its being a normal ascending section ; and accordingly this has always been a chief stumbling-block in the interpretation of the lower Himalayan sections. It is the feature that so fatally puzzled Herbert fifty years ago. We shall have to return to the sub- ject presently, and would only remark here that the very instructive 18 138 Til M/LAY AN 'DISTRICTS instance we have just seen occurs in a much frequented position, where many English people pass many idle hours. The same flaggy slates seem to continue for a long way north of Section a long ridge north Simla, for the most part with a moderate of Simla. north-easterly inclination. There are several lines of crush and strain, generally found at the gaps, but apparently unattended by great dislocation, for no new rock appears along these lines. The Blaini group has been identified on the ridge north of Theog bringing in the Krol beds towards Matiani, where there are symptoms of gradual general metamorphism. At Nagkanda this change is very decided, and here those slaty schists seem to pass into the flanks of Hatu, the top of which is formed of massive beds of gneiss, lying nearly horizontally. This rock is the same as the so-called central gneiss forming the southern basement of the great snowy range, where its chief characteristic seems to be the preva- lence in it of ramifying veins of albite-granite. These observations have suggested that the Krol beds had here overlapped the slate series, and are in original contact with the gneiss. We have now seen a general section up to the great mountain Parallel section in the range. It is taken for the most part along Satlaj valley. the watershed in a north-east-by-east direc- tion from Simla. The apparent simplicity of it is very encourag- ing ; but we have not far to go to dispel this illusion. It may be noted that no limestone appears on this section beyond Simla. The Shali mountain, however, only a few miles to the west of Matiani, is made of strong limestone, not unlike the Krol rock, with an accompanying sandstone, and underlaid by flaggy slates like those about Simla. If they are the same, and indeed in any case, their position is somewhat puzzling, for from Shali they dip eastwards under the schists of Matiani and northwards down to the Satlaj, where the limestone seems to pass under the gneiss of the Jalori ridge. It is not merely a case of dipping toioarcls these metamor- phic rocks ; the Y-shaped outcrop of the junction along the steep sides of the Satlaj gorge points up the valley, and is more or less parallel to the dip of the strata in both rocks. In the Satlaj valley above and below Suni, close to the north of Simla, the confusion of the limestones and slates is indescribable ; and there is profuse trap- pean intrusion : whereas, on the whole section through Simla, from OF THE NORTH-WESTERN PROVINCES. 139 The Kumaon section. tlie plains to Nagkanda, only one small dyke has been observed. The ■absence of fossils in these limestone and slate rocks makes it almost impossible to settle their stratigraphical relations with any certainty. 1 The distribution of these limestones and slates is as irregular to the- east as to the north of Simla. The Chor East of Simla. mountain — directly between Simla and Mus- sooree, and remarkable for being the highest summit (12,000 feet) occurring within such a short distance of the plains — is an isolated mass of gneiss. To east of it the limestone stretches again far into the mountains, along the valley of the Tons, forming Deoban hill ; along the Mussooree ridge it occurs frequently, as on the- Abbey and Camel’s-back hills. On the top of Landaur it is mixed with sandstones, and appears again by itself on the Tapuban point. The Blaini lime- stone and' conglomerate are well seen on the flanks of the Sarkanda summit, and again in the Ganges at the confluence with the ITiunalgar. In the Kumaon section we still find the limestone and slate rocks fairly represented. The ridge of Kami Tal is a broad synclinal range, with many local fractures and contortions, like its type the Kiol lango. The stiong limestone that forms the summits about the lake is very like the Ivrol rock. Here, however, and also at Mussooree, there is a good deal of trappean intrusion. In the- Syamkliet valley, north of Kami Tal, trap-rock is in great force, and immediately to the north we come upon crystalline schists. Along the heights of Sunthala and Gragai these are gneissose. The dip throughout is at a moderate angle to north-north-east, and about Almora one or moie bands of gianitoid gneiss occur in these rocks. Its general mode of appeal ance is that of interstratification with the schists ; but in one place it has beer described as intrusive, which would establish its character as a true granite. North of this, for some way, there is a reversal of the dip- to south-south-west up to a line of trappean intrusion, which has been traced for many miles along the strike. The rocns to the noitli of this band are of a more varied character ; some aie slaty ; and lime- stone is of frequent occurrence, often steatitic in the vicinity of the trap. The dip is less constant in these rocks, and their relation to. the crystalline schists of the snowy range is not well defined. 1 Much detail with suggestive conjectures regarding this region is given in Memoirs of the Geological Survey of India, v ol. ill., ai 140 HIMALAYAN DISTRICTS here we next get a section of the lower Himalaya through the The Nepal section. ^ ™ U< >y> there » littl ° outward resemh- lance to what we have seen to the west. The Churia Grhati range, between the plains and the Etounra Dun, is a pattern specimen of the Siwalik type. North of the Dun there is an equally characteristic representative of the Nahan range flank— ing the mountains. But inside this we no longer find the border mountain-range of slaty rocks capped by plain blue limestone that is so constant to the west of the Kali. We come at once upon schistose rocks. These, however, are not mica schists of the ordinary type, such as those north of Naini Tal. First there are earthy (slaty) schists, some quite black and with carbonaceous layers ; then flaggy quartzose schists, passing up into strong schistose quartzites ; and these are succeeded by a great mass of dense highly crystalline white limestone within three miles from the Nahan boundary. All are more or less vertical and folded with a prevailing northerly underlie the strike being 15° south of east. Beyond this steep ascending section there is a broad band of still greater disturbance, apparently a synclinal ; for the limestone is variously repeated, and the under- lying rocks brought in again. It would seem to be followed in the Chessa-garhi ridge by a crushed anticlinal, about the axis of which there are thick bands of porphyritic gneiss associated with flaggy quartzites. From here there is again a general ascending section through similar flaggy quartzitic schists to the Chandragiri range, bounding Nepal on the south-south-west. This ridge and all those to west-north-west and east-south-east of the valley are made of folded repetitions of one set of rocks, in which a calcareous element is more or less prevalent ; varying from strong beds of pure limestone to earthy schistose limestone, and prominently a thickly bedded fine- grained quartzite, with scanty calcareous bond. The Shiupuri rido- e on the north-north-east of the valley, is of' massive gneiss ; schists appear- ing again to the north in the valley of the Tadi and the Trisul Granga. There is sufficient resemblance in the two bands of limestone and Possible affinities. the flaggy quartettes of this sec- tion to suggest that they are repetitions of the same series ; and this has certain characters of resemblance to the rock- series at the Krol, which admit of our conjecturing their identity. The whole of this Nepal section exhibits an intensity of disturbance OF THE NORTH-WESTERN PROVINCES. 141 throughout, such as has not been observed in any other section of the lower Himalaya. Only one instance of a doubtful trap-rock has been noticed in the above section, in the schists near the outer boundary. We have one more section of the lower Himalaya to take note Sikkim section : of, far to the east, in Sikkim, and still more Damuda formation. unlike than that in Nepal to the sections of the north-west Himalaya. It is of the highest interest, because we find here in a recognizable state a formation well known to us in the peninsula of India, thus establishing almost the only link between these separate geological provinces. There are, indeed, the nummulitic deposits resting against the edges of the Deccan trap at the base of the western ghats to compare with the nummulitics of Subathu, and showing that the Himalayas are younger than the Deccan plateau. But this is a comparatively superficial connexion ; whereas in Sikkim we find a bottom formation of one of the great rock-series of the peninsula, intimately connected with the rock forming the mountains. It is now thirty-one years since Dr. Hooker discovered Damuda fossils near Pankabari, at the foot of the Dar- jeeling hills ; but it was only in 1874 that an examination of the mode of occurrence of the rocks was made by Mr. F. R. Mallet, of the Geological Survey, who was sent to investigate the prospect of a useful coal being found. He traced the band of Damuda rocks from Pankabari to Dalimkot ; at the Tista it is nearly a mile in width. In the western Duars it does not occur, but on or about its horizon there is a new formation, not found in Sikkim, consisting largely of massive dolomite, and called by Mr. Mallet the Buxa series. In 1875, Major Godwin-Austen, who accompanied the expedition into the Daphla hills, found the Damudas again in force at the base of the mountains in Upper Asam, the Buxa series being there wanting. It is, of course, possible that the Damudas may recur to the west also, in Nepal, though they do not appear at the Sikkim end of the frontier, and certainly they are not specifically represented in the section through Kathmandu. Lithologically as well as by fossils the formation resembles its Its condition and posi- prototype in the Damuda valley, consisting tion. 0 f strong sandstones, gray shales, and coal seams. In some few spots the rocks are' so little altered that the resemblance is complete, the coal itself being the only rock that has 142 hima'layan districts not escaped modification. It is always crushed to powder, and could only be utilized by being made into bricks. Very often, however, the whole group is as much altered as the contiguous rocks to the north, the sandstones being converted into foliated quartzites, and the shales into splintery slates or carbonaceous schists. The impor- tant point to settle is the stratigraphical relation of the group to the other rocks of the mountains. These are, first, a zone of slate rocks, some greenish and slightly unctuous, some ordinary clay state with bands of flaggy quartzite, rarely hornblendic and calcareous, and also rarely carbonaceous. These form the Dating series of Mr. Mallet. Next comes the gneiss of the upper hills : it is distinguished as the Darjeeling gneiss. The dip in all these rocks is into the mountain, and hence the immediate inference that they underlie each other in the above order. Here, then, we find again an instance of the puzzle noticed in the section at Simla, and on which Herbert made ship- wreck. Mr Mallet was unable to find any escape from the position ; the Daling beds pass most regularly with parallel interstratification into the gneiss by increase of metamorphism, appearing underneath it all up the gorges of the Tfsta and the Ranjft to the north of Dar- jeeling, but in a more altered condition. Also he found in several clear sections most completely conformable and transitional junction between the Daling and the Damuda beds. Their junction forms a re-entering angle up the Tfsta valley ; the Damudas, however, are not known to rise to the surface again in the interior of the mountains. The conviction was forced upon him that they are indeed what they appear to be, — the lowest and oldest rocks of the Himalayan series in this position. Yet so great is the prepossession in favour of gneiss as necessa- Theoretical considera- nty ^ fundamental rock, that doubt still pre- tlonp * vails amongst those who have not seen for themselves. It may then be well to mention some independent con- siderations which tend to remove this obstruction to the rationale of Himalayan geology. It has long since been shown experimentally that the silicious minerals entering into the composition of crystal- line rocks can, through the medium of moisture, be produced under very moderate temperature and pressure ; and, hence, that the hydro-metamorphism to which gneiss and even granite were due need not be a very plutonic operation. Also it can be urged that OF THE NORTH-WESTERN PROVINCES. 143 although when gneiss occurs extensively on the flat, we may he entitled to regard it as a fundamental rock, due to such hypogene action as would require any underlying rock to exhibit as great a degree of metamorphism as itself, yet when we come to mountain formation the case is very different. Here a special concentration of forces has manifestly occurred which may be adequate to the pro- duction of this apparently anomalous result. In a recent and very thorough discussion of this branch of geological dynamics we find a direct explanation of our difficulty ; that if a mixed mass of strata were subjected to compression, those portions which by position or texture were least capable of yielding, whether by shrinkage or con- tortion, would have to bear the brunt of the pressure, and to undergo in some other form its effects, prominently in the development of in- ternal heat. 1 In some such way overlying massive strata may have been converted into gneiss, while softer beds below underwent no crystalline metamorphism. If it should be shown, as in the Simla region, that the Darjeeling gneiss is the same as the central gneiss, the above interpretation of the Sikkim section would have to be abandoned. Geologists in India have been long on the look-out for a connect- Slight correspondence ing link between the rocks of the Peninsula ffiSya andTf the' Pel and of the Himalaya. So many of the forma- ninsula. tions in the former region are unfossiliferous, it was hoped that some clue to their homotaxis might be obtained through their representatives in adjoining regions ; and although the elevation of those mountains may have occurred in tertiary times, the rocks so upraised might, of course, be of any age. Thus this discovery of the Damudas, as apparently the oldest formation in the Lower Himalaya, at least in the east, comes rather as a surprise. Although the Damuda series is, according to the most recent estimate of its fossils, of lower mesozoic age, its appearance in the field amongst other Indian formations is one of comparative youthfulness. It is, for instance, immensely younger than the great Yindhyan formation, which cover such large areas in undisturbed stratification, but in which as yet no trace of life has been observed, and below which there are several groups of slaty and sub-metamorphic rocks before we come to the fundamental gneiss of the region. However, in these matters, what is, is best ; the object being to ‘know what 1 See R. Mallet on Volcanic Energy, Phil. Trans., Vol. CLXIII, page 147, 144 HIM/LAY AN DISTRICTS really has occurred. If the Himalayan sections would reflect to the geology of the Peninsula some light in return for that it has now received therefrom, by clearing up the doubts that still exist about the age of the Damuda formation, it is all we could expect. There is but one character found almost constantly throughout Frequent occurrence of the Lower Himalayan sections — the frequent througliout US the d Lower appearance of carbonaceous matter. It may Himalaya. be of no great significance, but it is worth notice. Coal-mining had been attempted near Subathu in the carbonaceous shale of the infra - Krol group, or rather where this rock has been compressed and glazed in fault-ground. And this appearance of carbon (some of it as volatile hydro-carbons) with fault-rock is very common throughout the Lower Himalaya. It occurs at Simla, below Niigkanda, at Mussooree, and east of the Ganges. Among the more highly metamorphosed rocks it is repre- sented by graphite, as about Almora. Its appearance in the Kath- mandu section, at the outer fringe of the mountains, next the tertiary sandstones, is about the only specific similarity between this section and that in Sikkim, where carbonaceous matter occurs in the Daling and theBuxa, as well as the Damuda horizon. It may provisionally be taken as a suggestive link of affinity between all these rocks. In this connection it is important to recall that in Dr. Stolickza’s independent classification the infra - Krol horizon corresponds with his Central Himalayan Kuling series of carboniferous age, which is also the age assigned by some to the Damuda formation. From what we have seen of the rocks of the Lower Himalaya, Conjectural affiliation of there is not much prospect of a near solution the Lower Himalayan sections. of this question. The main hope is in the present manifest want of information. Immediately west of Sikkim comes Nepal, taking up the whole middle region of the Himalaya for 500 miles in length, and which through the unaccountable for- bearance of our Government, is as much a forbidden land to Euro- peans as is Chinese Tibet. Except on the single track to Kathmandu, which has lately been traversed by a geologist visitor to the Resident, no Englishman dare set foot in Nepal, whose people are entirely dependent upon our good will for communication with the out- side world, and freely enjoy it. In the section to Kathmandu, which is only thirty miles from the plains, we have seen a general OF THE NORTH-WESTERN PROVINCES. 145 resemblance to the rocks of the Simla region, the contrast being chiefly the universally high clips and general metamorphism. Except in this latter character it has little in common with the Sikkim section ; specific resemblance in the two rock series cannot be made out. The great limestone has no equivalent in kind in the whole of Sikkim. Where distances are so great, much allowance must, however, be made for probable original change in the nature of synchronous deposits. The fact that the present base of these eastern Himalayas adjoined, or indeed formed part of the Damuda land surface, suggests a difference in the deposits near it from those at a distance. We have also had to notice all through our sections a dis- position in the Krol limestone to pass into a sandy rock. In some such manner it may yet be shown that the Darjeeling gneiss is on the same horizon as the fine calcareous schists of the Nepal valley. Every geologist will understand the very precarious nature of such a speculation. As an object to confute, it may be of some service. The Central Himalaya . — In treating of the Lower Himalaya we Consist largely ol well- have had almost entirely to depend upon known formations. local names for the various rock groups, and to be satisfied with conjectural identifications of them in different parts of the ground. This unsatisfactory result is owing to the want of fossils. For a great part of that ground it must be a permanent difficulty, owing to the high state of metamorphism of the rocks ; but there are large tracts where this condition does not obtain, and where we may hope that fossils will yet be found. At the snowy range and over a large part of Tibet the case is quite different. There numerous zones of strata are identifiable, not only locally, but in the established scale of formations, by the presence of well- known fossils. Our information of those regions is, however, in a very fragment- Rtractey, 1848-49. ary state, and must long remain so, owing Stolickza, 1864 - 65 . to the inaccessibility of the ground and the rigours of the climate at such great elevations. Numerous tiavelleis have crossed the mountains in various directions, and have brought back a few fossils and isolated observations of the rocks, but only two observers have given a connected geological description of any considerable area. One account is of a portion of Central Tibet in 19 146 htm/layan districts Chinese territory, north of Kumaun visited by Captain R. Strachey, R.E., 1848 and 1849. The description is quoted in extenso from his paper, the map attached to which is reproduced to illustrate this chapter. The second and fuller account is that of Western Tibet, by Dr. Stolickza, published in the fifth volume of the Memoirs of the Geological Survey of India, In the summers of 1864 and 1865 he explored the region between Spiti and Dras and the Indus. It will he recollected that he died in June, 1874, after crossing the Karakoram pass, on the return journey with the mission to Kashgar, having lost his life through his zeal for scientific research. His observations on this expedition complete a rough section across the whole Tibetan mountain region from the Panjab to the plains of Khotan. Western Tibet. Dr. Stolickza’s list of formations, observed in Western Tibet, is as follows : — Age. Group. Fossils. IV.— River and Lacustrine Deposits. III. — Tertiary. — Nummulitic ... Indus or Sliingo Beds ...Nummulites. Second- ary, Cretaceous ... Jurassic (Upper). ff Jurassic . . . Middle Lias ... V Lower Lias ... D Rhcetic Triassic (Upper). Chikkim Beds Gieumal Sandstone Spiti Shales (Braun Jura). Upper Tagling Lime- stone. Lower Tagling Lime- stone. Para Limestone Lilang series . . .Rvdista and Foramini- fera. ...Avicula ecliinata. Ammonites macroce- phalus ParMnsoni, triplicatus, etc. Trochus epulus, Cliem - nitzia undvlata, Te- rebratula sinemuri- ensis. Terebratula grevaria and pyriformis, Rliynclionella Aus- triaca, Belemnites. ...Megalodon triqueter. jDicerocardium Him • alayense. ... Ilalobia Lommeli, Ammonites fioridus etc. I. — Palaeozoic — Carboniferous, Ruling series „ Upper Silurian, Muth series ,, Lower Silurian Bhabeh series Gneiss, Metamorphic Schists, etc. ...Productus semireti- cula tus, Spirifer Keilhavii, etc. ... Tentaculites , Orthis etc. ... Orthis ? OF THE NORTH-WESTERN PROVINCES. 147 The distribution of these formations, though subject to many local irregularities, exhibit well the general struc- Synclical basins. . .. . r. . i • mi ■ tural features of the region, lhere are two main synclinal rock-basins, along the centres of which the younger members of the sedimentary series, with one important exception, are found. These geological features have no superficial relations to any geographical basins. The Indus receives a ■ great part of the drainage from both areas in this region, flowing nearly along the intervening anticlinal axis. The southern basin is best exhibited in the Spiti valley, where the fullest section of the upper secondary formations is found. The northern synclinal-basin forms the Kara- koram range. This latter ground has been very little searched, and as yet neither oolitic nor cretaceous strata have been observed in it. Dr. Stolickza describes the Karakoram pass as formed of liassic rocks resting upon trias. These long rock-basins are bounded by parallel areas of crystal- The principal crystalline 1 ™ metamorpllic rocks. The southernmost areas. 0 f these is that already spoken of as the cen- tral gneiss. Its peculiarity, as compared with the other crystalline ridges, is that we seem to have here what may be locally called the fundamental rock. On Dr. Stolickza’s type section at the Bhabeli pass, and in General Strachey’s ground, 200 miles to the east, the m/Vct-Silurian rocks in a non-crystalline state, and of great thickness, are represented as overlying the gneiss. There is no doubt a parallel- ism of strike in the two contiguous rock-systems, but the condition suggested or implied is that the conversion of the gneiss is ot pre- Silurian date ; although, in the east at least, granite seems to pene- trate both formations. It was in this sense of basal that Dr. Stolickza applied the word central to this gneissic axis. The gneiss and schists forming the middle region of the moun- tain mass, from 70 to 80 miles wide at the Middle crystalline axis. p angkong an( j Moriri lakes, are described of a quite different type, as being largely syenitic, and as more or less made up of metamorphosed Silurian rocks.. Along the north outcrop of the southern synclinal basin even the zone of carboniferous rocks is hardly recognizable, and all below it is converted into crystalline schists and gneiss, the south-westerly dip .continuing in these rocks up to the Indus : similarly along the north-east side of this gneissic 148 hima'layak districts mass the carboniferous formation is the first that is clearly recogniz- able ; all below it being strongly foliated and mineralized, passing with a north-easterly dip under the Karakoram synclinal basin. The gneissic axis of the Kuenluen is also described as formed Northern crystalline chiefly of syenitic gneiss and cjuartzose and axis ‘ chloritic schists, the relation of which to the adjoining slates has not been made out. Carboniferous rocks with fossils have been observed on both sides of the range. On the northern flanks of the Kuenluen, triassic and cretaceous deposits are the only secondary formations noticed by Dr. Stolickza. Some minor features in the distribution of the several formations Peculiar position of the wi ^ be mentioned presently. We must nummuhtic deposits. first notice the remarkable exception, already mentioned, in the general arrangement as above sketched. The nummulitic formation occurs in great force in the Central Himalaya of Ladak, but not even approximately in sequence with the next oldest group. The cretaceous deposits are found capping the sedi- mentary series in the centre of the southern synclinal basin; but no trace of nummulitic beds has been noticed near them. These occur in force along the valley of the Indus, in the centre of the middle gneissic area. Dr. Stoliczka remarked how strongly the rocks resemble these of the same eocene age at the south margin of the mountains, especially those of the Dagshai and Subathu groups. It may also be noticed how similar the statigraphical conditions are in both positions. In the Simla region we saw that the Subathu beds were deeply unconformable to the contiguous formations, the youngest of which is thought to be triassic. In the Central Himalaya the unconformity is even more striking, because the upper secondary period is well represented, yet the succeeding lower tertiary rocks are in a totally independent basin of deposition. Stoliczka estimates their thickness at 5,000 feet. There is yet another formation to be mentioned in the Central Extensive post-eocene Himalaya. We have seen granite in con- eruptive rock. nection with the central gneiss. Stoliczka frequently notices greenstone as locally associated obscurely with the Silurian rocks ; and intrusive trap (much of it of presumably tertiary age) is occasionally, as has been said, very abundant in the OF THE NORTH-WESTERN PROVINCES. 149 lower Himalayan rocks. There is, however, one exhibition of erup- tive rocks in the Central Himalaya that calls for special notice. It occurs in the middle gneissic zone, locally forming the axis of a mountain range. It is more than ten miles wide at the Hanle valley, and is continuous thence, with a variable thickness on the south edge of the eocene rocks, to Kargil. Stoliczka describes it as an epidote, diallage and serpentine rock. It appears to be, at least in part, the same rock which he speaks of as syenite to the west of Kargil, where the nummulitic rocks stop out. The eruptive rock there gets entangled in silurian schists, and becomes quartziferous. This igneous rock strongly affects the eocene strata and is therefore of younger date, and is probably connected with the similar rock described by General Strachey on the same strike far to the east. W e were able to draw some very instructive warnings from errors of the early school of Himalayan geologists, so we must not let the moderns escape the same ordeal. On Stoliczka’ s first visit he did not recognise the rocks on the Upper Indus as nummulitic. In that position they are considerably altered, and he took them to be a very old formation. In then writing of the contiguous eruptive rock, he remarked ( l. c., page 128) : “ From their dark colours these rocks have sometimes been referred to basalts, but they have certainly nothing to do with these more recent volcanic rocks.” His next season’s work proved that they cannot be older than middle tertiary, and therefore much younger than the great basaltic formation of the Deccan. The idea of the lithological criterions of age in eruptive rocks has still a strong hold upon the German school of geologists. It cannot be supposed that the rough cross section we have Range of tll0 nummu . sketched near the west end of the Tibetan litics. mountain mass can be taken as a type for the immense region to the east. Already within known ground, some interruptions can be pointed out to the longitudinal ex- tension of the several structural zones. Of the continuation of the Karakoram and Kuenluen, and even of the middle gneissic range, we may be said to know nothing. Stoliczka describes the nummulitic band as completely stopped out against the syenite at Kargil ; and although this obtruding rock is at least in part of later date, it is suggested that the termina- tion of the eocene beds here is probably aboriginal. The eastern 150 HIMALAYAN DISTRICTS extension of these deposits is quite unknown, save that num- mulitic strata occur in the far east north of Sikkim. Some doubtful observations of them in the Changchenmo valley and about the Pankgong lake are recorded. The southern synclinal basin of secondary rocks, continuous for Range of the southern d00 miles from Spiti to the north-west, is basm< also interrupted in the Kargil region against an upheaval of metamorphosed palaeozoic rocks. Any recurrence of regularity in this strike cannot be expected, for the whole Himalayan mountain system becomes confused there, towards the transverse gorge of the Indus, where the stratigraphy is complicated by other systems of flexure. The short break that occurs at the transverse gorge of the Satlaj between the secondary basin in Spiti and the perfectly homo 1 ogous one to the east, as described by General Strachey, is also due to a transversely obtruded mass of partially metamorphosed palaeozoic rocks, through which the stratigraphical continuity is so far maintained. Although the main elevations, constituting the chain of Himalayan Extension of the cen- peaks, aie sometimes, at least m this western- tral gneiss. region, formed of the older stratified rocks along the outcrop of the southern synclinal basin, the underlying, pseudo-conformable, central gneiss must be taken as the stratigra- phical axis of the range. Stoliczka’s type-section of it at the Satlaj and the Bhabeh pass is on the actual continuation of that described by General Strachey to the east, in a more central portion of the great Himalayan chain, where these gneissic rocks are much more prominent. The connection of this gneiss of the main chain with that forming the core of the ridges to the north-west of the Satlaj has not been proved. There are three such ridges. On the direct line of the great chain there is the Dhauladhar ridge, having an axis of coarse gneiss, with slates (probably silurian and lower) resting high on its northern shoulder and passing down into the valley of the Ravi in Ohamba. But the Dhauladhar is cut off from the Bhabeh section by the deep valley of Kulu, on the upper Bias, where no massive gneiss has been observed. The Dhauladhar ridge absolutely terminates at Dalhousie, the slates sweeping round the end of the gneiss at the bend of the Ravi. Again, Stoliczka observed his c central gneiss, ’ though greatly reduced, north of the OF THE NORTH-WESTERN PROVINCES. 151 Chinab, at the southern base of the Zanskar ridge, below the Bara- lacha pass. But on the south of the Chinab valley, on the northern flanks of the Rotang ridge, he observed slates which he conjectured to be continuous with those of the Bhabeh pass ; in which case the gneiss of the Zanskar ridge can hardly be continuous with that of Bhabeh section. This ridge of the Rotang pass is apparently from the maps the structural continuation of the Pir Panjal range, in which a coarse gneiss is again prominent. These three ridges are in a manner confluent in the mountain region of Lahul and Vaziri- Rupi, from which flow the head-waters of the Chinab, the Ravi, and the Bias. The Bhabeh gneiss strikes into it from the east. Thus it would seem as if the main Himalayan axis broke up into three minor features of the same type in its extension to the north-west. The gneiss of the Pir Panjal passes beyond Kashmir towards The Kashmir- Kistwar Ka « hfa ' Bl,t north-west of Kashmir, at the region. Zojila, the gneiss of the Zanskar ridge is extinct, the whole range being there formed of the palaeozoic schists and triassic limestone, which thus roll over from the Tibetan area into Kashmir. Carboniferous limestone occurs in the valley, strik- ing through the Marbal pass into Kistwar. Eruptive rocks have been frequently observed in Kashmir, but none of later than Silu- rian age. The whole Kashmir-Kistwar region, between the Pir Panjal and Zanskar ranges, is very little known. Its geological affinities are with the Central Himalaya rather than with the region specially designated as the lower Himalaya, east of the Satlaj. General Strachey’s description ofthe Central Himalaya, towards the sources of the Indus and Satlaj, is so brief that it can be given in full in his own words, with his summary of conclusions upon the mountain-formation. A few notes are added, giving additional information or suggesting other opinions : — “ Entering the region of the crystalline schists 1 of the great line of peaks, we find the strike still remaining the same, with the dip pretty constantly to the N.-N. E. Along the lines on which Central Tibet. 1 The term crystalline schists is often used, as above, to include gneiss. General Strachey hardly uses this latter word, which is now so much applied to distinguish the felspathic and often massive form of metamGrpliic rock. It is probable that some, at least, of the granite of General Strache3 r ’s description is really massive gneiss. 152 HIMALAYAN DISTRICTS Granite. tlie points of greatest elevation are found in this part of the range, we invariably see for a breadth of several miles, veins of granite in great abundance penetrating the schists, often cutting through them, but perhaps most frequently following the bedding of the strata, between which they seem to have been forced. The great peaks are, I think, in almost every case composed of schistose rock, but the granite-veins may be most clearly seen on the faces of the mountains to very great elevations. Karnet, one of the highest of the peaks in this region, seems, however, to be among the exceptions of this rule ; its sum- mit, which is upwards of 25,500 feet above the sea, appearing to consist of granite alone. This line of granite seems to be sub- divided into several branches, distributed generally along the strike, but otherwise not very regularly (see map). It appears to consist, where I have seen it, almost entirely of veins of moderate size, and such is probably its general character in the portion of the moun- tains between the Satlaj and the Kali ; but the veins occasionally expand into masses of considerable magnitude, and more rarely large outbursts are met with that constitute whole mountains. In the vicinity of the peak to which I have just alluded, Kamet, the granite- area is very large (see map), and a similar development of it also occurs in the vicinity of Gangotri, at the source of the sacred branch of the Ganges. The vein-granite is usually large-grained with schorl-crystals. It is very hard and durable, neither it nor the schists that accompany it being at all liable to decay. The felspar of all granites that I have seen in these mountains is white, and kyanite is of frequent occurrence in the veins. “ The schists that accompany this granite are very hard and crystalline, and comprise all varieties of mica-schist and gneiss. Beds of highly crys- talline limestones, some pure, others hardly to be distinguished by sight from mica-schist, are of frequent occurrence, and a band of such rocks seems to traverse the country near the line of greatest elevation. The strata, where penetrated by the granite, are often very much contorted, and the dip appears on the whole to increase as we approach the granite, where it reaches an angle of 45°, w T hich it does not often exceed. Thermal springs are met with in many of the valleys along the line of granite, and in several Schists. % * v OF THE NORTH-WESTERN PROVINCES. 153 tha£ 1 am acquainted with the temperature seemed pretty regularly to be about 128° Fahr. The whole of the appearances presented by the granite and crystalline schists of the great line of peaks in this part of the mountains seem to be universally repeated through- out the whole length of the chain when we reach the region of max- imum elevation ; and as we extend our examination, we still conti- nue to find additional reasons for concluding that the general geo- logical phenomena of the range, and the causes that have produced them, remain very similar over great distances. “ In immediate succession to the crystalline schists penetrated , by granite veins, we here come at once upon Slates and conglomerates. r slaty beds overlying them, along the bottom of which, near the mica-schists and gneiss, is a line of granite-veins differing somewhat in appearance from those of the larger eruption, and not producing any great alteration in the slaty beds themselves, as is shown by the occurrence of a coarse conglomerate, the component parts of which are perfectly distinct, only a few feet above the granite. Sufficient change, however,' has taken place to prevent our distinguishing much more than that the constituents of this rock are chiefly quartzose, and that it contains rounded stones of all size. I have met with this conglomerate in a similar position, and with much the same general appearance, thirty miles or so further to the east. Above these are slaty beds, in all perhaps 9,000 feet in thickness, consisting of coarse slates, grits, and limestones, all more or less affected by slaty cleavage, and all devoid of fossil remains. u It is after reaching the top of these strata, which is rarely done at a less elevation than 14,000 feet Fossilliferous rocks. above the sea, that we at length enter again a region of fossilliferous rocks, which extends as far as my exami- nations have been carried. And it is not a little wonderful to find at this immense elevation a regular succession of most of the more important formations, from the Silurian to the Tertiary Periods. The Palaeozoic beds met with immediately above the slaty rocks I have just mentioned seem to have a thickness of about 6,000 feet, but it is quite possible that organic remains may extend lower than I supposed ; indeed, from the very difficult nature of the country, the precise thickness of the deposits and the limits of the different formations cannot be determined properly without a much more 20 154 HIMALAYAN DISTRICTS careful examination of the country than I was able to give it. The lower portion of these strata are undoubtedly of lower Silurian age, and I am indebted to Mr. Salter for the following list of the species that he has been able to recognize on a somewhat cursory examina- tion of my specimens. “ Among the Trilobites are — Cheirurus (the Silurian form of the genus), Lichas, A sapiens (only as yet found in Lower Silurian beds), IUcenus, Calymens, Prosopiscus , Splicer exochus. u Of Molluscs are — Strophomena, a strongly ribbed Ortlvis , Terebratula , Leptama very like L. clepressa, Lingulla, Orthoceras, Cyrtoceras , Lituites, Theca , Bellerophon, Murchisonia , Pleurotomaria JRaphistoma, and Ctenodonta. “ Of Polyps — Ptilodictya, Chcetetes. “ Also Encrinites and Cystidos, Tentacidites and other Annelids and Fucoids. “ I had also an opportunity of showing these fossils io M. Bar- rande, who appeared to have little doubt, from their general cha- racter, that some of the beds from which they came were certainly of Lower Silurian age. “ The lowest beds of these Palaeozoic strata consist of dark- coloured thickbedded limestones, in some Stiatification. places filled with corals. They are succeeded by limestones mixed with slates, in which were found the strong-ribbed Orthis, Terebratula, Lingula, Bellerophon, and fragments of Encri- nites. Above these come flaggy limestones with grits, that contain the greater part of the Trilobites, Strophomena, Leptama, Lituites, Ptilodictyon, Cystidece, and Fucoids. The beds then become more argillaceous, and shales and slates mixed with an impure concretion- ary limestone follow. In these beds are found Cyrtoceras and Orthoceras, and amongst the nodular concretions of limestone a Chcetetes is common. Next in order come dark-red grits, sometimes marly, containing only a few fragments of Encrinital stems. Above these, pale flesh-coloured quartzite, and finally a white quartzite, in neither of which I ever found any fossils, and which form the highest peaks of the ridges composed of the Palaeozoic rock. The whole of these strata are in various degrees affected by cleavage and joints, which penetrate all the beds without regard to tlieir OF THE NORTH-WESTERN PROVINCES. 155 mineral character, although in a somewhat less marked degree in the limestones and quartzites. That the general sequence of these strata is pretty regularly maintained, I have seen over a longitudinal extent of about fifty miles, but it appears highly probable that their development has a far greater range, as we shall also see to be the case with some of the other groups of the fossiliferous rocks. “ Before passing on, I must observe the very remarkable simi- larity of general mineral appearance that Compared witli England. . -i . 1 1 0*1 • 1 subsists between the bilurian rocks 01 the Himalaya and of England. The peculiar pale tint assumed by many of these rocks answers most exactly to the descriptions given by Sir Roderick Murchison of the Silurian districts of Wales, and the characters of the concretionary limestones of both countries appear equally to correspond. Even in hand specimens the texture and appearance of the rocks and of the fossil impressions are so similar that they might most readily be mistaken one for the other. In pointing to these resemblances, however, I would not have it supposed that I should wish in any way to set up mineral character as a criterion by which to decide on the age of any rock. Never- theless, the facts, if they are to be relied upon, would appear to indi- cate that as we see the conditions of the existence of organic matter to have been generally similar over large areas, or even over the whole earth, during the same epoch, and to have changed with the progress of time, so likewise has it been with the conditions under which the mineral constituents of the earth have been aggregated. • > “ The Palaeozoic strata that I had an opportunity of examining in detail in situ , which I have just been Silurian predominates. 1 describing, appear to be exclusively Silurian, but the existence of rocks of Devonian or Carboniferous age seems to be shown by some of my specimens, not found in situ, which contain Productus, Clionetes , Athyris, Orthis, Aviculopecten, Spirifer. I may here be allowed to repeat that the higher portions of the .Silurian rocks being usually found at elevations of 17,000 or 18,000 feet, their examination is not a very easy task, and the difficulties occasioned by the great altitude are infinitely aggravated by the confusion into which the beds are thrown by the vast dislocations that have accompanied the elevation of these mountains. In con- cluding my remarks on the Palaeozoic beds I would observe that, T56 HIMALAYAN DIRTRT'CTS as a' general rule, to which, however, there are no doubt many exceptions, these rocks are to be found forming the summits of the highest passes between the British provinces of Kumaon and Grarh- wal and Tibet, which probably average 18,000 feet in elevation, and that the highest points of the ridges on which these passes are found not unfrequently reach nearly 20,000 feet in altitude. “ In proceeding along the section, we shall next observe some t . beds very remarkable from their apparently close similarly to the Trias of Europe. I can now only regret that, not having been sufficiently aware of their importance, their exact relation to the beds below them has not been better made out ; but their position in the series immediately above the Palaeozoic rocks is at least certain. In one place these strata were found in situ intermediate between the Palaeozoic and Secondary rocks, but the greater part of my specimens were obtained from fragments lying on the north slope of the Palaeozoic ridge, which appears to terminate with a line of fault, to the north of which a cliff of Oolitic age suddenly rises. From these strata I have obtained not less than twenty-five species of fossil shells, which is a remark- able Circumstance, considering the small bulk of the specimens that I was able to bring away with me. Mr. Salter, who has been so good as to examine these also, tells me that we have Ammonites several, Ceratites, Orthoceras , Natica, Exogyra, Halobia, ( Aviculci ), Pecten , Lima , Athyris , Walclheimia , Rynchonella , Spirifer. The Triassic beds were chiefly dark-coloured limestones and, where seen in situ , were associated with shales and dark-red grits, the latter of which seemed very similar to those found near the top of the Palseozoic series. The line on which they were seen was, however, a very bad one for determining such matters, for it was in one of the great valleys, and consequently on a great dislocation where accumulations of debris almost always greatly predominate over rock in situ. “ In our progress northward, we next come upon the strata that T . . form the representatives of the Jurassic sroun Jurassic senes. . ® 1 * As m the Palmozoic beds, so we here find the general dip to be to the north ; but it is impossible for me to offer any opinion as to the degree of conformability of any of these depo- sits one to another, owing to the great disturbances to which they have everywhere been subjected. It appeared to me, however, as OF THE NORTH-WESTERN PROVINCES. 157 probable that in the parts of the mountains that I examined, a great line of fault intervened between the Oolitic and Palaeozoic series. The mountain-ridge of Silurian age most carefully examined by me lies generally parallel to the line of strike, and along its north-east face runs a stream separating it from the Secondary rocks, which rise in an almost impassable precipice beyond. The section here exposed must be at least 5,000 or 6,000 feet in thickness, but the difficulties of the route prevented my extending my examinations into the' 'lower beds. The lowest that X reached weie of black lime- stones and shales, with very few organic remains, and those very imperfect. Above these lie several thousand feet of limestones of various descriptions, the rock in some places being almost made up of fragments of shells. Professor Forbes, who has kindly looked over my specimens from these beds, is inclined to identify some of the species with certain forms that occur in the Fuller’s Earth and Corn- brash of England ; and it appears that there is here no representa- tive of the Lias. “ Continuing to ascend in the series, we reach next a large devel- opment of dark-coloured shales which abound Oxford Clay. w jth remains of Ammonites and Belemnites, the former usually imbedded in spherical nodules, apparently of much the same nature as the shale itself, but exceedingly compact. The shale is for the most part, on the other hand, very rotten, and the band of country along which it is found is often depressed so as to form a valley, apparently in consequence of this disintegration of the rock. This shale Professor Forbes pro- nounces to be without doubt of the age of the Oxford Clay, a con- clusion indicated by the peculiar forms of the Ammonites , two of which seem to be identical with species found in beds of the same age in Kachh and Sind, which have been figured and described in PPq Transactions Greol. Soc. 1 The existence of these beds in the northern parts of the Himalaya was pointed out by Sir Roderick Murchison some years ago, as proved by the occurrence of some of these Ammonites, which he had seen. There is indeed direct evidence of the existence of these Oxford Clay strata for a distance of about 200 miles to the westward of the places where I have myself seen them, and their prolongation along the north of the > N. Ser., Vol. V. 158 HIMALAYAN DISTRICTS mountains for 200 miles more in an easterly direction is rendered highly probable by the well-attested recurrence of the Ammonites in the eastern parts of the kingdom of Nepal. Although we find stratified deposits apparently lying conformably on the Oxfordian strata, I cannot say anything definite regarding them, as they appear to be almost entirely devoid of fossils. They are very hard and compact, consisting of grits, shales, and limestones, and have not improbably been converted into their present state by the action of eruptive rocks which are of common occurrence in this region. 1 O [Subsequent to the publication of General Strachey’s papers in the Journal of the Geological Society, a description of his collections of fossils was drawn by Messrs. Salter and H. F. Blanford, and printed for private circulation. The following complete lists are taken from that work : — Si lu ei an Fossils. Asaphus emodi. Illaanus brachyonisus. Do. punctulosus. Cheirurus mitis, Prosopiscus mimus. Sphaeaexochus idiotes. Lichas Tibetairas. Calymene nivalis. Tentaculites sp. Serpulites sp. Nautilus ? involvens. Cyrtoceras centrifugum. Lituites iuliformis. Orthoceras striatissimum. Do. Kemas. Theca lineolata. Bellerophon Ganesa. Strophomena trachealis. Do . cheemerops. Do. umbrella. Do. aranea. Do. nubigena. Do. bisecta. Do. halo. Do. lineatissima. Orthis Thakil. Do. Tibetica. Murchisonia Himalensis. Do. pagoda Pleurotomaria turbinata. Raphistoma emodi. Trochonema htimifusa, Cyclonema rama. Do. subtersulcata. Holopea varicosa. Do. pumila. Ctenodonta sinuosa. Cyrtodonta ? imbricatula. Lingula Kali. Do. ancyloides. Leptfena Himalensis. Do. repanda. Do. cratera. Do nux. Orthis compta. Do. monticula. Do. uncata. Ptilodictya ferrea. Do. plumula. Spliaerospongia mclliflua. Oo. inosculans. Chaetetes ? Yak Heliolites depauperata. Carbonipeeous Fossils. Productus Purdonii. Do. Flemingii. Chonetes Vishnu. Athyris Roissyi. Aviculopecten hyemalis. , , J?., 1 873 p Mr * T - Hughes of the Geological Survey, brought some fossils from the Milam Pass. They were identified by Dr. Waagen as representing crestacJouT Jurassic, triassic, penman, carboniferous, and Silurian formations This briS the series here into fuller agreement with that described by Stoliczka in Western OF THE NORTH-WESTERN PROVINCES. 150 Ammonites floridus. Do. Aon. Do. Winterbottomi. Do. planodiscus. Do. diffissus. Do. Gaytani. Do. Ausseeanus. Do. Blanfordii. Ceratites Jacquemonti. Orthoceras pulchellnm. Do. salinarium. Natica subglobulosa. Belemnites sulcatus. Amonites acucinctus. Do. alatus. Do. bifrons. Do. biplex Do. communis. Do. concavus. Do. Eugenii. Do. Geravdi, Do. Griffithii. Do. guttatus. Do. Hookeri. Do. heterophyllus. Do. Himalayanus. Do. Hyphasis. Do. Jubar. Do. Medea. Do. Nepalensis. Do. octagonus- Do. robustus. Do. scriptus. Do. Spitiensis. Do. strigilis. Do. temiistriatus. Do. torquatus. Do. triplicatus Do. Tliouarsensis. Do. umbo. Do. Wallicbii. Triassic Fossils. Exogyra sp. Halobia Lommeli. Pecten scutella. Lima Stracheyi. Atbyris Deslongchampsii. Do. Strohmeyeri. W aldheimia Stopp'ani. Rhynclionella retrocita. Spirifer Oldliami. Do. Stracheyi. Do. Rajah. Oolitic Fossils. Anatina Avaginula. Myophoria Blanfordi. Cardium truncatum. Cyprina trigonalis. Astarte major. Do. unilateralis. Modiola sp. Nucula cuneiformis. Cuculhea virgata. Do. leionota. Inoceramus Hookeri. Lima acuta Do. gigantea. Do. mitiloidea. Monotis concenticus. Avicula echinata Do. imequivalvis. Pecten tequivalvis Do. comatus. Do. bifrons Do. monilifer. Do. Lens. Do. Sabal. Ostrea flabelloides. Do. acuminata. Terebratula numismalis. Do. - carinata. .Do. globata. Rhynconella variabilis. * Do. concinna. Acrosalenia ? Pentacrinites sp.] Turritella moutium. Pleurotomaria ? sp Turbo invitus. Cliemnitzia sp. « But the most striking feature of the geology of these mom- tains is probably that which I have next to Tertiary deposit. mention, viz., the existence of a great Terti- , ry deposit at an elevation of from 14,000 to 16,000 feet above the L; still preserving an almost perfectly horizontal surface. On crossing the watershed-ridge between the streams that flow to the uth into the Ganges, and those that fall into the upper part of the Satlaj to the north, which here constitutes the boundary between the British territory and Tibet (see map), we find ourselves on a plain 160 HIMA'LAYAN districts 120 miles in length and varying from 15 to 60 miles in breadth, that stretches away in a north-westerly direction. Its western por- tion is everywhere intersected by stupendous- ravines, that of the Satlaj being nearly o,000 feet deep. The sections afforded by these enable us to see that this plain is a deposit of boulders, gravel, clay, and mud of all varieties of fineness, laid out in well-marked beds that iun nearly parallel with the surface, and that hardly deviate from a horizontal position. The discovery of the fossilized remains of several of the larger mammalia distinctly marks the Tertiary age of this deposit. The existence of such fossil remains in the northern paits of these mountains had been long known, but we were alto- gether ignoiant of the precise locality whence they came, and had no facts before us from which any conclusions could be formed as to their geological import. The Mti Pass, from which it was said that the bones had been brought, was not the place where they were found, but one of the routes only by which they came across the great Himalayan chain from unknown regions beyond. Mi. Waterhouse, who has been so obliging as to examine So-called Niti fossils. ^ ie s P ec “ 2iens that I procured from these beds, informs me that he recognizes amongst them the following : — Metacarpal bone and distal end of tibia of Hippotherium ; patella of small horse ; distal end of radius of a larger species of horse ; distal half of tibia of a horse of very large size ; part of metacarpal of a horse ; upper end of tibia of bovine ruminant ; dorsal vertebra of a ruminant. Portion of head of an undescribed animal allied to goat and sheep, having, like them, prominent orbits, and the hords above the orbits; but which differs in the peculiar form the bony core of the horns. The horns are remarkable for being placed very near to each other at the base (their upper portions are broken off). There is a specimen in the British Museum, however, from the same locality, of an animal very like this, in which the horns are seen to be short, stout, and slightly bent outwards at the apex. Right wing of the atlas vertebra of rhinoceros ; phalanx of one of the outer hmd toes of ditto ? ; and portion of tooth of elephant ? Speci- mens of the bones of ruminants, pachydermata, and other animals from this district, presented to the Society by Sir Thomas Colebrooke and Dr. Traill, are in the Museum of the Geological Society I irmrlrm * OF THE NORTH-WESTERN PROVINCES. 161 u The bones that we have hitherto obtained from these strata are Actual Site as yet not almost all very miserable fragments, so that identified. jt is difficult even for the very learned natu- ralists that I have mentioned to do more than distinguish the genus to which they belong. It is therefore, I am afraid, at present impos- sible to come to any decided conclusions as to the identity or other- wise of the species here found with those of the Siwalik hills, a question of the greatest interest with reference to all our speculations on the geology of these mountains. The fossil bones I have not seen in situ nor indeed, curious to say, could I, in spite of every attempt, learn a definite locality in which any one knew positively that they had been found. But of the general position where they occur there can be no doubt, for, besides the common account of their being found in some of the ravines that traverse the plain, on many of the specimens quite enough of the rock in which they are imbedded has remained to enable me to recognize a fine-grained calcareous conglomerate exactly identical with beds such as I have seen intercalated with the boulder and gravel beds that consti- tute the mass of the deposit. Hills of limestone rise here and there above the general level of the plain, and it appears as though the calcareous matter derived from them had cemented together portions of the sands and gravels that were deposited near them. Probably of marine origin. “ The existence of such animals as I have mentioned as being found in these beds being a physical im- possibility in the present state of the country, there can be no doubt that the strata have been elevated, to their present height from some lower level since the time of their deposition. There is no direct proof that these beds are marine, no shells having been obtained from them, but I think on the whole that the probabilities appear to be in favour of this plain having been a true sea-bottom rather than of having been occupied by a detach- ed body of fresh water. The general extension of some of the older fossiliferous rocks along the northern face of the Himalaya over a great longitudinal distance is a fact of which we have tolerable proof, and it thence follows that the line on which they occur, distant about twenty or thirty miles to the north of the great line of peaks,, has probably been a sea-margin from the remotest ages of the earth’s history until as late as the Oolitic 21 162 HIMALAYAN DISTRICTS period at least. So far, therefore, there is nothing adverse to my supposition ; nor is the present interruption of the plain any proof that it did not once have a far greater extension. This is suffi- ciently proved hy my having traced these tertiary beds to the very top of the watershed-ridge in the vicinity of the Niti Pass, where they reach an elevation of upwards of 17,000 feet ; the summit of that pass being strewn with boulders that appear to be derived from the white quartizite capping the Silurian strata of the neighbourhood. Further, two or three miles to the south of the pass, a detached portion of this deposit is to be seen on the declivity of the moun- tain, which must have been separated from the general mass by the dislocations that have upheaved the whole country. It is, moreover, to be noticed that there seem to be grounds for supposing that plains, such as I have mentioned, are found in other parts of the chain under somewhat similar circumstances, which may not improbably have once formed portions of the same sea-bottom. The plain of Pamir, so long known from the accounts of Marco Polo, and the existence of which is fully corroborated by Lieut. Wood of the Indian Navy, in his Narrative to his Journey to the Source of the Oxus, may be its representative to the west ; while to the east the plains described by Turner as having been passed over during his embassy into Tibet, as well as others mentioned by Kirkpatrick as existing to the north of Nepal, the descriptions of which are quite confirmed by Dr. Hooker, are not improbably of a similar nature. Another argument in favour of the marine origin of this deposit is, I think, also to be derived from the very regular way in, which the beds of gravel and boulders are laid out, for which I should conceive that some action like that of the tides would be requisite. 1 1 No notice has been taken of these great detrital accumulations up to this, because they occur on the grandest scale in the regions described by General Strachey ; but every explorer in the Ladak country has noticed deposits of the same kind. In many cases they are very recent. The process of their formation has been very well described by Mr. Drew in the Quarterly Journal of the Geological Society for 1873. From the fossils enumerated above, it is, however, certain That some of them are very ancient The fact that General Strachey did not observe the actual site of these bones leaves it open to. conjecture whether they may not occur in some disturbed beds more or less covered by these horizontal gravels ; for it is very difficult to conceive how any great dislocation or upheaval of the moun- tains can have occurred without disarranging such incoherent materials. On the other hand, the fact that such large animals as the Yak, the Kiang, the Ovis Am- mon, &c., now flourish in the wild state in those bleak sterile regions suggests, that a moderate change of climate, without any great change of elevation, might make them habitable for the fauna now found fossil there. No evidence for marine action later than the nummulitic period is known within the Himalayan border, OF THE NORTH-WESTERN PROVINCES. 163 « X have already mentioned the occurrence of eruptive rocks in the Tibetan plateau. A great outburst, in Eruptive rocks. which are found hypersthene and bronzite, besides syenitic and ordinary greenstones, and various varieties of porphyry, occurs in the vicinity of the lakes which are found at the eastern extremity of the plateau (see map). The greenstone is known to extend considerably to the west, and forms, at an elevation of about 17,600 feet, the summit of Balcha, one of the Himalayan passes into Tibet which I have crossed. u Having thus given a general description of the geology of this General Strachey’s con- region, I shall, as shortly as possible, enu- clusions. merate the chief conclusions to which I have been led with regard to the physical forces that have been called into action in the formation of these mountains : — (a.) — The general extension of the chain along the direction of the strike of the strata is a phenomenon necessarily connected with the action of an upheaving force along a line. This longi- tudinal action is further evinced by the parallelism of the lines of eruptive action with that of the strike. The continuance of action of the upheaving forces along the same general line for a vast period of time, with occasional intervals of repose or of subsidence, is indicated along both the north and south faces of the Himalaya. The great depth at which the forces have originated seems to be proved by the regularity of the action along the entire length of the chain, as shown by the elevation of such a ridge as the Siwalik hills. (py — The granites appear to constitute lines of elevation, not of rupture ; but there seems to be no specific action produced by them on the dip of the strata, which they appear to leave generally unchanged. ( c .) — The greenstones, on the other hand, usually follow lines of dislocation of the strata, being sometimes apparently contem- poraneous, and at others intruded through rocks already consoli- dated. U.) The cause of the general north-easterly direction of the dip is obscure, although its occasional sudden reversal to south- westerly seems to indicate some connexion with the action of an upheaving force from below, or of violent lateial thiust. jtim Xlayan districts 104 (a) — T he lines of fracture of the strata are constantly either parallel or perpendicular to the direction of the upheaving force. The positions ot the rivers appear to be altogether dependent on the configuration of surface produced by these fractures ; while the con- figuration of surface, on the other hand, seems to be but slightly afiected by the action of the streams, of which there is rarely any visible sign at 200 feet above the present level of the waters, and never to my knowledge above 300 feet. (/•) — The fact of the granite of the great snowy peaks being seen in veins, penetrating the schists up to 20,000 feet, makes it highly probable that the granite must have been injected long- before the mountains received any considerable development. That this granite is older than the Silurian period is rendered probable by the comparatively unaltered state of the lower beds of the Azoic slates at the foot of the Pakeozic series, where almost in contact with it. ([/.') — The conglomerate bed near the bottom of these same Azoic slates shows the proximity of land at the time of its deposit, and indicates that some upheaval of land had already taken place near the present line of great peaks, possibly occasioned by the granite in question. (/«.) — The occurrence of pebbles of greenstone in the sandstones along the southern edge of the mountains shows that the exterior lines of greenstone are older than those beds of sandstone. (i .) — The frequent occurrence of boulders of the quartizites, slates, and greenstones of the outer ranges of mountains among the Ter- tiary deposits of the Siwalik hills shows that the Tertiary ocean washed the foot of those mountains. (j.) — The regular slope of the plains of Northern India up to the Siwalik hills, which rise suddenly from the flat ground, leads me to infer that the sea must have continued to reach at least as far as the foot of the Siwalik hills for some time after their upheave- ment. (/c.) — The rise of the Tibetan plain has not been caused by the granite eruption of the line of snowy peaks. That the greenstone rocks that abound in many parts of it have equally not caused it, is proved by the peculiar nature of the valleys among the hills to OF THE NORTH-WESTERN PROVINCES. 1G5 the west of the lakes, which must have been laid out level under water ; from which it is to be inferred that these eruptive rocks are older than the tertiary beds of the plain. The same thing is shown by the occurrence of worn pebbles of greenstone in the surface of the plain in the vicinity of some of the detached hills of that rock. (/.) — The former extension of the glaciers far beyond their present limits is a phenomenon that may be noticed almost every- where in these mountains, and may give rise at first sight to an Mea that there may here also have been some special period of cold corresponding to the glacial epoch of Europe. But it seems, I think, more probable that this is here only the result of a change of climate consequent on the upheaval of the great plains of North- ern India. (jjk) — The existence of ancient moraines on the tertiary plain of Tibet proves that the extension of the glaciers is post-tertiary. Now, if we conceive that after the rising of this plain to nearly its present elevation, the sea still continued to wash the foot of the Siwalik hills, as I have already said that I considered likely, it is clear that the climate of the Himalaya would have been far more moist, and that the quantity of snow that fell on the highest parts of the mountains would have been greatly in excess of what now falls there, causing a great extension of the glaciers beyond the limits to which they have now receded.” There are several points in the foregoing summary that might Remarks on the above be objected t 9 in detail, but it is hardly summary. necessary to point them out. With the much more extensive information iioav available than was at General Strachey’s disposal, one ought to be able to give a more precise account of the phenomenon under discussion. But one lesson of experience is caution. From all sides the geologists of Europe have been for long years hammering at the Alps ; yet the mode of formation of those mountains is still a subject of very vague specu- lation. What then can we expect from our fragmentary knowledge of Himalayan geology ? In one respect we seem to have the advan- tage : the much grander scale on which the phenomenon took place, and perhaps also the less advanced stage of the process, have result- ed in a somewhat less complexity of structure. 10(3 HIMALAYAN DISTRICTS The process of investigation is to find out as far as possible from these remnants of the formations, and their relations to each other, what were the conditions of the surface at the time of deposition of each, and what successive changes of conditions occurred. Thus General Strachey’s observations that the metamorphism of the rocks forming the crystalline axis and the introduction of the granite are of pre-silurian date ; that this axis of elevation was a shore of deposi- tion at that time, would be facts of prime importance in the early history of this region. It would give a prodigious antiquity to the be ginning of the Himalayan mountain system, for all subsequent disturbances have conformed in elevation with that which produced the gneissic axis. It may be remarked that this view is apparently in immediate opposition to what is now a very favourite theory of mountain-formation — that which connects these areas of special contortion and elevation with a preceding long-continued accumu- lation of deposits, and accompanying depression, in the same area ; whereby through the gradual rise of temperature in the sediments thus sunk to a considerable depth, expansion occurs, and also a softening of the rocks, including a yielding to the horizontal thrust in the earth’s crust, thus producing the compression and up-squeez- ing into mountains of the accumlated sediments . 1 In the simple application of this process the position of greatest elevation should approximately coincide with that of the preceding greatest deposi- tion, and not with the limit of the deposition, as we find it according to General Strachey’s observation. To this objection, and in defence of the theory, it may be very fairly argued, that the line of actual maximum elevation is due to denudation having removed the softer and more broken strata and left the more massive rock ; that according to the observation under discussion, the sedimentary series never passed across this primitive gneissic axis ; and that the position of greatest elevation (in the active sense of upheaval) occurred about the middle gneissic axis formed of meta- morphosed palaeozoic rocks, all the once overlying strata having been removed ; that but for this result of denudation we should have the crest of the Himalaya to the north of the upper valley of the Indus. 1 Notwithstanding the numerous recent claimants to this theory, the mechani- nal elements of it are essentially those given by DeBeaumont in his Systemes de Montagnes, p. 1318 ; the other ideas in it being due to two other equally eminent philosophical physicists, Herscliel and Babbage. OF THE NORTH-WESTERN PROVINCES. 167 The interpretation of the drainage system gives direct support to this view. It is an evident postulate of physical geology that along any line of elevation the drainage is originally transverse. The manner in which this primitive system becomes largely convert- ed into longitudinal drainage lines is explained in every text-book on geology. Now, making the fair assumption that the initial line of elevation coincides with the maximum line of upheaval, the main watershed of the future continent is determined by that initial line, and it is presumably a very permanent feature. Every geo- graphy book notes the fact that the Himalayan watershed lies far to the north of what is more particularly described as the Himalayan range, but the line of reasoning we have just indicated would sug- gest that the real axis of maximum elevation in the Himalayan system may coincide more or less with the watershed. We should thus have two magnificent examples of the process of drainage-con- versions above alluded to : the Indus and the Sanpo (Brahmapu- tra) now flow from about the same central position, having gradually worn back along the line of easiest erosion, cutting off in succession the originally transverse drainage along the whole line. The applicability of this theory of mountain-formation to the Himalaya system does not, however, depend upon the correctness of General Strachey’s view regarding the exceeding antiquity of the first gneissic axis. The gneiss there in early Palaeozoic times may have been a floor of shallow deposition Stoliczka’s views. ... ... .. ... .. , . without being a range limiting that deposition. Stoliczka does not adopt this latter view though, leaving it an open question. His own provisional identification of lithologically similar Silurian rocks in equal force to the south of the axis would, perhaps, suggest their original continuity across that axis. He hazarded very few remarks upon the general geology of the Himalaya, wisely postponing such considerations until the data would warrant something definite. He points out that the deposits of carboniferous age, filling only broken ground in variable thick- ness, represent the close of a general geological epoch. The Permian and lower Trias are not represented. He considers that after the Trias extensive upheavements occurred, laying dry large tracts that have not since been submerged. The J urassic basin was then approximately defined. The evidence for these conclusions is 168 iiima'layan districts of the n.-w. provinces. not given, and they seem difficult to reconcile with the general regularity of succession of the rocks. On his figured sections the Para limestone (Rlnetic group) is the only one that exhibits great inequality of distribution, being of considerable thickness on the north side of the basin, and altogether wanting to the south. His remarks would, however, assign at least an early Mesozoic age for the origin of some of the prominent features of disturbance now stamped upon the Himalayan system. The most notable features in the sequence of formations in the Himalaya is the position of the nummulitic deposits, as already mentioned. They are in greater thickness than any of the older formation sexcept the lower Silurian. Stoliczka speaks of them as having been deposited in the narrow basin where they now lie In- the very centre of the mountain region. This view strongly confirms that previously arrived at from the consideration of the same deposits at the south edge of the mountains : that long and extensive- denudation of the Himalayan area had preceded the Tertiary epoch. It seems to have been greatest, as would naturally occur, along the centre of the area of upheaval, wearing down to the metamorphic- rocks along what may then have been the back of a brord- flat tuberence of the earth’s crust. A comparatively slight settlement of the area, submerging only the more deeply eroded parts, would then have sufficed for the accumulation of those eocene deposits, and it seems possible that the production of the synclinal basins of the Central Himalaya — as was shown for the contortion of the infra- Ivrol beds of the Lower Himalaya — did not occur, or, at least, was not stron gly developed till the great compression upheaval in middle Tertiary times. CHAPTER IV. The Himalaya. contents. The outer Himalaya. Mountain systems; Jumna; Ganges; Kali. Subor- dinate boundaries. The Nayar. Western Ramganga ; Kali. The snowy range. Axis of highest elevation. The Tibetan plateau. Glaciers. Glacier of the Pindar ; feeders of the glacier ; moraines ; crevasses and ice tables. Glacier of the Kuphini. Motion of the Pindar glacier. Snow-line. Observations in the eastern Himalaya. Observations in Kumaon. Bisahr. Across the snowy range. Kumaon ; Garhwal ; Kunaor ; Western Tibet. Lakes. We have seen that the term ‘ outer Himalaya’ has different meanings according to the sense in which it The outer Himalaya. . g ugec p Geographers understand by it all the mountain systems lying between the snowy range and the plains of India, whilst in the western Himalaya geologists restrict its use to the limestone and slate formations that lie between the outlying tertiary series and the central crystalline axis. To the geologist Simla and Naini Tal are situate on the outer Himalaya, and Ka- sauli and Subathu are not ; whilst to the geographer all these hill sani- taria are on the outer Himalaya. To obtain a correct appreciation of the physical relations of the ranges of the outer Himalaya we cannot ignore their geological affinities, but we have as yet no geolo- gical details on which we can rely for the greater portion of their area. For the tract between the Tons and the Kali we have the record given in the preceding chapter and the map that accompanies it. A glance at this map will show us that the main line of gnei."^ and granite, which is almost conterminous with the region of perpe- tual snow, is met with between the eightieth and ninetieth mile from the foot of the Himalaya, and at a distance of from twenty to thirty miles south of the Indian water-parting. Between this line of per- petual snow and the plains there are numerous well-defined ranges, some seemingly spurs from the snowy axis, and of which the geolo- gical relation is not well established, and others having an apparent separate and independent existence. As we have already noticed, the traveller from the plains meets first an outer range, which has a general elevation of about 6,000 to 7,000 feet above the level of U 170 HIMALAYAN DISTRICTS the sea, and which in China above Naim Tal rises to 8,568 feet, and in a peak, on the Tirhi road, east of Masuri, to 8,565 feet This band or outer range has a general direction parallel to the plains, and is pierced by the greater rivers, such as the Tons, Jumna, Ganges, Ramganga (western), Kosi, and Kali. Between it and the ridges descending immediately from the snowy range we cross a number of subordinate ranges which are, as a rule, of considerably less elevation than the outer range. Between China and Dhakuri .Binayak, on the road to the Pindari glacier, a distance of forty-live miles as the crow flies, there is no peak having an elevation of 8,000 feet, and very few attaining to 7,000 feet. But further westward, in the same parallel, we have groups of peaks attaining an eleva- tion of over 10,000 feet, notably those connected with the Dudu- ka-toli range in Garliwal. When the river valleys close to the snowy range are reached, the increase in elevation is rapid and marked. The flanking ranges seldom fall below 10,000 feet, and aie clowned with peaks rising still higher, until the culminating ridge crowned with perpetual snow is met. If we carefully examine the great sea of mountains lying be- Mcrantain system. ' ^f n the outer Himalaya and the snows, we shall find that the dominating ranges are spurs from the great groups of peaks, remarkable alike for their elevation and the position they fill as the boundaries of the several river-basins. On the west, the western boundary of the Jumna system is found in the elevated ridge that has its origin in the group of peaks crossed by the Shatffl and Burenda passes. This ridge follows the left bank of the Satlaj in a south-westerly direction to Hatu (10,700 feet), where it bifurcates: one branch continuing Jumna system. tlie normal direction to Bilaspur, and the second proceeding in a south-easterly direc- tion by Chor (12,081 feet), where it forms the water-parting between the Giri and the Pabar branch of the Tons. A second great ridge, descending from the Jamnotri groups, and marked by the Deoban (9,347 feet), Chakrata (7,300 feet), Clhlmeri (7 160 feet), and Bairat (7,423 feet) peaks in British territory, separates the affluents of the Tons from those of the Jumna. The eastern boundary of the Jumna system is formed by a great ridge bavin o- its origin m the same group of peaks, and which joins the outer OF THE NORTH-WESTERN PROVINCES. 171 Himalaya near the Sarkanda peak to the east of Masuri (Mus- sooree). The eastern boundary of the Ganges system is found in the great ridge descending in a south-westerly direction from the Nandakot peak, and which passes along the left bank of the Pindar to its junction Ganges system. with the Alaknanda, and thence along the left bank of the Alaknanda to Deoprayag. It admits of two great bifurcations : one at the head of the Katyiir valley and one at the head of the Lohba valley. From the group of peaks at the head of the Katyur valley a branch passes in a south-easterly direction through Binsar and Dol and along the right bank of the Ladhiya to Barmdeo on the Sarda, and from the head of the Lohba valley a branch Y7’ * 1 * ll l ' runs south-by-east to Gujargarh, whence it passes almost due west to the Ganges at Kharak and Chandi. The tract to the south of these two arms is in shape a great obtuse- an cried triangle, with its base towards the plains and its apex in the group of hills to the north of Dwara Hat. It forms the mountain basin of the western Ramganga. The eastern boundary of this system forms the western boundary of the Kali system, of which the eastern boundary is found in a great ridge descending from the Api peak in Doti of Nepal. It is clear from the above brief description that it is the spurs from the snowy range that bound the river basins, and if we examine further the affluents of each system, we shall see that the ramifications from these spurs form the water-parting between each minor system. The principal affluents of the Jumna system are the Tons and the Giri. The Pabar, Rupin, and Supin unite to form the Tons, and are separated Subordinate boundaries. from each other by transverse ridges descending from the great boundary ridge. United they drain a delta-shaped basin having its apex at Kalsi. To the south-west the Giri drains a similarly shaped basin having its apex near Kalsi, and to the east the Jumna drains one having its apex at Kalsi. "W e find that the point of junction of the apices of these three deltaic basins lies within the Siwaliks, the outer range of geographers, and that the union of these three main affluents forms the Jumna of the plains. This basin, as well as the minor systems within it, is bounded by spurs from the great snowy range or transverse ridges descending from. them. If we 172 HIMALAYAN DISTRICTS . further examine the relations of the minor feeders of the three great constituents of the Jumna system, we see that, as a rule, they flow at right angles to their recipients, and that the affluents of these minor feeders obey a similar law. The ridge separating the Tons from the Jumna gives off feeders on the west to the Tons and on the east to the Jumna, at right angles to its direction. From the western slope the Dliaragad, Binol, Simula, and Manjgaon streams flow to the Tons, and from the eastern slope the Ihtlena, Kutni, and Silo seek the Jumna. Each of these minor feeders is separated from the other by lateral spurs, descending usually from some peak or knot of peaks, and all, as the veins on a leaf seek the midrib, flow towards the mid-depression and give it their moisture. The two great rivers that unite to form the Ganges are themselves the centres of subordinate systems. The Bhagirathi is divided from the Bhilang by a great ridge descending from the Gangotri group of peaks, whilst a second ridge having a similar origin separates the Bhilang from the Mandakini, an early affluent of the Alaknanda. The Bha- girathi unites with the Bhilang near Tfrhi, and the two rivers drain a delta-shaped ti'act having its apex at Deoprayag. Tire Saraswati and Dhauli, which form the head-waters of the Alaknanda, are sepa- rated from each other by a ridge of snowy peaks, and its more southern affluents, the Nandakini and the Pindar, are divided from each other by a great ridge descending from Trisul. The entire basin of the Alaknanda to its junction with the Bhagirathi at Deoprayag is thus a great delta-shaped tract, cut up by the minor feeders into subordinate systems that are bounded by great ridges descending from the snowy range. Between Deoprayag and Hardwar, the Ganges receives from the east the Nayar and the Hinnal, and from the west the Suswa that drains the Dehra Dun. All unite within the Siwaliks to form the Ganges of the plains. The Nay hr. We shall now take up the compact system of the Nayar in southern Garliwal, which at first sight would appear to be an exception to the general rules. We find that the boundary ridge that marks its exent is a continuation of the great ridge that, descending from the snowy peak of Nandakot, runs along the left bank of the Pindar to the head of the Lohba valley. Here, as already noticed, this ridge bifurcates ; one branch proceeding in the normal direction along OF THE NORTH-WESTERN PROVINCES. 173 the left bank of the Alaknanda to Deoprayag, whilst the second branch passes south to Gujargarh and then west to the Ganges at Kharak. These two branches mark the axis of highest elevation in the tract through which they pass. Following the western branch, we have the Dubri peak, 9,862 feet ; Dobri peak, 9,862 feet ; Gandkhola, 7,553 feet ; Devidatta, 7,034 feet ; Kankwala, 6,651 feet ; Gurdari, 5,893 feet ; Jhangarh, 5,878 feet ; and a peak about two ’miles from Deoprayag, 5,030 feet. Following the southern branch through Gujargarh, we find the second, Duda-ka-toli peak with an elevation of 10,180 feet above the level of the sea ; Barma- dungi, 9,190 feet; Nandatopa, 8,086 feet; Khamek, 7,152 feet; Gujargarh, 7,969 feet; Kliatti, 8,270 feet; Utai-n, 6,901 feet; Bukrari, 6,267 feet ; and Naugarh, about a mile above Kharak, 6,065 feet. Close to the point of bifurcation, the boundary ridge sends a lateral spur southwards, that divides the basin of the Nayar into two parts, that drained by the western Nayar or Chhiphalghat river, and that drained by the eastern Nayar or Kainyur stream. This great spur preserves the superior elevation of the boundary ridge, and is marked by the following peaks Barari, 8,499 feet; Bandani, 8,278 feet; Panjing, 8,810 feet ; Devitank, 8,849 feet ; Matikhal, 7,688 feet; and Chhatargah, 6,790 feet, when it is lost in the valley of the eastern Nayar near Kandui. Short ramifications from this spur or the boundary ridge itself determine the course of the minor feeders of the two great channels of the Nayar system. Thus a transverse ridge from Dubri, marked by the Tara-ka-kand (9,000 feet) and Banjkot (8,203 feet) peaks, divides the Clihiphal- ohat river near its source from its feeder at Paitliani on the left bank, whilst other ridges from Gandkhola, Devidatta, and other peaks, separate the other feeders the one from the other. A similar rule obtains along the course of the eastern branch, and we thus see that there is no real difference in principle between the arrangement of the drainage system of this apparently abnor- mal minor basin and that of the other greater systems already noticed. In the system of the western Bamganga, however, we have an arrangement for which we find an analogue Western Rdmganga. - n ^ a t 0 f the Bagmati in Nepal. As we have already seen, the basin of the Bamganga is in shape a great 174 HIMALAYAN DISTRICTS obtuse-angled triangle, with its apex towards the snowy range and its base towards the plains, thus filling up the gap between those systems that have their apices towards the plains and their bases towards the snowy range. Of its affluents, the Kosi alone has a considerable course within the hills, the remainder having their origin in or close above the elevated tract lying along the foot of the hills, and joining the Ramganga at some distance southwards in the plains. Here, although the main boundary ridges are still the spurs descending from the snowy range, the several streams do not unite within the outer range, but, like the Bagmati and its affluents, well beyond it in the plains. The Kali is known as the Yankti near its source, as the Kali during the greater portion of its course through the hills, as the Chauka T< o]l * or Sarda in the Bhabar and Tarai, and as the Sarju and Ghogra in Oudli to its junction with the Ganges, to the south of the Ghazipur district. The Kali basin is bounded on the west by that of the Ganges, and on the south-west by that of the western Ramganga. It receives from the west the Gori, Sarju, and Ladhiya, and from the east some small streams from Nepal, all of which unite within the hills to form the Sarda at Barmdeo. The Sarju is divided from its affluents, the eastern Ram- ganga, by a great meridional ridge, extending from their sources to their junction, whilst a second ridge, running in a south-easterly direction from the same group of peaks to Askot, separates the latter river from the Gori. The great Pancha-chuli range, running south-east from the line of water-parting, divides the basin of the Gori from that of the Hanna Yankti, and a similar snowy range having a like origin separates the Darma Yankti from the Kuthi Yankti. The great mass of peaks comprising Trisul, Nanda Devi, and Nanda-kot thus send forth great boundary ridges from their entire southern face to the west between the Riniganga and Nandakini : to the south-west between the Nandakini and the Pindar, and between the Pindar and the Sarju ; to the south be- tween the Sarju and the eastern Ramganga ; and to the south-east between the last river and the Gori. These indications are suffi- cient to mark the salient features of this portion of the Himalaya, and we reserve the details for the Gazetteer articles of this notice. OF TIIE NORTH-WESTERN PROVINCES. 175 The snowy range. The mountain system lying between the snowy range and the plains may therefore be said to consist of an outer range parallel to the snowy range and connected with it at wide intervals where it meets the great ridges descending therefrom. These latter bound the river basins, and the ramifications from them determine the course of the minor feeders of each system. We have now to consider the snowy range itself, and in these provinces at least it is a well-marked feature, lying from ten to twenty miles to the south of the Indian water- parting. The line of snowy peaks seen from Naini Tal and Masuri all lie to the south of the passes by which travellers cross into Tibet. The route by Nilang in foreign Garhwal through the Jadh valley crosses north of the Jamnotri group ; that by Mana in Bri- tish Garhwal lies to the north of the Kedarnath group ; that by Milam in Kumaon behind the Nanda Devi group ; and that by the Lanpiya-dhura, also in Kumaon, behind the Panchachuli group. The Jadh Ganga runs in a valley parallel to the snowy range and the line of water-parting, at an elevation of 15,000 feet above the level of the sea, near its source at Sumla, but gradually falling to below 9,000 feet at its junction with the Bhagirathi, near Bhairon- gliati. The horizontal distance between these two points is a little over 17 miles, and the fall is therefore over 350 feet in a mile. The Vishnuganga or Saraswati descends from the Mana Pass at 18,000 feet above the level of the sea to Vishnuprayag, a distance of some 35 miles, where it is little over 5,000 feet. Here we have an average fall of about 370 feet in the mile. The increase in elevation from the place where the river valleys enter the area of greatest elevation is equally marked in the valleys of the Dhauli, the Gori, and the Darma river. Dliarcliula on the Kali, before the line of snowy peaks is reached, is only 2,750 feet above the level of the sea ; whilst Golam La, to the north and above that line, and about 1,500 to 2,000 feet above the bed of the Kali, is 8,000 feet above the level of the sea. The bed of the Kali at Changru is 10,000 feet, and in the twenty-five miles between it and the Lanpiya-dhui a Pass the fall is over 8,000 feet, giving an average fall of 400 feet to the mile. These facts well illustrate the law that the river beds 1 to within a distance of ten miles in a direct line from. the snowy peaks seldom 1 See page 8. 176 HIMALAYAN districts exhibit a rise of more than four or five thousand feet ; but when we cross the line on which the great peaks are situated, the ascent very rapidly increases, and a very few miles carries the river-bed up to an altitude of nine or ten thousand feet, thus showing that the sudden increase of height of the mountains along this line is not confined to the peaks alone, but is a general elevation of the whole surface. This sudden and steady rise in elevation when the line of snowy Axis of highest eleva- speaks is reached appears to be a well- tl0n - marked feature of the entire Himalayan range. The snowy peaks, however, do not occur in a continuous ridge, but in masses separated the one from the other by deep depres- sions that form the line of drainage for all the surplus moisture of the tract between the snowy range and the line of water-parting to the north. These depressions are, so far as we know, a more distinc- tive feature of the Indian than of the Turkish slope of the Himalaya- Tibetan mass, a fact doubtless due to the greater rainfall received by the former. The influence of the monsoon on the southern slope is shown in its supporting a more dense and varied vegetation, and even on individual ranges and hills the southern exposure is similarly strongly marked in Kumaon. It is the ceaseless action of water that has furrowed out these valleys from the great mass, and natur- ally this has been accomplished on a greater scale and with more results along the southern slope that receives the full force of the periodical rains. The mass of peaks known as the Gangotri, Kedarnath, and Badrinath groups, are separated from the next group to the east by the valley of the Saraswati, and this group again from the Nanda Devi mass by the Dhauli river. The last is again divided from the Panchachuli group by the valley of the Gori, and the latter from the succeeding group by the Darma valley. All these valleys are inhabited and cultivated during the summer and rains, and some of them are comparatively of consider- able extent. The masses of snowy peaks are more like the terminal ends of huge spurs descending from the line of water-parting than a continuous ridge. They, however, occur in regular sequence along the entire line of the Himalaya, and, as seen from the plains, have the appearance of a connected chain. The following table, show- ing the principal peaks that occur throughout some eleven degrees of longitude, will give some idea of their number and importance. or THE NORTH-WESTERN PROVINCES 177 Points on the Himalaya mountains arranged in order of longitude by Mr . Trelaivny Saunders, from the records of the G. T. S. Number. Name of peak. Latitude. Longitude. Altitude. I. Chumalari , • 27° 49' 37" 89° 18' 43" 23,944 II. Gipmochi SB* 27 1C> 23 88 56 37 14,518 III. Pauhunri (Donkia)... • • • 27 5G 52 88 53 5 23,186 IV. Chumunkn ( Chola) . . . 27 27 28 88 49 38 17,325 17,572 V. Black rock (Guaream) 27 34 7 88 48 39 VI. Narsing... 27 30 36 88 19 28 19,146 VII. Pandim... 27 34 34 88 15 35 22,017 VIII. IX. Kanchanjlnga 27 27 41 42 26 5 88 88 11 11 50 26 27,815 28,156 X. Kabru 27 36 26 88 9 15 24,015 XI. Jannu 27 40 52 88 5 13 25,304 XII. 27 39 55 87 7 56 ... XIII. Sihsur 27 53 18 87 7 54 27,799 XIV. Chamlaug E. 27 46 27 87 I 21 24,020 XV. Mount Everest 27 59 12 86 58 6 29,002 XVI. Cliamlaug W. 27 45 16 86 51 56 22,215 XVII. Sankosi 27 45 11 86 36 57 22,826 XVIII. 27 52 46 86 31 57 21,987 XIX. 27 58 13 86 28 32 23,570 XX, 27 57 48 86 22 42 23,447 XXI. 27 57 24 86 9 8 19,560 XXII. Jabjibiya 2S 7 36 85 54 42 21,853 XXIII. 28 21 3 85 49 21 26,305 XXIV. • • • 28 10 20 85 48 17 22,891 XXV. Dayabang 28 15 17 85 33 35 23,762 XXVI. Akn 28 23 25 85 10 12 24,313 XXVII. 28 20 38 85 7 24 23,313 XXVIII. ■ 5 Yassa 28 25 58 84 41 0 25,818 XXIX. 28 30 7 84 36 34 25,729 XXX. 28 32 55 84 36 9 26,680 XXXI. 28 39 39 84 21 56 ,,, XXXII. 28 39 21 84 20 32 • . . XXXIII. Barathor 28 29 18 84 13 56 22,947 XXXIV. 28 32 0 84 9 52 26,069 XXXV. 2S 32 6 84 7 32 24,718 xxxvr. Morshiadi 28 34 58 84 1 57 24,780 XXXVII. 28 29 37 83 59 22 22,964 XXXVIII. 28 29 48 83 59 20 22,986 XXXIX. 28 35 38 83 51 46 26,522 XL. 28 30 59 83 50 55 23,641 XLT. 28 39 11 83 46 22 22,471 XLII. 5 ? Dhaulagiri 28 41 43 83 32 9 26,826 XLIII. Karayani 28 45 39 83 25 52 25,456 XLIV. 28 45 8 83 25 12 25,299 XLV. • • • 28 43 56 83 24 18 24,912 XLVI. 28 44 2 83 21 20 25,095 XLVII. 28 40 21 83 19 6 23,565 XLVIII. . . . 28 43 49 83 15 9 24,181 XLIX. 28 44 47 83 11 18 23,779 L. 28 44 30 83 9 29 21,727 LI. 28 45 53 83 8 27 21,472 L1I. Chanbisi 28 49 33 82 39 33 19,415 f, LIII. Api 29 59 7 80 56 22 LIV. Padchachuli 30 12 51 80 28 9 22,673 LV. ... 30- 15 12 80 25 5 21,471 23 178 iiimXiayan districts Points on the Himalaya mountains arranged in order of longitude by Mr. Trelawny Saunders from the records of the G. T. S . — ■ (concluded.) Number. Name of peak. Latitude. Longitude. Altitude. LVI. Nandakot lit 30° 16' 51" 80° 6' 39" 22,538 LVII. .Nan da Devi • •• 30 21 58 80 2 21 24,417 LVIII. Nanda Devi ... . . • 30 22 31 80 0 50 25,661 LIX. Do. # • • 30 22 35 80 0 45 25,587 LX. East Trisul • •• . . . 30 16 14 79 54 51 22,342 LXI. Do. 30 30 56 79 54 31 23,092 LX II. West Trisul ... 30 18 43 79 49 7 23,382 LXI1I. Nandakna • • • 30 22 9 79 45 40 19,916 LXIV. Do. Ml 30 20 56 79 45 36 20,722 LXV. Do. • • • 30 20 57 79 45 35 20,773 LX VI. Do. , , 30 41 6 79 44 53 22,093 LXVII. Kamet (Ibn Gamin) 30 55 13 79 38 4 25,373 LXVIII. Nilakanta • e • 30 43 52 79 26 56 21,661 LX IX. Badrinath • • • 30 44 16 79 19 20 23.210 LXX. Do. • • • 30 43 2 2 79 17 52 82,511 LX XI Do • • • • • • 30 46 44 79 16 58 22,347 LXX II. Kedhrnath • •• • • t 30 47 53 79 6 34 22,790 LX XIII. Tharl asagar ... • a. 30 51 40 79 2 14 22,582 LXXIV. Do. • • • Ml 30 51 41 79 2 13 22,628 LXXV. Jaonli • • • 30 51 18 78 53 53 21,672 LXXVI. Bas or Srikanta • •• 30 57 25 78 50 50 20,149 LX XVII. Bandarponchh 31 0 12 78 35 45 20/758 LX XVIII. Jamnotri ... ... '31 0 25 78 34 6 20,038 LXX1X. Swargaruini .. . 31 0 8 78 32 32 20,405 After crossing the line of water-parting which, as we have seen, , lies at the valley heads to the north of the 1 lUGttlll plclt6Rlli t line of snowy peaks, we come upon the great Tibetan plateau which has a mean elevation of from 13,000 to 17,000 feet above the level of the sea. Puling on the plateau by the Nilang route is 13,800 feet, Chiurkung on the Mana route to Totling is 15,700 feet, Chitung-dhar on the Unta Dhura route to the Satlaj is 15,810 feet, and Buljuing near the head- waters of the Karnali is 15,850 feet. Rabgyaling is 14,000; Gartokh, 14,240 feet; Tirthapuri, 14,820 feet; and lake Rakas Tal over 15,000 feet above the level of the sea. Captain H. Strachey has described 1 the Tibetan tableland lying between the Indian and Turkish water-partings “as the flat top of a great embankment exhibited in all its thickness in the scarp of the Indian Himalaya : the summit, though deeply corrugated with Valleys and mountains in detail, being in its general relief laid out horizontally at a 1 On the physical geography of Western Tibet : London, 1854; OF THE NORTH-WESTERN PROVINCES. 179 height little inferior to that of its southern scarp.” Although the highest summits yet known and measured lie along the Indian slope, very lofty peaks have been seen in all parts of the interior, “and the passes which must be crossed to get from one Tibetan valley to another, even in the very central axis of drainage, generally equal those by which Tibet is reached from India:” so that, on the whole, Captain Stracliey was of opinion that the medial depression is but faintly marked in the beds of’ the great rivers without much affecting the mean elevation of the mass. His description of the mountain system of that portion of Tibet lying to the north and west of Kumaon is the best that we possess, and will usefully conclude our brief review of the features of this portion of the Himalaya-Tibetan mass. “ The mountains that com- pose the bulk of West Nari are not easily understood or defined. On ascending the highest passes we can seldom see anything but a contracted view of mountain tops on all sides, looking very like chaos: no general view of. ranges under our feet is ever obtainable as the passes naturally select the ravine-lieads and lowest points of the ridge which are not only flanked but often almost surrounded by the higher summits ; and the valleys are commonly so steep and narrow, especially in the Bong country, that the view can hardly ever penetrate to an alluvial bottom and the sight of any inhabited place from a pass top is most unusual. When travelling along the bottoms of the valleys, we generally see nothing but a narrow tortuous passage between steep rocky walls, shutting out all extended view, and rather concealing than exhibiting the mountain ranges of which they form but the lowest outworks; consequently it is only by an extended series of observations and inferences, joined and assisted by maps, that any regular arrangement of these mountains can be distinctly established, and my account of them is liable to error in proportion to the defects of my own map. The general plan of the mountain system appears to me to consist of a series of parallel ranges running right across the breadth of the tableland in a direction so extremely oblique to the general extension of the whole as often to confound the one with the other, or to convert the transverse direction to a longitudinal one. The annexed figure may help to explain this. Short transverse necks connecting the main ranges in some parts, and cross fissures cutting through 180 HIMALAYAN DISTRICTS them in others, together with projecting spurs of a secondary- order, will / V Such connecting necks, when above 18,000 feet, become more or less confounded with the main ranges, and, if not above 17,000 feet, often appear as low watersheds, just dividing the heads of two val- leys lying in one line, but draining opposite ways. Secondary spurs also may be so high and so obliquely joined to the primary ranges as to make it difficult to distinguish between the two ; and the cross fissures may sometimes admit a main river to pass through a main mountain mass, in which case the continuity of the" range is often evidenced by the extreme narrowness of the rocky gorge or height steepness, and geological correspondence of its sides. Much of the Indian watershed seems to be formed in this way, the great snowy peaks lying mostly on the terminal butt-ends of the primary ranges, sometimes widened by lateral spurs, and the Tibetan passes crossing the low connecting links, whose alignment forms the main watershed, but not the main mountain crest.” It seems strange that so late as the year 1847 the occurrence of glaciers in the Himalaya was considered a matter of doubt by the learned in Europe. There is now no fact more widely attested and more thoroughly established than the Glaciers. ^ ' existence of glaciers at the head of almost every valley that descends from the ranges covered with perpetual snow. In size and importance they also fitly compare with those stupendous peaks around them that have placed the Himalaya in the foremost rank of all the mountains of the earth. Colonel Gordon gives us 1 illustrations and descriptions of the great glaciers 1 Hoof of the World, 17. / OF THE NORTH-WESTERN PROVINCES. 181 mot by the Yarkand Mission on the journey between Leh and the Karakoram pass. He mentions the lower Kumdan glacier that comes from the high peaks to the north-west, and continues down the right bank of the stream for over two miles, “ forming a perfect wall of ice, rising from the water about 120 feet, and showing a surface covered with countless pinnacles and points.” The Benin olacier, also seen by Colonel Gordon, rises amongst peaks and ridges from 19,000 to 24,000 feet high. “ It is about 21 miles in length and from one to one and three-quarters mile broad, termi- nating at an elevation of 15,800 feet above the level of the sea, with a width of about three miles of gigantic cliffs of ice fully 250 feet hi o h.” He adds : — “ the glaciers of the western Himalaya are twice as extensive as those of the Alps, and are probably the largest in the world, or at all events larger than any others out of the polar reo-ions. One in the Muztagh range is believed to be 34 miles long with fifteen distinct moraines ; while in its immediate vicinity is another, 31 miles in length, which may be said to join with it in making 65 miles of continuous ice.” Other glaciers have been described by travellers in the ranges between Ladak and Garhwal. In the tract with which we are more immediately concerned we have glaciers at the head of the Jadh Ganga, the Bhagirathi, Vishnu Ganga, Dliauli, Kailganga, Sundardliunga, Pindar, Kupliini, eastern Ham- ganga, Gori, and Darina Yankti. Lieutenant Weller 1 in his visit to the source of the Gori near Milam, describes that river as coming “ out in a small hut impetuous stream at the foot of appa- rently a mass of dirt and gravel some 300 feet high, shaped like a halfmoon. This is in reality a mass of dark-coloured (bottle-green) ice, extending westward to a great distance, and covered with stones and fragments of rock which in fact form a succession of small hills.” Here and there were circular and irregularly shaped craters (as it were) from 50 to 500 feet in diameter at top, and some of them 150 feet deep, and higher up these gave place to narrow fissures. This glacier is between seven and eight miles long, and terminates at an elevation of 11,600 feet above the sea. The glacier of the Pindar in Kumaon is the one, however, regarding which we have the most complete informatiom, and we shall confine ourselves, therefore, to its description in detail. i J„ A. S., Ben, XI., 1166 . 182 HIMALAYAN DISTRICTS Glacier of the Pindar. The Pindar river 1 is an affluent of the Alaknanda, and has its rise in a glacier to the west of the Nandakot peak and its valley, where the glacier ends, is about a mile across between the precipitous mountains that bound it. From the foot of the rocks on either side the bottom of the valley slopes inwards with a moderate inclination, leaving in the middle a hollow about 300 yards wide and 250 feet deep, with very steep banks, at the bottom of which flows the river. This comparatively level space between the precipices on either side and the river bed is observable for a mile or more below the end of the glacier, though much cut up by watercourses. The glacier occupies about two-thirds of the whole breadth of the head of this valley, leaving between itself and the cliffs on the east an open grassy slope, which extends along the foot of the moraine for upwards of a mile and a half above the source of the river, and which seems to be a continuation of the level space before mentioned. The first appearance of the glacier is thus described : — “ It seems to be a vast rounded mass of rocks and ground utterly devoid of any sign of vegetation, standing up out of a grassy valley. F rom the foot of its nearer extremity the river, even here unfordable, rushes in a turbid torrent out of a sort of cave ; the top of which is but a few feet above the surface of the water (May). The end, immediately over the source of the river, is very steep and of a dull black colour. It is considerably fissured, the rents appearing to arise from the lower parts, tearing themselves from the upper by their own weight. On a closer examination this abrupt end proves to be a surface of ice covered with sand and gravel and curiously striped by the channel made by the water that runs down it as it melts. Behind this, the glacier rises less steeply, like a bare gravel hill, to its full height, which is probably aboutJ).QfLfeet above the water of the river when it leaves the cave. In some places, however, are seen great fissures both vertical and horizontal, the latter evidently made by the separation of regularly stratified layers.” The glacier is formed by the meeting of two ice streams from gorges, one coming from the north-west and the other nearly from the east, and which 1 From “ A description of the glaciers of the Pindar and Kuphini rivers in the Kumaon Himalaya,” by Lieutenant R. Strachey, Ben. Eng., J., A. S B. XVI 794, and “ Note on the motion of the glacier of the Pindar in Kumaon”by the same. Ibid., XVII., ii., 203, and given as nearly as possible in the writer’s words as the only scientific examination of these glaciers that we possess. Feeders of the glacier. */. A. S. BenJXVL 706 ' — . OF THE N ORTH-WE STERN PROVINCES. 183 Kippt about two miles above the source of the river, as shown in the accompanying sketch. The feeder from the north-west is larger than that from the east, and its surface is at a considerably higher level for some hundred yards below their first junction. It descends with a great inclina- tion, entirely filling the gorge, down which it comes in a cascade of ice. It assumes the general appearance of a confused mass of irregular steps, which are again broken up transversely into peaks of every shape. The west side of this 'cascade continues nearly in its original direction after having passed the point below which the glacier bends sharply to the south-west, and in this way completely crosses the glacier. The steps in which it falls, however, also gradually change their direction so as to remain nearly perpendi- cular to the general current of ice. The transition to the regular level ice is very sudden, and begins much higher up on the west than on the east side. Near the foot of this ice-fall the steps were observed to have their tops considerably overhanging. A small tributary, also descending in cliffs of ice, joins the main glacier from a ravine on the east, not far above where it takes the sudden bend. The feeder from the east is formed by the union of two smaller glaciers, one from the north-east and the other from the south-east, which is the larger of the two. The north-eastern tiibu- tary appeared to have no very steep inclination, but was considei- ably broken up at its junction with the , ’other. Another small, glacier joins the main one from the north-west, a short distance below the point where it bends southwards. Its in clinatio n is \ei.y gieat, but it perfectly maintains its continuity of structure to the bottom. The lateral moraine of the west side of the northern branch of the glacier is first seen near the bend, where Morames ‘ it shows itself as a black-hand along the edge of the ice which in other parts of the fall is quite whi£g, The moraine is small between the bend and the tributary glacier below it, but very rapidly increases, and in its lo wer parts is a chaos of desolation. This great addition to the size of the moraine is owing to the quantity of ddbris brought down by the small glacier. The ice below the junction is much broken up by crevasses, and rocks and gravel from the moraines on both sides of the tributary glacier are scattered over the space between them, and the moraines at 184 HIMALAYAN DISTRICTS first sight seem to lose their distinct form. Although there is no clear ice between the moraine that originates on the east of the tributary and the west side of the glacier, the identity of that moraine is sufficiently marked by its colour and by the regular rise above the general surface of the glacier of its top, which remains tolerably even for some way down, being beyond the limit of the disturbance caused by the prevasses along the edge of the glacier. About half way down to the lower end of the glacier, however, the full action of these crevasses reaches the whole of the moraine, and it is scattered or lost sight of in the general confusion of surface. An epoch of peculiar destructiveness to the mountains is marked in one part of this moraine by the accumulation of huge masses of rock from 20 to 30 feet square and as much as 15 feet high, and the stone found on it are generally larger than those on any of the other moraines. The true west lateral moraine, below the tributary glacier, is not very large, nor is its top much elevated above the bottom of the valley, excepting quite at its end. The lateral moraine of the south-eastern side of tlio glacier is Its tojy rises, on an average, probably 250 feet above the bottonyof the _ valley. Along its foot runs a stream, gradually inci easing in size, that collects the open drainage of the outer slopes of the moraine. The lower part of this slope is a mass of loose stones and earthy gravel which rolls down from above, as the face of the ice which is visible in the upper fifty or sixty feet of the slope melts and recedes, a process that is constantly going on. On the inner side the slope of the moraine is thirty or forty feet above the level of the clear ice of the glacier. The upper part of the moraine comes down nearly straight from the point where it meets the foot of the north moraine of the east glacier. The north branch glacier being considerably higher than the eastern, the moraine slopes down from the bed of the former to that of the latter, forming a deep angular depression where they meet, that gradually diminishes in depth up to the top of this glacier, which i&Jiare ^en tirely cov ered with debris, the moraines of its two sides being scattered all over it for -some distance above its union with the north or mam branch. The resulting appearance is that the northern branch runs over the eastern, or that the latter runs into the former and is- absorbed by it. The eastern tributary brings VMM>5£ S ' '' '■■■ v\ '"|| PfMgPIP ■■■Pi?. ■ : - •- WM&& Foot of th& Pindar Grinder: OF THE NORTH-WESTERN PROVINCES. 18-5 down moraines that spread over the whole of its breadth at its i2iX extremity. Besides these lateral moraines there is a^medial one that is first seen as a dirty stripe along the 4s&. cliffs of the fall at the head of the north glacier. As it comes down the level ice it gradually begins to assume the decided appearance of a moraine, and increasing by degrees at last becomes very large. It conti- nues in a well-defined form for some short distance beyond where the western moraine is dispersed, but there it also is scattered over the ice, and the two become blended together, and ultimately extend to meet the debris, which is similarly dispersed by the eastern moraine from the opposite site of the glacier. The whole of the moraines, in the middle of the length of the glacier where it is most regular, are very considerably raised above the general surface of the ice, which in some parts may be as much as one hundred feet below the tops of the western and medial moraines. It would appear that this great elevation is not so much due to the accumulation of debris as to the protection afforded by the superin- cumbent rubbish to the ice below which prevents its being melted. The clear ice beyond the moraine is constantly depressed where ex- posed, and on the very tops of the moraines pure ice was often seen f hardly covered by stones. The protection afforded by the lateral moraines raises the sides of the glacier so much that a very consi- f derable hollow is caused in its middle, which is a striking feature in the first appearance of its lower extremity. 4 '2 The ice of which the glacier is composed is perfectly pure and clear, but where seen in considerable masses, Crevasses : glacier tables. , . „ , , , . . . i stripes of a darker and lighter bluish green are distinctly visible. It is composed of bands of ice containing small air bubbles, alternating with others quite free from them. In many places the surface presents a striated appearance, arising from the different degrees of compactness of these differently co- loured bands and their consequently different rates of melting. The direction of these coloured views as seen in crevasses showed a dip inwards or towards the longitudinal axis and a dip upwards or towards the origin of the glacier in every part, the stratification being more perpendicular towards the head and more nearly horizon- tal in the lower parts. The direction of the strata in place was also very clearly marked in many parts of the ice, and was placed in 24 186 HIM/LATAN DISTRICTS curves, having their branches nearly parallel to the sides of the glacier and their apices directed downwards, the curvature in the centre not being at all sudden. No dirt bands were observed. The crevasses were neither very numerous nor very formidable. They are developed across the direction of the glacier’s length on both of its sides, commencing from the small tributary on the west side and from the union of the eastern glacier on the other, and continuing almost to the end, those on the west side being, perhaps, the larger. They are generally wider towards the edges of the glacier, closing up as they approach the centre. They are nearly vertical, and are directed from the sides upwards or towards the head of the glacier, those on the west bearing nearly east and west, and those on the east bearing nearly north and south, thus forming angles of about 45° with the axis of the glacier. Many pools of water ( Ixdgnoirs ) were seen on the surface of the ice ; some of the largest were said by the guides, who are in the habit of visiting the glacier, to be found in the same place every year. The clear surface of the ice everywhere assumes a more or less undulating appearance from the action of the water that drains from it as it melts and the small ! streams, into which the drainage collects, end by falling into some of the crevasses. The remains of the last winter’s snow was hardly perceptible on any part of the glacier. The occurrence of stones standing up on bases of ice ( glacie r tables) above the general sur- face of the glacier is common, but those seen were small. The rocks below the bead in the north-western glacier were covered with grooves or scratches, sloping in about the same direction as the surface of the ice at the spot. These grooves extend to twenty or thirty feet above the present level of the glacier. Almost in every place a space was left between the rock and ice, the latter appearing to shrink from contact with the former, due doubtless to the heat i of the rock melting the ice. The Kuphini river, that rises on the side of the Nanda-kot j 5 T „ ... peak, opposite to the Pindar river, has also Glacier o± the Kuphim. its source m a glacier. Both rivers unite at Dwali, about eight miles from the end of the Pindar glacier and about six miles from the end of that of the Kuphini. General Strachey examined the Kuphini glacier also, and describes the valley for a mile or two below the end of the glacier as having OF THE NORTH- WESTERN PROVINCES. 187 very much tlio same general character as that ol the Pindar, but somewhat more rugged and desolate in appearance. The glacier commences about two m iles above the source of the river and fills the whole breadth. 'of the valley,, which is about three-quarters of a mile broad in its upper part. The glacier begins in a precipitous fall of ice some sixty or seventy feet high, which, however, still exhibits the rjbhqn-lfr e structure. From the foot of the fall the • surface was very even, though the slope was still considerable. The main glacier of the Kuphini is joined by two small tributaries on the east and by one on the west, all of which are highly inclined and bring d own considerable quantities of debris.. The moraines are confined, to the sides of the glacier, though many small stones are scattered over every part of the ice. As was obseived \\ \\ on the Pindar, the protection given, by the lateral moraines to the underlying ice leads to the promotion of a medial depression in the glacier at its end. The crevasses here, too, are most strongly marked near the sides and are inclined at an angle of about 45° from the longitudinal axis downwards. The structure of the ice was in all respects similar to that found on the Pindar. On the in- teresting question of the e ^ension o L glacier ,a^ ; rjpgotej^igd the inquiries of General" Strnchoy give.no precise information. He, however, considers that “some very decided change m the state of things is certainly indicated by thc^ long plateaus before mentioned running for a mile or tw,o below the present termina- tions of both glaciers nearly parallel to the rivers, but several hundred feet above them.” * He considers it “ impossible that these level banks above the rivers have been caused by deposits from the ravines in the sides of the valleys, for such deposits would have had very irregular surfaces, and indeed their present effect in destroy- ing the regularity of the plateaus is everywhere visible. Had the same appearance been noticed in any other part of the river’s course, it would at once have been attributed to the action of water at some former period, and it would have been supposed that the bed had afterwards been excavated to its present depth. It this was the case, the glaciers which the plateau was forming must either have terminated considerably higher up the valleys or have stood altogether at a much higher level. In either of these ways the water could have been delivered at a level sufficiently high to 188 HIMALAYAN DISTEICTS form the plateau. But it may admit of doubt whether the quan- tity of water in the rivers, as they are at present, is sufficient to account for such an extent of level deposit or for such a depth of erosion of their beds ; for at this great elevation they are not subject to those violent floods that occur lower down, and for nearly half the year too they are inert. The only other way of account- ing for the appearance is that it has been occasioned by an extension of the glacier, and that the le vel top of the plateau shows the limit to which the tops of the moraines reached, as the glacier gradually receded.” We have referred on a previous page 1 to the existence of evidence of glacial aetion far below the present limits of glaciers, and to those who wish to- pursue the subject further we commend the records of the Geological Survey and the summary 2 in the re- cently published ‘ Manual of the Geology of India.’ General Strachey has rendered us another important service in Motion of the Pindar his observations on the motion of the Pin- glacier ' dari glacier recorded in May, 1848. His procedure is thus stated. About 200 yards below the small tributary that enters the main glacier from the north-west a moraine was found heaped up against an almost perpendicular wall of rock, and suffi- ciently high to command a view of the greater part of the surface of the glacier along the line on which observations were to be made. This line, which is nearly perpendicular to the general direction of the glacier, was marked by two crosses painted white, one on the rock in contact with the old moraine and one on a cliff on the opposite side of the valley. A stake was driven into the moraine at its highest point, close to the rock, on the line between the two crosses, and a theodolite was set up over it. Five other marks were also made on the glacier at intervals along the same Jine by fixing stakes in holes driven in the ice with a jumper. These marks, which were all carefully placed on the exact line be- tween the crosses by means of the theodolite, were completed at about Oh. 30m. p. m. on the 21st May. On the following day the theodolite was again set up on the same place as before, and being properly adjusted, the cross-wires of the telescope were directed to the cross on the cliff on the opposite side of the glacier. A stick was then set up near the first of the five marks that had been made the 1 P. , l Pp. lxx., 372, 373, 586, 689. OF THE NORTH-WESTERN PROVINCES. 189 previous day, and was, by means of signals, moved up or down the glacier, till it appeared to coincide exactly with the cross-wires of the telescope, and consequently to be exactly on the line between the two crosses painted on the cliffs. The distance between the centre of the stick and that of the fixed mark was then measured, which evidently showed the downward progress of the ice at that point of the glacier, since the marks were made the day before. The same procedure was followed at each of the marks. The results were as follows : — Time of observation. Distances of fixed mar Its from standard line. On the west moraine. On tlie me- dial mo- raine. At east foot of me- dial mo- raine. Near the middle of the clear ice. On the eastern moraine. h. m. ft. in. ft. in. ft. in. ft. in. ft. in. 21st May 0 30 p. m. • • • ... ... • •• 22nd 1 15 p. m. 0 5J 1 01 1 0 1 Oj 0 6| 25tli „ 8 45 a. m. 1 9i 2 9| 2 Ilf 3 1 1 5 J The motion in 24 hours of the several marks will also be found to be — Mean motion (in inches ) of ice in 24 hours. Date. On the west moraine. On the medial mo- raine. * At east foot of medi- al moraine. Near the middle of the clear ice. o a o 05 P cS o rH o o o 0 O O O o o o o o o Leh 11.538 49-9 63-1 62-3 63-2 58-7 58-1 54-1 62-8 63-8 63-9 54-1 50-9 58-7 Cliakrata, 7,052 71*1 67-1 69-4 69-5 69-1 66-3 63-0 61-5 70-3 69-8 69-4 68-5 67-9 Ranikhet, 6,069 61-1 60-6 62-6 60-4 60-3 57-1 50'8 52-1 59-8 57-3 52-7 55‘7 57-5 Delira ... 2.232 51-0 52'2 57-6 57-1 56 '8 54-2 53-6 52-1 57-7 58-5 55'6 51-8 54-9 Roorkee... 887 568 l 52-2 51-5 55-9 54'6 53'7 51-2 51-9 51 '8 54-5 54 - 5 55-1 52-5 53-3 Bareilly . . 50-0 52-6 54-1 54‘4 55’3 | 54-2 50-7 50-1 49-3 52-0 52-4 48-9 52-0 208 HIM XL A VAN DISTRICTS If the air were absolutely diathermanous, tlie altitude of the sun above the horizon and the vertical thickness of the atmosphere above the place of observation should have no effect upon the temperature differences in the table, which should therefore ho the same for all the stations and for every month of the year. But the air having some absorbing power, the differences should be greatest when there is least air for the sun’s rays to pass through ; that is, at the highest stations and in the summer months. Up to Chakrata the excess temperature of the solar thermometer does increase with a fair degree of regularity ; but it appears to be less at Leh than at Chakrata, contrary to all theory. There is also no regular increase apparent in the heating power of the sun as the season changes from winter to summer. The truth is that the indications of the black- bulb thermometer are affected by so many disturbing causes, that after all possible corrections they are of little or no value for inter- comparison ; though with the same thermometer, at the same place, and under absolutely constant conditions of exposure, the figures for one year may be to some extent comparable with those for another. The results of observations with the nocturnal radiation thermo- meter are even more unsatisfactory, owing to differences in the height of the instrument above the ground and in the nature of the ground surface itself, whether grassy or bare. II. — Monthly mean dejpressicm of the grass thermometer below the minimum in shade. Stations. January. ' February. March. April. £ June. July. I August. i a CD +=> C CD m October. Novem- ber. Decem- ber. Year. O o O O o O O O o o O O O Chakrata, 9-5 6*5 7'2 7-5 6'3 6-0 3-1 4-3 5-S 8-8 9-8 11-0 7-2 Ranikliet. U-5 13-6 13-9 13-3 12-0 9-0 5 3 6-0 8'9 13*5 17-2 19-1 12-2 Dehra ... 4-4 4-4 4-2 4-7 4-8 3-6 2-2 1-5 2-3 3-5 4-8 4-6 3-8 Roorkee... 6-3 5-8 6-4 6-3 5-0 3-5 2-4 2*9 3-9 6-3 7-3 6-3 5-2 Bareilly... 7-0 7-5 8-0 10-0 10-5 8-8 4-3 3-3 3-4 6-4 8-2 8-0 7-1 The figures in table II. serve to show that the depression of the nocturnal radiation thermometer below the minimum in shade is less in the rainy season than in the dry, and that both at the hill stations and on the open plain the refrigeration of the earth’s surface during OF THE NORTH-WESTERN PROVINCES. 209 the night is probably greater than at Debra, where the observatory is situated in a well-wooded park. They do not throw any light on the question whether the ground surface cools more rapidly at night on mountain tops or on the plains ; though it is probable that in the clear, calm nights of the cold weather the difference, it any, is in favour of the plains ; since there the air cooled by contact with the ground remains in contact with it, whereas on the mountains the cooled air constantly drains away, and is replaced by warmer air from the surrounding free atmosphere. It has been already stated that, in the western Himalaya, every elevation has its characteristic mean annual Temperature. temperature. Each elevation has probably also a distinctive form of variation of temperature during the year, and the daily variation is different at different altitudes, in iangc if not in general form. For a proper discussion of the distribution of temperature in a hilly country a very large number of observations would in most cases be required ; and these should be made at places chosen so as to be at nearly equal distances from each other vertically, and at the same time fairly distributed in latitude and longitude. On the southern slope of the Himalaya it fortunately happens that differences of latitude and longitude make but/ little difference in the mean annual temperature. The sea-level values of the mean temperature at the Sub-Himalayan stations from Lower Asam to Ambala all lie between 76 and 78 degrees Fahrenheit, and the tempera- tures of places at about 7,000 feet elevation along the whole range from Darjiling to Marri in the north of the Panjab do not differ more than 2 or 3 degrees. Both along the plains and at the level of the hill sanitaria the highest mean temperatures are found to characterize the regions lying between the Kali and Satlaj rivers. Hie chief reason for the great uniformity of mean temperature at the same elevation that prevails over the whole Himalayan region— that is to say, through more than 7 degrees of latitude and 17 of longitude— is the greatly increased heat of summer in the north- west as compared to the east. In Bengal and Sikkim the sun s lays when most intense are to a great extent cut off b\ cloud, whereas 27 210 HIMALAYAN DISTRICTS in the Panjab and the north-west Himalaya the winter is almost if not quite as cloudy as the summer. For these reasons Darjiling lias very nearly the same temperature in January as Simla, Chakra ta, or Mussooree, while in May and June it is seven or eight degrees cooler. The comparatively low temperature of the summer at Darjiling renders the mean for the year nearly two degrees lower than that of Marri in the extreme north-west, though the effect of latitude is apparent in the low temperature of Marri in January. On account of this uniformity of temperature a small number of observations, at places chosen specially with reference to height above the sea, will enable us to ascertain the most important features of tem- perature distribution in the Himalayan districts of the North- W estern Provinces. The following table gives the mean monthly temper- atures of twenty-one places, including the two stations on the plains that were given in the previous tables. All the other places except Dharmsala lie in one or other of the three districts of Kumaon, Gfarhwal, and Dehra Dun, or in parts of Kunawar, Lahul, and Ladak to the north of Dehra Dun. The monthly means from a Government observatory at Dharmsala in the Panjab have been inserted, though this station lies nearly two degrees west of Dehra Dun, because it was considered desirable to have some trustworthy figures for places about 4,000 feet above the sea ; and the only other station near that altitude is Hawalbagh in Kumaon, for which we have but one year’s observations. III. — Mean monthly and annual temperatures of places in Kumaon, Garhwdl, Delira Dim, and adjacent districts. OF THE NORTH-WESTERN PROVINCES. 211 's jgsa jo aaquitiR H»HINNHIt5r-lNmCOCnO-#rH>nNHHl>.H 1 rH | | | | 1 | rl J (DNH CH hH C0 0005 CO O CO lO (MTHO^Nl>CpN’^

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Bareilly : Registers of the Government Meteorological Observatory, 1869 to 1879 Eoorkee : Ditto, ditto, 1863 „ 1879 Dharms vla : Ditto, ditto, 1871 „ 1S75 Ra'nikiiet : Ditto, ditto, 1871 „ 1879 Chakrata : Ditto, ditto, 1869 „ 1879 Leii : Ditto, ditto, 1871 „ 1877 Dehra : Registers of the Observatory at the G. T. Survey Office, 1868 „ 1879 Naini Tal : Registers of Government Observatory, 1863 to 1869 ; and observations by Dr. Payne in 1851-54, given at page 49(5 of the third volume of the Results of a Scientific Mission to India and High Asia, by the brothers Schlagintweit. Mussooree (1): Records of an observatory at Saint Fidelis’s School for 1877-80 ; somewhat fragmentary. (2) : November to April, Sir A. Waugh’s and Mr. Mackinnon’s obser- vations in 1855-5G, also one year’s observations from Dove’s tables ; May to October, observations at the Survey Office for 18(5(5-79, fur- nished by Mr. Hennessey, F.R.S. Land A ur : Registers kept at the Convalescent Hospital in 1852-54, and 1 8(5(5- (57. Observations for the three years 1877-79 have been communicated by the medical officer in charge, but the means deduced from them appear to be 4 or 5 degrees too high. K K lsi : Pigot — Calcutta Journal of Natural History, Vol. VI., 1837-38. Almora : Observations at the Regimental Hospital, 1S52-54 and 1866-69. Hawalbagii : Schlagintweit, page 494, on authority of Mr. Batten ; year unknown. Lohugha't : Clelland’s Geology of Kumaon, page 179 : parts of 1830, 1831, 1834, and 1835. Kardong : Schlagintweit, page 513 ; 1855-56. - Kan am : Cunningham’s Laddh, page 1S4 1827-28. Spiti Valley : Ditto, page 183 ; 2 1846. Srinagar : Pauri : Niti : Manuscript observations by General Strachey and his brothers 1847-49. The figures for the regular meteorological observatories (printed in small capitals in table III.) and those for the observatory at 'Recomputed from the maxima and minima and corrected by means of the obser- vations of Chakrata and Leh, Recomputed and corrected by the Leh observations. OF THE NORTH-WESTERN PROVINCES. 213 the Survey Office, Mussooree, are either directly calculated from observations at 4 a. m., 10 a. m., 4 p. m., and 10 p. m., or have been corrected to represent the means of observations taken at these hours. They probably differ very little from true daily means. The mean temperatures for the other places have been calculated in various ways, and many of them are open to consider- able doubt. The mean annual temperature diminishes pretty regularly as heio-ht increases. In the table there are only two exceptions to the rule that the higher a place is the cooler it is. It will be seen also on comparing places of nearly equal altitude and not very far apart that the highest temperatures belong to those which, lying behind the outer- most high ridge, are subject to a much smaller rainfall than stations situated on the ridge or in valleys opening out to the south and exposed to the full force of the rainy winds. Thus Ranikhet and Almora are too hot in comparison with Naini Tab The difference in temperature as well as in humidity between places situated at equal heights on the outer and inner ranges of Kumaon is suffi- ciently great to ho easily recognizable without the aid of instru- ments, and is well known to all who have ever resided in the hills. The variation of temperature between the hottest and coldest months and the daily range of the thermometer are also greater, as a rule, in the interior than on the outer hills, owing to the larger proportion of cloudy sky and greater humidity of the air in the latter region. Both the diurnal and the annual range of temperature decrease on ascending from the plains up to a height of 6,000 or 7,000 feet, and beyond that they again increase, their greatest values being attained at the highest stations where observations have been made. Those places, however, lie to the north of the Indian watershed, where the humidity is doubtless less than on the southern side, and the observed ranges of temperature are probably higher than they would be at equal altitudes on this side of the snowy range. Moreover, the annual range in Tibet and Ladak is greater than on the Indian side of the chain on account of the difference of latitude, as has already been pointed out. In table IV. the daily and yearly ranges of temperature at twelve places are compared, and from it these relations will be readily seen. 21 4 HIMALAYAN DISTRICTS 1 V- — Mean diurnal and annual ranges of temperature at places in the Himalaya. Place. Diurnal Range. Annual range of monthly means. Jauuary. F ebruary. 1 March. April. tA o{ S •June. July. j August. September. i October. i November. i I December. Year. O O O O o O O O O o O O O o Bareilly ... 26-3 25*5 28-0 310 28-3 22-1 14-2 14-2 15-0 24-3 30-4 28-0 23 9 33 0 lloorkee 26-5 24-6 28-3 31-4 28-9 22-2 14-5 14-6 17-2 27-8 32-9 29-3 24-8 34-1 Debra ... 23-4 23-1 24-0 26-3 24-9 18-6 12-8 12-5 15-0 23-4 25-9,24-3 21-2 30 1 Dharmsala 15-8 18-6 20-4 21-3 2P6 18-2 12-6 12-6 15-4 19-6 20-2 18-5 17-9 31-5 Mussooree, (1), 14-0 13-2 14-0 16-0, 19-3 15-4 9-4 8-0 10-3 13-6 1 , 16-3 12-3 13-2 25-2 Ranikhet 16-1 17-0 18-2 18'6 18-1 15-0 11-2 10-9 131 15"3 17-2 16-1 15-5 25-2 Mussooree, (2), Ml • • • ... ... 19-0 16-5 10-7 9-9 12-0 14-2 16-8 ■ • • ... 1 27-0 Chakrata 183 18*4 18-1 19'7j 19-4 16-3 12-5 11*3 12-0; 17-3 18-0 18*3 16-6 26-4 Landaur 15*3 18-7 18-2 19-7, 20-0 21-2 13 • 1 ( 9"5 12-2 16-5 17-0 18-2 16-6 28-8 Kanarn 15-2 17-2 22-0 19-0 18-5 17-3 16-3 15-5 88-9, 20-5 19-0 18-3 18*1 37-8 Leh 28-5 30-0 28*01 31-0,30-1 31-8 11-2 31-3 31-4 30-5 26*7) 25-2 29-6 42-9 Spiti ...| 193 27*7) 29*2 18-5, 22-0 29-0 32-1 31-3 28-4 28-0 18-0 32-2 i i 28-7 44-5 The table shows clearly that the minimum range for both day and year is reached at Ranikhet and the lower Mussooree station — that is, about 6,000 feet above the sea. The dependence of the diurnal range upon the humidity of the air and the proportion of cloud at each station is distinctly brought out in the variations from month to month. At all the stations but Leh and the Spiti valley, which lie beyond the snowy mountains, the months of the year which are driest in India — April and May — have the largest daily thermonie- tric range, and the most humid months — J uly and August — have the smallest. There is a secondary minimum of temperature range coinciding with a maximum of humidity in January, and a second- ary maximum in the dry and cloudless month of November. At Leh, where the most frequent precipitation of moisture during the year takes place in winter, the range is somewhat greater in the summer than in the winter months. Owing to the greater annual range of temperature on the plains than on the hills, the diminution of temperature in the first 6,000 feet of ascent is most rapid in the hottest months and least so in the cold season. Between lloorkee and Chakrata the difference is less than 11 degrees in December and more than 23 in May. In the clear still nights of the cold weather, especially in November and December, before the winter rains and snows set in, the nocturnal > s * % , OF THE NORTH-WESTERN PROVINCES. .■ - 21 5 loss of heat goes on almost as freely on the plains as on mountain peaks. It is thus not unusual to find the temperature of the exposed ^ thermometer at Roorkee nearly as low as at Chakrata, and it veiy frequently falls lower at Roorkee than at Dehra, where the obser- vatory is surrounded by trees. In December the mean temperatuie diminishes between Roorkee and Dehra at the rate of only one decree in 1,034 feet, while in May and June it falls one degree in 230 feet. The low temperature of the plains in the winter season, especially in the morning, is doubtless due in part to the draining down of cold air from the mountain slopes through the river gorges. This, however, cannot appreciably affect the temperatuie of places at a long distance from the mountains, though it may have a very considerable effect on that of Roorkee, close to the foot of the Siwaliks. The minimum temperature of the day is thus one or two degrees lower on the average at Roorkee than at Dehra in the months of November and December, and in January the minimum temperatures of the two places are equal. In the moun- tain country itself it often happens for the same leason that the temperature of the air at the bottom of a valley is distinctly lower than on the adjacent ridges. A similar inversion of the noimal variation of temperature with height has been noticed in Euiope during calm weather in winter. to From March to June the absorption of heat in melting and evaporating the snow on the outer hills, and in evapoiating the rain that falls there in frequent showers when no rain falls over the plains, keeps down the temperature so that in May and the fust half of June, when the plains are at their hottest, the decrease of tempei- ature on ascending through 6,000 or 7,000 feet is more than twice as great as in December. In the Panjab, where the latitude is higher and the humidity of the air over the plains is never great, the annual range of tempera- ture at places on the plains is higher than in the North- Western Provinces, while in the hills there is much less difference. The annual variation in the decrease of temperature with height is accordingly much more distinctly marked in the extreme west of the Himalava than it is in Dehra Dun. The difference of * 210 HIMALAYAN DISTRICTS temperature between Rawal Pindi and Marri is lb ‘5 degrees in J uly and only one-third as great in December. On the other hand, in the eastern Himalaya, where the air at all elevations up to 9,000 or 10,000 feet is nearly equally moist, and where the range of temperature, especially over the plain, is much less than in the north-west, the decrease of temperature with height is most rapid in Februai’y and March and least so in June and July. The slow rate of decrement in the rainy season is doubtless due to the libe- ration of latent heat in the condensation of vapour ; this heat ren- dering the atmospheric strata in which condensation occurs warmer than they otherwise would be, while the constant precipitation of rain prevents the lower strata from becoming very much hotter than the rain drops which pass through them. The effect of the rainy season in retarding the fall of temperature as we ascend is distinctly seen between Bareilly and Naini Till or Ranikhet, but is not seen between Roorkee and Chakrata. The great annual range of temperature at more elevated stations, especially such as lie behind the first snowy range and receive little or no precipitation, causes even greater differences in the rate of decrease of temperature with height, but in the opposite direction. In January, the difference of temperature between Chakrata and Leh is 24 degrees, but in August it is only 4 degrees. The greater length of the day in summer at Leh, and the absence of cloud to obstruct solar radiation on the surrounding mountain sides, render the summer months at that station, 11,500 feet above the sea, as hot as they would be on the southern side of the snowy mountains at an elevation of 8,500 or 9,000 feet. If General Cunningham’s figures for the temperature of the Spiti valley are to be trusted, the heat of summer at an elevation of 13,000 feet is still more excessive. The relation of this to the greater height of the snow-line on the northern than on the southern side of the Himalayan system is obvious. In the following table the mean rate of decrease of temperature in the first 6,000 or 7,000 feet of ascent has been worked out for each month. In Dehra Dun the lower station is Roorkee and the upper one Chakrata ; in Kumaon, Bareilly has been taken for the lower station, and instead of choosing either Naini Tal or Rani- khet for the upper one, the monthly mean temperatures of both OF THE NORTH-WESTERN PROVINCES. 217 places have been taken and assigned to the mean elevation of the two. This was considered preferable to taking the figures for either hill station alone, because Ranikhet appears to be a little 9 hotter than the average of places at the same elevation, and Naini Tal is probably somewhat cooler than the average. V. — Decrement of temperature with height in the Himalaya. Month. Delira Dun , differ- ence iff elevation , 6,165 feet. Kumaon , difference of elevation, 5,698 feet. Mean rate of decrease. Difference of tem- perature. Height for 1°. Difference of tem- perature. Height for 1°. Height for 1°. For 1,000 feet. O Ft. O Ft. Ft. O January 15' 1 408 12-9 442 425 2-85 February 17-4 354 15-7 363 358 2-79 March 20-1 307 17.1 333 320 3-13 April 22-9 270 20-6 278 274 3'65 May 23-3 265 22-2 257 261 3-83 June 22- 8 270 20-1 2S3 27 7 3-61 July 20'7 298 16-7 341 319 3-14 August 20-0 308 16-7 341 325 3-08 September 19-7 313 171 333 323 3'09 October 18-0 343 16-3 350 356 ’2-81 November 12-8 482 12-3 463 473 2-11 December 10-9 567 10-2 559 563 1-78 Year 18-6 331 16-5 345 338 2-96 In Deln-a Dun there is a regular annual periodic variation in the rate of decrease of temperature with height, but in Kumaon the regular variation is interrupted in July and August, when the rate of decrease is slightly retarded by the fall of rain, as has been explained above. When the mean for both districts is taken, the regular variation from month to month is only slightly broken in August. The figures given in the table include not only the decrease of temperature due to increase of elevation above the sea, but also a certain diminution caused by an increase of latitude equal to about a degree in 6,000 feet of elevation. The change of temperature with latitude in the Himalaya is small and to some extent masked by the contrast between the sunny valleys of the interior and the cool and cloudy outer ranges, but nevertheless it exists. On the plains of the North-West Panjab the temperature falls as the latitude increases at a mean rate of about Pl° F. for each degree of latitude, when corrections are made for differences of height above the sea. Probably much the same rate obtains in the western Himalaya at moderate elevations. The mean temperature of Yarkand, in latitude 28 218 HIM/LAYAN districts 89° N. and 4,200 feet above the sea, appears from the observations of Captain Trotter, R.E., of Drs. Bellew, Henderson and Scully, to be about 54°F. At the same elevation in Kumaon the mean tem- perature is between 65° and 66°, and since the difference of latitude is ten degrees, the temperature appears to diminish about 1*1° or T2° for a degree of latitude. There is also a certain variation of the mean temperature with the longitude, places situated towards the east of the chain being cooler than those towards the v r est on account of the cloudiness of the summer months. In order to deter- mine the true variation of temperature with height it is necessary to make allowance for these variations in latitude and longitude. The mean annual temperature of any place in the western Himalaya may thus be looked upon as a function of four quantities — (1) the sea-level temperature at a point taken as the zero of latitude and longitude, (2) a constant multiplied into the height of the place above the sea, (3) a constant multiplied into the latitude, and (4) a constant multiplied by the longitude. From the Schlagintweits’ ■work and the reports of the Indian Meteorological Department fairly trustworthy mean temperatures for about thirty places in the Himalaya between the Nepal frontier and the Indus can be obtained, more than half of these being given in Table III. When treated by the method of least squares the observations admit of being thrown into the form T=78*5°--00277A-1'20 (X- 29°) -*105 (L-73°), a formula which represents the observations with a mean error of about three-quarters of a degree. It ignores, of course, the differences of temperature between such places as Almora or Ranikhet and others of equal elevation on the outermost range. The decrement of temperature with height when latitude and longitude remain unchanged appears therefore to be 2"77 degrees in 1,000 feet or 1° in 361 feet. In the eastern Himalaya the decrease is more rapid, the observations taken at Darjiling and Gfwalpara giving a mean rate of 1° in 320 feet. At great elevations on the table-land, too, it is probable that the temperature diminishes more rapidly than on the southern slope of the mountains. General Cunningham’s observa- tions in Spiti and Rupshu during the month of September, 1847, give a mean increase of about 280 feet in elevation for one degree of fall in temperature; and from the observations taken by Dr. Scully on the return journey from Yarkand over the Karakoram OF THE NORTH-WESTERN PROVINCES. 219 pass and through Ladak in September, 1875, Mr. Blanford has deduced a mean fall of temperature equal to one degree in 227 feet. 1 The isotherms for equal altitudes in the western Himalaya and Ladak run from about W. 6° N. to E. 6° S., being thus three points less inclined to the parallels of latitude than the general direction of the mountain axis; but in eastern Tibet, Nepal, and Sikkim they probably bend to the southward. The mean temperatures of Kathmandu and Darjiling, at elevations of 4,354 and 6,912 teet above the sea, appear from the observations of ten years to be 61' 7 and 53' 9 degrees respectively, but according to the preceding formula they should be 66' 7° and 601°. The mean temperatures of the four stations, Darjiling, Kathmandu, Gwalpara, and Sibsagar, in the eastern Himalaya and Asam, may be represented very accurately by the formula T ^ 77*7° - -00312/*- D53 (X-26°)--23 (L-85°). In this part of the chain the temperature decreases at a mean rate of one degree in 321 feet of ascent, and the isotherms run from W. 10° N. to E. 10° S., the direction of the mountain axis being nearly due east and west. The isotherms are thus slightly curved, with the concavity towards the south-west, whilst the general line of the mountains is considerably curved in the opposite direction. This is merely another form of the statement in page 209, that the highest temperatures characterize theft part of the chain between the Nepal frontier and the Satlaj. Supposing the uniform rate of decrease worked out in Table Y . to hold good for the whole southern slope of the North-West Hima- laya, since the difference of latitude is nearly propotional to that of height, a mean temperature of 49°E., equal to that of London, would he attained at a height of 9,600 feet, and the annual range of temperature would probably ditier little from that observed in England.. The hill sanitaria, lying between 6,000 and 7,000 feet, possess climates comparable, as regards temperature, to those of Nice, Mentone, and other health resorts in the Riviera ; all the towns along the cost of France and Italy from Marseilles to Florence having mean temperatures between 58° and 60°F. The annual range of the monthly means at the Himalayan stations does not exceed 25 or 26 degrees, whereas on the Mediterranean coast it varies from 28 or 29 degrees at Nice to 35 or 36 at Florence and Rome. 1 Indian Meteorological Memoirs. Vo!. L, page 222. 220 HIMA'LAYAN DISTRICTS Nice and Ranikhet have exactly the same mean temperature, but Nice is seven or eight degrees hotter than Ranikhet in July and August, and several degrees colder all through the winter and spring months, except in January, when the temperatures of the two places are nearly equal. At the superior limit of natural forest in the Himalaya, about 12,000 feet above the sea, the mean temperature is probably ten degrees above freezing. In the Alps a species of pine, F. cernbra, forms natural forests on the borders of perpetual snow, where the mean temperature is several degrees under the freezing point. This differ ence of habit between the Himalayan and Alpine pines is very curious, and it is difficult to suggest any reason for it, since the natives of the Himalaya and Tibet find little difficulty in growing poplars and fruit trees in sheltered situations up to 13,000 feet or higher. 1 A mean temperature of 32° would be attained at a height of 15,400 feet, which is 2,000 feet above the upper limit of cultivated trees in Tibet. The zone which has a mean temperature of 32° in any month will piobably be near the lower edge of the snows in that month, especially in summer, when the light falls of snow on the outer hills have been all melted away. If the height of this zone be calculated for every month, the highest value obtained will be near the perpe- tual snow-line. With the uniform rate of decrease given in the last column of Table V., the result for July and August, when the snow line is highest, is about 17,630 feet. This result is very much higher than that given in Humboldt’s Asie Centrale, on the authority of some of the earliest European travellers who penetrated into the country. General Strachey has, however, shown 2 that some of these mistook the lower limit of glaciers for the line of perpetual snow. The elevations of the snow line on the Tils til and Nanda Devi groups of peaks, determined by trigonometrical observation from Almora in the latter part of 1848, before the winter snows set in, varied, according to Strachey, from about 17,000 feet on the eastern face of each group to 15,500 on the west ; this latter was, however, in part probably newly fallen autumnal snow. The conclusion from these observations was that the height of the snow-line on the “ more pro- minent points of the southern edge of the belt (of snowy mountains) may fairly be reckoned at 16,000 feet at the very least.” The Sclilagint- 1 Schlagintweit’s Meteorology of India, page 565. 2 Journal of the Asia- tic bociety of Bengal , April, 1849. OF THE NORTH-WESTERN PROVINCES. 221 weits found tliat the average height of the snow-line on the southern face of the Himalaya from Bhutan to Kashmir was 1 0,200 feet. At page 72 of General Cunningham’s hook on Ladak the mean height of the sndw-line on the peaks north of Simla, determined trigonometric- ally, is given at 16,665 feet, the highest point observed being about 1 000 feet higher ; and in Mr. Drew’s volume on the Kashmir terri- tories, published in 1875, the elevation of the snow-line on the outer- most zone is stated to be 16,500 feet. The height obtained by calcula- tion as above suggested is thus probably a little too great, though it comes surprisingly close to some of Strachey’s observations on Nan da Devi and those of Cunningham on the peaks of Kulu. Some obser- vations have recently been made by the Trigonometrical Survey officers at Mussooree to determine the height of the snow-line on the peaks above Jamnotri, but the results have not yet been published. For the ranges north of the Indian watershed we have not suffi- cient data to calculate the approximate height of the snow-lme from temperature observations ; but the high temperature of Leh and the Spiti valley in July and August show most distinctly that it must be much higher than on the southern side. The limit of perpetual snow on the ridges bordering on Tibet, especially those which lie beyond the Satlaj, is given by Stracliey as 19,000 feet at least. Dr. Gerard many years ago, and more recently Mr. Drew, assigned an elevation of 20,000 feet to the limit of the snow in Kiipsliu. One reason why this limit is so high — the intensity of solar radiation in summer } ia s already been mentioned ; another is the insignificant quantity of snow that falls each winter in these regions that are almost com- pletely cut off from the great southern vapour currents. The lower limit of the snow in winter is usually about 6,500 feet in Kumaon and somewhat lower in Dehra Dun and the hills north of the Panjab. While it lies the temperature does not rise much above 32°, but it seldom falls in sufficient quantity to lie more than a few days at a time. About one year in ten the snow comes down as low as 5,000 feet. The lowest level attained in the first half of the present cen- tury was about 3,000 feet in 1817 and 1817. In 1877 and 1878, thou oli the snowfall was heavier than it had been for many years, it did not come down much below 5,000 feet. A slight fall of snow is said to have been observed at Lahore on the 12 th of January, 1874, 1 1 Pioneer , 17tli January, 187-1. 222 HIMALAYAN DISTRICTS but no notice of this unprecedented occurrence was taken in the meteorological report for that month. One of the most important effects of solar heat upon the - atmos- Atmospheric pressure phere is the disturbance of its statical pressure and winds. relations, which in turn gives rise to those movements of adjustment towards equilibrium that are recognised as winds. The diurnal heating and cooling of the air causes certain oscillatory variations of pressure called the barometric tides, and gives rise to wind movements, such as the land and sea breezes and certain mountain winds that will be described below. The great annual change of temperature between summer and winter, in like manner, causes an annual variation in the height of the barometer and sets up those great currents of the lower atmosphere that are called the monsoons. Since the temperature is constantly changing no such thing as a simple statical distribution of pressure ever exists, though the averages of long series of observations may approximate more or less nearly to what a statical distribution would be. The air is constantly in motion either horizontally or vertically, and these movements cause variations of pressure, just as variations of pressure produce movements. Cause and effect, as regards pressure variations and winds, are thus so inextricably mixed up that it is next to impossible to disentangle them and show their relations clearly. There can be little doubt that both the daily and the yearly inequality of pressure grow less as we ascend ; and the annual vari- ation at least becomes quite altered in character at a moderate ele- vation ; but since the barometric variations depend upon the range of temperature which is possibly very great at great altitudes, while at a height of 6,000 or 7,000 feet it is less than on the plains, the decrease of the pressure variations with height is not strictly propor- tional to that of the total pressure. Table VI. gives the mean monthly pressures at a number of stations, and Table VII. the average daily ranee between 0-30 or 10 a.m. and 3-30 or 4 p.m. The figures for Bareilly, lloorkee, Delira, Mussooree (both stations), Ranikhet, Chak- rata, and Leh, have been corrected for the index errors of the baro- meters and are thus comparable with each other, except in so far as the different lengths of the periods of observation may cause the averages to differ ; the others involve an unknown barometer error, which does not, however, affect the range of pressure, either diurnal or annual. VI. — Monthly and annual means of Pressure at places in the Himalaya . OF THE NORTH-WESTERN PROVINCES. 223 Num- ber of years. — 2 CO t- H lO O 1 2 2 1 1 *° 1 1 1 r-H r—( JO r — 1 ^ 1 MUOX 1/ 29*187 28-888 27-567 25-446 24*603 24-238 24-046 23-807 23*222 19-659 .loqiuooOQ // 29-439 29-132 27-763 25-620 24-731 24-323 24-134 23-894 23-423 23-287 19-701 MoquiOAOjq 11 29-393 29 090 27-740 25-624 24-771 24-321 24-157 23-905 23-492 23-303 19-742 t uoqopo 11 29-263 28-959 27-638 25"545 24-710 24-290 24-106 23-879 23-439 23-293 19-722 Moqiucqdog 11 29-097 28-796 27-495 25-465 24*578 24-217 24-023 23-758 23-358 23-223 19-692 •;snSny 11 29-002 28-694 27-403 25-323 24-462 24-143 23-959 23-716. 23-294 23-158 19-640 'A n r r— IO005£s-^-HO£0<35C0e0 5CO(N-*05COOi‘o4n4to3 coca 5r+llOiOcqcO»OCLOCO • CO ^ r-H CO JO >0 03 O CO * 03 CO CO b* i'c -rfl rH rfi CO cb CO 0303030303030303 03’—' •qo.iuj\[ COt-- CO . 03 t— COOcp^fHCOOlOCO *oi»o m Ci b- IQ ^ -ti OO CO 02 030303 01 03030303 03 r-H ■iCrunuuf' n 29-417 29*123 27-734 25-478 24*704 24-287 24*096 23*865 23*259 19-604 ni aoi^UAO[g[ 568 887 2,232 4,495 5,546 5,855 6,069 6,463 6,881 7,052 11,503 Place. Bareilly Roorkee Deliar Dharmsala Almora 1 Mussooree (1), Ranikliet Naini Tal Mussooree (2), Chakra ta Leh From one year’s observations by General Strachey. VII. — Mean diurnal and annual ranges of pressure at places in the Himalaya. 224 HIMALAYAN DISTRICTS »o tr- 05 05 rH 04 o CO •siiuaut r-H r-H r-H i — 1 CO r-H 05 Ol co IQ 1C CO 04 04 04 1 — 1 r-H i-H oSirat prauuy CO co o rH 05 >o 05 CO *.re02L * o 05 co 05 JO »C IQ • r— 1 p o o o cp o o o co »o 05 o CO o CO 05 o 04 •JoqtitoooQ o i— i 05 o co o o r-H t- o CD o >o o o >o o CO o PM o ■< o Pi & ■«! PM M 3 M P MoqraoAOjsj // •108 •091 •093 •090 •042 •065 •057 •046 •053 • 0 S 9 Moqopo // •105 •094 •092 •100 •047 •062 •060 •054 •056 •079 uaqragylag // •107 •099 •092 •090 •060 •058 •058 •053 •051 •096 •cjsnSny // •097 •088 •076 •oso •057 "055 •049 •044 •047 •083 ’ A n r // •096 •083 •070 •080 •045 •052 •042 •040 •051 •070 •amif // •112 •106 •086 •090 •063 •052 •045 •037 •039 •071 'Xbm < 32 t-oo ft I m to 2 a *8 vc3 pH ’8 ft CO CO :=$ 3 r^ c3 r^ O Leh OF THE NORTH-WESTERN PROVINCES. 225 Tlie double barometric tide that occurs regularly every day, espe- cially in tropical countries, is still one of tlie least understood of atmospheric phenomena. It has been observed at all elevations in the Himalaya to which barometers have been carried, and with no con- siderable difference of phase, 1 though the range and general form of the oscillation are not the same at different heights. It is thus probably something of the nature of a wave of expansion and con- traction propagated upwards and downwards with a velocity equal to that of sound. The amplitude of the daily tide bears an obvious relation to the diurnal range of temperature, for it is greater over land areas than over the sea, and in table VII. it is seen to decrease pretty regularly from the plains up to stations situated at an elevation of 6,000 or 7,000 feet, where the range of temperature is least, becoming greater again at Leli, where the temperature range is large. Moreover, on the plains there is a well-marked annual variation of the daily range of the barometer, having its maximum in the hot-weather months, when the temperature range is greatest, and its minimum in the rainy season. But the inequality of temperature is not the only cause on which the observed barometric tides depend ; for their am- plitude, as well as their general form, varies with the season, the latitude and the position of the place with respect to the sea and to mountain ranges. 1 Professor Loomis, in the American Journal of Science for 1879, finds that at the top of Mount Washington the daily maxima and minima set in three hours later than at the foot, though the difference of elevation between the two stations is only a little over 3,000 feet. This is quite unlike anything that occurs in the Himalaya, and is doubtless due to other causes than those which produce the diurnal tides. Hourly observations made in India show that up to a certain moderate elevation the daily barometric maxima and minima are slightly retarded ; but this is due to the mountain winds described below. At Leh, in the upper Indus valley, the diurnal winds cause the morning maximum to occur nearly an hour earlier than on the plains. This will be seen from the following table : — Place. Height. Morning maximum. Afternoon minimum. Feet. H. M. H. M. Calcutta 18 9 35 16 26 Allahabad . . . 307 9 34 16 30 Hazhribagh . . • 2,010 9 47 16 24 Simla • . • .7,071 10 2(5 16 51 Leh ... 1 1 ,503 8 48 16 29 29 226 HIMALAYAN DISTRICTS The observed diurnal movements of the barometric column are in fact made up of several parts, only one of which is directly caused by the alternate heating and cooling which the air undergoes every day, though the others are all indirect effects of it. The direct effect of heating and cooling upon the pressure of the air has been more or less clearly explained by Espy, Davies, and Kreil,but it has not yet been shown by strict mathematical reasoning that their explana- tion accounts for the whole of the phenomenon. There is firstly, with a rise of temperature in the morning, an increase in the elastic force of the air, indicated by a rise of the barometer. I>ut the in- creased elastic force immediately sets up a movement of expansion, either vertically or it may be in some cases laterally, by which the pressure is diminished. The actual movement of the mercury in the barometer is determined by the difference of these two actions ; and consists of a rise at first, up to 9 or 10 a.m., on the average, followed by a fall which goes on until some time after the hottest period of the day. It is easily seen that as long as the temperature continues to rise more and more rapidly, that is up to 9 A.M. oi a little aftei, the first effect must outweigh the second, and the barometer will rise ; but as soon as the rate of increase of temperature begins to grow less, expansion will prevail and the barometer will fall. The expansion will not cease at the instant when the tempeiatuie leaches its maximum, but owing to the accumulation of motion it will go on for some time longer. Thus, there ought to be a barometric maxi- mum about the time of most rapidly increasing temperature and a minimum in the afternoon. In much the same way it can be shown that there should be a maximum in the evening, when the tempera- ture is falling most rapidly, and a minimum about the coldest time of the morning. The coincidence between the barometric minima and the extremes of temperature is usually very far from exact, the barometer in this country standing lowest in the mornings about two hours before the time of minimum temperature, and in the afternoon about an hour and a half or two hours after the hottest time of the day. This may perhaps be explained on the principle of forced oscillations, that in the successive transformations which the energy undergoes, the oscil- lations approximate more and more nearly to simple harmonic waves with the maxima and minima separated by equal intervals. The OF THE NORTH-WESTERN PROVINCES. 227 diurnal curve of temperature approaches more nearly to a simple wave form than that of the solar radiation which falls upon the earth at any place, and the double daily oscillation of pressure can he almost exactly represented by two waves superimposed. At most places in India and the Himalaya the minimum tem- perature of the day occurs about sunrise, that is at 6 a.m. on the average of the year, and the maximum is attained about 2 p.m. The daily rise' of temperature therefore occupies only eight hours of the twenty-four, and the fall the remaining sixteen. On the princi- ple that the height of the barometer varies with the rate of change of temperature, the morning maximum should be much more decided than that of the evening ; and this is found by observation to be the fact, especially in the interior of India and other continental countries. Over the sea in tropical regions the periods of increasing and decreasing temperature are probably more nearly equal, and there the difference between the day and night waves of pressure is less. At places near the equator the epochs of maximum and minimum pressure hardly vary from month to month ; but in higher latitudes the morning maximum and afternoon minimum approach each othei when the days are short, and become more widely separated in the long days of summer. * * ? Besides this primary oscillation of pressure caused by the heat- ing and cooling of the air every day, the barometer indicates other changes due to the transfer of air by winds blowing to and from the place of observation, and perhaps also in some places it indicates other changes again due to the repetition of previous oscillations in the form of free waves. The great regularity and considerable range of the barometric tides over tropical seas where the daily range ot temperature is small, may be thus to some extent caused by the repeti- tion of the waves of previous days. In high latitudes, where the days and nights are usually of very unequal length and the variation of temperature is irregular, the tides become feebler, and near the pole disappear altogether, for in forced vibrations of any kind regular periodicity in the cause is an essential condition. Near the coast the land and sea breezes modify the form of the diurnal pressure curves both at sea and on land. The transfer of air from sea to land during the earlier hours of the night renders the 228 HIMALAYAN districts nocturnal fall of pressure on land less,' and at sea greater, than It would otherwise be, while the land breeze which blows in the fore- noons has a similar effect in the opposite direction. Over the water the morning minimum thus comes to be the lower of the two, in opposition to the usual rule. 1 Among the mountains a very similar semi-diurnal transference of air takes place, causing two distinct types of barometric tides — the one characteristic of valleys and the plains near the mountain system, and the other of high ridges and detached peaks. These types can be readily distinguished in the following table, which gives the variations from the daily mean at the hours nearest the turning points of the tides : — 4 A. M. 10 A. M. 4 P. M. 10 P. M. tr n n n Bareilly ... — -021 + •060 —•047 + •008 Roorkee ... — -020 + •057 —•036 —•001 Ranikhet ... — ■ '025 + •041 —•018 + •013 Naini Tal ... — ■ '028 + •043 —•012 —•003 Chakrata ... —022 + •035 —•015 —•001 Simla 2 ... — ■ '047 + -063 —•032 + •022 Leh ... +‘011 + •037 —•049 + •001 At Bareilly and Roorkee, on the plains, the variation from mean at 4 p. m. is twice as great as at 4 A. M. At all the Himalayan stations except Leh, which is in a valley between two ridges, this relation is reversed. Over the plains and on the outer hills, as at Naini Tal and Chakrata, the pressure at 10 P. M. hardly differs from the mean of the day. There is a small positive variation for this hour at Bareilly, and as we recede from the mountains and approach the sea the variation becomes greater ; but there can be little error in concluding from the above table that along- the southern border of the Himalaya the pressure rises in the evening just sufficiently to touch the mean. At Simla and Hanikhet, some twenty or thirty miles in towards the centre of the mountain system, there is, how- ever, a well-marked evening maximum. This seems to indicate that the air continues to accumulate over the interior of the moun- tain zone for some time after the current has changed on the outer ranges and the air has commenced to flow back towards the plains. 1 Blanford, J. A. S. B., Vol. XLVI., Part TT., page 45. 2 From General Boileau’s observations in 1843-45. The daily range given by these figures is nearly twice as great as that of the other stations at the same altitude. The reason is probably some difference in the form of the barometer or in the mode of applying the correction for capillarity. OF THE NORTH-WESTERN PROVINCES. 229 The transfer of air from the plains to the mountains in the daytime and its retransfer to the plains at night, which, by partly counterbalancing the afternoon fall of the barometer in the moun- tains and correspondingly increasing it on the plains, cause the peculiarities of the pressure variations seen in the preceding table, are brought about by the expansion and contraction of the air under the influence of heat and cold. In the daytime the air over the plains expands more than that over the hills, because the total thick- ness of air is greater and the range of temperature is probably higher. The surfaces of equal pressure, which we may assume to be horizontal on the average, are thus raised more above the plains than on the mountains, and the air under the influence of gravity flows down the incline towards the mountains. At night the air con- tracts and these surfaces sink more above the open plains than in the hills, and there is thus a slope or gradient in the opposite direction. The following is General Strachey’s description ot the diurnal variation of the wind in Kuinaon : “ At most seasons of the year we find that on the Himalayan slope winds blow up the valleys during the day, that is from about 9 a. M. to 9 P. M., and down them during the corresponding hours' of the night, or from 9 p. m. to 9 a. m. At the debouches of the principal streams into the plains, these night winds blow downwards with great violence, particularly in winter. In the interior of the mountains they are more moderate ; and at great elevations, and in the central parts of Tibet, the nights are almost always nearly calm. The diurnal currents from the south, on the other hand, inciease in force as we ascend in height ; and along the Indian watershed and the neighbouring parts of Tibet they are excessively strong ; so that in travelling there, I have often looked forward to the after- noon, when they are at their height, with real dread ; and the natives of the country invariably endeavour to cross the high passes of the Indian watershed early in the day, for the purpose of avoiding the fury of the afternoon wind. As we advance further into the table- land, however, their power rapidly ceases. “ These winds, though on the whole blowing from the south-west during the day and from the north-east at night, that is peipendi- cular to the general line ot the mountains, are naturally constrained 230 HIMALAYAN DISTRICTS to follow the course of the deep valleys up which they pass, so that their direction is subject to endless local variation ; and, excepting on the tops of the hills, little information can be obtained by a register of the direction of the wind on the Himalaya, beyond the fact of there being an up or down current. In the part of Tibet I visited, near the Indian watershed to the north of Kumaon, the day wind seemed to commence in the south-east quarter about 9 A.M., and gradually to shift round with the sun as the day advanced, ending in the south-west quarter about 9 P. M. On several occa- sions in these localities I also noticed the wind blowing faintly from the north early in the morning. ********** u The calm nights of the table-land and the higher mountains would (according to the theory above stated) be a consequence of their position in the centre of the mountain area, where the down current would originate, and therefore have the least force, though it be still felt in the faint northerly winds that are often observed near the Indian watershed. “ The violent night winds from the gorges by which the principal rivers leave the mountains would not appear to be altogether due to the same cause which produces the ordinary down winds, but to the accumulation of cold air in the deeper valleys to which I have before alluded. The air collected in these aerial lakes, as they may be called, having no means of escape but the openings through which the drainage is carried off, pours from them iii a current the velo- city of which will be dependent on the depth and area of the mountain basin from which it flows.” General Cunningham also states that in Ladak and Spiti the southerly or south-westerly day wind usually begins about 9 A. m., the wind blowing faintly from the north about midnight and from the north-east in the early morning. The day and night winds are probably strongest about 4 P. M. and 4 A. M., and the pressure and temperature observations made at these hours on the plains and at the hill stations indicate clearly enough that the direction of the baric gradient is from the plains towards the mountains in the afternoons, and from the mountains towards the plains in the mornings. When the pressures of Roorkee and Bareilly at 4 A. M. are reduced to the level of Chakrata and OF THE NORTH-WESTERN PROVINCES. 231 Ranikliet respectively, and are corrected for any residual gradient to or from the mountains discovered by similarly reducing the mean pressures to the level of the hill stations, it is found that there is a pressure difference of *07 7" at Chakrata and -055" at Ranikliet, sending a wind towards the plains. At 4 P. M. the gradient is towards the hills, and is equal to •062 // at an elevation of 7,000 feet between Koorkee and Chakrata ; while between Bareilly and Rani- khet it is equal to ‘045" on the average of the year. On the southern border of the mountain zone the gradient causing the down wind at night is therefore rather greater than that which causes the up wind during the day. When the pressures of Roorkee at 4 A. m. and 4 p. M. are reduced to the level of Leh, a station beyond the Indian watershed, the gradients are found to be -033" in the morning and *182 // in the nfternoon. The pressure difference causing the day wind at great elevations thus appears to be nearly six times as great as that which causes the night wind ; but this relation is much exaggerated, no doubt, by the peculiar form of the pressure variation at Leh, which cannot be taken as a typical mountain station. This peculiar vari- ation is doubtless due to the position of Leh in a narrow valley between two parallel mountain ranges. In the daytime the air of the valley expands and flows towards the mountains, and at night it again accumulates over the valley. In this way the nocturnal barometric tide is completely obliterated, and the afternoon fall of the barometer is rendered much greater than it would be on an open plain at the same altitude. In April, May, and June the afternoon winds of the mountains blow with greatest violence, because in these months the range of temperature both on the plains and among the mountains is great- est. In these three months we find the afternoon fall of the barometer on the plains at a maximum, while at the hill stations it is less than in the cold weather. The nocturnal inequality of press- ure is then at a minimum on the plains and valleys and at a maxi- mum on the hills. The annual variation of pressure differs from the diurnal in that no part, or an exceedingly minute part, of it is due to diiect inciease or decrease of elastic force accompanying gain or loss of heat. The 223 HIMALAYAN DISTRICTS rise of temperature in the first half of the year and the fall in the latter half are accomplished so slowly that the increase or decrease of elastic force cannot accumulate, hut is lost in expansion or con- traction. The annual variation is thus almost entirely a secondary effect due to the movement of air both vertically and horizontally. When the temperature of the air over India changes the air expands or contracts, and the hypothetical surfaces of equal pressure widen out or come closer together than they were before ; and since the annual variation of temperature over the south of India is very small in comparison with that which occurs over the northern plain and in Central Asia, the vertical range through which these surfaces travel in the course of a year will be greater on the Himalaya than under the equator. In the cold weather, for example, the planes of 30, 29, 28, &c. inches are wider apart vertically over Ceylon than in Northern India, while at the end of the hot and in the rainy season the opposite relation obtains. If there were no lateral movements of the air the pressure at a station on the plains would be nearly constant all the year round, while at the hill stations it would be least in winter and o-reatest in summer, because in the latter season a larger fraction of the total atmosphere than usual would be elevated above the place, while in the winter less than usual would lie above it. In winter, however, the planes of equal pressure in the upper regions of the atmosphere over India all slope towards the north, and down this slope winds blow, causing an accumulation of air over Northern India which renders the total pressure observed on the plains at that season greater than in summer. As regards mountain stations, it depends entirely on the height of the place whether the influx of air from the south will be more or less than sufficient to compensate for the contraction and sinking of the atmosphere in winter. At all the hill stations in Table YI. above 5,000 feet elevation there are indications of a winter minimum of pressure, though this is not the lowest minimum except at Leh, the most elevated station of all. There the pressure is least in the beginning of February, whereas at all the other stations, as on the plains, it is least in June and July. During the cold weather winds are usually blowing out from Northern India towards the south along the surface of the ground at the same time that other currents are blowing northward in the OF THE NORTH-WESTERN PROVINCES. 233 upper strata ; the apparent direction being modified in either case by the rotation of the earth on its axis and by friction against the ground surface. On the plain of the Ganges the conformation of the surface makes the lower winds have a north-westerly direction. As the temperature rises the air over India expands and a larger and larger proportion of the total atmosphere is lifted above the level of the hill stations. In consequence of this the barometer at first rises at the higher hill stations ; and it simultaneously sinks over the plains and the lower hills owing to the outward movement of the air. As the season advances more and more air is removed from India by the strong day winds which blow in the hot weather as well as by the winds over the Indian watershed that have been already described, while but little is restored by the feeble night winds that come from the opposite quarters ; the barometer continues to fall over the plains, and the rise observed at the hill stations in spring is soon also chang- ed to a fall, except at Leh, where the barometer continues rising until May. In the upper half of the atmosphere, that is, above the plane of 15 inches pressure, the summer depression of the barome- ter, which at Leh is feebler than that of winter, probably disappears altogether, and the barometer stands highest in the hottest season as it would do at all elevations if there was no transfer of air from place to place by lateral currents or winds. When the temperature of Northern India is at its maximum in the latter half of June, the planes of equal pressure are widest apart, and they all slope towards the north in the lower half of the atmos- phere. Winds consequently blow in from the sea towards the land in the lower strata, and there are possibly upper currents in the op- posite direction, though the existence of such has not yet been estab- lished. This relation continues until the autumnal equinox, after which the temperature falls rapidly, and the atmosphere contracts and sinks so as to reproduce the conditions characteristic of the cold weather. The cooling of the air at this season, like the heating of it in spring, produces a differential effect on the height of the barome- ter at the hill stations, which again have a maximum of pressure in November. When the effects of the two actions above described— the expan- sion and contraction of the atmosphere vertically, and the lateral 30 234 HIMALAYAN DISTRICTS transference of air by winds — are borne in mind, some curious and at first sight inexplicable peculiarities of the annual variation of press- ure become intelligible. For example, on the plains the barometer almost invariably stands higher in December than in January, though January is the colder month of the two. This anomaly at once disappears when we remember that the total pressure of the air on the plains, considered statically, is made up of two parts — that of the air from the plains up to the hill stations, and that of the air lying above the hill stations. The latter part appears from the observations of Leh to be greatest in the first fortnights of May and November, and least in the corresponding parts of February and August ; and if the monthly means for any station on the plains or lower hills be subjected to harmonic analysis, the annual variation will be found to be very closely represented by two harmonic waves — one of annual period, reaching its maximum at the time of greatest cold in the beginning of January, and the other of six months’ duration nearly coinciding in phase with the pressure variation at Leh. The amplitude of the first of these undulations, which is as much as six tenths of an inch at some places on the plains, rapidly diminishes as we ascend, and passing through a zero value at about 10,000 feet elevation, re-appears at Leh in nearly the opposite phase, the minimum falling in Avinter. The amplitude of the half-yearly oscillation increases slightly as we ascend, but it appears to vary Avith distance from the plains in a horizontal direc- tion rather than with height. The observed pressure on the plains, being due to the superposition of the tAvo waves, is highest in December — that is, betAveen the dates Avlien each wave separately attains its maximum. The truth of this theory of the annual change of pressure may b© more clearly seen from Table VIII., Avhere the monthly variations of the barometric weights of three successive strata of the lower atmos- phere from their annual mean values are compared Avith the simul- taneous variations of temperature. The last double column gives the variations for the Avhole thickness of the atmosphere from the plains up to 11,500 feet above sea-level. OF THE NORTH-WESTERN PROVINCES. 235 53 S3 H-O SO O S3 -*o S3 £*. *40 OD SO CO O % Cs *40 C5 t> & § *40 £3 S 53 £ 53 CO Co CW §» S^H £ O ■ c-> -K3 53 * eS> 5s 53 ?> -^-O 53 3 £ £ s CO . £> ^ •40 3 S5 ZD S£ r~* r-*C ZD k O C> H 05 r< S * ^ -40 <£> ^ ■i3 .Sj 'S 53 Svj r— I 'a id ^ *5*4 a - -+T * ^ *§ 5 - pi£ *40 S3 JS pH r-t ^ A ts O Fh _^_3 Eh O c 3 ^ ?h 2 g CD P* EH CD P p-2 g p CD *rj fig CD Fh • d Pi *£ O 03 • r— ( Fh 4-3 CD C3 P/£ a g CD r Eh CD R H O £j -rH co -g CO 03 CD -T* H Pi Ph g CD 1 § Fh 4-3 CD c3 P4*rj a 3 O l> H d CM C5 ip r-H CO Cp t> cp do 4h b- CM b- do P do r-H i— i i — i r-H rH 1 t 1 + 4- 4- 4 + t- 00 »0 1C O 05 CM O b- o 4 + I 1 CO 1*0 zp (M co ib b- ZD O ZD *-H O + r— I o + co r— I O 1 o *rH o I > Fh C3 d d o3 bo c 3 d Fh rO CD rd > 4^> CO & a CD 4-» Ph Fh CD ■§ 4-3 c3 P4 ci . ^ d CD o <1 a bo I - :- < m o lO t- O 5z< a CD O CD P i** 1 From the average of the three stations — Roorkee, Chakrata, and Leh. 236 himXlayan districts The barometric weight of each stratum and of the whole thick" ness — that is, the difference between the observed pressures at the top and bottom — varies inversely with the temperature, and the one variation is as nearly as possible proportional to the other. The only exception worth noting is that in the month of November the stati- cal pressure of the stratum between Chakrata and Leh is less than it should bo according to the temperature figures. This anomaly, however, would probably disappear from the means of a longer series of observations. The annual variation of the wind in Northern India is for the most part such as should accompany the pressure variations above described, according to the usually received u convection current’ 7 theory ; but there is one important feature of the winds of the plain that has not yet been satisfactorily explained — namely, the prevalence during the hot weather of strong north-westerly winds when the distribution of temperature and pressure should, by the theoiy of convection currents, give rise to winds with a southerly element. These “ winds of elastic expansion,” as they have been called by Mr. Blanford, actually blow sometimes from places where the mean press- ure is low to others where it is slightly higher. They are the strongest winds of the year on the Indian plain ; they blow only in the daytime, and since there is no compensating current of any appreciable strength at night, they are probably the chief agency in that removal of air from Upper India which causes the great summer depression of the barometer. They are not confined to India, but are equally characteristic of Afghanistan ; and Colonel Prejevalsky encountered winds perfectly similar in everything except temperature in various parts of the Gobi desert and on the Alashan plateau north-east of Tibet. On the southern slope of the Himalaya these winds are sometimes met up to elevations of 6,000 or 7,000 feet, and when they blow the air is unusually dry and full of dust. At greater elevations, however, they are either not felt or become undistinguishable from the ordinary up currents that blow during the day. OF THE NORTH-WESTERN PROVINCES 237 *3 5 >. <3 I'"— > So C5 so ■Is '-e "55 s so £ so p**-o CO c*» £ J •jCi’BtuqQ^ m Lv^nw8£ CD o cS s •siua^ jo loqTimjq 9-12 10-13 9-10 4-5 7-10 7 6-10 4 M9qUI909Q[ ^ ^ pq & ^ O o O O o q o o iO-rHCacftO,—(OOt'- o t- cq io to -cH >— i i— i Jz; Jz; !z ; cq cq cd qq oq uoquioAO^ ^ H ^ ^ p 4 ^ pi O O O O O O O '+COCO CQ rH t cq cq iq co tH 04 [2J (25 32 CD OD OQ CQ •jsnStiy H H gi £=’ H & OOOOonon -H «g p 4 C<) lO lO eqeo-»q<>;t-.^ H1 o 10 CQ CQ CQ CQ qq CQ CQ CQ •Xpf H M p 4 pi pi oo9ooooo CO O *>“ »“ < l>- r-H lr-Ht>. cq r+f cq t>- -rH io io CQ CQ CQ CQ* CQ* CQ CQ CQ •9 unp H H pi pi pi p 4 pi <3 000000 0 »0 CO CO CO lO O -rH 04 cq ^ cq cq ^ t- iq [2^ CQ CQ* CQ CQ CQ CQ* •^w pi pi > £ pi M pi pi 0 0 00 0000 Mi-HcOC5COC5»00 00 -i>-cqcoio 3L OC-CQCQa) Jzi m m m lO £ o I — I iq t? & O t>- CO cq CO i>- OQ l>- IQ £ CD fH c3 PQ CQ 0 g4 05 05 rH *0 cq rH r-H CQ CQ CQ* CQ* p= 0 £ O f & pi r-H cq r-H tq r-H CO 05 •^H 05 co OO J25 CQ od CD CD CD CQ 0) CD r-l O O os fs rC| JO JQ JO -H CO CO CO tr •J8qUI909Q 5: lONOt OS CO CO CO CO (M (M H H CO os O *j:9qui3AO]£ =; (M CO CO ^ H CO CO 04 CO JO OS CO JO 04 rH CO CO (M cq cq CO CO JO JO CO 04 o o 04 •^snSny OS CO CO t> O CO C4 co o i>- cq cq os co 05 OS 00 CO CO JO JO CO o rH 04 CO CO o r— I 04 o CO o CO o JO •jfpipU CO 04 H CO CO l> CO o as o o o o o o o JO O OO ^ rt- OS CO • JO co JO o ■H* 04 CO 04 as as co co co jo jo • CO co 04 04 r-H rH rH rH rH # 9iinp H t> H o H N 1C JO N Cl CO N 1> JO ts COi> JO o o -4H O O t- O 04 rH rH i-H CO 04 04 o3 .i •jC'bm: O O r— I OS 04 rH 04 t> CO H JQ (M co JO ^ JO ^ CO CO W CO •ir.idy CO O 00 CS O ^ JO JO CO I— I CO OO co CO ^ CO ^ ^ 04 04 04 04 TpiVJ/l CO 04 04 04 cs JO 04 rH CO t> JO -rjH CO 04 ^ CO CO CO 04 04 04 o 04 04 riH CO •Xi^ruiq9^ CO 00 J O H co CO H JO CO 04 OO o o OS CO CO CO 04 04 04 rH o o 04 •jtranmsf o ^ h M o N CO H C5 l> O O. l> CO CO Cl 04 04 r rH CO o • PJ . 03 • rH 4 JJ > (H CD 0) g ffl >-< o =M W-J3 OOO OOOOOOO OOOIMIOOOSNOOOOOOOOOOOOOOOOOOOOOO tooocoo5>cno>oOoooooeoooooooOoooOooo lt)00lM-#00OOOO °„0 O O lO O^O^O^OO^O^O^OO.O o ©_©_©_ cT io~ cif t-~ oo os' o' cT i-T,-r cTco'co m co co t- e- od'ao'aT j . — i _ j —t r—l H r-H r-H r—H rH i— H rH rH rH r-H r— H r 04 O c3 S 'C3 * rfl S o : 1 O o3 P ' o « P p P 31 242 HIMALAYAN DISTRICTS The tensions in the foregoing table have been computed from observations of dry and \V p et bulb thermometers. The formula used for the most part has been Apjohn’s ; but all the figures for Leh and Musooree, and those for the last four years at the other stations, have been computed by means of certain tables based on August’s formula. On the southern slope of the mountains the annual variation of vapour tension is similar to that which obtains on the plains, though because of the considerable evaporation from the forest-covered slopes, and the occasional showers of rain which fall, the increase of vapour during the hot weather goes on much more uniformly than on the plains. At Leh, where hardly any precipitation occurs at any time of the year, but in the neighbourhood of which there is some cultivated land irrigated from the hill streams, the annual variation of vapour tension is determined almost entirely by the temperature. In the valley of Yarkand the quantity of vapour in the air is similarly determined by the temperature and the extent of irrigation. In the mountains the mean vapour tension decreases very rapidly with the height, on account of the rapid decrease of temperature as we ascend. If Dalton’s law, that in a mixture of gases or vapours the pressure of each is the same as if it filled the whole space alone, were applicable to the , atmosphere, as is sometimes supposed even yet, then the pressure or tension of vapour observed on the plains ought to be reduced one-half on ascending through 29,000 feet; but it is found by observation that a vapour pressure equal to half that observed on the plains is attained at an elevation of 7,000 or 8,000 feet. This was pointed out by General Strachey in the Pro- ceedings of the Royal Society for March, 1861, where he has shown that the observations of Mr. Welsh in balloon ascents, those of Dr. Hooker in Sikkim, and his own observations in Kumaon (most of which are included in Table XII.), make it perfectly certain that the proportion of water vapour which exists at any given elevation is determined, not by Dalton’s law, but simply by the temperature. The vapour raised from the earth’s surface is constantly diffusing upwards, and would go on doing so until it attained the state of equilibrium represented by Dalton’s law ; but the temperature falls so rapidly as the height increases that saturation point is reached and the vapour is partially condensed into cloud or rain long before the barometric equilibrium is attained. OF THE NORTH-WESTERN PROVINCES. 243 In the third column of Table XIII. the figures given in the previous table have been compared in a manner suggested by Strachey. The tension of vapour at sea-level under Kumaon and Garhwal has been computed for each month, by multiplying the mean of the observed tensions at Roorkee and Bareilly into the ratio between the tension of saturated vapour at the sea-level temperature and that ot saturated vapour at the temperature of the plain ; that is to say, the temperature is supposed to be corrected for elevation above the sea while the degree of saturation remains constant. The figures in Table XII. have then been divided by the corresponding tensions at sea-level, and the average of the fractions for all the months has been calculated for each elevation. Finally, from these results the ratio of the tensions at each even thou- sand feet above the sea has been found by interpolation. The second column of the table gives the results of Sir Joseph Hooker s observa- tions in Sikkim compared with those taken at the meteorological obser- vatory of Gwalpara near the foot of the hills, and the fourth column has been computed from the observations in General Cunningham’s Ladak and those taken by Dr. Scully on the way back from T arkand in 187o. The latter have been published in the Indian Meteorological Memoirs , Ho. VIII. The base station for the Kashmir group is Rawal Pindi. The figures opposite 7,000 feet in the second and fourth columns are derived from the monthly means of the Darjiling and Marri observatories. XIII. — Proportions, of vapour tension at various elevations in the Himalaya. Mean for Himalaya. Height. Sikkim. 1 Kumaon. Kashmir and Ladak. Observed. Computed by Strachey’s method. Computed by Hann’s method. Sea-level ... 1-00 1-00 1-00 1-00 1-00 1-00 1,000 feet .. •S9 •92 •92 •91 •91 •91 2.000 ,, ... •83 •89 •85 •86 •83 •82 3,000 „ ... •74 •87 •69 •77 •75 •74 4.000 ., ... •67 •74 •52 •64 •68 •67 5.000 •04 •70 '51 •62 •62 •61 6,000 „ ... •59 •60 •57 •59 '56 •55 7.000 ., ... '53 *56 •60 •56 *51 •50 8,000 „ ... *50 '53 •41 •48 •46 •45 0.000 •44 •49 •28 •40 •42 •41 10,000 ., ... •40 •47 •27 •38 •38 •37 11,000 „ ... •37 *35 •26 •33 •34 •33 12,000 „ ... •35 •28 •21 •28 •31 •30 13,000 ,, ... •30 •25 •23 •26 •28 •27 14,000 •27 •20 •19 •22 •25 •24 15,000 „ . ... •27 •17 •15 •20 ■22 ■ •22 16,000 „ ... •22 *15 •16 •18 •20 •20 17,000 „ ... •20 •15 •14 •16 •18 •18 18,000 ., ... •19 •14 •15 •16 •16 •16 19,000 ,, ... •18 •13 •14 •15 •14 •15 244 HIMALAYAN DISTRICTS Tlie mean of all three sets of observations probably represents very closely the actual diminution of vapour pressure on ascending in the Himalaya. It decreases with more regularity than either the Kumaon or Kashmir series of observations alone, and it agrees very closely with the series for Sikkim, where the relative humidity, or percentage of saturation, varies much less than in the western Himalaya. The last column of the table but one gives a series of ratios calculated on the assumption that the degree of humidity is the same at all elevations, and that the temperature of the southern slope of lhe Himalaya decreases at the mean rate above found — one degree in 361 feet. This series agrees very closely with the average of the results given by observation ; though from 2,000 to 10,000 feet the calculated ratios are all considerably less than those observed in Kumaon. During the hot-weather months the degree of saturation on the plains below Kumaon falls exceedingly low, while on the hills, as has already been stated, the air remains much moister ; at Dehra, for example, the vapour pressure in March, April, May, and June is greater than at Roorkee owing to local evaporation. Thus on the average of the year the relative humidity of the air in the Kumaon hills is considerably greater than over the plain. On the other hand, the observed ratios from 14,000 feet upwards are less than those given by calculation, because most of the observations at these altitudes were made at places lying behind the snowy range* In the last column are given the ratios calculated by the log- arithmic formula, log p — log P — —ft-- , where h is expressed in feet* Ik’. Julius Hann, in an article in the Austrian Meteorological Society’s Journal for 1874, page 193, has deduced from all the available obser- vations on mountains and in balloons a similar formula in which the numerical constant is 6,517 metres, or 21,382 feet. On the assump- tion that this formula holds good to some distance beyond the limits of observation, we find that an elevation of 23,000 feet, or about the average height of the snowy peaks, the quantity of vapour in the air is only one-tenth of the quantity at sea-level. The extreme dryness of Tibet and Ladak is thus easily accounted for. The logarithmic formula has the advantage of enabling us to calculate approximately the total quantity of vapour in the air at any time, by an application of the integral calculus. Using the generally received values for the density of water vapour and its OF THE NORTH-WESTERN PROVINCES. 245 co-efficient of expansion with heat, and extending the integration to an infinite height above the ground, it is found that the depth of water that would be formed by the complete condensation of the vapour over a given area is almost exactly three times the height of the mercurial column which measures the pressure of the vapour at the bottom. In the rainy season for example, when the pressure of vapour over the Indian plain is equal to about an inch of mercury, the complete precipitation of the vapour would yield only three inches of rain, that is, less than the quantity which sometimes falls in two or three hours. A continuous downpour amounting to fifteen or twenty inches, such as frequently occurs in India, must be fed by a powerful indraught of moist air. The relative humidity of the air is probably greater at all eleva- tions on the Himalayan slope than either on the plains or on the Tibetan plateau beyond the Indian watershed ; and it is doubtless greater on forest-clad slopes and valleys than on steep and bare mountain sides. On a high ridge, too, which intercepts and deflects upwards the prevailing south-west winds, thereby cooling them and partially condensing their vapour, the degree of saturation is greater than on the lower ridges or valleys behind it ; for the air in sinking after crossing the high ridge is warmed and rendered capable of absorbing more moisture than it has been able to retain in crossing the ridge. Thus Naini Tal, independently of the influ- ence of the lake, is always much moister than Ranikhet or the notoriously dry and bare station of Almora. The registers of the meteorological observatories do not, however, illustrate this very well ; for at several of them observations have only been taken in the daytime, when the relative humidity is below the mean ; and the humidities recorded at the old observatory of Naini Tal aie quite untrustworthy and in many cases impossible. At Bareilly, Roorkee, Ranikhet, and Chakrata observations were taken both night and day for some years, at the hours of ten and four. If the means of the four observations at these hours be adopted as daily means, Chakrata appears to be the most humid of the four stations, and Roorkee and Ranikhet the driest, though the difference between Chakrata and Roorkee or Ranikhet is less than might be anticipa- ted. The humidities of the other places in Table XI Y. hav e been .calculated approximately from the monthly means of tempeiatuie 246 HIMALAYAN DISTRICTS and vapour tension. The figures for Leh in the winter months- are doubtful; the psychrometer generally giving unreliable results when the temperature falls much below freezing. XIV. — Approximate mean humidities of places in the Himalaya. Place. January. February. March. April. May. June. 15 August. September. October. November. 1 December. | Year, Bareilly 69 63 51 39 43 59 82 83 81 70 65 69 65 Roorkee 69 65 53 36 37 54 78 80 77 65 62 68 62 Delira 69 69 58 47 45 63 86 90 86 69 62 67 70 Dharms&la 83 73 67 57 51 55 79 80 77 69 56 67 68 Mussooree 66 64 53 45 49 62 99 99 98 70 61 72 70 R&nikhet ..j 60 58 52 39 49 61 85 ' 86 79 60 53 54 62 Chakrata 68 64 56 49 57 68 94 94 89 64 49 58 67 Leh ... | 100 100 79 57 52 50 62 : 66 1 68 63 67 71 70 The relative humidity of the air at all elevations up to 11,500 feet is subject to a double annual variation, one maximum occurring at the time of greatest cold, and the other in the middle of the rainy season. At Leh the summer maximum is very faintly marked, nine-tenths of the vapour brought by the south-west monsoon being cut off before reaching the station, and at Dharmsala, north of the Panjab, the air appears to be slightly more humid in winter than in summer. At all the other stations the maximum degree of humidity is reached in August. In April and November the air is dry, especially in the former month, when, during hot winds from the north-west, the percent- age of saturation over the plains often falls as low as 5 or 6. In the hills, at Almora and Ranikhet, the humidity of the air frequently sinks to 25 per cent., but is seldom less than 20 per cent. The month of November and the beginning of December appear to be quite as dry as April at the higher hill stations, where these months are rainless, while showers sometimes fall in April ; but on the plains, because of the low temperature of November and the mois- ture left in the ground by the summer rains, the air is still compa- ratively moist. In the cold weather the Sub-Himalayan stations are more humid than the hill stations on the average of the twenty- four hours, probably because the air, which is cooled and has its relative humidity increased by radiation during the night, drains away from the hills and collects over the plain. At this season the air at the hill stations appears to be drier in the mornings than in the evenings. OF THE NORTH-WESTERN PROVINCES. 247 The humidity of the upper regions of the atmosphere, as indicated by clouds, is always greater in the daytime than at night. On the outer slope of the Himalayan chain the variation is doubtless quite as distinctly seen as anywhere else in the world, hut it has not been recorded in the observatory registers, where only the amounts of cloud seen at 10 A.M. and 4 P.M. have been entered. The variation is, however, probably very similar to that which occurs •over the plains, where the sky is most serene about 10 P.M. and most cloudy at the hottest time of the day, when the upward con- vection currents are strongest. In Table XV. the figures represent the means of the 10 A. m. and 4 p. M. observations, and they are therefore a little above the true mean for the day. X V. — Average proportion of cloudy sky in tenths of the expanse. Station. January. February. | March. April. May. June. July. August. September. October. I November. j December . I 1 Year. 1 Bareilly 2-87 3-12 2-97 1*96 1-46 3-98 7-11 6*18 4'50 0-73 0-72 1*85 3-12 Roorkee 2-96 3-47 3-12 2-25 1-71 2-90 4-97 4-50 4-58 0-99 0-82 2-18 2-87 Dehra ... 3-73 4-07 3-55 2-50 2-75 4-02 7-50 7-00 4-83 1-08 1-33 2-74 3-76 Dharmsala ... 4 99 3-91 3-42 2-17 2-60 3-26 7-60 6-76 4-09 0-74 0-95 2-02 3-54 Ranikhet ... 3-66 4-42 3-78 3-34 3-58 5-41 8-58 8-42 5-64 1-69 1-31 2-99 4-40 Chakrata 4-23 4-75 4-44 3-42 3-75 5-14 8-89 8-57 6-79 2-28 1-74 3.62 4-80 Leh. ... 6-32 6*38 6-27 5-78 5-77 5-50 4-89 4-68 4*44 4-19 5-12 5-91 5*44 The annual variation of cloud is similar to that of the relative humidity of the air near the ground. It has two maxima, in the cold weather and the rainy season, and two minima, in April or May and in November. April is cloudier than November, probably be- cause the upward movement of the air during the day then prevails over the downward movement at night, while in November the preva- lent movement is downward. In this way the air in the upper strata is dynamically cooled in the hot-weather months and dyna- mically heated in November. The variation ol humidity at the hill stations is intermediate in character between that observed on the plain and the variation in the cloud-bearing strata of the atmosphere. No direct observations of the heights of clouds above the ground have been made in the Himalaya. The ordinary clouds of the rainy season that look like broken cumulus from below are often not more than 5,000 or 6,000 feet above sea-level, hill stations like Naini Tal and Mussooree being frequently enveloped in them 248 HIMA'LAYAN DISTRICTS for days. They sometimes even extend down to the level of the plains, the whole mass of the mountains up to the snows being then shrouded in fog. From the vapour tensions given in Table XIII., and the temperature decrements in Table V., it is possible to calculate approximately the average height at which a mass of air rising up from the plain would reach the dew-point and begin to form cloud. In January this height is a little over 4,000 feet above the plain, or about 5,000 feet above sea-level. In April and May the height above the plain is 8,000 feet, and at this time of the year it is rare to find clouds resting on the outer ridges of the Himalaya, though great banks of them are formed every day along the southern face of the snowy range. In the rainy season, that is, between the middle of June and the end of September, the average height at which clouds would commence to be formed in a rising column of air is 3,100 feet above the plain or about 3,900 above sea-level. This probably coincides very nearly with the zone of greatest rainfall on the mountains. In August, when the air is most humid and rainfall most frequent, the average lower limit of cloud is probably about 3,200 feet above the sea. Regarding the upper limit of cloud nothing is known. The light feathery ice-cloud called cirrus, seen above the plains of Tibet and the passes over the Indian watershed, appears quite as hi o h as when viewed from the Indian plain. It is probably formed tt all elevations to which water vapour extends, though what the upper limit of vapour is we do not know. If we assume the cirrus clouds over the Tibetan plateau to be twice as high as the plateau itself say 30,000 feet above sea-level, the quantity of vapour in the air would be only one-twentieth of that observed on the plains of India but it would probably be quite sufficient to form light clouds. The distribution of rain both on the plains and on the mountains Rain and snow. ^ as already been described in a general way. The plains of Northern India, between the mountains and the Jumna river, or a line drawn north-westward from Delhi beyond the river, may be divided into roughly parallel zones of equal rainfall, that which receives the greatest amount of precipitation lying nearest to the Himalaya. The breadth of each of these zones gradually diminishes towards the north-west and widens out in the direction of Bengal, because, the prevailing wind of the rainy season OF THE NORTH-WESTERN PROVINCES. 249 being easterly over the plain, the supply of vapour gradually dimi- nishes and the rains become lighter as we pass from east to west. In Table XVI., the average monthly rainfalls of 15 places on the plains near the base of the hills of Kumaon, Garhwal, and Dehra Dun, are given. The first group of stations is at an average distance of 20 to 30 miles from the base of the hills, and the distance of the other group is under 20 miles. In both groups the stations are arranged in order from east to west. The table might be extended indefinitely in both these directions as well as southwards, but little would be gained by doing so, since the distribution of rain above described is seen clearly enough from the figures as they stand. The average rainfall of the line of stations at a distance exceeding- twenty miles from the Himalaya is 40' 1 inches, and that of the stations at a distance less than twenty miles is 46'6 inches. In each group the total rainfall gradually diminishes in passing from the extreme east of Rohilkhand to the neighbourhood of the Ganges, where it increases suddenly and again gradually shades off' to the westward. The mean wind directions for the rainy season at Roor- kee, Meerut, and Delhi indicate that there is frequently a sort of eddy formed at that season near the upper course of the Ganges, probably by the meeting of the south-east winds of the plain with south-west winds from the Arabian Sea that have been deflected northward by the Aravali hills in Rajputana, and this may be the cause of the increased rainfall that is observed. On the mountains the rainfall varies rapidly with height, and its quantity is to a very great extent dependent on the situation of the place to the windward or leeward of high ridges and peaks. At fairly exposed stations of nearly equal altitudes there is a gradual diminution of the annual rainfall on passing from west to east, and between the Ganges and J umna there is a slight increase perfectly comparable to that which occurs on the plain in the districts of Bijnor and Saharanpur. Thus the annual rainfall of Darjiling is 120 inches, that of Naini Tal 91 inches, that of Mussooree 95 inches, and that of Chakrata, Simla, and Marri 62, 68, and 58 inches respectively. The next table gives the average monthly and annual rainfall of twenty places on the Himalayan slope, classified into three groups according to their positions near the foot of the slope, on the outer high ranges or on the inner ranges and valleys. 32 X VI. — Rainfall of stations on the plains near the base of the Himalaya. 250 himXlayan districts 1 *>• Ih tH CO CO t- rH JO rH rH rH CO rH CO 04 D— rH CM rH rH H CO CO CO CO rH JO CO CO O to CO to to to .Toqiunjsf 1 rH rH rH CO rH CO cm r ”' 04 rH 1 — t r-r CM rH o JuO rH CO CO r—i to rH rH o to O r-H ■«. rH rH JO rH O IH rH rH op p Cp O CM JO 03 l> At JO rH to cb l> © cb cb o j’o O rH ■rH rH rH CO CO CO CO JO JO rH H4 H rH JO rH 1 03 CO CO o rH rH rH CM CO Sr 03 CO CM rH M9q 1 ^ rH rH to rH CO CO CO rH rH to to -ra303Q[ j O o o O o ° © O © O o o O o O •I9q M >o .CO CO rH 03 N • O • o o rH rH ' ' r • • * * rH -Ul9AOj£ o • o o © © o H to 03 CO 00 o rH JO CM CO o rH CO o CO tr- \raqcqoo rH rH o o © © © CM rH rH o o o o O ugq CM JO rH rH 03 CO tr O “ CM JO qsnSny ^ JO lH CO rH Ip tp © O cp cp O O rH r — i 03 OO 03 cb JO (M rH rH rH cb —H CM rH H rH r— 1 rH r-H rH rH rH CM o JO to to CO 03 JO rH JO b rH C3 rH rH JO CD JO , eg cm JO JO CO rH CO JO CO Cp rH jp J O tp p 6 o o o o © o © o o O o o o o jo CO CO CO o 03 rH CO JO O 03 rH rH CM JO •qoj^j\[ ^ p c p OO -d CO CO t- OO co 03 OO to to Ir tr CO CO CO : : • • d • I l z * • I l ; • • * t J • o *43 c3 -+-> m c3 •r— i *3 Fh Nawabgai d l rQ o 05 d d c3 vS •s o3 bs a Fh d Oh § H d -H -rH rd rO rH Fh d Oh rH o3 •d d Fh d Oh •rH rd CQ Fh 3 a V05 rd 03 d -rH do 05 ■a a Q> a> F4 O o w H w P OQ <1 p S p w P £ !2i C4 JT T II. —Rainfall on the Himalayan slope. 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CO O H (> O -+< O ^ ^ cb cq cq bn cq cq cq co ^ t-h 0 0 H l>- 00 50 50 Cq r-H cq bn rH rH cq cq 0 •(139J Ul) UOpCAO[[h[ OOOOOOOO OCOOWLOCCOO OO ^ H CO^ C^ CO^ O r-T H H c4 Cq rH cb 6,600 5,850 6,550 7,052 7,511 O O O 05 O O CO JO O 05 50 JO JO CO JO lO r^ t> JO lb l b' lb 50 JO r-H r-H r-H Station, Kilpuri Haldwani ... ... Hardwar ... Molian Bhogpur ... Dehra Ambari Kalsi Naini Tal ... ■ Mussooree (St. Fidelis's, School). Mussooree (Hospital) ... Chakrata ... Landaur Champawat Pithoragarh Almora ... Ranikhet Pauri Srinagar Leli ' ^ ' ^ ' V woq vanaa cr^ v •saojstva "SiJmvA aay ‘saiayAVig ‘avayHa aaj.no sasxva aaxaj Interpolated from upper station in some years. 252 him/layan districts The influence of an elevated ridge in diminishing the rainfall of the valley behind it is seen on comparing the rainfall of Almora with that of Naim Tal, or even by comparing Srinagar with Pauri, though both of these lie far in the interior of the mountain system. A much greater contrast is observable between Bhogpur, at the foot of the mountains overhanging the gorge of the Ganges above Hard war, and Dehra, in the Dun, behind the central and highest part of the Siwalik chain. The rainfall of Bhogpur, given by the observations of two and a half years is, however, probably too high. The variation of rainfall with height can only be roughly determin- ed, because every high ridge and peak thus cuts off the supply of vapour from the lower ground to the north of it. In Table XVIII. an attempt has been made to determine it approximately from the rainfall figures in the first two sections of Table XVII., together with those of two or three places in the hills north of the Panjab and the observations made by General Strachey at Niti in 1849. The ratio between the mean rainfall of each hill station and that of the nearest station or stations on the plains, for the same years, is given in the last column. A VIII. — Rainfall of the outer slope of the Himalaya compared to that of the neighbouring plain. Hills. Station. Kilpuri Hard war Pathankot Mohan Haldwani Ambari Kalsi Nurpur Dehra Bhogpur Palampur Dharmsala Mussooree (1) Mussooree (2) Naini Tal Simla Chakrata Landaur Niti .8. Plains. Difference of elevation. Height in feet. '"cS 'cS Ph Nearest station or stations. Height in feet. r— H r *i c2 SH .9 c3 P3 800 // 60-1 Rudarpur 720 n 43-9 80 1,100 45-7 Roorlcee | S90 40-2 210 1,100 50-2 Gurdaspur 1 900 30-1 260 1,330 65'1 Roorkee 890 39-8 440 1,430 74-1 Rudarpur 720 43-9 710 1,800 77-8 Saha ran pur and Ambala, 890 30-0 910 2,000 82-3 Ditto 890 34-0 1,110 2,05(J 2,230 79-3 Gurdaspur 900 30-1 1,150 74-9 Roorkee 890 41 ’5 1,340 2,450 157-7 Ditto 890 30-0 1 ,560 4,000 1180 Gurdaspur 900 28-7 3,100 4,490 123-2 Ditto 900 33-1 3,590 5,850 142-2 Roorkee 890 32-0 4,960 6,550 95-2 Ditto 890 4P5 5,660 6,600 90-9 Rudarpur 720 43-9 5^880 6,950 68-6 Ambala 820 36-2 6,130 7 ,050 62-2 Saharanpur and Ambala, 890 36-4 6^360 7,510 87-1 Roorkee 890 42-5 6,620 10,660 11,460 5*5 J Roorkee and Rudarpur, 800 450 1 Fh c3 t+H £ •H cs PS 1-37 1*14 1-67 1-64 1- 69 2- 59 2- 42 2-60 1-80 5-26 4-11 3- 72 4- 44 2-29 2-07 1-90 1-71 205 0-12 by GmSd StraS’ AUgUSt ^ Se P tember ’ 1849 5 the observations at Niti taken OF THE NORTH-WESTERN PROVINCES. 253 By grouping together the ratios for the places lying between the even thousands of feet, many of the irregularities that appear in Table XVIII. are cleared away and the results may be accepted with more confidence. The excessive rainfall of Bhogpur, for example, will to some extent counterbalance the defect at Dehra caused by the position of the latter station behind the ridge of the Siwaliks. The following figures are thus obtained : — Height above plain. Mean height. Rainfall ratio. Observed. Calculated. Feet. Feet. 0 to • • • 1,000 435 1-68 1-83 1,000 „ ... 2,000 1,290 3-04 3-01 3,000 „ • •• 4,000 3,350 3-91 3-77 4,000 „ ... 5,000 4,740 i 3-48 3'15 5,000 „ ... 6,000 5,770 2-18 2-39 6,000 „ • . • 7,000 6,370 1-89 1-89 10,000 „ ... 11,000 10,660 0-12 0 The ratios in the last column are calculated by means of a formula, B, = 1 + 2T2 h — 0 - 47 h 2, + 0025 7t 3 , given in the official Report on the Rainfall of the North- Western Provinces and Oudh, published in 1879. It was originally computed from some- what different data, but it represents the observed ratios in the above table as closely as can possibly be expected, considering the nature of the observations. At elevations greater than 9,585 feet above the plain this formula gives increasing values for the rainfall, and is therefore inapplicable; hut from 7,000 feet above the plain upwards the rainfall ratio may be approximately represented by a logarithmic formula, log 11 = 2 * 1 5 1 — 0'287 h. In both formulae A is to he expressed in thousands of feet. The mean rainfall along Rohilkhand and the Doab, at a distance of twenty miles from the hills, is about 43 inches, and the mean elevation of this line above sea-level is 800 feet. Applying the formulae in the preceding paragraph to these data, we find that 1 The observations for the lower Mussooree station being for a very short period only, the figures for the stations immediately above and below it in Table XVlil. have been included in striking the average. 254 HIMALAYAN DISTRICTS the average rainfall on the southern slope of exposed mountain ridges in Kumaon and Garhwal would probably be the follow- ing : At 800 feet above the sea 43 inches. 99 1,000 99 99 99 2,000 99 99 99 3,000 >> 99 5? 4,000 99 99 5? 5,000 99 99 99 6,000 5? 99 5? 7,000 99 99 99 8,000 99 >> 99 9,000 J? 99 99 10,000 99 99 99 11,000 99 99 IT 12.000 99 99 60 99 125 > 159 99 164 IT 149 9T 122 99 88 9T 52 99 27 99 14 99 7 99 4 rr From the table it appears that the maximum rainfall occurs about 4,000 feet above the sea. The exact height of the maximum zone determined by the formula is 2,948 feet above the plain, or about 3,750 above sea-level. This agrees very closely with the mean altitude at which a rising column of air reaches its dew-point in the rainy season. By far the most important if not the only cause of rain in the Himalaya is the cooling of the air by expansion as it ascends the mountain slope. It has been already seen that in the rainy season, the direction of the wind at all elevations in the Himalaya up to 15,000 or 16,000 feet, if not higher still, is from some southerly quarter. Near the foot of the hills the prevailing direction is south- easterly, but at most of the stations from the level of Dehra Dun upwards the wind blows from some point to the west of south ; that is, more or less nearly at right angles to the axis of the mountain zone. The air in rising to surmount the barrier has its heat rapidly converted into the work of expansion, and it commences to precipitate rain when the temperature falls to the dew-point. When once condensation begins, the rate of decrease of vapour with height will be a measure of the quantity condensed or the rainfall. This rate is greatest at the lowest elevations ; and thus rain should be heaviest at places on the outer slope of the mountains where a rising stream of airs usually begins to precipitate moisture, as the observations prove to be the fact. OF THE NORTH-WESTERN PROVINCES. 255 The slight rainfall of places like Almora and Srinagar, to the leeward of a higher mountain mass is caused by the partial exhaus- tion of the vapour in crossing the mountains and by the dyna- mical heating of the air as it streams down towards the valley, both causes diminishing the tendency to condensation. The rapid decrease of rainfall on ascending beyond 6,000 or 7,000 feet is due simply to the exhaustion of the vapour, but at all elevations the influence of high ranges in cutting off the supply of vapour is easily seen. Regarding the rainfall of 1849 on the Tibetan table-land, General Strachey says: — “In the country beyond Nfti no register was kept ; but during a week of rainy weather in the middle of August 1’5 inches fell at Niti, while at Sanjar, beyond the watershed, where I was then encamped, at 16,500 feet, the rain never exceeded a very faint drizzle, and could hardly have been susceptible of measurement.” At the Leh observatory all through the summer the rainfall hardly ever exceeds a few drops, and the greatest fall in a month during several years was an inch and a half. Sir Joseph Hooker’s experience in Sikkim supplies us with facts quite parallel to these. In August, 1849, he says 26*8 inches fell at Darjiling, while in the interior, at the same elevation, but in the rear of the first masses of snowy mountains only 12*5 inches were, measured. Between the 8th of September and the end of the month only 1'7 inches fell at Mome Samdong, about 15,500 feet above the sea, while at Darjiling- 10 inches fell, and other instances of a similar nature might be cited. The variation of rainfall with season is very distinctly marked in India. At all the stations in Tables XVI. and XVII., and at almost every station on the North Indian plain, the driest month of the year is November. In the great majority of years no precipitation whatever occurs in this month or in the first half of December, except perhaps on the higher mountains towards the north-west where the winter snows usually begin before the end of November. About Christmas a few showers of snow usually fall on the outer hills, and at the same time there is a slight precipitation of rain over the plains of the Panjab and the North-Western Provinces. These winter snows and rains increase in quantity and in frequency on the hills and in the north-west Panjab until February or March, 250 iiimXlayan districts but on the plains of the North-Western Provinces and Behar the maximum occurs in January. The cause of the winter rains and snows has already been pointed out in describing the annual changes of the winds. In October and about the beginning of November the air over Northern India is as near as it ever attains to a condition of statical equilibrium. It is subject to the diurnal oscillations called ihe barometric tides and to the accompanying mountain winds, but there is little permanent move- ment of the air in any direction. During the cold weather, however, the neutral plane of pressure gradually sinks and the south-west upper currents of the atmosphere are then forced to ascend the slope of the mountains where they precipitate more or less of the vapour they contain. On the lower hills the temperature increases so rapidly in March and April that the tendency to precipitation, and consequently the rainfall, becomes less than in January and February, though the upper currents continue to blow from nearly the same direction as in winter. Along the southern declivity of the great snowy range, however, thunderstorms are of daily occurrence at this time of the year, and above the snow line considerable quantities of snow are frequently precipitated. In Ladak the heaviest falls of snow observed by Captain H. Strachey in 1848-49 occurred in April ; but during the three years, 1876-78, there was no precipita- tion at Leh in that month. April and May are the months in which hail is most frequently noticed in the Himalaya. No regular registers of this phenomenon have been kept, but nearly every year several hailstorms occur in the outer hills, and the stones are often of large size. On the 11th of May, 1855, a hailstorm occurred at Naini Tal in which many stones of 6, 8, 10 and even 24 ounces were observed to fall, the circumference of these varying from 9 to 13 inches. In 1878 there was a storm in which large hailstones fell, some of them so heavy that they punched holes through the zinc roofs of the houses, while the quantity was so great that it lay in shady places, where covered with leaves, for nearly a month. About the middle of June usually, and sometimes before the end of May near the foot of the hills, the hot north-west winds of the plains give way to sea winds from the Bay of Bengal. The OF THE NORTH-WESTERN PROVINCES. 257 whole of the lower atmosphere over India is then moving towards the Himalaya ; and the upward deflection of the air currents by the mountains causes frequent precipitations of rain in the manner already described. The rainy season almost always commences sooner on the mountains than on the plains, for saturation is reached first at high elevations and then propagated downwards by the cooling effect of the falling rain drops and the cutting off of the sun’s heat by clouds. At most places in India, and in the inner parts of the Himalaya, July is the rainiest month, but on the outer slope of the mountains August is equally or sometimes even more rainy, especially towards the north-west of the chain. While the rainy season lasts, the parts of Ladak about Leh, and the Tibetan plateau generally, receive perhaps, on the whole, less precipitation than in winter, because the temperature is then so much higher than on thelndian side of the chain, this high temper- ature greatly decreasing the relative humidity of any air that may reach the plateau from the south. It is probable also that the high snowy peaks, lying above the limit of the monsoon current proper, receive less precipitation in summer than in winter. At the turn of the seasons, however, about the end of September, falls of snow amounting to several feet in thickness sometimes occur on the passes over the Indian watershed. Shortly after the autumnal equinox, about the end of September or beginning of October, the rains cease all ovei Hoi them India. The sudden cessation of the rainy season seems to be in some measure determined by the rapid diminution of solar heat, as the sun retreats to the south of the equator. It is possibly to this that we must attribute the somewhat remarkable regularity of the recurrence of two or three days incessant lain frequently experienced in Kumaon about the 20th of September. On the plains, also, it is well known to the natives of the country that if rain falls in the nakshatra (lunar mansion) of Hathiya — that is, in the last week of September or first week of October, it is likely to be heavy. Excessively heavy rain, like that of the 17th and 18 th September, 1880, when 30 inches fell in little more than two days at Naini Tal and produced a disastrous landslip, cannot, however be thus produced by a simple loss of heat, but requires a powerful indraught of moist air to keep up the supply of vapour. The 33 258 HIMALAYAN DISTRICTS OF THE N.-W, PROVINCES. heavy rain observed on the plains at “ the break-up of the monsoon,” and probably also that which falls at the same time on the outer hills of Kumaon, must be due chiefly to the minor storms of a cyclonic character that are frequently formed near the head of the Bay of Bengal at the turn of the season, and pass inland in a north-westerly direction. CHAPTER VI. Economic Mineralogy. CONTENTS. Mining history. Experiments in Garhwal. The Kumaon Iron Works Company. Causes of present poor returns. Mode of mining : excavation: removing the oie . crushing the ore : cleaning the ore : drainage. Smelting operations : refining the ore. Division of profits. Improvement needed in appliances: Chili furnace: English system. Outturn. Financial results of the settlement of the revenue derived from minerals. Gold : Tibetan gold-fields : Thok Jalung mines. Silver. Copper mines: Rai mine and its ores : Sira mines: Gaul and Sor Gurang. Bournonite. Copper mines of Garhwal : Dhanpur : Dhobri : Pokhri : Chaumattiya mines : Raja’s mine : Nota mine : Thala mine : Danda mine : Talapungla mine : Kharna mine : Agar Sera mine. Iron mines : Kumaon iron mines : Giwar mines : Garhwal mines : Nagpur; Dasauli : Iriyakot. Lead. Arsenic. Lignite. Graphite. Sulphur. Borax. Gypsum. Soap-stone. Asbestos. Silajit. Limestone. Building stone. Roofing slate. Alum. The mineral resources of the Kumaon division early obtained the attention which their traditional value Mining history. assumed to be due to them, and it was one of the directions to the first Commissioner to procure specimens of the ores to be found in Kumaon and transmit them to the mint for assay. Specimens of copper ore from the mines in Sira and Gangoli were accordingly forwarded to Calcutta in 1815, but the report was not favourable ; for, if the specimens sent were fair samples of the ores in general, it was doubted whether the mines could be worked to advantage. 1 The Government were, however, not satisfied with this report, and in 1817 deputed Mr. A. Laidlaw as mineralogical surveyor to accompany Lieutenant W ebb s pai ty thr ough Kumaon. Iiis orders 2 were to consider the examination of the mineral resour- ces of the country his primary duty, though at the same time he 1 To Government, dated 26th June, 1815 : from Government, dated 13th Jan- uary, 1816. For further information on the mineral resources of Kumaon see Moorcroft’s Travels, I., 7 ; As. Res., XVIII., 286 ; Rec Geol. Sur., 1871, 19 . II., 86 . (Lawder) III , 43 ; J. A. S , Ben., VI., 653 ; Glean, in Sc., K 230 . Graphite, Glean, in Sc., III., 280 ; J. A. S„ Ben., XXIV., 203 , N.-W. P. Rec., Ill N S., 371 ; G. India Rec., XVII., 58. „ TTT , iron ores and works, N.-W P. Rec., XVIII., 1 ; Rec. G. India, Sup., VIII., 37 • XVII , 1 : XXVI. : Bh&bar iron works, Agra, 18ob. Copper ores and works, J. A. S„ Ben., VII., 934 (Drummond) : VIII 471 (Glasfurd) : XII., 453, 769 (Lushington) : XIV., 471 (Reclcendoif) As. Res., XVIII., 239 ; N.-W. P. Rec., III., N. S., 22 ; Glean, m Sc., I., 228. ^Phonf* GovCTnme^^dated' 11th July, 1317. Mr. Laidlaw died at Pithora- garh in 1836 , and I have not been able to procure any of his ongmal iqoit. 260 HIMALAYAN DISTRICTS should not feel himself debarred from bestowing attention on any other matters deserving of scientific research, so far as such investi- gation did not interfere with his more immediate duties. These instructions further go on to say : — “You should ascertain the existence or otherwise of mineral productions applicable to purposes of public use, or available as a source of revenue ; and report on the practicability of bringing them to account. The existence of iron and copper ores in considerable quantity has already been ascertained ; but as the working of these metals might injuriously affect important articles of British import, it is not designed that your attention should be occupied in detailing any practical arrangements for that purpose ; you will not, however, consider yourself debarred from prosecuting enquiries into any circumstances regarding them which may be of sufficient interest to science to merit particular notice. In every part, indeed, of your researches it is the wish of Govern- ment that, in the first instance at least, you should contemplate rather the general capabilities of the country which you are to visit than the special means necessary for bringing them into action in any particular district ; though, of course, the facility or difficulty with which metallic ores or other useful minerals could be raised and brought to market must be a leading point in your observations on them. The minuter details of machinery, mode of working, &c., are what it is meant to postpone, as these will be the subject of future determination, when the whole result of your survey shall be before Government.” In 1826 Captain J. D. Herbert submitted his report on the mineralogical survey of the province. 1 This was followed by a report 2 in 1838 by Captain H. Drummond, of the 3rd Light Cavalry, on the copper mines at Rai in Gangoli and at Sira in Barabisi. Captain Drummond had brought with him from England an experienced Cornish miner, Mr. Wilkin, to examine the mines already worked, and proposed that, with a view of ascertaining their actual value, a certain sum should be advanced by “ Government for an experimental opening of such mines as might appear best suited to the object in view.” This proposal was accepted 8 by Government, and a sum of Rs. 2,415 (subsequently increased by Rs. 1,000) was 1 To Commissioner, dated 10th January, 1826. 5 J. A. R., Ben., VII., &31 ; andStat. Kum., p. 358. 3 To Commissioner, dated 26th November, 1838. OF THE NORTH-WESTERN PROVINCES. 261 allotted to carry out the designs furnished by Captain Drummond. A report 1 on the experiments then undertaken was rendered by Mr. G. T. Lushington, Commissioner of Kumaon, in 1842. The place selected for the important purpose of determining the advantages or otherwise of working the Experiments in Garhwal. European superintendence was the Pokhri copper mine in pargana Nagpur in Garhwal. The works were carried on from 1838 to 1841 with a net loss to Government of Rs. 7,384. The Commissioner considered this complete failure to be due to the poorness and scarcity of the ores found, and not in the least to any want of skill or industry on the part of Mr. Wilkin, or any injudicious selection of the places for experiment. Mr. Reckendorf, a mining engineer, visited these mines again in 1845, and in commenting on the deductions to be drawn from Mr. "Wilkin s experiment, gave it as his opinion that the operations then under- taken should not be considered as conclusive against the value of the mines. 2 The experiment should have been confined to driving a shaft some thirty or foi’ty fathoms below the old mines, and not to collecting ores which might have been a good addition in smelting other ores, but the smelting of which alone could never be profitable. Again, there were no proper appliances for smelting, the loss from which by the native method adopted was very great, and the ores used, from their nearness to the surface, had already lost much of their value by the slow metamorphosis of pyrites into sulphate of copper. On the whole, Mr. Reckendorf’s opinion was favourable to more extended and expensive operations in the hands of a private company. Nothing of importance, however, resulted from this the first attempt to obtain some accurate information regarding the mineral resources of the Himalaya. Captain Drummond also com- bated 3 the conclusions arrived at by Mr. Lushington as to the mines not affording a fair field for investment of capital, and in support of his views quoted the testimony of Captain Glasfurd (Executive En- gineer), Captain J. D. Herbert ( Superintendent of the Mineralogical Survey), and the experts Wilkin and Reckendorf, who had actually visited and partially worked the mines. He urged that the sums 1 J. A. S., Ben., XII., 454, and Stat. Kum., p. 367. 2 J. A. S., Ben , XIV , 471 ; and Stat. Kum., p. 385. 3 In a pamphlet published m London m 1845, and Stat. Ivum., p. 393. 262 HIMALAYAN DISTRICTS hitherto expended were barely sufficient to pay for the expenses of dis- covering and laying open the lode, and were utterly insufficient to carry on the experiment in the only way in which it could he made to pay. Nothing was undertaken until 1852, when the mines were again opened on the same footing, but the result was failure as complete as before. No attempt has since been made towards placing the copper mines of Garhwal under European superintend- ence. In 1872, however, a European leased the mines and con- tinued the extraction of the ore according to the native method, but was obliged to abandon the process, as he found the cost of the metal when manufactured more nearly approached the current rate for silver than that obtainable in the market for the best foreign copper. The copper mines in Kumaon have never been worked under European superintendence, and any remarks that I have to make on their value or fiscal history will be found under the notice of the mines themselves. * Connected with the history of mining enterprise in Kumaon Kumaon Iron Works special prominence must be given to the Company. Kumaon Iron Works Company still in exist- ence, and whose origin is no doubt due to the continued belief, in spite of successive failures, in the possibility of turning the utilisation of the mineral resources of the province into a profitable investment. These had again in the regular cycle of inquiries become the subject of much speculation. From a review of the information before Government and the results of certain experi- ments made in 1856 the Directors of the East India Company sent out a Mr. Sowerby and a large staff of mining assistants in 1857 to carry on the smelting of iron on account of Government in the interior. 1 The fact was soon established that iron of an excellent quality could be manufactured at rates below the cost of iron imported from England, and a number of private individuals under] the style of Davies and Co. were permitted to undertake oper- ations for the same pm*pose in other parts of the lower hills. 1 Report on the Government iron works in Kumaon, with plans, specifications, and estimates for establishing iron works in Kumaon, and remarks on the iron deposits of the Himalayas by W. Sowerby, C.E., printed as No. XXYI. of the Sel. Ree.. Government of India (Public Works Department), Calcutta, 1859. These papers give a review of the English, Ulverstone, Continental, Belgian and French, Rhineland, Black Forest, Bohemian and Styrian Iron Works, and estimates and plans for adapting the approved processes of those iron countries to the Kumaon mines. OF THE NORTH-WESTERN PROVINCES. 203 The avowed object of the Government enterprise was to induce private companies to work by demonstrating the financial and physical possibility of carrying on iron works as a remunerative industry in this province. Messrs. Davies proposed to take over the tract between the Dhabka and the Bhakra, and their proposals were accepted, with an assurance that they might proceed in confidence to make their arrangements, as Government would grant the lease sought. They therefore took over the Khurpa Tal works in the rains of 1858, and paid their cost price in 18(53. This company also erected buildings at Kaladhungi at a cost of Bs. 1,25,000. On the failure of the Government works at Deh- cliauri Colonel Drummond ottered to take them over at a valuation. These works were given over to Drummond and Co., who paid the capital under agreement into the treasury in 1861. The forest rules were relaxed in favour of both companies, so as to allow them entire control over the fuel supplies, and eventually in November, 1862, both companies were amalgamated under the title of the North of India Kumaon Iron Works Company (Limited). Soon after the formation of the company instructions were received from the Secretary of State to construct a tramway to Khurja on the East Indian Bailway, chiefly, it would appear, to afford an outlet for the iron manufactures of Kumaon. The tramway was to be laid with cast-iron rails manufactured at Dehchauri, and the company lost no time in making several thousand maunds of pig iron. Before the rails were made, however, the Government announced its determination not to undertake this line itself, but to hand its construction over to the Oudh and Bohilkhand Railwav. It was */ essential to the success of the enterprize that some such outlet should exist, and the company accordingly determined to close its works for a time and await the opening of the line. A license was granted by Government, but, unfortunately for the company, not executed till it was too late, and the deed of agreement contained briefly the following clauses 1. — That a capital of 3 % lakhs of rupees should be paid before execution of the deed. 2. — That the, company should pay Bs. 83,585 as the liquidated value of the works at Dehchauri, Bamgarh, and Khurpa Tal, made over to them by Government, in four instalments, on or before the 1st Sep- tember, 1862, 1863, 1864, and 1865, respectively; and in default of one 264 HIMALAYAN DISTRICTS payment the whole to become immediately due. 3. — To pay yearly, for the first three years from 6th June, 1861, a rent of Es. 1,500, and thereafter a yearly rent of Es. 2,500 and a royalty of one rupee per ton of cast or wrought iron produced, and eight annas per ton of iron ore raised and sold without being smelted ; the said royalties not to be paid unless they exceed, and only so far as they exceed, the rents of Es. 1,500 and Es. 2,500 before named ; payments to be made on the 1st May yearly. 4. — To erect during the third, fourth, and fifth years suitable furnaces with requisite appliances for the smelting or blasting of iron (no number men- tioned), and during these third, fourth, and fifth years to manufac- ture at least 750 tons of iron per annum on an average, and thereafter till the end of the term of 50 years manufacture 2,500 tons of iron per annum on an average of three years, to be struck in May each year. 5. — That the area of the forest at the close of every ten years should be covered with at least nine-tenths of such timber like trees as stood upon it at the commencement of the term, and when less than nine-tenths the company should plant to the necessary extent, failing which they should pay for each default Es. 20,000. 6. — Not to transfer their lease without the consent of Government. 7. — To keep all roads (not being public ways made by Government) used by them in repair, also their works. 8. — At the close of their term remove their buildings, &c., first giving Government the option of purchasing them at a fair valuation. — On the failure to pay or manufacture as stipulated, Government to enter upon and possess the works. 10. — But if such failure is not due to the neglect of the company, they shall be free from such penalty. The purchase-money of the Khurpa Tal works was alone paid up, but the forfeiture clause was suspended by the local Govern- ment in 1868. The forest tract was never given over to the company in the meaning of the agreement, but its revenue has been sepa- rately collected and credited by Government. The license was not sent up from Calcutta till June, 1864, by which time the company had begun to see that the speculation would not turn out a profitable one. In fact the license deed was not prepared for signature until after the company had suspended operations, and then it was ruled by the Solicitor to Government that it ought not to be signed. The- OF THE NORTH-WESTERN PROVINCES. 265 map of the tract to be given over to the company was not completed till 1869. So much for the relations of the company to Govern- ment, and the delay in dealing with its affairs which has been shown throughout. In June, 1861, permission was obtained for the company’s manager to draw against their capital. This was expended with little result, and in 1864, as above mentioned, the company was wound up. This result was in a great measure, no doubt, due to the company being unable to raise capital in the market, owing to the defect, or rather the want, of title, which appears to be ascribable to no fault of their own. Since 1865 correspondence has been carried on in reference to the affairs of the company and plans have been proposed for its resuscitation. In 1872 the works were visited by Mr. Jones of the Roorkee Workshops and valued ; he made them then worth Rs. 1,26,733, with a debt to Government of about Rs. 80,000. There can be no doubt that the works can hardly be said to have had a fair trial, and the valuable opinion of the Commissioner of Kumaon may be quoted to the effect that there is every reason to believe that, if carefully supervised and fed with capital, the works should at least turn out as favourable under any circumstances as the East Indian Railway. There is no doubt that, in the distance, the fuel difficulty exists, but at Dehcliauri and Kaladhungi for many years this can- scarcely be felt, and under penalties to replant, the company may fairly be allowed to have an unlimited supply from the neighbouring forest. At Ramgarh it is doubtful whether iron manufacture will pay, as the ore, though of the finest quality, lies at a considerable distance from any forests of any considerable magnitude, so that until it has been definitively settled whether coal does or does not exist in Kumaon the eventual absolute success of these Kumaon mines must remain problematical. 1 The increase of railways in Northern India and the development of the resources of this province must sooner or later press these diffi- culties into notice, and they will then obtain a final solution. “ Too much has been written and too little done” hitherto in this direction. In reviewing the causes of the poor returns from the different Causes of present poor mines, one that presses itself into notice on returns. the most cursory inquiry is the comparative ‘ 1 For the materials for this note I am indebted to the office of the Com- missioner of Kumaon and a note drawn up by Sir - Henry Ramsay, than whom the Company and Kumaon has no more warm well-wisher. ' 34 266 HIM/LAYAN DISTRICTS inaccessibility of the principal mines. The copper mines of Sira and Gangoli, equally with Pokhri and Dhanpur, are situated on high cliffs in the interior. The talcose and calcareous formations in which the ores are found occupy the high precipitous mountains which build up the outlying spurs of the principal range, and some lie within it. This chain itself is metalliferous, as the lead mines at Ghirti between Milam and Nfti, the copper indications at Tola and elsewhere in the Juhar country, and the copper and iron mines at Polar near Pudrnath combine to show. The absence of coal and the increasing cost of wood fuel, with the distance it has to be carried when the forests near the mines have been exhausted, materially enhances the cost of production, while the difficulties of carriage in the tracts where the mines lie are often such as almost to preclude the transport of ore for smelting, and the forests in the neighbour- hood of most mines only suffice for the most moderate requirements. Another difficulty is the want of labourers. The present work- men only come to work in the mines from the latter end of October to the beginning of April, and many of the less pro- ductive mines have been abandoned owing to the miner class turning to agriculture and to supplying the labour market at Ranikhet and Naim Tal. This want, however, could be supplied from Nepal were regular wages and constant employment once established. Sea-borne copper, though inferior to native copper, is fi om its cheapness piefeired, and until capital is invested in opening up the larger mines and conducting the whole operations on a sufficiently large scale to warrant the permanent investment of capital in machinery and proper furnaces, and other appliances for the more economical working of the ore, mining enterprise must remain as it is — a practical failure in this province. It may be said that these extended experiments have already been tried in the case of the Kumaon iron works, but this remark will scarcely apply, as that is another of those unsatisfactory operations which stopped just at the point where further progress would have decided the question for or against the possibility of making mining speculation a remunerative one in Kumaon. I shall now briefly describe the mode of working and the financial results of the settlements of the revenue from mines from the official reports and papers before describing each mine. OF THE NORTH-WESTERN PROVINCES. 267 Mode of excavation. The mode of working the mines is the same in Garhwal and Kumaon, and the suggestions for its improve- Mode of mining. m ent will serve for all classes of minerals. A gallery or passage is cut in the face of the hill with such slight declivity outwards as is sufficient to carry off the water. These adits have more of the nature of burrows than that of the shafts known in European mining. The section is always small, and in those parts where the hardness of the rock occasions any difficulty in working the passage is scarcely sufficient to admit of a person in a creeping posture. In no place will it allow of an erect position. Where necessary, frames of timber formed of unsawn branches of trees, rudely and even carelessly constructed, are set up to support the roof and sides. Accidents are therefore not uncommon, and the frequently falling in of the mines is one result of these imperfect protections . 1 The ore as well as the rock is excavated by a very different kind of pickaxe, the handle being made of a piece of wood with a knob at one end, into which a piece of hard iron is thrust and sharpened at the point. This with a miserable iron hammer, wedge, and crowbar, constitutes all the apparatus that the native miner has to depend upon. It is plain that with such tools no hard rocks can be penetrated nor can the softer ones be worked with much facility, and to this fact may be attributed the universal smallness of the passages throughout the mines, as the native miner can have his passage no larger than the rock which encloses the ore and its matrix will admit of. Proper pickaxes and steel gads (wedges) should therefore be substituted instead of the inefficient tools in use, and when blasting may be required the necessary materials should be provided. The miners work during the day, using torches made of dry pine, and clear out on an average from ten to twelve maunds of ore. The ore is removed from the mine by boys, who pick up the stuff with their hands and put it into skins, Removing the oie. which they drag along the floor by means of a rope and cross handle attached to their neck to the entrance of the mine. In most mines the greater part of this work must be done in a creeping posture, the string from the skin being fastened around the waist of the dragger. In place of this method wheel-barrows i Paras. 19, 20, Captain Herbert’s report, already quoted. 268 hima'layan districts or sledges on four wheels and shovels should be used when the passages are enlarged and properly supported with sawn timber. The ore or dhun being delivered at the mouth of the mine is Crushing the ore. reduced to a small size either by the water- mill or by the manual labour of women. A large stone is placed on the ground on which they lay the ores ; they then, either with a stone or a large hammer, and more frequently the former, proceed to pulverize the ore and pick out the im- purities. In this way a woman may manage one to two maunds (821b avd.) a day, according to the hardness of the ores. In Corn- wall a woman will pulverize from 10 to 15 cwt. per day, according, as in the former case, to the nature of the ores. The method m practice there is, first, to dispense with the picking ; secondly, to have the ores elevated, so as to enable the individual to stand while working, and to have a plate of iron about a foot square and two inches thick on which the ores are broken with a broad flat hammer. The impurities are then finally separated by a peculiar mode of dressing the ores with a sieve, by which a boy gets through with from one and a half to two tons per day. The ores are conveyed to the women, and from them to the boys by a man who attends for that purpose. The washing of the ore in Kumaon also is performed by women, Cleaning the ore. w stuff in baskets from the entrance of the mine to a stream, where they contrive by dabbling it with their hands to wash off the mud and finer particles of the earth. They then proceed to pick out all the pieces of ore they can get hold of; or, in the case of what may be submitted to the water in a commuted state, they work this against the stream, so as to gather it clean at the head of a small pit by handfuls ; but, from the bad construction of the pits it is with difficulty that this is performed. After picking up any larger P leces of ore which may have gone back with the stream they scoop out the refuse with their hands, and then proceed with another charge. In Cornwall, one woman provided with a wheel- barrow and shovel for the conveying and washing of the ores and a boy with a sieve for dressing them, as formerly mentioned, would accomplish a task equal to that of ten women on the system rl nari J OF THE NORTH-WESTERN PROVINCES. 269 The drainage of the mine is managed in a proper manner by an adit. But whenever any attempt is Drainage. niac l e to go below it, as is the case in most if not all of the mines, the water is then raised in wooden buckets, handed from one man to another until they reach the adit into which they are emptied. In this manner six, ten, or even more men may be employed, whilst only an inferior number can be spared for excavating the ores. At the Sira mine, for instance, six men were found constantly engaged in lifting up the water, and there were only two at the ores : the work done by these six men could be effected with a hand-pump by one man ; but in order to keep the pump constantly going, two men might be required, and the remaining four added to the number of those who are excavating. The furnace of the Dhcinauriya or smelter is very simple, and is made of common stone and clay faced with Smelting the oie. s l a bs of quartzose schist, luted with a com- post of chaff and clay. It is about 3%' long by i\' broad, with an ash-pit about six inches square, all of which are built inside a house about 12' by 14', of which the roof is composed of planks. (Figs. A.. B.) The operation of smelting takes about 28 1 hours, during Fig. A.- Kiimatjro j'umcu'^ /T| //h I I! FFf. B.- Vr-rtiml Section,^ from; thejrovF Sill!®®! JL Mill II III 270 HIMALAYAN DISTRICTS which time the fire is kept up, and after that the facing slabs and luting require renewal. The implements used are a crowbar, poker, shovel, and a pair of buffalo hides, dressed whole, to form the bellows, the neck of which forms the nozzle, and the buttock the valve for the ingress of air. The hides for making them are worth Its. 12 apiece. 1 The furnace being freshly luted, the ash-pit is filled with charcoal dust and chaff, and a fire being lit, six baskets of iron ore, each containing about thirty sers (the ser = 2Ib. 2oz. avd.), are placed round the fire. The blast is then commenced, one bellows being inflated while the other is undergoing depletion. In about half an hour the slag commences to flow from the floss- hole, which is kept open by a poker. In about two hours more, theory having subsided considerably, two more baskets of ore and a corresponding supply of charcoal is given with a new luting for the bellows nozzle. In another two hours, this having also subsided, the charge is deemed ready. The fire is then raked out through the flosshole, and the charge, consisting of a pasty mass called phalka or jhauj, is shoved out with a crowbar by the smelter. The same operation is repeated until seven blooms are obtained, consuming thirty-eight baskets of ore, thirty-one of which are converted into the seven blooms, and the remainder, comprising the partially roasted ore, become the property of the smelter. The charcoal consumed weighs 340 sers, or a little more than the seven blooms, which weigh 327 sers, or about one-third of the ore expended (930 sers). Each bloom consists of three qualities of metal, all intermixed with earthy particles. These are kept separate, and are broken into small pieces before being sent to the khatauniya or refiner. The furnace of the refiner is smaller than that of the smelter, and the implements required are a pincers. Refining the ore. poker, two or three sledge-hammers, an anvil, and bellows. The fire being lit, a mixture of one-sixth of first quality, one-sixth of second quality, and the remaining two- thirds of third quality, in all about six sers of bloom metal, is placed on the hearth opposite the bellows, with the larger pieces nearest the fire. The blast having commenced, in a quarter of an hour the slag begins to flow, and in another quarter of an hour the 1 Beckett, III., Sel. Rec., N.-W.P., 25. OF THE NORTH-WESTERN PROVINCES. 271 metal (now a porous, pasty mass) is taken out ot the fire and subjected to the blows of two or more sledge-hammers ; the blows being slight at first, to prevent the metal flying into pieces, hut as it becomes more solid, they are given with the full force of the workmen. Meanwhile a fresh supply of bloom-metal is placed on the hearth, as at first. The hammered mass, after several hammerings, assumes the shape of a small bar, weighing one and a quarter ser ; it is thick in the middle and tapering to either extremity, and six sers of charcoal have been used in its formation. This bar is now fit for the market, and is called by the workmen pjiala , but by the plains-people pain. The charcoal used by the refiner is made from the dry trunks of fir trees which have been felled for two or more years, while that made use of by the smelter is made from small green wood. The refiner class is subdivided into another, called Bhadeliya, who, instead of making the iron into bars, manufacture it at once into cooking utensils. Nine hundred and thirty sers of ore produce 327 sers of bloom-metal, which in its turn produce 82 sers of marketable bar-iron, or only 8*8 per cent. The bloom operation consumes 340 sers of charcoal and the refining process 667 sers, so that for every ser of iron produced 8*2 sers of charcoal are consumed. The Swedish furnace only consumes l'oo times the weight of the iron produced. The mines are leased for a term of years to contractors for a Division of profits. certain sum, and the lessee collects for the season from the different classes of workmen at the following rates : from each son or miner Its. 2^ ; from each gang of smelters Rs. 4£ ; from refiners of the Khatauniya class Rs. 4£, and from those of the Bhadeliya class Rs. 6. The miner is originally sole proprietor of the ore, which he takes to the smelter to reduce into blooms, giving him for his trouble one basket of ore (30 sers) and one basket of charcoal (5 sers) for each bloom turned out; also for each set of seven blooms 16 sers of grain, and food for one man for four days ; and at the end of the season a suit of clothes. Sometimes, however, owing to the smelter being largely in debt to the miner, he does not receive any charcoal from him. The smelter can only work for certain miners, generally five in number, not being allowed to work for any other miners ; or, in other words, each party of five miners employ one family of smelters exclusively. 272 HIMALAYAN' DISTRICTS Each party of smelters must consist of at least five persons, but they generally count eight to ten persons. The share of each party of refiners is one half of the bloom-metal made over to them to refine, no further remuneration being allowed them. Refiners, unlike the smelters, are not bound to work for any particular peison, but may work for any one that chooses to patronize them. In the roasting and smelting of the ore Captain Herbert Improvement needed in recommends a system of reverberatory fur- appiiances. naces for these two different processes. An excellent material is at hand in the indurated talc known as potstone, which, though soft, is infusible. The simple blast furnace in use in Chili would also be an improvement. It is of a circular shape, similar to a lime-kiln, covered with a dome to confine and concen- CMli furnace. ^ ra ^ e ^ ea ^- The ore is arranged in it in alternate layers with the fuel, which is wood, and being lighted it continues burning for a considerable time! II hen required, the heat is urged by a double pair of bellows worked by a crank turned by a water-mill. The methods of reduction practised in England, where the English system. subject is best understood, vary with the ore, an d even with the establishment. But the differences are trifling and only affect the minor details. The two great objects to be effected are, first, by a proper calcining heat to drive off the volatile ingredients sulphur and arsenic, and to oxidate the iron, thereby promoting the fusibility of the ore and consequent separation of the metal from the scoria when in fusion; and, secondly, by an intense and properly continued fusing heat to effect the vitrification of all the impurities which thus form a slag at the top and are skimmed off while the metal sinks down in a compara- tively pure state. To promote this vitrification of the ingredients occasional additions are made to the ore as the case may seem to require, though in general the run of the ores is such as to require little beyond a few slags of an old smelting. The operations of roastin g and smelting are repeated several times, each smelting being followed by a roasting, to expedite which effect in the case of copper the ore is, after each smelting but the last, let into water to be granulated. This separation of the metal into such small parts assists the calcining power of the furnace, and the work is more speedily effected than if OF THE NORTH-WESTERN PROVINCES. 273 performed on tlie mass. After the last smelting comes the process of refining or poling, which consists in keeping the copper in a melted state covered with charcoal, and introducing from time to time a wooden pole into the melted mass to produce the evolution of o-aseous matters. Lead is sometimes used both in Hungary and England to expedite the previous operations of the refinery. The oxides of this metal are amongst the most powerful verifiers known. As such they are effectual in the assay and refinery of the precious metals, and as such they may be also used with copper. But the process requires attention, for if not stopped in time, or if too much lead he added, the copper itself will be oxidated and vitrified. The process of manufacturing iron from the ores is different from that of copper, inasmuch as none but the oxides or carbonated oxides of the former metal are ever employed. In the copper ores, that is in those which occur in any quantity, the metal is combined with sulphur, which can only be driven oft' by repeated roastings. In the iron ores the metal is united to oxygen and mixed with various earthy impurities. In reducing these ores, then, there are three distinct points to be attended to : first, the provision of a substance which shall effectually take the oxygen from the ore, leaving the metal mixed only with its earthy constituents ; second, the proportioning the flux used to those earthy ingredients so as to insure a complete vitrification of them and separation from the metallic particles; and third, a sufficient heat to fuse the latter, that the separation and reduction may be more complete. The fiist point is attained by using a sufficient quantity of charcoal in the reduction of the ores ; the second by adding, as the ore may lequiie it, limestone or other flux ; and the third point is only to be effected by using a powerful blast furnace. It is not easy to give the outturn from the mines, the arrange- ments are so intricate and the returns so ’ imperfect. In 1868 about 29 maunds of copper were raised from the Kumaon mines, and in 1869 the same mines yielded the same amount, of which 21 maunds were exported. The Dhanpur mines in Grarhwal yielded 10 maunds of copper in 1869, but every year since the produce has decreased. In 1868 tie Kumaon iron mines yielded about 2,000 maunds of metal, and the Garhwal mines about 1,752 maunds, while the returns of 1869 give 35 274 hima'layan districts 5,153 raannds for Kumaon and 529 maunds for Garhwal. Besides tliis an immense quantity of copper is imported into Kumaon in the shape of manufactured vessels for culinary purposes : about 2,000 maunds of iron also are imported from the plains against 155 maunds exported. No reliance can be placed upon the estimates of outturn in recent years, as the mines have been leased for a term of years, and the lessees are not inclined to have their affairs too closely examined. Previous to the Gorkhali conquest of Garhwal the copper mines Financial result, of the ° f NA « >Ur are Snid to ha ™ R»- 8,000 settlement of the revenue Gk. a year, or about Its. 3,800 of our derived from minerals. ™ money. Hie entire mineral revenue of Kumaon and Garhwal, including mint dues 1 on the coinage of copper pice, had fallen in 1812 to Its. 4,800 Gk., equivalent to Bs. 3,600 British currency. 1 This was mainly due to the neglect of the Gorkhali Government, under which the mines had fallen in and become choked with rubbish. Their suspicious policy prevented them from trusting their own officers, whilst their want of probity precluded any private person from venturing to sink the capital necessary to re-open the mines. In 1815 the Nagpur mines were leased for Rs. 10, and in the following year for Rs. 15, and with the villages attached to them seldom brought in more than Rs. 1,850 a year, whilst those in Kumaon were leased at Rs. 850 a year. Up to the year 1826 the revenue of the Kumaon mines was included in the assessment of pargana Ramgarh, and that of the Garhwal mines in pargana Uhanpur, and subsequently was accounted for in the returns of the pargana within which they are actually situated. Between the years 1815 and 1840 the revenue derived from mines averaged as follows : — Kumaon. Garhwal. Total. Rs. Rs. Rs. Copper ... ... 801 2,086 2,887 Iron ... 1,905 226 2,131 2,706 2,312 5,018 The highest mineral revenue of the province for any one year amounted to Rs. 5,417. This return was not altogether due to the . 1 The f e mint dues were collected for a few years under British rule at the mines of Dhanpur and Gangoli, and at one-half per cent, yielded a revenue of Rs. 300 a year. To Board, dated 6th August, 1821. OF THE NORTH-WESTERN PROVINCES. 275 smelting of ore, and included the land revenue of villages attached to the mines for the location and support of labourers. Mr. Beckett in his report 1 on the settlement of Ghirhwal gives the revenue of each mine from 1839-40 to 1863-64. The revenue every fifth year from each class of mine during this period was as follows : — Class of mine. 1839-40. 1844-45. 1849-50. 1S54-55. 1859-60. 1863-64. Total revenue from 1838-39 to 1863-64. Iron Copper ... Lead Rs. 609 1,990 Rs. 727 2,442 5 Rs. 779 2,138 S Rs. 430 1,305 3 Rs. 272 81 Rs. 134 627 10 Rs. 3,764 21,304 64 Total ... 2,599 3,174 2,920 1,738 353 771 25,132 N u m ber of mines worked, 24 25 23 17 11 30 76 In 1865 there were 24 iron, 9 copper, and 2 lead mines worked in Ghirhwal, and 33 iron, 35 copper, and 3 lead mines had been abandoned. The lead mines have since been abandoned, and the revenue from copper and iron mines in 1878-79 was as follows: — Copper. Iron. Total. Rs. a. p. Rs. a. p. Rs. a. p. 1878 ... 86 8 0 136 12 0 223 4 0 1879 ... 89 0 0 153 8 0 242 8 0 There are no statistics of outturn for these years. In his Kumaon settlement report Mr. Beckett gives the revenue of each mine from the year lb44-4o to the year 1872-/3. The revenue every fifth year from each class of mine during this period was as follows : — Class of mine. 1848-49. 1853-54. 1858-59. 1863-64. 1868-69. 1872-73. Total revenue from 1848-49 to 1872-73. Copper .. Iron Rs. 100 2,274 Rs. 48 1,751 Rs. Nil. 1,532 Rs. 120 870 Rs. 67 929 Rs. 30 1,420 Rs. 2,831 46,126 v Total 2,374 1,799 1,532 990 996 1,450 48,957 •Allahabad, 1866. 276 HIMALAYAN DISTRICTS The following quotation from the Commissioner’s report in 1874 gives the opinion of those best acquainted with the subject on the future of the mining industry in Kumaon Iron and copper abound, but at the present value of labour the mines are worth very little. The sons or miners have, as a rule, given up their old trade and taken to contracts. The great attraction to miners in former times was the cheapness of grain in the Khetsari valley, where iron was most extensively manufactured. This advantage no longer exists, for the market at Ranikhet has doubled the price of grain, and the miners would be no longer content to exchange their labour for the small profits on iron. Copper mines are in no greater favour. Formerly some villages where the miners reside were included in the mining leases of Kumaon and Garhwal. These villages have been settled with the miners, therefore they are no longer servants of the contractor. Tea gardens and other labour markets offer much better terms than a contractor, who, at the least possible expenditure, tries to make the greatest possible profit. These contractors know nothing about the science of mining, and they have no money to expend in penetrating beyond the worked- out galleries. In fact the mines have collapsed, and without consi- derable outlay no reasonable profit can be expected. Labour is expensive, and English copper can be bought at a cheaper rate in the Ahnora bazar than the local miners can produce it with profit. I expect nothing more from native petty contractors than a pittance which they can realize by the resident miners working when convenient to themselves, when they give half of the ore to the contractors and keep the other half. No doubt there is abundance of copper in Gangoli ; but any mines, copper or iron, that are now worked barely produce sufficient for local consumption. Agricul- tural instruments are made for the people of the surrounding country, and a few copper vessels ; but all the mines in the interior are m remote places, and too far removed from a good market to be of much value.” The gold exported from Kumaon is either obtained from the Gold. streams within the province, or is brought doAvn by the Bhotiya traders from Tibet. Although no mine of this metal has been discovered in the province' there are indications of its existence in Garhwal. The sands of the OF THE NORTH-WESTERN PROVINCES. 277 Alaknanda, Pindar, and Sona furnish a small amount of gold-dust. The Ganges also is auriferous as far as Lachhman Jhiila, and the Ramganga for a short distance below its junction with the Sona. The washing is nowhere a profitable occupation, and scarcely gives an average of four annas a day for each workman. The gold obtained by washing the sands of rivers paid a small duty during the Gorkliali rule, and was leased with the forest duties for a short time after the British occupation, but the amount was too tiifling to render its continuance expedient, and it was accordingly abolished by Mr. Traill. Undoubtedly a greater return might be had from this source by the use of mercury, as in Australia, for the purpose of separating the gold from the sand; for as this is afterwards recovered by a simple process of distillation, the expense would be very little more than it now is. Captain Herbert found gold in a Tibetan gold mines. matrix of granite near the Alaknanda. The gold imported from Tibet by traders is chiefly taken in exchange for grain or cloth to balance their accounts, as rupees are taken by them at the hill fairs for the same purpose. The principal gold mines in Tibet, sdr-ckaJca , are ten days’ journey beyond the borax fields further north and north-east in a district otherwise uninhabitable, named Sdr-bachydd. These are farmed or managed by a sdr-pan or gold commissioner on a triennial contract direct from Lhassa. The lessee in 1845 was also Garpan Urku-wa at Gartoh, and paid Rs. 17,000 per annum for the lease. He had 170 miners at work, for whose subsistence he used to send supplies from Pruang. It would also appear to be sometimes the custom to sublet £ claims at a tax of a sdrjao or jao of gold, about 7* mashas, or ten rupees. 1 The gold mines are worked by pits and shafts under ground, where the gold is found in its pure native state, and undergoes no other process than washing and shifting, and after that requires little or no refining. In this state, tied up in little bags called sdr-shu (H. phatang), weighing about 90 grains, it forms the heavy currency of the country. A superstitious belief holds ground that no large nugget should be removed, as it belongs to the genii ot the place, bu^ the Lama of Gnari is said to have one weighing nearly a ser. > II. Strachey, J. A. S. Ben., XVIII. (2), 5 ; J. D. Cunningham, ibid, XIII, ; Herbert to Commissioner of Kumaon, l'Jth January, 182(3. 278 HIMALAYAN DISTRICTS Gold is sold at the same fairs as the borax, and is imported to the value of about Its. 10 to 12,000 annually. The gold in the bags commonly current has usually not more Thok JaJang mines. th ™ 7 ' 73 S P edfic 8 Tavit 7- Even the F cked yellow grains have only a specific gravity of 11-96, showing that they are alloyed with some other metal. The grosser impurities appear to consist of iron more or less oxidised. One of Montgomery’s pandits visited the gold mines oi Thok Jalang in Hob toll in 186 7, 1 and describes it as a great excavation from 10 to 200 paces in width and 25 feet in depth, access to the bottom being by means of steps and slopes, the eaith dug out being thrown on either side. The dixiafino' is caiiied on with a long-handled kind of spade or an iron hoe, the iron tor which conies from Tadak. A very small stream runs through the gold field, and the bottom is consequently a quagmire during the daytime. The diggers dam up the water, leaving a sloping channel for an escape. A cloth is then spiead at the bottom of this channel, and the channel is sup- plied by one man with the auriferous earth, and another gives water, so that the gold sinks to the bottom and is caught in the cloth at the end. Some nuggets weigh up to two pounds. The diggeis come from the Tsang province round Shigatze or Digarcha. There are numbers of abandoned gold fields in different dilections about Thok Jalang, and probably a whole series of them from Rolitoh to Lhassa. The Sarpan levies a tax of about half a tola ( saishu ), or two-fifths of an ounce, from each digger. There is no wood, and water can only be had from melted ice. A cold wind blows at all seasons, and, in consequence, the tents of the dio-o- e rs are pitched, m excavations in the ground to protect them from this wind. The dried dung of yaks, ponies, and sheep afford fuel. The Tibetans cook and eat three times a day, their food consisting chiefly of boiled meat, barley cakes, buttermilk, and tea stewed with butter : they also smoke a great deal. They always sleep with their knees close up to the head and rest on the knees and elbows, huddling all the clothing on to their backs. The price of gold at Thok Jalang was about 5^ to 6 rupees per saishu , or JO rupees per ounce. 1 Rec.,G. I., H. D., 3ti. OF THE NORTH-WESTERN PROVINCES. 279 ■Silvei\ Silver was brought down to these provinces from Tibet in former times. It was imported into that country from those surrounding it (probably China), and does not seem to be found in Tibet itself in any quantity. It was sent into Tibet in a crude state in lumps called doja or thaka, of a general value of Rs. 165 each. Importations from that source have ceased for some time, owing possibly to the great and growing influx of silver in the shape of rupees from British territory. Formerly all borax, salt, &c., was bartered for grain, cloth, &c., but now, while a large amount is still disposed of in that way (probably to procure actual necessaries), still, whether it proceed from the increase of trade and the portability of coin for hoarding purposes, or from the existence of a greater demand for silver in Tibet, by far the lar crest amount of borax is disposed of here for British money. The Bhotiyas, too, state that our coin is largely current in Gartoli and the other large towns, and is preferred by the inhabitants there to the coinage of other countries. They ask for the Che - hardddr Rupaija, or face-printed money. 1 The difference in the exchange now made up in Government rupees cannot be less than' eighty thousand to one lakh of rupees per annum. This trade in rupees dates from about 1820, when they began to dis- place the Srinagari and Ladaki rupees. The mines of copper in Kumaon and Garhwal have never been of much practical value either as a source Copper mines. su pply for local consumption or as offering a valuable return to labour and capital. They are still, however, deserving of notice, and we shall now describe each in succession, commencing with the Gangoli mines m Kumaon. The Rai mine in pargana Gangoli is the most important in Kumaon. The ore is chiefly pyrites in a Rai mine. matrix of indurated and sometimes slaty talcose and steatitic schists inclosed in dolomite. In some places the one, and in some places the other, forms the roof and sides of the mine. The dolomite has a large crystalline grain and great tenacity, and forms a perfectly durable work when excavated. The schists when massive may be depended on, and can be easily worked, 1 Lawder in Rec. Geol. Sur. 280 htma'layan districts but, as a rule, they occur of such inferior consistence, having much the appearance of re-united debris, that they require support, and often occasion much inconvenience and even danger. The ore occurs in the schists in numerous strings, having every appearance of being leaders, as they are called, to solid ore, and forming a dis- tinct lode. The strike or direction of the strata is nearly W.-N.-W. to E.-S.-E., dipping at an angle of about 45° to the N.-N.-E. The copper ore is accompanied by iron pyrites which are occasionally found in the pentagonal dodecahedron form, but most commonly in such irregular and anomalous forms as can with difficulty be described. There are a few specimens of grey copper, but the work- ing ore is undoubtedly pyrites. On visiting the mine in 1836, Captain Drummond found the lode about two feet wide, containino- a good yellow copper ore, but with a large proportion of its matrix talcose, twenty per cent, only being metalliferous. The ore is extracted in the usual way by means of drifts slightly inclining upwards, to allow for drainage. The adit at Captain Drummond’s visit was driven on the course of one of the lodes which continues west about 60 feet, when it falls in with another lode that alters its direction to 15,° and afterwards to 30° north, inclining nearly 50° to the east of north. At that time the adit had penetrated some 348 feet from the entrance. The ore had been taken away from beneath as far as the miners could excavate it, and the hollow had been filled up with rubbish. From above, too, the ore was taken away as far as it was found productive. The passage varied from two to four feet in height and from two to two and a half feet in width, beino- bounded by the hard dolomitic rock which the miners did not know how to remove. In 1868-69 these mines fell in and became flooded with water. About a couple of hundred yards to the north, and in the same hill, is another similar deposit of copper. This used to be laid open to the surface during the rainy season, and was then allowed to fall in, so soon as the water employed by the miners to carry off the talcose mud from the ore ceased to be plentiful. This also has ceased to be worked for some time. In 1815 one specimen of fused copper from the Grangoli mine Ore assayed. anc ^ several specimens of the ore in matrix were sent to the Mint at Calcutta for assay. The report showed that the ore was mixed with arsenic and sulphur, OF THE NORTH-WESTERN PROVINCES. 281 and produced 25 per cent, of malleable metal, but the specimens were too small to allow of any exhaustive examination of them. 1 In 1826 Captain Herbert valued the outturn at 35 per cent, of the pure ore, and in 1836 Captain Drummond gave the general result from the pyrites in their perfectly pure state as about 30 per cent, of metallic copper. 2 Pyrites, though not a rich ore, is the most important of any, from its abundance and from being generally more to be depended on for continuance than the richer varieties. In England more copper is obtained from it than from all the other ores together. The Gangoli, Sira, and Sor mines were farmed from the conquest until 1828, when they were leased for one year to the miners, 3 and were again farmed at a reduced rent in 1833. In 1815 they yielded a revenue of Rs. 850, increased to Rs. 1,201 in 1819 and 1820, and to Rs. 1,215 in 1821 and 1822, but in 1874 the whole of the copper mines of Kumaon brought in a revenue of only Rs. 30 a year. The Sira mines in Patti Barabisi in pargana Sira are situated on the northern side of a hill somewhat Sira mines. higher than the one at Rai. The ore here O too consists of copper pyrites, accompanied by iron pyrites in a gangue formed of dolomitie and talcose rocks. In 1816, a specimen of copper ore from the Sira mine was sent to the Mint at Calcutta for assay, with the result that it was found to contain only 24 per cent, of malleable metal, so that it was thought that this mine would not repay the working. 4 Captain Drummond found that nearly thirty-three fathoms from the entrance the adit struck on a copper lode on which a level passage was driven that continued westward, its course being about 10° south of west, and the dip northeily from 45° to 50°. The ore Avas harder and more mixed with iron pyrites than the ore at Rai. At the end of the level a second lode yielding a poor ore was met, and beyond it a pit Avas sunk which seemed to have yielded in former times fair returns. The Gaul mine in Patti Kharahi and the Sor Gurang are simi- Gaul : Sor Gurang. larly situated, but the ore produced is in very small quantities, consisting of grey 1 To Government, dated 14tli June, 1815. From January, 1816. 2 See further Stat. Kum, p. 3o9 9 To Board, dated 2nd January, 1829. •'from Jauuary, 1816. Government, dated 13th : J. A. S. Ben., VII., 935. Government, dated 1 3th 36 282 HIMALAYAN DISTRICTS Bournonite. copper, copper pyrites, and carbonate of copper. Steatite and lime- stone are the neighbouring rocks, the steatite forming the gangue. The Sor mine had not been worked up to 1833, although a lease at a small rental had been taken out in 1821. 1 Captain Herbert notices that all these ores are free from the presence of arsenic, which, above all other metals, deteriorates the quality of the copper and is most difficult to remove. In digging the foundation of a house at Hawalbagh the workmen oo o o came on a vessel containing three crystallized specimens of bournonite, the triple sulplmret of copper, antimony, and lead, and the only trace hitherto dis- covered of its existence in these hills (1826). Copper pyrites also exist near Ganai and Phadiali in Patti Athgaon in pargana Gangoli ; at Bujul and Rathayat in Patti Bel in a matrix of steatite and feldspar ; and at Tamba kan in Patti Gangoli in a matrix of tal- cose rocks. There are small mines in Patti Giwar, at Chin ka Kali, Beler, Sor, and at Kemakhet, on the east bank of the Ladhiya river in Kali Kumaon. The copper mines of British Garhwal are more extensive and have always borne a higher reputation than those of Kumaon. The principal are situ- ated at Dhanpur and Dhobri in pargana Dewalgarh. These mines yielded a considerable outturn in former times, but of late years operations have not been so vigorously carried on, owing to the intricacy of the workings, and the idea prevailing among the miners that very little ore remains in the mines. The Dhanpur mine is situated on the north side of a high and ^ . precipitous range in compact dolomite. 2 The Dhanpur mine. . r ores are principally copper pyrites and grey or vitreous copper ores, with the red oxide and green carbonate in smaller quantities, the latter being scarce. The ores are found in a bed about fifty to sixty feet wide, which runs nearly north and south, and underlies east about one foot in the fathom. It is divided by a bed of potstone or indurated talc, which runs through the copper formation longitudinally, conforming to the strata and having a frith 1 To Board, dated 14th February, 1829. 2 Mr. Wilkin’s report, J A S, Ben., XII., 454 ; Iteckenclorf’s report, ibid, XIV., 471 ; Captain Herbert to Com- missioner, 10th January, 1826. Copper mines of Garhwal. OF THE NORTH-WESTERN PROVINCES. 283 or ftukan on the western side. The seams of ore are sometimes one foot in thickness, but seldom more than one inch. In his report on Dhanpur, in 1816, Mr. Traill declared that these mines were inca- pable of much improvement, and that the ore produced was not rich. The lease of the mines, including the twenty-two villages attached to supply the requisite labour and grow grain for the miners, was fixed at Ids. 1,850 a year. Up to 1829 there was little improvement, as the lessees were too poor to undertake the cleaning out of the mines, and no capitalist would venture to take them. 1 In 1838, the best seam or vein seen by Mr. Wilkin was not more than half an inch thick, and in 1841 the best lode worked was about two inches. The veins are very close together, and being softer than the matrix, the ore used to he first removed, and then the miners burned the rock with wood and threw water on it to facilitate removal. The red dolomite is of such a consistence as to seldom require props for its support, thus enabling the miners to dispense with wooden frame- work and to work all the year round, while the situation of the mine on the top of a hill admits of adits for drainage. The interior consists of a network of chambers from end to end. The Dhobri mine is situated on the south side of the Dhanpur range in very nearly the same kind ot lock Dhobri mine. as t q e Dhanpur mine, but in this mine most of the veins are horizontal, running along the side of the hill. At the surface they are very small, containing oxide of iron and green stains of copper, and occasionally copper pyrites. . The present working mine is not extended very far from the outside of the pre- cipice or surface, the ores being much the same near the surface as at a distance from it. When the miners find their passages grow- ing long and tedious they begin outside on a new vein. There are several old mines west of the Dhobri village ; one of them is very extensive, and the ores seem to have been most abundant when the horizontal vein was crossed by perpendicular ores ; but the whole of the horizontal vein has been taken away. The most western of these veins is said to have been very rich, but it fell in about the time the Gorklialis entered the province, and has not been opened since. The ores of these mines are principally copper pyrites, containing 25 pei cent, of copper. There is water for machinery about a mile and a 1 To Government, dated 14th February, 1S29, 284 HIM/LAY AN DISTRICTS half below the mine, and wood for all purposes near that place. There is another mine on this range at Maulgiri, said to be in the same rock as the Dhobri mine. There are other mines of both copper and iron in Dhanpur, but few of them are worked, and they are for the most part of little value. The mines were leased in 1872 to a European, but even then western intelligence and energy could not make them a remunerative investment. There is a copper mine in Patti Lobha at Agar Sera 1 in the face of a precipice on the right bank of the Bamganga river which was leased in 1872 for three rupees. The lessee, however, makes little profit, as the shafts have been sunk so deep that men are afraid to enter them, and the rock is too hard to allow of fresh shafts being driven, unless at great expense. The Pokhri copper mines early attracted the attention of the The Pokhri mines. Government of the country. For many years they had been worked by the Garhwal Bajas, and subsequently by the Gorkhalis. They consist of several separate mines ; that known as the Chaumattiya is situated in talc Chaumattiya mine. whlch rests 011 dolomitic limestone. The lode after crossing the ridge east of the mine enters a very compact basin, in which is situated the Duined mine. This has not been worked much, owing to the softness of the talc and the abundance of water, but it is said to have a o- 00 d lode m one part of it. The lode then crosses the hill near Deothan a small village above the mine, and is found near Giigli and I eswara, where some ores have been extracted, but have never proved very profitable in working. 3 16 Kaja s mine is sitl *ated about 450 yards north of the Chau- Raja’s mine. mattiya mine in common dolomite which rests on talcose schist. A shaft of 70 athoms was dug by the early workers meeting an adit which must have been driven over 100 fathoms through dead ground. Several other adds were driven, and when they fell together, about one f, PL y 7 S T tll6re "' ere * hree P ]aces where copper was un e Gaja Chauk, Kuvera Chauk, and Bhartwal Kua all of which have now fallen in. The produce was about 300 sers of ore " T Pei '' Tw °- t,,irds were claimed sSnt in J. T' f 454, ’ % OF THE NORTH-WESTERN PROVINCES. 285 by the Raja, and the remainder was left to the miners, who had also grants of land free of revenue. The experiments of Mr. Wilkin already noticed were confined to these two mines and a new mine which he opened close by. In the new mine the lode was very promising and yielded good specimens of ores near the surface, but at a depth of fifteen fathoms it became poor, and was consequent- ly abandoned. During the time the experiment lasted the expen- diture on the Chaumattiya mine amounted to Rs. 2,847, and the return in copper to Rs. 231, besides about three to four hundred rupees worth of ore. Rs. 347 were expended on the Raja’s mine, and the experiment was then abandoned, and the new mine cost Rs. 246 before the operations were closed. The entire net cost of the undertaking when operations ceased w r as for labour, in working the mines, less sale proceeds of copper, Rs. 2,585, and for European superintendence Rs. 4,800, or a total of Rs. 7,385. These mines were then leased to a native contractor for Rs. 500 a year. In addition to the three mines mentioned above there are several others in the vicinity of Pokhri, some of which were worked by the former rulers, and some again have never been opened. Mr. Wilkin noticed the principal mines, and described them as follows: — • The Rota mine is situated about two and a half miles north-west of the Pokhri mines in talc, which rests on dolomitic limestone. The lode is a bed of yellow or buff-coloured talc, about four feet wide, dipping north- west at 50° ; it rests immediately on the dolomite limestone, and has a sulphuric effervescence on the surface. This mine is said to have been rich ; it is situated on the western side of an extensive basin or valley, on the eastern side of which ores have been turned up by the plough, but no mine has been worked. This is an extensive field for mining, as the lode may be productive throughout the basin or valley. There is wood and water for all purposes near this mine. The Thala mine is situated about a mile north-west of the Nota mine, probably on the same lode, in an ex- Thala mine. .... . . . . . „ tensive plain or comparatively level surface. It was first worked in 1810, and again in 1825, but there being no good facility for adits, the water prevented its being worked to any considerable depth. The miners who worked it state the ores to be 286 IIIMA'LAYAN DISTRICTS copper pyrites disseminated in a lode of two feet wide, one-fifth of which was metalliferous. There is plenty of wood for all purposes in the neighbourhood of this mine. The I)anda mine is situated on the hill, about 500 yards above the Thala mine, in chlorite slate and talc, Danda mine. which on the north-western side comes in contact with common dolomite. This mine has been worked to a considerable extent, and is said to have yielded Rs. 52,000 profit in one year. The ores are of good quality, and found in three or four different beds or holes which dip into the hill at an angle of 30°. The chlorite slate in which the beds of talc and ores are found is so hard as to stand without timber ; it also contains finely disseminated copper in small quantity. The lodes run into a fine fall or basin westward, in which Mr. Wilkin thought they would be found pro- ductive. There is abundance of wood near this mine, but no water for machinery nearer than the Thala mine. The Talapungla mine is situated about a mile north-east of the Danda mine in talc, which rests on dolomitic Talapungla mme. limestone. The strata in which the ores are found is about six fathoms wide, dipping south-west at various angles. The bed is extensive, but the ores are scarce ; however, this might improve at a distance from the surface. Ores have been found in a precipice, east of this mine, near the village of Bangtal, but at present the outcrop is covered with rubbish ; it is in the tal- cose formation, and has good facilities for working. The Kharna mine is situated in the ravine below Bangtal, near its junction with the Nagal river in talc ; it was discovered by the water of the ravine washing away the strata, and leaving a quantity of ores exposed to view ; these ores were taken away by the Pokhri miners and the mine was worked five or six fathoms under the surface, beyond which they were prevented from going by the water. They say that the lode at the bottom of the mine for two fathoms in length is one foot wide, of solid copper pyrites. Of late years nothing has been done at this mine beyond washing among the surface layer, which contains a small quantity of copper pyrites. There is plenty of wood in the neighbour- hood of this mine and water for machinery, but no facility for adits. Kliarua mine. OF THE NORTH-WESTERN PROVINCES. 287 Mr. Beckett has described the mode of mining and preparing the ore of the Agar Sera 1 mine from which the following account has been extracted. The gangue consists of white and yellow quartz much encrusted with green carbonate of copper, and is so difficult to work that not more than 40 to 601b. of ore can be excavated by one man in a day. The workings are dry and the lode has a dip of about 30° below the horizon with a north-westerly direction. The ore is pounded and moistened with water and receives an admixture of five parts in six of limestone as a flux. The charge, consisting of about 61b. of unmixed ore, takes about half an hour to melt and is placed from time to time in handfuls on the furnace, and covered with oak charcoal which is occasionally moistened with water. When the fire falls in after the last supply of ore, the charge is ready to be taken out. The door of the furnace is then taken away and the remains of the fire being raked out, there appears at the bottom a melted mass which, after being stirred about a minute or two to allow the heavier particles to settle down, is sprinkled with water to harden the surface. Three or four of these charges being taken away, the melted copper is found at the bottom in a small mass weighing about 2f ounces, for which twelve pounds of charcoal have been used. Thus from every 100 parts of ore about 2 T Vths parts of copper are procured, having consumed 200 parts of charcoal or, in other words, 1371b. of charcoal are required for the production of a little over two pounds of pure copper, which sells at about one rupee a pound. The iron ores found in Kumaon all belong to either of two varie- ties, the rhomb ohedral or the prismatic. The lion mines. first is a peroxide of iron containing in its best defined type 70 per cent, of iron and 30 per cent, of oxygen. The workable ore, however, often contains earthy impurities which reduce the proportion so low as 50 per cent, of metal. This is the common species. A variety of this, known as red haematite, also occurs in many places, and frequently contains small grains of specular iron ore of a highly splendent lustre. At B.amgaih it passes into the variety known as scaly iron ore, consisting of loosely cohering glimmering particles of a steel-grey or iron-black colour, strongly soiling and feeling unctuous to the touch. Captain Heibeit i See Sel. Rec., N.-W. P., III., N.S. p. 34, and Glean, in Science, I., 230 ; As. Res. XVIII. (1), 227 (Herbert) ;_Traill and Batten, Statistics of Kumaon, Agra, 851. 288 HIMALAYAN districts Kumaon mines. considers these beds connected with those at Dhaniya Kot on the Kosi. Both yield very good iron. The prismatic species or hydrated peroxide is only known to occur in the Chaugarkha pargana. The following are the principal iron mines in Kumaon. In Patti Agar of the Ramgarh pargana, as noted, the iron is of the species known as scaly, some- what laminated in structure, slightly micaceous, and influencing the magnetic needle. The names of the principal mines are the Lusgani, Nathua Kan, Gulla and Satbunga mines, the last of which has a rich haematite. In Patti Ramgarh, also, there are several mines that are largely worked. For the first 18 years of British rule these mines were leased to the headman of the Agaris at a nominal rent, 1 which up to 1826 included all the iron mines in Kumaon. In 1833 the min- ing industry in Ramgarh received its first check in the emigration of the miners to Khetsari in Pali, and has never since recovered its early importance. In the Chaugarkha pargana, the ore of the Muniya mine in Patti Lakhanpur is of the prismatic species. It is of two varieties, the ochry and compact. The former sometimes contains octahedral crystals and magnetic iron ore, and in the neighbourhood of the mine on the summit of a small hill there occur rolled pieces consisting of grains of quartz and small octahedral crys- tals of this mineral cemented together. These pieces are magnets, and have each two poles. The ores, too, contain manganese in notable proportion, and would consequently afford a very good steel ; as it is to the alloy of this metal that the superiority of the steel manufactured from brown ore is attributed. In Patti Damn there are mines at Digarhia and Jhiratoli of the same nature ; in Rangor Patti at Jalal and Digarhia ; in Patti Kharahi at Lob. A specimen of iron ore brought from the neighbourhood of Milam, called by the natives of Malla Juhar ‘ bulclunga ,’ seems a crystalline variety of red htematite. It is used there for a red dye, the colour being extracted by rubbing the stone on a hard surface while wet. The mines of Patti Giwar in pargana Pali are found at Chiteli, Sirauli, Khetsari, Simalkhet, Gudi, Bailgaon, Bonigarh, and close by at Mehalchauri and Tilwara. The valley in which the iron is produced runs nearly north and south, and extends from Dwarahat on the south to Pandua 1 To Government, 24th December, 1833. Giwar mines. OF THE NORTTI-WESTEEN PROVINCES. 289 Khal on the north. It is formed by the rivers Kotlar and Khetsari, both flowing into the Ramganga, the bed of the former being about nine miles long, and that of the latter six miles. The ores lie on the east side of the valley and occur along a range of hills about thirteen miles in extent. The Simalkliet mine 1 is the largest, and has four entrances penetrating upwards of 350 feet into the mountain. The ores here consist of red haematite of a good quality in a gangue of clay slate branching in every direction and at all angles. The lodes range from 3' to 18' in width and 2\ f to 15' in height, the average being from 3' to 5' by 4' to 6'. There is no water, and the sur- rounding rock is compact, requiring few supports. In Sayalgarh of pargana Kotauli there is some iron ore not at present worked. At Manglalekh in Talla Rao the ore is much esteemed for its quality, and is raised in some quantity. At Dehchauri, Ramo-arh, and Khurpa Tal the mines are in the hands of the Kumaon Iron Works Company. The Lugthan mine is in Malla Katyiir, and there is another in Baraon Patti in pargana Gfangoli. The burrows at Khairna are now unworked, likewise those atSimalkha and Uchakot. Garhwal iron mines. In the Garhwal district the iron mines in Patti Painkhanda exhibit specimens of granular iron pyrites imbedded in veins of quartz which occur in a dark-greyish talcose schist. "They are apparently not very rich in ore. In Patti Sili Chandpur the Rajbunga mine gives a rich haematite which is slightly attracted by the needle, and is still worked. The Khusli mine in the same patti gives a mica- ceous ore, scaling off easily and showing minute crystals resemb- ling garnets on the edges of some specimens. The adjacent beds seem to be chloritic schists ; this ore affects the needle. In Taili Chandpur magnetic ore is found with haematite, and a specimen from Patti Taili Kaliphat resembles specular iron ore. Specimens from the Biikhanda mine in Patti Bichhla Nag- pur are also of a micaceous nature, and seem to contain in parts minute crystals of quartz and pyrites, otherwise they much resemble graphite, and soil the fingers when touched. They do not influence the com- pass needle. The Jakhtoli mine in the same patti give an ore which Nagpur mines. 290 HIMA'LAYAN districts is probably a clay ironstone. It is of a light coffee colour and of little specific gravity. The Grflet mine close by gives an ore of a similar quality. In Malla Nagpur the ore is probably haematite. A vein of iron pyrites runs along the Alaknanda in this patti near the village of Hath. The people call them ‘ sona he paihar? or gold stone, and sell them to the pilgrims to Badrinath at high rates. The stones, in the form of powder, are used as an orpiment, and the stone itself as a flint. A specimen from Nagpur itself is probably a carbonate of iron. The Mok mine in Patti Malli Dasauli yields an ore of which Dasauli and Baclihan- specimens appear to be magnetic, rich in syun ‘ metal, black in colour and crystalline, and laminated in structure. It possesses highly magnetic properties. The Charbang mine in the same locality is of a similar character, very rich in iron, and, according to Mr. Lawder, exhibits its polarity in the direction of the planes of lamination. The Dungara mine in Patti Bachhansyiin gives specimens which may possibly be an earthy hydrated oxide of iron. Its colour varies from ochry to dusky black, streak the same. It is of little specific gravity, the clay seemingly predominating. The lion of Bachhansyun, however, has a wide reputation for hardness and toughness. Sledge-hammers (gan) made from it have been found to last out those of the best English metal. The ore of Pipali mine in Patti Iriya Kot is probably a hydrous form of sesqui-oxide of iron, the clay largely predominating. The Panda Toli mine in the same patti seems to give an argillaceous variety of brown hsematite. Eohba affords a rich haematite, raised in large quantities. The Chalya mine in Patti Painun gives a hard and brittle ore possessing the iron-black colour and metallic lustre of magnetic iron, but specimens of it failed to affect the compass needle in the manner characteristic of that ore. It may possibly on analysis be found to contain manganese. The deposits of lead are fairly numerous. The ore is found at Lead. Tachhira in pargana Dhanpur mixed with a little silver. A large mine also existed at Ghirti in the snowy range between Milam and Nfti, but this has lately been closed by a landslip. The mines at Ralum and Banskum on the banks of the Gori river and at Baidli Bao-hir to Iriya Ivot. OF THE NORTH-WESTERN PROVINCES. 291 Arsenic. are unworked. The ore is galena, and the matrix is silex, with varying proportions of feldspar and calcspar. The Nagpur mine is a fair one, hut somewhat inaccessible. Near the Gaul mine in Patti Kharahi and at Sor Gurang copper mines there are depo- sits of lead ore. The former is a galena traversing a silicious limestone, but neither are regularly worked. When the villagers require lead they burn the rock, and the lead, more or less sul- phuretted, trickles from the crevices. A large nodule of lead, the size of an eigliteen-pound shot, was found in Patti Maundarsyun, on the banks of the Nayar river. It consisted of pure galena, but though search was made no more could be discovered. In Jaunsar there are mines at Maiyar and Borela on the left bank of the Tons river and at Aiyar on the right bank. At Maiyar and Aiyar the matrix is clay slate, and at Borela, limestone supposed to be a bed in the clay slate. 1 The revenue from these mines is now nominal. Yellow arsenic, known as haritdl , is found in the northern parts of Ivumaon, near Munsyari. A small portion is brought down every year by the Bhotiyas for sale at the Bageswar fair in January. Indications of lignite appear near Ranibagh close to Haldwani, the Barakheri pass near Bhamauri, and in the streams of the sub-Himalaya near Najfb- abad in the Bijnor district. They do not give promise of any workable fuel, and, judging from the experience obtained in other parts of the hills, it is questionable whether any lignite deposits will ever be discovered of such extent and quality as to repay the expense of mining them. An analysis of a specimen of the Ranibagh lignite gave carbon 60'0, volatile matter 36*4, ash 3'6. The percentage of ash, however, contrasts favourably with Bengal coal. 2 Traces of a true peat are found at Blum Tal. In 1833 Mr. E. Ravenshaw reported 3 the existence of coal in the bed of the Dhela river near Laldhang in Garhwal, "where it occurred in thin seams varying from one inch to four inches broad. Similar traces were discovered in the beds of the Chala and Phika streams, but none of any commercial value. The specimens received in Calcutta were nearly all of the same character, “ strongly impregnated with 1 Gleanings in Science, I., 230. 2 As. Res., XVI., 387, 397. 3 J A, S. Ben., 11., 264. Lignite. 292 HIMALAYAN DISTRICTS sulplraret of iron which forms their fibres, streaking some of them and passes into thick masses of pyrites, decomposing in others. A clean lump had a specific gravity of 1’968 in consequence, and the residual ash was principally iron oxide.” Graphite 1 (plumbago) crops out at the Kalimatiya hill to the north of Almora and on the spur of Banini Graphite. Devi facing Almora on the Lohughat road. In 1850, specimens were sent to England and subjected to exami- nation, when it was found that it could he made serviceable as graphite. Excavations were also made by Major Drummond at Garjoli near Balti, and Palsimi, about three miles from Balti and the same eastward of Almora. The following is the report of Mr. Rose, the mineralogist who tested the specimens sent from Almora : — “ Graphite is applied to several purposes. When very fine, compact, and of a sufficient cohesion, it is cut up for drawing-pencils. When the texture is loose, or it is otherwise of inferior quality, it is ground down and deprived of foreign substances by washing, as ores of metals are prepared for smelting. The powder thus purified is then used for various purposes, such as crucibles (being refractory or infusible by heat) for burning iron, and reducing the friction of machinery. A new method is now adopted for making artificial pencils, which are scarcely if at all inferior to those sawn out of the finest blocks. The dust of such fine material as your specimens Eos. 4, 8, and particularly No. 10, properly prepared, is subjected to vast hydraulic pressure (several hundred tons), and thus acquires the compactness and solidity necessary for the best purposes. The best kinds of graphite may be known by a pale lead-blue colour, high lustre, unctuosity, and inferior specific gravity. The first nine specimens will answer for pencils, most of them sufficiently pure and compact to be divided for that purpose. All the varieties sent may be used, even No. 13, though connected with much matrix, as it can be deprived of this by grinding and washing. All the varieties of this substance must continue in demand and bring remunerative prices if the expense of mining and conveyance should not be too great.” It is also found in Patti Loliba of Garhwal on the Karnprayag road, and is there used as a dye. 1 See, further, Gleanings in Science, III., 280 ; J. A. S , XXIV., 203 ; In. Rec. (LI. D.), XVII., 58 : Rec., N.-W. P., III., N. S., 371. OF THE NORTH-WESTERN PROVINCES. 293 Sulphur is found both in Kumaon and Garhwal. In the former district it occurs in the tract called Mun- Sulphur. sjari, and mechanically mixed with carbonate of lime in the beds of the Ramganga and Ganjiya rivers. . It is also found as green sulphate of iron, and could be obtained in any quantity from the iron pyrites of the copper mines. There are also some sulphureous springs, as those at Naini Tal, Nargoli, and Katligodam. There are two sulphur springs in Garhwal : the first lies close to the snowy range to the north-east of the temple of Madli Maheswar in pargana Nagpur ; the other is on the left bank of the Biri river, two miles above its junction with the Alaknanda. The water of this last is so very strongly impregnated that its existence can be discovered by the smell long before arriving at the spring itself. Neither are made use of any way. Sulphur is also found in the galleries of the lead mines at Maiyar on the Tons in Jaunsar. Borax or tincal, a native saline compound of boracic acid and soda. The borax and salt fields of Gnari or Borax> Hiindes, Ihd-lhaka or Ihdli-lhdka, lie to the north of Bongbwa Tal, across mountains that round the north-east side of the valley of the Shajan river, parallel to the Gangn range, and in the eastern part of the Zjang of Rolitoh (Rudukh) and at the Chapakani lake. The two salts are obtained from different spots in the same vicinity, and are both worked in the same way by lixivia- tion from the earth taken from the surface of the ground in which the salts are developed by natural efflorescence. These salt fields are open to all who choose to adventure their labour in them on payment of one-tenth of the produce to the Lhassa Government, who have an excise establishment on the spot. 1 The borax is collected from June to September and sold at the different fairs Ganpa, Gartoh, Sibilam, Chajna, Taklakliar, Dabakliar. It is brought down by the Bhotiya traders and purchased by the merchants of Ramnagar, where it is refined. The process is as follows : The borax is pounded and placed in shallow tubes, and then covered with water to the extent of a few inches ; to this is added a solution of about two pounds of lime dissolved in two parts of water, for every ten maunds (820 pounds) of borax, and the whole mass is well stirred every six hours. Next day it is drained on sieves 01 1 StracRey : J. A. S. Ben., XVII. (2), 57. 294 HIMALAYAN DISTRICTS Gypsum, cloth, and after this is again dissolved in 2\ times its weight of boiling water, and about sixteen pounds of lime added for the above quantity. It is then filtered, evaporation takes place, and subsequently it is crystallized in funnel-shaped vessels, usually of kansa , an alloy of copper and zinc or lead. The loss in weight is about 20 per cent. Borax is used in medicine and the arts. Dry borax acts on the metallic oxides at a high temperature, melting and vitrifying them into beautiful coloured glasses. It is also used as a flux for soldering in goldsmith’s work and as a varnish combined with shell-lac. Its principal use is, however, in the manufacture of coloured glass, enamel, and glazed substances. 1 Gypsum is found in pargana Chhakhata. Perhaps the best bed is near the Nihal bridge on the road between Kaladhungi and Naim Tal. In 1850 the late Mr. Tregear, of the Bareilly College, made some very good plaster of Paris from it, which might be found useful in external plastering, as it has the property of expanding on cooling. Gypsum is found in Garh- wal, on the banks of the Alaknanda near Panai and Nagrasu. There is also a dark-green variety which the people sometimes make into saucers and bowls. 2 Captain P. T. Cautley noticed 3 the occurrence of gypsum at Sansardhara and Salkot near Dehra and described its appearance and origin, which was further discussed by the Bev. R. Everest, but these papers have now little practical value. 4 A white saponaceous stone resembling and used for the same purpose as pipeclay is produced in many fooapstone. places. In Garhwal various vessels are turned from it, which when polished have the appearance of marble. They retain liquid, but being extremely brittle are little used. Asbestos has lately been discovered in a hill to the north of and at a short distance from Ukhimath in Garhwal. It is said to be of very good quality, but it is too far inland to be profitably worked. The people use it medicinally for dressing wounds and burns, and as a wick for oil-lamps, but it may yet be turned to a profitable account as a packing for steam-joints and the like. 1 Ure, 1 , 381. * As. Res., XVIII. (1), p 216. 3 J. A. S. Ben., I., 289. 4 Ibid, 450, and Skerwill on Darjiling gypsum, ibid, XXI., 538. Asbestos. OF THE NORTH-WESTERN PROVINCES. 295 Silajit 1 or Salajit, a native sulphate of alumina, is found both in Kumaon, Nepal and parganas Pain- Sllajit ‘ khanda and Nagpur in Garhwal. It is much sought after and used as a dressing for wounds. It occurs in small light lumps, colour brownish white, externally anhydrous, internally semi-crystalline, fracture slightly fibrous, with a lustre resembling asbestos, porous, containing small cavities lined with scarcely percep- tible needle-like crystals, adheres a little to the tongue. Taste acidu- lous saline, soluble in twice its weight of distilled water, friable. Mr. Stevenson’s analysis 2 gives as its component parts : sulphate of alumina, 95 ; peroxide of iron, 3 ; insoluble matter (silex), 1, and loss, 1. This analysis would appear to point to a specimen of great- er purity than those commonly met with in the bazars which, as a rule, have seldom more than 66 per cent, of sulphate of alumina. The lumps generally have an admixture of red sand and frequently portions of micaceous stone are found embedded in them. Some of them have the smooth surfaces of stalactites and are not unlike those deposits. All are readily soluble in water, and when touch- ed with the tongue give the taste of common alum. Dr. Camp- bell has described 3 the Nepalese trade in Salajit. Limestone is found all over the division, both in immense masses exhibiting various shades of colour and structure, and as local tufa deposits. There are three distinct ranges of limestone hills in Garhwal : the first north of the Alaknanda in Nagpur, the second running from Lohba Patti to the Pindar, and again to the Alaknanda in Patti Bachhansyun, and the third running parallel to the plains and south of the Nayar river. There are also small patches of limestone scattered throughout the district, but not in such large quantities as in the abovementioned ranges. Lime is manufactured at Naini Tal, at Jyuli in the Kharahi range, half-way between Bageswar and Ahnora, at Chiteli, north of Dwarahat, at Simalkha, Baitalghat, and Dhikuli for Ranikhet, and on the new cart-road to Ramnagar. Lime is also made in Borarau, Sor, Sira, Dhyanirao, and Charal. Two kinds of limestone are used in the Tarai district, the one being obtained from the quarries at the foot of the Kumaon hills, which Limestone. 1 Derived from ‘ sila, ' a stone, and ‘jit, ’ principle or essence. Ben., II. 321. 3 J. A. S., Ben., II., 482. 2 J. A. S., 29G htmXlayan districts Building stone. give by far the best kind of lime ; the other is the tufa deposit obtained in the small nalas of the tract itself ; this latter kind, how- ever, is of a very inferior quality. First-class limestone costs at the quarries five to eight rupees per 100 maunds ; the tax levied by the Forest Department is eight rupees on that amount, and cartage may be averaged at half a rupee per mile for 100 maunds. Thus the stone is landed at most points in the district for 30 rupees per 100 maunds, and including the expense of burning, a maund of lime costs 10 to 12 annas. This lime will bear two or three por- tions of pounded brick or surki. Second-class lime ready for use now costs 25 rupees, and delivered in Naini Tal, 50-100 rupees per 100 maunds ; it will, however, only bear a proportion of one part of pounded brick to two parts of lime. Good building stone can be procured in most parts of the hills. At Ahnora fine-grained, evenly-bed- ded quartzites and mica-schist form the hill itself, and supply material not to be excelled for durability and facility of dressing. Mica-schist seems to form the principal beds for some distance to the east and west of Almora, reaching to Dwa- rahat and Masi on the west, Pali, Ranikliet, Siyahi Devi, Dol, and towards Kali Kumaun to the east, and also in the formation of the Jageswar and Binsar ranges to the north. At Naini Tal the stones used are limestone and clay schist. At Ranikhet a pale-coloured gneiss forms both a handsome and a lasting building stone having the property of hardening by exposure. Sandstone is abundantly found in the lower hills. Gneiss and chlorite-schists are used fre- quently as building stones in the district. In the Bhabar split boulders are found to answer the purpose of bricks. The Tarai is the only portion of the Kumaon division where bricks are extensively used for building purposes. Nine-inch bricks cost about Rs. 750 per lakh, and the small native bricks Rs. 100. Stone is sometimes carted from the foot of the hills for the better kind of work, but owing to the great expense is, so far as possible, dispensed withr- At Chiteli near Dwarahat there are roofing-slate quarries, now ■o „ i , unworked ; also at Dhari in the Bel Patti of Roofing slate. Gangoli ; in Borarao Patti, Suit Patti, and at Naini Tal. In Lohba of Garhwal the thin dark-blue slate is procur- able, but these last appear to be much inferior to the Chiteli quarry. OF THE NORTH-WESTERN PROVINCES. 297 Alum, known as ipldtlcari , is found in different parts of the pro- vince, and in abundance in the aluminous shales near Jak village, on the road from Naim Tal to Khairna and as an efflorescence on the micaceous schist in the bed of the Kosi below Almora. The shales contain minute particles of pyrites disseminated throughout their mass, which on becoming decomposed promote the formation of alum and the lixivia- tion produced by water leaves an encrustation of alum on the rock. A dark-coloured talc called jalposhi is exported to the plains and used as a tonic and febrifuge in medicine. In the neighbourhood of Kotgaon and Giwarsiu near Paori in Garhwal a bitumen or mineral resin is found. There is no doubt but that in both quantity and quality the metalliferous deposits in this division are good, but the absence of coal and the competition of sea-borne metal have hitherto ren- dered mining an unproductive speculation, nor does there seem any probability of it attaining any important position among the industries of the province. REFERENCES. The following list gives a reference to some of the works and papers on the geology and mineralogy of the North-Western Himalaya : — 1. Report of the mineralogical survey of the Himalaya mountains lying between the rivers Satlaj and Kali : with a geological map, by Captain J. D. Herbert. J. A. S. Ben., XI., 1, p. x. 2. On the mineral productions of the Himalaya mountains, by the same. Trans. A. S., XVIII., i., 236. 3. Journal of a tour from Almora through parts of the province of Kumaon and Garhwal, chiefly in the centre of the hills, by the same, edited by J. H. Batten. J. A. S. Ben., XIII., 734. 4. Some inquiries in the province of Kumaon relative to geology and other branches of natural science, by Assistant Surgeon J. McClelland, Calcutta, 1835. 5. Geological specimens from Kumaon and Garhwal, by the same. J. A. S. Ben., II., 653. 6. Notice of some fossil impressions occurring in the transition limestone of Kumaon, by the same. Ibid, VI., 653. 7. On the geology of part of the Himalaya mountains and Tibet, by Captain R. Strachey. J. Geo. Soc., VII. (1851). 8. Geology of Dehra Di'm, by Dr. Royle. J. A. S. Ben., I., 96, 249. 9. Geological sketch of Mussooree and Landour in the Himalaya, together with an abstract of the thermometrical register kept at Landour during the year 1831, by F. H. Fisher. Ibid, I., 193. 10. Geological observations made on a journey from Mussooree to Gangotri by Rev. R. Everest. Ibid, IV., 690. 38 298 HIMALAYAN DISTRICTS OF THE N.-W. PROVINCES. 11. Ontheoriginof the Kumaon Lakes, by V. Ball. Rec. Geol. Sur., XI., 2,174. 12. Note on a trip over the Milam pass, Kumaon, by T. W. H. Hughes, with a description of the fossils by Dr. Waagen. Ibid, 182. 13. A Manual of the Geology of India, by H. B. Medlicott and W. T. Bland- ford, Calcutta, 1879. 14. Sivatherium giganteum, a new fossil ruminant genus from the valley of the Markanda in the Siwalik branch of the Sub-Himalayan mountains, by Dr. H. Falconer and Captain P. T. Cautley. As. Res., XIX., I, and J. A.JS.Ben., V., 38. VI, 152. 15. Note on the fossil hippopotamus of the Siwalik hills, by the same. As. Res., XIX., 39. 16. The fossil gharial of the Siwalik hills, by the same. Ibid, 32. 17. The fossil bear of the same, by the same. Ibid, 193. 18. The fossil crocodile of the same, by the same. Ibid, 25. 19. The fossil tiger of the same, by the same. Ibid, 135. 20. The fossil camel ©f the same, by the same, ibid, 115; and by Lieutenant W. E. Baker. J. A. S. Ben., IV., 694 : IX. 620. 21. An additional fossil species of the order quadrumana, by the same. Ibid, VI., 354. 22. Specimens of the hippopotamus and other fossil genera in the Dadupur collection by H. M. Durand, As, Res., XIX., 54, and selected specimens of the Sub- Ilimalayan fossils in the Dadupur collection, by Lieutenant W. E. Baker. J. A. S. Ben., IV. 565, and Durand, V., 291, 486, 661, 739. 23. Discovery of fossils in the Siwaliks, by Captain Cautley. Ibid, III., 592. 24. Fossil elephant's tooth from the same, by Lieutenant Baker. Ibid, 638. 25. The fossil elk of the Himalaya, by the same Ibid, IV., 506. 26. Synopsis of fossil genera and species in the collection of Dr. Falconer and Captain Cautley. Ibid, IV., 706. 27. Collections of fossils presented by Colonel Colvin. Ibid, V., 58, 179. 28. Note on the teeth of the mastodon, by Captain Cautley. Ibid, 294, 768. 29. Fossil remains of the smaller carnivora from the Sub-Himalaya, by Lieutenants Baker and Durand. Ibid, 585, 30. Notice of the skull (fragment) of a gigantic fossil batrachian from the Nahan field, by Dr. T. Cantor. Ibid, VI., 538. 31. Note on the occurrence of fossil bones in the Siwalik range eastward of Hardwar, by Dr, Ii. Falconer. Ibid, VI., 233. 32. Note on a fossil ruminant species allied to Giraffidse in the Sewalik hills, by Captain P. T. Cautley. Ibid, VII,, 658, 33. Note relating to Siwalik fauna, by H. B. Medlicott. Ibid, XXXIV., ii., 63. 34. A sketch of the history of the fossil vertebrata of India, by R. Lyddelcer. Ibid, XLIX„ ii., 8. 35. Fauna antiqua Sivalensis, by Falconer and Cautley. London, 1846-49-66. 36. Palceontological Memoirs and notes of H. Falconer, by C. Murchison. London, 1868. 37. Paloeontologia Indica, published by the Geological Survey, Calcutta. 38. Memoirs of the Geological Survey of India, by the same. 39. Records of the Geological Survey of India, by the same. CHAPTER VII. Scientific Botany. contents. A list of the flora of Garhwal. Jaunsar-Bawar and the Dehra Dun, by Dr. King. Tract to which the list refers. The Siwaliks. Sub-Siwalik tract. Dehra Dun. Himalayan tract. Characteristic vegetation from the plains to Mussooree. From Mussooree northwards. A list of the Jiom of Kumaon, and the Kumaon Bhabar, by Dr. Watson. List 1 of the Plants of Garhwal, Jauns^r-BXwar and the Dehra Dun. Tile tract of country of which the vegetation is to be considered in the following pages presents very varied conditions in respect of physical configuration, soil, and climate. Its boundaries are — on the west the river Tons, a tributary of the Jumna, and on the east Tract to which this list the Bhagirathi branch of the Ganges ; on the refers. north the snowy range of the Himalaya, and on the south the Siwalik range. The Siwaliks run parallel to the Himalaya, and are separated from the latter by the Dehra Dun, a flat valley having an elevation of from 1,800 to 2,250 feet above the level Siwbliks. 0 f the sea. The highest peaks of the Siwaliks do not rise much above 3,000 feet, and the majority are much lower, but their outline against the sky is jagged and picturesque in the extreme, and the part of them with which we have to deal is about seven miles wide. Their southern slopes are ploughed by the force of the south-western monsoon into numerous deep narrow val- leys, and the steeply scarped cliffs have a singularly bold beauty, to- tally different from anything to be seen in the outer parts of the Hima- laya behind them. On their northern aspect, the Siwaliks slope gently into the valley of the Dun, and the scenery, though beautiful, is tamer than on the southern side. The rainfall on the range during the south-west monsoon is about 60 inches, but from the porous character 1 This list has been kindly prepared by Mr. G. King, M.B., F. L. & , Director of the Royal Botanical Gardens, Calcutta, for this work. 300 HIMALAYAN DISTRICTS of the soil and the steepness of the slopes, water drains off with extra- ordinary rapidity. The drainage passes away by innumerable channels, which, except for a few days in the year, are wide wastes of dry gravel and boulders. After each heavy shower these sud- denly become filled with rushing torrents, which subside as speedily as they rose. Except during the rainy season, the range is very dry, and water is so scarce as to make it almost uninhabitable. Where the Siwaliks merge into the plains on the southern side, there are tracts of forest and grass equivalent to those covering the Bhabar and Tarai of the Himalaya in the Sub-Siwalik tract. ,, . Q . districts where there is no Srvvalik range. The vegetation "of the sub-Siwalik belts is to a great extent but a reproduction jin miniature of that of the latter. The flora of the southern face^of the Siwaliks comprises many plants of the plains, with the addition of such species as Hypericum cemuum and Cochlos- permum Gossypium. Perhaps the most striking tree found in the Siwaliks is the long-leaved pine (Pinus longifolia), a Himalayan species, for which the Siwaliks form an outlying station. A large proportion of the arboreal vegetation of the Siwaliks consists of species which occur both on the lower slopes of the Himalaya and on the hilly districts of central and southern India, thus affording a good illustration of the width of distribution of Indian plants. As examples may be mentioned Bombax malabaricum , Buchancmia Iciti- folia , Spondias mangifera , Boswellia serrcita, Garugci pinncitci , Spatho- lobus Roxburghii , Albizzia stipulcita , Anogeissus latifolia , TJlmus integrifolia, and others. Epiphytal orchids are absent, and ferns are but few in the Siwaliks. One labiate plant ( Eremostachys superba ) is confined to one or two spots in the Siwaliks, and is one of the best examples known to me in India of a truly local plant. Sal (Shorea robusta) of very stunted growth is abundant in the southern sub-Siwalik tract and on both sides of the range, as also over the whole of the Dun. This tree is here near its western limit; a little way to the west of the Jumna it disappears altogether. The Dehra Dun is a charming valley. The Siwaliks on the south shut it in from the plains, and, until recently, not only most effectually protected it from the hot winds Debra Dim. . . , , . , . , , m summer, but gave it a higher winter tem- perature than the plains outside. The extensive and ruthless OF THE NORTH-WESTERN PROVINCES. 301 clearances of the Siwalik forest of recent years are, however, believed (and apparently with good reason) to have caused an increase of the summer temperature of the Dun. The soil of the Dun consists chiefly of sandstone debris washed down from the Himalaya. The drainage is excellent, especially near the base of the Himalaya where the larger debris has been deposited, and the water level is everywhere far below the surface. The drainage water passes off by the Asan into the river Jumna, and by the Son and Suswa into the Ganges. The watershed of these streams runs across the valley in the line of the station of Dehra. The rainfall is about 80 inches, but, although only a small proportion of this total falls during any other than the rainy season, vegetation is kept wonderfully green during the whole year by the moisture prevalent in the atmosphere. Formerly the greater part of the Dun was covered by forest, of which the prevailing tree was sal , but of late years much of the forest has disappeared. A certain proportion of the cleared land has been devoted to village and some to tea cultivation, but much of it has been invaded by tall, coarse grasses useless alike to man and beast. Like the Siwaliks, the Dun is ravaged every hot season by fires from which the arboreal vegetation suffers to a degree which can only be appreciated by one who has lived in the forest. Unless these fires are checked with a high hand, the utter destruc- tion of all forest vegetation in tlfe Dun is but a question of time. The flora of the Dun presents an interesting mixture of species com- mon on the plains outside, and of plants from the lower hills. No- table amongst the latter are the pretty little Gentiana pedicellate, and in the rains, here and there, Platystemma violoicles; whilst amongst shrubs and climbing plants Lespedeza, Indig of era pulchella, Jasminum pubescens , and Combretum decandrum are perhaps the most noteworthy. The dense canebrakes of the Tarai and Blnibar of the trans-Gangetic sub-Himdlayan tract are represented in the Dun by a few patches of a single species (Calamus Royleanus ), and this is not found westward of the Nalapani swamp, three miles from the station of Dehra. Epiphytal Scitaminece are unknown m the Dun : a few orchids, however, occur, the most prominent among which are Aerides affine and odoratum , Saccolabium Ghanvalicum , and Oberonia iridifolia. Peperomia reflexa is found here and there on trees in damp spots, and there are some epiphytal ferns, such as Polypodmm Imeare. 302 HIMALAYAN DISTRICTS The remainder of the region under review consists of a large irregularly shaped tract of the Himalaya proper, narrowed at its TT „ „ , southern limit, but expanding; towards the Himalayan tract. 10 snowy range, part of which it includes. The physical features of this area are so varied that it would be out of place to attempt to describe them here. It must suffice to remind the reader that, while the lower and outer ranges have a climate not very different from that of the plains of India, the higher peaks, rising as they do to 18,000 feet above the sea-level, are covered with perpetual snow. As regards vegetation, the tract may be divided into three zones : the sub-tropical covering the slopes of the lower and outer hills, and following the courses of the deep hot val- leys far into the interior of the range ; the temperate covering the middle elevations ; and the arctic confined to the greater heights and bounded on the north by the snow line itself. The transition between these zones is gradual. In consequence mainly of its greater distance from the sea, the rainfall of the western Himalaya is much less than that of the eastern part of the chain. But not only does the climate steadily increase in dryness from east to west, but the rainfall on the outer ranges is much heavier than in the interior. At Mussooree, for example, it amounts to about 80 inches, while at Harsfl, in the northern end of the Bhagirathi valley, the rainy season is repre- sented by a short period of misty weather, and actual showers are but rare. The intervening country has a rainfall graduated be- tween these two extremes. In ascending the Himalaya from the Dun to Mussooree, new speeies meet the eye step by step. Among; Characteristic vegeta- J 1 J 1 0 tion from the plains to trees, Bauliinia return , EngelJiardtia Cole- broolziana, Rhododendron arboreum , and the Oaks are the most striking new forms. Pinus longifolia , already met with on the Siwaliks, becomes abundant. Berberries, various Bcehmerias and other Urticacece, Hanviltonia, Leptoderrms , various species of Viburnum , Clematis and Rosa at first mingle with, and finally replace, the sub-arboreal woody vegetation of the base of the hills. During the rains the change in vegetation, as one ascends, is even more striking. On steep banks and faces of rock by the road- side the eye is delighted by such charming species as Chirita bifolia , j Vidymocarpus aromaticus and macrophgllus, Platystemma violoides, OF THE NORTH-WESTERN PROVINCES. 303 Selaginella Jacquemontii, Androsace sarmentosa and incisa, Frag aria indica , Saxifraga ligulata , Argostemma sarmentosum, and Begonia picta . Ferns too abound both on the ground and on trees. A few epiphytal orchids, the Peperomia already mentioned, and Remusatia vivipara are found on the trees. But the epiphytal vegetation here is but poor and scanty when compared with that of the eastern Himalaya, thus illustrating in the most forcible way the comparative dryness of the atmosphere throughout the year. On these lower slopes a dwarf palm ( Phoenix acaulis) and a pretty little bamboo called ringed ( Arundinaria falcata) are not unfrequent ; a larger species of bamboo ( Dendrocalamus strictus), which occurs in plenty, is common also in the Dun and Siwaliks. At the level of Mussooree temperate forms begin to appear and the botanist revels in plants belonging to such familiar European genera as Ranunculus , Thalictrum, Anemone, Geranium, PotentiUa, Rubus, Rumex, Peclicularis, and Habenaria. Umbelliferous plants and Polygonacece are common, and terrestrial orchids of northern „ forms are not unfrequent during the rains. From Mussooree north- \ ° . wards. As the higher elevations are appioached, the vegetation assumes the characteristic Alpine type. Astragali, Corydalis of different species, numerous Carijophyllece, Saxifrages, Seclums, Primroses, Gentians and Farices abound, and in the carpet of rich green grass are here and there studded the magnificent Aconites, Meconopsis and Pceonia emodi. Prominent amongst the forest vegetation are the stately cedar, the rigid silver spruce and the graceful weeping pine. The twisted cypress towers aloft, and the solemn yew stretches out its sombre arms. Lichens, mosses and fungi abound, and algce are numerous in the streams. The following list of the flowering plants and ferns does not pro- fess to be complete. It contains only the names of species of which there are specimens in the Herbarium of the Calcutta Botanic Gar- den, or in my own collection. The former Herbarium ought to con- tain every species occurring within the British Empire in India. It has, however, been brought together principally by desultory private effort, and is consequently unequal and defective. As a rule, there are included in this list indigenous plants only ; the few others that occur are marked either as naturalized or introduced. Certain plants which are believed to be natives, but which are 304 HTMA'LAYATST DISTRICTS found only in cultivation, are marked as cultivated. For much assistance in revising this list I am indebted to Mr. W. Water field, C. S. Natural Order 1 . — •Ranunculacecs. Clematis Nepaulcnsis. DC. „ mon tan a. Ham. barbellata, Bdgw. grata, Wall. Gouriana, Roxb. puberula, Hf. & T. graveolens, Lindl. orientalis. L. nutans, Royle. acuminata, DC. connata, DC. Buchananiana, DC. Anemone vitifolia, Ham. obtusiloba, Don. rupestris, Wall, rivularis, Ham. polyanthes, Don. naruissiflora. L. tetrasepala, Royle. „ elongata, Don. Thalictrum elegans, Wall. ,, platycarpum, Hf. & T. cultratum, Wall. Chelidonii, Hf. & T. reniforme, Wall, pauciflorum, Royle. rostellatum, Hf. & T. Punduanum, Wall, saniculaeforme, DC. Javanicum, Bl. foliolosiim, DC. minus, L. Callianthemum cachemirianum, Camb. Adonis aestivalis, L. Ranunculus aquatilis, L. Lingua, L. pulcbellus, C. A. Mey. lobatus, Jacquem. byperboreus, Rottb. affinis, Br. liirtellus, Royle. sceleratus, L. diffusus, DC. lsetus, Wall, pensylvanicus, L. arvensis, L. Oxygraphis polypetala, Hf. & T. Caltha palustris, L. Trollius acaulis, Lindl. Isopyrum thalictroides, L. „ grandiflorum, Fisch. Nigella sativa, L. naturalized. Aquilegia vulgaris, L. Delphinium denudatum, Wall. „ coeruleum, Jacquem. elatum, L. vestitum, Wall. 99 9J 99 99 99 )) 99 99 99 9* 99 9 J •n 9? 99 99 99 99 99 99 99 99 99 99 99 99 99 99 99 99 Natural Order 1. — Banunculaeece — (concluded). Delphinium Cashmirianum, Royle. „ Ajacis, L., introduced. Aconitum Lycoctonum, L. „ palmatum, Don. „ ferox, Wall. „ Napellus, L. „ heterophyllum, Wall. Actrea spicata, L. Cimicifuga feetida, L. Pmonia emodi, Wall. Natural Order 2. — Magnoliaeeae. Michelia Champaca, L., introduced. Schizandra grandiflora, Hf. & T. „ propinqua, Hf. & T. Natural Order 3. — Anona cece. Miliusa velutina, Hf. & T. Natural Order i. — Menispermaceoe. Tinospora cordifolia, Miers. Cocculus laurifolius, DC. „ villosus, DC. Stephania elegans, Hf. & T. ,, rotunda, Lour. Cissampelos Pareira, L. Natural Order 5.- — Berber idc v . Holbecellia latifolia., Wall. Berberis nepalensis, Spreng. „ vulgaris, L. „ aristata, DC. „ Lycium, Royle. „ asiatica, Roxb. Podophyllum emodi, Wall. Natural Order 6. — NympJiceaccce. Nelumbium speciosum, Willd., intro- duced. Nymphsea Lotus, L. Natural Order 7. — Papaveraeece. Papaver somniferum, L., cultivated. „ dubium, L. Argemone mexicana, L., naturalized. Meconopsis aculeata, Royle. „ robusta, Hf. & T. „ nepalensis, DC. Stylophorum lactucoides B. & Hf. OF THE NORTH-WESTERN PROVINCES. 305 Natural Order S . — Fumariacecc. Natural Order 10. — Capparidea — (concld.) TJ JJ J J Dicentra Roylei, Hf. Sc T. „ scandens, Walp. Corydalis rutaafolia, Sibth, ,, cachemiriana, Royle. „ crithmifolia, Royle. „ elegans, Wall. ,, Govaniana, Wall, sibirica, Pers. cornuta, Royle. cliteropliylla. DC. ,, meifolia, Wall, „ flabellata, Edgw. Fumaria parviflora, Lamk. Natural Order 9.— Crucifer oe. Nasturtium officinale, P>r. „ palustre, DC. „ montanum, Wall. Barbarea vulgaris, Br. Arabis glabra, Crantz. „ alpina, L. „ amplexicaulis, Edgw. Cardamine hirsuta, L. „ impatiens, L. „ macroptiyla, Will’d. Allyssum canescens, DC. Draba alpina, L. „ incana, L. ,, lasiophylla, Royle. ,, fladnitzensis, Wulf. Sisymbrium mollissimum, C. A. Meyer, himalaicum, Hf. & T. Tlralianum, Gay & Monn. rupestre, Edgw. strictum, Hf. & T. Wallicbii, Hf. & T. Sophia, L. Columnse, Jacq. 7J Alliaria, Scop. Eutrema primulaefolium, Hf. & T. Erysimum hieraciifolium, L. „ altaicum, C. A. Meyer. ,, Thomsoni, Hf. Bi’aya rosea, Bunge. Brassica nigra, Koch. ,, eampestris, L. juncea, Hf. & T. Fruca sativa, Lamk. Capsella Bursa-pastoris, Moench. Lepidium sativum, L. „ Draba, L. ,, capitatum, Hf. & T. Megacarnsea polyandra, Benth. Tlrlaspi arvense, L. ,, alpestre, L. Iberidella Andersoni, Hf. & T. Raphanus sativus, L., cultivated. Goldhachia ltevigata, DC. Chorispora tenella, DC. Natural Order 10. — Capparidece. Cleome viscosa, L. Grjnandropsis pentaphylla, DC. 5J )> JJ if 91 Mferua arenaria, Hf. & T. Capparis spinosa, L. „ horrida, L. f. Cratmva religiosa, Forst. Natural Order 11. — Viol acres. Viola biflora, L. „ Patrinii, DC JJ 39 serpens, M r all, kunawarensis, Royle. Ionidium suffruticosum, Ging. Natural Order 12. — Bixinca. Cochlospermum Gossypium, DC. Flacourtia Ramontchi, L’Herit. „ sepiaria, Roxb. Nylosma longifolium, Clos. Natural Order 13. — Pittosporeas. Pittosporum floribundum, W. & A. „ eriocarpum, Royle. Natural Order 14. — Poly galea. Polygala triphylla, Ham. „ crotalarioides, Ham, „ abyssinica, Fresen. ,, leptalea, DC. ,, persicaritefolia, DC. „ chinensis, L. „ sibirica, L. Salomonia cantoniensis, Lour. Natural Order 15. — Caryopliylleos. Gypsophila cerastioides, Dom, Saponaria Vaccaria, L. Silene inflata, Sm. ,, conoidea, L. ,, Fatconeriana, Benth. ,, Griffithii, Boiss. „ gallica, L. ,, Moorcroftiana, Wall. „ Webbiana, Wall. „ Stracheyi, Edgw. Cucubalus bacciferus, L. Lychnis apetala, L. ,, brachypetala, Hort. Berol. ,, multicaulis, Wall, inflata, Wall. indica, Benth, var. fimbriata, Wall. nutans, Benth. „ pilosa, Edgw. Cerastium dahuricum, Fisch. ,, vulgatum, L. „ Thomsoni, Hf. Stellaria crispata, Wall. ■ )} paniculata, Edgw. „ semivestita, Edgw. JJ JJ JJ JJ 306 HIMALAYAN DISTRICTS Natural Order 15.-— Caryophylleae — (concluded). Stellaria aquatica, Scop. „ media, L. „ Webbiana, Wall. „ latifolia, Benth. » longissima, Wall. » saxatilis, Ham. „ glauca, With. „ decumbens, Edgw. Arenaria foliosa, Royle. „ festucoides, Benth. „ serpyllifola, H. „ orbiculata, Royle. » glanduligera, Edgw. j, Stracheyi, Edgw. >, holosteoides. Edgw. „ Benthami, Edgw. Sagina procumbens, L. Spergula arvensis, L., in fields. „ pentandra, L., ditto. Drymaria cordata, Willd. Roly carp tea corymbosa, Lamk. Natural Order 16. — Portulacea. Portulaca oleracea, L. Natural Order 17. — Tamariscine ee. Tamarix gallica, L. » _ dioica, Roxb. Myricaria germanica, Desv. » elegans, Royle. Natural Order 18. — Elatineoz. Natural Order 22. — Malvaceae, Malva verticillata, L. „ silvestris, L. ,, rotundifolia, L. ., parviflora, L. Sida rhombifolia, L. „ cordifolia, L. Abutilon polyandrum, Schl. „ indicum, G. Don. „ graveolens, W. & A. Urena lobata, L. „ repanda, Roxb. Hibiscus Trionum. L. ,, furcatus, Roxb. „ Solandra, L’Herit. „ ficulneus, L. >, pungens, Roxb. ,, Abelmosehus, L. „ cancellatus, Roxb. ,, esculentus, L., naturalized. Thespesia Lampas, Dalz. & Gibs. Gossypium herbaceum, L., introduced. Kydia calycina, Roxb. Bombax malabaricum, DC. Natural Order 23. — Sterculiaceae. Sterculia villosa, Roxb. „ Roxburghii, Wall. „ fulgens, Wall. Helicteres Isora, L. Pterospermum acerifolium, Willd., rare. Melochia corchorifolia, L. Waltheria americana, L. Abroma augusta, L probably intro- duced. Natural Order 24. — Tiliacece. Bergia ammannioides, Roxb. Natural Order 19. — Hypericinece. Hypericum cernuum, Roxb. „ cordifolium, Chois. » lysimachioides. Wall. !, patulum, Thunb. „ perforatum, L. „ elodeoides, Chois. „ nepaulense, Chois. Natural Order 20.' — Ternstrcemiacece. Eurya japonica, Thunb. Actinidia callosa, Lindl. Saurauja nepaulensis, DC. Camellia Thea, Link. Tea, introduced and cultivated. Natural Order 21. — Dlpterocarpece, Shorea robusta, Gaertn., Sal. Grewia oppositifolia, Roxb. „ vestita, Wall. „ tiliaefolia, Vahl. „ asiatica, L. „ sapida, Roxb. „ scabrophylla, Roxb. „ polygama, Roxb. •» laevigata, Vahl. Corchorus fascicularis, Lamk. ,, acutangulus, Lamk, Triumfetta pilosa, Roth. >> rhomboidea, Jacq. „ annua, L. Natural Order 2b.— Linear. Linum usitatissimum, L. >; mysorense, Heyne. Reinwardtia trigyna, Planch. Natural Order 26.—. Malpigldiaceat , , ITiptage Madablota, Gamin. Aspidopterys Wallichii, Hf. » nutans, Hf. OF THE NORTH-WESTERN PROVINCES. 307 Natural Order 27. — Zygophyllacm. Tribulus terrestris, L. Natural Order 28. — Geraniacea. Geranium palustre, L. „ collinum, M. Bieb. „ Wallichianum, Sweet. „ nepalense, Sweet. „ polyanthes, Bdgw, & Hf. „ rotundifolium, L. „ molle, L. ,, Robertianum, L. „ lucidum, L. „ ocellatum, Camb. Oxalis corniculata, L. ,, Acetosella, L. Biophytum sensitivum, DO. „ Reinwardtii, Walp. Impatiens Roylei, Walp. „ Thomsoni, Hf. „ sulcata, Wall. „ amplexicauiis, Edgw. ,, Balsamina, L., Mujetlii. „ "scabrida, DC. „ bicornuta, Wall. „ ampliorata, Edgw. Natural Order 29. — Rutacce e. Bse main gliausenia albiflora, Reiclib. Dictamus albus, L. Xantlioxylon alatum, Roxb. ,, oxypbyllum, Edgw. Toddalia aculeata, Pers. Skimmia Laureola, Hf. Glycosmis, pentapylla, Corr. Limonia acidissima, L. Murraya exotica, L. „ Ksenigii, Spreng. Clausena pentaphylla, DC. Citrus medica, L. „ Aurantium, L. HCgle Marmelos, Coit. Feronia Elepliantum, Corr. Natural Order BO.—Simarubca. Ailanthus excelsa, Roxb. Picrasma quassioides, Benn. Natural Order 31 —OcJinacca. Oclma pumila, Ham. Natural Order 32. — Rursoracc(E. Boswellia serrata, Roxb. Garuga pinnata, Roxb. Natural Order BB.—Meliaeea. Melia Azedarach, L., Bukain. ,, composita, Willd. Azadirachta Indica, Juss, Nim. Cedrela serrata, Royle. „ Toona, Roxb. Natural Order 31. — Olacinece. Olax nana, Wall. Natural Order 35. — llicineee. Ilex dipyrena, Wall. ,, excelsa, Wall. „ oderata, Ham. Natural Order 36. — Celastrinca. Euonymus pendulus, Wall, „ ecliinatus, Wall. ,, grandiflorus, Wall. „ Hamiltonianus, Wall. „ lacerus, Ham. „ tingens, Wall. Celastrus paniculata, Willd., Malkagni. Gymnosporia rufa, Wall. montana, Roxb. „ Royleana, Wall. Elaeodendron glaucum, Pers. Natural Order 37. — Rliamnece. Ventilago calyculata, Tulasne. Zyzyplius Jujuba, Lamk. „ (Enoplia, Mill. „ vulgaris, Lamk. „ xylopyra, Willd. „ nummularia, W. & A. ,, oxyphylla, Edgw. Berchemia floribunda, Wall. Rbamnus purpureus, Edgw. ,, procumbens, Edgw. „ virgatus, Roxb . „ triqueter, Wall. Sageretia oppositifolia Brongn. „ theezans, Brongn. Scutia indica, Brong. Gonania leptostaebya, DC, „ nepalensis, Wall. Plovenia dulcis, Thunb. Natural Order 38. — Aj»ipclidc . Vitis capreolata, Don. „ latifollia, Roxb. „ vinifera L., introduced. ,, Linnsei, Wall. ,, adnata, Wall. „ lanata, Roxb. himalayana, Brand. „ parvifolia, Roxb. J} obtecta, Wall. „ divaricata, Wall. Leea sambucina, Willd. „ robusta, Roxb. „ alata, Edgw. „ aspera, Wall. Natural Order W.—Sapindacea. iEsculus indica, Colebr. Sclileichera trijuga, Willd. Sapindus trifoliatus, L. „ Mukorossi, Gasrtn., probably introduced. 308 himXlayan districts Natural Order 39. — Sapindacece — (concluded). feapindus Danura, Voigt., probably introduced. Acer oblongum, Wall, i, caesium, Wall. „ laevigatum, Wall. t, pictum, Thunb. „ villosum, Wall. » _ caudatum, Wall. Melianthus major., L., introduced. Staphylea Emodi, Wall. Natural Order 10.' — Sabiacecc. Sabi a paniculate, Edgw. „ campanulata, Wall. Meliosma simplicifolia, BI. », dilleniarfolia, Bl. Natural Order 41.* — Anacardiacece. Rhus- vemicifera, DC". „ acuminata, DC. „ semialata, DC. „ Cotinus, L. „ succedanea, L. „ parviflora, Roxb. Spondias Mangifera, Pern. Mangifera indica, L. Ruchanania latifolia, Roxb. Odin a Wodier, Roxb. Semecarpus Anacardduna, L. Natural Order 42. — • Coriariea Coriaria nepalcnsis, Wall. Natural Order 43. — -Moving ea. Moringa pterygosperma, Gaertn. Natural Order 44. — Leguminosce. Piptanthus nepalensis, Don. Thermopsis barbata, Royle. Crotalaria prostrata, Roxb. „ alata, Roxb. „ sericea, Retz. „ juncea, L. ,, tretragona, Roxb. „ albida, Heyne. „ neglecta, W. & A. Argyrlobium flaccidum, J. et S. „ roseum, J. et S. Parochetus communis. Ham. Trigonella Fcenum-Graecum, L. „ gracilis, Benth. Medicago lupulina, L. „ laciniata, All. „ satiya, L., cultivated. Melilotus parviflora, Desf. ,, alba, Lamk. „ officinalis, L. Natural Order 44 . — Legum inosi (continued). Trifolium repens, L. „ pratense, L. Lotus corniculatus, L. Indigofera linifolia, Retz. trifoliata, L. >>• trita, L-, » >» jj- »> )) tinctoria, L. pulchella, Roxb. Dosua, Ham. „ atropurpurea, Plam, ,, hirsuta, L. „ Girardiana, Wall. „ heterantha, Wall. Teplirosia purpurea, Pers. ,, tenuis, Wall. Millettia auriculata, Baker. Caragana brevispina, Royle. Colutea nepalensis, Sims. Astragalus graveolens, Ham. ,, tricbocarpus, Grab. „ adesmiaefolius, Benth. „ Ieucocephalus, Grah. hosackioid.es, Bentb. rbizanthus, Royle. Webbianus, Grah. ,, multiceps, Wall. Oxytropis micropbylla, DC. iEscbynomene indica, L. Smitbia sensitiva, Ait. „ ciliata, Royle. Zornia diphylla, Pers. Ougeinia dalbergioides, Bentb. Desmodium oxyphyllum, DC. „ gangeticum, DC. ,, laxiflorum, DC. „ gyrans, DC. „ podocarpum, DC. ,, tilisefolium, Don. » floribundum, G. Don. ,i concinnum, DC. ,, polycarpum, DC. » parvifolium, DC. ,, triflorum, DC. Uraria picta, Desv. ,, lagopus, DC. „ lagopodoides. DC. Alysicarpus vaginalis, DC. ,, bupleurifolius, DC. Lespedeza elegans, Camb. „ sericea, Miq. » eriocarpa, DC. _ )> juneea, Pers. Vicia sativa, L. „ rigidula, Royle. i) hirsuta, Koch. „ tenara, Grah. „ tenuifolia, Roth. „ tetrasperma, Mcencb. Lens esculenta, Mcencb, cultivated Lathyrus sativus, L. lute us, Bak. Apbaca, L. OF THE NORTH-WESTERN PROVINCES. 309 Natural Order ii.—Leguminosa—(concld.) Natural Order io. Rosacea (concld.) > cultivated. Pisum sativum, L., introduced. Abrus precatorius, L. Clitoria Ternatea, L. Dumasia villosa, DC. Shuteria involucrata, W. Sc A. Glycine Soja, S. et Z. Erythrina arborescens, Roxb. „ resupinata, Roxb. ,, suberosa, Roxb. Mucuna pruriens, DC. „ atropurpurea, DC. Butea frondosa, Roxb. Spatholobus Roxburghii, Benth. Pueraria tuberosa, DC. Phaseolus Mungo, L. 1 „ aconitifolius, Jacq. r Vigna Catjang, End. / Dolichos Lablab, L. V Cajanus indicus, L. / Atylosia scarabseoides, Benth. „ mollis, Benth. Rhynchosia minima, DC. „ Falconeri, Baker. Flemingia semialata, Roxb. „ strobilifera, R. Br. „ vestita, Benth. Dalbergia Sissoo, Roxb. „ lanceolaria, L. ,, hircina, Benth. „ volubilis, Roxb. Pongamia glabra, Vent. Sophora mollis, Wall. Caesalpinia Bonducella, Flemm. „ sepiaria, Roxb. Cassia Fistuta, L. „ Tora, L. occidentalis, L. Absus, L. pumila, Lamk. „ Wallichiana, DC. Bauhinia racemosa, Lamk. „ variegata, L. ,, retusa, Roxb. „ Vahlii, W. & A. „ purpurea, L. Mimosa rubicaulis, Lamk. „ pudica, L. Sensitive plant, na turlized. Acacia Catechu, Willd. „ pennata, Willd. „ cassia, W. and A. ,, Farnesiana, Willd, naturalized. ,, eburnea, Willd. Albizzia lucida, Benth. „ Lebbek, Benth. odoratissima, Benth. procera, Benth. Julibrissin, Boiv. stipulata, Boiv. » >> >■ •i i) >> Natural Order 45. — Rosacea. Prunus Puddum, Roxb. „ Padus, L. Prunus domestica, L. Alucha, Plum, in- troduced. „ armeniaca L., Zard Alu, Apricot, cultivated. Amygdalus persica, L., Aru, Peach, in- troduced. Prinsepia utilis, Royle. Spiraea canescens, Don. „ callosa, Thunb. „ Kamtschatica, Pall. ? „ sorbifolia, L. „ Aruncus, L. Rubus acuminatus, Sm. „ paniculatus, Sm. „ parvifolius, L. „ concolor, Wall. „ niveus, Wall. „ fruticosus, L. ,, flavus, Ham. „ lasiocarpus, Sm. „ rosaefolius, Sm. „ biflorus, Ham. „ asper, Don. Geum elatum, Wall. Fragaria indica, Andr. „ vesca, L. Agrimonia Eupatorium, Linn. Potentilla fruticosa, L. „ micropliylla, Don. „ multifolia, L. „ Leschenaultiana, Sm. „ fulgens, Wall. „ nepalensis, Hook. „ atrosanguinea, Lodd. „ supina, L. „ (Sibbaldia) procumbens, L. Rosa Lyellii, Lindl. „ moschata, Mill. „ Brunonii, Lind. „ macrophylla, Lind. „ Webbiana, Wall. „ sericea, Lind. Pyrus Aria, Ehrli. „ baccata, L., Gwala Mehal. „ variolosa, Wall, Mehal. „ communis, L., Nashpati, Pear, cultivated. „ Malus L., Seo, Apple, cultivated. ,, ursina, Wall. ,, foliolosa, Wall. „ Cydonia, L., introduced. Cratsegus Pyracantlia, Pers. Cotoneaster acuminata, Lindl. „ microphylla, Wall. „ bacillaris, Wall. „ nummularia, F. et M. Natural Order 46. — Saxifragca. Astilbe rivularis, Don. Saxifraga ligulata, Wall. „ Stracheyi, Hf. & T. „ imbricata, Royle. 310 HIMALAYAN districts Natural Order 4G. — Saxifragcce — (concld.) Saxifraga ramulosa, Wall. „ granulata, L. » odontophylla, Willd. jj micrantha, Edgw. „ pallida, Wall. » flagellaris, Willd. „ Bruuonis, Wall. •> filicaulis, Wall. , t brachypoda, Don. » diversifolia, Wall. » Jacquemontiana, Dene. Chrysosplen ium nepalense, Dene. Parnassia Wightiana, Wall. „ nubicola, Wall. Hydrangea altissima. Wall. Deutzia corymbosa, R. Br. ,, staminea, R. Br. Philadelphia coronarius, L. Itea nutans, Royle. Ribes Grossularia, L. „ glaciate, Wall. „ rubrum, L. » nigrum, L. Natural Order -17. — Crassulaccce. Tillaea pentrandra, Royle. Crassula indica, Dene. Bryophyllum, calycinum Salisb., in gar- dens. Kalanchoe varians, Haw. Cotyledon Oreades, Benth. et Hf. Sedum crenulatum, hi t'. & t. „ quadrifidum, Pall. „ Himalense, Don. » crassipes, Wall. a elongatum, Wall. 33 linearifolium, Royle. 33 pauciflorum, Edgw. „ trifidum, Wall. ,, rosulatum, Edgw. 33 adenotrichum, Wall. „ Ewersii, Ledeb. ii multicaule. Wall. 33 Rhodiola, DC. Natural Order 48. — Droseracece. Drosera peltata Var. lunata, Ham. Natural Order 49. — Ilaloragaccce, Myriophyllum spicatum, L. Natural Order 50. — Cumbretaccce. Natural Order 51. — Myracece, Eugenia Jambolana, Larnk , Jaman. ,, caryophylli folia, Lamk. Careya arborea, Roxb. Barringtonia acutangula, Gasrtn. Natural Order 52. — Melastomacece. Osbeckia stellata, Don. angustifolia, Don. Natural Order 53.— Lythracicce . Ammannia rotundifolia, Ham. „ vesicatoria, Roxb. Woodfordia floribunda, Salisb. Lawsonia alba Lamk., Mehndi, gardens. Lagerstrcemia parviflora, Roxb. Punica Granatum, It., wild and cultivat- ed. Natural Order 54. — Onagraciece. Epilobium tomentosum, Boiss. „ roseum, L. CEnothera rosea, Sims., 1 „ sinuata, L., i naturalized , „ grandiflora, ) Cireasa Lutetiana, L. „ alpina, L. Natural Order 55. — Sarny dacccs. Casearia tomentosa, Roxb. Natural Order 56.— Cucurbitavccs. Trichosanthes cucumerina, I. „ palmata, Roxb. Luffa cylindrica, Eaud. Cucumis Melo. L., cultivated. „ sativus, L. „ Hardwickii, Royle. Citrullus vulgaris, Schrd. Bryonia laciniosa, L. Mukia scabrelia, Arn. Zehneria umbellata, Thw. Natural Order 57. — Begoniaceos. Begonia pi eta. Wall, i, amcena, Wall. Natural Order 58. — Datiscaccce. Datisca cannabina, L. Terminalia belerica, Roxb. Baharia. „ Chebula, Retz . Har. 33 citrina, Roxb. Harira. ii Arjuna, Bedd., Arjan. ,, tomentosa, Roxb. Saj. Anogeissus latifolia, Wall. Combretum decandrum, Roxb. Natural Order 59. — Ficoidece, xuciuiucma penianara, L. . crystallina, Yahl. Mollugo hirta, Thunb. 33 pentaphylla, L. » cerviana, Ser. OF THE NORTH-WESTERN PROVINCES. 311 Natural Order 60. — Umbelliferce. Hydrocotylc asiatica, L. Sanicula europsea, L. Bupleurum tenue, Flam. „ longicaule, Wall. „ Candollei, Wall. „ falcatum, L. „ marginatum, Wall. Apium graveolens, L., introduced. Carum Copticum, Benth. et Hi. Ajwain, cultivated. Acronema tenerum, Edgw. Pimpinella diversifolia, DC. Chferopliyllum villosum, Wall. CEnanthe stolonifera, Wall. Selinum Candollei, Bth. et Hf, „ Brunonis, DC. „ Govanianum, DC. ,, angelicoide, DC. Heracleum candicans, Wall. „ nepalense, Don. Peucedanum graveolens, L. Sawa. Coriandrum sativum, L., cultivated. Daucus Carota, L., cultivated. Torilis Anthriscus, Gmel. Natural Order 61 — Araliacece. Aralia cacliemirica, Dene. Heteropanax fragrans, Seem. Hedera Helix, L. Heptapleurum venulosum, Seem. Natural Order 62— Cornaceoe. Marlea begonitefolia, Roxb. Cornus macrophylla, Wall. „ oblonga, Wall. ,, capitata, Wall. Alangium Lamarckii, Thw. Natural Order 63. — Cap rifoliacece. Abelia triflora, R. Br. Leycesteria formosa, Wall. Lonicera Myrtillus, Hf. & T. „ parvifolia, Edgw. „ purpurescens, Hf. & T. „ hypoleuca, Dene. „ orientalis, Lamk. „ alpigena, L, „ heteropliylla, Dene. „ angustifolia, Wall. „ spinma, Jacquem. „ quinquel ocularis, Hardw. Viburnum cotinifolium, Don. ,, stellulatum, Wall. „ integerrimum, Wall, ,, nervosum, Don. ,, coriaceum, Bl. Natural Order 64. — JRubiacece. Adina cordifolia, Benth. et Hf. Stephegyne parvifolia, Benth. et Hf. Hymenodictyon excelsum, Wall. Natural Order 64. — JRubiacece— (concld. Wendlandia exserta, DC. „ puberula, DC. Argostemma sarmentosum, Wall. ,, verticillatum, Wall. Hedyotis Burmanniana, R. Br. „ aspera, Heyne. „ brachypoda, DC. „ gracilis, Wall. Randia dumetorum, Lamk. „ tetrasperma, Roxb. ,, uliginosa, DC. Knoxia corymbosa, L. Pavetta tomentosa, Sm. Gardenia turgida, Roxb. Coffera bengalensis, Roxb. Hamiltonia suaveolens, Roxb. Leptodormis lanceolata, Wall. Spermacoce articularis, L. Galium asperifolium, Wall. „ acutum, Edgw. „ rotundifolium, L. „ sepylloides, Royle. „ confertum, Royle. „ aparine, L. Rubia cordifolia, L. Asperula cynanchica, L. Natural Order 65. — Valerianae ecu. Valeriana Wallichii, DC. „ Hardwickii, Wall. Natural Order 66 — Dipsacece. Morina longifolia, Wall. ,, breviflora, Edgw. Dipsacus inermis, Wall. Natural Order 67.— Composite . Vemonia anthelmintica, Willd. ,, cinerea, Less. Elephantopus scaber, L. Adenostemma viscosum, Forst. n var. elatum, Don. !> var. latifolium, Don. Eupatorium longicaule, Wall. „ Wallichii, DC. Solidago Virga-aurea, L. Cyathocline lyrata, Cass. Dichrocephala gracilis, DC. Grangea madraspatana, Poir. Myriactis nepalensis, Less. „ Wallichii, Less. Aster alpinus, L. „ molliusculus, Benth. ., junceus, Benth. „ Thomsoni, C. B. Clarke. ( = Calimeris fiexuosa, Royle.) „ peduncularis, Wall. Erigeron acre, L. ,, bellidoides, Benth. Conyza veronitefolla, Wall. 312 HIMALAYAN DISTRICTS Natural Order 67 . — Composites (contd.) Conyza absinthifolia, DC. „ viscidula, Wall. Bhmiea lacera, DC. ,, runcinata, DC. „ bieracifolia, DC. Sphaeranthus hirtus, Willd. Leontopodium alpinum, Cass. Anapbalis cinnamonea, Bentli. ,, triplinervis, Sims. „ nubigena, DC. „ nubigena, var. polycepbala, C. B. Clarke. „ chionantba, DC. „ araneosa, DC. Gnapbalium multiceps, Wall. „ indicum, L. Csesulia axillaris, Roxb. Inula vestita, Wall. „ nervosa, Wall. „ barbata, Wall. „ Cappa, DC. Carpesium cernuum, L. „ abrotanoides, L. Siegesbeckia orientals, L. Eclipta erecta, L. Bidens tripartita, L. Allardia tridactylites, Ilf. & T. Cotula anthemoides, L. Tanacetum tliibeticum, Hf. & T. „ longifolium, Wall. Artemisia vestita, Wall. „ vulgaris, L. Senecio deniflorus, Wall. „ graciliflorus, DC. „ laciniosus, Wall. „ coronopifolius, Desf. „ alatus, Wall. „ rufinervis, DC. „ Kunthianus, Wall. ,, Candolleanus, Wall. Ecliinops niveus, Wall. „ echinatus, Roxb. Arctium Lappa, Willd. Saussurea obvallata, Wall. „ taraxacifolia, Wall. „ Kunthiana, Wall. „ depressa, Wall. „ graminifolia, Wall. „ Candolleana, Wall. „ carthamoides, Bentli, „ albescens, Hf. & T, „ candicans, DC. „ Roylei, DC. Jurinea macrocephala, Bentli. Serratula pallida, DC. Tricholepis elongata, DC. Leucomeris spectabilis, DC. Aiuslhea pteropoda, DC. „ aptera, DC. Gerbera lanuginosa, Bentli. et Hf. Berniera nepalensis, DC. Tragopogon junceum, Wall. Youngia lyrata, Cass. Natural Order 67. — Composites — (concluded). Lactuca graciliflora, Wall. „ Brunouiana, Wall. „ hastata, DC. „ macrantha, Bentli. et Hf. „ longifolia, DC. „ auriculata, DC. „ sagittata. Hf. & T. ,, Tatarica, Bentli. Prenantlies hispidula, DC. Taraxacum Dens-leonis, Desf. Crepis foetida, L. Mulgedium Tataricum, DC. Microrliynchus sarmentosus, DC. Gynura nepalensis, DC. Emilia soncliifolia, DC. Doronicum Roylei, DC. Natural Order 68. — Camjjanulacea. Cyanantlius integer, Wall. „ linifolius, Wall. Waldenbergia agrestis, A. DC. Campanula latifolia, L. „ sylvatica, Wall. ,, canescens, Wall. „ colorata, Wall. Lobelia trigona, Roxb. „ pyramidalis, Wall. Natural Order 69. — Ericaccm. rernettya repens, Zoll. Andromeda ovalifolia, Wall. Rhododendron barbatum, Wall. „ campanulatum, Don. ,, arboreum, Sm. „ lepidotum, Wall. „ anthopogon, Don. Cassiope fastigiata, Don. Natural Order 70. — Primulaceas. Primula floribunda, Wall. petiolaris, Wall, purpurea, Royle. rosea, Royle. minutissima, Wall. » involucrata, Wall. 55 sibirica, Jacq. 55 denticulata, Wall. AndooSace sarmentosa, Wall. ,, Jacquemontii, Duby. „ rotundifolia, Hardw. „ incisa, Wall. „ elegans, Duby. Lysimachia lobelioides, Wall. „ pyramidalis, Wall. „ evalvis, Wall. „ japonica, Thumb. Anagallis arvensis, L. Micropyxis pumila, Duby. Samolus Valerandi, L. OF THE NORTII-WESTERN PROVINCES. 313 Natural Order 71.- Myrsinea. Mresa indica, A. DC. „ argeutea, Wall. JEmbelia robusta, Roxb. Myrsine semiserrata, Wall, „ bifaria, Wall. Ardisia humilis, Vahl. „ iloribunda, Wall. Natural Order 72. — Sapotacca. Bassia butyracea, Roxb. „ latifolia, Roxb , at lorn eleva- tions : planted. Natural Order 1$.— Menace*. Diospvros exsculpta, Ham. „ " Melanoxylon, Roxb. „ montana, Roxb. r/t Embryopteris. Pers. Natural Order li.—Styraeecz. Symplocos cratasgoides, Ham. „ spicata, Roxb. „ racemosa, Roxb. „ ramosissima, Wall. Natural Order 75. — Jasminea. Jasminum laurifolium, Roxb. „ pubescens, Willd. punetatum, Wall, arboreseens. Roxb. „ latifolium, Roxb. „ dispermum, Wall. „ revolutum, Sims. „ pubigerum, Don. officinale, L. ,, grandifiorum, L. „ Zarnbac, Ait., cultivated. Nyctanthes Arbor-tristis, L. Natural Order l&.—Oleace*. Fraxinus floribunda, Wall. Ligustrum nepalense, W all. „ compactum, Hf. & T. Olea cuspidata, Wall. „ glandulif era , Wall. Cliionanthus macro phylla, Wall. Syringa emodi, Wall. Natural Order 77. — Apocyne a>. Clarissa diffusa, Roxb. Opbioxylon serpentinum, Willd. Tabernsemontana coronaria, R. Br. Vinca pusilla, Murr. Vallaris dicbotoma, Wall. Natural Order 77.— Apocynece— (concld). Wrightia mollissima, Wall. Holarrhena antidysenterica, Wall. Alstonia scbolaris, R. Br. Nerium odorum, Solander. Cbonemorplia macrophylla, G. Don. Ichnocarpus fragrans, Wall. „ frutescene, R. Br. Natural Order 7 8 . — Asclepiadaceas. Cryptolepis elegans, Wall. Vincetoxicum canescens, Dene. „ montanum, Dene. Calotropis procera, R. Br. Dmmia extensa, R. Br. •Periploca calopliylla, Falc, Tyloplrora carnosa, WalL Marsdenia Roylei, Wight. Pergularia -odoratissima, L. Orthanthera viminea, Wight. Hoya parasitica, Wall. Ceropegia longifolia, Wall. ,, lanceolata, Wight. Natural Order 79. — Loyaniaaecs, Gardneria angustifolia, Wall, Buddleia paniculata, Wall. „ asiatica, Lour, Natural Order 80. — Gemtianacex. Exacum tetragonum, Roxb. „ pedunculatum, L. Canscora decussata, R. et S. „ diffusa, R. Br. Gentiana tenella, Fries. „ pedicellata, Wall. „ argentea, Royle. t) capitata, Ham. „ decemfida, Ham. ,, marginata, Griseb. )f venusta, Wall. „ depressa, Don. „ Kurroo, Royle. Crawfurdia fasciculata, Wall. Ophelia cordata, Don. „ lurida, Don. purpurascens. Don. „ nervosa, Wall. „ pulchella, Don. angustifolia, Don. ,, Chirayta, Griseb. Halenia elliptica, Don. Swertia speciosa, Wall. Natural Order 81,—Bignoniacea, Calosanthes indica, Bl. Stereospermum chelonoides, DC. suaveolens, DC. 40 314 HIMALAYAN DISTRICTS Natural Order 82. — Pedaliacece. Martyniaproboscidia, Glox, naturalized. Sesamum indicum, L., Till, cultivated. Natural Order 83. — Convolvulacect. Argyreia speciosa, Sweet. „ capitata, Choisy. „ setosa, Choisy. Quamoclit coccinea, Mcench, | » vulgaris, Choisy, Patatas pentaphylla, Choisy. Pharbitis Nil, Choisy. Calonyction speciosum, Choisy. Ipomoea Pes-tigridis, L. „ Turpethum, R. Br. „ vitifolia, Sweet. „ pilosa, Sweet. ,, sessilillora, Choisy. Convolvulus pluricaulis, Vahl. Porana paniculata, Roxb. ,, racemosa, Roxb. E volvulus alsinoides, L. Cuscuta reflexa, Roxb. Natural Order 84. — Boraginacece. Gynaion vestitum, A. DC. Cordia Rothii, R. et S. „ Myxa, L. „ latifolia. Roxb. Ehretia laevis, Roxb. „ serrata, Roxb. Rhabdia viminea, Dalz. Heliotropium ovalifolium, Vahl. „ strigosum, Willd. Macrotomia Benthami, DC. Mertensia echioides, Hf. and T. Mvosotis caespitosa, Schult. ,, rotundifolia, R. Br. Eritriehium rotundifolium, DC. ,, sericeum, Rojde. „ spathulatum Royle. Echinospormum glochidiatum, DC. Cynoglossum furcatum, Wall. ,, micranthum, DC. „ longiflorum, Benth. ,, grandiflorum, Royle. Trichodesma indicum, R. Br. Natural Order 85. — Salanace at . Solanum tuberosum, L., Potato, intro- duced. Solanum nigrum, L. „ verbascifolum, L. „ sanctum, L. ,, xanthocarpum, Schr. „ indicum, L. Pbysalis minima, L. Natural Order 85. — Solanaceaz. — (conehL) Physalis Peruviana, L., introduced and almost naturalized. Capsicum frutescens, L., LAl-mireli, Chilli, introduced and naturalized. Nicandra physaloides, Gasrtn, natur- alized. Withania somnifera, Don. Nicotiana Tabacum, L., Tamaku, intro- duced and naturalized . Datura Stramonium, L. „ fastuosa, L. Natural Order 86. — Scrop hula riaoecs. Verbascum Thapsus, L. Celsia coromandeliana, L. Linaria ramosissima, Wall. Antirrhinum Orontium, L. Mimulus nepalensis, Wall. „ gracilis R. Br. Mazus surculosus, Don. „ rugosus, Lour. Lindenbergia grandiflora, Benth. f, urticmfolia, Lehm. » macrostachya, Benth. Limnophila gratioloides, R. Br. Herpestis Hamiltoniana, Benth. „ Monnieria, H. B. K. Torenia cordifolia, Roxb. Vandellia Crustacea, Benth. Bonnaya brachiata, Link. „ veronicasfolia, Spr. Hemiphragma heterophyllum, Wall. Scoparia dulcis, L., naturalized. Veronica Anagallis, L. „ Beccabunga, L. „ deltigera, Wall. „ lanosa, Benth. „ alpina, L. „ biloba, L. „ agrestis, L. Buchnera hispida, Lamk. Striga euphrasioides, Benth. „ densiflora, Benth. „ hirsuta, Benth. Leptorhabdos parviflora, Benth. Sopubia trifida, Don. Euphrasia officinalis, L. Picrorhiza Kurrooa, Royle. Pedicularis tubiflora, Fiscli. „ carnosa, Wall. „ pectinata, Wall. „ pyramidata, Royle. „ gracilis, wall. „ porrecta, Wall. „ abrotanifolia, Bieh. „ megalantha, Don. Natural Order 87.— Lentibulariee, Utricularia flexuosa, Vahl. OE THE NORTH-WESTERN PROVINCES 315 y> » » Natural Order 88. — Orobanchece. Phelipsea indica, G. Don. JSginetia indica, Roxb, Natural Order 89. — 6fes>ieraceoe. Didymocarpus snbalternans, Wall. atomaticus, Wall, macrophyllus, Wall, pedicellatus, R. Br. ,, lanuginosus, Wall. Chirita bifolia, Don. Rhynchoglossum obliquum. Bl. Platystemma violoides, Wall. Lysionotus fernifolius, Wall. Natural Order 90- — Acanthacece. Thunbergia grandiflora, Roxb. „ coccinea, Wall. Ebermaiera glauca, N. ab. E. Hygrophila polysperma, T. Anders. „ spinosa, T. Anders. Petalidium barlerioides, N. ab E. HemigraphiS’ Pavala, T. Anders. Strobilanthes auriculatus, N. ab E. „ glutinosus, T. Anders. alatus, N. ab E. „ Wallichii, N. ab E. „ isophyllus, T. Anders. „ anisophyllus, T. Anders. Jiehmanthera Wallichii, N. ab E. Dfedalacanthus nervosus, T. Anders. Barleria cristata, L. Lepidagathis cuspidata, N. ab E. )t purpuricaulis, N. ab E. t> hyalina, N. ab E. fasciculata, N. ab E. Phlogacanthus tliyrsiflorus, N. ab E. Justicia Adhatoda, L. „ peploides, T. Anders, ,, procumbens, L. Ruugia pectinata, N. ab E. ., repens, N. ab E. Dicliptera Roxburghiana, N. ab E. Peristrophe bicalyculata, N. ab E. speciosa,N. ab E. Natural Order 91. — Verhenacer. Verbena officinalis, L. Lippia nodiflora. Rich. Lantana alba, Mill. Premna viburnoides, Wall. „ mucronata, Roxb. „ barbata, Wall. ,, herbacea, Roxb. Caliicarpa arborea, Roxb. ,, macrophylla, Vahl. Clerodendron serratum, Spr. „ infortunatum, L. ,, Siphonanthus, R. Br. Natural Order 91.- — Verbenaccae. • — (concluded). Caryopteris Wallichiana, Schauer. Gmelina arborea, Roxb. Vitex Negundo, L. Hclmskioldia sanguinea, Retz. Natural Order 92. — Labiatt e. Ocimum canum, L. „ sanctum, L, naturalized. Orthosiphon rubicundus, Benth. Plectranthus scroj^hularioides. Wall. ,, striatus, Benth. „ Coetsa, Don. „ ternifolius, Don. ,, cordifolius, Don. Coleus barbatus, Benth. Pogostemon plectranthoides, Desf. Dysophylla cruciata, Benth. „ purnila, Benth. Colebrookia oppositifolia, Sm. Elsholtzia polystachya, Benth. „ flava, Benth. „ incisa, Benth. „ eriostachya, Benth. ,, strobilifera, Benth. Mentha arvensis, L. ,, incana, Willd, var. Hoylean a, Benth. Origanum normale, Don. Melissa calamintha, L. Micromeria biflora, Benth. Hedeoma nepalensis, Benth. Salvia glutinosa, L. ,, Moorcroftiana, Wall. » ■ ,, lanata, Roxb. ,, plebeja. R. Br. Nepeta spicata, Benth. „ distans, Boyle. ,, ciliaris, Royle. „ ruderalis, Ham. „ leucophylla, Benth. ,, Govaniana. Benth. Lailemantia Royleana, Benth. Anisomeles ovata, R. Br. Prunella vulgaris, L. Scutellaria grossa, Benth. „ repens, Ham. „ linearis, Benth. ,, scandens, Don. Carniotome versicolor, Benth. Leonurus Royleanus, Benth. ,, pubescens, Benth, „ cardiacus, L. Lamium amplexicaule, L. „ petiolatum, Royle. Colquhounia coccinea, Wall. Stachys sericea, Wall. „ splendens. Wall. Roylea elegans, Wall. Leucas urticaefolia, R. Br. „ Lanata, Benth. ,, mollissima, Wall. 318 HIMALAYAN DISTRICTS' Natural Order 92 . — Labiata — (concluded). Leucas diffusa, Benth. „ hyssopifolia, Benth, „ cephalotes, Spr, Leon otis nepetsefolia, R. Br. Phlomis lamiifolia, Royle. Eremostachys superba, Royle, Ajuga remota, Benth. „ bracteosa, Wall, Teucrium Royleanum, Benth. „ quadrifarium, Ham. Natural Order 93, — Plantaginece . Plantago major, L. „ Ispaghula, Ro-xb. Natural Order 94. — Chen opodia eea. Chenopodium album, L. ,, Botrys, L. Natural Order 95. — Pasellaceai. Basella rubra, L. cultivated and natu- ralized. Natural Order 96. — Aniarantacea. Deeringia celosioides, Moq. Rodetia Amherstiana, Moq. Celosia argentea, Moq. Amaran thus caudatus. L. cultivated and naturalized. Amaranthus paniculatus, Moq. Gangeticus, L. » frumentaceus, Roxb, Ram- dan a, Anardana, culti- vated and naturalized. ,, spinosus, L. iErua scandens, Wall. ,, lanata, Juss. Achyranthes aspera, L. Digera arvensis, Forsk. Pupalia Iappacea, DC. Cyathula prostrata, Bl. Alternanthera sessilis, R. Br. Natural Order 97. — Nyctagineae. Boerhaavia diffusa, L. Mirabilis Jala pa, L., introduced and na- turalized. Natural Order 98.—P7iytolaccaccce. Pircunia Latbenia, Moq. Natural Order 99. — Polygonacetx. Rumex Walliehii, Meissn. „ nepalensis, Spr, „ hastatus, Don. Natural Order 99. — Polygonace'a. — (concluded). Rumex vesicarius, L. Koenigia Islandica, L. Rheum emodi, Wall. „ himalense, Royle. Polygonum Roxburghii, Meissn. ,, plebeium, R. Br. „ herniarioides, Del. „ recumbens, Royle, „ aviculare, L. „ barbatum, L. „ amphibium, L. „ lapithifolium, L. » sphEerostachyum, Meissn. r , amplexicaule, Don. „ vaccinsefolium, Wall. f , affine, Don. nepalense, Meissn. „ sphterocephalum, Don, ,, capitatum, Ham, ,) chinense, L. „ pterocarpum, Wall. , , ru mi cifol i um . Royl e . Fagopyrum esculentum, Mcench. „ cymosum, Meissn. n tataricum, Gaertn. Natural Order 100. — Laurinctt. Cinnamomum Tamala, N. ab E., var. albiflorum, Tejpat. Phoebe lanceolata, N. ab E. „ pallida. N. ab E. Machilus odoratissimus, N. ab E. Tetranthera Roxburghii, N. ab E*. yy monopetala, Roxb. Litssa consimilis, N. ab E. „ lanuginosa, N. ab E. Natural Order IQl.—Thymelacea. Daphne papyracea. Wall. Wikstrcemia virgata, Meissn. Natural Order 102. — Loranthacew » Loranthus ligustrinus, Wall. » pulverulentus, Wall. >> vestitus, Wall. yy longiflorus, Desv. yy cordifolius, Wall. Viscum album, L. „ articulatum, Burm. „ attenuatum, D.C, Natural Order 103.' — Elceagnees. Hippophae salicifolia, Don. E laeagnus umbellata, Thumb. „ latifolia, L. Natural Order 104. — Santalaccz. Osyris arborea, Wall. OF THE NORTH-WESTERN PROVINCES 317 Natural Order 105. — Aristolochiacea. Aristolochia bracteata, Retz. Natural Order 106. — Euphorbiacea. Pbyllanthus nepalensis. Milll. „ parvifolins, Wall. „ velutinus, Mull. „ Miruri, L. „ Emblica, L & Antidesma diandrum, Tine. Securinega obovata, Mull. „ Leucopyrus, Mull. Putranjiva Roxburghii, Wall. Andrachne cordifolia, Milll. Bischoffia javanica, Bl. Briedelia montana, Willd. „ stipularis, Bl. Croton oblongifolius, Roxb., Introduced. Trewia nudiflora, Willd. Mallotus philippinensis, Mu.ll, (Rottlera tinctoria, Roxb). Ricinus communis, L., cultivated. Homonoya riparia, Lour. BaKospermum polyandrum, Wight. Exccecaria insignis, Milll. Euphorbia indica. Lamk. „ pilulifera, L. „ neriifolia, L. „ Sikkimensis, Boiss. „ longifolia, Don. ,, Helioscopia, L. „ nepalensis, Boiss. „ Nivulia, Ham. ,, Royleana, Boiss. Sarcococca pruniformis, Lindl. Natural Order 107. — Cupulifera. Quercus semecarpifolia, Sm. 99 Ilex, L. 9) dilatata, Lindl. J) lanuginosa, Don. 9) incana Roxb. an nu lata, Sm. Natural Order 108. — JMyricicea. Myrica sapida, Wall, Natural Order 109. — Betulacea. Betula Bhojpattra, Wall. ,, acuminata, Wall. „ nitida, Don. Alnus nepalensis, Don. Natural Order 1 10.— Corylacea. Carpinus viminea, Wall. „ faginea, Lindl. Cory 1 us Colurna, Linn. Natural Order 111. — Juylandea. Juglans regia, L. Engelhardtia Colebrookiana, Lindl, Natural Order 112. — Salic inca. Salix tetrasperma, Roxb. „ babylonica, L., introduced. ,, elegans, Wall. „ daphnoides, L. „ flabellaris, Anders. „ Lindleyana, Wall. Pop ulus ciliata, Wall. Natural Order 113. — UrticacecE. Ulmus integrifolia, Roxb. ,. erosa, Roth. Celtis caucasica, Willd. „ australis, L. Sponia politoria, Planch. ,, orientalis, Planch. Cannabis sativa, L. Urtica parvi flora, Roxb. Girardinia lieterophylla, Dene. Pilea scripta, Wedd. Lecanthus peduncularis, Wedd. Elatostemma sessile, Forst. „ diversitolium, W edd. „ Stracheyanum, Wedd. Bcehmeria rugulosa, Wedd. „ macrophylla, Don. „ platyphylla, Don. Pouzolzia indica, Gaud. „ viminea, Wedd. Debregeasia longifolia, Wedd- „ bicolor, Wedd. Memorialis pentandra, W edd. ,, liirta, Wedd. Villebrunea frutescens, Bl. Maoutia Puya, Wedd. Cudrania javanensis, Tree. Streblus asper, Lour. Morus atropurpnrea, Roxb , introduced. „ lasvigata, Wall. ,, indica, L. „ alba, Willd, cultivated. Ficus bengalcnsis, L., Bar. „ infectoria, Willd. „ religiosa, L., Pipal. „ cordifolia, Roxb. „ nem oralis. Wall. „ caudata, Wall. „ scandens, Roxb. „ foveolata, Wall. „ tuberculata, Wall. „ Roxburghii, Wall, 318 Himalayan districts' Natural Order 113. — Urticacece. — (concluded). Ficus hispida, L. f. „ Cunia, Ham. „ glomerata, Willd , Gular. ,, Carica, L. introduced. „ virgata, Roxb. Natural Order 114. — Piperacece. Peperomia reflexa, Dietr. Natural Order 115. — Gnetaceai. Ephedra vulgaris, Rich. Natural Order 116. — Conifer re. Pinus longifolia, Roxb. ,, Gerardiana, Wall. „ excelsa, Wall. Abies Webbiana, Lindl. „ Smithiana, Forbes. Cedrus Deodara, Loud. Cupressus torulosa, Don. Juniperus communis, L. „ excelsa, Bieb. „ recur va, Ham. Taxus baccata, L. Natural Order 117. — Palmaceee. Phoenix acaulis, Roxb. „ sylvestris, Roxb. Chamaerops Martiana, Wall. Calamus Koyleanus, Griff. Wallichia densiflora, Mart. Natural Order 118. — Aroidece. Arisaema Jacquemontii, Bl. „ utile, Hf. & T. „ costatum, Mart. „ speciosum, Mart. ,, curvatum, Kunth. Sauromatum guttatum, Schott. Remusatia vivipara, Schott. Amorphophallus campanulatus, Bl. Colocasia, species. Scindapsus officinalis, Schott. „ decursiva, Schott. Typhonium, species. Pothos scandens, L. Acorus calamus, L. Natural Order 119. — Lemanacece Lemna minor, L. „ polyrrhiza, L. Natural Order 120. — Typacece. Typha elepliantina, Roxb. Natural Order 121. — Juncayinacete. Potamogeton pectinatus, L. Aponogeton monostachyus, Roxb. Natural Order 122. — Scitamineee. Globba Orixensis, Roxb. Zingiber capitatum, Roxb. „ Caisumunar, Roxb. „ ligulatum, Roxb. Curcuma angustifolia, Roxb. „ Zerumbet, Roxb. Roscoea elata, Sm. „ alpina, Roxb. „ spicata, Sm. ,, purpurea, Sm. Amomum subulatum, Roxb. Hedychium coronarium, L., in gardens. „ spicatum, Sm, „ coccineum, Ham. Costus speciosus, L. Musa paradisiaca, L. plantain, cultivated. „ nepalensis, Wall. Natural Order 123. — Orchidacece. Oberonia iridifolia, Lindl. Dienia cylindrostachva, L. Liparis obcordata, Yalil. Ccelogyne cristata, Lindl. ,, ocellata, Lindl. „ ovalis, Lindl. Eria convallarioides, Lindl. „ alba, Lindl. „ flava, Lindl. Dendrobium eriseflorum, Gritf. alpestre, Royle. Otochilus, species. Apaturia Smithiana, Lindl. Eulophia, campestris, L. „ harbacea, Lindl. Cyrtopera fusca, Wight. Vanda cristata, Lindl. Saccolabium guttatum, Lindl. „ Gharwalicum, Reiclib. f. Aerides affine, Wall. ,, odoratum, I, owe. „ Hystrix, Lindl. „ ditforme, Wall. Calanthe puberula, Lindl. Orchis latifolia, L. Gymnadenia cucullata, Rich. „ spathulata, Lindl. Aceras angustifolia, Lindl. Platanthera orchidis, Lindl. „ clavigera, Lindl. „ obcordata, Lindl. „ Susanna, Lindl. „ Candida, Lindl „ acuminata, Lindl. OF THE NORTH-WESTERN PROYINCFS 319 Natural Order 123. — Orchidacea — (concluded). Gamoplexis orobanchoides, Falc. Epipactis latifolia, Sw. „ macrostacliya, Lindl. Spirantbes australis, R. Br. Habenaria pectinata, Lindl. „ intermedia, Don. „ marginata, Lindl. „ longifolia, Lindl. Peristylus Goodyeroides Lindl. Herminium Monorchis, Sw. „ species. Satyrium nepalense, Don. Monocbilus flavus, Wall. Tripleura pallida, Lindl. Goodyera marginata, Lindl. Cypripedium cordigerum, Don. Natural Order 124 ,~—lridaceaa. Iris sulcata, Wall. „ decora, Wall. „ Ramaonensis, Wall. ,, nepalensis, Wall. Natural Order 125 — .Amaryllidacece. Crinum toxicarium, Roxb. „ amcenum, Roxb. Cnrculigo recurvata, Roxb. Hypoxis aurea, Lour. „ orchioides, Kz. Natural Order 126. — Dioseoreee. Dioseorea deltoidea, Wall. „ sagittata, Royle. „ pentaphylla, L. Natural Order 127. — Liliacea. Tulipa stelleta, Hook. Gagea thesioides, Fisch. elegans, Wall. Iphigenia indica, Kth. Lloydia serotina, Reichb. Fritillaria cirrhosa, Don. „ verticillata, Royle. Lilium giganteum, Wall. „ Wallichianum, R. et. S. „ nepalense, Wall. „ Thomsonianum, Ilf. „ roseum, L. Gloriosa superba, L. Allium. Victoriale, L. „ Wallichii, Kth. „ tuberosum, Roxb. „ Govanianum, Wall. „ consanguineum, Kth. „ rubens, Schrced. j Natural Order 127. — Liliacea. — (concld.) Urginea indica, Kunth. Asphodelus clavatus, Roxb. Asparagus racemosus, Willd. „ tllicinus, Ham. Polygonatum multiflorum, All „ sibii’icum, Red. i „ verticillatum, All. Fliiggea intermedia, Sch. „ Wallichiana, Kth. Smilax maculata, Roxb. „ elegans. Wall. „ macrophylla, Roxb. „ ovalifolia, Roxb. Paris polyphylla, Sm. Trillidium Govanianum, Kth. Disporum Pitsutum, Don. „ calcaratum, Don. Natural Order 128. — Alismacea. Alisma Plantago, L. ,, reniforme, Don. Sagittaria sagittifolia, L. Natural Order 129. — Pontedsra.:ece, Monochoria hastata, Presl. Natural Order 130. — Commelynacex. Cyanotis axillaris, R. et S. „ barbata Don. Commelyna salicifolia, Roxb. ., bengalensis, L. „ obliqua, Ham. Aneilema lierbaceum, Wall. Natural Order 131. — Juncaoeac. Juncus concinnus, Don. „ leucomelos, Royle. „ castaneus, L. „ bufonius, L. „ effusus, L. „ leucanthus, Don. Natural Order 132. — Restiacecc. Eriocaulon quinquangulare,L. „ trilobum, Ham. ,, sexangulare, L. Natural Order 133. — Cyperacca. Carex rigida, Good. „ Thomsoni, Boot. . „ mitis, Boot. „ nubigena, Don. „ foliosa, Don. 320 HIMALAYAN DISTRICTS Natural Order 133. — C'l/peracece — (concluded.) Carex longipes, Don. „ Moorcroftii, Falc. „ alopecurioides, Don. „ Wallichiana, Presc. „ setigera, Don. ,, cruenta, Nees. „ uncinoides, Boot. „ vesiculosa, Boot. „ fllicina, Nees. „ condensata, Nees. „ bengalensis, Boxb. Rhynchospora aurea, Nees. „ Wallichiana, Nees. Fimbristylis quinquangularis, Nees. „ dichotoma, Vahl. „ aestivalis, Vahl. ,, complanata, Link. Scirpus juncoides, Boxb. „ affinis, Both. „ mucronatus, L. Abilgaardia monostachya, Vahl. Eleocharis uniglumis, R. Br. „ palustris, B. Br. „ ovata, R,. Br. Isolepis setacea, B. Br. „ trifida, Nees. „ supina, R. Br. „ Boylei, Nees. Kyllingia monocephala, L. „ brevifolia, Itottb. „ triceps, Nees. Eriophorum comosum, Wall. Cyperus pygmaeus, Vahl. • „ alopecuroides, Bottb. ,, compressus, L. ,, niveus, Betz. „ difformis, L. „ Iria, L. „ rotund us, L. Mariscus paniceus, Vahl. Natural Order 134. — Graminea. Oryza sativa, L., Bice, cultivated. Zea Mays, L., Makai, Bhuta, Indian Corn, introduced, and cultivated. Coix Lachryma, L. „ gigantea, Koen. Milium effusum, L., introduced . Paspalum pedicellatum, Nees. „ scrobiculatum, L. cultivated. „ Royleanum, Nees. Coridochloa semialata, Nees. Panicum sanguinale, L. ciliare, Retz. 9> miliaceum, L., cultivated. >9 maximum, Jacq. 99 ovalifolium, Poir. 99 longipes, W. & A. 99 miliare, Lamk. 9 9 vestitum, Nees. 99 plicatum, Roxb. Natui at Order 134. - Graminea — (contd.) Panicum prostratum, Lamk. „ repens, L. Oplismenus colonus, Kth. „ compositus, R. &. S. „ frumentaceus, Kunth, culti- ^ vated. ,, stagninus, Kth. Setaria glauca, Beauv. ,, italien, Kth., naturalized ; cul- tivated. „ verticillata, Beauv. Penicillaria spicata, Lamk, Bajra, cul- tivated. Pennisetum cenchroides, Rich. „ triflorum, Nees. Gymnothrix flaccida, Munro. Arundinella setosa, Trin. Sporobolus diandra, Beauv. „ elongatus, R. Br. Agrostis alba, L. ,, ciliata, Trin. Miililenbergia sylvatica, Trin. „ geniculata, Nees. „ viridissima, Nees. Polypogon littoralis, L. Calamagrostis Epigejos, Roth. Orthoraphium Roylei, Nees. Piptatherum aequiglume, Munro. Alopecurus pratesis, L. Phleum arenarium, L. Phragmites Roxburghii, Kunth. Chloris barbata, Swartz. Eleusine indica Gsertn ,, Coracana, Gsertn, cultivated, ,, verticillata, Roxb. Cynodon Dactylon, Pers, Diib. Avena fatua, L. „ pratensis, L. Poa annua, L. ,, jiratensis, L. „ bulbosa, L. Eragrostis plumosa, Link. „ pilosa, L. „ verticillata, Beauv. „ unioloides, Nees. „ poseoides, Beauv. „ nardoides Trin. ,, diandra, Boxb. Melica ciliata, L. Kceleria cristata, Pers. „ phleoides, Pers. Dactylis glomerata, L. Festuca duriuscela, L. Bromus squarrosus, L. „ arvensis, L. „ giganteus, L. Arundinaria falcata, Nees. „ Falconeri, Kz. Thamnocalamus spathifiorus, Munro, Bambusa arundinacea, L. Dendrocalamus strictus, Nees. Hordeum hexastichon L., Jau, Barley, cultivated . OF THE NORTH-WESTERN PROVINCES. 321 Natural Order 134. — Gramince — (concld.) Hordeum vulgare, L., cultivated, Elymus sibiricus, L. Lolium speciosum, Stev. „ temulentum, L. Triticum vulgare, Vil., Gehun, Wheat, cultivated. Mnesithea laevis, Kth. Rottboellia exaltata, L. Ophiurus corymbosus, Grtn. Manisurus granularis, Sw. Andropogon Gryllus, L. ,, acicularis, Rets. „ involutus, Stend, „ montanus, Roxb. „ Ischaemum, L. Heteropogcn contortus, R. & S. ,, Roylei, Nees. Sorghum vulgare, Pers., Joar, cultivated, „ Halepense, L. Apocopis Royleanus, Nees Batratherum molle, Nees. „ lancifolium, Trin. „ echinatum, Nees. Anatherum muricatum, Beauv. Cymbopogon laniger, Desf. „ flexuosus, Nees. „ Martini, Munro. „ Schoenanthus, L. „ Nardus, L. Anclroscepia gigantea, Brongti. Anthistiria arundinacea, Nees. •„ Anathera, Nees. „ scandens, Roxb. Apluda aristata, L. „ geniculata, Roxb. Imperata arundinacea, Cyrill. Saccharum spontaneum, L. „ procerum, Roxb. ,, officinarum, L.,, Sugarcane cultivated , introduced. „ Sara, Roxb-. „ filifolium, Nees. Erianthus Ravenna;, Beauv. „ japonicus, Beauv. Cryptogams. Filices or Ferns. Woodsia elongata, Hk. „ lanosa, Hk. Dicksonia appendiculata, Wall. ,, scabra, Wall. Davallia pulchra, Don. „ divaricata, Bl. „ immersa, Wall. „ nodosa, Hk. Adiantum lunulatum, Burrf.. ,, caudatum, L. n Capillus-Veneris, L. Filices or Ferns— (continued.) Adiantum venustum, Don. Cheilanthes Dalhousias, Hk. „ farinosa, Kaulf. Onychium auratum, Kaulf. „ japonicum, Kunze. Pellea, calomelanos, Link. Pteris longifolia, L. „ cretica, L. „ quadriaurita, Rez. „ aquilina, L. „ Walliehiana, Agdh. Vv T ood\vardia radicans, Sm. Asplenium, alternans, Wall. „ varians Hk. and Gr. ,, viridie, Huds. „ Trichomanes, L. „ planicaule, Wall. „ fontanum, Bernh. ,, bulbiferum, Forst. ,, tenuifolium, Don. „ Filix foemina, Bernh. „ polypodioides, Mett. „ dilatatum, Wall. „ esculentum, Persl. „ Ceterach, L. ,, australe, Brack. Aspidium auriculatum, Sw. „ aculeatum, Sw. „ Thomsoni, Hk. „ aristatum, Sw. „ falcatum, Sw. Nephrodium unitum, R. Br. „ prolixum, Bak. ,, sparsum, Don. „ molle, Desv. 5 ,, cicutarium, Bak. „ polymorphum, Bak „ Filix-mas, Rich. „ cochleatum, Don. „ odoratum, Bak. Oleandra Wallichii, Hk. „ neriiformis, Cav. Polypodium erubescens, Wall. „ proliferum, Presl. „ lineatum, Colebr. „ amoenum, Wall. „ lachnopus, Wall. „ malacodon, Hk. „ trifidum, Don. „ Lingua, Sw. „ stigmosum, Sw. „ fissum, Bak. „ flocculosum, Don. „ lineare, Thunb. „ normale. Don. „ membwanaceum, Don. „ propinquum, Wall. „ juglandifolium, Don. „ quercifolium, L. „ himalense, Hook. „ leiorhizon, Wall. Acrostichum virens, Wall. Gymnogramme vestita, Hk. 41 322 hima'layan districts Filiees or Ferns — (conoid.) Gymnogramme Andersoni, Bedd. „ javanica, Bl. ,, lanceolata, Hk. „ involuta, Don. Osmnnda Claytoniana, L. Schizsea digitata, Sw. Lygodium, scandens, Sw. ,, japonicum, Sw. Botrychium daucifolium, Wall. ,, Lunaria, Sw. „ Yirginianum, Sw. Lycopodiacece. Selaginella Jacquemontii,. Springs „ setacea, Spring. „ subulifolia, Spring. Marsiliacece. Marsilea qudrifolia, L. Characea. Chara yeticillata, Roxb. OF THE NORTH-WESTERN PROVINCES-. 323 PLANTS OE K U M A 0 N.' The following Area under notice. list gives the names of all plants known to have been found in Kumaon, Garhwal and the Bhabar, three of the districts which are in- cluded in the Commissionership of Kumaon. Plants of the plains of India, plants growing in Tibet, and plants only found in the Independent States of Nepal and Tihri, do not appear in this list. The words, “ common, ” “ frequent,” and “ rare ” have been employed to denote the comparative occurrence of the various species ; but as the European stations of Almora, Naini Tal, and Ranikhet are all situated at a height of between 5,000 and 7,000 feet above the level of the sea, it will be easily understood that plants growing about that level are more likely to meet an observer’s eye than plants which grow either at a very high, or at a very low elevation. Plants which are marked “rare” without any locality being given, are those which have been found by former observers, but which have never been seen growing within the limits of the division by Colonel Davidson, Mr. Waterfield or Dr. Watson, In the arrangement of the orders, genera, and species, Hooker s < pq ora 0 f British India,’ has been followed as far as published, that is to say, to the end of Poly petalce . With regard to the other groups the books chiefly consulted have been Brandis’ Forest Flora, Madden’s Papers in the Journal of the Asiatic Society, Royle’s Illustrations of Himalayan Botany, C. B. Clarke’s Composite and Commelynacem, Steudel’s Grasses, and Cyperacem, Hooker and Baker’s Ferns, Mitten’s Mosses. Synonyms have rarely been given except where the name adopted in the list is different from that given by Hoyle. Royle’s Illustrations, published in 1839, is still a standard work on Hima- layan Botany, and most of the plants figured Range of plants. * n p. are f oun d i n the Commissionership of Kumaon. There are, however, in Royle’s book a certain number of plants which are common near Mussooree, where the book was written, but which are not found east of the Alaknanda river, the i This notice and list has been prepared for this volume by Mr. W, Watson, M.D., Deputy Sanitary Commissioner. Almora. 324 HIMA'LAYAN DISTEICTS boundary between the Kumaon Commissionership and the Native State of Tihri. As examples of these Mussooree plants not found in Kumaon may be quoted — Dictamnus albus , Berberis Lycium, Rosa Lyelli , Sonerila tenera , Genticma Karroo, Ricrorhiza Kurroo, Eremostachys superba. On the other hand, the common phalel tree of Eastern Kumaon ( Bassia butyracea) is apparently not found at Mussooree, as it is not mentioned by Hoyle as occurring there. The same remark ap- plies to the very common and very beautiful Silang tree of Kumaon ( Olea acuminata). This tree, conspicuous from its sweet scented yellow blossoms, is never alluded to by Hoyle, so that he probably never met with it near Mussooree. It is found in Kumaon at all elevations from 3,000 to 7,000 feet. There are fine trees of it at Debi Dhura at a height of 6,800 feet, and at Kapkot at a height of 3,400 feet. The Kumaon Division includes a tract of country varying much in elevation. On the south, the Bhabar strip along the foot of the hills has a mean height of about 1,400 feet, whilst the passes that lead into Tibet have an elevation exceeding 18,000 feet. It might be expected that European forms would be more abundant towards these passes than in the Bhabar, and this, on the whole, is the case. There are, however, some European plants that are only found at low elevations and are never seen above Eastern depression. 6,000 feet. I he most common of these are : — Ranunculus sceleratus, Geranium molle, Veronica Anagallis, and Verbena officinalis, and it is difficult to assign an adequate reason for this phenomenon. Another remarkable fact connected with the montane flora is the eastern depression of many Hima- layan plants. By this term is understood that plants which occur only at high elevations near Simla are found to grow at lower elevations at Mussooree and at still lower heights near Naini Tal. The following plants may be named as affording examples of eastern depression — (a) The shrub Coriaria nepalensis , which gives its name to the station of Mussooree, is said by Royle not to grow under 5,000 feet at Mussooree. In Kumaon, however, it descends as low as 2,000 feet. OF THE NORTH-WESTERN PROVINCES. 325 (5) Hemip hragma heterophylla, one of the Scrophulcmaceoe , is never found at Simla below 10,000 feet, whilst it occurs in Kumaon at 7,000 feet, and is common there at 8,000 feet. (c) The Tilonj oak, Quercus dilatata, is found at Simla about 7,000 feet, and near Naini Tal it grows abundantly down to 3,000 feet. {d) Dipsacus inermis is one of the most common plants at Almora (5,500 feet), but is not found towards Simla at elevations below 8,000 feet. {y >> „ rivularis (Omalocarpus) polyantlies, „ „ elongata Thalictrum (Physocarpum) elegans ... platycarpum ... cultratum Chelidonii reniforme [neu- rocarp im, Royle.] „ pauciflorum ... (Euthalictrum) Punduanum, „ saniculse forme, Jaranicum foliolosum minus Callianthemum cachemirianum Adonis aestivalis Ranunculus (Batrachium) aquatilis... (Hecatonia) sceleratus ... 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 33 hirtellus diffusus laetus (Echinella) fiaccidus arvensis » 33 Ghantiali Ghantiali Ghantiali ... Ghantiali ... Kakriya Pengla jari. 33 Shim Dainiya Ainwa December, near streams ; rare. April, common. May; rare. Common. Bhabar and valleys ; October. Colonel Davidson. Above 10,000 feet. May. Common. Rare. August, September. Very common. October. Very com- mon. Rare. June and July ; com- mon. May. Very common. Above 6,000 feet. June. Above 10,000 feet. Common. Rare, 10,000 feet. 33 33 33 33 ^ Rare. Badrinath. Rare. 33 Common; high eleva- tions, July. Frequent. Common. On trees ; autumn. 33 Very common, summer. Frequent. Above 10,000 feet. >> . » Bhim Tal. Common up to 4,000 feet. High elevations. Common. Very common. Rare. Common at low levels. 328 HIM A' LAY AN DISTRICTS' DIVISION I. — POLYPETAL2E — ( continued ). No. Scientific name. Vernacular Note. name. ORDER 1. — RANUNCULACEiE— (concluded). 39 Oxygraphis glacialis Above 16,000 feet. 40 „ polypetala ... „ 10,000 „ Common. 41 Caltha palustris [Govaniana, Royle], 42 Trollius acaulis Above 10,000 feet. 43 „ pumilis „ 12,000 „ 44 Isopyrum grandiflorum ... 45 Aquilegia vulgaris Common. 46 Delphinium denudatum [pauciflorum, Munila 47 Royle.] „ canruleum ... • • • Above 15,000 feet. 48 „ elatum • . • China hill 8,000 feet,. 49 „ vestitum ... , , , „ 8,000 „ 60 ,, Cashmirianum , . , „ 10,000 61 ,, Ajacis Munila Naturalized. 62 Aconitum Lycoctonum ... Bish Above 8,000 feet. 63 64 ,, palmatum „ ferox ... » yy yy „ 10,000 „ 66 „ Napellus 66 „ heterophyllum Atis ” 8,000 ”, 57 Actsea spicata Rare. 68 Cimicifuga fcetida 59 Paeonia emodi Bhunya madin, Young shoots eaten.. ORDER 2. — DILLENIACEiE. 1 Dillenia indica ... Rare. ORDER 3.— MAGNOLIACEiE. 1 Michelia Kisopa Ban champa, Common ; Beripul and Schizandra grandiflora ... Ukhimath. 2 Silangti Frequent ; Gagar. 3 „ propinqua Sindrayan ... Common. ORDER 4.— ANONACEJE. i Polyalthia Ivorinti [Guatteria Korinti, Madden.] ... Swamps. Bhabar. 2 Anona squamosa Bella Ditto 3 Miliusa velutina 4 Saccopetalum tomentosum Kangri Kotdwara. ORDER 6 . — MENISPERM ACEjE. 1 Tinospora cordifolia Gurcha Comm on 2 Cocculus laurifolius ... Tilbarapanya- „ about 4.000 „ villosus liandkakra. feet. 3 Rare. 4 Stephania elegans 6 „ rotunda [RoxburghianaJ ... Ganjara yy Common. 6 Cissampelos Pareira [convolvulacea], Pari yy OF THE NORTH-WESTERN PROVINCES 329 DIVISION I. — POLYPETALiE — ( continued). No. Scientific name. Vernacular name. Note. ORDER 6.— BERBERIDEJE. 1 Holboellia latifolia Gophla May, common, Rani- khet and Binsar. ■C-# • „ var. angustifolia ... 2 Berber is (lVIahonia) nepalensis Goplila Frequent, Thakil and Binsar. 3 „ (Euberbcris) vulgaris . . . High elevations. 4 „ ,, umbellata . . . Rare. 5 „ „ aristata Chotra Common. High ele- vations. 6 i „ „ Lvcium Rare. 7 „ „ asiatica Kilmora Common. 8 „ ,, Wallichiana ... . . i China hill, Colonel Davidson. 9 Podophyllum emodi ... High elevations. ORDER 7. — NYMPHACEiE. 1 Nelumbium sneciosum ... Kanwal Frequent, Buwali po- kar. ORDER 8. — PAPAVERACEiE. I Papaver dufeium [glabrum, Roylel| ... Takuvia Common. 2 Argemone mexicana Bhar bhand, Bhabar; introduced. 3 Meconopsis aculeata Kanda Above 10,000 feet 4 „ robusta >5 5 ,, nipalensis » n £ Stylophor um lactucoides ... ■5 ... **• ORDER 9.— EUMARIACEJE. I Dicentra Roylei . . • Rare. 2 „ scandens ... . Common. 3 Corydalis rntsefolia [diphylla] 4 „ cachemiriana ... Above 9,000 feet. 5 ,, crithmifolia ... . . . Rare. f. „ elegans Above 10,000 feet. 7 „ Govaniana „ 8,000 „ 8 „ ramosa ... „ 12,000 „ 9 „ sibirica [filiformis] Common. 10 „ cornuta Blmtkes Very common, 11 chasrophylia ... Common, Binsar. 12 „ nieifolia ... . Above 10,000 feet. 13 „ flabellata „ 9,000 „ 14 Fumaria parvifolia [VailLantii] Khairmva ... Very common. ORDER 10.— CRUCIFERiE. Tribe Arabideae. 1 Nasturtium officinale Piriya halim, Cultivated. 2 „ palustre ... Common. 3 „ montanum ... ... J) 4 Barbarca vulgaris . . . 5 Arabis glabra ... Frequent. 42 330 HIMALAYAN DISTRICTS DIVISION I.— POLYPETAL iE— ( continued ). No, 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 Scientific name. Vernacular name. ORDER 10.— CRUCIFER2E— (continued). Tribe ARABiDEna — (concluded). Arabis alpina „ amplexicaulis ... ... Rai ghas Cardamine hirsuta „ iinpatiens ... ... Slieliya „ macrophylla ... Tribe Alyssine^e. Alyssum maritimuin „ canescens Darba (Chrysodraba) alpina „ (Leucodraba) incana „ „ lasiophylla .. ,, „ fladnitzensis .. Tribe Sisymbrie^s. Sisymbrium mollissimum himalaicum Thalianum rupestre strict urn Wallichii sophia Columnse Alliaria Eutrema primulsefolium . Erysimum hieracifolium Tribe Brassiceze. Brassica nigra „ campestris 99 99 )> 99 99 9 ) 99 99 Jaua glias >» » var. dicliotoma ... vat. glauca, Box var. glauca, Royle trilocularis „ luncea Eruca sativa ... Kali sarson, . . Jariya Rara, pila sar- son. Dain toriya... Rai Dua Tribe Lepidineze. Capsella Bursa-pastoris Lepidium sativum „ capitatum ,, ruderale Halim Tribe Tiilaspideze. Megacarpcea polyandra Thlaspi arvense „ alpestre Iberidella Andersoni Dhapriya ... Note. F r equent. Common. Very common. Common, Naturalized. Above 14,000 feet » 12,000 „ • „ 10,000 „ 12,000 „ 13 000 „ 99 99 Above 8,000 feet. ,, 10,000 „ Common. Above 8,000 feet. Common. Frequent. Rare. 99 99 Cultivated. 99 99 99 99 feet. up to 11,000 Weed in fields. Cultivated. Common. Very common. Common. Above 10,000 feet. Common, May and June, Almora. Above 10,000 feet. Common. Above 7,000 feet. „ 12,000 „ Ox itfc OS t>s OF THE NORTH-WESTERN PROVINCES. DIVISION I. — POLYPBTALiE — ( continued ). 331 No. 41 Scientific name. Vernacular name. Note. _ ORDER 10. — CRUCIFERJE— (concluded). Tribe RaphanE.®. Raphanus sativus ... ... I Muli ORDER 11.— CAPPARIDACEJ3. Cleome [Polanisia, Madden] viscosa... Gynandropsis pentaphylla Capparis spinosa [yar. leucophylla] ... „ horrida Mserua arenaria [Niebuhria oblongi- folia, Royle, 111.1 Ulta kanta . . . >y ORDER 12.— RESEDACEiE. Reseda odorata ... ... I ORDER 1 3. — VIOL ACEiE. Viola biflora [reniformis] Patrinii [csespitosa] diffusa... serpens [canescens, Wall] kunawarensis )) >5 ORDER 14.— BININEiE. Cochlospermum Gossypium ElacourLa Ramontchi ... \ „ sepiaria Xylosma longifolium Kumbi,katira, Kandai Katari ORDER 15.— PITTOSPORACEiE. Pittosporum floribundum „ eriocarpum . . . ... l . . . \ Gar siling Cultivated. Common, Bhabar and valleys. Bhabar and valleys. Common. Bhabar. Rare. Naturalized. Common. Rare. Common. Above 1 1 ,000 feet. Common, Bhabar, Rare. Common, river banks,. ORDER 1 6.— POLY G ALACK® . 1 Polygala triphylla[glaucescens, Wall], crotalarioides ... abyssinica lepta'ea [oligophylla. Wal- lich]. persicarisefolia... chinensis, [Rothiana, W. and A. sibirica [elegans, Wallich], ORDER 17.— CARYOPHYLLACEjE. TbIBE SlLENESd. 1 Gypsophila cerastioides ... 2 Saponaria vaccaria 3 Silene inflata Common, autumn. Very common. Rare. Common up to 4,000 feet. August, frequent. Common, Bhabar, » Common about 10*000 feet. Introduced. Common. 332 HIMALAYAN districts DIVISION I. — POLYPETALiE — ( continued ) . No. Scientific name. Vernacular name. Note. 4 ORDER 1 7. — CARYOPELLACEAt- Tribe SiLENEiE — (conclu Silene conoidea —(concluded). ded). Common. 5 „ gallica Introduced. 6 „ Ealconeriana Co i moa. 7 „ Stracheyi ... , Rare. 8 Cucubalus bacciferus 9 Lychnis multicaulis 30 „ inflata, Blink worth Very rare. 11 „ indica [fimbriata, Madden], ... Very common. IS Tribe Alsine^s. Cerastium dahuricum ... Rare. 13 „ Tulgatum [triviale, Mad* . . . Very conn nou 14 den], „ Thomsonii Rare. 35 Stellaria (Schizostegium) crispata . . . Coin man. 16 [monasperma, Don], „ „ paniculata [media, Rare. 17 Wight. „ (Malachinm) aquatica ... 18 „ (Eustellaria) media [mono . . . 19 gyna, Don]. „ „ semivestita Painkhanda; commw«. 20 „ „ Webbiana, [Lea- . Very common. 21 costemma angus- tifolia, Wall]. „ „ latifolia, [leacos- Rare. Ilanipani. 22 temma latYolia, Wall]. „ (Larbriea) longissima ]pa- 23 tens, Don], „ (Adenonema) decumbens... Above 11,000 feet. 24 Arenaria (Alsine) foliosa ... . Painkhanda ; common. 25 „ (Eremogone) festucoides ... June. Rare. 26 „ (Eutlialia) serpyllifolia ... Common, May & June. 27 „ ,, orbiculata 28 „ (Lepyrodiclis) holosteoides, ... . 29 „ Benthami . . . Rare. 30 Spei'gula arvensis ... Introduced. 31 „ pentandra [Arenaria flaeci- 32 da, Roxb.] Tribe Polycarpe2e. Drymaria cordata Common. 33 Polycarpaeacorymbosa ... ... 1 Order 18. — PORTULACEiE. Portnlaca olcracea ... ... j Luniya-kulfa, Common. 1 2 3 4 1 o 3 4 5 6 7 8 1 2 *) 4 1 1 2 3 4 5 6 7 8 9 OF THE NORTH-WESTERN PROVINCES. 333 DIVISION I. — POLYPETALiE — ( continued ). Scientific name. Vernacular name. ORDER 19. — TAMARISCINEJE. Tamarix gallica „ dioica Myricaria germanica „ elegans ORDER 20. — HYPERICINEiE Hypericum (Androsasmum) cernuum, cardifolium lysimachioidea patulum [uralum, Don]. (Euhyper icu a. ( perfora- tum. elodeoides ... nepaulense ... (Brathys) japonicum [pusillum]. ORDER 2 1 . — TERN STRiEMI ACEiE Deura Eurya acuminata Actinidia [Troclrostigma, Madden] callosa. * * Saurauja nepaulensis Camellia thea Gogana Cha ORDER 22.— DIPTEROCARPEiE. Shorea robusta ... ... I Sal Sakhu ORDER 23.' — MALVACEAE. Tiube Malvb^e. Malva verticillata silYestris, [mauritiana, Mad- den). ,, rotundifolia ,, parvifiora Sida rhombifolia „ cordifolia Abutilon polyaudrum indicum Note. Ulua-bena ... Tilciioni Bhoa Kalabali Tribe URENEiE. Urena lobata Sujiya Cliat- kura. Bhabar. Frequent, above 10,000 feet. Frequent, above 1 1,000 feet. Common. April. Rare, Bamni. Frequent above 8,000 feet. Common, September. „ August, and September. „ August, and September. Low elevations. ! Common. Bhabar and banks of Sarju. Common. Introduced. Common up to 4,500 feet, March- Frequent. Gardens and wild. Common. Up to 2,000 feet. Common. Bhabar and up to 3,000 feet. Common, banks of streams. 334 HIMALAYAN DISTRICTS DIVISION I. — POLYPETALiE — ( continued ). No. Scientific name. Vernacular Note, name. ORDER 23.— MALVACEiE— (concluded). Tribe FIibisceie, 10 Hibiscus (Furcaria) fnrcatus Introduced. 11 „ (Lagunea) solandra , . , Common. 12 „ (Abelmoschus) ficulneus . . . 13 „ pungens Hao Kapasya y> 14 „ cancellatus 15 Thespesia lampas Kapasya Tribe Bomba cum. 16 Kydia calycina Pata Common, September. „ Bhabar, up 17 Bombax malabaricum [Bombax hep- Semal taphylluin, Iioxb.] to 4,800 feet. ORDER 24. — STERCULIACEiE. 1 Sterculia urens Katira Bhabar. 2 „ villosa Udyal 33 3 ,, (Firmiana) fulgens [Wal- lichii, Madden.] Bodala Common. 4 Heiicteres isora Maror phal, Bhabar, May,-Septem- ber. 5 Pterospermum acerifolium Muchkunda, Introduced. 6 „ lanceoefolium [P. sub- Bhaber. erifolium, Madden] 7 Melocliia corchorifolia, [Riedleia cor- • « • Up to 4,000 feet. cborifolia, Dec.] 8 Waltheria indica, [Melocliia corcho- rifolia, Wall.] ... yy yy ORDER 25.— TILIACEAE. 1 Grewia oppositifolia Bhekla, bhen- Common. gal. 2 „ tilisefolia . . . Frequent, va’leys. 3 „ asiatica [elastica, Royle, III.] Pharsiya ... Common, cultivated. 4 „ sapida [nana., Wall] Common. 5 „ scabrophylla [scleropbylla, Gar bheli ... Wall] G „ laevigata [didyma, Roxb] ... Bhimul 7 „ polygama . . . Bhabar. 8 Triumfetta pilosa [oblongata, Wall] Leshwa, ku- Common. „ rhomboidea [angulata, mariya. 9 Chat kura ... Up to 4,000 feet. Wall.] 10 Corchorus fascicularis ? Introduced. 11 ,, acutangulus ? • • • 12 Eloeocarpus Yarunua Jalpai Rare. ORDER 26. — LINEiE. 1 Linum usitatissimum Alsi Introduced. 2 Reinwardtia trigyna Pyura Very common, March. 3 „ tetragyna ... ... Rare. OP THE NORTH-WESTERN PROVINCES. 335 DIVISION I. — POLYPETALiE — ( continued ) . No. Scientific name. Vernacular name. Note. ORDER 27.' — MALPIGHIACEiE. 1 Hiptage madablota ... March ; common up to 3,000 feet. 2 Aspidopterys Wallichii [Hiroea mi- ... June ; frequent up to tans, Wall], ORDER 28.— ZYGOPHYLLI LE. 4,000 . 1 Tribulus terrestris ... ••• | ORDER 29.— GERANIACEiE. Common. 1 Geranium pratense . . • Ra,re, Painkanda. 2 „ collinum . . . >> 3 „ palustre ? [grandiflorum, Edgeworth] ... „ Mana Pass. 4 „ Wallichianum ... Common, Naini Tal and Binsar, July. 5 „ Grevilleanum [eriostemon, Don] ... 6 „ nepalense . . . Common, May, June. 7 „ polyantlies ... . . . Rare. 8 „ rotundifolium . . • 9 „ molle • . • Eebruary. Banks of Ganges up to 1,500 feet. 10 „ Robertiannm • • • 11 ,, lucidum ... •••' . . . Common. 12 ocellatum [bicolor, Royle, 111] Ankri Very common, April, May, 13 Tropasolum majus Chalmori ... Introduced. 14 Oxalis corniculata Very common. 15 „ acetosella . . • Rare, Pindari, April. 16 Biophytum sensitivum ... ... Common up to 4,000 feet. 17 „ Reinwar dtii... . . • 5 ? 33 18 Impatiens (Brevicapsulae) Balsamina, . . . Gardens. 19 „ (Longicapsulse Boy lei var. moschata, Edge. ... Common. 20 „ Thcmsoni . . ■ 12,000 feet. Erequcnt. 21 „ sulcata [gigantea, Edge.], . . . 22 „ amplexicaulis . . . Rare. 23 „ scabrida [tricornis, Lind, Hamiltoniana, Don], ... Common, May, June. 24 „ bicornuta . . . Rare. 25 „ amphorata . . . Common, autumn. var umbrosa, Edge, [bi.co- lor, Royle, 111.] ... 33 26 „ racemosa ... Frequent. 27 „ laxiflora . . . 33 28 ,, micranthernum . . . Rare. 29 „ brachycentra . . . Frequent, summer. 30 „ glauca . * * * Rare, Diwali. 836 HIMALAYAN DISTRICTS DIVISION I. — POLYPETALiE — ( continued ). No. Scientific name. Vernacular name. Note. ( RDER 30.' — RUTACEiE. Tribe Timms. 1 Baenninghausenia alb i flora, [Ruta Pisu glias and Very common, autumn. albiflora, Wall.] upauya ghas. Tribe Zantiioxyue.®. 2 Zanthoxylum alatum, [Z. hostile, Timur and Common. Wall.] tejbal. 3 ,, acanthopoidum [hostile, Simur Rare, Budh Jageswar. Wall.] 4 „ oxyphyllum . . . Frequent, Gagar. 5 „ Budrunga ... Rare. Tribe Toddalie.®. 6 Toddalia acnleata Kliaseru Bhabar and valleys 7 Skimmia [Limonia, Wall. Anque- Nehar, kas- Very common. Tilia Dece.] Laureola. turi, gural pata. Tribe Aurantie®. 8 Glycosmis pentaphylla ... Potla Common. 9 Murraya exotica Jnti 10 „ (Bergera) Kcenigii G ani Very common. 11 Clausena pentaphylla Bhabar. 12 Limonia acidissima [L. crenulata, Roxb.] 13 Citrus medica Bijaura var. limonum Jamlra 14 „ aurantium Rare. 15 Feronia Elephantum Kait Bhabar. 16 iEgle Marmelos Bel ORDER 31.— SIMARUBEJE. 1 Bicrasma quassioides ... ... 1 Valleys ; frequent. ORDER 32. — OCITNACEZE. 1 Ochna pumila ... Rare. ORDER 33. — BURSERACEJE. Tribe Aura nth: as. 1 Boswellia serrata [thurifera, Roxb.] Sale, gugar... Bhabar. var. glabra Gugai 2 Garuga pinnata Kharpat 33 ORDER 34. — MELIACEiE. 1 Melia Azadirachta [indica] Nim Introduced. Bhabar. 2 „ Azadarach [sempervirensRoxb], Betain Common. 3 Heynea trijnga, [Zanthoxylon con- • • • Bhabar. naroides, W. & A.] 4 Cedrela Toona Tun Valleys. 5 „ serrata Dai Very common. OF THE NORTH-WESTERN PROVINCES. 337 DIVISION I . — P 0 L YPETE J3— ( continued ) . No. Scientific name. Vernacular name. ORDER 35.— 0LACINEA3. 1 Olax scandens , , , 2 „ nana ... ORDER 36. — ILICINEA5. 1 Ilex dipyrena Kandali 2 „ odorata Gar — kaula, garshun. 3 „ excelsa Kandali ORDER 37. — CELASTRINEiE. 1 Euonymus grandiflorus [lacerus, Don], . . . 2 3 ,, tingens fimbriatus Kasuri 4 „ frigidus . . . 5 echinatus , , . G pendulus [japonicus, Wall], Agnu 7 Hamiltonianus 8 Celastrus paniculata [nutans, Roxb]... Malkagni . . . 9 Gymnosporia rufa, [Celastrus rufa, Brandis.] 10 Royleana, [C. spinosus, Gwala-darim, Lam], 11 montana [C. senegalensis, . . . Lam.] 12 Elfeodendron glaucum, [Roxburghii, Shauria jam- W. & A.,Neerijadichotoma,Roxb]. rasiand dehbri. 13 Microtropis discolor ... ORDER 38. — RHAMNACEiE. 1 Ventilago calyculata [madraspatana, Rakt pita, Roxb.] kala lag 2 Zizyphus jujuba Bair 3 nummularia yy 4 vulgaris yy 6 „ oxyphylla yy 6 „ xylopyrus yy 7 8 „ rugosa Berchemia doribunda yy Kala lag . . . 9 flavescens ... 10 Edgeworthii ... Chadua 11 Rhamnus dahuricus [virgatus, Boxb.] 12 „ purpureus ... ... Ghont 13 ,, triqueter 14 procumbens . . . 15 Hovenia dulcis Aglaia 16 Sageretia oppositifolia ... 17 Gouania leptoetachya ... Kala lag 18 nepalensis • • • 19 Ilelinus lanceolatus • • • Note. Bhabar. Frequent. Very common. Frequent. Common. Bhabar, & to 3,000 feet. Frequent, April. Rare, 9,000 feet, April. „ 10,000 „ Frequent, April. Common. March. Bhim Tal. Rare. Common. Rare. Common. A white aphis feeds on this tree. Frequent. Common. Cultivated. >> J! Frequent up to 6,000 feet. Bhabar. Frequent. Rameshwar. Common, April. Common. About 7,000 feet ; on limestone. Rare; cultivated. Common. Bhabar . Common ; valleys. 33 S HIMALAYAN DISTRICTS DIVISION. — POLY PETAL iE — ( continued ). No. Scientific name. Vernacular Note. name. ORDER 39.— AMPELIDEiE. 3 Yitis (Simplicifolire) quadrangularis Har jora Bhabar. [Cissus edulis]. 2 „ pallida . . . Rare. 3 „ repanda [rosea, Royle 111.} . . . Frequent ; Bhabar. 4 ,, adnata • . . Rare.. 5 „ pedicellata • . . 6 „ lanata Purain Common, May. „ var. rugosa Assanja „ July. 7 „ latifolia Pan-laguli ... „ Bhabar. 8 „ vin'ifera Wild ? 9 „ parvifolia Barain Common. 10 „ (Trifoliatae) carnosa Bhabar. 11 „ [Ampelopsis, Wight} lii- Chappar-tang, Common. malayana. 22 „ divaricata [tomentosa, W. Amila and A.] 13 „ (Digitatae) obtecta 14 „ (Pedatae) capriolata [Cis- sus serrulata, Roxb.] 15 „ lanceolaria [Cissus femi- Panj-pata ... Ranibagh, nea, Roxb.] 18 Leea (Simplicifolise) maerophylia ... Frequent. 17 „ (Pinnatas) alata , , . 18 » aspera Kurmali Common. 19 „ (Bipinnataa) sambucina ... ... Rare. ORDER 40. — SAPINDACEJE. Tribe Sa binder. 1 Cardiospermum Halicacabum Bhabar. 2 jEscuIus (Pavia) indica Pankar, pan- Common. 3 Schleichera trijuga gri. Kusam Bhabar. 4 Sapindns Mukorossi Rita. „ var. detergens Rare. ,, var. acuminatus Com iron. 5 Acer (Integrifoliaj) oblongum Patangtiya... Common ; cups are 6 „ laevigatum made of the wood. Common. 7 Acer (Trilobataa) pentapomicum Bhabar. 8 ., (Quinquelobatae) caesium Kilu Frequent. 9 „ villosum [sterculacium Wall?]... 8,000 feet ; cups made „ caudatum [pectinatum Wall.]... of the wood 10 10,000 feet 11 „ (Septemlobatae) pictum fcultra- tum, Wall.] j ... Very common. Tribe Dodonb.®. 22 Dodonaea viscosa ... ... | • • i Rare ; Bhabar. Tribe Melianthe.®. 23 Melianthus major ... ... j i • • Introduced. OF THE NORTH-WESTERN PROVINCES. DIVISION I. — POLYPETALuE — {continued). 339 14 1 | 2 ; 3 ORDER 40.— SAriNDACEiE— (concluded). Tribe Staphyre^e. Staphylca emodi ... | Chitra ORDER 41 . — SABIACEiE. Gwep Gardar Meliosma dillenioefolia „ pungens Sabia campanulata „ parvidora Bakal pata. . . n panicu’.ata ORDER 42. — ANACARDI AC ? J£. 1 2 3 4 5 <6 7 8 9 10 U » >> Rhus (Simplicifolias) cotinus (Trifo'.iatae) parvidora (Tui pari pinnatae) semialata ... Wallichii [vernicifera, Royle], succedanea [acuminata, Dec.]... Pistacia integerrima, [Rhus integer- rima, Wall ] O.lina Wodier Semecarpus Anacardium Mangifera indica Buchanania latifolia Spondias mangifera ... «... ] Tung-ami 1 Eanel j Dakmila Bholiao Titari Kakar singi, Jhingho Bhilawa Am ... Pial Amra Note. ORD R 43. Coriaria nepalensis -CORIARIACETE- Mansuri mo- kola. ORDER 44. — MORINGEiE. Moringa pterygosperma... ... I Sainjan ORDER* 45. — LEGUMINOSAE. Tribe Podalyrie.®. Shalgari 4 6 6 7 8 9 10 Piptanthus nepalensis ... Thermopsis barbata Tribe Genisteje. Argyrolobinm flaccidum [Cytisusdac- cidum, Royle] „ roseum Crotal aria (Diffuse) humifusa ,, hirsuta (Alatae) alata ... (Calycinae) mysorensis albida calycina 1 >> »> >5 >> » >5 Gungri Gungri T requent : Gagar and Siahi Dabi. Common about 7,000 feet. Frequent ; banks of streams. Common. „ about 5,000 feet. „ Bhabar. Very common. Common. Valleys; common. Common ; valleys Bhabar. Common ; valleys. Bhabar. „ and valleys. Common. Common ; Bhabar. Above 8,000 feet. i „ 10,000 „ Common, July and Au- gust, on limestone. >•> >> Common. Bhabar. Common, autumn. Valley. Common. Frequent. 8 40 HIMALAYA X DISTRI CTS DIVISION I. — POLYPETALiE — ( continued ) . No Scientific name. Vernacular Note name. ORDc.lt 45.- — LEGUMINOSAL — (continued). Tribe Genisteae — (concluded). 11 Crotalaria (Calyeinie sessili flora Common. [anthylloides, Lam], 12 13 „ (Erectse)sericea „ (Kriocarpae) tetragona Gungri Valleys, common. 14 „ (Trifoliolatae) medicaginea, . . Very common. 15 )j j) mcana , . . ... Naturalized. Tribe Trifoltece. Section Digit ax®. 1G Trifolium pratense ... Cultivated ; rare. 17 „ repens • • • ,, common. 18 Parochetus cummunis [oxalidifolia. • • « Common, damp ground. Royle.] Section Pinnax®. 19 Trigonella Esenum-grsecum Methi Cultivated. 20 „ polycerata [incisa, Royle] • . • 21 „ gi-acilis ... July, on limestone. 22 „ pubescens ... Col. Davidson. 23 „ cornieulata • . i Frequent. 24 „ emodi Col. Davidson. 25 1 Melilotus parviflora Cultivated. 26 ,, alba Garila Common. 27 Medicago lupulina 28 „ denticulata ... yy ‘ Tribe Lotece. 29 Lotus corniculatus ... ... ] a « « Very common. Tribe Galeg-eze. 30 31 32 33 34 35 36 37 38 39 40 Cyamopsis psoraliodes ... Indigofera (Sphceridiophora) linifolia „ (Paucifoliolatae) trifoliata ... >> )j trita ,,, „ (MuUifoliolatge) hirsata ... „ Gerardiana [hete rantha. Wall. atropurpurea . . . pulchella [arb o- rea, Itoxb], „ „ Dosua [hetcran- tha, Wall. Colutea arborescens, var. nepalensis. V >5 Mellettia auriculata [Robinia macro- pbylla, Ro b], 41 T'ephrosia Candida Nana-sakina, Mus-sakina... Kala-sakina, Sakina Saki ma 42 purpurea Gojha Lehtia Bhabar. 5 ) yy Common. Very common, May. Common, August. Very common, March. Very common, May, June. Above 1 0,000 feet, J idy, August. Very common; valleys. May. Bhabar. Leaves used to poison fish. Bhabar. OF THE NORTH-WESTERN PROVINCES. 341 DIVISION I. — POLY PETALiE — (continued ) . No. Scientific name. Vernacular name. Note. ORDER 45. — LEGUMINOSiE — (continued). Tkibb Galkgehs (concluded). 43 Sesbania aegyptiaca Jait Cultivated. -44 Caragana pyginaea [Genista, versico- lor, Hoyle], Darna Common above 10,000 feet. 45 „ Gerardiana [Caragana spi- nosissiu a, Royle.] „ 8,000 feet, May. 4G .,, polyacantha 55 Rare. 47 „ brevi^pina 55 Common above 8,000 feet. 48 „ crassicaulis ... ,, ,, 12,000 feet. 40 Guldenstaedtia himalaica Dama ,, ,, 11,000 feet. 50 Astragalus (Pogonophace) trichocarpvs [sesbanoides, Royle], ... Common. 51 „ (Po.lolotus) hosackioides Common. 52 ., (Hypoglottis) himalayanus Above 10,000 feet. 6.1 ,, Maddenianus 55 55 54 „ leucocephalus Common. 65 „ (Phaca) chlorostacbys 55 56 Jf „ viir. trichocarpoides Kurz, . 4 4 W. Waterfield, Naini Pal. 57 ,, ,, emodi ... Above 10,000 feet. 68 „ gravcolens • . . . Frequent. 50 „ (Myobroma) Candolleanus Above 8,000 feet. 60 ,, (-ZEgacantha) polyaeantlms ► 9 Tribe IIedysarkae Section Exstipeleat/e 1 i requent. 61 Onobrychis sativa ... ••• • • • Cultivated. 62 Lespedesa (Eulespedeza) sericea ... Common. 63 Gerardiana, Very common. 64 ’’ (Oxyrambhis) macrostyla, ... Common. 65 ,, criocarpa ... . . . 55 Rare ; found by Stra- chey and Winter- bottom. 66 Hedysarum kumaonense ... 67 Zornia diphylla [angustifolia, D.C.] . . . Common. 68 Smithia sensitiva ... Bhabar. 69 geminiflora 55 70 ciliata . . . Common near streams. 71 JEschynomene indica Section Stipellateje. t t • Up to 4,000 feet. 72 Uraria picta ... ... Common. 73 ,, crinita 55 74 „ lagopus 55 75 pruned lie folia Valleys. 76 Alysicarpus (Microcalycinae) vagi- nalis. Common to 4,000 feet. 77 (Microcalycinae) bu- p'.eurifolius. » « • » 55 55 312 HIMALAYAN DISTRICTS DI\ ISION I. — POLYPETALjE— (continued). No. 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 Scientific name. Vernacular name. ORDER 45 — LE JrUMINOSiE — (continued). T KIBE H BDYSAREiE — (coiicl uded ) . Sectio < StipeeeatvE — (concluded). Alysicarpus (Microcalycinse) rugosus, Ougeinia dalbergioides [Dalbergia ou- jeinensis, Kcxb.] Desmodium (Phyll odium) pulcbelium, „ (Ptero'oma) triquetrum, ,, (Scorpiurus) laxiflorum, ,, (Polocarpiur) po !ocar- pum. „ (Dollinera) floribundnm [multifloru n D. C.] „ „ oxyphyllum [po'ycarpum, Wall.] „ „ tiliaefo’ium [nutans, Wall., argent eum Wall.] „ (Htteroloma) Gangeticum, lati folium ... sequax „ concinnum [penduliflorum, Wall.] (NicoVonia) polycarpum D C. [angulatum, Wall.] (Sagotia) triflorum 55 55 55 55 55 „ parviflorum ... (Pleurolobium) gyrans ... „ gyroh'es... Tribe Viciove. 96 Acrus precatorius 97 ,, pulchellus 98 Cicer arietinrm 99 .. soongaricum Rovle.] 100 | Vica (Ervmn) tetrasperma 101 „ ,, hirsuta 102 j „ (Cracca) tenera [microphyllum, 103 104 105 106 107 108 109 no in 112 „ ,, mollis ,, ,, pallida „ „ rigidula ... ., (Euyicia sativa Lathyrus (Ealathyrus) aphaca „ „ sativus „ „ spbsericus [an- gulatus, Royle.] „ (Orobus) lutens Pisum sativum ,, aivense S a indan asainda. Gunchi rakti, Laguli-imli, Chana Kuri Kur-kosha ... Ghora-kolon, Matar Ningla-koslia, Kolai Note. Common to 4,000 feet. Up to 4,000 feet, March. Bhabar. Common. „ Naini Tal. Rare. Very common, August. Common ; Binsar „ Very common, July. Va'leys. Frequent. 55 Common up to 7,000 feet. Very common, autumn. 55 Common. Bhabar. Bhabar and valleys, 55 Cultivated ; Bhabar. About 12,000 feet ; rare. Rare. In cultivated fields. Frequent ; Adwani, April. High levels ; rare. Common. F are. Cultivated. Common. Cultivated. Common. Frequent. Cultivated. Cultivated and wild. OF THE NORTH-WESTERN PROVINCES. 343 DIVISION I. — POLYPETALiE — {continued). No. | Scientific name. 1 Vernacular name. Note. ORDER 45.' — LEGUMINOSiE — (continued). '4'KIBE PhASEOLE®. Section Glycine.®. 113 Sbuteria vestita, var. involucrata ... Common. „ var. densifiora ... , . . Rare. 114 Dumasia villosa . . . Common. 115 Glycine soja [Soja hispida, Mcench,] Section Erythrine® Bhat Cultivated ; very common. 116 Mucuna atropurpurea Baldaka Bageshwar. 117 „ pruriens Goncha Valleys ; common, May. 118 Erythrina indica Rungra February ; Bhabar. 119 „ resupinata ... ... ... Frequent ; Hawalbagh, March and October. 120 „ suberosa Rungra March, up to 4,000 feet. 121 „ arborescens ... ... Section Galactie® August, common. 122 Spatbolobus Roxburghii [Butea par- Yiflora, Roxb.] Maola Bhabar. 123 Butea frondosa Dhak Up to 4,000 feet. 124 Butea superba • « » Near Taili Mainari hill Loch, Septem- ber. 125 Pueraria tuberosa Billi-kand ... Very common, March, April. 126 „ Stracheyi Section Euehascole. ®. Rare ; Kalimandi, 7,300 feet. 127 Phaseolus vulgaris ... Cultivated ; Bhabar gardens. 128 „ trilobus Chhihin „ Bhabar. 129 aconitifolius ... Moth „ Bhabar. 130 „ mungo Mung „ not common. „ var. radiatus Urd „ common. 131 „ calcaratu8 [torosus, Roxb.] Gurush „ and wild red and white varieties. 132 Vigna (Euvigna'i catiang [Dolichos sinensis, Linn.] Riansh „ common, three varieties. „ „ var. sinensis Lobiya 133 „ (Plectropis) vexillata [Pha- seolus angustifolius, Wall.] Ban-mung ... Very common, autumn. 134 Pachyrrhizus angulatus ... ... Cultivated; Bhabar, root edible. 135 Dolichos Lablab Shimi Gardens, cultivated up to 7,000 feet. 136 „ biflorus [unifiorus, D. C.] Gahat Cultivated up to 3,000 feet. 137 „ falcatus Gahatiya? ... Common. o4 No. 138 139 140 141 142 143 144 145 146 147 148 149 150 151 152 163 154 155 156 157 158 159 160 161 162 163 164 HIM A LAY AN DISTRICTS DIVISION I.— P0LYPETALJ3— (continued). Scientific name. Vernacular name. Note. ORDER 45.- — LEGUMINOSiE — (continued). Tribe Puaseoekae — ( concluded). Section Cajane/e. Atylosia (Atylia) mollis • • • Common. „ „ grandiflora . . . Rare ; Bageshwar. „ ., [Cantharo spcrmum] Common ; Bhabar and scaraboeoides. outer hills. „ „ platycarpa, Rare. Gajanus flavus Arliar Cultivated ; Bhabar. Eriosema chinense [Crotalaria tube- . . . Common; Simtotahill. rosa, Don.] Rhynchosia pseudo-cajan Sliiali, ph(i- sarpata. >> „ minima Low elevations; rare. „ himalensis ... J) Flemingia (Ostryodium) strobolifca, Very common. „ var. fruticulosa ... Ch^ppur i • ■ Rare. „ (Chalaria) paniculata ... At low elevations. „ (Flemingiastrum) con- Bhatua Common. gesta [semialata]. ,, „ var. nana . . . Common. „ (Rhynchosioides) vestita, Muskila Edible tuber ; com- mon. Tribe Daebergieae. Section Aeternifoliol a tje. Dalbergia Sissoo Sisu Bhabar and valleys. „ rimosa . . . 5) >> „ lanceolaria [frondosa, . . . Frequent. Roxb.] „ volubilis Bhatia Common. Pterocarpus marsupium ... Bijai-sal Near Barmdeo. Section OppositifolioeatjE. Pongamia glabra ... ... Pit papar ... Bhabar, April. Derris robusta Baro Up to 5,000 feet. Tribe Sopiioreao. Sophora mollis [Edwardsia mollis, Pahar-gungri, Very common, March. Royle], Tribe Caesaepinie^e. Csesalpinia [Guilandina] Bonducella, Karon j Up to 2,500 feet. „ [Poinciana] pulcherrima, Krishna chu- ra. G arden. „ „ sepiaria ... Aira Common. Parkinsonia aculeata Wilayati ki- kar. Introduced. Poinciana regia ... Gardens ; rare. OF THE NORTH-WESTERN PROVINCES. DIVISION I.— POLY PETALiE — (continued). N o. Scientific name. Vernacular name. Note. ORDER 45 , — L E G U MINOSFK — (continued). Tribe Gassier. 165 Cassia (Fistula) Fistula. Rajbriksh, ki- tota. ;i May, June, up to 4,000 feet. 166 „ (Senna) eccidentalis Banal’ Bhabar. 167 „ „ Sophera (purpurea, Roxb], ,, 108 „ „ Tora Common. 169 „ „ angustifolia [laiiceolata, Royle.] Sanna, mak- ki. Cultivated; Bhabas, 170 „ (Psilorhegma) glauca [arbores- cens, Roxb. Banar Bhabar. 171 „ (Lasiorhegma) Absus [cocci- nea, Wall.] Common. 172 pumila ... Silpatiya ... 173 „ mimosoides Very common. „ var. dimidiata )) Common. ... „ var. Wallichiana »> ” Tribe Amiierstic^e. ,, 174 Saraca indica [Jonesia asolta, Roxb.] 1 Tribe Bauhinieas. Asok ... Introduced ; Sitaban, Bhabar. 175 Bauhinia (Decindrse) racemosa [par- vifiora Vahl.J Amli Up to 5,000 feet, com- mon, April. 176 ,, malabarica ... Rare, October. Common, September. 177 ' „ (Triandrae) retusa [einargi- nata, Wall.] Kandla . . . 178 „ ,, Vahlii Main Very common, April, May. 179 „ „ purpurea Khairwal ... Bhabar and valleys, October. 1.80 „ (Pentandraj) variegata )9 Common, April. ... }} „ var. Candida, ... Tribe Mimoseas. 181 Entada scandens Rare. 182 Parkia biglandnlosa ... Cultivated ; Bhabar. 183 Leucaena glauca [Acacia frondosa,... D. C.] Lajwanti ... Common, valleys, July. 184 Mimosa pudica Naturalized, Bhabar. 185 „ rubicaulis [octandra, Roxb.], Tribe Acaciead. Agla August ; common up 4,000 feet. 186 Acacia (Globiferae) Farnesiana Wilayati babul. Bhabar and valleys. 187 ,, arabica Babul 188 „ eburnea Bhes Banks of streams. 189 (Snicatae) Catechu Kliair Very common; Bhabar. 190 modesta Philai Rare, Bhabar. 191 lenticularis Khain Barmdeo. 192 „ (Vulgares) concinna [rugata,D.C], Ban-ritha ... Bhabar. 193 „ Intsia [Csesia, Linn.] Katrar Very common, Bhabar. 194 „ „ pennata Agla >> 99 44 346 HIMALAYAN DISTRICTS DIVISION I. — POIATETALiE — ( continued). No. Scientific name. Vernacular name. Note. ORDER 45.— LEGUMIN0S2E— (concluded). Tribe Ingeie. 195 Albizzia (Multifoliolatae) Lebbek ... Tantiya, halsis Common, A p r i 1, June. 196 ., „ odoratissima Siris Bhabar, April, June. „ „ var. mollis JJ 197 „ ,, proccra Baro „ May 198 „ „ Julibrissin Lai siris Up to 5,000 feet. May. 199 „ „ stipulata [Smith- iana, Wall. ... Up to 4,000 feet, May. SOO „ Paucifoliolatae) lucida Bhabar, April. 201 Pithecolobium (Unguiscati) dulee ... Wibiyati imli, Dakhni babul. Gardens, Bhabar. 202 „ Clypearia) bigeminum ORDER 4G. — ROSACEJE Tribe Pruneje. Kachlora . . . Up to 3,000 feet, April. 1 Primus (Amygdal ns) per sica Aru Cultivated ; very com- mon. 2 „ (Armeniaca) armeniaca Cliuaru and zardaru. 3 „ (Cerasus) avium ... Cultivated up to 8,000 feet. 4 „ „ cerasus • • • 5 „ „ Jaequemontii Padam puya Rare, Malari, Edge- v r orth. 6 „ „ Puddum ... Very common, Novem- ber. 7 „ (Enprunus) communis var., domestica var. Bhotiya b a - dam. Cultivated ; Almora. Ladaki >> 8 „ (Laurocerasus) Pandus [cornu- ta, Royle], Jaman Common. 9 „ „ nepalensis >> About 6,000 feet. 10 „ „ undulata [caprici- da, Wall]. f) 11 Prinsepia utilis Tribe Spireze. Bekla, jhatila, Very common. 12 Spirasa (Ulmaria) vestita [Kamtschat- ica, Lindley. ... Above 8,000 feet. 13 „ (Aruncus) aruncus [triternata. Wall]. ,, (Sorbaria) sorbifolia ["Lindley and Wall.] ... „ 10,000 feet. 14 Dhaniyali ... ,, 8,000 „ 15 „ (Chamasdrya) bella Jhar Common. 16 ,, „ canescens [cunci- folia, Wall]. >) ••• }> 17 „ „ vaccinifolia Rare. OF THE NORTH-WESTERN PROVINCES. DIVISION I. — POLYPETAL2E — {continued ) . 347 18 19 20 21 22 23 24 25 20 27 28 29 30 31 33 34 36 37 38 39 40 41 42 43 41 45 46 47 48 V ernacular name. ORDER 4 6 . — RO SACEiE— (conti nued) . Tribe Rub.!::.®. 99 99 n 99 ?> 99 » 99 Rubus (Sinsplicifolias) calycinus [D.ili- barda calycina, D.C.] acuminatus paniculatus [ti 1 i a- ceus, Wall], „ moluceanus [rogosus, Smith]. „ reticulatus lanatus [tiliaceus, St. & VV.] (Digitatai) alpestris (Trifoliatse) saxatilis „ nutans ni vetis var. concolor maeilentus [as per Royle.] „ ellipticus [rotundi- folius, Wall; Gov- ry-phul, R o x b. flavus, Don.] (Pinnataa) biflorus lasiocarpus [rosadlo- rus, Roxb.] foliolosns •••- rosiefolius 99 99 99 99 99 99 99 Tribe Potkxtille^e. Geum (Engeuui) urbanum ... (Sievcrsia) elatum [Potentilla adnata, Wall]. Fragaria (Duchesnea) indica „ (Eufragaria) vesea [nub: col a. Wall] Potentilla (Sibbaldia) Sibbaldl n „ axillitlora „ (Trichothalamus) iruticosa ... „ „ ambigua „ eriocarpa ” (Enpotentilla) Mooniana [poly- pliylla, Wall]. dens, Wall]. 99 99 99 99 99 99 99 99 99 fulgens [splen- Leschcnaultiana, fragarioides ... peduncularis ... leuconota microphylla ... Lai hisalu Kala „ Lai „ Kala ,, 99 Lai liisalu,. . Pingla „ ganger. Lai „ Pingla „ ... 99 99 Hisalu Pingla hisalu, Kala ,, Safed „ ... Lai „ ... Kaphaliya Note. Rare. 99 Common. „ low levels. „ high levels. About 6,000 feet. Rare. Above 10,000 feet. Very common at high elevations. Very common. Common, China hill. March, very common. Fruit much eaten in April and May. Frequent. Very common, Blnibar, and up to 7,500 feet. Frequent. Rare. Common, above 8,000 feet. „ up to 8,000 feet. „ above 7,000 feet. „ Dakuri, at 10,000 feet. Rare. Above 12,000 feet. Colonel Davidson. Above 12,000 feet. High elevations. Common. Very common. Rare ; Malar i. Rare, high levels. 99 348 HIMALAYAN DISTRICTS DIVISION I. — POLYPETALiE — (continued}. No. Scientific name. Vernacular name. Note. ORDER 46. — R( JSACEiE — (continued). Tribe Potbntieeje — ( concl nded). 40 Potentilla (Enpotentilla) multiftda ... ... Rare, Niti pass, 1 6,000 fe t. 50 „ „ sericea • • • Rare, high elevations. 51 „ „ nepaslensis . r. Common. 6-2 „ „ argyrophylla ... . . • Rare. . . . ,, „ vur. atrosan- guinea. Common. 63 „ „ nivea ■ Rare, high eleva- tions. 64 „ „ Kleiniana « ' . Common. 66 « „ „ snpina Tribe PoTERrEiB. rr 56 Agrimonia Eupatorium Tribe Rose.®. ... Common, June, July. 6 7 Rosa (Eleutlierostylae) macrophylla, ... Frequent ; China and Binsar. 58 „ „ Webbiana ... Above 8,00o feet, com- mon. 59 „ „ sericea [tetrape- tala, Royle.] ... >> >> 60 ,, (Systylae) moscliata [Brunonis, Wall], Tribe Pome.®. Very common ; May- J une. 61 Cydonia vulgaris Bihi Cultivated up to 5, 000 feet. 62 Eriobotrya japoniea Loquat „ Bhabar. 63 Pyrus (Malus) malus Seb „ and perhaps wild. 64 yy IltlCCcltcl . ■ • , , a Ban meha.l . . . Com on ; sometimes cultivated. 65 „ (Eupyrus) communis Nashpati ... Cultivated. 66 „ „ Pashia [variolosa, Wall], Melial Very common. 67 „ „ kuniaoni Common. 68 „ (Aria) lanata ... Galion Above 8,000 feet, com~ mon. 69 „ ,, vestita ... Mauli Common. 70 „ (Sorbus) Aucuparia Above 12,000 feet. 71 „ „ foliolosa [ursina, Wall]. Salia halia... „ 8,000 feet, very common. 72 Stranvassia glaucescens [Photinia du- Garmehal, Very common about bia, Madden]. sund. 5,000 feet. 73 Cratasgus 0 xyacandtha ... Cultivated ; rare. 74 „ crenulata Gingaru Very common. 75 Cotoneaster (Planifolia) bacillaris ... Raus, rois ... Common. Walking sticks made of the wood. No. 76 77 78 79 80 81 1 2 3 4 F t h f < 1( 1 i: l OF THE NORTH-WESTERN PROVINCES. DIVISION I. — POL YPETALiE — (continued) . 349 Scientific name. Vernacular name. ORDER 46.— ROSACEiE- (concluded). Tries . Pomece (concluded), otoneaster (Planifolia) acuminata ... I Runs, rois „ multi flora ... nummularia . . . (Recurvifolia) microphyl- la. „ thvmifolia ... buxifolia Gat'i ORDER 47. — SAXIFRAGACEiE. Tribe Saxifrages. Btilbe ri vularis [Spiraea barbata, Wall], axifraga (Nephrophyllum) odonto- phylla. „ (Hirculus) palpebrata „ t , saginoidcs „ divtrsi folia ... „ (Boraphila) micrantha ... „ (Microphylla) imbricata „ (Spinulasse) brachypoda... ( „ flmbriata fillcaulis >5 V „ (Flagellares) Brunoniana, „ (Bergenia ligulata „ var. ciliata, Royle hrysosplenium (Oppositifolia) nepal- ciiBe. „ var. sulcatum, „ trichospermum, „ (Alternifolia) tenellum ... Parnassia nubicola Tribe Hydranges. Hydrangea (Truncate) altissima „ asptera „ (Coronata3)ves- tita. Deutzia corymbosa Silphora Note. Com m on . W alk i n g sticks made of the wood Rare ; Niti pass. Colonel Davidson. Very common every- where. Common. Bliujhata ... ,, Tribe Escaet.onies. Itea nutans Garkath Common. Above .10,000 feet. Rare ; found near Ra- lam at 13,000 feet. >> >> >5 )) ,, 10,000 „ 10,000 „ 12,000 „ 10,000 „ 11,000 .. „ 10,000 „ Pin- dar i. China peak. March ; very common. Very common. Common. Near Kedar Kanta. Common. „ staminea ,, macrantha ••• •• Phifadelphus coronarius, var. tomen- j Bukyal, dha- tosus. 1 niyali. Frequent. May, common, high elevations. May, very common. May, rare. June, frequent at high elevations. Wan. Common at low eleva- tions. 350 HIMALAYAN DISTRICTS DIVISION I. — POLYPETALiE — (continued ) . No. ! Scientific name. Vernacular Note. name. ORDER 47.— SAXIFRAGACEiE- (concluded). TllIBK RlBKSIJinS. 25 Ribes (Grossularia) grossularia • • • Common about 10,000 feet. 20 „ (Ribesia) glaciale [acuminatum, lvokaliya ... ,, above 10,000 Wall]. feet. 27 „ „ nigrum ... Paphar „ about 10,000 feet. 28 „ „ rubrum ... ?? y> ORDER 48. — CRASSULACE2E. Tribe Isostbmones. 1 Tillsea pentandra Common. 2 Crassula indica . . . Frequent, Gagar. 3 Cotyledon oreades ... Above 13,000 feet. Tribe Dipl'ostemonus opposjtifolia. 4 Bryopbyllum calycinum ... .?. . . . Bliabar ; introduced. 5 Kalanchoe spathulata [varians, Wall], Bakal patta, Very common. ' Goats poisoned by eating this plant. Tribe Dipbost emones alterkifolia. 6 Sedum (Rhodiola) Rhoiiola [rosea, Common above 12,000 Linn], feet. 7 „ „ crenulatum Frequent above 12,000 feet. 8 „ „ quadrifidum Common above 12,000 feet. 9 „ „ asiaticum „ above 11,000 feet. 10 „ „ linearifolium „ on trees. 11 „ „ trifldum [sinu- >> >> atum, Royle] ,, (Eusedum) rosulatu n September. 12 Coannon, April May. 13 Sedum [Eusedum) adenotrichum Co moil, April, and ,, „ trulUpetalum May. 14 Above 1 1 ,000 feet. 15 „ „ Ewersii [rubrum... Royle]. Frequent. 16 „ „ multicaule Com non, July. 17 Sempervivutn mucronatum Above 10,000 feet. 18 „ seloides ... „ 10,000 feet. ORDER 49.— DROSERACFiE. 1 Drosera Burmanni ... ... Bliabar. 2 „ peltata ... Very common. ( RDER 50. — HALORAGEJE. 1 My ri ophyllum spicatum ... « t > Naini Tal lake. 2 Call itriche verna ••• OF THE NORTH-WESTERN PROVINCES. 351 DIVISION I. — POLYPETALiE — {continued). No. Scientific name. Vernacular name. ORDER 51. — COMBRETACEiE. Trice Combretejb 1 Tcrminalia (Catappa) belerica Behara 2 „ „ Chebula Har, harira, 3 „ (Fentaptera) Arjuna [gla- bra, RoxbJ. Saj 4 „ „ tomcntosa 5 Anogeissus latifolius Bakla 6 Combretum (Poivrea) decandrum ... 7 „ (Eucombretum) nanum... Pharsiya ... 8 Quisqualis indica ... ORDER 52.— MYRTACEJE. Tribe Leptospermeje. 1 Eucalyp tus obi i qua Stringy bark, 2 „ globulus Tribe Myrteje. Blue gum ... 3 Psidium Guyava Amrdd 4 Myrtus communis ... ..« W i 1 a y a t i mendhi. 5 Eugenia (Jambosa) Jambos Gulab jaman, 6 „ (Syzygium) operculata Rai „ 7 „ „ Jambolana • Tribe Barringtonteje. Jaman. 8 Barringtonia acutangula ... 9 Careya herbacea Kumbh 10 ,, arborea ORDER 53.— MELASTOMACEiE. 1 Osbeckia chinensis [angnstifola,Don]. 1 Kukar-makri, 2 „ stellata 1 ORDER 54.— LYTHRACE^S. Tribe Ammanniete. 1 Ammannia (Rotala) peploides • » • 2 „ rotundifolia Darmiya . . . 3 „ (Euammannia) salicifolia, ... 4 „ „ senegalensis, • Note. Frequent ; G a n ai, March. Common np to 5,000 feet, April, May. Bliabar, April, May. Common up to 4,000 feet, April. „ onter range. ,, Feb., March. Bliabar; very common, March, April. „ gardens. Introduced. Introduced. Cultivated, up to 8,000 feet. Cultivated ; Bhabar. Bhabar. „ and valleys. Banks of streams ; Bhabar. Bhabar, Mat ch. Frequent, autumn. Common „ Rare. In damp places. Very common „ Bhabar swamps, and up to 4,000 feet. Frequent up to 5,000 feet. 352 HIMALAYAN DISTRICTS DIVISION I. — POLYPETALiE — {continued) . No. Scientific name. Vernacular name. Note. ORDER 54.— LYTHRACEAE— (concluded). Tribe Lytjireye. 5 Woodfordia floribunda [Grislea to- Dliai Very common, April. uietosa, Roxb.] 6 Lawsonia alba Mend hi Common gardens. 7 Lagerstroemia (Velaga) indica Gulbahar ... August, com m o n, gardens. 8 „ „ parviiiora ... Dhaura Very common, Bliabar. 9 ,, (Adambea) Elos-Reginae, Jaral Rare. Gardens. 10 Punica Granat :.m Darirn Very com ron up to 5,000 feet. ORDER 55.— ON AGE ACE JE. Section Polyspermeas. 1 Epilobium (Chamamerium) angusti- • • • Frequent. folium. 2 „ ,, latifolium High elevations. 3 „ (Lysimachion) Iprsutum, Common. 4 „ „ roseum Bhim Tal. 5 „ ., tetragonum . . . Naini Tal. 6 ,, „ laxum, Royle, 7 Aenothera rosea Naturalized. 8 „ nocturna )> 9 „ grandi flora Section Oeigosperma. 10 Circsea lutetiana [repens, Wall] Common. „ alpina [intermedia, Wall] ... ... ORDER 5G.— SAMYDACEA3. 1 Casearia graveolens Chila, c h i 1- Fruit used to poison ra. fish. „ tomentosa >> >> » » ORDER 57. — PASSIFLORACEiE. 1 Passiflora, species ... ... 1 Cultivated. ORDER 58. — CUCURBIT ACEAE. Section Sigmatoperze. 1 Trichosanthes palmata ... Indrayan . . . Common. 2 ,, cucumerina Bliabar. 3 „ anguina ... Chichinda ... Cultivated. 4 Herpetospermum caudigerum Rare. 6 Lagenaria vulgaris Lauka, lauki, Cultivated. tumri. 6 Luffa segyptiaca [pentendra, Roxb.] Ghia torai . . 7 „ acutangula [triandra] Torai 8 Benincasa cerifera Bhuja, petha, ‘ kumhra. 9 Momordica Charantia Karela i >> OF THE NORTH-WESTERN PROVINCES 353 DIVISION I. — POLYPETALiE — [continued). No. Scientific name. Vernacular name. Note. ORDER 58. — CUCURBIT ACE^E' — (concluded). Section Sigma toperje — ( conclnd ed) . 10 Momoi-dica dioica ... ... . . . Frequent. 11 Cncumis trigonns Airalu Common. 12 „ Melo [ufcilissimus, Roxb.]... Kakri Cultivated. 13 „ sativus Kakri, khira, 14 Citrullus Colocynthis Tarbuza Wild and cultivated. 15 ,, vulgaris 55 Cultivated. 16 Cephalandra indica £Coccinia indica, Kunderu . . . Bhabar. W. and A.]. 17 Cucurbita maxima Kadu Cultivated. Section Okthopeb.®;. 18 Bryonia laciniosa • . • Common. 19 Mukia scabrella . . • 20 Zelmeria umbellata Gwala-kakri, 55 „ var. nepalensis . . . 55 21 Melotliria odorata . . . Rare. 22 Edgaria darjeelingensis ... ... 55 23 Gynostemma pedata • t • 55 ORDER 59/ — BEGONIACEJE. 1 Begonia (Knesebeclda) picta . . . Common, autumn. 2 ,, (Trilobaria) amcena [tenella, ... 55 55 Don.]. * ORDER 60.— DATISCACEiE. 1 Datioca Cannabina 1 Bhang-j ala,.. Common. ORDER 61. — CACTACEiE. 1 Opnntia Dilienii Nag-phansa, Introduced. Common up to 6,000 feet. ORDER 62. — FICOIDE.ZE. 1 Trianthema crystallina • • . Bhabar. 2 „ pentandra ... 55 3 Mollugo stricta ... Common. ORDER 63.— UMBELLIFERiE. Section Hetekosciadj/e. 1 Hydr oco tyle j avani ca • . . Common. 2 „ rotundifolia . . . Rare. 3 „ asiatica Bhabar. 4 Sanicula europasa [elata, Don.] ... Common, June, Ban]- • • bagr. 45 354 HIM A' LAY AN DISTRICTS DIVISION I. — POLYPETALiE — [continued] . No. Scientific name. Vernacular name. Note. ORDER 63. — UMBELLIFERiE — (concluded). Section Ha nozicia. Tribe Ammine.®. 6 Yicatia coniifolia ,,, Khati Pindari, May. 6 „ Stewartii ... Rare, Garhwal. 7 Bupleurnm lanceolatum ... Common, June, Banj- bagr. 8 „ Candollii . .. Above 8,000 feet. 9 „ diversi folium . . . „ 7,000 „ Naini Tal, common. 10 „ falcatum, var. marginata, . . . 11 „ longicaule ... . . . Above 8,000 feet. Common. 12 „ tenue . . . 13 Carum (Glabrse) Carui ... ... Rare. 14 „ (Hispidse) Roxburghianum ... ... Cultivated. 15 „ „ anethifolium . . • Almora, common. 16 Pimpinella (Glabrae) achilleifolia ... ... Common. 17 „ [Reutera, Edgw.] acumi- nata. • • • Naini Tal, common. 18 „ [Acronema, Edgw.] tenera... • • • Naini Tal, on oaks, common. 19 „ (Papillosas diversifolia tri- foliata, W all. Dhanjari ... Very common. 20 „ „ Stracheyi . . . Rare; banks of Dhauli. 21 „ „ csespitosa ... 99 9} 22 Osmorrhiza Claytoni [laxa, Royle] ... ... Frequent. 23 Chaerophyllum villosum ... ... 99 „ reflexum ... Tribe Sbseeine;e. Rare. 24 Seseli trilobum Rare ; Niti and Milam. 25 Eaeniculum vulgare [panmorinm, Roxb.] Sonf Cultivated. 26 iEnanthe stolonifera ... Low elevations, com- mon. 27 Ligusticum marginatum ... Naini Tal, common. 28 „ elatum [Cortia elata, Edgw.] ... >> 99 29 Selinum tenuifolium [Selinum Can- dollii, Edgw.] ... Common. 30 „ vaginatum [Cortia vagina- ta, Edgw.] ... Frequent. 31 Cortia Lendeii . » . 32 Pleurospermum [Hymenolsena, D. C.] Govanianum. ... High elevations. 33 99 99 Candollii. ... 99 34 „ angelicoides „ ... Rare ; Ralam river, 11,500 feet. 35 „ dentatnm „ ... Frequent. 36 „ stel latum „ . * . Rare ; Milam glacier. 37 „ denBifiorum „ ... High elevations. No. 38 39 40 41 42 43 44 45 1 2 3 4 5 6 7 € 9 1 2 3 4 5 6 OF THE NORTH-WESTERN PROVINCES. 355 DIVISION I.— POLYPETAL2E— {concluded) . Scientific name. Vernacular name. Note. ORDEli 63.— UMBELLIFERiE — (concluded). Suction Haplozygi;e — ( concluded). Tribe Pectcedane.®. Peucedanum graveolens [Anethum sowa, Roxb.] „ Dhana Heracleum Brunonis „ candicans ... ., nepalense ... Sea Section Dipi/'ztgias. Coriandrum sativum Daucus Carota Caucalis Anthriscus Dhaniya ORDER 64.— ARALIACEiK. Section Imbricate. Aralia cissifolia „ cachemirica [Panax tripinna- tum, Wall.] Pentapanax parasiticmn • ,, Leschenaultii, var. urn- bellatum [Hedera f vagrans, Don.] [Panax brijugum, Wall.] Kot semal Cultivated, Up to 4,000 feet. Rare. Common. Frequent. Cultivated. » Very common. Rare. Pindar i, autumn. Up to 7,000 feet. Section Falvatje. ■Heptapleurum impression [tomento- sum, Don.] „ elatum ... venulosum [Hedera terebinthacea, Wall.] Hetoropanax fragrans [Panax fra- grans, Roxb ] Hedera helix, var. sesculifolia Banda ORDER 65. — 'GORNACEJE. Alangium Lamarckii [hexapetalum, Roxd., decapetalum, Wight]. Marlea bigoniiefoUa Cornus macrophylla „ oblonga „ nervosa, Royle „ capitata [Benthamiafragifera], Tumri Kagshi Bamaura Common. Rar^. Up to 3,000 feet. Low elevations, No vember. Very common. Bhabar, rare. March. Bageswar, May. Common, May. Frequent, September. Rare. Common. Fruit edible, summer. 356 HIMA'LaYAN districts DIVISION II.— MONOPETALiE. No. Scientific name. Vernacular Note. name. ORDER 1 . — CAFRIFOLIACEiE. Tribe Sami UCE2E. 1 Viburnum cotinifolium, Don. Gwiya Very common, June, 2 „ Mullaha, Don. [stellulatvm, Lai titmuliya, Common, July. Wall.]. 3 „ cylindricum, Don. [coriace- Kala titmuliya, „ January. um, Blume.}. 4 „ punctatum, Don. [acumina- tum, Wall.]. (Triloculares) nervosum, Don. [gran- ... Common, Binsar, July. 5 • . • „ Upper Sarju. 6 difiorum, Wall.]. „ erubescens, Wall.] ... Common, April- June. • Tribe Loxiceruo. M / Triostium himalayanum Dur-bank ... Above 8,000 feet. 8 Abelia tri flora Munri Common, June. 9 Lonicera diversifolia, Wall. [L. quin- quelocularis, Hard.]. Bhat-kukri, „ June and July. 10 Lonicera oriental is [Govaniana] . . . Rare; Bhatkot. June. 11 ,, alpigena[Webbiana, Wall.]... Nalkaru, kar- Rare ; Bindari, June.. 12 Leycesteria formosa [Lonicera quin- Common. Confused by quelocularis, Hard.]. naliya. Hardwicke w i t lx No. 10. ORDER 2. — RUBIACEJE. Tribe Naucle^e. 1 Anthocephalus (Nauclea) Cadanba, Kadam Cultivated, June. 2 Adina (Nauclea) cordifolia Haldu Common ; Haldvv a ni, Phaldu July. 3 Stephagyne (Nauclea) parvifolia „ Bhabar, June. Tribe Cinciionaceje. 4 Hymenopogon parasiticus Bhainai y a - On oaks at Binsar. 5 Hymenodictyon excelsum padera. 6 Bhalena Common, June. 7 ,, flaccidum Rare, June. Wendlandia exserta [W. cinerea Chilkiya ... Common, March. 8 Rondeletia exserta]. „ tinctoria ... ... Bhabar, February. Tribe Hedyotide;e. 9 Argostemma sarmentosum ... Frequent. 10 Hedyotis Lindleyana . . . Common. 11 ,, calycina 12 Oldenlandia Burmanniana 13 I „ (Kohautia) coccinea ... • f • 5‘ 14 1 „ gracilis • . . 15 „ stipulata . • . Rare. 16 Ophiorliiza nana 17 ,, Mangus • • • 18 „ bracteolata ... ... >> OF THE NORTH-WESTERN PROVINCES. DIVISION II. — MONOPETALiE — ( continued ). 357 No. Scientific name. Vernacular name. Note. ORDER 2 — EUBIACEH:— (concluded). 10 Tribe Gardenias. Gardenia turgida [longispina, Mad- Thanela Bhabar. 20 den.]. „ latifolia Pindalu ) T 21 Randia tetrasperma Bhotiya gin- Very common. 22 23 „ dmnetornm gar u and Bara gari. Mainphal . . . Bhabar. „ uliginosa Pindalu. >> 24 Tribe Knoxias. Knoxia mollis ... ... f , . • Frequent. 25 Tribe Ixoreas. Pavetta tomentosa [Ixora tomentosa, Padera Common. 20 Roxb ]. Colfea bengalensis, Kath jahi ... Frequent, March. 27 Tribe Pasderiao. Hamiltonia scabra, Dec. [suaveolens, Jogiya-padera, Common, November. 28 var. azurea, Wall.] Leptodermis lanceolata ... Padera Very common, summer. 29 Tribe Spermacoceje. - , Spermacocc articularis ... Common. 30 „ lasiocarpa [s t r i c t a, ... 99 31 Roxb] Tribe Gaeiaceas. Rubia cordifolia Majethi Common. 32 „ nervosa, Edge. ... ... Rare; Gangoli bridge. 33 ,, Munjista ... Rare. 34 i y alata • • ♦ • • * . . . 35 Galium asperifolium Kuri Common. 36 „ elegans jj 99 37 „ Hamiltonii [G. latifolium, Frequent. 38 Don.] ,, hirtifiorum [G. cilia turn, ?) ... „ Binsar. 39 Don.] ,, aparine. >) ... Introduced. 40 aspevuloide, Edge., [tricorne, Dr. Very com non ; above 1 King.] ORDER 3. — 'VALERIAN! Nardostachys grandi flora LA 5. 10,000 feet. Rare. 2 Valeriana Wallichii Shami Frequent. 3 „ Hardwickii [V. elata, Don.] Com on. 4 ,, tenera 9} ... Frequent. 358 HIMALAYAN DISTRICTS DIVISION II.— MONOPETALiE — ( continued ). No. Scientific name. Vernacular name. Note. 1 ORDER 4.— -DIPSACEA Morina Wallichiana [bre riflora, Common. 2 Edge.?] „ longifolia Above 10,000 feet. 3 Dipsacus strictus, Don. ... . . . China, 8,700 „ 4 ,, inermia Very common. 5 ,, levis? Narao Common. 6 Scabiosa Candollii ... „ May. 1 ORDER 5.— COMPOSITE Tribe Vernoniaceie. Vernonia (Stengelia) anthelmintica, 1. Rare ; autumn. 2 ,, (Tephrodes) cinerea Kalajira Very common up to 3 SJ „ va montana ... „ (Xipholepis) teres ,, 8,000 feet. Common. Col. Davidson. 4 Tribe Eupatori;e. Adenostemma viscosum, var. latifo- Common up to 2,500 5 lium. Ageratum conyzoides feet. Autumn, common up 6 Eupatorium longicaule ... ... to 6,000 feet. October, common. 7 Tribe Asteroide.*. Solidago virga aurea [Amphiraphis Summer, common. 8 pubescen' , D. C.] Dichrocephala latifolia ... ... >> 9 Cyathocline lyrata ... Common up to 4,000 10 Myriactis nepalensis [oleosa, Edgw.] feet. Autumn, common. 11 „ Wallichii [gracilis, Edgw.j ... JJ 12 ,, Gmelini . . . October, frequent. 13 Rhynchospermum verticillatum Naipala Autumn ; rare. 14 Callistephus chinensis ... Introduced. 15 Aster (Euaster) amellus ... . . . Aug., above 8,000 feet. 16 „ (Alpigenia) alpinus ... July, above 1 1 ,000 feet. 17 „ (Orthomeris) molliusculus ... ... May and June; fre- 18 „ „ altaicus quent. Aug., above 9,000 feet. 19 „ „ spartioides ... 20 ,, (Calimeris) peduncularis ... September, October ; 21 Erigeron canadense Sallo common. Introduced, but now 22 ,, acre [Roylei, D. C.] Mirch mul ... very common. May, August ; very 23 „ multiradiatum common. July, August ; rare. 24 J 25 Microglossa cabulica [Aster ferrugi- . . . Rare ; Badrinath. neus, Edgw.]. Conyza veronicsefolia September, common. 26 „ viscidula [polycephala, Edgw.], . . . Feb., up to 4,000 feet. 27 „ absinthifolia Very common, autumn. OF THE NORTH-WESTERN PROVINCES. 35 $ DIVISION II. — MON 0 PE T A LiE — ( continued ). No. 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 61 52 63 64 65 56 57 68 Sc'entific name. Vernacular name. )) ORDER 5. — COMP OS IT JE — (continued). Tribe Inueoide®. Blumea Wightiana „ lacera hieracifolia runcinata [laciniata, Roxb.], „ oxydonta Blumea densiflora Laggera alata Sphaerantlius hirtus [mollis, Roxb.], Eilago arvensis, var. lutescens Leontopodium alpinum ... Anaphalis cinnamonea ... triplinervis ... nubigena >> » >> mucronata tenella [contorta, Don.] margaritacea ... adnata araneosa var. semidecurrens Phagnalon niveum Gnaphalium hypoleucum „ luteo album Caesulia axillaris Inula [Corvisartia] Royleana „ (Bubonium) vestita nervosa [nitida, Edgw.] barbata (Cappa) Cappa Amdok Jhula, bokla, >) 5 ) 5 > cuspidata rubicaulis Vicoa indica Carpesium cernuum var. nepalense ... „ var. pedunculosum, Tamagari Note. Spring ; Bhabar. ,, very common. May, common. „ frequent. November ; Col. Da- vidson. October ; common. Spring ; „ Common. Above 12,000 feet. Autumn ; common. yy yy yy above 9,000 feet. yy above 12,000 feet. yy very common. yy Col Davidson. yy common. yy yy very common. June ; banks of Dhauli near Niti pass. Autumn ; very com- mon. „ common. October ; rice fields ; Ganai. Above 10,000 feet. Spring ; up to 3,000 feet. Autumn ; frequent. 5? yy November ; very com- mon. October ; common. March ; frequent. Common. Autumn ; common. 69 „ abrotanoides [racemosum. Wall], Tribe Heuanthoide.®. Autumn ; rare. 60 Adcnocaulon himalaicum * • • September ; rare. 61 Xanthium strumarium ... Up to 5,000 feet. 62 Zinnia elegans ... Naturalized. 63 „ multi flora ... yy 64 Seigesbeckia orientalis ... Gobariya . . . October ; very com mon. 360 HIM A' LAY AN DISTRICTS DIVISION II. — MON OPETALiE — ( continued ). No. Scientific name. Vernacular name. Note. 65 ORDER 5.— COMPOSITE— (cc Tribe II e bi a n t ii oide ns — (con Eclipta alba, var . erecta ... mtinued). eluded). Common. GG ,, ,, prostrata Blainvillea latifolia Karshaniya. . . )9 Very common. 67 Wedelia biflora ? Rare 68 Coreopsis (Calliopsis) tinctoria Naturalized. 69 Bidens (Platycarpaea) tripartita June, October ; com- 70 [repens, Don.] „ (Psilocarpaea pilosa mon. Very common. 71 >, „ d 2 composita, 7 2 Giossogyne pinnatifida . • • Low elevations. 73 Chrysantheilum indicum , , , September; introduced. 74 Galinsoga parviflora • • « 99 75 Tribe Helehioid eje. Tagetes patula ... Gardens and natural- ?S „ erecta ... ized. >9 77 Tribe Anthemiders. Achillea millefolium, var . cuspida- Rare. 78 ta, Wall. Allardia tridactylites ? Above 15,000 feet. 79 ,, tomentosa Contula anthemoides ? ... • • • Above 12,000 feet. 80 ... February ; rare. 81 Tanacetnm longifolium ... • 8 ■ September, about 82 Artemisia (Dracunculus) scoparia ... Jhao 11,000 feet. October, common. 83 » „ parviflora... • • • 84 „ (Abrotanum) vestita Deo pati ... September, October ; 85 » ,, vulgaris [in- Pati rare ; Jageswar. September, October ; dica, Roxb.] >, „ var . hypoleu- • • • very common. Common. 86 ca, Edgw. „ (Absinthium) sicversiana, About 12,000 feet; 87 Tribe Senecienidrs. Tussilago farfara Jhelam. Common; banks of 1 88 Doronicum Roylei [Fullartonia Ru- streams above 10,000 feet. High elevations. 89 maonensis, D.C.] Gynura nepalensis, var . Tliomsoni ... March, common, Rani- 90 Emilia sonchifolia bagh. Very common. 91 Senecio (Synotis) alatus... . . . October, November ; 92 „ „ densiflorus • t • Pindari, China hill. October to April; very 1 ! common. No. 93 94 95 96 97 98 99 100 101 102 103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 181 119 120 121 122 123 124 125 126 127 OF THE NORTH-WESTERN PROVINCES. 361 DIVISION II. — MONOPETALiE — { continued ). Scientific name. Vernacular name. ORDER 5 . — COMPOSITE — (continued). Tribe Seneciejiid as.— (concluded). Senecio (Synotis) rufinervis ,, Kunthianus )> >> „ Candolleanus (Eusenecio) gracUifior m, ... ,, chrysanthenoides, „ pallens [violancus, Wall]. (Ligularia) sibiricus „ arnicoides Caealia) quinquelobus Tribe Cynaroidejs. Ecliinops niveus Carduua nutans Cuicus arvensis „ eriop'iorus vur. involucratus, „ ferox, Edgw. „ argyracanthus ... „ vur. nepalensis ... „ W allichii (arachnoidea, W all), Saussurea (Bracteatas) obvallata » » 5> (Acaules) Kunthiana (Congestas) gossypina (sacra,’ Edgw). „ grammifolia ... (Coarctatse pterocaulon . . . (Corymbosas) candicans ... „ vur. scaposa. >> » JJ albescens . . . denticulata, hypoleuca ... Jurinea macrocephala (Dolomiaaa ma- crocephala, D. C.). Serratula pallida TricholepiB furcata „ elongata Volutarella divaricata ... Carthamus tinctorius Rat patiya Kanaila, jao- ltanda. Kanwal Kala tagar . . . Kusarn TRIBE MUTISIACEJE Section Sub2E qu a eii'lo raj . Leucomeris spectabilis ... Ainsliaea pteropoda „ aptera Note. November, frequent. September, above 10,000 feet ■5 n October, high levels. „ Pindar i. March, June, very common. September, Pindari. r> ’*> Above 10,000 feet. Very common. Above 8,000 feet, Jhe- lam near Niti. Rare. Autumn, common. May. common. June common. October, common. S> September, above 10,000 feet. September, common above 10,000 feet. „ about 10,000 feet. „ about 10,000 feet. Very common. Common, April, Pan- wa Naula. September, frequent. September, common. » >> Pindar i. May, June, very com- mon. November, Pindari. October, common. March, Haldwani. „ Cult i v a t e d, Bhabar. May, common. Spring, very common. )> >> 46 362 ’HIMA'T.AYAN DISTRICTS DIVISION II. — MONOPETALuH — ( continued ). No. Scientific name. Yernacular name. Note. ORDER 5.-- COMPOSITE— (concluded). Section Labia tjefeorje. 128 Gerbera lanuginosa (Chaptalia gos- sypina, Royle). ... June, high elevations. 129 „ nivea . . • September „ 130 „ macrophylla (Chaptalia max- ima, Don). Tribe Ci chora ceze. 131 Cichorium intybus Cultivated. 132 Picris hieracioides ... Mai pat near Lohaghat, October. 132 Crepis (Barkhausia) fastida ... May, Jime, very com- mon. 133 (Yonngia) lyrata [runcinata Wall], ... Very common. An Lactcca ? 134 Taraxacum Dens leonis . • . Very common. -> >) High elevations. ... ,, v ar. eriopodium . . . ... „ var. parvulum . . . 135 LacVca (Brachy ramphus) obtusa ... Jangli gobhi, April, May, very com- mon ; yellow. ,, [Microrhynchus nudicaulis and patens, D.C.] ... 136 ,, (Scariola) scariola ... Low elevations ; yellow. ... „ „ var. sativa Cultivated 137 „ (Cicerbita) auricnlata ... May, July, very com- mon ; blue. 138 ,» „ longifolia ; October, fields, com- mon; blue. 139 „ (Lactucopsis sagittarioides, ... February, common ; blue. An Crepis ? 140 „ „ Brunoniana [Prenanthes Brunoniana, D.C.] • • • August, October, com- mon ; blue. 141 „ (Melanoseris) hastata ••• Autumn, common, Loh- ba ; blue or white. 142 „ „ laevigata [macror- hizon, Royle.] ... September, very com- mon ; blue. 143 „ „ violaefolia ... September, high ele- vations ; blue. Common, October ; blue. 144 „ „ Lessertiana • • * 145 „ „ dubyasa [Dubyaea hispida, D.C.] V. September, very com- mon ; yellow. 146 „ (Ixeris) glabra ... Winter, low eleva- tions ; yellow-. 147 „ „ polycephala 148 Prenanthes hispidula Rare. 149 Sonchus asper Ufat kancla nalslia. Spring, very common. 150 „ oleraceus Spring, common, edi- ble. 151 „ arvensis >> Spring, common. 152 Miclirorhynchus secundus Rare ; Royle. 153 Tragopogon junceum * * * June, July, very com- mon. 63 44 • e> t jk w bS r* 0O <4© Or ^ bi OS bS t)F THE NORTH-WESTERN PROVINCES. DIVISION II. — MONOPET ALiE — ( continued ). 363 No. Scientific name. Vernacular name. Note. ORDER 6. — LOBELIACEiE, 5 Lobelia trigona, Roxb., [trialata, Don,] pyramidalis, Wall rosea, Wall Common. Frequent. Rare 5 Malwa Tal. ORDER 7. — CAMPANULACEiE. Cephalostigma hirsuta ... Wahlenbergia viridis, Edgw. „ agrestis ... Gol ghanna, Campanula latifolia „ sylvatica [integer r i m a Don]. „ canescens „ argyrotricha [pa 1 1 i d a, Madden]. , color ata ramulosa, Wall]. ORDER 8.— ERICACEAE. Gualtherla nummular i a ... Bhalu bor ... trichophylla ... Andromeda (Bieris) ovalifolia, [A. capricida,’ Don.] (> (Cassiope fastigiata [A cupressiformis, Wall]. Rhododendron arboreum ... „ vai. roseum „ campanulatum „ anthopogon „ lepidotum ... Aiyar Kamba Burans Chimul Talisfar Frequent. Wacham.near Pindari. Frequent, Banks of Kosi. Rare. Common under trees. Very common. )> Rare. Common, Dakuji, Bhatkot. Frequent, above 10,000 feet. Very conmon. Milam and Pinda r i , 12,000 feet. Very common. Abov 8,000 feet. „ 10,000 „ ,, 12,000 ,, „ 12,000 ,, l ORDER MONOTROHEJE. Monotropa nepalensis Chhao Binsar, Septem b e r 5 found by Mrs. Go- van. ORDER lO.-LENTIBULARIiE. 1 Utricularia flexuosa [stell a r i s , ... Wight]. 2 Pinguicula alpina ORDER 11.— PRIMULACJE. 1 Primula (Sphondylia) floribunda ... 2 „ (Primulastrum) petiola r i s [nana, Wall]. 3 „ (Athritica) purpurea Common. Rare. Down to 2,500 feet. Above to 10,000 feet. >7 364 HIMA'LAYAN DISTRICTS DIVISION II. — MON OPETALiE — ( continued ), No. Scientific name. Vernacular name. Note. ORDER 11. — PRIMULACEiE — (concluded). 4 Primula Stuartii 5 » (Alcuritia) speciosa Bisb lcopra... Common. 6 „ involncrata Above 10,000 feet 7 ,, denticulata, var. erosa ... Common, high eleva- 8 Androsace sarmentosa, Wall tions. 5) „ lanuginosa, Wad ... Above 12,000 feet. 10 ,, rotundilo ia, Hardw. ... Common. M incisa Wall,. [rotundi folia, . . . Valleys and Bbaba r ~ 12 Don]. Lysimachia (Epliemerum) lobclioides. ... winter and spring. Very com on above „ pyramiflalis 10,000 feet. 13 ... Common. 14 „ (Lysimastrum) alternifolia. . . . . . 15 „ debilis 1C Anagllis arvensis, var. coerulea Samolus Yalerandii Junk-mam ... 17 ... >v Rare, Sual river. ORDER 12. — MYRSINACAE. 1 Miesa (Baeobotrys) indica ... i Kalsis Common. Low eleva- tions 2 „ argentea Phusera Frequent, Binsar. S Myrsine africana Pahar i cha, Common, March., „ semiserrata baiberang, 4 Chupra 5 „ acuminata 6 Embella r tbusta Baiberang ... Bhabar. 7 Ardisia fioribunda Rare. ORDER 13.— SAPOTACEiE 1 Bassia butyracea ... ... i Cliiura and Common at 4,000 feet,. „ latifolia phaiel. near Petoragarli. 2 Maiiua Bhabar. ORDER 14.— EBENACEiE. 1 Diospyros Melanoxylon ... ... Tendu Bhabar. 2 „ montana Ten du 3 „ lancesefo'ia Ardinia Kota Din. 4 „ Embryopteris Oab Bhabar. ORDER 15. — SYMPLOCE-dS. 1 Symplocos (Hopea) saicata L rdh, bholya, Bar ndeo, November. Rate,. Si a hi devi. 2 ,, sumuntia . . . 3 „ racemosa Bhabar, November. 4 „ ramosissima [nervosa. . M Rare, Gagar, Binsar. Madden.] May. 5 „ (Palura) cratoegoides [S. Lodli Very common, June paniculata, Madden]. and July. OF THE NORTH-WESTERN PROVINCES. 365 DIVISION II.— MONOPETALiE— ( continued). No. Scientific na e. Vernacular name. Note. 1 ORDER 16. -OLEACEiE Fraxinus excelsior i. Align Common. 2 ,, (Ornus) fioribunda Angu Common. 3 Syringa emodi Ohia Common, above 10,000 4 Olea cuspidata [ferruginea, Royle III.] Kalap briksh, feet. Fatal debi near Alrno- 5 „ acu ■ inata var. longi- Silang ra. Very common, wild 6 folia. ,, glandulifera Gair and planted. Com . on. 7 Ligustram nepnlense ... Banks of streams, May, 8 „ b acteatum ... . . . Frequent, Binsar, June. 2 ,, robustum ... Common, May. 10 „ compactum ... ... >> 1 ORD.R 17.— JASMINEH Jasmnum (Simplicifolise) Sambac ... L Cultivated. 2 ,, pubtscens . . . Frequent, Ganai. 3 ,, arborescens ... . . . „ Bhabar. 4 ,, nepaiense [dicliotomu n Jahi Common. 5 Don]. ., (trifo ia3) dispcrmum Surmali. Common. Leaves, gen- 6 Jasminmn (Alternifoliae) revolutuin Sonajahi ... erally trefoil, but sometimes sin pie and sometimes pin- nate. Common. 7 f chrysanthemum, Roxb ] „ „ pubigerum ... Chambeli . . . Rare. 8 (Pinnatifoiias) otlicinale, Introduced. 9 „ „ grandiliorum, Chambeli and jahi. Common. 10 Nyctanthes Arbor-tristis Parijat, har- 11 Schrebera swietenoides ... singhar of plains. Moka Bhabar tree. 1 ORDER 18 .— APOCYNACEiE. TRIBE CARI8SE2E. Carissa diffusa ••• ••• | Timukiya ... Bhabar. 2 TRIBE PlUNERIEJE. Tabernsemontana coronario ! Chandi 3 Vinca pusilia [V. parviilora, Roxb.J... I 99 4 Tribe Pars nsie^e. Vallaris dichotoma | Dudhi Common. 5 Tribe WRiGHTtEns. Wrightia mollissima i Darliela ..." 1 99 366 HIMALAYAN DISTRICTS DIVISION II. — MONOPETALiE — {continued ). No. Scientific name. Vernacular name. Note. ORDER 18.— APOCYNAC.'JE- (concluded). Tribe Alstoxiebs. 6 Alstonla scholaris Bhabar. 7 Blabeaspus l. cidus Dudhi Common, Tribe Echiteae. 8 H olarrhena antidysenter ica Kuer HA „ pubescens . . • Neriutn odorurn Kanyur Cnonemorpha macrophylla, [Echites Garbadru ... Bhabar. macrophyl'a, Roxb.] Ichnocarqus frute scens ... Dudhi Common, ORDER 19. — A SCLEPIADEJE. TiilBE PeRIPLUCKAB. i Cryptolepi s reticulata Rui kosa ... Up to 4,000 feet 2 Periploca calophylla [Streptocaulon Dal bhengla, Common. calophyllum, Wright.] Tribe Asceepiadeas. s Vincetoxicum canescens [Cynanchum Common, glaucum, Wall. J 4 „ montanum [V. kuna- • • • Frequent. warense, Madden.] 0 Calotrepis gigantea Ak, madar ... Common, Bhabar. 6 „ procera [Hamiitonii] Rare, Bhabar. 7 Cynauchum iialhousiie ... Frequent. Tribe Stapeliie. Sub-tribe Pergulariae. 8 Tylopliora tenerrin a Frequent. 9 „ Goxanii [Tphisia Govani- ana, Wight.] 10 Maradenia Roylei Murkila Common. 1.1 „ lucida, Edgw. Dudhi Frequent. 12 „ tenacissima ... Up to 4,000 feet. IS Pergnlaria pallida Surkila Common, Bhabar. 14 Gongronema nepalense ... . . . i ... Frequent on rocks. Sub-tribe Ceropegibs. 15 | Orthanthera viminea Chapkiya ... Bhabar. J 6 Hoya lanceolata . . . Common, Bhabar, and 17 Oeropegia longifolia up to 7,000 feet. Rare. 18 „ Wallichii • • • F requent. 19 „ gracilis, Edgw. ... yf OF THE NORTH-WESTERN PROVINCES. 367 DIVISION II.— MONOPETAL2E— ( continued No. Scientific name. Vernacular name. Note. ORDER 20. — LOGANIACEiE. 1 Gardneria ovata Banjahi Frequent. :2 „ angiiBtifolia ... 11 3 Buddleia crispa [paniculata, Roxb.]... Dhiriya, bhati, Common. dhaula. 4 „ asiatica [neema, Hamilton], ... 11 ORDER 21.— GENTIANACE2E. Tribe Chironie;e 1 Exacum tetragonnm ... ••• 1 Uda, titkana, Frequent, Bageswar. Tribe CHLORas. 2 Pladera pusilla . . . Common. •8 Canscora diffusa [virgata, Roxb.] . . ... Bhabar. 4 „ decussata ... 11 Tribe Swertice^e. 5 Gentiana (Chondrophyllum) pedicil- ... Common. lata. 6 „ capitata ... 11 7 „ aprica ... Bhabar. 8 decemfida ... ■ ... Common. 9 „ marginata ... 11 lO Ophelia pan'culata Chiretta Tit- kana. Autumn annual. 11 „ purpurescens 11 11 11 12 „ cordata 11 1> 11 13 var fioribus dilute roseis ... ... W. Waterfleld, Naini Tal. 14 (Agathotes) angustifolia ... 9l Autumn annual. 16 „ chi rata 11 „ perennial. 16 ” „ alata 11 ,, annual. 17 Halenia elliptica ... Above 10,000 feet. 18 Swertia cuneata ... Rare. 19 casrulea 11 20 speciosa [perfoliata, Royle], Simariya ... Common, above 10,000 feet. ORDER 22.— BIGNONIACEiE. 1 Calosanthes indica Pharkath . . . Bhabar. 2 Millingtonia liortensis [Bignonia sub- erosa, Roxb], Nim chambeli Introduced. 3 Stereospermum [Bignonia, Roxb.] sua- veolens. Patal Bhabar. 4 Amphi come arguta ... Banks of Patalganga. 6 Tecoma undulata * * * Ganai valley. May. 368 tiimXlayan districts DIVISION II. — MONOPETALiE — ( continued ) . No. Scientific name. Vernacular name. Note. ORDER 23. — PEDALIACEiE. 1 Martynia proboscidea [ M. diandra, Naturalized. Madden]. 2 Sesamum indicum Til >5 3 Pedalium murex. Gokhru Bhabar. ORDER 24.— CRYTANDRACEiE. 1 Lysionotns ternifolia [L. serrata, Common up to 4,000 Don]. feet. 2 Didymocarpus subalternans Rare. 3 ,, aromatica Frequent. 4 „ (Acau'.es) macrophylla Pathar laung, Common. 5 ,, pedieillata Bhabar. 6 „ lanuginosa . . • Common. 7 Chirita Edgeworthii Sankh pushpa, >> 8 „ bifolia 9 Rhynchogiossum obliquum [Wulfenia „ up to 6,000 feet. obi i qua, Wall], 10 Platystemma vio’oides ... • . « Common. 11 iEschynanthuB Perottetiana « . . Bhabar. 12 „ grandiflonis • • * Ear silang. October. 13 Polyneuron dimidiata ... Col. Davidson. ORDER 25. — POLEMONIACEiE. 1 Cyananthus lobata • • • Pindari, above 10,000 feet. 2 „ integra ... Ivedar 12,000 feet. ORDER 26.— CONVOLVULACEiE. Tribe Argyreiete. 1 Rivea ornata • * • Bhabar. 2 Argyreia speciosa ... 3 , setosa ... Sarju, bank near Kap- 4 „ capitata ... kot, September. Tribe Convolvuli:.®. 5 Quamoclit vul garis Bhabar. 6 Batatas pentaphylla • . • 7 Pharbitis Nil Baunra Very common. mr. intergrifolia [caerulea, Roxb.] )) Common. 8 Calonyction sped osum Bhabar 9 Ipomiea vitifolia 10 „ Pes-tigridis 11 „ Pilosa Kota Dun. 12 „ sp. [hirsuta, Madden] OF THE NORTH-WESTERN PROVINCES. 339 DIVISION II. — MONOPETAL — { continued ). No. Scientific name. i Vernacular name. Note. ORDER 26.—* CONVOLULACEJS— (concluded). Tribe Convolvulus — ( concluded). 13 Ipomoea’ sessiliflora [ phaerocephalus, Roxb.] ... Very common. 14 „ chryseides [muricata, Mad- ... Bhabar. 15 clenj. Aniseia barlerioides Kosi bank, Khairna. 1 6 Convolvulus pluricaulis Bhabar. 17 ,, arvensis [Malcolini Roxb.] ... Naini Tal, Mr. Water- field. 18 Porana racemosa Maseti Common. 19 ,, paniculata >> ... 5) 20 Evolvulus alsinoides [sericea, Madden], Tribe Cuskntes. Very common. 21 Cuscuta reflexa [verrucosa] Akash leguli, Common. 22 „ macrantha [ grandiflora, Wall], ORDER 27.— BORAGINAC Tribe Cordies. J ? EiE. i requent. i Gynaion vestitum Pyu Common up to 3,000 ft. 2 Cordia latifolia. Roxb. Borla Bhabar variety. 3 „ Myxa, Linn. Tribe Eiiretics. Kodah Common. 4 Ehretia serrata Panya Common, April 5 ,, lasvis Kodak ,, Bhabar, March. 6 viminea [Rhabdia sericea ... Madden], Tribe Heliotropes. „ in river beds. 7 Heliotropium strigosum [brevifolium Wall]. Tribe Borages Sub-tribe Echies. Common. 8 Macrotomia Benthami ... ... I Sub-tribe Lithosi ermes. Badri nath. 9 Onosma echioides • • • Above 10,000 feet. 10 MyosotiB pallens » • » „ „ Chau- patta. 11 „ longiflora ... >> 12 Bothriospermum tenellum [Cynoglos- sum prostratum, Don], Rare, Binsar. 47 370 hima'layan districts DIVISION II. — MONOPETALiE — ( continued }. No. Scientific name. Vernacular Note. name. ORDER 27. — BOR AG IN ACEiE — (concluded). SU3-T3IBE CTNOGLOSSE-aE. 13 Eritriehium rotundifolium Above 10,000 feet ; rare 14 Echinospermum gloehidiatum [Cyno- Kura yy yy • r > glossum uncinatmn, Royle], 15 Cynoglossum furcat um rr Very common. 16 „ micranthum [canescens. yy yy )> Wall]. 17 „ glochidiatum Frequent. 18 Trichodesma indieum ! Common. ORDER 28.— SOLANACEJE. Tribe Sobane.®.. 1 Lycopersicum eeculentum Wilayati bai- Cultivated. gan. 2 Solanum (Pachysteraon) tuberosum... Alii 3 „ Roxburghii [rubrum] Chhota ghi- Common. wain. 4 „ verbasc'. folium Ushita 5 „ (Leptostemon) indieum Kant kari . . . C „ xanthocarpum ,, var. Jacquinii ... „ var. Schraderi [diffusum]. ... • • • 7 ,, esculentum [melongena], ... Bai gan Cultivated. 8 Capsicum frutescens Lai mirch ... 9 Nicandra physaloides ... Introduced. 10 Physalis peruviana ... yy Tribe DATUREns.. 11 Datura Wall i chi i [ferox. Madden] ... Kala dhatura, Valleys. 12 „ var. double Cultivated. ,, alba ... Dhatura Very common. „ var. double ... Cultivated. Tribe Nicotian*:.*. 13 Nicotiana Tabacum ... ... j Tamakn Cultivated. 14 Petunia Phoenicea ... ... ... Introduced. . ORDER 29.— SCROPHULARIACEJE. Tribe A ntirrhinieae. 1 Verbasc um Thapsus Ekalbir Common. 2 3 Ceisia coromandeliana ... Linaria ramosissima Rare, valleys. Common. 4 ,, incana 5 Antirrhinum orontium . yy ,, May fields. Above 12,000 feet,. ‘1 Scrophularia Edgeworthii ... 7 8 9 10 11 12 13 34 15 1*6 17 1.8 19 20 21 22 23 24 25 26 21 26 2 ! 3< 3 3: 3 3 3 3 3 3 3 4 4 ‘OF THE NORTH-WESTERN PROVINCES 371 DIVISION II.— -MONO PETALS — ( continued ), Scientific name. Vernacular nanae. )RDER 29 .— SCEOPHULARIACEJE— (continued) Tkibe Aktirhinijb — ( concluded). Gajaila icrophularia polyantha ... ,, himalensis ... ,, obtusa (Madden) limulus nepalensis ,, gracilis dazus surculosus ,, rugosus jindenbergia grandiflora „ urticaefolia [Stemodia ruderalis, Wall]. ,, macrostacliya [jimnophila ment hast rum „ liypevici folia Herpestis Monnieria L'orenia cordifolia Vandellia Crustacea [pedunculata, Madden]. ,, nummulari folia Bonnaya brachiata „ grandiflora Tkibe Rhina.ntuiuk. Hcmiphragma heterophyllum .j. Digitalis purpurea ... ' Wulfenia Ainherstiana [Fsederota Amherstiana, Wall]. Veronica (Beccabunga) himalensis [grandiflora, Wall], n anagallis punctata „ (Chamasdrys) de’.iigera „ laxa... var. of V. chamaedrys? (Ompha’.ospora) biloba 99 99 99 99 „ ,, Maddcnii Edge. ... „ „ agrestis... Buchnera hispida Striga hirsuta ,, var. lutea „ euphrasioides ... Leptorhabdos parviflora [Gerardia and Sopubia parviflora], Sopubia trifida Centranthera hispida ,, var. nepalensis Euphrasia officinalis Note. Jangli sonf... 97 Jal nun Common. 79 Frequent. Common. F requent. Common. Very common. Rare. Common. Very common. August. Frequent. September. Common at’ 10,000 feet, Dakuri andDyurital. Introduced. Common near water above 8,000 feet. Above 10,000 feet. Up to 5,000 feet. 77 Common. Above 1 1 ,000 feet. Kedarnath. Common at 5,000 feet. March. 99 99 Grassy slopes at 6,000 feet. Bageswar. Frequent. Above 7,000 feet. 4f 46 1 2 I 2 3 4 5 6 7 8 0 10 11 12 13. 14 15 16 17 HIMALAYAN DISTRICTS DIVISION II. — M ON 0 PE T ALiE — ( continued ), -> Scientific name. Vernacular name. Note. ORDER 29. — SCROPHULARIACEJE — (concluded). Tribe Ruinanthe^s — ( concluded). Pedicularis ( Cyc'ophyllum ) pecti- nata. n „ porrccta, „ [elegans, Madden] „ ( Siphonatus ) megalan- tha. >> (Edentual) carnosa Frequent. yr yy Above 10,000 fectJ Common. ORDER 30. - OROBANCHEACEiE. Phelipoea aegyptiaca ... I jEginetia i'ndica ... ! ORDER 31 .— AC ANTE AGILE Tribe Thunbergie.®. Hexacentris coccinea ... j Ivaljug Rare. Frequent, Bageswar, Bhabar and valleys. Wiu.cr. Tribe Htgroriiieeje. Hcmiadelphis polysperma .... 1 Tribe Ru.j.ekge. Bhabar. Petalldium barlerioides Hemigraphis latebrosa, latebrosa]. TEchm anther a Walli ehii na, Madden]. [Ruellia [gossypi- Bakraola Jaundela Goldfm Strobil; n pentsteinenoides es auriculatus Wallichii Tilkapuri ... attenuates glutinosus Kapur nali . . . Common. Very common. From this bees make the best honey. Frequent. Bhabar. Above 10,000 feet. Common. >> Tribe Barlerieas* larleria dichotoma „ nepalensis ,, ciliata (rosea) ,, cristata itpidagathis hyalina „ ustulata „ cuFpidata Sarp jiba Frequent, September. yy Common. yy About 4,000 feet. Common. OF TIIE NOIITH-WESTERN PROVINCES. 373 DIVISION II . — MONO PE TALiE — ( continued ). No. Scientific name. V ernacu’ ar name. Note. 18 ORDER 31.— ACANTHACIUE— Tribe Justices. Rhlogacanthus thyrsiflorus (concluded). Bhabar and valleys. 10 Erantliemum nervosum common. March Bhabar and up to 6,000 20 Rostellularia procumbens feet. May, Very common. 21 Adliatoda vasica [Justicia Adhatoda], Bashang. Arus Common. 22 Rungia parvifiora of plains. >> 23 Dic'.iptera Roxburgliii ,, up to 5,000 feet. 24 Reristrophe speciosa Bhabar. 25 ,, bicalycu'.ata . . . 26 Rliaphidospora ciliata Rare, Vishnuganga. 1 ORD ER 32.— PHR Y MAC EVE. Phryrna leptostachya ... 1 Common in woods. 1 ORDER 33. — V ER B EN AC Tii BE V ERBKNEiE. Verbena Bonariensis EJE. Naturalized. ,, officina’is . . . Common. 3 Lippia (Zapania) nolifiora Up to 4,500 feet. 4 Lantana alba [L. dubia, Royle 111.] ,, 3, '.00 ,, 5 Gmelina arborea Kumar ,, 2,000 ,, 6 Tribe Viters. Caryopteris Wallichiana [Clerod- . Mohini Very common up to 7 enuron odoratum, Madden.] Premna (Gumira) serratifolia [spi- 6,000 feet. April, Bhabar. 8 nosa, Roxb.] ,, (Premnos) mucronata Agniun Common. g ,, ,, barbata 10 ,, ,, herbacea Ghiwali Rare. 1 1 Callicarpa arborea, Roxb. Common. 12 ,, macrophylla, Vahl Daiya Frequent, Sarju bank. 13 Clerodendron serratum . . . Common. „ var. ternifolium . . . ,, Bageswar. 14 ,, infortunatu n . . . 15 ,, siphonanthus Shiwali Bhabar. 16 Vitex negundo Bhabar and outer hills, 17 Holuskioldia sanguinea Kubtoliya ... April. Common, October. 1 ORDER 34.- — LABIATiE. Tribe Ocime^o. Geniospormn stroboliferum Banks of Sarju. 2 Ortho iphon rubicumlus . . . Common. 3 ,, virgatus . . . Banks of Ivosi. 4 Plectrantlms (Isodon) scrophulari- ... Frequent. 5 oides, ,, ,, Gerardianus... 6 , ,, striatus. • • • Very common October. 37-1 HIMALAYAN DISTRICTS DIVISION IL— MONO PETAL | continued ). No. Scientific name. Vernacular name. Note. 7 ORDER 34. — LABIATJE —(continued). Tribe Ocimk^e— (concluded). Plectranthus (Isodon) C'oetsa Very common. Octr. 8 „ „ rugosus > . . Common up to 6,500 ft. 9 ,, (Pyramid! urn) ternifolius, , , , „ low elevations. 10 „ (Co’.eoides) cordifolius ... . . • 11 Coleus barb atus Fiwai Very common. 13 Tribe Satyre/e. Sub-tribe Elsiioi.tzii P ogostemon jilectranthoidcs M. Rudra Common. 13 Dysophylla cruciata ,, in swamps. 14 Coltbrookia oppositifolia Du! shat 15 Elsholizia. flava Bhangria ... ,, down to 5,000 feet. 16 ,, prdystachya ... Bhangria . . . Very common. 17 ,, incisa Set bhangria. Rare. 18 Elsholizia pilosa * . . Frequent. 19 ,, crioslaejgva... • • • Rare. 20 „ (Cyc’otegia) strobolifera C' mmon. 21 Sub-tribe Memiiije. Perilla ocimoides Bhangria ... Cultivated, September. 22 Mentha viridis Pudina Naturalized. 23 „ Royicana ... Rare. Near Bhim Tab 24 Sub-tribe Thyme.*. Origanum normale? [vulgare?] Ban tul si Very common, autumn. 25 Thymus serpyllum ,, ajwain... Common, except outer 26 Sub-tribe Melliss me. Micromeria biflora range. Very common. 27 Calamintha (Clinopodium) repens ... . . . >> 28 ,, „ [Melissa, ' Madden] umbrosa Hedeoma ncpalensis June, under trees. 29 Frequent. 30 Tribe Monarde*. Salvia (Drymosphace) glutinosa Frequent, outer range. 31 [hians, Royle.] Salvia (Aethiopis) lanata Ganiva Vevv common, March. 32 „ „ Moorcroftiana ... . . . Above 10,000 feet. 33 „ (Notiosphace) plebeia ... Bhabar and valleys. 34 Tribe Nep.tkik. Nepeta (Pycnonepeta) spicata, var. Common, Binsar. „ ,, eiata, Royle ... . . . Yellow, morning, blue 35 „ „ clliptica afternoon. Common, Binsar. 36 „ (Cataria) rnderal s • • . Frequent. 37 „ ,, lencophylla ... , . , Common. 38 „ „ gracilitlora ... • • i Bhabar. 39 „ (Macro nepeta) Govaniana ... . • . Frequent. 40 Dracocephalum acantlioides Niti. 41 Lallemantia Royleana Balangu Rare. OF THIS NORTH-WESTERN PROVINCES. 375 DIVISION II. — MON OPE TA L M — ( concluded). No. Scientific name. tao, Vernacular. name. Note. ORDER 34.— LABIATiE - (concluded). Tribe Stachydeas. Sub-tribe Scutellarieau. 42 Prunella vulgaris . . . Common, June, Binsar. 43 Scutellaria linearis ... „ spring. 44 „ repens ... „ spring and autumn. 45 ,, angulosa [scandens,Don]. Sub-tribe MARRUBiEiE. „ autumn. 46 Craniotome versicolor ... ••• Sub-tribe Laniceas. . . . Very common. 47 Anisomeles ovata . . . Common. 48 Colquhounia coccinea [vestita, Wall] Bhilmoraand angiriya. „ at Naini Tal and Badrinath. 49 Stacliys sericea . . . Common. 50 ,, splendens Bhainsia aj- wain. Rare. Common. 51 Leonurus pubescens ... 52 Lamium amplexicaulc ... Tit pati 55 53 ,, petiolatum 55 54 Roylea elegans Gnma Frequent. 55 Leucas [Hemistoma] urticaefolia . . . 55 56 „ [Ortholencas] lanata ... Common. 57 „ ,, mollissima ... . . . Rare. 58 „ [Plagiostoma] hyssopifolia, ... Common. 59 ,, „ aspera [cephalotes, Blume.] 55 60 Leonoiis nepetaefolia Bhabar & Haklwani. 61 Phlomis lamiifolia Tribe A-jugeas. Rare. 62 Teucrium Royleanum (■ vur .) albi- dum. ... Common, valleys. 63 ,, quadrifarium 55 64 Ajuga lobata Bhabar. 65 „ remota Very common. 66 ,, parvifiora High elevations. 67 ,, bracteosa Very common. 68 „ decumbens ORDER 35.- PLUMB AG IN^ lCE^E- Rare. 69 Plumbago Zeylanica ... ...1 ' ORDER 36. — PLANTAGINACEJE. Common. 1 Plantago (Polyneuron) major, var. asiatica. Bar tang . . . Rare. 2 „ „ erosa, Don, [lon- giscapa, Jaeg.] Lohuriya ... Very common. 3 „ „ lanceolata. . . . Rare. <* 37G HIMALAYAN DISTRICTS. DIVISION III.— APETALiE. No. Scientific name. Vernacular name. Note. ORDER 1 . — PHYTOLACCACIJE. • 1 Phytolacca, decandra, var. acinosa, ... Jirrag Cultivated up to 10,000 feet. ORDER 2.— CHENOPODIACE^E. 1 Beta vulgaris, var. Bengalensis, Roxb., j Palang Cultivated. 2 Chenopodiu n album ] Bhatuwa ... Common. 3 „ (Ambrina) Botrys 1 ORDER 3.- — AMARANTACExE. Tribe Cel jsieje. 1 Deeringia celosioides Kala lohari... Common. 2 Celosia argentea Sirali and >> ghogiya. TbIBE ACHYRANTHK-iK. 3 Amarantus caudatuB Gardens. 4 ,, anardana [farinaceus] ... Ramdana and Cultivation. chua. 6 „ spinosus . . . Common. 6 JErua scandens Saji 7 Achyranthes aspera. . . . 8 „ species Tbidentata ?], ... . . . Not known at Kew 9 Cyathula tomentosa [Pupalfa sequax,] Jhat kuri ... Very common. Madden. 10 ,, capitata. ... Rare. Tribe Gomphrene.*. 11 Alternanther a nodi flora ... 1 Bhimraj Common. Bhim Tal. ORDER 4. — Nyctaginacf^e. 1 Boerhaavia diffusa Com ron. 2 Mirabilis Jalapa ... Introduced. ORDER 5.— POLYGON ACE JE. Tribe Terygocarpe.*. 1 Rheum emodi Dolu Above 10,000 feet. 2 Oxyria e'.atior ... „ 9,000 „ Tribe Apterocarpeie. 3 Rumex (Lapalium) Wallihchii Bhabar. 4 ,, nepalensis Haluniya ... Common. 6 „ (Acetosa) hastutus Almora Very common. 6 Koenigia monandra or islandica • . • Above 12,000 feet. 7 Polygonum (Avicularia) effusum • • • Common. [herniarioides.] 1 „ Roxburghii ... • • • Rare. 9 „ illecebroides ... ... No. 30 31 32 13 .14 15 16 17 28 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 85 36 37 88 39 40 41 42 1 2 3 4 5 OF THF NORTH-WESTERN PROVINCES. 377 DIVISION III. — APETALiE — ( continued). Scientific name. Vernacular name. ORDER 5. -POLYGONACEiE— (concluded). Tribe Apterocarpe.® - (concluded). Polygonum ciliosum „ cognatum ... ,, recumbens ... ,, (Persicaria) Hamiitonii [hispidum, Don.], barbatum Donii Posumbu flacci dum [gl abr um ,Roxb . ] , amphibium... lanigerum ... scabrinervum (Bistorta) viviparum [bnlbiferum, Royle]. sphaerostachyum amp! ex i caul e affine [Brunonis, Wall.], ,, emodi (Didymocephalon) delicatulum numm ul aci folium, filicaule [ciliatum, Don], humile perforatum [punc- tatum, Don], ncpalense sphaerocephalum, eapitatum [repens, Wall.], sinuatum (Corymbocephalon) chinense, (Echinocaulon) horridum ... (Tiniaria) convolvulus pterocarpum ... (Aconogonon) f rondosum . . . polystachyum Fagopyrum esculentum [vul- Ogal gare, Madden]. emarginatum ... Papar cymosum [corymb o s um Ban-ogal Madden], ff . ff if ff if ff ff if if ff fi if ff ff ff ff ff V ff ff ff ff ff ff ff ff ORDER 6. — LA URINEJE. Section ExiNvoi.trcROTEiE. Cinnamomum Tamala, var. albiflo- rum. Phsebe lanceolata „ pallida ,, paniculata Machilus odoratissimus ... Note. Tejpat, dal chi - ni. San kanwal... Kanwal Kapua kanwal, Rare. 14,500 feet. Common. September. Frequent, Bhabar, No- vember. Bhabar. Common. Frequent. Bhabar. Naini Tal lake. Frequent. Naini Tal lake. 15.000 feet. Very common. Common . At high elevations. Rare. 12.000 feet. 14.500 feet. Rare. if ff Common. Frequent. Very common. 8.500 feet. Very common. Bhim Tal, Common. 7,50o’feet. 12,000 feet. Cultivated, lower hills. Higher hills. Common. The native names given by Royle are incorrect. Common. February— May. Bhabar and valleys, February— M ay. Common. Bhabar and valleys. Common. Ma r c h — > August. 48 378 HIMA'LAYAN DISTRICTS DIVISION III. — APETALiE — ( continued ). No. Scientific name. Vernacular name. Note. OR DER 6 . — LAURI NE2E — (concl uded). Section Invot bcrate-i®. Tetranthera lanrifolia [a petal a, Gar-bijur ... Valleys. June. 7 Roxb., var Roxburghii], „ monopetala Katmara, Common. April. 8 singrao. Q Litsoea lanuginosa ... Rare. „ consimilis [T. pallens, Don.], Chirira and Common, interior of chirchira. hills. 11 Daphnidium pulcherrimum . . . Erequent. „ bifarium ... ... ORDER 7. — THYMELACEiE. i Daphne papyracea [D. cannabina, W all .], ... Common. „ var. purpurea ... Barmva >> 8/1 1)8 ... ... Set baruwa... Used, for paper-making. 2 Wikstroemia salicifolia [Daphne seri- Chamliya ... Common, used for mak- cea, Madden] ing inferior paper. ORDER 8. — EIuEAGNACE/E. 1 Hippophase salicifolia ... Dur chuk ... Common above 10,000. feet. 2 Elseagnus parvifolia G hi wain Common. 3 „ latifolia [ferruginea, D.C.] ... Bhabar. ORDER 9. — SANTALACEJE. 1 Osyris arborea, [nepalensis, Madden.], Bakar dhara, Common. 2 Thesium himalense ... ... ... Rare, Binsar. ORDER 10.— ARISTOLOCHIACEA3. i Aidstolochia saccata ... ... 1 Frequent ; about 7,000 feet. ORDER 11.— EUPIIORBIACEgE. Tribe E hyleaj. the.®. i Andrachne cordifolia [Leptopus cor- • . * Very common. difolius, Deee], 2 Antidesma diandra Sarshoti amli Bhabar. 3 Phyllanthus (Hemiglochidion) nepa- Bair mao ... . . . lensis [Bradlcia ovata, Wall. Glo- Very common. chidion bifaria, Royle], 4 „ velutinus . . • 5 „ (Emblica) Emblica Amla Erequent. 6 (Paraphyllanthus) urinaria Siahi Common. 7 (Euphyllanthus) parvifolius . . . Erequent. 8 Putranjiva Roxburghii ... Putra jiva ... Bhabar. 9 Securinega (Eluggea) obovata [Phyl- Dhani Common. lanthus retusus, Wall], 10 „ leucopyrus [Phylla nthus Ainta * • • albicans, Wall]. 11 Bischoffia Zeylaniae [Andiachne trifo- Korsa ... liata, Roxb], 12 If. u 15 10 17 18 19 20 21 22 23 24 2.i 26 27 28 29 30 31 32 1 1 2 1 2 OF THE NORTH-WESTERN PROVINCES. 379 DIVISION IIL— APETAL2E— ( continued ) . Scientific name. Vernacular name. Note. ORDER 11.— EUPHORBIACEJE— (concluded). TRIBE BrIDEEIEAS. Bridelia stipularis „ (Cluytia) montana „ retusa Karnaliya ... Khaja Rare. Common. Up to 3,000 feet. Tribe Acaebpiie.®. Trewia nudifloi-a Mallotus philippinensis (Iiottlera tinetoria]. Ricinus communis Homonoya riparia [Adelia, Madden], Tumri Byuni Ind, rendi ... Kandagar ... Bhabar. Very common. Common. Frequent. Tribe Hippomane.®. Jetroplia Curcas Baliospermum montanum [Crotonpol- yandrus, Roxb.] Excascaria (Triadica) s.bifera „ (Fa’.coneria) insignis „ (Eucxcsecaria) acer i f o 1 i a [sapium, Madden, Stillingia hima- layensis ] Safed ind ... Phutkiya ... Naturalized, Bhabar. Common, Sarju bank. Introduced. Common. Very common, Sarju bank. Tribe Eupiiorbie-®. Euphorbia pentagona [Royleana] ... „ anguetifolia [dracunculoi- des, Roxb.] „ hirsuta [longifolia, Don.], „ pcploides „ pilulifera ,, notoptera „ hyperieifolia ... „ thymifoha „ pilosa Sohund Dudhila and Mahabir. » • • 0 Up to 6,000 feet. Common up to 6,000 feet. Above 6,000 feet (like Helioscopia). Frequent. Very common. Ganai valley. Col. Davidson. >> >> ORDER 12.— DAPHNIPHYLLACE2E. Daphniphyllum himalense [Gyrandra laurina, Wall. Ilicineas sp ., Royle.] Rakt chandan [ rakt angliya. Frequent. Used in marking the tika mark on forehead. ORDER 13. — -BUXACEJE. Buxus sempervirens Sarcococca saligna Dee. [S. nepalen- sis, Royle]. Papar Sukat sing... Milam and Wan. Common, high levels. ORDER 1 4. — CANNABINACEiE. Hum nl us lupulus Cannabis sativa , • • o Bhang Introduced. Very common. I 380 HIMA'LA.YAN DISTRICTS DIVISION III. — APETALiE — ( continued). No. Scientific name. Vernacular name. Note. . ORDER 15.-ULMACEAE. 1 Ulrnus Wallichiana [erosa, Roth Chambar ma- Frequent. Flower® ya. precocious. 2 „ parvi folia [virgata, Roxb.J ... Frequent. Flowers coetaneous. 3 Boloptelea integrifolia [Ulmus integ- Kanju Common. rifolia, Roxbl. 4 Celtis australis [tetrandra,, Roxb] ... Kharak V ery common ami pi an ted . 5 Sponia politoria [Celtis tetrandra, Khaoi, khak- Bhabar and valleys. Wall ?] si. ORDER ] 6. — MORACEJE. i Streblus asper [Trophis aspera Rusa Bhabar. 2 Plecospirmum spinesum [Batis spi- • • • Rare. nosa]. 3 Morns indica ... ... Shahtut Frequent. 4 ,, lasvigata >> 5 „ serrata Kimu Common. Diosceou®. 6 Eicus indica Bar Valleys. 7 „ infectoria Pakar B hi bar. 8 „ Tsiela Kathbar Planted. 9 „ religiosa Pi pal Valleys. 10 „ cordifolia Kabai pipal, Common. 11 „ retusa [tritida] ... . • • Bhabar. 12 ,, Carica Anjir Cultivated. 13 ,, virgata Beru Very common. 14 „ parasitica . • • Bhabar. 15 „ scandens • • « Valleys. 16 „ trachycarpa • • i, 17 „ Cunia Kunia Common. 18 „ glomerata Gular Planted and banks of Kali. 19 „ macrophylla Timla Fruit eaten. 20 ,, oppositifolia Totmila Common. 21 „ Luducca Kabhila 22 „ laurifolia Dudhila 23 „ ovata Betuli 24 „ Chincha Kismira 25 ,, saxatilis 26 „ laminosa 27 „ acuminata ... Bhabar. ORDER 1 7.— ARTOCARPEvE. 1 Artocarpus Lakoocha Dhao Introduced. 2 Cudrania javanensis Miinda Bhabar. ORDER 1 8.' — URTICACE2E. Tribe Urereje. 1 Urtica parviflora Shishauna ... Eaten ; very common. 2 Girardinia heterophyila ... Awa bichhu, Very common. i OF THE NORTH-WESTERN PROVINCES. 381 DIVISION III. — APETALVE — ( continued). No. | Scientific name. Vernacular name. ORDER 18. — URTIC ACE M— (concluded). Tin uk Fii iciUDEnfi. s Pilea scripta [goglado, Wall.] , , , 4 Lecan thus peduncular is ... Saochala . . . 6 Elatostemma sessile [Procris puncta- ta, Don]. 55 6 „ platyphyllum Gargela 7 ,, Stracheyauum ... 8 „ diversi folium Tkibe Bcbhmekicjb. 9 Bcehmeria rugulosa [nervosa, Madden] Geti 10 ,, macrophylla ... Saochala gol- ka. 11 ,, platyphylla, var. rotnndi- folia. Gargela 12 Chamabaina squamigera . . . 13 PouzoUia viminea [sanguinea] 14 Memoiialis pentandra [Urtica pen- tandra, Roxb. Jaiphal jari, 15 ,, hirta 1G ,, quinquenervis Poi dhaula 17 Yillebrunea frutescens, [Urtica fru- - tescens, Madden ] and kagshi. 18 Debregeasia longifolia ... 19 ,, bicolor [Bcehmeria salici- folia, Madden]. Tushyari ... 20 Maoutia Puya, [Boehmeria frutecens, Phusar patta Don.] and dhaula- kagshi. ORDER 19.' — PIPER ACEiE. 1 Piper sylvaticum Pippula mul, 2 Piperomia reflexa. [saxatilis, Mad- • • • den]. ORDER 20. - CORYLACEiE. 1 Carpinus faginea Gish cham- kliarak. 2 ,, viminea 55 3 Corylus lacera Kapasi, bho- tiya badam. 4 Castaneopsis tribuloides Katonj 5 Quercus incana Ban] Note. Common; Naim Tal. Very common ; July, August. 55 Common. Rare Common ; August. Common ; dishes made of the wood. Common. 55 Bhabar. Frequent. Common. Frequent. 55 Common. Rare. Very common ; April. Common up to 4,000 feet ; Bliim Tal and Bageswar. Common ; Bhabar and valleys. Yery common on trees. Common. Above 10,000 feet. Common, J o s h i « math. Frequent. Yery common. 382 HIMALAYAN DISTRICTS DIVISION III. — iA.PETAL.ZE — ( concluded ). No. Scientific name. Vernacular name. Note. ORDER 20. — CORYLACEiE — (concluded). 6 QuercuB lanata Rianj Frequent ; Lariya kan- ta. 7 ,, semicarpifolia ... Karshu Common, high eleva- tions. 8 „ dilatata Tilonj Very common. 9 „ annulata 1 Phalyant ... Common, valleys. ORDER 21.— JUGLANDACEiE. 1 Juglans regia | Akhrot, akor Common. 2 Engelliardtia Colebrookiana | Mao >> ORDER 22. — MYRICACEJE. 1 Myrica sapi 'a Kaiphal Very common. ORDER 23.— B .TULACEJE. 1 Betula Bhojpattra Bhojpatra ... Above 10,000 feet. 2 ,, fBetulaster) acuminata li aoul 8,000 n [cylindrostachysj Shaoul Common. 3 ,, nitida Puya-udesh, JJ 4 Alnus nepalensis Udesh Banks of all rivers. ORDER 24. — SALICACEiE. 1 Salix (Pleiandrse) tetraspcrma Gar-bains ... Common near streams. 2 „ „ acmophyLla [deal- . . . Frequent. bata, Jacq.]. 3 ,, (Diandrse) babylonica Majnun Introduced. 4 „ „ Wallichiana Bains Common. 5 ,, „ elegans] kumaon- . . . Top of China. 6 ensis, Lindley]. £ ,, daphno'.dcs • r • Above 10,000 feet. 7 „ ,, Lindleyana , , , 8 Pop ulus nigra [fastigiata] Introduced. 9 ,, ciliata Gar pipal ... Common. ORDER 25.— LORANTIIACEAL. 1 Vi cum stellatum, Don. Banda Common on Pyrus. 2 „ (Aphylla) articulatum Ditto Common on Quercns. incana and dilatata. 3 „ attenuatum Ditto Ditto. 4 Loranthus (Euloranthus) ligustrinus, Frequent ; June. 5 „ (Scurrula) pulverulentus, Common ; winter. 6 ,, ,, cordifolius ... Rare ; December. 7 ,, „ vestitus Frequent ; winter. 8 „ (Pentamera) longiflorus Common ; spring. [bicolor, Roxb.] OF THE NORTH-WESTERN PROVINCES 383 DIVISION IV. — GYMNOSPERMiE. No. Scientific name. Vernacular name. Note. ORDER 1.- — GNETACEiE: 1 Ephedra vulgaris [Gerardiana] ... Above 10,000 feet ; fruit edible. ORDER 2. — CONIFERiE. 1 Pinus longifolia Chir, salla ... Very common. 2 „ Gerardiana ... Above 12,000 feet. 3 ,, excelsa Rai salla ... „ 10,000 feet, Ka- nol, Painkhanda. 4 Abies Smithiana Ragha Above 10,000 feet. 5 „ Brunoniana [dumosa] Rare ; found by Cap- tain Webb. 6 Picea Pindrow 5 ) Common above 10,000 feet. 7 ,, Webbiana >> „ 5i 12,000 feet. 8 Cedrus Deodara Diyar Introduced. ORDER 3.— CUPRESSINE^E. 1 Cupressus torulosa Sarai Naini Tal and JoBlii- math. 2 ,, Bempervirens ... Introduced. 3 Juniperus (Oxycedrus) communis, ... Chichiya ... Milam and Niti, 12,000 feet. 4 „ „ recurva Bhedara Rare. „ var. squamata ... Bel bhedara, Ilani Pani, 8,000 feet. 5 „ (Sabina) excelsa Padam Milam, 12,000 feet. 6 „ „ Wallichiana Bhedara Milam and Niti. Var. squamosa, Madden ... Bel bhedara, Pindari, Painkhanda, Rikholi gudri. A. kind of yeast is made from this plant. ORDER 4. — TAXACEiE. 1 Taxus baccata Thuner Common. 2 „ nucifera Rare ; only found by • Royle. 384 HIMA'LAYAN DISTRICTS DIVISION V.— ENDOGEML No. Scientific name. Vernacular name. Note. ORDER 1.— -ZINGIBER ACEJE. 1 Curcuma angustifolia Ban haldi ... Up to 6,000 feet ; May. 2 „ longa [kuchoor, Eoyle] Haldi Cultivated up to 4,0o0 feet. 3 Hedycliium spicatum Kachur-kac- Common. 4 ,, coccincum hri, 5 „ villosum [Madden] Rakt haldi ... 99 6 „ tenuifiorum Murdan Ali] Rare, Piytira. 7 „ coronarium [fiavum, 99 Madden], Gardens. 8 Roscoea purpurea 9 „ alpina Common ; autumn. 10 „ lutea [gracilis] 99 11 „ elatior 9 12 Zingiber capitatum Daknri binayak. 13 „ ligulatum Bhabar. „ var. chrysanthemum 99 14 , cassumunar relation, Mad- Bhim Tal. den?]. Bhabar ; eaten by pigs. 15 „ officinale Adralc Cultivated. 13 Amomum subulatum Ilaichi G ardens 17 Costus speciosus , , . Rare; valleys. Autumn. 1-8 G lobba secunda * . • . Bhabar. „ Orixensis? ... ORDER 2.— MARANTACEiE. 1 Canna speciosa Iviwara Gardens. ORDER 3. — MUSACEJE. 1 Musa sapientum • • • Cultivated. 2 „ nepalensis . . • River banks, Askot to Dharcliula. ORDER 4.— AMARYLLIDACEA5. 1 Crinum toxicarium Chandar kan- Common ; July. wal. 2 „ species ... Introduced. ORDER 5.— HYPOXIDACEiE. 1 Curculigo recurvata Pitari Bhim Tal. 2 „ orchioides Common up to 6,400 feet. 3 Hypoxis minor ... ... Very common. ORDER 6. — IRIDACEiE. 1 Pardanthus sinensis Katar pata ... Very common. 2 Iris nepalensis Nil-kanwal Common. 3 ,, kumaonensis • • • 4 „ decora • . . Frequent. 5 Tigridia pavonia . . . Introduced. l OF THE NORTH-WESTERN PROVINCES. 385 DIVISION V. — ENDOGEN2E — ( continued ). Scientific name. Vernacular Note. name. ORDER 7.— H YDROCIIARIDEiE. 1 2 Vallisneria spiralis Hydrilla verticillata ORDER 8.' — ORCHIDACEiE. Bliim Tal. Tribe MaeaxidEj® (End.) Sub-tribe Pleurotu alee^s. 1 Oberonia iridifolia 2 Microstylis Wallichii ... 3 Dienia cylindrostachys ... Banda 4 Liparis ncpalensis 5 6 7 8 Pholidota articulata Cadogyne uitida „ praecox ,, ovalis Sub-tribe Denprobiive Low elevations. Colonel Davidson. Common, Binsar, Chi- na, August. Lariya Kanta, Colonel Davidson. August. Common, April. Valleys. Kotahgar. October. Binsar; common, May. 9 10 11 Eria convallarioides [Octomeria spi- cata]. Dendrobium alpestre „ Pitrardii [roseum ?] ... Garar panja, Common on oaks, June. Frequent. Common, June. Tribe Epidendre^ (End.) 12 Apaturia Smithiana ... IS Phaius albus 14 bi color Bhabar. Very common near Bliim Tal, June. Colonel Davidson. Tribe Vande.®. 15 Cymbidium triste [Luisia trichor- hiza.] ... 16 Eulophia campestris ... 17 ,, herbacea ... 18 Cyrtopcra fusca (flava, Royle 111.) ... ... 19 Vanda cristata Banda 20 Saccolabium guttatum ... ... 21 „ bapillosum [Cymbidium priemorsum, Roxb.], ... 22 Aer ides affine . . • 23 „ odoratum [cornutum, Roxb.], . . . 24 Calanthe plantaginea Hyacinth or- chis. Frequent, low levels. Rare Bhabar. Salep made from root. Frequent, sweet scent- ed. Common up to 4,500 feet. May. Common, on trees. June. Very common, low ele- vations. May, June. Haldwani, on Ulmus integrifolia. Common. June. Colonel Davidson. Very common. April. 49 zm HIMALAYAN DISTRICTS' DIVISION V. — ENDOGrENiE — ( confirmed }. No. Scientific name. Vernacular name. Note. ORDER 8 .— ORCHID-AGE-®— (concluded). TBIBE OPHBYDEiE. 26 Orchis lotifolia ... Phulsain near Joshi- math, June. 26 Aceras angustifolia r r ♦ Very common. 27 Platanthera Susannae ,,, Ramgar, September. 28 „ obcordata ... ... Near Naini Tal Brew- ery. September. 29 „ acuminata ... ... Naini Tal. Colonel Davidson. 30 Hemipilia cordifolia ... Near Khairna, Sep- tember. 31 Peristylus goodyeroides ... ' . < ; Frequent. 32 Herminium Monorchis ... ... Top of Lariya Kanta, August. 33 „ graminenm ... • . • i Rare. 34 Habenaria pectinata . . 1 Common, September. T7- ” V ery common, August, September. 36 „ intermedia ... » » • 36 „ marginata ... ... 37 „ ensifofia ► . % Colonel Davidson. 38 „ piantaginea ,,, yy 5 ? 39 ,, rostrata, Madden ... Perhaps same as emar- ginata. No. 36. 40 Gymnadertia coinmelynaefolia, Mad- den. ... On Kali math, 6,000 feet. 41 Satyrium nepalense Tbibe Gastbodie^j. Pakwa-dimni, Very common, August, September. 42 Epipogiutn Gmelini Tbibe Neottieje. ... Colonel Davidson. 43 Spiranthes australis ... Very common, August, September. 44 Epipactis latifolia Common. 45 , , m acr ostachya ... 46 Goodyera repens yy 47 „ procera Binsar, August. 48 Zeuxine sulcata Tbibe Abethuseje. Winter, Bhabar. 49 Cephalanthera acuminata ... 1 Tbibe Cypbipede.®. ... Common, under trees. May. 50 Cypripedium cordigerum ... Lariya Kanta, May. Colonel Davidson. m THE NORTH-WESTER!* PROVINCES. 387 DIVISION V. — ENDOGrENiE — ( continued ). No. Scientific name. Vernacular name. ✓ Note. 1 ORDER 9.— PALM AC EH Chamserops Martiana 5. Thakil Frequent. „ vur. khasyana, Madden... Common, valleys. 2 Wallichia densiflora [Harina oblongi- Kala-aunsa... 3 folia.] Phoenix sylvestris var. humilis Mad- Khajur Up to 5,000 feet. Bin- 4 den. ,., acaulis sar. Bhabar. 5 Calamus Eoyleanus, [C. Rotang?] ... Bet >> 1 ORDER io.— PONTEDEKIA Pontederia (Monochoria) liastata. CEHS. Common. Rice fields. 1 [P. vaginalis, Madden.] ORDER 1 1, — MELANTHAE Disporum Pitsutum )EHS. Common. 2 „ Leschenaultianum [Uvularia ... 3 Leschenaultii, Madden.] „ Wallichii Frequent. 4 ,, Hamiltonianum . . . 6 Iphigenia indica [Anguillan* indica, 0 8 « Common. 1 Brown.] ORDER 12. — LILIACEE Tribe TuLimiiE. Tulipa stellata E. Majaula, nalku, Common up to 7,000. 2 Gageaelegans ... ..., ... „ above 10,000 feet. 3 Lloydia serotina? ..." . . . Com i on. 4 ,, liimalense ... Above 10,000 feet. 5 Eritillaria verticillata ... • . • Plmlsain, 8,000 feet. 6 „ Thomsonianum . . . Common, April. 7 Lilium Wallichianum ... Findora Common, Ranibagh. 8 ,, nepalense ... ... . . . 9 „ giganteum Bhuniya nar, Bish nangal, Above 10,000 feet. 10 Methonica [Gloriosa] superba ... Valleys. 11 Hemerocallis fulva [disticha] ... Above 10,000 feet. 12 Tribe ALOiNEiE. Aioe perfoliata Ghikw&r ... Valleys, April. 13 Yucca gloriosa Rambans . . . Naturalized. 14 Tribe Hv.'.cintueze. Uropetalum Rare, Kalimath. 15 Urginea indica [Scilla indica, Mad- den]. Allium leptophyllum Gesua Common. 16 Piriya lahsan Outer range. 17 ,, Wallichii Paderiya lah- 18 „ ellipticum san. Sheolia lah- t 8 * 19 „ Jibbu san. Jibbu About. 10,000 feet. 20 „ Argand Argand Uanipani, 8,000 feet. 388 HIMALAYAN DISTRICTS DIVISION V.— ENDOGENiE— ( continued ). No. Scientific name. V ernacular name. Note. ORDER 12.— LILIACEiE -( concluded ). Tribe Asparagei®. 21 Asparagus racemosus Ail ora Bhabar. 22 „ fllicinus Khairuwa ... Common, edible. 23 adscendens Common. 24 Polygonatum verticillatum 9) 25 „ multiflonum ... )> 26 „ cirrhiflorum ? [Sibiricum ?] 3> 27 Smilacina pallida 28 „ alpina ... Kcdar. Tribe Ophiopogone^s, 29 Ophiopogon intermedins Frequent. 30 „ Wallichianus [spicatum, Common. Madden], „ ORDER 13.— COMMELYNACEJS. SliCTI )N OlJGANDREiE. 1 Commelyna (Eucommelyna) salici- Frequent. folia. 2 „ „ bengalensis ... • « • 9J 3 „ (Trithyro carpus) obliqua... Kama Very common. 4 Aneilema scapiflornm, [Murdannia Common up to 4,000 ft. scapifiora, Royle], 5 „ lined atom Aboye 5,000 feet. 6 „ pratensum ... Rare. Section Hexandre.®. 7 Dithyrocarpus, paniculatus [rufus, Kandera Common. Kuntli], 8 Cyan otis axillaris Bhabar. 9 „ cristata 10 „ barbata Common. 11 „ racemosa Bhabar. 12 Streptolirion yolubile ... ... Rare. ORDER 14.— ALISMACEJE. 1 Sagittaria sagittifolia ... ... | ... • »0 ORDER 15. JUNCEiE. 1 Juncns bufonius Shim Common. 2 „ glaucus t • « Frequent. 3 „ concinnus 4 „ Wallichianus ... ... ... ORDER 16.— SMILACEAE. 1 Smilax villandia, Royle Kukar dhara. Common. o „ macrophylla Frequent. 3 „ maculata 4 „ raginata Rare, China. OP THE NORTH-WESTERN PROVINCES. 389 DIVISION V. — ENDOGrENiE — ( continued). No. 1 2 3 4 5 1 2 3 4 5 6 7 8 9 10 11 12 13 1 2 3 4 1 2 1 2 3 4 5 Scientific name. Vernacular name. Note. ORDER 17.-DIOSCOREACEJE. Dioscorea versicolor „ sagittata „ pentaphylla „ delto'.dea Genti Ta r tagur... Magina mu- ni ya. Gun Frequent. Tubers edible. Tubers edible. Above 6,000 feet. ORDER 18. — AROILEiE. TlUBE DkACUXCULE/E. Arissema speciosa „ Jacquemontil ... ,, costatum „ curvatum Arum hastatum Sauromatum guttatum ... „ punctatum? Amorphophallus campa n u 1 a t u s [Arum campanulatum, Roxb.]. Typhonium? Sarp lea goga, j, j y Nala bank . . . >> Common. Very common. Common. Common, July. Kaladhungi. Bhabar. Common, July, very foetid. Tbibe Caeadie^e. Remusatia vivipara „ capillifera milum, Don ? Colocasia Roxburgliii ,, himalensis [Caladium pu- Baghpindalu, Banj pindilu, ^Jangli gwia Gar papar. Gwia and pa- par. Up to 4,500 feet. Above 5,000 feet, flow- ers, June. Very common. Cultivated. ORDER 19.— ORONIACEEE. Acorus calamus Scindapsus officinalis, Rothos offici- nalis, Roxb ] „ decursivus [I’oJios deeur- sivus]. Rothos scandeus Bach baj Hatlmngliya, Kelauniya ... Rare. Near Bhim Tal. Binsar. ORDER 20.— TYRIIACEiE. Typha elephantina „ angustifolia ... J Radera, pe- ... tara. Bora Bhabar. Marshes. ORDER 21.— JUNCAGINACEiE. Rotamogeton natans „ mucronatum „ cri spurn „ pectinatum „ perfoliatum Bhim Tal and Naini Tal. >> » )> >> 390 HIMALAYAN DISTRICTS DIVISION V. — ENDOGrENiE — ( continued ) . No Scientific name. Vernacular name. Note. 1 ORDER 22.— LEMNACI Lemna minor EE. Bhabar. 2 „ polyrhiza [orbiculata, Roxb.]. • • • Streams, up to 4,000 1 ORDER 23. — GRAMINEZE. Tribe Oryzeie. Oryza sativa ... ... 1 Dhan feet. Cultivated. 2 Tribe Phalarideas. Zea Mays Bhuta Cultivated. 3 j Coix Lacryma Lakocbiya ... Common. 4 | „ gigantea )} Frequent. 6 Tribe Fanicea:. Paspalun longiflorum Kana Rice fields. 6 Panicum (Digitaria) cruciatum [Ro- Frequent. ylei, Madden. J ,, var. distachyus ... >> ,, octostaehyus 7 Panicum (Orthopogon) acuminatissi- Colonel Davidson. 8 mum. Panicum (Echinochloa) colonum Jangli rnandi- Common. 9 „ frumentaceum 1 U. Jhangora and Cultivated. 10 ,, homonymum cliamaeraphis mandira. Very common. 11 Madden], » (Setaria) glaucum 12 „ Italicum Kangni koni, Cultivated. 13 „ (Virgaria) miliaceum China 14 Penuisetum trifiorum Bimalsiya ... Common. 15 Arundine'la setosa [hirsuta, Madden] >> 16 ,, nepa’ensis [miliaria, Madden, 17 Thysanolaena agrostis Aunsa Very common. 18 19 Tribe Stifaceie. Arachne (Piptatherum) ho'.ciformis, Aristida cyananlha Binniya & ka- Co’onel Davidson. 20 Tribe Agrostidive. Vilfa elongata [Sporobolus elongatus kal sena. Very common. Common. 21 Madden]. Agrostis alba Colonel Davidson. 22 Muhlenbergia sylyatica ... Rare. 23 ,, geniculata ... 24 Polypogon fugax Giwagioliya, Common. 25 Perotis latifolia ... ... | 26 Tribe Arundinaceas. Phragmites Roxburghii ... Bichra, nal... Common. 27 ,, Karka Karka ,, ... 28 „ nepalensis Nal tura Bhim Tal. OF THE NORTH-WESTERN PROVINCES. 391 DIVISION V.— ENDOG-ENiE— ( continued ). No. 1 Scientific name. Vernacular name. Note, 29 ORDER 23.— GRAMINEJE — (coi TRIBE CHLORIDE.*. Chloris decora atinucd). Common. SO Cynodon dactylon Dub Very common. 31 Eleusine coracana Manduwa . . . Cultivated. 32 „ indica ... Common. 33 Tribe Avene.*. A vena sativa Jai Cultivated, 34 „ fatua Jai-ata Common. 35 Tribe Festuce^e. Poa annua ... Introduced. 36 „ bulbosa » 37 „ trivialis 99 38 Eragrostis- cynosuroides Common. 39 ,, caudata 9f 40 „ nutans Col. Davidson. 41 „ amabilis 99 42 ciliata Common. 43 „ plumosa Very common. 44 „ diarrhena Col. Dav.dson. 45 „ nardoides Common. 46 „ orientalis October. 47 Ivoeleria cristata Very common, April. 48 Dactylis glomerata Frequent. 49 Festuca (Brachypodium) nepalensis, Common. 60 Tripogon (Plagiolytrum) filiforme, 99 61 Tribe Bambuseas. Arundinarla falcata Ringal and Very common. 52 (Two varieties ') Thamnocalamus spathiflorus Ningal. Ringal Dudatoli. 53 „ Falconeri Kali ringal... Common, May. 64 Dendrocalamiis str ictus Bans Bhabar. 55 „ sp . 99 ... Dhamas ; cultivated. 56 Tribe Hordeace.*. Lolium temulentum Bhabar. 57 Triticum vulgare Lai geliun ... Cultivated. 68 „ striatum . . . Rare. 59 Hordeum hexastychum ... Jao Cultivated. 60 „ himalayense [coeleste] Ua jao ., above 10,000 ft. 61 Tribe Rottboerliace.* Ophiurus perforatus Very common. 62 Rottbcellia exaltata . . . Frequent. 63 „ hirsuta . . . Rare. 64 „ laevis [Mnesithia laevis], ... 99 65 Manisurus granularis • ’ * Frequent. 302 hima'layan districts DIVISION V.— ENDOGEN/E— ( continued ). No. Scientific name. Vernacular name. Note. 66 • ORDER 23. — GRAMINEiE -(cor Tribe Andropogonehs. Andropogon, with number in £ Heteropogon contortns, 37 „ polystachyus, 42 Lcluded). JTEUDEE. Kumariya ... Common. 67 99 Frequent. 68 Ischsemum corollatus, 65 Noniya 69 Ischsemonca speciosns, 132 Spodiopogon involutus, 117 ... 99 70 ... 99 71 Apocopis himalayensis, 168 ... Rare. 72 Bathratlrerum lancifolins, 237 ... Common. 73 „ micans, 239 ... 99 74 Tribe Andropogoneje. Bathratherum snbmnticus 240 Common. 75 Cymbopogon pachnodes, 297 . . . 99 76 „ distans, 298 . . . 99 77 ,, versicolor, 301 Piriya Very common.Naini Tal 78 „ pendnlus, 303 Common. 79 ,, Iwarankusa, 306 Miriya 99 80 „ Martini, 309 . . . Bhabar. 81 ,, flexnosns, 310 Bujara Very common A mora. 82 Andropogon erythrocoleos, 341 . . . Common. 83 ,, pnnctatns, 343 Pagrimalsi... Very common. 84 ,, controversus, 349 • • « Very common, October. 85 „ montanns, 352 . . . Colonel Davidson. 86 Sorghum halepensis, 384 Gandar, kashas, Common. 87 Anatherum muricatus, 393 99 88 Chrysopogon coernleus, 404 Gweriya, par- 99 89 „ Trinii, 408 mal. Rare. 90 „ Royleanus, 425 Salim Common. 91 ,, echinulatus 426 99 92 ,, villosnlus, 427 ... 93 „ glaucopsis, 429 . . . Rare. 94 „ subrepens, 420 ,, parvispica [Rh aphis 99 95 Palkiya, chir- Very common. 96 microstachys,] 431 ... Spodiopogon petiolaris, 443 aula Common , Naini Tal, 97 Anthistiria arundinacea Ullu, kanyur, .1 uly. Bhabar and valleys. 98 ,, onathera Jyotish-mati, Roots luminous. 99 Imperata arundinacea [cylindrica Lam] J Shiro 100 Saccharum spontaneum ... Jhansh 99 101 ,, Sara Sarur Bhabar. 102 ,, semidecnmbens Tat, mora ... 99 103 ,, exaltatum 99 104 ,, Munja Munj 99 105 Erianthus olivaceus, Edgw. Kans Common. 106 ,, vulpinus, Edgw. . . . 99 107 ,, fllifolium, Nees. . . • 99 108 „ rufum, Nees. ... ,, rufipilum, Stend. • • . 99 109 . . . 99 110 Leptatherum Royleanum ... Rare. 111 Pollinis sp. ... Frequent. 1 12 Eulalia japonica 99 OF THE NORTH-WESTERN PROVINCES. DIVISION V.— ENDOGENtE— ( continued ) 3.93 No. Scientific name. Vernacular name. Note. ORDER 2 4.— CYPERACEiE. Tribe Cyperecehs, i Cyperur (PycrenB) capillaris ? 2 „ diaphanus ? • " 3 „ angulatus . . . 4 ,, alopecuroides ? ... 5 „ (Eucyperus) compressus ... . . . 6 „ diffiormis Common. 7 ,, Iria S Cyperus niveus Very common. 9 10 „ tegetiformis tenuiflorus Motha ... Cultivated. Common, August. 11 rotundus [hexastachyos, 99 Roxb.] 12 „ obliquuB 99 13 „ pusillus [pygmseus, Retz.] ... 14 „ Wallichianus ... 15 „ fimbriatus Very common. 16 „ dilutus 17 Mariscus cyperinus Panmoth a Common. and nagar- motha. 18 Kyllingia monocephala ... Nirbisi 99 19 „ triceps 99 9 } Tribe Scirpe.®. 20 Abilgaardia monostachya , . . ... 21 Eleocharis palustris 22 „ uniglumis ... 23 Eleogenus ovata ... 24 „ capitata ... 25 26 Scirpns juncoides [muticuaj „ lacustris Bhim Tal. 27 „ affinis [maritimus] ... 28 Isolepis setacea . . . 29 ,, supina 30 31 „ Roy lei „ trifida Common. 32 Eimbristylis pallescens ... Very common, August. S3 „ junciformis 34 „ subtristachya [communis] ... Common. 35 quinquangularis Babar 99 36 Eriophorum comosum V ery common, au- tumn. Tribe Hypoeytre.®. 37 Lipocarph a argentea Very common, July and August. 50 No. 38 39 40 41 42 43 44 45 46 47 48 49 60 61 62 63 64 66 66 67 68 69 60 61 62 63 64 66 66 1 1 2 HIMALAYAN DISTRICTS DIVISION V. — ENDOGENiE — ( concluded). Scientific name. Vernacular name. Note. OEDER 24. — CYPERACEiE — (concluded). Tribe Rhyncospnre.®. Rhynchospora chinensis „ Wailichiana Tribe Caricineje. Carex (Androgynse) longipes 99 foliosa 99 nubigena 99 noteleia 99 Vahlii [alpina] )9 hasmatostoma ... . » setigera 99 myosurus 9} condensata yy filicina 99 (Bifidse) saxatilis [ r i g i d a , Good]. Carex notha 99 acuta [gracilis, Curtis] 99 (Trifidae), ligulata 99 cardiolepis 99 Royleana 99 Moorcroftii 99 emodorum [alopecuroides Don], 99 obscura ... 99 fusiformis 99 Wailichiana 99 cruenta 99 (Incertas) Thomsonii, Boott., 99 mitis, Boott. 99 uncinoides, Boott. 99 vesiculosa, Boott. Uncinia nepalensis ORDER 25.— ERIOCAULONEiE. Eriocaulon sexangulare ... ... | Common. Above 5,000 feet, May. Common. » Very common, swamps. ORDER 26.— TRILLIACEiE. Paris polyphylla Trillium Govanianum, Royle Common. Kulara Pass, 11,000 feet. OF THE NORTH-WESTERN PROVINCES. 395 DIVISION VI.— ACROGEKE. Ho. Scientific name. Vernacular name. Note. ORDER 1.— FILICES. Tribe Gleichbniaceas. I Gleichenia dichotoea Tribe Dicksonie.®. 2 S 4 Woodsia lanosa „ elongata ' ... _ ••• Dicksonia appendiculata [Sitolobium, J. Smith]. Common. Rare, DudatolL Common. » > Tribe IIymenofhylle;®. Hymenophyllum poyanthus [exser- | turn ?] Tribe Davaletezb. Davallia (Leucostegia) membranulosa, immersa multidentata? pulchra.? n cliaeroph y 1 1 a [cystopteris, D. C] J5 nodosa [Acro- phorus Presl.] (Endavallia) divaricata (ele- gans, Madden). (Microlepia) Hookeriana ... „ spel uncas „ . (Stenoloma) tenuifolia » On trees, Binsar, Oc- tober. J. H. Batten. Frequent. Rare. Common, Binsar. Rare. Very common. Bhabar. Common. Tribe Pteriheie. 15 Adlantum lunulatum ... 1*0 caudatum [rhizophorum Swartz], Mubaraka ... 17 „ Capillus- veneris 18 „ venustum Hansraj 19 „ pedatum 20 Cheillanthes Dalhousiae ... ••• ... 21 } , farinosa [dealbata ... 22 Onycliium auratum ... 23 ,, japonicum ... ••• Pellaia [Cheiloplecion] gracilis . . . 24 • . . 25 „ [AllosoruB nitidula Bish kutra . . . 26 „ [Platyloma] ealomelnnos 27 Pteris (Eupteris) longifolia ... 28 „ „ cretica ... „ „ var. stenophylla . . . ... 29 „ quadri aurita ... 30 (Paesia) aquilina ... 31 (Campteria) bianrita ... 32 „ Wallichiana ... ... 33 „ (Litobrochia) inciea ... Common. Very common. Common. » >> Very common. Common. Rare ; resembles Cryp- togramma crispa. Rare. On rocks at i oiv levels. Very common. >> >> Common. Very common. Very common. Rare. Common. Near Ramghar, J. H. Batten. No. 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 60 51 62 63 64 56 66 67 68 69 60 81 62 HIMALAYAN DISTRICTS DIVISION VI. — ACROGENiE — ( continued ). Scientific name. Yernacular name. Note. ORDER l.—EILICES— (continued). - Tribe Beechne-e. Woodwardia radicans . .. i Low levels, very com- 1 mon. Tribe Aspleniete. Asplenium (Euaspienium) ensifor- • » • Common. Binsar, July. me. 33 33 alternans . . . Very common on walls. 33 33 viride Above 12,000 feet. 33 33 trichomanes . . .* Common. 33 33 resectum . . . . Frequent. n 33 planicaule . . . Common. ji 33 adia n t n m ... Rare. ni_rum. 33 33 fontanum, ... Frequent. 33 33 varians . . . » 33 bulbiferum, . . • Rare. 33 33 tenuifolium ... [concinnum Wall]. 33 (Athyrium) thelyp t e r- * • • Colonel Davidson. oides. 33 33 macro c a r- .. . Common. pum [fo'io- losum Wall]. y? 33 nigripes . . . .t • Co’onel Davidson. 33 33 filix femina Common. [pec t i n a- turn]. ?> 33 ox y p h y !- * • • Colonel Davidson. lum. 33 33 fimbriatum, 33 33 umbro s u m . . . Rare. [Allantodia australe] 33 (Dipiazium) pol y p o d i- Lingra Common. oides. 33 33 maximum ,j edible. >3 (Amsogonium esculen- „ not edible. turn. Rave; Very like Asnle- 33 (Hemidictyum) Cetera c h nium alternans. [(Jeter a c h Common, walls, Sri- Actimopteris radiata • • • ••• Morpuchh ... nagar. Tribe Aspidiece. Aspidium (Polystichum)’auriculatum, Common. 33 33 ilicifolium... 33- 33 Thomsoni ... . • « Above 8,000 feet. 33 33 aculeatum ... . • « Common. 33 batum Wall. var. rufo bar- » ♦ « Very common. 33 33 Prescottianum, * * • Colonel Davidson. OF THE NORTH-WESTERN PROVINCES. DIVISION VI.— ACROGENiE— ( continued ). 397 63 64 65 66 67 68 69 70 71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 >> >> » )> >> » » » >> » >> ORDER 1 . — FILICES— (continued). Tribe Aspidibie — '( concluded). Aspidium (Polystichum) aristatum (coniifolium Wall). „ (Cyrtomium) falcatum ... „ „ var. caryoti- dium. Nephrodium (Lastrea) patens canum prolixum tilix mas var. coclilea- tum. flaccidum spiuulosum ... sparsum o d o r a t u m (eriocarpum, Id. K.) „ angustifrons, (Eunephrodium) uniturn ... „ coca 1 1 a t u m (unitum, Sieb.). ,, aridum „ molle (Sagenia) polymorphum ... „ variolosum „ cicuta ium Nephrolepis cordifolia [tuberosa. H. Iv.] Oleandra nernformis ,, Wallicliii Tribe PoLYPODiE-as. Eolypodium (Phegopteris) e r u b e - 11 11 11 11 11 91 91 ecens. 91 91 11 11 11 j, di stans (Goniopteris) urophyllum, proliferum, lineatum ... multilinea- tum. ii ii ii 11 (Goniophlebium) amsenum, H 11 laclmopus... 11 subauricula.- turn (argutum, Wall). Polypodium (Niphobolus) adnascens, i y 11 linqua ... jj 11 stigmosum, ly flssum . . . ii 11 (floccul o - sum). ly (Phymatodes) hneare [Pleopellis nudaj. 91 ii normale ... Katra Lingra Note. Bhabar. Frequent. Very common. Colonel Davidson. 99 Common. Very common. Common. Very common. Common. Very common; edible. Frequent. 11 Bhabar. Colonel Davidson. Frequent. Up to 4,000 feet. Rare. Common. Rare ; Pipa kothi. Common. 11 Low elevations. Commo n. Bhabar. Valleys. » Common. 11 Frequent. Common. 11 Valleys. Common, June. Rare. Scented fern ; very common on trees. Common. 398 HIMALAYAN DISTRICTS DIVISION VI. — ACROGENiE — ( continued'). No. Scientific name. Vernacular name. Note. 100 ORDER ].— FELICES— (cone Tribe Polypodies*: — (concl Polypodium (Phymatodes) membra- luded). uded). Common. 101 naceum. „ ,, tr ifidum Frequent. 102 [oxylobum, Wall]. „ „ ma'acodon, Rare. 103 „ „ ebenipes ... • • • >> 104 „ (Drynaria) propinquum, • . • Common. 105 „ „ rivale • • • 106 „ ,, querci folium ... • « • Bhabar. 107 ,, ,, juglandifolium, „ „ liimalayense • • • Common. 108 * t . Frequent. 109 [venustum, Wall]. Tribe Grammitide^s. Gynmogramma (Leptogramma) Totta, Colonel Davidson. 110 „ (Engymnogramna) Mouse ear Pyura and China. 111 vestita, „ „ Andersoni, fern. About 13,000 feet. 112 ,, ,, javanica... . . • Binsar. August. 113 „ (Sellignea) lanceolata, « • « Rare. 114 „ „ involuta... , , , Common. 115 Yittaria (Euvittaria) elonmta • • • Binsar. 116 ., (Toeniopsis) scolopendrina ? ... Binsar, June. 117 Tribe Acrostichte.®. Acrostichum virens Bhabar. „ var. deltigerum [Menis- • • « 118 ciurn deltigerum, Wall]. Tribe Osmuxdaceae. Osmunda Claytoniana [interupta] ... Very common 10,000 119 „ regalis var. japonica feet Chaupatta. Rare Khati 10,000 feet. 120 Tribe Schiztaceul Schizaea digitata May. Common. 121 Lygodium scandenle Marora, ban- Bhabar. 122 „ japonicum dhaniya. » Common. 123 Tribe Marattiace^i. Angiopteris erecta ... ... ] Rare. 124 Tribe QpmoGLOSSAcEiE. Ophioglossum vulgatum • • • 125 Botrychium lunaria Binsar. 126 „ daucifolium •• • Common. 127 „ virginianum ••• Very common. var. lanuginosum ... Common. OF THE NORTH-WESTERN PROVINCES. 399 DIVISION VI. — ACROGENiE — ( continued ) . No. Scientific name. Vernacular name. Note. ORDER 2 — EQUISETACEJE. 1 2. Equisetnm debile ... „ difEusura, Don [s c o p a- rium, Wall]. « • • • 03 Bhabar. Hill streams. ORDER 3. — LYCOrODIACEiE. 1 2 3 4 Lycopodium tenellum „ setaceum „ circinatum „ subuiifolium ... Ml Tula muka .. Very common. Rare. Frequent, 4,000 feet. Common. ORDER 4. — MARSILIACEjE. 1 Marsilia quadrifolia ... ... ... Bhabar. OBDER 5, — SALVINIACEJE. 1 Azolia pinnata ... ... Tarai ... Common in pools. ORDER 6.— CHARACEiE. 1 Chara verticillata ... Naini Tal and Bliim Tal. ORDER 7. — BRYACEiE. Tribe Dicranaceae. 1 2 3 4 5 6 Leptotrichum inclinatum, Mitten. () molliculum, Mittin ... himalayanum Mitten. Dicranum himalayanum, Mitten M refiexifolium, Muller. Didymodon laxifolius ... Floti. Common. >j Tribe Leucobrtace^:. 7 Octoblepharum albidum Bhabar. Tribe Trichostcmaceae. 8 9 10 11 12 Tortula squarrosa „ anomala Ancectangium Roylei, Mitten „ Thomsoni, Mitten „ Stracheyanum, Mitten ... Common. • • • 400 HIMALAYAN DISTRICTS DIVISION VI. — ACROGrENiE — ( continued ) . No. Scientific name. Vernacular name. Note. ORDER 7. — BRYACEiE— (continued). Tribe Trichostomaceas — ( concluded). 13 Hymenostylium aurantiacum, Mitten, • • • 14 „ cur drostrum 15 Barbula vinealis , , , 16 ,, sub-pellucida, Mitten ... . . . • ■ • 17 „ gracilenta, Mitten . . . ... 18 „ nigrescens, Mitten . . . 19 Desmatodou Laureri . . • 20 ,, Wallichii . . . 21 „ involutus . . . 22 Eucalypta ciliata ... ... Tribe Grimmiace.®. 23 Grimmiaapocarpa t • • Rocks, common. 24 „ (Rhacomitrium) subsecunda, . . . 25 Glyphomitrium tortula, Mitten ... Tribe Ortiiotrichace.®. 26 Orthotrichum Hookeri ... 27 Macromitrium Moorcroftii ... • • 0 Tribe Funariaceas. 28 Eunaria hygrometrica . • . Very common, sum- mer. 29 „ leptopoda ... ... Tribe Splachnace.®. 30 Tayloria indica 31 „ (Dissodon) tenella, Mitten, ... October. Tribe B artr a mi a cea3 . 32 Bartramin Halleriana 33 „ leptodonta ... Near Ithyphylla, 34 „ subpellucida, Mitten Resembles „ 35 Philonotis Turneriana • • • Common. 36 „ falcata ... 9 ) Tribe Bryace.®. 37 Mielichoferio himalayana ... Pindari, 11,000 feet. 38 Webera elongata • . « 39 Bryum filiforme, Mitten • • « . • • 40 „ argenteum ... Very common. OF THE NORTH-WESTERN PROVINCES. 401 DIVISION VI. — ACROGENiE' — ( continued). No. 48 49 50 51 62 63 54 55 56 57 58 59 60 61 62 ORDER 6. — BRYACEiE — •(continued). Tribe Bryace;e — ( concluded). 41 Bryum hemisphoevicum... 42 » alpinum 43 9 7 cernuum 44 9 > Warneum 45 99 turbinatum 46 99 roseum ... 47 99 nepalense Common. Common, summer. Very common, sum- mer. Common, summer. TrRIBK HYPNACEAS. Fabronia minuta Hypnum a’gentatum, Mitten Buchanani cameratum, Mitten kamounense p'nmosum rusciforme commutatum ... „ fllicinum Meteoriutn squarrosum ... Stereodon condensatus, Mitten „ caperatus, Mitten „ taxirameus, Mitten „ plicatus [Neckera] „ prorepens, Mitten 99 99 99 99 99 99 99 Common. Ditto, summer. 63 macrocarpus ... ... ... 64 „ serrula, Mitten ... Diwali, 8,500. Tribe Neckera ceas. 65 Neckera Straclieyana ... ... 66 „ crenulata • . • ... Tribe LEUconoNTACEiE. 67 Hedwigia attenuata ••• Above 10,000. 68 Leucodon secundns ... ... Common. 69 Cryplisea concavifolia • •• Binsar. June. Com- mon. Tribe Leskeaceas. 70 Anomodon tristis ... ... 71 acutifolius, Mitten ... • t • 72 Trachypus blandus [Neekera] • • • 73 Buchanani [Neekera] ... ... 74 Leskea scopula, Mitten ... • • • 51 m HIMALAYAN DISTRICTS OF THE N.-W. PROVINCES. DIVISION VI. — ACIiOGENiE — ( concluded ). No. Scientific name. Vernacular name. Note. ORDER 7. — BRYACEJ5 — (concluded). Tribe Lbskeaceae— ( concluded). 75 Leskea Wallichii [Hypnu n] On trees, May. Askot. 76 „ assimilis, Mitten 77 „ haplohymenium [Hypnum] . , , , 78 „ cymbifolia ... Common, May. Tribe Mniaceje. 79 Fissidens sylvaticus 80 „ viridulus • • . 81 Mnium rhynchophorum ... Common, summer. 82 ,, tricliomanes ... 83 Mniadelphus humifusua ... Tribe Hypopterygiaceie. 84 Cyathophorum intermedium ... ... Tribe Polytrichace^b. 85 Atrichum flavisetum 86 Pogonatum himalayanum, Mitten ... Resembles urnigeruna. 87 ,, micrqstomum 88 „ aloides Ground. Blnsar, April. .89 „ fuscatum, Mitten 90 Polytrichuni perichaetiale 91 Lyellia crispa ... ... ■ CHAPTER Y 1 1 1 . r Scientific Botany — ( continued ). CONTENTS. Plants found in Kumaon, Garhwal and the adjoining parts of Tibet by Captain (now General) Richard Strachey and Mr. Winterbottom. The following extract from- Hooker and Thomson’s “ Introduc- tory Essay 2 to the Flora Indica ” regarding the value of General Strachey’ s and Mr. Winterbottom’s botanical work in India appears to be a fitting introduction to tide list of plants discovered by them in Kumaon, Garhwal, and in the neighbouring parts of Tibet.- « The collection distributed by Captain Strachey and Mr. Winter- bottom consists chiefly of the plants of Kumaon and Garhwal, and of those of the adjacent parts of Tibet. Captain Richard Strachey was appointed by the Indian Government to make a scientific survey of the province of Kumaon, and was occupied on the task about two years, during which time, in addition to the important investigations in physical science which occupied his attention, he thoroughly explored the flora of the province, carefully noting the range of each species. He was joined by Mr. Winterbottom m 1848, and they travelled together in Tibet. Their joint collections, amounting to 2,000 species, were distributed, in 18o2-53, to the Hookerian Herbarium, the British Museum, the Lmnsean Society and some foreign museums ; and the scientific results are now m course of publication. The beautiful preservation of the specimens, and the fullness and accuracy with which they are ticketed, render this herbarium the most valuable for its size that has ever been distri-* buted from India. The original printed list was put into Mr. Dutliie’s hands by General Strachey in 1876, shortly before starting for Imha to take up his duties at the Saharanpur Botanical Gardens. N ot having si cient time to revise the whole of it by an examination of the specimen. i The materials for this Chapter were placed at my Qu-ator “of the R. Strachey, and have been edited and anangeU by ^ Botanical Gardens, Saharanpur. 404 hima'latan districts preserved in the Kew Herbarium, his notes were left behind to be completed by another hand. These notes together with the single copy of the original catalogue were missing for a time. The list however was found, and since then Mr. C. B. Clarke has under- taken to revise it up to the end of the Polypetalse, as well as the willows, the grasses, and the two families of Urticacece and Piperacece. After completing the revision of the polypetalous orders Mr. Clarke remarks, u I may add that the only use of the above verification must be to show how very good the names in the list are ; it would be useless to carry it on further, for in the next order (as Composites ) it would be better to name up the Herbarium by the list than to reduce the list by the Herbarium. For unless the order has been specially worked up, as to the Indian plants in the Herbarium, it is not so carefully sorted out as were the Strachey and Winterbottom plants originally.” The following explanatory notes by the same botanist should also be recorded: — “ In the above reduction all that is asserted is that I have seen the ticket of Strachey and Winterbottom copied on the left-hand side of the page, and that when I saw it, it was in the new bundle having the name on the right-hand side: nothing beyond this. As regards the missing tickets, it appears that some of the common plants (as Nelumbium, #c.), were never laid in. Secondly, that where these were duplicates of the same plant under several numbers, some of the duplicate numbers were distributed. Thirdly, that some of the fragmentary or critical species were set aside and named in MS. on the sheets, no printed ticket being placed on the sheet, but the name being carried into the printed list. I only discovered this in the beginning of Leguminosas , and have found several of the written-up sheets since. They are among the most important to find ; but without printed tickets they can hardly be found in a Herbarium of this size unless they are lighted on by a fortunate accident. Lastly, after these three causes have been allowed for, there are certain plants, as Mucuna atropurpurea, which I cannot find anywhere, though I have made a special and long search for them. I can only suppose that Mucuna atropurpurea was named on a flowering specimen or fragment that it was consi- dered useless to paste down.” OF THE NORTH-WESTERN PROVINCES. 405 The arrangement of the revised list has been made to correspond with that of the Flora of British India, as far as that work has been completed ; the names of many plants have consequently been altered in accordance with the nomenclature adopted in that work. As the reference number of each species in the original catalogue is given in column 2, the old name is not added except in the case of plants now referred to a different genus. As the reference number of each species in the original cata- logue is given in column 2, the old name is not added except in the case of plants now referred to a different genus. ABBREVIATIONS USED IN THIS LIST. In Column 3. H. for herb S. or Sh. for shrub. H. cr. )) creeping herb ,. S. H. herbaceous shrub. H. fl. )) floating herb .. S. P. parasitical shrub. H. pr. >> prickly herb . S. sc. „ climbing shrub. H. sc. }) climbing herb . . . S. T. arborescent shrub. Herb S. & W. per herbarium of Strachey and Winterbottom. In Column 5. Bl. for blue ... Or. for orange Sc. for scarlet. Br. „ brown ... Pk. „ pink W. white, Gr. „ green ... Pr. „ purple Y. yellow. Li. „ lilac ... R. ., red. 406 HIMALAYAN DISTRICTS List of Kumaovb Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. t Time of flowering. Locality. I.— RANUNCULA- CEiE. 1- Clematis. montana, Ilam. (7) S. sc. 10'— 12' W. April Naini Tal, &c., var. major (?i) S. sc. 10'— 30' w. May Madbari Pass, barbellata, Edgcm ... (6) S. sc. 6' Y. Pr. May &c. Dwali, Madbari grata, Wall. (12) S. sc. 10' Y. Gr. October .. Pass. Almora, See. ... Gouriana, Roxb. (9) S. sc. 10' Y. Gr. December, Kota-dun, Kap- puberula, Hf. S' T. ... (14) S. sc. 10' Y. Gr. March kot. Outer hills, orientalis, L. Pr. Ukhimath. var. acutifolia (3 & 4) S. sc. 2'— 3' August ... Milam, Niti nutans, Royle (13) S. sc. 10' Y. Gr. March Laptel, Guge. Outer hills, acuminata, DC. (1) S. sc. 6' <-8' • * • July Ukhimath. Naini Tal, Bin- connata, DC. (2 & 6) S. sc. 6'— 8' W. Y. J u 1 y-A u- sar. Naini Tal, Ra,- Bucliananiana, DC. 11 S. sc. 10' Y. Gr. gust. October . . . lam liiver, &c. Almora, &c. ... grewiadlora, DC. 10 S. sc. 8' Y. Gr. December, Thai, &c. 2. Anemone. albana, Stev. ... • • • . . . . • . • • • rupicola, Camb. 1 H. 9" Wh. June Pi n d a r i , vitifolia, Ham. 8 H. 2' — 3' Wh. July Kogila. Naini Tal, &c., obtusiloba, Don. 4 H. 9" Wh Bl. June Namik, Kam- ni, Bompras, Rim- var. Govaniana, Wall, 9 H. 3"— 6" Or. Pr. August ... rnpestris, Wall. kim. • •• rivularis, Ham. 3 H. 9" Wh. A ugust . . . Ralam ... var. hispida, Wall. 7 H. 1' Wh. May Naini Tal polyanthes, Don. . . • . . . Wh. • • • var. villosa, Royle .. 2 H. i'— ii' May Pindari, Rogila narcissiflora, L. .. ... • . • • • • Rirnkim. • • » tetrascpala, Royle ... . . • . . . ... Wh. • •• • • • elongata, Don. 5 H. 1'— 2' June ... Chechani-khal, ©F THE NORTH-WESTERN PROVINCES 407 Plants.. i o 3 3- Thalictrum. elegans, Wall. 3 H. 1' ... June ... Ralam River ... platycarpum, Hf. Sf T, 4 & 13 H. to 2' July Milam reniforme, Wull. 10 IT. 4' June Ralam River ... paucifiorum, Royle ... 5 H. 2' ... July Piti & Gori Rivers. peduncul &tx\.vo.,Edgew , alpinum, L. ... ... ... var. acaule 2 II. 3"— 4" July Pindar, Hoti, Guge, „ microphyllvm... 1 H. S" — 4" ... August ... Bar j i k an g Pass, &c. Punduanum, Wall. ... 9 H. 1'— 2' Wh. July Naini Tal, &c , eaniculaeforme, D. C., 7 H. 1' Wh. July Naini Tal, &c. , javanicum, 111. 8 II. 2'— 4' Wh. May Dwali foliolosum, DC. 11 H. 4' W. Pr. July Naini Tal, &c. r minus, L. 12 H. 2'— 3' ... August ... Niti, Laptel ... 4. Callianthemum. cachemirianuni, Cavib, 1 H. 2" y. Pk. J une Pindari, Bom- pras. 5. Adonis. chrysocyathus, Hf. § T. ... H. 9" Y. July Rajhoti 6. Ranunculus. aquatilis, L. 1 H. fl. 1'— 2' Y. Wh. August . . . Baiqrhu, Gya- nima. Cymbal arise, Pursh ... 23 H. cr. 1" Y. September, Guge Yalleys, pulchellus, C A. Mey., 18 H. 11" 1 2 Y. August ... Bompras, Niti Pass. var. 19 H. 6"— 9" Y. September, Shangcha. &c.. lobatus, Jacc[. hyperboreus. Rotlb. ... 3 & 20 H. 2"— 3" Y. Y. September, Burphu, Guge, var. natans 22 H. 3" September Topidhunga ... „ radicans 21 H. cr. S' Y. September, Topidhunga ... Chferophyllos, L. ... affinis, Dr. 15 H. 6"— 12" T. June Knlhara hirtellus, Royle 4 H. 6" I " August .. Bar jilcang Paso OF THE NORTH-WESTERN PROVINCES. 409 Plants — (continued). d • r-H o > o pQ c3 -4-3 i) Hima- laya. r* 4-1 0 CQ 1 +3 • pH n—< d o O ^ a» ' w i 3 M n 4 s a Remarks. Open 11,000 R. d'. | Do. 1 1,500 . . . = TJiaUctrum No 10, in Herb. S. Woods 8—10,000 R. ... On rocks 7,500 R. ... ... & W. . . . ..• ... ... Herb. Winterb. No. 53. Open 12,500—15,000 R. D. T. ? = T. alpinum, & No. 793, Herb. Do. 11—15,000 R. ... ... 4 Winterb. Banks 4—8,000 •R. ... ■On trees 7 — -.8,000 E. ... ... W oods 8,000 E. ... Open 3—7,000 E. b. T. Do. 9—15,000 ... Do. 12,500—14,500 R. * ^ D. ... Wet, open 15,500 T. — A. pyrenaica and Trollius No. 2 Ponds 11,500—15,500 D. T. in Herb. S. & W. Near water 14—15,000 T. Open 14—17,000 ... b T, - In water 14—15,000 . . . D. T. Open 11,500—15,000 ... T. Do. 14—16,000 ... T Do. 14—15,000 T. ... . . . Herb. Winterb. 736. Do. 11,000 ... Do. 14,700 R. ... 1 52 * 410 hima'layan districts List of Kumaon ^ l £ 3 bb S . C3 ^ -d is 4* d c3 d O * O .S *C o fe Name. l-i o 02o td O +3 MH o o o Crf rQ J=l 5 »rH t; cq tu 3 fcX) o a c3 O a W w o H i-i hirtellus var. 6 H. i"— n r/ Y. June Kalhara G H. 4" — G" Y. June Lahur 8 & 9 H. 2" Y. June Ealam, Pindari Valley. 55 1G H. 3"— 4" Y. August ... Bompras 17 H. 2" Y. August ... Bompras sceleratus, L. diffusus, D.C. 13 H. 2' Y. February, Plains, Almora, Lahur, Chami var. mollis 10 H. 3"— G" Y. June Pass. „ obtectus ' ... 11 H. 1' — 2' Y. June Jagesar, &c. ... lsstus, W all. 12 H. 2'— 3' Y. February, Common flaccidus, Bf. T., 2 H. 4"— 1" Y. May Lahur arvensis, L. 14 H. i'— 4' Y. February, Almora, &c. ... 7- Oxygraphis. glacial is, Bunge 1 H. 3" Y. July Bar jikang Pass. polypetala, Bf. fy 2\, 2 H. 3" Y. May Champwa, &c. 8- Caltha. palustris, L. var. Govaniana ... i H. 9"— 15" Y. May Madhari Pass, „ Bimalcnsis . . . 2 H. 2' — 3' Y. May J huni 9- Trollius. acaulis, Lindl. 1 H. 6" Y. June Pindari, Kulha- ra. pumilus, Bon. 2 H. r— 2' Y. August ... Bar ji kang Pass. 10- Isopyriim- grandiflorum, FisoTi ., 2 H. 3" — 6" Bl. Or. July Niti, Topi- dhunga. var. miorophyllum.. 1 H. 3"— 6" Bl. Or. June Pindari, &c. ... 11. Aquilegia. • vulgaris, L. . • . , • • . . . . . « Naini Tal var. pubiflora 2 H. 1'— 2' Pr. July „ pyrenaica 1 H. 2' Fr. June Pathakori 1 i . : OF THE NORTH-WESTERN PROVINCES 411 Flants — (continued) . 6 C<3 •X • r-H o > .3 3 Ps >> Jh ft Tibet. Remarks. Open 10,000 E. . . . ... Wet 9,500 R. ... Open 1 1,000 R. . . . ... Do. 14,500 E. ... . . . Do. 14,500 R. ... Fields 1—1,500 R. • • ‘ ... Open 7,600—10,000 E. ... ... Do. 6—9,000 E. ... • • • Do. 3-7,000 R. ... »■* Wet 10,000 R. ... *•« Fields 5,000 R. Open 14,500 R. ... • • • Do. 12,000 E. ■? = CaTlianthemum No. 2 in Herb. S, and W. © • * R. ... Wet, open 9,000 ... ... Do. 8,500 R. Open 11—12,000 E. . . . <•« Do. 13,000 E. ... » • • On rocks 11,500—15,600 • . • D. T. Do. 11—13,000 R. ... »•« • •• Woods 7,500 E. ... Open 10,500 R. . . • 412 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 12- Delphinium- denudatura, Wall. ... 3 PI. 2'— 3" Bl. June Naini Tal, &c.. caeruleum, Jacq. 10—18 H. 3"— 2" 2"— 3" Bl. August . . . Laptel, Niti, Guge. datum, Wall. • • • . . . ... . . . . . . var. ramincvlifoli/wm... 2 H. 3 / Pr. August . . . Ralam River ... vestitum, Wall. «. 7 H. 1' Gy. August . . . Tola cashmirianum, Wall., 5 H. V Gy. August . . . BarjikangPass, var. 6 H. 2' Bl. September, Pindari Brunonianum, Hoyle. 4 H. 2' Bl. August . . . BarjikangPass, 13- Aconitmn- Lycoetonum, L. ... 4 PI. 3' Bl. May Madhari Pass, ferox, Wall. ... 3 PI. 3' — 4' Bl. August .. Bar j i k a ngP ass, Pindari. Napellus, L. 5 PI. 6" S" Bl. August ... BarjikangPass, Leptel, Milam, var« multip.dwn 2 H. 6" — 12" Bl. September heterophyllum, Wall., 14- Aetsea- i II. 2' Bl. July Pindari, Milam, spicata, L. Ml IP. 2' Wh. May Kulhara .. 15- Psecnia- emodi, Wall. ... II.- MAGNOLIA- • •1 II. 2'— S' Wh. May Naini Tal, &c. CEAC. 1- Michelia- Kisopa, Ham. ... III. — MENISPER- T. 50' Wh. May Gagar MACE25. 1- Cocculus- iaurifolius, D.C. ... 1 T. 20' Gr. March ... Outer hills, Al- mora. OF THE NORTH-WESTERN PROVINCES 413 Plants — (continued). Conditions of soil, & c. Elevation in feet above the sea. ; 1 Hima- laya. Tibet. Remarks. .2 5 K S-. ft d o & C 5—7,500 R. Do. 12—15,500 D. T. Do. 9,500 R. ... Oi t • Do. 11,500 b. . 4 4 Do. 12—15,000 E. D. • • t Do. 12,000 R. 4<>* Do. 14,700 E. l«l Near water in 8—9,500 R. Ml woods. Open 12—13,500 R. D. Mt Do. 13,500 R. • • 4 Do. 12,500 — 15,000 ... D. T. Do. 12—13,000 R. D. • •• * 9 \ Shady woods ... 9—11,000 R. • •• Ml Woods 5 — 8,000 R. • • • ... Forest 6—7,000 R. ... Open woods .. 1—5,000 R. • • t ... / 414 HIMALAYAN DISTRICTS \ List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). Habit of plant. Height of growth. Colour of flower. Time of flowering. Locality. 2 Stephania- hernandifolia, Walp., 3 H.sc. • • » •M ? elegans, ///'. T. 2 H.sc. 2'— 3' Pk. June Kathi, &c., ... rotunda, L. 1 H.sc. 10' Gr. Y. May Bagesar ... 3- Cissampelos- Pareira, L. Ml S.sc. O'— 8' Gr. Y. May Almora, Bage- sar. IV„ — BERBERI DA -• CEH£. 1. Holbsellia- latifolia, Wall. 1 S.sc. 15' Pr. April Shamket, &c.. var. anghstifolia ... 2 S.sc. 15'— 20' M< Ml Binsar 2 Berberis. nepalensis, Spreng. ... vulgaris, L. 1 Sh. 6' Y. February, Binsar, See. ... var. cretica 11 Sh. 6' Y. May Pindari, Bam pa. umbellata, Wall. 10 Sh. 10" Y. May Dwali aristata, D . C. 2 & 5 Sh. 8'— 12' Y. April-May. Binsar, N a i n i Tal. D u d a- toli. var. jloribunda 3,4 & 8 Sh. 10'— 12' Y. May Dwali, Namik, Lycium, Royle 7 Sh. O'— 10' Y. April Kazi, Nandaki Kiver. asiatica, Roxb. 6 Sh. G' Y. April Alnrora, &c. ... concinna, H. f. . . . • • ■ it* ... • •• Ml var. 9 Sh. U' Y. May Eazi ... 3- Podophyllum. emodi, Wall. ... H. 1' — 2' W. May Pindari ... Y. — NYMPHJSA- CEH5. 1 Nelumbium. speciosum, Willd. ... HI H. Ml W. August ... Bhirn Tal ... / OF THE NORTH-WESTERN PROVINCES 415 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hir la\ .9 c3 « itf- ia. >> ft Tibet. Remarks. • •• 5,000? R. Open 6—7,500 R. ... Forest 3,000 R. • « • Open 3—6,000 R. ... • •• Opeu woods ... 5—7,500 R. m Forest 7,000 R. • •• •5 Woods 6—8,000 R. *•• • • • • •0 Open 10—11,000 ii! D. .•» Ml Do. 9—10,000 R. • • • ..t Do. 6,500—10,000 R. i«n Do. •• 8—10,000 R. « • • • •• Do. 3,5—9,500 R. • •• • • • Do. 2,5—7,500 R. » 0 i ... • •• Woods ... 9,500 R. • •• ... Open 10,500 R. • • • • •• In water 4—5,000 R. • •• • •• • 416 HIMALAYAN DISTRICTS List of Kuma on Si fl bb 0 Pi ^ rd 4-3 +3 U .2 Name. S •0 T. Do. 15,000 • • • ... T. Do. 10,000 ? R. ... ... Do. 11—12,000 R. D. ... | Do. 14—15,000 R. D. • •• Woods 6—8,000 R. ... • •• Rocks 7—8,000 R. • • • ... Open 10,000? R. ... ... Do. 9—11,500 • • • . D. 53 418 HIMALAYAN DISTRICTS List of Kumaon Jh l gj d 3 ^ » bo 2 £ & 4-3 -UJ u Name. 3 "S' d 5>o u bo 7+ <4-1 > o • p-H h +J ^ "o o «H o o +3 ri O £ o -4-3 S3 ^ §3 i .5? o 0) 9 d o W O ' w W o a 3- Fumaria- par vi flora, Lam, var. Vaii until •• • • • H. 6" — 12" R. January • ••• Plains,Almora, VIII.— CRUCIFERiE. 1. Parrya- maerocarpa. Br. i B. . .. ... August ... G mge lanuginosa, ti.f Sf T, 2 H. 2" 3 W ? September, Lanjar 2- Cheiranthus- himalayensis, Camb... • •• H. S' 7 Pr. July Unt a-d h u r a. &c. 3- Nasturtium- officinale, Br. 2 II . 6" Wh. June Alniora, &c. indicum, B C. 1 H. 1'— 2' ? March .. Outer hills 4- Barbarea- vulgaris, Br. H. 1' Wh. AnguSt ... Ralam 5- Arabis glabra, Crantz ... ... ... • •• Ml • • • alpina, L. 14—15 II. 1' 2' Wh. August . . . Niti a'liplexicaulis, Edgem, 1, 2 &3 H. 6"— 18" W. Pk. May Nadhari Pass, 6- Cardamine. hirsuta, L. 3 & 8 H. 1' Wh. March ... Almora impatiens, L. macropliylla, Willd. j r 9 H. 1'— 2' Wh. March ( June- ) l July, £ Outer hills Namik, Kulha- 1,2, & 4 II. 1'— 3' Pk.W.Y. ra Sing-jari. var. foliosa ) Naini Tal 7- Alyssum. caneBcens, 1) C. ... • • • H. 2" • «« July Tisum 8 Draba. alpina, L. ... 2, 7 H. 1" Y. August .. Kyungar, Barji | kang Pass. incana, L. 8, 9 H. 2"— 8" Wh. August .. Niti, Gugd, | Riinkim. lasiophylla, Royle .. l H. 1" — 4" Wh. July Milam, Gugd... I OF THE NORTH-WESTERN PROVINCES. 419 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the area. Hi la% * .5 5 md- /«. ti « Tibet. 1 .1 Remarks. Fields 1—5,600 £ • • • » « * Open ... 14—15,000 * • » T. Do. 17,500 • •• T. Do. 16—17,000 D. T. Water 1—12,000 R. Open 1—6,000 K. o • » • • • Do. 6—12,000 R. ... = Cruciferce ignoicR No. 10 in Herb, S. & W. Open 11,500 ... D. . . . = Cruciferce ignotsB Nos. 11 and 12 in Herb. S. & W. Wet 8—10,000 R. ... ... = Cardarnine No. 5 in Herb.S. & W._ Open 5—6,000 R. = Cardarnine No. 3 in Herb.S. & W. Do. 5—7,000 R. .. j Wet 6—10,000 R. ... ... = A rains No. 5 in Herb. S. & W. Open 15,000 » • • T. = Dr ala No. 5 in Herb. S. & W. Do. 14—16,000 R. D. T. No. 2 in part Herb. S. & W. Do. 11,500—15,500 ... D. T. Do. 15 -16,500 D. T. ’ = No. 2 (partly] Herb. S. & W. 420 htma'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 9- Cochlearia. scapiflora, H. f. T., 10- Sisymbrium. ... H. 2" Wh. August ... Guge mollissimnin,C.H. Mey, 3 H. 4" — 8" Pk. July Rimkim himalaicum, B. f. $• T. 7 H. 6" 1 Pk. August ... Milam Thaliannm, Gay 8f 8 H. r-y Wh. March .. Alinora Monn. rupestre, Edgew . G H. 1' — 2' Pk. August .. Palarn strictum, H.f. T. ... 5 H. 1' . . . July Garhwal Wallichii, H.f. &■ T. ... 9 IT. 1 ' — 2' Pr. March ... Almora Sophia, L. 2 II . 2'- 3' Y. May Almora Columna3, Jacq. .. 4 H. 2' - 3' ... July Rimkim Alliaria, Scop. .. 1 H. 2' Wh. May Almora 11- Eutrema. primularrefoliuai, H /., H. 4''- -6" Pr. May Madliari Pass, s- T. 12. Erysimum. hieraciifolium, L. 1 H. 1 2' Y. July Rimkim, Joshi- math. Sp. 2 H. 1" Y. August . Guge 13- Christolea erassifolia, Carnb . « ■ « H. 1' ... July Sattag river in Guge. 14- Braya. rosea, Bunge .. ... H. 2" £ Wh. July Sagta-deo, Guge. 15- Brassiea, nigra, Koch. H. 1'— 3' Y. March Almora, See. campestris, L. ,.. • •• H. V— 3' Y. March Almora, Milatn, juncea, H.f. Sf T. ... ... II . 1'— 3' Y. March Almora, & c. .. 16- Eruea. sativa, Bam.. • •• H. U' Wh. May Almora, &c. ... OF THE NORTH-WESTERN PROVINCES. 421 Plants — (continued). o o ax o ax (3 O T 3 0 O O Open Do. Do. Fields Open Do. Fields Do Open Fields Rocks Open Do. Do. Do. Cultivated Do. Do. Do. a> > o 33 o3 o CJ S-l n o cS D ' S 15,500 13,500 13.000 5— 6,000 12.000 6 — 8,000 6 — 6,000 6 — 6,000 13,500 5—6,000 9—10,000 6—14,000 15.500 13.500 10—16,500 1 — 6,000 6 — 11,000 1 — 6,000 1 — 6,000 H im a - laya. a c5 R. R. R. R. R- R. R R. (H Q R. R. R. R. R. D. Remarks. a) 33 T. .. ! T. D. D. D. T. T. ■ Arabic No. 10 Herb. S. Sc W. Aribis No. 8 and < rucif. ig tot, No. 14, Herb. S. & W. ‘ : Arabis Nos. 7 & 9, Herb. S. ScW. = Crucifer, lynot. No. 5 Herb. S. & W. ss Crucifer, lgnot. No. 1 Herb. S. & W. = Arabis No. 6 in Herb. S. S<, W. T. Draba Nos. 3 & 13 Herb. S. & W. = Sinapis No. 5 Herb. S. & W. = Sinapis Nos. 2, 3 and 6 Herb. S. & W. = Sinnpi< Nos. 1 and 4 Herb. S. and W. 422 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. 17- Capselli Bursa-pas tori s, Manch. • •• H. Thomsoni, H,f. 18- Lepidium- Sativum, L. capitatum, H./.Sf T., 1 H. 2 II 19- Msgacarpsea- polyandra Benth. ... » • • II. 20- Thlaspi. arvense, L. 3 II. alpestre, L. II. 21- Iberidella- Andersoni, FJ.f. 8f T., t • X H. 22- Crambe- cordifola, Stev. H. 23- Raphanus- sativus, L. • • • H. 24. Chorispora sabulosa, Camb. « • • H. IX. -CARP ABIDED. 1- CleomB. viscosa, L. • M II. 2. Capparis. horrida, L. Sh. Height of plant. Colour of flower. Time of flowering. Locality. 1'— 2' Wh. All the year. Ubique * * * • • • 1' Almora 4" Wh. August ... Mi am, Top id hunga. 5'~G' Wh. May Champwa, Pin- dari. 1" Wh. July Almora 6" Wh. J uue Rajhoti 2" - 4" Wh. July Sagta-deo, Gu- ge. 4' — 5' Wh. July Rimk m 1' ... Vlarch Plains to Al- mora. 3" • • • Tuly Rimkim 3' — 4' Y. August ... Sarju river, outer hills. 10' | W. Gr. March Bhabar OF THE NORTH-WESTERN PROVINCES. 423 FI ants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. HimA- layn. j Tibet. Remarks. Rainy. Dry. Open 5—12,000 R. • •• Ml » » ... • •• ... Herb. Strachey No. 15. Fields 5-6,000 R. Open ... 13—15,000 R. D. T. Do. 12,000 R. * • • • •• — Crucif. iqnot. No. 15 in Herb. S. and W. Fields 5—6,000 R. Open 15,000 *• * * * T. Open 10—16,500 R. » ? D. T. = Draba Nos. 8, 4, 11, 12, in Herb. S. and W. Do. 14,000 *• • T. = Crucif. ignot. No. 4 in Herb. S. and W. Cultivated 1—6,000 R. • •• Open 13,500 ... ... T- Do. 2—3,000 R. Ml = Polanisia viscosa in. Herb. S. and W. Forest 1—2,000 R. • • 1 • •• Forest 424 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. X.— VIOLACErE. 1. Viola. biflora, L. ., , 1 II. 3" Y. May Naini Tal, &c., Patrinii, DC. ... 3, 4, 10 If. 2" — 5" Bl. March- Outer hills, serpens, Wall. 5,6, 7,8, H. 2"— 6" Bl. W. July. March- Batnpa. San i an gent h a, kunawarensis, Royle , 9,11. 2 H. 1"— 2" Bl. J une. July Almora, Nai- ni Tal, &c., Kyungar XI. — BIXINEiE. 1- Flacourtia- Ramontchi, L'Herit... • • • var. occ idental is • • • T. 26' i • * February, Bhabar ... XII.— PITTOSPO- REJ£. 1- Pittosporum. fioribundnm, W.SfA., 1 T. • x • Bhabar eriocarpum, Royle ... 2 T. 20'— 30' • • • April Outer hills ... XIII.— POLYGALA.- CE/E. 1. Polygala, triphylla, Ham. 1 H. 2" — 3" R. August ... Paton var. glaucescens .. 2 H. 3"- 4" Y. August ... Ramari crotal arioides, Ham. 7 H. 6''— 12" Pk. May Almora, &c. •• abyssinica, Frcsen. ... 6 H. 12"— 15" Pk. jApril Kapkot, outer persicariasfolia, DC., 4 Id. 6" Pk. 1 July hills. Jagesar chinensis, L.. 3 H. 6" Y. Gr. July iAlmora sibirica, L. 5 H, 6" Pk. May Kosi river XIV.-CARY OPH YL LACEAE. l. Gypsophila. cerastioides, Don. ... I H. 2" Pk. I August ... Namik, Ralam 2- Saponaria- Vaccaria, L. Mt H. 2'— 3' Pk. March Outer hills .. OF THE NORTH-WESTERN PROVINCES 425 \ Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Himd- laya. 1 | 'F>qtX Remarks. Rainy. (-1 ft Open wet 8 13,500 R. D. • • i Banks, & rocks, 4 — 1 1,000 R. D, ... Do. 3-11,000 R. D. ... Open wet 15,500 ... ■ • • T. Forest 1—2,500 R. • •• • •• it. = F. sajrida, in Herb. S. & W. Forest 1—2,000 R. Open 4,000 R. • •a Do. 6,000 R. Do. ... 4,500 R. ... ... Do. 4-7,000 R. ... • • Do. 2,5—4,000 R. ... • • • Do. 6 — 6,500 R. ... . • . Do. 4,000 R. ... Do. ••• 6,000 R. ... • 0 • 8—12,000 R. . r * 1- 4,000 R. »*# = Vnccaria parviflora , Mccnch & Silene -No. 9 in Herb. S. fis VV. 54 42(3 HIMA'LAYAN DISTRICTS List of Kumaon U I > *3 a; 44? ft cS ft ■s 1 ft *3 O O 3. Silene- inflata, Sm. i H. 1' 9' Wh. June Outer hills, Mi conoidea, L. lam, Niti. 2 H. l'—2' Pk. March Alu ora Moorcrofiiana. Wall., 4, 10 Id. 6" — 9" Pk. August ... Gothing, Eakas Falconeriana, Benth., tal . 5 H. 3' Gr. Y. July Almora Griffithii, Bo ss. 7 H. 2' Wh. July Bampa Stracheyi, Edgew .. 8 H. 3' Wh. August .. Piti river 4- Lychnis. apetala, L 4,6 H. 4"— 7" Wh. July Ralam, Guge.. macrorhiza, Boyle .. 3 H. 4" Wh. September, Top i d h u n g a , brachypetala, Hort. .. LI an jar 5 H. 8" Wh. July Laptel, Ralam, indica, Benih. var. fimbriata 1 ii. 3' W. Pr. August ... Piti river pilosa, Edyew. 2 H. l'—»' Wh. August, Ra’ am, Tung- Septem- ber. nath. 5 ■ Cerastium- vulgatum, L. 2 H. 4" Wh. May Almora, &c. .. Thomsoni, Hook. f. . i H. 4" Wh. May Madhari valley, 6- Stellaria. paniculata, Edgew. ... I, 2 & 3. H. 1'— 3' Wh. May, July, Binsar, Shai- media, L. H. September, devi. 7 6" — 12" Wh. All the Outer hills, &c , scmivestPa, Edgew. ... Webbiana, il all. 9 Id. H. 1' 3"— 4" Wh. Wh. year. May March .. Chaur .. Almora latifolia, Benth. • • « H. 4" Wh. August ,. China, Naini longissima, Wall. ... 5 H. 1 ' — 2' Wh. Vlay ,,, Tal. lladhari I J ass, uliginosa, L. 8 H. l' 7 — 6 C/ Wh. VTarch .. Naini Tal. Almora, Barji- decumbcns, Edgew. ... 6 a | 6 " 1 Wh. August ... ] kang Pass. Milam, Eaiam, OF THE NORTH-WESTERN PROVINCES 427 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks. >> .5 3 O Do. I 5-11,500 R. D. 1 Do. 5 — 6,000 R. • • • Open 11—15,000 • • • D. T. Do. 4-6,000 R. < • • • • • Do. 11,000 D. t ( . near water 7,500 R. = Mlliandrium pilusum in Herb.. S. and W. Open 12—15,000 R. D. T. Do, * 15 — 17,000 •• D. T. Do. 12 -14,500 R. D. • •• = Mdiundruim pilosum in Herb, S. & W. • •• Do. 7—8,000 s- T* % 9 . • • Rocks, open 9 12,000 R. Open 5—7,500 R. • • Do. 10,000 1 R. Woods 7—8,000 1 R. Do, 1—6,000 R. ... Wet 6,000 1 R. *•1 Open 4-6,000 R. = Leucostemma No. 2 in Herb. S. and W. Rocks .0 6 - 8,000 R. • ■ • . , = Leucostemma No. 1 in Herb. S. and W. Open 6-9,000 R. • #* ... Wet 4—13,000 R. • • > • •9 Open 12—13,500 R - D. I • •• = Arenariu No. 9 in Herb. S. Sc W S 1 1 428 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth, Height of plant. — 1 Colour of flower. Time of flowering. Locality. 7- Arenaria- foliosa, Royle (M H. 2" Wh. June Jelam festucoides, Benih. ... 2 H. 3" Wh. August .. Pindar i,Karnali river . Tar. imbricata ... 3 H. 2" — 3" Wh. Ditto Balam musciformis, Wa//. ... 1 H. l" Wh. Ditto Balchha Pass ., scrpyllifolia, L. 10 H. 4" Wh. Ditto Jelam, Milam . glandulifera, Edge.iv. .. 13 H. 1" Wh. Ditto Barjikang, C h or h o t i Pass. Stracheyi, Ed yew. ... 1 • • ... ... holostcoides, Edyew. .. • • • H. 2" September, Rakas-Tal 8- Sagina- procumbens, L ... • ». ... .. • »« var. pentamtra 9- Thylacosper- 2 II. 1"~ 1*" • • ( June Jelam, Singjari, muni rupifragum, Schrenk., H. 1" — 2" Wh. July Huge 10- Spergula pentandra, L. ... • • • H. 4"_ 6" Wh. • • • Bhabar 11. Drymaria- cor data, Willd. • •• H. cr. 6" ... February. Kota Dun 12 Polycarpsea- corymbosa, Lam. ... H. 6"— 9" Wh. July Almora XIV*. — PORTULA- CEAi. 1. Portulaca. oleracea, L . «•( H. 6 i Y. July Do. OF THE NORTH-WESTERN PROVINCES. Plants — (continued) . 429 Condition of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks. Rainy. Open 9,000 D. — A! sine Roylei in Herb. S. and Do. •• 10—15,500 R. D. T. W. Do. • n 12,000 R. « • * Do. 15—16,500 T. Do. • • • 9 — 1 1 ,500 D. Do. • • • 14—16,500 R. D. 1(1 Do. 15,000 ... ... — Gyvsophila, No. 3 in Herb. S. & W. *• • Do. •• 9—10,000 R. d! >•• • • « Do. *»• 15—16,500 ... • • • T. Do. • • • 1—2,000 R. ... Ry water • • • 2,000 R. • •« ... In fields 5,500 R. jt * Do. t • 5,500 R. • • • • • • 430 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Straelic-y and Win- terbottom). Habit of growth. Height of plant. — 1 Colour of flower. Time of flowering. \ Locality, XY. — TAMAEISCI- NEAE. 1. Tamarisc. dioica, Roxb. Sh. 6' — 10' ■ «* • •• Kosi and Ganges 2- Myricaria- elegans, Royle. 1 Sh. 6' YVh. Pk. June rivers. Niti, Satlaj germanica, Desv. 2 Sh. 3' YVh. Pk. J une river in Guge. Pindari, Milam, XY*. — HYPERICI- NEAE. 1. Hypericum cerauum, Roxb. 6 Sh. 4'— 6' Y. February, Tisum. Almora, &c. . cordifoliu ", Chois. ... 5 Sh. 3' Y. August R dinar i patulum, Thunb 4 Sh. 4' Y. July Almora, & c. ... Naini Tal perforatum, L 7 Sh. 6" Y. July elodeoides, Chois. 1,2 Sh. 1 ' — 4' Y. July Jagesar, Hal am, nepalense, Chois. .. 3 Sh. r Y. July Almora, Kalamandi japonicum, 'l'hunb 8 Sh. 6" Y\ July Almora, &c. .. XVI. — TERNSTRAE- MIACEAi. 1- Eurya. acuminata, D C. .. Tr. 25' Wh. March .. Naini Tal, &c 2- Actinidia. callosa, Lindl. S. sc. 30'— 40' Wh. May Outer hills, 3- Saurauja nepalensis, D C. Tr. 10' Pk. November, Kapkot. Outer hills, &c., XVII — DIPTERO- CAEPEAE. 1- Shorea. robusta, Gctrtn. • •• Tr. 60' -80' April Outer hills ... OF THE NORTH-WESTERN PROVINCES 431 Flantc — (continued). Conditions of soil, & c. Elevation in feet above the sea. Hima- laya. Tibet. « Remarks. Rainy. Dry. 1 River beds ... 1—1,500 R. • •• j Open river beds 11—13,500 D. T. Do. • 11—15,000 R. D. T. Do. 3—6,000 R. • a » Do. 4,500 R. ... Do. 3—6.000 R. ... Do. 6,000 R. • •• • a - Do. 5—11,000 R. • •• Banks 8,700 R. • •• • • . Open ... 4—6,000 R. • •• Woods ... 3—8,000 R. • • • Forest 2—3,500 R. «*• • a a Forest 3 — 5,000 R. » • • ... Forest 1- 2,000 \ R. ... .« • = Vaticarobusta, in Herb. S. and W. Forest 432 HIMA'LAYAN DISTRICTS List of Kumcion Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flower. Locality. i XVIII.— MALVA- CEAfi. 1. Malva. verticillata, L. 2 H. l'— 6' Pr. August ... Piti river silvestris, L. 1 H. 1'— 2' Li. February, Kota 2- Sida. humilis, It illd. 2 PI. 3' Or. March ... Outer hills rhombifolia, L. 3 „ , Ain ora cordifolia, L 1 Sh. 3' Y. • • • Aim ora, Bage- sar. 3. Abutilon. polyandrum, S chi edit. 2 Sh. 2'— 8' Y. Or. August ... Outer hills, Bagesar. inJicuin, G. Don. 1 Sh. G 7 — -8' Y. March ... Bhabar ... 4- IJrena. lobata, L. • •• Sh. 4' Pk. August ... Outer hills, Bagesar. 5 ■ Hibiscus. radiatus, Willd. 3 ... 5' Y. August ... Below Almora, Solandra, Id Her it. .. • M H. 1' • •• August ... Hawalbagh ... vitifolius, L. 1 Sh. !•» Y. August ... Outer hills pangens, Roxb. ... PI. 6' Y. August ... Almora, & c. ... cancellatus, Roxb. ... 6. Thespesia. H. 3' — 4' Y. August ... Almora, &c. ... Lampas, Dalz.Sf Gibs. lit Sh. 4' • • i August ... Bhabar 7- Kydia. calycina, Roxb. ... • •• Tr. 20' Ml ... Bagesar, outer hills. OF THE NORTH-WESTERN PROVINCES Plants — (continued). 433 • o <*3 a> ► o Himd- .a c i lay a. • !— ( o QJ Cfi 4H o O 4-1 Remarks. d o o a> +3 a o o css aj !> -3 4) -M s Rainy. >> Tibet. 1 Open ••• 7,500 . R. Do. 2—2,000 R. ... ... 1 Do. 4,000 R. • « * Do. 5,000 R. ! ... Do. 3—5,000 R. Do. 1-4,500 R. ... ... Do. 1,000 R. > • • • 1 % Do. 1 — 3,000 j R. •• ... Do. Do. 4,000 4,000 R. R. • • . ... ' = Lagvnea lobata in Herb. S. and W. Do. 4,000 4-6,000 R. R. ... 1^ o Abelmoschus No. 3 in Herb. S. and W. Do. 3—5,000 R. • •• ... = Abelmoschus No. 1 in Herb. b. and W. Forest 1—2,000 R. p*. ... — Hibiscus No. 4 in Herb. S. and w. Do. „.J 2—3,000 1 R. 1 55 434 hima'layan districts List of Kumaon Name. Herbarium number (Stracliey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. XIX.— STEECU- LIACEJE. 1- Sterculia. villosa, Roxb. fulgens,' Wall. 2 • Helicteres- 1 Tr. Tr. 20' — 30' 30—40' • •• l« March March Outer hills Bhabar, outer hills. Ieora, Wall. 3- Pterospermum • •• Sh. 5'- 6' January .. Bhabar acerifolium, Willd. lanceaefolium, Roxb., XX. — TILIACEiE. 1 2 Tr. Tr. 30' • * • March Hardwar ... Bhabar 1- Grewia. oppositifolia, Roxb. ... asiatica, L. ... var. vestita leevigata, Vahl. 2. Triumfetta. 4 2 5 I Tr. Tr. Sh. 40' 20'- 30' 15' Buff Buff • « • May May Ml BhimTal below, Kota, Bagesar, Outer hills .. pilooa, Roth. rhomboidea, Jacq. 3. Corchorus. 2, 3 1 S. sc. Sh. 4'— 5' i' — i*' August ... August ... Kota, Alrnora, Bagesar. Hawaibagh. ... olitorius, L. acutangularis, Lam.... XXI.— LINE m. 1 2 H. H. 2 r l f , — 2 r Y. Y. August ... August ... Hawaibagh Hawaibagh .. 1* Linuxn. usitatissimum, L. 2- Eeinwardtia. 2 H. 2 r Bl. January ... Cultivated trigyna, Planch. ... Sh. 2'— 5' Y. I 1 anuary ... Cuter kills ... OF THE NORTH-WESTERN PROVINCES, 435 Plants — (continued) . 6 a> Himd- & d lay O CD '■H pi Remarks. c a ri o s *4- 3 • r -1 +a nd ri o O > r£3 — 2 ' Pk. September, Pandukesar ... 2 H. 9"— 1 2" Pk. March Naini Tal 8 H. 1' Cr. March . . . Outer hills ... 1 IT. 6" Y. All the year. Common 2 H. 4" Wh. March ... Dwali ... H. 4" ... ... 1 Kota Dun OF THE NORTH-WESTERN PROVINCES. 437 Plants — (continued) . Conditions of soil, See. k o .Q c3 4-3 <1> Hima- laya. r oi 4-3 I O H | Remarks. <4-4 .5 g cfl O 0) •43 ® at 0) ► X) ir Sh. 4' • •• February, Kota OF THE NORTH-WESTERN PROVINCES. 439 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Himd- lay a. 1 Tibet. > -1 Remarks. d 3 w Dry. Open 4—5,000 R. Do. 11,5— 12,500 D. Do. 8,5—12,000 • • « D. Shady woods ... 5—7,500 R. ... ... Do. 7,000 R. ... .. Do. 4,5—9,500 R. ... ... Shade 5,-9,000 R. Shade 6,-7,500 R. • •• - Shady woods... 9,500 R. '** • • • N Woods ... 4—7,000 R. • Q« — Rula albijlora in Herb. S. and W. Open 4—7,000 R. f *1 • 0 0 Do. R. 1 • * • •« Forest 7—8,500 R. • • • • *• Woods 1,5—3,000 R. • • • • •« Forest 7,-9,500 R. *•• • it = Limonia Laureola in Herb. S. and W. Do. 2,000 R. ... » 0 » * 440 hjma'layan districts List of Kmnaon Name. u L « c £ ^ 03 /A _ thg 1 c £ o .2 "5 S | ai 3 oS £ X5 jz ii (-< c/j a, ; * 1 Habit of growth. Height of plant. Colour of flower. Time of flowering. 1 Locality. 6- Murraya. Sh. 1 10'— 15' Wh. March ... Outer hills .. Kcenigii, Spreng. • * » T. 20' 1 March ... Bhabar 7- Citrus. medica, L. E2 Sh. 10' Wh. May ... Bagesar, outer 8- iEgle. M arm el os, Correa T. 20' • •• hills. Bhabar XXV.— simaru- 13 ACE M 1. Picrasma. quasso ides, Benn. ... T. 20' *•« BandkcBar XXVI.— BURSERA CEH£. 1. Garuga. pinnata, Hoxb. • • T. 40' • • • February, Bhabar XXVII.— MELXA- CEJ3. 1 Melia- Azadirachta, L. • • • T. 15'— 20' Li. March Almora, &c. ... 2 ■ Cedrela- Teena, Koxb. 1 T. 30' — 60' Wh. March Kota Duu, &c. var. serrata ... 2 T. 20'— 40' l J k. June Bandari-de vl , XXVIII— OLACI- NEH£. 1. Olax. nana, Wall , 1*1 Sh. 9"— 12" • •• July &c. Damus OF THE NORTH-WESTERN PROVINCES Plants — (continued). 441 Conditions of soil, &c. Elevation in feet above the sea. t Him a- laya . Tibet. Rainy. 1 Dry. Open ... 2—1,500 R. ♦ » • Forest 1—2,000 R. • « • ' * * Woods 2—3,000 R. ... ! Forest 1—2,000 R. ... ... Open 6,5 — 8,000 u. ... ... ♦ * « Forest 1,000 R. ... ... Gardens 1—5,000 , R - ... ... Forest 1 - 3,500 R. Do. 6—7,500 R. Open 4,500 R. i Remarks. Serger x Koeiiyii in Herb. S. and W. 56 442 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). 1 Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. XXIX.-ILICI- NEJE. i- Ilex. dipyrena, Wall. 3 T. 0 >• 1 o W. April N a i n i T a 1 , outer hills. odorata, Ham 2 T. 40' W. May Do. excelsa, Wall. 1 T. 25" W. May Binsar XXX.— CELAS- TRINEiE. - 1. Euonymus. tingens, Wall. ... 6, 7 Tr. 20'— 30' ... April, May, Naini Tal, Bin- sar, Madhari Pass. fimbriatus, Wall 4,5 T.orS. 10'— 30' ... May Dwali, N i t i Dugli, &c echinatus, Wall. 3 S. sc. 20' • ■ • May Dwali, &c. pendulus, Wall. 2 T. 30 r — 40' . . ■ March Gagar, &c. ... Hamiltoniamis, Wall. 1 Sh. 12' 30' ... ... Almora 2- Celastnis. paniculata, WUld. 2 Sh. 15' ... ... Bhim Tal 3 Gymnosporia- ruta, Wall. 1,4 Sh. 4' — 12' W; G. M arch, May, Sarju Valley, Bagesar. Royleana, Wall. 3 Sh. 12' ... ... Bhim Tal 4- Elseodendron- glaucum, Pers. XXXI.- RHAMNEiE T. 20'— 30' ... May Outer hills, Bhim Tal. 1. Ventilago. calyculata, Tulasne ... 2- Zizyphus. IM S. sc. 20'— 30' ... March ... Bhabar CEnoplia, Mill. 2 T. • • . Bikikhes rugosa, Lain, 1 T. 15' ... March ... 1 Kota Dun OF THE NORTH-WESTERN PROVINCES 443 Plants — (continued). Conditions of soil, &c. Elevation in feet above 1 the sea. Hit lai >> *3 p? n a- /a. >> n ® 1 Tibet. Remarks. Forest 5—9,000 ✓ k. Do. 3 - 4,000 R. . . . . . . Do. 4—7,000 R. Forest 5,5—10,000 R. Do. ••• 8—11,000 R. • so Do. 7—8,000 R. ... Do. 6—7,000 R. 9.8 ... Open ... 5,000 R. • •• Do. 4—5,000 R. ... it* Forest ... 3,000 R. • •• Open 4—5,000 R. »•« Forest 2—4,500 R. 1 • • • • •0 Forest 1—2,000 R. . • » ... Do. 1—2,000 R. ... «•« Do. 2,000 R. »49 HI 444? HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 3- Berchemia. fioribunda, Wall. . . . S. sc. 15' . . . ... Almora 4. Rhamnus. pei'sicus, Boiss. 7 Sh. 3' June Niti. Milam ... daliuricus, oil. 1 Sh. 15' G. Y. April Naini Tal, B;i- purpirreus, Edgew. ... 4,5 T. 20' — 30' M arch, gesar. Naini Tal, Bin- triqueter, Wall. T. 15' April, August . . . sar, Madhari Bass. Outer hills, Al- procumbens, Edgew. 3 Sh. 4' May mora. Naini Tal, Jag- thana. 5- Hovenia. dulcis, Thunb. • •• T. 40' Y. G. June Bagesar „. 6- Sageretia. oppositifolia, Brongn., • •• Sh. 10'— 12' August ,. Almora ... 7 Gonania. leptostachya, DC. ... 2 S. sc. 20' Ml • •• Bhabar 8 Helinus. lanceolatus, Brand. ... S. sc. © I f— 1 to • •• February, Kota Dun, &c., XXXII.— AMPELI- DEAL 1. Vitis. pallida, and A. ... »«* S. sc. • • • lanata, Roxb. 2, 3, 5 & 6 S. sc. 6'— 20' Ml May, June, Naini Tal, Al- parvifolia, Roxb 1 S. sc. 10'— 15' ru April mora, Gagar, Namik,Kathi, Dewali-khal. Pyura, Almora, himalayana, Brand.,.. 9 S. sc. 20' i • • May Madhari Pass, divaricata, Wall. 8 S. sc. 10' Ml June ... Dhakri-binaik. Naini Tal, out- capriolata, Don. • • • S. sc. 20' III May er hills. Naini Tal, Ka- lanceolaria, Roxb. ... til S sc. 20'— 30' Ml March ... j thi. Kota Dun, &c., i OF THE NORTH-WESTERN PROVINCES. 445 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Open 4,500 Do. 11,500 Forest 3—6,500 Do. 7—8,000 Open 5,500 Do. 6- 7,000 Forest 3—5,000 Open 2—5,000 F orest 1-2,000 Open 2—3,000 Woods or open, 4,5—7,000 Open 4—6,000 F orest 7—8,000 Open 3—7,000 Forest 6—7,500 Do. 3,000 Hima- laya. >> a • pH c3 M R. ... ... D. R. R. R. R. R. R. R. R. R. R. R. R. R. R. OJ Remarks. = Ceanothus No. 2 in Herb. S. & W. = Ceanothus No. 1 in Herb. S. & W. = Gouania No. 1 in Herb. S. & W. = Cissus No. i in Herb. S. & W. -.Ampelopsis No. 1 in Herb. S. & W. ■ Ampelopsis No. 2 in Herb. S. & W. = Cissus No. 2 in Herb. S. & W. 446 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth, Height of plant. Colour of flower. Time of flowering. Locality. 2 Leea. • aspera, Wall. ... • •• Sh. 4'— 5' June Almora, & c. ... XXXIII— SAPIN- DACEiE. 1. Cardiospermum Halicacabu n, L. • •• H. sc. 10' • •• Bagesar ... 2 iEsculus. indica, Colebr T. V r—1 CO 1 V o Tfi Pk. Y. May Dwali, &c. 3. Selileicliera. trijuga, Willcl. T. 30' in • • • Bhabar 4- Sapindus. Mukorossi, Geer in. ... T. 30' in t • • Bagesar 5- Acer. oblongum, Wall. ,. 1 T. 30' Gr. April Naini Tal, &c... lasvigatum, Wall. 2 T. 40' ( r. April Gagar, &c. caesium, Wall. 4 T. 50' Gr. March Dwali villosum, Wall. 5 T. 50' Gr. March ... Madhari Pass; caudatum, Wall. 6 T. 30' Gr. March ... &c. Ditto pictum, Thunb. 3 T. 30' Gr. Mach ... Naini Tal 6. Staphylea. Etnodi, Wall. Sh. T. 20' Wh. May Gagar, Binsar, XXX1Y.— SABIA- CEJ5. 1- Sabia. campanulata, Wall. .. 1 S. sc. 10'— 15' Pr. March ... Gagar, Namik, purpurea, H.f. and T., 3 Sh. 10' ... May Sarju valley, paniculata, Edgeiv. ... 2 S. sc. 30'— 40' ... March ... Bagesar. Outer hills ... OF THE NORTH-WESTERN PROVINCES 447 Plants — (continued'. c3 • r— < o GQ t> o & ci -+J 0) Hima- laya. O QQ d o • rH >r 3 G o o Elevation in fi the sea. Rainy. — Dry. | Tibet. 1 Remarks. V Open 4—5,000 R. 9*1 ••• Forest 3,000 R. ... • • • Do. 6 — 9,000 R. • • t ... = Pavia inched and Engelhardtia No. 2 in Herb. S.& W. Do. 1,500 R. ... ■? Do. 3,000 R. Do. 4—7,000 R. . . . • • . Do. 6—7,000 R. . . . ... Do. 8,500 R. . . . ... Do. 7—5,900 K. ... Do. 7, 5—11,000 R. ... ... Do. 6-8,500 R. . . . ... Do. 7—8,000 R. ... • • . Do. 6—8,000 R. • • • Do. 3,000 R. ... Do. 1—2,000 R. ... 1 • • 448 hima'layan districts Name. 2- Meliosma dilleniasfolia Wall. .. pungens, Wall. XXXV.— AN AC AR DIACEAC. 1. Rhus. Cotinus. L. parviflora, Roxb. semi a! at a, Murray ... succedanea, L. 2- Pistacia. integerrima, Stfivart, 3- Mangifera. indica, L. 4. Buchan ania. latifolia, Roxb. 5- Qdina. Wodier, Roxb. 6. Semecarpus. Anacardium, L.f. .. 7- Spondias. mangifera, mild. .. XXXVI.— COBIA- BIEiE. 1- Coriaria. nepalensis, Wall. List of Kumaon Herbarium number (Strachey and Win- tevbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 2 T 40' Wh. June N.imik, &c. 1 T. 40' Wh. May Lvapkot, Binear, 2 Sh. 10' Pk. April Gagar, Almora, T. 20' • • • .. Almora, &c. 4 T. 15' i • • June Almora, &c. ... 3 T. 20' March Bagesar ... T. 30'— 40' May Thakaio, Kosi River. ... Tr. 40' V. April Bhabar, plains, Almora, &c. ... Tr. 30' Wh. March Outer hills ... ... Tr. 30' Wh. March Bhabar Tr. 30'— 40' ... January ... Outer hills ... ... Tr. ... ... ... Bhabar . • • • Sh. 10'— 12' ... February, \ Common OF THE NORTH-WESTERN PROVINCES 449 Plants — (continued;. o > o Hirna- & lay a. 'o +» 0) 45 4 o .2 Remarks. § fl Oj o O CD *4-3 • >— < 00 433 d d» 4^ d • rH CD X s P5 Q H Do. 7,5—9,000 R. Do. 3,5-7,500 R. Do. 5—5,000 R, Do. 3—5,000 R. ... ... Do. 4—6,500 R. ... ... Do 3—3,500 R. Do. 2—5,000 R. ... ... = Rhus integer rima in Herb. S. and W. Cultivated 1—2,500 R. ... ... Forest 1—2,000 R. ... ... Do. 1,000 R. ... ... Do. 1—2,000 k s R. ... ... Do. 1—2,000 R. ... • •• Open 2—7,000 R. ... ... • 57 450 HIMALAYAN DISTRI GTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. XXXVII. — MOKIN- GIEiE. 1. Moringa. pterygosperma, Gosrtn. ... T. 40' Pk. March Bhabar XXXVIII. -LEGU- MINOSiE. ^ Piptantiius. nepalensis, D. Don. ... ... Sk. 10' Y. May Kathi Pass 2- Thermopsis. barbata. Boyle. 1 H. 2' Y. ?. July Milam, Ralam, inflata, Carnb. 2 H. 6"- 9" Y. July Raj-hoti 3- Argyrolobmm- flaccidum, Jaub. Sf 1 Sh. 1' R. July Naini Tal Spach. R. July roseum, Jaub. Sf Spach. 2 Sh. 1' Kal a p athara, &c. 4. Crotalaria. prostrata, Boxb. 9 H. 6" Y. ? July Almora humifusa, Grah. 11 H. 5" Y. ... ... alata, Bam. 3 H. 1' Y. July Almora mysorensis, Both. 4 H. Y. ? August ... Hawalbiigh ... albida, Beyne 7 H. i' Y. April Almora, &c. ... calycina. Sc b ank 5 H. G"' — 9" Bl. ? August ... Almora sessiliflora, L 2 H. 11— 2' Bl. July Almora sericea, Betz. 6 H. 3'— 4' Y. February, Naini Tal, Ba- gesar. tetragona, Boxb. 1 H. 6' Y. September, Sarju valley ... medicaginea, Lam. ... . . * . . . ... . . . var. neglecta 8 H. 2" Y. March ... Kota Dun incana, L. 10 H. 2' Y. July Almora 5 Parochetus- communis, Ham. ... H. cr. 6" Bl. May Chaur, Ralam, &c. OF THE NORTH-WESTERN PROVINCES. 451 Plants — (continued). Conditions of soil, &c., Elevation in feet above the sea. Hin hy a •3 PC? la- ta. >-» ** o Tibet. _ . 1 Remarks. ► * Forest 1—2,500 R. ... ... Do. 2,000 R. ... ... Open 10—12,000 R. D. Do. 13—15,000 •* D. T. •5 Do. 7—8,000 R. ... ... Do. 2,5—6,500 R. ... ... Open 3—4,500 R. • •k • • • V ... • •« ... Do. 3—5,500 R. • Cl m Do. 4,000 R. < A • Do. 4—6,500 R. til ». Do. 5,500 R. • • 1 Do. *i* * 6—8,000 R. ! m t Do. 3—5,000 R. * • • Do. 3,500 R. • •• ... Do. 2,000 it. IM • • > Gardens 5,500 R. • • • Open 6—12,000 R. 1 • • <•« - 452 hima'layan districts List of Kumaon Name. Herbarium aumber (Strachey and Win- tcrbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. Trigonella. Foenum-graecum, L... 7 H. • • • • • • Altnora gracilis, bemh. 3 H. 3' Y. July |Naini Tal pubescens, Edgeio . .. 6 H. 14' Y. J une Naini Tal emodi, benlh. 1 H. 2' Y. July ISaha cornieulata, L. 2 H. G"—9" Y. June Ramri, Niti ... Melilotus. parviflora, Desf, 1 H. w Y. March Almora, &c. ... alba, Lam. 2 H. 3' Wh. February, Haldwani Medicago. lupulina, L. 1 H. cr. 3" Y. March Outer hills ... denticulara, Willd. ... 2 H. 9" Y. March Bhabar Lotus. corniculatus, L. ... H. 6" Y. All the year. Almora &c. ... Indigofera, trifoliata, L. ’2 H. 9" Pr. August ... Almora, Sarju valley. hirsuta, L. 1 H. 12" Pr, July Almora Gerardiana, Wall. ... • • • , , , « • • . . . . . . var. heterantha 3 Sh. 3'— 5' Pr. January ... Almora, Binsar, atropurpurea, /Jam. . . . 4 Sh. 8" Pr. June Gangoli, &c. ... hebepetala, Benih. ... 4* Sh. 8' Pr. June Katlii pulchella, Roxb. 5 Sh. 8' — 10' Pk. February, Outer hills, Ba- gesar, Binsar, &c. ... Dostua, Ham 6 Sh. 2'— 3' Pk. June Milletia. auriculata, 3 aker ... T. sc. ; 10'— 40' ... Bhabar Tephrosia. Candida, DC. 1 Sh. 8'— 10' ... January ... Cota Dun purpurea, l ers. 2 Sh. 1'— 2' Pk. March Do. Sesbanea. aculeata, Pers. ... H. 2' Y. August ... ] dawalbagh ... OF THE NORTH-WESTERN PROVINCES Plants — (continued) . 453 Conditions of soil. &c. Elevation in feet above the sea. Hima- laya. j Tibet. Remarks. Rainy. Dry. Cultivated 5,000 R. • •• • • • Open • • • 7,000 R. • •• * • • Do. *• 7,000 R. .. . tit Woods • • • 9,000 R. ... • • • Open i • ■ 9—11,500 R. D. • • • Do. • • • 1—5,50.0 R. Do. • li 1,500 R. • • • . . . Do. • •• 4,000 R. • • • Do. 1,000 R. * * * • . . Do. • •• 4,700 R. • •• Do. in 4,000 R. ... ... Do. • • • 4—5,000 R. it* • • Do. • . « 4 — 7,000 R. ... .. Do. • •• 4—6,000 R. • •i Do. • •• 7,000 R. ... Do. • • • 2—6,500 R. ... ... Woods !*• 6—8,500 R. • • • ... Forest • • • 1—3,500 R. ... Open 2,000 R. ... ... Do. 2,000 R. Fields • • 4,000 R. » . > ... 454 HIMALAYAN DISTRICTS List of Kumcion Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. Cai agana, pygmaea, DC. 1 Sh. 1'— 4' Y. July Guge p'ains .. Gerardiana, Royle ... 2 Sh. S' Y. July Dliauli river ... polyacantha, Royle ... 4 Sh . . . • • • 9 crassicaulis, Benth. ... 3 Sh. 3"— 4" Or. July Pindari, Milam, Astragalus, trichocarpus, Gruk. ... l H. S' Pk. April Naini Tal hosackioides, Benth ... H. l'— 14' Y. Or. March Naini Tal strictus, Grah. 11 Id. 4"— 6" Bl. September, Shelong melanostachys, Ben h 12 H. 6" . , July Rajlioti inconspicuus, Baker, hiix alayanus, Klotzsch., 10 H„ 6" Bl. August Rilam valley . 13 Id. 6" August ... Milam leucocephalus, Grah. ... H. 2" Bl. July Milam, Niti . chlorostachys, Lindl., 5 Id. 2' Y. July Tola (Gori R.), emodi, Stend. 4 H. 2' July Ilwali . Gori river graveolens, Ham. 2 H. 2 '— 3' Y. March Outer hills .. Web ianus, Grah. 7 Sh. 6"— 8" Y. July Guge plains ... po'yacanthus, Royle 6 Sh. ir Y. August . Dhauli river multiceps, Wall. 8 Sh. 3"— 4" Y. Kugust ... Milam Oxytropis. lapponica, Gaud 7 H. 4" 6" Pr. July Rajlioti Stracheyana, Benth. . 5 H. 2" Bl August ... Guge plains tatariea, Jucquem. .. 3,4 H. 2"— 4" Pr July - A u - Rajhoti, Guge microphylla, DC. ... 2 H. 3" gust July plains. Guge plains Lezpedeza. sericea, Miq. 4 Sh. 4'— 8' Pk. February, Ramganga ri- Gerardiana, Grah. ... 2 Sh. 1 A' 1 2 Pk. August ver. Almora, &c. .. eriocarpa, DC. 3 Sh. 4' — 5 ' Pk. February, Gagar,Kalimat, Hedysarum. Kumaonense, Benth... • •• Sh. 9" • •• A ugust .. Gori river Stracheya- tibetica, Benth. ... H. 1"— 2" l July Tisum J OF THE NORTH-WESTERN PROVINCES 455 ■ Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Him layi £ c3 P5 Dry. • * * .2 *Sh paniculara, Wall. 3 Sh. 1' August . . Outer hills ... congesta, Roxb. 5 Sh. 2' — 3' Pk. August .. Bhabar var. semialata 1 , 2 Sh. 1'- 3' ... July Bagesar, Almo- ra, &c. Dalbergia- Sissoo, Roxb. 1 Tr. 25' Pk. February, Bhabar confertiflora, Benth ... 2 S. sc. 15' Li. March Do. volubilis, Roxb. 3 Tr. 20'— 30' Pk. May Kosi valley, ... Sophora- mollis, Grab. ... Sh. O'— 8' Y. February, Common Csesalpinia- 11 onducella, Fleming , ... S. sc. 10' — 15' Y. March Kota, &c. sepiaria, Roxb. ... S. sc. 10'— 15' Y. March Do. OF THE NORTH-WESTERN PROVINCES 4G3 Plants — (continued) . 6 ■ I— < O CD f> O •§ 43 CD Hima- laya. *H O CO 0 O • — < 43 • pH T3 0 O O Elevation in fe the sea. Rainy. i Dry. Tibet. Remarks. Woods ... 1 — 4,000 R. • • » Do. 3,000 R. • • • • •• Open 4—5,000 R. • •• • •• Cultivated 3,000 R. ... Not found in Herb S.& W. Open 5—6,000 R. ««• • • • D?. 3—4,000 R. , Do. 6 ^ 7,000 R. Do. 2—5,500 R. •• ; >•« Do. ... 6—7,500 R, ... Not found in Herb. S & W. Do. 3, 5—8,000 R. • • • < • • Forest 2,500 R. i • • • O* Do. 1 — 2,000 R. • •• Woods & open, 3—6,000 R. • •• Forest 1 — 2,000 R. • • • Do. 1 — 2,000 R. • • • Not found in Herb. S. & W. Do. 3—4,000 R. ... Open 3,5—5,000 R. * *« = Edwardsia mollis in Herb. S. & W. Do. 2—3,000 R. ... = Guilandina Bonducella in Herb S. & W. Do. 2-5,000 R. • •• • 464 HIMALAYAN DISTRICTS t: List of Kumaon * Name. Herbarium number (Strachey and Win- , terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. Cassia- Fistula, L. 1 Tr, 25' ‘ Y. April Outer hills occidentals, L. ... 2 H. 2'— 3' Y. March Bagesar, &c. — Sophera, L. 3 H. 3'- 4' Y. March Outer hills Tora, L. 4 H. 3' Y. All the year. Bagesar, &c. ... Absus, L. 6 H. 1' Y. August . . . Almora, &c ... mimosoides, L . .. ,,, . . . ... • • • var, Walliehiana .. 7 H. I'-IJ' Y. August ... Do. Saraca- indica, L. ... Tr. 25' R. Or. March ... Kota Dun Tamarindus. indica, L. in Tr. 0 00 1 o CD • • • Bhabar Bauhinia- malabarica, Ruxb. Tr. 25' ... • •4 Bhabar retusa, Ham. • •• Tr. 20' 40' Pk. September, Kosi valley .. Vahlii, W. Sr A. •a S. sc. 20' - 40' Pk. January ... Bhabar, outer hills variegata, L. ... i • • Tr. 25'— 30' Pk. W. March ... Outer hills ... Mimosa- pudica, L 1 Sh. 2' Pk. April Kota Dun rubricaulis, Lam. .. 2 Sh. 6'— 10' R. June Ramgarh val- ley, &c. Acacia- Farnesiana, Willd. ... 2 Sh. 10' Y. June Almora eburnea, Willd. 3 Tr. 15' Wh. January ... Bhabar Catechu, Willd. 1 Tr. 20' — 30' . . * January Bhabar Intsia, Willd. 4, 5 Tr. or S. sc. 20' — 30' Y. July Bhabar, Bage- sar. Albizzia- Lebbek, Benth. ... 3, 4 Tr. 20'— 30' Y. May Bagesar, Bha- bar. Julibrissin, Durazz.... • • • • « • •f ,,, var. mollis. 2 Tr. 25' W. May ... Naini Tal, &c., stipulata, Boir. i Tr. 30'— 40' Y. May Outer hills, Baisani. OF THE' NOETII-WESTERN PROVINCES. Plants — (continued ). ci CD \> O Himd- ,0 & layu. o 4-3 > d • r— < d >> U 4-3 Not found in Herb. S. & Wi Do. 1—4,000 R. ... ... ) Do. 4—5,000 R. ... ... Cultivated ... 2,000 R. ... ... =Jonesia Asoca in Herb. S. & W. Forest 1,000 R. ... ... Do. 1,000 R. ... ... = Piliostiqvid malabaricum in Herb*. S. & W. W oods Forest 1—3,500 R. * ?• • = Fhanera retuna in Herb. S. & W. 1 - 3,000 R. ... = Fhanera Vahlii in Herb. S. & W The flowers of this species are usually yellowish white. J. F. D. Woods . ••• 3 — 4,000 R. ■ * * • • • — Fhanera vanegata in Herb. S. & W. Cultivated 2,000 R. ... Not found in Herb. S. & W, Open 1 — 5,000 R. Gardens 5,500 R. • • • Not found in Herb. S. Poorest Do. 1—2,000 1—2,500 R. R. . . . • • • Not found in Herb. S. & W. Do. 1—3,000 R. . . . • • • Do. 1—3,000 r R ‘ ... ... No. 3 not found in Herb. S. & W. ••• Do. 6—7,000 r! ... ... Not found in Herb. S. Ss W. Do. 2—7,000 R. . 5U 46 (? hima'layan districts Name. ROSACEJE. Prunus- persica, Benth. SfHook., armeniaca, L. J acquem onntii , Hook.f. Puddum, Roxb. Padus, L. nepalensis, Ser. nudulata, Ham. Prinsepia. utilis, Boyle Spirssa. vestita, Wall. sorbifolia, L. bella, Sims. canescens, Don. vaccini folia,. Don. ... Rubiis. paniculatus, Sm. reticulatus, Wall. ... lanatus, Wall r alpestris, Bl. eaxatilis, L, nutans, Wall. niyeus, Wall. macilentus, Camb. ... ellipticus, Sm. biflorus , Ram. lasiocarpus, Sm. var.membranaceus ... List of Kumaon Herbarium number (Strachey and Win- terbottom). . Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. Sin March . . . Almora ... Sh. ... ... March ... Do. • • • Sh. 5' June Niti ... Tr. 20' Pk. November, Almora, &c. ... ... Tr. 30'— 50' Wh. April Naini Tal, Dwa~ li, &c. Chaur . . . Sh. 10' — 15' Wh. April . >. Tr. 20'— 30' . . . April Naini Tal, Bin- sar. ... Sh. 6' Wh. January ... Almora, &c. ... 5 H. 2' — 3' Wh. August . . . Ralam, Sc c. . . „ 4 Sh. 10'— 10' Wh. J une Dwali, Niti ... 1 Sh. G' Pk. May KathiPass,Che- chanickhal. 2 Sh. 10'— 15' Wh. May Common 3 Sh. G' Wh. June Almora, &c. .... 9 Sh. 10' Wh. May Tola (Sarju valley). 8 Sh. 10' Wh. June Lahur, Dwali .. 10 Sh. 15' Wh. 1 . April Gagar, Binsar, 17 Sh. ... ... 1 Tungnath 5 Sh. 1' July Vfartoli 6 S. cr. 1'— 3' Wh. May Lahti r 4,7 Sh. 10' -12' Pk. June ST ami k, Ramri, Rur Pass. 1 Sh. 10' Wh. May Binsar, Madhari Pass. 11, 12 Sh. 6' — 8' Wh. April-May, Outer hills,. Binsar, &c. 13, 15 Sli. G' — 8' Wh. April Slaiui Tal, Bin- sar, &o. 3^ 1 4 S. cr. 6'— 12' R, Pk. May-Feb- ruary. iota Dun, Nai- ni Tal, Bin- sar, &c. .13 Sh. 6' Wh. June ...'< 1 JhiringPass .... - OF THE NORTH-WESTERN PROVINCES. Plants — (continued) . 467 a o '•a 3 o O a os O aj •— aa c3 CD l> XJ > Q Tibet. Remarks. R. » • • — Persica vulgaris in list. Not found in Herb. S. & W. R. • • • « • • — Armeniaca vulgaris in list. Not found in Herb. S. & W. ■ »• D. = Cerasus No. 5 in Herb. S. & W. R. ft = Cerasus No. 4 in Herb. S. & W. R. • • • • • * = Cerasus No. 1 in Herb. S. & W. R. • •• = Cerasus No. 3 in Herb. S. & W. R. • • « ... = Rhaiimus No. 5 in Herb. S. & W. R. D. ... R. D. t • • R. D. . • . R. • •• Not found in Herb. S. & W. R. • • « R. • t e • •i R. • « • • • * R. • •• R. • • • • •• R. . . . • • . . - . D. *ii R. *• « • • R. ... ... R. til R. ... R. • • R. • *» ... R. Ml r ■ • 468 htma'layan districts List of Kmnaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. rosoefolius, Sm. 2 Sh. parvifolius, L. ••• 15 Sh. Geum- urbanum , L. ••• • • • II. elatum, Wall. i • • H. Fragaria- indica, Andr. 3 H. vesca, L. 1 II. yar. nub i col a ... 2 H. Potentilla- purpurea, Boyle ... • •• H. aibifolia, Wall. • « H. procumbens, L. • •• II. fruticoea, L. 1 , 2 , 25 , & 3. Sh. ambigua, Ccimb. ... 6 H. eriocarpa, Wall. 4 Sh. Mooniana, Wight 14 H. fulgenB, Wall. ... 13 H. Leschenaultiana, Ser., 9, 20 H. var. bannehalensis, 15, 1C H. peduncularis, Don. .. • • « yar. obscura, 17 H. leuconota, Don. 29 II. micropbylla, Don. ... 19 H. var. commutata ... 18 H. bifurea, D. ... 27 H. multifida, L. 22, 23 H. var. Saundersoniana, 23 (in part). H. sericea, L. 21 H. nepalensis, Hook. 10 H. Height of plant. Colour of flower. 1 Time of flowering. Locality. 10' Wh. May Nainl Tal 8' Pk. April Naini Tal,Bin- sar. 2'— 3' Y. June Namik, &c. ... 9" Y. June Patliar, Kori ... 3"- 4" Y. April Outer hilis .. 2" - 3" Wh. May Pindari Rogila, 3" 4" Wh. May Naini Tal, Dwali. 2" Pr. August ... Barjikang, &e.,. 4" — 12" Y. May Namik, Rala u, 3"— 9" Y. July Madhari Pass, Ralam, &c. 4"— 35' Y. August ... Milam, Niti, Pitti and Go- ri rivers, Pin- dari, &c. 4" Y. August - Ralam, Milam,. 1' Y. August Pindari, Sing- jar i. 1'— 35' Y. August .. Kalimundi, Ra- lam. 1' Y. July Naini Tal, Rrn- sar. & c. 9" — 2' Y. March- Au- gust. Naini Tal 2'— 3' Wh. August ... Jalat, Tola (Gori valley). « •• 1' Y. July Ralam 1' Y. June Ralam, Duda- toli. 1" — 2" Y. July Barjikang, & c. 3"- 4" Y. July Do. fcV/ _ Y. Inly Milam, Guge, 3"— 12" Y. Inly Niti pass. Hots, &c. Ml Y. July Do. 3"— 9" Y. July Malari, Guge .. 1' R. April Naiui Tal, Bin- sar, See. OF THE NORTH-WESTERN PROVINCES Plants — (continued) . 469 6 • f— t O GQ o CD § »»— » -t- 3 >r 3 c o o Elevation in feet above the sea. Hh lai .3 P3 u il- ia. M ft Tibet. Remarks. Woods *• 7,000 R. • •• ... Do. 7,500 R. . • . t« • Do. 7—11,000 R. 1 I • • it Open • • 10—11,500 R. '•* • • * = Sieversia elata in Herb, S. & W. Do- • . • 3-7,500 R. I • I in Do. •e.i 11—12,500 R. III « • « Open or woods, 8-10,500 R. • • I m Open 11—14,500 R. D. Ml = Sibbaldia No. 4 in Herb. S & W. Do. 8, 5—12,000 R. ... • • • — Sibbaldia No. 1 in Herb. S. & W. Do. • « 9, 5—14,000 R. D. = Sibbaldia No. 3 in Herb. S. & W. Open, rocky 8 — 1 G,300 R. D. T. places. *\ Open * . . 11—15,000 R. D. T, Open rocks •• 9—12,000 R. • •i Open ... 9 — 11,500 R. • • • Do. G— 10,000 R. ... ... Do. 6-7,000 R. ... Do. • • » G— 11,500 R. D. in HI • •• • •• i • » • •• Do. 13,000 K. • • • HI Do. » • • 10—12,000 R. ... • •• = Sibbaldia No. 2 in Herb. !S. & W Do. • •• 10—14,500 R, tii 11*1 Do. 10—14,500 R, • •i ... Do. • • • 12—16,000 Ml D. T. Do. • •• 15—17,000 • • • • •• T. Do. • •• Ditto • •• T. Do. lit 10 — 15,500 D. T. Do. • •• 7 — 8,500 R. • •i ••• • 470 HIM XL AY AN DISTRICTS List of Kumaon U * co a es bo H a 4^ 4-3 <0 a • »-H Name. * ,-A £ o t-. rS £ o a * o c S o pfl is .a q bO o =4-4 o > g a « s o pH bo Ph qn o q-i o S3 P cj O C3 £ X2 +3 s-i 7} 05 ► o 0) * o .2 2 S Fh O o HH o HH O >» ci £ ^ ££ s Qj +S 4^2 • r-H rO £ .bp *-« 3 C> o •> .2 § nd - fa. n ft Tibet. Remarks. In water 15,000 ... ... T. Do. 4—6,500 R. ... ... Forest 1,000 R. Not found in Herb. S. & W. Do. 3,500 R. • t • . . . Do. 2,500 R. ... . . . — . Pentaptera No. 1 in Herb. S. & W. Do. 1—2,000 R. ... ... — 1 Conocarjjus latifolia in Herb. S. & W. Open 3—6,000 R. ... . Cultivated 1—5,000 R. . • • Forest 1—3,000 R. ... ... = zSyzygium Jambolanum in Herb. S. & w. Do. 1—2,000 R. ... ... — -S. venosum , DC. in Herb. S. & W. Do. mi 1—2,000 R. ... ... Open 3—5,000 R. ’ll* Do. 4—6,500 R. • • • • •• 480 HIMA'LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). | Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. XLVIL— LYTHRA- CEAE. 1- Ammannia. rotundifolia, Ham. ... 1 t •• H. 3"— 4" Pk. February, Almora salicifolia, Monti. ... 2, 3 H. 12" ... ... Ivosi river, Al- mora. 2. Woodfordia- floribunda, Salisb. ... Sh. 0 r-“* 1 00 Sc. February, Outer hills 3. Lagerstrsemia- parviflora, Roxb. ... Tr. 40'— 50' Wh. ... Bhabar 4. Punica- Granatum, L. ... ... Sh. 8'— 10 Sc. June Outer hills ... XLVTII. — ON AGRA- CEiE. 1 1. Epilobium- angustifolium, L. 2 H. 3' Pk. August . . . Niti, Rimkirn, latifolium, L. 1 H. 9" Pr. August ... Milam, Badari- nath. hirsutum, L. 10 H. 3' • i • • i • Naini Tal var. lastum. 14 H. . . • 0 • • . Almora roseum, Schreb. ... 5, 1, 9 11, 12,13 II. ... ... ... ... var. cylindricum ... 8 H. . . . . . • Naini Tal palustre, L. 4 H. 4" Pk. August . . . Laptel origanifolium, Lam.... 6 H. 4" Pk. August . . . Milam 2. Circsea- lutetiana, L. cordata, Royle 3 H. 8" Wh. Tuly Binsar 1 H. 1'— 2' Wh. August . . . Naini Tal,Kali- mundi, &c. alpina, L. 2 H. 4" Wh. August . . . Saba XLIX.— SAMYDA- CJE-ZE. 1. Casearia* tomentOBa, Roxb. tit T. 25' GY. February, Bhabar OF THE NORTH-WESTERN PROVINCES 481 Plants — (continued) . 6 <8 a> t> o Ilima- jJT rQ c3 lay a. o o Hi .3 Remarks. S3 o o ^ • r—< '43 oo . g o O CD 4* w £ •F— 1 c3 Dry. Tibel Open 4—5,500 R. — Amcletia rotundifolia in Herb. S. & W. Open and by 4,000 R. ... ... No. 3 not found in Herb. S. & W. water. Open 3—6,000 R. = Grislea tomentosa in Herb. S. & W. Forest 1,000 R. ... ... Open woods, cul- 1* — 5,500 R. tivated. 0 Open 11,5—13,500 D. T. Do. 11,5—14,000 . . . D. ... Woods 6,500 R. . . ■ • • # Open • • t 5,000 R. • • . ... Woods 6,500 R. ... Open 15,000 ... D. T. Do. 13,000 Forest 7,000 R. ... ' Do. 7—8,000 R. ... ... Do. 9,000 R . . . . . . Do. 1—2,000 R. ... •V ■ 61 4-82 HIMALAYAN DISTRICTS List of Kumaon Name, Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. t Time of flowering. 1 Locality. L.— CUCURBITA- CEJE. 1. Trichosanthes- palmata, Roxb. ... H. sc. 10' Wh. July Sarju yalley, 2. Herpestosper- mum- caudigerum, Wall. ... H. sc. 6' Y. August . . . &c. Kalimundi 3. Cucumis. satirus, L. 1 H. BC. 1' Y. August . . . Pasc. Jalat 4. Zehneria- umbellata, Thun. ... var. nepalensis ... H. sc. 6' Wh. May Sarju valley ... 5- Melothria- odorata, Ilf. $ T. ... H. sc. 10' Y. July Almora 6. Gomphogyne- cissiformis, Griff. ... • • t H. sc. 6' Gr. Y. August . . . Kalimundi Pass 7. Gynostemma- pedata, Bl. H. sc ? LI. —BEG ONIACE JE . 1. Eegonia- picta, Sm. 2 H. 8" Pk. August ... Outer hills. .. amsena, Wall. 1 H. 6" Pk. August . . . ^ a i n i Tai, LII.-DATISCACEJ3E. i. Datisea. eannabina, L, • « • H. 7 » t » July Dagesar, &c. Almora LIII.— EICOIDEiE. 1. Mollngo- stricta, L. Ml H. 4" Wh. July Naini Tal, &c. ©F THE NORTH-WESTERN PROVINCES. 4'83 Plants — (continued). 6 <=8 • rH o O •s "S Hima- laya. O CD § • ph *rg rt o O Elevation in fe the sea. i fl c3 cd « Tibet. Remarks. ©pen 4,500 R. Do. 8,600 R. ... ... — Gymnopetatum pedunculosum in Herb; S. & W. Do. 6,000 R. ... ... Do. 6,600 R. ... ... =Karivia umbellata in Herb. S. & W. Do. 5,000 R. ... ... Do. 6—8,000 R, ... ... • • • ? ... ... • • • —Euhjlia trigy na in Herb. S. &. W=. W et banks 4—6,000 R. Trees & rocks, 7,000 R. River-bed 4,000 R. ... • M Open 4—7,000 R. • • • 484 HIMALAYAN DISTRICTS Name, LIV. — UMBELLIFE- RJE. 1. Hydroeotyle, javanica, Thnb. rotundifolia, Roxb. ... asiatiea, L. 2. Saniciila. europasa, L. 3- Vicatia- eoniifolia,. DC. 4- Trachydium Roylei , Lindl. 5. Bupleurum. lanceolatum, Wall. ... Candollii, Wall. falcatum, L. var. marginata ...! longicaule, Wall. Iienue, Don 6. Carum., carui, L. anethifolium, Benth. Falconeri, C. B. Clarke. 7- Pimpinella. achilleifolia, C. B. Clarke. acuminata, C. B. Clarke. tenera, Benth. diversifolia, DC. Stracheyi, C. B. Clarke. ctespitosa, Benth. List of Kumaon Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 1 H, cr. 6" « March Gagar , Almora, 3 H. 3" , , , ? 2 H. cr. 6" ... March ... Kota-Dun, &c. # • • H. 1'— 1*' ... May Karim, Naims Tal, &c. 1,2 H. 6" — 4' ... May Chaur, Lahur... • • • H. 4" Wh. September, Lanjar 4 H. V. 1 V CO Wh. May Karim 2 H. 2' Br. August ... Kalam 6 H. 3'— 4' . . . February. Outer hills 1 H. 2' — S' Y. May, Sarju Talley ... 3 IT. 1'— 2' Br. August . . . Ralam, Niti . 5 H. 2' • — 8' . . • September, Naim Tal, Ga- gar i • • H. 2' Wh. July Tola • • • H. 12' ... Naini Tal, Al- mora, t • • H. 2' — 3' % « t September, Binsar • • • H. ... . • • • • • ? ... H. 3' Wh. August . . . Naini Tal, &c. (»< H. 1' — 1*' ... Naini Tal ... 1 II. 2'— 4' Wh. , August ... Dudatoli, Naini Tal. 2 H. 9" Wh. t fune ... Dliaoli river ... • • • h. 3"— 4" Wh. ; fuly Niti OF THE NORTH-WESTERN PROVINCES Plants — (continued) . 485 d r» i 1 "H o a> > o rO c3 +3 Hima- laya. o OQ fl o -4-a • 1—4 d o o Elevation in fei the sea. Rainy. Dry. Tibet. Remarks. By water 5—6,500 9 R. Open 2—4,000 • • • ... ... Woods. ... 3,5—7,000 R. ... ... N ear water, open. 6—9,500 R. ... «*• Open 16—17,500 • •• ... T. Near water ... 6,500 R. Open 10,000 R. ... ... 1)0. 3 — 6,000 K. ... 5* * Do. 3,5—6,500 R. ... Do. 11—12,000 R. D. ... Do. 2,5—7,000 R. . . . ... Do. 11,500 D. Do. 6—6,500 R. • •• • • • = Ptyehotis No. 2 in Herb. S. & W. Woods 7,000 R. • •• ... = Ptyehotis No. 1 in Herb. S. & W. • • i ? - • ... ... = Ptyehotis No. 3 in Herb. S. & W. Woods ... 7,000 R. ... zsBeuiera acuminata in Herb. S. & W. On oaks 8,500 R. ... = Acronenia tenerum , not found ic S. & W. Woods 5—9.500 R. ... ... On rocks ... 7.500 R. ... On rocks ... 12,000 R. D. ... — Pctrosciadium cesspit osum in Herb S. & W. 486 HIM A'LAYAN DISTRICTS List of Kumaon U 1 o o3 Hima- laya. CD *+H o CD rt o «>■« a o O CD O .Q -4-3 Himd- layi. “S OQ fi O 4-3 ^3 a o O Elevation in fei the sea. Rainy. H a Tibet. Remarks. Open 13,500 R. D. 1 = Tordylio’psis Brunonis in Herb. Do. ... 6—11,000 R. . • . ... S. & W. Do. 5, 5—6,500 R. Probably = Torilis Anthriscus of list, t *4 Forest ,,, 8,600 n. ... ... which is not found in Herb. Strachey, though Caucalis An- thriscus is there, named in ma- nuscript without a printed ticket. Do. 8—10,000 R. ... ... Forest near wa- 10,000 R. = Heeler a tomentosa in Herb S. & W. ter Forest 1—3,000 R. = Paratropia and Hedera No. 6, in Do. ... 1,000 R. ... ... Herb. S. & W. = Pana.v fragrans in Herb. S. & W« Do. • •• 2, 5 — 4,000 R. ... ... = Hedera No. 3 in Herb. S. & W. Do. ... 6,500 R. ... ... = Hedera No. 5 in Herb, S. & W. Do. tv 3—9,000 R. ... ... Open • • 3—6,000 R. . . • • • • • • 62 ‘HIMALAYAN DISTRICT'S 494) List of Kumaon 1 £.5 S ^ 03 /A xi += * -4-a § J-H CD £ -.3 a> Name. erbarium (Strachey terbottom ho «4H o • rH Ph o 4-> '53 o S3 O n P o o £ •o q-H o F THE NORTH-WESTERN PROVINCES 491 Plants — (continued). 6 <% o k o Himd- d lay a. *»* o 4-a ^ o +a a >> d iH d Dry. Tibet. Forest 5—7,500 E. Open & woods 4 — 7,000 R. ... = Bent.hamia fragifera in Herb. S. & W. Open 5—7,000 Ei Forest ... 7—10,000 E. . . a Do. 7 8,500 E. - * • Do. 8- 0,500 R ... Do. 7,500 E. .a. Do. 4,000 R. ... Open and woods 5-8,500 R. >• a . • a Forest 7—9,000 R. • • • a • • Do. 9,5—11,000 R, ... • • t Open rocks ... 10,500 R. ... • • a Woods 6,-10,500 R. D. ... Open ... 11,000 R. *•< Do. 12, 5—14,500 ? D. ... Do. ... 13,500 . a « T. Forest ... 8—9,000 R. • • • T. Open 13,500 • •• D. Do. 11,5—13,500 ... 1. Do. ••• 12,000 R. ... ... Do. ••• 12,500 R. D. ... Open & woods, 3-7,000 ... ... Open 9,000 R. D. ... Open & woods. 8. 5-11,500 D. ... Cultivated 5,500 R. * * * ... Forest ' 7-9,000 i R, ... ... 492 HIMALAYAN DISTRICTS List of Kumaon 1 £ C rP 4-3 -4-3 S-i P Name. _ ^ a as § .s«s £ o s- bG 4H o s 1 '1 PH O * O qp qn O f-i CD £ o qp 03 *3 -g •£» S -♦-3 • rH rO rP be *-H P o O O -4-3 c3 CD a o K W m o H o LVII1.-RUBIACE2E, 1. Adina cordifolia, Hook.f. ... Tr. 60' Wh. January ... Bhabar 2, Stephegyne- parvifolia, Korth. ... ••• Tr. 40' Wh. Do. Do. 3. Uncaria- pilosa, Boxb. ••• Sh. Ml ... June Sarju valley ... 4. Hymenopogon. . - parasiticus, Wall. ... in Sh. r. I ' -2 ' Wh. J uly Binsar, &c. „. 5. Hymeiiodictyon. excelsum, Wall. ... 2 Tr. P. 30' HI Kal apathar, flaccidum, Wall. ... i Tr. P. 20' ill . • . &c. Mohargari 6. Wendlandia. exsrta, DC. i Tr. 30' Wh. May Bhabar, Bage~ tinctoria, DC. o Tr. Wh. Bar. 15' Do. Bagesar 7. Argostemma. sarmentosum, Wall. ., 2 H. H. Wh. Wh. August . . . Do. Verticiilatum, Wall.,.. i 3" 3" Sarju valley ... Do. 8. Clarkella- nana, tiaoh.f. ••• II. 2"— 3" Wh. Do. Mohargari 9- Hedyotis- stipulata, Br. 3 H. 12" Wh. Do. Alniora , „. 10- OldenJandia. Heynei, Br. ,,, gracilis, DC. III H. H. H. 4" Wh. Do. Do. coccinea,Rc/?//e 0" — 9" 6" — 15" Br. , April t J Wy ...j] Do. 3insar OF THE NORTH-WESTERN PROVINCES 493 Plants — (continued) . Conditions of soil, &c. o .a o3 CJ Hima- laya. Tibet. Remarks. Elevation in fe< the sea. Rainy. Sh Q Forest 1,000 R. • . • —Nauclea No. 1 in Herb. S. & W. Do. 1,000 R. ... ... =Nauclea No. 2 in Herb. S. & W. Do. 2,500 R. ... ... On trees 6-7,500 R. ... ... Forest 2,500 R, ... ... Do. 4 000 R. » ... Do. 1-3,000 R. . . . . . . Do. 2-3,000 R. ... ... Wet banks 3—4,500 R. Do. 3—4,500 R iet ... Do. 4,000 R. • • • — Ophinrrhiza No. 2 in Herb. S. & W. Near Abater ... 4,000 R. • •• • Open 5,500 R. in — IJedy otis No. 2 in Herb. S. & W. Do. 4 5,500 R. • •i — Kohautia No. 1 in Herb. S. & W Open grass 7,000 R. »•« ... zzKohauiia No. 2 in Herb. >S. & W 494 HIM A'LAYAN JJISTRI0T& List of Kumaon Name. Herbarinm number (Strachey and *Wm- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 11. Anotis- calycina, Wall. ... Ml H. 3"— 6" Wh. August ... Na : ni Tal, &c., 12- Ophiorrhiza- fasciculata, Don ... • •• H. 6" Wh. Do. Mohargari 13 Adenosacrae- Iongifolia, Wall. • • • H. 3' Y. Do. Mohargari, Sar- ju valley. 14- Randia- tetrasperma, Roxb. ... dumetorum, Lam. ... 15. Gardenia- • ■ • Sb. 2' — 3' Y. May Sarju valley ... • •• Tr. 15' Y. Do. ••• Sarju valley Bhabar, Ba> gesar. fcurgida, Roxb. 2 Tr. 30' ... • •• Bhabar 16- Knoxia- eorymbosa, Willd. ... H. 6" August ... Almora, & c: ... brachycarpa, Br. • •• 12"- 15" Pk. September, Baijnath ... 17- Pavetta- 1 indica, L. • • < var. tomentosa • •• Tr. 15' Wh. June Kota Dun, Sar- ju valley. 18- Coffea. bengalensis, Roxb. ... • •• Sh. 2'-3' Wh. March ... Bhabar 19- Hamiltonia- suaveolens, Roxb. • •• Sh. 10' -12' Bl. October ... Kalimat, Sarju valley. 20 Leptodermis- lanceolata, Wall. 1 Sh. 10' Bl. June ... Binsar, &c. e P 2 Sh. Ml Ml ... Dudatoli 21- Spermacoce- lasiocarpa, Hr. ... H. 12" Wh. September. Almora articularis, L. f. ... 2 H. 12" • • * | Do. ... Do. ©F THE NORTH-WESTERN PROVINCES 495 Plants — (continued) . Conditions of soil, &c. .*• t Elevation in feet above the sea. Hima- laya. Tibet. Remarks. Kainy. M P Shady banks ... 6—7,000. K. III • • • = Hedy otis No. 1 in Herb. S. & W. Wet rocks 4,000 R. ... • •i — Ophiorrhiza No. 1 in Herb S. & W. Woods 3—4,000 R. ... hi Open ••• 4-6,000 R. • •• ss Gardenia No. 1 in Herb. S. & W. Forest ... 1—3,000 R. III • •• Do. 1,000 R. • • • ... Open 4-500 R. * * —Spermacoce No. 1 in Herb. S. & Do. in 4,000 R. * ' ' ... W. • • « Forest ... 2-3,500 R. • . • • • • Do. 1-2,500 R. ... ... Open 2,5-6,000 R. ... ... Do. 5-8,000 R. Forest 10,000 R. . . • ..« By water 4,000 R. —Borreria lasiocarpa in Herb.S. Open 4,000 R. ... •••* & W . i-iima'layan districts 49 G List of K umaon Name, Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 22. Rubia. cordifolia, L. Manjista, Roxl>. 1 H sc. 6'-10' R. July Outer hills ... 2 H. sc. 3' Gr. Do. Niti Edgewortliii, Hovk.(r )• 3 H. pr. 6' Y. Gr. August ... Sar ju valley ... 23. Galium- triflorum, Mich. v. ... 1 H. 6"— 12" Pk. May Naini Tal, Dwa- li, Milam. elegans, Wall. 2 & 8 H. 6" — 2 ' Wh. Do. & June Naini Tal, Ka- lirnundi, Rur Pass. Mollugo, L. 3, 5, 9, H. sc 2'— 14' R. Pk. June, Au- gust. Gori valley, Rainni, Bin- sar, Girgaon. sp 4 H. sc. 2 r August ., Binsar, Milam, acutum, Edgeiu. ... 6 H. sc 1 ' — 2' Y. September, Badarinath ... aparine, L. ... 7 H. sc 3'— 5' Y. August ... Ralam, Niti ... hirtiflorum, Req. 10 H. sc. 3' Ml May Almora ... LIX — Y ALERIA N- CE^E. I. Triptostegia- glandulifera, Wall. ... • i • H. 1 ' — 2' Wh. May KalimundiPase, 2, Valeriana. Hardwickii, Wall. ... 1 H. CO 1 Pk. August Naini Tal, Ra- lam valley. var.— 2 H. 12" — 15" . . • Do. Milam, Niti ... sp. 3 H. 2" — 3" Pk. July Bompras sp. 4 H. 9" • • » Garhwal Wallichii, DC. ... 5, 6 II. 9" — 12" Wh. March, May. Almora, Naini Tal, Madhari Pass. sp. 7 H. 6" Wh. May Dwali ©1? THE NORTH-WESTERN PROVINCES. 497 Plants — (continued)- 1 Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. t Remarks. Rainy. ft ft O pen 5-7,000 R. I • Do. 11,500 ... D. • «« Do. 3,500 R. Shade St open, 7—11,500 R. D. HI Do. St woods ... 5—11,000 R. tk« * • % Shade St open... 5—8,000 R. • •• III Do, ««• 7 — 11,000 R. D. ... Open 10,000 ... D. ... DO. BOO 1—12,000 R. D. ... Do. 9—11,000 R. ■ •« ... Do. 5,000 R. *•« Forest 9,000 R. » i • ... Do. *o* 6-8,500 R. Open 11,500 ••• D. .01 Do. 14,500 IM D. ... Do. 5—8,000 • •r R. HI ... Do. | 9,500 R. »»« ... -# - — 6‘d 41)8 'himAlay'an districts List of Kumaun Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 3. Nardostachys- Jatamansi, DC. ... 1 & 2 H, 9"-l¥ Pk. August ... Kalam, Milam, LX. — DIPSACEJE. 1, Scabiosa- Candolleana, Wall., IP. \ ' liVll. April Pindar i. Almora, &c. ... 2. Dipsacns. inermis, Coult. H. 4' -6' Wh. August . . . Binsar, &c. ... 3. Morina- longifolia, M all. ... 1 PI. 3' Pk. Do. ... Kalam, Pindari, persica, L. 2 IP. 2' Y. J une Naini Tal Coulteriana, Boyle , 8 PL, 1 1 r Y. J uly Bampa LXI.— COMPOSITE 1. Vernonia- anthelmintica, T Villd. 1 H, 3' Pr. August ... Almora cinerea, Less. 2 H, 2' Pr. Do. ... Do., &c. ... 2. Adenostemma. Yiscosum, Font. ... 3 IP, 2' Wh. Do. ... Gori river Yar. elatum, Don, 2 H. 2' Wh. Do. ... Almora „ latifolinm, Don 1 H. 2' Wh. September, Do. 3. Eupatorrum- Reevesii, Wall. ... 1 PI. 3' Wh. October ... Kalimat, Binsar, cannabinum, L. ... • • • Ml • • • . . . . . . rar. indi visum ... 2 H. 3' Y. Do. Sarju valley ... 4. Solidago. Virga aurea, L. ... IP. 3'-4' Y. September, Almora, Naini Tal. OF THE' NORTH-WESTERN PROVINCES, 499 giants — (continued) , Conditions of soil, &c. Q >■ O •§- 4*. O +a S. Hima- laya, | Tibet. Remarks.' V Rainy. Sh ft ©pen' ... 12,5—13,500 R. D. Do. 4—6,500 R. 1 Woods 5—8,000 R. ... <•< s. Open 11—12,000 R. • • e tea Do. 8,000 R. ... ... Do. 10—11,000 ... D. ■ X V r % Do. 5,500 R. Do. 2,5—5,500 R. Woods 5,000 R. . . • Open 5,000 R. . . . • • • Do. 5,000 R. ... ... Forest 6- 7,000 R. ... ... Open 4,000 R*. ... ... Woods 6_7,000 R. « . « ... 500 * HIMALAYAN DISTRICTS List of Kumaon U i .3 I 'oh Name, 3 d e ' 3 ^ a si 4^> £ o r-* fcJD 4-3 § Fh CD £ O trt .3 CD £ O trt p 71 « .-H ^ +3 n cS O O a o >> S £ & ’gco.S 4-3 • i— < rO rCT *4 rt o o CD rt 4-3 "oS a CD K o O •r— ♦ H O 1-3 5, Dicrocephala- latifolia, DC. h 2 H. June Naini Tal, Al- mora, &e. 6, Cyathocline- lyrata, Cass. ••• » H. l'-li' Pr. [February, Almora, &c. ... 7. Myriactis- 1 nepalensis, Less. ... Gmelini, DC. 2 1 H. H. 2' 1 r — 2 r W. Y. Li. « August ... Bo. ... Almora, Bwali, Naim Tal, &c.. 8. Rhyncospermpm. Terti eillatam, Beinw. • •• H. 2' ... September, Binsar 9, Aster. tricephalus, C. B. Clarke. H. 2 r B1 August . . . Milam, Nairn Tal. Kalam diplostep h i o i d e 3, BP7l1.ll. ... H. 9" —12" Bl. Bo. ... molliusculus, Benth ., ... H. 1' Li. May Common Thomsoni, C. B. Clarice. • • • H. l'-2' Pk. August . . . Gangoli, &c. ... asp e viilus, Nets tibeticus, Hook f. Stracheyi, Hook. f,„. t • • • • • H. H. H. 1'— 2' 9" 2" 1 Pk. Li. ? Bo. September, October ... Ralam river ... Laptel Pindari 10. Erigeron. acre, L. trt • < 1 j 1 ... var. monticola ... „ alpinum „ multi caule ... 4 5 2 u. H. H. 6"— 9" | 6" ! 1'— 2' Bl. Bl. Wh. August ... April ...1 August ... £alimat Bompras Naim Tal, &e. mul tiradiatum, Benth. 6 II. 1'— 2' Bl. Do. ... ; tfaini Tal, Sp, ... • •• H. 3"— 8" Li. July ... ] Budatoli. £alajawar, Niti OF THE NORTH-WESTERN PROVINCES. 501 Plants — (continued). Open near ■water Open Woods Do. Open Do. Do. Woods Open Do. Do. Open Do. W oods Forest Open Remarks. 5 — 8,000 5,6—10,000 6,5—7,500 R. 7—11,500 13.000 6,-8,500 6,000 9,000 15.000 12—12,500 5—7,000 14—16,000 5,5—7,000 7—9,000 14—17,000 R. R. R. R. R. R. • • » R. R. R. D. Leptocoma raoemosa in Herb, S. & W. D. D. = Erigeron, No. 3 in Herb S & W. = Diplopappus No. 6 in Herb. S. & W. = Diplopappus No. 1 in Herb- S. & W. = Calimeris flexuosa in Herb. S. & W. = DiplopappusNo. 2 in Herb. S & W, = Heteroc/iceta No. 2 in Plerb. S. & W. T. T. = Heterchceta No. 1 in Herb, S. & W. i 502 MTMA'LAYAN DISTRICTS List of Kurnaon, o pj bb rd +3 Name; _ a as s = oS (.So £ o r— ( bJO O c3 «H O -♦-3 rCl o> £ o tp. <4H o- r— < o> £ o iC u CO O Qj ^ *Jq c3 .Sf '8 rjJ o O a ■ H W a w _ o 1 H o Hi 11. Microglossa. albescens, C. B. Clarke. ... H. Sh . 2'-— 3* Li. August .. Dugli, Tola .. 12. Conyza- japonica, Less. 3 H. 9" Pk. March . . Aim ora, Naini viscidula, Wall. absinthifolia, DC. ... sp- 2 1 H. Sh. H. 3'— 4' 3' Pk. Y. February, August ... Tal. Outer hills ... Almora, Saba, 4 H. ; 9"— -12" Bl. Bo. ... Pajhoti, lia- lam 13. Blumea. lacera, DC. 4 T-T Almora Do. Garhwal Bhabar laciniata, DC. oxyodonta, DC. aromatica, DC. 3 7 2 H. H. H. 8" =9" S' 3/ ... March March 14. Laggera. alata, Benth. pterodonta, Benth. aurita, Benth. ? ... ... H. H. H 3' 4'— 5'- Pk. Pk. September,. March Kapkot Outer hills ... ? 15, Sphseranthus. indicus, L. ... ... H. 6" Pr. April Almora 16. Leontopodiiim- alpinum, Cass. sp. 1 2 H. H. 1"— 1J" 1"~ 1J"' August ... Do. Uhor-hoti Pass, Valleys in >5 „ var. Stracheyi, 3 4 H. H. 6" 1'— 1J/ ... Do '...] Do r Guge lalam Cola 17. Anaphalis- cinnamonea, Benth., 9 H. 2'— 3' Wh. |S September, I linsar, Naini trip! iner vis, Sims..., nubigena, DC. 12 10 H. H. 2'— 3' 6" Wh. i Wh. August ...I Do. ..Jl Tal. Jinsar larjikang, To- cortorta, Hooh.f. ... pidhunga. 3, 4, 8 H. 6"— 1 ' Wh -{s Do. ...C lothi ng. AI- eptember. mora, &c s 504 him a'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- ter bottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. l Locality. Anaphalis— ( conoid .). ehion.au tha, DC. ,, 2 H. 12" -16" Wh. September, Tola, M i 1 a m, var. 7 H. 6" Wh. Do. . Bagdwar adnata, DC. 1 H. 1'~1J' Wh. Do. .. Binsar, Naini Tal. intermedia, DC. ... 11 H. 8" Wh August . . . ? sp. 5 Ii. 8" Wh. September, Dhauli valley, sp. 6 H. 6" • Tk. June Pindari 18, Phagnalon. niveum, Edgew. ... ... H. 6" ... J une Samangentlia... 19. Gnaphalium- hypoleucum, DC. ... 3 H. ixr 1 2 ... May Alrnora, Kathi, luteo-album, L. 2 H. 1 ' Y, March Do. indicum, L. 1 H. 1' Y. Do. ... Do. 20, Csesulia. axillaris, Roxb. 21. Inula- ... H. 6"— 9" »•* September, Kota, Retagar, vestita, Wall. 4 H. 1' Y. March ... Alrnora, Hard- war. nervosa, Wall. 3 H. 2' Pk. September, Kapkot, Naini Tal. barbata, Wall. 5 H. 2' Y. August ... Raiam river ... Cappa, DC. 1 IT. 3' — 4' ■ . • March ... Pyura, &c. ... cnspidata, Hf.fy 7’., 6 Sh, 4'— 6' Y. F ebruary, Alrnora, Naini Tal. sp. 2 H. o I f Y. ... 22. Vicoa. auriculata, Cass. ... H. 6"— 8" Y - March ... Alrnora 23, Carpesium- cernuum, L. 1 H. 3' Gr. Y. August ... Naini Tal var. pedunculosum, , . • . . • . . . • • • abrotanoides, L. ... 3 H. 2' • •• August .. VL o li a r g a r i Pass, Binsar. OF THE NORTH-WESTERN PROVINCES 505 Plants — (continued) . . > o Himd- PQ aua. • f* o GO +3 CD CD 4-1 *+H i o on .5 Remai’ks. o O CD 4-3 • H nd d O o +3 £ 2 A H Remarks. Forest 7,000 R. ... ... Open 5,500 R. ... ... Forests 5—8,500 R. ... • • % Open 6,500 R. ... ... Do. 6-6,500 R. ... ... Do, 4,000 R. • • • Do, 3—7,000 R. ... ... Do. 4—6,000 R. ... ... Naturalized in gardens. 6 — 6,000 R. ... • • • • Open' 16,600 T. Do. 13—15,000 • » * D. T. Do. 16—17,000 to * ' ' T. Do. 4,000 R. • » • • • • Do. 2,600 R. ... • • • tsMachHs kcemispherica in Herb S. & W. 508 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 34, Tanacetum- nubigenum, Wall.... 2 H. V Y. September, Pindari, Tung- nath. tibeticum, Hf. §• T., 3 H. 1' Y. August . . . Milam ... longifolium, Wall. ... 1 H. 2' Y. September, Pindari, Tung- nath. tomentosum, DC. ... 4 H. 1' Y. August . . . Gothing gracile, H. J $ T. . . . 16 H. . . . . . . September, Satlaj river in Guge 35- Artemisia- scoparia, W. Sf K. ... 1 H. 3' ... August ... Hawalbagli ... stricta, Edgew. 11 H. ... ... Ho. ... Milam, She- long. maritima, L. 5 H. 2' . . • Ho. ... Jelam ... vestita, Wall. 4 H. 3' . . . Do. Common Bacrorum, Ledeb. ... 15 H. • •• ... September, Satlaj river in Gugd. var. 6 H. 2' Br. August ... Tola, Milam ... vulgaris, L. Roxburgbiana, Bess, 2, 8, 9, 14 H. l'—3' ... Do. Almora, Ke- darnath. var, grata 3, 7 II. 3' Br. Do. ,.. Binsar, Ralam fasciculata, Bieb. ... 17 H. . . . ... September, valley. Satlaj valley in hypoleuca, Edgew. . . . 12, 13 ... ... August ... Gugd. Milam, Shelong, Satlaj valley in Gugd, Ba- darinath. Stracheyi, Hf. &f 7 19 H. 1' Y. September, Manasarowar... macrobotrys, Ledeb. 18 H. ... 1 ... Do. Milam, Topi- dhunga. sp* ■ , ••• . . • ... ... ... • •1 36- Tnssilago- Farfara, L. ... H. 6"— 12" Y. Vlay Dwali Pindari, 37- Doronicum. iloylei, DC. • •• H. 14' Y. August ... Tuugnath OF THE NORTH-WESTERN PROVINCES, 509 Plants — (continued) . c5 • rH o oo Elevation in feet above the sea, Hivid- laya. O OQ o • r— 1 >r 3 g o O Rainy. n Pi Tibet. Remarks. Open • • • 12,000 R. ... ... Do. ®e 18,000 ... D. T. Do. an 12,000 R. ... »•« Do. 13,500 • • • D. • • • Do. Ml 13,500 • • • T. Do. • II 4—11,500 R, D. • •• Do. ... 11 — 12,000 ... D. ... Do. • • • 9,000 R. • • • Do. • •• 6,000 R. D. ... Do. • •• 12—13,500 ... T, Do. • •• 11,500 ... D. Do. 1 — 11,500 R. ... Do. ... 7—9,000 R, ... Do. 13,000 • •• • • • T. Do. • •• 11—13,500 ... D. T. =A Roxburghiana, Bess. Do. • •• 14 - 15,500 T. Do. » • 11—15,000 D. T. • •• • • • • •i • • • ... Open, debris .. O o r~ *1 1 oo R. • • • 1 Woods • • 10,000 R. ... ... = D. P ardalianches in Ilerb. S. & Vi . 510 HIMALAYAN DISTRICTS Name. 38 Gynura. nepalensis, DC. ... 3 9. Em ilia. sonchifolia, DC. ... 40- Senecio. alatus, Wall. ... rufinervis, DC. ... Kunthianus, Wall., Candolleanus, Wall., graciliflorus, DC., c h r y santhemoides, DC. diversifolius, Wall., nudicaulis, Ham. coronopifolius, Desf. pedunculatus, Edgew. Ligularia, Hook. f. ... arnicoides, Wall. ... 41- Werneria- nana, Benlh. 42- Echinops- cornigerus, DC. ... niveus, Wall. 43. Carduus. nutans, L. ... yar. lucida ... List of Kumaon Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant Colour of flower. Time of flowering. Locality. Ml H. 3' Or. March ... Outer hills ... Ml H. 1 ' Pk. April Almora ... 8 H. 2 r Y. August , . . N a i n i T a 1, Kathi, Rdlam. T H. 2 r Y. July N a i n i T a 1, Kathi 5 H. Y. August ... Ralam riyer ... 6 H. 11'— 2' Y. Do. ... Pindari 3 H. 5' Y. Do. ... Pindari, Ralam, 10 H. l' Y. July Gothing 4 H. 3' Y. August ... Binsar, &c. ... 2 H. 12"— 18" Y. July Almora, &c. ... 9 H. 2" Y. September, Rakas Tal, 1 H. 9"— 12" Y. July Shelshel Malari, Niti. • •• H. 4' Y. August ... Ralam river, Dudatoli. Ml H. 6" Y. Do. ... Sajhoti, Chor- hoti,andNxti Passes. III H. 4"' Y. Do. .., Rajboti and Chor ho t i Passes. 1 H. 2' Bl. Do* iM 1 1 Bhim-ud i y a r, Malari. 2 H. 2' Bl. February, , Almora, &c. ... • • • H. • • • • • • • ■ • • •• Ml H. 5' Pr. August ... Galana ... ©F THE NORTH-WESTERN PROVINCES, 511 Plants — (continued) . Conditions of soil, &c. > O -tfe cJ (D Hima- laya. Tibet. / Remarks. Elevation in fe the sea. Rainy. P ■ Open -2,5—4,000 R. ... .»• ■ Do. 5,000 R. Do. ... 8—11,500 R. ••1 • •* Woods *.■ 7—8,000 R. Open 11—13,000 R. Ml Do, ••• 11,000 R. • • • ... Woods ... 9 — 11,000 R. Ml' Open ... 13,000 ... D. >•» Do. 5—9,000 R. • •• Do. 4—5,500 R. ... ... Do. ... 14—16,000 ... • • T. Do. 10—11,500 • a. D. 8—9,000 R. = Ligularia No. 2 in Herb. S. & W. Do. ... 16—17,000 • •• it. T. = Ligularia No. 4 inHerb. S, & W. Do. .. . 16—17,000 ... T. Ligularia No. 8 inHerb. S. & W. Do. »< . 9,000 R. D. • •• Do. • .. 4—5,000 R. • • • ... Fields , 12,000 R • •• ••• 512 HIMA'LAYAN districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Height of growth. Habit of plant. Colour of flower. Time of flowering. Locality. 44- Cnicus- arvensis, Hoffm, ••• • •• II . 2' Pr. March Outer hills ... eriophorus, Hoffm., ... ... Ml • •• involucratus, DC..., H. G r Pr. W. August Jalat, Ralam var. horrida .. • river. argyracanth us, H. 5' Pr. W. April Naini Tal, Ra- Benth. lam. var. nepalensis ... • • t H. 6 r Pr. W. August • •• Do. Walliehii, Benth. ... • . • H. 6' W. Do. 1 > Lohathal, Al- mora. 45 . Saussurea- obvallata, Wall. ... 4 H. 1'— 2' Pr. Do. Mt Pindari, Barji- kang Pass. braeteata, Dene. ... 2 H. 3"- 6" Pr. Do. . • . Balchha Pass, Lanjar. Kunthiana, Wall.... 8 H. 2"- 3" • • • Do. ... Ralam, Kala- sorocephala H.f , 5 H. 2"— 3" Pr. jawar. Sf T- Do. • i. Balchha Pass... eossypiphora, Don,.. 1 H. 2"— 6" Pr. Do. . . . Barjikang, Ke- darnath. graminifolia, Wall., 3 H. 3" — 9" Pr. Do. *• • Barjikang Pass, Candolleana, Wall.... 13 H. 3 r Pr. Do. Pindari piptathera, Eclgew., 12 H. 3' Pr. Do. • 1 • Do. candicans, Clarke ... • • • H. l'—2 r Pk. March 1 » . II a w a 1 b a gh, albescens, Hf .$ T., 15 H. 5' Naini Tal. August • •• Josimath, Ga- gar. denticulata, Wall.,,, 11 H. 4 r Pr. Br. Do. *•< Dwali, Ralam, Niti. hypoleuca, Spreng., H. 4' ... Do. • •• Jalat, See. deltoidea, Clarke ... ... H. 6 ' Pr. Do- • it Do. sp. 6 II. 1" — 2" Pr. Do. Unta-dhura ... 99 ' ••• 7 H. 3"< — 6" Pr. Do. • •• Balchha Pass... 99 ' ' 9 H. 1' »•• Do. • • • Plain of Guge, „ ... 10 H. 4"— 6" IM Do. Gothing 46. Jurinea. macr oeephala, Ml H. 1' Pr. Do. • • • Ralam, Pin- Benth. dari. 47- Serratula- • I pallida, DC. IM H. 1£'— 2' Pr. June Ml Binsar, Gagar, 1 OF THE NORTH-WESTERN PROVINCES. 513 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. H ill layt >> a '3 P3 d- l. rH ft Eields 1—3,000 i R. ©pen 9—10,000 R. »• 1 Do. »*• 4,5-7,500 R. ... Do. 7 — 11,500 R. ... Do. ••• 3—7,000 R. • •• Do. ••• 12,5—15,000 R. III Do* • • • 16 — 17,000 t a • ... Do. 12,5—15,000 R. D, Do. 16—17,000 ... DO. r«i 12—14,500 R. ... Do. 13—14,000 R. D. Do. ... 12,500 R. Do. 12,500 R. ... Banks ... 4—7,000 P. • a o Open 6,500 R. ... Do. 7 — 40,000 Ml D. Do. 6—7,000 R. • •• Do. 6 -7,000 R. ... Do. 16,000 ••• ... Do. 16,000 • «• ... Do. 16.000 . . . ... Do. 13,500 R. D. Do. ••• 12,000 R. Do. 5,5—7,500 R. Ml - 4 — > CD T. T. Remarks. Cirsium No. 4| in Herb. S. & W. — Cirsium No. 3 in Herb. S. & W". = Cir siu'n No. 2 in Herb. S. & W. Cirsium No 1 in Herb S. & W. = Cirsium No. 4 in Herb. S. & W. T. T. T. — Aplotaxis No. 2 in Herb. S. & W. -Aplotaxis No. 6 in Herb. S. & W. = Aplotaxis No. 5 in Herb. S & W. = Dolomieea macrocephala in Herb. S. & W. 65 514 'HIMALAYAN DISTRICTS List of Kumcion M 1 s.a [' t bi) 5 ^ fl e3 • * 4-3 u Jh 0) a u o Name. a s s 3 o £ "go !r< B. A o be ‘H O +3 ‘,3 Ph M-f O 4-3 rP o O i-< 53 O * o '33 qn O 433 © Cr o © 4-3 - S' & S-l~ ft S' Op on 8,000 R. »* Do. »OB 5,500 K. ... • • • Cultivated ... 1—4,000 R. ... ... Dry, op m • •• 3—5,000 R. ... Woods 9 •• 6—7,000 R. Do. ... 6,5—7,500 K. . . • . . . Open rocks • • • 6 5 — 8,500 R. ... =Oreoseris lanuginosa in Herb. S. & W. Open • •1 6,5—7,500 R. . . . . . . = Bern-' era nepahnsis in Herb. S. & W. Do. 7,5—11,500 R. D. ... Do. 5—7,000 R. = Barkhausia foetida in Herb, S & W. Do 1—5,500 R. = Yd ung i a No. 1 in Herb. S. & W. Do. • 0 • 11—12,500 ... b. • . . = Youngia No. 2 in Herb. S & W. Do. 14,000 ... • • • •• • •• Do. »«• 7-10,000 R. b. ... Do. ... 5—10,000 R. • •• ... Do. 11,500 ... . • • T. Do. no 16,000 ... . • i- . . • HIM A' LAY AN DISTRICTS 5X6 Name. 56- Lactuca. obtusa, Fenth. dissecta, Don longifolia, DC. sagittarioides, C. B. Clarke Brunoniana, Wall., gracili flora, DC. ... macrorhiza, Hook, f., var. saxatilis Lessertiana, Wall ...... Dubysea, Benth. ... ap. 57- Sonchiis. asper, Vill. arvensis, L. 58- Tragopogon. gracile, Don. LXIII.- CAMPANU- LACEAE. 1. Lobelia. Wallicbiana, Hf. fr T. pyramidalis, Wall., trialata, Ham. 2. Cephalostigma hirsutum, Eilgew ... 3- Wahlenbergia. gracilis, DC. List of Kurnaon Herbarium number (Stracheyand Win- ter bottom). Habit pf growth. Pleight of plant. Colour of flower. Time of flowering. Locality. H. l'-OJ' Y. February, Almora, &c. .. 3 PI. 1' — 2' Pr. April Alrnora 2 H. 2' Pr. August . . . Eamganga val- ley, Almora. 1,4 H. l r — ]*' Pr. August ... Gangoli ... H. 2'— 3' Li. A ugust . . . Kalimundi ... H. 1 >. g' Bl. August ... llalam, Milam, ... H. 1'— 2' Bl. August . . . Kalam, Niti ... ... H. n r Bl. August . . . Niti ... PI. H'—8' Bl. August ... Niti, valleys of Guga, P.alam. ... H. 3' Y. August . . . Saba, Pindari, * * * H. 2 r Y. May Sar ju valley .. . 2 ii. 3' Y. February, Outer hills 1 H. 3'— 4' Y. February, Ditto « •+ II. G"— 9" Y. April Almora 1 H, 4 r Pk. February, Naini Tal 2 PI. 6' Pr. October ... Namik,Jagesar, 3 H. 4' September, Dhanpur . . ... H. 1"— 2" ... Almora 2 II, 6" Bl. | 1 if arch ... Almora OF THE NORTH-WESTERN PROVINCES. Plants — (continued) > 517 O _Q Himd- o c3 4-3 D lai/a. CQ O-l o GQ ri • pH Remarks. rt o S c3 ••pH 4-3 '» pH 00 4-3 rt o O > J3 CD 4-3 S .s s >> •n A Open 6—7,000 E. = Campanula No. 8 in Herb. S. & W. R. • • . ... Do. 6,000 R • • • Do. 10,000 R 1 • • • • • = C. rotundifolia, Benlh ? Do. 6,5—7,000 R. • •• Do. *• • 10—12,000 R. • •• • •• Do. • i t 12—13,000 R. ... Open rocks • • • 10—11,000 R. • •• Open 8,5—11,000 R D. in Do. • ■ • 8—1 1,000 R. D. Do. 13—15,000 «»• D. T. Do. 7—8,000 R. • •• • •• = Peracarpa carnosa, H. F. Sf 1 , Forest 8,500 R. ... Open Do. 12—13,000 6—12,000 ... R- D. •HI • » = C. color ata No. 13 Do. • •• 5—7,000 R. »•* Do. • •• 5,500 R, • » » Do. 5—8,000 R. • •• in Open banks • •• 10— 12,00C R. • •• • • i Do. • •• 7,5— 10.00C • R • «« » • • Open 11— 14,50( R. D. Forest 5— 9,00( R. *• • - Pieris No. 1 in Herb, S. & W. Do, 0* 10,000^ R. • n = Ditto No. 2 in Herb. S. & W. 520 HIM /LAY AN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant, Colour of flower. 4- Rhododendron- lepidotum, Wail. ... 1 Sh. 1"— li" Pk. anthopogon, Don ... 2 Sh. 1'— 2' Y. campanulatum, Don 3 Sh. 10' Li. nobile, Wall. 4 Sh. 8' ? 5 Tr. 20' R. barbatum, G. Don, 6 Tr. 20'— 25' R. arboreum, Sm. ... ... var. roseum 7 Tr. 25' R. ,, puniceum ... 8 Tr. 25'— 40' R. ] LXV.-PRIMUL- ACEJ5. 1. Primula- speciosa, Don ... 1 H. i'— H' Pr. i denticulata, Sm. ... 2 H. i' Pr. capitata, Hook. ... 3 H. 9" Pr. ] Stuartii, Wall. 4 H. 1 ' — 2' Pr. . Moorcroftiana, Wall., 5 H. 3" -4" Pr. i; sibirica, Jacquem. .. 6 H. 1 f li' I 1 2 Pr. j var. tibetica 15 II. 1" Pr. £ floribunda, Wall. ... 7 H. 4"— 6" Y. J pulverulenta,i?., 8 H. 6" Pr. 1 nana, Wall. ... 9 H. 6" Pr. A sulphurea, Hookf... 10 H. 3" Pr. I petiolaris, Wall. ... 11 H. 4"— 6"i Pr. A autumnalis, Hook.f. 12 H. 4" Pr. C Stracheyi, Hook. f. 13 H. irr 2 Pr. ; minutissima, Jac- quem. ... 14 H. i rr 4 Pr. J 2. Androsace- rotundifolia, Hardw., 1 H. 3" Wh. F incisa, Wall. 2 H. 3" Pk. A lanuginosa, Wall.... 3 H.rn. 3" Pk. a sarmentosa, Wall.... Jacquemontii, Duby, 4 1 H.rn. 6"— 9" Pk. J 5, 10 H.rn. 1"— 3" Pk. Pr. A pedicillata, Royle ... 6 H. 6" Pk Afl a £ O *4— I o o a * — < H June +-a *65 o o Hi February, Pindari, Bom- pras. Ditto Pindari, &c. ... Champwa Jhuni Madhari Pass, i •• Namik Naini Tal, &c., Almora, &c. ... Naini Tal, &c., Pindari, Raj- hoti. Pindari, &c. ... Niti Pass Pindari, Niti, &c. G-yanima ... Naini Tal Madhari Pass, Champwa, Pin- dari. Suring Aladhari pass... Namik Barjikang Pass, Barjikang Pass, Bompras. Plains, Bage- sar. Almora Naini Tal ... Ralam, &c. ... Topi dli ung a Hangar. Dwali V>F THE NORTH-WESTERN PROVINCES. 521 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. j Tibet. Remarks. Rainy. Dry. ■Open IOI 9—14,000 R. D. • •« Do. •10—14,000 R. D. • •• = Osinotliamnus in Herb. S. & W« Do. • 00 9—12,500 R. D. • • • Do. •e • 10,000 R. • •• • • • Forest 9,000 R. ... • •• Do. in 9—10,500 R. **• ••• . • •« • •• • • • ■ •• Do. • • 10—11,000 R. • •« Do. ••• 4—10,500 R. D. "Near water »*» 4—6,000 R. Ml Woods • •• 7,5—10,000 R. ... ... Open • •• 12—15,000 R. D. T. Do. • 0 9 11,5—14,000 R. D. T. Do. • «■ 16,800 • «i . T. Open, wet • •• 11—16.000 R. D. T. Wet • 0 • 15,500 • «■« • • • • •• Wet banks • •• 3—7,000 • • 0 • •• • •• Wet rocks • •• 8,000 R. Ml • »• Open 12,000 • •• • •• • •• ■Shady banks'... 4,500 • • • Ml ... Open & woods, 9—12,000 1 K - • •• Ml Woods, wet • •0 8,000 R. • •• «•• Open It • 14—15,000 R. ... Do. 14—16,000 R. D. T. Fields • •» 1— 3,00C R. • •i !•• Open «» 5— 7,50C > R. • •« . . • Do. DO 6 — 7,500 R. .«« ... Do. banks .. 8— 12,00( ) • •• ... Open • • 15— 17,00( ) ... ... T. Banks •• 8,00( ,|B. • •• Ml • 66 522 HIMA’LAYAN DISTRICTS List of Kumaon Name. f Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 2- Androsace— ( concluded ). sp. 7 H. 3"— 4" Tr. July Bampa, Nvti ... villosa, L. 8, 11 H. st. l" — 2" l J r. July Milam, Rogila, G Hire. globifera, Duby. ... 3- Lysimachia- 9 H. 1" Pr. July Barjikang Pass, debilis, Wall. ... 1 IT. cr. 6" Y. June Gagar " ... pyramidalis, Wa 11 , 2 H. H f Dk. July Binsar sp. 3 n. 4" — G" Pk. May Madhari Pass, Dwali. al term folia, Wall., 4 H. G" Pk. July Almora, See. ... lobelioides., W all., 4- Anagnathis- 6 II. H' Pk. August ... 4 Jagesar arvensis, L. ... • •1 H. G" Bl. February, Outer hills ... LXYI. — MYRSINA- CEJE. 1- Msesa. argentea, Wall. ... 1 Sh. 5'— 6' Ml May • Binsar indica, A. DC. ... 2 Sh. 15'— 20' • •• March ... Kota, outer hills. 2- Myrsine. bifaria, Wall. 2 Sh. 3'— 4' R. February, Binsar, &c &c., semiserrata, Wall., 2 Sh. 20' ••i March ... Naini Tal, &c., 3- Embelia. robusta, Boxb. ... III Sh. 15' in ... Kota- Dun ... 4- Ardisia. floribunda, Wall. ... • • • Sh. 10' Pk. May Below : Binsar, humilis, Vahl. ... ••• Sh. 8' mi • • • Punagiri ... LXVII.— SAPOTA- CE2ES. 1. Bassia. buiyracea, Roxb. ... 1 Tr. 35' • • • January ... Bhabar ... ep. 2 Tr. 25' ... January ... Sarju r alley ... OF THE NORTH-WESTERN PROVINCES Plants — (continued) . 523 6 « r—* o CD >> O & cd -1-3 a Hima- laya CO SH o DO £ c *4-» ^3 a o O Elevation in fe the sea. d 3 Ph X rH « Tibet. Remarks, Rocks 11—12,000 • • • D. Open 11—15,500 it. D. T. Do. 14,700 it. * • i ... Wet, shade ... 6-7,000 it. Woods ... 7,000 it. ... ... Damp woods ... 9,000 it. ... Open 5—6,500 R. Open, by water, 4—7,000 It. Fields 1—5,000 It. ... ... Forest 5,000 It Do. ... 2—5,000 It. Woods ... 5—7,001 It. Do. ... 7,00C It. • • • Forest 1 , 50( > It. . « « ... Do. #»• 4,00( ) It. • ■ • 2 — 4,00( ) It. . < • Surest .. 1,00 0 it. Do. « > 0,000 li. 1 1 • •• 1 • • 1 524 HIMALAYAN DISTRICTS' List of Knmaou Name; Herbarium number (Strachey and Win- terhottom). Habit of growth. Height of plant. Colour of flower. l Time of flowering. LXVIII. — EBENA- CKiE. 1- Diospyros. lanceaifolia, lioxb ► .. • Tr. 30" Wli. m LXIX . - ST YR ACEJE. 1. Symplocos. cratsegoides, Don ... 1 Tr. IS' — 25' Wh. May ... 1 Hamiltoniana, Wall , 2 Tr. 20' Wh. March ... ] ramosissima, Wall., a Tr. 20' Wh. May ... polystachya, Wall., 4 Tr. 35' Wh. September, LXX— OLEACEJE. 1- Jasminum. rcvolutum, Sims ... 1 Sh. 15' Y. May var inodorurn ... 2 Sh. 10' Y. April pubescens, Willd . ... 3 S. sc. 10'— 15' Wh. March officinale,. L. ... 4 S. sc. 10' Wh. May **« grandiflorum, L. ... 5 Sh. 8'— 10' Wh. March IWI dispermum, Wall.,., 6 S. sc. 10' Wh. Anril arborescens, Roxb. .. b* S. sc. V. 0 r— ( 1 l 00 Wh. February. glandulosum, Wall., 8 Sh. 10' Wh. May 2 ■ Nyctantlies. arbor-tristis, L. ... to* Sh. 10'— 20' • « • May eM 3. Schrebera. swietenoides, Roxb o#» Tr. 20'— 30' Wh. June 4. Syringa. Emodi, Wall . ... Sh. 15' Wh. May ... 5. Fraxiims. floribtinda, Wall. 1 Tr. 40' Gr. April ... santhoxyloides, Wall, 2 Tr. 20' in May "‘I c3 o o t-1 Kota Dun Bhabar, Bage sar. Naini Till, Ka thi. Almora, outer hills. Ramgar valley, Bhabar Bhainskhet Do. sar. OF THE NORTH-WESTERN PROVINCES 525 Plants — (continued) . Conditions of soil, & c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks Rainy. >> Q Forest 2,000 R. • • • • •• Do. 4-8,000 R. • • i #!• Do. 1,000 R. ... • •• Do. 7—8,000, R. itl • • i Do. 5,500 R. itt • • * Do. 8,5—9,500 R. o • » Woods 0,5 — 7,500 R. Do. 1—3,000 R. ... • •• ■5 Do. 7—8,000 R. ... • • • Open 4—8,000 R. lit ... Do. »«• 4—7,000 R. • ll ... Do. 1 — 2,500 R, . . • . • • Do. 2,5—3,500 R. » .» DO. m 2,5— 3,50( ) R. .«! Forest 1 ,50( » E, ... in Do. it . 8,5—11,50 .) R. D. *09 Do. .. , 6,5—8,00 0 R. • •• III Open .. . 9—10,00 [ 0 «•» D. III • 526 HIM X LA Y AN DISTRICTS List of Kumcion Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant Colour of flower. Time of flowering. Locality. 6 Olea- glandulifera, Wall... 1 Tr. 30' Wh. April Naini Tal, out- er hills. acuminata, Wall. 2 Tr. 40'— 50' Wli. June Kapkot euspidata, I Vail. ... 3 Sli. 10' . . J une .. Josimath compacta, Wall. ... 4 Tr. 30' Wh. May Satrali valley, 7 Ligustrum. nepalense, Wall. ... 1 Sh. 15' Wh. June Biusar bracteolatum, Don, 2 Tr. 20' Wh. May Kapkot rob ust nm, IJj . Sf 1 . 3 Tr. 15' Wh. May Tola (S a r j u LXXI.— ABOCYNA- valley). CKJE. 1- Carissa. diffusa, Rcxb. ... *•» Sh. 10' W. June Outer hills ... 2 ■ Vinca. pusilla, Murr. « •« H. \ r Bl. October ... Ilawalbagli ... 3- Alstonia- scholaris, R. Br. ... • •• Tr. 30'— 40' Wh. March Kota Dun ... 4- Tabernsemon- tana- coronaria, R. Br. ... • a • Sh. 0' Wh. July Bagesar 5 ■ Holarrliena. antidysenterica, Wall. 1 Tr. 25' Wh. January ... Blrnbar pubescens, Wall. ... 2 Tr. 20' Wh. January ... Do. 1(1 6- Vallaris- clichotoma, Wall. .. ... S. BC. 15'— 20' Wh. March ... Do. 7 • Wriglitia- molliseima, Wall ... »•« Tr. 30' Wh. January Do. OF THE NORTH-WESTERN PROVINCES 527 Plants — (continued). 1 1 Conditions of soil, &c. Elevation in feet above the sea. Him layi a • r— * C3 Ph d - t. Sh ft Tibet. Eemarks. Open Wi 3,500 E. Forest • ft • 3,500 E. • « • ... Woods • ft. G— 8,000 E, • ft « ... Do. * . . 5—6,000. R. • ft • Forest • « < G— 7,000 E. Do. ft • • 3,500 E. • •• ... Open • 1 6,500 R. 1*4 Forest • •• 1—3,600 E. • •ft ■5 Open 4,000 E. ... • •• Forest • •• 1—2,000 E. • Oft • • • Cultivated • ft* 1—3,000 E. ft ft ft • ft* y Forest • ft* 1,00C > R- ... • • • Do. • * i,oor E. • • • Open • ft 1— 3,00C E. • •• Ml Forest •ft 1— 2,60C E. • •• • • • 528 HIMALAYAN DISTRICTS List of Kumcion Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 8- Nerium. odorum, Soland. ... Ml Sh. 6' Pk. May Bagesar, &c. 9. Cbonemorpha. macrophylla, G. Don , Tr. • •9 Ml Ml LXXII.— ASCLEPIA- HACEJE. l. Cryptolepis- reticulata, Wall. ... • It S. sc. 10' • • • • II Bagesar, Bha- 2- Periploca. calophylla, Falc. ... • • • S. sc. 40' Gr. Br. March ... bar. Outer hills ... 3- Calotropis. procera, R. Br. ... 1 Sli. CO =5 1 O Wh. Pr March ... Bhabar ... gigantea, R. Br. ... 2 Sh. Ml ... March ... Do. ••• 4- Vincetoxicum, ep. • •• II. 1' • • • July Bampa,Bhatkot 5. Cynanchum. auriculatum, W.8f A. 1 II. Sc. 8' Gr Y. August ... Ralam Valley, glaucum, Wall. ... 2 II. 1'— 1^ Y. Augusf . . . Almora, Naini Dalhousiffi, W. Sf. A. 3 II. Sc. 2'— 3' ... August ... Tal. Damus, &c. ... 6- Pentasachme. Wallichii, Wight ... Ml Sh. G"— 12" Wh. May Kapkot ... 7- Gongronema. nepalense, Dene ,,, Ml II. Sc. 10' Y. August ... Bagesar, Moh- 8. Tylophora, Goyanii, Dene. ... 1 Sh. 12" Pr. June argari. Jagthana Pass. liirsuta, Wight 2 • • • ... • •• • •• ? ©F THE NORTH-WESTERN PROVINCES. 52 $ Plants — (continued). 6 f—i «f— < o > O & c3 ■4-3 o Hima- laya. o 00 PS o •H ■U3 d o O Elevation in fe the sea. Rainy. >> fi Tibet. Remarks. If eat water ... 1—4,000 R. • «r ... »«0 R. » • • oil Open .. 1—3,500 R. • •• ... Forest 4,500 R. » • • ■Open 1—1,500 R. - 1 lit Do. 1—1,500 R. • •• Do. ... 9—10,500 R. D. • •• Forest ... 8,500 R. «• i Ml Ditto. 5 -8,000 R. • • « Open. ... 5—6,500 R. Ml «lt Shady, wet. ... 3,500 R. Ml = Marsdenia No. 5 in Herb S. & W„ Open 3—5,000 R. • •• Ml Ditto. 8,400 R. Ml ? • •• «•« • • 67 530 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower Time of flowering. Locality. 9- Marsdenia. tenacissima, W Sf A. 1 H. Sc. 8'— 10' • • • July Almora. „. Calesiana, Wiglit ... Boylei, Wight ... 2 S. So. ... July Ditto. 3 S. Sc. 10' Or. May Sarju valley, Naim Tal.. lucida, Edgew. 4 H. Sc. 30 Pr. August ... Binsar, Naini Tal. sp. 6 »•« ... ... ? 10- Pergularia. odoratissima, L. ... ... H. Sc. 15' • M June Almora, outer hills. 11. Hoya lanceolata, Wall. ... 1 S. sc. 20' Wh. March ... Kota Dun, Kap- kot. longifolia. Wall. ... 2 S. sc. 15' Bagesar 12 Leptadenia. viminea ... ... Sh. 4'— 6' if t May Bhabar ... 13- Ceropegia- elegans, Wall 1 II. Sc. 10' Pr. July Almora Wallichii, Wight ... 2 H. 1' Pr. April ... Naini Tal LXXIII.-LOG A- NIACEiE. 1. Buddleia. crispa, Benth. 1 Sh. 6'— 10' Li. March ... Almora ... Neemda, Ham. 2 Sh. 6'— 10' Wh. April Bhabar ... 2. Gardneria- angustifolia, Wall. • •• S. sc. 15' Ml March ... Binsar, Gagar, LXX1V.— GENTIA- NACEJE. 1. Crawfurdia- fascicu'ata, Wall. ... ... H. se. I o Bl. August ... i Madhari Pass. OF THE NORTH-WESTERN PROVINCES, 531 Plants — ( continued) . CJ <8 o 02 00 PI O T3 a o O Open Ditto. Ditto. Woods. Do. Do. Forest Open. Forest On rocks ... Iviver beds Open Do. o f> o c3 +3 o CD SH g <3 2 CC O) +3 ■a 4,500 4,500 5 — (3,000 5—7,50o 2— 4,000 3,500 3— 3,500 1 — 2,000 4.500 6.500 5—8,000 1—1,500 Hima- laya. C 3 R. li. it. li. 6,5—7,000 li- lt. li. li. ... li. li. li. li. ,• . 13 b .-2 ft I H D. Remarks. = Orthanthera in Herb. S. W . 532 HIMALAYAN DISTRICTS List of Kumaon be Name. § i a .3 « e h ? O cS i ,P £ O U bjj 4H O -4-3 d d PH O +3 Sh > o pO o3 O Hima- laya DO O m d O • r— < 4-i • rH d o O Elevation in fe the sea. .2 3 P3 Dry. Tibet. Remarks. Shady banks ... 2,000 it. • • • » •• Open 14,000 it. ••• * • • Do. 14,000 R. ... ... Do. 12,000 ... D. ... Do. 6,000 R. ... ... Do. ... 8,2,000. It. IM ... Do. 5—7,000 R. ... a • • Do. 12,000 R. ... Open ... 7—8,500 R. ... . a . Do. ... 5—8,000 R. ... ... Do. 11,500 R. • 1 Do. ... 11,500 It. Do. 12—15,000 R. D. r i. Do. 15,000 • •> ... T. Wet open 13,5—1500 « • i D. T. Open ... 15,000 • • • D. T. Do. ... 15-17,000 • • • ... T. Do. 14,500 It. • •• T. Do. 15,000 ... • • • Do. 13—17,000 .. D. T. Do. 12,000 R. ... •• Do. 15,000 T. Do. * • t 12-15000 Ml 4 # * D. t • • T. in = Swertia No. 1 in Herb. S. and W Do. 6 — 10,000 It. ... ... Do. 7— 8,00C Ml 534 HIMA'LAYAN DISTRICTS List of Kumaon 1 £.5 bi) a ^ rG -*a Jh Ch Name. P c3 ^ a fra 5 |S O 4J o u* bo 4H O P rS 4-1 O £ o on o CD £ o S3 SH (A S -5 A t—i c/J 4-3 ’rQ rC Jb 0 fH c o CD g 4-3 H CD o O o hJ 4- Ophelia— icon- eluded ). alata, Griseb. 3, 5 H. 2 r — 3' Mt August ... Biusar, Almo- purpurasccns, Don, augusti folia, Don ... 4 6 H. H. 2'— 3' 1 ' — 2' » • • August ... August .. ra. Do. Naim Tal, Almora, Sarju valley. Biusar, Gagar, paniculata, Don ... pulchella, Don *7 1 9 H. H. 2' ... August .. Dalhousiana, Griseb., 10 H. 1'— 2' ... August ... Ralani 5 • Swertia. speciosa, Wall. 2 H 3'— 4' W. BI. August .. Bindari. Ra- ccerulea, Royle 3 H. 9"— 12" Bl. August . . . lain. Ralarn ... 6- Halenia- elliptica, Don ... • •• H. 2' Li. AllgUBt ... Tola, K a 1 a - muudi . LXXY.— rOLEMO- NIACEiE. 1. Polemonium. * coeruleum, L. • •• H. 3' Bl. August ... Tola, Milam ... LXXVI. — BOEA- GINEiE. 1. Cordia. Myxa, L. latifolia, Roxb. ... 1 2 Tr. Tr. 40' • •• • 9 A • •a March In Bhabar ... Ditto. 2 Ehretia- gevrata, Roxb. kevis, Roxb. 1 2 Tr. Tr. 40' 30' w w. May ... March ... "Inter hills ... Bhabar 3' Ehabdia. viminea, Dalz. 4 Heliotropium- ... Sh. 6' Wh. 1 March ... f Sarju valley ... brevifolium, Wall. ... Ilf H. 8" Bk. J hily ... i Minora OF THE NORTH-WESTERN PROVINCES, Plants — (continued). 535 Conditions of soil, &c. Elevation in feet above the sea. H im lay S • f - i c3 W ti- ll. >> n o Tibet. Remarks. Open 1 1—7,000 R. • «« • • « Do. 0—10,000 R. • • • Do. 3—6,000 R. • II Do. G— 7,500 R. #• * . . . Do. . • • R. • •• • • • Do. 12,000 R. • • . ... Wet open 10—12,000 R, ... • •» Open " ... 12,500 R. Ill Ml Do. 7, 5—11,500 R. til ... * Do. ••• 11—12,000 R. D. Ml Forest 1 — 3,00C R. Do. 1,00< R. • •• Open .. 3—5,501 ) R. • • • • •• Forest .. 1—2,501 » R. • • . Ml River bed 2,50( 1 R. ... ... = Ehretia No. 3 in herb. S. & W. Open 5,50< 3 R. Ill 53 G HIMA'LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. i Height of plant. [ Colour of flower. i Time of flowering. Locality. 5 Trichodesma. indicum, JR.Br. ... Ml H. 6"— 12' Pr. March .. Outer hills ... 6- Cynoglossmn- microglochin, Benih 1 H. 3' - 4' Bl. August ... Ralam valley .. sp.- 2 H. 3'— 4' Bl. August ... Gori valley... furcatum, Wall. ... 3 H. 3^' Bl. June Binsar, Gagar... sp. 4 H. 3' Bl. August . Milam Wallichii, Don ... 5 II. 2' Bl. August ... Ralam valley .. furcatum, Wall. ... 6 H. 2'— 3' Bl. March ... Samkhet Bp. 7 11. 2' Bl. June ... Dhauli valley, .. micranthum, Desf., 8 H. 2'— 3' Bl. 1 June Almora sp. 9 H. ... ... August ... Kalamundi ... sp. 10 H. ... sp. ••• 11 H. * ... Dudatoli grandiflorum, Benih. 12 H. 9" Bl. June ... Patharkori ... 7. Solenanthus- sp. 1 H. 1' Bl. August .., Laptel sp. 2 II. 2' Bl. July Do. Rajpot... 8- Echinospermum. barbatum, Lekm. ... 4 H. 9" — 12" BL July Dhauli valley, glochidiatum, .DC. 5 H. O' BL | May Dwali, Pindari, sp. - ■ “ 6 H. 3" Bl. Mhy Do. 9. Eritrichium- sp.' — • 1 H. 2" BL August ... Kyungar Pass rotundifolium, DC. 2 H. 3" Bl. lime Patharkori .. nemorosum DC. ... 3 II. 8" Wh. 1 Jay Dwali longifolium, Don ... 4 H. 3" ... 1 August ... Suge, Milam... sp. ... 5 H. 2" Wh. i August . . . lalam sp. ••• 6 H. 2" Wh. i August . . . Ho. 10. Asperugo. sp ... H. 2" BL 1 August ... I kyungar Pass, 11. Bothriosper- muin. terellum, Fisch and Mey. ... ... | H 1 9" | BL P ebruary, jE iapkot. <0F THE NORTH-WESTERN PROVINCES 537 Pleads — (continued). o * f— 1 o CD !> O rQ d •4-3 CD Hima- laya. ✓ <4H o ec rt o +•> rt o a Elevation in ft the sea. a "S M hH Tibet. Remarks. Open 1—5,500 • •• o* • ... Bo. 8,000 R. Bo. 6—8,500 R. • • • ... Woods 5—7,500 R. • •• Open ... 11,500 -• B. .0. Bo. 8,500 R. • • • Bo. 5,500 E. . . • . . . Bo. 8—11,000 R, D. Do. ••• 5,000 R. «•» Woods • •1 8,500 • •• R. • . Woods 8,000 R. • • • = Lithospermum No. 1 in Herb. S. & w. Open 11,000 R. • o • ... Bo, 15,000 • •• • • • Do. 14-15,000 lit • « • * <>• Bo. 7—12,000 R. B. • <* » Do. 8—12,500 E. ... Bo. 8—12,500 R: • • . • a* Do. 16,000 T. = Myosoiis No. 1 in Herb. S. & W. Do. 11,000 E. ■ i« W oods 8,600 R. ,,, ... —Myosotis No. 4 in Plerb. IS. & W. Open ... 15-15,000 D. T. =Echinospermum No. 3 in Herb. Bo. ... 12,000 R. ... S. & w. Do. ... 12,000 R. • • • Do. ••• 16,50C R. IM T. Fields ... 3,50( ) ... i > -+-a "cS o utfi s S v - /+a O 3 c3 -+J * O SI a o -d W 4-3 12,000 11,000 11 - 12 - - 12,000 -15,000 12,000 Hima- laya. a ' 3 P3 15.000 14.000 6,000 3—5,000 11,500 6,000 4,000 1—5,000 1—4,500 4,500 1—5,500 1—5,000 11 — 12,000 Remarks. o a E-t R. D. E. R. R. R. D. T. R. R. R. R. R. R. R. R. R. R. R. R, R R, = Makar angti in Herb. S. &. W. D. ■. C atony ction speciosum in Herb. S. W. : Pharbitis Nil in Herb, S. &. W. Anise ia in Herb. S. &. W. D. 540 HIMALAYAN DISTRICTS’' List of Kumaon Name, Herbarium number (Straehey and Win- ter bottom). Habit of growth. Habit of plant. Colour of flower. Time of flowering. Locality. LXXYIII . — SOLA- NACKAE. 1 . Solaniun- nigrum, L. 1 H. 1 ' Wh. March ... Outer hills xan thocarpum, Schrad., var. Jac- quinii 2 H. 9 " Pr. All the Do. lysimaehioides, Wall, 3 H. 9 " Pr. year. August ... Gori valley ... verbascifolium, L. ... 4 Sh. 12 ' — 15 ' Wh. February, BIG bar, Bage- indicum, Nees. 5 Sh. S' sar. Bhim Pal sp. 6 Sli. 4' . • . • • • Alaknanda sanctum, L. 7 H • 4 4 valley. Bhabar sp. 8 PI. 1' ... • • • Outer hills 2. Physalis, flexuosa, L. ... 1 H. 2 '— 3 ' > February, Kaladhungi ... peruviana, L. ... 2 H. 6" Wh. July Almora 3 Datura. Stramonium, L. ... 1 II. S' Wh. July Almora, Naini sp. 2 H. 4' Wh. July Tal. Do. . ... 4- Scopolia. praealta, Dene. ,,, ... H. i'—iy Gr. Y. July Niti, Tisum ... 5- Hyosciamus- niger, L. ... H. 3' Pr. July Malari, &c. ... 6- Nicotiana- sp. IP. • M Almora LXXIX — SCROPlIU- LARIACEAE. 1- V erbascum Thapsus, L. i IP. 3' Y. August ... Ealam, Milam var. — - .c, 1 2 “• ! S'— o' Y. June ... Naini Tal, OF THE NORTH-WESTERN PROVINCES, 541 Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Open 1—7,000 Do. • • • 1—5,000 Do. 4— ,5000 Do. ■ • • 1—3,500 Do. 5,000 Banks •o 4,500 Open li« 1,000 Do. • •• 4,000 Do. 9 • • 1,000 Do. 5,500 Do. III 5—7,500 Do. 5,000 Do. • 91 11,5 — 15,000 Do. • • 10—11,000 Cultivated • * 1—5,000 Open • • 12,000 Do. • • « . 5 — 8,000 Remarks. 542 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 2 Celsia coromandeliana, V«hl. ... Id. 2'— 3' Y. May Bagesar 3- Linaria- ramosissima, Wall ... H. 6"— 9" Y. All the year. Alrnora, &c. ... 4. Antirrhinum Orontium, L. ... H. 1 r — 2' Pk Y. March Do. 5 Scrophularia. decomposita, Route. ... ] H. 2' July Milam variegata, Bieb. 2 H. 2' — 3' • • • J une Malari, &c. ... obtusa, E(h,ew. 3 H. 2' • . • Do. ... Alrnora himalaiensis, Roi/le.... 4 H. 4'- — 5' • • . July N ai ni Tal Edgeworthii, Benth. 5 H. 3' Pr. Gr. A ugust . . . Saba calycina, Benth. 6 H. 1' ... June Pindari, Pa- tharlrori . sp. 7 H. i'—n' • o July Laptel 6- Mimulus. gracilis, R.Br. • •• H. iV ... April Lodh 7- Mazus. dentatus, Wall. 1 H. 6"— 9" Pk. August ... Betuli Pass ... rugosus, Sour. 2 H. 6" Pr. March Alrnora surculosus, Bon 3 H. 6" Pr. Do. ... Kapkot 8- Lindentergia- urticnefolia, T.ehm. ... 1 H. 6" Y. August ... Jagcsar, &c. ... grandiflSra, Benth. ... 2 H. 1' Y. January ... Bagesar, &c. ... macrostachya, Benth., 3 H. 2'— 3' Y. March Kaiapathar ... 9. Limnophila. menthastrum, Benth., 1 H. 6" July Alrnora ... Koxburghii, G.Dott, hypericifolia, Benth., 2 Id. 4" • • • February... Patli Dun 3 ... + ... ... 10- Herpestis. Monmeria, B B K. ... • • • H. 6" Li. August ... Bhabar, Ram. ganga valley- OF THE NORTH-WESTERN PROVINCES 543 I'l ants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. j Tibet. Remarks. .5 3 « ft Open ... 1—3,000 R. f • • ... Banks 1- — 5,500 R. ... ... Fields 1—5,000 E. • •• ... Open 13,000 ... D. (|t Do. 10,500 ... D. Do. 5—7,000 K. ... W oods 6—7,000 R. ... Open 8,500 R. ... Do. 10—12,000 R. . . • ... Do. 15,000 ... ... T. Do. 5,000 R. «•» • •• Wet rocks 8,000 R. • • • Open ... 1—5,000 R. ... ... Do. 3—9,500 R. ... * * * Shady banks ... 1—7,000 R. . • Do- 3—5,000 R. ... It! Open 1—2,000 R. ... . • « Wet 4,000 R. • •• Do. * • i ... • •• ... • •• • •• DO. at 1—5,000 R. ■ ••• • • * HIMALAYAN DISTRICTS 544 List of Kumaon Name. Herbarium number' (Strachcy and Win- ter bottom.) Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 11. Dopatrium- juncetim, Ham. ... H. 9" ... ... ... 12- Torenia- edentula, Griff . ... H. 1"- 2' Pr. September, (Naini Tal, Sar- in valley. 13. Vandellia. Crustacea, Benth. 1 H. 2" Pk. July Almora pedunculata, Benth 2 H. 12" Bl. July Do. uummularifolia, Don, 3 H. 3"— 4" Pk, August ... Naini Tal 14 Bonnaya- bracliiata, Link. ... e. 3" Pk. July Almora, &c. ... 15 Hemiphragma. heterophyllum, Wall., ... H. cr. 6" ... May China, Dhakuri Pass. 16- Picrorhiza. Kurrua, Beyle. 1 H. 6" Br. Pr. Do. ... Madhari Pass... sp. 2 H. 9" ... July Milam ... 17- Wulfenia. Amherstiana, Benth . . . . ... H. 8" Bl. June Binsar 18- Veronica. Anagallis, L. 1 H. I'— 2' Pk. March ... Ramgar, & c. ... laxa, Benth. 2 H. 6"— 9" Bl. May Dwali ciliata, Fisch. 3 H. 3"— 4" Bl. August ... Barjikang Pass, sp. 4 H. 6" Bl. September, Milam, Topid- hunga. Berpylli folia, L. 5 H. 2" 6" Rl. August ... Ralam cana, Wall 6 H. 6" Bl. Do. ... Saba agrestis, L. 7 H. &"■ — -9" Pk. March Almora Maddeni, Edgew. 8 H. 4" Bl. Do. ... Do., Naini Tal. biloba, L 9 H. 6" Bl. March Naini Tal, Mi- lam. capitata, Boyle 10 H. 3"— 4" Bl. August . . . Barjikang Pass lanosa, Benth. 11 H. 1' Bl. July Niti OF THE NORTH-WESTERN PROVINCES 545 Plants — (continued). 6 O CD t> O rQ 03 -v=> CD Hima- laya. *H O CQ rt o -t-3 >r 3 a , o o Elevation in ft the sea. Rainy. Dry. Tibet. Remarks. ... »•« • H. ... ... Wet 4—7,000 R. ... ... s' Do. 4,000 R. . . • ... Do. 4,000 R. ... . . . Shady damp . . . 5—6,000 R. . . . Open 5,500 R. ... ... Do. 7,5—11,000 R, ♦ 7 % Do. 10—12,000 R. . . . ... Do. 12,000 R. D. . . . Woods 7—10,000 \ R, ... ... Wet 6—6,500 R. • . • Open 8,500 R. ... ... Do. 13,500 R. ... Do. 13—15,000 • • • D. T. Do. 12,000 R. • • . ... W oods 9—10,500 R. ... 1 ••• Walls 5,000 E. ... Open 6 — 7,500 R. ... Do. 5—13,000 R. D. ... Do. 13,500 R. ... ... Do. 10—13,000 ... ii. ... • 69 546 HIMA'LAYAN DISTRICTS Name. 19— Buchneva- hispida, Ham. ... sp. 20— Striga- enphrasioides, Benth ., hirsuta, Benth. 21— Centr anther a. hispida, fi.Br. 22— Sopuaia- trifida, Barn. 23— Leptorhabdos . parviflora, Benth. ... 24— Euphrasia- officinalis, L. 25— Pedicularis- megalantha, Don Ditto gracilis, Wall. Ditto carnosa, Wall. siphonantha, Dun ... pectinata, Wall. tubiflora, Fisch. verticellata, Wull. ... versicolor, Wall. Ditto Hookeriana, Wall. ... rhinanthoides, Schrenk. e P- List o f Kumcton [ Herbarium number (Strachey and Win- terbottom). Habit of growth. H eight of plant. Colour of flower. Time of flowering. "cS o o 1 H. 1' Bi. October ... Gopesar, Almo- ra. 2 H. 1' Bl. Do. ... Alrnora, &c. ... 1 H. 6" W. August . . . Tejam, &c, ... 2 II. 6" Y. Do. ... Gangoli, &c. ... ... H. 6" Pr. July Alrnora ... H. 2' Y. August . . . Do. ... H. 2'— 3' ... Do. ... Gagar, Binsar, ... H. 3"~ 9" Y. W. June Dhakuri-bina- ya, &c. 1 H. 1'— 2' Pr. August ... Kalimundi, Mi- lam. 7 H 6" R. Do. ... Ralam 2 . H. 1'— 2' Pr. Do. ... Girgaon, Pitti river. 11 A. 9" R. Do. Gothing 3 H. 6"— 12" R. August . . . Nami Tal, Al- mora. 4 II. 6" R. Do. ... Ralam 5, 15 H. 3' R. Do. Saba 6 H. 4" Y. Do. ... Milam, valleys of Gugd. 8 II. 4"— 6" R. Do. ... Bar jikang Pass. 9 H. 6" R. May Pindari 13 H. 4"— 9" Br. Y. September. Rimkin, Balch- ha Pass. 10 H. 4"— 6" R. June Rogi-la 12, 13 H. 6" R. September, Balcliha Pass ... 14 H. 3" R. Do. ... Do. OF TH 1C NORTH-WESTERN PROVINCES, 547 Plants (continued). Conditions of soil, &c. Elevation in feet above the sea. Hit la I .3 3 nd- /a. (H Q | Tibet. i Remarks. Open 3—5,000 E. Do. 4,000 R. • •• ... Do. 4,000 R. Do. 4—5,000 R. ... . . . Wet 3—4,000 R. ... ... Open 5-6,500 R. ... ... Do. 6-8,000 R. ... ■5 Do. 8—1 2,000 R. D. Do. 7—1 ',500 R. D. ... Do. 12,000 R. ... ... Do. 1 2,500 D. . . . Do. 5—7,000 R. . . . . . . \ Do. 12,000 R. . . . Do. 8—9,000 R. Do. 11—15,000 b. T. Do. 14,700 R. ... ... Do. 10,500 R. . . . Do. 13—16,500 ... T. Do. 11,000 R. . . . Do. 13—16,500 ... ... T. Do. 16,500 , . , . . . T. 0 548 HIMALAYAN DISTRICTS List of Kurnaon rH t S.s be Name-. r barium nr Strachey and erbottom). A 4-3 £ O be o 4-3 IS +=> a & 'Ph O +3 oc Sh 0) £ o 4-f O Sh 2 O .2 *Sh a> £ o '-H o Q) 4-3 • H "c3 0> W+J hh HH o3 K 0/ a 'o O a H O O h4 LXXX — OROBAN- CHACEAE. 1— iEginetia. indica, Boyle. ... II. i' Br. Pr. August . . . Kapkot, Bilim- 2— Orobanche- tell . indica. Wall. 1 9"— 12" March Hard war S]X' 2 ... 6"— 9" * . . May Dwali, Ramni, sp. 3 . . . • • • July Tola epithymum, DC. 4 V 00 V Jnly Ralam, Milam, LXXXI — PLUMBA- GINACEAE. 1 — Plumbago- zeylanica, L. Sh. 4"— 5" Pk. March Bhabar, Bage- LXXXIL— GESNER- sar. ACEtE. 1.— .ffischyiiaiitlius. ramosissima, Wall. ... H. sc. i' — 14' Sc. August . . . Mohargari 2 .— Lysionotus. ternifolia, Wall. ... H. 9'— 15' Pr. Do. ... Bagesar 3 — Rhynchoglos- sum. obliquum, DC. Ml H. i'— 14' Pr. Bl. October ... Outer hills ... 4-— Platy stemma ■ violoides, Wall. • • • H. 3" Bl. August . . . Naini Tal 5 — Didymocarpus- lanuginosa, Wall. ... macrophylla, Wall. ... 1 H. 3" Pr. Do. ... Almora 2 H. 9" Pr. Do. ... Mohargari, Ba- subalternans, Wall. ., 6— Chirita. ... H. l' Pr. Do. gesar. Dyari Pass, Ramni. bifoiia, Don 1 H. 4" Pr Y. Do. Outer hills Edgeworthii, DC. ... 2 H. 6" Pr. Do. 1 Gangoli, & c. ... | OF THE NORTH-WESTERN PROVINCES 549 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. j Tibet. i Rainy. t. 0 Open 3—4,000 R. ... ... Fields 1,000 R. *»• On trees 8—10,000 R. ... Fields 11,500 . . . D. ... On Thymus . . . 12—13,000 R. D. W oods 1—3,000 R. ... ... / ■9 Trees 4,000 R, Trees & banks, 2,5—4,000 R. ... Shady banks . . . 1,5—4,500 R. ... ... Trees & rocks. 6—8,500 R. ... ... Dry rocks 5,000 R. Wet rocks 3—5,500 R. . . . Do. 6,5—8,500 R. ... ... Shady banks .. 2—5,000 R. Do. 4—5,000 R. . . . * * * Remarks. / 550 HIMALAYAN DISTRICTS List of Kurnaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. bb • >— < r-*' CD o <4H O CD H a H Locality. LXXXIII.- — BIGrNO- N I ACE AO. 1— Calosanthes- indica, Bl. Tr • •• Bhabar a n d 2 ■ — Stereospermum suaveolens, DC. »•* Tr. • • • outer hills. Bhabar 3 •— Amphicome- Emodi, ( Royl I 1 H. 6" Pr. March J Deoprayag arguta, ( Uuyle ) 2 S. H. l'-l*' Pr. July Dhauli valley, 1 LXXXIV — PE DA- LINEAL 1 — Sesamum. indicum, L H. 3' — 4' Do. ... Bhabar, Almo- LXXXV. — ACANTH- 1 — Thunbergia coccinea, Wall. Sh. 10 r — 15' Sc. December, ra. Baliya bridge, 2-— Hygrophila- polysperma, T. Anders. H. • #« Harara, Mohan 3— Kuellia- hirta, Vahl. Sh. 2' Bl. March Outer hills .... 4 — Petalidium barlerioides, Nees ... ... Sh. o' Wh. February, 3habar 5— Strobilanthes. Edgeworthisnus, Nees, 1 Sh. 3' Bl. ] December, 1 dota Dun auriculatus, Nees 2 Sh 3' Bl. Do Do. glutinosus, Nees 3 Sh. 2'— S' Li. ] 0 ebruary, 1 vapkot Wallichii, Nees ... 4 H. 2' Bl. , August ... 1 iur Pass alatus, Nees 5 Id. 3' Bl. Do. ... 1 )iyari Pass ... attenuatus, Jacq. 6 H. 3' Pr. Do. ...I ^ohathat sp. 7 H. 2' Pr. Do. Ounghasi OF THE NORTH-WESTERN PROVINCES, 551 Plants — (continued) . 6 o o t> o rO c3 > n ft ! Tibet. Remarks. Forest 1—3,000 Ml ... Do, 1,..3,000 ... • • • Open 1,500 R. ... On rocks 7,000 R Open and cul- tivated 1—5,500 R, • •• * ... Forest 2,500 R. ... = Heceacentris in Herb. S. & W. 2,000 R. ... ... = FJemiadelphis in Herb. S. & W. Shady woods ... 1—5,000 R. ... ... Forest 1,500 R. ... ... Do. 2.000 R. Do. 2,000 R. • • • . . • Woods 3—5,000 R. . . . ... Open .. 11,000 R. ... W oods 6—7,000 R. . . . ... Open 6,000 R. ... Woods 9,000 R. . . . . . . • 552 HTM/LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). j Habit of growth. Height of plant. Colour of flower. 1 Time of flowering. Locality. 6 — Goldfussia- eapitata, Nees 1 H. 3' Bl. August ... Kalimundi ... bracteata, Nees 2 H. 3' Pr. August ... Mohargari . . » penstemonoides, Nees, 3 H. 3' Li. August ... Naini Tal . . • divaricata, Nees 4 H S' ... August . . . ? 7 .■ — M climanther a • Wallichii, Nees in Sh. 8'— 10' Bl. August . . . Sarju valley ... 8— Barleria. dichotoma, Roxb. 1 H. 2 f Pr. August G angol i • • • cristata, L. ... 2 H. s' Pr. September, Bagesar • • • var. 4 H. Pr. September, 'Kalapathar • •• cilialata, Roxb. 3 H. 2' Pr. Sep tear 1 er, Outer hills • • t nepalensis, Nees ... 5 H. 3' Wh. September, Satrali • • • 9 — Asystasia. macrocarpa, Nees • • • H. 3'— 4' Pr. October ... Kota Dun 10 — Eranthemum. nervosum, R.Br, • « Sh. 3' Bl. March Outer hills ... 11 .— Plilo gac anthus thyrsiflorus, Nees ... ill Sh, 3'— 4' Or. Br. Marrh ... Kota Dun l"i 12— Lepidagathis- euspidata, Nees 1 Sh 1'— 2' Wh. Pr. March ... Outer hills Kl ustulata, Nees ... 2 Sh. 1'— 2' Wh. March Do. • •• purpuricaulis, Nees... 3 Sh. 1 '—2' Wh. March ... Do. • •• hyalina, Nees ... 4 H. 1' Wh. March ... Do. 13 — Justicia- micrantha, Wall. H, 9" Li. August ... Ratnari Ml procumbens, L. H. 6"— 9" Pk. March .. Outer hills • • • Adhatoda, L. ... • •• Sh 00 f o Wh. March ... Plains, Bagesar, 14— Eiingia- parvifiora, Nees • •• H. 3"- 4" Bl. March ... Sirmoria • •• «5E THE NORTH-WESTERN PROVINCES 553 Plants — (continued). Conditions of soil, &e., CD > o rO oS +3 Q) . ^ i Him d- laya. Elevation in fc the sea. tA c3 t, ft Tibet. Remarks. Woods 8,500 R. J)o. (>,500 R. . . . .. . Do. 7,000 R. . . • ... Do. * * * Open 4,000 R. ... Do. 3—5,000 R. Do. 3,000 R • . . ... Do. 2 — 6,000 RE , .. . Do. 8,-5.000 R. „ , Do. 4,000 R ... .. . Shady banks . . . 2,000 R. ..T ' • • • Woods ... * / 1—4,000 R. *»w M. Forest 1,5—3,000 R ... Open 2—5,000 R. Do. 2—4,000 K. ... Do Do. 2—4,000 R. ... ... . 2—4,000 R ... Shady banks ... 4,500 R • •« = Rnstellarid. No. 2 in Herb. S. & W ( )pen 3—5,000 R. >• • =•= nostellaria No. 2 ditto ditto. Do. 4—5,000 R | "• ... = Adhatoda vasica ditto ditto. ' Do. 4,000 ' l R L ... 70 554 hima'layan districts List of Kumaon Name, Herbarium number (Straeheyand W in- terbottom). Habit of growth. Height of plant. i Colour of flower. Time of flowering. Locality. 15 Dicliptera. bnpleuroideB, A hes ... *•* H. o' Pk. IM Outer hills ... 16- Peristrophe speciosa, Nees 2 H. Sh 3' — 4' Pk. February, Outer hills, B&- g p, 1 H. Sh. 2' Sc August ... gesar. Gangoli ... LXXX VI. — SEL A - GLNACELE. 1. Gymnandra- kunawarensis, Boyle • •• H, 6"— 9" Bl. July Raj-hoti, Ra- LXXXVII.— VER- BEN ACEiE 1. Phryma. leptostachya, /-. ... f •• H. ! 2' Pk August „. kas Tal. Naini Tal, &c., 2- Lantana. alba, Mill. Sh. 4 ' Wh. March ... Outer hills ... 3. Lippia. nodiflora, llich. t»< Ii. cr. 1' Pr. Br. March ... Kalapathar, &c. 4 Verbena- officinalis, L. .. H. 2' Li. March ... Outer hills 5 Callicarpa- macrophylla, Vahl. ... 1 Sh. 10' Li. August ... Outer hills, Ba- arborea, Roxb. 2 Tr. CO 1 V. o 04 Ml May geBar, Do. do. ... 6- Premna. herbacea, Roxb. 1 H. 2"— 3" W. Y. May Bagesar interrupta, Wall. 2 Sh. s 1 V o Wh. May Supi barbata, Wall. 3 Tr. 25' Wh. May Bhabar, B£ge- integrifolia, L. .. 4 • •a Wh. • •• sar. Do* OF THE NORTH-WESTERN PROVINCES 555 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks. Rainy. | b Q Woods 2—4,000 R- ... Shady woods ... 1—8,000 R. Ml » # » Open 4 5,000 R • • . • • • Wet open 15—16,000 ... • • 1 T. Damp woods . . . 6—7,500 R, ... » • * Open 1—3,500 R. ... Wet 2—4,000 , R. • •• Open 1—6,000 R. Do. 1—4,000 R. ... ... • Do. 1—3,000 R. • t* Do. 3,000 R. Do ... 4—6,000 R. • •• Forest ... 1—3,500 R ... Do 1,000 R. • • • M* 556 HIMALAYAN DISTRICTS List of Kurnaon Name. Herbarium number (Strachey and Vi in- terbottom). Habit of growth. Height of plant. Colour of flower Time of flowering. -4-a § 7- Gmelina. arborea, Roxb. ... Tr. V. 0 1 S Y. March ... Bhabar 8. Vitex Negundo, L. !•« Sh 10' — 15 ' Pr. April Bhabar, outer billB. 9- Clerodendrnni. infortunatum, L. 1 Sh. (>' Pk. February, Bhabar gratum,. [Yuli. 2 Sh 6' Sc. VV. M arch Naini Ta!, outer hi Is. serratum, Spreng, 3 H. 3' Pr. June Bagesar 10 Holmskioldia- Banguinea, Retz. 11. Caryopteris. • • * Sh. 15' Sc December, Ivalapathar ... W allichiana, Schuuer., t • • Sh 10'— 12' Pk. February, Bhabar, Bage- sar. LXXX Vll I. —LABI- ATE. 1- Geniosporum- Birobilifcr um^ Wall , ... II. 1 1 2 Pr. August ... Sarju valley ... 2 Orthosiplion- virgatus, Benth. 1 H. 1' May Bagesar rubicundus, Benth. ... 2 • • • 1' Pk. August .. Kosi valley ... 3- Plectranthns. tfcrnifolius, Don ... 1 H. 3 '— 4 ' October ... Bhabar, Sarju valley. rugosus, Wall. 2 Sh 4 ' Naini Tal Costsa, Don 3 H. 3 ' Li. February, Kota Dun, Al- in or a. eordifolius, Don 4 H. 3 ' Bl. Almora scrophu'.arioides, Wall. 5 Ii. 3 '— 4 ' W. Y. August ... Kalimundi Gerardianus, Benth.... 6 , 10 II. 1 '— 3 ' Wh. October ... Gori valley, Almora. Maddeni, Benth. 7 H. 4 ' Li. August ...; Ka’imundi Striatus, Benth. 8 II. 2' Almora Stracheyi, Benth. 9 II. H' Li. 1 October ... 1 Sarju valley .. OF THE NORTH-WESTERN PROVINCES 5-57 Plants — (continued) . o «3 e o T ) sa O Cf Forest Open Forest \V oods Open Woods Do. Open < L > > Q .£5 c3 0} OJ s ^ o a > (H « Open 12—15,000 R. D. T. Do. 5—8,000 R. . . . Do, ••• 5 — 7,000 R. it* ... Near water ... 4,500 R. Ml Open 12,000 R. ... Do. 5—8,000 R. Woods ... 7,500 R. • •• Do. 5 — 6,500 R. • • • Open ... 4—8,000 R. 101 Open woods ... 10—11,000 R. • • • Open 7—11,000 ... D. f »« Do. 7,000 R. mo i •• Do. 1 — 5,000 R. • • • Ml Naturalized .. 4,000 R. • •• • •0 Open .] 1—5,000 R, • •• ... Do. 8,5—12,000 R. D - Do. .. 7,000 R. 1 Ml • •<1 Do. 1,000 R. 1 ... ... Do. 8,500 R. ... . . . Do. 6,500 R. ... ... Do. . 7,700 R. ... ... Do. 11—15,000 ... D. T. Do. 15,500 u< ... • . * Do. 15—15,500 ... ... T. Do. . 17,000 ••• T. \ Remarks. 71 562 -hima'layan districts List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 20- Dracocepha- 1am- acanthoides, Edgeiv ., 1 H. 6" Y. August ... Kyungar speciosum, Benth. ... 21- Scutellaria. 2 Id. 9" Bl. August ... Kalajawar discoloT, Calebr. 1 H. 6" Pic. August ... Jagesar ... linearis, Benth. 2 H. 4" Kk. Y. March Ain ora angulosa, Benth. 3 H. i'—iy Pk. Y. March Almora, Naini Tal. ' sp.— 4 Id. 2' Pk March Do. repens, Ham. 5 11. 2'— 3' Pr. March Kota Dun prostrata, Jacq. 6 H. 6" Pr. Y. August ... Milam grogsa, Wall 7 H. S' Bl. August ... Gagar Pass ... 22. Brunei! a- vulgar is, L. ... H. &"■ — 9" Pr. August ... Naini Tal, & c., 23 Marrubium. lanatum, Benth. ... II. 6" Br.? August . . . Shelshel 24 Craniotome- 1 versicolor, Reich. 25- Anisomeles- ... H. 2' Pk, W. September, Almora, &c. ... ovata, Br. • • . H. 2'-4' Bl. August . . . Almora, &c. ... 26- Colquhounia vestita, Wall. 27- Stachys- ... Sh. 4'— 8' Sc. June Naini Tal, Gori valley. sericea, Wall. 1 H. 2' Li. July Almora splendens, Wall. 2 II. 2'— 3' Li. July Naini Tal 28- Leonurus- Cardiaca, L. . • . II. 2'— S' Wh. June Naini Tal 29- Lamium. araplexicaule, L. 1 H. 9" Pr. March ... Almora, Naini Tal, Naini Tal, Sa- ba. petiolatum, Royle 2 II. i' — 1§' Wh. May rhomboideum, Benth., 3 H. 9" Wh. September, Kyungar, &c.... sp ?■ . 4 H. 6" • • . June Sagtia-deo 30 Roylea- elegans, Wall. ... Sh. 6'— 8' Br. March Almora, Naini Tal. I OF THE NORTH-WESTERN PROVINCES. 563 Plants — (continued). d o CD o nO c3 -8 Hima- laya. OQ O OQ fl O- • r-< +3 • • r— < pi o O CD 4H .2 5 ^ O CD * c3 q; \> ,£2 CD 7a . S >> .2 8 M i-. ft- 4^ •■ 3 H. 5" July Niti Do. 4 H. 1'— 2' May Naini Tal, &c., Do 5 H. 1' August . . . Pal am valley... XC.-NYCTAGIN- ACE.®. 1. Bcerhaavia- sp. 1 H. 2'— 3' Pk. July Joshimath, Je- 1am. sp. 2 H. 2'— 3' Pk. July Tapuban cliffusa, L. 3 H. 2'— 3' Pk. January ... Kaiadhungi ... XCI.— AMARANT- ACEiE. 1. Deeringia- baccata, Moq. ... Sh. 20' ... October ... Jyari OF TIIE NORTH-WESTERN PROVINCES. 565 Plants — (continued) . Condition of soil, &c. Elevation ’n feet above the sea. Hima- laya. .s c3 P4 P s- p Open 3—4,000 R. Fields 1—4,000 R. ... Open 4—5,000 R. ... Do. 5—6,000 E. . . . Cultivated 1—2,000 R. ... Remarks. Open Do. 10,000 9—11,500 Woods Open Do. Do. 8,000 5,800 5,000 4,500 R. R. R. R. Do. 4__8,000 R. • • • Do. 4,000 R. . • • Near water ... 1, 5—4,000 R. , ^ Open 12,500 R. . * . On rocks ... 8,500 R. Open 5—7,000 R. Do. 9,500 E. Do. 11,500 . . . D. Do. O O © r—i 1 xo R. . . . Do. 11,000 R. ... Do. 7—9,000 R. D. Do. 7,000 R. . * * Do. 1—7,000 R. Woods 3,500 R. HIMALAYAN DISTRICTS 5 (? 6 ' List of Kumaon Name. Herbarium number (Htracheyand Win- terbottom). Habit of growth. _ i Height of plant Colour of flower. Time of flowering. O O 2- Celosia argentea, L. ... H. 1'— 2' Pk. W. March K a 1 a p athar, &c. 3- Amarantus- spinosus, L. I H. 2' Gr. August . . . Kota, Almora, ; Anardaua, Ham. 2 II. 3'— 4' R. Y. August ... Kathi, &c. caudatus, L. 3 H. 3'— 4' R. August ... Almora, &c. ... 4- Cyathula capitata, Moq. 1 II. 3' August . . . Jagesar tomentosa, Moq. 5- Pupaiia. 2 Sh. G/ * * * J une Almora, &c. .... lappacea, Moq. t • i ... ... ... ... Kaladhungi ... 6 iErua. ecandens, Wall. ... II. 2' —3' Wli. March Outer hills 7- Achyrantlies- sp 1 H. 3'— 4' Wh. August . . . Lohathal argentea, Lam. 2 II. 3' Wh, August ... llawalbagh aspera, L. 3 II. 4' Wh. August ... Naini Tal 8- Alternanthera- sessilis, B.Br. ... II. er. 1" ... August ... Almora XCII. — CIIENOPO- DIACE^E.. 1. ChenopocLium. multiflorum, Moq. ... 1 H. 2'— 3' ... August ... Badarinath ... album, L. 2,4, 5 II. 1'— 2' Gr. August ... Tola, Almora, sp. .3 H. . . . ... A ugust . . . Milam sp-— 6 11. . . . Botrys, L. 7 II. 9" ... ... Almora 2. Blitum. virgatum, L. ... II. 9" . ••• August . . . Malari i ■OF THE NORTH-WESTERN PROVINCES 56-7 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hi)i lay >> £ c5 P3 Dry. ? P Tibet. Remarks. In fields 2—5,000 R. ... ... > . Do. 2—6,500 K. Cultivated 4—9,000 R, ... ... Do. 6—8,000 R. • • . • . . Shady 6—9,000 R. Open 5—7,500 R. ... Do. 1,000 R. ... ... Do. ••• 1—5,000 R. * 9 ... Shady 6,500 R ... Do. 4,000 R. ... ... Do. 4—7,000 R. . • . Open 4,000 R. ... • • t Do. 10,000 D, - In fields 6—11,500 R. D. ... Do. 1 1 ,500 D. ... . . . R. . » • ... Cultivated 5,000 R. . . . . . . Open . ’ 10,500 ... D. ... 568 HIMA'LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. bi) .2 CD £ o <33 O CD a Locality. 3. Beta- vulgaris, Moq. t • • . . . , , var. orientalis ... ... H. ... ... ... Almora 4. Atriplex. sp. — - 1 II. 2" 3" . • « August . . . Topidhunga ... sp. 2. II. cr. 3" ... August . . . Milam 5- Eurotia- ceratoides, C.A. Mey., ... Sh. 1 ir 1 2 ... August , . . Laptel, plains of Guge. 6- Salsola- Kali? L. ... H. 4" • . . August ... Tisum XCIII— PHYTOLAC- CA CEiE. 1. Phytolacca. | tlecandra, L. • * * H. 1 ' Gr. May Bagesar, &c.,... XCIY.— POLYGONA- CEJE. 1. Polygonum- macropliyllum, Don, 1 II. 9" Cr. June Dudatoli, Cha- mi Pass. Brunonis, Wall. 2 H. 9" Cr. September ,Ralam, P i n - dari. vaccinifolium, Wall. 3 H. 4" Cr. August . . . Do. &c. ... viviparum, L. 5 ir. l'-ll Pk. August ... Ralam, Laptel, var. 4 H. 6" Pk. August . . . Valleys in Guge. var. gracilimum, 6 H. 6" Pk. June Rogila horridum, Roxb. 7 II. S' — 4' Pk. July BhimTal capitatum, Don . . • H. cr. ... ... / var. pingue 8 4" Pk. 'March ... Almora, outer hills. nepalense, Meisn. ... 9 H. 2 ' Pk. May Naini Tal, &c. sphcerocejihalum, 10 H. cr. 1' — 2' Pk. Pr. May Kathi Wall. perforatum, Meisn. ... 11 H. 1' Pk. May Naini Tal amplexicaule, Don ... ... . . . . . . . . • May var. ambiguum 12, 14, H. 3' Pk. Do., Kathi, &c. var. oxyphyllum ... 13 ... ... ... ... OF THE NORTH-WESTERN PROVISOES. Plants — (continued). O <3 o in O w a •© § o CD > a x c3 • 4-3 CD CD ■ 4-4 g c3 O CJ +3 * C$ 0) > -3 CD +J Hima- laya. .5 +a . - a> fc> ! r2 fi i H 1 •Cultivated 500 U. ... ... Open 15,000 T. Do. 13,000 * * * D. ... Do. ... 15—16,000 ... ... T. Do. 15,000 ... ... T. Cultivated 3—7,000 - E, • . • Open 10—12,000 R. • • • ... ... 11—14,000 K. D. ... 11,-13,000 R, D. • . • Open 11—14,5000 E. D. T. Open rocks ... 14—16,000 ... ... T. 11,000 E. ... • • • Near and in 4,400 R. ... ... water. Open 6,000 R. ... ... Do. ... 6—11,500 R. • . • • . • Forest 7-8,000 R. ... ... Do. 7,000 R. ... ... Do. 6—8000, R. , . . ... * * * *•* • « • ... 569 Remarks. 72 570 HIMA'LAYAN DISTRICTS Li M of Kumaon Name. Herbarium number (Strachey and Win- ter bottom). Habit of growth. Height of plant. Colour of flower. i Time of flowering. Locality. lanigerum, R. Br, ... var. indicum 15 H. 2' Pk. July Bhim Tal, Al- flaecidum, Roxb. 16 H. 3' Wh. IN' 1 ay mora. E agesar, near Posumbu, Ham. 17 H. 2' R. June Naini Tal Na ni Tal, &c.. strictum, All. 16 H. 2' Pk. August ... Sarju valley ... Hamiltonii, Spreng., 19 H. 2' Wh. July Almora barbatnm, L. 20 H. 2' Pk. jlebruary, Bhabar aTicuIare, L. • . • , , , . . . ... var. difEusum 21 H. cr. 1' Pk. August ... Milam Dryandri, Spreng. ... 22 II. cr. i" Pk. Nay Naini Tal, &e. illecebroides, P elsn .... quadrifidum, Ham. ... 23 H. cr. \r/ Pk. March . . . Outer bibs 24 H. 4' Wh. June Naini Tal glabruui, Willil. 25 H. 2' Pk. July Do., Kosi ri- amphibium, L. 26 II. 4' Pk. June ver. Do. pterocarpum, Wall. ... 27, 28 11 . sc. 4'— 5' Wh. A ugust Almora, Naini • polystachyum, Wall, - September. Tal, Dhauli valley. var. glabrum 32 H- 3'— 4' w. August ... Vishnugauga var. pubeseens 33 II. 3' — 4' Pk. A ugust . . . valley. Pal am, Milam. frondosum. Meisn. 24 Sh. 8' Pk. May Lahur, Kathi ... rumicifolium, Royle , 42 H. 1 1 r 1 2 Gr Y. A ugust . . . Ralam var oblongum 35 H. 2' ? May Jhuni chinense, L • . • , , , • «. . • « var. Tlmnbergia- 36 H. 1 ' — 2' Pk. May Naini Tal nmn. var. corymbosum ... 36i H. 1'— 2' Pk. May Ho. filicaule, Wall. ,, , var. extenuatnm ... 37 II. cr. 4" Pk. August ... Ralam, Milam. delieatulum, Meisn.... 38 II 3" Pk. August ... Gothingy Ra- sp. 39 H. 1 rr 2 K. August ... lam. Barjikang sinuatum, Royle 40 H, 4" Pk. August ... Pass. Ralam, &c. reeumbens, Royle ... 41 H cr 6"— 9" Pk, August ... Naini Tal, nummul ari f o 1 i u m , 43 H. G" Pk August ... Dyari Pass. Barjikang Pass. Meisn. perforatum, Meisn. ... var. glacial e 44 H. 2" Pk. August . Milam ... hntaile, Meisn. 45 H. 3" Wh. August ... Ralam valley... cognatum, Meisn. . , • . . var. alpestre 46 H. 11" J 2 W,Pk. August 3ompras OF THE NORTH-WESTERN PROVINCES Plants — (continued). 571 Conditions of soil, &c. Elevation in feet above the sea. Hi/ lay V, s « )&- a , & i Tibet. Remarks. | Near water 4,000 E. ... ... Do. 3,000 R. ... ... Do. 4 6,500 R. ... . . . Open 4,000 I?,. Near water ... 4,000 R. ..a ... Open i— 2 ooo K. " 1 . . . Do. 11,500 D. ... Do. 5—7,000 R. .. Do. 1—7,000 R. ... In water 6,100 R. ... ... Do. 1—6,100 R. ... • ** Do. 6,400 R. ... On bashes 5—7,000 R. . . . ... • •• a • • ... Open 9—10,000 R. D. M * Do 9 — 12,000 R. D. ... Near water 7—8,000 R. ... ... Open 1 1,500 R. ... Do. 7,500 lv. . . . ... Near water ... 6— -7,000 R. ... ... Do. 6—7,000 R. ... ... Open 12,000 R. D. ... Do. ... 11,-13,000 R. D. . • . Do. 1 4,500 R. D. ... Do. 8,5 — 10,000 R. . . . ..a On rocks 6—8,000 R. ... ... Open 11,500 R. ... ... Do. 13,000 D. . . . Do. ! 8,500 R. ... ... Do. ... 14,500 ... D. r 572? HIMALAYAN DISTRICTS \ List of Kumoan [Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. -M ■ F— 4 "rt O O i-4 tortuosum, Aids?). ... V rar. tibetanum 47 ii. 1 r 2 Pk. August ... Plains of Guge, Bp.- 48 H. 1! * August . . . Do. Glivierii, Jaub.&f Spaeh 49 H. sc. l/r 4 ... August . . . Milam, Niti ... 2- Fagopyrnm, esculentwm, Manch. ... H. 2'— 3' Pk. July Tola, &c. cymosum, Mei s n. ... ... H. 3' Pk. August ... Chaur, Almora, rotundatum, Bab. ... ... H. 2 A— S' Pk. July Tola, &c.. XCV. — ARISTOLQ- CHI AGILE. - 1. Aristolochia- saccata, Wall. • • « S. sc. co I i — j o Pr. E. May Naini Tal,Ma- XCVI.— PIP ERA- dhari Pass. CEAL l. Peperomia. reflexa, L. ... 1 H. 2" February, Sarju river. Binsar. Heyneana, Mlq. 2 ... ... ... • • • 2. Piper- longum,/,. II. t t » ... The Bhabar ... XCVII.-LAURI- NEAL 1, Cinnamomran. Tamala, Nees. » • • S. 10'— 12' Wh. May Bagesar valley, 2 Maciiilus. odoratissimus, Nees. 1 Tr. 20' — 30' Gr. Y. March Outer hills, See., Tar. 2 Tr. 40' Gr. Y. March Do. Sar j u river. 3. Plicebe- lanceolata, Nees. 1 Tr. 40'— 50' May Baisani pallida, Nees. 2 | Tr. I 20'— 30' Wh. j May ...j Jak Pass OF THE NORTH-WESTERN PROVINCES 573 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks. r A >> P Open 15,500 ... l ... | T. Do. 15,000 • • • T. Cultivated 6—11,500 R. D. • • • = Polygonum No. 29 in Herb. S. and W . Open 6—7,000 R. ... i •• = Polygonum No. 30 in Herb. S. and W. Cultivated 7—11,500 R. D. = Polygonum No. 31 in Herb. S. and W. Forest 6,5—8,000 R. ... • • • Trees & rocks. 3—6,000 R. ... i« i Forest 1 1—2,400 I R. Do, 3—4,500 R. ... Ml = C. albifiorum in Herb. S. and W. Do. 1—4,500 | R. Do. 4—6,500 1 R. Do. 4,500 E. Do. .1 5,000 R. Ml 574 hima'layan districts List oj Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. H eight of plant. Colour of flower. Time of flowering. £ *03 o o Hi ' 4. Litsea- consimilis, Nees. Sh. O [ o Wh. March Naini Tal lanuginosa, Nees. .. ... ... ... • • • ... ? 5 Tetranthera, tomer.tosa, Roab. I Kosi river monopetala, Liuxb. . . . 2 ... . . . March . . Outer hills, Sri- 6 Daphnidium. pulcherrimum, Nees, 1 April nagar. Naini Tal, Biu- bifariutn, Nees. 2 Tr. 25'— 30' May fear. Satrali valley, sp. 3 ... ... ... May Binsar XCVIII.— THYME- LACEYE. 1. Daphne. papyracea, Wall. I Sh. 3'— 4' Wh. June Naini Tal, Bin- olcoides, L . 2 Sh. 4'— 5' w: y. June sar, &c. Jtlam 2 Wikstraemia- virgata, Mtisn. Sh. 6' Wh. J tine Naini Tal, &c. 3 Stellera- concinna, Edgew . • •• H. 1"— 1*' Pk. June Bampa XCIX. — EL^EAGNA- CEAE. 1. Hippophae. rhamnoides, L. 1 Sh. 1' • • • ... VI i lam, plains salicifolia, Don. 2 T. 1 5' — 20' • « J of Guge Jwali, Gori ri- 2. Elaeagnns. umbellata, Tliunb. ... 1,2 S. T, 3'— 20' ipril ... i ver. Umora, Naini latifolia, L. 3 T. • • » HI I Tal. iota Dun ... OF THE NORTH-WESTERN PROVINCES 575 Plants — (continued). 6 o O o & CS Hima- laya. qq O w fl O *4J ^3 G O O Elevation in fee the sea. E • rH c3 Ph Q 1 Tibet. i Remarks. Forest « 6—7,000 R. = Telrndenia in Herb. S. and W. R. • • • = Daphnidium No 4 in Herb. S. & Do. .1,600 R. • • W. Do. 1, 5—6,000 R. . '<• • • • Do. 7,000 R. • •• ... Do. 5,000 R. ... e*4 l Do. 8,000 R. Woods 6—9,000 R. Ill *5 ... Open 8,500 ... D. ... Woods ••• * 6—10,000 R. D. Open ••• 1 1 ,000 ... D. ... = rasserina in Herb. S. & W. Do. 12—15,000 D. T. Forest by wa- 6,5—9,000 R. ... • ir ter. Open 5—7,000 R. ... ... Forest 2,000 R. . . . • • 576 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. C.-LORANTHA- CEiE. 1. Loranthus. longiflorus, Desr. ... 1 Sh. p. 3'— 4' Sc. March ... Bhabar cordifolius, Wall, ... 2, 3 Sh. p, 4'— 5' Br. R. March Outer hills .. puiverulentus, Wall. 4 Sh. p. 3' — 4 ' Y. Gr. March ... Bhabar, Bage- vestitus, Wall. 5 Sh. p. 2'— 3' R. May sar. Gangoli, Naini- ligustrinus, Wall. ... 6 Sh. p. 2'— 3' Sc. May ... Tal Bagesar ,. sp. 7 Sh. ? ... ... ... Baisani ... 2 Viscum. attenuatum, DC. ... 1 Sh. p. 1 ' — 2' June Bhabar, Gan- album, L, 2 Sh. p. 1'— 2’ ... May goli. Common articulatum, Burm. ,, 3 Sh. p. 4"— 6" ... May Gagar &c sp. ... 4 Sh. p. 1" ... ... ? CL— SANTALA- CEiE 1. Thesium. multicaule, Ledeb. ... ... H. 6" Wh. July Binsar, Niti ... 2. Osyris- arborea, Wall. ,,, Sh. 5'— 8' • • . March ... Kilimat, &c. ... CII. — EUPHORBIA- CEL®.. 1. Euphorbia- pilulifera, L. 1 H. 3" — '12" Wh. Do. ... Kaladhungi ... indica, Lam. 2 H. i' — 14' Pk. August ... Sar ju river ... Stracheyi, Boiss 5, 18 H. 3" « • • Do. ... Barjikang Pass, Bp. 6 H. 6" ,,, Do. ... Karnali river, sp. (E. procera, Bieb ?) 7 H. ? Laptel. ? sp. 8 H. i r — ... June Singjari cognata, Boiss. 9, 10 H. i'— ir • . . March ... Kalimat, Na- nepalensis, Boiss 11, 13 14 H. i' Do. ... mik Almora Maddeni, Boiss. 15 H. 4' ... Do. ... Naini Tal Bp. 16 H. 8" — i" ... June Rarnni .1 OP fHE NORTH-WESTERN PROVINCES 577 Plants — (continued) . ci o © > o ,5 c3 CD Himd- laya. o CO d o ■+» d o O Elevation in fe the sea. Rainy. Dry. Tibet. f Qnultnus 1—2,500 R. On dalbergia ... 4—5,000 E. ... ... On trees 1—3,000 R. • *« »*• On quercus ... 6—7,000 R. ... On trees ... 3,000 R. • . . ... ? 4,000 R. • . . ... On trees 1—5,500 R. • • • ... On pyrns and 3—7,500 R. ... ... ulmus. On quercus ... 6—7,000 R. . . . ... ? ? R. »M Open ••• 6—11,500 ... D. ... Do. ••• 4—6,000 R. ... ... Do. ••• 1,000 R. . . » Do. 4—5,000 R. ... ... Do. 13,000 R. ... T. Do. ••• 15—16,000 • •• ... Do. ••• t • « it! ... ... 9—10,000 ... ... Do. ... 6—8,000 R. ... ... Do. ••• 5_6,000 R. ... ... Do. 7,500 ... ... Do. 9,000 • * • . o . ... Remarks. 578 HIMALAYAN DISTRICTS List of Kumaon Name, Herbarium number (Strachey aud Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. Bp. 37 H. 4"— 6" July Rimkim Bp .— 19 H. 1" ... Juiy Raj -hot i, Bom- nras. sp. 20 II. 1" a . . May Champ w a Royleana, Boiss. * Sh. 10' ... March ... Sarju river & c., 2. Sarcococca- Baligna, Mull. ... Sh. 4' ... April Naini Tal 3- Buxus- Bempervirens, L. ... Tr. 20' ... July Ramni, Bagd- war. 4- Bridelia. stipularis, Bl. 1 Sh. 0 • 0 a a a a a a Bhabar retusa, Spreng. 2 Tr. 25' ri* ... Sarju river ... 5- Andrachne. cordifolia, Mull. 6- Phyllanthus- Sh. 6'— 8' . • M February, Iiamganga ri- ver. Urinaria, L. 1 H. 3"— 6" July Aim ora Niruri, L. ... 2 H. V a«« September, Bagesar reticulatus, Foie. ... Sh. 10' W. Gr. August ... Mohargari Emblica, L. • • • Tr. 15' ... March ... Outer hills, Sar- ju river. nepalensis, Mull. ... Tr. aaa ... July Bhabar, Sarju river. BP- 5 Sh. 3'— 4' ... July Almora sp. • •• Tr. 15' ... Kota sp. ... Sh. 15'— 20' Y. May Bagesar 7 — Securinega- obovata, Mull. » • * Sh. 3'— 12' W. Gr. May Bhim Tal, Kosi valley. 8- Putranjiva- Roxburghii, Wall. ... ota Tr, ... ... 09« Bhabar 9- Daplmiphyllum. himalense a • a Tr. 30' aaa ... Gagar OF THE NORTH-WESTERN PROVINCES 579 Plants — (continued) . d <£3 o Him a - layct. o -t-3 a> o .s Remarks. § *3 a o c3 0 !> ^ 03 . >> pi • i - l c3 15 a P3 0 s Open 14,000 D. T. Do. 15,000 ... T. Do. ... 12,000 R. ... . . 1 Do. ... 2—4,000 R. . . . • * . Forest ... 7,000 R. ... Do. 8—9,000 R. ... Do. 1,000 R. • •• Do. 3,000 R. • • • 1 « • Open ... 8,600 L. ... <«< ss Leptopus cordifolius in Herb. S. and W. Wet 6,000 R. « • • * Open Do. 3,000 4,500 R. R. • •• »ac &=Fluggea No. 1 in Herb- S. and W Do- 1 — 4,600 R. ... = Bmblica officinalis in Herb. S. and W. = Bradleia ovata in Herb. S. and W. Forest 1_ 4,000 R. ... ... Open 6,000 R. » a • sac = Ph. juniperinus , Wall, in Herb. S. and W. Forest 2,000 R. • •• 099 Anisoneina in Herb. S. and W. Do. 4,000 R. • • • • O 0 — Glochidion bifarium ? in Herb. S. and W. Open 4—5,000 R. ... =iFluggea Nos. 2 and 3 in Herb. S. and W. Forest 1,000 R. • • • • «< Do# " «o 6-7,000 R. tit = Goughia in Herb. S. and W. 580 HIMALAYAN DISTRICTS List of Kumccon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 10- Antidesma- diandrum, Tulasne ... 11. Jatropha. » * 0 T. • •• im • •• Kota Dun Curcas, L. ... »•« ... ... ... Bhabar ... 12- Acalypha. calyciformis, Wight, • •• H. 1' September, Dhanpur 13- Adelia. ep. t • a Tr. 30' ... ^February, Outer hills, Sarju vadley. 14. Trewia. nudiflora, L, ... Tr. 20'— 30' Gr. Y. March . , . Bhabar 15- Mallotas. philippinensis, Mull., • it Tr. 26' ill December, Sarju river ... 16- Ricinus- communis, L. » « • Sh. Ol r—i I 00 R. ill » » i 17- Excaecaria- acerifolia, Mull. • •• Sh. 4'— 5' ... All the year. Kapkot, Gango- li. insignia, Mull. Tr. 20'— 30 Y. January ... Outer hills, Sarju river. CIII.— URTICA* CEHi, 1- Ulnius. I Tr. 40'— 60' March ... Bhabar integrifolia, Uoxb. ... parrifolia, Jacq. H Tr. 30'— 40' February, Bagesar ... Tr. , , . campestris, L 2 Tr. 30'— 40' March . . . Naini Tal var. macrophylla ... » " 2. Celtis. 3 Tr. 601 April Dwali australis, L. 2,3 Tr. 25'— 40' March ... Kota, Namik, Almora. eriocarpa, Dene. 4,5 Tr. 20' ... March Kota, Almora, &e. OF THE NORTH-WESTERN PROVINCES 581 Plants — (continued) . Conditions of soil, &c. G> > O pO & -4-3 o rO d •4-a CD Hima- laya. Elevation in fe the sea. Rainy. Dry. Tibet. Remarks. 2,000 B. ... 2—5,000 R. »•« ... 1,000 R. ... ... = Epicarpus in Herb. S. and W. 2,000 R. 500—2,000 R. 6—9,000 R. ... ... 1—5,400 R. *5 1,500 R. ... • •• 1—4,000 R. ... * * » 3—5,000 R. = F. brachycarpa, Miq., in Herb. S 3,000 R. and W. 2—5,000 R. . . . . . . 500 — 4,000 E. . . . . a r 500 4,000 E. ... ... 2,500 R. • i a ,,, 1—2,000 E. • • • • • • 1,000 E. ... ... i 2,500—3,000 R. ... ... 3,000 R. 6—7,000 R. ... ... 1,000 R. 4,000 R. R. ... ... z=F. densa, Miq., in Herb. S. & W. 6,000 R. ... a a a 1,000 R. ... ... - 584 Himalayas districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 8. Artocarpus. Lakoocha, Roxb. Tr. ... 30'. — 40' ... • . • Near Kota 9. Urtica. o parviflora, Roxb. 1, 3, 16 H. 3'— 8' ... February, July. Paton, Kota ... dioica, L. 2, 15 H. 4' • • • ? hyperborea, Jacquem., 4, 18 H. 1'— 2' ... August ... Kyungar 10. Laportea- evitata, Wall. • • • H. S' Ml July J elicit 0 * . 11. Girardinia- heterophylla, Dene. ... • • • H. 10' ... August ... Paton 12. Pilea. umbrosa, Wedd. 1 H. 1 ' — 2' July Binsar scripta, Wedd. 2 H. S’ • • • Do Gagar ... trinervis, Wight 3 H. U f Wh. August . . . Kalimundi ... 13- Lecanthus. Wightii, Wedd. ... H. 2" — S" Pk. August ... Ramganga ri- ver, Jagesar. 14- Elatostemma. obtusum, Wall. 1 lit 6" • • • June Kathi, Lahur... sessile, Wedd. • • • • ■ « • • • • • • ... . . . var. polycephalum, 2 H. 1' ... August . . . Naini Tal, Na- mik. „ cuspidatum ... 3 H. 1'— 2' ... May Lahur diversifolium, Wall.... 4 H. 6" ... August . . . Lohathal Stracheyanum, Wedd., 5 H. 8" ... June Tola, Binsar ... sp. 6 H. 4'-6' • . » February, Sarju river ... 15- Bcehmeria. platyphylla, Wedd. ... 1, 2, 3, 6 H. or S. 1'- 10' 1 1 1 May to Au- gust. Dhakuri-bina- yak, Bagesar, Sarju river, Almora. macrophylla, Don ... 4 S. 6'— 10' ... August ... Sarju river ... rugulosa, Wall. 7 Tr. 20' Wh. ... Ditto OF THE NORTH-WESTERN PROVINCES. 585 Plants — (continued). a> CJ <*3 o Him a- c3 lay a. a> 4h A o ^ Q QJ c3 > ^ O 4-» Jh P3 a N Forest 3,000 R. Open 2,5—10,000 R. Do • • • R. Do. 14—17,500 • . • Woods 7,000 R, Open . • • 4—9,000 R. Woods 5—8,000 R. Do by water, 5—7,500 R. Woods 8,700 R. Damp shade ... 4—9,000 R. Wet banks ... 7,000 R. Do. 7—8,000 Ditto 6—7,500 R. Ditto 5—6,500 R. Wetshady 4,000 R. rocks. Forest & open, 2—7,500 R. Open . . 2—4,000 R. Ditto 3—5,000 • • . D. Remarks. = Urtica No 1 . 2 in Herb". S. and W, = Urtica No. 9 in. Herb. S. and W . = Urtica, No. 1 in Herb. S. and W. =-• Urtica No. 19 in Herb. S. & W. = Urtica No. 17 in Herb. S. and W ^ =; Procris Nos. 3, 4, 8, & 9 in Herb. S. and W. = Procris No. 1 in Herb. S. & W; — Procris No. 7 in Herb. S. & W. ±= Procris No. 6 in Herb, S. and W 0 Procris No. 2 in Herb. S. & W. = Procris No. 5 in Herb. S. & W. = Urtica No. 23 in Herb. S. & W. = Urtica Nos. 4, 5 and 20 in Herb. S. and W. = Urtica No. 7 in Herb. S. & W, = Urtica No. 21 in Herb. S. & W. \ 74 586 HIMALAYAN districts List of Kumaon Name. Herbarium number (Strackey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. 1 Locality. 16- Chamabakia. cuspidata, Wedd. H. 9" Pk. August ... Mohargari, 17. Memorialis- ciliaris,- Wedd. H. 1 1 2 i«« Tungnath. Baijnath 18- Pouzolzia- ovalis, Wedd. 1 ? quinquenervis, Bl. ... 2 H. 4 r ... August . . . Alrnora 19- Villebrunia- f rutescens r Bl. Sh. lO H .1 < o Bagesar 20- Debregeasia. velutina, Wedd.. 1 Sh. 5'— 15' August ... Gori river, Sar- hypoleuca, Wedd. 2 Shi 15' March ... ju river. Ramganga ri- 21 Maoutia- Pay a, Wedd. Sh. 5'' August ... ver. Sarju valley ... 22 ■ Parietaria, debilis, Forsh. H. 1' September, Below Milam & CIV.— JFGLANDA- CEiE. 1- Juglans. regia,, L. Tr. O r ox O March ... Badarinath. Dwali 2 Engelhardtia. Colebrookiana, Lindl., 1 Tr. 30'— 40' » 1 1 March Kota, Bagesar. sp- 2 Tr. • • * ... ... ? C V. — MYRIC ACE M. 1- Myrica. sapida, Wall. T K 20'— 30' April Suring, Almo- ra. OF THE NORTH-WESTERN PROVINCES 587 Plants — (continued) . 6 & e o OQ CD > O ■§ +=> CD Hima- laya , O OQ S • r-t ■+3 • pH n3 !=3 o u ■Elevation in fe the sea. 1 a '3 95 Dry. Tibet. Remarks. Wet banks ... 6—10,000 R. ... '•4 = Urtica No. 8 in Herb. S. & W. Open 3,500 B. ... ..... Open banks . . . ? 5,000 B. ... ... = Urtica No. 24 in Herb. S. & W* = Urtica No. 10 in Herb. S. &W . Forest 3—5,000 B. ... ... = Urtica No. 22 in Herb. S. & W. Open Ditto 2, 5—5,000 3—5,000 R. R. ... ... = Urtica Nos. 12 and 13 in Herb S. and W. = Urtica No. 14 in Herb. S. & W. Banks 2—4,000 R. ... ... = Urtica No. 11 in Herb. S. & W. Open 8,500—13,000 R. D. ... Forest 4—8,500 R, ... ... Do. ? 2—5,000 ? R. R. ... ... Open .» 5—6,000 R. ... ... 588 HIMA'LAYAN DISTKICTS List of Kumaon Name. Herbarium number (Strachey and Win- ter bottom). Habit of growth. j Height of plant. Colour of flower. Time of flowering. Locality. cvi — cupuLi- FEKAL. 1. Carpinus. viminea, Wall. 1 Tr. 60* ... March Naini Tal,Bin- sar. faginea, Lindl. ... 2 Tr. 60* ... March Naini Tal, Bin- sar. 2. Corylus. Colurna, L. 3. Gtuercus- ... Tr. 60* • * * May Dwali Tongha- ri. semicarpifolia, Sm — 1 Tr. 100' ... April China, Kathi, &c. lanuginosa, Don o Tr. 40* •V April Naini Tal, Bin- sar. dilatata, Lindl. ... 3 Tr. GO' ... April Naini Tal, Bin- sar. incana, Roxb. 4 Tr. 60' ... March ... Ubique annulata, Sm. 5 Tr. 60' ... March ... Bagesar valley, 4- Castanea. fcribuloides, A. DC. ... » • « Tr. 40* ... August ... Gangoli, &c. ... 5- Betula. Bhojpattra, Wall. ... 1,2 Tr. 16'— 30' . • * May Champ wa, &c. s acuminata, Wall. ... 6- Alnus. 3,4 Tr. 40'— GO' April Binsar, Naini Tal. ncpalensis, Don Tr. 30'— 40* • • • October ... Binsar, Naini Tal. CVII.-SALIGINE2E. 1- Salix- acutifolia, Willd. 1 Sh. 12' ... Ramni, Betuli Pass elegans, Wall. 2, G, V Sh. 6'— 15' ... May, June, Naini Tal,Dug- li, NainikjNi- ti. tetrasperma, Roxb. ... 4 Tr. 25' » . < May Satrali valley, Wallichiana, Anders., 3, 11 Sh. 12' ... April Gagar OF THE NORTH-WESTERN PROVINCES 589 Plants — (continued) . Conditions of soil, &c. Elevati on in feet above the sea. Hima- laya. Tibet. Remarks. Rainy. fen P Forest • • • 7—8,000 R. Do. • • • 7,000 R. ... ... Do. • • • 7—9,000 R. ... • • • Do. • •• 7—11,500 R. • • i • i • Do • •• 7—8,000 R. hi ... Dq. • •• 6, 5—9,000 R. hi • •• Do. 4, 5—7,500 R. • • • • • • Do. • •• 3—5,000 R. t • « Do. 4—6,000 R. • •• ill Do. Ml 11—12,000 R. D. T. Do. 6—8,000 R. Hi Do. • •• 4—9,000 R. III • « • Do. III 8—10,000 1 R. ill ill Do. • • • 7—11,500 R. D. ... Open • • • 1—4,500 R. ... ■ • • Forest • •• 5—6,500 R. • •« • • • 590 HIMALAYAN DISTRICTS Name. Grisea, Wall. sclerophylla, Anders . , Lindleyana, Wall. ... furcata, Anders. CVIIL— GNETA- CEiE. 1. Ephedra. vulgaris, Rich. CIX.- CONIFER JE. 1. Cupressus- toralosa, Don 2 Jnniperns. excelsa, M. Bieb. ... recurva, Don ... var. squamata, Wallichiana,///. Sf T. communis, L. ... 3. Taxus. baccata, L. ... 4. Finns. longifolia, Roxb. ... excelsa, Wall. 5. Cedrus. Deodara, Loud. List of Kumaon Herbarium number (Strachey and Win- ter bottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. £ •H l“—4 cS o o Hi 5 Sh. 16' ... April Gagar, Sarju valley. 8, 10 Sh. 3'— 10' ... July Rimkirn, Raj- hoti. 12, 14 Sh. 2"— 2' ill June, July, Pindari, Barji- 1 kang Bass. 13 Sh. 9" — 12" May Pindari, Barji- kang Pass. • • • s. l'.— 2' ... June Pindari, Milam, Tibet. ... T. 100' ... February, Naini Tal 1 T. 20'— 30' June Milam, Malari, 2 Sh. 4' ... J une Dugli, &c. 3 Sh. 6' * •« May Pindari, Mi- lam. 4 Sh. 4' May Milam, Rim- kim. ... T. 60' ••• April Dwali, & c. 1 T. 100' • • « February, Ubique 2 T. 100' May Above Joshi- math. • • • T. 160' • •• September, 1 Jelam OF THE NORTH-WESTERN PROVINCES, 591 Plants — (continued) . Conditions of soil, &e. Elevation in feet above the sea. Himd- laya-. ■£ 5 H Remarks. >> '3 «■ Dry. Open 5 — 6,500 R. • • i Do, C 13,500 D. T. \ ( — 15,500 Do. 11 — 14,000 R. ... ... Do. 12,000 R. ... . . • Open 9 - 16,000 R. D. T. Forest 4 , 5 — 9,000 R ... Open 9 — 14,000 • • • D. T. Do. 10,500 R. ... T. , Do. in 9 — 14,000 R. D, • •• Do. 9 — 14,500 ... D. T. Forest ... o 0 © r—i 1 R. D. Open forest „ 2 — 7,500 R. ... hi • Do. •• 5 — 11,500 R. D. ill Forest 9 — 11,500 R. D. • •• • HIMALAYAN DISTRICTS? m List of Kumcion • Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 6- Abies. Webbiana, Wall. ... 2 T. 150' ... May Champta, Dwali. var. Pindrow 1 T. 150' • . . May Kathi, &e. Smithiana, Wall. CX.—HYDBOCHA' 3 T. 150' ... April, ... Above Joshi- raath. PIDEvE. 1. Hydrilla- verticillata, Rich . ... H. • •• HI • •• Bliim Tal, Nai- rn Tal. 2- Vallisneria. spiralis, L. CXI.— SCITAMI- Ml H. HI ... • •• B him Tal, Nai- rn Tal. NBAS. 1. Globba- orixensis, Roxb. ... • M H. 3' Of. HI DyariPass, Ha- walbagh. 2- Zingiber. capitatum, Roxb. 1 H. 4' Y. August .. Sarju valley ... chrysanthum, Rose . ... 2 H. 4' Y. August ... Moliargari 3 Curcuma. long - a, Wall. ... H. 1'— 2' Or. August . . . Bagesaf ... 4- Koscoea- purpurea, Sm. ... 1 H. 1'— li' Pr. May ••• Naini Tal alpina, Royle ... 2 H. 4"- 6" Pr. June Karim Pass, China. gracilis, Sm. ... 3 H. 1'— li' ... June ... Naini Tal elatior, Sm. 4 H. 2' Y. August ... Kalimundi ... 5 ■ Hedychium- coccineum, Sm. 1 H. 5' S. 0. August . . . Jagesaf spicatum, Sm. ... . . . . . • * • • var. elatum 2 H. 5' W. Pk. August ... Naini Tal densiflorum, Wall. ... 3 H. 4' W. Pk. July Near Bagesar... ellipticum, Sm. 4 H. 3' Y. August . . . Du. OF THE NORTH-WESTERN PROVINCES 593 Plants — (continued) . ■Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. • pH H Remarks. & XQ r* p— n Dry. Thick forest ... 9,5—11,000 R. IM — Do. 7,5—10,000 R. D. i.l Forest ... 6—11,000 • •• D. Ml In water ... 4—6,400 R. • • • • »•« \ . Do. ... 4,400 R. Mt Ml W oods 4—7,000 R. ? % Open 2,500 R. . o * M< Banks 3—4,500 R. • ♦ • ... Open 3—6,000 R. »«• • t • Woods 6—7,500 R. Ml Open 7—11,000 R. Ml « I • On trees 6—7,000 R. ... Ml Woods 8,600 R. • •• Open 4—6,000 R. ... ... . • • Woods 5 — 8,000 R. ... Banks 5,000 R. ... ... Open 3—4,000 R. • . • • . . 75 504 himXlayan districts List of Kumaon *4 ' © S3 — & r be S a 9 , ■+3 £ o J-l bC <4H o +3 s © ► o S3 © Jh p* o Tl Name, erbarium (Strachey : terbottom) r— i SH O +3 .bp ’© % o q3 SH O © a «r*t o W K w o H o 6- Costus. speciopus, Sni. • •• II. 3' Pr. August . . . Sarju valley .. 7- Musa. papientum, L. • • • H. 6'~~8' • . • ? Sarju and Kali CXIL— QRCHI- river. DKJE . Epiphttai.. 1. Obgronia. iridifolia, Lindl. 2 H. 4" — 6" ... . . . Bliabar,Bagesar, 2- Empnsa- paradoxa ? Lindl. 3 H. 9'f G. Y. August . . . Lohathal 3- Dienia- C ylmdrostachya,Z.i?id/ 0 , 4 H. 1' G. W. August ... Jagesar 4 Liparis- nepalensis, Lindl . 1 IJ. 8" ... July Binsar 5- Phalidota- articulata, Lindl. 17 n. 4" Pk. July Bagesar, outer ipibricata, Lindl , 16 H. i'—iy Wh. August . . . hills. Ramganga ri- ver, Sarju, 6- Ccelogyne. elata, Lindl. cristata, Lindl. 14 15 H. H. i'-i ? i' Wh. May April Sar j u river . . . Champ a wat, 7* Bolbophylhmx. &c. ujnbellatum, Lindl. ... 10 H. 4" ... ... Ramganga river 8- Cinhopetalum- Wallichii, Lindl. 11 H. 3" • . • Bagesar valley, OF THE NORTH-WESTERN PROVINCES, 59-5 Plants — (continued) . Conditions of soil. &c. Elevation in feet above' the sea. Hima- laya. Tibet. Remarks.- Rainy. R Open 2,500 R. ... ... Woods ... 3-4,000 R. ... ... \ On trees 1—3,500 R ... ... Open ... 6,000 R. ... • • • Do. 7,000 R. ... ■5 On trees 7,500 R. #•« t • • Do, 3 — 3,500 R. ,,, ... Do. 3,500 R. ... ... Do. 3,700 R. Do. 5,500 R. • * * • • • Do. • • 3,500 R. ... • • • Do. 3,700 R. ... ... ■ 596 hima'layan districts List of Kurnaon Name. Herbarium number (Strachey and Win- $erbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 9. Elia. excavata, Lindl. 12 H. 6" Wh. August . . Jagesar sp. 13 H. Qf' Gr. Y. August .. Mohargari 10- Dendrobium. denudang, Don 5 H. 3" September, Jalath sp. 6 li. 1' Or. May Jagthana, &c., sp. 7 II. . . . • > • sp.— 8 H. 6''— -8" ... • M Kamgangariver sp. 9 H. 2 r ... ... ... 11 Phajns. albus, Lindl. 18 B. 1 f 2 Wh. August . . . Bagesar valley, 12. CymMdium. giganteum, Swartz. . . . 26 H. 1 X f* 1 2 Br. R. October ... Bagesar valley, 13- Vanda. cristata, Lindl. 21 H. 9"— 12" ... Hay Bagesar, outer sp. 22 H. Ml Hay hills. Bagesar 14. Chiloschista- sp. 23 H. 0" Pk. May Below Binsar. 15. Saccolabium. guttatum, Lindl . 24 H. K Pk. Tuly ... B/igesar, outer 16- Aerides. affine, Wall. 25 H. 1" Pk. * Tuly ... hills 3habar, Bage- Tjsbrestriai,. 17. Enlophia- arupestris, Lindl. 19 H. 9" Pk. I Hay ... 1 sar. Bagesar OF THE NORTH-WESTERN PROVINCES 597 — Plants — (continued). Conditions of soil, &c. Elevation in feet above the area. Hir lay .s P3 na- il . u « Tibet. Remarks. On trees 6,000 R. Do. 4,000 R. • • • On rocks 4,700 R. On trees 4,000 R. ... ... Do. 4,000 ? R. . . . ... Do. 3,500 ? R. . .. ... Do. 4,000 ? R. • . • ••• . Do. 3,000 R. ... ... Do. 4,000 R. ... Do. 3,500 R. ... ... Do. 3,000 R. ... ... Do. mi 3,600 R. ... ... Do. 3,000 R. ... ... Do. 1—3,000 R. ... Open ... 3,500 R. • •• t ' 598 HIMA'LAYAN DISTRICTS Name, 18- Cyrtoptera- flava, Lindl. 19- Calanthe- plantaginea, Lindl. ... 20- Orchis. latifolia, L., var. ... 21- Gymnadenia. Chusua, Lindl. orchidia, Lindl. 22- Aceras- angustifolia, Lindl.... 23- Platanthera- Susann®, Lindl. obcordata, Lindl. acuminata, Lindl. ... Candida, Lindl. 24. Hemipilia. cordifolia, Lindl. ... 25- Peristylns- fallax, Lindl. goodyeroides, Lindl., 26. Herminium. gramineum, Lindl. ... congestu in, Lindl. ... List of Kumaon Herbarium number (Strachey and W in- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. •4-3 § 20 H. 2' Y. July Below Almora? 27 H. 1' Pk. May Binsar, &e. ... 28 H, 1' Pk. June Kulara, Tola. 35 H. 4" Pk. June Rogila 42 H. 1' — 2' ? August .. Naini Tal 29 H. 4"— 6" Gr. August ... Naini Tal 39 H. 2 r Wh. August ... Almora. 40 H. 6" Pk. August ... Kali mat, Jage- sar. 41 li. 6" Wh. July Almora, Naini Tal. 44 h. 9" Wh. August ... Bagesar, Loha- tlial 37 H, 5" Pk. August .. Shaidevi Peak, 32 H. 1' Gr. Y. August ... Naini Tal, Ral- am. 33 H. !'•— Gr. July Almora 31 H. 4" Gr. August ... Kalimundi ? ... 34 H. 8" Gr. August ... Tola OF THE NORTH-WESTERN PROVINCES 599 Plants — (con tinned) . Conditions of soil, &c. Elevation in feet above the area. Hima- laya. Tibet. Remarks. £ • r— 1 PS a Open 4,500 E. ... ... » Woods 7—9,000 E. ... ... Open 11,500 E. D. ... Do, 11,000 E. Woods 7—8,500 E. ... Open 5— 7,000 R. ... ... Do. 5,500 E. Do. ••• 6—7,000 E. ... ... Do. ... 5—6,000 R. • •• ... Do. 3—5,000 E. • • « ... Do. 7,000 R. ... ... Do. 7—12,000 R. * . • • •• Do. 4,000 R. ... ... Woods 8,500 ? R. Open, Wet . . 11,500 ... ... 600 hima'layan districts List of Kumaon U 1 CD rj b 0 \ Name. * /A r-- &V* 3 •d +3 £ o f-i +3 c a. f-4 a> £ o *C3 a • u o £ o S Jo r* rG +3 .2 0+3 bo O O q-i • p cj O o -«3 fH O ■ess • .-H •i bB • r— < o CD 3 c3 O S3 k w o 27 • Habenaria. plantaginea, Lindl. ... marginata, Lindl. ■■ 36 H. • 8" ... August ... Binsar .38 H. 6" Y. August . . . Almora commelynsefolia, Wall., 43 H. ir Wh. August .. Ratnganga, ri- ver intermedia, Don 45 H. Wh. August . . . Jagesar, Naini Tal. pectinata, Don 46 H. 1'— 2' Y. G. August ... Naini Tal 28- Satyrium. nepalense, Don 30 ... Ml • • • • •• 29- Cephalan- tliera- acuminata, Lindl. ... 47 H. 9" August ... Rogila, Dudu- toli cnsifolia, Rich. 48 H. 1' • •• August ... Naini Tal ... 30. Listera. sp. 49 H. ... ... ... ... 31- Epipactis. jnacrostachya, Lindl., 50 H. 1'— 4' Y. Gr. July Binsar, Naini Tal. consimiliB, Don 51 H. r— 2 ? Gr. Pr. March Kapkot, outer hillB. 32- Spiranlhes- amsena, Bicb. 52 H 6" — 9" Pk. August . . . Naini Tal 33- Zeuxine. sulcata, Lindl. 53 H. 4" Pk. February, Kota Dun 34. Goodyera. marginata, Lindl. ... 64 H. 6" Pk. August ... Gagar, Kali- mundi. 35. Cypripedium. cordigerum, Don 55 H. 4' Wh. May Pindar valley. OF THE NORTH-WESTERN PRVINCES 601 Plants — ^continued). Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Rainy. Dry. 1 Woods 7,000 R. Open • ♦ ♦ 6—7,000 R. ... Do. • •• 3 — 6,000 R. ... Do. 6,000 R. ... Open and 6—8,000 R. woods. t « • o » 4 V Woods and 11,000 R. • . • open. Woods • % • 7,000 R. • l * 7,000 R. ♦ : Woods • •• 6,6—8,000 R. • • • Open 4*4 3—5,500 R. ... Do. 9*4 6—7,000 B. ... Wet • 4 • 1,500 R. ... Open 7—8,500 R, ... Do. • • 7,000 R. ... Remarks^ 76 602: HIMALAYAN DISTRICTS List of Kumaon Name.- Herbarium number (Strachey and W in- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. CXIII.— IRIDEJE. 1. Iris. nepalensis, Don 1 Id. 2 Bl. April Almora Kumaonensis, Walt., 2 H. Bl. June Pindari, Niti... sulcata, Wall. 3 H. ] i" 1 2 Bl. July Pindar Talley, 2. Par dan thus. cliinensis, Wer. H. S'— 4' Se. June Almora CXI V.— AM ARYL- LIDEHS. 1, Curculigo, orchioides, Gcertn. ... I H. 9" Y. July Almora gracilis, Wall. 2 H. 2' —S' Y. August ... Bagesar 2 . Hypoxis- minor, Don 1 H. 3" Y. July Almora, Katlii, CXV.— DIOSCO- RIDEiE. 1. Dioscorea. deltoidea, Wall. I H. se. 15'— 20' May Naini Tal, Kap- bulbifer, L. 2 H. sc. 16' July kot. Almora glabra, Roxb. 3 H. sc. 0 1 f u> c ... July Bbabar, Bage- pentaphylla, L. 4 H. se. 10 ' ... July sar. Almora ... sagittata, Roxb. 5 II. sc. 10' . . . July Almora quiuata, Wall. 6 H. sc. s' ... August ... Lolia-thal dsemona, Roxb. 7 H. sc. 25' ... July Sarju river ... CXYI— SMI- LACEJE. 1 Smilax. elegans. Wall. 1 S. se. •v. 0 rH 1 lO Pr. May Samkhet, Naini sp. (Hook cat. No. 7), 2 S. sc. 10'— 36' Hr. May Tal. Katlii Pass vaginata, Dene. 3 S. sc. 2' ... May Naini Tal, Bin- maculata,. Roxb. 4 S. sc. 10' May sar. Almora, &c. ... sp. ovalifolia, Roxb. 5 6,7 S. sc. S. sc. 25' 25' ... July March . . . Bagesar Kota Dun OF THE NORTH-WESTERN PROVINCES, *603 Plants — (continued) . Conditions of soil, &e. Elevation in feet above the sea. laya. Tibet. a * r-t cS M | Dry. i Cultivated 3,500 R. Open. 11,5-15,500 ... D. T. Do. ••• 6,500 R. • • « . . . Da. 5—6,000 R. ... ... Do. 6,000 R. ... Woods 3—4,000 R. t • • . . . Open 5—7,000 R. • • • ... W oods 3—7,500 R. ... Open 5,500 R. ... ... Woods 1—3,000 R. ... ... Open 5,500 R. ... . . • Do. 5—6,500 Ei ... Do. 6,000 R. ... ... Woods 2,500 R. Open woods 5,5—7,500 E. ... ... Forest 8—9,000 R. ... • • . Do. 7—8,000 E. ... ... Open 4—6,500 R. ... . . • Forest 3—4,000 R. ... Do. 1—2,000 R. ... ... Remarks. 604 hima'layan districts List of Kurnaon H ' d a 1 43 5h a> SB d ^ H d •*2 .5 Name. 03 S I s o ► o 5-1 be | ft £ o s O q3 ^ +=» C c3 O 4H o o o C M >> cS £ S3 ■goQ S w — +3 ■s M £ be *E3 tn 5h d o § O o> a EH 4j> § i-i CXVII. — LILIA- CEAE. 1. Lilium- giganteum, Wall, ... H. 6' Wli. June Dwali Wallichianum, Schultz. ... H. 5' Wh. August ... Almora oxypetalum, Balter ... • t • H. 9" — 12" Gr. Y. June Pindari nepalense, Don IT. S r — 4 r Wh. June Naim Tal ... 2- Fritillaria. cirrhosa, Don ... H. 6"— -12" Gr. Y. May Champwa, Pin- macrophylla, Don ... ... H. 2'— 3' Rose. March . . . dari. Almora 3. Tulipa. Btellata, Hoolt. ... H. 6" — 18' ; Wh. Feb. Almora, &c. .., 4- Lloydia. scrotina, Reich. 1, 2 H. 3"— 6" Wh. May to Ju- Pindari Pathar- iy- kori, Bom- 5. Gagea. pras, Raj- hoti. lutea, L. • • » H. 4" Y. May Pindari 6- Iphigenia. intlica, Kill, • t t H. 9" Pr. June Almora 7- Gloriosa- superba, L. » o • H. 4'— 15' Sc. August ... Almora, Bha- Or. bar. 8- Allium. Govanianum, Wall. ... Wallicaii, Kih. ... victoriale, L. ... 1 2 3 H. H. H. 9" 1'— 2' Wh. Pk. 1 Wh. 1 June June June Sing-jari 3hma, Ralam, Binsar, Duda- toli. OF THE NORTH-WESTERN PROVINCES. Plants — (continued). 605 Conditions of soil, &c. Elevation infeet above the sea. Hin lay Pi • i— t o3 « a- 2. >> « , Tibet. Remarks. W oods 7—9,000 R. • • i Open 4—6,000 R. ... ... Do. 11—12,500 R. • • • . . . = Fritillaria sp. in Herb. S. & W. Woods 7,000 R. ... Open 11—12,000 R. • « • = Lilium No. 2 in Herb. S. & W. Do. 3, 5—5,000 R. ... ... = Lilium No. 2 in Herb. S. & W. Fields 3—7,000 R. ... ... Open 11—15,000 R. D. T. Open 11—12,000 R. ... ... Do. 1—6,000 R. ... ... Do. 1—5,000 R. ... • • • Wet 11,000 R. Open »• 8—12,000 R. • • 9 ... W oods . 7 — 10,000 R. 606 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). | 1 Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. sp. (No. IS Hook cat.). 4 H. 2' Wh. June Sing-jari mbens, Schrced. 5 H. 9" Pk. August . . . tRalam sp. (No. 15 Hook cat.), lineare, L. 6, 9 H. 9"— 12" R. J une, J uly, • •0 Rajhoti, Lap- tel, Tazang. var. junceum 7 H. 6"— 8" Pr. August ... Rakas Tal, ... ellipticum, Wall. ... 8 H. 9" Pk. June ... Jaliya khal, Mi- lam. schasnoprasum, L. ... 10 H. 6" ? July Plain of Tibet ? 9. Urginea. indica, Kth. t • • H. • •• • (I » • • Plains 10 Asphodelus- fistulosus, L. • « • H. Uf ... January ... Hard war ,.. 11. Asparagus. ascendens, Boxb. ... 1 S. 6" Wh • <« Outer hills ... laevissimua, Stend. ... 2 S. S'- — 4' Wh. Jnly Ramganga river filicinus, Ham. 3 s. 3'— 4' Wh. June Sing-jari, Na- milr. 12. Polyonatum. multiflorum, All. ... 1 H. 2'— 2-3 Wh. April Gagar Pass ... roseum, Led? 4 H. n W. V. July Rimkim yerticillatum, All. ... 2, 3, 6 H. 2'— 3' Wh. April to June, Naini Tal,Na- mik Kamni, Sing-jari. sibiricum, Bed. ... 5 H. S'— 4' Wh. May Bagesar valley, &c. 13. Theropogon. pallidus, Maxim. ... 14- Tovaria. • •• H. 2' Wh. May Samkhet pallida, Roxb. 2 H. 2' — S' Wh. May Dwali purpurea, Wall . Ir » 1 H. v-n Pr - i May Madhari Pass, OF THE NORTH-WESTERN PROVINCES, 607 Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks, >> .2 *3 PS Dry. Open 11,500 R. Do. • • • 12,000 It. ... ... Do. ... 14—16,000 • • • j . . . T. • •• Do. 16.500 . i* • . « • •• T. Do. • • • 10—13,000 R. D. T. Do. ••• 15,500? ... ... T. Fields 1,000 r. «•» = Scilla No. 2 in Herb. S. and W. Do. tit i 1,000 it. • ti Open ti» 3—7,000 R. Do. • •• 3—6,000 R. ... ... Woods • • * 7—9,500 it. ... Do. • it 7—7,500 R. ' Do. • •4 13,500 ... •• T. Do. IK 7—10,000 R. • •• ... Open ... 4—8,000 R. .«« • • On trees • #« 6—7,500 R. • it • •• csChloopsis No. 2 in Herb. S. & W. Woods 8—9,000 R. • ■ . • •• <= Smilacina No. 2 in Herb. S. & W. Do. 9—10,000 R. lit .it es Smilacina No. 1 in Herb. S. & W. 608 HIMALAYAN DISTRICTS List of Kumaon S H tab 5 ^ pi Js § pH CD £ .S CD Name. - M i O fH tX) 'PH <4-1 £ o cp ^ n O •r-l W ?h 03 o hCJ Ph O _Q ■*-» _Q 6 4S >• O Hiirui- l-aya. o 02 s O 43 • r-H Remarks. 8 2 o S *43 82 >4 4-S CJ o O > ^3 £ b£) .s *Jh • r— 1 ■s .SP d c» o o a "d a o HH fi a o 6-* si bufonius, L. gp. (No. 9 Hook, cat ), 8 H. 9" May Hawalbagh ... 9, 11 13 H. 3"— 10" • •• May A a- Bindari. liajho- grist. ti, Barjikang Pass. concinnus, Don ... 10 H 15" 9*6 August .. Jagesar, Naini Tal. sp. ( — No. 10 Hook. 12 H 8" lit August ... Milam, Ralain, cat..') 2- Luzula. plumosa, Wall. ... 1 II. 9" Pk. May Madhari Pass, campostris, L. 2 H. 3" Pk. May Do. epicata, DC. ... 3 H. 2" Pk. July Bopipras CXXI. — AROIDEiE. 1- Arissema- costatum, Mart. 4 H. 1'— 11' • • * May Madhtiri Pass, speciogiun, Mart. 5 H. H' • •• May Kathi consanguineuir, Schott. 6 H. 2'— 3' • • • 'June Naini Tal curvatum, Roxb , 7, 9 H. 4'— 2' # • • ■ June Bampa, Jelam, s P 8 H. r— 2 ' • . • May Kathi Jacquemontii, Bl. ... 11 H. 2' ,,, June Naini Tal, China. sp.( Wall. cat. 8920)... 12 H, Oi' — 2 July Ralam, Rilkot, erubt scons, Sch, 13 H. 2'-^-3' • t • May Kathi 2- Sauromatum- guttatum, Sch, ... 10 H, 3' • • • July ... Almora, outer 1 lulls. 3- Remusatia- Ilookeriana, Sch. 2 H. 3" June Kathi •• vivipara, Sch. ... 14 H. 1'— 2 7 ... September, Bagesar, Bhim Tal 4. Colocasia. antiquorum, Sch. 3 IT. r— 2' September, Almora, Sarju j river OF THE NORTH-WESTERN PROVINCES Plants — ( continued) . 613 o % • 1— < o GQ O t> O X2 o> CD Hi Ma- lay a. O co rt o 4-> • w* rt o a Elevation in f the sea. 1 a • r^ a hH Dry. -4-3 QJ -2 H Remarks. Open, wet . 0 . 4—6,000 R. D Do. 10,500 —15,000 li. T. Do ... 6—9,000 R. ... • •• Do. ••• 11,500 R. D. •• Open ••• 10,000 R. • «.« Do. ... 10,000 R. ... ... Do. 14,500 D. • •• Forest 7—8,000 R. »<• Open ... 6-7,500 R. •1 • •• Forest 6—7,500 R. ... Open ... 6—11,000 R. D. ... Open 6—7,500 R. ... ... Woods 8,000 R. ... ... Open ... 9—12,000 R. ... !•# Woods 6—7,500 R. . . • * * * In shade 3—5,000 R. ... On rocks 7,200 R. Woods ► 3—4,500 R. • • » • • • Cultivated .. 1—5,000 R. « » • ... 614 HIM A'LAYAN DISTRICTS List of Kumcion Name. 5. Scindapsus- decursiva, Sch. sp. 6 Typlionrum, diversifolium, Wall. 7. Gonatantlms. sarmentosus, Rlotsch ? CXXII-— TYPHA- CE2E. 1 Typha. elephantina, Roxb. .. CXXIII— LEMNA- ce^:. 1. Lenina- polyrhiza, L. CXXIV. -NAIA- DEJE. 1. Triglochin- palustre, L. maritimum, L. 2 - Potamogeton- natans, L. lucens, L. ruf escens, Schra d crispum, L. perfoliatum, L. sp.-— pectinatum, L. sp. sp. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 1 PI. 30' Baisani 3 H. 20' ... Sarju river, outer hills. 1 H. 6" ... July Binsar, near, Almora. 15 PI. 6"— 9" ... September, Kali-mat, Bin- sar. ... ... CO I o Ml ... Tarai ... ... ... ... • • » Almora, &c. ... 1 IP. 9" G. R. July Tisum, Rajhoti, 2 PI. 6" July Rajhoti 1 H. 9" • • • Naini Tal, &c., 2 H. 6' • • • . , . Do. 3 IP. 6" • • • • • • Rajhoti 4 H. 2' ... Below Almora, 5 H, 2' ... ... Naini Tal, Bhim Tal 0 H. 2' Above Milam, 7 PI. 6' • • • Naini Tal ... 8 PI. 1' • • • Rajhoti 9 H. 1' ... • • • Above Milam, OF THE NORTH-WESTERN PROVINCES. 615 P lants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. | Tibet. Remarks. Rainy. O On trees 2—4,000 R. • Do. 2—4,000 R. Shady banks ... 4—7,000 R. ... ... On trees. & c, ... 5 -8,000 R. ... ... Swamps 1,800 R. ... ... In water 4—6,000 R. •• •** Open., wet 15,000 T. Do. 15,000 ... ... T. In water 4—6.400 R. • •• ... Do. 6,400 R. « . • Do. 15,000 ... ... T. Do. •> 4,000 R. . • • • • • Do. .. 4—6,400 R. • it . •« Do. .. 18,000 • «« . • . D. Do. .. 6,400 R. *•« ... Do. •• 15,000 ... ... T. Do. • • . 13,000 ... T* 616 Name. CXNV • — ALISMA- CEiE. 1- Alisma. reniforme, Don CXXVI.— ERIOCA- ULEJL 1- Eriocaulon- oryzetorum, Mart. ... luzulsefolium, Mart. hexangulare, L, (quinquangulare,) ... B P ' — CXXYII.- CYPE- RACEDE. ' 1. Car ex- sruciata, Nees. Icondensata, Nees. ... filicina, Nees. var. meiogyna foliosa, Don nubigena, Don Wallichiana, Presc. ligulata, Nees. cardiolepis, Nees. ... hsematastoma, Nees. fusiformis, Nees. ... psychrophila, Nees — orbicularis, Boon. ... Moorcroftii, Pale. ... obscura, A'ees. seti ;era, Don var. fasciculata ... HIMALAYAN DISTRICTS List of Kumaon Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. ... 4 11' 1 2 Wh. June Baijnath 1 H. 12" Wh. July Hawalbagh ... 2, 5 Id. 4" V\h. July Do. 3 H. 4" Wh. July Do. 4, 6 Id. 4"— 6" Wh. July Do. (& Mad- hariP.? 10,000 ft). 7 H. 2" Wh. July Hawalbagh ... 1 3' July Shaidevi 2 ... S' ... July Almora,Binsar, &c, 3 ... 2'— 3' ... May Kathi 4 2'— 3' May ... Do., Binsar... 5 l'-H' ... August ... 1 Binsar Ralam river. 6 ... l ' — 2' March Bhabar 7 * . . 2' ... July Shaidevi 8 ... 4"— 12" ... May Narnik, Pin- dar i. 9 • * • • • • ? 1 ? 10 li' 1 2 • . • July Binsar 11 . . . 11' 1 2 • . . May Dudutoli 12 . . • 4"— 12" ... August ... Laptel • 13 ... 6"— 9" August Damchen, val- 1 leys of Tibet. 14 • • • U 5 April ... Ralam R. 16 • • • 1' • • • April ... Naini Tal 16 9" May Jagthana PaBS, 617 OF THE NORTH-WESTERN PROVINCES. Plants — (continued) . 6 «rH o c5 +3 CD Hima- laya. o 0Q o •1-1 •4-3 • r— t rt o O Elevation in f< the sea. >> •H c3 £5 Dry. Tibet. Remarks Open, wet ..* 3,500 R. ... ... Wet ••• 1—4,000 R. Do. 1—4,000 R. ... ... Do. 1—4,000 R, ... ... Do. 1_ 4,000 R. ... . • • Do. •" 1_4,000 R. • it • a a Woods 8,000 R. Do. 5—7,500 R. ... . . . « . « ... ... Open, near water. 7,500 R. a.. Open, wet 7,200 R. a a a ... Do. 75—10,500 E. ... ... Near water ... 1,500 R. a a a ... Open 7,000 R. a a • ... Do. 10—12,500 E. • •a ? ? • a • lit at Open 7,000 R. a a a Do., wet ... 10,000 R. • at • a a Do. 14—15,000 a a a att T. Do. 15—15,500 ... ... T. Do., wet 10,500 R. Ml ... Do. 6,500 R. .•# • a a Do. 8,000 R. Ml • . « 618 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. snpina, Wahl. 17 3" June Bagdwar Stracheyi, Booit. 18 ... 1' ... May Below Madhari Pass. Essenbeckii, Kill. ... 19 i • • 6" — 9" June Patlmr-kori ... gracilenta, Booit. ... 20 • • • 4" G" May Madhari Pass, Lehmanni, Drej. 21 . . . 6" -8" ♦ •A August ... Dung erostrata, Booit. 22 ... 3"- 8" ■ M August ... Barjikang Pass, Danichen. nivalis, Booit. 23 * * •' H • • • August ... Barjikang Pass, Damchen, val- leys of Tibet. cruenta, Nees. 24 ... 1' — li' Ml August ... Barjikang Pass, Damcben. var. mutica 25 • • • G"— 12" .4. August . . . Damchen coriophora, Fisch. ... 26 ... 8" August ... Balchlia Pass... 2 Trilepis- Koyleana, Nees. • •• .... 6" Ml • •• Hoti, Karnali river. 3- Elyna- sclioenoides, C.A M. • 6" • • • Ml ? 4. Hypopomin- pergracile, Ness. ... • •• 1' t • • III Almora ... 5 HypoJytrum- argenteum, Valil. ... 6- Eimibristylis- • • • • • O' 1' • •4 • •• Almora ... choetoriTiiza, Nees. ... 1 • • • 9 •• Almora complanata, Link, ... 2 9" • M Jagesar pallescens, Aees. 3 • • * 6"— 9" • ■ » oe« Almora communis, Kth. ... 4 • •• 2 f 0 0# Binsar, Jagesar, Loha-thal. 7- Isolepis. trifida, Nees. ... 1 • •• G" — 8" Ml • 01 Loha-thal, above Jalat. setacea, B. Br. 2 • •• 6" M • Near Milam. barbata, 11. Br. 3 ... 4" »•• » • • ? or THE NORTH-WESTERN PROVINCES 619 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. , Him d- laya. ■4J CD rO •pH H Remarks.. Rainy. J-i A Open, wet 8,000 R. Near water ... 8,000 R. ... ... Open 1 1 ,000 R. ,, . « . » Do . wet • • • 10,000 E. ... ... Do. 13,500 .w D. ... Do. ... 14,5 — 15,500 R. T. Do. ... 14,5—15,500 R. T. Do. . 14,5— 15., 500 R. >l> T. Do. 15,000 • • • D. T. Near water • * > 16,500 T. Open, wet e i > 15,500 m T. ? ? ... • a. Wet • IV 4,000 R. in . lay d '3 03 a- a. b Tibet. ' 1 Remarks. Wet ••• 3,5-6,000 R. • •• • •• 4,000 R. ,, In water »•« 4—4,400 R. • •• Open ••• 15 — 16,000 • • • T. Wet • »> 7,500 R. • • • • •• Dry banks c*» 4,500 R. • •• = Trichophorum No . 1 & 2 in Herb, S. & W. ■? Wet 6,000 R. ... mo 4—6,000? R ••• Ml Wet • • • 4,000 R. ... •M Open, dry • • • 5—7,000 R. Ml • •• Wet • • • 5—9,000 R. • • 1 <•• Do. • * • 4-6,000 R. ... • M Do. 4,000 R. 1 M • •• Do. Ml 3—4,000 R. . • 1 ... Do. Ml 4,000 R. ... Ml Do. 4—6,000 R / i • • • II Do. 0 • • 4,000 R. •M • •• 4,000? R. • •• ... Open 7,000 R. • •1 Do. M< 5—6,000 R. . . . . . . ... ? r. • •• ... 622 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. . Colour of flower. Time of flowering. Locality. 14- Maris cns- umbellatus, Vahl. ... 1 2 r tot Almora ... puniceus, Link. 2 1' ... tot Ho. CXXVJII. — GRAMI- NEiE. 1. Oryza. sativa, L. t ■ I Ml rot tat Almora, &c. 2 ■ Zea. Mays, L. • •I 999 tat Mt Almora, See. ... 3 Coix. lacliryma, L. • • • 4' Ml ttt Bagesar, Almo- 4- Alopecimis. fulvus, Sm. ttt III 1' tta »• a ra. ? 5 ■ Phlenm. alpinum, L. 1, 2 • •• 11' i 4 ... Ralam 6- Phalaris- minor, Retz. • •• Ml tat tat tta Sirmoria ,.. 7- Hierochloa. laxa, R. Br. • •• • 0 I 2' act Pindari : above 8. Paspalum. scrobicalatum, L. 1 Ml tat Milam. ? Roylcanum, JS’ees. ... Ml • • a e* i ttt ? fliiculine, Nees. ... Ml • • • • •• ail tat Almora ... 9. Milium. *efEusum, L. ... • • « tM ... Vladhari Pass, OF THE NORTH-WESTERN PROVINCES f>23 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hin lay a • i—4 0 3 P3 id - a. j Tibet. Open 5,500 R. Do. 5,500 R. Cultivated 1—6,000 R. ... ... Do. 1—7,000 R. ... Open, wet 1—5,000 R. ... ... Open 1—5,000 R. • • • Do. 7—11,000 R. ... ... Do. 4,000 R ... 12—13,000 R. D. ■ • • Do* m 1—5,500 R. ... • • • Do. im 5,500 R. ... * • • Do. 5,500 R. ... ... Do* ••• 8,500 R. ... 1 Remarks. 624 hima'layan districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. i Height of plant. Colour of flower. Time of flowering. Locality. 10- Digitaria- *sanguinalis ... 1 in 2' • • • Ml Almora *commutata, ISees. ... 2 Ml • •• Aim ora ... *cruciata, Nees. 3 Ml • •• • •t • •• ? 11. Panicmn. *flavidum, Retz. ... 1 • •• Ml Ml Somesar *miliaceum, L. ... 2 2'— 3' • « • • ■I Almora ... *Helopus, Trin, ... 3 • •• l' • •• Do. *vestitum, Nees. ... 4 • •• 9' • • • Do. *psilopodium, Trin .... 5 • • • 2' Ml • •• flagesar *frumentaceum, Roxb. 6 Ml • •• • •• • •• Almora 12. TJrochloa. semialata, Kih. Ml • •• ... Ml Binsar ... 13. Thysanolsena. Agrostis, Nees. ... • •• • •• 6' — 8' Ml III Ramganga ri- ver, Kota ri- ver, 14. Isachne. albens, Trin. 1 Ml ]±' 1 4 Ml • • t Girgaon murioata, Nees. ... 2 • •• 11' 1 2 • • • III Somesar, near Almora, 15. Oplismeims. $rus-Galli, Ktli. 1,2, 2' III • •• Almora, Gori valley. *undulatifolius, R. 8f 3 III 1' • •• Jagesar S., 16 Pennisetum. *triflorum, Nees. ... Ml • • • 2' III Ml Almora ... ep. ••• 1*1 Ml 1* ... Ml Jelam, Niti ... 17 Penicillaria. *spicata, Lamk. ... IM *»• • « ■ ... Ml Almora OF THE NORTH-WESTERN PROVINCES. I Plants — (continued). 625 Conditions of soil, &c. Elevation in feet above the sea. Bin lay .3 « id- le. u ft Tibet. Remarks. Open 1—5,500 R. Do. 5,500 R. ... ... lit 6,500 R. • ' • *•' X Open • • • 1—5,000 11. ... Cultivated 1—5,000 R. Open ... 5,500 it. ... • • • 5,500 R. ... 1—6,000 R. • •• Cultivated ... 1—6,500 R. • •• Open tc » 6,500 R. ... ... szCaridochloa In Herb. S. & W. • Do. 2—5,000 R. * ... Do. 6,000 R. t • • Do. ... 4—5,000 E. . . • • • • * Do. ... 1—6,000 R. ... ... Shade ... 6,000 R. ... tt* Open »•* 5,500 R. Do. • •• 9—11,000 R. ... . . . isa Gymnothrix in Herb. S &. W, Do. 5,500 R. ... ... \ 79 626 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). Habit of growth. i Height of plant. 1 Colour of flower. Time of flowering. Locality. 18- Setaria- glanca, Beauv. ... 1, 2' • •a Near Almora ... vertieillata, Benth. ... 2, • •• 2' , , , *•• Naini Tal ... ita'ica, Ktk 3, » • 0 3' • • * Almora viridis, Beauv. 19 Piptat’aerum. 4. • 01 2' • * * • • • ? i, H' , , , • •• Shelshel river, eoongarieum, ... 2, . . • hi ? saquiglume, Munro, ... 20- Lasiagrostis. mongholica, Trin. ... 21 Stipa- . . . H' ... ... Shibchilarn ... pallida, Munro • •• in U' ... i*i Plains of Tibet, 22 Aiistida. cyanant’ria, Nees. ... It* in 2' • •« in Almora 23 Sporobolus. elongatus, RBr. ... • •• ... ... hi Almora, Jtige- sar. 24 Agrostis 3/lbdn Is. 1, ... ... iii ? Koyleana, Nees. ... 2, . . • ... Almora ciliata, Nees. ... 3, 4, 2' ... ... { Ralam river ... BarjikangPass, Roylei, Trin. 25 Polypogon. 5, • ■ • ... • •• Above Namik, monspeliense L. ... 1 • t« • •I iii ... Bhabar, below Almora. Sp. <1\ fugax, frees), 2 • •• ft! ... Mt Almora 26 Calamagrostis nepalensis, Nees. 1 1 1 3' in • •• Above Jalat, Dwali. OF THE NORTH-WESTERN PBOVINCES Plants — (continued) . 627 Open Do, ... Cultivated ... Open Do. Do. Do. Do. Do. Wet Open Wet Water Open Do. Elevation in feet above the s ea. Hvmd- lay a. Tibet. Ren: arks. a • F-H c3 P3 « 1 1—4,000 K. 6,500 R. ... ... 1- 6,500 R. ... ... 6,000? R. • • • • . . 14,500 T. 14,500 ... T. 14,500 ... ... T. 15,000 ... ... T. 4—5.000 R. ,... ... = Chataria in Herb S Sc W. 5—7,500 R. ... ... — Vilfa diandra. in Herb, S & W. ? R, 5,500 R. ... • • i 11,000 > R. —1,41.500 ) 10,000 R. . • . ... 1 — 4,500 R. ... ... 5,600 R. ... ... 7, 5—9,000 R. ... ... 628 HIMALAYAN DISTRICTS List of Kumaon r f-4 \ G) r- — bi S, d -d £ •43 d' CU £ **£h o Name. erbarium Strachey a erbottom). O bfl qn 0 4-* 1 PH qn o 4-3 [S) o O C® "3* <4-i o £ O o fM a> £ o 33 o -u . 1 w ‘53 W S3 3 o 1' a H i o 36- Danthonia- kashmiriana 1 , 2 ... 1'— 2' • • • ... Milam, R&lam, Niti, near Tola. 37- Poa- tibetica, Munro. ... *pratensis, L *Koyleana, Nees. *bulbosa, L. ... *var, vivipara. * annua, L. ... *flexuosa, Wahl. var. sterilis, Bieb. ... femora 1 is, L. *serotina, Ehr , ... *alpina, L. nepalensis, Wall. ... 1 2 3 4 5 6 7 8 9 10 11 11 • •• U' ir i' 4" -6" 6"— 9" 6" 6" 1' • •• • • • « • • • • • • M Ml Ml Ml «•! Ml • •• Plains of Tibet Do. Kulhara Topidhnnga ... Do. Kulhara Pindari Milam, Jung- bwatal. Barjikang Niti Dugli Do. plains of Tibet. Binsar ... 38- Eragrostis. Brownei, Nees. elegantula, Kth. verticillata, Nees. ... amabilis, W. 8f A. ... bifaria, W 8f A. ... *megastachya, Link. nigra, Nees. 1,2, 3 4 5 5 7 8 9 111 ir i' i' 2' 2'— 3' Ml , • # • •• Sirmoria ? Hawalbagh ... Almora ... Do. Do. Above Jalat, K a 1 i m u n d i Pass. 39- Melica- micrantba, Griesb. var. insequalis. ... • • • 8' t • t • • « _ Niti 40- Kseleria. cristata, Pers. ... • » • lit H' - ... N a i n i T a 1 , Kathi. OF THE NORTH-WESTERN PROVINCES. «31 Plants — (continued) . 6 » iH o CD > o •s CD Hima- laya. «4H O GG d o T. Do. 13,500 R. . • • ... Do. 12,000 • • • D. • •• Do. 10,500 R, ... Do. 10,-15,500 R. ... T, Do. 7,000 R. • • • Do. 4,000 R. • • • 4,000 1 • • • ... Open 4,000 R. ... .. • Do. 6,000 R. 00 Do. 5,000 It. ... Do. 5,500 R. ••• »•* Woods 7,500 R. in ... Open .. 11,500 til D. • • • Do. • 6—7,500 R. ... 632 HIMA'LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 41- Dactylis glomerata, L. 42- Tripogon- * • • 3 ' Ml • ai N a i n i Tdl, Kathi, Jalat, Jhuni. filiformis, Nees. h 2 • • • 1' Ml aaa Ditto, Thakil, abore Jalat. 43- Festuca- *elatio’ - , L. ... 3 • M ... • •4 a a a Binsar sp. • • • • •• 4 ' tan a • » Ditto, Kathi, &c *pumila, Vill. 1 6" a «a aaa Valleys of Ti- bet. sp. 2 • •• 9" ... • • • Ditto ditto, Chorhoti Pass. sp • • • • •• IV 2' • •• • a • Plains of Tibet, 1 44. Bromus- giganteus, L. ... 1 • t * 4 ' Ml aaa Dwali eonfinis, Nees. 2 < • • 2V . • • aa Ralam arvensis, L. ... 3 • •• H' a a a aaa Above Jhuni, *tectorum, L. 4 1 '—iv ... ... Milam ... 45- Brachypodium. 6caberrimum, ISees. i • a I'—iy • •• aaa China, Naini Tal. 46. Dendrocala- mus. strict > £ 3 id- z. >> n Q Tibet. Remarks. Open 6—8,000 E. ... ia« Rocks open ... 7—8,700 R. Ml Ml Woods ••• 7,500 . • • 7—8,000 R. • •• = Schcenodorus No. 1 in Herb. S. & W. Open 15,000 •»« • •• T. Do. 15—16,000 • •• D. T. Do. ... 15,000 ... • •• T. = Sch O rO c3 +3 CD Hima- laya. o OQ d o • H -4-3 *73 d o O d • 1— < O d) jd GQ ci q) CD +2 r 1 w .s c3 P3 ft +» CD rO H Remarks. Forest ... 7—8,500 R. • • • Ml = Bambusa No. 1 in Herb. S. & W. Open woods ... 4,000 R. • •• • •• s £ Corn fields ... 4,000 R. ••• • •• Cultivated 1—11,500 R. D. Do. Open ... 11,500 12,5—16,000 R. D. T. — Ayr opyrum Nos 2 & 3 in Herb. S. & w. Do. 5,500 R. • « « — Agropyrum No. 6 in Herb. S. & W. Do, 5—15,000 R. D. T. Do. 5,500 R. • • • Do. .. 12,000 in D. ... Do. 15,000 tii T. Do. ••• 12—15,000 ii. D. ... Do. 14,500 Ml • • • T. Do. 14,500 •M T. Cultivated ... 1—14,000 R. D. T. Open ... 1—4,000 R. D. • •• e=IIamarthria in Herb. S. & W. 636 HIMA'LAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 56. Rottboellia. exaltata, L. •at 10' • #e aaa Hawalbagh ... 57- Mauisuris- granular is, Swartz. ... ... taa ... ill aaa Almora 58. Perotis- latifolia, Ait. ••• cal aa* 1 r. o' ... ... Below Almora, 59. Eriochrysis. Narenga, Nees ... ill id 6' a a a a a o Sarju valley ... 60. SaccEarum. Sara, Rotb. aaa "«* a 3'— 4' • a a aaa ? officinarum, L. ... tea a a a 5'— 8' a* • aaa The plains, Al- mora. 61- Imperata Koenigii, Beauv. 1,2 ... 3'— 6' aaa ... Bhabar, Almo- ra, Shaidevi, Sarju valley. 62. Pogonatkernm. polystacliyum, R.SfS. ... ... 1' ... ... Sarju river near Almora. 63- Eriantlius. yelutinus, Munro ... • aa aa* 3' aaa aa* Almora near Jalat. rufipilus, Griseb. .. 2 taa 3'— 4' 111 • aa Kami Tal, Ga- gar pass Jacquemontii, Munro 3 a aa 3'— 4' aaa aaa Above Kota, Ramganga ri- ver. *rufus, Nees 4 • • a 2' aaa a a a Below Jalat ... sp. 5 • *• 3 ' aae aaa Almora, above Jalat, 64. Eulalia- nepalensis, Trin. • • « ... 2 ' aaa • 1/ Naini Tal OF THE NORTH-WESTERN PROVINCES 637 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. l Hima- laya. 1 Tibet. Remarks. Rainy. Dry. Open o • • 1—4,500 R. • a* aaa Do. ... 1—4,500 R. ... aaa Do. 4,500 R. • • • ... Do. at* 1—3,500 R. aaa aaa =Saccharum No. 1 in Herb. S. & W ? ? R. • t* aaa = Eriantlius No. 1 in Herb. S. & W Cultivated n 1—5,000 R. • • a Open 1—7,200 R. ... ... Do. • •• 1—4,000 R. ... • a a Do. • •• 5—6,000 R. tat aaa = Pollinia No. 1 in Herb. S. & W. Woods M 7,500 R. ... • • • Open M 2,5—5,500 R. • tt aaa * Do. • • 5,000 R. tat aaa Do. • • 5—7,000 R. tat aaa Woods a • 7,500 , K - aaa tea HIMALAYAN DISTRICTS e*8 List of Kumaon Name. Herbarium number (Stracliey and Win- terbottom'). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 65. Pollinia- Lehmanni, Nees 2 2'— 3' ... Almora, near Jalat. 66- Anthistiria anathera, Nees 1 ... 2'— 3' in ... Almora, below Jalat ciliata, L.f. 3 ... 3' ... aaa Above Jalat ... 67. Androscepia gigantea, Brogn ■ • • • ... 15' • •• • •a Kota, Almora, 68. Apluda. aristata, L. 1 • • * 2'— 3' • • • Almora var. 2 ... 2'— 3' ... • aa Do. 69. Batrarotherum lanceolatum, Nees ... 1 ... 1' ... Air ora submuticum, JSees ... } 2 i r 7 plumbeum 5 2 * * * 1 • • • ... UO. ... molle, Nees 3 ... i' ... Below Almora, 70. Hologamium- nervosum, A'ees ... • • « • • • 3'— 4' • at • • • Below Almora, 71. Gymnandropo- gon. annulatum • • • » • • 2'— 3' • • • aaa Kalidhungi ... triste ... ... 4 ' • at ... Above Jalat ... 72- Anatherum. muricatum, Beauv. ... . « • ... 6'— 7’ aaa i • • Bhabar ... 73. Sorghum. muticum, Nees ... 1 4 ' . • 0 Bagesar ... halepense, Pers. 2 • • t • « • • • . • . • Bhabar vulgar e, Pers. ... 3 ... • • • « « « • • t Almora 74- Heteropogon. contortus, Nees ... 1 ... 2' . . • Almora melauocarpon ... 2 ... 4 ' ... ... Do. O'F THE NORTH-WESTERN PROVINCES G39 Plants-^- (continued) . ii • i— < o m O > o rQ c3 CD Hima- laya. HH O DQ a .0 %-a • !— 1 n3 g o Elevation infe the sea. Rainy. Dry. Tibet. Remarks. Open 5,500 R. • •• ... Do. ©•• 4—5,500 R. • •• • • • Do. •»« 7,500 R. Do. 7,500 R. ... • • • = Anthestiria No 2 in Herb. S. & W. Do. 1—5,500 R. • •• • n Do. 5,500 R. «• * • • • Do. ... 4,500 R. • •• «•* Do. 4,500 R. M • • •• Do. ••• 4,000 R. • • • Do. 4,500 R. Do* 1,000 R. • •• = Lepeocercis in Herb. S. & W. Do. ... 7,500 R. • • • • • • = Amlropoyon No. 1. in Herb. S. & W. Do* m* 1—2,000 R. «•« Do. 3,000 R. » • * Do. 1—3,000 R. • . . in Cultivated 5,000 R. • •• Ml Open ... 1—6,000 R. Do. 5,000 R. in i. • 640 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 75- Aiidrop ogon. pachnodes, Trin. S • • • 5' ... . . • Adhbadri, &c , *Iwarancusa, Roxb. 7 ... ... ... - Bhabar and low valleys. 76- Cymbopogon. distans ... ... • • % 3 r — 4' ... • • • Naini Tal Gidarba, Ham. ... ... Ml W 1 >» ... ... Kalimath, Nai- ni Tal. laniger ... 77- Chrysopogon. • •• • • • 4'— 5' s' Ill Kalapathar ... montanus, Trin. ... 7 III 3' ill Almora? ... serrulatus, Trin. 1 III 2—3 • • • Almora cceiuleus Nees 2 • • » ! 2' ... in Do. Gryllus, Trin. 3, 4, 5, »«• 3’ — 4' * • i i • • China, Binsar, Paton. villosus, Nees 6 1 •• u' J 2 in • • • Below Jalat ... 78. Garnotia. polygonoides, Wight, 79. Ischseimmi- • • • • III m ill Near Jalat speciosum, Nees It* • •• 3' in HI Almora ... var. • K . • I 2'— 2\' • •• • • • Naini Tal 80 Spodiopogon- angustifolius, Nees ... ill 2' • •I • • • Naini Tal? ... I find the following note by Mr. C. B. Clarke at the end of his MS. list unequal, I have turned over the bundles marked “Ind Or” or “ Cosmopali have been worked by Gen. Munro, some are passing through his hands, some not large residuary bundles marked “ spp. ” and in these sometimes the Strachey many other cases where the Strach. and Winterb. plant is found in a particular since the ticket was put on, and it may have been hastily sorted into the bundle very partially renamed .' — Triticum seems not to have been touched since the list Even where the genera have been thoroughly worked and written, up, it would part of Bumbusa, sp. 2., into Bambusa , part into Thamnocalumus, but it would were not cut by Strachey from the same plant. Kew, 1 1th November, 1879. The names which are not included in Mr. Clarke’s list are marked with an astc- mentioned, he did not come across in the Kew Herbarium. OF THE NORTH-WESTERN PROVINCES, 641 Plants — ('continued). * Q ® •— < O CD > o c3 4-3 CD Himd - lay a. O d . o • r4 • »— < d o O Elevation in fc the sea. jr a 03 Dry. Tibet. Remarks. Open 2-4,500 R. • •• • «o Do. 1—4.000 K. • •• Do 4— 8,000 R. ... =Androgoeon No. 2 in Herb. S. & W. Do. 6—8,000 R. • • • hi = Andropoqon No. 4 in Herb. S. & W. Do. 2,500 R. • •• ea Andropoqon No. 5 in Herb . S & W. Do. 5,500 R. »•« t= Andropoqon No. 6 in Herb. S. & W. Do. ... 5,300 R. • • • • •• Do. 5,500 R. nt Do. 6—8,700 R. • •» • • 0 Do. ••• 5,000 R. Ml » 0 0 Do. 7-000 R • t • ... =Nov. Genus near Polypogon in Herb. S. & W. Do. 5—8,000 R. • • • Do. 5,000 ? R. » « « IM Do. 6,000 R. ill of grasses of the >S and W. Herbarium. “ The above reduction of the Grasses is tan,” not any others (in general). The grasses are in various states; some yet touched, or at all events not yet written up. To many of the genera are and Winterbottom tickets remain. In this case they cannot be reduced, but in bundle (with a name outside) there is no sign that the plant has been examined merely as being “ inter affines ” From these various causes the grasses are only was made. Why I found all the Eragrostis and very little of the Poa I cannot guess take a long time to verify the species carefully ; thus Gen. Munro lias sorted nevertheless take me some time to assure myself that the two pieces of No. 2 C. B. CLARKE. risk. Amongst these are no doubt several, such as from the various causes above J. F. D. 81 642 HIMA'LAYAN districts List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. CXXX — PILICES.* 1. Gleichenia. linearis, C. B. Clarke, 2- Woodsia. til Ml 2’ — 3' • •• • •• Eamganga val- ley, &c. elongata, Hook. ... l ... 6"— 12" • M Kalimundi, Bagdwar. lanosa, Hk. 8f Baker... 2 • • • 2" • •• in Pindar i ... sp. ••• 3- Dicksonia- 3 Ml 3"— 4" Ml Pindar and above Namik. appendiculata, Wall. • • • • • • 3' III 114 Gori valley, Karim. 4- Hymenophyl- lum. exsertum, Wall. 1 4" • • • Madhari Pass, polyanthus, Swartz . ... 2 • •• 2'— 3' III • It Dwali, Namik, 5. Davallia. polypodioides, Don ... 1 III 2’ • M • •• Eamganga river. chinensis, Sioartz. ... 2 ... 1' — 2' • •• III Bagesar membranulosa, Wall. 3 Ml 9" • •• V 111 Mohargari pulchra, Don 4 Ml 11' 1 2 » •• III Eamganga river, Binsar. immersa, Wail. 5 • •• 6"— 9" • •• Ml Binsar ... 6- Cystopteris- fragilis, Bernli. hi • •• 6"— 9" • • . • •• T o p i d h u n g a, Sangcha. 7- Adiantum. Capillus- Veneris, L — i III 1' Ml » • • Jagthana *, vennstum, Don 2 • •• H' • •• in Naini Tal, See., pedatum, L. 3 ... 1' III • •1 Dwali, Sing- jar i. caudatum, L. ... 4 Ill 1'— s' i •• IM Bagesar, Phar- ka. var. rhizophorum.. 6 6"— 12" III • •• Jagthana, Bin- sar. lunulatum, Barm. 5 Ml 1' — 11' • M III S a’r j u river, Bhim-Tal. * These have been arranged as far as possible in accordance with Mr. C. B. Clarke’s OF THE NORTH-WESTERN PROVINCES 643 Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. [ Tibet. Remarks. Rainy. Dry. Open • •• S— 6,000 R. ill • •l Forest • •• 8,000 R. CM Open in 12,000 R. Ml Do. in 11—12,000 E. • •• • II Shade ••• 5—7,000 R. • •1 • • • Wet rocks 8,000 R. *• * Trees and rocks, 8—9,000 K. *•• Ml Banks • •• 2,500 E. HI • •• V % Do. 3,000 R. m • •• Do. 6,500 R. • •• • • • Trees 4,5—7,500 R. • •• Rocks Ml 6—7,000 R. • •• Do. • • • 14—15,000 • • » D. T. Rocks near wa- 3—5,000 R. hi • •• ter. Forest • • • 6—8,000 R. VII • • • Do. Ml 9—10,000 R. .•« in Banks 3—6,500 R. • • • • •• Do. ••• 4—8,000 R. • • • Do. Ml 3—4,500 R. ... Ml i recently published “ Review of the Ferns of Northern India.” 644 HIM A* LAY AN DISTRICTS ✓ List of Iiumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 8- Cheilanthes- farinosa, Kaulf. ... 1 • tt l'— 14' • •0 • •• Bagesar, Alrno- ra, &c. sp. — — M » 2 ••• 1' • •• • « • Pharka ... Bp.— ... 3 • • • 1" • • « • •• Moliargari 9- Onychium. japonicum, Kunze ••• 2 ill 2' 1 •• Ml Naini Tal &c., var. nmltisecta 1 in 14' • • • • • • Do. 10- Cryptogram- me. crispa, R.Br. ... 1 & 2 Mt 3"— 4" Mt III Champwa, Tola, Kalam, 11 Pellsea. calomelaaos, Link. ... Ml 6" • •• III Below Almora. 12- Pteris- pellucida, Presl. ... i • t • • • • • * • • • i var. stenophylla ... 1 l'— 14 ' Mt • •a Bagesar cretica, L. ... longifolia, L. ... 2 • M 2' •tc mo NainiTal,Kathi, 3 Ml 3 ' • M Ml Sarju river ... quadriaurita, Retz. ... 4, 5,6 Mt V—3’ • * » • •• Bagesar, Jalat, Pharka, Barmdeo. sp. Mt Mt 3'— 4' IM III Kathi, &c. ... Wallichiana, Agardk., • •• 4'— 6' • n 111 Bagdwar ... 13- Woodwardia. radicans, Smith ... • • • IM 6' HI • M Pyura, &c. ... 14. Asplenium- Nidus, L. ... 1 • * • 14'— 2 ' «M Ml Ramganga river. ensiforme, Wall. ... 2 « t i 14' Ml Kathi alternans Wall. 3 « • « so i III IM Bagesar, Almo- ra. septentrionale, L. ... 4 • » • 4" • • « Milam, Niti ... viride, Buds. ... 5 » • • 3"— 4" i • • Ml Pindari Trichomanes, L. 6 • « • 3"— 4" III Milam OF THE NORTH-WESTERN PROVINCES 645 Plan ts — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. ; Tibet. Remarks. Rainy. Dry. t Rocks • • • 3—7,500 R. • •• Do. *• < G,500 R. ... ... Banks 4,500 R. ... «•« Forest • •• 6—8,000 R. ... Do. • • • G— 8,000 R. On rocks • • « 10—12,000 R. ... Dry rocks • • • 4,000 R. • :>• ... = Allcsorus No. 1 in Herb. S. & W * 9 ... ••• ... • • • Forest 3,000 R. • •• Do. 8—7,000 R. t • • ... Do. • •• 2—4,000 • • • R. • •• ... Open • •• 7 — 8,000 R. ... = Allosorus No. 2 in Herb. S. & W Forest 8,000 R. . . . =sCampteria in Herb. S. & W. W et banks • •• 4—6,500 R. • •• • J« On trees • •• 2,500 R. • • • • t t Do. 8,000 R. • • . . i Banks • • 3—6,000 R. ... • • • Rocks • • 11,-12,000 • • • D. Ml Do. 12,000 R. • « • Do. • • 11,500 i • t D. • •• 64G HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Straehey and Win- terbottom). Habit of growth. 1 Height of plant. Colour of flower. Time of flowering. Locality. faleatum, Sw. ... ... ... I*'— 2' ... Cl Dwali, Naini Tal. sp. ... 7 ... 4" — 6" ... ••• Jageear laciniatum, Don ... 8 ... 10" • • • ... Jak, upper To- la. yarians, tik.Sc Grev. 9 • • * * • . ... ... Dwali ... sp. • • • . . * 2' . . . • • . Naini Tal ... Filix-foemina, Bernh., ... ... 1'— 2' ... ... Do. ... var. pectinata * * • n r • • • ? sp. ... ... • . . ... Jagesar esculentum, Presl. ... • « * . . . S'— 4' . • e ? sp. — • — ... • • i . . • S'— 4:' ... • •• Gori valley ... japonicum, 1'hunb. ... . . « ... 1 ir 1 2 ... . . . ? sp. 15- Aspidium. ... ... 2' ... Ml Kathi ... auriculatum, Sw. Ml ... • • • • •• var. lenta ... • • • 1J'— 2' Ml • •• Ramganga ri- ver. „ casspitosa ... ... ... 1' • • • • • • Sarju river ... ,, marginata ... • •• »tn H'-2' ... Dwali sp. • •• ••• 1' ... Kathi ... ilicifolium, Don ... • •• 6"— 9" Madhari Pass, aculeatum, Sw. Ml Ml **»* var. rufo-barbata ... 1 • 4 ... S' Ml Binsar sp. M« Ill C'— 12" Ml • • • Dwali, Ralam, Tola. Prescottianum, Wall., Ml 1 1 f 1 2 Ml Ralam, Milam, aculeatum, Sw. • •• Ml • 'i var. setosa !M 3'— 4' Kathi ... angulare, Willd. ? ... • • • 3' • • • III Naini Tal, Ka- rim. var.? ... 1 • • Ml 2' 1*1 ... Kaphini ... sp. ... Ml III 2' * . I Ill ? 16. NephrocLium. parasiticum, C. B. Clarke? • •• • M • •• Ml III ? var. multijuga • •• III 2'— 21' . 1 . ... Karim Sp .*”■"* ‘ Ml Ml III • •• Ill • •• ? sp. ... III HI 2' Ml «•« ? OF THE NORTH-WESTERN PROVINCES 647 Plants — (continued). Conditions of soil, &e. Q > O rO a> Himd- laya. Tibet. Remarks. Elevation in ft the sea. Rainy. Dry. Forest • - . 7—8,500 R. • •4 = Cyrtomium in Herb. S. & W. (named “ plebeium?” and ,( ruta t Banks • • • 6,000 R. J LV’ in original, probably = A. [ varians. Rocks 5 - 6.000 R. ... ... Do. 8,500 R. • • • • 44 Forest # , 7,000 R. • • « ... — Athyrium No. 1 in Herb. S &. W. Do. !«' 7,000 R. • 4* « 4 • = Athyrium Nos. 2 & 4 in Herb. S. & W. • •• R. • •4 4*‘ e= Athyrium No. 5 in Herb. S. & W. Forest 1* 6,000 R. • a# ... = Athyrium No. 3 do. • • • R ... . 4 . = Diplazium No. 1 do. Open • • • 8,000 R. *44 = Diplazium No. 2 do. . . R. IM ... s= DiplaziumTSo. 3 do. Forest • •* 7,800 R. • •• 4 4 4 c= Diplazium No. 4 do. Forest • 44 2,600 R. • 41 4 4 4 *•« .44 = Polystichum No. 1 in Herb. S. & W. Rocks • • • 4,500 R. 444 444 = Do. No. 2 do. Forest 44 • 9,000 R. • 14 = Do. No. 3 do. Do. 4 # » 7,000 R. . = Do. No. 4 do. Do. • • . 9,000 R. • 44 =s Do. No. 5 do. • • * ,,, • 4 4 = Do. No. 6 do. Do. 444 6,5—7,500 R. » 4 = Do. No. 8 do. Wet rocks ... 8—12,000 R. D. 444 = Do. No. 9 do. Open • •4 11—12,000 R. D. 4 4 4 = Do. No 10 do. • • • Forest 7,700 R. *4 4 = Do. No, 7 do. Not in Clarke’s review of N. Indian Ferns. Do. M 6—7,000 R. ♦ 44 • 1 « = Do. No. 11 in Herb. S. & W. Open • If* 10,000 R. 4 4 4 = A 1 ephrodium No. 1 in Herb. S. & W. ? R. • 4* 444 • •• Ml R. 444 4 4 C = Lastrea No. 2 in Herb. S. & W. Open 6,500 R. 444 • 4* Do. No. 1 do. #•« R. 44 4 Do. No. 3 do. • • • ... R. ... |= Do. No. 4 do. 648 hima'layan districts List of Kumaon H 1 O £ o .rH feb Name. 03 /A s|*I ~ O g 8 5 rd £ o Jh bX) 4H O +3 43 d rS Pi qn o 43 rd Jh a> £ o qq O f-4 d • >— < CD £ O qp q-< O 43 -SS S3 • r— < .Q c3 bfi • r— l 0) o o a r— 1 o3 Binsar. 19- Poly-podium- erubescens, Wall. ... I • •• 3 f • •• Ramganga ri- ver. sp. 2 » • • 1 ' — 2' m • • « ? sp. 3 ... 4"— 6" • •• 0.1 Kalimundi sp- 4 in 3' hi 001 ? argutum, Wall. • •• • • • l r — 2' • • * • . 1 Binsar ... BP- • •• •i • 1'— H Jngesar lachnopus, Wall. • • • • i • 1 r 2' * • • Naini Tal, Mo- amcenum, Wall. hargari. l'—U r Kathi proliferum, Roxb. ... 2'— 3' Bhabar, &c. ... lineatum, Colebr. • • • • • • 2'— 3' Bagesar, Phar- ka? OF THE NORTH-WESTERN PROVINCES 649 P lants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. 1 ' V Hima- laya. j Tibet. Remarks. Rainy. I th t. P Forest 8,000 R. Ml • • • = Lastrea No. 5 in Herb. S. 5c W. Open 11,500 ... D. ... = Do. No. 6 do. Do. 12,000 R. ... = Do. No. 7 do. Do. t • • 11—12,500 R. • • • e®a = Do. No. 8 do. Open banks and 4—8,000 R. • ii > • • = Do. Nos. 9 & 12 do. forest. Forest 3—4,000 R. » • i Ml = Do. No 10 do. R. ... • •• = Do. No. 11 do. Forest 8,000 R. Ml III ... Do. No. 13 do. . = Do. No. 14 do. Forest • •• 2, GOO R. ... «« = Aspidium in Herb. S. & W. • • « Forest 3—4,500 R. * • . *•« = Sagenia in Herb. S. 6s W. Do. ... 3,000 R. |M ... Trees & banks, 6, 5—8,000 R, ... ... Forest 2,5—6,000 R. ... R. 1 • • ... Forest 8,500 R. ... ... name P. pendulum in Herb. S. 6c W R. named P. angulosum Lab. in Herb. S. & W. Trees 7,000 R. • . . • « • =marginaria No. 1 in Herb. S. 6s W. Do. G,000 R. . . « • » * = Do. No. 2 do. Forest • •• 6—7,000 R. ... Ill = Do, No. 3 do. Banks 7,500 R. = Do. No. 4 do, Forest 1—2,000 R. • • • • . . s=Goniopteris in Herb. S. 6s W. Trees 3,5,— G.000 R. • . . • I I = Nephrodium JSio. 2 in Herb. 6c W. 82 650 HIMALAYAN DISTRICTS List of Kuviaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. membranaceum, Don • •• ... 3' ... • . • Below Naini Tal. hastatum, Thunb. .. » . . ... . . . var. oxyloba • • 9 * • . 1 ' ... . . . Binsar juglandifolium, Don, ... ... 2'- — 3' ... ... Sarju river, Ja- gesar. ebenipes-, Hook. » • • r.. 1'— li' ... i . . Binsar, Kali- mundi sp. III ... 6"— 9" ... ... Binsar sp.- III ... 9" . . . ... Ditto. sp. • • 9 ... 6"~8" . . . . . • Do.,Kalimundi, piopinquutn, Wall. ... . . . • . • 1 1 1 1 r 9 . . ... Binsar Rainari, Wightianum, Wall.... ... ... 9"— 12" ... . . • Jagthana lineare, 7 hunb. ... ... i'-ir . . . . . • Naini Tal, &c., sp. ... . . . 4" . . . . . • Pathar-kori, ... iStewartii,C. B • •• . . . 1'— li' • • 1 ... Binsar Clarke. ep. — — »* • 6" \ ... ... Bagesar, Jak Pass sp. ... . 9 . i' ... ... Bamari, Bage- sar. flocculosum, Don ... H'-2' • • • • . . Bagesar adnascens, Sw. ... ... 3" — 4" ... ... ? 20- Gymnogram- ma. vestita, Hook. . >9 9" ... China flavescens, fresh ... ... 9"— 12" ... ... Sirring sp. . . . ... 9" ... ... Mohargari sp.- ... ... ... 3' ... ... Ramganga ri- ver. Totta, Schlecht. ... ... V ... Jagesar sp. ... G" ... ... ? 21- Meniscium. sp. 22. Vittaria. • . • n r • . 1 ... Bagesar valley. elongata, Sto. • 9* . . • i'-ir ... £athi, Sarju valley. OF THE NORTH-WESTERN PROVINCES 651 Plants — (continued). & o o> > o ja d Him a.' lay a. 00 o 00 d o -4J • r>* d o O Elevation in fet the sea. d < c3 M A Tibet. Remarks. Trees ... 4—6,500 R. ... ... = Phjmatodes No. 1 in Herb. S. & W. Forest 6' — 7,000 ii’. in = „ No. 2 clo. Do. 4,5-7,000 R. • • • ... =s „ No. 3 do. On trees 7—9,000 R. ... ... = „ No. 4 do. Do. « «-• 7,500 R. • • « = „ No. 5 do. Do. 7,500 R. • . • • •a — ,, No. 6 do. Do. ,,, 7—8,000 R. • • • . • . = „ No. 7 do. Do. »• 4,5—7,000 R. . . . • . . = „ No. 8 do. Do. 5,000 R. • « . . . . = „ No. 9 do. Do. 6,5 8,000 R. * • • . . • = „ No. 10 do. Open 10,500 R. ... ... - = „ No. 11 do. On trees ... 7,000 it* ... ... — Pleopeltis in Herb. S. & VV. Do. 3—6,000 R. ... ... a Dtiphobolus No. I in Herb. S. 8 W. Do. ... 3,5—6,500 R. ... ... = „ No. 2 do. Do. • • 9 3,500 R. = „ No. 3 do. ..a R. « • * . . • = „ No. 4 do. On rocks 7 — 8,000 R. = Nothol tna m Herb. S. & W. Forest ... 4,000 R. ... ... — Loxogramme No. 1 in Herb. S. W. Do. 4,000 R. ... = „ No. 2 do. Do. ... 2,5 — 8,000 R. ... ... named G. caudata in Herb. S. & V On rocks ... ... 9. « ... ... = Graminitis No. 1 in Herb. S. W. • a * ? R. •«« = „ No. 2 do. F*orest a . 3,500 R. ... ... Trees • • 4,8—8,000 R. ... ... 652 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and Win- terbottom). Habit of growth. Height of plant. i Colour of flower. Time of flowering. Locality. 23. Osmunda- regalis, L. 1 • • • 2' • •• ... ? Claytoniana, L. 2 2' — 3' ... ... Above Namik, Rogila. 24- Lygodium. japonicum, Sw. 1 & 2 • •• 4' — 5' Ml ... Bagesar, Bha- bar. 25. Botrychinm. virghuanuni , Sw. 1 • • • 2" -3" ... ... Almora Lunaria, Sw. 2 ... ... Tola CXXXI.— MARSILI- ACEiE. 1. Azolla- piunata, Ham. Ml • •• • •• ... ... Satrali valley, Almora. CXXXII— LYCOPO- DlACEiE. 1. Psilotum. triquetrum, Sn. ... ... ... 6" Ml ... Gagas river 2. Lycopodium- Hamiltonii ,Spreng. ... 1 ie« 9"— 12" • M ... Sarju & Ram- ganga val- leys. setaceum, Ham. 91 ... 9"— 12" • •• ... Sarju valley, Jagthana. var. subulifolia ... 2 ... g" 12" ... . • . Do. claratum, L. ... s • • • 3'— 6' ... Madhari Pass, Dwali. 3, Selaginella. caulescens, Spring. ... 4 • . • 6" Near Bagesar... sp. 5 • •• 2" • « • Deopryag ap. ■... G ... 2" Rinde river ... radicata. Spring. ... 7 ... 6" ... Bagesar integerrima, Spring . ... 8 ... 6" ... Naini Tal, Ta- puban. semicordata, Wall. ... 9 ... i 9" ... ! Naini Tal OF THE NORTH-WESTERN PROVINCES 65 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. ■ t ! Remarks. Rainy. — Dry. 9,000? R. Open 8—10,000 R. • •• On bushes, scan- 1—4,500 R. dent. Open 5—7,000 R. , , , Do. 12,000 R. D. On water 1—5,600 R. « • • ■5 % • •• On trees • * • 4—5,000 R. ... • Do. 4—6,000 R. ... ... Do. 4—5,000 R. • • i ... Woods &open... 8 — 10,000 R. ... Shady banks ... 3,000 R. • •• • •• River banks ... 2,500 R. y ... On rocks ... 7,000 R. • • « . • • On banks 3,000 R. ••• *.« Open rocks ... 7—8,000 R. •• » • •• Damp woods ... 4-7,000 R. «•* • •• 654 HIMA'LAYAN districts List of Kumaon U 1 £ & bo Name. a a a? 3 S xi 3 4-3 £ o Jh bfl 4-3 a cZ PH U CD O 'Th q-i .s CD * o .2 « £ i-i a o g *-e H CC ■ < a M H-i HH w 1 3 H o i-i CXXXIII - EQUI- SET ACE AC 1. Equisetum. arvense, L. ... 1,3 t • • 6"— 18" . . • • . • Pindari, Rim- • lcim. palustre, L. ... ... ... ... . . • ... var. ••• 2 ... 6"— 12" ... « • . Below Almora, debile, Roxb. Naim Tal. 4,5 ... 4' ... • . • Bhabar, Naini CXXXIY. — MUSCI. Tal, Baton. 1. Braunia. sp. ••• I ... ... ... ... Rur pass 2 Ancectangmm- sestiyum ••• ... ... var. ? 2 ... ... ... ... Devi-dhura ... var. ?• curvirostrum, H.SfT. 3 4 ... ... ... ... Dwali Dwali? var. ... 5 . . • ... ... ? var. 6 . . • ... ... Below Jalat ... involutum, Hook. ... 7 1 • • • *• mi • at ? 4. Neissia. serratula, Bey. ... 8 ... • tt • • a Above Namik, 5. Khabdoweissia- fugax, Btxj. 9 ... ... • •• ... Champwa ... 6. Symblepharis- Bp. 10 ... *•• Ml Dwali ,. r 7. Disticlmm. inclinatum, Bry. 11 #•> •r • •• « . a Raj-hoti 8- Desmato&on. Laureri, Bry. 12 it* • at it* a a a ? OF THE NORTH-WESTERN PROVINCES 655 Plants — (continued). 6 o 1 1 d o Himd- . Ztn/a. <4-1 o DO d o • rH •4-i • r-4 d o O Elevation in fe the sea. 1 J* M Sm o Tibet. Remarks. Open, wet 11—13,500 R. • • • T. ... • •« • it Wet places ... 4-7,000 R. ... Open wet 1—0,000 R. ... ••• Open ground ... 10,000 R. 1 0* • •• Trees, &c., in 7,000 ii. • •• . . . forest. • • < 8,500 R. • • • 8,500 R. • •• • •• ? ? R. • a • 5,000 R. . . . • «. ? ? R. ... ... 9,000 R. tit • « 1 • •• 9,000 R. * • « • at • 01 9,000 ... ... • a • Open wet 15,000 tM T. — Didymodon inclination , Hk. ground. ? 1 ? R. ... ... = Tortula bryoides , Hk. i G56 HIM A' LAY AN DISTRICTS List of Kumaon Name. Herbarium number (Straohey and Win- terbottnm,. Habit of growth. Height of plant. ' Colour of flower. Time of flowering. Locality. 9- Tortilla- sp. 13 • • • Ml Dwali fallax, Sw. . . . ... • • # Ml i*. var. 14 • •• ... Ml (M Do. unguiculata, Hk. Sf T 15 • •• ... • • • ... ? 10- Dicranum. sp. .16 • •• ... Champwa .. 11. Didymodon. cylindricus, Bry. ■ a • . . . • •• • •• Ml • . • var. 17 • • . . . Ml ? Tortula Harv. ? 18 »•» • • • CM ... D wiili 12- Campy lopns- sp. 19 ... « • • Ml IM Devi-dhtira ... 13- Fissidens. bryoides, Hedw. 20 Ml Devi-dhura ... taxifolius, Hedw. ... • •• • • • Ml ... var. ... 21 t • • • •• . . . Do. nobilis, Griff. 22 • •• • • # ... ... Pharka 14. Atrichum. crisp urn, LPi/s. 23 • •• ... Ml • • • Bagdwar 15- Pogonatum- cirrhatum, Sw. 24 ... • M III Sarju valley ... urnigerum, Bry. ... Ml • • • • •• . . . var. crassum .. 25 • •• • it Ml Bagdwar, Sarju micrastomum, Hook., 26 • • . ... ... valley. Dwali 16* Eucalypta. sp. 27 Ml ... • • • IM ? 17- Qrthodon. serratus, Schw. 28 • •• • • • • •• • • • ? OF THE NORTH-WESTERN PROVINCES 657 Plants — (continued) . 6 • PH o CD c3 Himd- l»ya. *H 0 w 1 Va • PM PH o O Elevation infei the sea. Rainy. « Tibet. Remarks. Banks & trees, 9,000 R. m • • ■ • • ... ... ... ... 8,500 R. ... i •• ? ? R. . . . • i« IM 9,000 R. • •• Ml »«• ? R. ... ... ? Banks & trees. 9,000 R. ... ... = Weissia tenuirostris , Hk. and T. Banks 7,000 R. ■9 ... • M 7,000 R. t . • . • •• R. • « • 1 •• • » » 7,000 • t • • . » • • • 6,500 R. . . . III • • • 8,000 R. =*= Polytrichum, Hook. & T. Ml 3,500 I R. • •• . . • • it IM 3,5' — 9,000 R. ... 1 Ml 8,000 R. 1 Ml IM ? R. Ml . • • Ml ? R. • •0 Ml = Octoblepharum serratum, 83 658 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and \V in- terbottom). Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 18- Bissodon. Bp. 29 Ml *#• • tl Champwa 19- Ptychomi- trium. polyphyllum, Bry. ... SO • •• • • • ... Dwali ... 20. Schistidium- apocarpum, Bry. Ml ... ... IM var. — — 31 Ml • •1 Ml ... Do. 21- Eacomitrium- Bp. 32 « • • • * • It* » . • Katlii 22- Mielicliho- feria. sp. ... 33 • •• ... » I I ttt Pindari ... 23- Brachynie- nium. nepalense, Hook. • • • • » . . r » . . • var. 34 • • • • « • ... • •• Dwali 24. Bryum. elongatum, Hk. &c T., 35 • • • • .1 ... Do. sp.’ 36 . r. . . . • •• • •• ? sp. 37 . . . • .. . . . Jagesar sp. 38 . . ( . . . • • • ... 1 Do. Diwalii ? Bry. ... 39 • • • • •1 • . . Ml Bagdwar turbinatum ? Bry. ... 40 • •0 • •• s » . » . . ? latifolium ? Bry. 41 , , . • •• ... Ml ? sp. 42 ... HI • . . ... Barjikang versicolor, Bry. ... • • • • • • » . • 9 . » Pass. * . i rar. 43 ... ... • • . ... Saba ... giganteum, Hook. 44 Ill Near Kathi ... sp. • 45 ... « • • ... Jagesar ©F THE NORTH-WESTERN PROVINCES 659 Plants — (continued) . Conditions of soil, &c. Elevation in feet above the area. Himd- i lay a. Tibet. Remarks. Rainy. ft Banks & trees, 9,000 R. • •4 • 44 444 9*000 R. 4 4 4 = Trichostomum pdlpTii/Uum, Ilk. and \ T. R. • 44 t •■*•4 9,00® • • • ... = Grimmia, , Ilk. and T. 7,500 R. • 4 4 = Trichostomum, Hook, and T. Open ground, 1 1,000 R. •M • • • 4 4 9,000 R. * • • 44 4 «i *1 8,500 R. • •• • 44 ? R. • ■ • • • • Banks 7,500 E, ... • • 4 • •• 7,500 E. • •4 444 9,000 E • • • • •4 Open ground ... 14,000 • • » • • • T. Do. 15,00o • •• • < T. Do. 14,500 R. • •• • 44 ... Wet banks and 9,000 E. • 44 rocks. ■Banks & trees. 8,000 E. *44 4 44 7,000 E. <•4 . . . 660 HIMALAYAN DISTRICTS List of Kumaon g£ 5 ^3 a <*5 /A « ^ 3 ||S fee Name, > o M bJD 4-3 3 O o o *H O .2 s £ o L. cfl O 5? if t-i TCC O' 5 w 4^ ’r3 c3 W 4J .S 3 *s w fH 3 O » — < o O O G> a H 4-3 i-— < c3 O o 14 25- Mnium- rhyncophorum, Harv., 46 ••• Ml ••• Kathi ... sp. 47 ... • ». Ml ... ? sp. 48 ... • •• Kathi, Jalat, 26- Funaria. hygrometrica,. Hedw. • •• . • • • ♦ • ... ... Tar,- 49 ... . . . • •• ••• Kapkot ... var. 50 ... • •• III Ml Jagesar 27- Orthotriclmm- sp.— ' — 51 ... ... ... ... Dwali 28- Eartramea. patens, Sclav. ... • . . . * • var. 52 Champwa ... sp. 53 Do. faleata* Hook. .. 54 • • . Kalimundi var. ••• 55 • • • Gagar Pass ... 29- Leucodon. sp. — - 56 *•4 » » « Ml » * • Dwali, near Jalat. 30- Leptodon- sp. 57 • ii ... 1 M Jagesar 31. Pterogonium. coespitosum, Wils. ... 58 • M * ... Bagdwar 32 . decker a- sp. 59 • •• Sarju valley ... sqnarrosa, Hook. 60 Jalat crispatula, Hook. ... 61 ... Above Jalat ... pcnnata, Hedio. 62 ? dendroides, Hook. ... • . . var. 63 Kathi sp. 64 Do. acuminata ? Hook. ... 65 ? blanda? Harv. Griffithiana, Sclav, ... 66 67 Bagesar valley* Julacea, Harv. 68 • M Jagesar OF THE NORTH-WESTERN PROVINCES 661 Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. Hima- laya. Tibet. Remarks. d • rH i K b o • •• 7,000 R. • • • ? ? R. ... ... 7,000 R. ... ... « 0 9 • • • ... Banks 3.500 R. » ... ... 6,000 R. ... ... Trees 9,000 R. *•« ... • • • Banks & trees, • •• 9,000 R. ... 9,000 K. » *» 8,000 R. ... Banks wet ... 7,000 R. • •• Banks & trees, 5—8,500 R. ... — Scleroduntium secundum, Harv. « • • 6,000 R. ... *•« HI 9,000 R. ... . • • Banks 3,500 R. ... • •• 5,000 R. 7,500 R. ... ... ... ? R. ... ... • •• 6,800 R. *” 7,000 R. ? R. 3,500 R. «a« 8,500 R. = N. aurea , Griff. • • • 6,000 R. ••• ... 662 HIMALAYAN DISTRICTS List of Kumaon Name. Herbarium number (Strachey and W in- terbottom). Habit of growth. Height of plant. j . 1 Colour of flower. Time of flowering. Locality. 33. Cylindrothe- cimn. sp. 69 • •• ... ... Ml Bagesar valley, 34. Anmodon ? sp. 70 • • * Kathi sp. 71 Ml ... lit ? 35- Pilotrichum sp. 72 • M ... ... ? 36. Isotheciinn. sp. 73 Ml ... Ml ... ? 37- Pylaisxa. polyanthos, Bry. • M • II • •• IM var. 74 • •• ... ... • •• Jagesar 38- Hypnum- sp. 75 • • • • •• • • t 1.4 Sarju valley ... sp. 76 III • • • • •I Do. ... confer turn, Vicks. ... • • . • • • var. — 77 • •• ... ? plumosum ? Hook. ... 78 . . . • •• Kathi var. 79 Ml Ml . . • ... Madhari Pas'!, sp. — — — — ••• 80 • •• • •ft Ml • •• Kathi sp. 81 • »• • •• Do. ... salebrosum, Hedw. ... 82 • •• B • • • •• Do. sp 83 I •• • • • • •• ... Sarju valley & Kathi. sp. fluviatile, Sw. 84 III . . . ... • •• Samkhet ... var. 85 ... • * I Ml ... Wallichii, Hook. 86 • •• • . • • . • Pharka sp.- ■— • »• 87 • • * ... III ... Sarju valley ... sp. 88 • •1 • •• ... dwali sp. 89 III • • • ... ... Sarju valley ... macrocarpum, Schw , • « 1.. • •1 • . • var? 90 ... ) • • ... ... ] Garnik & Jalat, proliferum, L. 91 ... ... • • I 1 £athi, Naini Tal. recognitum, Hedw. ... 92 • • • • • I • IB ... I £athi OF THE NORTH-WESTERN PROVINCES 663 Plants — (continued). Conditions of soils &c. Elevation in feet above the sea. Hin lay ‘3 « d- a. >> !h ft Tibet. i Remarks. 3,500 R. • •• ... = Neckera myura, Hook. Banks & trees, 7,000 R. ... ? ? R. Ill i«i = Neckera minor ? Hcdw. ? ? R. • • • ... ? ? R. • •1 «•* • • • R. • • • • 0* 6,000 R. *«• • •• = Leshea polyanthos , Hook, and T. Banks ... 3,500 R. III = Leskea sp ? ... 3,500 R. #• • ... = Les/tea acuminata ? Hedw, Banks & trees, ’? E. • •• 7,000 R. • n 8,000 R. • • • 7,000 R. • •• ... 7,000 R. in 7,000 R. • • I m ! ~ • • • 3,5—7,000 R, • • • ... In water 5,500 R. W et banks ... 9,000 R. • • I in Bo. 6,500 R. • • • Banks 3,500 R. i • 1 Banks & trees, 8,500 R. • • • • •• Ml 3,500 R. • • • III ... • •• • • • III • • • 7—9,000 R. • • I III = H. Strongylum, Taylor. 6,500 R. • • 1 • •• • •• 6,500 R. 1*1 • •• 664 hima'layan districts List of Kumcion Name. Herbarium number (Strachey and Win- ter bottom). Habit of growth. Height of plant. o £ o O Sh 3 O o O Time of flowering. Locality. / commutatum, Hedw., • * • • • ■ Ml • • • var. ? 93 • ■ • • • • • • • • •• Raj-hoti Palustre, L i • • Bagdwar var, subsphterocar- 94 i • • • ■ • • . • • € • pum. sp. 95 ... , . . Sarju valley ... sp. 9G ? filicinum, L. 97 ... Ml • •• Gagar Pass ... 39- Leptohyme- nium. microphyllum, Schw., 98 Katlii tenue, Schw. 99 »». m in ? 40- Dicranodon- tium. longirostrum, Bry. ., 100 • •• • • • • •• ? 41. Hookeria. sp 101 • •• •H • •• Dwali ... 42- Hypoptery- gium. sp. ••» 102 « • • • •• • I I Pharka „. HEPATICAE, 1. Riccia- sp. 1 • •• m » •• in Samkhet ... sp. 2 • . . Ml • •• Do. sp. 3 » • • Ml • •• Ml Do. 2. Marchantia. sp. .. 1 • • • * • ♦ III • a t ? sp. 2 • • • • •• 0 10 • • a ? sp. 3 >•« 1 •• ... • • • Near Jalat sp.' 4 • •• • 0 0 Do. sp. ... 5 Hi III * • • ... Sarju river ... sp. G • • • • •• III ? sp. 7 • . • • •• ... Sarju river ... sp. 8 • • • Vlason sp. — — . 9 IAI III Ml ... Sarju river ... OF THE NORTH-WESTERN PROVINCES 665 Plants — (continued). d *s o O > o a> Hima- laya. <4H O m d o • rH • a a . a ? ? R. Ml a a « Do. 3,500 R. a « • Do. 5,000 R. • •• • a* Do. 3,500 R. • •• Ml 666 HIMALAYAN DISTRICTS List of Kumaon S ei A £ tS> u ^ i • C3 x-n -4-3 1 U CD * rt • !— * 5-4 O Name. Herbarium (Strachey terbottom O 5-1 bJD q-< O +3 ■ 1 w r — < o- qn o 2 be w o qn O rH D O o O £ O q-4 O -3 > a '3 P3 R. R. R. R. R. R. R. R. R. R. R. R. IH 111 • M R. R. • • • • o >» P -< ft !«• Ml • •• • •• >0* D. D. D. •i« D. CD rO Ml Ml Ml * •» Ml III • • • D. Ml • ■ • Ml • •• Ml • II Remarks. HIMA'LAYAN DISTRICTS 668 List of Kumaon n h faX3 a A £ 4-3 §

e o Pass, Madha-I 7. Urceolaria- ri Pass. calcar ea ... • tf ... • tt Shelong 8- Parmelia' melanaspis, Wahl. ... 1 • ft . . . . i . • tt Shelong pulverulenta, Ach. ... ... • . » •• • ... • • • • at var.. 2 ..r ... t • . • tt Gori river elegans, Ach. B • f . • • i Ml 1 . « Shelong oreina, Ach. ... 4 Ml in Ml • » • Do. vitellina ? Ach. 5 Ml • It Ml Do. ... calcarea ? Fries. .. 6 • •• * •• • tt . . . Do. scruposa ? Ach. 7 • • • • t • • tt . . . Do. chrysoleuca, Ach. 8 • •• tit ... • . . Do. ... b ax i col a, Ach. ... 9 i • • It. • • • Ml Do. coesia, Ach. ... 10 Ml Ml ... • tt Do. gtellaris, Ach. ... 11 t • • ■ M • tt Ml Do. speciosa, AcA. 12 Ml • • Ml • •• Gori river, Chi- Igevigata, Ach. >• 13 ... • ft • tt • tt na. China perlata, Ach. 15 . . . Ml • tt • •• Karim Pass ••• var. saccatiloba ... 14 Mi • . . ... • tt China perforata, Ach. ••• 16 • t • Ml • tt Do. tiliacea, Ach. ••• 17 • •• • • • ... Ml Do. Bcortea, Ach. 18 . • . Ml • •• • • • M;idhari Pass, caperata, Ach. .. 19 Ml ••• • •• • at China leucomela, Ach. 20 • tt ... Ml • tt Do. cirrhata, Fries. ... 21 • •• • tt * 1 1 • •• Do. 9- Sticta. pulmonacea, Ach. .. lit Ml Ml III • •• var. hypomela .. 1 • •• ... • tt • tt China retigera, Ach. 2 III Ml IM • tt Dugli herbacea, Del. ,. 3 • * 1 • •1 III ... Karim and Ka- 10. Pettidea- th'i Passes,] China. horizontal is, Ach. 1 Ml **' • • • Above Dwali... canina, Ach. 2 • M . * • IM • • • Chinar Dwali J OF THE NORTH-WESTERN PROVINCES. 669 Plants — (continued). Conditions of soil, &c. Elevation in feet above the sea. 1 Ilimd lay a. Pi 05 >> fH Pi 4-3 < V rO • r-t Remarks 1 • • • 4,700 R. r • • Earth 12,000 R. lit ... •- • • • ... Rocks 8—11,500 R. ... • •• III 13,000 « • ♦ D. • •(1 13,000 i • * D. ... in . ... ... ... 4,700 R. ... • * . 13,000 D. • •I 13,000 ... D. . • 1 13,000 D. . . « 13,000 ... D. 13,000 U. . •• 13,000 D. ... 13,000 D. .« * 13,000 tea D. • • • « • • 1 3,000 ... D. Rocks and trees, 4, 7—8,700 R. ... »•« On trees 8,700 R. . . * III 7,500 R. i ••• • • • On trees ... 8,700 R. ... Ml 8,700 R. * I « 8,700 R. • • • 8,200 It. . • * . . I 8,700 R. • • • • • . 8,700 R. • •• •I • • it 8,700 R. til « •• o«» • • « M III 8,700 R. t • i • 10,500 R. • • • « ill 7, 5—9,000 R. a • 9,000 R • • • • • • * 8—9,000 R tl •. at 670 HIMALAYAN DISTRICTS List of Kumcton Name. Herbarium number (Strachey and W in- terbottom). [ Habit of growth. Height of plant. Colour of flower. Time of flowering. Locality. 11. Solorina. saccata, Ach. ... • •• Ml • af Ml Kathi Pass ... 12. Cetraria. Straclieyi, Bab. 1 • • • • •• Near Kathi ... ambigua, Bab. 2 • •• » «a • • • ... Bompras 13. Ramalina- farinacea ? Ach. ... * • i • • • • •• • •• Pindari 14 Evernia. Stracheyi, Bab. • at • • • • • • • ai Pindari, Bom- 15- Usnea. • pras. himalayana, Bab. ... 1 • •• ... Binsar ... longissima, Ach. 2 ■>*• u< • at ... China ceratina, Ach. ... 3 • • • • • • • aa • • • Do. sp.? » • • lit Ml IM • • t Do. sp.? ... * * * •** • • « • • • ... Hot valleys ... Note.— The whole of this chapter has been edited and prepared by Mr. F„ nished by General R. Strachey. My work has been confined to seeing that the proofs.— E, T. A. OF THE NORTH-WESTERN PROVINCES. 671 Plants— (concluded). Conditions of soil, &c. CJ t> O rQ d 4-3 > R Ml 8,000 R. »•» 7,200 R. in Stones ... 16,000 • • • D. in Do. ... 11,500 R. • • • •i • Do. 11, 5—16,000 R. D. t»i Trees 7,000 R. • •• ••• t • i 8,700 R. • •« hi • • • 8,700 R, • • • 8,700 R. • • • • •» On oberonia .. . 2,000 R.. i III Duthie, Superintendent of the Botanical Gardens, Saharanpur, from the list fur- corrections made in the first proofs by Mr. Duthie were carried out in the second i CHAPTER IX. Economic Botany. contents. Arrangement of the subject. Food of the people. Analysis of the food- grains. Watson’s formula. Cultivated food-grains. Cereals. Pulses. Ama- ranths. Polygonaceae. Cultivated vegetables. Gourds. Vegetables. Condi- ments and spices. Greens. Fruits, cultivated and wild. Uncultivated products used as food. Drugs. Narcotics and spirits. Oil-seeds. Dyes and tans. Gums and Gum-resins. Fibres. Woods. The economic botany of the Himalayan districts of these provin- Arrangement of the ces > actual and potential, opens out such a subject. wide field for investigation that it would be impossible to do more than review the information that we possess. The materials are to be found scattered over numerous memoirs, articles, reports, and notes, and are as practically inaccessible to the general public as if they had never been collected. The form of this chapter will, therefore, be more that of a suggestive classified list than of a treatise which would, in the first place, be more than could be usefully prepared by one person ; and, in the second place, will come more fitly into the general review of the economic products that is about to be undertaken by the Department of Agri- culture in these provinces . 1 For the more orderly arrangement of our subject, we shall divide the useful products of the vegetable kingdom into the following classes: — I . — Vegetable substances used as food by men and animals. a. Cultivated food-grains. 1). Cultivated vegetables. c. Spices and condiments. d. Greens. e. Fruits, cultivated and wild. /. Uncultivated products used as food. II . — Vegetable substances used in pharmacy. a. Drugs. | b. Narcotics and spirits. 1 Progress has been made in this direction by tire publication of my “ Notes on the Economic Products of the North-Western Provinces.” Part I . on ‘ Gums and gum-resins Part II., on ‘ Economic Mineralogy Part III, issued by the Department of Agriculture, contains, ‘ Tans and Dyes” Part IV./‘ Cultivat- ed food-grains’ ; Part V., ‘Gourds: vegetables: condiments and uncultivated products used as food. The remainder are under preparation and will comprise ‘ Drugs,’ ‘ Fibres,’ ‘Woods, and ‘ Narcotics.’ * fst a; ‘A' OF THE NORTH-WESTERN PROVINCES. 673 I a. b. a. b. III . — Vegetable substances used in manufactures. Oil-seeds. i c. Gums and gum-resins. Tans and dyes. I d. Fibres. e. Woods. IV. — Special subjects. Forest history. I c. Rhea experiments. Tea cultivation. I d. Sericulture. e. Miscellaneous. . — Vegetable substances used as food by men and animals. The population of the Himalayan districts is essentially Hindu, and consequently the vegetable kingdom Food of the peop e. affords most of the substances used as food by the people. Few of the hill-men, even amongst those who have had much communication with the plains, have any prejudice in regard to eating animal food. The majority partake of the flesh of kids, short-tailed sheep, and young male buffaloes at festivals and marriages, and whenever sacrifices are offered to the consort of Siva. With but few exceptions all eat the flesh of deer, pheasants, and partridges, but not of jungle fowl ; whilst in Garhwal, all, includ- ing Brahmans, eat the flesh of the wild pig. The servile classes (Dorns, &c.) eat meat of all kinds whenever they can get it, even of animals killed by wild beasts or which have died from disease, and in their habits differ little from the Chamars of the plains. Uncul- tivated products are used as food chiefly by the inhabitants of the jungly tract lying along the foot of the hills and along the banks of the Kali, and, in times of scarcity, by the people of the upper Pattis. At all times, however, the young leaves of nettles, of several species of ferns, sorrel, and the like, are used- as a spinach by all classes. An examination of the list of cultivated products use das food will show that the greater portionbelong to the great natural orders Graminece or grasses, Leguminosce or pulses, and Cucurbitacece or gourds. The two former afford life-supporting substances abounding in albuminous matters and those capable of repairing tissues accompanied with starch, gum, and sugar in such proportion as to support respiration and promote animal heat. They also provide the inorganic substances necessary to keep the circulation in a healthy state and to renew the solid frame-work of our bodies. Of these two orders the Graminece or grasses is the more important, containing as it does wheat, barley, rice, millets, 85 674 HIMALAYAN DISTRICTS' maize, and sugarcane, which enter so largely into the food-resources not only of this country hut of every country in the universe. To the Leguminosce belong peas, beans, lentils, and gram. The gourds and cultivated vegetables are eaten more as a relish or to eke out a scanty supply of food-grain than as a sole food resource, and then only at certain seasons when their abundance and cheapness render them a favourite. The same may be said of fruits, culti- vated and wild, and of the wild plants collected for food. There are three forms of nitrogenous substances common to both Analysis of the food- animal and vegetable organizations distin- S rains - guished by the names albumen, fibrine, and caseine ; and it has been found that, when introduced into a living organism, each of these is capable of being converted into the other? The principal ingredients of the blood of animals is found to be fibrine and albumen, and these substances contain, besides the carbon, hydro- gen, and oxygen found in farinaceous products, such as the cereals, nitrogen, sulphur, and phosphorus, which abound in the pulses. These elements are also found in all parts of the animal organism except water and fat. It follows, therefore, that nutritious food must possess both albuminous and nitrogenous ingredients. The former are composed of carbon, hydrogen, and oxygen; the hydrogen and oxygen being in proportion to form water, thus leaving the carbon wholly unoxidised ; or if we suppose the oxygen to be divided between the carbon and hydrogen, a surplus of carbon and hydrogen that is unoxidised remains. We are now speaking of what takes place after the food has been taken into the body and there submit- ted to assimilation. From the moment an animal is born until it dies oxygen is taken into its body through the skin and lungs, and given out again by the same channels in the form of compounds of carbon and hydrogen, or, in other words, as the vapour of water and carbonic acid. The latter is derived from the food eaten ; for, when an animal is unable to take food, so long as it lives, it continues to inspire oxygen and give out compounds of carbon and hydrogen, which it obtains from the waste of the tissuesof its own body. In fact death ensues from the action of the inspired oxygen, on account of its powerful affinity for carbon and hydrogen. When the animal has no longer superfluous carbon and hydrogen capable of combining i Based on the researches of Professor Mayer, OF THE NORTH-WESTERN PROVINCES. €75 wit'll oxygen, it seizes on the carbon and. hydrogen of the animal s ewn body ; and, in the first instance, on the fat, which is almost all carbon and hydrogen, in order to satisfy the oxygen absorbed in the circulation, which afterwards goes off as carbonic acid in water. From the above it will be seen that food containing a surplus of carbon and hydrogen is necessary to an animal in order to support respiration without destroying its structure. But, besides defending the animal tissues and other parts from the action of oxygen, food maintains animal heat ; for, whenever oxygen combines with a com- bustible, heat is developed ; and that this does not depend on outward influences is shown by the fact that the heat of the body is the same in the tropics and in cold countries. There are thus two great uses to which food is adapted by its composition — the nitrogenous to renew the blood and the noil-nitro- genous to support respiration and maintain animal heat. But besides these there are other ingredients in food, the salts, such as iron, phosphate of lime, chloride of sodium with other salts of sodi- um, potash and magnesia, which occur also in the blood and bones, nails and hair. The following analyses of the principal cultivated food-grains are intended to show separately the quantity of these three principal ingredients present in each class of grain, and in doing so its comparative value as a food resource. A study of the tables will corroborate in most cases the empirical verdict on the value of each grain formed by the natives of these provinces, and give a scientific basis to their estimates, which would otherwise appear to be based on arbitrary data arising from their habits of life. The first series refer to the cereals, the second to the pulses, and the third to other vegetable products. We shall first, however, give Liebig’s analysis of the three forms of nitrogenous substances found in animal and vegetable organisms for comparative purposes, and then Professor Mayer’s ultimate analysis of the various food-grains. Analysis of Albumen. Caseine. Fibrine. Sulphur ... ... ... ••• 1-30 0*9 1*0 Carbon ... ... ... ... 53*50 43*6 53*2 Nitrogen 15*50 15*8 17*2 Hydrogen ... 7*16 7-1 6*9 Oxygen ... ... ... 22*54 22*6 21*7 100*00 100*00 100 00 676 HIMALAYAN DISTRICTS Results of analysis A. These are arranged in percentages so as to show the composition of the different substances existing in each vegetable product examined with their separate uses as life-sustaining compounds. Names of products. Nitro- genous ingredi- ents. Non- nitro- genous ingredi- ents. Inorga- nic in- gredi- ents. Cereals. Triticum vulgare, wheat, gehUn , B. 14-45 83"I5 2-40 Ditto, H. Ml 19-15 79-77 0-70 Hordeum hexasticlwn , barley, jao, H. IN .14-72 84-80 2-84 Oryza sativa, rice, d/idn, M. Ml • •• 9-08 89-08 0‘47 Ditto, H. ... • • » 7-40 91-60 0-36 Zea Mays , maize, makai , II. ... •91 • •• 14-66 84-52 1-92 ••• • •• • • • • • • 10-70 87-00 2-30 Do., H. Ml Ml 11-92 85*65 1-33 Peniciltaria spicata , millet, bdjra, M. • « • 13-92 83-27 0-73 Eleusine Corocana, mandua , M. III 18-12 80-25 1-03 Avena saliva, oats, jai, B. • 0* • 1 1 13-93 82-07 4-00 Ditto, H. ... • •• Ml 15-24 86-05 3-26 Sorghum vulgare, jodr, M. ... t » • • •• 15-53 83-67 1-26 Pulses. JErvum Lens, lentils, masitr, II. • •• 30-46 65-06 2-60 Pisum sativum, peas, mattar, B. IN Ml 26-52 70-38 3-10 Ditto, H. III • •1 28-02 67-31 3-18 Phaseolus vulgaris , bean, sent, H. • •• Ml 28-64 66-70 4-38 Other vegetable products. Solanum tuberosum, potato, alu, B. • •• Ml 9-50 86-50 4-00 Ditto, H. ... Ml III 9'96 86-36 3-61 Brassica Rapa, turnip, shalgam , B. IN in 10-70 81-70 7-60 Ditto, H. M9 Ml 12-62 81-33 7-02 Beta vulgaris, beet, chauhandar , B. • •• III 10-70 83-00 5-30 Ditto, H, • •0 »• 15-50 73-18 6 43 Daucus Carota, carrot, gajar , H. Ml ••1 10-66 84-59 5-77 Brassica Napus, colza, H. Hi Ml 9-24 90-32 4-01 Mag., November, 1816, p. 365. OF THE NORTH-WESTERN FROYINCES 677 Results of analysis B. Here the arrangement is in percentages so as to show the ultimate composition of each product examined, without reference to the different compounds existing in them or their uses as life- sustaining compounds : — Names of products. Carbon. Hydrogen. Oxygen. Nitrogen. Asli. Cereals. Trilicum vulgare, wheat, B. « • • 46-10 5-10 43 50 2.30 2:40 Ditto, IT. ... ... • • • 45‘69 6-76 43 23 3-00 0-70 Hvrdeum hexastichon, barley, H. ... 45-50 6 89 44.68 2 34 2-84 Oryza saliva, rice, M. ... ... 44-87 5-85 46-10 1-43 0-47 Ditto, H. 44-61 6-53 46-62 1-16 0-36 Zea Mays, maize, H. ... • • • 45-04 6 60 44-62 214 0-86 Rye, B. ... 46-20 5-60 44-20 1.70 2-30 Do., H ... ... ... • . . 44-37 6 65 44 55 1 87 1-33 Fenicillaria spicata, bajra, M. 44-48 6 43 44-09 2-19 0 73 Eleusine Corucana, mandaa, M. ... ... 48-64 6-10 43-77 2-86 1-03 Avena sativa, oats, B. ... ... • 0 . 50 70 6-40 36-70 2-20 4-00 Ditto, IT. ... 46-50 6 64 ‘ 45-59 2 39 3 26 Sorghum vufgare, jodr, M. ... 45-69 6-24 44-82 2-45 1-26 Pulses. Ervum Lens, lentils, H... 45*35 6-75 38-50 4-77 2-60 Visum sativum, peas, B. • •• 46-50 6-20 40 00 4-20 3-20 Ditto, H.. 45-12 6-73 38.92 4-42 3-18 Fhaseolus vulgaris, beans, H. ... ... 45-07 6-63 39 03 4-47 4-38 Other vegetable products. Solarium tuberosum, potato, B. ... ... 44-00 5'80 44-70 1-50 4-00 Ditto, H. ••• ••• • • • 43-86 6-00 44-79 1-56 3-61 Brassica Rapa, turnip, B. ••• 42-90 5-50 42-30 1-70 7-60 Ditto, H* . .. ••• HI 43-19 5-68 42-96 1-98 7-02 Beta vulgaris , beet, B.... • . e 42-80 5-80 43-40 1-70 6-30 Ditto, H, ... ... ... 40-99 5-72 39-37 2-43 6-43 Baucus Carota, carrot, H. ... ... 43-34 6 22 43-90 1-67 5-77 Brassica Napus, colza, H. 45-32 6*01 46-68 1-45 4-01 G78 HIMALAYAN DISTRICTS Tlie results of the preceding tables are supported by a further examination of the pulses grown in these provinces. The following table gives the average result of an analysis of several samples of each product taken from ‘ Panjab Products,’ 1., 243 : — Names of products. Nitrogenous ingredients. Carbonaceous or starchy ingredients. Fatty or oily matter. In 100 parts : varies in specimens from different parts of India. Cicer ariet.inum, gram, channa ] 8-05 21-23 60-11 63-62 4-11 4-95 Ervum Levs , lentils, masur ... ,.. 24-57 26-18 59-34 59-96 1-00 1-92 Lathyrus sutivus , kisari (Calcutta speci- 31-50 54-26 ... 0-95 • men). Pi sum sativum, yea,*, inattar ... Ph iseulus aconitifulius, moth (Calcutta spe- 21-80 25-20 58-38 62-19 1-10 1-12 23-80 ... 60-78 ... 0-64 • • • cimen). Phnseolus Munqo,mung ... ... 23-54 24-70 59-38 60-36 1-11 1-48 P. var. radiatus , urd (Bombay speci- 22-48 • • • 62-15 1-46 • • • men). Vigna Catjang, lohiya (Bombay speci- 24-00 59-02 ... 1-41 men). Dolichos bifjnrus, qnliat ... 23-03 23-47 61-02 61-85 0-76 0-87 ,, Liblab , shlmi ... 22*45 24-55 60-52 60-81 0-81 2-15 Cajanus indicus, arhar ... Glycine Snja, bhat 19-83 20-38 61-90 64-32 1-32 1-86 37-74 41-54 29-54 31-08 12-31 18-90 Cyamopsis psoralioides, gawar (Puna spe- 29-80 ... 53-89 ... 1-40 • •• cimen). From an inspection of the preceding tables it will be seen that the pulses abound in nitrogenous elements so efficient in repairing the tissues, and next to them the cereals. A comparison with the analysis of the constituents of the blood will show that the composi- tion of both is almost identical, and will also explain why experience has taught the natives of these provinces to mix together in their food, in certain proportions, cereals and pulses, the one supplying what the other is wanting in. Thus the flour of gram and peas is mixed with that of the cereals and especially with millet flour. Pulse bread is very seldom eaten alone, and then only locally and for some special reason. The millets and the coarser pulses form the staple food of the hill population. Amongst the former the manclua, janghora, koni, china , and mana, and amongst the latter the gahat , bhat , and rains. The mandwa is either made into bread or into a porridge called bari , and the china and koni are also made into bread or boiled whole and OF THE NORTH-WESTERN PROVINCES. 679 eaten as rice. When travelling, the lower classes live chiefly on satu, the meal of parched barley, which only requires the addition of a little water to prepare it for eating. The following remarks ot Traill still hold good : — « Rice forms the favourite food of all those who can afford to pur- chase it. Wheat is only in partial consumption, chiefly on occasions of entertainments at marriages, &c., when the peculiar scruples of Hindus prevent the use of rice. Vegetables of all kinds, both cul- tured and wild, are objects of universal consumption ; among the latter description, not already noticed, may be mentioned the nettle, fern, tulip, maU, &c., of which the shoots, root, and bean, respec- tively, are eaten: the list of herbs, roots, and leaves, considered ed- ble by the natives, is endless ; indeed, from their indiscrimination in this respect, fatal cases of poisoning sometimes occur. During' the periodical residence of the agricultural classes in the Bhabar their principal food is the “ guiya” or sweet potato, boiled and eaten with buttermilk. Animal food is in much request among all classes; with the exception of those animals the use of which as food is prohibited by their religion, and excepting also reptiles of all descrip- tions and carrion birds or beasts, every sort of animal is converted to food in some part or other of the hills: by the southern Garh- W alis rats and mice are considered as dainties. The favourite flesh is that of the goat, or of the she’ep, where bred : against the sheep of the plains an universal prejudice exists, its long tail rendering it in the eye of the highlander, a species of dog. Ho scruple as to the mode of decease exists, and animals dying a natural death from disease, or other cause, are eaten by the Hindus as well as by the Dorns.” Stewart also in his interesting report on the food of the people of the Bijnor district, which lies at the foot of the Garhwal hills, notices many points which have an interesting bearing on the lessons learned by experience as to the dietetical value and effect of each food-grain. He writes : “The prices of the various staple crops would appear to have a Greater effect on the relative quantities of those consumed at different periods of tile year than opinions connected with their wholesomeness, &e. Still, the latter consideration has its weight in 680 HIM A' LAY AN DISTRICTS determining the choice of certain kinds of food at certain seasons. Thus, in the cold weather, much more bajva^ which is considered “ heating,” is consumed, with a large proportion of salt and spices, than at any other time ; and in that season generally, one meal a day, at least, consists of pulse with rice in the form of khijri. Ba- ghar, or rice made into meal with its inner husk, is also a favourite kind of food in the cold weather. In the hot season, again, rice is the cereal most used, and this accords with the fact that its com- parative consumption is found gradually to increase towards Cal- cutta, and to decrease towards Afghanistan, so that in the Upper Panjab it constitutes a very small proportion of the food of the people, and wheat and maize are very much used. In the rainy season more wheat appears to be eaten than at any other time of the year, very often in the form of gochni bread, with about one part in four of pulse-meal. The labourer, if not in straits, always has two meals a day, the fullest being the morning one, at 6 to 8 a.m., before he begins, or during an interval of, his work ; the evening one, after the day’s labour is finished : but, of course, the change of the seasons, the weather, and the nature and place of his work, cause considerable variation in this respect. “ Tlie staple of food of the labouring classes in this as in most other countries consists of one or other of the cereals, here generally combined with a considerable amount of pulse. From very many enquiries the average consumption of adult labourers, male and female, appears to be about ten or twelve chhattaks (20 to 24 oz.) a day of meal, or rice, with about two chhattaks (4 oz.) of pulse. The average weight of the adult males admitted into Bijnor jail in six months was— Hindus, one maund and ten seers (1001b.), and Musal- mans, one maund and eight seers (961b.); and since this may be assumed as a tolerably close approximation to the average weight of the adult male inhabitants of the district, the above quantity^of food seems liberal when compared with the amount which has been found to support healthy persons in Europe, where the average weight of individuals is probably considerably higher than here. Less invariable (than pulse) but still very frequent concomitant? cf the bread or rice consumed are greens and tcirkdri of gourds and other vegetables, and, in the season, one or two kinds of fruits, OF THE NORTH-WESTERN PROVINCES. 681 ©specially the mango. These not only have their uses in supplying fresh vegetable juices to the economy, but also add to and vary the sapid elements of the food, and thus, besides satisfying the natural craving for flavour, they also aid in stimulating the process of diges- tion, although, both theoretically and practically, an excessive amount of such food taken habitually is deleterious, A more constant error of the labourer is that of making his cakes too thick and under- cooking them. The reasons for this practice are, that it saves trouble, time, and fire, and produces the feeling of satiety with a smaller quantity. It is barely necessary to observe that the practice is calculated to injure digestion seriously (and in native regiments I have very often found that it materially inter- fered with convalescence from certain diseases of the alimentary canal). Hill men eat greedily all kinds of fruits, both cultivated and wild, and very rarely allow either to ripen thoroughly. The number of wild fruits and berries is very large, and the supply lasts from April to October, forming a welcome, though not perhaps always a healthy addition to their food. : 1. Let the number of parts in the given substance be a, and the number required to be added be x. then- X- I om in Q+i) Q+i)-j?0+i) o + i) O -») O+i) 'Or simplified, x — f P~P) 0+0 l a . This will be clear fr 1 (.<0-70 0 + 1) J an example. Let it be required to know what proportion of a pulse, say gram, should be added to a hundred parts of arrowroot to give the best combination. By analysis we know that the proportion of carbonaceous to nitrogenous in arrowroot is 165*5 : 1, and in gram is 3*8 : 1 : then in the formula m will be represented by 165*5 ; n by 3*8 ; p by (the standard known) 6, and a by 100 : so f (165-5-6) (3-8 + 1) _ r 765-60 T a ~~ | (6-3-8) (165-5 + 1) J 100= | 366-96 J 100 = 2*09X 100 = 209*0 = the number of parts required; that is, that 209 parts of gram to 100 parts of arrowroot makes the best combination. This formula is of great value in settling jail and hospital dietaries. A —CULTIVATED FOOD-GEAINS. The cultivated crops are divided into those of the rabi or sown . , in the autumn and reaped in the spring and Cultivated food-grams . 1 ) 1 1 ® those of the hhcirif or chaumas, sown in the summer and reaped in autumn, exactly as in the plains, for the 1 A botanical description of eacli of these plants will be found in my ‘ Noteu on the Economic Products of the North-Western Provinces,’ Part IV., Allahabad, 1881. OF THE NORTH-WESTERN PROVINCES. 683 influence of the periodical rains is felt in all the hills on this side of the snowy range. In the hills ? the staple crops are the same as they were sixty years ago, wheat and barley in the spring, and lice and mandua in the autumn ; in the tract along the foot of the hills rice and arum are the principal rain-crops, and wheat, barley, and mustard the chief spring crops. Dividing the cultivated food-grains amongst the great natural orders, we have as follows : Grammes or Grasses. Triticum vulgare , Linn., wheat — gehun, najihal. Hordevm hexastichon, Linn., barley — -jau. „ himalayense, Linn,, celestial barley — ua-jau. Onjza sativa, Linn., rice — dhdn. Zea Mays, Linn., maize — hhutta, junala, mungari. Paspalum scrobiculatum, Linn. — kodo, Itodra. Panicum. miliaceum , Linn. — chiita, gandra. Oplismenus fruvientaceus, Link. — viandira , jhangora. Set aria italica, Kth —kauni, koni, kukni, Penicillaria spicata, Lam. — bdjra. Eleusine Coracana, Goertn . — mandua. Arena sativa, Linn., oats — -jai. Sorghum, vulgar e, Pers . — -joar, junali. Saccharum officinarwn, Linn., sugarcane Ikh, rihhti, ganna, Leguminos.e or pulses. Cicer arietimm, Linn., gram— clmna, chola. Ervwn Lens, Linn., lentils — masur. Vida Faba, Linn., bean — ha Ida. Lathyrvs saiims, Linn., kisari, cliapta. Pisuin sativum, Linn., pea — lialon, kulai. Phaseolus acomtifolius, Jacq. — moth. „ Mungo, Linn. — mvng, chhimi. P. Mungo var. radiatus, Linn. — urd, mash, chhimi, ruindar. „ torosus, Roxb. — guransh. Phaseolus vulgaris, Linn., bean — shimi, sent. „ multi jhvrus, Willd., scarlet runner. „ coccineus, Lam., ditto variety. Vigna Catiang, Endl. — loibiya, riansh. JDolichos biflorus, Linn. — gahat. ,, Lablab, Linn. — shimi. Cajamis indicus, Spreng. — arhar, rahar , Mr, Glycine Soja, Sieb. — bhat. Cyamopsis psoralioides, D. C. — gamar. CHENOPODIACEiE. Chcnopodium album, Linn. — bethua. 684 HIMALAYAN DISTRICTS Amarantacrle or Amaranths-, Amaranthus frumentaceous , Buch. — chua- » caudatus, Moq. — iteddri chua. » Blitum, Linn. — chamli. Poly gon a ceje. Fagopyrxm esculentum, Moench., buckwheat —ogal, pdltv. „ tataricum, Geer in., buckwheat — -phdpar. Cereals . 1 Triticnm vulg-are, Linn.— Wheat, and Hordeum hexastichon, Linn.— Barley. There are four recognized varieties of wheat (1) geUn safed or white wheat ;• (2), ddU-klidm or dchm, a white- awnless variety grown in large quantities in the Kosi valley near Somesar ; (3), daidat-khdni and (4) Idl-gehun, tdnga or j usher, the bearded varieties. Wheat is called generically kanak or gehun r and by the Bhotiyas ndphal The flour is known as dta or kaunik. There are also several varieties of barley known generically as j au ; a sliort-awned variety is called vena. When barley is sown and reaped together with wheat, the mixed grain is called gojai - and with gram or peas or lentils, it is known as bijru. In both these cases^ the grains are grown together and cooked and eaten as one-. Mixed wheat and gram is called gochni below the hills. Wheat and barley usually follow rice in the same fields. These are prepared in Asauj (September-October) by ploughing and clean- ing, and, when practicable, they are irrigated by turning into them a stream from some river. The irrigated fields are sown in October- November and the uplands in November-December. The seed is- sown in furrows {siya), which are again covered in by the plough, whilst the clods are broken by the dalaya and again smoothed by a heavy flat wooden log {may a), drawn by oxen and kept steady by a man standing on it. Barley ripens in March-April and wheat a month later, and yield about tenfold the seed sown. Both are cut in the middle of the stalk with a sickle and tied in sheaves {dntha) and stacked near the homestead to dry. When dry, the sheaves are unbound and threshed out by a flat wooden board with a short handle known as mungra. In some of the north-eastern &cc wUl'b^fourul fnm * species and full notes on localities, uses. Provinces; Part IV? 7 MteS ° U ^ Ecouomic Relucts of the North-Western OF THE NORTH-WESTERN PROVINCES. 685 Pattis of Kuinaun a primitive form of flail is used in the shape of a long pliant stick. The chaff is used as fodder ; cow-dung ashes (khariya) are mixed with the grain when stored, to pre- vent the attacks of insects. The variety II. JEgiceras , mentioned by Thomson (p. 102) as that 1 curious, awnless, monstrous barley,’ is peculiar to the highlands of Tibet, where it is extensively culti- vated. It ripens in August in the Pruang valley. At the same time that wheat is sown, and often on the borders of the same fields, masur ( Ervum Lens ) and gram ( Cicer arietinum ) are cultivated in quantities. Hordeum himalayense {ccdeste)— Ua-jan, the chama of the Bhotiyas of Darina. This species is only grown in villages bordering on the snowy range and at high elevations, 7-12,000 feet. The seed is sown in first-class unirrigated land in October and ripens in May. The average yield per acre is about fifteen loads, worth one rupee a load, and raised at a cost of about eight rupees an acre. The produce is consumed locally by the Bhotiyas, being esteemed much too poor a food for the lowland folk. Oryza sativa, Linn. — Rice. This widely-distributed grain is, as may be supposed, the principal rain-crop 111 ce ' in the lowlands, and is also largely cultivated in the hills up to 6,500 feet, where some of the most valuable varie- ties are raised in the deep, hot valleys. It is an annual, belonging to the natural order Graminece, having numerous culms, erect, joint- ed, round and smooth, the leaves sheathing and long, scabrous out- side and the panicles terminal. The local names of the varieties are almost endless ; the principal recognized in the Kumaon Division are the following : — Dli an. dhesima. sathiya. dli&ni. makani. batasuma. Ddnsmdti. duda. dhaniya. badatiya. jogydna. ma liar at. Hansraj. sisliali. banpasa. haltuniya. ratuma. rdjbhati. Gajlo. anjan. iauliya. motiya. altari. rupasma. Ilya. amdrasi. Idrmuli. adarat. r ashy a. haldv/ma. Jamol. sal. nauliya. maisuwa. parayai. mandkuri. Bahurva. ltatyuri. rakasuma. andi. chunkuli. salam. Timiliya. gajaliya. muthamuth. gemma. chinablmri. pdliya. In the hills, the agricultural year commences about the middle of February, when the land has to be prepared for the rice-crop, 686 HIM A'LAYAN DISTRICTS which is usually sown where mandua has been raised in the pre- vious season. The manure from the cattle-sheds is spread over the ground which is then ploughed and freed from stones. The terrace walls are repaired and the roots of the mandua from the last crop are collected and burned. In Baisakh (March-April) or Jeth, (April-May), the land is ploughed again and the seed is sown in the furrows, which are closed by a flat log of wood drawn along them. When the young plants have risen to some three or four inches in height, a large rake or harrow is drawn over the ground to remove the weeds and thin the plants. Where water is abundant, the better sorts of rice are sown in a highly- manured and irrigated nursery (bihnora) or seed bed. This is first flooded with water and then ploughed until the soil becomes a semi-liquid mass. Manure is then added and the seed is sown on the top and covered over with leaves, especially those of the chir, which are said to decompose easily in water and form an excellent top-dressing manure. The young plants are transferred (ropa) from the nurseries by the women and children in June-July to the open field. The manure used is commonly the sweepings of the cattle-pens, which are collected in regular heaps on a place set apart for it in the field, usually that in which the cattle have been regularly penned ( kliatta ), to economise the collection of their droppings. Leaves also are collected and allowed to rot in heaps on the field, and twigs and branches of trees are burned and the ashes made use of. The latter are usually taken from the village forests and cost nothing but the labour in gathering and stacking them. When the field is a small one, the earth is loosened and the weeds removed by a small iron sickle (Jcutala). In July-August the weeds are again removed, whilst the land is kept inundated with water, and by the end of August the poorer highland varieties are ready, and by the end of September or beginning of October the finer sorts grown on the lowlands. Iiice is cut from the root and stored on the field in stacks ( hanyura ) with the ears inwards. There it is left for four or five days to dry, and after that the grain is trodden out by cattle on a threshing-floor paved with slates (Jchala) or simply by men on mats ( moshta ). The stalks ( puwdl !) are made up in bundles (ptila) and stored round a pole or in the fork of a tree and afford food for cattle and bedding for the poor. The grain is taken home, OF THE NORTH-WESTERN PROVINCES. 687 and, after being dried on the roof of the house, is stored for use in boxes (bhaJcdr) or in baskets plastered with mud or cow-dung, called korangas or cldlas. Unhusked rice is known as dhdn m Kumaun ; and before husking it is again dried in the sun and then pounded in a wooden or stone mortar called an ukhcd. The pestle (mused) in use is tipped with iron, and the grain is pounded three different times before the clean rice or chanwal is produced. The chaff {child) is used as fodder for cattle, and the husk {pithi) of the third pounding, by the poor. Winnowing is performed by a shovel-shaped basket ( supa ) which is held at such an angle to the wind as allows the chaff to fly off, or the grain is placed on the ground and the basket is used as a fan. One nali or about four pounds of rice-seed produces in irrigated land 35 ndlis of unhusked or one-half that amount of husked rice, and rice-seed in upland unirrigated land about half as much. Dry upland rice ripens from early September ; common irrigated rice from early October and the better irrigated sorts from the middle of October. In Dehra Dun there are three principal varieties, 1 the chaitru, hcdtyu , and kydri or transplanted. The first, which is also known as chambu or anjana, is sown in unirrigated land in March-April {Cheat) and is cut in August-September. Haltyu is sown a month later in similar land and is cut in September ; it is also known as anjani and naka. The kydri furnishes rice of the best quality ; the seeds are sown in nurseries in April-May, and the young plants are transferred in the following two months to wellirrigated fields, where they are carefully weeded. The principal varieties are the ramjawdin and basmati , and these grow best in warm valleys and alon°' the great rivers where there is much moisture. Chcinwcil cooked in water is called bhc'it, but the broken grains {kcinikci) when cooked are called jciula. Khijri is a mixture of rice with urd or bdjra boiled together in water ; and khir is rice boiled in milk. The commoner varieties are often made into bread, and in that case the grain is only husked once and the inner husk is left on to be ground into flour, called baghar in Garhwal. Zea Mays, Linn. — Indian-corn, maize ; — Bhi'Uta, mukui (Ku- maun) ; mungari , junala (Garhwal). The maize plant is grown in 1 Memoir, 22. 688 HIMALAYAN DISTRICTS small quantities in the hills for the heads which are usually roasted whole, and the seed is then eaten from the cob (clinch). The seed is sometimes ground into flour and made into bread either alone or with the flour of moth. Paspalum scrobiculatum, Linn.; P. kora , Willd. — Kodo, kodra , koclram. An annual belonging to the natural order Graminece and sub- order Panicece, cultivated in the sub-Himalayan districts. Dr. J. L. Stewart writes 1 of the Bijnor district : “ Kodra is said to produce cholera and vomiting, and I find that some authors mention a similar phenomenon as occasionally occurring in all three presi- dencies. The natives generally hold that with the ordinary kodra, and undistinguishable from it, grows a kind that they call majna or majni which produces the above effects, but it has been suggested with greater probability that these depend on the use of the new grain under certain conditions.” These results are, however, un- common, as they are seldom met with, and the grain is a favourite one for home consumption amongst the poorer classes. It is husked with the pestle (mused) and frequently eaten unground called chdnwal in the Bijnor district, a term usually applied to husked rice. P. longifiorum, the kdna of Kumaon, grows wild and its seeds are also used as food, lloxburgh, 93 ; Drury (F. P.), III., 565. Panicum miliaceum, Linn. — The china of the hills and chimia sdnodn of some places, of which the ganara or gandri variety ( P. zdiginosum ? ) is grown extensively in the Bhabar. It is an annual with erect, round culms, belonging to the natural order Graminece and the sub-order Panicece. It is cultivated in the hills up to 6,000 feet and the sub-Himalayan tract, and is noted by Madden as apparently wild at Hawalbagh. It is a very delicate plant, sown in March ; it ripens in May in the Bhabar, and is grown chiefly for immediate consumption. In the hills it is occasionally sown in May- June up to 6,000 feet in a few villages and ripens in August. The average outturn per acre in the hills is about 25 loads of unthreshed grain, worth about Us. 20, and raised at half that cost. The seeds are white and smooth like sago, and are considered a fit 1 J. Agri.-Hort., XIII., sec. 50. OF THE NORTH-WESTERN PROVINCES. 689 food for invalids. They are husked by the pestle and mortar, and, like kodra, are often eaten unground under the name chanwal in the Bijnor district. It is known as a tinpdkh or “ three-fortnight ” grain, that being the time required for its production from sowing to cutting, and is therefore one of those allowed as food to devout Hindus during fasts. P. brizoides, Jacq., is occasionally cultivated under the name bdrti for the same purpose. Roxburgh, 104. Oplismenus frumentaceus, Link. — the mandira and jhangora of Kumaun, jhungara of Gtarhwal, the saman of the Bhabar, and smvcm of the plains ; sgdmdk, Sanskrit. This is a small hardy annual belonging to the natural order €h 'aminece and sub-order P anicece , cultivated throughout the hills up to 6,500 feet and in the submontane tracts. It thrives best in soils tenacious of moisture or which receive plenty of rain, and is sown in July and gathered in September. The ears are cut first, and the stalks afterwards as fodder for cattle. It is also one of the “ tinpdkha ” or “three-fortnight” grains, coming to perfec- tion in about six weeks. It has culms erect, 2-4 feet high, panicle erect ; spikes secured, incurved; flowers three-fold unequally pedi- celled ; leaves large, margin hispid. The grain is considered heating, but when kept for four or five years loses that quality. It is chiefly consumed by the pooler classes made into khir ( boiled with milk), khuskhdb, khijri, &c. It is th ePanicum frumentaceum of Roxburgh, 102. 0. colonus, Kth., occurs w r ild and occasionally cultivated or rather allowed to grow under the nam e jangli-mandira* Setaria italic a> Kth. ; Panicum italicum, Linn. ; Pennisetum italicum , R. Brown. — Italian millet. The Jcauni, koni of the hills, hukni of Bijnor, and kangni of the plains. This is an annual with culms erect, 3-7 feet high, round, smooth ; roots issuing from the lower joints ; margins of leaf hispid ; mouths of the sheaths bearded ; spikes nodding ; spikelets scattered ; seeds ovate ; cultivated in the hills up to 6,500 feet and in the submon- tane tracts. In the hills it is sown with mandira or along the edges of rice-fields for home consumption in April and gathered in September. An unmixed field of kauni is very uncommon. The ears are cut off while the crop is standing and the stalks are only used as bedding for cattle. As a food, natives consider it to 87 690 HIMALAYAN DISTRICTS be cool and dry, astringent and diuretic, and to be of use exter- nally in rheumatism. When taken as the sole food it is said to be apt to produce diarrhoea. It renders beer more intoxicating. In Madras its flour is highly esteemed for pastry. Roxburgh, 102 ; Drury (U. F.), 338. Penicillaria spicata, Willd. — Spiked millet — Bajra. This millet is also occasionally grown along the foot of the hills and in the lower valleys within the hills, but bajra , joar, and maize are essentially plants of the plains proper, Roxburgh, 95. Eleusine Coracana, Goertn. ; the mandua or maruwa of the hills, k odo of parts of the western hills and ray Id of the south of India. Mandua belongs to the natural order Graminece and sub-order Cldo- ridece, and has an erect culm supporting from four to six spikes, digitate, incurvate, from one to three inches long, composed of two rows of sessile spikelets, each consisting of from three to six flowers. Calyx formed of jtwo glumes : seed covered with a thin, pellucid, membraneous aril. It is the staple autumn or chaumds ( saoni in Dehra Diin) crop of the highlands (up to 8,000 feet) between the Tons and the Sarda, and forms the main food-resource of the agricultural classes. It gives a larger yield than other crops, and is said to increase in bulk when ground, qualities that have probably led to its more general cultivation, as it is a poor and very coarse grain. Indeed, Madden terms it u a bitter and indigestible food.” Mandua is cultivated both in ordinary agri- cultural land and in freshly cleared jungle. In ordinary land, it usually follows a wheat crop which is gathered in April-May, and the land is at once prepared for the mandua in the same manner as for rice. The seed is sown broadcast, and, instead of a harrow, the bough of a tree is drawn over the newly-sown land to cover the grain. When the young plants have risen two or three inches, the whole field is harrowed two or three times and the vacant spaces are filled up from those where the plants are in excess. Seeds of the g alicvt , urd, bhat, and other similar grains are then sown in the midst of the mandua , and their produce is collectively called lean in Kumaun. Later on the crop is well weeded with the kutala, and in October-November the ears of the mandua are cut off' and the kdn OF THE NORTH-WESTERN PROVINCES. 691 are rooted up. Afterwards the stalks (naluwa) of the mandua are out and tied in bundles and stacked like those oi rice to serve as fodder, or cattle are driven into the field and allowed to consume them. The ears of the mandua arestacked ( thupard ) for some twenty to twenty-five days, when they begin to ferment, and, when warm, they are spread out and dried and are then threshed out by a flail ( -saila ) , or are trodden out by cattle. Winnowing is performed by the supa as in the case of rice, and the heap formed is then passed through a sieve (rangra) before being stored. The chaff ( dhusi ) is used as fuel for cooking and its ashes as a dye and for washing clothes. The chaff ( nat ) of the kan is useful for fodder. Mandua is ground into flour of a somewhat rough and astringent taste, and made into unleavened cakes or a kind of porridge called bciri. A spirit called dura is also made from it and sells at from three to six annas per bottle. A variety called mandin has usually 3-4 spikelets which are not incurvate and ripen in September. E. indica , the mandavi of the tract along the base of the hills, is common in the hills and Bhabar. The rent per bisi, which is only forty square yards less than an acre, varies from one-fourth to ono-lialf the crop, and may be set down as about two rupees. The cost of ploughing and harrowing where cattle are hired would be about two to two and-a-half rupees per bisi, and for labour whilst the crop is on the ground about the same amount. Seed, sowing, cutting and cleaning the grain about three rupees, 1 giving a total expenditure of ten rupees per bisi. The aver- age outturn is between fifteen and twenty maunds of forty seers each, worth about one rupee a maund. Mandua is one of the favourite crops with squatters in the forests. Their mode of operation consists in felling the timber and clearing patches along the ridges in autumn, and when the timber is dry it is burned in spring, and mandua is then sown in the ashes and lightly ploughed in or hoed in by hand. No other labour is required beyond roughly fencing in the patches with the half-burned logs and watching them at night to prevent the incursions of wild animals. The cost of production is much less than in ordinary land, and no rent is paid, as but one crop is taken, after which the patch lies fallow for from six to twelve years. This 1 Sowing four annas ; seed at twelve seers per bisi, eight to ten annas ; cutting and winnowing, for the former eight and the latter four men, wo dd cost from to 36 annas. 692 HIMALAYAN DISTRICTS mode of cultivation is, according to the nature of the soil, known as Jcatil, kcila banjar or ijran in Kumaun and as khll ©r kdndala in Garh- wal. In ordinary land there is a formal rotation of crops. Thus, rice is sown in April and gathered in September, after which the land is pre- pared and yields a crop of wheat or barley, which is cut in April, and is succeeded by manduct , and as the last is not ready for the sickle until November, the land is allowed to remain fallow until the follow- ing spring, when rice is again sown.. Where land has been long allowed to lie fallow, a crop of mandua or chiki or buckwheat is usually taken first, and, as a rule, a field is allowed to lie fallow after every third crop, except in a bad year. In the Bhabar, mustard is sown in August and gathered in February, when it is followed by the gandra variety of millet which is ripe in May. Then wheat is sown, which is followed by rice in the next spring. In the older vil- lages nearly half the land, especially that on which rice has been sown, is allowed to lie fallow one season. In new villages land is cropped without intermission for several years. Roxburgh, 115.;. Drury (U.P.), 206. Avena sativa> Linn. — Oats — Jai, unldyaii-jau . Jai is grown in small quantities in the hills (6-10,000 feet) and in the Dun for local consumption. In the hills it is usually sown mixed with bar- ley and the two are eaten ground up together. A. fatua seems to occur wild. Sorghum vulgare, Vers.; Ilolcus Sorghum , Linn. — Great mil- let — The junali of the Bhabar and joar oi the* plains. This millet is grown in very small quantities near houses here and there in the Bhabar and in parts of the hills up to 5,000 feet. S. JIalepense , Linn., occurs wild in the Bhabar, under the names buru and rikhonda. Junali is grown in the plains for its seed and sown closely as a fodder, which is acceptable to, and greedily eaten by, cattle of all sorts, notwithstanding the size of the stalks. Rox- burgh, 90; Drury (U.P.), 413 ; Steudel, 384. Saccharum officinarum, Linn. — Sugarcane — Ikh, rikhu •, ganna T puna-rikhu ( large variety ) , kanthi-rikJm ( small variety ) . Though the- sugarcane is not a food-grain, it may be noticed here as belonging to the Graminece. It is only occasionally cultivated in the hills, notably near Dvvara Hat and Gangoli Hat, but is largely grown m OF THE NORTH-WESTERN PROVINCES. 693 the submontane tract and the Tarai. The details of manufacture for export do not differ from the system generally observed else- where. Pulses. The pulses belong to the natural order Leguminosce or pea-tribe, and afford a large quantity of the food-resources from the vegetable kingdom in these provinces. Of those raised by field cultivation, mung, mash, and masur are often eaten unhusked by the poor. The two first and gram or cliana are held in high repute, though all are considered, when eaten alone, to be apt to produce colic and flatu- lency. Gram, peas, and a few others are occasionally ground into a flour called besan and made into bread either alone or in the propor- tion of one-fourtli with cereals. Thus, wheat is ground with gram, maize with urd, and the millets with moth. Pulse bread alone is only resorted to when nothing better can be obtained. Mash and mung split in two and then known as dal are usually eaten separately or with rice, when the mixture is called Jchijri. Mimg and arhar are reckoned as good nutritious food for invalids, but moth and master are considered less valuable as causing heat and thirst. Master is said to be the source of the well-known Du Barry’s Revalenta Arabica Gram, peas, mung, moth, and lobiga are frequently parched by trades- men known as bhwijas, and, under the name chabena, form the usual food for persons going on a journey or employed so as to prevent their being able to cook their regular meals. The usual mode of preparation, however, is to boil the pulse, after removing the pod, and serve with condiments of various kinds as shred onions, turme- ric, spices, &c. Eaten with boiled rice, they form one of the staple dishes of the country ( dal-bhdt ), and in this form are said to be most wholesome, the cereal correcting, to a certain degree, the heating properties of the pulse. Cicer arietinum, Linn. — Gram — Ghana. The gram plant is sparsely cultivated in the hills. It is a naturalised plant, a native of Europe, deriving its name from the pea having a supposed resem- blance to a ram’s head (aides). It belongs to the natural order Legumi- nosce and sub-order Viciece. There are four varieties, black, white, red, and yellow, the last of which is that usually found here. It is cultivated in the warmer localities, usually as a border to wheat, and 694 HIMA'LAYAN DISTRICTS ripens in February. The bhiisa of the stalks and leaves forms a valuable fodder for cattle and horses, and the green leaves are eaten as a pot-herb. Hook. FI. Ind., II., 176: Roxburgh, 567. C. micro- phyllum , Benth., a wild species growing in Tibet, is remarkable for a very viscid exudation and its strong odour (Thomson’s Travels, 371): Drury (U.P.), 134. Ervum Lens, Linn.; Cicer Lens, Willd. — Lentils. — Masur, an annual belonging to the natural order Leguminosce and sub-order Vicieoe, is sparsely cultivated in the hills, but is increasing in favour in the Bhabar. The seeds split in two are used as a ddl, but they are commonly regarded as heating. It also is sown at the border of fields and ripens in February. Roxburgh, 567. Vicia hirsuta, Koch. This plant is found wild near Ahnora, and is occasionally cultivated as a fodder under the names mamri, mamr-clianci, a n d j h anj ha nig a-kuri up to 5,000 feet in Kumaun and also in the Tarai. Hook. FI. Ind., II., 177. Vicia Faba, Linn. — The garden bean — Bahia. This bean is cultivated occasionally for its seed and straw up to 8,000 feet. There are several varieties sown from introduced seed or native seed either in fields or gardens. V. sativa, Linn., var. angustifolia (Hook FI. Ind., II., 178) and V. tenera occur wild. Lathyrus sativus, Linn. — The chickling vetch — Kisdra , churdl, chapa, mattar , kcisa. This species is occasionally cultivated below the hills and in the hills up to 8,000 feet. The evil effects of this pulse is unknown in Bijnor and the Bhabar, though it is said to produce paralysis in Allahabad. L. sphcericus, Iietz., and L. Aphaca, Linn., are found wild. Pisum sativum. Linn. — The field-pea — Kalon , hulai, batana (Jaunsar). This well-known annual has been introduced from Europe. The seeds are round, of uniform colour, and there are 5-6 leaflets. Another species, P. arvense, Linn., having 2-4 leaflets and compressed marbled seeds, is said by Royle to be a native of India. It is cultivated in small quantities up to 8,000 feet in the hills. Hooker, FI. Ind., II., 181. Phaseolus aconitifolius. Jacq. — The aconite-leaved kidney bean — Moth. This species is chiefly grown in the submontane tract in the poorest soils and is of little account amongst food-resources OF THE NORTH-WESTERN PROVINCES. 695 here except in dry seasons. Hooker, ibid., 202 : Roxbui gh, 558. Phaseolus Mungo, Li tin. — The small-fruited kidney bean. Mung, chhimi, cJiikcin , and var. rculiatus, Linn. — rayed kidney bean ; urd, mash, chhimi ruinddr. Both these varieties are cultivated in Eumaun up to 4,500 feet. The former is rare and has greenish yellow flowers, pods 10-15 seeded, and seeds with numerous longitudinal close streaks. Theie are four varieties, green, black, yellow, and white, of which the first is most common : ripens in October. The second has yellow flowers, pods very hairy, 4-6 seeded ; two varieties, black and green, and a third smaller plant occurs called urdi. It is a rain crop and is more commonly cultivated in the hills up to 6,000 feet. It is considered the most heating of all the pulses and is seldom eaten alone. Hooker, l. c., 203 ; Roxburgh, 556. P. Mungo of Roxburgh is the common green mung ; the black variety is his P. Max and the yellow variety is his P. aureus, whilst P. Roxburghii, W. et A., is the same as P. radiatus, Linn., urd or mash, now reduced by Aitchison (p. 389) to a variety of P. Mungo, Linn. Phaseolus torosus, Roxb. — Guraush, gdrdnsh. This species is grown at a higher elevation than any other pulse (6,500 feet), chiefly in Kali Kumaun, but '’also in Ahnora and the Bhagirathi valley up to 4,500 feet. It is apparently a cultivated form of P. calcaratus, Roxb. (Hooker, II., 204). There are two varieties, one of which has a red and the other a cream-coloured seed : ripens in October. Roxburgh, 558. Phaseolus vulgaris? Linn. — French bean — Shiuchcina, bakula. This and P. multifiorus, Willd. (scarlet-runner) are chiefly grown in gardens as pot-herbs. P. coccineus, Lam., differs by its bright scarlet, casually white, flowers arranged in long racemes which often overtop the leaves. Hooker, ibid., 200. Vigna Catiang, Endl. ; Dolichos sinensis, Linn. : both are now united — Lobiya ridnsh, rdish, riensh. * The first is low and sub-erect with pale purplish flowers ; the latter is tall and voluble. There are several varieties differing in the •colour of the flowers and seeds (white, brown, yellow, black). Three G96 HIM A'LAYAN DISTRICTS oi tom mo cultivated in Kumaun (up to 4,000 feet), of which one is known as sonta. All the varieties are usually sown with other crops. The young legumes are eaten as a vegetable and the ripe seeds in curries. Hooker FI. Ind., II,, 205 ; Roxburgh, 559, 560. Dolichos biflorus, Linn.— Horse-gram— Gahat, Math, the Jculthi of the plains. The horse-gram is occasionally grown in the hills up to 6,000 feet and in the submontane tract. In the Bhabar it ripens in October. Hooker, l. c., 210 ; Roxburgh, 563. Dolichos Lablab, Linn. — Black seeded kidney-bean — Shimi, cMmi. Six varieties of this species are commonly cultivated in gardens and very occasionally as a field-crop. Hooker, l. c., 209 : Roxburgh, 560 : Drury (U. P.), 282. Cajanus indicus, Spreng. ; C.flavus and bicolor, D. C. ; Cytisus Cajan, Linn. Pigeon-pea. — Arhar, rahar, tor, thohar. The pigeon-pea is occasionally cultivated in the hills up to 4,000 feet and in the submontane tract as a border to other crops and has a reputation for being easily digested and nutritious. C.flavus has the vexillum yellow, whilst C. bicolor has it beautifully veined with purplish red ; the latter is more commonly cultivated in Kumaun. Glycine Soja, Sieb. ; Sojahispicla, Moench. — Soybean — the bhat of Kumaun, bhatncis and bhatwas of Nepal and northern Tirhut, and Khajuwa of the Tarai. This bean, though a poor food resource, is extensively grown in the hills 4-6,000 feet, as food for men and cattle. It ripens in October. Hooker, l. c., 184 ; Roxburgh, 563. Cyamopsis psoralioides, D. C.— the gawdr of Meerut and kauri, syamsundari, phali-gawar, kawdra and kachMr of the submontane tract. It is sown with other rain crops or along the borders of the fields in the rains in favourable places, but will not stand either excess of moisture or high winds. The legumes are delicate and aie used in vegetable curries when young, and when mature they are boiled and with a little mustard-oil given to cattle as a condi- tion fodder. Drury (U.P.), 179. CHEN OPODIACEiE. Chenopodium alburn, Linn.— Goosefoot— Bethuwa, chardi, jau-sag. An annual which occurs ( cultivated occasionally ) in the hills up to 4,000 feet. It is gathered for its seed, whilst the young OF THE NORTH-WESTERN PROVINCES. 697 loaves are used as a vegetable. It is entirely a rain crop and attains a height of six feet. The seeds ripen in October and are considered nutritious. Roxburgh, 260. Amaranths. Amaranthus frumentaceus, Buch. — Prince’s feather — Clda, ehua-mdrsa, ramdana, ancirddna of these hills and bcitu , bdthu f batliua of Bisahr. There are two varieties, the red and yellow, both of which belong to the natural order Amarantacece and sub-order Achyranthew, pentandrous ; steins and branches erect ; leaves broad-lanceolar ; panicles erect ; leaves of the calyx daggered ; capsules wrinkled, seed, solitary, round, pellucid with callous white margins. Calyx longer than the stamens ; leaflets in both male and female with subulate points. Male flowers with five stamina : female flowers with 2-3 styles. Chua is largely grown in the northern par- ganahs up to 9,500 feet, where it forms the staple food of the poorer classes and is a favourite crop in newly-cleared jungle, as it is not easily inj ured by bears and deer. It is sown in May and J une in first and second class unirrigated land and yields about twenty loads to the acre. The produce of an acre is worth about sixteen rupees, and the estimated outlay is about half that sum. From an experiment conducted in the Botanical Gardens in Calcutta it was found that forty square yards of ground sown with this plant in June yielded twenty-one pounds weight of clear ripe seed in September, or thirty-one rnaunds to the acre. It also grows well from October to February in the plains. Some identify cluia with A. Anardcina ( farinaceus ) , and much remains to be done to clear up the synonymy of the amaranths. Roxburgh, 663. Amaranthus caudatus, Linn. — Love lies bleeding — the Jceddri chiia of the hills. This species has an erect stem angularly- striated, glabrous, green ; leaves long, petioled, ovate or rhombo- vate, narrowing at both ends, bluntish, emarginate, glabrous, green ; spikes ascending : flowers sessile, green : bracts longer than the sepals, which are three in number. Cultivated in gardens or near the homestead in the hills for local consumption. The seed is sown in May-June and the crop is ripe in October. Drury (F. P.), III., 21. Amaranthus Blitum, Linn. ; Var. poly g on oi den, A. polyga- mus , Linn. Hermaphrodite amaranth . — Chamli sdg, chauldi. This 88 HIMALAYAN DISTRICTS £98 common species is sometimes grown along the edges of fields in the submontane tract as a pot-herb. Like all the amaranths, it is one of the phaldhas or food-grains which Hindus may eat during' fasts. POLYGOFACEJE. Pagopyrum esculentum, Moench. — Buckwheat — The ogal of , Kumaun, kotu of Garhwal, and paid of the Bhotiyas. The Himala- yan buckwheat belongs to the natural order Polygonacece and sub-order Apterocarpece. It is grown chiefly as a vegetable in the hills and is recognisable by its red flowers. It is frequently sown in newly-cleared forest land and ripens in September. The grain is exported to the plains under the name kotu and is eaten by Hindus during their fasts ( bart ), being one of the phaldhas or food- grains lawful for fast-days. It is said to be heating, but palatable, and is sold by the pansdri or druggist, and not by the general grain-dealer. F. cymosum, Meissn., the ban-ogal of Kumaun, occurs wild in the lower hills. Eagopyrum tataricum, Goertn. ; F. emarginatum. — Buck- wheat, — called phdpar or pdphar by the Kumaunis and hhe by the Bhotiyas. It has a white or yellow flower and only grows at high elevations, 7-12,000 feet. It ripens towards the end of September or beginning of October. The seeds are oval, acute, nearly tri- angular with acute, smooth, brilliant angles, the size of a hemp seed, of ash-brown colour, whilst the seeds of the ogal are rounded. B.— CULTIVATED VEGETABLES. The vegetables grown in the Kumaun division are those noted below, which may be divided into three classes : (1) those like the gourds and melons that are eaten raw or cooked ; (2) those general- ly boiled in water with salt and spices or cooked with ghl (clarified butter) or oil, as the ordinary garden produce , such as radishes, onions, carrots, turnips, and the legumes of various plants and which are known generically as tarkdri ; and (3) the leaves and stems of various herbaceous plants, cultivated and wild, which are boiled in water and form what is known as sag or greens and when cooked merely with sufficient water to prevent their burning, hhangi or OF THE NORTH-WESTERN PROVINCES. 699 bhangiya. The first class comprises a great proportion of the food of all classes during the months that they are in season and form one of the most important dietetical products of native horticulture. The second class forms the staple of curries eaten with split pulse or dal and the third class includes both plants specially cultivated as greens ; the leaves and parts of plants cultivated for seed, fruit or fibre, but not specially cultivated for greens, and the roots, bark, leaves, and flowers of an immense number of wild plants which are edible, and form a substitute for the cultivated plants with the poorer classes and with all, indeed, in times of scarcity. We shall divide the vegetables therefore into gourds, ordinary vegetables ; thirdly, those plants that are cultivated as greens ; and lastly, the principal wild plants that are considered edible and form a portion of the food of the people. Gourds . 1 Gourds belong to the natural order Cucurbitacece , and are grown in the hills and submontane tract. They are annuals, climbing, hav- ing clasping tendrils on the stalk, hairy, drastic, pulpy and refresh- ing, but apt to produce evil effects if taken in inordinate quan- tities. The principal species, cultivated and wild, are noted below in order to give a general view of the entire order. They may be divided for their dietetic properties into three classes : — (a) the plea- sant tasted, with a refreshing juice, usually eaten raw like the melon and water-melon : (b) the other edible gourds which are either insipid or bitter, and are all cooked before being eaten and (c) those cultivated or used for their medicinal properties only. The prin- cipal genera represented in the Kumaun division are Trichosanthes, Luffa, Cucumis, Citrullus, Cephelandra, Bryonia, Mukia, and Zeh- neria. Trichosanthes palmata, Roxb. — The indrdyan of Kumaun and pahval of the plains. This species may be known from its red glo- bose fruit which is possessed of severely drastic properties when wild, though edible under cultivation when boiled. T. dioica, Roxb., the palical of Bijnor, is also edible. Hooker, FI. Ind., II., 606 : Drury, (F. P.), I., 467 ; Roxburgh, 695. 1 For a botanical description of each plant see my ‘ Notes on the Economic Products of the North-Western Provinces,’ i’art V. 700 HIMALAYAN DISTRICTS Trichosanthes anguina, Linn. — Common snake gourd. — The ehachindct of Kumaun and chaclringa of Rohilkhand. This species is cultivated throughout the hills and plains. The fruit is greenish white, 2 '-3' long, and is usually eaten cooked. Hooker, FI. Ind. y II., 610 ; Roxburgh, 694 : Drury (F. P.), I., 467. Trichosanthes cucumerina, Linn. — The jangli-ehachinda of Kumaun. The jcmgli-chachinda appears to be the wild representa- tive of the preceding ; the fruit is chiefly used in medicine, though it is edible. Hooker, l. c., 609; Roxburgh, 094; Drury (U.P.), 440; Royle, 219. • Luffa aegyptiaca, Milk— GUya tarm or ghiyci tori. It may be known by its 5-angled leaves and 10-angled fruit. It is used much in curries-, dressed as a vegetable with clarified butter and spices. Hooker, l. c., 614; Roxburgh, 698-; Drury (F. P.), I., 459. Lllffa acutangula? Roxb . — Kali taroi or tori. It has the lower leaves 5-angled, the upper leaves palmate, the seeds black and irre- gularly pitted and the fruit usually smaller and is commonly culti- vated and highly valued as a vegetable. Hooker, l. 615 ; Rox- burgh, 698 ; Drury (U.P.), 291. Lagenaria vulgaris, Sering.— Pumpkin or bottle gourd— Lanka , tumid (small variety), gol kciddii. It is from this gourd that the bottle carried by mendicants is made; it is extensively cultivated along the foot of the hills. Tire pulp is eaten with vinegar or mixed with rice as a cTihachM or vegetable curry. Hooker , l. c. 613 - Drury (U.P.), 383; Roxburgh, 700. This fine species was brought to Almora from Jabalpur in 1846 by the Bengal Artillery. The tumri variety is not edible. Benincasa cerifera, Savh— White gourd melon— BMnja, petha, chdl-kumhra. Cultivated for its fruit, which is used in curries and as a vegetable. Fruit 1-1 1 feet, cylindric, without ribs, hairy, ulti- mately covered with a waxy bloom. Hooker, l. e., 616 ; Drurv (U.P.), 76 ; Roxburgh, 700. 7 Momordica Charantia, Linn. — ITarela, karola. There are two varieties well marked; the one with longer and more oblong fruit, and the other with fruit smaller, more ovated muricated and tuber- cled and numerous gradations between them. The fruit is steeped OF THE NORTH-WESTERN PROVINCES. 701 in water with a little salt and then eaten cooked in curries. Hooker, l. c., 616 : Drury (U.P.), 306 ; Roxburgh, 696. Momordica dioica, Roxb. — Gol kdnkra. There are several varieties, of which the unripe fruit and tuberous roots form an article of food. M. Balsamina also occurs along the foot of the hills in wild state and in Bijnor. Hooker, FI. Ind., II., 617 ; Drury (U.P.), 306 ; Roxburgh, 696. Cucumis trigonus, Roxb. — Bislombhi. Found wild along the foot of the hills. Hooker, l. c., 619 ; Roxburgh, 701. Cucumis Melo, Linn. — Melon — Kharbdz, and C. var. utillisimus , kakri. Both these varieties may be seen at Srinagar, but they are not cultivated in the hills generally or in the submontane tract. Hooker, l. c., 620; Drury (U.P.), 172; Roxburgh, 701. Cucumis sativus, Linn. — Cucumber — KMra, khirai, kakura. This species is also cultivated for its fruit, and C. Hardwichii, Royle, the air-dlu of Kumaun and pahdri-indrayan of the plains seems to be only a variety of it. Both the latter and C. himalensis occur wild in the hills and Bhabar. C. Afomovdica , Roxb. ( Ulta-kanta ■„ „ 110 ... „ 173 ... Flacourtia Earuont- chi. Flacourtia sepiaria... Saurauja nepalensis, Bombax malabari- cnm. Sterculia urens ... K andi, Kandai .., Gogina , gogana Semal ... „ 193 ... „ 194 ... „ 280 .. „ 349 ... „ 355 ... Portions edible. Bads, calyx, leaves and fruit. Fruit (Banndeo), wild. Fruit : other species also eaten. Fruit often dried like raisins. Flower-buds pickled as capers ; fruit. Fruit. Fruit. Do. Calyx of flower-buds. Roasted seeds. Grewia asiatiea ... Dhdman , pharsiya ... „ oppositifolia, „ sCabrophylla, Elaeocarpus Varu- nua. Bhevgul (Sur-bheli J alp ut • • • Ml 387 ... Palatable sub-acid fruit. 384 ... Ditto. » 387 ... Ditto. )> 407 ... Fruit : very rare. OF THE NORTH-WESTERN PROVINCES. 717 Scientific name. Vernacular name. Reference. Portions edible. Glycosmis penta-' phylla. Ban-nimbu pilru, pota- . la. Hooker, I., 499 . Fruit : very rare in Bhabar. Limonia acidissima. Beli „ 507 ... Pulp of fruit in sher- bet : wild. Feronia Elephant- um. Kait, hath bel „ 51G ... Fruit: cultivated and wild. JEgle Marmelos Bel , sriphala ... „ 517 - Ditto: ditto. Garuga pinnata Kitmira, kharpat ... „ 529 ... Fleshy black drupe. Zizyphus Jujuba ... Ber, her a Kandidri, hul phal, hhalis , bcri. „ 632 ... Fruit : cultivated. „ vulgaris ... „ 634 ... Ditto : cultivated and wild. „ CEnoplia ... Ma/w, bamolan „ 634 ... Ditto : wild. „ oxyphylla ... Giyar ... „ 634 ... Ditto : do. Hovenia dulcis • •• „ 640 ... Ditto: cultivated and wild. Sageretia oppositi- folia. Agluia » 641 ... Black, succulent fruit. Vitis lanata Asaujiya, pahdr.phuta, purain. » 651 ... Fruit. iEsculus indica Pdnkar ... „ 675 ... Seeds steeped and ground. Tistacia integerrima, Kakra-singi (fruit) ... Hooker, II., 13 ... Fruit. Semecarpus Anacar- dium Bhilatva, bhela „ 31 ... Fleshy receptacle around seeds. Buchanania latifolia, Piyal, muriya, katli- b/nldwa. „ 23 ... Kernels of the fruit. Spondias mangifera, Amra , bahamb, amara , „ 42 ... Fruit. M o r i nga p t ery gosp ei - ma. Sahujna, schjna ... „ 45 ... Bark, leaves, flowers, pods. Bauhinia malabarica, Anili „ 277 ... Leaves. „ variegata, Kachnar, khainwal, burial. „ 234 ... Ditto and flower- buds. „ purpurea . Kaniyar, kandan, yu- ridl. „ 284 ... Flower-buds. ,, Vahlii Maljan , mala „ 279 ... Seeds. Tamarindus indica Imli „ 273 ... Fruit: cultivated. Cassia Fistula KitwuV , kitola, itola.,., „ 261 ... Young pods. Brinsepia utilis Bhekara , dhulela, jha- tela. „ 322 ... Oil of seeds. Rubus lanatus Hindi u „ 331 ... Fruit. „ paniculatus Kdla-hisdlit , anchu, patharola. » 329 ... Black fruit. „ mo’uccanus ... Katsul, his ala , 3 . „ 330 ... Red fruit. „ niveus ... Pila-hinalu jj 3.35 o # « Brownish-yellow fruit common. „ lasiocarpus ... Flisdlu, kdla } and lal ... ,, 339 ... Red and black fruit ; common. „ ellipticus ... Guuri-phal, jogiya- hisalu. ,, 336 ... Yellow fruit, common. „ nutans Langur, sinjang (Bhot ). „ 334 .. Red fruit. Tcrminalia bellerica Bahera ,, 445 .. Kernels of fruit. Eugenia operculata, \Rdi-jdman „ 498 .. Fruit. . Alangium Lamarekiv A kola, gkaul „ 741 .. Do. Cornus macrophylla,' Kdgshi, ruchiya „ 744 .. . Do. „ capitata j Bamaura „ 744 .. . Do. 718 hima'layan districts Scientific name. Vernacular name. Reference. Portions edible. Lonicera angustifo- Geang (Jaunsar) ... Hooker, III., 13... Fruit. lia. Viburnum stellula- Ldl tlt-maliya ... „ 4.. Do. turn. Anthocephalua Ca- Kadam ... ,> 23... Do. : cultivated. damba. Randia uliginosa ... Pindaru „ 110.. Do. „ dumetorum, Mainphal, manyul ... ,, 1 10 .. Do. Maesa argentea Phasera, gogsa Brandi a, 283 ... Do. Ortliantheraviminea, Chupkiya „ 334 .. Flower-buds. Cord i a Myxa D uirata, baurala „ 336 ... Fruit. „ reatita ... Fin , hum ... „ 338 ... Do. Eliretia aerrata Puna, p widen, .. „ 339 ... Do. „ lsevis Cham ror ... „ 340 ... Do. Ilippophae rliarn- noides. Dhur-chukf tarwa- c/tuk. 388 ••• Do. Elaeagnus latifolia, Ghiwai, m ijhaula ... „ 390 .. Do. Morus indica ••• Tut tueri ... „ 408 ... Do. „ serrata Klmu , himu „ 409 ... Do. „ laevigata Shah-tut , siydh-tut .. „ 409 ... Do. „ multicaulia ... tH • II Leaves for silk- worms. „ chinenaia ••• HI • • • Do. Ficus Carica ... Anjir 418 . Fruit. „ macrophylla... Timla Roxburgh, (’45... Do. yt virgata Bern Brandis, 419 Do. }} Cunia Kunia, kuinau „ 421 ... Do. „ glomerata Gular , pariwa, lelha... „ 422 ... Do. Artocarpua Lakoocha, DahUjbarhal „ 426 ... Do. and male flower heads. Celtia auatralia ... Khar ah „ 428 ... Fruit. AntideBma diandrum, Amli, sarshoti, sar- sheti. „ 447 ... Do. Bricdelia retusa Gauli ... „ 449 ... Do. Fhyllanthus Embliea, Aonla, arnla, amlika,.. „ 454 ... Do. Securinega obovata, Gwala-ddrim , dhani... „ 455 .. Do. Myrica aapida Kdiphal „ 495 ... Do. Ephedra vulgaria ... Khana ... „ 501 ... Do. MuBa sapientum Kela Roxburgh, 223 ... Do., wild and culti- vated. Dendrocalamus atric- Bdns ... Brandis, 564 Tender shoots. tua. ^ OF THE NORTH-WESTERN PROVINCES 719 F.-PARTS OF WILD PLANTS USED AS FOOD IN THE HILLS OR SUBMONTANE TRACT. The following list 1 gives some of the wild plants of which parts are used for food in seasons of scarcity. Some of them, such as the lotus, yams, and wild millets, are always eaten by the poorer classes : — • Scientific name. Vernacular name. Reference. Parts edible. Nelumbium specio- Kaniaal , padam, am- Hooker, I., 116... Stalk, leaves, and sum. bnj. roots. Triumfetta rhomboi- Manphora, jhinjhru .. „ 395... Leaves and seeds. dea. „ pilosa ... Leshwa-kumariya „ 394... Ditto. Tribulus terrestris ... Gokhru „ 423... Leaves and fruit. Leea aspera Kim ali, kurmali „ 666. Fruit. Pueraria tuberosa ... Bildi-hund, hiralt. puna , sardl (Jaun- sar). Hooker, II., 197... Tuberous roots. Flemingia congesta, Mus-hela „ 229... Pods. Cassia Tora Bandr. panuodr ... „ 263... Leaves and stems. Trianthema mono- Bishkhapra .. „ 6G0... Ditto. gyna. Leaves. Hydrocotyle asia- Thalkari „ 669... tica. Ipomcea sessiliflora, Haran-khuri, liara .. Roxburgh, 169... Ditto and stems. Solanum verbascifo- Aseda ... „ 189... Fruit. lium. Celosia argentea ... Strati, qhogiya i ... „ 228... Leaves and stems. Digera arvensis Das Drury, III., 29... Ditto. Euphorbia angusti- folia. Dudhila-ghds, maha- bir. „ 120... Seeds. Urtica parvifiora ... Berain, shishona Roxburgh, 664... Leaves. Aloe vulgaris Gaikwdr ... Drury (U.P.)27... Seeds and leaf pulp. Commelyna obliqua, Kana, kanjura ,. Drury (F.P.)III., 310 Leaves and stems. Dioscorea sagittata, Tair, iarur R,oyle Roots. „ versicolor, Genihi, githi gajir,- Drury (E.P.)III., ghanjin. 277 Do. ,, pentapliylla Taguna , takuli ... Magiya , munnja „ 276. Do. „ quinata ... • • • „ deltoidea ... Gun • •• Do. „ aculeata ... Man -a tu 276 ... Do. Oplismenus col onus, Satin, jangli-mandira, „ 570 ... Seeds. Saccharum Sara Sarhar sarur Roxburgh, 82 . . . Do. in Bhabar. Scirpus Kysoor Kaseru „ 77 ... Roots. Asplenium polypo- Lingura • •• Fronds. dioides. Nephrodium odora- Kutra ... » • * Do. turn. 1 Descriptions of all these plants will be found in Part V. of my * Notes on the Economic Products of the North-Western Provinces,’ Allahabad, 1881. 720 HIMA'LAYAN DISTRICTS II. — Vegetable substances used in medicine or for INTOXICATION. A. — Drugs. B. — Narcotics and Spirit. A.-DRUGS. My object in the following list of the vegetable drugs fonncl and used in or exported from the Himalayan districts of these Provinces is to give a reference to a work where each one is botani- cally described and also to a work where their medicinal properties have been noticed . 1 It would be out of place here to do more than briefly indicate the therapeutic virtues attributed to them by European and Native practitioners. The following remarks 2 of Dr. Burton Brown on the vegetable drugs collected for the Lahore Exhibition will form a fitting introduction to this section of our subject : — “ The medicinal use of preparations of vegetable drugs has been for a long time of the greatest importance, and until a comparatively recent period the number of drugs obtained from plants and animals greatly exceeded that of preparations from the mineral kingdom. This depended on the fact that until chemical knowledge was fixed on a firm basis, it was only with great difficulty and after many failures that chemical products could possibly be obtained ; while, on the other hand, the different parts of plants to which a medicinal use was assigned were easily distinguished and procured without much trouble. In Europe, owing to the progress of science, mine- ral preparations are now most extensively made and used for medicinal purposes, and many of our most valuable drugs are derived from this kingdom. But in India the knowledge of chemistry is confined to those among the natives who have been instructed by Europeans, and therefore medicinal substances procured from the mineral kingdom are comparatively seldom made or used, except- ing by those who have been so taught ; or those mineral articles are used which are procurable without much skill in preparation and are often of little efficacy. The use of vegetable drugs would probably be the first to recommend itself to those seeking relief from 1 A full description of each plant or tree and a more detailed noticeof uses of each drug will be found in my “Notes on the Economic Products of the North- Western Provinces,” Part VII. * Panj. Products. OF THE NORTH-WESTERN PROVINCES. 721 pain and disease, because plants are everywhere at hand, their num- ber is very great, and their forms are distinctive and often peculiar, and in some cases they have been supposed to bear a more or less obscure resemblance to certain parts of the body, either in health or when diseased. Thus, in olden times, we find in Homer that Nestor used a poultice of onions, cheese, and meal, mixed with wine, to Macliaon’s wound ; and the former substance was used by the ancient Egyptians in cases of dropsy. The hellebore of Anticyra was long extolled by the Greek writers, and is said to have been used by Melampus of Argos to cure the daughter of king Proclus of melancholy. It has also been supposed that opium was the Nepenthe of Homer. “ Enough has been adduced to prove the antiquity of those sim- ples or Galenical preparations as medicinal drugs derived from the vegetable kingdom, and it is well next to consider in what manner the use of drugs was probably commenced. The use of each vege- table preparation was, probably, at first brought about by the expe- rience of individuals, each of whom had found that certain plants were useful in the diseases which afflicted himself or his neighbours, and this knowledge was more rapidly spread owing to the ancient custom of placing the sick in public roads and markets, so that passers-by might communicate information respecting such remedies as were employed in similar cases. As observed by Herodotus, in this way a knowledge of a great number of medicines would be acquired, at first chiefly of those which were indigenous to the coun- try, but gradually the drugs of other countries would become known, especially those which were found to be of undoubted efficacy in the disease for which they are used. Hence it is to be expected that there will be found a larger number of substances, which are inert or nearly so in a Materia Medica which comprises indigenous plants only, than in a collec- tion of drugs brought from a distance. Moreover, as the imported drugs must always be more costly than the indigenous ones, there will always be a tendency to substitute some indigenous substance which may resemble the foreign one in appearance or action, espe- cially as the description of the drugs or of the plants from which they are derived was formerly much less carefully attended to than now. Thus it will be seen, as above stated, that an Indian plant, 91 722 HIMA'LAYAN DISTRICTS Picrorhiza Kurrooa , has been substituted for the more remote 1 hellebore of the Greek physicians. Similarly a kind of Valerian takes the place of Asarabacca , and fruits of Gardenia that of the’ juniper. This substitution would certainly bring the kind of remedy in which it was employed into disrepute, as the substance used for adulteration would differ greatly from the original drug in its powers and mode of action. u Besides the above modes of ascertaining the natures of reme- dies, which, being founded on actual experience, must be termed improved methods, there is another mode called the Doctrine of signatures. This is founded on the belief that every natural substance possessed of medicinal virtues indicates by its external character the disease for which it should be employed. Tlius turmeric, rhubarb, and other roots, which have a brilliant yellow colour, were supposed to be specially useful in jaundice and diseases of the liver. Cassia fistula ( amaltds ), from the peculiar septa of the fruit resembling the valves of the intestines, is supposed to be especially destined for the cure of diseases of those organs ; and similarly, poppies, from the shape of their capsule, were sup- posed to be useful in diseases of the head ; and roses, from the colour of their petals, in those of the blood. Many small red or yellow Seeds, especially those of cruciferous plants, were supposed to be useful in cases of gravel, the deposit of which they sometimes resemble in appearance ; and sdlap misri is used in diseases of that organ to which the name of Orchis (applied usually to the plant) is assigned. The convoluted pod of the Helicteres Isora is employed in colic, since it is supposed to resemble the twisting of the coils of the intestines. But although it is probable that the use of differ- ent drugs was commenced in some of the ways already spoken of, yet at the present day the native physicians have adopted, with some modifications, the idea of Galen respecting the method of operation of medicines : this was, that the uses of all medicines were derived from their elementary or cardinal properties — namely, heat, cold, moisture, and dryness ; and that all diseases could also be classed under the above heads, but that in the treatment of dis- ease a medicine should always be employed which was of a con- trary nature to the disease treated. Thus a cold disease requires a hot remedy and the converse. It is probable that ignorance of the OF THE NORTH-WESTERN PROVINCES. 723 attachment to this theory (which is well known to native patients and haMms ) is often an obstacle to the employment of European medicines in the hands of European practitioners among natives, as either a remedy which they consider hot is employed for a dis- ease which is also considered hot, or the prescriber does not state whether the remedy given is a hot or cold one even when asked* Although the theory that medicine acts by being hot or cold only is entirely erroneous, yet it has so strong a hold on the confidence ■of many natives that, without some attention to it, it would be difficult in many cases to induce them to take the medicine ■ordered. “ The following is a list of some of the drugs employed, show- ing their nature according to native ideas, and also their real use in European medicine : — Scientific name. Phyllanthus Emblica, Linn. Rosa centifolia, Linn. Rosa alba, Linn. Citrus Aurantium, Linn. Tamarindus indica, Linn. Terminalia Chebula, Retz. Rhus Coriaria, Linn., Vernacular name. Reference. Real use. Cold medicines. Aonla, amlika Gul-surkh Gul-seoti Narangi Imli Harera Samak » Semecarpus Anacar- Bhilawa dium, Linn. Corylus Colurna, Findak Linn. Zingiber officinale, South Roxb. Moschus ... Mushk Aquilaria Agallocha, tJd Roxb. Amber .. Kahruba Hot medicines. Brandis, 124 „ 494 Drury, 1G3 Brandis, 387 Brandis, 454 „ 200 200 53 163 223 120 Astringent and acid purgative. ... Astringent and purga-. I tive. ...Astringent. ...jAstingent, tonic. ... Refrigerant. ..^Astringent. Ditto. Acrid. i ... Demulcent. I ... Aromatic. Ditto. Tonic. Ditto. i The references are to Brandis’ Forest Flora, Drury’s Useful Plants, Hooker’s Flora of British India , and the Pharmacopeia of India. 724 HIMALAYAN DISTRICTS Scientific name. Vernacular name. Reference. Dry medicines. Prunella (species) ... Ustukhudus Raw silk ...lAb-i-reshm Centaurea Behhen, Bahman Psoralea corylifolia, Babe hi Linn. | Cinnamomum zeyla- Dalcliini nicum, Bayn. Cinnamomum Tama- Kirkiriya la, Nees. Mentlia sativa, Padina Linn. Crocus satirus Linn. Zafran Hooker, II., 103 , Brandis, 375 ... „ 374 ... Phyllanthus Emblica, Aorila Linn. Silica (of the bambu), Tabashir Vilis vinifera (rai- Jzirishk sins). Camphor ... 'Kafur Onosma echioides, Gau-zaban Sm. Coriandrum sativum, Dhaniya Linn. Nymphaea stellata, Nilofar VVilld. I Moist remedies. ... Brandis, 454 )> 566 98 ••• Hooker, II., 717, Real use. Aromatic. Inert. Tonic. Ditto. Aromatic. Ditto. Ditto. Inert. Astringent. Inert. Demulcent. Aromatic. Tonic. Aromatic. Inert. “ From the above list it will be seen that many of the cold reme- dies aie what are used in European therapeutics as astringent medicines, while the hot remedies are principally aromatics, while remedies having various properties fall under the dry and moist categories.” A. Abrus precatorius, Linn.— A Indian liquorice— GuncM, raM, rcitnaliya; described by Baker in Hooker, FI. Ind., II., 175. The red or white seeds are used as a weight and as beads in a rosary ; hence the specific name, and also for fistula m native practice .The root is used as a substitute for, and to adulterate, true liquorice, and an ex- tract from it, like that from the latter, is officinal. Pharm., 74, 446. Abutilon indicum, Don. — Kangai ; described by Masters in Hooker, I., 326. The leaves yield a mucilaginous extract used as a demulcent. The root is used in leprosy and in infusion as a cooling di ink, and the seeds ai e considered laxative and are given in coughs. OF THE NORTH-WESTERN PROVINCES. 725 Acacia arabica, Willcl. — Babul; described by Baker in Hooker, 11., 293. This tree and others of the same genus yield a gum which is used as a substitute for gum-arabic. The bark is considered a powerful astringent and is used as a substitute for oak bark, and the leaves enter into preparations for sores and cutaneous affections Pliarm., 62, 77. Acacia Catechu, Willd. — Khair; described by Baker in Hooker, 11. . 295 . The extractcalled hath yields an active principle consisting of mimo tannic acid and catechu and is used as an astringent and tonic. Pharm., 62, 63. Achyranthes aspera, Linn. — Chirchira ; described by Drury (U. P., 4). The seeds are given in cutaneous diseases, the flower- ing spikes in hydrophobia, the bruised leaves as an application for stings, and the dried plant in colic. Pharm., 184. Aconitlim ferox, Linn. — Aconite — Mitha-zahar (bazaar), mau- ra-bikh (root), rnahitr; described by Hooker and Thomson, I., 28 : see also Pharm., 3, 434. This species is found above 10,000 feet and is largely export ed. It yields a deadly poison used in rheumatism and neuralgia. Aconitum heterophyllum, Linn. — Aconite — Atis (root) ; de- scribed by Hooker and Thomson, I., 29. This species also grows at high elevations above 8,000 feet. It is used as a tonic, febrifuge, and aphrodisiac, and with A. Lycoctonum ( Bish .) and A. Napellus ( Piliya-kachang and dudliiya , the roots), occurring at similar eleva- tions, is exported in small quantities to the plains. Pharm., 4, 434. Acorus calamus, Linn. — Gur-bach, bach (root); described by Drury (U. P., 13). The dried rhizomes are used as a bitter, aromatic tonic in fevers, rheumatism, and dyspepsia, and are exported to the extent of about 26 tons every year from the Kumaun forest division. Pharm., 249. Actiniopteris radiata. — The Asplenium radiatum of Boyle — Mor-pankhi, Mor-pachh. This fern is used as an anthelmintic. The root of Goniopteris proliferum is used in fevers and that of JS ephrolepis cordifolia in electuaries. Adiantum Capillus-veneris, Linn. — Maiden’s hair fern — the mubdraka of Kumaun. This fern and A. venustum ( Pareseoslian , hansrdj) are exported from the Kumaun forest division, both as a 72$ HIMA’LaYAN districts medicine and a dye, to the extent of ahont 10 maunds a year. They are both considered astringent, aromatic, tonic, and emetic in large doses. The rhizomes and dried leaves of various other species of ferns are sold in the bazaars under the names iskidikandriy4n and baliikanbim, corruptions of the names Seolopendrium and Polypodium iEgle Marmelos, Corr. — Bael — Bel ; described by Hooker, I., 516. The fruit is a specific in atonic diarrhoea and dysentery. Pharm., 46, 441. Albizzia Lebbek, Benth. — Siras; described by Baker in Hooker, II., 298. The bark is applied to sore eyes and the root in making an ointment used in ophthalmia and in cutaneous affections and is given in decoction for diarrhoea. Allium Cepa, Linn. — Onion — Piydj. This common vegetable is used in special diseases as a stimulant, diuretic, and expectorant. A. sativum — Garlic — Lalisan — is supposed to have similar proper- ties in native medicine. Aloe indica, Royle — Gliikawav ; described by Drury (U.P., 26). The bitter inspissated juice contains a cathartic principle. A. per- foliata, Hoxb., occurs rarely in gardens in Kumaun. Pharm., 242. Alstonia scholaris, R. Br. — Chhatiy'dn, satiyiin of the Bhabar ; described by Drury (U. P., 29). The bark is a powerful tonic, an- thelmintic, and antiperiodic : the milky juice is applied to ulcers and mixed with oil in ear-ache. It is also valuable in dysentery and diarrhoea. A. lucida, the diidhi of Kumaun, is found on the first range and is said to possess similar properties. Pharm., 137, 455. Amarantus farinaceus and others of the same and allied genera are held to possess diuretic and purifying properties. Pharm., 184. Anagallis arvensis, Linn., var. ccerulea — Pimpernel — •Jonkh- mari, jainghani; described by Drury (F. P., II., 128). Triturated it is used to intoxicate fish and to expel leeches from the nostrils. It is also used in cerebral affections, leprosy, hydrophobia, and dropsy. Anatherum muricatum, Beauv. — Kas or khas ; described by Drury (U. P., 38). The roots are given in infusion as a febrifuge and in powder in bilious affections and also yield an oil. OF THE NORTH-WESTERN PROVINCES. 7*27 Alieilema tuberosa, Ham., Murdannia scapiflora , Hoyle Musli-siyah and safed (roots). The rootlets furnish an astringent, tonic preparation and are exported for this purpose from Ivumauri. Pliarm., 235. Anisomeles ovata, R. Br — Gobara; described by Drury (F. P., II., 557). This plant has carminative, astringent, and tonic pro- perties and also yields an oil. Pharm., 168. Anona squamosa, Linn. — Custard-apple — Sitaphal, sharifah . Hooker, FI. Ind., I., 63. The powdered seeds mixed with flour of gram and water make a hair-wash and the bruised leaves with salt make a cataplasm to induce suppuration. Artemisia vulgaris, Linn. — Pdti; described by Roxburgh, 599. This species is common in Kumaun ; it has stomachic and tonic pro- perties and is given in fevers. A. scoparia, Wall. — Jhao — has simi- lar uses. Pliarm., 122, 126. Argemone mexicana, Linn. — Kantela ; described by Hooker and Thomson, I., 117. An introduced plant now completely naturalized. The seeds yield an oil, used as a mild, cooling laxa- tive. The juice of the plant is diuretic, relieves blisters and heals excoriations and indolent ulcers. Pliarm., 22, 440. Argyreia speciosa, Choisy — Gao-patta, bich-tarcik ; found wild in the Delira Dun and the Bhabar, described by Drury (U. P., 49). The leaves are used as emollient poultices for wounds and externally in skin diseases, having rubefacient and vesicant properties. A. setosa occurs in the Sarju valley near Kapkot. Pharm., 157. Artocarpus iiitegrifolia, Linn. — Jack-tree kuthcil / described by Brandis, 425. The juice of the trunk is used in glandular swell- ings the voung leaves in skin diseases, and. the root in decoction in diarrhoea. Asparagus adscendeus, Roxb. Khairuwa ; desciibcd by Rox- burgh, 291. The tuber of this species is used as a demulcent and tonic. Asparagus racemosus, Willd. — Sitrdwal (plant), bozidan (root), haliyun (fruit). The root is used in special diseases and has also demulcent properties in veterinary medicine. I liaiin., 243. 728 bimXlayan districts B. Bcenninghausenia albiflora, Reicli. — White rue — Pisu-ghds ; described by Hooker, I., 486. Exported and used as a medicine for poultry. Balanites Roxburgdiii, Planch. — Inguwa; is found in Dehra Dun (Royle), and is described by Bennett, I., 522. The leaves have anthelmintic properties and the bark is used as a cattle medicine. The unripe drupes have strong cathartic proper- ties, but when ripe are pleasant and the seeds are given for coughs. Baliospermum indicum, Dne. — Croton — Jangli jamdlgota ; described by Drury (P. P., III., 192). The seeds are used as a pur- gative, but in over-doses are an acro-narcotic poison. They are also used externally as a stimulant and rubefacient. The oil is a power- ful hydragogue, cathartic, and useful for external application in rheumatism. Pharm., 201. Barleria cristata, Linn. — Gorp-jlba , kdla-bansci (leaves) ; described by Roxburgh, 471. The seeds are supposed to be an anti- dote for snake-bites and the roots and leaves are used to reduce swellings and in coughs. Bassia butyracea, Roxburgh (see page 715 anted). The butter is used for rheumatism and as a pomade and lip-salve. The oil of B. latifolia is used for soap and emollient ointments and the spirit distilled from the flowers as a stimulant. Pharm., 130 131. Bauhinia variegata, Linn. — Khwairdl, kachndr ; described by Baker, II., 284. The root in decoction is useful in dyspepsia and flatulency ; the flowers with sugar as a gentle laxative; and the bark, flowers or root triturated in rice-water as a cataplasm to promote suppuration. Benincasa cerifera, toavi Bhunja^ pethct , kumhra (see page 700). This gourd has alexipharmic and tonic properties and is given in dysuria in native practice. Berberis Lycium, Royle— Kashmal ; described by Hooker and Thomson, I., 110. The root is known as king ora- hi-jciT in the hills and ddr-hald and ddr-cJwb in the plains. An extract from the roots OF THE NORTH-WESTERN PROVINCES. w m 729 is known as rasaut , and it is chiefly from this species that it is obtained in Sirmor and Gfarhwal. The medicinal extract is highly esteemed as a febrifuge and as a local application in eye-diseases. It is said by some to have been known to the ancient Greeks and Romans as ‘ Lykion,’ and pots labelled “ Best Himalayan Lykion” have been found in the ruins of Pompeii, but this identification is disputed. In Kumaun B. aristata and B. asiatica yield rasaut. The average annual export of the root from the Kumaun forest division is about two maunds and from Grarhwal about double the quantity. Pharm., 13, 436. Boerhaavia diffusa, Linn. — Gdcla-purna ; described by Drury (F. P., III., 34). The root of this common weed is given in infu- sion as a laxative, anthelmintic, and cooling medicine. Pharm., 185. Bombax malabaricum, D.C. — Senial ; described by Masters in Hooker, I., 349. The gum is given in asthenic cases ; the root fur- nishes one of the musali and is used as a stimulant and tonic and in large doses as an emetic, and the leaves are employed as an aphro- disiac and in. special diseases. Pharm., 36. Boswellia thurifera, Cole — Indian frankincense — the salhi of Grarhwal ; described by Drury (U. P., 84). The gum is prescribed with clarified butter in special diseases, with cocoa-nut oil for sores, and as a stimulant in pulmonary diseases. Pharm., 52. Brassica nigra, Koch. — Black mustard — Kali sarson. This and the allied species, B. alba and B. juncea, are frequently used in medicine as rubefacients and vesicants. Pharm., 25. Briedelia mentana, Roxb. — Kangnaliya ; described by Rox- burgh, 705. Reported to possess astringent and anthelmintic pro- perties and found at 3-4,000 feet, Buchanania latifolia, Roxb, — Chironji ; described by Brandis, 127. The oil extracted from the kernels of the fruit is used as a 'substitute for almond oil in native medicinal preparations and con- fectionery. Butea frondosa, Roxb. — Balds, dhdk; described by Brandis, 142. The inspissated juice obtainable by incision is used as a substitute for kino : the seeds as a vermifuge and anthelmintic and when 92 730 HIMALAYAN DISTRICTS made into a paste as a remedy for ring-worm. B. parvifora maula — has similar properties. Pharm., 73, 74, 79, 446. Buxus sempervirens, Linn. — PapH , shamdj ; described by Brandis, 447. A tincture from the bark is used as a febrifuge, c. Csesalpinia Bondncella, Fleming — Karaunj ; described by Baker, II., 254. The kernels are used as a tonic in fevers and made into an ointment with castor-oil and applied externally in hydrocele. An oil is extracted from the leaves which is used in palsy and rheumatism. Pharm., 68, 446. Callicarpa arborea, Roxb. — Ghiwala ; described by Drury (U. P., 97). The bark is aromatic and bitter and is applied in decoction in cutaneous affections. Calosanthes indica, Blume — Pharkath ; described by Drury (U. P. 100). The bark is astringent and used in applications to cuts and fractures. The seeds are applied to abscesses and the offi- cinal syonak seems to be procured from the leaves. Calotropis procera, R. Br. — Maddr , ah; described by Brandis, 331. The root, bark, and inspissated juice are used extensively for their emetic, diaphoretic, alterative and purgative properties. Pharm., 141, 457, 458. Canna indica, Linn. — Indian shot — Kiwara ; described by Drury (U. P., 106). The root is used as a diaphoretic and diuretic in fevers and dropsy. Cannabis indica, Linn. — Bhang. See intoxicating drugs, posted, and Pharm., 216, 463. Capparis horrida, Linn. — Ulta-kdnta , bipuwa-kanta ; described by Hooker and Thomson, I., 178. Found in the Bhabar. A cata- plasm of the leaves is considered useful in boils, swellings, and piles. Capsicum frutescens, Linn. — Mircha , kursdni ; prescribed in native practice in gout, dyspepsia, cholera, and ague. Careya arborea, Roxb. — Vakamba, kdmbhi ; described by Clarke in Hooker, II., 511. The flowers are given as a tonic in sherbet after childbirth. Carum copticum, Benth. — Lovage — Ajwdin ; described by Clarke, II., 682. This plant possesses valuable stimulant, 93 OF THE NORTH-WESTERN PROVINCES. 731 carminative and antispasmodic properties ; it aids digestion, and is used in colic, colds, rheumatism and fever and is also esteemed as a diuretic. Pharm., 98, 99, 447. C. Carui, Linn. — Carraway — Kdlajira — (Hooker, l. c., 680) occurs at the same elevations (8-10,000 feet) and possesses similar virtues. Both are exported to the plains. Cassia Absus, Linn. — Bctndr ; described by Baker, II., 265. The seeds are used in powder applied beneath the eyelids or in the form of an ointment in ophthalmia. Pharm., 78. Cassia Fistula, Linn. — Kitola, itola , rdj-briksh of the Bhabar ; described by Baker, II., 256. This tree yields the commonest cathartic used in native medicine. The pulp around the seeds is a valuable laxative, the flowers are used as a febrifuge made into a confection known as gdl-kand , and the root is a strong purgative. The bark and leaves are applied to cutaneous eruptions. Pharm., 65. Cassia Sophera, Linn. — Bandr of the Bhabar ; described by Baker, II., 262. The bark, leaves, and seeds of this tall weed are cathartic and the juice of the young leaves is applied in ringworm. C. Tora has the same native name in Kumaun ; its leaves are eaten by men and animals and the seeds are used as a remedy for itch. Pharm., 78. Cedrela Toona, Roxb. — Tuni ; described by Drury (U. P., 128). The bark is astringent and has been found a fair substitute for qui- nine in fevers and bowel complaints, especially with young children. Pharm., 55. Celosia argentea, Linn. — Sirali, sarwdli, gogiya ; described by Drury (F. P., III., 15). The seeds are used chiefly in special dis- eases. Chavica Roxburghii, Miq. — Piper longum, Linn, fruit pipla- mill ; described by Drury (U. P., 131). P. longum, var. silvaticum, grows wild and the fruit is largely exported as a condiment and a stimulant in medicine. Pharm., 208. Chenopodium album, Linn. — Bhatuwa ; described by Drury (F. P., III., 5). It is used in special diseases and as a laxative in spleen and bilious disorders. 732 HIMALAYAN DISTRICTS Cicer arietinunb Linn. — Gram — Ghana (see page 693). The hairs of the stem and leayes exude an acid used as a refrigerant in fevers ; the seeds are considered stimulant and when roasted are used as a substitute for coffee berries. Pharm., 80. Cinnainomum Tarnala, Nees — Taj (bark), tejpdt (leaves) ; described by Brandis, 374. The bark and leaves are used as a car- minative, aromatic and stimulant in coughs and dyspepsia and generally as a substitute for true cinnamon. Pharm., 196. Cissampelos Pareira, Linn. — Pari ; described by Hooker and Thomson, I., 203. The dried root has diuretic, tonic and slightly aperient qualities and forms part of the pili-jari or ‘ yellow-root’ of the native Materia Medica. The leaves are applied to abscesses. Pharm., 7. Citrullus Colocynthis, Schrad. — Indr dy an (see page 701). The fruit affords a safe and active cathartic in hepatic and visceral congestion. C . Hardwickii , the air-alu of Kumaun and pahdriindrdyan of the plains, has similar properties. Pharm., 94. Citrus Anrantium, Linn. — Orange — jT dr any i — (2) C. medica — Bijaura — (3) G. var. Limonum — Jdmira — and (4) C. var. Limetta — Amritphal — are all used in medicine as tonics and purifiers of the blood, refrigerants in fevers, Savouring materials in infusions, pomades, &c., anti-scorbutics, stomachics, and carminatives. The juice is exported from the Kumaun forest- division to a great extent every year. Pharm., 42, 43, 45. Cleome viscosa, Linn. — J anyli-harhar ; described by Hooker and Thomson, I., 170. The seeds are considered anthelmintic ; the leaves are used as a vesicant, and boiled in clarified butter are applied to wounds, and the juice to ulcers. The root is administered in decoc- tion as a febrifuge. This plant is often confounded with Gy nan- dr op sis pentaphylla. Clerodendron serratum, Spr .— Ganth-baharanyi; described by Drury (U. P., 141). The leaves of this common plant are boiled in oil for applications in ophthalmia : the roots boiled in water with ginger and coriander are given in nausea, and the seeds are slightly aperient. The leaves of C. infortunatum, Linn .—Bhat— also aftord a cheap and efficient tonic and antiperiodie. Pharm., OF THE NORTH-WESTERN PROVINCES. 733 164. C. Siphonanthus, R. Br.— Ami— also occurs and its roots and leaves are officinal in native practice. Cochlospermum Gossypium, D. G. Ivatera , gajra ; described by Hooker and Thomson, I., 190. This small tree yields a gum used as a demulcent in coughs and special diseases. Pharm., 27. Colocasia antiquorum, Schott— Kachu, arwi ; described by Drury (U. P., 155). The inspissated juice of the petioles is a capital styptic for wounds. Pharm., 250. Cominelyna obliqua, Don. — Kanjura, lcdna. The root is use- ful in vertigo, fevers, and bilious affections, and is said to be used as an antidote to snake-bites. Cor chorus olitorius, Linn. — Banphal ; found in Dehra Dun ; described by Masters in Hooker, FI. Ind., I., 397. The leaves are emollient and used in infusion as a refrigerant in fevers and special diseases. The dried plant toasted and powdered is used in visceral obstructions. Cordia latifolia, Boxb.—Bairdlu, baurdla; described by Drury (U. P., 160). The fruit is used as an expectorant and astringent. Pharm., 157. Cordia Myxa, Linn .—Kocla; described by Drury (U. P., 161). The pulp of the fruit is used as a laxative and the seeds mixed with oil are deemed a specific in ringworm. The juice of the bark in infusion is given with cocoa-nut oil in gripes. Pharm., 157. Coriandrum sativum, Linn. — Coriander — Dhaniya ; described by Clarke, II., 717. The dried ripe fruit and the volatile oil are both used in medicine as an aromatic stimulant in colic and the like. Pharm., 101. Costus speciosus, S. M .—Keyu, keoli, kut-shirm (root) ; des- cribed by Drury (U. P., 164). From the root a strengthening tonic is made and it is also used as an anthelmintic. Crinum asiaticum, var. toxicavium , Herb. — Chindar, kanwal , pindar, Icanmu ; described by Roxburgh, 283. A valuable emetic ; in small doses nauseant and diaphoretic. The dried sliced roots are also emetic i the leaves with castor-oil are used m lheumatism and the juice in ear-ache. Pharm., 234. 734 HIMALAYAN DISTRICTS Cucurbita Pepo, Linn. — Bhunga, petha ; and C. maxima — ga- duioa (see page {02). Both these gourds are used in medicine ; the leaves as applications for burns and the seeds as anthelmintics. Pharm., 96. Cuminum Cyminum, Linn. — Jira (see page 705.) Both fruit and oil possess carminative properties allied to dill and coriander : the seeds are largely exported to the plains. Pharm., 108. Curculigoorchioides, Groertn. — Petdri; described by Drury (F. P., III., 458). The tuberous roots are some of those known as musli-siyah and are held in the highest esteem by native physicians as a specific in special diseases. Pharm., 235. Curcuma longa, Roxb. Turmeric — Haldi (see page 706.) This is much used as an application in bruises ; the fresh juice as an anthelmintic ; the fumes of the burning root in coryza and the root in decoction for relieving catarrh and purulent ophthalmia. Pharm., 231. Cymbopogon Martini, Munro— Bujina, pdla-khari. The oil, known as raus-ha-tel and Nimar oil, enters largely into native per- fumeiy. The loots of C. laniger Piriya — are also used as an aro- matic stimulant (see Drury, F. P., III., 641). Pharm., 256. Cynodon Dactylon, Pers.— Ddb ; described by Drury (U. P., 180). This glass yields a cooling decoction from the roots and young leaves found useful in fever. Cyperus rotundus, Linn. — Motha ; described by Drury (U. P., 182), The roots are held to be diaphoretic, diuretic, and astringent Pharm., 250, D, Dalbergia Sissoo, Roxb. — Si&u ; described by Drury (U. P., 186). The leaves and saw r -dust in decoction are esteemed in erup- tive and special diseases and to allay vomiting. The oil is also applied externally in cutaneous affections. Datisca cannabina, Linn. — Bujr-bhanga , bhang-jala (roots) ; described by Clarke, II., 656. The roots are exported as a medi- cine useful as a sedative in rheumatism and to aid in dyeing red. OF THE NORTH-WESTERN PROVINCES. 735 Datura alba, Linn. — Dhatura ; described by Drury (U. P., 188). The leaves and seeds are used as anodynes and antispasmo- dics. Pharm., 175, 460. Daucus Carota, Linn —Carrot— Gdjar. This common vege- table is used as a poultice for ulcers and boils. Delphinium Brunonianum, Boyle — JSepdri; described by Hooker and Thomson, I., 27. Occurs at 14,000 feet and is exported for its highly musk-scented leaves, used in native perfumery and for temple offerings. Dendrocalamus strictus, Nees— Bambu— Bdns, bdsila; described by Brandis, 529. The bambu yields a siliceous secretion 11 in the joints of the female plant, called bdns-loehan or tabashir , considered by the Baids to be useful as a stimulant and aphrodisiac. The root is said to be a diluent, the leaves are used as an emenagogue and anthelmintic and the dried steins as splinters in surgery, which seems to be the only really valuable use that the products of the bambu are put to in medicine. The product bans- lochcin is exported in small quantities from Kamaun. Pharm., 2o6. Desmodium triflorurn, D. C ,—Kudaliya ; described by Drury (U. P., 190). The fresh leaves are applied to wounds and abscesses that do not heal well. Dioscorea versicolor, Wall. — Yam Genthi, gcijir. Thetubeis yield a farinaceous food for invalids. Diospyros Melanoxylon, Boxb. — Tendu ; described by Bran- dis, 294. This and the other species of ebony afford an astringent from the bark which is used in decoction in diarrhoea, dyspepsia, and the like as a tonic. Phann., 132. Dolichos sinensis, Linn.— Lobiya (see page 695). This and other similar pulses are prescribed in special diseases and as stomachics. Drosera peltata, Gm .—MuJcha-jali ; described by Clarke, II., 424. The leaves bruised and mixed with salt are used as a blister in Kumaun. E. Eclipta erecta, Linn.— Moch-kand, bhangra, bdbri ; described by Drury (U. P., 202). The fresh plant is applied with sesamum 736 HIMALAYAN JDISYRI£TT§ oil m elephantiasis ; the expressed juice in affections of the liver, spleen, and dropsy, and in large doses as an emetic ; also as a black hair-dye. The average annual export from the Kumaun forest division is about 5 maunds. Pharm., 128. Elseagnus umb ellat a, Thunb. — Ghiwain , kankol common in the hills from the Jumna to the Sarda ; described by Brandis, 390. The seeds are reported to be used as a stimulant in coughs, the expressed oil in pulmonary affections, and the flowers as a cardiac and astringent. .Elgeodeildron glaucum- Pers. — Shauriya (Kumaun) and jamu- w a (Delira Dun) ; described by Roxburgh, 214. The root is held to be an antidote in snake-bites ; a decoction or cold infusion of the fresh bark of the roots is applied to swellings. Embelia robusta? Roxb. — Bayabirang (fruit) ; described by Brandis, 284. The fruit is said to be used to adulterate black pepper like that of E. Ribes , which has the same vernacular name and is given as an anthelmintic and internally for piles. The greater portion of the bayabirang exported from Kumaun seems to be the fruit of My r sine, africana . Eragrostis cynosuroides, Ret. — Bdbh. A common grass said to possess diuretic and stimulant virtues. Eugenia Jambolana? Lam. — Phaunda ; described by Brandis, 233. The leaves and bark are astringent. Euphorbia pentagona, Bois.— Sehund. This and other species of the same genus yield an acrid milky juice having cathartic and anthelmintic properties. Pharm., 204. Exacum tetragonum, Roxb. — Titakhana ; described by Rox- burgh, 133. It is used as a tonic in fevers and a stomachic bitter. Pharm., 149. F. Feronia Elephantum, Corr. — Kath-bel; found in the Siwaliks and Bhabar ; described by Drury (U. P., 220). This tree yields a gum used for the same purposes as gum-arabic ; and the leaves are- carminative and stomachic, especially with children. Pharm., 48, Ficus Carica> Linn. — Fig — Anjir ; described by Brandis, 41§„ The fruit is used medicinally as a laxative. OF THE NORTH-WESTERN PROVINCES, 737 Ficus indica, Roxb. (F. bengalensis, Linn.)— Bar, bat ; described by Drury (U. P., 221). The juice collected from incisions in the bark of the banyan-tree is considered a specific in cracked heels, excoriations, and sometimes for toeth-ache, lumbago, and croup. Pharm., 217. Ficus religiosa, Linn. — Pipal ; described by Drury (U. P., 225). The young shoots are used as a purgative and have some rej^ uta- tion in skin diseases ; the bark of this and the preceding is used as a tonic in desoction. The seeds are given in electuary as a purifier of the blood. Ficus hispida, Linn.,/. — Kagoha,gobla, dhtira, totmila; described by Brandis, 423. The fruit, seeds, and bark are possessed of emetic properties. Pharm., 217. Ficus glomerata, Roxb. — Gular ; described by Brandis, 422, The bark is used as an astringent and a wash for wounds. The milky juice is given in piles and diarrhoea and in combination with sesamum oil in cancer. The root is useful in dysentery. Flacourtia sepiaria, Roxb. — Kandai; described by Brandis, 18, This tree yields an antidote to snake-bites from an infusion of the leaves and roots : the bark triturated in sesamum oil is used as a liniment in rheumatism. Fceniculum vulgare, Linn. Fennel — Sonf; described by Clarke in Hooker, II., 695. It is used as a carminative and stomachic, cultivated. Pharm., 100. Fraxinus floribunda, Wall. — Angu ; described by Brandis, 302. A concrete saccharine exudation (manna) from the stem is obtained by incision and is a substitute for the officinal manna. Pharm., 136. Fumaria parviflora, Lam.; Var. Vaillantii, the Khairuwa of Ku- maun, also known as pitpdpra , mijcilu ; described by Hooker, /., and Anderson in Hooker, I., 128. The dried herb is employed as a diuretic, anthelmintic, diaphoretic, and aperient, especially as a blood purifier. The average annual export from the Kumaun forest division is about 32 maunds. G. Gentiana Kurroo, Royle. — Kuru , kutkb — Llimalayan gentian. This plant occurs near the snows. There are four or five allied species, 738 HIMALAYAN DISTRICTS all of which are exported to the plains to the extent of about five tons a year, and are there sold as a valuable bitter tonic. See Royle, 111. Bot., Him. Moun., pi. 58, fig. 2, and Pharm., 149. Geranium ocellatum, Camb . — Bhdnd; described by Edge- worth and Hooker, / ., in Hooker, I., 433. A very common plant in Ivumaun, which possesses diuretic and astringent pro- perties. Gloriosa superba, Linn. — Bish nangal , bish ningala; described by Drury (U. P., 234). The root is used in special diseases, but is said to be poisonous in large doses. Pharm., 242. Gmelina arborea, Roxb. — Kumbhdr , gumbhar ; described by Drury (U. P., 234). The root is given in coughs, rheumatism, and special diseases, and is said to have anthelmintic properties like A. asiatica. Pharm., 164. Gossypium herbaceum, Linn. — Cotton — Kapds. The down of this well-known shrub is applied to burns ; the seeds to increase milk, also in epilepsy and as an antidote to snake-poison ; the root as a diuretic, emenagogue, and demulcent, and the leaves in decoction as a tonic in fever and diarrhoea. Pharm., 33. Grewia asiatica, Linn. — Pharsiya ; described by Masters in Hooker, I., 386. The leaves are used as an application to pustular eruptions and the fruit in sherbet as a refrigerant in fevers and a gargle for sore-throat. Gynandropsis pentaphylla, D. C. — Kathal parhar; described by Hooker,/., and Thomson in Hooker, I., 171. It occurs common in the Bhabar ; the leaves are used as a rubefacient and vesicant ; the expressed juice is given with salt in earache ; the seeds in powder are given with sugar internally in fevers and bilious complaints, and the entire plant with sesamum oil is used as an ointment in cutaneous affections. Pharm. 25. This plant is often confounded with Cleome viscosajn native shops. H. Hedychium spicatum, Smith — Kachur-kachu, kapdr-kachri, ban- lialdi. It possesses carminative and stimulant properties and is especially used as a cattle medicine : it is exported from Kumaun to the extent of a few tons annually. Pharm., 232. OF THE NORTH-WESTERN PROVINCES. 739 Helicteres Isora Linn. — Jhonkha-plicil , maror-phal; described by Masters in Hooker, I., 365. The seeds accordingto ‘ thedoctrine of si e-natures’ are considered useful in colic and diarrhoea and as a blood O purifier: and are exported from the Kumaun forest division to the extent of about a ton per annum. Heliotropium brevifolium, Wall. — Safed-bhangra, chiti phul. The whole plant is laxative and diuretic ; the juice is used as an application to sore-eyes, gum-boils and sores generally to pro- mote suppuration and as a cure for the sting of nettles and insects. Herpestis Monniera, H.B.gtf K. — Jal-mm; described by Drury (U. P., 249). A dose of six mdshas of the leaves steeped in water is an esteemed aperient ; the water may be used as an embrocation in skin diseases and croup, and the juice with kerosine-oil is used in rheumatism Pharm., 161. Hiptage Madablota, Goertn. — Aita-lugala ; described by Hooker, I 418. The leaves are esteemed useful in cutaneous diseases. Holarrhena antidysenterica, R. Br.—Kudr and moriya of Bijnor and IciU 3 r, Jcuda , kuva of Kumaun; described by Brandis, 326. The bark is a specific in dysentery : hence the name, and the seeds are also said to possess similar properties. Pharm., 137, 455. Hordeiim hexastichon, Linn. — Barley— Jau. The husked seeds form pearl barley, a favourite food for invalids and in decoction a drink in fevers. Pharm., 253. * Hymenodictyon excelsum, Wall. — Bhulan, bhalena , bhamena, dhauli; common in the Kota Dun; described by Brandis, 267. The inner coat of the bark possesses the bitterness of cinchona and its astringent properties. Pharm, 117. HyoscyamilS niger, Linn. — Henbane — Kliorasani ajwdin (seeds) ; occurs wild and is also cultivated. The seeds are given in native medicine as an anodyne and sedative in mental diseases. Pharm., 178. I. Ichnocarpus frutescens, R. Br. — Dddhi ; described by Drury (U. P., 259). The root possesses alterative, tonic properties and is employed as a substitute for sarsaparilla : the stalks and leaves are used as a decoction in fevers. Pharm., 138. 740 HIMA'LAYAN DISTRICTS J. Jasminum grandiflorum, Linn. — Jdhi; very abundant in low valleys ; described by Brandis, 313. The flowers and their essence are used as an application in skin diseases, headache and weak eyes : the leaves are used in toothache. Other species of this genus are also found in Kumaun and are employed in making perfumed waters. J atropha Curcas, Linn. — Safed ind; described by Drury (U. P., 27 6). The oil from the seeds is used as a purgative, but is uncertain : it is also applied diluted in rheumatism : the leaves warmed with castor-oil form a poultice for bruises : the seeds in over-doses are poisonous, and the milky juice is used to destroy maggots in sores on sheep. Pharm., 203. Juglans regia, Linn. — Walnut — Akor, akhrot , kharot. The bark is used as an anthelmintic : the leaves are astringent and tonic and in decoction a specific in strumous sores : the fruit is given in special diseases and rheumatism. Justicia Adhatoda, Linn. — Bashing ; described by Drury as Adhatoda vasica (U. P., 16). The flowers, leaves, and roots are considered antispasmodic and anthelmintic; the juice is found useful in pulmonary affections, and a tincture is also commonly given as an expectorant. Pharm., 162. K. Kydia calycina, R. W.—Puta ; described by Masters in Hooker, 1., 348. The bark is mucilaginous and is used to clarify sugar. L. Lepidium sativum, Linn. — Cress — Halang. The seeds of this common vegetable are used as a tonic laxative and antiscorbutic and as a gentle stimulant in indigestion. Lilium wallichianum, Royle — Findora. The dried bulb scales possess demulcent properties and are used like salep in pectoral complaints. Limonia acidissima, Linn. — Bali ; described by Hooker, I., 507. The root is purgative, sudorific, and used in colic : the leaves in epilepsy and the dried fruit as a tonic and disinfectant. Pharm., 43. Linum usitatissimum, Linn. — Flax. The seeds are the linseed of the pharmacopoeia, of which the uses are well known. Pharm., 37» OF THE NORTH-WESTERN PROVINCES. 741 M. Mallotus phillipinensis, Miill. — Roini, roli ; described by Drury as Rottlera tinctoria (U. P., 378). The powder on the seeds is a valuable anthelmintic, vermifuge, and purgative. Pharm., 202 . Malva rotundifolia, Linn. — Sonchala ; described by Masters in Hooker, I., 320. The seeds are demulcent and are used especially in bronchitis, inflammation of the bladder, and haemorrhoids, and externally in cutaneous affections and coughs. Malva sylvestris, Linn. — kanji , tilchuni ; described by Masters in Hooker, I., 320. It is a valuable demulcent in pulmonary affec- tions and a substitute for the marsh mallow of Europe. Mangifera indica, Linn.— Mango— Arnb. The sliced rind of this well-known fruit is astringent and used as a stimulant tonic in debility of the stomach : the kernels are styptic in haemorrhoids, astringent in diarrhoea, and tonic in fever. Pharm., 59. Melia Azedarach, Linn. — Bakayan, dek, jek, betain ; described by Brandis, 68. The bark of the root and the pulp of the seeds are anthelmintic in small doses and poisonous in large doses. Pharm., 55. Melia indica, Linn — Nim; described by Brandis, 67. The bark, leaves, and seeds are all really valuable ; the bark as a febrifuge and substitute for quinine ; the leaves as a cataplasm for wounds and sores; and the seeds for their oil, which is used as an anthelmintic and an application to foul sores. Pharm., 55. Mentha viridis, Linn. — Spearmint — Pahari pudina. The oil obtained by distillation from the fresh herb in flower is inferior only to peppermint and is useful in cholic, nausea, and flatulence. Pharm., 166. Mimosa rubicaulis, Lam.— Agio, ; described by Baker in Hooker, II., 291 ; M. pudica, Linn. — Lajawanti; described by Hooker ( l.c .) The seeds of both are used as purifiers of the blood, and the leaves are given in infusion in piles, and pounded they are applied to burns. Mirabillis Jalapa Linn. — Gdl-bdnsa. The root forms a safe and efficient purgative equal to jalap, and the leaves are applied to abscesses. Completely naturalised in Kumaun. Pharm., 184. 742 HIMALAYAN DISTRICTS Momoidica charantia, TV illd. — Karela ; described by Druary, U. P., 306 (see page 700). Used as a laxative and in preparation as an ointment for sores and the juice of the leaves as an anthelmintic. Moringa pterygosperma, Gcertn. — Sahajnct— Horse-radish tree ; described by Hooker, II., 45. The fresh roots are vesicant and rubefacient and useful in rheumatism. Used internally, the fresh juice of the roots has stimulant and diuretic properties and the root in decoction furnishes a gargle. The seeds yield a fine oil useful in rheumatism, and the tree itself a gum used as an anodyne in headache and as an application to buboes. Pharin., 61. Morus indica, Linn. — Indian mulberry — Tutri ; described by Brandis, 408. The fruit forms a sherbet used as a refrigerant and the bark a vermifuge and purgative. The fruit of M. serrata, Roxb. — Kemu — and M. Icevigata, Wall., Siyah-tut — is said to possess similar properties. Brandis, 409. Mucuna pruriens, JD. C.— Cowhage— Goncha; described by Baker in Hooker, II., 187. The hairs of the legume are mechanically anthelmintic and are given in round worm : see Pharm., 73. The seeds are given with milk in special diseases and snake-bites and the leaves as a vermifuge. M. atropurpurea , the ba Iclhalci of Kumaun, is said to possess similar properties. Murraya Kcenigii, Spreng. — Gani , gandla; described by Hooker, I., 503. The seeds yield a clear transparent oil known as simboli oil ; the root is laxative and both bark and roots are stimulant and used in cutaneous diseases and to check vomitino-. Pharm. 49. Musa Sapientum, Linn. — Plantain — Kela. This well-known fruit is demulcent, antiscorbutic, and alterative ; the tender leaves are used as a dressing for wounds, blisters, and sores, and as eye-shades in ophthalmia ; the root and stem are considered in native practice purifiers of the blood and are good in scorbutic complaints and special diseases. Pharm., 233. Myrica sapida — Kdiphal ; described by Brandis, 493. The fruit is eaten, and the bark is used externally as an anthelmintic, stimulant, and rubefacient, and in the arts as a tanning agent. Natives use it in epilepsy and to rub the body after illness. The OF THE NORTH-WESTERN PROVINCES. 743 average annual export of this bark from the Kumaun forest division is about fifty tons. Pharm., 217, Myrsine africana, Linn., the so-called box — PaMri-cha , chiipra ; described by Brandis, 286. The fruit is said to be a power- ful cathartic vermifuge. It is sold in the bazaars as bdyabirang , a name also of Embelia Ribes ; used also in dropsy, colic, and as a laxative. About a maund is exported every year from the Kumaun forest division. M. semiserrata, Wall., also called chupra, is said to possess similar properties. N. Nardostacbys Jatamansi, D. C.— Spikenard— Bdlchhar, sham- bed, balkar. Hoyle, t. 54,/. 2. This plant occurs above 12,000 feet and its roots with those of certain species of Valerian, especially V. Ilardwickii ( shameo , roots), are exported through the Kumaun forest division to the extent of about twenty maunds per annum. They occur in the form of short pieces of an underground stem, about the thickness of a quill, covered towards one extremity or almost entirely with coarse, dark, hair-like fibres. It has all the properties of Valerian in a high degree and is used as a stimulant and antispasmodic in hysteria and epilepsy. N. grandiflora, a larger species, also occurs in Kumaun at similar elevations. Pharm., 120. : Bird., 46. Nelumbium speciosum, Willd.— Lotus— Kanwal; described by Hooker/, and Thomson in Hooker, I., 116. The nuts are eaten as a tonic in disorders of the digestive functions. Nerium odorum, Aiton.— Oleander — Kaniyur ; described by Drury (U. P., 323). All parts of the plant are poisonous and are used in native practice in leprosy, cutaneous affections, and as an anthelmintic. The bark in paste is used in ringworm and itch and a decoction of the leaves externally as a vermifuge. Pharm., 139. Nicotiana Tabacum, Linn. — Tobacco — Tamdku, dhamdku . For the medicinal uses of tobacco see Pharm., 178, 460, and O’Shaughn., 471. Nyctanthes Arbor-tristis, Linn.— Ktiri, harsinghar; described by Drury (U.P., 323). Used in native practice for ringworm 744 HIMALAYAN DISTRICTS and to promote the adhesion of broken bones, also in indigestion : the bark is an astringent and is used as a gargle and in applications to sores and ulcers. 0 . Odina Wodier, Roxb. — Jingan, jlban; described by Hooker, II., 29. The bark is used in decoction as a lotion in impetigo and obstinate ulcers : the gum and leaves have also astringent properties and are applied to bruises and wounds. Pharm., 60. Olea glandulifera, Wall. — Gair , galdit, garur ; described by Brandis, 309. The bark and leaves are astringent and are used as an antiperiodic in fevers. Onosma echioides, Linn. — Maharanga , lal-jari, and ratan-jot (root), gauzaban (leaves), gul-i-gau-zabdn (flowers). The bruised root is applied to eruptions, the leaves as an alterative, and the flowers in cases of rheumatism and palpitation of the heart as a cardiac and stimulant. Exported through Dehra Dun. The root is also used as a dye. It appears that under the name ‘ ratanjot ’ the roots of Geranium nocbsum, Linn.; of Potentilla nepalensis, Hook.; Macrotomia euchroma, H. /. et. T.; and Jatropha Curcas, are also collected and sold. Ophelia Chirayta, Gris. ;Agathotes chirayta, Do n.-Tita-khdna, chirayta. Some call this species the true Ddkhini chiretta or true Nepal chiretta. The former name is properly applied to a South- Indian species, Andrographis paniculata, and the latter name may perhaps suit, as 0. Chirata occurs in Nepal. Equally good chiretta is obtained from 0 . purpurascens, 0 . cordata, 0 . speciosa , Agathotes angustifolia and A. alata. All yield a valuable bitter extract used as a tonic and febrifuge and corrector of biliary dis- turbance. About six tons are exported every year from the Kumaun forest division. See further Pharm., 149 : As. Res. XI. 167. Oxalis corniculata, Linn. — Chalmori ; described by Edge- worth and Hooker/, in Hooker, I., 436. The leaves, stalks, and flowers possess refrigerant and antiscorbutic properties and are used internally in fevers, dysentery, and scurvy, and externally to remove warts. The juice is useful in removing iron-moulds. OF THE NORTH-WESTERN PROVINCES. 745 P. Poeonia emodi, Wall. — Chandra (the plant), sujuniya (the young edible shoots), bhiima-madiya , yet ghas of the Bhotiyas ; described by Hooker/, and Thomson in Hooker, I., 30. The tubers are some of those exported under the name bikh and are proha oly those known as padam-chhal. There is nothing in the local Materia Medica re- quiring further investigation more than tne roots exported under the name ‘bikh’ and 1 nirbisi.’ Under the former come the various spe- cies of aconite. A. erox is the maura , maur or mahur bikh, and Madden tested it to see whether it deserved the name ‘ rnitha ,’ sweet, and found it was so : but this was soon succeeded by the most distressing burning all over the mouth and fauces, though nothing was swallowed. Dr. Royle says that Polygoncitum verticillatum, Linn., is called mitha-dudhiya in Sirmor and Smilacina pallida is called dudhiya-mohura, and both are poisonous. The cylindrical tuberous roots of Delphinium Jcashmerianum, Royle, found at Pindari in Kumauu and Bhojgara on the south side of the Kawari pass in Garhwal (11,000-14,000 feet), are absolutely identical with the ordinary nirbisi roots. See Madden, An. Mag., N. H., 2nd Ser., XVIII., 445. Parmelia kamtschadalis, Esch.— Lichen— Chalchalira, pat- tharke-phul. Several species are exported to the plains and are used in native practice as a tonic febrifuge and antiperiodic. See Pharm., 260. Peucedanum graveolens, Benth.-Dill-Soya ; described by Clarke in Hooker, II., 709. An excellent carminative for relieving flatulence in children. Pharm., 101. Pharbitis Nil, Ghoisy — Baunra ; described by Drury (U. P., 350). A safe and effectual cathartic. Pharm., lo5. Phyllanthus Emblica, Linn.— Amla, aonla; described by Bran- dis 454. The dried fruit is astringent and when fresh is given as a tonic aperient : the flowers are refrigerant and aperient and the bark is astringent. See Pharm., 204, and O’Shaugh., 551 The leaves of Paraphyllanthus urinaria ( serdhi ) and of Phyllanthus niruri, Linn., are given in infusion as a diuretic and the fresh roots of both in jaundice. See Drury. 94 746 HIMALAYAN DISTRICTS Picrorhiza Kurrua, Roxb. — Kuruwa. Found only at high elevations about 11,000-14,000 feet : the bitter roots are exported with Saxifraga ligulata under the name pakhdn-bed , and with Gentiana Kurroo under the name Mtki, to the extent of about three tons a year and are used as a tonic. Nima quassioides occurs in upper Grarhwal (5,500-8000 feet) and is known as Iccirivi and has similar uses. Pinus longifolia, Roxb. — Pine — CMr. This pine is very com- mon in Kumaun and yields a turpentine and resin : for uses see Pharm., 222, 219. The turpentine from P. Gerardiana is used principally in special diseases, and that from P. JDeodara in cutaneous diseases and as a diuretic. Pharm., 225. Pistacia integerrima, j. L. S. — KaJcra, haTcra-singi ; describ- ed by Hooker, II., 13. The gall-like excrescences formed on the leaves and petioles in -October are exported as a medicine and are esteemed useful in coughs, asthma, fever and dysentery, and as a sedative. They occur black, hard, rugose, hollow, irregularly crooked, often 6 '-7' long. The average annual export from the Kumaun forest division is about seventy maunds, Brandis, 122, 574. Pithecolobium bigemimim, Mart. — KaeMora ; described by Brandis, 173. A decoction of the leaves is used in leprosy and as a stimulant to promote the growth of hair. Plantago major, Linn. — Luhuriya. It is doubtful whether this has the properties of P. decumbens, Forsk., the isbaghol of the bazars. Pharm., 182. Plumbago zeylanica, Linn. — Chita, chitra ; described by Rox- burgh, 155. The roots triturated in water form a vesicant and in tincture a good antiperiodic : they are exported from the Kumaun forest division to the extent of about twelve maunds annually. Pharm., 170: O’Shaugh., 508. Pongamia glabra, V ent. — Pdpar, SuTch-chain ; described by Baker in Hooker, II., 240. The seeds yield an oil much used in skin diseases and as an embrocation in rheumatism : the leaves are also officinal. Pharm., 79, and J. Agri.-H., Cal., X., 223. 95 OP THE NORTH-WESTERN PROVINCES. 747 Pontedera vaginalis, Linn. — Nauka ; described by Drury (U.P., 364). The root is chewed for toothache and the bark is eaten with sugar for asthma. Populus ciliata, Wall. — Chalniya , chauniya , chan , gar-pipal ; described by Brandis, 475. It is occasionally used as a tonic stimulant and purifier of the blood. Portulaca oleracea, Linn. — Small purslain — Liiniya-Mlfah ; described by Drury (U.P., 364). The bruised leaves are used as an anodyne and are given as a refrigerant and antiscorbutic in cutaneous diseases. Bird., 38. Premna integrifolia, Linn. — Bakarcha of Garhwal ; described by Drury (U.P., 365.) The root is given in decoction as a cor- dial and tonic ; the leaves beaten up with pepper are also adminis- tered in colds and fevers. The whole plant is given in decoction in rheumatism and neuralgia. The milk of the bark of P. mucronata, the agniun of Kumaun, is applied to boils and the juice is given to cattle in colic. Primula speciosa, Linn. — Bisli-kopra , jal-Mtra. It is found along streams from 3,500-5,500 feet in Kumaun : it is said to be poisonous to cattle and is used externally as an anodyne. Prinsepia utilis, Royle. — Chirara, jhatela , dhatela, phalawa, bheJcla; described by Hooker, II., 323. This shrub yields an oil used as a rubefacient and as an application in rheumatism and pains from over-fatigue : a small quantity is exported from the forests and pays a duty of five rupees per maund. Prunus Communis, var. domestica, Linn. — Prune. See page 712. The dried drupe is considered a laxative and emollient and is used in medicinal confections. Pharm., 86. The alu-bukhdra is used as a refrigerant and laxative both in a cold infusion and a con- fection. P. persica — the peach — is given as a demulcent and anti- scorbutic and stomachic. The oil from the kernels is considered a valuable vermifuge and strengthener of the hair. The kernel of P. Puddum is used in stone and gravel, and that of P. Padus yields a poisonous oil, like oil of almonds, much used in medicinal preparations. Psidium Guyava, Linn. — Guava — Amrud ; described by Baker inHooker, II., 148. The bark of the root is given in decoction in 748 hima'iayan districts. infantile diarrhoea and the young leaves as a tonic in diseases of the digestive functions. Pharm., 92. Pueraria tuberosa, D.C.; Hedysarum tuberosum, Roxb. — JBildi-kand , bill, birali-panwa (Kumaun), sural (Jaunsar), sarar, sarwala (Bijnor); described by Baker in Hooker, II., 197. The tubers are dug up and exported in large quantities to the plains, where they are considered demulcent and refrigerant in fevers and useful as a cataplasm for swollen joints. Punica Granatum> Linn. —Pomegranate — Anar (cultivated) ; ddrim (wild) ; naspal, kushiala (rind of fruit). The root-bark and dried rind possess powerful astringent properties from the presence of tannin. The former is considered anthelmintic in European practice and the latter astringent. See Pharm., 93, 447. Putranjiva Roxburghii, Wall. — Ji'iti, putrajiva; described by Drury (U. P., 372). Given in decoction in colds and fevers. Pyrus Cydcnia, Linn. — Quince — Bihi. See page 713, Cydonia vulgaris. The seeds are used as a demulcent in native practice and as a tonic ; also in decoction in dysentery and special diseases : Pharm., 86. Q. Quercus incana, Roxb. — Bdnj ; described by Brandis, 482. The acorn ( sil-supdri ) washed and powdered is used as an astringent in indigestion, diarrhoea, and asthma. Pharm., 209. R. Randia dumetorum, Law. — Mainphal, manydl, Icarhar ; des- cribed by Drury (U. P., 373). The fruit is highly esteemed as an emetic and is used to poison fish and the bark of the root in infusion to nauseate. Pharm., 118. Raphanns sativus, Linn. — Radish — Muli. The seeds of this common vegetable have diuretic and laxative properties and the roots are prescribed in native practice for special and urinary diseases. Rheum emodi, Wall. — Dolu. This species is found near the Pindari glacier and at similar elevations in Kumaun and Garhwal ; the average annual export from the Kumaun forest division is about l,0C0tb. This and R. Webbianum, Royle, are used as a OF THE NORTH-WESTERN PROVINCES. 749 substitute for Turkey rhubarb. R. emocli is less active as a pur- gative and more spongy in texture. See Pharm., 187 : O’Shaugh., 519 : Panjab Products, 370 : J. A.-PI. Beng., I., 76 : Birdwood, 70 : Pereira Mat, Med., II., 485. Rhododendron campanulatum, Don. — Chirw'd; described by Brandis, 281. The leaves are exported to the plains, to be made into a snuff called hulds-kashmiri , useful in colds and head- aches. Ricinus communis, Linn. — Castor bean — Rendi. This well- known plant yields the medicinal oil used as a purgative, &c. Pharm., 201, 462 : O’Slmugh., 556 : Drury (U. P., 375). Roylea elegans, Wall. — Tit-patti , kauri. The leaves are used as a bitter tonic febrifuge. Rubia cordifolia, Linn. — Majethi. The natives consider the roots most useful in cases of poisoning, cutaneous eruptions, dysen- tery, and as a tonic to promote menstruation. Pharm., 118 : Drury (U.P., 379). RumOX acutUS, Roxb. — ■ Jangli pdlak ; described by Drury (F. P., IIL, 49). This plant has cooling properties : the leaves are applied to burns and the seeds are applied as the Uj-band of the bazars. R . acetosa is also widely distributed and known under the same vernacular name and also as ‘ Almora ,’ whence the name of the capital of Kuraaun, as Mussooree is derived from the verna- cular name of Coriaria nepalensis. s. Salix tetrasperma, Roxb. — Gar-byush ; described by Bran- dis, 462. The bark in decoction is of some account as a febrifuge. Pharm., 213 : O’Shaugh., 606. Saxifraga ligulata, Wall. ; Var. ciliata , Royle. The roots of this and perhaps P. Kurrua ( antea ) and G. Kurroo [anted) are all exported to the plains as pdkhdn-bhed or pcithan-bhed and jintidna and are used as a tonic in fevers and also in diarrhoea and coughs and as an antiscorbutic. The average annual export from the Kumaun forest division is about thirty maunds. Sapindus detergens, Roxb. — Kanmar, ritha; described by Drury (U. P., 393). The nut is used externally in cutaneous 750 HIMALAYAN DISTRICTS affections and internally in epilepsy and headache and as an ex- pectorant ; also in the arts as a detergent. It is exported from the Kumaun forest division to the extent of about twenty tons per annum. ScindapSus officinalis, Schott. — Ga,j-pipali , hcith-ungliya. The dried and sliced fruit has stimulant, diaphoretic, and anthelmintic virtues. Pharm., 250. Semecarpns Anacardium, Linn., F. — Bhildwa, bhaliau, bhdla ; described by Hooker, II., 30. The acrid viscid juice between the laminae of the shell possesses powerful caustic properties and is used as a vesicant : see further Pharm. 60 : K. Dey, 105. The average annual expor from the Kumaun forest division is about five maunds. Sesamum indicum, Linn. — Till. See page 764. This plant furnishes the sesamum or sweet oil, used as a substitute for olive oil in native practice. Pharm., 151 : Drury (U. P. 402) : O’Shaugli., 479. Sesbania segyptiaca, Pers. — Jcdnt; described by Baker in Hooker, II., 114. The seeds have stimulant and emenagoguic pro- perties and are used in cutaneous diseases and itch : the leaves are used in poultices to promote suppuration, and the juice of the bark internally as an antiscorbutic. Shorea roblista, Roxb. — Sal ; described by Drury (U, P., 405). The resin (rdl or dhamar ) is an efficient substitute for pine resins in plasters : in native practice, the resin is taken internally in special diseases and applied as a styptic to wounds. Pharm., 33. Solanum indicum, Linn. — Katang-kari ; described by Drury (U. P., 408). The root is used in decoction in dysuiia and in fevers and coughs: and when powdered as an anodyne. The juice of the leaves boiled with ginger is used to stop nausea. Pharm., 181. Solanum tuberosum, Linn. — Alu. The tubers are occasionally used as a substitute for salep. Solanum esculentum — Baigan, bhutta. See page 703. The leaves possess narcotic properties : nearly every species of this genus in Kumaun affords some aid to the native Materia Medica. Pharm., 181, OF THE NORTH-WESTERN PROVINCES. 751 Spondias mangifera, Pers.— Hog-plum— Ambara ; described by Hooker, II., 42. Tlie bark is used in dysentery and a decoc- tion of tlie wood in special diseases ; tbe juice of the leaves forms an application in earache and the gum and fruit are eaten. Sterculia urens, Roxb.— Kuli, lulu ; described by Masters in Hooker, I., 355. The leaves and tender branches steeped in water yield a mucilaginous extract useful in pleuro-pneumonia in cattle. Streblus asper, Lour. — Sihora, rusa; described by Drury (U.P., 211). The milky juice is applied to cracked heels, sore hands, and has astringent and septic qualities. The bark in decoction is given as a lotion in fevers. Symplocos cratcegoides, Ham. — Lod, lodh ; described by Brandis, 299. The leaves are considered astringent and are used in diarrhoea and as an application to fresh wounds and the bark in tanning. About nine tons are exported every year from the Kumaun forest division. T. Taxus baccata, Linn.— Yew— TMner, brdhmi ; described by Brandis, 539. The leaves are used in native practice in epilepsy and indigestion. Tephrosia purpurea, Pers. — Sarphonla ; described by Baker in Hooker, II., 123. The leaves^and seeds possess astringent, tonic, febrifugal properties. The leaves of T. Candida , the lelitiya of Kumaun, are used to poison fish. Terminalia Chebula, Retz. — H&r ; described by Drury (U.P., 431). This and other species of the same genus yield nuts much used in medicine and the arts. See Pharm. b9 . Iv. L. Dey, 117 . Birdwood, 34. Tetranthera laurifolia, Jacq .— Gar bijaur , meda-lakri; described by Brandis, 379. The oil from the berries is used in rheumatism ; the bark triturated in water or milk, or even dry, is applied to bruises and is given internally in infusion in diarrhoea ; the leaves have a rich aromatic odour. Pharm., 88 : O’ Shaugh., 548. Thalictrum foliolosum, D.C .-Pila-jari, pengla-jari, barmat ; described by Hooker /. and Thomson in Hooker, I., 14. The roots are exported from Kumaun under the name mamira and are highly alued in ophthalmia and as an antiperiodic. Pharm., 5. 752 HIM A' LAY AN DISTRICTS Tinospora COrdifolia, Miers — Gulancha ; described by Hooker /• and Thomson in Hooker, I., 97. The stems yield the well-known extract known as gulancha or giloi, a much-esteemed specific in stings as well as infever and rheumatism. The leaves bruised and mixed with honey are applied to ulcers, with oil to the head in neuralgic affections, and in decoction for gout. The extract is made from the root by boiling for twelve hours and then strain- ing and evaporating the water. The annual average export of the extract from the Kumaun forest division is about two maunds. Pharm., 9, 435. Toddalia aculeata, Pers . — Kauj ; described by Hooker, I., 497. The root-bark has tonic, stimulant, and anti-periodic pro- perties. Pharm., 47, 442. Tricliodesma indica, R. Rr. — Ratmandi. The natives con- sider it to be an antidote in snake-bites ; the leaves are used as a poultice and in cold infusion as a purifier of the blood. Pharm. 158. TricllOSanth.es palmata? Roxb . — Indray an; described by Clarke in Hooker, II., fi06. The roots and fruit are poisonous and are used in pleuro-pneumonia in cattle. Pharm., 9fi. T. cucum- erina, Linn., gives seeds, tender shoots, and dried capsules, all of which are used as medicine. O’Shaugh., 351. Trigonella Fcenum-grsecum, Roxb.— Fenugreek — Methi ; described by Baker in Hooker, II., 87. The seeds are stimulant, aromatic, and laxative, and are given in colds, coughs, diarrhoea, and special diseases. Typha angustifolia, Linn. 13oro. The down of the ripe fruit is used as an application to burns and the lower succulent parts of the stem to clear muddy water. IT. Urgmea indica, Kunth. ; Scilla indica, Roxb — hUl, Undn or “ ld ffh ‘ SUWa ° f Kuma ™ ; described by Drury (U. P., 399). It is exported largely from the lower hills. The nauseous bitter young bulbous roots have expectorant and diuretic proper les in small doses, and in large doses they are emetic and cathartic. Pharm., 211 : K. L . Dey> U)L OF THE NORTH-WESTERN PROVINCES. 753 V. Vallaris dichotoma, Wall . — Duclhi; described by Drury (P. F. II., 198). The juice is applied to wounds. Valeriana Hardwickii, Wall. — Shumeo, asdrun. The roots are exported and are said to possess anti-spasmodic properties : when dry they are burned as a perfume, and are also used as a flavoring agent and to keep off insects from clothes. Pharm., 120. Vernonia anthelmintica, Willd . — Kali-jiri; described by Drury (U. P., 449). The bitter seeds are powerfully diuretic and anthelmintic and are given in infusion in coughs and flatulency. Powdered and mixed with lime-juice they are used to expel vermin from the head, and mixed with oil in scabies and anasarca and in plasters for abscesses. Pharm., 126. Viola serpens, Wall. — Thungtu, banafsha ; described by Baker in Hooker, II., 184. The flowers are considered diaphoretic and laxative : the seeds are diuretic and the root emetic (like ipeca- cuanha) and purgative (Brown). Vitex Negundo, Linn. — Shiivdli, simdli, filjil-bdri (fruit) ; described by Drury (U. P., 452). The root and fruit have anodyne, diuretic, and emenagoguic properties, and the leaves are given in colic. Exported from Kumaun. Pharm., 163 : O’Shaugh., 484. ’ W- Withania somnifera, Don .—Asgand (root); described by Dru- ry (U. P., 355)- The leaves are bitter and narcotic and are used • n i n f us ion in fever : the seeds coagulate milk and the roots are aphrodisiac and diuretic. Pharm., 182 : O’Shaugh., 466. The seeds of W. coagulans, Don., have also sedative properties and are given in colic. Both are exported from Kumaun. Woodfordia floribimda, Salis. ; Grislea tomentosa , Roxb. — Dhaula, dhdi ; described by Clarke in Hooker, II., 572. The dried flowers are used as an astringent tonic in affections of the mucous- membrane, hoemorrhoids, and bilious complaints. The leaves are also officinal in native practice. Exported from Kumaun. Z. Zanthoxylum alatum, Roxb .—Tejbal, timi'ir ; Sansk. jwardn- tika, 1 fever ender ; described by Hooker /. and Thomson in 754 HIMALAYAN DISTRICTS Hooker, I., 193. The bark and seeds are used in native practice as a tonic in fevers and bowel complaints : the small branches are used as toothbrushes and the thorns as an application in toothache : the fruit is used to intoxicate fish. Supposed to possess generally stomachic and carminative properties. The average annual export from the Kumaun forest division is about half a maund. Pharm., 48. Zingiber officinale, Ros. — Ginger — Adrak, sonth. This well- known plant yields the ginger of commerce, extensively used in medicinal preparations. See Pharm., 228. B- -NARCOTICS AND SPIRITS. Tobacco, opium, hemp, and the preparations made from them, are the principal vegetable substances used for their narcotic and intoxi- cating properties in these provinces, but to them we may add the various forms of alcohol obtained by distillation and the prepara- tions of betel and areca. The use of tobacco in the plains is universal amongst males from their twelfth year, and the practice has so far entered into the social arrangements of the people that few matters of importance are discussed without the Tiukka being passed around. In the hills tobacco-smoking is becoming more common every year, and now, perhaps, all except a few Brahman families smoke tobacco either pure or mixed, and these even chew the leaf pounded with lime, a practice common to every caste. Opium is principally consumed by Musalmans, and its use in the hills is very limited. The prepara- tions of hemp are in great request amongst Hindus, and are much indulged in by Jogis and others of the wandering religious mendi- cant classes. Spirits are consumed chiefly by the lower castes of Hindus. Brahmans and Baniyas profess to hold it in abhorrence, and the use of it is forbidden to Musalmans by the Koran. As a general rule these restrictions are observed, but still there are very many individuals of these classes who openly disregard the rules of their religion and many more who do so in secret. The statistics derived from the Excise Department would otherwise be inexplicable. Still, taking into account the quantities of opium, hemp, and spirits that must be consumed in a country like India without paying any license or contributing in any way to the revenue, there is only a OF THE NORTH-WESTERN PROVINCES. 755 moderate consumption on the whole. It has often been observed that you may pass through any fair or assembly, except during the Diwali, the Hindu carnival, without seeing a drunken man, and there can be no doubt but that the consumption is very small and quite insufficient in the hills, at least, to have much effect upon the public health. Although hemp is produced in such quantities in Garhwal and Kumaun, the preparations from it are not a favourite form of intoxication in the hills and are seldom used by the permanent inhabitants. Tobacco. Uicotiana Tabacum, Linn. Tobacco — Tcimdku, clhamoku. Tobacco is raised in large quantities in the forest clearings along the foot of the hills, where the conditions Tobacco. necessary — a rich alluvial soil, warmth, and abundance of manure — exist. The last is furnished by the cattle which are sent there for grazing in immense numbers from Novem- ber until May. In the Garhwal Bhabar the cultivation of tobacco is carried on by men of the gardener caste from the plains, who remain long enough to plant and gather the crop. The indige- nous Bhuksas of these parts consider that they are prevented by their caste rules from growing tobacco, or rather are too in- dolent to undertake its cultivation. Further east all classes cultivate the plant, and great quantities are exported to the plains from the Kumaun Bhabar and the Tarai. The quality of the leaf is not so delicate as that of the better sorts of the plains varieties, but the quantity produced from a given area is greatly in excess of that raised elsewhere. In the hills, a far superior variety is cultivated from Jaunsar to the Kali, but not in quantity sufficient to be of much commercial importance. That grown on both banks of the Alaknanda near Srinagar in Garhwal is specially esteemed. The Kumaun vernacular names above given represent two varie- ties, N. Tabacum and the N. rustica or Latakia, which latter seems to have been grown in the hills from time immemorial, and when carefully prepared is palatable to Europeans. Dr. Stewart, writing of its cultivation in the western Himalaya, states that “ more of it than of the ordinary kind can be grown per acre, especially as in many places the flowers are not plucked off, but are mixed with the leaves for smoking, and it brings in a greater 756 HIMALAYAN DISTRICTS price than the ordinary species. It is said to be much stronger than the latter and to be generally smoked mixed with a large proportion of it. Its qualities when smoked in the European pipe give assurance that, if properly cured, it would rival Turkish tobacco.” Some efforts have been made lately by Mr. E. C. Buck to improve tobacco cultivation in Kumaun, but the experiments have failed and their history will be found in the annual report of the Department of Agriculture and Commerce. The Sikhs, Wahabis, and certain Hindu sectaries are forbidden the use of tobacco by their religious guides, but the first console themselves with the preparations of hemp and the second use opium. The earliest mode of procuring and inhaling the smoke was to make two holes in the ground, in one of which the fire and tobacco were placed and a pipe connected the two. The smoker then crouched on the ground and sucked the smoke through the second hole. This method may still be seen in the hills. Another mode was to twist a leaf and smoke through the narrow end, still a favourite with coolies in the hills. An improve- ment was then effected by drawing the smoke through a bambu, and thus avoid the uncomfortable crouching position, and eventually the hukka was invented. The cocoanut served as the first form of the hukka, and though metal is now used for the receptacle for water and the original form has been modified, the cocoanut is still the basis of all the forms of the hukka from the elaborate and costly pechicdn of the nobleman to the simple pipe of the cooly. Musalmans seem to affect those hukkas that have stands, whilst Hindus adopt the round or oval shape, which are fitted chiefly to pass from hand to hand. In the plains tobacco is seldom smoked in its pure state ( sacla ), but is mixed with from a half to an equal weight of molasses, either of the sort known as gtir or that known as shira, to which a little saji, or impure carbonate of soda, is added. In the interior of the hills, however, the pure leaf is generally the only sort procurable, but in the principal bazars the fashionable mixtures may be obtained. One of these in high repute amongst the wealthy is known as khamera and consists of a certain quan- tity of tobacco of the Latakias sort, to which is added the sence of the Pandanus odoratissimus or keora ; the dried leaves of the musk- plant, Delphinium hrunonianum ; sandal-wood dust ; a conserve OF THE NORTH-WESTERN PROVINCES. 757 of roses known as gi'cl-kand ; the fruit of the Zizyphus jujuba ; apple-preserve, cardamoms, and the wilted leaves and stems of the betel palm known as pdnri , in certain proportions kept secret by each maker and which form his particular brand or manufacture. Snuffing tobacco, though not unknown, is rarely seen. Its use, however, as one of the ingredients of ‘betel’ should perhaps come under the head of chewing. Opium. Papaver somniferum, Linn. — Poppy — Post, posta; juice of the capsule, opium ; afydn, afim. A plant be- 0lUU11, longing to the natural order Papaveracece. The cultivation of the poppy is a Government monopoly and is chiefly confined to the plains. The capsules, whilst immature, yield by incision a juice which on solidification is known as the opium of commerce. When ripe or dried they yield an intoxica- ting liquor by inspissation. The use of the drug was known to the ancients, and some say that it was the pharmakon nepenthes of Homer. Dr. Royle considers that it was introduced into India from Persia, and in this suggestion he may, perhaps, be correct, as the common names for opium are of Persian origin. The Ain-i- AJcbciri refers to theo pium monopoly in Sirkars Kora (Fatehpur district), Allahabad, and Ghazipur in the time of Akbar, and we know that from time immemorial the opium poppy has been culti- vated in Nepal and Kumaun. The three principal preparations of poppy in use are the abkari or excise opium, madak and chondu. The first is supplied from the Ghazipur factory and is sold at the rate of sixteen rupees per seer of eighty tolas. As a rule, abJcari opium is taken in the form of pills, but many soak the preparation in water for some hours and drink the solution thus formed, leaving the impurities at the bottom of the cup : very moderate consumers take about one tola or 180 grains Troy or 11 -6 6 2 grammes per month, and the average con- sumption of habitual opium-eaters may be set down at five tolas each per mensem. In some cases as much as two tolas a day are taken boiled in milk. Opium-smoking has of late years increased very much in these provinces. The results are the same as iu other countries, the drug inducing stupor, reverie, and voluptuous 758 HIMA'LAYAN DISTRICTS listlessness. Still the individual can easily be roused to business, and, unless taken in excess, the effects are not more injurious or lasting than those attendant upon a too liberal indulgence in spirituous liquors. The temptations to excess are, perhaps, stronger in the case of opium, and with over-indulgence come sickness, consti- pation, indigestion, want of appetite, emaciation, impotency, and premature old age. In small doses as far as one grain, opium when eaten acts as a stimulant, increases the pulse in strength and frequency, and excites the mind by a happy train of thought. It is believed to promote digestion, and for this purpose it is taken usually in the afternoon or evening, so that its effect may come on before the time for the evening meal. This condition is however succeeded by drowsiness, thirst and loss of appetite, and the habitual eater then increases his dose, when after a smoke of tobacco from the hukka the excitement again begins and is followed by a period of stupor and eventually a profound sleep, “ the pupils are slightly contracted, the pulse slow and full, the breathing slow, and the temperature of the body somewhat increased.” Beyond four grains to healthy persons not accustomed to opium it may be consi- dered to act as a poison. Milk is taken by opium-eaters to keep the bowels open, and as in the case of lhang and, indeed, spirits when once the habit of using the drug has been fixed, it is almost impossible to shake it off. Kahars and men who have much trying physical labour to get through in a short space of time can, fre- quently, take large doses without apparent injury . 1 Madak and chandu are forms of opium extensively used in these provinces. In preparing them the opium Madak and chandu . # 1 is first reduced to a watery extract, which is then strained two or three times through cloth and afterwards boiled over a slow fire until it thickens somewhat. The impurities left in the process of straining are again washed and strained two or three times to extract any portions of the active principle which may remain. The refuse, called joga , is then thrown away and the resi- duum of pure extract of opium that remains is called Teimam and forms the basis of both madak and chandu. One ser of excise opium yields a little more than half a ser of kimam. To make 1 I am indebted to several sources, official and private, for these notes on opium and hemp. OF THE NORTH-WESTERN PROVINCES. 759 madaJc, the leaves of the guava, pdn, or, in some cases, the rose are collected and cut into very fine pieces and then boiled in water. When they become soft they are strained in a cloth and dried and then fried on an iron pan over a slow fire. These leaves thus pre- pared are called jesa, and equal quantities of jesu and kimam form madak. This preparation is made up into small pills about the size of a pea, which sell in the retail shops for a pice each. The consu- mer buys these pills, breaks one of them into six to twelve parts, which are called 1 chittas each of which serves for one operation or whiff. The ordinary hukka is used, hut the chillam or upper portion for receiving the drug and fire is much smaller. The cMtta is placed on the cliillam and lighted by a charcoal pencil, and the smoke is taken inwards in one inspiration and swallowed. The result is considerable pleasurable excitement, which as it begins to wear off is renewed by consuming another chitta until satiety is produced. One pill is sufficient to intoxicate a new smoker, but many consume a dozen pills with impunity. The basis of chandu is the same Jcimam from which madak is made, but instead of leaves the half-burned ashes of the chittas of madak are mixed with the kimam in equal quantities and the resulting compound is called chandu. For this preparation there is a particular pipe made of wood and about twelve to fifteen inches long. A small brass or tin bowl is fixed towards one end and communicates with the stem by a small aperture. The chandu formed into a paste and made up into pills is placed in the bowl, and this is lighted from a lamp and gives a gurgling noise while burning. The smoker reclines on a pillow with his eyes closed, and the pipe is lighted by an attendant and refilled when necessary. Like the madak- smoker, the chandu- smoker takes in all the smoke arising from one application of the chandu by one deep inspiration and swallows it. After every inspi- ration there must be a rest, and the heated tongue is moistened by chewing sugarcane or by the application of a rag moistened in sherbet. Two or three applications are sufficient to affect a beginner, but there are many who can doze away over pipes of chandu the whole day. The effect of madak and chandu smoking is equally pernicious with opium-eating, with this difference that intoxication 700 HIMA'LAYAN DISTRICTS supervenes at a much earlier period, because the smoke containing the active principle of the opium is directly absorbed by the blood in the lungs, and being carried into the circulation acts, at once, on the brain ; whilst in eating opium the process of solution, absorption, and digestion is much slower. Muhammadans are by far the greater smokers and eaters of opium as compared with the Hindus, and they make up by indulgence in this vice for the prohibition of spirituous liquors. Love of sexual intercourse has much to do with inordinate indulgence in opium, and for a time, like the preparations of hemp, it acts as a powerful aphrodisiac, but in the end it induces impotency and leaves the opium-drunkard a physical and moral wreck, utterly careless for the present or the future and a mere semblance of a human machine. Hemp. Cannabis sativa, Linn. — Hemp — Gdr-bhanga (female plant), phul-bhanga (male plant). (See Fibres posted.) The principal parts of the hemp that are used as intoxicating ^ agents are the char as, gdnja and bhang , or sabji and their preparations. The best charas is obtained from the female plant and consists of a resinous exu- dation from the leaves, stems and seeds when ripe, and is collected from them by rubbing them in the hands or on the naked thigh or by scraping the resin from the plant with a blunt iron knife. The quantity and quality of this resin differs with the soil and locality. In some places the plant developes a woody tissue, whilst in others the bark splits and a resin is secreted. In the plains in many places the hemp plant yields excellent gdnja , but neither charas nor bhang ; and again in the hills the charas is the principal product. The best qualities of charas are imported from Yarkand, Bukhara, and Afghanistan. In former times only the pure resin collected by the scraping process was imported, but now a sys- tem of manufacture has sprung up by which a much larger return is effected. When the plants have arrived at maturity, which is known by the bark commencing to split, they are cut down and soaked in water and when well moistened the resinous juice is pressed out. This is then boiled and reduced to the consistence of a paste, in which form it is imported by the Afghan fruit-sellers. It OF THE NORTH-WESTERN PROVINCES. 761 contains, in addition to the resin, much of the juice of the plant, its colouring matter and other foreign substances, and is altogether inferior to the resin collected by the old scraping process. The Kabulis sell this preparation to the contractors at about one and a half rupee per ser, and they again to the licensed vendors at fiom four to five rupees per seer, and the latter retail it at about two chhcit- tdks for a rupee or eight rupees a seer. The drug is consumed in the following manner : — About the weight of a two-anna silver piece or 22 grains Troy is taken and covered up with twice its weight of prepared tobacco in the shape of a ball. This is dried over a charcoal fire, and during the process the charas melts inside. The dried ball is then reduced to powder and mixed with tobacco is placed on the chillam of an ordinary cocoanut huJcka and smoked in the same way as tobacco. Charas seems to be a mildei foim of the drug than gdnja and is used by the better class of people and those who do not care for intoxication pure and simple. GXnja. Ganja consists of the dried flower heads and smaller leaves from which the resin has not been removed. It Gdn J a - yields to alcohol twenty per cent, of resinous extract composed of the resin ( charas ) and green colouring matter. Distilled with a large quantity of water traces of essential oil pass over, highly odoriferous of the drug. The colour of the bundles of gdnja is dusky green, the odour narcotic and the touch adhesive. The gdnja produced iu Kumaun and Garhwal is considered of little value and is not, so far as I am aware, expoited. The gdnja consumed locally is imported from the lower districts. Two sorts of gdnja are sold in these provinces the patten and the biluchar. The pattar is imported chiefly from Holkar’s territories and is of quality inferior to the Bengal gdnja. It is purchased at from five to six rupees per maund in Indur in the rough state, including the stalks and useless leaves, and also pays a duty of about four annas per maund on exportation to British territory. The farmer of the drug revenue pays the cost of carriage and sells it to the licensed retail vendors at from Bs. 20 to Us. 22 per maund. The retail sellers separate the real gdnja from the rough plant and throw away the refuse, which amounts to from five-eighths to 96 7 62 HIMALAYAN DISTRICTS two— thirds of the whole, or in one raaund of rough plant only thirteen to fifteen sers of real gdnja will be found. This sells at from three to four rupees per ser, and about one quarter of a ser will form a month’s supply for an ordinary smoker. This pattar ganga is chiefly consumed by the lower classes of Hindus, and espe- cially by all the mendicant sects of Bairagis, Nagas, Sanyasis, &c. The biluchar variety is imported from Lower Bengal and is far superior to the pattar. It is grown in the Rajshalii district and sells there in the rough at from Us. 18 to Rs. 22 per maund. The Ben- gal Government charge a duty of from Rs. 2 to Rs. 2-8 per ser, or Rs. 100 per maund, on all exports of gdnja to these provinces. The farmers of the drug revenue separate the real gdnja from the rough plant and sell to the licensed retail vendors at tromRs. 10 to Rs. 12 per ser, and the latter retail the drug at one rupee per chhatak (loz. 17dwt. 12grs. Troy), so that Bengal gdnja is as dear as excise opium in these provinces. One or two chliataks are sufficient for a month’s consumption to an ordinary smoker. The Bengal gdnja is much stronger than the pattar variety, so that a much smaller quantity produces the same result. It is used only by the better classes, being the more expensive of the two. Gdnja is not in general used so much as tobacco. Kahars when they complete a portion of their journey often take it as a stimulant, and others with weak digestions smoke a little before a meal to excite a feeling of hunger and promote digestion. It may serve as a stimulant for the time, but its after-effects are lassitude and depression. Gdnja is also used as a sedative to promote sleep, which it does after an interval of excitement by intoxication. Gdnja is prepared for smoking by taking a portion of the dried leaves, say 20 grains in weight, in the palm of the left hand; these are rubbed with the right thumb, a few drops of water being added to moisten it. Then an equal quantity of dry but soft tobacco leaf is added, and the whole is formed into a paste. This is then cut into thin layers with a knife and again rubbed and pressed into a paste with more water. The compound when well mixed is again sliced ? and the process is continued tw r o or three times until the gdnja and tobacco are thoroughly amalgamated. It is then smeared with the fingers over a very narrow, small, earthen chillam , and a small cake 97 OF THE NORTH-WESTERN PROVINCES. 763 of lighted charcoal is placed on the top. The chillam is placed on the ordinary hukka, consisting of a hollow wooden cylinder fitted into a dry cocoanut shell which is half full of water ; another cylin der attached to the middle of the cocoanut forms the stem through which the smoke is swallowed. Gdnja smokers are, as a rule, sociable, and the pipe is passed around after each one has had one good pull at it. Each smoker swallows the smoke, which conveys the active prin- ciple in that form to the lungs and stomach. With strong Bengal gdnja it is difficult to retain all the smoke inspired at a single time, and a cough usually interrupts the operation. This custom is as much due to economical considerations as to good-fellowship, foi no one could smoke time after time and the gdnja keeps burning away all the same. One dose of gdnja is quite sufficient to give a moder- ate feeling of intoxication to four or five persons. To those unac- customed to it a single inspiration produces giddiness and even stupor for a time, whilst habitual smokers can take their turn fox half an hour. Heaviness, laziness and agreeable reveries ensue, but the person can be readily roused and perform routine duties. As in the case of opium, gdnja is often made use of as an aphrodisiac. Bhang. Bhang comprises the larger leaves and capsules of the hemp without the stalks. In these provinces there are three varieties of bhang in common use, viz., the Hard war bhang which comes from Garhwal, the Oudh which comes from the Gonda district, and the Panjabi which comes from Jalandhar. Of these the Oudh variety is the strongest and there- fore the best, so much so that one part of it intoxicates as quickly as two parts of the other varieties. The bhang -'g r o d uc ing hemp grows wild and is sold in the rough with the stalks and refuse leaves at about one rupee per maund in the producing distucts, hut to this must he added the cost of carriage. The farmer of the drug revenue sells the cleaned plant to the licensed vendors at from ten to fifteen rupees per maund according to the distance from the base of supply. The latter retail the drug to consumers at eight annas per ser or Rs. 20 per maund. The names sabji and siclhi are, also, applied to bhang in its gree i state, and mdjvm is a conserve of bhang which is noticed hereafter. 764 HIMA'LAYAN DISTRICTS Bhang is prepared for use by soaking the dried leaves for a time in cold water and carefully washing and freeing them from all sorts of impurities, such as dust, seed, kunkur, and the stalks and stems. The leaves are then bruised in a mortar or on a flat stone and made into a thick paste. The paste is then ready for use, and when required is diluted with water according to taste and the so- lution is drunk. Many persons mingle spices with the paste during the pounding operation, such as black pepper-corns, aniseed, cloves, cardamoms, sugar, and melon and cucumber seeds, but the pepper forms the pi’incipal ingredient. An ordinary drinker will consume one ser of bhang or eight annas worth per mensem. Most Hindus who do not indulge in wine, such as Brahmans, Ba- niyas and the like, take bhang. It is the special drug of the Hindu mendicant classes as madak is affected by the Musalman fakirs. The Chaubes of Muttra, the Pragwals of Allahabad, and the Gangapu- tras of Benares, are noted for their indulgence in excessive bhang- drinking. In the Panjab, the Bhangi misl, or sub-division of the great Sikh confederacy, was so called from the real or fancied fond- ness of its members for the use of the drug. Bhang taken in moderate quantities is exhilarating and tonic : it creates an appetite and promotes digestion. In large doses, when the intoxication is severe, its effects are very remarkable : the patient is raised to a state of ecstacy and cares neither for his own life nor the lives of others. Sometimes he cries in a delirium of joy and then again breaks out into exulting laughter. Even in moderate doses its effects are noteworthy. Dr. O’Shaughnessy made several experi- ments to ascertain the effects of the drug on men and animals, and in the course of them several of his pupils commenced experiments on themselves which are thus reported : — “ In all, the state of the pulse was noted before taking a dose, and subsequently the effects were observed by two pupils of much intelligence. The result of several trials was that in as small doses as the quarter of a grain, the pulse was increased in fulness and frequency ; the surface of the body glowed ; the appetite became extraordinary ; vivid ideas crowded the mind ; unusual loquacity occurred ; and with scarcely any exception great aphrodisia was experienced. In one pupil, Diuonath Dhar, a retiring lad of excellent habits, ten drops of the tincture, equal to a quarter of a grain of the resin, induced in OF THE NORTH-WESTERN PROVINCES. 765 twenty minutes the most amusing effects. A shout of loud ancl prolonged laughter ushered in the symptoms, and a transitory state of cataleptic rigidity occurred for two or three minutes. Summoned to witness the effects, we found him enacting the part of a Raja giving orders to his courtiers ; he could recognize none of his fellow-students or acquaintances ; all to his mind seemed as altered as his own condition ; he spoke of many years having passed since his student’s days ; described his teachers and friends with a piquancy which a dramatist would envy ; detailed the adventures of an imaginary series of years, his tra- vels, his attainment of wealth and power. He entered on discus- sions on religious, scientific, and political topics with astonishing eloquence, and disclosed an extent of knowledge, reading, and a ready apposite wit which those who knew him best were alto- gether unprepared for. For three hours and upwards he main- tained the character he at first assumed, and with a degree of ease and dignity perfectly becoming his high situation. A scene more interesting it would be difficult to imagine. It termina- ted nearly as abruptly as it commenced, and no headache, sick- ness, or other unpleasant symptom followed the innocent excess.- Dr. Groodeve and more than thirty students were present at this occurrence. In the symptoms above described, we are unavoidably led to trace a close resemblance to the effects produced by the' reputed inspiration of the Delphic Oracles ; perhaps it would not be very erroneous to conclude that it was referable to the same kind of excitement.” MXjum. Majwm or conserve of bhang is a preparation much affected by the better classes. In one maund of jndjum, Mdjum. ag used in these provinces, there are three sers of bhang , two sers of ghi or clarified butter, and thirty-five sers of sugar. It is prepared in this way : — take three sers of clean bhang and soak it for a night in cold water ; next morning take out the bhang wash it well and put it into a basket, to allow the water to drain off. Then place a large shallow iron-pan on a slow fire and throw into it about two and a half sers of good ghi. When this melts and begins to boil throw into it the bhang and fry it until it becomes crisp. Then add water and boil for some hours 766 HIMALAYAN DISTRICTS until the bhang becomes soft and pulpy. Then strain through a cloth and pound in a mortar until a paste is made. You next take a maund of sugar and put it in the pan, adding a sufficient quan- tity of water to melt it. The sugar is then boiled, and while boiling is clarified with milk ; when properly purified the bhang paste is added in small quantities at a time and carefully stirred to ensure its mixing with the sugar. When thoroughly amalgamated, the compound is taken out and spread on flat brass plates about an inch thick, and when this hardens by drying, it is cut into small square pieces with a knife. The quantity of ghi and bhang make up for the loss in clarifying the sugar, and the result is one maund of indjum. The confection costs about Rs. 18 to 20 per maund and is sold to the licensed vendors at Rs. 40 per maund, and these latter retail it at one pice per square to their customers . Two squares are sufficient to produce a moderate amount of intoxica- tion to an ordinary person. People seldom get used to taking majum daily, and it is generally taken for purposes of pleasure and as an excitant to debauch. Another mode of preparation is as follows : — Four ounces of siclhi and an equal quantity of ghi are placed in an earthen or well- tinned vessel, a pint of water is added, and the whole is then warmed over a charcoal fire. The mixture is constantly stirred until the water all boils away, which is known by the crackling noise of the melted butter on the sides of the vessel ; the mixture is then removed from the fire, squeezed through cloth while hot, by which an oleaginous solution of the active principle and colouring matter of the hemp is obtained, and the leaves, fibres, &c,, remaining on the cloth are thrown away. The green oily solution soon concretes into a buttery mass, and is then well washed by the hand with soft watei so long as the water becomes coloured. The colouring matter and an extractive substance are thus removed, and a very pale green mass, of the consistence of simple ointment, remains. The washings aie thrown away, for if used they are intoxicating and produce constiic- tion of the throat, great pain, and very disagreeable and dangerous symptoms. The operator then takes two pounds of sugai, and adding a little water, places it in a pipkin over the fire. When the sugar dissolves and froths, two ounces of milk are added , a thick scum rises and is removed, more milk and a little water aie OF THE NORTH-WESTERN PROVINCES* 767 added from time to time, and the boiling continued about an hour, the solution being carefully stirred until it becomes an adhesive syrup, ready to solidify on a cold surface ; four ounces oi new milk, dried before the sun, in fine powder are now stirred in, and lastly the prepared butter of hemp is introduced, brisk stirring being continued for a few minutes. A few drops of atar of roses are then quickly sprinkled in, and the mixture poured from the pipkin on a flat cold dish or slab. The mass concretes immediately into a thin cake, which is divided into small lozenge-shaped pieces. A ser thus prepared sells for four rupees. One drachm by weight will intoxicate a beginner and three drachms one experienced in its use. The taste is sweet and the odour is very agreeable. The pure resin of the hemp is very soluble in alcohol and ether, partially soluble in alkaline and insoluble in acid solutions. When pure it is of a blackish grey colour, hard at 90°, softens at a higher temperature and fuses readily. It is soluble in several volatile and fixed oils. Its odour is fragrant and narcotic ; the taste is slightly warm, bitterish and acrid. The late Sir W. O’Shaugnessy gives 1 a very interesting historical account of the plant and of the experi- ments made by him on its properties and uses. Mention of the drug is made by the Sanskrit, Arabian, and Persian writers at a very early date. Some trace a reference to it in the gdnja mentioned by Manu, but Williams refers the name to the Abrus precatorius, whilst giving the adjective gdnjakini to anything made of hemp. It is noticed as early as 658 H. { 1259 A.D.) by Musalman writers, and was early introduced into Egypt, where, under the name of hashish , it is still eagerly consumed by the lower classes. As in India, its use by religious zealots has led to terrible scenes of slaughter and rapine, so in Egypt, the sect most addicted to it was called the Hashi- shin or Assassins. 2 Throughout the east, from an early period, it has been used as a medicine and now forms an article of the Indian Pharmacopoeia, prescribed in cases of tetanus, hydrophobia, cholera, delirium-tremens, and neuralgia. A careful chemical examination of the different forms of Indian hemp and their preparations is still a desideratum and worthy the attention ol the many able chemists residing in India. i Bengal Dispensatory, 579-604; Waring’s Dispensatory 16. 2 See Yuie’s Marco Folo, 1., 132. 768 HIMALAYAN districts Spirits. Tlie ordinary country spirit is manufactured in all the hill dis- tricts. It is made from shira and yiir, two forms of the products of the sugarcane. These are placed in a covered tub with water, barley, and certain spices and allowed to ferment. When fermentation has taken place, the tub is filled with water and after two or three days the mixture is ready for distillation. The still in common use is the ordinary rude apparatus of two vessels of metal connected by a tube of bambu. In one the liquor to be distilled is placed and a fire lighted under it ; the liquor passes through the tube into the other vessel which is kept cool by being placed in water. This once distilled liquor, known as tharra, is of two qualities : the rdsi or weaker and the pla'dka or strong spirit. If re-distilled the pro- duct is known as makattav. The process of fermentation takes from ten to twelve days in the hot-weather and double that time in the cold season. The liquor produced from molasses is dearer, hut much stronger than that produced from the mcihua. By one distillation, however, it seldom reaches to 50° under proof by the Syke’s hydrometer, but by several distillations spirits even above London proof may be obtained. In Kumaun, as a rule,, the use of spirituous liquors is confined to the lower castes, though gradually spreading to the better classes ; but in Garhwal the Hindus are less scrupulous, and, according to Traill, all but a few Brahman families drink spirits manufactured there from rice or barley. At the same time, however, they will not drink the spirits manufactured in the plains or after the plains method, objecting both to the materials employed and the caste of the makers. In Garhwal the spirit is made by Rajputs, not Kalwars as in the plains. A coarse spirit is also manufactured from mandna, and the Bhotiyas prepare another called ddru. Betel. Chavica Beteh Miq. — Pan. The pan is imported from the plains. The leaves are used in chewing and are membranaceous or the adult ones coriaceous, shining above, glabrous on both sides ; the inferior ones ovate, broadly cordate, equal-sided ; slightly une- qually cordate or rounded at the base, five to six nerved. The ingredients in the masticatory in common use are the pdn leaves ; OF THE NORTH-WESTERN PROVINCES. 769 sitpdri, the nut 1 of the Areca catechu or betel-nut palm, a native of the eastern islands and cultivated in Lower Bengal and Tia- vancore ; chiina or lime ; and hath or catechu, the produce of the hhair tree (Acacia catechu). Women usually add a small quantity of tobacco to the compound and many add the small cardamom. The average quantity consumed by pan-eaters is about five leaves a day, costing about one and a half pice, or if- fai things. The mix- ture is pleasant and refreshing, but like other things its inordinate use is injurious to the digestion. Marco Polo mentions the use of the plant, which he calls tembal ; the name of the caste still employed in its sale and preparation is Tamboli. The shreds of the unused leaves and the juice of the stalks (pdnri ) are made use o.t in the preparations of tobacco for smoking. XXI. — Vegetable substances used in manufactures. A.— OIL-SEEDS- The only oil-seeds of importance grown in the Kumaun division and the tract under the hills are the rapeseed and linseed of com- merce. The medicinal and other oils have no great value as arti- cles of export and are only procurable in very small quantities. The Bhabar exports great quantities of rapeseed, for which the cli- mate and soil appear to be eminently suited. As so much confu- sion exists in the synonymy of the mustards, the botanical descrip- tion of the more important species is given here to aid in distin- guishing it. Brassica nigra, Koch. Hook, FI. Ind., I., 156. S. erysimoides , Boxb., FI. Ind., 499 — A si rdi, glior rdi, makara rdi, and bandrasi rdi of Kumaun and sarshaf of the hospitals, where the seeds are used for poultices and also in veterinary practice. The leaves are used as a cress. The oil is used chiefly for medicinal purposes. Brassica campestris, Linn., Hook. FI. Ind., 156. S. dichotoma, Roxb., FI. Ind., 497. Erect, lower leaves lyrate, upper auricled, flowers corymbose, beak of pod flat, seedless. An erect, stout, simple or branched, 1 This nut is yellow, oval, the size of a small egg, enclosing an oily kernel like a nutmeg, conical, rounded, pointed and marked with white and reddish veins ; inodorous, but oi a very astringent taste. It contains a large protiou of tannic and gallic acidB. 770 HIMA'LAYAN DISTRICTS glabrous or slightly hispid annual, l-3ft. high. Leaves large, petioled, more or less pinuatifid, upper oblong or lanceolate. Flow- ers large, bright yellow, pedicels fin., ascending or spreading. Pods l^-3in., glabrous, sub-erect; valves with midrib and flexuous veins. Seeds small, smooth, pale or dark. Yar. dichotoma , Roxb., the jariya, jadiya of the hills and lahota laita of the Bhabar, where it is grown only in a few valleys in Kota, and kali sarson of Northern India. Yar. glauca , Roxb., the rdra, rdda, rdra-sarson of Kumaun, banga-sarson of Dehra Dun, and pila-sarson of Oudh and Rohil- khand : seldom grown in the Bhabar, as it yields a crop good in quality, but poor in quantity. Yar. glauca , Royle, the dain, dain , and lai of Kumaun and Garhwal : sometimes khetiya , tori , and toriya of Northern India, where this variety is in general cultivation : grown very largely in the Bhabar. The jariya variety is sown in the beginning of September in fields where manure has been lying. The stalks are cut from the root and when dry the grain is threshed out and the oil is expressed in the common kola or oil-press. It is a favourite crop near Almora. The rdra variety is grown all over the hills in small quantities only, as it requires much manure and is liable to injury from hail. It is sown in first-class unirrigated land in November-December and gathered in April. It yields about three maunds of oil to an acre. The lai variety is cultivated all over the hills up to 11,000 feet and is the staple mustard crop of the Bhabar. These three varieties are grown as oil-seeds and afford the rape-seed of com- merce. Brassica juncea, H./. et T. : Sinapis juncea, Linn. — Rai, sarson. There are several varieties of this species. The S. ramosa, Rox- burgh (498), is the barldi of Kumaun, and the Roxb. — Turmeric — Haldi (root). See Condi- ments. This root is chiefly grown as a condiment, but one variety which when cut has a rich unctuous appearance also yields a yellow dye. When it comes into contact with an alkali it turns red, and is seldom used except for the commonest purposes and by the poorer classes. Berberis aristata, D. C. — Chitra , totar. The bark and root of this species and B. Lycium , known as kingora-ki-jar or ddrhcdd, ddrchob , yield a yellow dye. They are both common in the Hima- laya of these provinces. The colouring principle is found chiefly in the root and affords an excellent dye for leather. The average annual export from the Kumaun forest division is not more than two maunds. Mariscus cyperinus — Nagarmotha , panmotha. The roots are used in dyeing to give a scent to the cloth and also in medicine. Some identify nagarmotha with Cyperus juncifolius. Datisca cannabina, Linn. — Afcalbir (root) , bajr-bhanga (plant). The yellow root is exported to aid in dyeing red and is also used in medicine. Hedychium spicatum> Em. — Kachdr-kachri , Kapur-kachri. The root has a strong perfume and is used in dyeing to scent cloth, also to scent tobacco and as a medicine. The average annual export from the tract between the Ganges and the Sarda is about ten tons. OF THE NORTH-WESTERN PROVINCES. 775 (h.) — Extracted from the bark or stem. Acacia Catechu? Willd .- — Khair (the tree) — Catechu, cutch — ■ hath , Jcatha (the dye). The manufacture of catechu or cutch, or terra japonica as it is variously called, has gone on from time immemorial at the foot of the hills. The men employed are of the Dom caste and are called Khairis from the vernacular name of the tree. They continue at work from November until the rains set in and are aided by their families. Madden’s description of the manufacture still holds good. He writes “One portion of the Khairis is constantly employed in cutting down the best trees, and for these they have to search far in the jungles ; only those with an abundance of red heart-wood will answer. This is chop- ped into slices a few inches square. Under two large sheds are the furnaces, shallow and with a slightly convex clay roof, pierced for twenty ordinary sized earthen pots. These are nearly filled with chips, and water is then poured in and boiled until the contents of twenty will only fill two pots. This operation takes place in about an hour and a half. The liquor resembles thin light port, and the hatha crystallizes on leaves and twigs thrown into it for the purpose. Each pot yields about a seer of an ashy white colour. The work is carried on for twenty hours out of the twenty- four by relays of women and children ; the men merely preparing the wood, which, after being exhausted, is made use of as fuel.” The best samples of hath are clean and whitish or of a pink colour, but some are dirty and mixed with foreign matter. In 1848, hath was worth six rupees a maund in the forests. In the Dun the hath is not allowed to crystallize on twigs, but is poured into clay moulds and made into cakes. Kath is used as an ingredient in the prepared pan so commonly chewed by natives and gives the red colour to the saliva. As a dye it gives brown tints and is largely used for colour- ing sails and fishing-nets. The average yearly export from the forests between the Granges and the Sarda is about 120 tons, though but little catechu is now made west of the Ramganga. The bark of this tree is also used in tanning. Taxus baccata? Linny— Yew — Thaner, geli, gallu, hist. The bark yields an inferior red dye only used in the Bhotiya parga- nahs. 776 HIMALAYAN DISTRICTS Symplocos cratsegoides, Ham. — Lodh , loci. The baric and leaves yield a yellow dye and are used in combination with madder. The average annual export from the tract between the Granges and the Sarda amounts to about twenty tons, of which about nine tons come from the Kumaun forest division. Alnns nepalensis, Don. — Himalayan alder — Udis , kunch , Jcoish. The bark is used in tanning and in dyeing red and is one of the ingredients in the native-made red ink. (c .) — Extracted from the leaves. Justicia Adhatoda, Linn.— Artisa. This plant yields a yellow dye from its leaves by boiling them in water in the proportion of 101b to 161b until half the water has evaporated. In combination with, indigo it gives a dark-blue green. The leaves are procurable at from 20 to 25 seers per rupee. Cinnamomuin Tamala, Kees. — Ddlchini, kirkiriya, sinkauri , and leaves tejpdt. The leaves are more commonly used as a condiment (see Condiments ), but they are also of use in calico-printing in combination with myrobalans. The average annual export from the tract between the Ramganga and the Sarda is about 33 tons of the leaves and 24 tons of the bark. ( Salis. — DTiai, clhaura, tbdwa, dhdrla. The red flowers of this large shrub are used in dyeing silk ; the average annual export for this purpose from the tract between the Jumna and the Sarda being about 27 tons, of' which about 200 maunds come from the Kumaun forest division. The leaves and twigs also yield a yellow dye. Parmelia kamtschadalis? Esch. — Rose lichen — GJiarda, dial- ptiri, charchubilu, chalchalira. This lichen is used in calico-print- ing to give a perfume to the cloth and a rose tinge. The average annual export from the tract between the Ganges and the Sarda is about 25 tons. OF THE NORTH-WESTERN PROVINCES. 779 Tans. (a.) — Tanning agents derived from the baric. Acacia arabica? Linn. — Babul. The bark of this tree is the most plentiful and effective of all those used for tanning purposes. The legumes and leaves also have similar properties in a less degree. Besides tanning a skin, the babdl bark dyes it a buff colour. Cassia Fistula, Linn. — Amaltas^ Jcitola , itola , Jcitwah , svtnhara , sim. The bark of this tree yields a tan and dye and, like the preceding, the pods contain much tannin. The average annual export of the bark from the forests between the Ramganga and the Sarda amounts to about sixteen tons. Shorea robusta, Gkertn. — Sal. The bark of this tree, so well known for its timber, contains tannin, though it is not much used as a tanning material. Butea frondosa, Roxb. — Dhdk , palds. The bark contains an excellent tanning agent much used where babul is not procurable. Myrica sapida, Wall. — Kaiphal. The bark is used in medicine and as a tanning agent. The average annual export from the tract between the Jumna and the Sarda amounts to about seventy tons. » . Bauhinia purpurea, Linn .—Kachnar, Jchdirwal , gurial. A common small tree, the bark of which is used in tanning. Buchanania latifolia, Roxb. Kath-bhildwa , muriya , piydL The bark of this tree is also a tanning agent. Garuga pixmata, Roxb.— Kharpat. The bark yields a tan- ning material. Zizyphus Jujuba, Lam. Ber, Jchalis, guter. This tiee yields a much valued tanning material in its bark. The export of oak bark of various kinds from the Kumaun forest division alone amounts on an average to between 50 and 60 tons per annum. (&,) — Tanning agents derived from fruits. Terminalia Chebula, Retz .—Ear, haraira. This and the fruit of T. belerica form the Chebulic and Beleric myrobalans of com- merce, used as an ingredient in tanning mixtures. 780 HIMALAYAN DISTRICTS Semecarpus Anacardium> Linn. — Bbrilawa. The fruit of this tree, better known as the ‘ Marking-nut tree,’ is used in medicine and as an ingredient in varnish. When pounded and boiled in rape oil it is applied to stay putrefaction in hides. The babul, dhao, bahera, har and dhauri or bdkli ( Anogeissus latifolia , Roxb.) are also used as tanning agents, and the milky juice of the ak or maddr in curing catgut and cleaning leather. C— GUMS AND GUM-RESINS. There are six classes of gums known to commerce, each of which admits of numerous varieties : (1) gum-arabic ; (2) gum-senegal ; (3) cherry gum and the gum of other stone-fruit trees ; (4) gum- iragacanth ; (5) gum of Bassora, and (6) the gum of certain seeds and roots. 1 The first five spontaneously flow from trees and the sixth is extracted by boiling water. Representatives of (1), (3), (4), and (6) occur in Kumaun, and in addition we have the oleo-resin bhilawa and tar and turpentine. The better classification, however, is that proposed by Cooke, viz,: — I — Gums — A. — True gums — (а) — Arabic kind as babul ( Acacia arabica). (б) — Cherry kind as padam (. Primus Puddum). B. — Pseudo-gums — if 1 ) Tragacanth kind as kulu ( Sterculia urens). ip) Baik or Moringa as sahajna (Moringa pterygo- sperma ) . C. — Astringent gums as dhak ( Butea frondosa ). II.— Gum-resins— A. — Emulsive as gota-ganbci or gamboge. B. — Foetid as bring or asafoetida. C . — F ragrant — (a) — Bdellium kind as giigal. (b) — Benzoin kind as luban. *For a full account of the ‘Gums and Gum-resins’ in these Proving “ Notes on the Economic Products of the N.-W. Provinces,” Pari l AUahabmf OF THE NORTH-WESTERN PROVINCES. 781 IIL— Resins— A, — Hard or Copaline — (a) — Pale resins as safed damar ( Vateria indica). (b) — Dark resins as kola damar. B. — S 0 ft or elemi as jangli-b addm ( Canarium commune ). IV-— Oleo-resins— A. — Balsams as bdlsan-ki-tel. B. — Varnishes as bhildioa. 0. — Turpentine and tar. The average annual export of gums, some years ago, from the G-arliwal forest division was about 265 maunds, and of birja or pine- resin about 30,500 pitchers of 2^Bb. each. From the Dehra Dun the export of semli gum is about 786 maunds, and of dhak gum about 27 maunds, whilst about 200 maunds of gum are exported every year from the Kuraaun forest division. Taking gums alone, the average yearly outturn from the Himalayan forests o± these provinces is about 1,300 maunds. If encouragement were offered and trained collectors were employed, the quantity of produce of each kind of gum would be much more than at present ; but so long as African gums can be sold in the London market at their present low rates, there is little hope that this branch of industry can be extended with pro- fitable results. * . I.— GUMS. A. — True gums. Acacia arabica? Willd. — Babdl. This common tree yields the East Indian gum-arabic or gum gattie of commerce used in medicine and the arts. The bazar collections, however, contain the gum of allied species under the same name, babul-ki-gond. The gum exudes spontaneously or is procured by incisions in the bark, when the sap runs out and hardens into small lumps varying in form and size. There are two kinds, the brown and white gum; the former is more esteemed in medicine and the latter in the arts. The gum exudes principally in March- April, and a good tree should yield about 21b in the year. The bazar specimens occur in broken tears of a brownish red to brown, light-brown and white colour, rather brittle with a shining fracture and wholly soluble in water, forming a dark-coloured 782 HIMALAYAN DISTRICTS mucilage. With this gum is usually collected and sold the gum of the following allied species : — A. Catechu , Willd. — Khair. A. Farnesiana, Willd. — Wilayati babul. A. lenticularis, Ham. — Khain. Albizzia procera , Benth. — iSafed-siras, kharanji. A. Lebbek , Benth. — Siras. A. odoratissima, Benth. — Wilayati siras. iEgle Marmelos, Corr. — Bel. This tree yields a good gum- arabic, occurring in tears like coarse brown sugar and of a similar colour. Prunus Puddum, Roxb. — Padam , ptiya, paya. This and the other species of cherry yield a gum-arabic of the stone-fruit kind which, however, is not of commercial importance owing to the smallness of the yield and the presence of other gum-bearing trees. Buchanailia latitolia, Roxb. — Piyal, muriya, kath-bhilawa . This tree occurs commonly in the Bhabar and yields a pellucid gum by incision, known in the plains as chironji-ki-gond. Bauhinia variegata, Linn. — Kaclmdr. This and its allied species yield a gum known as sem-ki-gond. It is said to be a brownish mild gum that swells in water and is only partly soluble. Careya arborea, Roxb. — Kurnbh. This tree yields a greenish gum regarding which but little is known. Cassia Fistula, Linn. — Kitwdli, amaltas. A red juice exudes from the bark and hardens into a gum called kamarkas, regarding which further information is desirable. Cedrela Toona, Roxb. — Tun. This tree yields a resin rather than a gum. Sponia orientalis, Planch., yields a gum of the cherry tree kind. Anogeissus latifolia, Wall. — JDhdivd, dhaura , hdkli. It yields a fine white hard gum used chiefly by calico-printers. Odina Wodier, Roxb. — Jhingan, jiban, sindan. The gum is obtained from incisions in the bark and when solidified appears much like glue. It is used for ink-making and in the finer parts of stucco work. There are two sorts exported from Kumaun ; the OF THE NORTH-WESTERN PROVINCES. 783 white ( Jeanne ) picked from the tree and sold at about ten seers for the rupee, and the black ( jingan-ki-gond ) gathered on the ground and sold at fifteen seers for the rupee. Elseodendron glaucum, Hook. — Bakra , shauriya , mdmri . The gum produced by this tree is known as the jamrasi gum in the Central Provinces. It occurs in roundish tears and is soluble in water. Feronia Elephantum, Corr. — Kath-bel, kait. The gum of this tree is recommended as a substitute for gum-arabic in medicinal preparations. Woodfordia floribunda, Salisb.— DMi, dhaura. The gum of this tree deserves further examination. It appears to be of the tragacanth kind and swells in water. Specimens of the gum from the following trees known to yield gum should be collected and subjected to examination : — Scientific name. Vernacular name. j Pagein | Brandis. Scientific name. Vernacular name. Page in Brandis. Citrus Aurantium ... Narcmgi .. 53 Semecarpus Anacardium, Bhilawa... 124 „ medica Bijaura ... 51 Terminalia Arjuna Arjun 224 rhyllanthus Emblica, Amlika 454 „ tomentosa... Sain 225 Erythrina indica P angara ... 139 „ belerica ... Baker a ... 222 Garuga pinnata Khar pat ... 62 „ Cliebula ... Har 223 Jatropha Curcas Safed-ind 442 Zizyphus oxyphylla ... Jigar 85 Melia Azedarach Ba/tciyan ... 68 „ GSnoplia fieri 86 Morus indica Tut, 408 „ Jujuba Ber 86 Tunica Granatum ... Uarivi 241 ,, rugosa D kauri ... 89 Sapindus detergens ... Ritha 107 Schleichera trijuga Kusumbha, 105 B. — Pseudo-Gums. (a.) — Pale or tragacanth kind. Cochlospermum Gossypium, D. C. — Kumbi. This tree yields the gum katira of the local Materia Medica. It occurs in semi- . ; and if the first filtering yield not such a produce, pass the juice through the ashes a second time. Next, pour this extract of ashes into the metal pot already describ- ed, and boil the extract ; and so soon as it begins to boil, throw into it as many slips or peelings of the inner bark of the paper plant as you can easily grasp, each slip being about a cubit long and an inch wide ; (in fact the quantity of the slips of bark should be to the quantity of juice of ashes, such that the former shall float freely in the latter, and that the juice shall not be absorbed and evaporated with less than half an hour’s boiling) . Boil the slips for about half an hour, at the expiration of which time the juice will be nearly absorbed and the slips quite soft. Then take the softened slips and put them into the stone mortar, and beat them with the oaken mal- let till they are reduced to a homogeneous or uniform pulp, like so much dough. Take this pulp, put it into any wide-mouthed vessel, add a little pure water to it, and churn it with a wooden instrument like a chocolate mill for ten minutes, or until it loses all stringiness, and will spread itself out when shaken about under water. Next, take as much of this prepared pulp as will caver your paper frame (with a thicker or thinner coat according to the strength of the paper you need), toss it into, such a sieve as I have described, and lay the sieve upon the paper frame, and let both sieve and frame float in the cistern : agitate them, and the pulp will spread itself over the sieve ; the grosser and knotty parts of the pulp will remain in the sieve, but all the rest of it will ooze through into the frame. Then put away the sieve, and taking the frame in your left hand, as it floats on the water, shake the water and pulp smartly with your right hand, and the pulp will readily diffuse itself in a uni- form manner over the bottom of the frame. When it is thus pro- perly diffused, raise the frame out of the water, easing off the water in such a manner that the uniformity of the pulp spread shall con- tinue after the frame is clear of the water, and the paper is made* To dry it, the frame is set endwise, near a large fire ; and so soon OF THE NORTH-WESTERN PROVINCES- 797 as it is dry, the sheet is peeled off the bottom of the frame and folded up. When (which is seldom the case) it is deemed needful to smooth and polish the surface of the paper, the dry sheets are laid on wooden boards and rubbed, with the convex entire side of the conchshell ; or, in case of the sheets of paper being large, with the flat surface of a large rubber of hard smooth-grained wood ; no sort of size is ever needed or applied, to prevent the ink from run- ning.” See also As. Res., XIII., 385. In Nepal this paper is manufactured exclusively by the tribes inhabiting cis-Himalayan Bliot, known as Murmis, Lepchas, &c., or generically as Rongbo, in contradistinction to the Sokpo, the name given to the inhabitants of trans-Himalayan Bhot. The manufac- tories are mere sheds, established in the midst of the great forests of the upper ranges which afford an inexhaustible supply of the material as well as of wood ashes and good water, both of which are essential to the manufacture of the raw material into the blocks from which the paper is made. Specimens of these blocks sent to England have been pronounced by experts to be of unrivalled excel- lence as a material for the manufacture of that sort of paper upon which proof-engravings are taken off. Wikstrcemia virgata, Meisner ; the chamliya of Kumaun ; is also common in the lower ranges from 5,000-7,000 feet. The paper made from its bark is considered inferior to that made from the bark of the preceding, as it allows the ink to run unless sized, but the bark also affords a strong cordage material, and ropes made from it are used in Naini Tab Brandis, 386 : Drury, F. P., III., 86. Bcehmeria nivea, H. et A. ; China-grass, Rheea ; grown expe- rimentally in the Dehra Dun and at Saharanpur. Yields the well- known rheea fibre which is specially noticed hereafter. Brandis, 402. Bcehmeria macrophylla, Don. — Gargela; occurs common in the lower hills up to 4,000 feet. B. platyphylla, Don., is also very com- mon and is known as gargela ; both yield a fine fibre fit for twine. Dr. Jameson notes that B. lobata, under the native name ullah, is found in Kumaun and also yields a fibre. Brandis, 403. Girardinia heterophylla, Decaisne, the aiva-bichhu of Kumaun and bdbar of Simla, is a very common weed in the forests along the 798 HIMALAYAN DISTRICTS foot of the Himalaya and yields a fine, strong fibre much used for cordage and twine, but cannot stand much moisture. Brandis, 404. Villebrunea frutescens, Blume, the plvdsar-patta , poi-dhaula and kdgshi of Kuuiaun, is commonly met with along the foot of the hills ascending to 5,000 feet. It occurs in the neighbourhood of Naini Tal and Bhim Tal and along the valley of the Sarjn and Ganges. It has the appearance of a small bambu and grows 6-8 feet, varying in the thickness of the stem from the size of a quill to that of the thumb. It is cut down for use when the seed is formed. The bark or skin is then removed and dried in the sun for a few days ; when quite dry it is boiled with wood-ashes for four or five hours and allowed to cool. When cold it is macerated with a mallet on a flat stone while cold water is applied and gradu- ally the woody matter disappears, leaving a fine fibre which is admirably adapted for fishing lines and nets as well for its great strength as for its power of resisting moisture. Brandis, 406. Maoutia Puya, Wedd. ; the ptiya ofKumaun and Nepal, though sometimes known under the same vernacular names as V. frutescens , is common in the lower hills and Bhabar, ascending to 5,000 feet. Debregeasia bicolor, Wedd. ; the tushiydra of Kumaun ; is very common all over the lower hills ascending as high as 7,000 feet and is particularly abundant in the Siwaliks. It yields a very strong- cordage fibre. Brandis, 405. Memorialis pentandra, Wedd. the juiphal-jctri of Garhwal s is also somewhat common in the lower hills and yields a useful cordage fibre. Drury, F. P., III., 210. Swetenham notices a large nettle as occurring in Garhwal, from the bark of which a fibre is obtained after only three days’ steeping by merely peeling off the rind from one end to the other. He considered it to be in every way far superior to the fibre of hemp. Huddleston mentions the jarkcind- alu, kand-dlu or kalra as yielding a fibre from which sandals and ropes are made in the north of Kumaun. It grows 8-9 feet and the stalks are about as thick as a man’s finger. They are gathered in the cold season and, after being steeped in water for a few days, yield a fibre by peeling from the thick end in the manner of hemp. Both these notices probably refer to G. heterophylla, Decaisne. OF THE NORTH-WESTERN PROVINCES. 799 Artocarpus integrifolia, Linn., (Jack-tree) and A. Lakoocha, Roxb., both yield a cordage fibre from their bark. The former is but rarely seen in the Kumaun division, and the bark of the latter is seldom used for this purpose. Cannabis sativa, Linn. ; C. indica , Humph. ; gur-ldiangci (female plant), pMl-bhanga (male plant). An annual 3-14 feet high according to soil and climate. Root white, fusiform, furnished with fibres. Stem erect, branched, green, angular, covered all over with an extremely fine but rough pubescence. The stem is hollow within or only filled with a soft pith, which is itself sur- rounded by a tender, brittle substance con- Hemp - sisting chiefly of cellular texture with some woody fibres, which is called the 1 reed, ‘ boons, and shov e of the hemp. Outside this we have the thin bark composed of fibres extending in a parallel direction all along the stalk. Lhese fioies consist of delicate fibrils, united together by cellular tissue and all covered by a thin membrane or cuticle. Found abundantly in the Himalayan districts of the North-Western Provinces. The wild hemp known as ganara-bhanga, ban-bhanga or jangli-bhanga , is of little use for fibre. The female plant yields seed for oil and the drugs gdnja (see page 755), charas, &c. The male plant yields only fibre from which the bhang ela cloth of Garhwal is manufactured ; also called kothla, bora and gdji, and the ropes ( sel ) for bridges. For the history of the plant see Royle (Fib. PI., 315) and Drury (U. P., 106). The possibility of attaining success in the cultivation of hemp in these provinces was pointed out by Dr. Roxburgh as early as 1800, and on the cession of these provinces, skilled Europeans were sent to carry on experiments in the Muradabad and Gorakhpur districts. In Garhwal and Kumaun its cultivation was encouraged, and for many years the East India Company procured a portion of its ‘annual investment from the Kumaun hills in the shape of hemp.’ With the abolition of the Company’s trade the cultivation lan- guished and is now entirely dependent on the local demand, which, however, is by no means small. 1 iq P p < I’aners regarding the cultivation of hemp in India,’ Agra 1855 : Royle’s Fibrous Plants of India, Londou, 1855, and Drury’s Useful Plants of India, Madras, 1858. 800 HIMALAYAN DISTRICTS Cultivation The following account of the cultivation is derived from Hud- dleston and Batten’s notes. There are two varieties common in Garhwal, the wild and the cultivated. The former is practically useless either for fibre or the drug, so we shall confine our notice chiefly to the latter. The cultivated variety in Garhwal is grown chiefly on high lands having a northern exposure in well-prepared and abundantly manured soil close to the village site. Occasionally freshly cleared forest land gives a crop for one year without any need for artificial manure. Irrigation is never resorted to, nor is it needed if the soil be properly prepared. The plant does not flourish below 3,000 feet, as the heat of the valleys is prejudicial to its growth, and it seems to thrive best at elevations of 4-7,000 feet. The mountainous region occupied in Garhwal by the Badhan, Lohba, Chaundkot, Chandpur, Dhanpur and Dewalgarh parganahs, has the greatest area under hemp cultivation. These parganas are marked by lofty ranges, extensive forests and a fairly even temperature. The northern parganahs bordering on the snowy range have no hemp cultivation whatsoever, and there is very little in the parganas bordering on the plains, so that it may be said that the hemp- producing area in Garhwal lies between the Pindar on the north and the southern Nayar on the south and is bounded on the east by the western Ramganga and on the west by the Ganges. The cultivation of the plant as practised in this tract is as follows. The ground, after being well cleared and prepared for the seed, is sown, in the end of May or early in June, at the rate of 26 to 33 sers per hi si. 1 During the early growth of the plant the ground is kept free from weeds and the young plants are thinned, leaving a few inches between each, and until the crop has attained a good height, the ground is kept free from all rank vegetation, after which it attains a height of 12-14 feet and is cut in Septem- ber-November. There are two classes of the cultivated plant, the female and the male. The latter is cut some 4-6 weeks earlier than the former and yields a much stronger and superior fibre. On the stalks being cut green, they are dried for several days in the sun by being piled against the walls of the terraced fields until they * The bisi is 40 square yards less than an acre, and the seed used for it is 20-25 pa than, or 52-66 lt>. avoirdupois. OF THE NORTH-WESTERN PROVINCES. 80l become quite brown. The charas is extracted by rubbing the hands oyer the tops of the plant when the seed is ripe and is best in the female plant. The exudation collected is scraped off the hands and made into rolls for sale. The leaves are also pounded for gdnja and sabzi. When the stalks are sufficiently dry they are tied up into bundles and steeped for 15-16 days in tanks or running streams, being kept under water by stoiies laid upon them. When taken out, they are beaten with wooden mallets and then dried in the sun. The fibre is then peeled off from the thick end of the stalk to the top, and after being again beaten and freed from impurities is tied up into hanks for sale and manufacture of sack- cloth for wear and for bags. For wear, the people simply fold the cloth around the shoulders and fasten it in front with an iron skewer, in the manner the inhabitants of the upper parganahs Wear their blankets. Hemp-cloth is still the chief clothing fabric of the poorer classes in Garhwal during the summer months. In Kumaun, hemp is cultivated chiefly in Chaugarkha, especially in pattis Lakhanpur, Darun, Bangor, and Salam. There is also a considerable quantity grown in patti Baraun of the Gangoli par- ganahs, and in a feAv villages in pattis Assi-Chalisi, Uchyur, Mahr- yuri, Gumdes, Dhyanirau, and Malla Chaukot. As in Garhwal there is much prejudice against growing the plant, and it is left almost entirely to the Doms, the Bajputs considering it degrading to them to be styled “hemp-growers. ” So much is this the case that the phrase c tera glmr bhang bono liolo ’ — ‘may hemp be sown in thy house’ — is one of the most common abusive imprecations. Still there are some differences in the obloquy attached to hemp cultiva- tion, for whilst the Khasiyas may, Avithout loss of caste, grow hemp and manufacture rope therefrom for house consumption, they must abandon the manufacture of hempen sack-cloth to the Doms, of whom the Koli, Bora and Agari sections possess almost an exclu- sive monopoly of hemp-weaving. All tribes, however, can traffic in the seed and rope, and even in the charas , without prejudice to their social position. In Kumaun the sowing takes place from the middle of May to the end of June. In warm situations the hemp is soavii rather later, in order that the heat and damp of the rains may cease 101 802 HIM/LAY AN DISTRICTS before the plant shall have time to run into useless stalk and excess- ive seed. During July-August the ground about the plants is hoed and fresh earth is heaped up about the roots. The female plant ripens from about the middle of October to the middle of November, and the male plant, that yields the more valuable fibre, somewhat earlier. In Kumaun, the situation of hemp-growing villages is rarely so high as in Garhwal, and a cold climate, though preferred to that found at elevations below 5,000 feet, is not consi- dered absolutely necessary. The favourite situation for the culti- vation of hemp in Kumaun is a cool, dry, upland ground with a good soil and' with facilities for manuring. Sites near the home- stead or close to cattle-sheds in the pasturing grounds of the upper ranges are consequently chosen for the abundance of manure. Hemp is supposed to exhaust the soil, and the wheat and barley, which are commonly sown in succession thereto, are said to be defective both in quality and quantity. When Dr. Rutherford held his contract for the supply of hemp for the East India Company’s investment, he seems to have managed his enterprise by making advances to the headmen of villages or the principal cultivators ; and should the cultivation of hemp ever again become a commercial speculation, this would seem to be the best method for obtaining success. The produce of a Usi has been estimated at about three seers (bib.) of cJuivctSj foui' maunds (3201b.) of hemp fibre, and 30-35 seers (60-701b.) of seed, yield- ing about five seers (101b.) of oil. In 1814, the fibre was pro- duced for four rupees per maund delivered at the cultivator’s doors or five rupees delivered at Kotdwara or Chilkiya, and it would appear that now a price of from six to seven rupees per maund of 82tb. would ensure a constant supply. In 1840, the entire value of the hemp produce in Kumaun, including seed, fibre, and drug, was little more than Rs. 1,000, and Captain Huddleston estimated the total area under hemp in Garhwal during the same year as only 250 acres, yielding about forty tons of fibre per annum ; but there is every reason to believe that the outturn has since considerably increased in quantity, and a rough estimate would point to 780 acres under hemp in Garhwal alone in 1880. The seed is collected to be used as a vegetable food, for which purpose, indeed, it is chiefly cultivated in the Sor and Sira parganahs, or to be pressed for the OF THE NORTH-WESTEEN PROVINCES. 803 extraction of hemp-oil or to be dried and retained for seed. The cluxras or juicy essence is collected for exportation, being hardly, if at all, used in the hills. It now sells at from four to five rupees per seer, and is resold by the farmer of the drug monopoly at eight rupees per seer. The farm of charas in Kumaun alone during 1880- 81 was sold for Rs. 3,357. The leaves, too, are dried and exported for use in the various preparations of bhang. The fibres, as already noticed, are made into ropes or sack-cloth. In Kumaun the sale of the untwisted fibres is more common than that of the twisted or manufactured stuff. In 1840, the seed sold at about three rupees per maund, and is now worth about three to four rupees per maund, and in some places where it is chiefly used for culinary purposes is even cheaper. The fibre where it was produced sold at from two to three rupees per maund in 1840 and is now worth from three and a half to four rupees a maund. The bhangelci or hemp -cloth is made up into sheets for weaving or into Icotlas or sacks, and the finer sorts into thailis or bags for carrying flour and lime. A large sack-cloth baa: cost but six annas at Almora in 1840 and is now worth twelve annas. Bags of a smaller size cost about two rupees per dozen in 1840 and are now proportionately more expensive. The produce is so small and the demand for bags for sending potatoes to the plains so great that these sacks are yearly advancing in price, and a consi- derable trade in them exists at Ramnagar and Kotdwara. Mr. J. H. Batten, in one of his reports, gives the following opi- nion on the prospects of hemp cultivation in Kumaun : — “ If a large demand for hemp, the produce of these mountains, were to arise and it were to become generally known that capital to a Prospects of the hemp considerable amount was ready to be ex- industry. pended for the purpose of procuring the article, a very great increase of hemp cultivation might be expected even in Kumaun Proper, but especially from the Chaugarkha par- ganah. If European capital should hereafter be employed in increasing the growth of the excellent hemp existing in this province, I should certainly recommend that the means first used for the purpose should be an outlay of money in advances to and purchases from the present growers and manufacturers, rather than in the attempt on the part of any enterprising individuals to procure land and grow hemp for themselves. Notwithstanding 804 HIM A' LAY AN DISTRICTS their prejudices, I think that the example of their neighbours, if the latter attained to any fair degree of prosperity from the increase of trade, would soon he followed by many villagers throughout Kumaun, who now are indifferent to or despise their advantageous situation for the growth of hemp, and large tracts of land now waste would be brought under cultivation. There are not in Kumaun, .as in Garhwal, many waste villages still left unowned and unclaimed ; and from what I have seen of the character of the people in Kumaun Proper, I think that any stranger who should purchase or rent land within the boundary of a village, for the purpose above indicated, would be quite as liable to litigation, inconvenience with his neighbours, and prejudices against his position, as in any part of India, however populous in compari- son. In the case of advances and purchases on the contrary, the transactions of capitalists would be confined to simple contracts, of a nature to which, if found necessary, the law is open at a cheaper cost, and under simpler forms, than in most other parts of the country.” Captain (now Sir Henry) Ramsay, in a report on the same subject, writes : — “ I would not advocate the system of making advances to individual cultivators : it is not improbable that some ill-disposed persons might create a suspicion that Government intended evil instead of good and actually produce the effect of making those who now grow hemp discontinue its cultivation for a time ; the best plan I think would be to enter into engagements with respectable zamindars for large quantities and allow these contractors to make their own arrangements. The cultivators are quite equal to taking care of themselves in such dealings.” Hemp is also grown in the northern parganahs of Nepal, and the mode of cultivation there is thus described by Mr. B. H. Hodgson:— “ The seed is sown from March to April. Damp soils, comprising black earth, are fitted for this crop. Before Cultivation in Nepal. . . n m • i ploughing the held, sufficient manure is to be sprinkled over it, then completing the work of the plough, the seeds are to be sprinkled, and having broken the clods into dust, the field is to be made even. At seven or eight days after sowing the seeds the plants come up, but their rapidity of growth and their size and strength depend on the abundance of the rains or artificial watering. If the plants be OF THE NORTH-WESTERN PROVINCES. 805 very thick, they must be thinned, so as to stand three inches dis- tance from each other. They flower and fruit in Sawan (July), and at the beginning of Bhadon (August) are in their full growth ; but while yet succulent and in flower they are to be cut, with the exception of some seed plants, which are not to be gathered until October. It is the bark of the young but full-grown or Sawan plants (which is soft) that is used for making bhungela. That of the old or October plants is hard and not suitable for manufacture. After the plants have been cut off at the ground, they must be placed in the sun for eight or ten days, or until they be dried suffi- ciently. They must then be steeped in water for three days, and on the fourth day the plants must be taken out of the water and peeled. The peelings are to be washed and put in the sun ; and when quite dried, they are ready for manipulation. They are then to be torn into thin threads with the nails of the hands; next twisted with a spinning-wheel ( tikuli ), and when the threads are thus pre- pared, they are to be boiled with ashes of wood and water in a pot for four hours, and to be washed again for the purpose of whiten- ing. This is the w r ay of preparing bhangela thread, out of which sack-cloth is woven. One mdna (half a kachcha ser ) of seed is sufficient for a ropini of land (one-fifth of a badshahi biglici or 60o square yards), which produces ten or twelve loads of bliang. Hemp grows equally well on slopes and flats, and neai the tops as well as on the sides of the mountains, if not too low. But a moist rich soil is indispensable. The plant attains to a height of eio-ht to ten feet, and should be cut when the flower is falling and the seed forming.” For an account of its cultivation in other countries, see Boyle (Fib. PL, 3bh). Hemp prepared for the European market should have the fibres laid parallel to each other and then be simply tied near the thicker end so as to form heads like the Petersburgh hemp, not twisted, plaited and tied, as is the custom in our hills. The Himalayan hemps show strength, divisibility, fineness and softness of fibre- in fact all the essentially good qualities which a fibie should possess. Clia, interops ‘Martiana, Wall., the jhangra, jager, and thdhl of Kumaun, occurs' on Bhatkot, Tlmkil, Dhnj, and in the valley of the 806 HIMALAYAN DISTRICTS karju. The fibre is used for cordage and the leaves for mats and baskets. Brandis, 546. Calamus Rotang, Linn. — Rattan — bet; occurs abundantly in the Eastern Dun, in places in the Siwalik tract and along the outer hills eastwards. It yields the common rattan so much used in uphols- tery and for basket work. Brandis does not consider C. Royleanas, Griffith, as distinct. This species has also its western limit in the Delira Dun and is known under the same vernacular name and used for the same purposes. About fifty bullock-loads are exported every year from the Kumaun forest division. Brandis, 559. Typha angustifolia, Linn. ; Yar. elephantina, Roxb. — Bora . This species occurs throughout the North-Western Provinces and Oudli, ascending the hills in the Kali valley, and indeed in most of the valleys bordering on the plains. It is the reri of the upper districts, and the variety elephantina is the pacleri or pateri of the hills. The leaves are much used in the manufacture of soft matting, and from Kumaun alone about twenty bullock-loads of the raw material and 3,500 pieces of the matting are exported every year. T. lati folia , Linn., is called patera in Bijnor and kanda-tela in Garhwal, and the leaves are largely employed in the manufac- ture of a coarse matting called boriya , of which some 900 maunds are annually exported from Kumaun. In fact these two species afford the chief matting materials in common use. I am not aware that the leaves have ever been used for other purposes. Roxburgh, 648 : Drury, F. P., III., 495. Arundo Karka, Roxb., the Jcarka and nal of the Kumaun Bhabar, is of common occurrence in suitable localities. A. ( Phrag - mites) Roxburghii , Kunth., is the bichhra of Garhwal and the Jchaila and khailuioa of the Kumaun Bhabar, ascending up to 3,500 feet in the valleys. A. nepalensis is the nal , nal-tura, and tot-nal, common in the Bhabar and found at Bhim Tal. All these are sent to the plains under the generic name ‘ nal ’ and are applied to cane-work in chairs, matting and similar uses, and the fibre of the flower-stalks is manufactured into rope. About 220 bullock-loads are yearly exported from the Kumaun forest division. Roxburgh, 117. Saccharum Munj a, Roxb. — Munja. The upper half of the culm is known as sirki-munja or sirki; the lower half as sent ha or sarpat; OF THE NORTH-WESTERN PROVINCES. 807 the blade twisted and beaten yields the strong cordage known as munj ; the tufty leaves are called sarlcctra towards Hardwar. Munj abounds along the banks of rivers and in sandy places and generally along the base of the hills from the Jumna to the Sarda and up the valleys to 3,500 feet. The fibre is made from the sheathing leaves of the culm and forms the material from which the janeo or sacri- ficial thread of the Hindus is made. Munj is commonly employed as a tow-rope from possessing great elasticity and strength, with a power of resisting moisture common to few other fibres. It is also used for the riffo-inc of boats, the bottoms of cots, chairs, and footstools, mat- ting, in the manufacture of coarse paper, and as a string for fastening the bambu framework for the roofs of houses, and indeed for all com- mon purposes in every district. The sirlci is used for thatching, a covering or pawlin for carts, and for chairs and the like. Under the names bind and mdnj a considerable amount of the various products of this grass are sent to the plains. The returns for four years from Kumaun give an average export of 1,600 bullock-loads of the unmanufactured article and about 75 maunds of the rope. Drury, F. P., III., 653. Saccharum spontaneum, Linn., is the Msh, jasha or jhdnsh of Kumaun, according to Madden. It occurs commonly in the Bhabar and lower hills and is found near Almora, where its long- rooting surculi are substituted for the Jcuska grass in religious ceremonies by the local Brahmans. The leaves yield a thatching grass and matting material and a fibre useful for string for common purposes. Roxburgh, 79. Eragrostis cynosuroides under the names ddbh and kasa is used in the religious ceremonies of the Hindus. Saccharum fuscum, Roxb., is a common reed of the Bhabar, where it is known as tat, neja (grass), and mora ; it is the kilik of the plains. The culms are used in the manufacture of screens and pens. The average annual export of this reed from Kumaun amounts to over 800 bullock-loads. Drury, F. P., III., 653 : Roxburgh, 79. Saccharum Sara, Roxb., is the sarhar or sar-ur of the sub- montane tract, where it is very common. This reed is also used as a matting material and for chairs and the like, but the fibie is inferior to that of S. Munja, with which it is often confounded. 808 HIMALAYAN DISTRICTS It is said, however, to be employed as a tow-line ill Mirzapur, and must therefore possess tenacity and strength. Roxburgh, 82. Eriophorum comosum, Wall., Scirpus comosus, Roxb.; babar, bab, bdbilci, and at Almora pan-babiyo, only found in the Siwaliks and in low hot localities in the interior on base and steep slopes. It forms but a small portion of the fibre exported to the plains as babar or bliabar grass. The jlitila or rope bridges erected where sangas or planked bridges cannot be made are chiefly formed of this fibre in Kumaun. They are safe for men and sheep and last about a year, when the ropes require renewal. The chhinkas or bridges of a single cable bearing a transverse seat are sometimes made from it, and it is also extensively used in rafting timber. The principal portion of the babar grass of commerce is derived from the Spodiopogon angustifolius , Trin. Drury, F. P., III., 530. Cyperus tegetum, Roxb.; Papyrus pangorei, Fees ; motha ; grows wild and is also cultivated on the edges of inundated fields for the sake of its culms, which form an excellent material for matting. The culms whilst green are split into three or four pieces, which, in drying, contract so much as to bring the margins into contact, in which state they are woven into mats and thus show nearly a similar surface on both sides. C. rotundas , Linn., also known as mothci , is applied to similar uses in a lesser degree. Roxburgh, 68, 70. Imperata arundinacea, Cyrilh, is the shiro of the Bliabar and lower hills, ascending to 7,500 feet. The culms are used for the same purpose as those of mtinj, and the leaves for thatching and matting. Drury, F. P., III., 652. Anthistiria arundinacea, Roxb., is the ulu, ullah , kangtir and kandura of the Bliabar and affords the same products as the pre- ceding. Drury, l. c., 650. Anatherium muricatum, Beauv., is the gandar of the sub- montane tract. The roots are commonly known as has or khas and the culms as sink. The latter are exported from Kumaun with the sirki of the mtinj under the same name and are used for the same purposes. The roots are exported for making tatties, dyers’ brushes, and fans. Drury, l. c., 644. OF THE NORTH-WESTERN PROVINCES. 809 Spodiopogon angustifolius Trin.; Andropogon involutus, Steud.; the bdbar of the tract from the Jumna to the Sarda. Dr. J. L. Stewait writes : — “This grass, which is abundant in the Gfarhwal Himalaya and occasional on the skirts of the Siwaliks, appears to furnish almost all the material called bdbar so largely used for string in these parts (Bijnor). Botanists from Wallich and Hoyle downwards have stated this to be the produce of Eriophorum comosum, of which, however, only a very small proportion of that brought to the plains consists. Dr, Brandis first drew my attention to the probability of the ordinary belief being erroneous, and subsequent inquiry has shown the case to be as above stated. The string is very coarse but strong, and, although there is great waste in the manufacture, exceed- ingly cheap. It is well adapted for boat-ropes, the rope-work of bedsteads and other ordinary purposes. Possibly the bdbar may come into play as a paper material ; at least it is worth the trial, and probably larger quantities of the raw article could be got than of any other fibre in this part of the Himalaya.” (J. Agri.-Hort. Cal., XIII., 293). The raw material is procurable for about eight annas per matmd and the fibre at four times that price. About 25,000 bullock-loads are yearly exported from the Kumaun forest divi- sion. Cymbopogon laniger, Desf.; Andropogon Iwarancusa, Roxb.; is known variously as miriya , ban, ganguli , dab, and piriya in the submontane tract. It ascends the hills up to 5,000 feet at Almora and is found along the Sarju as far as Bageswar ; flowering in April. The culms are exported with those of the mora for similar purposes, and the leaves are used for thatching and coarse matting. The culms and leaves of C, Martini, Munro, are applied to similar uses. Roxburgh, 92. Bambus. — The genera included under the common name bambus are sufficiently numerous and important to deserve special notice here in connection with their use as a half-stuff for paper-making. Following the arrangement of Brandis, we shall briefly refer to each in the order given by him in his 1 Forest Flora’: — 1. Arundinaria falcata, Nees — NingdL Madden notes that the people of the Danpur pargana in Kumaun enumerate no less than eight kinds of ningdla or ringdl as it is pronounced in Garhwal, 102 810 HIMALAYAN DISTRICTS viz., — thcim, utham , kutino, malingo, jhumro or jhungra, cleo-ningdla , gorningdla, and dom-ningala. The last is probably the common or kali-ningala found abundantly along the Gagar range, and, like the jhumro , in much request for pens. Dr. Falconer referred it to the genus Thamnocalamus. The tham is said to be the largest of the whole and is sent down to the plains for hukka pipes. The deo- ningdla is the A. utillissima of Edgeworth, and occurs in great abundance in the snowy range, especially in the upper valley of the Pindar. It affords excellent material for matting, baskets, fishing- rods and the like. The gor-ningdla is the gol of Bisahr, with their culms eighteen feet high, occurring in dense clumps of a hundred or more each. Brandis (p. 562) gives to A. falcata a range of 4,500-10,000 feet, ascending to 12,000 feet from the Ravi to Nepal, abundant in places, gregarious, often forming underwood in moist forests of Abies Smithiana, A. Webbiana, and Quercus seme- carpifolia. It flowers in May and the seeds ripen in August. 2. Tharnr, oca Iannis spatliijlorus , Munro — Ringal. This is probably the kdli-ningdla of the preceding notice, occur- ing in Danpur. It is recorded from Deoban in Jaunsar, Diidatoli in Garhwal, and Kumaun at elevations 8,000-11,000 feet. T. Fcil- coneri, Hook. /., is also recorded from the Madheri pass in Kumaun. See Brandis, p. 563. 3. Dendrocalamus strictus, Nees. — Bans. To this species belongs the great mass of the bambus exported as minor forest produce from the Jumna to the Sarda. For the Garhwal forests, Dr. J. L. Stewart gives the following classification of cut bambus, beginning with the least valuable : — 1. Chhaneju, [chhaneju, K.), long and thin, used for roofing purposes. 2. Lathi or IdthicMr [lathi-baha, K.), thicker, shorter, solid, for walking-sticks and clubs. 3 Bdlu, similar, but thicker, for sides of cots. 4. Kanemva ( kanderu , K.), between the last two in thickness but chiefly used for roofing purposes. 5. Sardicha ( sardinchu, K.), much thicker, shorter, hollow; also used for roofing purposes. 6. Dash'itta, similar, but much longer. OF THE NORTH-WESTERN PROVINCES. 811 7. Bhengi ( baliaga , K.), thickest of all and less hollow, used for tent and dooly poles. See further Brandis, p. 569. Bambus form the most important portion of the minor forest produce of all the forest divisions and one that increases in value every year, but it is to the materials for half-stuff in paper-making which they afford that we wish to invite attention here, and for this purpose will refer to a paper 1 by Mr. J. Routledge on the subject. In his opening paragraph, he writes : — “ Of all the fibre-yielding plants known to botanical science there is not one so well calculated to meet the pressing requirements of the paper-trade as ‘ bambu,’ both as regards facility and economy of production as well as the quality of the ‘paper- stock’ wdiich can be manufactured therefrom. Grown under favourable conditions of climate and soil there is no plant which will give so heavy a crop of available fibre to the acre and no plant that requires so little care for its cultivation and continuous production.” Attempts have been made in England to obtain from the bambu a half-stuff or pulp for paper manufacture, but these have failed chiefly from using the plant when it had attain- ed to some degree of maturity and the fibre had become extremely dense and the external skin hard and silicious. In this state the processes for softening the material and converting it into pulp by long-continued boiling or digesting in very strong solutions of caus- tic alkali at a high temperature were troublesome, expensive, and dangerous. Mr. Routledge would therefore take the young plant, and by a system of close plantations well watered and systematical- ly cropped ensure successive growths available for preparation into stock. His estimate is as follows: — “Allowing 208 feet square to represent one acre divided into {twelve beds each 96 x 26 feet with twelve paths 96' x 8'8" wide and one intersecting road 208' x 16' wide, leaves a space for planting equal to 2,496 feet, or 29,952 feet in the twelve beds ; allowing the stems to be 2 feet apart and (say) only 12 feet high, we have 7,488 stems, which at 121b each will yield 40 tons to the acre.” Assuming that these 40 tons of green stems will lose 75 per cent, of moisture in drying, ■we have 10 tons of dry stems to the acre, which will yield 60 per i Bamboo considered as a paper-making material, by T. Routledge : London, 1875. 812 HIM X LAY AN DISTRICTS cent., or six tons of unbleached fibrous paper-stock baled up in merchantable condition. It is unnecessary to enter into Mr. Routledge’s system of treating the bambu for the manufacture of paper-stock, our object being merely to show that a practical paper- maker considers it possible to turn the preparation of bambu fibre into a profitable commercial speculation. Nothing has yet been attempted in this direction in India. WOODS. The timber-producing trees of the Himalaya of these pro- vinces are sufficiently described in the admirable work of Dr. Brandis on the Forest Flora of North-West and Central India , to which the reader must be referred for Timber trees. . descriptions of those trees noticed hereafter and of those which do not claim a reference in a work like the present one. The forests themselves will be enumerated in the succeeding chapter, and here we shall only refer generally to their more valuable timber-products. The forests below the hills and those clothing the outer spurs contain sal, sisu, tun, and trees belong- ing to the genera Acacia Terminalia, Anogeissus, Adina, and Stephe- gyne, besides the grasses popularly known as bambus, all of which are of the first importance for house-building, furniture, agricultu- ral implements and boat- building. From them is derived the greater portion of the revenue in the State forests, and omitting them, there would be little of any practical value to record. In the upper hills, the conifers clothe almost every ridge and valley within the zone of arboreous vegetation, and with oaks and rhodo- dendrons, the box, maple and birch afford, if proper precautions be observed, an inexhaustible supply of every class of wood equal in quality to that procurable in Europe. The sal of the submontane tract and the cedar of the hills are held in the highest esteem and have been much worked in all easily accessible forests, but there are other trees that afford a timber equally suitable for most of the pur- poses to which the former are now applied. The bdkli, sain, lialdu , and gosam of the submontane tract and some of the oaks, the pine, spruce and fir of the hills give very valuable timber fit for every- thing except perhaps railway-sleepers, and it will be necessary, should the existing demand continue, to call on the reserve of these OF THE NORTH-WESTERN PROVINCES. 813 trees to supply all common wants. This can best be done by rais- ing the duty on the more valuable timber, and the sooner a move- ment of this so.t is made, the better it will be for the future of the sdl and deodar forests, which now require rest and care. Bambus have already been sufficiently described on a previous page (p. 809) , and it will not be necessary to notice them further here. We shall, therefore, restrict ourselves to a brief description of the most impor- tant trees in the forests of the submontane tract and of the coni- fers, oaks, and a few other timber trees in the hills. All of these have an ascertained value and are the chief sources of the timber supply for the plains. Shorea robusta, Goertn. — Scil, Jcanddr, sakhu (plains). Brandis, 26 : Hook., I., 306. The sal occurs along the foot of the hills from the Jumna to the Sarda and also in the Duns. It ascends the hills in places to 3,000 feet and is found in the valleys to a great dis- tance inland, notably along the Sarju and Ramganga. It is the most valuable and most sought after of all the timber trees of the submontane forests and from time immemorial has been exported to the plains. It is usually the characteristic tree of the tracts which it affects, and though other trees occur, the sal predominates. In the Patli Dun and other places where pure sdl forests exist and. thrive, the soil is usually composed of alluvial deposits, and drift in the valleys and plateaus and sandstone or conglomerate interspersed with blue shale on the ridges. Brandis notes that the climatic con- ditions favourable to its growth are a rainfall of 40-100 inches and a mean temperature during the four seasons within the following limits: — cold-season, 50-70°: hot season 77-85°: rainy season, 80-88°: autumn, 74-77°. The sdl grows, as a rule, to a height of 60 to 90 feet with clear stems 30-40 feet long and 6-8 feet in girth. Further east under Nepal it attains much larger proportions and measurements are recorded of trees 100-150 feet in height and 20-25 in feet girth. Captain Wood has estimated the growth to be on an average (in the Oudh forests) 54 feet in 65 years and 72 feet in 95 years. The wood is reddish coloured, coarse-grained, even-fibred, hard, strong, tough, and so heavy that it cannot be transported by water without the aid of floats. The average weight of a cubic foot is 50-60fb. — with variations 40-691b. — and its specific gravity is over 1,000. The transverse strength as ascertained 814 HIMALAYAN DISTRICTS from numerous experiments varies from 609 to 972. Baker found that a six-feet bar, two inches square, broke at 12381b., and Brandis also records a number of experiments. Cedrela Toona, Roxb. — Tim , trim. Brandis, 72. The trim is not now very common west of the Ramganga except in the low moist valleys leading into the Path Dun and in parts of the east- ern Dehra Dun, and even to the east of that river the reserves have been denuded of most of the mature trees. The tun attains a height of 60-70 feet, with a girth of 6-10 feet. The heartwood is close-grained, hard, capable of taking a high polish like mahogany, and when properly seasoned is deservedly known as an excellent furniture wood. A cubic foot weighs 29-361b, and the co-efficient of transverse strength ranges from 420-560. In one of Baker’s experiments, a six-feet bar, two inches square, broke at 8001b. Stewart notes the interesting fact that in the small family to which the tun belongs there are four other valuable timber-trees, only one of which, the mahogany ( Swietenia Mahogani), is extra- Indian. The others are Satin-wood ( Ohloroxylon Swietenia, D. C.) ; rohuna (Swietenia febrifuga, Roxb.), and Chittagong wood ( Chickrassia tabularis , A. Juss.), all of which are indigenous in Southern India and the last also in Eastern Bengal. The tun ranks as a first-class timber in the forest tariff. The wood of C. serrata , Royle (Bran- dis, 73) the dala of Kumaun and ‘ bastard-toon ’ of Europeans, is of a lighter colour than that of the true tun and is used in the hills for house-building and the like. Schleichera trijuga, Willd.— Gosam, gausam, hosam. Bran- dis, 105. This tree occurs in the Siwalik tracts and Duns, ascend- ing the valleys to 3,000 feet. It attains a height of 60-70 feet and a girth of 5-6 feet. The wood is reddish brown, close-grained, tough, hard and heavy, and weighs 66-7 01b. to the cubic foot. It is much used for the crushers (cMran) for oil and sugarcane mills, pestles, rollers, agricultural implements and carts, and all work in which toughness and strength are desirable. Dalbergia Sissoo, Roxb. — Sliisham, sissu. Brandis, 149 : Hooker, II., 231. The sisu occurs throughout the submontane tract and Duns in moist places on the banks of streams and on islands in the rivers. It attains a, height of 40-60 feet, with a OF THE NORTH-WESTERN PROVINCES. 815 girth of 6, and in very rare cases up to 12 feet. The sap-wood is light coloured and the heart-wood is of a deep brown colour, close- grained, hard and capable of taking a high polish. A cubic foot of seasoned wood weighs 45-50fb., of unseasoned wood 64-70fb. The co-efficient of transverse strength ranges from 700 to 900, be- ing superior to nearly all other woods. A six-feet bar, tw r o inches square, broke at 1,1041b. in one of Baker’s experiments. Sisu is useful for all work requiring strength and elasticity, and is much employed for furniture, house-building, boat-building, carts, beds, saddle-frames, and agricultural implements. It is considered a first-class wood in the forest tariff. Ougeinia dalbergioid.es, Benth.; Dalbergia Oogeinensis , Roxb. — Sdndan , sanan, ckandan. Brandis, 146 : Hooker, II., 161. It occurs chiefly in the valleys of the outer hills, ascending to 5,000 feet and attains a height of 40-50 feet with a girth of 3-5 feet and occasionally 7-8 feet. The wood is close-grained, hard, strong, tough, and very durable. A cubic foot weighs 57-601b., and it is much valued for wheels, ploughs, furniture and indoor household work. It is one of the first-class timbers in the forest tariff. Acacia Catechu, Willd.; Mimosa Catechu , Linn., M. Sundra, Roxb. — Khair. Brandis, 186. The khair occurs along the sub- montane tract and in the Duns,'- ascending the valleys to 3,000 feet. It has been much worked for the extraction of hath, and in the more accessible tracts few large trees remain. It attains a height of 30-40 feet, with a girth of 4-6 feet and occasionally 8-10 feet. The heart-wood is of a deep red colour, close-grained, hard, tough, elastic and heavy. It is admirably suited for crushers ( cliuran ) for oil and sugarcane mills, and for this purpose yields only to the tamarind. It is also largely used for axles, pestles, pins, plough-shares, cotton-rollers, wheels, bows, spear-handles and the like, and is one of the most valuable of the second-class woods. Its product, hath, has been noticed elsewhere (p. 775). Terminalia tomentosa, W. et A.; T. crenulata and coriacea, W. et A.; Pentaptera crenulata , coriacea , and tomentosa , Roxb. Sain , a sin, asain, sdj. Brandis, 225. This tree is common in the .submontane tract and the Duns, attaining a height of 80-100 feet, 816 HIMALAYAN DISTRICTS with a girth of 8-10 feet. The heart-wood is dark-brown, tough, strong, elastic, and very durable. A cubic foot of seasoned wood weighs 601b, varying from 50-70tb. The co-efficient of transverse strength is 860, varying from 591-1,104. In one of Baker’s experiments a bar six feet long and two inches square broke at 9031b. It is used for indoor household work, carriage shafts, agricultural implements, rice-pestles and boat-building, and is one of the best of the second-class woods now coming into general use. Terminalia Chebula, Retz. — liar , harara. Brandis, 223. This tree occurs in the Siwalik tract and outer hills ascending to 5,000 feet and along the hot valleys in the interior. It attains a height of 60-80 feet and a girth of 5-10 feet. A cubic foot of seasoned wood weighs 54-60fb. The timber is of a brownish colour, close- grained, heavy, capable of taking a high polish and fairly durable. It is used for furniture, indoor household work, and agricultural implements. T. belerica, Roxb., the bahera of the submontane tract, yields an inferior wood, of little value, though used for planks. Anogeissus latifolia, Wall., Conocarpus latifolia , Roxb. — Dhaa - ri , bdkli, clhawa. Brandis, 227. This handsome tree is common over all the submontane tract and is found in Dehra Dun, imparting a fine copper tint to the foliage of the forests in winter. It attains a height of 60-70 feet, with a girth of 6-9 feet. The timber is close-grained, of a brown colour, hard, tough, and elastic. A cubic foot of the seasoned wood weighs 57-65ib, and of the unseasoned wood 75-80!b. The co-efficient of transverse strength, according to Skinner, is 1,220, but is placed much lower by others. From its elasticity, the bdkli variety is especially fitted for cart-poles, axles, axe-handles and the like, and it is gradually coming into great demand as the prices of the superior timbers have risen. It is well fitted for all house-building and agricultural purposes, though said to be not very durable when exposed to moisture. The bark of the bdkli variety appears to be of a lighter colour than that of the dhauri variety, while the leaves are smaller and it grows to a greater height. Adina cordifolia, II. f. et Benth.; Hauclect cordifolia, Roxb. — Haldu. Brandis, 263. The haldu occurs abundantly in the open OF THE NORTH-WESTERN PROVINCES. 817 plain along the foot of the hills from the Sarcla to the Ramganga and less commonly westwards through the Dehra Dun to the Jum- na. It ascends the valleys to 3,000 feet. It is not gregarious and is remarkable for its trunk being often buttressed like that of the semal. Trees GO-100 feet high and with a girth of 10-18 feet are not uncommon in the Bhabar. The average weight per cubic foot is 42fb., varying 36’3-49Ib. The co-efficient of transverse strength is about 700. The wood is yellow, smooth fibred and fine-grained and is fairly durable. It seasons well, works easily and takes a fine polish, and is suitable for turnery, though some- times apt to warp and crack. It is now much used for indoor household work, planks, boxes, the keels of boats, combs, writing- tablets, gun-stocks, and agricultural implements. Stephegyne parvifolia, Korth.; Nauclea parvifolia , Roxb.— - Kaim , kangai , phaldu. Brandis, 262. This tree is gregarious, though occasionally met solitary in the open plain. It grows to a height of 50-60 feet, though specimens of 80 feet have been recorded and the average girth is 6-7 feet. The weight of a cubic foot of sea soned timber is 35-47tb., of green timber 54th., and the co-efficient of transverse strength is 586-683. The timber is durable if not exposed to moisture and is applied to the same purposes as the preceding. This and all other woods of the sub- montane forests, except sal, sissu, tun , and sdndan come under the designation ‘ Katrukh.' Quercus semecarpifolia, Smith — Rarslm, sauj. Brandis, 479. This species occurs at high elevations 8, 000-10, 000 feet. Madden records it at Naini Tab It attains a height of 70-80 feet, and a girth of 7-8 feet is not rare. It grows slowly and gives a hard, heavy tim- ber that will not easily bear export, but on the spot is used for house- building, bedsteads, poles, helves and ploughs. It is said to warp on exposure and to be liable to the attacks of insects. Quercus lanuginosa, Don. ; Q. lanata, Wall. — Rianj, rai-bdnj. Brandis, 481. This species occurs at Naini Tal and a few other places in Kumaun, 6,000-7,500 feet. The word is of a greyish- brown colour, hard and very heavy, and is not easily worked. It is much liable to the attacks of a small black hymenopterous insect which often riddles it completely in a few years. 103 818 HIMALAYAN DISTKICTS Quercus dilatata, Royle ; Q. floribunda, Lind. — Tilonj , kilonj , moru. Brandis, 482. This species is common on the outer ranges from the Jumna to the Sarda at 4,500-9,000 feet. Pearson notices the noble forests of this oak in the valleys of the Bhagirathi and Jumna rivers. It attains a height of 80-90 feet and a girth of 8-9 feet, and Madden records one 100 feet in height and 19' 8" in girth. The wood is of a brownish colour, hard, durable and heavy. It is used for agricultural purposes and house-building and is considered the best of all the oaks for carpentry. Quercus incana, Roxb. — Bcmj. Brandis, 482. This species is common on the outer hills from the Jumna to the Sarda. It generally attains a height of 20-30 feet, with a girth of 4 — 5 feet. The wood is used for house-building and agricultural purposes and ranks second to the preceding in popular estimation. Madden records Q. annulate /,, underthe names ‘ phaliaut ’ or phaniat ,’ as occurring in Naim Tal ; it is the pharonj of Eastern Garhwal. Buxus sempervirens, Linn.; B. Wallichiana, Baillon. — Box — Papari. This tree occurs in the upper hills at 6,000-8,000 feet and is common in the Bhagirathi, Jumna, and Tons valleys. The wood is very close-grained, hard and heavy, weighing 60-651b. per cubic foot, and selected pieces are fitted for all the purposes to which European box is applied. Acer oblongum, Linn. — Patangliya , kirmali. Brandis, 110. This species occurs up to 6,000 feet in the great valleys. It is used for agricultural implements and from its knots some of the better wooden drinking-cups exported to Tibet are made. A consi- derable number of these cups are made from the knots of A. pictum , Thunb., which is common in the hills above 7,000 feet, and is also used for agricultural purposes and house-building. Betula acuminata, Wall. — Himalayan Birch — Puya-udish or utis, Brandis, 458. This tree occurs in sheltered places 6,500- 10,000 feet on all the outer ranges. The wood is close-grained and takes a fine satin polish. It is particularly good for panels for doors, and the examples in the Government-house at Naini Tal show that it is a valuable acquisition for ornamental work. The alder, known as 1 udish,’ is the A Inns nepalensis , Hon., which occurs at lower elevations and is also used for house-building pur- OF THE NORTH-WESTERN PROVINCES. 819 poses and gives a fair-sized log, from which planks may be cut for tea-boxes and the like. The wood is light and somewhat brittle, but takes a satiny polish like the birch. The people towards the snows use the bark of the silver birch ( Betula Bhojpatra, Wall.; Brandis, 457) for writing and packing in place of paper. CONIFERS. As already noticed, the conifers constitute the most valuable section of the timber-producing trees of the upper Himalaya both for quantity and quality. In many parts of the country they occur in unbroken masses extending over many miles and present a scene of magnificent grandeur unknown elsewhere. Each species has its own peculiar beauty, but perhaps the wide-spreading cedar with its branches almost reaching to the ground is the finest and well deserves the epithet ‘divine-tree’ given to it by the old Hindu poets and still in common use to designate it from Kashmir to the Ganges. We have added Stewart’s analytical key to the conifers and a list of vernacular synonyms compiled from the writings of C leghorn, Madden, Stewart, and Brandis, which seem necessary in order to understand the very confusing local nomenclature : — i i Analytical ley to the chief arboreous Conifers of the North-Western Himalaya by the late J. L. Stewart, M.D. 3 OF THE NORTH-WESTERN PROVINCES. 821 Local names of the Conifers of the North-West Himalaya. 822 HIMA'LAYAN DISTRICTS s 3 cS a 3 W ■ VS 3 M ■-3 8 '2 v£ o & 2 P 5 3 W rc 3 • bfi d M/a 3 od £ a i a v“ 'os a WWW £*-i S3 -3 c3 CO O CZ 2 fca 3 $ o -►3 O d GO G» O P vc3 £ cl © Ph S • O CD .pH PP o 3 ’ I ^ . 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Badar ■ •> DQ Vi 'D Oi < d d 4-a 02 d 0 O • 03 x d 03 OQ w $ v ' V P4 a ^ r- 5 0) M K d ' H S ^ P -rH V C3 03 rj ft 3 ^ Oi d d *-s 824 hima'layan districts Pinus longifolia, Roxb. — Long-leaved pine. Madden, J. Agri.- Hort. Soc. Cal,, VII., 75 : Brandis, 506 : Cooke, 125 : Roxb., 677, The long-leaved pine. CMr (in Sanskrit “ kshira ,” or “ milk”), sula (Sansk. sarala, “ straight”) in Kumaun ; kolon, kolan, kolain in Garhwal ; saral in Jaunsar ; thansa above the Dun ; dhiip in Oudh. To the west of Grarhwal the name chir or clnl is applied to P. excelsa , except in Kunaor, where P. longifolia preserves the name chir with the indigenous affix 1 sthV or ( shthi’ (M.) The chir occurs all through the Ivuinaun Division, dividing the forest with oak, from 1,600 feet above the level Distribution. . of the sea at Sitakoti, eight miles above Deo- prayag in Garhwal, to 7,200 feet on the Pindar river. The limits at which it is found vary much in different parts of the Himalaya between Afghanistan and the Tista, and apparently the upper limit descends the further east we proceed from Kumaun. 1 As a rule, however, 2,500 feet is the lowest height at which it seems to flourish. The chir appeal’s to have the power of driving out all other vegetation from the tracts it occupies, and forests of these trees are interpersed only with scanty underwood of the smallest shrubs. Madden and Brandis note the curious phenomenon observable in many of these pines in Kumaun. This consists in the spiral arrange- ment of the bark and woody fibre, the coils being sometimes as much compressed as those of an ordinary corkscrew, and in some instances the stem itself is thus distorted. Straight trees are found mixed with these contorted specimens in the same forest in Kumaun, and they do not appear to occur in Garhwal or in the higher ranges in Kumaun. The straight variety is known in Kumaun by the term sapin. The wood of the straight variety is usually of a reddish white colour, and is preferred for building purposes, as the other is liable to warp and split in working, though in the log form capable of bearing heavy strains. It is, however, rarely used except as fuel. Dr. Jameson thinks the crooked variety is confined to localities with a southern aspect and under 5,000 feet, but the fact remains that crooked and straight trees occur in the same forest with the same aspect, as may be observed near Ganai and Pyura. 1 Hooker gives the upper limit in Sikkim as 2,000-2,500 feet ; Grifith fives the lower limit in Bhutan at 1,800-2,000 feet. At Ramesar bridge on the Sarju in Kumaun, 1,500 feet above the sea, it descends to within a few hundered yards of the river. OF THE NORTH-WESTERN PROVINCES. 825 The forest survey of 1865-66 estimated the total area under chir as 413,650 acres in Kumaun and 152,264 ^ acres in Garhwal. Many acres of forest contain 20 large and 50 small trees per acre ; but in a square mile the bare places bring down the average to 20 trees per acre. First- class trees are those having a girth at five feet from the ground of eight feet and over ; second class have a girth five to eight feet ; third class, two feet to five feet, and fourth class under two feet. The first-class trees average about one-twelfth, the second about one-fifth, and the third about one-third of the total number per acre. This would give a total of about twelve million cMr trees in the Kumaun Division, of which one million beiong to the first class. The forests lying along the Gumti, western Ramganga and east- ern Ramganga approximately contain the following trees : — Trees per acre . Acres. 1st. 2nd. 3rd. 4th. Sources of the Gumti towards Baijnath ... 61,440 3 5 5 7 Upper Sarju from Kapkot and Phungar 42,380 2 4 5 6 valley to Bagesar. Middle Sarju from Bagesar to Naini bunga- 28,280 1 3 5 7 low. Lower Sarju and Ramganga from Naini 40,020 2 3 5 7 to junction with the Kali. Middle western Ramganga from Ramari .. 11,790 1 2 6 7 Lower western Ramganga and Katyur 22,985 1 2 4 7 river. Between Bino and the Ramganga beyond 32,300 2 5 8 12 Lohba. Between Badliangarh and Latugarh 16,000 3 12 12 12 In the Tarag Tal valley ... 5,760 2 12 9 12 In the Gumti valley 8,960 3 10 10 7 To the west of Budha Kidar and Bikya-lce- 11,460 1 3 7 13 sain, to the east of Masi bungalow. The Soni jungle ... ... 2,560 4 5 9 31 Nearly all these trees grow on slopes rising from the river-beds, and near enough to repay the cost of cutting and launching. The trees on the upper western Ramganga and its tributaries are mostly twisted, though towards Bungidar they are straight and so placed as to be easily shot into the Bino river. Following the stream of the Ramganga, the north-east banks from Garoth down to Bagri have 104 826 HIMALAYAN DISTRICTS first-class timber covering all the slopes of the Badhangarh and Gopalkot ranges, and could be easily worked into the Ramganga. The Syuni jungle near Chaun Debi is one of the finest in Kumaiin. The large trees have all straight boles without a knot and with much red wood. The soil is light, micaceous sand on loose beds of earth and stones, which appears to be eminently suited to the chir. In Garhwal there are extensive chir forests in the valley of the Alak- nanda and along the Pindar from Chuding (4,800 feet) to Gwaldam (4,300 feet), a distance of thirteen miles. In the three upper miles the timber is small, but lower down there are fine straight trees close to the river-bank, and a flat near Chiringa suitable for a timber depot. All along here and up the Kailganga, for two miles, the forest could easily be worked. The forests on the Mandakini and Madmahesvar rivers have been worked for railway sleepers, but in many places tlie timber is too remote from the river for removal. The forests along the N ay ar and Chlnpkalgkat rivers are extensive and yield good straight timber. In native Garhwal there are almost inexhaustible forests of c/uV, along the Bhagirathi between Sainsu, some twenty miles above Tihri „ and Bhatwari, a distance of fifty-five miles. There are numerous patches along the head-waters of the Jumna and the Tons, and the left banks of both rivers are clothed with one immense forest capable of supplying all possible wants. Describing these forests Colonel Pearson writes: — “It would be difficult adequately to describe the enormous seas of chir forest which line its bank. In these the trees must be numbered not by thousands but by hundreds of thousands, and many of them are of huge size.” The lower hills towards the Dun and the Siwaliks themselves contain large quanti- ties of pine, and taking the entire forest area of the hills, the long- leaved pine may be considered the characteristic tree for quantity, but for quality it ranks below several other conifers. The great object at present is to find some inexpensive process for preserving' it from the effects of exposure by creosoting or covering it with a permanent silicious coating. The chir grows even in the plains and ; specimens can be seen at Meerut and Saharanpur. It occurs, as we shall see, in every sub-division in the hills in abundance and in places from which it can be easily removed. It is often used for boat-building, but boats made of it seldom last for more than seven OF THE NORTH-WESTERN PROVINCES. 827 though ranking below the cypress for durability. It does not stand exposure to excessive moisture. In the form of planks it is said to warp badly when exposed to the sun, and to become affected by dry-rot if placed in contact with damp earth. The highly resinous, small, knotty branches are used for torches, and the charcoal of the entire tree for smelting iron. The tree grows to a great size, the average girth of the larger trees being 13 feet. The rings average fifteen to the inch and the weight of a cubic foot is about 251b, with a specific gravity of *686. A piece of this timber of average quality, 22 inches long and one inch square, broke with a pressure of 368fb. Cedrus Deodara, Loudon; Pinus Deodara, Roxb — Himalayan cedar — the deodar , diyar of Kumaun and Garhwal ; the kelon, kelu of W estern Garhwal and Jaunsar, where the name deodar is given to the Cupressus torulosa : deva-ddru (divine tree), Sansk. Madden, J our. Agri.-Hort. Soc., Cal., VII. : Brandis, 516 : Cooke, 128 : Roxb., 677. There are no natural groves of deodar in Kumaun and only one large forest in Garhwal. There are numerous plantations around tem- ples in Kumaun, aggregating about 800 acres. Amongst them may be mentioned those at Lodh, Bala- Jagesar, Pharka, and the groups at Sui, Rikhesar, Mankesar, Kalsia, Simalti and Ghatot near Lohu- ghat, and Kshetrapal near Somesar. Along the western Dhauli be- tween Kak and Malari there is a natural forest having an area of about 1,500 acres and giving one second-class, three third-class and eight fourth-class trees to the acre. At Lata on the Rishiganga there are about 70 acres of fine, healthy trees, one giving a girth of 30 feet, and at Parbati, near theNandakini and Shatul, there are some fine groves. The average girth of the largest trees in these provinces appears to be OF THE NORTH-WESTERN PROVINCES. 831 about 15-20 feet. Major Garstin measured some near Malari over 20 feet in girth at six feet from the ground. The cedar yields an oleo- resin similar to that of the chir ; the oil is used in medicine and the twigs and branches are also said to possess medicinal properties. j ' k - , . The great cedar forests of these provinces occur along the Bha- girathi valley and in Jaunsar-Bawar, and these are fully noticed in the accounts of those forests given hereafter. Dr. Brandis writes : — “ The deodar for the first three or four years of its life grows slowly, attaining 12-20 inches in height with spreading roots that do not go deep down. In this shrubby and stunted state the young plant can maintain its existence under the shade of other trees for considerable number of years without making much progress : but when light overhead is given, then a leader is at once formed which shoots up rapidly. At a more advanced age, the rate of growth of the deodar is determined without difficulty by counting the annual rings.” The existing records show that the growth is influenced very much by the climate. In the dry valley of the Bhagirathi the rate of growth is much slower than in Jaunsar, where there is a heavy rainfall, so that in the former tract a tree takes 86 years to increase from 4/6 " to 6 feet, whilst in Jaunsar this is accomplished in 23 years. Within each tract also the rate of growth differs considerably. Colonel Pearson noticed in the Bha- girathi valley a stump 6'9" in diameter with only 305 rings, and. in another part of the same valley a tree with a diameter of only 4 feet showed 480 rings and two having a diameter of only 18 inches had 145 and 147 rings respectively. The wood in these slow-growing tracts usually has a closer grain and a deeper colour than the timber grown on southern aspects and in a moister climate. The soil too in these tracts is generally poor and is formed from the decomposition of granite, gneiss, and clay slate, and in the rapid- growing tracts the soil is richer and deeper. Isolated trees, such as those at Wan, often attain a great size. Dr. Stewart measured one at Kuarsi in the Ravi basin, at an elevation of 7,500 feet above the level of the sea, 44'2" in girth at two feet from the ground and 36'4" in girth at six feet. Dr. Brandis records that one was measured at Parbani in Kunaor 34'4", and that the girth attained by the largest trees there is 30-36". Madden measured one between 832 HIMALAYAN DISTRICTS Nachar and Turanda in lower Kunaor (in 1830) having a girth of 36f feet at five feet from the ground. The tallest deodar measured by him was in the Nachar forest on the Satlaj, 250 feet high, 20 feet in girth at the base, and more than 550 years old, and there was a considerable number of trees in the same forests more than 200 feet high. Moorcroft measured a fallen tree on the Tugasi hill in the Dhauli valley and found it 159 feet : another was 180 feet in height. Many experiments have been made to ascertain the transverse strength of deodar taken from the Panjab, the Garhwal, and the Kumaun forests. The weight of a cubic foot appears to vary from 25 to 401b., but in Garhwal approaches more the latter ; in one series giving an average of 371b. A well, seasoned piece, 22 inches long and one inch square-broke at 3451b. It had a specific gravity of *655 and showed eight rings to the inch. The result of eight experiments on Garhwal timber made at Rurki (390-798) gave an average of 592. The result of a series of experiments at Almora in October, 1844, conducted by Captain W. Jones, ten with timber cut in the preceding month and ten with seasoned timber, is shown in the following table. In the first ten experiments the distance between the supports was four feet and the pieces were two inches square : in the second ten the distance between the supports was increased to eight feet and the pieces were 2J X 3" Specific gravity. Weight pro- ducing deflec- tion of Breaking weight. Remarks. £ inch lb. Ib. •608 1,036 1,588 Good straight grained wood. •710 1,024 1,636 Lower side split a little at 1,060. Not straight-grained and Blightly flawed. •698 736 880 •669 1,060 1,540 Lower side split at 1,308. •620 904 1,456 Ditto 904. •585 680 976 Broke suddenly. •574 680 708 Ditto. •614 344 • •• Ditto No flaw perceptible. •586 568 1,204 Ditto. •604 624 • » • Lower side went at 624 ; uneven grained OF THE NORTH-WESTERN PROVINCES. 833 Specific gravity. Weight pro ducing deflec- tion of Breaking weight. Remarks. 1 inch. 2 inches. ft. ’641 350 764 820 Snapped suddenly : light-coloured ; said to be outside of tree. •618 400 788 1,028 Heart of tree red and oleaginous. '644 344 660 908 Snapped short suddenly ; light-coloured. '679 428 876 1,116 Heart of tree very good and red. •678 344 736 964 Snapped suddenly, but was in appearance the best piece of all five. •566 •629 344 344 680 576 750 624 0 Good sound wood, but knotty, coarse > and wavy in grain ; snapped suddenly ; at knot. •619 512 960 1,188 Dark cedar- coloured, fine grained ; broke at knot. •630 598 1,080 1,700 Dark cedar-coloured ; under-side very fine straight grained and light- coloured. •603 484 876 1,092 Dark cedar-coloured, but rather coarse in grain. The timber of the deodar is the most highly prized of all the conifers for house-building, granaries, chests, boat-building, and railway sleepers. It appears to be little affected by extremes of heat, cold or moisture and is easily worked. In a climate like that of Kashmir it appears to be almost imperishable. Moorcroft states that the pillars of the great mosque erected by Aurangzeb at Srinagar showed no vestige of decay from exposure or insects at the time of his visit, and that pieces of deodar from the Zain-ul- kadal bridge were found little decayed, although exposed to the action of water for four hundred years. Many of the other bridges still standing in Srinagar may perhaps claim a greater antiquity. Gerard records some timber in a house in Basahir as being 200 years old and as sound as the day it was cut. The cedar is a sacred tree in the hills and is in much demand for the temples, for the doors, walls, and roofs. Madden notes that he saw some beams in a Kunaor temple that were said to be 600 to 800 years old and showed no signs of decay, and though this may be an exaggeration of his informants, it indicates the popular belief. Boats built of deodar and lined with clixr last from thirty to forty years, and for railway sleepers no other wood can compete with it. White-ants eat the sap-wood and but rarely attack the heart-wood, and neither the sap-wood nor the heart-wood is liable to dry-rot. Immense numbers of sleepers of this w r ood have been supplied from the 105 <834 HIMALAYAN DISTRICTS Bhagirathi and Jaunsar forests during the last fifteen years. The Jaunsar forests on the Deoban ridge between the Jumna and the tons were estimated by Colonel Pearson in May, 1869, to contain -34,000 available first-class trees and the Bhagirathi forests (exclud- ing the Bhilang valley) 116,700 first-class trees. If to these are added the probable contents of the valleys of the Tons and Jumna rivers, the total number of first-class trees available in 1868-69 was about 500,000. The proportion of smaller trees may be gathered from the following estimate of those in the Bhagirathi valley : — First-class or above 6' in girth Second-class or 4'6"-q' „ Third-class or Fourth-class, below 1'6" ... 116,700 ... 53,660 ... 127,536 ... 213,281 Since 1868-69, however, there has been a great diminution of first-class trees to supply the numerous requisitions for railway- sleepers and public works. Abies Smithiana, Forbes ; A. Khutrow, Loudon ; A. spinulosa, Griffith; Pinus Smithiana , Wallich; P. Khutrow, Boyle; Picea Morinda , Link. — the Himalayan spruce ; Smith's spruce — the morinda and rdi of Jaunsar ; kandre , re, rhai, rdo, kudrau , rdi ala , rdglia, kail, kdluchilu and kiu of Garhwal. Madden, Jour. Agri- Hort. Soc., VII., 87 : Powell, I., 564 : Cleghom’s analytical key to the Conifers : Brandis, 525 : Cooke, 127. Smith’s spruce, according to the survey, is found in the north of Garhwal near Joshimath and in the Dhauli and Vishnuganga valleys. The forest survey of 1865-66 estimated the area under this tree in Garhwal at 26,908 acres. The following are the principal localities, with the size of the forest and the number of each class of tree per acre : — Trees. Locality. Acres. 1st. 2nd. 3rd. 4th, Near Kanol, Peri and Shatul on the upper Nandakini On the slopes of Tamba Deo near the 6,328 2 3 4 4 western Dhauli ... Near Golabkoti on the left bank of the 50 1 3 3 3 western Dhauli ... ••• 2,050 5 5 5 7 On the Biriganga and Rishiganga • • • 13,000 5 4 5 7 Further up the Rishiganga ... 4,980 2 4 6 8 OF THE NORTH-WESTERN PROVINCES. 835 Dr. Griffith describes this spruce as growing abundantly on the northern ranges of Bhutan, 7,800-11,600 above the level of the sea, preferring northern aspects and occurring in masses below A. Webbiana. It is rare in Sikkim and confined to valleys of the inner range at 8,000 to 9,000 feet mixed with A. dumosa and seldom exceeding 50 feet in height. It has not been found in Kumaun, and Madden states that he was unable to detect a trace of it in Danpur, Juhar, or along the snowy slopes of Nan da Devi and Nanda Kot. Nor were Bhotiyas of Milam, accustomed to traverse the mountains, able to recognise the cones or dried specimens. It is not mentioned in Webber’s survey as occurring in Kumaun, but is said to be indigenous on Rikholi Gudari and occurs, as we have seen, in the valleys of the Nandakini and western Dhauli. On the left bank of the Bhagirathi above Jliala it is found with cedar, silver fir, and birch on the slopes having a northern aspect. It occurs also in the forests of the upper Jumna and Tons and in Jaunsar. The spruce grows to an immense size. Webber mentions one on the Nandakini 18 feet in girth and 110 feet in height. Hodgson records the length of a fallen tree as 169 feet, and Madden gives the girth of ten trees as varying from 13 \ to 20 feet and showing an average girth of 16 feet. Dr. Stewart has record- ed one of 21 feet, but the average girth is from 8-12 feet with a height of 100-150 feet. As has been noticed, the spruce prefers a northern aspect, and this is but one of many instances of the pheno- menon which strikes every traveller in the Himalaya, that of the northern and north-western aspects being densely wooded, whilst the south and south-eastern are wholly or almost bare. Baron Hugel, as quoted by Madden, thus refers to the valley of Perhamgala in the Pir Panjal range : — “ Strange to say the south side (aspect) of the valley is everywhere wild and dreary, while fine trees grow up to the very summit of the mountain on the north face. The reason may possibly be found in the fact that on the south side the repeated action of alternate freezing and thawing destroys every kind of vegetation except a few grasses.” The wood is white ; the outer part turns red and decays rapidly if exposed to moisture, so that it is seldom used except for indoor work. A very dry piece 22 inches long by one inch square broke at 2881b., being the weakest in a series of experiments of all the conifers. The specific gravity was 836 HIMALAYAN DISTRICTS only 426, though the piece in question averaged 14 rings to the inch. The bark is used for roofing purposes and to make rough water-troughs for cattle, and the young cones form a part of the drug sold as gaj-pipal in the bazars. Abies dumosa, Loudon ; Pinus dumosa, Don ; P. Brunoniana , Wallich — Hemlock spruce of Nepal — the tungsing of the Bhotiyas of Darma in Kumaun ; changathasi dhup of Nepal. Madden, Journ. Agri.-Hort. Soc., VII., 95 : Brandis, 527. The forest survey in 1865-66 gives the total area in Kumaun under this tree at 3,650 acres. The principal localities, with the size of the forest and the number of trees per acre according to class, are as follows : — Trees. Locality. Acres. 1st. 2nd. 3rd. 4th. Lola Kot and IvalaMundi, to the west of the 140 1 2 2 4 Gori river, mixed withA/hes Webbiana. In Chaudans and Byans, to the north-west 650 2 6 5 6 of the Dhauli. Manktil danda and in the valley of the 1,160 1 2 3 3 Chirkila gar, falling into the Dhauli. At Titala Kot near the Kali 600 2 3 3 4 Spurs of Panch Chula above Tunik 920 2 4 6 6 In Byans near the Kali ... 1,000 2 4 4 10 It was first discovered by Captain Webb in 1810 and again by Mr. Webber in 1863. Dr. Hooker found it in Sikkim in narrow gorges on the southern flank of Kanchinjinga at an elevation of between 9,000 and 10,000 feet. In the innermost valleys the limits are 8,500 and 10,500. The Gorkhali name there is 4 thingiyd or 4 tingtiri-sallaj and the Bhotiya name is 4 semadting .’ One specimen measured 27 feet in girth at five feet from the ground. Griffith found it in Bhutan at 6,500-9,700 feet above the level of the sea, and it is said to be indigenous on Gosainthan and Banepa. In Kumaun, it occurs in Darma and about the Chipula range at 9,000-11,000 feet, and here it is called 4 tungsing ’ and attains a height of 80-100 feet, with an average girth of 10-12 feet. The timber is white, fine-grained and light, having a specific gravity of •612, but is said to warp much from exposure. The bark is used for thatching purposes. OF THE NORTH-WESTERN PROVINCES. 837 Abies Webbiana, Bindley ; A. Pindrow , Boyle ; A. densa , Griffith ; Picea Webbiana, Loudon and Wallich ; Pinus spectabilis, Lambert — Himalayan silver-fir. Madden separates the variety known as Picea Pindrow , Hoyle, from A. Webbiana, Wallich., though the names of both are the same in the vernacular ; rdglia and rdo rdgha in Kumaun ; wuman amongst the Bhotiyas of Darma ; bang, dodlima rdglia, teliya or chili rdgha in South-eastern Garhwal ; chilrao in Central Garhwal ; mornnda in North-western Garhwal and Jaunsar ; raunsla or rdi salla about the sources of the Kosi in parganahs Barahmandal and Danpur and on the Dudu-ki-toli range near Lohba in Garhwal. Madden, Jour. Agri.-Hort. Soc., Cal., VII., 96 : Brandis, 528. Madden thus describes his Picea Pindrow of Hoyle : — “ It flowers in April and May, when the young shoots are of the brightest green, the old leaves being nearly black. The trunk is branched nearly to the ground, but cones are produced only on its loftiest boughs. By the middle of May the cones are about 3 inches long by one in diameter and more or less cylindrical. As the sea- son advances, they become more or less completely so, and of a rich dark purple colour. They ripen in October and November. The cones of P. Webbiana are less cylindrical, thicker and shorter, and the bracteoles more rounded, scarcely emarginate, and with a thicker and longer apex. The spiral arrangement of the scales seems identical, and each has the same copious supply of white resin. The cones of P. Pindrow are perfectly cylindrical ; the scales more prominently eared ; bracteoles oval, obtuse, eroded, emargi- nate, the mucro of the same length as the border of the sinus.” This variety forms dense forests on all the great spurs towards the heads of the Pindar, Sariu, eastern Ram- Localities. , ganga and Kali rivers : near the sources of the Kosi at Bhatkot and on the Dudu-ki-toli range, near the sources of the western Bamganga. The other variety is thus described as the Picea Webbiana of Wallich. .— “ Tree tall, very narrow and like the cypress. Branches short, thick, scrubby, and declining at the extremities. Foliage very dark green ; near its upper limit of a grayer colour. Bark somewhat 838 HIMALAYAN DISTRICTS smooth, tessellated by shallow farrows into small squares ; young branches silvery. Leaves three-quarters of an inch to two inches long, flat with three small points, in two rows on either side of branches and twigs. Cone erect, rather short, cylindrical, dark purple, scales broad, dark-coloured near edge, deciduous. Ripe in October. The tree flowers in May, when the strobili are of a pur- plish red. Remarkable for its upright columnar appearance.” It occurs at Ramni on one of the spurs of the Trisul, between the Pindar and Alaknanda up to the glaciers, Localities. and on the summit of Dudu-ki-toli. The forest survey, 1865-66, gave an estimated area for Kumaun of 13,110 acres, and for Garhwal of 53,280 acres. The principal localities, with the number of each class 1 of tree per acre, are as follows : — Locality. Acres. Trees. 1st. 2nd. 3rd. 4th. On the left bank of the Nandakini in Garh- 790 1 1 7 6 wal, atChati Bukiyal andGudari Bukiyal. At Sliik,Kanol and Sliatul, near the same river 5,600 2 3 3 3 Above Kiraoli in the Pindar valley 1,040 2 6 7 12 On the Kailganga and above the Pindar ... 1,230 1 6 8 9 On the Pindar from Gumra Pani to Chuding, 3,680 1 4 4 7 Between the Pindar and Sarju and east of 1,890 2 2 3 3 the Ramganga. About Munsyari 670 2 2 4 5 In Darina, Chaudans, and Byans 2,900 2 4 6 8 On the spurs of Tungnith, and in the valleys 4,370 2 4 4 5 of the Nigholi and Balsukhi rivers. To the left bank of the Alaknanda, on the 6,070 4 4 6 8 Pilkanta and Ramari ranges. On the left bank of the western Dliauli 15,100 5 5 • • 8 On the npper Nyar ... 3,200 2 6 8 10 Dudu-ki-toli range ... ... 8,800 2 6 8 10 On the spurs of Ranch Chula ... 3,910 5 5 7 8 • Deo Thai in Agar Patti, Kumaun 3,200 1 3 4 4 The forests on the Pindar could easily be worked, and that river can carry the largest logs with ease. Those on the Balsukhi and on the Mandakini, near Kedarnath, are too high up to be access- ible. In the Bhagirathi valley, above Jhola, it occurs with cedar, spruce and birch, and in the upper valleys of the Jumna and Tons and their tributaries is abundant, associated with oaks. It is also found throughout Jaunsar along the ridges of the main range and of the lateral spurs and on Surkhanda near Masuri at an elevation Classes as in chir ; first, 8 feet in girth and upwards ; second, 5 to 8 ; third, 2 to 5 ; and fourth, under 2 feet. OF THE NORTH-WESTERN PROVINCES. '839 of 8,200 feet. It occurs on the Dudu-ki-toli range in Central Garh- wal at 7,500-10,000 feet and on Tungnath up to 11,200 feet. Brandis notes the limits in Jaunsar, Garhwal, and Kumaun to be. 7,500-13,000 feet ; it nearly reaches the latter elevation in the Mun- syari district and in the Nandak valley ceases at 12,000 feet. Griffith states that it forms vast forests at 12,000 feet in Bhutan, below the belt of rhododendrons, and in Sikkim, under the Gorkliali name ‘ gobriya-salla and the Bhotiya name £ dung siring’ it occurs abundantly in the zone 9,700-11,500 feet. The limits in the south- erns flanks of Kanchinjinga and crests of the inner sub-Himalaya are 10,000-12,000 feet, hut in the inner valleys and rearward ranges 9,000-13,000 feet. In the north-west Himalaya, it thrives best in cold damp glens with a north or west aspect, and in such places, according to Brandis, constitutes alone or associated with the Alpine birch the upper forest belt. The silver-fir attains a height of 120-150 feet and an average girth of 9-15 feet, though specimens exceeding 20 feet in girth have been noticed. The wood is white, soft, rather coarse-grained and inodorous and is not much esteemed. It is not durable when exposed to moisture or the sun and is chiefly used for indoor work, though in dry climates where better wood is not obtainable it is split up and used for shingles. A piece 22 inches long and one inch square broke with a weight of 3791b. The specific gravity of this piece was ‘491 and it showed 16 rings to the inch. The following table shows the results of some experi- ments on the transverse strength of the silver-fir made by Captain W. Jones at Almora in 1844. The distance between the supports in the first five experiments was four feet and the pieces used were two inches square. The distance in the last five experiments was increased to eight feet and the pieces used were 2j% inches in depth by 3 inches in breadth : — Specific gravity. Weight produc- ing deflection of Breaking weight. Remarks. £ inch. Ib. •472 680 940 Broke at a knot one foot from the centre. •559 512 880 Broke suddenly ; no flaws perceptible ; •546 820 1,206 deflection £ths. •518 820 1,084 •560 736 904 840 HIMALAYAN DISTRICTS Specific gravity. Weight produc- ing deflection of Breaking weight Remarks. - 1 inch. 2 inches. n$. •436 344 652 780 ) Broke gradually ; all very moist and *481 514 944 1,064 S soft. •434 372 740 788 Broken at a knot. •458 456 848 930 •483 400 764 968 Cupressus torulosa, Don — Himalayan cypress — Surui , surdi, Kumaun and Grarhwal ; rdi scilla, Naini Tal ; leauri of Jaunsar ; to the west and towards Simla it is called deodar ; and the name surai is given to Juniperus excelsa. Madden, l.c. : Brandis, 533. Found in Chaudans, Naini Tal, and of remarkable size near Ramni and Wan on the Kailganga in Grarhwal, and from Joshimath to Niti. The forest survey of 1864-65 estimates 1,200 acres of cypress in Kumaun and 4,938 acres in Grarhwal. The principal localities, with the number of trees in each, are as follows : — Trees. Locality. Acres. 1st. 2nd. 3rd 4th. Right bank of the Nandakini near Ramni, Guni, Bura, Barkuna, Shik, Ali Bukiyal 17 1 3 6 10 601 3 3 6 6 and Wan, near the source of the Kail- ganga. On the Kailganga and at Ketha and Mel- 378 3 4 5 4 khet, on the Bindar and higher up. Near Pandukeswar on the Yishnuganga, 150 • • • 2 3 4 a difficult river. On the left bank and near the slopes of 1,790 1 2 3 4 Tamba Deo. In the valley of the western Dhauli, from 1,585 1 2 4 5 Samaughata to Malari. Near Turag Tal ... 100 2 2 4 4 Naini Tal 160 2 4 6 6 In north-eastern Kumaun, it occurs along the Kalimundi range, separating the Ramganga from the Grori, but is apparently wanting in north-western Kumaun. The older trees in a favourable climate grow up in a slender column like the A. Webbiana, and, except that the foliage is a yellowish green, considerably resemble it in its sombre colour and columnar appearance. The thick contorted boughs also give it a rough appearance. At Naini Tal the boughs OF THE NORTH-WESTERN PROVINCES. 841 with a southern aspect are fuller and more regular, giving the tree a lop-sided appearance. The cypress occurs also in the Bbagirathi valley and along the head- waters of the Jumna and the Tons, and in Jaunsar-Bawar on the Lohkandi and Moila hills and below the Karama peak. In Munsyari it occurs at 7,000-9,000 feet ; in Naini Tal at 6,500-8,000 feet and in the valley of the western Dhauli it abounds from 7,000-8,000 feet : “ after leaving the oaks, elms, hornbeams, &c., the wood becomes entirely cypress, and from summit to base of the mountains no other tree is seen. The larger trees not unfrequently attain an enormous size, some of them having a girth of 27 feet.” Major Garstin measured one at Wan over 38 feet in girth and several were over 20 feet. Madden writes : — “ The famous cypress grove at Ming, four or five miles south-east of Joshimath, stands on the north- east aspect of the mountain at 7,500 feet elevation, surrounding the temple of Chandika Devi. Most of the trees are 12-16 feet round : but there is one 27 feet, measured flush with the ground on one side, 10 or 12 feet above it on the other : it is branched nearly to the base with enormous root-bole embracing rocks and is probably not under a thousand years old.” The cypress has an average height of 60-120 feet and an average girth of 6-12 feet. These measurements vary much with the position and elevation. Above Malari, in the Niti valley, it is so dwarfed as to appear a mere bush, and its limits as a tree in Garhwal may be set down at 4,500-9,000 feet, but when introduced, it flourishes consider- ably lower, as at Hawalbagh (4,000 feet) and Diwangiri (2,000 feet). The wood is hard, tough, long-fibred and of a reddish colour, and was formerly extensively used for house-building in ISTaini Tal. Throughout Kumaun the timber is freely used for indoor work, and there is apparently no religious consideration prohibiting its use, but to the west of the Tons it assumes the name deodar and is solely used for incense. The timber when used is considered very dur- rable, but too flexible for any position where great weights have to be sustained, and for this purpose oak is preferred. A piece 22 inches Ion o- and one inch square broke at 4321b., it had a specific gravity of ‘695 and showed 18 rings to the inch. C. semper virens, Linn., is occasionally cultivated in gardens in Kumaun at low eleva- tions. 106 842 HIMALAYAN DISTRICTS Juniperus communis, Linn. Varieties alpina, nana; ground cypress ; padma and parpinja of Niti ; clmrpunja ot the Mana valley ; Ihdla of Byans, but H. Strachey names the Ihdla of Byans J. religiosa ; the cMchiya of Milam. Madden, Journ. Agri.-Hort. Soc., Cal., VII., 153-5 : Brandis, 535. It is found on Chitu Binayak (10,500 feet) ; at Milam and Tola (11,000-12,000 feet), Bampa, Malari (10,500 feet); Jelam (9,000 feet), and Rimkim (14,000 feet), on the glacier-moraines of the Vish- nuganga, west of Mana and in Kunaor. It is said to be used as one of the sources of incense and rarely attains a height of more than 7-8 feet with a stem 18-24 inches. It is used for fuel in Juhar. The aromatic berries are added to spirits distilled from barley and are also exported to the plains under the names abhdl, alvdber , and are used in medicine as a stimulant and diuretic. Juniperus recurva, Ham. — Weeping blue juniper; the letter, Ihedara, jhora, gi'gal, ciru and agaru of Kumaun and Garhwal ; the HI of Milam ; padbank and pdma of Byans. Brandis, 530. There are two varieties : one with acute spreading leaves, found at 12,000 to 13,000 feet ; the other with imbricated cupressiform leaves and extending to nearly 15,000 feet. It flowers May- August and the fruit ripens July-November. It occurs beyond Milam and Niti (to 15,000 feet); in the valleys of the Dhauli (lower limit, 9,000 feet), Vish- nuganga and Kedarganga, at Pindari and most other glaciers. Hodgson found it on the Bhagirathi at 12,914 feet, and describes it as having there the form of a large creeper, not a tree ; some of the branches were 6 inches in diameter and of a considerable length ; in some places they were above the spongy soil and in others below the surface. The wood is of a red colour, has a brittle and soft grain and the characteristic odour of the pencil cedar. It is- one of the sources of incense and is apparently the thalu, ihelu or telu of Basahir. It is used in the manufacture of the yeast called balma, which forms an adjunct in the preparation of spirits from rice. The yeast is made by moistening coarse barley flour, which is formed into a ball and covered all round with the leaves and twigs of juniper. The whole is then closely wrapped up in blankets kept in a warm place and allowed to ferment, which usually takes place in three or four days. Localities. OF THE NORTH-WESTERN PROVINCES. .843 Juniperus excelsa, M. Bieb. — Himalayan pencil cedar — Skur- buta, shilrgu, shukpa of Tibet ; dhup, padmak , siirgi of N.-W. P. ; padmak of Milam. Madden, Journ. Agri.-Hort. Soc., Gal., YII., 138-146 : Brandis, 538. This is another of the sources of Tibetan incense. It occurs at the upper limits of A. Webbiana (8,900-11,500 feet) beyond Mi- lam ; at Jelam on the Dhauli (9,000 feet) and in the valley of the Girti. In Nepal it grows to a height of 60 to 80 feet, and is there a fine large tree with dense branches of a dark colour and close foli- age. In Sikkim it falls to from 15 to 20 feet. Hooker notes that o the Sikkim tree has a scaly bark ; the heart-wood is red and odorous, and the leaves are quadrifariously imbricated, and the wood is burned as incense. The juniper is often confounded with the cy- press ; the former, though the ultimate ramifications are very numer- ous, has them much shorter and less pendulous than the cypress, and the green is more brilliant. The leaves are closely imbricated in decussate pairs, somewhat obtuse, with a central gland or raised line on the back ; four-ranked and imbricate ; or slender, acute, disposed in threes and spreading. The fruit ripens in September- October, of a purplish blue colour, the size of a small pea, one or two-seeded, with a strong aroma when bruised. The tree does not usually attain any great height, seldom being more than 15-30 feet, with a disproportionately thick stem 2-5 .feet at six feet from the ground and often 6-8 feet and in some cases much more. One at Sungnam girthed 13 feet at 5-6 feet from the ground, and Brandis mentions another in Lahul with a girth of 33^ feet and only , about the same height. The pencil-cedar occurs also in the valley of the Jadh-ganga at over 11,000 feet, and was first found thereby Captain Herbert. Some logs of this valuable wood have been removed and exported by the Bhagirathi river to the plains, but in the lulls it is only used for fuel or incense. Taxus baccata, Linn.; T. mteifera , Wall., T. Wallichiana , Zucc. — Yew — Thaner, Kumaun ; Met, Sor ; nhare , Byans. Madden, Journ. Agri.-Hort. Soc., Cal., YII., 155 : Brandis, 537. The yew is found at Bala Jagesar, 5,900 feet ; Puya-pani, on the road to Deo Dura, 6,500 feet ; on Thakil in Sor ; Kanol on the Nandakini ; Chula in Chaudans ; Laduli ghat on the Nayar 844 HIMALAYAN DISTRICTS OF THE N.-W. PROVINCES. (7,000 feet) and near Tungnath, but is indigenous only on the spurs from the snowy range. It occurs with box and cypress in the Bhagirathi valley between Bhatwari and Jhola and along the head-waters of the Tons and Jumna. Griffith notes its occurrence in Bhutan between 7,100 and 9,800 feet, and 8,000-9,000 feet would seem to be the limit within which it flourishes there. On the outer ranges in Sikkim it does not descend below 9,000 feet, but on the inner ranges it is found as low as 7,000 feet, and in Basahir Madden has not seen it below 8,000 feet. In Garhwal poor scrubby speci- mens ascend as high as 11,200 feet at Kedarnath and to 11,000 feet on Tungnath. Hoffineister records a tree near Gangotri, 15 feet in girth, and Dr. Hooker notes one of 18 feet in girth on Tonglo in Sikkim; but the average girth is not more than 5-8 feet and height 20-30 feet. The sap-wood is whitish, but the heart-wood is heavy, close-grained, and eminently fitted for turnery, taking a very high polish. The tree is held in high veneration and the wood is burned as incense and the branches are carried about in processions in Kumaun. The people of Ladak import yew-bark from Kashmir and use the inner part dried and prepared as tea or for mixing with tea and as a dye. The tree is there called sungcha and the bark chatting. The leaves ( birmi ) are exported to the plains and are used in medicine and the berries are eaten by the poorer classes. There is little export of the timber, which would seem to be well adapted for shafts and the purposes to which its European representative is applied, if it could be procured in sufficient lengths. CHAPTER X. Economic Botany — ( continued ). CONTENTS. Forest history. Grazing tax. Boundary disputes. Government forests. Kumaun forest-division. Naini Tal forest-division. Ranikhet forest-division. Garhwal forest-division. Dehra Dun forest-division. Ganges (Bhagirathi) division. Forest at the head of the Tons and the Jumna. Jaunsar forest-division. Rheea cultivation. Cinchona. Tallow-tree. Ipecacuanha. Cork-oak. Sweet- chestnut. Carob. Mezquit and others. Tea. From time immemorial, tlie forests along the foot of the hills to which alone any fiscal value pertained as Forest history. we ll as those within the hills were consi- dered the property of the ruling power and as such invariably formed a source of revenue to the State. The most simple mode of realising this revenue was that actually adopted by subjecting the products of the forests to a small proprietary due in the shape of duties payable by the exporters. The products consumed within the hills by the people themselves were, as a rule, too inconsiderable to be taken into account and » where exceptionally large, as in the case of fuel for smelting ores, were included in the revenue demand. These duties on ordinary forest produce were collected at stations along the foot of the hills, whilst the duty on catechu was fixed at so much per kiln and was paid by the manufacturers. For the first three years of our rule the forest dues were leased with the transit duties on merchandise, and on the abolition of the latter source of revenue, Mr. Traill was authorised to farm out the forest dues or kdth-bdns and kath mahals as they were called from their principal items kdth (timber), bans (bamboos) and kath (catechu), to the zamindars of the parganahs in which they were collected. 1 The revenue from this source in 1818-19 for Kali Kumaun, Chau- bhainsi, Chhakhata, Kota, the Path Dun and Udepur amounted to Rs. 3,200, as compared with Rs. 2,841 in the previous year. The 1 From Commissioner, 14th September, 1818. To Commissioner, 25tli Septem- ber, 1818,' 846 HIMALAYAN DISTRICTS following table shows the collections in sonat rupees for nine years under the new system : — Year. 1820-21 4 ’s“ -{“i ::: ^ 1822-23 - •>?“ t Garhwal ... 934 Rs. Rs. 3,200 3,989 4,850 6,503 6,302 Year. -{g“i JgS isos 0-7 S Kumaun .. 2,266 i82b-27 •••[ Garhwal ... 1>100 1827-28 ( p U | aU ^ ■“ ^’ool t Garhwal ... 1,381 DO (Kumaun ... 2,620 18-8--9 ... | Garhwal .. 1,406 Rs. Rs. 7,101 3,366 3,675 4,025 In 1824, the collection of these dues was intrusted to the authorities of the Muradabad and Bareilly districts in consequence of the difficulties regarding boundaries that had occurred, but in 1826 the duty of collecting them was restored to the hill-districts. In 1828, the forest dues were leased to the farmers of the ch'irai or grazing-tax at the same rate, as it was found that the two could not be then usefully separated. This grazing-tax was one of the many miscellaneous items of revenue that descended to the British from Grazing-tax. former Governments. I rom the earliest times, the landholders in the hills were all subject to a tax on their cattle known as ghikhur which with other cesses was abolished at the first settlement. 1 The practice of collecting these dues, whether for the Government or for the landholders, extended to the Bhabar and Tarai and was continued there under the name gdi-ch irdi ; but the cattle of the hill-men were exempt from this tax, which was levied chiefly on the cattle of the villages in the plains that came into the forests during the hot season. During the two or three years succeeding the conquest the number of cattle pro- ceeding from the hills to the Bhabar and Tarai was not so great as to render any cess on them an object of interest to the Government, but the security afforded by the abolition of the old rural guard (i chaukidari ) system and the introduction of an efficient police led J To Board, dated 16th July, 1822. These cesses were called gliikhar, gobar, and puchhiya in the hills and were farmed out as jogat, and under the Heris and Mewatis in the Bhabar were called donia , from the dona or wooden bar to which the cattle were tied at night, and each of which paid one kuehcha ser of ghi and four pice a year. OF THE NORTH-WESTERN PROVINCES. 847 to increased resort to the plains. It was therefore resolved in 1822 to subject all cattle sent to graze in the Bh&bar and Tarai to a uniform tax of three annas for each female buffalo, two annas for each cow, and one anna for each bullock a year. The farm of this tax for the year 1822-23 was given out in three leases, aggre- gating Rs. 2,077 per annum. The unsettled state of the boundaries between Kumaun and Rohilkhand became a fertile source of dis- pute between the farmers of this tax for the hill and plains portions of the submontane tract. Many of the hill-men having made their arrangements with the Rohilkhand farmers paid the duties to them and were again called upon to pay by the hill farmers, who claimed the right to levy these dues in all places in which the chaukiclari cattle dues had formerly been collected. In 1823, the cattle belonging to the Kamins, Sayanas, and Thokdars or head-men of parganahs in the hills and to Padhans or head-men of villages in the Bhabar and those belonging to permanent residents were exempted from these dues. In 1826, the boundary between the hills and Rohilkhand was finally arranged and separate farms for the grazing dues were established. The principle on which the collec- tions were made was that the farmer within whose jurisdiction the cattle-pens were situate was entitled to collect the tax. The dues were very rarely collected per head, the plan being to count in each goth or cattle-pen the agals or donas , that is the wooden bars to which the cattle were tied at night. The customary rate was to consider each agal as containing eight buffaloes and eight cows liable to a tax of two rupees. To make this point in the history of the management of the forests more clear, it will be necessary to Boundary disputes. refer to these boundary disputes. In the earlier years there were no exports of any value from the portion of the lowland tract lying below the chain of custom posts estab- lished to levy the export duty, and it was thought that no difficulty could arise in regard to the collections made there, but the unset- tled state of the boundary between the Bhabar and Tarai and the conflicting claims of the landholders of the frontier villages, both of the hills and of the plains, soon led to innumerable complaints in which the district authorities on both sides found themselves partizans. The records show a voluminous correspondence on 848 HIMALAYAN DISTRICTS this subject extending over several years. Early in 1819, Mr. Traill reported on the encroachments made by the zamin- dars of Bilhari on the forests lying along the foot of the hills now included in the Tallades Bhabar. This tract was valuable to the hill-men as affording them pasture for their cattle during the winter months when the grass in the hills dried up and became useless for fodder. During the Grorkhali rule a joint com- mission had been appointed by the Nepal Government and the Nawab of Oudh to settle these disputes, and the Saniha nala was fixed upon as the boundary between the two states. The hillmen had always occupied the jungle to the north of this boundary and were anxious to undertake the cultivation of the portions lying at the foot of the hills which had recently been taken possession of by the Bilhari landholders. 1 It was agreed that an attempt should be made to settle the disputed boundary on the basis of that which existed in 1802, when Rohilkhand was ceded to the British, and that advantage should be taken of this arrangement to demarcate the whole line of boundary between Rudrpur and the Nepal fron- tier. The difficulty was much enhanced by the claims set up by Major Hearsey, who, in 1814, had purchased the entire taluka of Bilhari at auction for arrears of revenue and now demanded posses- sion of a portion of the Kumaun Bhabar, on the plea that it belonged to the lowland parganah. A commission was appointed to investi- gate these matters, and it was at length decided that the Saniha nala had always been, and should continue to be, the boundary between the hills and the low country. 2 The collection of all dues was handed over to the plains authorities, but, in 1826, was again intrusted to the Commissioner of Kumaun. 1 To Board, dated 5 th February, 1819. From Board, dated 6th February, 1819. To Collector, Bareilly, dated 1st March, 1819. From Collector, Bareilly, dated 8th March, 1819. To Collector, Bareilly, dated 20th March, 1819. From Collector, Bareilly, dated 26th March, 1819. To Collector, Bareilly, dated 5th April, 1819. From Collector, Bareilly, dated 10th April, 1819. To Collector, Bareilly, dated 5th No- vember, 1819. From Collector, Bareilly, dated 18th November, 1819. To Collector, Bareilly, dated 24th No- vember, 1819. From Collector, Bareilly, dated 1st December, 1819. To Collector, Bareilly, dated 16th Feb- ruary, 1820. From Collector, Bareilly, dated 24th February, 1819. 2 From Board, dated 27th June, 1820. To Board, dated 19th July, 1820. From Board, dated 4th August, 1820. OF THE NORTH -WESTERN PROVINCES. 849 The first notice 1 that I have been able to discover in regard to the reservation of forests for Government Government forests. uge a ] one occurs in 1826. The whole of the forests had always been recognised as belonging to Government, and any part of them could therefore be appropriated to the ex- clusive use of Government without the slightest infringement of the rights or claims of a single individual. Mr. Traill recom- mended the reservation of the thdplas or terrace land immediately adjoining the lower range for the timber and bambus required by Government, whilst the extensive forests below it should still remain open to private individuals. A proclamation was issued in 1826, prohibiting the cutting of sal within the reserves, which were at once excluded from the lease of forest produce, and thus the system of Government forests commenced. In 1828, as we have seen, the lease was fixed for four years, but in 1831-32 I find the total forest revenue amounted only to Rs. 4,328, of which Rs. 2,923 were realised in Kumaun and in 1832-33 it reached Rs. 4,457, of which Rs. 2,932 were collected in Kumaun. No attempt was made to enforce any system of conservancy and the old system of leasing out the forest dues to contractors continued. In the report on the settlement of Garhwal in 1840, Mr. Batten remarks that large portions of waste lands, including whole ranges and their vast forests, were included from olden time in the bound- aries of the adjacent villages, though not in their recorded area. No change in this nominal allotment of waste was then attempted, as such a division was found useful in assigning separate tracts for pasture for the cattle of different villages ; but, at the same time, the inhabitants of the villages within whose area these tracts of waste land were nominally included were prohibited from levying any grazing dues unless it had been a custom of immemorial date, and even then the burden of proof rested on those claiming the dues. A similar clause was entered in the lease given to the head-man and in the several agreements signed by the shareholders in the village. Mr. Batten further states that his report 2 should be considered, in a measure, declaratory of the principles on which the settlement was formed, and adds : — “I therefore take this opportunity of asserting that the 1 To Board, dated 22nd .Tune, 1826. To Collector, Bareilly, dated 26th Septem- ber, 1826. ! Stat. Kumaun, 125, 336. 107 -850 HIMALAYAN DISTRICTS right of Government to all the forests and waste lands not include d in the assessable area of the estates remains wholly unaffected by the inclusion of certain tracts within the boundaries of villages, and 110 one has a right, merely on account of such inclusion, to demand payment for the use of pasture-grounds or for the permission to cut timber and firewood. Neither does such inclusion interfere neces- sarily with the right of Government to accept offers for clearance ( naudbad ) leases. But as ordered in the case of the Tarai forests, so in the hills (where, too, claims to proprietary rights are rare), the inhabi- tants of the villages most adjacent to the tract, or having it recorded within their boundary, should have the first refusal of such leases.” In his Kumaun report Mr. Batten distinctly states that these prin- ciples apply equally to Kumaun. In his report on the Kumaun Bhabar in 1846-47 Mr. Batten gives the revenue from the hath bdns and chardi mahals as fol- lows : — Name of patti. Forest dueB. Pasturage dueB. Total. Rs. Ks. Rs. Kota ... »*• • • • 4, GOO 3,801 8,401 Chhakhata • •• 1,451 | 3,705 2,650 4,101 Kali Kumaun • •• 2,522 6,227 Total ... 1 9,756 8,973 18,729 He states that though the injury said to be done to the reserved Government forests was somewhat exaggerated in some places, the Government rights had been suspended and in others the older trees had been removed, and recommended that steps should be taken to preserve the few patches of old sal that remained and the young sisu plantations. In the eastern Bhabar cultivators were allowed to clear the ground and sell the timber. The restriction as to cutting sal in the thdplas or plateaus of the lower hills which was issued ill 1826 had been removed, when Mr. Traill saw the farms falling in one after the other owing to the scarcity of sal in the lower sites. In the Kota and Chhakata Bhabar the farmers were allowed to cut down and sell the sal timber which is there confined to the thdp- las and does not occur also in isolated patches in the plains as it does farther east. In appendix A. will be found a list of rates according to which farmers of the forest dues in Kumaun were OF THE NORTH-WESTERN PROVINCES. 851 Sub-Himalayan forests. authorised to collect from the exporters in 1847, and we shall now proceed to describe the forests as they now exist. The sub-Himalayan forests of the Kumaun and Garhwal districts extend from the Ganges to the Sarda, cover- ing the lower spurs and ridges of the Hima- laya and running down some distance into the Bhabar. The Tarai forests contain a little sal , of inferior growth, barely sufficient for the requirements of the cultivators, and are not included in the tracts under the Forest Department. With the exception of a por- tion of the Chandni Chauk which belongs to the Tarai, almost all the islands in the Sarda below Kumaun have been given to Nepal. A cart-road running along the foot of the hills from the Ganges to the Sarda generally forms the southern boundary of the forests in Garhwal, but further east several blocks reserved for Government purposes lie to the south of the road and are included in the existing reserved forest area. The western Ramganga and its tributaries, the Barsoti and Kotirao, form the boundary between the two great forest-divisions of Kumaun and Garhwal, whilst the outer Himalaya give a well-defined boundary on the north. Except the Kumaun Iron Company’s grant and a number of villages, all of whose rights have been recorded and for whom blocks of forest have been left open, the entire area described forms one vast State forest in one compact block perfectly marked out either by natural or artificial boundaries. Within these limits no private rights exist which can prove injurious to the best sal forests, and cattle-grazing is prohi- bited in all portions which are free of village' rights, except where it is entirely harmless. The most valuable timber is sal, which grows with great vigour in many parts and covers about one-fourth of the forest area. Ttin ( Cedrela Toona) and sissoo ( Dalbergia Sis sit ) are plentiful in the low, moist valleys and flats, whilst other jungle trees, especially the Terminalias, Lagerstroemias, Acacias, various species of Anogeissus, Adina, and Ougeinia, are found mixed with sdl everywhere, even when the last predominates. Amongst the minor forest produce the bambu takes the first rank, and next the matting and cordage materials and indigenous drugs, tans and dyes. We shall now proceed to give a short account of the existing forest- divisions and their origin. The contract arrangements for felling continued in Kumaun until the year 1858, and as a consequence no 852 hima'layan districts system of conservancy could be introduced. The forests of the present Kumaun forest-division 1 were denud- Kumaun forest-division. ..... ...... ed oi good trees m all easily accessible places, and were it not that nature has happily made the sal, sisu, Jchair, and dhaurilargely reproductive, the new Forest Department would have had little to conserve. Between 1855 and 1857, the demands of the railway authorities induced numerous speculators to enter into con- tracts for sleepers, and in order to secure a certain favourite area for themselves, these men were allowed, unchecked, to cut down acres of old trees very far in excess of what they could possibly export, so that for some years after the regular forest operations commenced the attention of the department was chiefly directed to cutting up and bringing to the depot the dead timber left behind by the contrac- tors. 2 Major (now General) Ramsay was the first Conservator. He abolished the contract system in 1858 and gradually introduced a better arrangement, by which the cultivation of patches of land in the forests proper was discouraged and the cultivators were induced to take up lands chiefly south of the cross-road from Hardwar to Barmdeo, leaving the valuable forest land to the north untouched. This the first attempt at real conservancy would, probably, have suc- ceeded better had not the management of the forests been taken from the Commissioner of Kumaun in 1868, for arrangements of this kind take much time and trouble to elaborate. In his report for the year 1867 the Commissioner writes : — “As yet cattle have notin all cases been excluded from the tracts recently made over to the Forest Department, because some time must be allowed to the villagers to make other arrangements. A great many cattle-sheds have been removed from the vicinity of the sal forests of the outer rano-e between Haldwani and the Sarda river and the cross-road has been declared the boundary nearly the whole way.” In his report for 1868 the Commissioner writes : — “In another year or two I hope that all the Kumaun valuable sal forests will be as free from cattle as those of Garhwal.” Unfortunately this is hardly true even at the present day. The same officer introduced the system of having 1 This division extends from the Sarda on the east to the Phika river on the west and from the base of the outer hills on the north to the boundary of the Tarai district on the south. I am indebted for the materials for the notice 0 f this division to Major Campbell through the Conservator, Mr. G. Greig. % See Major Kamsay’s report on the condition of the forests in 1861 in ' Nurtli- \ \eattrji t rovinces Gaztilt Supplement, lSth December, 1861. OF THE NORTH-WESTERN PROVINCES. 853 all trees marked by responsible officers before permission was given for felling and commenced arrangements for protecting the reserved forests from fire. Operations, however, appear to have been con- ducted on too large a scale or were too irkso me to the squatters, for, though successful for a time, the occurrence of an unusually dry season led to great loss by fires. But, on the whole, the administra- tration of the forests was a marked success. From the table given in the appendix the receipts and expenditure for the years 1859-60 to 1867-68 show an excess of receipts over charges amounting to considerably over fifteen lakhs of rupees. 1 The forests not only gave a better return but were conserved for the first time, and arrangements were made for the better protection of the young plantations and planting out the denuded tracts. Major Pearson took charge of the Kumaun forest-division in Under the imperial Fo- 1868, but made little change in the working rest Department. arrangements. In 1877 the reserved forests in the Kumaun Bhabar were formally demarcated, 2 and it will be convenient to adhere to the arrangements then sanctioned in the following brief description of each block : — Block 1 comprises the Cliilkiya forest, tvhich is one of the largest and most valuable, having an area of about 126 square miles and containing- much fine sal timber. The more accessible forests in this block were worked by contractors before 1858, and the remain- der have furnished the chief part of the timber brought to market since that year. The entire block has been worked, but there are still numbers of mature trees that have been reserved for shade and shedding seed and which may be cut down when the young stock have been established. Fire conservancy has also been successfully enforced for some years and the young trees bid fair to produce good timber. Block 2, comprising the Garhi Balchand forest, has an area of 17 square miles, all of which have been demarcated, and of this about 11 square miles have been enclosed with fence and ditch and are protected from fire. The forest is chiefly sal , but the soil does not seem suited to produce large sound trees, and its fittest use 1 Receipts, Rs 32,90,459 (Kumaun, Rs. 15,01,050; Garhwal, Rs. 17,89,309). Charges, Rs. 17,43,542 (Kumaun, Rs. 8,33,477 ; Garhwal, Rs. 9,10,065). 5 See G.Os.No. 407 F.C., dated 5th September, 1877,andNo. 173, dated 29th February, 1879. 854 HIMALAYAN districts will be to supply saplings, which can be carted from the spot and will find a ready market in the plains. Block 3 comprises the western Kota forest, which has an area of about 55 square miles and contains much valuable sal forest. Gene- ral Ramsay writes : — “ There is no part of Knmaun where sal thrives so well as in the Kota Dun, west of the Dhabka river.” The Kota forests have been worked like block No. 1 and have supplied much timber to the market during the last twenty years. Fire conser- vancy has been introduced since 1877. Block 4, comprising the forests below the Chhakhata parganah, has an area of about 103'5 square miles and consists of sal on the thdplas or plateaus and some very fine haldu below. The western portion between the Bhakra and the Gaula streams has been worked for many years by the Nawab of Rampur, 1 and the eastern portion from the Gaula to Chorgaliya by contractors and for canal-works and building purposes in Haldwani. The only large tract remaining unworked in this block is the Nandhaur valley. Block 5 is known as the Horai forest. It has an area of 14 square miles and lies below the hills. It contains some valuable sal forest, of which the eastern half has been enclosed with fence and ditch. Block 6, or the Kali Kumaun forest, has an area of about 230 - 5 square miles and consists entirely of hill-forest, of which the lower slopes and more easily accessible parts have been worked out by contractors. Still there is a larger area of unworked sal forest here than in any other block of the Kumaun Bhabar. Block 7, or the Dhyanirao forest, has an area of 68 square miles, of which about one-third is sal forest and the remainder is chiefly Jchair and mixed jungle and open plains, on which immense numbers of cattle graze. Block 8, known as the Chela forest, has an area of about seven square miles, of which about a quarter is sal forest and the remainder is chiefly halclu and bambu. Block 9 comprises the Barmdeo forest, which has an area of 7-3 square miles and lies at the foot of the hills near the Sarda 1 The Nawab of Rampur is allowed to export every year 200 trees, not less than 6£ feet in girth, free of duty. OF THE NORTH-WESTERN PROVINCES. 855 river. It contains some promising young sal forests, besides khair, sisii, and bambus. Block 10, known as the Sarda forest, comprises a number of islands in the Sarda which are covered with sisu and khair forest and have an area of about eight square miles. — Block 11 comprises a small patch of sal forest on the Sarda about three miles above Banbasa measuring 320 acres, recently transferred to the Imperial Forest Department, which has charge of all these demarcated forest blocks, and the remainder ot the forest area is managed by the Commissioner of Kumaun. As a rule, the good sal forests consist chiefly of sal, but there are also patches of tun , kliair, sisu, sandan , gosam , sain, haldu, dhauri, hakli, and bambus, all of which are rising in value every year. The cart-road from Barmdeo to the Ganges is connected with cross-roads to the different blocks and temporary roads are made when necessary. In the young forests the trees differ materially in different localities. In some places where the soil is suitable and other cir- cumstances have favoured the growth of the young trees, they are exceedingly fine and show straight stems, clean barks, and fine heads. In other places where the soil is poor, but more especially where the numerous cattle stations formerly existed, and where in consequence the young trees suffered continually from being lopped, barked, and otherwise injured* and where they were more exposed to repeated fires, the trees are knotted, crooked, and with poor heads. The best forests in the eastern tract are perhaps those above Barmdeo, near the junction of the Ladliiya with the Sarda, where, owing to the favourable nature of the soil, the sal has developed to a remarkable degree and, owing to the difficulty of carriage, the trees have been left uninjured by speculators and contractors. Next in importance come those to the west and north of Chorgaliya and those on the flats and plateaus above the Jagbura and Kulauniya streams, and next the sat forests in the valleys of the Nandhaur and Sararagadh streams. The geological formation in the last tract is sandstone and massive boulders. Further west there are still valuable forests between the Kosi and the Ramganga, and there can be little doubt that in the course of time the forests under a careful system of conservancy will renew their HIMALAYAN districts 856 Iron Company’s forests. pristine vigour and well repay the core and money expended upon them. The only important private forest is that belonging to the Ku- maun Iron Company, whose grant extends from the Manar Gadhera, about one mile west of the Dhabka, as far as the Bhakra river, about half way be- tween Kaladhungi and Haldwani. The grant is bounded on the north by the Himalaya and on the south towards the Bhabar by a line of pillars, and the area is about 350 square miles. The collec- tions from this tract for timber and minor forest produce from 1861 to 1881 have amounted to more than two lakhs of rupees, and it now constitutes one of the most valuable forests in Kumaun. It is difficult to say what portion of their rights Government resolved to grant to the company, for the deed was never executed, but from the draft it would appear that only fuel-rights were intended, and certainly none other is expressed. The subject of these forests and the company’s claim to them being now under the consideration of Government, it will not be necessary to allude to them any further. 1 The climate in some parts of the tract below the Kumaun hills is fair from November to J une, but in other parts it is very fatal in November and after April. During the cold-weather the Bhabar forests present a busy scene. They are then filled with wood and bambu cutters, labourers haul- ing out timber, men and women collecting babar grass, making mats and baskets, gathering roots, leaves and plants used in medicine or the arts, or herding cattle. After April all, except those who have become acclimatised, leave the forests, and during the rains they remain practically closed. Ordinarily every hill stream becomes then a raging torrent often impossible to cross for several days. Elephants and tigers, though now less numerous than in former times, return to the haunts from which they had been driven dur- ing the hot weather : the prairies become a sea of grass and the undergrowth in the thick jungle presents an obstacle to moving about most difficult to surmount. To the unacclimatised these forests are deadly during the rains, and few survive the malarious fever that a night’s residence within them then frequently gives rise to. There is no doubt, however, that the clearances effected 1 See for a sketch of the Company’s history. . Climate, &c. OF THE NORTH-WESTERN PROVINCES. 857 by the Bliabar cultivators have done much towards ameliorating the climate, for places where man could not formerly exist are now the centre of flourishing colonies, the inhabitants of which remain all the year round in their villages. The forests in and around the settlement of Naini Tal were demarcated in 1865 and now form the Naini Naini Tal forest-division. „ , ,. . . , T) . , 10 . K .. lal iorest-division/ .Previous to 1845, all the trees in the neighbourhood were considered to belong to the villages within whose boundaries they were situate, and those within the valley were alone protected. Some years later, the Commissioner took over the forests in the neighbourhood of the settlement and allowed no timber to be felled without his permis- sion. A small establishment was entertained to patrol the forests and a royalty was levied on each tree felled to meet the expense. In 1865, the forests were taken over by Government, and have since then been managed chiefly with a view to supply the local wants of Naini Tal. CMr of a good quality for building purposes is abundant and the various species of oak and the rhododendron afford materials for charcoal. In 1879, these forests were gazetted as ‘ protected/ and now comprise about 38 square miles. Deocldr plantations have been made with marked success along the slopes of Lariya kanta, and bdnj and tilonj and Jcharsu oaks, also walnuts, horse-chestnuts, and ash have been extensively sown and planted. An attempt to reproduce the cypress was thought to have failed, but the seeds have germinated after remaining a long time in the ground. The Kanikhet forest-division is, like the preceding, intended to control and provide for the local supply of timber and fuel to the Ranikhet settlement The Imperial Forest Department deputed an officer to take charge of the forests around the intended military station in 1867, but it was not until 1873 that the forest boundaries were finally settled and operations regularly commenced. The tracts now conserved 2 are fifteen in number, of which one having an area of about seven square miles is closed and surrounded by a ring fence of thorn and is ‘reserved ’ and clear of all private rights. It contains pine, oak, 1 Reserved by Nos. 149 and 150, dated 21st February, 1879. 2 See G. Os. Nos. 176 and 177, dated 26th February, 1879. 108 ' Ranikhet forest-division. 358 HIMALAYAN DISTRICTS rhododendron, and other woods of minor value. The other forests which are ‘ protected ’ and cover an area of about 59 square miles are situated at distances varying from one to 24 miles from Rani- khet, and are held conjointly by Government and the inhabitants of the villages within whose area they occur. The latter have a right to graze their cattle and cut wood for fuel or for building or agricultural purposes, but no power to cut for sale to any one. But the great feature of this division is the nursery which, though commenced only in 1871, has done much good in distributing 1 fruit and timber trees all over the province and in conducting acclima- tisation experiments. In Garhwal, as in Kumaun, the contract system remained in Garhwal forest-divi- force and, in 1839, we find the right of collect- * 10n ‘ ing the forest and pasturage dues of the Patli Dun leased to one Padam Singh for twenty years at a fixed annual rental of Rs. 2,750, of which Rs. 1,649 were on account of the Icdth-bdns section. The forests here are amongst the most valuable both for timber and bambus that exist along the whole line of hills between the Jumna and the Sarda, and the loss that must accrue should this arrangement continue was brought 2 to the notice of Government in 1853. The result of the correspondence that then took place was that Padam Singh’s rights were purchased for Rs. 15,000, and the forests were taken under direct management and transferred from the Bijnor district 3 to Garhwal, whilst the col- lection of the dues from the Khoh river westward still remained with the plains authorities. Posts were established at the outlets of the Ivotri and Patli Duns for the collection of dues from exporters, and the surplus revenue was devoted to opening up roads and improving the forests. In 1854, Captain Reid took over the management and remained in charge until 1858. Captain Reid attempted little in the way of conservancy, but commenced felling operations on a large scale and erected a saw-mill that could not be worked owing to a 1 12,000 grafted plants have been distributed to villagers and householders, besides some 32,000 forest and ornamental plants, and about 400,000 forest trees have been planted in the reserve from the nursery. 2 By Mr. (now Sir John) Strachey, to Commissioner, 4th August, 1853 ; from Government, No. 3747, dated 17th September, 1853. 3 The collections of the forest and pasturage dues from the Kotri Dun, including Udepur, was handed over to the Superin- tendent of the Dun and the Collector of Bijnor in 1849. In 1853, the dues from the Kotri Dun and the Rawasanwar part of Udepur amounted to Rs. .1,403, and from the Rawasan-par portion to Rs. 1,011 a year ; total of Garhwal, Rs. 5,104. OF THE NORTH-WESTERN PROVINCES. 859' defect in the slope of the canal that was to afford the motive power. The mutiny then intervened, and in 1858 the forests came under Major Ramsay, who introduced the system of conservancy that we have noticed in the account of the Kumaun forest-division. His administration was marked hy the control of felling operations, the removal of squatters from the valuable forest tracts to available land fit for cultivation below the forest boundaries, the construction of roads and the establishment of stations for the collection of revenue at convenient intervals. In 1861-62, cultivation in the Patli Hun was put a stop to by assigning lands to the people in the Bhabar, and the cattle-stations were broken up and removed from the reserved forests. This operation occupied three years, from 1862 to 1865, the cattle stations being removed from all the Garhwal forests, and in Kumaun from all the forests above the main line of road. In the meanwhile excellent roads were opened out, and the forests, especially those of Garhwal, were made accessible from all sides : at the same time a regular system was instituted of working only certain forests, the remaining ones being kept rigidly shut up, and the selection and marking of all trees previous to felling was insisted on. The felled timber left by the old contractors and Captain Reid was exported and sold and the machinery of the saw-mill was transferred to Rurki. Colonel Baugh acted as Conser- vator under Major Ramsay and an establishment was entertained to prevent the felling of timber without license, to protect the forests from fire, to cut down creepers and to mark trees for felling. The management of the forests was transferred to the Imperial Forest Department in 1868, and, in 1879, the whole forest-division of Garhwal from the Ramganga to the Ganges was divided 1 into five blocks, an arrangement that we shall observe in the following brief description : — Block 1 comprises the Patli Dun forest with an area of 237-5 square miles. It is bounded on the east by the Kumaun boundary and on the west by the Palain river to its junction with the Ram- ganga, and thence down by the Ramganga to the Bijnor district. Block 2 comprises the forests of the Kotri Dun with an area of about 180 square miles, and is bounded on the east by the Patli 1 F. 162, dated 24th February, 1879. 860 HIMALAYAN DISTRICTS Dun' forests and on the west by the Klioh river to the Kotdwara mart, thence by Jamangarh and the Lalpani ridge to the Saneh depot on the Granges road. Block 3, known as the Saneh forest, has an area of 17 square miles and lies between the Khok river on the east and the Malin river on the west as far as the Chaukighata mart. Block 4, known as the Laldhang forest, has an area of 36-5 square miles and lies between the Malin oil the east and the Rawasan river on the west. Block 5, comprising the tract between the Rawasan and the Ganges known as the Khara forest, has an area of 88 square miles. Block 6, known as the Kartiya forest, has an area of about 800 acres. It consists chiefly of sdl and is situate on the left bank of the Mandhal stream. The northern boundary of all these blocks lies between the culti- vated area of the hill villages and the forests proper, and the southern boundary is found in the road between Kotirao on the east and the Ganges on the west. The Patli Dun forests occupy the valleys of the Ramganga and . , its affluents and the ridges which run between their watersheds, the geological formation of this tract consists of alluvial deposits and drift in the valleys and plateaus, and massive grey sandstone interspersed with blue shale on the ridges. The whole Dun has been a noble forest of sdl, the lower and more accessible portions of which have been worked out, but in which enormous tracts of virgin forest still remain, from which under judicious treatment inexhaustible stores of timber may be drawn. Excellent roads were constructed though the principal valleys by Major Ramsay, and these have been kept up by his suc- cessors. The forests of this tract may be conveniently divided into those (1) of the Palain or Taimuriya ; (2) those of the Mandhal ; and (3) those of the Ramganga, south Patli Dun and Sona river. (1) The whole basin of the Taimuriya and its affluents con- tains a noble sdl forest. This tract was considerably thinned out many years ago for wood for the gun-carriage agency, but not io a too great extent, as the result has been satisfactory in the OF THE NORTH-WESTERN PROVINCES. 8(11 improvement of the growth of second-class trees as compared with the condition of the same class of trees in those portions of the forest wdiich have never been overworked. Throughout this tract since conservation has been enforced the growth of sal saplings gives hope of an unlimited supply of this valuable timber. This growth is fostered by the ground becoming thickly clothed everywhere with bambus, by which the moisture is retained in the soil and the increase of other grasses is prevented, and thus the risk of fires is materially diminished. (2) The forests of the Mandhal owing to their remote position have never been much worked. There are here in consequence to be found a large number of first-class sal trees as well as an abundance of trees of every age and size. The good forests may be said to extend over about fifteen miles in length through all the lower portions of the valley below Jarat, on the slopes and plateaus facing the north and on the opposite bank of the Mandhal over the last five miles. On the plateaus above the river the sal has attained a very large size and fine tun trees exist in the valley which seems particularly well adapted to their growth. (3). The forests of the valley of the Ramganga, the south Patli Dun and the Sona are all situated on the hills sloping down to the Ramganga and its affluents, the Sona and Gaujhera nala on the right bank and the Maira Sot, Patharpani and Dharau streams on the left bank. These forests were ‘ felled even to desolation’ years ago and many parts of them have been permanently injured. No attempts at reproduction were made, and the land where fine sal forest once stood is now too denuded by exposure to admit of efforts in this direction proving successful. There are, however, some good young plantations springing up and some mature trees, as already noticed, exist in the Mandhal valley. The exceptions are places where the old trees have been completely cut away, and here, there being no natural shade or seed-sowing, the dense grass effectually prevents all artificially sown seeds from germinating, and though measures have been taken from time to time to reproduce the forest, they have met with only very partial success. There is still, however, some sal in the highlands, some sisu along the rivers and tun in the valleys, and a fair amount of khair and good grass in the open level ground. Below the Siwaliks there are great 862 HIMALAYAN DISTRICTS bambu forests on the level flats that afford a considerable revenue. The great question of fire conservancy has always engaged the attention of the establishment, and up to 1879 no great injury had been done for several years. In 1879, however, the cholera- stricken pilgrims returning from the Hardwar fair spread fires in every direction, and considerable damage to the young plantations resulted. Roads have been opened to all the principal blocks in connection with the road from Kotirao to the Ganges that forms the southern boundary of the division. Blocks 3 and 4. The forests of the Kotri Dun lie between the Patli Dun on the east and the Khoh river on the west. The formation of the soil is sandstone and drift and there is little water and few good forests. The trees are almost entirely sal differing in value in different places accord- ing to the soil and other natural circumstances. Few tracts in this forest have not been worked more or less, but there still remains some good timber on the more inaccessible ridges. Since this forest has been rigidly protected the young trees have made con- siderable progress, and the keeping out of cattle and fires will in a few years do much to restore them to their original condition. Blocks 3 and 4 lie between the Rawasan and the Khoh rivers, a distance of about sixteen miles. The soil is a dry sandy loam with outcrops of gravel and blue clayey slate in the hills. The entire tract appears to have been extensively cultivated in former times, but there is a great want of water through all the lower forests. There are here three large sal patches. The first along the Rawasan has been extensively worked and little valuable timber remains ; the second along the Chaukighata stream contains some mature sd l trees and in the valleys tun; and the third is a young sal forest in the south-east corner of the division, about three square miles in extent. Bahera , sain, and haldu are also found on the lower plains along the southern boundary, but bambus, which grow luxuriantly everywhere, form the main article of export from both blocks. The early history of the forests of Dehra Dun has much in com- mon with that of the eastern forests in Kumaun and Garhwal. Both the Gurhwfd Dehra Dun forests. OF THE NORTH-WESTERN PROVINCES. 86 ? Rajas and the Gorkhali Government derived a considerable revenue from the various items of forest produce grown in the Dun and adjacent hills. This was usually levied as a transit duty and was collected with the export and import duties on every article of commerce entering or leaving the Dun. The aggregate amount of these duties in 1809-10 was Rs. 16,000, and in the following year was Rs. 15,200, of which over one-third was absorbed in paying the collecting establishment. The transit duties were abolished at the conquest, and with them the duty on the export of forest produce, which, though a legitimate source of income, tvas lost sight of until Mr. Moore took it under his management in 1819. For three years the duties on exports yielded a revenue averaging Rs. 4,000 per annum, and in 1822 tvere leased to one Surjan Negi for four years at Rs. 5,000 a year. In 1825, Mr. Shore gave new leases for five years to various persons for all the collecting stations, except that at the Kheri pass, at an aggregate demand of Rs. 8,500. In making these arrangements it was distinctly laid down that these dues were not to be regarded as transit duties, but as rent for the use of the forests and as a royalty on their products, and on this principle all subsequent settlements were made. 1 Curious to say, Mr. Shore 2 was averse to preserving sdl and devoted all his attention to the propagation of sisu , going so far as to import seed for this purpose from Fatehgarh. It does not appear that any attempt was ever made to conserve the forests on any system or to control fell- ing operations, and in 1829 the revenue had fallen off so much that balances amounting to Rs. 6,000 had to be written off on account of the leases granted in 1825. Major Young then took charge of the forests and offered the right of levying the forest duties to pub- lic competition by auction. The experiment was fully justified by the results, giving a revenue of Rs. 6,425 for the ghats on the Jumna and Ganges and of Rs. 9,595 for the passes to the plains, or a total of Rs. 16,020. The duties were farmed at these rates for the years 1830-31 to 1832-33, when another auction sale gave an income for three years longer of Rs. 25,345 a year. From 1839 to 1844 the farm was leased to Atmagir, a Mahant of Hardwar, for Rs. 35,000 a year, and at the conclusion of his lease the forests were taken *To Commissioner, Kumaun, 15th September, 1896. 5 In appendix A. 2. -will be found a list of the iatee authorised for collection by Mr. Shore. 864 HIMALAYAN districts under direct management by Mr. Yansittart and so remained until 1855, when a forest establishment was formed. A sal log which would then fetch at Meerut between forty and fifty rupees and could be carried on a four-bullock cart paid an export duty of only eight annas. Five of these carts could carry out one hundred maunds of good lime worth over Rs. 100, the duty on which was only twenty annas. A four-bullock cart of catechu sold for Rs. 200 in the plains, and a similar load of bambus (about 400) was worth eighteen rupees. It can therefore be readily understood how eager speculators were to enter into this profitable business, especially as no control what- ever was exercised over their operations either as to the quantity of timber cut down or the localities to be worked. Mr. Williams writes : — “ Every one continued to hack and hew away at the trees as he pleased, only paying certain dues to the farmer in the event of the wood being exported. The latter made his own arrangements to secure the collections at the different passes. Reckless waste was inevitable and the fine sctl forests began to disappear rapidly. The absence of conservancy was absolute. The district still abounded in fine trees from one hundred to two hundred years old and upwards. All these fell before the axe, and probably the rest would have gone with them had the roads been a little better. The consequences of this bad system are most perceptible in the western Dun whilst in the eastern Dun large numbers of hhair trees were cut down to burn lime for the Riirki workshops and the canal head at Maya- pur. With the introduction of a regular forest establishment in 1855 the revenue rose enormously, but unfortunately even then no sys- tem of conservancy was attempted. The mutiny intervened and in 1860 the revenue began to fall, and in 1867-78 reached the low figure of Rs. 23,332. In 1864, regular forest operations commenced under Mr. F. Williams, C.S.I., Commissioner of the Meerut divi- sion, within which the Dehra district is situate. His jurisdiction extended over the whole of the Dun forests, the Siwaliks and a por- tion of the Saharanpur district, besides certain forests of the outer range leased from the Raja of Tirhi. The story of the sub-Siwalik forests in the Saharanpur district has been noticed in the Memoir of of that district. No attempt of any kind was made to preserve the forests there ; on the other hand efforts were directed to induce OP THE NORTH-WESTERN PROVINCES. 865' squatters to take up the land and clear it for agricultural purposes, and grants of so-called waste land were made to any one that could be prevailed on to accept them. Up to 1839 the forests were left entirely in the hands of the Rajput zamindars within whose boundaries they were nominally included, but in that year some 142,420 acres were demarcated as forest under the names Kheri, Kansrao, and Pathari Nadi. Within these boundaries the grants were made and the tracts unlet were handed over to the new Forest Department in 1864. Mr. Williams devoted his attention to a survey of the forests, to making roads and securing and defining the rights of Govern- ment and individuals. This was no easy task owing to the neglect of former years which permitted the growth of prescriptive rights by lapse of time. It was not until 1877 that the forests were pro- perly demarcated, 1 and we shall follow the arrangements then made in our brief description of the existing forest sub-divi- sions. Block 1, called the Siwalik range, is bounded on the west by the Existing forest-di- Jumna and on all other sides by a forest line visions. marked by pillars. It has an area of 449’12 square miles and contains sal, sain , and cl dr. The two former are the prevailing trees, but are all young, and the last occurs along the slopes of the hills and on the higher peaks. There is a consider- able export of bambus and the range affords pasturage for numerous herds of cattle. Block 2, known as Majhera, lies in the Rurki parganah and consists of islands in the Ganges well stocked with sis a and /chair. The area is only 6 ‘74 square miles. In the western Dun we have block 3, known as Ram pur Mandi on the Jumna, devoid of trees and only yielding a revenue from grazing dues and grass. It has an area of only 1'54 square miles. East of this comes block 4, comprising the sal forest of Ambari and having an area of 6*4 square miles. The sal here is immature and is mixed with sain, bci/cli, and inferior forest trees. Block 5, or Cliandpur, has an area of 3*38 square miles and con- tains sdl mixed with a few tun, sain, and bdkli trees. 1 The following references are to the notifications of Government demarcat- ing and reserving the forest lands : — 73, dated i6th March, 1 877 (all the Dunl : 74, of same date (closes Thano and Balawala): 443. dated 24th September, 1877 (reserves the eastern Dun): 190, dated 19th July (reserves the Pathari forests): 184, dated 27th February, 1879 (reserves all the forests). 109 866 HIMALAYAN DISTRICTS Block 6, or Dholkot, lias an area of 7‘94 square miles and consists of sal with an admixture of sain , dliaura, and a few tun trees, but none are mature. Block 7 comprises the scd forest of Thano in the eastern Bun and has an area of 9*96 square miles. There are no mature trees, but there is a very promising crop of sal interspersed with bciJdi, haldu, semla, sisu, and /chair. Balawala and Thano have been closed since 1877. Block 8, or Nagsidh, has an area of 25‘38 square miles consisting of sal , sain , hdkli , and haldu. Block 9, or Tirsal, is situate near Rikliikes and has an area of 28 - 22 square miles. All the mature trees have disappeared and only young sal remains, intermixed with dhdman , haldu , sain, jdman, and khair. Block 12, or Saora Saroli, comprises a small patch of semla, hdkli and dhdman near Raipur, with an area of only 1*82 square miles. Block 13, or the Song forest, consists mainly of khair trees and grass. Block 14 comprises the Patri or Pathari forests in pargana Jawalapur of the Saharanpur district and contains mainly dhdk and grass appropriated tor the use of the Rurki workshops. Attempts are, however, being made to introduce timber trees, with what suc- cess is not yet apparent. The Bhagirathi or as it is now called the Ganges division com- Ganges (Bhagira- prises the forests on either bank of the river of that name in the Raja of Tihri’s territories. These were leased by Mr. Wilson from the Raja of Tihri in 1859, and in 1864 the lease was transferred to Government for twenty years. About one-third of the drainage area of the Bhagirathi and its feeders is covered with forest and cultivation, of which the forest occupies about one-tenth, or on a rough estimate 600 square miles. 1 Prom the village of Jliala, close to the point where the Bhagirathi cut its way through the snowy range, to Gangotri, the valley lies nearly due east and west for a length of about seventeen miles and is filled with deodar. For a few miles above Gangotri deodar is c“> 1 Sec report by Major Pearson, Sel. Bee., N. W. B. (2nd Scr.), II., 117, and III OF THE NORTH-WESTERN PROVINCES. 867 also found, but stunted and of little value. The excelsa pine also extends eight miles up the valley above Gangotri, and the birch is found in patches to within half a mile of the glacier. The forest on both sides of the river is divided into blocks, each of which has been roughly surveyed, giving some 12,500 acres of deodar and a fair average of second class, third class and fourth class trees. Before taking over the forests they had been much neglected and injured. “The ravages committed by the cultivators in the west- ern portion of the valley, where thousands of dead trees, all killed by fire, disfigured the hill-side in every direction, were only equalled by the destruction committed by avalanches higher up the valley.” The former practice has been stopped, but the latter influence continues, and the damage wrought by the cyclone of 1880 will be visible for many years to come. Great forests of Quercns dilatata occupy the ridges between Ma- suri and the Bhagirathi, and noble forests of cl dr extend from Sainsa, some twenty miles above Tihri, as far as Bhatwari, a dis- tance of about fifty-five miles along the valley. The latter tree clothes the mountains on both sides of the river and its affluents up to 3-5,000 above their beds, filling every ravine and occupying every plateau. Above Bhatwari the forests of box, yew, and cypress commence and cover the hills on both sides of the river as far as Jhala, a distance of about thirty miles, and from Jhala to Gangotri, as we have seen, the deoddr is the principal forest tree. On the right bank of the river above Jhala, where it has a southern aspect, the forest is nearly pure deoddr , but on the left bank, with a northern aspect, there is a large admixture of silver-fir, spruce, and birch. Up to Darali the deoddr extends to about a thousand feet above the river’s banks, but further north it rises to fully two thou- sand feet, where it meets the vast forests of spruce and silver-fir already mentioned. The valley of the Jadli-ganga is also full of deoddr, and towards its head the valuable pencil-cedar occurs in appreciable quantities. As a rule the growth of the deoddr, except in very favourable localities, is much slower here than in the com- paratively warmer valleys of Jaunsar. From an examination of the stumps of many trees it was found that a diameter of 16 inches was attained in 64 years, of 24 inches in 105 years, and of 30 inches in 230 years ; the nearer the northern limit, the slower the HIMA'LAYAN districts ■868 growth. To recapitulate, the forests in the lower parts consist chiefly of pine. Higher up we have the yew, box, birch, three species of oak, two of juniper, cypress, silver-fir, spruce, deodar , and ■excelsa pine, and in small quantities the sycamore, horse-chestnut, and walnut. Only those useful timbers found in the more access- ible valleys bordering on the Ganges below Deoprayag and between the Hiunalgadh and the Dun have hitherto been exported, and the revenue collected has chiefly been from deoddr sleepers and small logs for building purposes and bambus. The lease from the Raja of Tihri includes the forests in the remaining portion of his territories about the heads of the Tons and Jumna rivers . 1 These lie to the south and west of the Bhagirathi Forests at the head of sub-division and may be noticed in order the Jumna and Tons. from the Bhagirathi westwards. There are the remains of a considerable forest of deoddr above Barahat near Saida and Uparikot in the Bhagirathi valley, and above it a splen- did strip of moru oak (Q. dilatata). Crossing the water-parting into the J umna valley, there is a small deoddr forest above Shalna and small patches of the same tree about the Bonk and Nagtiba peaks, whence there is water carriage by the Jumna to the Dun. Cross- ing the Jumna to the Kedar-kanta ridge which separates the Jumna from the Tons, there are the remains of what was once a very fine deoddr forest in the valley of the Banal, a tributary of the Jumna that joins it just above Barkot. There are also small patches of deoddr in the Ramasera valley to the south of the Banal, but of no great value. The chief glory of the Jumna is, however, the immense fo ests of the long-leaved pine (chir) that line its banks and in which there are numbers of magnificent trees fit for any purpose. Unfortunately, sleepers of pine are not esteemed by railway con- tractors, being liable to dry-rot and requiring frequent renewal, and no means for effectually preserving them have yet been discovered. The left bank of the Tons is also covered with immense forests of cMr. On the upper part of this river near Datmer, the cMl ( P.excelsci ) takes the place of the chir (P. longifolia ) . When the range that sepa- rates the Tons from the Pabar is crossed, we come again into a tract of which the characteristic forest tree is deoddr. The deoddr commences on the north of the Tons near Gangor,and is scattered all i Sel. Kec., N.-W. P. ; III. (2nd Ser.,) 129. or THE NORTH-WESTERN PROVINCES. 869 over the ridge that separates the Tons proper from the Panch-ganga river which joins the Tons opposite Shankuri. The hills here are rocky and precipitous, and the deodar is chiefly confined to the small ravines and streams that run down from them to the river. The more important forest lies between Gangor and Datmer and on the further side of the ridge above Lyor and opposite Kahsol and Raksha. Following the course of the Tons southwards, we find a consider- able amount of deodar on the spur that comes, down to the river a little above the village of Koarbo, also in the valley of the stream next to it on the west. The Rupin joins the Tons on its right bank at Naintwari, and on both its own banks and on those of its feeders are large and valuable forests, the lower part of which con- sists of deodar and the upper part of excelsa pine and silver fir. The valley of the next tributary of the Tons on its right bank also contains a very large proportion of deodar forest interspersed in places with silver fir, spruce, and oak. If we take the country from the junction of the Rupin and the Tons as far as the junction of the Tons and the Pabar, some of the finest deodar forests in the hills may be met with; and here the Forest Department found a valuable addition to their resources for meeting the demands for sleepers. In 1869, the forests of the upper Tons were estimated to contain 50,000 deodar trees fit for felling and to be able to supply a lakh of sleepers per annum, but no such great demand has yet been made on their resources. It is the Jaunsar-Bawar and Bhagirathi divisions that have had to provide the largest number of sleepers in recent years. In the year 1879, the forests on the upper Tons with those in khats Deogai’h and Bawar of Jaunsar-Bawar were formed into a new division known as the Tons division. The forests of the Jaunsar division now comprise the whole of Jaunsar-Bawar except khats Deogarh and Bawar to the north of the Dharmigadh and Banal, Shalna and Jaunpur in Tihri. They had little or no practical value in the earlier days of British rule, owing to their distance from the plains. With the denudation of the Dun, however, their real value became known, and some rough attempts at management were undertaken. Up to the year 1868, the Commissioner of the Meerut division was ex officio Conservator of the Jaunsar-Bawar forests, and when the latter came into the hands of the Forest Jaunsar-Bawar. 870 IITMA'LAVAN DISTRICTS Department, everything connected with conservancy had to he taken in hand. Here, as in the eastern hills, the people, though nominally in possession of immense tracts of forestland, were never considered proprietors, but occupiers entitled to the usufruct and whose rights were sufficient to prevent people from other Mints— as the local sub- divisions of the district are here called — from entering upon or using the nominal waste in their possession. They could pasture their cattle in every part of this nominal area and cut down trees for fuel or for building or other agricultural purposes, but could not alienate these rights to others. The Dun forests were being worked out whilst the demand for sleepers for the railways was increasing every year, so that it became necessary for the authorities to examine closely their timber resources, so as to meet the wants of both the Government and private persons, present and prospective. It had been shown that permission to graze cattle in a forest was absolute- ly incompatible with forest conservancy. Provision had also to be made for stopping the destructive fires that, hitherto, regularly swept away every year the young trees that a suitable soil and climate had raised to fill up the gaps caused by felling. The people were accustomed to obtain early grass in the hot weather by setting on fire the old grass, provided rain fell at the right time. This is the chief reason given for their adherence to this practice, but it has been shown that the rank crop of grass that occurs after firing is much coarser and less nutritious than if nature had been allowed to deal with the reproduction of the plant in its own way. Each one, too, imagined that he had a prescriptive right to hack and hew when and where he desired. The weak establishment hitherto kept up was insufficient to control the felling of timber, and it was not uncommon for a Jaunsari, who wanted one tree to repair his home- stead, to cut down eight or ten and sell the surplus. To remedy these evils, the forests had to be demarcated, then grazing and the felling of timber in unauthorised places had to be restricted, and, again, fire conservancy had to be introduced. To prevent unlawful felling in the demarcated tracts an officer was usually deputed to inspect the work before a pass was given to fell trees. The people objected to this, as it gave them trouble, caused delay, and cut off one source of their irregular gains ; so that in a short time a great cry was raised against the demarcation of the waste lands as OF THE NORTH-WESTERN PROVINCES. 871 Government property. As already noticed, at the former settlement, the right of each khat in the lands within its own boundary was declared absolute as against all , other khcits; the use of the wood and jungle products was allowed to them, hut it was held that they had no right as against Government — i. e ., Government could at any time step in and appropriate any portion required for its own use or for settlement with others, so long as sufficient lands were left for grazing purposes to each village. Since that time circum- stances have greatly changed and almost every considerable tract containing forest useful for timber or fuel has been appropriated and marked off as first or second class forest. A large area has been taken possession of at Chakrata, sufficient for all the require- ments, present and prospective, of the cantonment there. What remains is good for grazing or for grass and jungle produce or possibly for some extension of cultivation. It is good for little else, and there is no prospect of its being turned to any other account. There is probably no portion of this land that can be used either for tea cultivation or for any kind of plantation. Under these circumstances the question arose whether the restric- tion as to proprietary right being acknowledged in anything more than the cultivated and occupied spols should be maintained. Sir W. Muir resolved 1 that only such waste lands in excess of the requirements of a khat should be marked off* as “ Government waste ” that were in excess of one thousand acres. That within the khat proprietary right should be exercised over all third-class forest land to such extent as each khat might require, with the pro- vision that had always existed that there should be no power to alienate the lands. The restrictions as to grazing and collecting firewood were confined to first-class reseved forests. Such con- cessions as were then granted and such restrictions as were then enforced were entered in the wdjih-ul-arz or 1 record-of-rights’ of each village, so as to prevent any disputes in future. The Jaunsar division is entirely surrounded by Native States, except on its southern boundary, where it adjoins the Debra Dun. The main physical feature is the great central ridge that forms the water-parting between the Jumna and the Tons. Commencing at Haripur-Bias near Ivalsi, it runs west of Chakrata to Deoban, and 1 G. 0. No. 30A., Revenue Department, dated 4th January, 1873. 872 HIMA'LAYAN DISTRICTS then in a north-easterly direction to the Karamba peak. It next turns round the head-waters of the Dharagadh and proceeds east- wards into Tihri. It is along this ridge and its numerous spurs that the chief forests are found. The rocks are principally lime- stones, shales and slates. The first-class forests within this tract measure 8,795 acres, and the second-class forests cover 88,282 acres. The first-class forests are entirely within the control of the Forest Department with the exception of some 575 acres, within which grazing rights are permitted. Of the. second-class forests some 13,917 acres are temporarily closed and are preserved from fire to allow of reproduction. The division forms a section of the outer Himalaya and the forest vegetation varies accordingly. At Kalsi on the south we have such trees as sal, bakli, dhaora, kusam, haldu , khuir, and sisu, some of which run a long way up in the hot and confined valleys of the Tons and Jumna to an elevation of nearly 4,000 feet. We have next the grey oak, rhododendron, and Andro- meda between 5,000 and 7,500 feet. At the lower limit we have the chir pine and at the upper the blue-pine and the deodar. Above these, 7,500-10,000 feet, come the deodar, moru and karshu oaks, four species of maple, horse-chestnut, walnut, cypress, spruce and silver fir, yew and several species of Pyrns and the willow. Of all these, the deodar is the most valuable, and it is now found in the Lohkandi and Kotikanasar forests in khat Misan : the Konain forest in khat Lakhan ; the Tutwa, Maura and Lakhan forests on the Dharagadh ; the Chijal or Kathiyan forest in khat Phanyar, and the Ivoti forest in Bawar. Of these the Lakhan forest is the finest, but it is doubtful whether the Dharagadh can be utilized for the transport of timber. The revenue and exports of timber will be found in the appendix. The forests of the Upper Himalaya in Kumaun and British Garhwal contain very little deodar and are Forests of the Upper „ 7 , Himalaya in British ter- composed principally of c/nr pine, spruce, rltory - silver-fir, oaks, horse-chestnut, and other trees of small economical value, and consequently, except those on the upper feeders of the Alaknanda, 1 have hitherto been little 1 See Webber’s forest survey of Kumaun and Garhwal, 1864-65, which gives colored maps ou the scale of one mile to an inch in sheets of twelve inches square, accompanied by tabular statements showing the acreage and number and class of trees in each block. OP TH® NORTH-WESTERN PROVINCES*- STB worked. Front these fatter a large number of chir sleepers lias been supplied to the East Indian Railway. There are several fine forests of Abies Smithiana, A. Webbiana and Pinus excelsa along the left bank of the Alaknanda from Joshimath to Pipalkoti, but they occupy the tops of the ridges at some dis- Northern Garhwal. . ^ tance from 1 the river; I lie long-leaved pine covers the slopes of the Nagoli valley opposite Nandprayag, the Nagpur hills opposite Chhatwapipal, and the valley up to Pokliri. The forests on the upper part of the Mandakini and in the valley of the Mad mail esh war rivers are too distant to be of economical value. Similarly, the fine clrir on the slopes of Tungnath are too far from the river to bear the expense of export, though, perhaps, the box- wood, of which there are some good examples, may prove- of use. The cypress and excelsa forest on the Bishuuganga near Badrinath is also too far removed from the means of carriage to be suitable for working. The pine forests near Tapuban on the Dhauli a^e the most extensive in Garhwal. They stretch in one unbroken olock from the western spurs of the Pilkhunta range to above Rindi, a distance of sixteen miles with a breadth of from one to three miles. All this is a mixed forest of Abies Webbiana , A. Smithiana , P. ex- celsa, cypress and a few deodar , with box, yew, and Quercus semecar- pifolia. The sycamore (Acer pictum, Thunb.), from which the Tibetan bowls known as lahauri-doba are made, is found' in the valley of the Rluiganga with horse-chestnut ( yPJsculus indica) and silver fir. Higher up the Dhauli as far as Malari similar forests occur, and here also' is the only natural deodar forest in British Garhwal, hut unfortunately so placed as to be useless for export. In Southern Garhwal, there are chir forests on the Nayar at Kainur, Sungarkhal, and Juniyagarh, and on the Dudukatoli range, great forests of silver fir and spruce cover all the summits up to 8,000' feet. The western slopes of the same and adjoining ranges are clothed with dense forests of oak and other trees of some value to the extent of about fifty square miles, of which the silver fir occupies eleven square miles. Below Kainur, the Nayar might be used for transporting small timber during the floods, but the Chhiphalghati river is too shallow for this purpose and too much obstructed by boulders, 110 Southern Garhwal. 874 HIMALAYAN DISTRICTS though fine cMr trees are to he found on both its banks and at Saimkhet and Tal. The Dhanpur hills have been cleared of jungle for the mineral works. The eastern slopes of the Dudukatoli range are covered with oaks and some seven square miles of silver fir and they drain down to the Ramganga. A fine cMr forest nearly fifty square miles in extent occupies the valleys leading to the Ram- ganga between Lohba and Ganai, and the pine-clad slopes of Badhan- garh and Bhatkot have a similar direction. The Ramganga appears to be large enough for floating down sleepers during the time of flood, and these forests may prove a useful reserve hereafter. All the hills below Ganai are covered with stunted and twisted clur. Extensive cMr forests of good quality exist at Ranikhet and Syuni, and have already been noticed: also along the Gagar range and in the Malwa Tal, Ramgarh, Saimkhet, and Khairna valleys, and at Badhandhura on the Kosi. The Kosi appears to be unfit for rafting except in the floods, when small timber might be sent down it to Ramnagar. The pine forests on the Pindar from Betuwa to Ivulsari adjoin „ the river where it is 3-600 feet wide. From North-eastern Garhwal. May to October, the floods are incessant and sufficient to float the largest timber to the Alaknanda at Karn- prayag, and thence to the Ganges at Hardwar. There are no rocks, rapids or obstructions the whole way, and the fall is about fifty feet to the mile. The cost of felling is about two annas per tree, and the cost of carrying and shooting down large trunks would be from two to five rupees each according to the distance or, if pre- viously cut into sleepers, about one anna per sleeper per mile of land carriage. Sawing can easily be arranged for by imported labour. For three or four miles above its junction with the Pindar, the Kailganga might be used for sending down small scantlings of the pine which grows abundantly along its banks, but the cypress appears to be too far up to admit of working. The Nandakini, for the first fifteen miles from its junction with the Alaknanda, possesses sufficient volume in times of flood for the transport of sleepers from the magnificent forests along its banks. The extent and variety of the pines here are nowhere surpassed. They grow over the entire valley, six different species being indigenous and a diameter of five feet is a usual size. The spruce forest above Kanali is the most 875 OE THE NORTH-WESTERN PROVINCES. important, but cypress and deodar also occur with yew, hazel, box, and all the other pines except Abies dumosa . The upper valleys of the Sarju and its tributaries contain over & hundred square miles of fine pine forest. Northern Kumaun. About and above Kapkot there is nothing but pine ; much of it, however, is practically inaccessible, and as the Sarju is not a snow-fed stream, rafting can only take place in time of occasional floods in the rains. The valley of the eastern Ramganga down to its junction with the Sarju has a considerable extent of cMr and silver-fir forest along its banks, but the river itself presents some obstacles to rafting, Sdl also occurs in the valleys of the Sarju and Ramganga, but of little value as timber. There is a con- siderable amount of pine forest near enough to the Kali, and about Askot and Balwakot some very fine timber. Indeed, almost all the valleys leading down to the Kali between Askot and Barmdeo con- tain an abundance of chir of very fair quality. The Grori has a volume iu time of flood nearly equal to the Pindar, and there is no obstacle in its course from the pine districts to the Kali. The chir forest along its banks, especially near Mastoli, are inferior to none in quality or quantity. The banks also are well-adapted to shooting down logs into the river, and labor is cheap and abundant. A mixed forest of silver fir and A. dumosa with box occurs on Hum Dli lira, but apparently too high up to be available for timber. The forests around Chipula abound with horse chestnut, sycamore, birch, yew, poplar, and wild fruits which grow up to 11,000 feet, above which is bare grass and rocks covered with snow till June. These are all too remote from the river to be available for timber for export. In the upper valley of the Kali there are numbers of chir along the precipices close to the river, scattered patches of the hemlock-spruce {A. dumosa) intermixed with the excelsa pine and considerable blocks of the silver fir, here called ivtiman, which occurs also in the Darina valley, too far from the river for export. Box is found in the Gori valley near Milam, and in the Byans patti und er the name papri. The grain of the wood appears to be coarser than that of the European species. The yew is as good as the European species for turnery and all purposes. The holly is close and even grained, and fit for turnery, and the species of birch known as piiya- utis yields a wood for doors and panels that bears a very high 876 HIMALAYAN DISTRICTS polish and is one of the best that we have. Besides these, maple, hazel, birch, wild apples, wild cherries and pears abound, all of which have their value as timber for turnery and other purposes. It can - not be denied that, as in the case of mines, much of the valuable timber trees of the Inner Himalaya are in such a position as to render them practically useless for export ; but should the necessity arise, some mechanical contrivance will doubtless be invented for the better and more easy removal of the logs to a stream that can carry them to the plains. The shoots that have been in use in Jaunsar for some years have materially assisted manual labour, and when advisable, the same princi pie can be applied to the removal of valu- able timber from the fores ts of British Garhwal and Kumaun. We have now briefly sketched tbe character and position of each of the great State forests, and shall proceed Forest Department. to describe the system under which they are managed. The expenditure under ‘ fores is’ is divided broadly into that incurred on account of 4 conservancy’ and that for 1 establishment/ The establishment protects the forests from trespassers, prevents unauthorised felling of timber, cuts down creepers and noxious undergrowth, marks trees for felling, repairs the fire lines, and superintends felling operations, both those undertaken on behalf of Government and those carried on by private individuals. The forest officer himself decides when felling operations may be under- taken, the principle observed being to work out distinct blocks as well for the sake of more easy supervision as to enable the depart- ment to open or close distinct areas at the same time. It is also the duty of the forest officer to superintend the felling, sawing, collect- ing and carriage to the depot of the timber collected for Govern- ment ; the counting, stacking, and classification of the logs in the depot and the settlement of the accounts of contractors ; the repair of old roads and the construction of new ones. The forest officer has charge of the collection of tolls at the forest stations. These are situate along the main lines of forest road, and in each there is a clerk and several peons. On the arrival of produce of any kind liable to toll, the clerk examines it, and the quantity and the duty received are entered in a book arranged in the form of a receipt and counterfoil. The clerk hands the receipt over to the exporter, and forwards a copy of the counterfoil to the head-office of the OF THE NORTH-WESTERN PROVINCES. 877 forest-division. The exporter proceeds with his load until he is stopped at a second line of posts established where the forest roads converge on the main public roads. Here he gives up his pass, and the goods are again checked and any deficient duty is collected. These passes are also sent to the head-office and compared with the copies of the counterfoils previously forwarded by the clerks in charge of the first line of posts. Deputy overseers inspect each post, and rangers patrol the intermediate spaces to prevent smug- gling ; and in addition the smallness of the tax makes it hardly worth the trouble and risk necessary to successfully evade the pay- ment on petty ventures. It is only when the exporter bribes the whole establishment and removes valuable timber wholesale that any profitable result can be expected, and this may be considered a very remote contingency. The revenue collected is forwarded day by day from post to post to the nearest treasury, and the official in charge reports the amount received from each post to the head- office of the division, and this is again compared with the total entered in the passes and counterfoils. Timber marts. The principal timber depots in the Kumaun forest-division are those at Ramnagar and Moradabad, and the markets for minor forest produce are at Chorgaliya, Haldwani, Kaladhungi, Chilkiya, and Ramnagar. The Nairn Tal forest-division finds its market in the settlement itself. It has a special local conse rvancy staff, who superintend the felling of trees for timber, fuel and charcoal, the dues on which are col- lected according to a special table of rates. The Ranikhet forest- division is purely conservative and supplies only the local demand in the Ranikhet settlement. Khohdwara or Kotdwara, as it is more commonly called, is the great mart for the exchange of minor forest produce in Garhwal, and, for the sale of timber, depots have been established in this division, both on the Ramganga and on the Ganges. Hardwar on the Ganges and Rajghat on the Jumna are the two great timber depots for the whole Himalayan tract between the Ganges and the Tons, including the Dehra Dun, Jaunsar, and Bhagirathi forest- divisions. A considerable amount of timber and minor forest produce, however, finds a way to the plains through the passes in the Siwaliks to Saharanpur, Dehli, and Meerut. Good roads connect all these marts with the different lines of — 878 HIMALAYAN DISTRICTS railway, and with the extension of the existing line from Bareilly to Pilibhit and Naim Tal, the communication, so far as Kumaun is concerned, will be complete and the value of the minor forest pro- duce will be enhanced considerably. In appendix A. will be found a table showing the rates now levied on timber of all kinds and minor forest produce in the Kumaun forest-division. It has not been considered necessary to give these tables for every forest-divi- sion, though they vary slightly in details in each tract. Enough has been given to furnish a fairly accurate idea of the extent and character of the State impost on forest produce. Perhaps the most curious fact elicited is the number and variety of the articles coming under the head ‘minor forest produce.’ Here we have the drugs, tans, dyes, 4 gums, reeds, fibres and grasses of the preceding pages, with the toll that is levied on them by Government, and the average annual export from the forest-division based on the returns of four years. It has been found impracticable to give a correct selling price for these articles : so much depends upon the locality and circumstances. The greater part is collected and exported by the poorer classes who exchange their goods for grain or clothes and earn but a scanty subsistence. Still confining our remarks to the Kumaun forest- division, some idea of the extent of the felling operations will be gathered from the fact that, between 1859-60 and 1879-80, the tim- ber cut and and sold by Government agency amounted in this divi- sion alone to 3,040,241 cubic feet and the quantity cut and exported by private agency amounted to 2,620,607 cubic feet between 1865- 66 and 1879-80. The greater portion of this timber was sal of good quality, though of late years second-class timber has come into considerable repute. In addition to this, great quantities of dry timber were exported by merchants at lower rates, and in the Kumaun Bhabar, many thousand acres of sal, haldu, dhami, and other trees were cut down and exported to make room for cultiva- tion. No detailed account of the quantity can be given as the duty was usually levied by cart or bullock load. If we remember that similar operations are going on in each of the other forest-divisions bordering on the plains, some, idea may be formed of the extensive nature of the forest operations. In Jaunsar and the Bhagirathi valley the principal export is timber for railway sleepers cut and exported by Government agency. Appendix A. gives the revenue and ■ i OF THE NORTH-WESTERN PROVINCES. 879 expenditure of all forests for as far back as the records appear accurate enough for reproduction. Rheea. Boehm eria nivea, Hook, et Arn . ; Urtica nivea, Linn. ; U. tena- cissima, Roxb. — China grass, rhea, rheea, ramie (Malay). Brandis, 402. The rheea is indigenous in China, Japan, the Phillipine Islands, Java, Sumatra, the Indian Archipelago, Siam, Burma, Singapur, Penang, Asam, and Rangpur and Dinajpur in Eastern Bengal. It is cultivated in China, Japan, and the Indian Archipelago, where it is stated to like a moist soil, and flourishes best in alluvial deposits along the banks of rivers and generally in the fertile flats such as are found in its native haunts in China and Sumatra. The cultiva- tion of the rheea in these provinces dates from the year 1863, and in 1865 there were several small plantations in the Dehra Dun. The Government plantations were begun in 1867 by devoting a small portion of the Chandwala garden in the Dun to the propaga- tion of the plant for distribution to those who desired to embark in its cultivation. In 1870, the regular cycle of inquiries as to the value of the economic products of India brought rheea prominently to notice, and orders were issued for the extension of the existiuo- Government plantations both in the Dtin and at Saharanpur. In 1871, a prize of £5,000 was offered to the inventor of the best machine or process for the preparation of the fibre, and in the same year, instructions were issued for the supply of stems for a trial between competitors for the prize and for distribution for prelimi- nary experiments to all who were likely to make use of them both in this country and in England. During the year 1871-72, the area under rheea in the Dun and at Saharanpur exceeded 37 acres, and upwards of nine tons of stems were forwarded to England for the use of intending competitors. First competition. The first trial for the prize took place at Saharanpur in August, 1872, when a machine, the property of Mr. J. Greig of Edinburgh, was entered for com- petition. The following extract from the official report of the trial will show what degree of success was obtained : — “ The machine, as a piece of mechanism, is good ; it is well-made and well-pro- portioned, the relative strength of the various parts having been well considered. 880 HIMA'LAYAN DISTRICTS It is calculated to wear well, and deserves commendation so far as being a good substantial piece of work. The machine, however, as must always be the case with machines of this kind, i. e., contrived to do a work of which there is little or no experience available and without means of obtaining the natural material to work upon, is far from matured. Few, if any, of such machines are ever con- structed at once able to do the work for which they are intended ; most are generally perfected by degrees through numerous partial failures ; experience gained in the process of working alone enabling many defects to be seen and remedied and a perfect machine to be produced, and such appears to be the case with this mill ; for, independent of whether it is or is not the best description of machine for preparing the fibre, it is, on the one hand, in many points very deficient in the work the exhibitor sets it forward to perform, while, on the other hand, it is certain that it can be improved in much that is faulty.” Mr. Greig was awarded £1,500 for his machine, in considera- tion of the skill, labour, and expense incurred in its construction, and in recognition of its being a real attempt to meet the wants of Government. In 1873-74 and 1874-75, the area under rhea was maintained at 37 acres, and in 1875-76 further instructions Second competition. . . ,. . _ were received to continue the supply ot stems for experimental purposes. In August, 1877, the offer of a prize of £5,000 was renewed, and the following specification of the machine required was published for general information in India, Europe, and America : — “What is required is a machine or process capable of producing, by animal, water, or steam power, a ton of dressed fibre of a quality which shall average in value not less than £45 per ton in the English market, at a total cost, including all processes of preparation and all needful allowance for wear and tear, of not more than £15 per ton, laid down at any port of shipment in India, and £30 in England, after payment of all the charges usual in trade before goods reach the hands of the manufacturer. The processes of preparation are to be understood to include all the operations required subsequent to the cutting of the stems from the plants in the field, until the fibre is in a condition fit to be packed for conveyance to the market. The machinery employed must be simple, strong, durable, and inexpen- sive, and should be suited for erection in the plantations where the rhea is grown. It must be adapted for treatment of the fresh stems as cut from the plant. The treatment of dried stems offers certain difficulties, and the fibre prepared from them must, moreover, always be much more costly than the fibre produced from green stems. Except during the hot, dry, weather preceding the rains in Upper India (where rhea grows best), it is very difficult so to dry the stems that no fer- mentation or mildew shall occur. But during this season the stems are compara- tively short and the crop poor and stunted, unless it is artificially irrigated, and such greatly increases the cost of cultivation. In the rainy season the plant is in fine condition, but at this season it is almost impossible to dry the stems in quantit OF THE NORTH-V/E STERN PROVINCES. 881 without injuring the fibre, unless recourse is had to artificial means of desicca- tion, which greatly increase the cost of the material. It is therefore obvious that the attention of inventors should be given to the discovery of a process for the treatment of the green stems.” The trials commenced in September, 1879, at Saharanpur, and ^ ^ ten competitors entered machines of differ- ent kinds, of which three were withdrawn. The following is an abstract of the results : — - Competitor. Green stems worked up. Total fibre obtain- ed. Percent- age of fibre. Cost per ton. Tons, qrs cwt. fi). m. Es. a. p. M. Z. P. Vander Ploeg 1 14 0 0 H 8 i 311 337 8 0 Dr. Collyer 1 0 0 0 147 660 112 0 0 Paris machine ... 104 . . • 483 14 0 M. Nagona 3 7 3 0 337k 4-44 38 14 4 Mr. Cameron ... 1 2 3 0 9 4 3-61 270 12 0 Mr. Aruery 1 10 0 0 3-21 418 0 0 Mr. Blechynden 0 11 1 0 685 4-68 251 4 6 The judging committee consider that the limit of £15 per ton for the cost of preparation and laying down the fibre at a port of shipment in India would render competition practically impossible from a place so distant from the sea-board as Saharanpur. Fur- ther, that the plant grown at Saharanpur is not calculated to give such good results as that grown in more suitable localities, but that, on the whole, the experiments made during the trials, though not decisive, have gone far towards establishing the conditions under which a fair verdict can be awarded and have advanced an impor- tant step in the progress made towards the solution of the problem. The awards have not yet been published, as they depended on the valuation of the fibre in the English market. The advance made in this competition shows that the invention of a successful machine is merely a question of time and justifies the resolution of Govern- ment to continue the supply of rheea stems for experimental purposes. The Dutch botanist Blume, in his report on the cultivation of rheea in Java and Sumatra, states that Cultivation and prospects. . . , . . ... “ the plant thrives best in shade, m a moist and fertile soil : conditions such as are usually found in abandoned 111 882 HIMALAYAN DISTRICTS coffee plantations. * * The plant thrives best in the hilly parts of the country in which rain is frequent. In the plains it would require irrigation.” The conditions under which the plant flourishes in the countries best adapted to its growth are a moist tropical atmosphere, a shady situation and a low-lying alluvial soil. These conditions do not exist in Saharanpur. In the cold season, so soon as the temperature falls to about 40°F., the whole crop, leaves and steins, become black and fall to the ground. The roots then remain dormant until January, when the fields become green again with the young shoots. As the weather becomes warmer, the plants require irrigation at regular intervals of time, and weeds must be removed until the plants are strong enough to keep them down. The stems also are very short, owing to the effect of the hot dry winds which prevail in these provinces, and they ripen irregularly from the same cause, the tops being often green and soft, whilst the lower portions are ripe and hard. Until the meeting of the com- petitors in 1879 it was not known how inferior the Saharanpur stems were when compared with those raised in more suitable cli- mates. During this trial, stems grown in Dehra and Calcutta were found to give better results than the local produce, presumably owing to their having been raised in a moister climate. A healthy stem is described as an evenly shaped flexible wand of a length varying from 5-7 feet with the same colour throughout and ripening in all parts simultaneously. The Saharanpur stem was generally an irregularly shaped stick, 3-5 feet high, of uneven growth, with irregular distances between the joints. Many of the stems were stunted and imperfectly nourished and unequally ripened. The conclusion arrived at by the committee was that either the cul- tivation was insufficient or the climate is unsuitable. Experiments are now being made to ascertain whether trenching and heavy manuring will correct the defects observed, but it is believed that, as with most plants, climate is the first consideration, and therefore rheea cultivation in the drier parts of these provinces can never be more than partially successful. There is no difficulty in raising the plant from seed or in propagating it by cuttings. Dr. Jameson has estimated that an acre will yield four crops in the year, aggre- gating ten tons of green stems. Taking the yield of fibre at one- twentieth of the green stem, the return of marketable fibre per acre OF THE NORTH-WESTERN PROVINCES. 883 will be half a ton. The value of rheeasfibre in the English market at present is from £40 to £60 per ton, according to quality, a price that should always leave a fair margin of profit to the cultivator of the plant and the preparer of the fibre. CINCHONA. For several consecutive years previous to 1872, experiments were undertaken in the valleys and hills of these provinces for the cultivation of the cinchona plant. It was tried at Chandwala and other localities in the Dehra Dun at 2,500 feet, at Chhajauri in Garhwal at an altitude of 4,500 feet, and at Mussooree at an altitude of 6,500 feet. In Kumaun, experiments were made in the Bhabar at 2,000 feet, at Hawalbagh at 4,500 feet, at Ayar-Toli and Rani- khet at 6,000 feet, and at Arkalli at 6-7,000 feet. In all these places, except the Bhabar, the plants progressed during the hot weather and rains. It was considered necessary to protect the young trees from the frost during the cold weather, and this was done for three years and until many of the plants had attained a height of 4-6 feet. These, with many others ranging 2-3 feet, were then left uncovered during the cold weather, with the result that every one of them perished in all the localities mentioned. Similar attempts proved unsuccessful in the Kangra Valley and Panjab Himalaya. In Kangra, where many of the plants had reach- ed 4-5 feet in height, a single winter’s frost was found enough to destroy them, and at Ranikhet, plants of C. succirubra , 4-5 feet in height, were cut down by the frost, though partially protected. Dr. Jameson closes his account 1 of these operations with the following remarks : — ■“ To continue the growth of the plant as an experiment in view to the cultivation for economic purposes would be a mis- take, and the time therefore has come to close the experiment which has been carried on with the utmost labour, care, and attention, and to declare that the valleys and hills of the Himalaya of the North- Western Provinces and the Panjab are not fitted for the cultivation of the cinchona plant.” TALLOW TKEE. Stillingia S’ebifera, Michx. — Tallow-tree. A tree belonging to the natural order Eupliorbiacece , introduced from China. This tree fruits abundantly in all climates in India 1 Sel. Rec., N.-W. P. (2nd Ser.), VI., 602, and Dick’s Report, ibid., I,, 79. 884 HIMALAYAN DISTBICTS from Calcutta to the Himalaya. There are large plantation® its Saharanpur, the Dun, and on the several tea-plantations in Kumaun. The seeds were sown in the Saharanpur gardens in 1858, and so rapid was their growth that, in 1866, they measured 6 feet in cir- cumference 3 feet from the ground. Plantations were esta- blished in the Dehra Dun, at 4-5,000 feet in the hills at Hawalbagh, Ayar Toll, and Paori, and in all these places there was an abundant yield of fruit. The seeds lie within a capsule and are enveloped in a fatty matter which yields a tallow. Animal tallow consists of stearine and elaine, both of which are found in nearly a pure state in these seeds. The mode of extracting 1 the tallow is very simple. It is merely necessary to boil the seeds and strain through cloth into water; and to purify the fallow, boil again in water and strain through a cloth as before. For burning purposes the tallow is excellent, as it gives a clear, bright, inodorous flame without smoke. It has also been tried with some success as a lubricator for railway wagons. The wood is close-grained and yields a timber well fitted for printing-blocks, and the leaves afford a dye. It was thought, at one time, that the cultivation of this tree in Kumaun would yield results second only to tea, but actual experiment has shown that the labour and expense involved in collecting the seeds and extracting the tallow are far in excess of the value of the product ; and in Calcutta, where it was introduced over thirty years ago, the result has been the same. IPECACUANHA. Cephcelis Ipecacuanha.— In 1870, Dr. Jameson procured two plants at the Kew Gardens and brought them out to India, where they arrived safely and were planted in the gardens at Chandwala in the Dehra Dun, but ultimately perished from frost. CORK OAK. Quercus suber, Linn.— Cork oak. Brandis, 485. At various times seeds of the Italian and Spanish cork oak have been planted in Dehra Dun and have germinated freely. The young trees thrive well and may, hereafter, prove of value, but the ultimate success of the experiment has yet to be seen. 1 For Dr. Macgowan’s description f the process of manufacture in China. se3 J. Agri.-Hort., Ben., VII., 164. OF THE NORTH WESTERN PROVINCES. 885 SWEET CHESTNUT. Castanea vulgaris, Linn.; C.vesca, Gsertn. — Sweet chestnut, Spanish chestnut, chataignier. Brandis, 491. The seeds of this tree were introduced by Sir John Strachey, and subsequently consignments were received by the Superintendent of the Botanical Gardens, Saharanpur, by whom they were planted and the young trees distributed all over the Don and Kumaun. The chestnut yields freely in the Duns and Lower Himalaya, and now forms an appreciable addition to the fruit resources of the Debra bazar. In Italy, Greece, Central France, Spain, and Corsica, it forms an important article of food for the inhabitants of the mountainous regions of those countries, and from the success of the experiments tried here, it appears that the establishment of the chestnut in suitable localities in these hills presents no difficulties that cannot be easily surmounted. CAROB. Ceratonia Siliqua, Linn. — Carob or St. John’s bread-fruit tree : the Algaroba beans of commerce (fruit). Brandis, 166. The carob was introduced by Dr. Jameson from Malta in 1861, and by 1863 it was extensively propagated and distributed in the Dun. The trees, though they flourish well, do not seem to give pods in such quantities as they yield in Malta and Italy. In 1866, the same report was received, and in 1880, it has been decided to try to improve the quality of the seeds by grafting, which, in Italy, not only produces better fruit, but gives a yield in a much shorter space of time. The trees appear to be unaffected by any extremes of temperature or excessive moisture. The sweet nutritious pulp of the pods is ground and mixed with grain and then baked and eaten by the poorer classes in Italy, the Levant, and Malta. The pods are also given to draught cattle in the proportion of one measure of carob beans to two measures of barley, and on this food they both work and thrive well. This tree is indigenous in Spain, Algeria, the eastern part of the Mediterranean region, and Syria. MEZQUIT. Prosopis glandulosa— The Mezquit bean. This plant, a native of Texas, was introduced in 1878, and has been successfully propagated in Kumaun. It produces pods freely 886 HIMALAYAN DISTRICTS during the rains, not all at once, but in succession, and seems to stand the extremes of heat, cold, and moisture very well. The beans are used as fodder for cattle. Acacia tortuosa , a native of Jamaica, has recently been introduced. It yields a fodder pod and might be cultivated as a hedge as well. It thrives well at Saharanpur. The Euchlcena ( Reana ) luxurians , which yields a good fodder grass, is also under trial in the Government gardens, as well as a series of Australian grasses. The Pithecolobium Saman , or ‘ rain tree,’ has been found a failure, not being able to withstand the frosts in the cold weather. Several experimental sowings of fibre plants have also been made. Dr. Jameson recommended the cultivation of Agave Cantala and americana , Aloe angustifolia and intermedia , Sanseveria zeylanica and Tacca stricta. A recent report on Malaehra capitata shows that it grows to a fair height and seeds freely, producing a fibre, however, in no way superior to the indigenous patsan ( Hibis- cus cannabimis) , but useful for mixing with jute in the manufacture of bags. Some forty species of Eucalyptus have been cultivated. All seem to thrive faiidy, and some of them remarkably well in Saharanpur and the hills. Catalpa speciosa, Engel., a tree indige- nous to North America, yields a timber especially adapted for under- ground work, such as posts, sleepers, and the like, and is now under cultivation in Saharanpur, and will also be tried in Mussooree. Olives have been received from Florence and are now planted out at Chajauri, where they appear to thrive well, the climate and soil being very suitable. They are of the same species as that from which the famous Lucca oil is extracted. A considerable number of seedlings of the oil-plant, Lallemantia iberica, raised in Saharanpur have been planted at Mussooree, but it will take some time before a correct estimate of its value can be obtained. Madden records that hops were raised with some success in Hawalbagli in Kumaun over thirty years ago, and experiments in the Dun in 1862-63 showed that they grow well there also. In the plains, however, the flowers do not seem ever likely to be useful for brewing purposes. Hops grow well at Saharanpur, and during the rains become most luxu- riant ; but it also happens that the flowers are produced at that time and the heavy rain prevents their proper development. This would appear to be a matter that should affect the culture of the hop plant in this country wherever the periodical rains are felt, and OF THE NORTH-WESTETtN PROVINCES. 887 Tea. History. would apply to the whole of the Himalaya of these provinces equally with the plains. In conclusion, mention may be made that fruit trees of all kinds, vegetables, flowers, and ornamental shrubs, have been introduced and propagated and distributed all over the hills from the Tons to the Sarda, and that for this purpose the gardens at Mussooree, Chajauri and Ranikhet have well fulfilled the object for which they were established. TEA . 1 The history of the cultivation and manufacture of tea in the hill districts of the North-Western provinces having originated simultaneously with the introduction of the plant in India generally, and with its discovery as an indigenous plant in Asam, it will be advisable to commence with a brief sketch of the circumstances which have led to the undoubted success of tea culture in these provinces. The claim of first originating the idea of cultivating the tea plant in India is variously attributed. As early as 1788 it appears that Sir Joseph Banks, at the request of the East India House, wrote a memoir on the subject, 2 recommending the introduction of plants from China to Behar, Rungpur, and Kuch Behar. Some years afterwards considerable interest was aroused by the reported discoveries oi indigenous tea plants in Burma, Asam, Nepal, Kumaun, and Basd.hr. It was in Asam only, however, that the discovery of the truly indigenous plant was confirmed. Mr. Burrell is inclined to believe that the discoverer of the wild tea plant in Asam was Mr. David Scott, an Indian civilian, who, when Asam was ceded to us, took charge of the settlement of that province. It appears that sometime between 1819 and 1821 he sent a specimen of the Asam wild tea plant to Calcutta to his friend Mr. James Kyd, whose father, Colonel Kyd, corresponded with Sir Joseph Banks about tea cultivation in India amongst other matters. This specimen was handed over to Dr. Wallich, and Mr. Burrell has succeeded in identifying it in the Walli cliian herbarium now 1 1 am indebted to Mr J F Duthie, Superintendent of the Botanical Gardens, N.-W. P., for this notice of the tea industry in Kumaun 2 See an interest- ing paper read by Mr. A. Burrell before the Society of Arts on February 2nd, 1877, and published in the Society’s Journal, Vol. XXV., p. 199. 888 HIMALAYAN DISTRICTS belonging to the Linnean Society. Attached to the specimen he found a portion of Mr. Scott’s letter, but without any indication as to tho date. The conclusions arrived at by Mr. Burrell are fully borne out by Mr. Thiselton Dyer, who, being the author of a monograph on the Indian Ternstrcemiaceai, must have made a special study of this subject ; also by the late Dr. Anderson and Dr. McClelland. In a letter from the latter to Mr. Clerk Marsham the following passage occurs : — “ The circumstances brought to light by Mr. Burrell coincide exactly with what I hare always understood to be the fact, that specimens of the plant and seeds of the indigenous tea plant had been sent by Mr. Scott through Mr. Kyd to Dr. Wallich as early at least as 1821.” And further on he remark “ Had Mr. Scott’s discovery in 1821 been taken up in an active and enlight- ened spirit, several years might have been gained, but public spirit was not pre- pared at that period for much enterprise, and we were content to receive our teas from China. Besides, Mr. Scott had not at that time reduced the tribes on the frontier to subjection, and their troublesome character was kept alive by our war with Burma, and, above all, we wanted Lord William Bentinck, without whom the second discovery of the tea plant might have shared the fate of the first. What we have most to regret is that Mr. Scott’s discovery was not properly recorded, when steps might have been taken, with his assistance, for the transmission of seeds and plants to the Botanic Garden in Calcutta, where the tea plant could have been propagated twelve years before its subsequent discovery in Asam.” Other writers on the early history of Indian tea have mentioned Mr. Bruce as having first discovered the true tea plant in Asam, but as his discovery was only made in 1823, his claim must give way to that of Scott. The Kumaun plant noticed by Bishop Heber on his visit to Almora in December, 1824, as well as that of Basahr, described by Moorcroft in 1821, must be referred to an evergreen shrub called Osyris nepalensis and belonging to the sandal-wood family. Bishop Heber thus writes concerning this plant. “ The tea plant 1 grows wild all through Kumaun, but cannot be made use of, from an eme- tic quality it possesses. This might, perhaps, be removed by culti- vation, but the experiment has never been tried. For the cultiva- tion of tea I apprehend both the soil, hilly surface, and climate of Kumaun, in all which it resembles the tea provinces of China, are 1 Regarding the same plant Dr. Royle in his “ Illustration of the Botany of the Himalayan Mountain,” p. 322, says : — “ The leaves of this plant are in Kumaun employed as a substitute for tea : hence some travellers have been led ; into the error of stating that the true tea plant was to be found in this part of the mountains.” OF THE NORTH-WESTERN PROVINCES. 889 extremely favourable.” The plant observed in Nepal was a true tea plant in cultivation, and which Dr. Wallich afterwards ascer- tained to have been brought from Pekin on the occasion of one of the triennial embassies sent to China by the Gorkhali government. The idea of cultivating tea in the hill districts of Northern India Tea cultivation in the was first originated by Dr. Royle in 1827, Himalaya. who was at that time in charge of the East India Company’s Darden at Saharanpur. In a report to the Gov- ernment of India, at the close of that year, he pointed out the resemblance of the Himalayan vegetation with that of tea-producing districts of China, as well as the suitability of the soil, especially in Kumaun. Four years later he again expressed these opinions 1 to the Governor-General, Lord W. Bentinck, during the visit of the latter to Saharanpur. The representations of Dr. Royle from Saharanpur, and of Dr. Wallich at Calcutta, and of other writers, (eventually led in 1834 to the formation by Lord W. Bentinck of the Tea Committee. The chief object of this committee was to ascertain the best mode of introducing the Chinese tea plant into India, and of its cultivation in carefully selected localities. One of the first acts of the committee was the deputation of Mr. G. J. Gordon to China in order to arrange as to the best modes of obtaining both the gennine plant as well as Chinese cultivators. In the meantime,- arrangements- were being made to select the best localities in India for sowing the seeds which -were expected to arrive before the end of the year (1834). At the same time a set of queries was circulated by the committee for the purpose of obtain- ing the opinions of those who were most competent to give their advice on this matter. Two important communications were received in reply — one from Captain J enkins, Agent to the Governor- General in Asam ; and the second from Dr. Hugh Falconer, who had recently succeeded Dr. Royle as Superintendent of the Saharan- pur garden. After describing the conditions under which the tea plant was being cultivated in China, and the attempts which had been made to introduce the plant to other countries, he observes : — “ There is, perhaps, no part of the Company’s territories in India which supplies all the conditions of tea districts in China in respect of climate ; but there are situations which approach it so nearly as strongly to bear out the 1 See also his *• 111. Him.,” pjr. 1*24-27, where these views are more fully stated. 112 890 HIMALAYAN DISTRICTS conclusion that tea may be so successfully produced in this country as to be object of high commercial importance * * * * It has been seen that the annual heat of the southern limit of the tea cultivation In China, assumed to extend to Canton, is 73° F. At [Saharanpur, which may be considered as at the northern limit nearly of the plains of Hindustan, 3° of latitude higher, and 1,000 feet above the sea, the mean temperature of the year is 73° F. ; the temperature of June is 90°, and of January, 52°. “ In the Himalaya mountains this case is widely different, excepting periodi- cal rains ; here all the conditions of the temperate climate are found, and here; above all parts of India, we ma.y look for successful cultivation of tea.” After describing the geological feat ares of these mountains, having made a special study of the subject, he summarizes his opinions as follows r — 1. “ That the tea plant may be successfully cultivated in India. 2. “ That this can be expected nowhere in the plains from 30° north down to Calcutta. 3. ci That in the Himalaya mountains near the parallel of 30°N\, notwithstanding some circumstances of soil and moisture of climate, the tea plant may be cultivated with great prospect of success ; that a climate here may be found similar in respect of temperature to* the tea countries in China ; that in the direction and great slope of the hills, the absence of table-land or elevated valleys, and the con- tracted figure of the existing valleys, are the chief difficulties in the way of cultivation, which may prevent tea from being produced in great quantity on any one spot. 4. “ That the most favourable ground for a trial is a tract on the outer ridges, extending from 3,000 feet above the sea, or the point where the hot wind ceases, up to the limit of winter snow. 5. u That in the valley of the Dhoon, if not the better, the inferior sorts of tea might be produced.” The opinions expressed by Dr. Falconer in the above letter are remarkably similar to those of Dr. Hoyle submitted from England about the same time ; and, as the latter declared, u without any communication of ideas, for the two essays must have crossed each other at sea.” Among the localities recommended by Dr. Hoyle were Bliim Tal, Hawalbagh, Delira, and Pinjor in valleys from 2-2,500 feet in elevation above the sea; also Almora, Jerrapani, Nahan, and Subathu at elevations of 4 to 5,000 feet ; also Mus- soorie at 6,500 feet. OF THE NORTH-WESTERN PROVINCES. 891 Dr. Falconer. Shortly after this Dr. Falconer received orders to examine the hill country situated between the Jumna and the Ganges for the purpose of selecting suitable sites for tea nurseries. In view also of the experiments that were to be undertaken in Kumaun, a letter was addressed to Mr. G. W. Traill, Commissioner of that province, by Dr. Wallich, Officiating Secretary to the Tea Committee, dated 28th June, 1834, requesting him to render what assistance he could in order to carry into effect the object in question. In Mr. Traill the Government found an officer well qualified to undertake this tvork. He was assisted by Mr. R. Elinkworth, who was then at Almora acting as plant-collector under Dr. Wallich for the Calcutta Botanical Gar- den. Two sites were chosen for nurseries in which to sow the seeds that were shortly expected from China. They w r ere — Lackh- inesar near Almora and Bhartpur near Bhim Tab They are thus described by Mr. J. H. Batten, B.C.S., who was afterwards Commissioner of this province, 1 — “the former occupying three acres of old and easily acquired crown land on the north-west slope of the hill below the capital town at 5,000 feet above the sea, the latter occupying four acres at 4,500 feet above the sea in the near neigh- bourhood of the Bhim Tal lake, which is situated on the first step of the mountains above the Bliamauri Pass.” It was in this same year (1834) that through the energetic researches of Captain Jenkins and Lieutenant Charlton some specimens of the true tea plant of Asam were obtained, and thus confirmation was secured as to its being really wild in that country. The question of selecting sites gave rise to much discussion ; some, such as McClelland, Griffith, &c., be- ing in favour of restricting cultivation to Asam, or to countries with a similar climate, on the assumption that a damp and equable climate was necessary for its proper growth. As far as the Asam plant was concerned, this has been proved to be good advice, and results have shown that though the Asam tea plant is botanically the same species as that of China, 2 it is not sufficiently hardy to bear the extremes of temperature to which the Chinese variety is exposed in the tea gardens of North- 1 “ Notes and recollections of tea cultivation in Kumaun and Garlrwal, foyJ.H Batten, b.c.s., retired, Journal, Agri -Ilort. Society of India, Vol. V,, Fart IV., p. 5-3, 1878. 3 Sso F . Ind., i., p. 292. Sites. 89 2 HIMALAYAN DISTRICTS Western India. In China itself, where the area of tea cultivation extends over nearly twenty degrees of latitude, there must he many degrees of hardiness in the plants which are grown throughout this wide extent of country. Previous to the rediscovery of the tea-plant in Asam, the sites Tea-plant discovered recommended for cultivation in India had m Asam. reference solely to the Chinese plant, as far as was known about it at that time. In most cases these sites have proved successful so long as cultivation was restricted to the Chi- nese variety, or with hybrids only slightly crossed with that of Asam. The pure Asam plant, on the other hand, requires a hot and moist climate ; in fact the more unhealthy the locality may be from the above cause, the greater the chances of success. The discovery of the true tea-plant in Asam naturally gave rise to a considerable amount of partiality in favour of restricting the cultivation of tea entirely to that country or its neighbourhood ; and consequently attention was diverted from the more distant nurseries in Kumaun and Grarhwal. These nurseries, however, were in good hands, and, in spite of all drawbacks, the success of the experiments soon became evident. At this point, it will be advisable to confine attention to matters more immediately connected with the subject of this notice, viz., the progress of tea cultivation in Kumaun and Grarhwal. The first batch of plants numbering about 20,000 were despatch- Cultivation in Ku- ed from Calcutta in 1885, but very few of these arrived at their destinations alive ; and of the seeds sent to Dr. Falconer not one germinated, a fact not to be much wondered at, considering the length of the journey they had to undergo, and the short-lived nature of the seed. The plants flourished in the two Kumaun nurseries and produced abundant crops of seed. In the Saharanpur garden plants were also to be seen, the offspring of seed produced at Koth in T ihr i- Grarhwal . In 1841, Dr. Falconer, who was then in charge of all the tea plantations in Northern India, visited the two Kumaun gardens. At the Bhartpur nursery he found 1,344 plants. Of these, 291 were original plants introduced in 1885 ; 153 were seedlings of 1840, and the remainder were from layers made in this and the two preceding years. At Lachhmesar there were 3,840 plants ; viz., 250 of the original plants of 1835, 2,0 r 72 seedlings of 1839 and OF THE' NORTH-WESTERN PROVINCES. 893 1840, and the rest layers. The greater success of the latter garden he attributed partly to its better site, but in a great measure to Mr. Blinkworth, who happened to be residing in the neighbourhood. On the whole, he considered the results up to this time as most encouraging. Shortly after this he paid a visit to the Garhwal nurseries and reported similar progress. As far, therefore, as the plants were concerned, everything looked promising ; but nothing was known as to the quality of the leaves for the manufacture of good tea. At that time there was very little practical knowledge in India regarding the various processes of tea manufacture, and in order to avoid unfavourable opinions at the outset through the attempts of unskilled workmen, Dr. Falconer strongly recommended that two complete sets of Chinese tea manufacturers should be supplied for the nurseries fin Kumaun and Garhwal, especial care being taken that these men should be of the best descrip- tion. A small manufacturing establishment was accordingly sanction- . , , . ed by Government. Some men who were Chinese labour imported. J selected for this work by the Commissioner of Asam declined to go to Kumaun. Dr. Wallich, however, suc- ceeded in engaging the services of a party of Chinese artizans in Calcutta. These were accordingly sent up to Kumaun, together with a set of implements all under the charge of Mr. Milner, who happened to be on his way to Saharanpur to take up his duties there as Read Gardener. They arrived at their destination in April, 1842. The Chinamen, as soon as they saw the Kumaun tea bushes, all declared that it was the genuine China plant ; and, in their opinion, far superior to that of Asam. They recommended that the plants should be pruned down close to the ground, so as to encourage the production of a fine crop of young leaves in the suc- ceeding spring. They managed to make a small quantity of tea with the leaves of that year, a sample of which was taken to Eng- land by Dr. Falconer a few months afterwards. This sample was submitted to the celebrated tea-brokers Messrs. Ewart, Maccaughly, and Delafosse in London in September, 1843, and they reported as follows : — a The tea brought by Dr. Falconer as a specimen of the growth of the China plant in the Himalaya mountains resembles most nearly the description occasionally imported from China under 894 hima'layan districts the name of Oolong. This resemblance is observable in the appear- ance of the leaf before and after infusion. The colour of the liquor is also similar, being paler, and more of the straw colour than the general description of black tea. It is not so high flavoured as the fine Oolong tea, with which we have compared it, and it has been too highly burnt in the preparation, but it is of a delicate, fine flavour, and would command a ready sale here.” After the departure of Dr. Falconer, the Saliaranpur garden was _ T put under the charge of Dr. W. Jameson, whose energy and indomitable perseverance contributed mainly to the success of tea cultivation in Northern India. He was also an active witness of the progress of tea culti- vation from its experimental stage to the period when its profitable cultivation justified the Government in handing it over to private enterprise. A sample of probably the same tea as that of Dr. Fal- coner above referred to was sent by Dr. Jameson to the Calcutta Chamber of Commerce, where it was pronounced to be a tea of very good marketable value, and worth in London about 2s. 6d. per pound. Another portion of this sample sent to London was reported on by Messrs. Thomson of Mincing Lane, and pro- nounced to be of u the Oolong Souchong kind, fine-flavoured and strong. This is equal to the superior black tea generally sent as presents, and better, for the most part, than the China tea import- ed for mercantile purposes.” Dr. Jameson visited the Kumaun plantations in April, 1843, and found them in a very satisfactory state. The Chinamen were manufacturing a different kind of tea which appeared to be far superior in quality. Some samples of the above contained in sixteen small canisters were despatched in Au- gust to the India House. The flavour of this tea was somewhat spoilt by the wax-cloth in which the canisters were wrapped. In other respects, however, the reports were most satisfac- tory. The history of the progress of the various tea plantations in North-Western India from this period, i.e., 1844 . 1 ’ ’ from the year 1844 until a few years ago, when the last of the Govennnent gardens passed into private hands, is chiefly to be gathered from Dr. Jameson’s annual reports to Gov- ernment, some of which have been published in the Journal of the OF THE NORTH-WESTERN PROVINCES. 895 Agri-Horfcicultaral Society of India. 1 In his report, dated 28th February, 1844, he gives a full account of the Kumaun nurseries, their number and extent, as well as the number of plants contained in each ; he also enters into some particulars regarding the mode of manufacturing the tea. There were at this time five separate nurse- ries scattered over four districts ; their total area amounted to 55 acres, and they contained 4,306 tea-bearing plants. More land being required, new nurseries were marked out by Dr. Jameson, and some of the old ones were extended, making in all an addition of 66 acres. Dr. Jamesows intimate knowledge of geology enabled him to select these new sites with great advantage. The total quan- tity of tea manufactured in 1843 was 1911b. In discussing the future prospects of tea, Dr. Jameson clearly shows the success of the experiment so far, and urges the necessity of greatly extending the cultivation of tea in the provinces of Kumaun and Garhwal. He says : — “ The plants now amount to 150,000, and these will be doubled, I trust, or trebled annually ; and were there only seed in sufficient numbers, as they germinate most freely, provided they are fresh, the aspect of the nurseries in an infinitely short space of time would be changed ; for instead of patches there would soon be districts covered with tea plants * * * * * The nursery at Ivaulagir in the Dehra Dun contains about 4,500, and here the plants arejhriving as well as in any other of the nurseries. It is, however, to be proved whether the leaves yielded by the plants in this locality are fitted for making tea of a superior quality, as it has been ascertained that all the tea grown in China at low elevations is of an inferior description. If, however, it does prove to be a marketable article, and equal to that produced in the neighbourhood of Canton, avast field for enterprise will be opened up, whether Government consi- dered it worthy of their own attention, or it be brought about by private capital. Water carriage will soon, it is hoped, be within two or three marches of this valley, which will also be a strong inducement, in addition to the above, to make capital- ists invest their capital in this channel, and thus we trust ere long to see the hill provinces, which at present yield but a trifling sum to the revenues of the State, become as important, in an economical point of view, as any of those in the plains of Hindustan.” In a letter to Dr. Royle dated 1st July, 1844, Dr. Jameson after havino- made an inspection of all the nurseries writes : — “ At Koth, Rama Serai, and Gadoli in the Garhwal Hills, the tea plants are thriving admirably, many of them being nearly six feet high.” In 1 See Vol. II., p. 323; Yol. IV., p. 173; and Vol. VI., p. 81. For the first few years Dr. Jameson corresponded regularly with Dr. Royle, and the sub- stance of his letters is contained in a paper by the latter published in the Journal of the Agri.-Hort. Soc , Vol. VII. ; part II., p. 11. 89 6 hima'layan districts a later letter lie informs Dr. Royle that the Chinese manufacturers denied that gieen and black tea were made from different plants, and that it was only a difference in the mode of manufacture. In another letter he mentioned that 4361k. of tea had been made, and that three acres yielded 1621k. of tea ; that he had then 120 acres under cultivation, and hoped soon to have double this area. In Dr. Jameson’s next report, published in 1845, he gave a lg45 detailed account of the progress made during the preceding year at the several gardens in Kumaun and Garhwal. Seventy-six acres of land were added and 94,100 plants were put into them. In September and November upward of four lacs of seeds had been sown, of which 167,000 ger- minated and were still germinating. Three hundred and seventy- five pounds of tea were manufactured, showing an increase of 185 Ik. on the preceding year ; and as the plants were still young, Dr. Jameson was confident of a steadily increasing quantity per acre every year. In this report he entered into the subject of cost and profit, and shows by the following estimate the amount of profit that might be realized from 6,000 acres of tea, on the assumption that an acre was capable of yielding one maund of tea : — Rs. The expenses of cultivating 6,000 acres ... ... 87,000 Ditto of making the tea ... ... ... 39,975 Ditto of packing the tea ... ... ... 2,259 Land rent, carriage to Calcutta, &c. ... ... ... 36,500 Total ... 1,29,734 To value of 6,000 maunds of tea or 240,000 seers at Rs. 2 per seer ... ... ... ... .. 4,80 000 Or say that the tea sold at Re. 1-8 per seer ... „. 3,60,000 Expenditure ... ... ... ... ... 1,29,734 Balance ... ... ... ... ... 2,30,266 Re garding the Garhwal nurseries, Dr. Jameson reports that Garhwal that of Kaulagir in the Dehra Dun consist- ed of six acres and contained 8,000 plants. At Ivoth in the Bhaddri valley, elevation 5,000 feet, there were 729 plants ; and in the Rama Serai nursery, elevation about the same, 728 plants. About a quarter of the total number in the two latter nurseries were a portion of the plants which came originally from Calcutta. Another nursery at Gadoli near Paori, established by OF THE NORTH-WESTERN PROVINCES.. 897 Dr. Jameson in 1843, contained 5,000 plants. Shortly after this Dr. Jameson sent a sample of Dehra Dun tea to Dr. Royle for an opinion, which was favoured by Mr. R. Twining, who reported as follows : — “ I have carefully tasted your sample of Himalayan tea, and I really think it a promising specimen. The flavour is not strong, but it is delicate and pleasant, and a little, methought, of tha Orange Pekoe character. The complexion of the leaf is rather good, and pains seem to have been taken in the manipulation.” This favourable account was very gratifying to Dr. Jameson, who at once foresaw the profit that would result by extending tea cultivation throughout the Dun. Other samples were submitted through the Court of Directors for professional examination in London, and the reports, on the whole, were most satisfactory. Dr. Jameson receiv- ed about this time from the Court of Directors grateful acknowledg- ment for the good work already done by him. The sales of tea at Almora, two of which had lately been held, showed an increasing appreciation of Indian tea by natives as well as by Europeans. The average price offered for black tea was seven rupees per seer. In 1847, Dr. Jameson wrote to Dr. Royle : — “ The tea this year will, I think, be very superior to anything yet made, as it has been manufactured and packed under advantages which were not pro- curable until now ; that is, there is now a sheet-lead maker attached to the manufactory.” Another sale was held this year at Paori. The amount realized for green tea varied from Rs. 10-8-0 to Rs. 9-4-0, and black from Rs. 7-8-0 to Rs. 4 per seer. About this time, Dr. Jameson received orders to select sites for new plan- tations in the hilly districts between the Satlaj and the Ravi, which resulted in the establishment of the Kangra valley nur- series. Dr. Jameson’s third report 1 gives further details regarding the condition of the different nurseries. His Third report. . observations as to soil were to the effect that the tea plant thrives well both in stiff and free soils, but appa- rently better in the latter, or in a mixture of the two ; with regard to elevation, that it thrives equally well at heights ranging from 2,200 feet above the sea to 6,000 feet. The area under cultivation at this time was 162^ acres, and the minimum yield of tea per acre 1 J., Agri-IIor., Cal., VI., pt. ii. 113 898 HIMALAYAN DISTRICTS was 801b. It is also stated in this report that about half the quan- tity of the < ~ P ouchong ’ (black tea) was bought up by natives at an average price of Rs. 6-8-8 per seer. The coarse Boheci tea was sold to the Bhotiyas at from Rs. 2 to Rs. 2-4-0 per seer for export to Tibet, where it successfully competed with the tea imported to that country from China. Other interesting matters are discussed by Dr. Jameson in this report, but space will not permit to give more than the headings of these subjects : — 1. On the method of preparing ground prior to forming a plantation, viz., fencing, draining, ploughing, trenching, &c. 2. On seeds when ripe, the season of ripening, and the methods to be adopt- ed to ascertain it. 3. On the method of sowing seeds and season, and on the treatment of the young tea plants after they have germinated. 4. Method of rearing plantations, by sowing seeds, by layers, and by cut- tings. 5. On the method of transplanting, and the season. 6. On pruning, best season and mode. 7. On irrigation. 8. On the tea plant ; season of flowering ; its character and species ; and on the advantages to be derived from importing seeds from China. 9. Method and season for plucking and gathering leaves. 10. On the method of manufacturing black tea. 11. On the method of manufacturing green tea. 12. Packing tea. 13. Manufacture of sheet-lead. 14* Tea manufacture. 15. Implements required in manufacturing tea. In a letter to Dr. Royle, dated 25th January, 1849, Dr. Jame- son states that 2,6561b. of tea had been manufactured in the pre- vious season, of which 6001b. (black and green) had been sent to England, that there would be 400 acres under cultivation at Kau- lagir by the end of the season, and at Priori he expected to have 2-3,000 acres. One hundred thousand plants were sent to the Kangra valley, and he hoped in the course of eight or ten years to have a sufficient number of plants in the Kaulagir plantation to plant the whole of the Dun. Mr. Fortune. In 1848, the services of Mr. Robert Fortune, already well known as a horticulturist, were engaged by the Court of Directors to make an expedi- tion to the northern part of China in order to obtain plants of hardier varieties, as well as to investigate the mode of manufacture OF THE NORTH-WESTERN PROVINCES. 899 in that part of China. In all this he was completely successful. About 8,000 plants and several packets of seeds were despatched by him to India from localities celebrated for the good quality of their tea. He returned in 1851, bringing with him 12,000 more plants, together with a large quantity of seed in a germinating state. With these he proceeded at once to the Himalayan nurseries, which he after- wards inspected officially by request of Government. In his report on the condition of the nurseries he mentions eight as being at this time under Government control, viz., one in Hehra Dun, one in Garhwal, and six in K umaun. Their names are : — Kaulagir (Dehra Dun) : Gadoli (Garhwal) : Hawalbagh, Lachhmesar, Kapena, Anu, Kuasar, Bhartpur, and Rasiya (K umaun). Some remarks of his on each of the above may be briefly given here : — 1. Kaulagir plantation. — The soil is composed of clay, sand, and vegetable matter, on a gravelly subsoil of rocks similar to the surrounding mountains. The plants ap- peared less healthy than in good Chinese plantations owing (according to Mr. Fortune) to — (a) The flatness of the land : (5) , the system of irrigation: (c), too early plucking: (d), hot drying winds. 2. Gadoli . — Soil composed of loam, sand, and vegetable matter, very suitable for tea. Very like a Chinese plantation ; plants healthy and prospects good. 3. Hawalbagh. — Land undulating similar to Chinese tea coun- try ; soil a sandy loam mixed with vegetable matter ; land terraced and sloped. Terrace cultivation is not adopted in China. 4. Lachhmesar and Kapena. — Situation steep ; soil light and sandy, rarely irrigated ; plants in good order. 5. Bhim Tdl. — (a) Anu and Kuasar : land low and flat, area 46 acres ; bad situation : (b) Bhartpur : 4^- acres of terraced land ; soil, light loam mixed with clay, slate, and trap rock and a small amount of vegetable matter ; well adapted for tea : (c) Rasiya, 75 acres of sloping land, plants most healthy, which are not irrigated. 9 00 HIMALAYAN DISTRICTS Mr. Fortune also visited two plantations belonging to zamindars, the first called Lohba in Eastern Garhwal, 50 miles west of Almora, and at 5,000 feet altitude ; excellent land. In 1844, 4,000 plants from the Government plantations were put here, hut failed owing either to want of knowledge or intentional carelessness. The other plantation called Katyur was situated near Baijnath in Western Kumaun ; the ground was undulating ; there were numerous streams, and the soil was fertile. Captain (now General Sir H.) Bamsay^s two plantations each of four acres were planted in 1850. Good management produced good results. The labour and manure of the two neighbouring villages were secured in lieu of taxes. At the close of his report Mr. Fortune gives some advice on certain points connected with tea cultivation in this part of India : (.1) The land best suited for tea, he considered, should be undulating and well drained, and such as would produce good crops of mandua or wheat, moist but not stagnant. (2) Irrigation he declared to be generally injurious and should be resorted to only on emergen- cies. (3) Plucking in China was never carried on until the third or fourth year after planting, and was only necessary up to this time for forming good bushes ; sickly plants should not be plucked. (4) The most suitable climate was to be found in Eastern Garh- wal and Kumaon. At H&walbjigh, the thermometric readings showed a great similarity of climate with that of China. The rainy season in China is earlier, and the hottest time is in July and Au- gust, whereas in India the hottest month is June. In appendix B. the annual yield of manufactured tea for each garden (between 1848 and 1868-69) is given Outturn. & ' . as far as could be ascertained from scattered reports and office records. With the exception of the deductions from these figures, there is little to add regarding the later history of tea culture in these provinces beyond the general conclusion as to the ultimate success of the part which Government undertook with the able assistance of Er. Jameson in order to bring about the complete establishment of the tea trade in North-West India. As early as 1864 Dr. Jameson was of opinion that, owing to the increase of private enterprise and the production of seed in private gardens. Government would be justified in handing over the tea plantations to private capitalists. “ Government,” he says, “ has done its work OF THE NORTH-WESTERN PROVINCES. 901 in proving tliat tea can be profitably cultivated in North India. Seeds and seedlings . have been distributed and skilled workmen supplied to planters in various parts of India.” The extraordinary progress which occurred within a few years may be understood from the following facts : — In the year 1847, and up to 1859, tea cultiva- tion was confined entirely to Government plantations, the total area being 166 acres. In 1859 the land under tea in Delira Dun did not exceed 700 acres, and in Kumaon there was only one small private estate besides the Government plantations. In 1880 the area was as follows : — ■ Number of gardens. Area. Acres. Roods. Roles. Kumaun • • • 33 3,342 3 10 Garhwal • •• ... 10 634 3 O Dehra Dun • • • • • • 20 6,960 O O Total ... 63 10,937 2 10 On the occasion of the recent International Exhibition at Mel- Indian teas in the Aus- bourne the opportunity was taken of bringing traiian markets. to the notice of the Australian people the merits of Indian-grown teas. The undertaking was entirely success- ful, and the prospects of Indian tea-planters have thereby received a great impulse. They will now have abetter chance of satisfying a demand for Indian tea on its own merits, and the prejudice in favour of Chinese tea which went so far as to encourage the doubt- ful practice of selling Indian tea as that of China will undoubtedly lose ground. The planters in Asam and Bengal will be more directly benefited by these imports to Australia. For the teas of North-West India a market closer at hand is required. Efforts are now being made to renew and extend the Indian tea trade beyond the borders of the North-Western frontier where the demand is practically unlimited. Mr. J. B. Fuller in his report on the foreign trade of the North-Western Provinces and Oudh makes the following remarks as to the advantages of opening up a trade between Kumaun and Tibet : — “ So far as the commercial interests of these provinces are concerned, the most interesting point in the traffic they transact with Tibet is the opening it 902 HTMA'LAYAN DISTRICTS might afford for the inferior classes of Kumaun tea, which will not bear the cost of carriage to the sea-board. At present the markets of Tibet are closed by the uni- ted influence of the Chinese Government and the Tibetan Lamas, who, having the monopoly of the wholesale and retail tea supply of the country, are naturally averse to the competition of a traffic in Indian tea, which might be more diffi- cult to engross. The strict monopoly to which the tea trade between China and Tibet is subject is fully described in a recent report by Mr. Colbourn Baker, H. B. Al.’s Consul at Chung Cliing : his remarks, which specially relate to the prospects of a tea trade between Assam and Tibet, apply no less pertinently in the case of Kumaun, and the result of the system which he describes is that during the year under report not only was no tea exported to Tibet from these Provinces, but Chinese tea was actually imported into native Garhwal by the Nilang pass. ‘ Tea’, Mr. Baker writes, ‘is to the Tibetan more than a luxury : it is an absolute necessity.’ Yet the Tibetans on our frontier are compelled to pur- chase tea of atrocious quality, the price of which has been swelled by a long and difficult transport from the eastern extremity of the country; while immedi- ately across the frontier there are tea gardens whence they could be supplied with a better article, at a cheaper price, and with profit to the Kumaun tea- planters as well as to the itinerant traders (Bliotias) through whose hands it would pass. The price of brick tea per lb. on the Kumaun-Tibet frontier is not known with accuracy, but since Air. Baker shows that its price is increased from 4J annas to 8 annas per lb., by transport from Bathang to Lhassa, which is not one-third of the way, its price on the Kumaun frontier must be very con- siderable and much in excess of what Kumaun planters could supply it for. Were the trade opened therefore the Tibetans would get cheaper as well as far better tea than what they at present consume, which in the words of Air. Baker is ‘the merest refuse,’ consisting of little else than the twigs and brushwood of the tea plant, and vastly inferior to the very sweepings of Indian tea godowns. The tea-planting industry of Kumaun would benefit largely by the opening out of a trade, which would enable it to dispose of its coarser produce easily and cheaply. So heavily is Kumaun tea handicapped by the expense of transport to Calcutta that the most profitable portion of the trade even now is that transacted in green teas with merchants from Central Asia who purchase the tea at the fac- tory and carry it away themselves, saving the planters the expense and trouble of packing. Kumaun planters are well aware of the advantages which a trade with Tibet would give them, and a former manager of the Kousani Tea Company actually manufactured brick tea and endeavoured, but unsuccessfully, to get it into Tibet. Lastly, the Bhotias, in whose hands the Tibet trade lies, would derive great benefit from the substitution of a new article of commerce for borax, the price of which has fallen under American competition too low to afford substantial profits on its import.” The great success which has attended the cultivation of tea in Tea in Dehra Dun. Pehra Dlin ™ 8 hard b’ anticipated by Dr. Royle, who appeared to be decidedly in favour of a higher elevation. The locality which he recommended as being the most suitable for experiments in this district was a OF THE NORTH- WESTERN PROVINCES. 903 place called Jarrapani halfway between Raj pur and Mussoorie and about 5,000 feet above the sea. The flatness of the ground in the Dun however was probably the chief cause of its being rejected m the first instance ; for it had been observed that in China the finest tea plantations were situated for the most part on sloping ground. 1 Dr. Falconer, who succeeded Dr. Royle at Saharanpur, on finding that the tea plant would grow even at Saharanpur, was naturally led to a different conclusion, and it was at length decided to commence operations in the Dun. The first tea plants were introduced in 1842, and two years later the Kaulagir plantation was started under the superintendence of Dr. Jameson, who is still living to witness the successful results of his energy and perseverance. In 1847 this piece of ground covered about eight acres. The plantation was added to from time to time Kaulagir. until over 300 acres were under cultivation. It was visited in 1850 by Mr. Fortune, who was deputed by Govern- ment to inspect the tea plantations in India and to submit a report on their condition. The result of his visit led him to condemn the Dun as altogether unsuited for the cultivation of tea. The Kaula- gir plantation happened just at this time to be in an unsatisfactory condition, but for reasons depending on the mode of cultivation, and not, as time has shown, on account of any radical defect in the locality. At any rate the defects, such as they were, were soon remedied by Dr. Jameson, and the good prospects of tea cultiva- tion in the Dun were ensured. At a lecture given by Dr. Royle at the Royal Asiatic Society a letter from Captain Cautley was read in which he gave the following description of the Delira Dun plan- tations : — “ I saw the Government garden near Kaulagir, m which there were 4,000 plants growing most luxuriantly, the whole m full blossom. I believe that the whole of these, with the exception of a few brought from the hill plantations, are seedlings ; and certainly, as far as luxuriance of vegetation goes, I never saw anything so pro- mising in my life. There cannot be a doubt of the tea growing luxuriantly in all this part of the Dun.” Dr. Falconer was also present at this meeting and spoke strongly m favour of extending cultivation in the Delira Dun, not only on account of the suitable iMr. Fortune was no doubt similarly influenced when criticising the condi- tion of the plants at Kaulagir during his inspection tour m 1850. 904 HIMALAYAN DISTRICTS climate and soil, but also because of the large amount of cleared land that was available in that locality ; labour too, he maintained, was cheap as well as carriage. The yield of tea and seeds from Kaulagir plantation during the years 1861 to 1865 is given below : — 1861-62. 1862-63. 1863-64. 1 864-65. 1865-66. tv „ ( Green Tea \ Black • •• ft 1,756 14,982 ft. 1b. ft ft. Total • * • 1 6,737 18,915f 1 9,878 £ 25,078 36,202 Seeds • • • Mds. fc.60 Mds. 1,307 Mds. 860 Mds 1,050 Mds. 1000 Remarks •i Outturn lessened by severe drought. Ten acres added to planta- tion. Two acres added to plantation. This plantation after having remained for upwards of 23 years under Government management was sold in 1867 to the Itaja of Sirmor for two lacs of rupees. In 1868 the receipts amounted only to Rs. 1,401, but the garden now promises to become a valuable source of income to the purchaser. In 1866 the road over the Mohan pass was constructed and a much more direct route was thus established for the carriage of tea from the Duti. Shortly after the formation of the Government plantation _ 3 several other gardens were started in the Other gardens. . Dun, including Harbanswala and Arcadia, both now belonging to the Dehra Dun Tea Company, the largest and at the present time the most successful concern in the Dun. Many of the other gardens however failed, either from want of capital to start with, or because the managers were totally ignorant as to how the plant should be cultivated or the tea prepared. Sinee the year 1850 however the prospects of tea-cultivation have gone on improving and every year sees an increase in outturn and a finer quality of tea. In 1857 Dr. Jameson estimated regarding the tea- bearing capabilities of the Dun as follows : area 100,000 acres ; yield 10, 000,0001b ; average per acre 1001b Although the additional land hi ought uuder tea cultivation is annually considerable, it seems improbable that such a large area as calculated by Dr. Jameson will OF THE NORTH-WESTERN PROVINCES. 905 ever be utilized for this purpose. On the other hand his estimate of outturn per acre was far too small, as will be seen by some detailed statements which follow. In 1863-64 only 1,700 acres were under tea cultivation. The question as to the effect of canal irrigation on tea plants _ . , . seems to be finally disposed of. Fine Irrigation. J L healthy plants are now to be seen where formerly, when artificial irrigation was practised, the plants were sickly and sterile patches of soil were frequent. These patches were caused, it is supposed, by the excess of lime contained in the water ; the low temperature of the water no doubt contributed to bring about the injurious conditions as described above. Artificial irrigation has therefore been altogether given up by most of the tea-planters in the Dun, and a marked improvement in the healthiness of the plants has been taken place in consequence. Other causes have also combined to bring about better results. Greater attention for instance is being given to the advantages of manuring. Firewood, an equally indispensable article, is yearly becoming more scarce, and is likely to prove a cause of anxiety for the future. Until recently a large quantity of tea used to be bought up by merchants from Kabul and Central Asia, who took it away with them in their own bags. Tea of very average quality was thus sold at from 13 annas to one rupee per lb. The trade with Kabul will in all probability be renewed now that hostilities with that country have ceased. The quality of the Dun teas as regards flavour and aroma has a close resemblance to that of the other kinds produced on the Himalaya in Kumaon and Kangra. Two varieties of the plant are cultivated, vis., the China and a hybrid between it and the Asam plant, the latter being more closely related to the China than to the Asam variety. The Asam and Asam hybrid are found to be too delicate for cultivation in this part of India. There are at present twenty plantations in the Dun, making up a total area of 6,960 acres. The Dehra Dun Tea Company have lately introduced at their factories sets of rolling machinery which have proved to be a great saving of labour. The outturn of tea from the Dehra Dun Tea Company’s plantations in 1879 was 313,058 lb., an average tint is of 439 lb. per acre. The cost per acre amounted to Rs. 133-10-7. 114 906 HIMALAYAN DISTRICTS M M i— i P P p p CQ O l-H EH CO l—l EH Q fp oo •qo*ia ft. 5,388 «0 IQ 00 H *»eaqog; ft. 534 'qotqg • CO •& 00 rf-H iO co^ 1852. •■Baqog ft. 178 •^ia ft. 1,103 1851. •Eaqog ft. 132 • 000.10 • h* £ 2 •qon[a • o> fi 5 o VO oo "eaqog; ft. 247 •naoaQ ft. 385 •qo®ia ft. 58 o> 00 H "B3qoa . X* itS ^ * 000.10 & 2 r — 1 ■qonig ■■r> t'' - 3d to 1848. *08010 fi S3 *qoBig jO 3d co Name of plantation. ___ Kaolagir P *r— I R £h £ _ vc3 '“j HH H-t CO HI «p * 2 » 55 *£ a IT. ' 1 d H3 fldB: < ,rH 0 d c? P "* as 2«fi H'uPn oS m i — i « nT-° m N •vHH 50 ** S’-® oo *8^-9 a „ w . —• s ? fi. cs a; .’flifO C0 - io c „: w. ® T) © -T’S g « ' *. C3 03 Oi c3 bJD— ® CD GO +3 **— ' , gJ|.S "o sT' “5.5 -' O* q, O o . e Oa Oa • CO co CO *"• ■ oa VO ov to VO O 00 •e CO VO^ • to o oo t-H pH CO* CO VO CO N r-H £ r-H • • CO r-^ o QO c-H C-H r*4 to t— GH to e ! i c\ o. o ■ to vo Oi' •* • 00 r-H r— < r— « • to pH o (M to oa O vo £* « Oa^ CN to eo i—i to' uo CO &g CO § 4^ CO a cS cd n3 O d rO c5 *4 o3 a> H ^ ci ^ S' 'g t* 2 CD rj £ 5 o g rd t+4 a" | * a CD fH. » 03 . S'S H | §i n3 1,2 .s-g •g I § a flS o _ 05 2 © 2, 02 O 1 •>- a to ■s -§ a ^ 43 «3 Cj _!2 c3 . 2o5 ^3 g O 4J ^ QQ be of 2 d r e ^ r C +3 ^ rj CO nd “S^rd '3 Tx3 O m O 'o jd ^ 0> ^ a £^5 S H Q> „ S' as « “ u . a> **H >• o £ T3 rH a> • p4 tf: • H a> m. eS 0> ?-» o Q> n3 CD dl 4^» U2 Q> £ d 4JI ?-* o a Ol d o d c3 ft a> rd c8 ■73 CD +3 CD (D o3 >> ci 2 »73 d 03 ^4 04 <4 be a • H f-4 d M CD d 4-3 35 (D >a H 'rJ CD -d H 908 HIMALAYAN DISTRICTS Receipts and Expenditure of the Government plantations , 1862-1S6"9. I 1862-63. 1863-64. 1864-65. 1865-66. 1867 68. 1868-60. Rs. Rs. Rs. Rs. Rs. Rs. Receipts ... *1,11,006 1,04,387 82,180 7,275 • »o- Expenditure, 65,000 64,300 59,199 68,000 26,000 14,507 Balance 46,006 40,087 24,180 • M * This does not include credit for 700,^00 plants distributed gratis ; also seeds for which Rs. 14,060 might have been realized by selling to planters in Kangra. The records are too imperfect to give the full details for eacb year. Actual outturn of tea from plantations of Kumaon, Delira Dun, and Kangra Valley for tlie last ten years : — 1871 619,072 lb. 1872 • • • 741,769 99 1873 • •• 981,854 99 1874 • it 1,217,975 » 1875 • • • 1,289,532 99 Estimated crop for 1881 • •• 1876 Ml 1,535,300 lb. 1877 • •t 1,398,785 99 187 a • M 1,632,054 99 1879 Ml 1,800,000 99 1880 • •• 1,945,181 99 • •• • • • 1,868,900 99 uncertain. Distribution of Tea Seeds. From the Kumaon } Garhwdl and Dehra Diin Nurseries , 1860-67. 1860-61. 1861-62. 1862-63. 1863-64. 1864-65. 1865-66. 1866-67.. Mds. srs. Mds. srs. Mds. srs. Mds. srs. . Mds. srs. Mds. srs. Mds. srs. 2,220 0 No record found. 2,859 32 2,361 0 2,842 0 2,103 0 1,643 O The records for 1861-62 are not procurable. OF THE NORTH-WESTERN PROVINCES.- SOS'' The following references are to some works bearing on the Botany, Scientific) and Economic, of the Hiniiilayan districts of these provinces : — REFERENCES. Scientific Botant. 1. Hortus Indicus Malabaricus continens Regni Malabarici omnis generis- plantas variores, by W. Van Rheede Van Drakeustein and J. Casearium. Amsterdam, 1678-36. This work contains many plates with names in the Persian and Hindi characters. « 2. Herbarium Amboinense, by G. E. Rurnph, edited by Burmann. Amsterdam, 1741-5. The descriptions are in Latin and Dutch, and refer to many Indian plants. 3. Flora lndica, by N. J. Burmann. Amsterdam, 1768. It contains a number of good plates of rare Iniadn plants. 4. Indian Cyperaceae, by Professor Rottler. Copenhagen, 1773. 5. Flora Cochin- chinensis, by J. de Loureiro, ed. Willdenow. Berlin., 1793. 6. Plants of the coast of Coromandel, by Dr. W. Roxburgh. London, 1795- 1819. 7. Flora lndica: or description of Indian plants, by the same, edition Carey. Serampur, 1832. The same, edition C. B. Clarke. Calcutta, 1874; this is the edition referred to in the preceding pages. 8. Flora of British India, by J. D. Hooker and others. London, 1875-8.1. This work is constantly referred to in the preceding pages. 9. Genera plantarum ad exemplaria imprimis in Herbariis Kewensibus ser- vata definita, by G. Bentham and J. D. Hooker. London, 1862-67. Con- tains Rauunculacece-Cornacece. 10. Descriptions of the genera and species of plants of the order Labiatae, by G. Bentham. London, 1832-36. 11. Le jardin fruitier du Museum, ou iconographiedes toutesles especes et vari- etes d’arbres fruitiers cultives dans cet etablissement, par J. Decaisne. Paris, 1858-69. 12. Prodromus sive ennmeratio contracta ordinum, generum, specierumque plantarum hujusque cognitarum, by A. P. De Candolle. Paris, 1824-73. 13. Genera Plantarum secundum ordines naturales disposita, by Endlicher. Vindobonoe. 1836-40. Supplementa to the preceding. 1842-47. CnuipositEe India Cae, by C. B. Clarke, Calcutta, 1876, Commelynaceas and Cyrtandracc-ae by the same. Calcutta. Ferns. 14. The Ferns of Southern India, by Captain R. H. Bcddome. Madras, 1863-64. 15. Ferns of British India, being figures and descriptions of the ferns of Bri- tish India, exclusive of those figured in the preceding work, by the same. Madras, 1866-70. 16. Species Filicum: or description of the known ferns, by the same. London, 1846-64. 17. leones Filicum : or figures and descriptions of ferns, by the name and Gre- ville. London, 1831. Century of ferns and a second century of ferns, by the same. London, 1854-64. 9-10 HIMALAYAN DISTRICTS' 18. Filices Exotic® r or coloured figures and descriptions of exotic ferns, by the same. 1859. 19. Synopsis Filicum, by the same. London, 1868. 20. Genera Filicum: or illustrations of the ferns and other allied genera-, by F. Bauer and Sir W. J. Hooker. London, 1842. 21. Index Filicum: A.-Gon., by T; Moore. London, 1857-63. 22. Ferns, British and Exotic, by E. J. Lowe. London, 1872. 23. Natural history of new and rare ferns, being a supplement to the preceding-, by the same. London, 1868. Ferns of northern India, by C. B. Clarke. London, 1880. Mosses. 24. Musci exotici : containing, figures and descriptions of new or little known foreign mosses and other cryptogamic species, by W. J. Hooker. Lon- don, 1818-20. 25. Historia muscorum in qua 600 species describuntur cum appendice et indice synonymyormn, J. J. Dillenii. Edinburgh, 1811. 2 6 Synopsis muscorum frondosorum, by C. Muller. Berlin, 1849-51. Mosses of northern India, by Mitten. London. Lichens. 27. Introduction to Cryptogamic Botany,, by Revd. M. J. Berkeley. London,, 1857. 28. Selecta Fungorum carpologia, by L. R. and C. Tulasne. Paris, 1861-65. 29. Lichens : J. A. S. Ben., X. 828. 30. Systema Mycolagicum, sistens Fungorum genera et species, by Fries. Fun- dee, 1&21-28. Pines. 31. Synopsis Coniferarum, by Endlicher. St. Gall, 1847. 32. Pinetum : being a synopsis of all the coniferous plants as yet known, by G. Gordon. London, 1875. 33. Description of the genus Pious, illustrated with figures, directions as to, cultivation, and remarks on the several species of the family Conifer®, by R. K. Lambert. London, 1828-37. Others. 34. Melastomacearum in Museo Parisiensi monographic® descriptionis ten- tamen, by C. Naudin. Paris, 1849-53. 35. Rumphia sive commentatio botanic® imprimis de plantis Indite orientalis* by Blume. Leyden, 1836-48. 36. Flora orientalis sive enumeratio plantarum in oriente a Grcecia et ^Egypto ad Indi® fines observatarum. Basil, 1867-72, 37. Illustrations of the genus Carex (Cyperacece), by F. Boot. London, 1858- 67. 38. Orchids and how to grow them in India, by S. Jennings. London, 1875. 39. Genera and species of orchidaceous plants, by J. Lindley. London, 1830- 38. 30. Sertum orcliidaceum, by the same. London, 1838 . OF THE NORTH-WESTERN PROVINCES. 911 •41. -Flora Indica, being a systematic account of the plants of British India, by J. D. Hooker and T. Thomson. London, 1855. Though superseded by the ‘Flora of British India,’ this volume is valuable for its introduc- tion, giving a history of Indian Botany and the geographical distribu- tion of plants. 42. Exotic Flora : or figures and descriptions of new , rare or interesting exotic plants, by Sir W. J. Hooker. Edinburgh, 1823-27. 43. Historia naturalis Balmarum, by C. F. de Martius. Munich, 1823-50. 44. Balms of the British East Indies, by W. Griffith. Calcutta, 1 850. 45. Rhododendrons of the Sikkim-Hiinalaya, by J. D. Hooker. London, 1849-51. 46. Panjab plants, comprising botanical and vernacular names, and the uses of most of the trees, shrubs, and herbs of economical value, growing within the province ; intended as a hand-book for officers and residents in the Panjab, by J. L. Stewart, M.D. Lahore, 1869. 47. A catalogue of the plants of the Pan jab and Sindh, to which are added some others that from their present geographical proximity may be found hereafter to occur in the Panjab, by J. E. T. Aitchison, M.D. London, 1869. 48. Illustrations of the Botany and other branches of the Natural History of the Himalayan Mountains and of the Flora of Cashmere, by Dr. J. F. Royle. London, 1839-40. 49. Plantce Asiatic* Variores: or descriptions and figures of a select number of unpublished East India plants, by Dr. Wallich. London, 1830-32. 50. List of dried specimens of plants in the East India Company’s Museum, by the -same. (Calcutta? 1840-48). 61. leones Plantarum Indioe orientalis, by R. Wight. Madras, 1838-56. 52. Prodromus Florse Peninsula} Indise orientalis, by R. Wight and G. A. Walker-Arnott. London, 1834. 53. Illustrations of Indian Botany : or figures illustrative of each of the natural orders of Indian plants described in the preceding works, but not confined to them, by R. Wight. Madras, 1838-50. 54. Illustrations of Indian Botany, principally of the southern parts of the Peninsula, by R. Wight. Glasgow, 1831. 55. The Indian Botanical works of W. Griffith, arranged by J. MacClelland. London, 1848-54. Containing notes on, and plates of, many species. 56. A hand-book to the Indian Flora, by Major H. Drury. Travancore and Madras, 1864-69. Economic Botany. My main authorities on the economic botany of Kumaon are Madden, Stewart, and Brandis. Madden’s articles will be found in the Journal of the Asiatic Society of Bengal, XV., 79 (1845) ; XVI. j 226, 596 ; XVII. (I ), 349, and XVIII., 603. Also in the Journal of the Agri-Horticultural Society of Calcutta, IV. (184o) ; 223 : VII., 75, 129; and VIII., 99; and An. Mag. N. H. on Nepalese flora. Notes upon the pines of the N. W. Himalaya by Dr. Cleghorn. J. Agri-IIort. Cal., XIV. (1866). 912 HIMALAYAN DISTRICTS Report on the deodar forests of Basahir, by Drs. Brandis and Stewart and Cap- tain E. Wood. Calcutta, 1865. Keport on the food of the inhabitants of the district of Bijnor, by Dr. J. L. Stewart. Sel Bee., North-Western Provinces, XXXVIII., 25 ; II., N. S., 463. The same writer’s article on ‘ The Sub-Siwalik Tract, with especial reference to the Bijnor forest and its trees, and an account of their useful products,” appeared in the J. Agri-IIort., XIII., 265, in 1864. Statistics of Kumaon, p. 344, Agra, 1851, gives a list of the principal agricul- tural products based on Madden. The Garhwal Settlement Report, Allahabad, 1866, gives a similar list (app. 13) based on the same authority. Forests of Kuraaun. In. Rec. Supp., VIII. 5— -15. Records, North-Western Provinces, Pt. XVIII , 374. on the Bhabar and Tarai On the cultivation of Imphee, by N. A. Dalzell, J. R. A. S., XIX., 39. Forests. Timber trees, timber and fancy woods, as also the forests of India and of East- ern and Southern Asia, by E. Balfour. Madras, 1862. Collins’ Report on the caoutchouc of commerce. London, 1872. The useful plants of India, by Major H. Drury. Madras, 1858. English index of the plants of India, by H. Piddington. Calcutta, 1832. Cyclopcediaof India and of Eastern and Southern Asia, commercial, industrial, and scientific, by E. Balfour. Madras, 1873. The Forest Flora of North-West and Central India ; a hand-book of the indige- nous trees and shrubs of those countries, commenced by the late J L. Stewart, M.D., continued and completed by D. Brandis, l’li. D , London, 1874. By far the most valuable of all the preceding for its accuracy and its practical applicat : on of science to economic purposes. Report on insects destructive to woods and forest^, by R. Thompson. Sel. Rec., North-Western Provinces (2nd ser.), I., 377. On the seasoning of wood for practical purposes, by G. Paton. Ibid., V., 444. Experiments on the strength of Sal timber, by C. B Thornhill. Ibid., V., 454. Report on the present state of the Sub-tlimalayan forests below Kumaon and Garhwal (1861). by Major H. Ramsay, Gaz., Norik- Western Provinces , Suppt., December, 19th, 1861 and Webber’s forest survey. Report on the forests in the Bhagirathi Valley, by Major G. Pearson, Sel Rec., North-Western Provinces (2nd ser.), II., 117 ; III , 106. Report on the Sub-Himalayan forests of Kumaun and Garhwal, by the same. Ibid. ,11., 125. Report on the Deodar forests of Jaunsar-Bawar by the same. Ibid., II., 373 ; III., 129. Tobacco. Report on the production of tobacco in India, by J. E. O'Connor. Ca'cutta, 1873. This work gives a summary of all the information available up to the date of its publication. Synopsis of our knowledge of tobacco cultivation and manufacture, by P. Robinson, Cir. H. II. H of Board of Revenue, North-Western Provin- ces, dated 6th September, 1872. Contains anwers to some fifty -five questions, compiled from reports and works, a list of which is given. OF THE NORTH-WESTERN PROVINCES. 913 Papers regarding the tobacco monopoly in the Presidency of Fort St. George, and the proposed levy of a tax on tobacco in the other presidencies. Calcutta, 1870. Silk. Some account of Silk in India, especially of the various attempts to encourage and extend sericulture in that country, by J. Geoghegan. Calcutta. Annual Reports on sericulture in Dehra Dun in the Proceedings of Govern- ment, 1878-81. Notes on the Bombyeidse as at present known to us, by Captain T. Hutton, Suppi., Gaz. of India , for September 2nd, 1871. Cotton. Cotton : an account of its culture in the Bombay Presidency, by W. R. Cassels. Bombay, 1862. The Cotton Hand-book of Bengal, by J. G. Medlicott. Calcutta, 1862. This work gives from official sources a digest of all the information available on the subject of the production of cotton in these provinces to the date of its publication (pp. 166-217.) Parliamentary papers on * Cotton Cultivation in Bengal.’ 1857. Culture of cotton in India, by J. F. Royle. London, 1851. Review of measures for the improved cultivation of cotton in India, by the same. 1859. Cotton in India, by Dr, Forbes Watson. London, 1859. Experiments in cotton cultivation in the North-Western Provinces, Sel. Rec., North-Western Provinces, I. N S., 114. Ibid., III., S. S., 91. Thomason despatches, II., 38. Area and outturn of cotton crop, North-Western Provinces, 1869-70 — 1874-75, in Sel. Rec., North-Western Provinces, IV.-VI. Cotton in India, Cal. Rev., XXXVII., 1. Cotton soils, J., A. S., Ben., V., 314. Reports of the Cotton Commissioner with the Government of India. Reports of the Manchester Cotton Supply Association from 1858. Hand-book of the Cotton Trade, by Ellison. London, 1868. Administration of the East India Company, by Kaye. App. (c.), 689. Annual Reports of the Board of Revenue, North-Western Provinces, on the culture and outturn of cotton in these provinces. Notices of experiments in the Saharanpur Botanical Gardens. Reports passim. Cotton trade in India, J. R. A. S., XVII., 346. Cotton in Dharwar by Marshman. Ibid., XIX., 351. Fibres, &c. Fibrous plants of India fitted for cordage, clothing, and paper, with an account of the cultivation and preparation of flax, hemp, and their substitutes, by J. F. Royle, M.D. London, 1855. This valuable work gives a sum- mary of nearly all that was known up to its publication regarding the fibres of grasses, sedges, liliaceous plants, plantains, palms, flax, jute, hemp, and nettles. 115 914 HIMALAYAN DISTRICTS The cultivation and manufacture of flax in the North-Western Provinces, by Dr. Jameson. Sel. Rec., North-Western Provinces, Pt. XXXV., 4, and III., N. S., 332. Notes on the subject of paper-making in India, by W. S. Stiven, M.D. Sel. Rec., North-Western Provinces, III., N. S., 249. Report on the process of tanning observed in the Government tannery, Cawnpore. Ibid. (2nd ser.), III., 201. Note on the Chu-ma or grass-cloth plant of China. J. , Agri-Hort. Calcutta, VI., 219 ; VII. Part 1, 18 ; Part II., 36. Notice of the Rheeas or nettle-grasses and other textile fibres of Assam. Ibid., VII., Part I., 216 ; Part II., 62. Report on the trial of Greig’s machine for extracting Rheea-fibre at Saharanpur in 1872, by Lieutenant-Colonel Hyde. Calcutta, 1872. Report on the preparation and uses of Rheea-fibre, by Dr. J. Forbes Watson. London, 1875. Preliminary report of the Committee appointed by Government to test Rheea- fibre-extracting machines in the competitive trial held at Saharanpur in Septembr-October, 1879. Allahabad, 1879. Note, — The works marked, with an asterisk have been consulted by Mr. F. Duthie in his notice of Tea^cultivation in these provinces. Tea. Report on the tea-plant of Upper Assam, by W. Griffith. Calcutta, 1836. Account of Assam, by W. Robinson. Calcutta, 1841. Notes on the cultivation of tea in Assam by J. C. Marshman, J. R. A. S., XIX., 316. * Tea cultivation in Kumaon, by J. H. Batten, Ibid., X., n. a., 131, and J. Agri.- Hort., Col. V., Pt. IV. (1878). * Report on the culture and manufacture of Tea in Kumaon and Garhwal, by Dr. W. Jameson. Calcutta, 1843-46 (J., Agri -Hort., Ben., Vols. II. and IV.) * Report on the progress of the culture of the China Tea plant in the Himalayas from 1835 to 1847, by J. Forbes Royle. London, 1849. * Report on the Tea plantations in the North-Western Provinces, byR. Fortune. Agra, 1851 : and Sel. Rec., N.-W. P. (2nd ser.), V., 401. Journey to the Tea-countries of China, by the same. London, 1852. Suggestions for the importation of Tea-makers, implements, and seeds from China to the North-Western Provinces, by Dr. W. Jameson. Agra, 1852. Report showing the present condition and progress of the Government Tea plan- tations, by the same. Gaz., N - W. P., Suppt., 26th March, 1861. Government Tea plantations : the yield of the factories and the support given to private capitalists, by the same (1862). Sel. Rec., N.-W. P. (2nd ser.), V., 422. * See also the annual reports on the working of the Government Tea plantations : that for 1862-63 is given in Sel. Rec., N.-W. P., V. (2nd ser.), 430; for 1863-64 in Ibid., Pt. XLIII., 1 ; for 1864-65 in Ibid , Pt. XLIV., 1 ; for 1865-66 in Ibid., Pt. XLVI., 1; for 1866-67, Ibid., 82; for 1867-68 in Ibid., I., 1 ; for 1868-69 in Ibid., II., 433, &c. * Indian Agriculturist, passim. * Indian Tea Culture, by A. Burrell. J. Soc. Arts, xxv. (1877). * Kumaon Tea. Saunders’ Month. Mag., March, 1851, p. 389. OP THE NORTH-WESTERN PROVINCES. 915 * Tea Committee Reports, including letters from Wallich, Falconer and others, 1834-38. * Tropical Agriculture, by P. S. Simmonds, 1877. Drugs. Materia Indica, or articles employed by the Hindoos and others in medicine, arts, and agriculture, by Dr. Ainslie. London, 1826. The Bengal Dispensatory, chiefly compiled from the works of Roxburgh, Wallich, Ainslie, Wight, Arnott, Royle, Pereira, Bindley, Richard, and Fee, by W. B. O’Shaughnessy. Calcutta, 1842. The Pharmacopoeia of India, by E. J. Waring, M.D. London. 1868. Remarks on the uses of some of the bazaar medicines and common medical plants of India, by E. J. Waring. London, 1874. The Indigenous Drugs of India : or short descriptive notices of the medicines, both vegetable and mineral, in common use amongst the natives of India, by K. L. Dey. Calcutta, 1867. Supplement to the Pharmacopoeia of India, or a catalogue of Indian synonyms of the medicinal plants, products, inorganic and organic substances con- tained in that work, with explanatory and descriptive remarks, & c., in fourteen languages, by Moodeen Sherriff. Madras, 1869. APPENDIX A. 1. Table of rates according to which farmers of the forest dues in Kumaon were authorised to collect in 1847. Each cart-load of wood ... „ of sal logs ( lattas ) ... wooden sugar- mill cart-load of rafters ( Itaris ), „ of ebony ... „ of bambus pony-load of ditto ... head-load of ditto bhangy-load of ditto cart-load of bhdbar grass... pony-load ditto ... head-load ditto cart-load of tat reeds pony-load of ditto ... head-load of ditto cart-load of grass „ of munj bullock-load ditto ... head-load ditto • •0 gun of catcehu >» » 99 >9 ft It tt tt tt tt tt It tt tt it tt it it tt A. p. 6 0 8 0 8 0 8 0 4 0 6 0 0 6 0 3 1 0 6 0 0 6 0 3 6 0 0 6 0 3 6 0 4 0 0 6 0 3 8 0 A. p. Each cart-load of burnt lime HI 12 0 „ kunkur ,,, 6 0 pony-load of lime in 0 6 }> ass-load ditto Ml 0 3 >> pony-load of lac ■ . • 4 0 5) head-load of ditto in 2 0 >> pony-load of piparmor • • • 4 0 >5 head-load of ditto Ml 2 0 55 cart-load of charcoal ... 4 0 55 bhangy-load of baskets • •• 1 0 ditto of wooden utensils. 1 0 55 head-load of ditto III 0 6 >5 pony-load of ruina • • • 4 0 yy head-load of ditto • •• 2 0 Catechu furnaces. Rs. a. One in Kota 7 8 5 ) „ Chaubhainsi... • • • 4 0 yy „ Tallades • •• 2 8 yy „ Chhakhata ... 0«« 5 8 The grazing dues were three annas for each buffalo and one anna for each cow or bullock pasturing in the Bhabar during the year, with the following exemp- tions: — Calves of all kinds up to two years of age, all cattle actually employed in carriage, all cattle bond fide the property of a hill head-man possessing a lease, all cattle passing through and not stay'ng more than five days, all cattle belong- ing to the head-men of the Bhabar villages, and all belonging to cultivators actually residing in the Bhabar all the year round. 916 HIMALAYAN DISTRICTS APPENDIX A. 2. The following table shows the duties which the farmers were permitted to levy by Mr. Shore 1 in Delira Dun in 1826: — Table of duties levied in the Ddn forests in 1826. Article. Per 4 bullock cart = 20 maunds. Per 3 bullock cart = 15 maunds. Per 2 bullock cart = 10 maunds. Mule or buf- falo = 4 maunds. Bullock or pony = 3 OQ P r* cS s Hc« i—i II m 'd'g c3 H O P $ a Head-load = ri g d a -|C* Rs. a. P- Rs. a. p. Rs. a. P- Rs. a. p. A. p- A. p. A. p- Sisu, tun and ebony of 5 0 0 3 12 0 2 8 0 1 0 0 12 0 6 0 3 o any size. Each wooden sugar-mill, 0 12 0 0 12 0 0 12 0 • • • ... . • • .. • Bambus 0 6 0 0 4 6 0 3 0 0 1 0 0 9 0 6 0 3 Beam for sugar-mill ... 1 0 0 0 12 0 0 8 0 0 3 0 2 0 1 0 0 & Sal of any size 0 8 0 0 6 0 0 4 0 0 1 6 1 0 0 & 0 3 Eire-wood and timber 0 6 0 0 4 6 0 3 0 0 1 0 0 9 0 6 0 3 not expressly specified. Bdbar and munj grass 0 8 6 0 6 0 0 4 0 0 1 6 1 0 0 6 0 3 Ringals for hukka stems, 3 0 0 2 4 0 1 8 0 0 10 0 7 6 4 0 2 O A 'al reed for matting ... 1 4 0 0 15 0 0 10 0 0 4 0 3 0 1 6 0 9 Khat or catechu 5 10 0 4 3 0 2 13 0 1 2 0 14 0 7 0 3 & Lac ••• ••• 1 12 0 1 5 0 0 14 0 0 6 6 4 0 2 0 1 0 Lime ... ... 0 4 0 a 3 0 0 2 0 0 0 9 0 & 0 3 0 & Charcoal ... 0 8 0 0 6 0 0 4 0 0 1 6 1 0 0 6 0 . 3 APPENDIX A. 3. Revenue of each Forest Division, Year. Kumaon. Naini Tal. Ram- ie het. Garh- wal. Dehra Hun. Bhagi- rathi. Jaunsar Bawar. Rs. Rs. Rs. Rs. Rs. Rs. Rs. 1865-66 • •• 2,59,544 • •• • •• 2,48,305 40,431 ... 1866-67 1,60,369 » » t 2,28,357 43,729 ... 1867-68 • •• 1,78,459 ... • • 1,77,359 41,156 • •• 1868-69 • •• 1,72,601 . • • lit 1,88,733 40,333 . . . ... 1869-70 • •• 2,55,333 • • • 1,48,972 84,252 4,508 *•« 1870-71 • •• 1,05,601 ... ... 1,11,745 31,943 15,451 36,689* le7 L-72 1,10,152 1,295 1,30,380 90,819 5,36,924 1,28,891 1872-73 2,67,339 1,016 1,981 2,08,700 90,233 6,94,013 3,23,834 1873-7-1 » « • 3,65,687 1,346 3,292 1,53,796 78,270 4,66,591 6,12,336 1874-75 • • • 2,76,372 1,729 6,000 1,16,948 81,806 2,84,376 2,62,017 1875-76 • • • 2,97,334 5,124 15,697 2,00,946 67,521 1,00,480 2,22,247 1876-77 2,18,166 18,010 11,885 1,40,322 67,033 87,964 2,03,628 1877-78 • •• 1,79,364 15,285 12,073 1,73,348 77,221 1,21,129 2,07,098 1878-79 1,70,856 17,155 53,364 1,31,875 48,490 1 ,02,822 2,62,436 1879-80 ... 1,65,574 21,426 7,165 1,11,794 41,482 50,970 2,14,456 A 'uie. — In 1879-80 the Tons division was separated from Jaunsar-Bawar, and ior that year the adjusted accounts show Rs. 43,875 for Jaunsar-Bawar and R». 1,70,581 for the Tons division. 1 Mr. Shore to Commissioner, Kumaon, 16th September,. 1826, OF THE NORTH-WESTERN PROVINCES. 91 7 X I— I Q 55 W Ph a* <4 A O m > Q H c n W pq O W o H pq fe o w pH t3 H « fz; pq PM M W £ >» CO •t<> i~o .-O e K> -00 K) !3> S • *» © CO e £ CO rH GM 05 I> CO a fc^* iO JV- G'l in PP QQ CO t- 05 rH CO r-i CO ft pq in o CO to o? »> A 05 o •S fN •'Cj S'* o co G'l r-H » co in in co h b (M O CD si co CO t'- CO 05 CO xn o < CO pq • • • 9 m 5 : CO r— 1 iO ccf rfT ^ co r>' o CM^ 05 m & *■3 TJ4 X"- ^ 05 O 00 rH of rH H r-H (M r-4 •— i 00 "4* co co 05 O t— rH CO CO o CO 05 lOOlD in r-H in rt« • • • • • • o in Tt4 CO hN CO CO CO o CO r-H • H 43 pq pq ? • : CO CM co CO CO ^ CO 05 Til 4-3 r— i I-H r-H r— i r-H r— 1 r—4 r—4 o3 1-4 60 o3 & CM CO O m CO 05 o CM t- to s>* -4 05 co co Tf< r- ^ CO 05 r- rH • m • « • • Cl oo O o CO O 05 CO CO r-H CO PP <3 pq • t • • Jtf ocT 05 Gq O O 05 05 CO of TjT t- r— i 4f! r-H 1 — 1 CO co sq hi 00 rH Cl co Hi Hi CO rH o 00 05 o 05 __ in in HUO CO rH cs « CO 00 cm CO co in G^i 05 o o co CO CO r-H O (3 pq m *> o to 05 05 CO co co in co © HI in pq 00 00 cm CO T* CM 05 CO cf GQ T*< 05 GO" n o 6' Q o3 Ol CM G1 CM GM O'! r-H CM GN G^ ^ r-H Ol GM rH 05 05 CO f— 4 rH Tfl Tfi o CO rH CO CO 05 O m a? ft CO CM X- r— 4 X- O iO 05 G'l in co O 00 c 05 Tfl ■4* *n iC co CO Tfl m oo CO o pq CD CO r— O iO CM Tfi 05 O Ml rH iO r-H CO Ol £ pq r—4 o cm os' CM rH H*" 00 CO o O 05 rH Tf4 r—4 r—4 r—4 rH r-i r-H rH r-H rH rH O'! G'l rH S'* S'* x^ m CO O -4* GO o N O l>iO O o 1—4 CO CO o Cl 05 05 GO rH t— Ol oo m < GO GM t*4 r— 4 X^ CO o in t'OCO CO 05 oo o pq rH in o H< CO co CO CO Xrf iO hJI CO t> "Tfi CO 05 tji m iO Tfl T# Tfl IQ Tfl CO CO CO CO TJ4 o 05 05 rH rH rH CO rl © lr- O in m G'l co in 05 O pq QQ O in t- co CO O 05 05 +3 pq • • * • * CO* CO *~ © -i oo co s* o r-H r-H r-H »—4 rH 44 • rH d Hi 05 05 rH H tn W pq CO GN co G'l m O t- r—4 m 4 QQ o o\ iO o co CO Ol CO Tfi pq • • • »> *\ Hi « si s-*’ hi tV io GM CO CM Hl>OC0 HI lo 05 o o CO O r-H 05 CO rH Tfi CO H pq CO pq • • • • • • *• • • : 00 GN^ 1—4 o\ of in co Ol r-T iH d • 1-4 co CO CO G'l 05 co cn in o3 l> Tfi O CM co oi A DO pq • 1 : • • : : : H< m co co r-H CO CM n *\ CO r-H in' of rH r— ( CO gm tf 00 Hi CO ^ 05 CO HI © 00 CO CO t~- tH co 1—4 o H CO co ■vfi IO Ol r-H pq CQ CO f— 4 CO i — i —4 CO ^ co 00 r-H r—4 CO CO a pq CO to CO co' co*' r — 1 r-H iff icf co" N r~4 co co d GM O'* rH Cl Cl tM Gq Ol G^ GH rH 01 St S'* o3 a o ~ CO d r-i t~ r-H H* 00 r- \n H< — i O) H< io Tfi CO w CO CM to 00 X^ 05 CO iO ^ 05 »o in co co CO o o Tfl in rH GO 05 co m *> O in o < pq to CO* 05 X-f co Hi" of xf o’ co Tfi' i> cf CO 00 Tfl ■*tj4 o iO CO in in co ® io H< m r-H : CO r- co 05 O r—4 CM CO Ttl m CO 00 05 o Jh CO CO CO CO t- t- r- r- xr- X- 00 c3 in CO 00 05 o r-4 G'l CO Tfi in CO r- 00 C5 CO co co CO CO X- X- x^ r* 00 GO oo oo co 00 00 00 co 00 GO 00 00 CO 00 r-H r-H rH r—4 r-i rH r-H • rH rH r-H r-H rH r-H rH Ks. 68,318 (Ks. 66,282 A. and Ks. 2,036 B.) belongs to the latter. APPENDIX A. 5. Schedule of tolls on the export of minor forest produce in the Kumaun forest division. 318 hima'layan districts " 7 “ 0) bX +-> c: 2 v Vl 3 O o> p a, ► P H <3 x c co* t>r CO CM T3 c« © © O •v (M VO CO OQ CO •O T3 • p* s s 'o io"o§ XT'- 00 00 r* — • ^-i P. Oi co CO CO © 3 0 3 O o CO © o © © CO © •puai-peaq aaj c3 O o o © © o — o rH rH rH r-H 00 rH r— o CM CD tc O o c © © 0 0 0 © © © c © © © © © O. cc CO Oi © © to © to © © © © o 20 © © •ifqSuBq J8j c3 r-H © © © 0 2 0 _ r-r 01 CM _ CM © co CD a c © o © © 0 0 fl © o © © © © © © © &. CO CO 05 © © © © © © © © © © © © © ® Xaqnop jaj c8 r-* © © © © © CQ © CM rH CO CM CM CM © T* ^2 1) © C3 o

© CO o P5 o © o © © © © © o © © © © © © © © c3 co o © CO 03 o o © © o © © © © © o •oirjjnq jaj c3 Ol •-H rH rH O © © 00 CM 00 © Vi O rz oa C3 Qj •s a 5 cd .g S3 2 H ,Q cfl i— H H3 P c3 b0 p CD >■ c3 --s II JZ W Ij nd 4 ^> p c3 co co CO rp C3 CD Vl (U ca a tV 03 tn o go ^ 1 — 1 *3C •<<* © O Co "-'O' 03 r— O ci O C ■ * g 2^ • rH h- . O p rP P N N < < s*» »© <55 © S M CD a o c3 1 P 51 O 03 D % O. o ,-a u M f-» rl 01 z; H s I = a o fflddW ’°N OF THE NORTH-WESTERN PROVINCES 919 'lo. English and bota- nical or vernacu- lar names. Measurement. Royalty. Average annual export. * Its. a p- 18 Acacia Catechu Length up to 1 (t ' Per score 14 0 0 ' ( churan ) girth to 3u". 19 D). (mumla) ., 5' „ 30" t i 6 4 0 20 l)o. ( [balli ) ... Length as it may it 4 1 0 Scores. be 12". • 2,000 21 Do. ( musal ) Length up to 8' Per each 0 3 0 girth 8". 22 Dj. ( parts of carts) „ 14' 8" ... tt 0 1 0 23 Do. (ditto) „ 6' 10" ti 0 1 0 24 Large bedsteads Girth of legs, )) 0 12 0 made of sal, sisu, heads above 17" sandan. 25 Do. of other woods Ditto )> 0 5 0 26 Do. as 24 Girth of legs. Jl 0 8 0 heads up to 16" 27 Do. as 25 Ditto tt 0 3 0 28 Legs of bedsteads Girth of heads »> 0 2 0 as 24. above 17" Pieces. 29 Do. as 25 Ditto tt 0 0 9 4,800 30 Do. as 24 Girth of head up tt 0 1 0 to 16" 31 Do. as 25 Ditto *44 9t 0 0 6 32 Small bedsteads Length up to 7' 1) 0 1 6 as 24. girth to 10" S3 Do. as 25 Ditto ti 0 0 9 34 Do. as 24 Length up to 4' II 0 0 9 girth to 10" 35 Do. as 25 Ditto it 0 0 6 36 Boxes as 24 Length up to 3' ti 1 4 0 girth above 60" 37 Do. as 25 Ditto it 0 10 0 38 Do. as 24 „ girth 3 1" to 60" a 0 10 0 39 Do. as 25 Ditto 0 5 0 40 Do. as 24 ,, girth up to 30" 99 0 4 0 41 Do. as 25 Ditto 0 2 0 42 Bambus saraincha Per 100 12 0 0 37,800 scores. baliga. scores. 43 Kanderu ... 9 0 0 96,000 „ 44 Chhaneju and Ml »i 7 0 0 190,000 „ chhari. 45 Paina ... • •• 4 0 0 23,000 ,, 46 Balk ••• ••• Long up to 24 feet Each 0 0 6 3,000 „ 47 Dolt ... „ 25' or over. 0 1 0 2,000 „ 48 Bhabari Per 100 14 0 0 with 44. Bcores. 49 Chiralu'od for uten- (M Per head- O 4 0 • • • sils. load. 50 Large bambu box, Ml Each 0 1 0 « ) 61 Small ditto and • •• 0 0 6 [ Pieces. basket. , 16,000 52 Ditto basket • M 0 0 3 63 Sticks and fishing Ml 0 0 2 13,000 rods. D 54 65 66 67 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 76 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 100 101 102 103 104 105 j06 1 07 108 109 110 111 112 HIMALAYAN DISTRICTS Royalty. Each Rs. 0 a 0 P- 1 Per yard 0 0 3 Each 0 1 0 99 0 0 9 99 0 8 0 19 0 4 0 99 0 2 0 99 0 1 0 99 0 0 6 99 0 0 6 99 0 0 6 99 0 1 0 99 0 0 3 99 5 0 0 9l 1 12 0 99 1 4 0 99 0 4 0 99 0 1 6 99 0 1 0 19 0 0 9 99 0 0 9 99 0 0 6 99 0 0 3 99 0 0 3 99 0 0 1 99 0 0 3 99 0 2 0* 99 0 1 6 99 0 0 3 99 0 0 6 Per seer 0 0 3 99 0 0 1 >9 0 0 9 99 0 0 6 99 0 4 0 99 0 2 0 99 0 1 6 99 0 2 6 59 0 1 0 9> 1 10 0 »9 0 1 3 Per maund 9 0 0 » 1 4 0 99 1 0 0 99 0 8 0 >9 0 4 0 V 0 4 0 99 0 4 0 99 0 4 0 99 0 2 0 99 0 3 0 99 0 12 0 M 0 6 0 99 0 3 4 >9 10 0 0 59 1 4 0 99 0 8 6 99 0 12 0 ” 0 4 0 English and botanical or vernacular names. Scale plates .. ... ... Matting ( chatdi ) ... Box made of cane, large Do, small ... ... 8kin of Barasingha ••a Do. cow, buffalo, camel, large ... Do. do. deer, middling Do. do., small ... ... Do. sheep and goats ... Shoes Horns of stag, deer, &c.... Footstools (mora) Ropes of mdljan and boddla Each gold-washing sieve Cart wheels, large ... Ditto, small, Parts of carts Stools (pfra) ... Wooden platters and pots, large Ditto, small ... Ditto, large of B. malabaricum, Ditto, middle Ditto, small Wooden shoes Seal a beams, spoons, and sieves Nigali ( dewat and takhti) Spinning wheels Drums Native musical instruments ( dutara ), Gun stocks ... Various seeds dry and gums Diito green Ditto do. and resins, Ditto roots and fibres „. Bark of the pomegranate ... Powder of Malloius phillipinensis ... Various drugs • •• ••• Piper longum ... Piper Bubia, cordifolia , honey, &c. ... Banslochan ... Lac ... ... ... Catechu • •• • • • ••• Seeds of Prinsepia utilis ( tatuwa ) ... Dried root of Datisca cannabina ... Myrica sapida, khas-khas, and gum... Cinnamonum Tama la, &c. Wood/ordia Jloribunda, §•» 19 >1 99 99 99 99 19 99 99 99 99 >9 99 99 99 99 99 99 99 99 9> 99 99 99 99 >9 •OF THE NORTH-WESTERN PROVINCES. 921 Notes on the above list. Includes — (a) — BLbar, the grass of E. comosum , S. anguslifolius , and others referred to at p. 80S. £ b ) — Bind, the leaves of S. munja, used for thatching. (c) — Hindu, the leaves of other reeds used for the same purpose. (7 /) — Munj and sir hi, parts of S. munja . (e) — Tat, the culms of S.fuscum and C. laniger. (/) — Sink, the culms of Anatherium muricatum. а. Includes small reeds of the patera ( T. Elephantina ), the reeds of the motha { Gy per us tegetiformis ) and the leaves of the khajur ( Phoenix sylvestris ). 5. Includes the reeds of the nal-tura ( Phragnntes nepalensis'). б. Includes the leaves of th e sirdlu (Andropogon species') and bambu used for fodder. 43. See page 810. 67. These are ropes made from the mdlj an (Z? a uhinia Vahlii), page 793, and bodala ( Sterculia coloraia), page 792. 68. A royalty is levied on each sieve or rocker used by the gold- washers. 85. Under this head comes the following: — Dry aon la, the fruit of P. Emblica known asEmblie myrobalans, page 777. Dry haraira, the fruit of T. Chebula known as Chebulic myrobalans, page 779. Mocharas, the gum of the Bombax mala bar icum -(page 784) and Moringa pterygosperma (page 784), Mochkand, the root of Eclipta erecta , page 735. Roli-ki-dana, the seeds of Mallotas phillipinensis (page 776). $6. Under this head we have the green fruit of the aonla and haraira. Dry bahera , the fruit of T. belerica, known as Beleric myrobalans, page 777. Amalias, the pods of Cassia Jistula, page 779. Tulsi, the leaves of Ocimum sanctum , and the flowers of the dhdk or Butea frond&sa, page 77-8. 87. Under this eome; — The resin of the s&l (page 785) and the galls of Pistacia integerrima known as kakrastngi, page 746. 88. Under this head are included the following fruits, roots and fibres Green pipla, the fruit of Piper silvaticum, page 705. Kdla-j.ra, the fruit of Car uni Carui, page 705. Bildi-kund, the tubers of Pueraria tuberosa, page 748. The fibre of the pods of the cotton-tree, Bombax malabaricum , page 791. 91. Under this head we have the following: — Kadui. Kutki, plants of the genus Ophelia used for bitters, page 744-46. Bdlchar, root of Nardostachys Jatamansi , page 743. 93. Under this head the following are included : — Plplamor, the Piper silvaticum, page 705. Manjit-ka-jar, root of Rubia cor difolia, page 773. Rutti, seeds of Abrus precatorius, page 724, and sahut , honey. 116 922 HIMALAYAN DISTRICTS 94. Is the silicious secretion from the joints of the bambu, also known, as iaba- shir. 98. See page 742. 99. See pages 705. 100. See page 705 for C. Tamala. This head also includes : — Roots of various kinds exported as hand and Kinjora-ki-jar, the roots of the different species of Berberis , page 728. The seeds of Pliarbiiis Nil (f 'tdla-ddna ), page 745 ; and the roots of Hedy- chium spicatum ( k apu r-hachrif page 738. 201, This head includes the following : — Dhai-he-phul, the flowers of Woodfordia jloribunda , page 778, Chhalara oak-bark. Pahhan-bed, the root of Saxifraga ligulata, page 749. Nisot, the root of Ipomoea tiapethum, and the bark of Symplocos craiagioides ( lodk ), page 776. 102. Under this head come the following : — Tung> the bark of Rhus Cotinus, flowers and bark of Cedrela Toona, page 778. Nagarmotha, roots of Cypcrus juncifo/ius, page 774. Pit pdpra y seeds and leaves of Fumaria parviflora, page 737, fruit of Elceaguus umbellcita , page 736, and seeds of A. Catechu. 103. Includes Ritha, the seeds of Saplndus deter gens t page 749 ; Selkhari, a white clay and man jit. 104. Comprises giloi, the roots of Tinospora cordifolia, page 752, medicinal herbs of sorts and phindaru ( Colocasia himalensis ?) 105. Includes various mineral drugs. 107. Includes Rhus vernici/era, page 785, and makoi. APPENDIX A. 6. List of rates for the sale of timber at Rdmnagar and Moradabad Government Forest Depots. Name of timber. Measurement Class. Rate per cubic foot at Ranraagar. Morad- abad. Rs. a. p. Rs. a. p. Sal karis ... 12' X5"X4" I 1 5 0 1 8 0 Ditto • « » • • • Ditto ... II 0 15 6 12 0 Ditto « • • • • • Ditto ... III 0 6 0 »•! Ditto 10X5X4 I 1 5 0 1 7 O Ditto o • a • • » Ditto II 0 15 6 • M Ditto Ditto ... III 0 6 0 Ditto 13X6X5 I 1 6 0 • •• Ditto • if* ••• Ditto ... 11 1 0 0 ... Ditto 8X4X4 II 0 15 6 OF THE NORTH-WESTERN PROVINCES 923 List of rates for the sale of timber at Rdmnagar ancl Moradabad Government Forest Depots — (concluded). Name of timber. Measurement. Class. Rate per cubic foot at Ramnagar. Morad- abad. Sal karis. <•* ••• ••• 8X4X4 Ill Rs. a. 0 6 P- 0 Rs. a. p. • 44 Ditto >f« ••• i«i 6X4X4 II 0 14 0 • 44 Ditto ••• • •• Ditto III 0 4 0 Jaman karis ... 10X5X4 II 0 4 0 Ditto Ditto III 0 2 0 Haldu karis ... ... 12 X5X4 I 0 6 0 »4« Ditto mi u< Ditto ... II 0 4 0 Cliir karis ... Ditto ... I 0 8 0 » . « Ditto •«« mi Ditto ... II 0 6 0 • •4 Ditto »•« •• « ••• 10X5 X4 I 0 8 0 Du to m« ••• Ditto ... 11 0 6 0 •44 Sal sleeper ... ... ... 10' x 32" Ml 0 8 0 4*4 Sal karis Sal logs squared with axe if pur- 15 X 5 X 4 »(• II • •1 1 • •* 10 0 14 0 • 44 chased unselected from one end of the line five logs or over. Ditto ditto selected ill • • • 1 14 0 • • 4 Ditto round, class I., if purchased • as • •• 1 8 0 1 14 0 unselected from one end of the line 10 logs or over. Ditto ditto selected ... <«t *•4 1 12 0 2 0 0 Ditto round mixed class if pur- • • • 1 6 0 • 44 chased unselected from one end o£. the line 10 logs or over. Ditto ditto selected ... ... • •• 1 12 0 • 44 Ditto round, class II., if purchased • • 0 • •< I 4 0 • 44 unselected from one end of the line 10 logs or over. Ditto ditto selected ... Ml • 4 4 1 12 0 1 • • Sal kolhus selected M» 1 10 0 1 US © 9 INDEX I GENERAL. Page. Page. A. Bodos ... 22, 24, 27 , 28 Bodpas ... 23, 24, 31 , 38 A.bors ••• i 3 Gerbera lanuginosa ... 793 „ globosa ... ... 703 Girardinia heterophylla, 797, 798 „ pentaphylla ... 7 03 Gloriosa superba ... ... 738 quinata ... ... 703 Glycine Soja ... 696 sagittata ... ... 703 Gmelina arborea ... 738 versicolor, .. 703, 735 Goniopteris prolifernm ... 725 Diospyros Melanoxylon ... 735 Gossypium herbacenm ... 738 Dolichos bitiorus ... 696 Graminese, ... 485, 692 Lablab ... 696 Grewia asiatica. 738, 792 „ Binensis, 695, 735 ,, oppositifolia... ... 792 Grislea tomentosa ... 753 E. Gynandropsis pentaphylla, 732, 738 Eclipta erecta ... 735 H. Elcusme Corocana ... 690 „ indica ... 691 Hedychium spicatum, 738, 744 Elceagnus umbellata ... ... 736 Hedysarum tuberosum ... 748 INDEX. 933 Page. Page. Helicteres Isora, 722, 7 39 Luffa acutangula ... ... 7 ' >0 Ileliotropum brevifolium ... 739 „ aegyptiaca ... 700 HerpeStis Monniera ... ... 739 Hibiscus canccllatus ... ... 791 M. „ cannabinus, ... 7 -9, 791 „ esculentus ... ... 702 Macrotomia euchroma ... 744 „ ficulneus ... ... 791 Malachira capitata ... 882 „ pungens ... 791 Mallotus pliilipinensis, 74!, 776 „ sa.bdariffa ... ... 702 Malva rotundifolia ... ... 741 Hiptage Madablota ... ... 739 ,. sylvestris Mangifera indica, ... ... 741 Hoi arrhena. anti dysenterica ... 739 711, 74i Holcus Sorghum, ... 35, 692 Maoutia buy a ... ... 798 Hordeum iEgieeras 685 Maranta arundiuacea ... ... 704 „ hexasticlion, 682, 739 Mariscus cyperus ... 774 „ himalensis ... ... 685 Marsdenia Koy'ei ... 794 Humulus Lupulus ... 707 „ tenacissima ... 794 Hymenodicyton excelsum ... 739 Melia Azedarach ... 741 Hyoscyamus niger ... 739 „ indica ... 741 Memorial is pentandra ... 798 I. Memha viridis, 703, 741 Mimosa Catechu ... 815 Ichnocarpu8 frutescens ... 739 „ Pudica ... 741 Impatiens Balsa u ina .. ... 774 „ rubicaulis ... 741 Imperata arundiuacea ... 808 „ Sundra ... 8'5 Inga dulcis ... ... 789 Mirabilis Jalapa ... 741 Momordica Balsamina .. 701 J. „ charantia... 700, 742 „ dioica 701 Jasminum graudiflorum ... 740 Moringa pterygosperma 742, 784 Jatropha Curcas, 740, 744 Morus indica ... 742 Juglans regia, 716, 740 „ lcevigata ... 742 Juniper us alpina ... ... 842 „ serrata ... 742 ,, communis, ... 7S8, 842 Mucuna atropurpurea... ... 742 ,, excelsa, ... 788, 840, 843 ,, pruriens ... ... 7 2 „ nana . 842 Mukia scabrella ... ... 702 „ reeurva, ... 788, 842 Musa sapientum ... 742 ,, religiosa ... ... 842 Murdannia scapiflora ... ... 727 Justicia Adhatoda, ... 740, 776 Murraya Koenigii ... 705, 742 Myrica sapida, 742, 779 K. Myrsine africana, ... 736, 743 „ semiserrata ... ... 743 Kydia calycina, ... 740, 791 N. Nardostachys grandiflora ... 743 L. „ latamansi ... 743 Nasturtium officinale... ... 708 tactuca sativa ... ... 703 Nauclea cordifolia ... ... 816 Lagenaria vulgaris ... ... 700 ,, parvifolia ., ... 817 Lallemantia iberica ... ... 883 Nelumbium speciusum ... 743 Lathyrus Aphaca ... ... 694 Nephrol epis cordifolia ... 725 „ sativus ... ... 694 Nerium odor urn ... ... 743 „ sphcericus ... ... 694 Nicotiana rustica ... ... 755 Lauracese ... 705 „ Tabacum, ... 743, 755 Leguminosce ... 693, 694 Nima quassioides ... 746 Lepidium sativum, ... 702, 708, 740 Nyctanthes Arbor-tristis, 743, 748 Lilium Wallichianum ... 740 0 . Limetta ... ... 710 Limonia acidissima ... ... 740 Ocimum Basilicum ... 708 Limonum ... .., ... 710 Odina Wodier, 744, 782, 785, 792 Hineaceae ... ... ... 771 Olea glandulifcra ... 744 JLinum usitatissimum, 740 ; 771 Onosma echioides ... 744 934 INDEX. Pjge. Ophelia Chirayta ... ... 744 Pinus longifolia, 33 cordata ... ... 744 33 Massoniana 33 purpurascens ... ... 744 33 pend u' a 3 » speciosa ... 744 33 Peuce Oplismenus colonus ... 6J-9 33 Smithiana 33 frumentaceus ... 689 5) spectabilis Orthantera viminea ... ... 794 Oryza sativa ... ... 685 ()ugein.ia dalbergioides, 784, 815 Oxalis corniculata, ... 708, 744 P. Pandanus odoratissimus ... 756 Panicum brizoides ... ... 689 frumentaceum ... 6 C 9 italicuin ... ... 689 miliaceu’n ... ... 688 „ uliginosum ... ... 668 Paniceae, ... ... 685, 692 Papaver eomniferum, 704, 757 Papaveraceie ... ... 75 7 Papyrus Pangorei ••• ... 8' 8 Paraphyllant.hus urinaria ... 745 Parmelia Kamtschadalis, 745, 778 33 33 33 746. Piper longum „ silvaticum, Pistacia integerrima Pisum arvtnse „ sativum Pithecolobiuui bigeminum ,, saman Plantago decumbens ... „ Major Plumbago zeylanica .. Pceonia emodi Polygonacete Polygonatum verticillatum Polypodium Pongamia glabra Pontedcra vaginalis ... Populus ciliata Portulaca oleraeea, Page. 785, 824 ... 786 ... 829 ... 829 ... 884 ... 887 ... 731 705, 731 ... 746 ... 694 ... 694 ... 716 ... 8 8a ... 746 .. 746 ... 746 ... 745 ... 698 ... 745 ... 726 ... 746 ... 747 .. 747 708, 747 Paspalum Kora ... 688 Potentilla nepalensis ... ... 744 „ scrobiculatum ... 688 Premna integrifolia .. ... 747 Pedaliacece ... 771 « « mucronata ... 747 Penicillai ia spicata ... ... 690 Primula speciosa ... 747 Pennisetum italicu n ... ... 689 Prinsepia utilis ... 747 Pentaptera coriacea ... ... 8 1 5 Prosopis glan lulosa ... ... 882 „ crenulata ... 815 Prunus amygdalus ... 711 ,, tomentosa... ... 815 armeniaca ... 711 Perilla ocimoides ... 708 Avium ... ... 7 i 2 Peucedanum graveolens, 705, 745 >y Cerasus ... 712 Pharbitis Nil ... 745 33 can munis, ... 712, 747 Phaseolus aconitifolius ... 694 33 domestica, 712, 747 „ aureus ... 694 3 > Jacquemontii .. ... 7 1 2 ,, calcaratus ... ... 695 33 nepaleusis ... ... 712 „ coccineus ... ... 695 » padus, ... 712, 747 „ Max ... ... 695 33 persica, ... 712, 747 ,, multiflorus ... 695 3 Puddmn, ... 7 12, 747, 782 „ Mungo ... ... 694 ' 3 undulata ... ... 713 „ radiatus . . 695 Psidium Guyava ... 747 „ Boxburghii ... 695 Pterocarpus marsupium ... 784 „ torosus ... 695 Pueraria tuberosa ... 748 „ vulgaris ... ... 695 Punica gran at um ... 715, 748, 777 Phyllanthus embliea ... 745, 777 Putranjiva Boxburghii ... 7 48 „ Niruri ... ... 745 Pyrus baccata ... ... 713 Phytolacca acinosa ... 708 33 communis ... ... 713 Picea Morinda ... ... 834 33 Cydonia ... ... 748 ,, Webbiana ... ... 837 33 foliolosa ... 714 Picrorhiza Kurrua, ... 722, 746, 749 33 Kumauni ... 714 PL.us Brunoniana ... ... 836 33 lanata ... 713 „ C'embra ... ... 220 3 > malus ... 713 ,, Deodara, ... 746, 830 33 Pashia, . M 713, 714 ,, dumosa ... ... 836 33 vestita ... 714 ,, excelsa, ... 787, 829, 872 O ,, Gerard iana, ... 746, 788, 828 „ Khasyana ... 786 Quercus annulata ... 818 „ Khutrow ... 834 33 dilatata ... 818 INDEX. 935 Paye. Querciis floribunda ... 818 yj mcana, <-«• 748, 818 jj lanata ... 817 „ lanuginosa ... M 7 „ semecarpifolia ... 817 R. Randia dumetorum Ml ... 748 Raphanus sativus, • •• 702, 748 Remusatia capillifera ... 704 „ vivipara ... ... 704 Rheum ernodi, 748, 749 ,, Webbi annin • • • ... 748 Rhododendron campanulatum ... 749 Rhus succedanea . . . ... 785 „ vernicifera • •• ... 785 Ribes acuminatu n • •• ... 714 „ glaciale, 714, 715 „ grossularia ... ... 714 „ nigrum ... 714 ,, rubrum ••• ... 715 Ricinus communis, • •• 749, 77 i Royiea elegans • II .. 749 Rubia cordifolia, 1 •• 749, 7 73 ,, Manjistha • • • ... 774 „ tinctorum • . 1 ... 774 Rumex acetosa • « • 749 „ acutus BD- ... 749 „ vesicarius ... ... 708 S. Saccharum fuscum ... ... 807 Munja, • •• 806, 807 „ officinarum ... 4592 ,, Sara • M ... 807 „ spontaneum ... 807 Salix tetrasperma il. ... 749 Sterculia colorata, III 784, 792 ,, urens 751 , 780, 783 „ rillosa • •• ... 783 Stereospermum suaveolens ... 784 Stillingia sebifera ... ... 881 Streblus asper • «« ... 751 Swietenia febrifugia Ml ... 814 ,, Mahogani • • • ... 814 Symplocos cratcegioides, 751, 776 T. Terminalia coriacea ... Page. ... 816 „ crenulata .. ... 815 „ tomentosa ... 815 Tetranthera laurifolia ... 751 Thalictrum folioiosum ... 751 Thamnocabimus ... 810 „ Falconer i ... 810 ,, spathitlorus ... 810 Tinospora cordifolia ... ... 752 Toddulia aculeata ... 752 Trichosanthes anguina ... 700 ,, cucumerina 700, 752 „ dioica ... ... 699 „ palmata 699, 752 Trigonella Foenum-gr •• ... 687 Chiti-phil ... ... 739 Clial-kumhra • • • ... 700 Chita ... 746 Ohahnori ... • S > 708, 744 Chitra 746, 774 Chalpuri ... • • • ... 77S Chitta ... ... 759 Chalniya ... ... 747 Chiura 715, 772 Chama • ftf ... 685 Chiura-ka-pina ... 772 Chamara ... • •a ... 793 Chola ... 711 Chambu ... » • • ... 687 Chua 692, 697 Chanli sag ... 697 Chila- marsa ... 697 Chauiliya ... ... 797 Chuaru ... ... ... 7 1 1 Chan • »• ... 747 Chuchi ... 688. Ghana ... 693, 732 Chuka-palang ... ... 708 Chandan ... • •• 784, 816 Chuna ... ... 769 Ckandu ... • . . 757, 758, 769 Chupra ... 743 Chandra ... . . . ... 745 Chnral ... ... 694 Chang . . . ...31, 39 Churan ... ... 814 Changathasi dhup • a * ... 836 Churpunja ... ... ... 842 Chankan . . . l.< ... 702 Chyura ... 715 Chanwai . . . t.l 687, 688 Chyura-ka-pina ... 715 Chapa ... ... 694 Chapkiya ... ... ... 794 D. Chara ... ... 708 Charai ... 696, 708, 846 Dab ... 807 Charaa ... 760, 761, 771 Dabh ... 735, 807 Charila ... ... 778 Dain ... 770 Chaukandar ... ... 703 Dai ... 770 Charchubilu ... 778 Dakhang ... ... ... 711 Chaulai ... • •a 697-708 Dal 692, 694, 099 Chaumas ... ... 682, 690 Dala ... ... ... 814 Chauiliya ... • o o ... 747 Dalas ... 687 Cheharadar rupaiyia ... ... 279 Dalaya ... ... 684 Chhahki ... • • • ••• 700 Dal-bhat ... ... 693 Chhaneju ... ... ... 810 Dalchini ... ... ... 776 Chhatiyun... ... ... 726 Dao 21 Chhattak ... 680, 761, 762 Darchob ... 728, 774 Chhimi ... ... ... 695 Darhald ... 737, 774 Chhinkas ... • . . ... 808 Daritn 715, 748, 777 Chkota-alu ... ... 712 Darn ... 691, 768 Chichiya ... ... ... 842 Dasatta ... ... 810 Chichra ... 778 Daud-khani ... ... 684 Chick ... ... 686 Dawa ... ... 684 Chikan ... ... 695 Dek .,. ... 741 Clill • •• ... 829 Deodar 325, 320, 788, 830, 831. 833, 840, Chila ... • •• 687, 777 [867, 868, Chilghoza ... • •• ... 828 Deo-ningala ... ... 810 Chili-ragha .«• ... 837 Dhai 753, 778, 783 Chilla ... • o a ... 829 Dbak 18, 729 778, 779, 784, 789, 792 Chilians ... ... 759 Dhamaku ... 743, 755 Chilrao • •• ... 837 Dhamar ... ... ... 750 Chiln ... ... 829 Dhamin ... ... 792 Chimi ... 696 Dhan ... ... ... 687 Chimia-sawan ... 683 Dhanauriya ... ... 269 Chimul • •• ... 749 Dhaniya ... ... 705, 708, 733 China it* 678, 688 Dliao ... 780 Chindar • at ... 733 Dharla ... 778 Chipsa ... ... 24 Dhatela ... ... 747 Chir 746, 786, 787, 788, 824, 829 Dhatura ... 735 Chirara ... ... 747 Dhaula ... ... 753 Chirayta ... »•« ... 744 Dhauli ... ... ... 739 INDEX 939 ' Page . rage. Dhaura ... 778, 783 Gao-patta ... ».i ... 727 Dhauri • ■ • 780, 816 Gar-bijam ... ... 751 Dhawa Ml 782, 83 6 Gar-byush ... ... 749 Dhun III .. 268 Gargela ... 797 Dhup ... 788, 824, 843 Gar-pipal ... ... 747 Dliura ... 737 | ( arur • • • V 44 Dbusa ... 691 Gauzaban .. .. . ... 744 Diyar ... 830 Gawar ... 696 Do ihina ragha ... 837 G chan ... 684 Doja ... 279 Gehun, safed . . . ... 684 Dol chilla ... • •V ... 829 Geli ... 775 Dolu tm * ... 748 Genda ... ... ... 778 Dom-ningala III ... 810 Genthi ... 703, 735 Donas ... 846 Ghesuwa ... • •• ... 752 Dongole ... 714 Ghi ... 698 Dua ... 708 771 Ghikar ... ... 846 Dual’s 99 Ghikawar .. ... ... 726 Dudhi 726, 739, 753 Ghiwain ... ... ... 736 Dudhiya ... 725 Ghiwala ... 730 Dudhiya-mohura ... 745 Ghiya-tori ... ... ... 700 Dun 85, 99, 118 Ghiya-taroi in ... 700 Dungshing... ... 839 Ghor-rai ... ... 769 Durbui Ml ... 714 Ghuiya ... ... 703 Ghwiya ... 703 F. Gilas m .. 712 Giloi ... • «« ... 752 Filfil-bari ... *•0 ... 753 Gobara ... ... 727 Findora ... ... 740 Gobi ... 707 Gobli ... 737 G. Gobriya-salla ... ... 839 Gochni 680, 684 G ada-purna • • • ... 729 Gogiya ... 731 Gaderi • • • ... 704 Gojai ... ... 684 Gaduwa • • • 701 734 Gol ... ... 810 Gtihut ••• • • • 678, 690, 696 Gol-kaddu... ... 700 Gair »•* ... ’744 Gol-kankra ... ... 701 Gajar Ml 703, 735 Goncha ... 742 Gaji • • • ... 799 Gor-ningala ... 810 Gajir 703, 735 Gorp-jiba ... ... 728 Gaj-pipali ... ... 750 Gosarn ... 812, 814 GcijrJi mi • . , ... 733 Guba ... ... 704 Galdara ... Ml 711, 714 Gugal ... i«« 842 Galdu ... • . • ... 744 Guiya ... 679 Galion ... 714 Guiancha ... ... 752 Gallu • • • ... 775 Gular ... ... 737 Galtigal ... • •• ... 788 Gul-bansa ... ... 741 Gan • •• 290 Gul-i-gau-zaban ... 744 Gandra III 688, 692 Gul-kand ... ... 731, 757 Ganara-bhanga ... 799 Gulu ... 783 GclLlMl’i »•« • • • ... 688 Gumbhar ... • • • ... 787 Gandar III ... 808 Gun ... ... 703 Gandela ... 705 Gonchi ... • •• 724 Gandla Ill 705, 742 Gundi ... ... 705 Ganguli ... ... ... 809 Gur ... 756, 768 Gani ... Ill 705 742 Gural ... • •• ... 793 Ganja • . » 760, 761, 762 Guransh ... i*. ... 695 Ganjakini ... • •I ... 767 Guraush ... 69f> Ganjira III ... 703 Gur-bach ... ... '725 Ganna Ml ... 692 GGr-bhanga 760, 799 Gansam ... III ... 814 Gurial ... 779 G anth-baharangi ... 732 Guter • • * ... 779 940 INDEX Page. Page, Gwala-kakri • * • ... 702 Jangli palak ••ft ... 749 Gwala-mehal • •• ... 713 Jao • •« ... 277 Jariya • ft • ... 770 H. Jarkund-alu ... 798 Jasha • «« 807 Hakim ... • •• ... 723 Jau ... ■ • • 684, 739 Halang 702, 708, 740 Jaula ... ... 687 Haldi ... ... 706,734,774 Jaundela ... ... 772 Haldu ... 83, 812, 816 Jao sag ... 696 Halim CIO 702, 708 ,, ivikiyati ... ... 692 Haliyun ... • •• ... 727 Jek ... ... 7H Haltyu ... « • • ... 687 Jesu ... ... ... 759 Har ... 751, 777, 778, 779, 780, 816 Jhangora . . . • •• ... 689 Haraira ... • •e ... 779 Jhangra ... ... 805 Harara • • • 777, 816 Jhanj • •• ... 270 Harital ... • • • ... 291 J hanj haniya-kur i ... ... 694 Harsinghar • •• 743, 778 Jhansh ... ... 807 Hashish • • • ... 767 Jhao ... ... ... 727 Hathiya ... »•• ... 257 Jhatela ... ... 747 Hath-ungliya ... 750 Jhil ... ... ... 81 Hindwana... • •• ... 701 Jhingan • • • ... 782 Hukka • • • 754, 756 Jhonka-phal .• « ... 739 Hulas-Kashmiri • • • ... 749 Jhora • • • ... 842 Huliya-suliya ••• ... 714 Jliula ... ... 808 Jhumro . . • ... 810 I. Jhungara ... ... .. 689 Jhungra ... 810 Ikh • •• ... 692 Jiban ... 744, 782, 792 Ilaichi ... • • • ... 707 Jingan *•* 744, 792 Ind ... 1 1 • ... 772 Jintiana • •• ... 749 Indrayan ... 699, 701, 732, 752 Jira ... 705. 734 Inguwa • •• ... 728 Jirrag ... ... 708 Ishagol • • • 746 Joar ... 690, 692 Iskil ... • • • ... 752 Joga ... ... 758 Iskulikandriyun • • • ... 726 Jonkhmari... ... ... 726 Itola ... 731, 799 J unal a ... ... 687 Junali ... • * » ... 692 J. J usher • * . ... 684 Juti . . . ... 748 Jadiya ... • •ft ... 770 Jwaran-tika »•• ... 753 Jager • •• ... 805 Jahi ... • •• ... 740 K. Jai ... • •• ... 692 Jaint ... • • • ... 750 Kachlora ... . . . ... 746 Jainghani ... ... 726 Kachnal . . . ... 793 Jaiphal-jari • • • ... 798 Kachnar • •• 728, 779, 782 Jald-aru • • • ... 711 Kachra ... »•• ... 701 Jal-kuira ... < • • ... 747 Kachu ... ... ... 733 Jal-nim • • • ... 739 Kachur • • . 696, 706 Jalposhi ,. • • • ... 297 Kachur-kachri ■ » • ... 774 Jamana , M • • • ... 712 Kachur-kachu • . • ... 738 Jamira ... • • • 710, 732 Kaddu »• • ... 701 Jamuwa ... • • t ... 736 Kaddu, safed • • • ... 702 Janeo ... * • • ... 807 Kaghazi • ■ • ... 710 Janghora ... • •ft ... 678 „ akhrot ... 716 Jangli-bhanga • • • ... 799 Kagoha ... ... 737 „ chachinda »• • ... 700 Kagshi ... 793 ,, dalchini • • • ... 705 Kahu ... 703 „ harhar • •* ... 732 Kail ... 829, 834 „ jamalgota • •tt ... 728 Kaim - 817 „ mandira ... ... 689 j Kaiphal ... 742, 779 INDEX, 941 Kait • •• Puge. | ... 783 j Karsliu m Pag e. ... 817 Kakra * • ... 746 Karwi • •• ... 746 „ smgi • •• ... 746 Kas ... 726, 808 Kakri • • * ... 70 1 ! Kasa ... ... 694 Kakura t «t ... 701 Ivasli ... 807 Kala bausa ... »« i ... 728 Kashmal ... ... 728 ,. b. injar . ... 692 Katang-lcari ... ... 750 ,, ijran ... • • • ... 692 Katera ii. 7 33 ,, jira ... 731 Kath 725, 7G9, 775, 815 „ kaliya • • • ... 714 Rath a ... ... ... 775 Kalath « •• ... 696 Kathal ... ... 727 Kalijiri ... 763 Kathal-parhar ... ... 738 Kali-sarson • •• 729, 770 Kath-bans ... ... 845, 850 ,, taroi ... • • • ... 700 Katli-bel ••• 7 3G, 783, 789 „ tori • • • ... 700 Kath-bhilawa • • • 779, 782 ,, tulsi ... • • • ... 708 Katil ... ... 692 Kalon ... ... 694 Katira • . • ... 783 Kalra ... 798 Kato ... ... 23 Kalucliilu ... ... ... 831 Kauj ... ... 752 Kamarkas ... . . . 782, 784 Kauni *•* ... 689 Kamela ... - ... 776 Kaunik ... ... 684 Kamera ... ... 766 Kaunla . . . ... 710 Kan ... 690 Kauri . . • 696, 749 Kana • • • 688, 733 Kawara ... ... 696 Kanak . . • ... 684 Kedari-chfia Ml ... 697 Kandai ... ... 737 Kela ... IM ... 742 Ivandala ... 692 Kelon • it ... 830 Kand-alu ... ... 798 Kelu ... ... 830 Kandar ... 813 Ketnu ... ... ... 742 Kanda-tela .. • • • ... 806 Keoli • • . ... 733 Kanderi-ki-bel ... ... 701 Keora • •• ... 756 Kandre ... 834 Keyu ... ... ... 733 Kandura ... ... 808 Khadir . . • 63 Ivanerwa ... ... 810 Kb aila ... . . . ... 806 Kangai 724, 817 Khailuwa ... ... ... 806 Kangnaliya ... - 729 Khain ... ... 782 Kangni • • • ... 689 Khair ... 83, 725, 769, 775 , 782, 815 Kangur ... • •• ... 808 Khairuwa ... . . . 727, 737 ... 779 Kanika ... 687 Khairwal ... ... Kanji ... 741 Khala • 4. ... 686 Kan jura ... ... 733 Khalis ... ... 779 Kaniyur ... ... j 43 Khar an ji ... • •• ... 782 Kankol i. • ... 736 Kharbuz ... ... ... 701 Kanmar ... • • • ... 749 Kharif . . • ... 682 Kanmu ... • •• ... 733 Khariya • « « ... 684 Kansa ... 294 Kharot * . • 716, 740 Kantela . . . ... 727 Kharpat ... ... ... 779 Kanthi-rikhu • •• ... 692 Khas • •• 726, 808 Kariwal 733, 743 Khash-khash ... 704 Kaniyura ... ... ... 686 Khatauniya • * • ... 270 Kapas ... • •• ... 738 Khatla ... • •• ... 686 Kapasi • •• ... 716 Khetiya . . . ... 770 Kapasiya ... ... 791, 793 Khijri 680, 687, 689, 693 Kapur-kachri ... 738, 774 Khil Ml ... 692 Karan-phal • • • ... 710 Khir • . • 686, 687 Karaunj ... »•« ... 730 Khira ... ... 701 Karchilla ... ... ... 829 Khirai ... 701 Karel a ... • • • 700, 742 Khorasani-aj wai n • •• ... 739 Karhar ... ... ... 748 Khuskhab ... ... 689 Karka • •a ... 806 Khwairal ... ... ... 728 Kaiola ... ... ... 700 Kikra ... 705 942 INDEX Page. Page. Kilik • ti ... ... 807 L. Kilonj • • • • •• ... 8:8 Kimam * . « 758, 759 Ladaki ... ■ • • ... 7 i 0 Kingora-ki-jar 728, 774 Ladu • •• ... 772 Kino • •• ... 784 Laduri Ml ... 778 Kipaliya Kirkiriya • • • • II ... 713 Lahauri-doba ... 873 • • • • • . 705, 776 Laliota laita . . • . 770 Kirmali ... Ml ... 818 Lahsan 707, 726 Kisara • • • ... ... 694 Lai • • • ... 770 Kitola • . • • •• 731, 779 Lajawanti ... . • • • ... 741 Kitvvali • •• ... 779, 782 Lakh III ... 789 Kiu Ml . •• ... 834 Laksha 1 • • ... 789 Kiwara • •• ... 730 Lal-gehun ... • « • ... 684 Kiyera • •• • *• ... 778 Lal-jari ... • . . ... 744 Koda • • • • •• ... 7?3 Lil-niirclia... • •• ... 705 Kodo • • • Ml ... 690 Lamshing ... • M ... 820 Koish • • • ... 776 Langar • • k ... 16 Kolain • • • • • • ... 824 Lassa • • . ... 785 Ivolan • •• • •• ... 824 Lathi • •• ... 810 Kolon • • • . • . 785, 824 Lathichur ... • M ... 810 Kolu • •• • • • 770, 771 -i . a 1 1 k a ... • •• 700, 702 Kondha • • • III ... 702 Leauri ... ... 840 Koni • •• 678, 689 Lchtiya ■ • • ... 751 Koranga * • • ... 687 Lepcha ... ... 714 Kosam • • • • •• ... 814 Lobiya 693, 695, 709, 735 Knthla t • • • • • ... 799 Lod Mi 761, 776 Kotu III • •• ... 698 Lodh ... n 751, 776 Knar • •• ... 739 Lhala • • • ... 842 Kuda III ... 739 Lha-lhaka .. Ml ... 293 Kudaliya ... • •• ... 735 Lhali-lhaka Ml ... 293 Kudram Ml ... 834 Lira • • • ... 829 Kiier Ml ... ... 739 Lisha • •• ... 785 K akni • •• ). • ... 689 Luet • •1 ... 843 Kukri • • • • • • ...25,27 Luhuriya ... III ... 746 Kukuliya I •• ... ... 714 Lunak ... III ... 708 Ivul . . . ... 2 Luniya kulfah • •• ... 747 Kulai • •• • • • ... 694 Luet Ml ... 775 Kuli Ml • • • ... 750 M. Kut-shirm • « ... 733 Kulu • •• • • • ... 750 Madak 757, 758, 759 Kulthi • •• .. 696 Madar 730, 780, 788, 794 Kumbh • •• • •1 ... 782 Madkakari • • • ... 710 Kumbhar ... Ml ... 738 Magiya Ml ... 703 Kumbhi • • • • • • 730, 794 Maha-nibu ., M ' ... 710 Kumbi ... ... ... 783 Maharanga • •• ... 744 Kumhra • . Ml 702, 728 Mahua ... • . • 768, 7 72 Kunch ... • • • ... 776 Ma.hur • •a ... 725 Kunda • »l • . 1 ... 752 Mahur-bikh • • • ... 745 Kundri Ml Ml ... 752 Mainphal ... Ml ... 748 Kura ... lV1 ... 739 Majethi • •• 749, 773 Kuri . . • ... 743 Majna ... • • I ... 688 Kursani • • • . . . 705, 730 Majni III ... 688 Kuru . • • ... 737, 783 Makara-rai • •• ... 769 Kuruwa >•« ... 746 Makattar ... • •• ... 768 Kusha » • • ... 807 Malingo ... ... .... 810 Kushiala • •• • • • 715, 748 M:iljau • •• ... 793 Kushm-aru Ml ... 711 Malu • • • 679, 793 Kutala 1 «• ... 686, 691 Manura • M ... 751 Kutino I • • ... 810 Mamri f • •0 ... 783 Kutki ... 737, 746 Maua III 678, 805 Kyari ... ... 687 Mandavi ... • •1 ... 691 INDEX 943 Page. | Page • Mandin ... ... 691 1 Munja . • • ... 806 Mandira ... • •• ... 689 1 Muriya ... 779, 782 Mandua 678, 686, 690, 691, 768 Murkula ... • •• ... 794 Mangle ... Ml* ... 714 Musal ... 687, 688 Man iit ... 21, 773 Musali .. 729 Many ill ... ... ... 748 Musli-siyah ... 727, 734 Maii • • • ... 99 Maror-phal • •• ... 739 N. Marusthali... • • • 79 Maruwa ... t ». ... 690 Nagarmotha ... ... 774 Mash ... • • • 693, 695 Nak ... 713 Masha ... 277 Naka ... ... 687 Masur ... 686, 693, 694 Nakshatra ... . . . ... 257 chana • •• .. 694 Nal ... ... 806 Masuri ... 6.; 4 Nala , 296 MilttSi ••• ... 793 Nali * • • ... 687 M attar • • * ... 694 Nal-tura ... ... 806 Mmils, • •• ... 730 Kaluga ... 691 Mauli • •• ... 714 Naphal ... 684 Maulvi ... 34 Naspati ... 713 Maund ... ... .. 268 Nasbphal ... 715, 748, 777 Maura ... • t • ... 746 Nat • • • ... 691 M lura-bikh • • • ... 725 Nauabad ... 850 Maur-bikh ... ■ • • ... 745 Nauka in ... 747 Miya • • • .. 684 Neja ... 807 Meda-lakri » • • ... 751 Nepari ... . • . ... 735 Mehal ... • • • ... 713 Nhare ... 843 Mehali «*« ... 7)4 Nianga ... 715 Methi • • • 708, 752 Nibu ... ... 710 Mijalu ... Ml ... 737 Nim ... 741 Mirclia ... • •• ... 730 Ningal .. 809 Miriya • •• ... 809 Ningala ... ... 809 Mitha-dudliiya ... ... 745 ,, kaddu • • • ... 701 0. nibu • •• ... 710 Mitlian '21 Ogal ... 698 Mitha-tel ... ... ... 771 zaliar . . • ... 725 P. Mocharas ... ... 784 Mock-kand ... 735 Padam 712, 782 Mol * * » ... 713 Padam-chhal ... 745 Mora ... * . • 807, 809 Pad bank ... • •• ... 842 Morinda ... • . * ... 834 Pad dam ... . ... 712 Moriya ... III ... 739 Paderi III ... 806 Mor-paohh... • . • ... 725 Padma .. • • • ... 842 „ pankhi . • . ... 725 Oadmak ... • • • ... 843 Morunda ... . . • ** ... 837 Pahar • •• ... 843 Morn ... ... 818 Pahari-cha • . • ... 743 Moslita . • * ... 686 Pahari-indrayan • • » 701, 732 Moth ... 688 , 693, 694 Pahari-kaghazi III ... 710 Motha li* 734, 808 Pahari-nimbu • * • ... 710 Mubaraka ... • II ... 725 Pahari-pudma 703, 741 Mukha-jali • . • ... 735 Paijamas 27, 30 Mukui ... 687 Pain III ... 271 Muli ♦ *• 702, 748 Paiya • • * ... 712 Mullah ... • •• 34 Pakhan-bed 746, 749 Mung • •• 693, 694 Pakura ... III ... 778 Mungari ... • . • ... 687 Pala-kliari • •• ... 734 Mnngra • • • ... 684 Palak ... ... 707 Muniya • •• ... 703 Palang . . • ... 703 Munj ... • •• 807, 808 Palas ••• 729, 778 779, 784, 793 944 INDEX Page. Page. Palwal ... • • * ... 699 Pindar • •• ... 733 Pama • •• ... 842 Pipal • •• 737, 789 Pan • • i 757, 768 Pi'pala-mor ... 705 Pan-babiyo • • • ... 808 Piplainul • r • ... 731 Panmotha ... ... ... 774 Piriya • • • 734, 809 Panri > . • 757, 769 ,, liiiliin t • • ... 708 Pansari • •• ... 698 Pisu-ghas ... ... 728 Papar 704, 714, 715, 740 Pithi ... 687 Papari ... • • • ... 8.18 Pitpapra ... Ml ... 737 Paphar ... 698 Piyaj • • • 703, 726 Papri i a a ... 730 Piyal • • • 782, 799 Paral ... • •• ... 784 Poi-dhaula • » « ... 798 Parhar • . • ... 738 Post-anar ... ... 715 Pari • •• ... 732 Pui • • • .. 708 Parpinja ... • • « ... 842 Pula • •r ... 686 Patangliya III ... 818 Puna-rikhu • at ... 692 Patera ... 806 Puta ... • •• ... 740 Pateri • mi a v a 806 Putrajiva ... »*• ... 748 Pathan-bed • • • ... 749 Puwal ■a • ... 686 Patiia • • • • •• 800 Puya • • • 712, 782, 798 Ptxti ... • • • ... 727 Puya-udish • aa ... 818 1 (ittdi ••• III — 791 Pattar a a a 761, 762 R. Pattliarke-phul • •• ... 745 Patti • • • ... 698 . Rabi • aa ... 682 Pattiya ... ... 791 Rada >aa ... 770 1 att u. ••• • a a ... 714 Ragha «• « 834, 837 Paya ... • •• ... 782 Raghi ... 690 Pechwan ... • • • ... 756 Rahar ... 696 Pengla-jari • « • ... 751 Rai • • • 707, 770, 834 Petari • a • ... 734 Raish • • • ... 695 Petba ... 700, 728, 734 Rai-banj ... • • • ... 817 Rhala • • i as* ... 271 Rains • aa ... 678 Phalaha ... , , , ... 698 Rai-salla ... • a • 829, 837, 840 Phalawa . ... 747 Raj-briksh .. • aa ... 731 Pkaldu ... 817 Rakshi ... aaa ... 27 Phalel . . • 715, 772 Rakti ... • • • ... 724 Phaliant ... Ml ... 818 Ral MO ... 750 Phali-gawar a a • ... 696 Ramdana ... ... ... 697 Plialka ... 270 Ramjawain • •• ... 687 Phalsa ... ... 792 Rangra aaa ... 691 Pbalwa ... 772 Rao • ... 834 Phalwara . »*• 715, 772 Rao-ragha ... aaa ... 837 Phaniat . . . ... 818 Rara • aa ••• 770 Phapar ... Pharkath ... • •• • a • ... 698 ... 730 Rara-sarson Rasaut • aa • •a ... 770 ... 729 Pharonj • a • .. 818 Rasi • a a ... 768 Pharsiva, ... a • • 738, 792 Ratan-jot ... • aa ... 744 Phatang ... a . « ... 277 Ratmandi ... aaa ... 752 Phaunda ... • • • ... 736 Ratnaliya ... • aa ... 724 Phedi at* ... 16 Raunsala ... a a ■ ... 837 Phitkari ... ... 297 Raus-ka-tel • a a ... 734 Phul-banga • •a 760, 799 Rg mi ... 834 Phul-gobi ... a a • ... 707 Rek • a* ... 711 Phulka aa a ... 768 Rena ... aaa • aa 684 Pliunt a. a ... 701 Rendi aa 749, 772 Phusar-patta HI ... 798 Reri ... • aa ... 806 Pila-sarson • aa ... 770 Rhai ... •r a ... 834 Pili-jari ... • «1 732, 751 Rianj ... • aa ... 817 Piliya-kachang Ml ... 725 Riansh a a a , .o 695 Pindalu ... a a a 703, 704 Riensh ... III ... 695 'S’ii - - S f ly INDEX. 945 I | Rikhu ... • •• Page. ... 692 Rikonda ... • •• ... 692 Ringal • • • 809, 810 Rxtha ... • •• ... 749 Roini ••• ... 741 Roli 741, 776 Ropa ... 686 Ropini ... ... 805 Roti ... • •• ... 708 Ruina ... • # • ... 776 Ruindar ... ... 695 Kusa m lit ... 751 Sabji ... S. • •• 760, 763 Sada » • • ... 756 Sadaphal ... i*ei ... 710 Safed-ak ... in ... 794 „ bhangra ••• »«• 739 „ ind ... • • • ... 740 „ sir as... • a* ... 782 Sag »*• • • • 698, 707 Sahajna • •0 742, 784 Saila ... ... 691 Sain .... in 812, 815 Saishu • •• ... 278 Saj • •• ... 815 Saji • •• .. 756 Sakha ... lit ... 813 Sal 7, 28, 83, 86, 301, 750, 779, 784, 785, • M • • • [812, 813 Salajit • •• ... 2~9S Salap misri i • • ... 722 S al I) i a «ii • • • ... 703 Saleri ... r . . ... ”703 Sallii ... , • • ... 729 Sal la im • i • 785, 829 Sallo III ... 326 San III ... 791 Sanan Ml 815 Sananbar-saghar III ... 828 Sandan o • • 784, 815 Saoni ■ II ... 690 Saraichu ... ■ • • ... 810 Saral Ml 785, 824 Sarar • •• ... 748 Sar-bachyad • • • ... '277 Sar-chaka ... • • • ... 277 Sarjao til ... 277 Sarhar *• • ... 807 Sarkara ... ... ... 807 Sar-pan ... • • • ... 277 Sarpafc ... 806 Sarpbonka... m ... 751 Sarshaf ... 769 Sarshu & • • ... 277 S arson in 707, 770 Sarur ... 807 Sarwala ... • • • ... 748 Sarwali ... 731 Page. Satiydn • • • ... 726 Satpura • •• ... 795 Satn • • • ... 679 Sauj • • « ... 817 Sawan • •• ... 689 Sob ... Mi ... 713 Sehund .. • «« ... 736 Selu ... • • • ... 793 Sem • •• 702, 709 Sernal • • • 729, 784, 791 Sem-ki-gond • • • ... 782 Sentlia ... • •• ... 806 Seo ... in ... 713 Ser ... • •• ... 270 Serahi ... 745 Set-baruwa.., • • • ... 795 Shakrband.. • • • ... 703 Shalgam ... ••• 702 Shanraj ... • • • ... 730 Shambal ... Hi ... 743 Sharifah ... • •• ... 727 Shauriya ... e«t 736, 783 Shib-wala ... Ml ... 118 Shimi • •• ... 696 Shincb ana ... Ml 695 Shira • • • 756, 768 Shiro ... !*• ... 808 Shisham ... III ... 814 Shiwali * • • ... 753 Shukpa ... ... 843 Shukr-ul-uslir ■ • • ... 788 Shumeo • •• 745, 753 Shurbuta ... • • • ... 843 Shurgu • •• ... 843 Sidhi • o» ... 763 Siga • • • ... 33 Sihora ... ... 751 Silajit ... Ml ... 295 Sil-supari ... III ... 748 Sim ■ •• ... 779 Simali ... • •• ... 753 Sir liara ... • • • ... 779 Sindan ... ■ ■ • 782, 792 Sink • • • ... 808 Sinkauri ... ... ... 776 Sirali • •a ... 731 Siras • • • 726, 782 „ wilayati ... ... 782 Sirgochi ... 714 Sirki ... • • • 806, 808 Sirki-munja ... 806 Sisu ... • •• 83, 734, 812 Sissu • . • 814, 851 Sitaphal ... 727 Sitrawal ... • •• ... 727 Siyah-tut ... • M ... 742 Siya III ... 684 Son (M ... 271 Sona-ke-pathar III ... 290 Sonchala ... 1 II ... 741 Sonf «M 705, 737 Jt 119 ' i * ; INDEX, Sonta ... Sonth • M Soya ... Sujuniya ... Sukh- chain Sula ... Sundras ... Snnadung ... Sujia ... Supari Surai ... Sural ... Surgi ... Surki ... Syamak Syamsundari Tiibahshir Talr ... Taj ... Takuli Ta. ... Tamaku ... Tauja ... Tarai ... Tarbhui Ml Tarkari Tarpin-ki-tel Tarur Tat ... Teguna ... Tejbal Tej-pat ... Teliya ... Telu ... Tembd ... Tendu ... Thaka ... Tbakil Thalu ... Tham ... Thana Thaner Thansa Thapla Thelu Thohur Thuner ... Thungtu ... Thupara ... Tikuli ... Til Tilchuni ... Tin ... Page. Pnge. Ml ... G96 Tilonj Ml ... 818 III 706, 764 Timur ill ... 753 706, 745 Tinpakh ... • • • ... 689 at* ... 745 Tisi ... 771 • • • ... 746 Tita-khana • • • 736, 744 • •• ... 818 Tit-patti ... • • ... 749 Ml ... 786 To’ar M • ... 774 III ... 836 Tor III ... 696 Ml 687, 691 Tori • *• ... 770 III ... 769 Toriya ... ... 770 • •• ... 840 Totnula ... ... 737 • M ... 748 Tot-nala ... ... ... 806 Ml ... 843 Tumri ... ... ... 700 Ml ... 296 Tun