CORNELL UNIVERSITY LIBRARY 3 1924 096 224 872 In compliance with current copyright law, Cornell University Library produced this replacement volume on paper that meets the ANSI Standard Z39.48-1992 to replace the irreparably deteriorated original. 2003 Cornell University Library The original of this book is in the Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924096224872 WSk Alacown (J.), F.L.S., Manitoba and the REAT North- West, a full and Complete latory of the Country, inoluaiog the Educa- ONAL and Religious History of Manitoba id the North-west, the History of the Oman Catholic Kissiona in St. Boniface, eto, iii illustrations, a stout 8vo vol of 687 pp, leep, 1.25, 1882. T BOUGHT WITH THE INCOME FROM THE SAGE ENDOWMENT FUND THE GIFT OF fienrg ^- Sage 1891 JOHN BRITNEI^L. Bookseller 280 YoNGE St., Toronto, ( Canada Upwards of ioo.cxm voliimes o/ he best Old European Kooks in Stock. Frequent consigiuiients from our depot in London, Eng', CATALOGUES MONTHLY. HISTORY OF THE GREAT NORTH-WEST. 70/ ""X" 65/ 60/ :x>i ^\ \^ \ ■/^ / ^. ^? 1« \ \ ,<;."**^ V-f' i,^J jv-^"" >>-^ rfjoo^* ?.^J \ "'Sn.'":'..! >?«. \ ''r."»r"r «^ ^ '1?g r**"^' :»j»*- .i^ Jw.i-*'^" iV ^ 1/ ' 'i - jjC^ii'i ys^ rtl>^^ /J»V ?3P1»»1 Gl/I'*'' STlL^ W%f^\ \ \ \ ^ V \ v^ / / \ / f. c ,^- / y.C^ lUt^, L* t>r \/ DOMINION OF SHEWING WE EXTENT AND SITUATION OE ITS PIJBLIC IlAMDS;, V ^tl^X ("^ -^j ti iy^-<. r7»)* ^ s^^- iT- , en .eP^ X. 'ALSO ITS GEOGRAPHICAL RELATION TO THEk :oTi^; f> mc eiimAMi uthociiaphic co uonrnEAi ■*o" tU" 'tri' ' A 's;22':^:;i^ 'le Hc.Kt w5 ^/;7t Qreenwich. Gol ,so^, IX \ *o\ :l_ / ■■ON <«;^ MANITOBA AND THE GREAT NORTH-WEST: THE FIELD FOR INVESTMENT; THE HOME OF THE EMIGRANT, BEING A ^nlX and (f^ompXcU ^tst0i;;g of the (e>onntvvif ITS GEOGRArHY, AREA, SITUATION, AND BOUNDARIES ; ITS EARLY HISTORY AND PROGRESS ; INCIDENTS OP THE SETTLEMENT FROM THE EARLIEST PERIOD UP TO THE PRESENT TIME; TOPOGRAPHY AND GENERAL CIIAUACTER OF THE COUNTRY — ITS CLIMATE, TOGETHER WITH TABLES OF TEMPERATURE AND CLIMATIC CHANGES ; FUEL SUPPLIES — COAL, TIMBER, ETC. ; THE SOIL— ITS WONDERPUI, RICHNESS AND FERTILITY; NATURAL PRODUCTS — GRAIN, FRUITS, GRASSES, AND FLOWERS; NATURAL HISTORY, WITH ENUMERATIONS OP ITS MAMMALS, REPTILES, INSECTS, BIRDS AND FISUES ; STOCK RAISING — SPECIAL ADVANTAGES AND ADAPTABILITY; MINERAL RE- SOURCES AND PROSPECTS OF DEVELOPEMENT ; THE WATER SUPPLY — RIVERS, LAKES, ETC. ; STEAMBOAT AND INTERPROVINCIAL COMMUNICATION; THE RAILWAY SYSTEM — ITS RISE, PROGRESS, AND DEVELOPEMENT ; THE INDIANS — THEIR PAST HISTORY AND PRESENT STATUS; THE HUDSON'S BAY COMPANY AND ITS RELATIONS WITH THE COUNTRY — ITS PAST AND PRESENT HISTORY, LANDS AND LAND POLICY ; THE GOVERNMENT AND RAILWAY LANDS — MODE OF SURVEY AND LAYING OUT TOWNSHIPS, LAND REGU- LATIONS OF EACH ; ADVICE TO IMMIGRANTS AND SETTLERS, BY JOHN MACOUN, M.A., F.L.S., Dontinion Field Naturalist and Botanist, and for nine years past Gover7imevt Explorer of the North- West ^/bnnerly Professor of Botany in Albert University , Belleville. TO WHICH HAS BEEN ADDED THE EDUCATIONAL & RELffilOUS HISTORY OF MANITOBA & THE NORTH-WEST, By GEORGE M. GRANT, D.D., Principal Queen's University, Kingston, Ont., Autlwr of" Ocean to Ocean" dr'c, fir'c. B 3T0EY OF THE EOMAH CATHOLIC IISSIOIS IN ST. BOUIFACE, CONTRIBUTED BY His Grace THE ARCHBISHOP TACHE'S Secretary ; also MONTANA AND THE BOW RIVIR DISTRICT COMPARKD FOR GRAZING PDRPOSES, By ALEXANDER BEGG, ivko spent the season o/i^'&i exofnining both sections tuitk a view of establishing a Ranche ; also SKETCH OF THE RISE AND PROGRESS OF WINNIPEG, By J. C. McLAGAN. ITie whole profusely Illustrated with Lithographs and Engravings, City and Town Plans, and the most complete system of Maps yet issued, to which has been added an APPENDIX OF STATISTICS OF THE DOMINION OF CANADA, t)f much value and prepared with great care. AN ENCYCLOPEDIA OF INFORMATION in regard to the Great North-West. puilisijtll is THE WORLD PUBLISHING COMPANY, GUELPH, ONT. 1882. ^.\^^lB'b Entered according to Act of Parliament of Canada, in the year one thousand eight hundred and eighty-two, by James Waiter Lyon, in the office of the Minister of Agriculture. M ONTR EAL: Ef)t BurlanB iHttogtapfiic ffiompans, ELECTROTYPERS * PRINTERS. TO HIS EXCELLENCY THE RIGHT HON. K.T., G.C.M.G., GOVERNOR GENERAL OF CANADA, ETC., ETC., ETC. IS MOST RESPECTFULLY DEDICATED EY SPECIAL PEEUISSIOK- PREFACE Frequent demands upon my time and patience for information regarding the North- West have compelled me to put in book form the gleanings of the past ten years. In the volume now offered to the public I have attempted to give a truth- ful description of the greater part of the country suitable for the habitation of civilized man. Several chapters are devoted to its Natural History and Botany. These may be considered as a compendium of our present knowledge. In the chapters on the capabilities of the soil, stock-raising, climate, &c., I have spoken from my own knowledge and on my own authority. Where my own knowledge of any matter was considered insufficient, I have quoted from other writers of known ability and truthfulness. Statements from actual settlers are in their own words, and as their addresses are given these can be verified. Nearly every matter pertaining to the country has been touched upon, and where thought worthy elaborated. To give the work that completeness to which it aspires appendices have been added by other writers on matters for wliich their knowledge specially fitted them. As qualifications for writing the work I may mention a twenty years study, theoretical and practical, of Botany, Natural History, and Physical Geography. After ten years study of these subjects I accompanied, as botanist, Mr. Sandford Fleming, and the author of " Ocean to Ocean,'' on their cele- brated expedition across the continent. In the year 1875 I was appointed botanist to the expedition, which, under the leadership of the Director of the Geological Survey, explored the Peace Eiver and Rocky Mountaina Two VI PEEFACE. yeais later I ■was asked by the Dominion Government to write a report on the North- West Territories, and availed myself of all reliable information regarding the country. The summers of 1879-80-81 have been spent in traversing the least known parts and investigating the forma, flora, meteoro- logy and physical phenomena of the country. It will thus 1 ■ seen that my opportunities have been ample. Of the imperfections of the book I need not speak. The tiitics wUl point out these. In writing I have had the delight of revisiting in imagination many a cheery camp-fire, and many a scene of vast and lonely beauty, on which memory loves to dwell, and of feeling that I was endeavoring to describe to my fellow-countrymen, with simplicity and truthfulness, a portion of that magnificent heritage of which as yet they know so little. JOHN MACOUN. CONTENTS. CHAPTER I. General Geography. The Dominion as a whole — Its Extent and Area — Nova Scotia — New Brunswick — Prince Edward Island — Quebec — Ontario — Keywadin — Manitoba — North- West Ter- ritories — British Columbia — North-West and Manitoba a vast Plain — Southern or Prairie Section — Middle or Partially Wooded Section — Region of Continuous Forest — Basin of Lake Winnipeg — Its Kivers and Lakes — Mackenzie River Basin — Th« Churchill and Nelson Rivers — General View of the Rocky Mountains. CHAPTER II. Physical Geography of Manitoba, Its Situation and Boundaries — Area — General Characteristics — Red River Prairie — Pembina Mountain — Wet Country along its Base — Riding Mountain — View from its Summit — Dauphin Lake— Duck Mountain — Lake Winnipeg — Lakes Manitoba and Winnipegoosis — South Western Manitoba — Turtle Mountain — Red River — Graphic Picture of the Prairie near Winnipeg — Fort Garry — Assiniboine River — Land on Assiniboine — Souris River — Snake Creek— Oak Lake — Vicinity Suited for Stock- farming — Sand Hills, at Snake Creek — Little Saskatchewan — Land on Little Saskatchewan — Settlements in its Valley^Shoal Lake— Bird Tail Creek — Surrounding Country — ShellRiver — Country North to Fort PeUy — Indian Farm — General Character of Soil — A Desert changed to a Paradise — Timber for Building Purposss — Where Located — Building Stone— Brick Clays — Water Supply near Winnipeg. CHAPTER III Character of Gmmtry between lat. 49° and 50° west of Manitoba. Description of Moose Mountain — Plain from its Top — West side of Moose Mountain — Timber on the Mountain— View from High HiU — Souris Plain — West of Moose Moun- tain — Character of Soil — of Vegetation — of Surface — Great Clay Plain — Its Rough Surface — Scarcity of Water — Wild Roses — A Visit to the Coteau — Cactus Plain — Wood in the Coteau — Description of Coteau — Resemblance to Turtle Mountain — Ab- sence of Wood — Plateau of Lignite Tertiary — Wood Mountain — Disappearance of the Buffalo. Viii "tX CONTENTS. / 4/ CHAPTER. IV. '"dhiracter of Country between lat. 50° and 51° West of Manitoha. Assinitoine below Brandon— Brandon— Assiniboine Rapid- Land near Brandon— Bran- don Hills— Land along the C.P.R.— Flat Creek— Gopher Creek— Land "West of Gopher Creek— Pipestone Creek— "Weedy and "Wolf HiUs— Rich Country along the C. P. R.— Qu'Appelle River— Navigation of the Qu'AppeUe— Country North of the Qu'AppeUe— Pheasant Plain, Leach Lake— "Very rich Land in this Region— Long Lake— Fish in Long Lake— Waterfowl— Creeks at the Head of Long Lake— Country "West of 102nd Meridian— "Wood for House building and other Purposes— Country "West of Touchwood HiUs— Estimate of good Land in Qu'AppeRe Valley— Unequalled tract for "Wheat- Early Ripening of Grain— Absence of Summer Frosts— Early Spring —Moose Jaw Creek —Dry Country in its "Vicinity— Sand HiUs "West of it— The Coteau— Old "Wives Lakes —Country West of Lakes — Excellent Pastures— Nutritious Grasses— Their Distribution —Sage Brush and Cactus no Proof of Aridity— Bullrush Lake— Strong Current Creek "Want of "Wood — High broken Country — Appearance of Cypress Hills, CHAPTER V. Character of Country between lat. 51° and 52° West of Manitoba. Country "West of the Assiniboine — Beaver and Touchwood Hills — Heavy Forest — Rich and Lovely Country — Great Salt Plain — Immense Plain to the South — Tract North of the Qu'AppeUe— Rich Soil and Rank Grass— Last Mountain— "Water Scarce on Sur- face — Broken Country, Twenty-two Miles "Wide— Fine Pasture Lands — No Bad Soil m Eighty Miles — Lines of Boulders, near Humboldt — Cause of "Wood at Certain Points — Extensive Plain Southwest of Touchwood HiUs — Salt Marshes — Little Touch- wood Hills — Mission at this Point — File Hills — South Saskatchewan, "Voyage Do>\ ii It — Moose Woods — North of Moose "Woods — Land East of River — Soil of Great Depth — Aroline, or Telegraph Grossing — Rich Land — Country "West of River — Fine Level Tract — Eagle Creek — Eagle Hills, Fine Country for Stock CHAPTER VI Character of Country between lat 52° and 53" West of Manitoba Porcupine Mountain — Country on Red Deer River — Soil very Rich — Exhaustless Fertility of the Carrot River Country — Prince Albert Settlement — Its Early History — "Wonderful Progress in a few Years — Description of the Settlement — Many Houses in Course of Erection — Fall Sowed Wheat a Success — No injury from Frost — Duck Lake Settlement — Fort Carlton and its "Vicinity — Country between the Rivers — Eagle Creek — The Bear and Eagle Hills — Land South of Them — Description of Battleford and Vicinity — Its Future Sketched Out — Laud in the Neighborhood — Character of Soil — Police Farm at CONTENTS. IX Battleford — The Government Farm— Remarkable Vitality of Seeds— Depth of Roots in the Soil— Plain South of Battleford— Coulees of the Plain— Their Origin— Country- North of Bear Hills — Splendid Pasture Land — Water Abundant — Grasses of the Plains — Cause of Absence of Wood — Constant Prairie Fires^Why the South side of a Hill is without Wood — What Causes Aridity — Description of Hand Hills — Cactus not a Proof of Aridity of Climate — Fine Rich Land South of Battleford— Immense Area of Good Land — Manito Lake— Sounding Lake — Neutral Hills — Fine Pastoral Land to the Southwest — Land around Sullivan's Lake — Fine Land West of Sounding Lake — Rich Country at the Head of Battle River— Millions of Tons of Hay in This Re- gion — General View of the Country — Lakes Filled with Fish — Beaver still Numer- ous — All Lakes and Ponds Filled with Birds in Spring and Fall — Bears and Wolves. Numerous some Seasons, but Never Injurious Except to Small Stock. CHAPTER VII. Description of the Gowntry Drcdned hy the North Sixskatche- ivan and Athahasca Rivers Extensive District South of North Saskatchewan — One Solid Block of 13,000,000 Acres — Large Area of Fertile Land North of River — Star Mission, its Success — Multitudes of Whitefish — Lac La Biche Mission — Farmingjat the Lake — Wheat, Barley, &o. — — Victoria Mission — Small-pox Ravages — Rev. George McDougall his Death, the Edmonton Pioneer — Former Lawlessness at Edmonton — Change Caused by the Police- — Edmonton, its Mills, Churches, Stores — Coal and Iron at Edmonton — Review of the Country — Ninty-six per Cent. Good Soil over a Vast Area — Lands for the Irish without Rent — St. Albert Mission, its History and Success — Catholic Mis- sionaries, their Work and Success — Rocky Mountain House, Fine Timber — Gold Washing — Beaver River, very Rich Land — Green Lake, Abundance of Fish — Chipweyan Indians — Athabasca River and Country — Size of the River and its Tribu- taries — Little Slave River — Pembina River, Coal in its Banks — The McLeod — Baptiste's River — Jasper House and Valley — Climate of the Valley, Snow Fall very Light, Warm Winds, Dry Climate, Spring Weather — Horses Living out all Winter — Source of Warm Winds — Fertile Belt — Richness of It — Where Located — Prairie still Better — Wet Lands — Summer Frosts — Late Sowing — Fall Sowing, its Success. CHAPTER VIII. Peace River, Position of the Lands Described — Area of the Region in Question — Character of Rocks and Soil — Its Composition and Disposition — Peace River Prairie — Location of Prairie — Sandy Soils along Athabasca— Origin of Peace River Prairie — Wonderful Vegetation — Climate of Peace River — Summer of 1879 — All Sorts of Grain and Vege- tables Mature — Ripening of Grain at Dunvegan and other Points — Depth of Snow — Setting in of Winter — Opening of Spring— Breaking up of the Ice — Difference in Climate of Valley and Plateau — Occurrence of Frost — Comparison of Temperatures — Peace River Spring as Early as in Manitoba — Cause of Exceptional Climate — Chinook Winds — Length of Day and Increased Sunlight give Warm Summers — I CONTEKTS. Immunity from Grasshoppers — Description of Little Slave Lake — Eipening of Grain at this Point — Wliitefish in the Lake — ^Abundance of Beaver — Climate Unchanged to the North— Soil of the Northern Plain— Eipening of Grain at Vermilion — Summer Climate of that Region— Milder Climate Farther North at Little Red River — "Vicinity of Fort Chipweyan — Extraordinary Wheat on Poor Soil — Crops at Fort Simpson on Mackenzie's River — Climate and Crops at Fort Liard, Lat. 61" — Barley Ripens under the Arctic Circle — Farming on Peace River a Success— Lakes Teeming ■with Fish— Birds in Countless Flocks — Rocks of Peace River, Limestone, Gypsum — Abundance of Salt— Bituminous Shales on Athabasca River — Tar Springs— Descrip- tion of the River — Appearance of its Banks — Land Between the Athabasca and th» Peace Rivers. CHAPTER IX. Climate of the North- West. Notes from Blodgett's Climatology^Its Great Value — Lake Superior Compared with North-West — Summer Heat Decisive of Climate — Thermal Lines Curve Northward — Spring opens Simultaneously on a Northwest line Between St. Paul's and Mackenzie Rivers — Deserts not Found North of Lat. 47°— Rain Sufficient on the Northern Plain — Buffalo more Abundant in the North — Peace River Compared with Germany and Russia — Canadian North- West the Better — A Prophecy Thirty Years Ago— Size of our North- West — Lord Selkirk's Opinions Seventy Years Ago — 500,000 Square Miles with a Mild Climate. CHAPTER X. Practical Semarhs on Climate. ilr. Anderson, of Listowel, Ireland, on Climate — Great Heat Causes no Inconvenience — Intense Cold Hardly Felt — Manitoba Winter Climate Better than that of Ontario — Snow Seldom over Twenty Inches in Depth — Seasons in Manitoba — Manitoba in the Middle of the Continent — Long Days of Summer — Autumn Weather— Snowfall — Heat and Humidity — Comparison of Summer Temperatures — Warm Summers and Dry Cold Winters — Table of Mean Temperatures — Summer Temperatures Compared — Peace River Climate — Manitoba Climate — Hardness of Wheat— Grains in the Cluster — Min- nesota Nowhere — Peace River Wheat — Isothermal Lines — Com and Wheat Zones — Temperature Necessary for Successful Wheat Culture — The Wheat Zones — Probably Three-fourths of the Wheat Lands of America in the New North- West — 200,000,000 Acres — Extent of the Territory — Lord Selkirk's Opinions Seventy Years Ago — Great American Desert— Its Effect on Climate — Changes Observed Passing North — How the Isothermal Lines Curve — Where the Heated Air comes From — Two Currents passing North— Summer Temperature the same over 300,000 Square Miles— Moisture in Sum- mer, its Absence in Winter — Rainfall of the Year — -Progress of the Seasons — Fall Frosts not Injurious, Climate Unsurpassed for Farmers — Its Possibilities Unlimited — Depth of Winter Frost— Its Beneficial Effects on Soil— Table of Rainfalls for 1879 and 1880 — Rainfall and Cloudlessness — Testimony of Settlers Regarding the Healthiness of the Climate. CONTENTS. Xi CHAPTER XI. Natural JProd^icts of the Soil. Comparison of Floras — Peace River Flora Compared with that of Ontario— Forest Flora — Flora of the Prairies— List of Species — " Sugar Maple" — Syrup from the Birch — Wild Plums — Cherries — Service Berries — Their Value — Berries in Pemmican — How Pemmican is Made — Berries for Breakfast — Strawberries — Currants and Gooseberries — Black " Jurrants very Valuable — High Bush, Cranberries^ Raspberries of Many Species — Jam from the Cloud Berry — Common Cranberries — Blueberries — Wild Sarsaparilla — Silver Berry— Buffalo Berry — Beautiful and Valuable Shrubs — Wild Hops — Hazel Nuts — Flowers and Shrubs at Brandon — Their Beauty and Utility — Strawberries at Brandon — Shmbs of the Prairie — Moose Mountain Flowers— Flowers at the Sand Hills and Flat Creek — Line of C. P. R. — Pipestone Creek — Flowers of the Plain — Great Souris Plain — Acres of Lilies — Gardens of the Prairie — Roses Fill the Air with Perfume — Flowers at Moose Jaw Creek — Flowers of the Cypress Hills — Wild Lupines Covering Square Miles — Mushrooms, their Great Value and Enormous Size and Numbers — Mushrooms over 200 Miles of Country — Lycoperdons (Puif- balls) not Poisonous — Flora at Long Lake, Lilies, Anemones, Pentstemons, Poten- tillas and many Others — Common Poplar a Remedy for Intermittent Fever. CHAPTER XII. liaising Wheat. Red River Prairie, Description of its Soil — An Old Countryman's Views — Extent of the Wheat Lands — 150,000,000 Acres of Wheat Lands — Manitoba Excluded from the Calculation — Good Land Continues for 100 Miles at a Time — Fixed Laws Regarding the Growth of Wheat — Northern Limits of Wheat Zone — Northern Wheat more Pro- lific — The Cause Explained — How Wheat Grows in Spring, and Summer — Why Mani- toba Wheat is Hard — Roots Penetrate to a Great Depth — ^Analysis of Soil, far Supe- rior to the Best Wheat Land in Europe — Best Soil in the World in the North- West — Manitoba Formerly an old Lake Bottom — Soil of the Second Prairie Steppe — Soil of the Third Plateau — Gypsum very Abundant — Cactus no Proof of Aridity — Setter's Farm Described — AVheat Growing amongst Cactus — ^Appearance of the Land — Results of 1880 — of 1881 — Seed Bought in Minnesota in 1876 — Progress since Then — Mani- toba Wheat Admitted Duty Free into Minnesota — Opinions of Pioneer Press of St. Paul's, Minnesota, regarding North- West Wheat — Statements of Residents — Average Crop for Four Years — Average Yield of Canadian North-West Compared with the best States in the Union — Great Weight of the Grain — Qu'Appelle Region as a Wheat District — Prince Albert and Edmonton as Wheat Districts — Description of Edmon- ton — Cust's Farm at Edmonton — Country on Peace River — Excellent Wheat Lands far to the North — Cucumbers Ripen in. Lat. 60° — Wheat in Lat. 61° First-class — Spring Frosts not Hurtful — Fall Wheat not Suited for the North-West — Fall Sowing Recommended — No Doubt of its Success — Instances of Fall Sowing — FaU Sowing the True Policy of Settlers on the Prairie — Wheat Production of the Future beyond Cal- culation — England should Realise that we have the Greater part of the Wheat Lands of America — England's True Policy — Farmers Testimony Regarding the Soil. Xii CONTENTS. CHAPTER XIII. dermis, Boot Crops, Seed Time and Harvest, Boads, &g. Barley— Its great Weight in the North— Bay of Quinte Barley— Additional 100,000,- 000 Acres Suited to Barley North of the Wheat Belt— Uses of Barley in the West- Testimony Regarding its Culture in Manitoba— Average Yield for Four Years— Com- pared with the United States— Enormous Yield of Oats— Testimony of Residents in Manitoba— Average sixty Bushels per Acre— Nearly Three Times Greater than Ohio — 100 Bushels per Acre often Raised — Potatoes a sure Crop to the Arctic Circle — Rotten ones Unknown — Chipweyans as Potato Cultivators — Remarkable size of Potatoes at Hay Lakes— Late Growth of Potatoes— Feeding Stock an Easy Matter — Pumpkins, Melons, and Cucumbers in the North — Melons Grow and Ripen North of St. Petersburg, or 1,200 Miles Northwest of Winnipeg and 900 Miles North of the Boundary — Extent and Capacity of the Country Beyond the Range of Average Com- prehension — Testimony of Residents Regarding the Productive Powers of the Soil — Timothy an Excellent Crop— Good Fall Pasture— Wild Hops— Clover— Flax— Hemp Why all Crops Succeed so Well — Southern Russia a Parallel Case— Commencement of Spring — Setting in of Winter — Seed-time in the North-West— Varies in Certain Localities— Harvest Time— Earliest in the Qu'Appelle Valley— Always Free from Frost — Qu'Appelle Valley Compared with Saskatchewan — Time for Taking up Roots — Testimony Regarding Seed Time and Harvest — Roads of the West merely Cart Trails — No real Roads other than Railways in the Country — Description of Leading Trails — How Trails are Formed — Where they Lead to — No Attempts made to Improve them — Travellers Tell of their Own Incapacity — Experienced men Never get "Stuck" — How to Cross a "slew" with Loaded Carts — Trails or Roads of Ten Years Since — How they were Formed — Indian Trails — Roads of the Future. CHAPTER XIV. Grasses of the Plains, Forests, and Mountains. Pastures of the Prairies — Their Value in Various Sections — Design of the Chapter — List of Grasses, their Habitats — List of Cyperaceae, their Habitats — List of Rushes — List of Legummosffi (Pea Family) — Why Certain Grasses have Various Names — Effects of Burning the Grass — "Wild Oat" of Southwestern Manitoba a Bugbear — Sheep Killing by its Awns a Myth — Description of the Grass — How it Injures Man or Beast — Hay made of this Grass — Its Effects on Horses — Really the best Grass on the Plains — Hay Grasses — Manitoba Hay — Practical Remarks on Manitoba Hay — Testi- mony of Residents Regarding the Hay Crop — Sand Hill Grasses — Bunch Grasses — Buffalo Grasses — "Grama-grass" — Grasses of the Alkali Lands — Valuable Grasses — Grasses of the Bow River Country — Spring Food of Horses — Summer Food — Winter Grass of the Prairie — Winter Pasture in the Forest — Only one Poor Grass in Ninety- six — Value of the Pea Family — Artemisia Frigida as a Forage Plant — Eurota lanata — Analyses of Grasses. CONTENTS. xii: CHAPTER XV. Stock Raising. Method of the Chapter — Cypress Hills — General Description, Altitude, Wood, Water, Grass — Value for Summer Pasture — Winter Pasture North of the Hills — Shel- ter in the Coulees — Plain North of the Hills — Its Description and Character — Bow Eiver and Cypress Hills Compared — Summer Pasture Everywhere — Enumera- tion of Localities — All Equally Valuable — Ponies can Winter Anywhere — The Reason of This — Prairie Grass real Hay in Winter — Why Canadian Horses Die — How to Remedy This — Mr. Mackenzie's Opinion — Canadian Horses must be Fed — Cattle Succeed Well as they are always Grass Fed — Ponies use the Hoof ; Cattle the Nose to Procure their Food in Wintei- — When Cattle must be Fed — Incidents on the Prairie in AVinter — Mr. Selwyn's Testimony — Dr. Dawson's Testimony — Wild Cattle Winter out — Winter Shelter a Necessity — Other Locations as Good as Bow Rivei' — Country West of Cypress Hills — Hand Hills as They are Now — Descrip- tion of the Hills— The " Store "—Country West of Sounding Lake— Tail Creek— Remains of Former Fights — Bow River Country — Natural Hay — Country Better Suited for Pasture than Farming — Description of the District — Root Crops easily Raised for Cattle Feed — Winter Storms Never do Harm if Food is Abundant — Sheep Raising — Keeping Hogs, easily Fattened — Animals easily Fattened in the North — Illustrations of this Fact — Riga Exports Hides and Tallow — Our Plains of same Character as Russian Ones — Food Abundant Everywhere — An Irish Delegate's Views on Stock Raising — Mr. Spence's Opinions Regarding the same Matter — Testimony of Settlers Regarding Cold. CHAPTEE XVI. /Stock liaising in the Bow River District compared with Montana. [Chapter Written by Alex. Bego, Esq.I American Writers Ignore our North- West, or Speak of its Sterility — Bow Eiver District Defined — Montana Stock-raisers Testify to the Superiority of the Bow River District — Description of North-Western Montana — It Improves as We Go North — Cattle now in the Bow Elver Country — No Loss from Winter Storms — Renting Grazing Lands — Statistics of Stock in Montana — Chinook Winds — Description of the Rocky Mountains — How to Stock a Ranche — Sort of Cattle to Choose — Comparison of Varieties of Stock — Capital Necessary to Establish a Ranche — Size of a Ranche — The Rate of Increase — Profits on the Investment — Will There be a Market? — Another Estimate of Cost and Profit — Is it Wise to Lay in Some Hay — Sort of Men for Herds- men — Men and Cattle Should be Comfortable — The C. P. E. to cross the Bow Eiver District — Sheep-farming as a Future Business — Eveiy Eequirement in the Eegion in Question — A Perfect Sheep's Paradise — No Sheep Ever Lost by Severe Weather in Montana — Little Disease among Sheep — Profit from Sheep Farming in Colorado — Equally as Good in Bow Eiver Country — Breeding and Bearing Horses — Conclusion. Xiv CONTENTS. CHAPTEE XVII. Water Swpply. Supposed Insufficient Eainfall — Souris Plain Thought to be a Desert — Settlement Proves the Contrary — Brackish and Pure Water; — Where Saline Lakes and Ponds are Situated Want of Running Streams Accounted for — Rainfall quite Sufficient — Prairie Fires the Cause of Apparent Scarcity — Surface Water Scarce in many Locali- ties — Brackish Water always Preferred by Horses and Cattle — Moderately deep Wells Supply good Water — Cause of Poor Water on the Manitoba or Red River Prairie — Artesian Wells a Success at Winnipeg — How to Obtain good Water in any Part of the Country— Statements of Actual Settlers Regarding the Water Supply. CHAPTER XVIII. Fuel Supplies. Scarcity of Fuel not Real — Views of the Canadian, the Englishman, and the Yankee — Supply of Southwestern Manitoba — Turtle Mountain — Moose Mountain a Source of Supply — Scarcity of Wood West of This — Cypress Hills — Government Reserves Fuel — Fuel Generally Sufficient in Manitoba — Supply for Pheasant Plain — Scarcity of Wood West of Touchwood HiUs— Eagle Hills Supply — Fuel Abundant North of the Prairie — Peat Deposits Abundant — Their Distribution — Peat on nearly all Farms now — Mineral Fuels near the Boundary — Analyses of Coals — Value of the Lignites — St. Mary's River Coal — ^Analyses of Coals by Prof. Haanel — Souris Coal Field — Coal at Cypress Hills — Coal on Bow River — Its Value as Fuel — Red Deer River Coals — Crawling Valley Coal — Saskatchewan Coal — Eighteen feet Seam above Edmonton — Analyses of these Coals — 211 MUes of Coal Exposures on the Saskatchewan — 25,000 Square Miles of a Coal Field — Edmonton the Centre of this Coal Field — Coal on the Pembina River — Peace River Coal — Coal at the Arctic Sea — Extent of Coal Field — No want of Fuel in the Future. CHAPTER XIX. Timber Supply. Minnesota Considered — Lake of the Woods — Line of the C. P. R. — Varieties of Timber — Where Located — Beren's River — No Pine West of Lake Winnipeg — Distribution of White Spruce — Black Spruce — Scrub Pine — " Cypress " — Balsam Poplar — Aspen Poplar — Cottonwood — Oak — Elm — Ash — " Sugar Maple " — Birch, Tamarac and Black Willow — Timber on Winnipegoosis — Supply for Rapid City, Minnedosa, Odanah, Birtle — Riding Mountain — Duck and Porcupine Mountains — Timber North of the Saskatchewan— Athabasca Valley — At Edmonton — On Turtle Mountain — ■ Cypress Hills— St. Mary's River — Timber in Bow River Country — Pheasant, File, and Touchwood HiUs — Eagle Hills — Battle River — Red Deer River— Tributaries of South Saskatchewan — Conclusion. CONTENTS. XV CHAPTBE XX. Mammals of the North-West. Introduction — Emimeration of the Garni vora, of the Ungulata, of the Chiroptera, of the Insectivora, of the Eodentia — The American Panther, its General Appearance and Eange — The Canadian Lynx, its Description and Distribution — Hunting on Peace River — Foxes, Anecdotes Respecting them — Wolves — The Coyote — The Grey Wolf, his Habits — Occurrence on the Plains — When easily Taken — Anecdotes Illustrative of their Cunning and Tenacity of Life — Pine Marten and Fisher — Wolverines, the Enemies of the Trappers — Anecdotes of the Wolverine — Mink and Otter — Skunks — Eaten by Hunters — Badgers and their Habits — Danger of Riding on Horseback — Mode of Killing Badgers — Notes on the Black Bear— Their Habits — The Terrible Grizzly — Fears of the Indians on Peace Eivei' — Nearly all Carry Scars Inflicted by Bears — Description of One Killed at the Hand Hills — Indian Woman Killed by a Grizzly — The Cabree or Prong Homed Antelope — Black Tailed Deer — Wapiti or American Elk, its Distribution — The Moose — Hunting Moose an Art — Starvation on Peace River in 1875 — Caribou Found in the North — Hunting on the Barren Grounds — The Rocky Mountain Goat — Description of It — Hunting in Bow Eiver Pass — The Big Horn or Rocky Mountain Sheep — Measurement of their Horns — Musk Ox of the Barren Grounds — Its general Appearance and Habits — Warmth of its Covering — The Butlalo, its Distribution — Wood Buffalo on the Athabasca — Their Present Scarcity — Buffalo Hunting in the Past — Mode of Camping in the Indian Country — Mode of Eunning Buffalo — Exciting Scenes — The Charge, Conflict and Pursuit^The Buffalo Pound in Former Days — How the Indians Slaughtered the Buffalo — Doctor Hector's Account — Moles and Shrews, Eich Soil where they Are— Gophers and Prairie Dogs, their Habits — Mode of Catching Prairie Dogs — Beaver — Stories Related of their Instinct— Con- struction of their Dams — Beaver Houses — Their Construction — Muskrats, their Num- bers and Habits — Character of Country they Inhabit — Muskrats as Weather Prophets — The Foolishness of the Prophets — How the Muskrat Builds his House — Pouched Gopher and Jumping Mice — Porcupines and their Habits — The Prairie and Woodland Hares — Great Numbers of the Latter — Rocky Mountain Hare. CHAPTER XXI. Birds of the No7-th-West. Large Numbers Breed in the Country — Enumeration of Singing Birds — Notes on the Thrushes, Warblers, SwaUows, Finches — Prairie Birds — Peculiarities of the Cow-bird — Blackbirds a Great Nuisance — The Fly-catchers, Enumeration of the Species — Night Hawks, Humming Birds, and Woodpeckers — All these are Forest Species — Range of the Humming Birds — Hawks and Owls— The Owl of the Prairie— Hawks very Beautiful and Abundant— Their Habits— The Wild Pigeon— Prairie Chicken, Ptarmigan and Grouse — Enumeration of the Waders — Numerous both in Species and Numbers — Plover — Avocets — Godwits — Sandpipers and Snipe in Myriads— Bitterns and Cranes often Numerous — Enumeration of the Ducks, Geese, and Swans — Their Breeding Places — Notes on the Eiver Ducks— Countless Myriads in the Fall — Game B XVI CONTENTS. Birds Around or in a Pond — A Common Sight — How to Procure a Supper — The Mer- gansers or Sheldrakes — Pelicans, their Habits and Breeding Places — Their Modes of Fishing — Gulls and Terns — Very Abundant on the Larger Lakes — Their Summer Haunts — Loons, Grebe and Dah-chicks — Habits of the Grebe — The Great Western Grebe — Synoptical Table of the Birds — Notes on the Prairie Birds — Birds near Bran- don in 1880 — At Flat Creek — At Moose Mountain— Souris Plain — Around Salt Ponds — Multitudes of Ducks and Prairie Chickens — Taking to the Stubble Fields — Notes on the Hawks — On the Owls — On the Gulls. CHAPTEK XXII. Notes on Reptiles, Fishes, and Insects. List of Reptiles — Snakes in Spring and Autumn — Gathering of Snakes at Livingstone — Snakes in BuUrush Lake — Fishing for Siredons — Rattlesnakes — Lizards — Toads and Frogs— List of Fishes— The Perches — The " Dore " — Carp Family — Their Great Numbers — Not Considered Good Food — Dried for Dogs and Bait — The Pike or Jack Fish — Its Habits — The Cat Fish — Salmon Family — Ai'ctic Salmon — Mountain Trout — Arctic Trout — Anecdotes — Bow River Trout — White Fish — Their great Value — White Fish in the Prairie Region — In the Forest Region — West of the Mountains — The little White Fish or Herring — The Gold-eye — Fishing for Gold-eyes in the Rivers of the Prairie — Western Pickerel — Its Value — The Loche or Burbot — The Sturgeon — Fish Supply of the Saskatchewan Valley and Prairie Country — Qu'Appelle and Long Lake Fisheries — Notes on Insects — Butterflies of the Prairie — Myriads in June — Absence of Moths — Coleoptera or Beetles — Grasshoppers and their Allies — Grasshopper Plague— Its Causes and Prevention — Conclusion. CHAPTER XXIII. Minerals of the North- West. Boundary of the Laurentian Series — Lower Silurian Rocks — Limestone at the Stone Fort near Winnipeg — Building Stone of Winnipeg — Devonian Series along Lakes Manitoba and Winnipegoosis — Salt Deposits in these Rocks — Pure Salt Collected in 1881 — Description of the Manufacture of Salt on Lake Winnipegoosis — Devonian Rocks on Peace River — Gypsum, Salt, and Petroleum — Gypsum on Peace River Salt Springs of Salt River — Tar Springs on the Athabasca — Cretaceous Series Its Extension— Limestone and other Boulders — Gravel and Sand — Niobrara Limestone Souris Coal Field— Coal in the Peace River Country — Lignite Tertiary — Its Probable Extension— Coal Deposits of Immense Extent — Pure Hematite in connection with the Coal — In the Saskatchewan Country — At Edmonton — Along Peace River Its Probable Value— Gold on the Saskatchewan— On Peace River— Gold Washing Seldom Remunerative— Brick Clays— Their Great Value and Probable Extent— Concluding Remarks. CONTENTS. XVU CHAPTER XXIV. History of the North- West, from the discovery of America to the year 1821. First Voyage of Jacques Cartier — "What he Intended Doing— Second Voyage— The Dis- covery of the St. Lawrence — Montreal Beached — Eoherval's Attempt at Settlement — His Want of Success — Champlain Founds Quebec, in 1608 — Interferes in Indian Quarrels — Lake Superior heard of, in 1615 — Missionaries Traverse its Shores, 1641 — Frenchmen Cross by the Dawson Eoute and Lake Winnipeg to Hudson Bay, in 1666 — Offers of Service to the Quebec Merchants, Renewed in Paris, Accepted in England — Gillam's Voyage — Formation of Hudson's Bay Company, in 1670 — Establishment of Forts on the Bay — Quarrels with the French — English Left in Possession of the Bay — French Trade Extended "Westward — Duluth on Lake Superior — Red River Reached and Forts Erected, 1732 — Fort a la Come Reached, before 1763 — Cession of the Coun- try — Canadian Traders in the "West — Hudson's Bay Company move Inland, in 1774 — Canadians in the Interior Nearly 100 years Before them — The Athabasca Beached by the Canadians — Hudson's Bay Company Beach Red River, in 1793 — The Trade open to all Parties — Formation of the North- West Company, 1783 — Fort William, on Lake Superior, their Head-quarters — Quarrels with the Hudson's Bay Company — Lord Sel- kirk Buys Shares, gets Control of the Concern, Obtains a Grant of Land, and Attempts Settlement — The North- West Company Deny his Bight to the Land, and Claim Prior Eights — They Publicly state their Determination to Fight — Counter Preparations by the Hudson's Bay Company — Settlers Leave for Canada, in 1815 — Arrival of Governor Semple — Preparations to Expel the North- West Company — Both Sides Prepare for War — Forts Gibrdltar and Pembina Taken by Semple — North- West Property Confiscated — Bed River Blockaded — Attempt to Provision the Boats — Governor Semple Interferes and Loses his Life — Hudson's Bay Company Account of the Fight — Opposite Account — Apathy of the British Government before the Fight — Warned Repeatedly by the North- Westers — Lord Selkirk's Preparations — Takes Possession of ]?ort William — The Colony Re-established in 1817 — Troubles with the Grasshoppers — Union of the Companies in 1821. CHAPTER XXV. History from 1821 to 1870. Arrival of th« Swiss — Settlement of the old Hudson's Bay Company's Servants — Terri- ble Winter of 1825 — Disastrous Flood of 1826 — Emigration of the Swiss — Bed River Colony Prosperous — Sir George Simpson's Policy — Attempts at Various Industries — Sheep Farming Cause of Failure — Lord Selkirk's Title to the Land Eeverts to the Hudson's Bay Company — Farming Tried on a large Scale — Schools Established — Everything Done to Prevent Successful Farming-^Half-breeds Frighten the Com- pany—The Council of Assiniboia Formed — Duty Imposed on Imports and Exports — Regulars Sent into the Colony — People Petition for their Bights — They take the Law into their Own Hands and Trade becomes Free— Red Biver Flood of 1852 — Captain Palliser's Expedition — Expedition under Dawson and Hind — Arrival of Dr. Schultz — XVlll CONTENTS. The iVbr-TTfister Established — Hudson's Bay Company's Opposition — The Dominion Established — A Demand made for the North-West Territories — Country Systemati- cally Be-littled — Bishop Tache's Book — He sees no Good in the Countiy — Purchase of the Territory — Steamboat on Red River — Dr. Schultz Imprisoned — The Power of the Company Broken — Portage la Prairie — Grasshopper Plagues — Canada Takes Steps to Acquire Possession of the Country — Conflicting Interests — Mutterings of the Storm in the Fall of 1869 — The Claims of the French Half-breeds — Surveyors Stopped by Louis Riel — Hudson's Bay Company and Roman Catholic Fathers Decline to Interfere — An attempt at Independence — Fort Garry given up to Riel — Governor McTavish's Explanation — His Evident Complicity with the Rebels Almost Admitted — His Child- like Simplicity — O'Donohue Joins the Rebels — He Introduces the Fenian Element — His Letter to the Canadian Government — Bill of Rights drawn Up — The Movement is seen in its proper Aspect — Canadians Attempt to break Riel's Power — Their Imprison- ment — Murder of Scott — Arrival of Bishop Tache — Riel changes fi-om a Wolf to a Lamb — Fenian Flag Pulled Down — Arrival of Colonel Wolseley with his Troops, and Flight of Riel and Lepine — Conclusion. CHAPTER XXVI. Ten Years' Reminiscences and Notes on the Various Settlements and Villages. Purport of the Chapter — Manitoba and Winnipeg as They Were in 1872 — Grasshopper Plague— Crop of 1875— Stage Ride in the Winter of 1875— Disappearance of the Grasshoppers — Settlements Extend to the Second Plateau — Nelsonville Founded Wet Seasons Commence — Many Observers Condemn the Country^ Rapid City Com- menced in 1878 — Land in the Neighborhood Rapidly Settled— The Assiniboine Ascended to Fort EUice in May, 1879 — Crowds enter the Country East of Port EUice — Birtle Founded — Rock Lake Settlement — Winter of 1879-80— Odanah and Minnedosa the Rage in the Spring of 1880 — Grand Valley Comes into Notice Stiff-necked and Soft-hearted Immigrants — Mosquitoes Prove too Much for Them — English Ideas of Canadian Kindness — Canadian Notions Regarding Englishmen's Inability to Fall in with the Ways of the Country — No Stealing on the Plains — Settlements North of Birtle — Formation of the " Syndicate" The " Boom" at Portage la Prairie — Winnipeg and Emerson take the Fever — Route of the C.P.R. Changed in the Spring of 1881 — Brandon Founded on the Assiniboine Vigor of the Syndicate — Railway Opened to Brandon — Speculation at Fever Heat Conflict- ing Statements Regarding the Country— Short Notices of Selkirk, Emerson, Portage la Prairie, Morris, Brandon, Rapid City, Minnedosa, Odanah, Birtle, etc., etc. CHAPTER XXVII. Description and History of Winnipeg. Position of Winnipeg— Fort Rouge— Fort Selkirk— The Founders of Winnipeg— Winni- peg in 1870 — Railway Surveys— Pembina Branch— Winnipeg the Outlet of the Inter- ior Trade— The " Boom " in 1881— Statistics of the Trade of Winnipeg— Enumeration CONTENTS. XIX of the Chief Buildings — Present Area of the City — The Business Corporations — City Schools — Former Trade with "Winnipeg — Contrasted with the Present — Railway Grounds and Offioes — Postal Facilities Past and Present — Leading Societies — The Press of "Winnipeg — Agricultural Society — Extracts from Lord Dufferin's Speeches — Geographical Position — Rivers and Lakes of Canada — Mennonites and Icelanders — The Future of the City — Appearance of "Winnipeg to a New- Comer — How Business is Transacted — Preponderance of Males — Occupation of the People — Their Steady Habits. CHAPTER XXVIII. Churches and Schools in the North-West. [A Chapter "Wkitten by G. M. Geant, D.D., Pkincipal op Queen's UsrvEESiTY, Kingston, Ont.] First Settlers in Manitoba Presbyterians — Their Piety — Attachment to the Church of their Fathers — First Anglican Missionaries — Their Zeal and Prudence — High- land Tenacity — Arrival of Rev. John Black — Kildonan Church — Roman Catho- lic Missions — Establishment of Churches and Schools by Missionaries from the Church of England — Rupert's Land Divided into Four Dioceses — One Episcopal Church for Canada — Methodist Missionaries — Rev. George Macdougal — Rev. George Young — Methodist Churches in "Winnipeg — Missions of the Presbyterian Church — Knox and St. Andrew's Churches — A Common Mission Board for the Protestant Churches Required — First School Act — Its Provisions and Amendments on it — Educational Development — Difficulties Caused by Sparse Settlement — High School "Work — Colleges — St. Boniface — St. John's — Manitoba College — Manitoba University — Harmonious Co-operation in it of all Churches and Colleges — Happy Solution of Difficulties Considered Insuperable Elsewhere — Omens for the Future. BoMAH Catholic Missions, by Archbishop Tache's Secretary — Missions' of St. Boniface — East St. Boniface — Colleges — Charitable Institutions. CHAPTER XXIX. Indians of the Prairie and the Forest. The Intention of the Chapter — Extinction of Indian Titles — Enumeration of Different Indian Treaties— Location of the Lands Ceded— General Terms of the "Various Treat- ies — Indian Characteristics — Former Habits— Horse Stealing no Crime — Considered a "Virtue and still Indulged in — How Conducted around the Cypress Hills in ] 880— How I Saved my Horsrs — The Union Jack Versus the Stars and Stripes — Settlers need have no Fear— Indians and their Occupations on Lakes Manitoba and Winnipegoosis — Food, Game, and Furs — Potatoes and Garden Vegetables— Indian Reserve at Fort Pelly— Cote's Medal— Reasons for Marrying More than one Wife— Minnesota Sioux— Gener- ally Hard "Working and Peaceable— Plain Crees— Their Feuds with the Blackfeet— Extract from Palliser— Peace made Ten Years Ago— Big Bear— His Desire for Better Terms— The "Wood Crees— Quiet and Industrious— The Chipweyans as Farmers— Food of the Indian Tribes— The Assiniboines— Anecdotes Regarding their Pecuharities — Conclusion. XX CONTENTS. CHAPTEK XXX. The Western Indians and the North-West Mounted Police. [This Chapter was Weitten by Alexander Begg, Esq.] Indians Previous to 1874 — The Blackfeet — Their Number — Eeport of Eev. C. Scollen in 1876 — "Whiskey Traffic Destroys Many— Small-Pox — Eesults of Illicit Liquor Busi- ness—Mounted Police to the Rescue — Treaty in 1877 — Location of the Tribes — Instructors in Agriculture and Stock-Eaising— Text of Treaty — Yearly Subsidies — Ammunition — Salary of Teachers Paid — Supply of Tools, Stock, and Agricultural Implements — Agreement on Part of Indians — Success of this Policy — Opinion of Lord Lome — Conduct of Hudson Bay Company Eulogized — Also that of Mounted Police — Increase of Latter to Five Hundred — Cost of Indians and of Police — Officers of the Force — New Headquarters. — Indian Question still a Delicate one — Extract from Toronto Mail — Account of Distribution of Food — Contractors for Food Supply. CHAPTER XXXI. Steamboats and the Development of our River and Lake Navigation. First Steamboat on Eed Eiver — Attempts to Establish a, Trade — Want of Success — Opening of the Northern Pacific— Eegular Trade Established on Eed Eiver in 1872 — In Three Years it Increases to 50,000 Tons — Doubts cast on the Navigation of the Eed and Saskatchewan Elvers in 1876 — Mr. Trow's Statement made in 1877 — Eed Eiver Fleet in 1879— Navigation of Lake Winnipeg — Assiniboiue Opened up — Its Capacity and Present Facilities — The Qu'AppeUe and Souris — The South Saskatche- wan — North Saskatchewan — .Steam Navigation on the Athabasca, on Peace Eiver, on the Mackenzie — Lake Athabasca and Great Slave Lake — Impediments to Naviga- tion — The Future of the Lake and Eiver Trade — Summary of Navigable Waters. CHAPTER XXXII. The Past, Present, and Future of our Railway Systems. PalUser's Expedition — His Eeport on the Country and Mountain Passes — Canada acquires the Hudson's Bay Company's Territories — British Columbia unites with the Domin- ion — Sandford Fleming appointed Chief Engineer — Yellow Head Pass — Trip of the Chief Engineer — My trip to Peace Eiver — " Ocean to Ocean " published — My report on the Flora and Climate — Continuation of the Surveys — My second Eeport — Called before a Committee of the House — My third Eeport considered Extravagant — Surveys draw to a Close — Diverse Opinions regarding the Country — My views regarding Peace Eiver Confirmed — Exploration of the Buffalo Plains — Sir Charles Tupper Endorses my Staternents — A General Awakening as to the Value of the Country — Eailway Commu- nication Effected with Winnipeg — Formation of the " Syndicate" — Eeview of the Surveys and their Eesults — ^Constraction of the Lake Superior Branch — Lines Snr- CONTENTS. XXI veyed — Cost of Surveys — Increased value of the Country — " Syndicate " carry the £oad South — Brandon Located — Lines Located by the " Syndicate " — Lines in Opera- tion — South Western Colonization Railway Company — A net work of Railways Contemplated— Only Two Outlets Calculated at Present— The Future Traffic— The Nelson River Route — The Churchill and Saskatchewan Route — Prince Albert and Peace River — The Great City of the Future. CHAPTER XXXIII. Advice to Immigrants both as Regards Beaching the Country and What to do when They get there. Where Information can be Obtained — Fare to Canada — Articles Required on the Voyage — From Whom to get Information — A Government Officer at each Ship- ping Port — How to Label Bonded and other Goods — How to Act on Board Ship — Articles Needed for the Voyage — Household Articles to be Bought — Mechanics' Tools — Farmers Should bring no Furniture— Warm Clothing to be Brought — Routes from Quebec to Manitoba — Agent at Duluth — Agents in Manitoba — Fare from Quebec to Manitoba — Carrying Heavy Freight a Mistake — Agents' Duties — Dominion Land Offices — Correspondence with Officials — How to Address Letters — Points to be Noted — Cautions to Immigrants — No Purchase of Homestead Land Valid until Title is Obtained — All Titles or Assignments should be Registered at Ottawa — Bounty War- rants and Land Scrip — Duties of Homesteaders — Make Entry of Homestead as soon as Possible — See that no One has any Claim to the Land Selected — Titles to all Lands Purchased should be Examined into — Land Guides will Assist at Selections of Lands — How to Select Good Land — How to get Good Sweet Water — Hay and Wood Secon- dary to Good Soil and Water — Spring best Time to Emigrate —Good Crops Raised on Spring Ploughing— New Plan of Sowing in Spring — Old Country People should fall into the Ways of the Country — Deep Ploughing in Manitoba a Mistake— How to Bring Money and Where to Place it— Illustrations of How much can be Saved in Five Years— Success Depends on the Settler— Canadian North-West Compared with Dakota and Minnesota — Opening of Canadian Pacific Railway— Statements of Settlers Regarding Outfit — Mode of Procedure— Prices— Amount of Money Necessary— Success in Fanning — Climate — Wintering Cattle, Oxen, and Horses — The Kind of Settlers Needed. CHAPTER XXXIV. Advice to Settlers and Travellers. Protection against Sudden Storms in Winter— Thunder, Rain, or Wind Storms in Sum- mer—How to Protect Horses and Cattle from Flies— Smudges— Keeping the Tent Clear of Mosquitoes — Care of Horses when Travelling — How to Find Lost Horses — Precautions to be Used— Where to Pitch a Camp in Summer— In Winter— How to Find Water— How to Know Sweet Water— Protection against Prairie Fires— Saving Hay and Fences—How to Travel Over the Prairie With or Without a Eoad— White Mud Swamps— Carelessness of Travellers as Regards their Personal Comforf^How to Pre- vent a Prairie Fire— Penalty for Starting One— Crossing Streams with Bridges— How- to Cross, &c., &c . XXll CONTENTS. CHAPTER XXXV. North-West Land ' Regulations and Mode of Survey. Inauguration of the Surveys — The International Boundary — Principal Meridians — Size of Townships — Numbering of Ranges and Townships — Base Lines — Correction Lines — Size of Townships — Road Allowances — How Survey Lines .are Marked on the Ground — Dominion Land Regulations — Diagram showing the Division of a Township into Sections— General Regulations— Homesteads and Pre-emptions — Colonization Plan Number One — Plan Number Two — Timber for Settlers — Pasturage Lands — General Provisions — Canadian Pacific Railway Lands— Conditions of Sale — Liberality of Canadian Land Regulations — Hudson's Bay Company's Lands — School Lands — Lands at Private Sale. CHAPTER XXXVI. Statistics. Populatioi} of the Dominion in 1881 as Compared with that of 1871 — Population of the Cities and Towns — Place of Birth — Religious Belief. — Areas of the Provinces, etc. ^^d m 'XT PHOTO LITH BY THE aURLANO LiTtI CO MONTREA(_. BIRDS* EYE VIEW OF WINNIPEG. MANITOBA AND THE GREAT NORTH-WEST. CHAPTER I. General Oeograjphy. The Dominion as a whole — Its Extent and Area — Nova Scotia — New Brunswick — Prince Edward Island — Quebec — Ontario — Keywadin — Manitoba — Nori;h-West Ter- ritories — British Columbia — North-West and Manitoba a vast. Plain— Southern or Prairie Section — Middle or Partially Wooded Section — Region of Continuous Forest — Basin of Lake Winnipeg — Its Rivers and Lakes — Mackenzie River Basin — The Churchill and Nelson Rivers — General View of the Rocky Mountains. The Dominion of Canada includes at present all British America, except Newfoundland, which still elects to re- main a Crown colony. Beginning at the East, it includes the Provinces of Nova Scotia, New Brunswick, and Prince Edward Island. These were formerly called the Maritime Provinces. Upper and Lower Canada are now Ontario and Quebec. Manitoba and the North-West Territories extend from the boundary of Ontario to the crest of the Rocky Mountains, and west of this range and the 120th Meridian lies British Columbia, which includes the two old Crown colonies of Vancouver's Island and British Columbia. This vast dom.ain extends from the Atlantic to the Pacific, and is equal in size to the United States, or a square of 1,770 miles. It includes about 3,000,000 square miles. The Province of Nova Scotia consists of the Peninsula of Nova Scotia and the Island of Cape Breton. These lie to the south-east of New Brunswick and Prince Edward Island, and form the most eastern part of the Dominion. The Peninsula of Nova Scotia is of a triangular shape, and 2 18 MANITOBA AND THE GREAT NORTH-WEST. is connected with New Brunswick by an isthmus sixteen miles wide. Its surface is undulating and picturesque and is dotted over with many small and beautiful lakes, which contain multitudes of fine fish. Nova Scotia is rich in minerals, having no less than three extensive coal fields, which are destined, owing to the fostering care of its Government, at no distant day, to be a large source of revenue to the Province, as it owns the mines and receives a royalty on all coal taken from them. Iron, gypsum, and gold are not only abun- dant, and a source of present wealth to many, but hold out future prospects of large returns for foreign invest- ments. The best agricultural lands of Nova Scotia are situated at the head of the Bay of Fundy, though the soil almost everywhere is good. Nova Scotia has been long noted for its apples, of which vast quantities are shipped to England. Halifax, the capital of Nova Scotia, is situated on one of the finest harbors in America. Owing to its proximity to the Gulf Stream, the harbor rarely freezes over. This fact and the position of the city as the terminus of the In- tercolonial Railway have made Halifax the winter port of the Dominion. Owing to the excellent construction and management of the Intercolonial, it is fast growing in favor with the travelling public. Besides farming and mining, a large number of the in- habitants are engaged in the coast and deep sea fisheries, which are very remunerative. Ship-building is exten- sively carried on and gives employment to numerous mechanics and others. On the whole, taking into con- sideration its mining, fishing, farming, and ship-building. Nova Scotia can support a far larger population in afiiuence than she now possesses. New Brunswick lies northwest of Nova Scotia, and has many points in common, but differs in shape, being very GENERAL GEOGRAPHY. 19 compact and little broken by narrow bays. Numerous large bays indent its coast on the side of the Gulf, and here ship-building and lumbering operations are extensively carried on. The surface of the Province is very much diversified, and mountain and valley, noble rivers and clear lakes follow each other in quick succession through- out its whole extent. Much of the surface is still covered with forest, but along the rivers and in the valleys excel- lent farms and farming lands are to be seen. • This Province possesses three fine rivers which add much to its value, as by means of these the timber cut in the forests can be floated down to the sea or used in the construction of ships for which New Brunswick is justly noted. The St. John is 450 miles long, and is navigable from Fredericton, the capital, to its mouth, a distance of eighty -four miles. Small steamers ply on the river above the city for 1 20 miles further, or up to the Great Falls,' which are eighty feet high. The Miramichi is 225 miles long and navigable for thirty miles from its mouth, which is very wide, and here many large ship-building establishments are located. The Resti- gouche is 200 miles long, and forms the boundary between Quebec and New Brunswick. Both the latter rivers flow into the Gulf of St. Lawrence, while the St. John empties into the Bay of Fundy. Like Nova Scotia, New Brunswick possesses mines of coal and iron, and she has also abundance of lead, asphalt, granite, marble, and other valuable minerals. Besides timber and ships, her exports are grain, fish, iron, coal, lime, and gypsum. The resources of the Eastern Pro- virices have of late been greatly developed, and their trade is every month increasing in volume. Prince Edward Island is very fertile and possesses a sa- lubrious climate. Its inhabitants are chiefly engaged in fat ming and fishing, and are well repaid for their labor in both cases. The island is crescent-shaped, about 130 miles 20 MANITOBA AND THE GREAT NORTH-WEST. long, with an average breadth of thirty-four miles. In general the land is very, level, and being free from rock is easy of tillage and very productive. Immense quan- tities of potatoes are raised and exported to Boston and other cities along the coast, where they bring ready sale at remunerative prices. The climate of all three Provinces is alike as regards the autumn, which is delightful in the extreme. Nova Scotia has less extremes of heat and cold, but is more subject to chilling fogs than either of the others. New Brunswick has cold winters and late springs, but the summers are warm 9,nd growth is rapid. Owing to the insular position of Prince Edward Island, its climate is less liable to extremes than that of the other Provinces. As a rule, the air is dry and bracing, the winters are cold and the summers tempered by the sea breezes. Quebec may be said to lie in the valley of the St. Law- rence. It extends from the mouth of the river to some distance west of Montreal. The 45th parallel separates it from the United States, while the Ottawa river is its boundary on the side of Ontario. Since its disco- very, Quebec has been noted for its vast Pine forests, its noble rivers and lakes, and its magnificent scenery. The increasing trade of Montreal, owing to the develop- ment of the west, has caused business men to bestir them- selves, so as to retain the traffic that is flowing to their doors, and a consequence of this action is the development of their railway system by which they are in communica- tion with all points of the compass. The St. Lawrence has been deepened, and vessels drawing twenty feet of water come to Montreal to load. Besides the Western trade in grain and other products, the Ottawa and its various branches send large rafts of timber to Quebec, from whence it is exported to England. Much fertile land is to be found in Quebec, especially in GENERAL GEOGEAPHY. 2l the Eastern Townships and in the Ottawa valley, £ind there are large deposits of iron, copper, and lead, which are worked with success in many parts of the Pro- vince. Many other minerals of use in the arts are obtained, but of late years, none have been more talked of than the Phosphate mines, north of Ottawa. Gold is obtained by washing in many streams to the south of the St. Lawrence, the principal of which is the Chaudiere, near Quebec, where for a number of years, gold washing has been carried on. Ontario presents the appearance of a triangular penin- sula, and is bounded on the south and southeast by Lakes Erie and Ontario, and the Riv6r St. Lawrence, and on the west by a line still undefined. To the north and northwest, there are immense forests, which are now, and will be for years to come, a source of great wealth to its inhabitants, as all the public lands belong to the people of the Province. The surface rises in no place into what may be called a mountain, but, as a rule, the whole of the country is un- dulating, and where not encumbered with rock, fit for the plough. It is only along Lake Superior and the Georgian Bay, where high rugged hills and precipitous cliffs give a barren and desolate aspect to the scenery that other than fertile lands can be seen. The Laurentian Hills run west- ward from the Thousand Islands, below Kingston, to the Georgian Bay, and continue northwestward by Lake Superior to the Lake of the Woods and Lake Winnipeg. North of this line of hills the country, instead of being continuously fertile, is much broken by rocky ledges, small lakelets, swamps, and sandy tracts ; but, nevertheless, there is still much fine rich land throughout this region, and experience proves that the farmer can plough up to the rocky ledge without any difficulty. All the rivers of Ontario flow either into the St. Law- rence or the Great Lakes. Owing to the diversified charac* 22 MANITOBA AND THE GREAT NORTH-WEST. ter of the country, these are numerous, but unimportant as regards internal communication. Besides rivers, many- beautiful spring brooks traverse the country in all direc- tions, and these connecting with multitudes of small lakes filled with the best of game-fish, enable the sportsman or farmer to have pleasure or profit, or both, without going far from home. The small clear streams spoken of are now be- coming of great value and will be increasingly so in the future. Within a few years, cheese factories have become very numerous, and the manufacture of cheese a leading industry. Soon butter factories will be added, and then Ontario's rich pastures " by the brooks " will be valued as they should, and grain raising become a thing of the past. Water power sufl&cient to grind all our wheat and manu- facture all our clothing has been going to waste for ages, but now the spirit of enterprise has taken possession of our people, and manufacturing establishments are rising on every hand. On the Trent alone, there are over twenty miles of rapids, where innumerable mills could be erected for every purpose. At present, the Government contem- plate the formation of a canal by means of this river, to connect the waters of Lake Ontario with the Georgian Bay, so that the grain of the West may find a sure and speedy transit to the East. Should this c^nal be built, manufacturing towns will, as a matter of course, rise along its track, and the dream of many will be a glad reality. To the capitalist, there is no better field on the American continent for investment, than is presented by Ontario to-day. Minerals 'of almost every description are abundant in the Laurentian Hills. Silver mining on Lake Superior, gold mining in Madoc, iron mines in various places, of surpassing richness and great extent, would surely place Ontario in a prominent position as a mining country, yet these are not all ; on the shores of Lakes Huron and St. Clair are large GENKKAL GEOGRAPHY. 23 deposits of salt and petroleum, which seem well nigh inex- haustible. Northeast of Kingston, phosphate is found everywhere. Lead, gypsum, marble, copper, graphite, lith- ographic stone, and numerous other metals and minerals exist in workable quantities in many places, but hitherto, the want of capital has prevented their development. Of the fruits of the soil, Ontario may justly be proud; her apples to-day stand A 1 in the English markets. Peaches and grapes are grown in enormous quantities, and the latter are now raised without difficulty in everj'^ part of the Province. Barley grown along Lake Ontario is alto- gether superior to anything that can be produced in the United States, and always commands a good price. All other grains are raised in abundance. Ontario wheat has long been known as a first-class article, and is only excelled now by that of its sister Province, Manitoba. Keywadin is a tract of rough, broken country, lying between Ontario and the North-West Territories. Its southern boundary is the United States, and its northern the shores of Hudson's Bay. This region is but little known in its eastern part, but may be characterized as a land of rocks, lakes, rivers, marshes, and muskegs, with occasional Islands, or small patches, of good land intermixed. Along Kainy River, there is a belt of very rich land, but this is overshadowed at present by the fertile lands of Manitoba, which fill men's minds to the exclusion of everything else. The boundary question is not yet settled, but when it is, Keywadin will pass out of existence and become merged in Ontario and Manitoba. Manitoba, by the Act of 1880, had its boundaries ex- tended, so as to include the greater part of the existing settlements formed, during the past few years, along the western boundary. As now extended, it reaches from the Ontario boundary on the east to 101" 30' west long.. 24 MANITOBA AND THE GREAT NOETH-TTEST. and from the International Boundary on the south to the Saskatchewan and Lake Winnipeg on the north. The North-West Territories extend from Manitoba westward to the crest of the Rocky Mountains. Where the Rockies cross the 120th Meridian, that line is taken as the eastern boundary of British Columbia. All the vast tract enclosed between these lines and extending indefinitely to the north, is known by the general term of North-West Territories. British Columbia is that portion of the Dominion which extends from the western boundary of the North-West Territories to the Pacific, and includes Vancouver Island and Queen Charlotte's Islands. Its west- ern boundary is the Pacific, from lat. 49° to the head of Portland Channel, in lat. 56°. From this point, the line passes at a distance of twenty-five miles from tide water, northwesterly, until it reaches the 143rd Meridian. The 60th parallel is its northern boundary. As a separate chap- ter will be written on this Province, I shall merely notice that, were it for no other reason than its position, British Columbia is a necessity to the Dominion. Besides posi- tion, it has forests of unsurpassed excellence, fisheries with- out a rival, coal fields unequalled on the West coast, a climate at once mild and salubrious, and rivers flow- ing over " golden sands." It is well known that from its southern boundary to its most northern explored point, gold in paying quantities has been found. The North-West Territories and Manitoba may be char- acterized as a vast plain, gentlj^ sloping to the north and northeast. Its southeastern extremity (at Emerson), is about 700 feet above the sea, and rises gradually as we proceed west, until it reaches an altitude of nearly 4,000 feet at the base of the Rockies, on the International Boun- dary. Lake Winnipeg, which receives the waters of the interior is only 627 feet above the sea. It will be seen that from the Rocky Mountains to Lake Winnipeg, a distance, in GENEKAL GEOGRAPHY. , 25 round numbers, of 1,000 miles, the fall is about 3,000 feet, or three feet to the mile. In this 1,000 miles there are two lifts, of over 600 feet each, which serve to divide the prairie country into three great subdivisions, having the same general characteristics. Under the name of the First Prairie Steppe, is included the low plain of Manitoba, bounded by a line of elevated country which commences on the International Boun- dary, at a point some distance west of Emerson, and extends northwestwardly under the names of Pembina, Riding, Duck, Porcupine, and Pas Mountains to near Cum- berland House, on the Saskatchewan, in long. 102° west and lat. 53° 37' north. This plain, in its southern part, being more elevated, is drier and better fitted for agricul- ture than the northwestern part, where Lakes Manitoba and Winnipegoosis and their surrounding marshy lands take up much of the surface. The soil, however, in the northern part is exceedingly rich, and marshy meadows covered with tall grass, take the place of the weedy or grassy prairies of the south. The soil of this lower plain is a dark-colored or black alluvium of great depth and almost inexhaustible fertility. Ascending the broken hills, or face of the escarpment which is the eastern slope of the " Mountains " spoken of above, the traveller is surprised to find that the " Moun- tain " has disappeared, and he stands on a plain almost as level as the one left behind, but much better adapted to farming purposes, as the soil is warmer, the surface more rolling, and therefore drier, and water of a better quality and more plentiful in the form of brooks. This is the Second Prairie Steppe, and contains an enormous quantity of excellent land. Its boundary on the east has been already described, and the International Boundary, for 270 miles, is its south- ern one. The Coteau de Missouri, crossing the Boundary 26 MANITOBA AND THE GREAT NOETH-WEST. in long. 103° 30' west, sweeps up to the northwest and crosses the South Saskatchewan in lat. 50° 45', where it takes the name of the Bad or Bear Hills. Passing north- ward it becomes the Eagle Hills, about fifty miles to the east of Battleford. This range of hills is about ten miles to the south of Battleford, in lat. 52° 35', and from thence the elevated country extends northwesterly to Lac la Biche, in lat. 55°. Groups of drift hills are scattered at intervals over this plateau, but anything to be called a mountain has no ex- istence. The Turtle and Moose Mountains, Brandon Hills, Pheasant Hills, File Hills, Touchwood Hills, and other small groups found at various points can scarcely be called hills. They are in most cases merely t, series of ridges, and rounded drift eminences encompassed by marshes and lakelets, which prevent the destruction of their forests at uncertain intervals. Therefore the wood ranges on them from mere twigs of a year old, up to trees eighteen inches in diameter. The Third Prairie Steppe, or Lignite Tertiary Plateau, is bounded on the east by the western boundary of the pre- ceding one, and includes the remainder of the great plain south of Lac la Biche. Wood Mountain and the Cypress Hills are both on this plateau, and deserve the name of hills, the latter even that of " mountain," as the western part attains an elevation of 4,000 feet above the sea, or 2,000 feet above the plain to the north. This section of the country is more broken than the others, and large tracts are better suited for pasturage than for the plough. Salt lakes and ponds, rolling hills, alkaline flats, deep ravines called coulees, and rivers flowing in deep channels, are the leading features of the district. Cactus flats, hills of pure sand, and large areas of excellent agricul- tural lands will attract the attention of different observers, so that varied and conflicting accounts are being and have been given of it. GENERAL GEOGRAPHY. 27 Leaving out the areas covered with gravel, or which consist principally of drifting sand, the remaining level country will sooner or later become farming lands, and the broken country pasturage. It is within this area that all, or nearly all, the coal exposures noticed in this book are to be found, and as a rule at no great distance from the surface. Ninety per cent, then of the first two areas consists of excellent soil. On the third steppe are areas such as the one south of Battleford, where 10,000 square miles of good land may be found in one block. Further inves- tigation is required before the more southern part can be definitely described. That part of the prairie lying west of Moose Mountain, and a line connecting it with the Touchwood Hills, may be said to be wholly without wood, between the Boundary and lat. 52° north. Wood Mountain and the Cypress Hills, together with the narrow river valleys, are the only ex- ceptions. Although at present without wood or even a bush for more than one hundred miles at a stretch, yet the only cause of this absence of trees is the ever recurring fires which burn off the grass and shrubby plants almost every season. Permanent water in abundance is found where not a willow or poplar twig has been seen for years. Should a range or group of sand hills intervene, shrubbery and even trees are found amongst them, though the plain in the vicinity is without a single twig. It requires very little observation to detect the reason. All fires cease when they touch those hills. Theories regarding an insufiicient rainfall, based on the absence of trees, are fallacious, as all grasses form a sward on every part of the southern prairie, except where the soils are either too sandy, or the opposite — Cretaceous clay. With these exceptions all the surface is covered with grass, though much of it is very short. Passing north of lat. 52° west of the Touchwood Hills, 28 .MANITOBA AND THE GREAT NOETH-WEST. the traveller advancing from the south will notice first little tufts of willows nestling close to the north eastern corner of a little pond of clear water. Still advancing north, he will notice these clumps becoming more common and occasionally showing stems two or three years old; these are soon followed by little poplars, and should a larger pond than usual be seen, a small group is sure to cling to it. Having frequently passed from south to north on the great prairie, and never having seen any change in the mode of arrangement as above briefly described, I came to the con- clusion that the prairie fires explain the absence of wood. In the partially wooded region which lies north of the prairie, ponds are more frequent and often marshes abound. The soil is very rich, and as the newly cleared land produces longer grass, this section and the more northern forest belt along the Saskatchewan were called the " Fer- tile Belt" by Captain Palliser, and others, who merely reiterated his statements. The mixed forest and prairie extending from Rapid City westward, including the Pheas- ant, File, and Touchwood Hills, and the country north of lat. 52° and south of the North Saskatchewan is of this nature. All the surveyors who have located the lands in this mixed prairie and poplar belt complain of numerous ponds and marshes that retard their work and cause them to suffer much from wet clothes while " chaining " in the fall when the water is cold. The broken /roni of prairie and forest land has no defi- nite line either to the north or to the south. The wetter the land towards the south the farther the wood extends in that direction, and the drier towards the north the farther the prairie extends northward. Prairie then means a dry and generally level tract in the north ; and the occurrence of wood towards the south implies an eleva- ted region of ponds and lakelets, as the Turtle and Moose Mountains. GENERAL GEOGRAPHY. 29" Continuous forest extends from the soutli end of Lake Manitoba by the Riding, Duck, and Porcupine Mountains, and northwestward to Fort a la Come, east of Prince Albert. It thence ascends more to the north and follows the height of land south of the Beaver Kiver, and includes the whole valley of the Athabasca and its tributaries. Lake Winnipeg, as may be seen by an examination of the map, is the lower part of a basin, of which the First Prairie Steppe was formerly a part. On the east it receives Winnipeg River, a large and turbulent stream, which discharges the Lake of the Woods and its accumulated waters. Farther to the north, Beren's River flows into the lake, and by means of this stream and the Severn, which flows north, the Hudson's Bay Company kept open a summer route independent of the more regular highway of Hayes River, usually spoken of as the Nelson River Route. At its southern extremity Lake Winnipeg receives the Red River, which at the city of Winnipeg is 900 feet wide, and averages ten feet in depth. Winnipeg is at the confluence of the Red and Assiniboine Rivers, and from its situation must be a city of great importance in the future. The Red River rises in Northern Minnesota, and after forming the boundary of this State and Dakota, enters Manitoba at Emerson. Many people think that because Min- nesota and Dakota are south of Manitoba they must neces- sarily be warmer, but a little reflection shows that the greater altitude more than compensates for the higher latitude. Manitoba is actually warmer, both in winter and summer, than either Northern Dakota or Minnesota. In ascending the Assiniboine we have, in succession, the Souris and Qu'Appelle, both draining a very extensive region, which is nearly all prairie, and both flowing in deep narrow valleys through the Second Prairie Steppe. On the north side of the river we have the Little Saskat- chewan and Bird Tail Creek, both taking their rise in the 30 MANITOBA AND THE GREAT NORTH-WEST. Riding Mountain. Farther to the north, Shell River, a rapid stream rising in the Duck Mountain, enters from the east ; about fifty miles above, the White Sand, which is really the main river, enters from the west. On the west side of Lake Winnipeg another Little Sas- katchewan is found, and this apparently insignificant stream drains an area of not less than 30,000 square miles. All surplus waters of Lakes Manitoba and Winnipegoosis empty by it into Lake Winnipeg. What this means will be understood by simply enumerating the rivers that flow into Lakes Manitoba and Winnipegoosis, and considering that the only outlet of these is by this Little Saskatchewan. The White Mud River enters the head of Lake Manitoba and drains much of the wet country crossed by the C. P. R. between Portage la Prairie and the " Big Plain." It is worthy of note that this river rises quite close to the Assini- boine and flows northeasterly. Mossy River discharges Lake Dauphin ; Pine River and two others drain the eastern slopes of the Duck and Riding Mountains. Swan River, a large stream 300 feet wide, drains the Porcupine Mountain, and, greatest and last of all, the Red Deer River enters the head of Lake Winnipegoosis, and with its tributaries drains the whole country as far west as the 106th meridian. All the waters flowing into the great Saskatchewan come from the Third Prairie Steppe, except the Carrot River, which runs parallel with the Red Deer River and enters the Saskatchewan near Cumberland House. The main affluents all take their rise in the Rocky Mountains, and uniting on the plain become one mighty river. Thus the South Saskatchewan is formed by the union of St. Mary's, the Belly, the Bow, and another Red Deer River, which rises in the Rocky Mountains and joins the main stream about long. 110° west and lat. 51° north. Below this the river widens, and at the Elbow, near the source of the Qu'Appelle, GENERAL GEOGRAPHY. 31 is 1,848 feet wide and with a channel ten feet deep. The only streams which do not originate in the Mountains are Strong Current Creek and Maple Creek, the latter draining the west end of the Cypress Hills, while the former receives the waters of the eastern end. The chief tributaries of the North Saskatchewan are Battle Eiver, which enters at Battleford, and the Brazeau, which it receives southwest of Edmonton. The Mackenzie Kiver drains an immense area, both east and west of the Rocky Mountains, and pours a mighty flood into the Arctic Sea. Its great southwestern branch — the Peace Eiver — takes its rise on the west side of the mountains, and flows northwesterly along their western base to lat. 56°, where it receives the Finlay Branch, which drains a large area in the northeast of British Columbia. The united stream now turns east and, after a course of nearly seventy miles, emerges from the Eocky Mountains. It flows through the plateau east of the range, in a channel 1,000 feet below its level. Turn- ing more to the north, it sweeps in majestic curves through a rich and fertile plain, which constantly dimin- ishes in altitude as the river gets to the north and north- east. For 770 miles it flows through a most lovely and fertile region, receiving in its course many rivers, the most notable of which are the Smoky and Pine, which drain the district of country lying between the Peace and Athabasca. When the river leaves the mountains, its channel is under 500 yards in width, but before it enters Slave Eiver, twenty-five miles north of Lake Athabasca, it is over 1,000 yards wide. A branch stream, named the " Quatre Fourches " Eiver connects it with Lake Athabasca, and by this stream, in early sum- mer, there is a steady flow of water into the lake, but in autumn this is changed, and the waters of the Lake flow into the river. The author found this to be the case in 32 MANITOBA AND THE GREAT NORTH-WEST. August, 1875, when there was a strong current flowing from Lake to River. Lake Athabasca is about 250 miles long, by some twenty- five in breadth, and receives the drainage of a very exten- sive region, which is almost wholly covered with forest. The Athabasca River, which enters the western end of the lake, takes its rise in the Rocky Mountains, close to the sources of the Columbia, and flows in a general northeast course, till it enters the Lake. In its course, it receives the Macleod, Pembina, and Lac la Biche Rivers from the south, while on the north it receives Little Slave River, which, after a course of fifty miles from Little Slave Lake, empties into it a little north of lat. 55°. Little Slave Lake is an extensive sheet of water lying nearly east and west, about seventy-five miles in length and five in average breadth. In lat. 57°, the Athabasca receives the Clearwater — a fine stream of pure water which comes from the elevated coun- try east of Portage la Loche. Lake Athabasca discharges its accumulated waters by Slave River which, twenty-five miles below, receives the Peace, and both, under the former name, discharge into the still larger basin of Great Slave Lake. At the efflux of this lake, the real Mackenzie commences. At Port Simp- son, in lat. 61° 50' north, it receives the Laird from the west, some of the branches of which have their rise close to the sources of the Finlay, far west of the Rocky Mountains. It is on the upper waters of the Liard, that the rich gold fields of northern British Columbia are located, where hundreds of miners are engaged every summer. After receiving the Liard, the mighty flood, increased in volume and power, flows on, without break or obstruction, to the Arctic Sea, a distance from Fort Simpson of 700 miles in a straight line. A little south of the Arctic Circle, Great Bear Lake River enters from the east. Here was Fort Franklin, where the Arctic explorers wintered. North GENEEAL GEOGRAPHY. 38 of the Arctic Circle is Fort Good Hope, the most northerly of the Hudson's Bay Company's posts in the North -West. The Churchill and Nelson are the great Rivers of Hudson's Bay, and enter its southwestern extremity ; the latter about lat. 57°, while the mouth of the other is more than a degree further to the north. The Churchill^ under the name of the Beaver River, rises in the high lands, north of Fort Edmonton, and flows generally eastward to the meridian of Fort Carlton when it turns north and flows into Tsle la Crosse Lake. This lake also receives the drainage of that extensive region lying northwesterly towards Portage la Loche. From this lake, under the name of English River, it flows easterly through a chain of beautiful lakes, connected by more or less rapid dis- charges, and often bordered by cliff's of Laurentian g;iiess. Before receiving the " Great River," which discharges the waters of Rein-deer Lake, it turns northeasterly, and, keeping the same general direction, enters Hudson's Bay nearly 100 miles farther north than the Nelson. Owing to the peculiar character of the region traversed by this river, its waters are quite clear, and in marked contrast with all the other western rivers. Before it re- ceives the Little Churchill, it is one-third of a mile wide, but below that it widens out to nearly a mile. Nelson River discharges the surplus waters of Lake Winnipeg, and will be fully described in another place. The Rocky Mountains are the only mountains of the North-West. It is true that groups of hills and so-called mountains are occasionally met with, but nearly all these are composed of gravel and sand, and with the exception of the Cypress Hills, are very slightly elevated above the plain. The Rockies cross the International Boundary about the 114th Meridian, and run northwesterly, being in lat. 56° north on the 122nd Meridian, and ten degrees farther north on the 131st Meridian. They form one continuous 3 34 MANITOBA AND THE GREAT NORTH-WEST. chain, composed of a number of separate transverse ridges, between which the multitude of small streams that form the large rivers have their sources. The larger lateral valleys receive many of these small streams, and it is up these that the various passes are to be found. The Kootanie Pass to the south, in lat. 49" 30' north is 6,000 feet above the sea. As we go northward, the passes get much lower, so that the Peace River Pass is only 2,000 feet above the sea, while the mountains decrease very little in altitude. Peace River and the Liard are the only rivers which break through the chain. These have their sources in a series of mountains farther to the west. The highest part of the chain in British America, is where the Fraser and the Columbia, running to the west, almost unite with the North Saskatchewan and Athabasca flowing to the east. Here Mounts Brown and Hooker rear themselves to the height of over 15,000 feet, and their glaciers are the sour- ces of those mighty rivers which flow on the one hand to the Pacific and on the other to Hudson's Bay and the Arctic Sea. CHAPTER II. Physical Oeograjphy of Manitoba. Its Situation and Boundaries — Area — General Characteristics — Bed Eirer Prairie—" Pembina Mountain — Wet Country along its Base — Biding Mountain — View from its Summit — Dauphin Lake— Duck Mountain — Lake Winnipeg — Lakes Manitoba and Winnipegoosis — South Western Manitoba — Turtle Mountain — Red Eiver — Graphic Picture of the Prairie near Winnipeg — Fort Garry — Assiniboine River — Land on Assiniboine — Souris River — Snake Creek— Oak Lake — Vicinity Suited for Stock- farming — Sand Hills, at Snake Creek — Little Saskatchewan— Land on Little Saskatchewan — Settlements in its Valley — Shoal Lake — Bird Tail Creek — Surrounding Country — Shell River — Country North to Fort PeUy — Indian Farm — General Character of Soil — ^A Desert changed to a Paradise — Timber for Building Purposes — Where Located — Building Stone — Brick Clays — Water Supply near Winnipeg. The eastern boundary of Manitoba is still undefined, but as originally formed, its limit was the 95th Meri- dian, which touches the Lake of the "Woods. On the south, the International Boundary separates it from Minnesota and Dakota. Its western boundary is about 101° 20' west long., and its northern, lat. 53°. Within these limits is comprised a total area of about 50,000 square miles, but that part of the country in the vicinity of Lakes Manitoba and Winnipegoosis, is low and marshy. Its general character is that of a level plain, sloping gently to the north, and becoming swampy as we approach the lake basins. The greater part is included in the First Prairie Steppe, defined in the preceding chapter. This includes Lakes Winnipeg, Manitoba, and Winnipegoosis, and . the low lying lands in their vicin- ity ; that part of the Eed Eiver Valley, north of the Inter- national Boundary ; and the Assiniboine Valley for twenty- five miles west of Portage la Prairie. The whole of this dis- trict was evidently at one time a lake basin, and the pre- sent rich soils are largely derived from the silts deposited (35) 36 MANITOBA AND THE GREAT NORTH-WEST. during a long series of years, when the present surface was under water. These rich alluviums have been the theme of many writers, and it is not necessary for me to enlarge on their fertility, or capacity for growing grain crops continuously. Suffice it to say that the cause of the poor water and alkaline soil in numerous localities, can be traced, in every instance, to the exceeding richness of the soil, and as long as it retains its salts, so long will it be noted for fertility. The following extracts from the Report of Dr. George M. Dawson, Geologist and Naturalist to the British North American Boundary Commission, will be found of great interest, as giving an exact account of the region in quep- tion from the standpoint of a competent observer : — " Of the alluvial prairie of the Red River, much has already been said, and the uniform fertility of its soil can- not be exaggerated. The surface, for a depth of two to four feet, is a dark mould, composed of the same material as the subsoil, but mingled with much vegetable matter. Its dark color is, no doubt, in part due to the gradual accu- mulation of the charred grasses left by the prairie fires. The soil may be said to be ready for the plough, and in turning the tough thick prairie sod, the first year, a crop of potatoes may be put in, though it is not efficiently broken up till it has been subjected to a winter's frost. When the sod has rotted, the soil appears as a light friable mould easily worked, and most favorable for agriculture. The marly alluvium underlying the vegetable mould, would in most countries be considered a soil of the best quality, and the fertility of the ground may therefore be considered as practically inexhaustible. " The area of this lowest prairie has been approximately stated as 6,900 square miles, but of this the whole is not PHYSICAL GEOGRAPHY OF MANITOBA. 37 at present suited to agriculture. Small swamps are scattered pretty uniformly over its surface, and in some places very large areas of swampy land occur, as will be seen on refer- ence to the large map of Manitoba, lately published by the Government. The greater part of these swamps are, how- ever, so situated as to be easily drained, either into the Red River or some of its tributaries, which are usually de- pressed thirty or forty feet below the level of the surface. At present, the swamps in the vicinity of the settlements are made to yield supplies of natural hay ; and until hay- grass is sown and regularly cultivated, the " hay -swamps" will continue to be a necessary part of the economy of the settler. The wide overflow of these swamps in the spring, when the season is wet, or when the dissolution of the winter's snow takes place very rapidly, is shown by the large area often found to be strewn with the dead shells of fresh-water molluscs, chiefly of the genus Limnaea. " As a measure of the possible agricultural capacity of this great valley, take one-balf of the entire area, or 3,400 square miles, equalling 2,176,000 acres, and, for simplicity of calculation, let it be supposed to be sown entirely in wheat. Then, at the rate of seventeen bushels per acre — which, according to Prof. Thomas, is the average yield for Minnesota — the crop of the Bed River Valley would amount to 40,992,000 bushels. " The wooded area of this lowest Prairie Steppe is quit6 small. The Red River and its tributaries are fringed with trees, of which Oak ( Quercus macrocarpa, var. ) , Elm ( Ulmus Americana), Poplar {^Populus tremuloCdes, etbalsami/era), and Ashleaved Maple {Negundo aceroides), are the most abun- dant. In some places the trees attain a large size, and the Oak woods bordering many of the streams are especially beau- tiful. Much of the best timber has, however, already been culled out, and it is yearly decreasing, without any sys- tematic attempt for its preservation. The steamers running 38 MANITOBA AND THE GREAT NOETH-WEST. on the Red River are among the largest consumers. Away from the immediate borders of the streams, the prairie, though covered with luxuriant sod, is absolutely treeless. It is fortunately the case, however, that the Red River valley is bordered on the east by the forests already de- scribed, and on the west by the wooded district of Pembina Mountain and its northern extensions." The Pembina Mountain is par excellence the ancient beach in the valley of Lake Winnipeg. Dr. Owen describes it as it occurs a few miles south of the 49th Parallel. " After a hot and fatiguing ride over the plains, we arrived an hour after sunset at the foot of the Pembina Mountain. In the twilight, as we stood at our encampment on the plain, it looked as if it might be 800 feet or more in height ; but in the morning, by broad daylight, it seemed less. When I came to measure it, I was somewhat surprised that it did not ex- ceed 210 feet. I observed on this as on many other occa- sions, that a hill rising out of a level plain, appears higher than it really is, especially when, as in this case, the trees on its flank and summit are of small growth. Pembina Mountain is, in fact, no mountain at all, nor yet a hill. It is a terrace of a table-land, the ancient shore of a great body of water, that once filled the whole of the Red River Valley. On its summit it is quite level and extends so, for about five miles westward, to another terrace, the summit of which, I was told, is level with the great Buffalo Plains, that stretch away toward the Missouri, the hunting grounds of the Sioux and the Half-breed population of Red River. " Instead of being composed of ledges of rock, as I was led to suppose, it is a mass of incoherent sand, gravel, and shin- gle so entirely destitute of cement that with the hand alone a hole several feet deep may be excavated in a few minutes. The Pembina River has cut through this material a deep narrow valley, but little elevated above the adjacent plain." Fifteen miles north of the Boundary Line, the PHYSICAL GEOGRAPHY OF MANITOBA. 39 escarpment rises by four distinct terraces one over the other, three of which are from twenty to twenty-five feet high. Beyond this there is a gradual ascent of two miles, covered more or less with boulders, before the level of the next plateau is reached. It runs northwesterly from a point about thirty miles west of Red River, and merges into the Riding Mountain, west of the head of Lake Manitoba. In front of this broken escarpment, there are numerous marshes and pools of water which, north of the Assiniboine, prevent settle- ment for long distances. In rear, or to the west of this marshy tract, sand hills and sandy slopes rise one over the other, until the level of the plateau is attained. This pla- teau is the Second Prairie Steppe. Riding Mountain rises from the lower plain at its south- eastern termination by three successive steppes, each one separated from the other by a gently sloping plateau. The greater part of the mountain is densely covered with forest. On the ridges the soil is dry and gravelly and precisely like that of Pembina Mountain. High above the Pembina Mountain the steppes and plateaux of the Riding and Duck Mountains rise in well defined succession. On the southern and western slopes of these ranges the terraces are distinctly defined ; on the northeast and north sides they present a precipitous escarp- ment which is elevated fully 1,000 feet above Lake Win- nipeg, or more than 1,600 feet above the sea. Standing on the edge of the escarpment of the Riding Mountain and looking in the direction of Dauphin Lake, a gulf, two or three miles wide, and some two hundred and fifty feet deep, is succeeded by two ranges, one lower than the other, of cone-shaped hills covered with boulders. The hills are parallel to the general trend of the escarp- ment. In some places they are lost on the plateaux on which they rest, in others they stand out as bold eminences, showing the extent of denudation which gave rise to them. 40 MANITOBA AND THE GREAT NORTH-WEST. These ranges of conical hills correspond with terraces on the west side of the mountain. Dauphin Lake, lying at the base of the Riding Mountain, is about 750 feet above sea level. It is twenty-one miles long, and twelve miles in breadth. It receives several streams which rise in the Duck and Riding Mountains and discharges its surplus waters into Lake Winnipegoosis by Mossy River, a stream about 125 feet wide and averaging from five to seven feet in depth. This lr.ke is altogether surrounded by marshes which are separated from one another by narrow ridges of dry ground. Northeast of Dauphin Lake is Duck Mountain, a high range of table land similar in every respect to that of the Riding Mountain described above. To the west this range is cut off from the Porcupine Mountain by Swan River which flows in a wide valley between the two ranges. On the west the Assiniboine cuts it off from the great prairie so that it is almost isolated by these two rivers. The " Mountain, " as you proceed from west to east, consists of a series of broken or gently swelling hills very slightly elevated above the plain. These hills are covered with brush, brule, or forest and are extremely difficult to travel through owing to the tangled pea and other vines which constantly retard the footsteps. As the hills are penetrated the forest becomes denser, and before the eastern escarpment is reached^ Poplar, Aspen, and Spruce of large size are very common. Standing on the edge of the escarpment, Lake Winnipegoosis lies at your feet. From this point, over 1,000 feet above the Lake, the view is very fine. As a whole the hills may be considered as forest and the soil uncommonly fertile. Lake Winnipeg receives the waters of numerous rivers, which drain in the aggregate an area of 400,000 square miles The Saskatchewan is its most important tributary. The Lake, at its southern extremity receives the Red PHYSICAL GEOGRAPHY OF MANITOBA. 41 "River, -which, together with its important affluent, the Assiniboine, drains an area of extraordinary fertility and ■extent. In length Lake Winnipeg is about 300 miles, and in several places fifty miles broad. Lakes Manitoba and Winnipegoosis together are nearly as long, and the broad- est part of the first named is not less than thirty miles across. Nearly the whole country between Lake Winnipeg and its western rivals is occupied by smaller lakes, so that between the Duck and Riding Mountains and the western shore of Lake Winnipeg, one half of the country is per- manently covered with water. These lakes are shallow, being seldom over sixty, and often for long distances under ten feet in depth. As to the second Prairie Steppe along the Boundary, or what is now South- Western Manitoba, Dr. Dawson says, at page 287 of his report, " The extreme western margin of the Red River prairie in the vicinity of the Pembina Mountain, is diversified by groves of oak, which stretch out from their base, and would, no doubt, be much more extensively wooded but for the constant recurrence of prairie fires. The front of the escarpment, and its summit, forming the edge of the Second Prairie Steppe, are in some places thickly wooded, and always show extensive patches of timber. The forest covered area increases north-west- ward. In the vicinity of the Line, the woods owe their preservation to the protection against fires afforded by the broken nature of the edge of the escarpment, by the great valley of the Pembina River, and its systems of tributary coulees, and to the frequent occurrence of patches of swamp. Poplar is probably the most abundant tree, though, even after ascending the escarpment, groves of oak are found. The wooded region has, however, in all localities suffered much from local fires ; most of the trees at present living are small, while traces of a former heavy forest growth frequently appear. 42 MANITOBA AND THE GREAT NORTH-WEST. " In some places pretty extensive prairie areas occur between Pembina Escarpment and Pembina River, and witb the exception of a few localities, near the edge of the escarpment, where the Cretaceous Clays are near the sur- face, the soil is of excellent quality, and differs from that of the Red River Valley by the addition of a considerable proportion of sandy material. Swamps are here pretty thickly scattered, and some of them attain large dimensions in spring. Those parts of them which are permanently wet, however, bear luxuriant crops of natural hay-grass, and the general aspect of this region is favorable. "On crossing the Pembina River the eastern margin of the great treeless plain is entered. No woods now appear, except those forming narrow belts along the valleys of the streams, and soon even the smaller bushes become rare. The shrubs met with are generally stunted, from the absence of shelter against wind, and the frequent passage of prairie fires. The little thickets consist, according to situation, of dwarfish snow-berry {Symphori- carpus occidentalis) , Spiroea, roses and willows, fringing the small swamps and pools. The metallic-leaved silver-berry {JElcegnus argentea), comparatively rare in the Red River Valley, now begins to occur in abundance on the drier areas. In the last week of May, 1874, the common flowering plants on this eastern part of the First Prairie Steppe, were : Viola cucullata, V. pedata, Ranunculus rhomboideus, Anemone patens, then going to seed, and the whole prairie covered with its brownish woolly heads; Geum triflorum, found most abundantly near the edge of the escarpment, less common westward ; Astragalus caryocarpus, becoming rapidly more abundant westward, Antennaria plantaginifo- lia, Lithospermum canescens, first blossoms. " The undulating character of the prairie between Pem- bina Escarpment and Turtle Mountain, and the occasional occurrence of stony and gravelly hillocks, has received PHYSICAL GEOGRAPHY OF MANITOBA. 43 mention in the chapters on the drift. With reference to the soil, west of Pembina Eiver, nearly the same remarks apply as to that east of it. It is fertile, though not so deep or inexhaustible as that of the Red River Valley, and rests on a gravelly, drift sub-soil. Swampy bottoms bearing a good growth of hay-grass abound, but their area is quite small as compared with that of the dry ground. Toward the end of the summer, most of these swamps dry up completely, and extensive regions are then Avithout other water supply than that derived from the streams and rivers, which lie in deep valleys, and are often far apart. I do not think, however, that difficulty would be found in obtaining water by wells sunk in any of the lower parts of the prairie. The rainfall of this region is probably slightly less than that of the Red River Valley, but appears to be sufficient for agricultural purposes. It seems probable that at a period not very remote, a great part of this dis- trict was covered with forest trees. The humidity of the soil and climate is sufficient for their growth, and in some places little hummocks, resembling those formed in a forest, and known as "cradle hills," were observed. On approach- ing Turtle Mountain, the tendency of this part of the prairie to reclothe itself, is shown by the recurrence of thickets of seedling poplars on the sheltered sides of the undulations, wherever the fires have not passed for a few years. Between Pembina River and Turtle Mountain, and especially toward the latter place, the deep narrow paths, or ruts, made by the buffalo when travelling, are still quite apparent, though the animal has not been known so far east for many years. They have here a remarkably uniform northwest and northeast direction. " The water of the swamps and ponds of this part of the prairie is generally sweet, but one distinctly saline lake was seen. It had not the thick fringe of grasses and sedges of the other ponds, and here, for the first time, the 44 MANITOBA AND THE GREAT NORTH-WEST. Salicornea was met with in some abundance. There were also many dead shells of Limncea and Planorhis parvus, but whether these molluscs lived in the saline water, or were washed thither from some neighboring swamp, I was unable to determine." The Red River rises in Otter Tail Lake in the State of Minnesota, in lat. 46° 24', and at first flows to the south- west, but in lat. 46° 9' it turns to the north and shortly after enters on the great prairie, through which it cuts its tortuous course, without a break, to its entrance into Lake Winnipeg in lat. 50° 20'. To get a proper idea of the Red River in Manitoba it is merely necessary to imagine a stream from 300 to 600 feet wide, with a moderate current, which has in the course of ages excavated a winding trench or canal to the depth of from thirty to forty feet, in a tenacious clay, through a nearly level country, for a distance exceeding one hundred miles. As the river winds through the plain it forms peninsulas of varying size, and these are generally covered with heavy forest. This remark applies only to that portion of the river from twenty miles south of Winnipeg to Emerson. As the primitive features of the Red River prairie are fast disappearing, and towns and villages springing up in every part, the following extract from the pen of Prof. Hind will be read with interest, as it is a typical descrip- tion of what can be seen, in part, on the great prairies beyond the settlements at the present time. The scene is laid close to Winnipeg. " Here stretching away, until lost in the western horizon, the belts of wood on the Assini- boine rise above the general level, while from the Assini- boine towards the north again is an uninterrupted expanse of long waving prairie grass dotted with herds of cattle, and in the fall of the year with immense stacks of hay. This is the ordinary aspect of the country, comprising that portion of Red River settlement which lies between Mill PHYSICAL GEOGRAPHY OF MANITOBA. 45 Creek and Fort Garry. Remove the farm houses and churches, replacing them on the river banks by forest trees of the largest growth, and the country between Fort Garry and the 49th Parallel, as seen along the road to Pembina, a distance of seventy miles, is continually reproduced in its ordinary aspect of sameness, immensity, and unclaimed endowments. " But it must be seen in its extraordinary aspects before it can be rightly valued and understood, in reference to its future occupation by an energetic and civilized race, able to improve its vast capabilities and appreciate its boundless beauties. It must be seen at sunrise, when the vast plain suddenly flashes with rose-colored light, as the rays of the sun sparkle in the dew on the long rich grass, gently stirred by the unfailing morning breeze. It must be seen at noon- day, when refraction swells into the forms of distant hill ranges the ancient beaches and ridges of Lake Winnipeg, which mark its former extension ; when each willow bush is magnified into a grove, each far distant clump of aspens, not seen before, into wide forests, and the outline of wooded river banks, far beyond unassisted vision, rise into view. It must be seen at sunset, when just as the ball of fire is dipping below the horizon, he throws a flood of red light, indescribably magnificent upon the illimitable waving green, the colors blending and separating with the gentle roll of the long grass, seemingly magnified toward the horizon into the distant heaving swell of a parti-colored sea. It must be seen too by moonlight, when the summits of the low green grass waves are tipped with silver, and the stars in the west suddenly disappear as they touch the earth. Finally it must be seen at night, when the distant prairies are in a blaze, thirty, fifty, or seventy miles away ; when the fire reaches clumps of aspen, and the forked tips of the flames, magnified by refi^action, flash and quiver in the horizon, and the reflected light from rolling clouds of smoke above tell of the havoc which is raging below 46 MANITOBA AND THE GREAT NORTH-WEST. " These are some of the scenes which must be witnessed and felt before the mind forms a true conception of these prairie wastes, in the unrelieved immensity which belongs to them, in common with all the ocean, but which, the everchanging and unstable sea, seems to offer a bountiful recompense, in a secure though distant home, to millions of our fellow men." Fort Garry is situated a few hundred yards west of the confluence of the Assiniboine and Red Rivers. A bridge has been built across the former at this point. Common report makes the river nearly double the width now that it was forty or fifty years ago. At present the breadth is over two hundred feet and this it preserves up to the mouth of the Souris where it is 230 feet wide. Above this point the river decreases in width but increases in depth, and after " the Rapids" are passed, seven miles below Brandon, no other obstructions are met with until we pass Fort Ellice. At this point the river is still 135 feet wide, and for nearly 100 miles, by land, north of this to the mouth of the "White Sand River, its breadth and depth change very little. Fifteen miles above Fort Ellice are the Marquette Rapids which are caused by sand-bars and gravel. The Assiniboine rises in about lat. 52° 20' and long. 103" 15' west, and runs southeasterly to the great southern bend, thirty -five miles west of Brandon, where it changes its direction nearly east and joins the Red River in lat. 49° 54'. The country on both sides of the Assiniboine, for thirty miles west of Winnipeg, is of the same general char- acter as that of the Red River, except that there is much more wood in the vicinity of the Assiniboine, especially on the south. The soil is of the best quality, but owing to the unbroken uniformity of the surface it is very wet in many places, and in a few, as at Bale St. Paul, subject to overflow from the river. Twenty miles west of Portage la Prairie the banks increase in height, the country be- PHYSICAL GEOGRAPHY OF MANITOBA. 47 comes more elevated and sandy and we enter on the Second Prairie Steppe and soon after' reach, the mouth of the Souris. This stream rises near the Squirrel Hills, up north of the great Souris Plain, very near the line of the C. P. R., and joins the southern branch of the river coming from the Coteau. Keeping a southeasterly course it crosses the International Boundary into Dakota about the 102nd Meridian and flows southeasterly to about lat. 48° 10', when it turns again to the north and enters Manitoba east of the 101st Meridian. Its course is now northeast through a level plain supposed formerly to be of no value but now considered the garden of the southwest. North of this the Sand Hills are entered. Plum or Snake Creek discharges Oak Lake, a sheet of waiter several miles broad, which during the summer is the abode of numerous water-fowl of many species. The land around this lake is very rich but much of it is low and marshy, producing enormous crops of hay, and from the presence of timber the whole tract is well suited for stock- farming on a large scale. The low hills about Snake Creek are sand dunes, and on their sides is a lovely Cactus [Mamillaria vivipara), which is quite common in many other localities where sand pre- dominates. The prairie on both sides of the Souris is tree- less, but there is a thin belt of wood, more or less broken, along Snake Creek. The Souris at its mouth is 125 feet wide and about three feet deep. Further up stream it becomes deeper, and, although it is obstructed by rapids near its mouth, report says it is navigable as far south as the Boundary The Little Saskatchewan rises in the Riding Mountains and for over a hundred miles flows through a rich and generally fertile country. The flanks of the Riding Moun- tain are cut up with numerous rivulets. These joining form the Bird Tail Creek and Little Saskatchewan. The latter 50 MANITOBA AND THE GREAT NORTH-WEST. stream issues from the forest through an excavated valley filled with balsam poplar, and an undergrowth of choke- cherry, dogwood, and cranberry, with thickets of roses, raspberry bushes, wild peas, vetches, convolvuli (^Galystegia se]}ium), and wild hops. For the greater part of its course this is the character of the valley, but below Minnedosa and Odanah wood is not so abundant as higher up. All the district drained by this stream is generally fertile but much broken by ponds and hay marshes ; these, however, can be easily drained in most cases, and lands now rejected from this cause will be sought for in the future. Ponds and lakes are numerous ; wild fowl in great numbers visit them every spring and fall, and the river itself abounds in fish of which great numbers are caught in the spring. The waters of the river are beautifully clear and of sufficient depth to float down logs from the Riding Mountains, for the use of the settlers on its banks or the country on either hand. The rising towns of Rapid City, Minnedosa, and Odanah have been located in this valley and the country around is fast filling up with an intelligent and geiierally well-to-do 'class of settlers. Between the Little Saskatchewan and Bird Tail Creek, on the west, is an extensive tract of very excellent land in the midst of which is Shoal Lake, described by a writer in a recent publication as follows : — " Shoal Lake is distant about one hundred and seventy- five miles from the city of Winnipeg. On reaching it, the eye of the traveller is suddenly caught with the view of a magnificent sheet of pure, crystal-like water stretching away to his right some four miles, surrounded by gravelly and sandy shores, and frmged here and there with thick belts of timber, mostly poplar. This is said to be only one of a suc- cession of beautiful lakes stretching from the Riding Moun- tains, some twenty -five miles to the north, to the Assiniboine River about thirty miles to the south. In spring and autumn PHYSICAL GEOGRAPHY OF MANITOBA. 51 especially, myriads of wild fowl are to be seen popping over the surface of these waters, which also abound with fish. All of this, in connection with deer hunting (which can be had within easy distance), affords excellent pastime for the sportsman. The advantages for settlement, particularly for stock-raising, although the excellence of the soil for agricul- tural purposes cannot be doubted, are not only numerous, but strongly inviting. The picturesque and undulating country for many miles around, thickly dotted with bluffs of poplar, with occasional large marshes intervening, afford abundance of both fuel and hay for the settler. There is also a Post-Ofl&ce and mail station, established here in con- nection with the mail line between Winnipeg and Edmon- ton. It is also a station of the Mounted Police, and will no doubt become very soon a place of some importance. The large increasing immigration continually moving westward, will create an excellent market at this point." Bird Tail Creek, a fine stream of pure water, takes its rise in the western part of the Riding Mountain, and enters the Assiniboine some distance east of Fort EUice. This stream passes through a very rich section of country, which is far less broken with ponds and marshes than the tract along the Little Saskatchewan. In its northern part, it is almost all forest, but after the stream leaves the " Mountain," the country becomes more diversified, and prairie and aspen bluffs give it a park-like appearance. The village or town of Birtle is situated on the creek, twelve miles east of Fort Ellice, in the midst of a very rich section, and at present surrounded by fine farms, though the first house was erected in the settlement in 1879. Between Bird Tail Creek and Shell Eiver, m a north- westerly direction, is a magnificent tract of country where a few settlers have gone in, but where there is room for thou- sands. The land is of the very best quality, and there is abundance of wood and water. 52 MANITOBA AND THE GREAT NOETH-WEST. " From Shell Eiver to within ten miles of Fort Pelly, on the left bank of the Assiniboine, is a tract of country un- surpassed for beauty of situation and richness of soil in the North-West Issuing from the Duck Mountain, are numerous streams, which meander through a beautiful and fertile country This area may be said to commence at Two Creeks ten miles from Fort Pelly, thence on to Pine Creek, fifteen miles further. The vegetation is everywhere luxuriant and beautiful from the great abundance of rosebushes, vetches, and gaudy wild flowers of many species. After passing Pine Creek, the trail to Shell River pursues a circuitous route through a country of equal richness and fertility. Shell River is forty -two miles from Pine Creek, and in its valley small oak appears, with balsam poplar and aspen, covering a thick undergrowth of raspberry, currant, roses, and dogwood." Numerous settlers are located in the Shell Eiver country, and all express themselves highly pleased with it. Dur- ing the past summer the writer examined the Indian Farm north of Pine Creek and obtained samples of wheat so fine that they were the wonder of all beholders. About one hundred days ripen wheat in this region, which is between lat. 51° and 52°. The general character of the soil in Manitoba, west of the Pembina Mountain, is a rich sandy loam, often varying to a very rich black loam, and at other times passing into sand as the Souris is approached. In no section of this district is frost injurious, as the land is generally dry and the soil warm. On the Souris Plain, both east and west of Turtle Mountain, the early explorers found short grass and little water and called it a desert. Practical men break up the dry and apparently sandy soil and produce crops that astonish the world. To-day South-Western Mani- toba is called the garden of the Province ; five years since it was supposed to be a barren, irreclaimable waste. PHYSICAL GEOGRAPHY OF MANITOBA . 53 North of the Assiniboine the surface is more broken in many places, the soil is deeper and richer, wood is more abundant, but late-sowed grain is in danger of frost in unshel- tered situations; water is abundant and good, and every requisite for successful settlement is at hand. There is no part of Manitoba where an immigrant cannot find good land, but it is advisable at this early stage of settlement, when land is abundant, to keep clear of wet lands, as drainage at present in most localities on the lower plain is out of the question. Abundance of timber for building purposes can be obtained on the Eiding and Duck Mountains. At present it is floated down the Little Saskatchewan to Kapid City, down Bird Tail Creek to Birtle, where it is sawn into lumber for the use of settlers On Shell River, in the Duck Mountains, there are fine groves of spruce, from which large numbers of logs were cut and floated down to Brandon last year. Around Lakes Manitoba and Winnipegoosis there are quantities of spruce of large dimensions, which up to the present remain untouched, except on the Fairford River, at the outlet of Lake Manitoba, where Mr. Pratt, who owns the saw mill at Totogon, obtains his logs. Pine groves of elm, ash, maple {Negundo aeeroides), bal- sam poplar, with occasional spruce and tamarac, are still to be found in the Assiniboine Valley, and outside of the river flats there are large quantities of fine aspen in many places. Although there exists areas where wood of any kind is scarce, still it is a mistaken notion that there is a general scarcity of wood in Manitoba. Stony Mountain, as its name implies, is largely composed of rock. It is a whitish limestone, lying in horizontal beds of varying thickness, very easily worked and said to be uninjured by frost. As the quarries are only about six miles from Winnipeg, it is of inestimable value to that city. About twenty-five miles above Portage la Prairie, on the 64 MANITOBA AND THE GREAT NORTH-WEST. Assiniboine River, there is a fine outcrop of limestone of another variety, which will be easily worked and ought to be a source of supply for Portage la Prairie and possibly Brandon. A few other localities where rock is exposed have been noted, but up to the present no action has been taken regard- ing them. Up to 1873 no brick clay was supposed to exist in the country, but since that year knowledge in this line has so increased that practical brickmakers now say that "Winnipeg bricks are unsurpassed in any country for hardness and durability. As towns increase, brick clays will be found with- out difiiculty, and each locality will produce its own brick as the variety worked at "Winnipeg is known to exist in other parts of the province. One difiiculty, which has been a serious one in the past, has about disappeared, that is, the power to get good sweet water in "Winnipeg and its neighborhood. At first all wells sunk into the clay invariably gave brackish water, and owing to this the supply for drinking purposes had to be drawn from Red River. Last season a number of wells were bored through the clay into a stratum of gravel below, and in every case good water was obtained. It is now a matter of certainty that excellent water exists in abundance under the clay, and when this is struck and the surface water kept out, pure water will be assured. CHAPTER III. Character of Country between lat. 49° and 50" west of Manitoha. Description of Moose Mountain — Plain from its Top — West side of Moose Mountain — Timter on the Mountain — View from High Hill — Souris Plain — "West of Moose Moun tain — Character of Soil — of Vegetation — of Surface — Great Clay Plain — Its Rough Surface — Scarcity of Water — Wild Eoses — A Visit to the Coteau — Cactus Plain — Wood in the Coteau — Description of Coteau — Resemblance to Turtle Mountain — Ab- sence of Wood — Plateau of Lignite Tertiary — Wood Mountain — Disappearance of the Buffalo. In the preceding chapter we described that part of the Souris Plain lying east and south of Moose Mountain. This "Mountain " is part of an elevated group of drift hills that extend to the northwest, under the name of Weedy, Wolf, and Squirrel Hills. In the distance it presents the same appear- ance as Turtle Mountain, and forms a blue line on the horizon of considerable length. The distribution of wood upon these hills and their environs, presents an exact counterpart of that on Turtle Mountain. The east end of Moose Mountain rises into a somewhat conical peak 340 feet above the gen- eral level, and from it a wide view over the plain to the south and west is obtained. Far as the eye can reach stretches the naked plain, characterized a few short years ago as a barren desert,- but now known to be of wonderful fertility. Like Turtle Mountain this group of hills is com- posed altogether of drift, and incloses numerous lakes of con- siderable size; these lakes are the sources of a few small streams, but in most instances they have no outlet, and in the autumn their water becomes brackish and unfit to drink. Moose Mountain, as seen from the prairie on the east side, rises with a gentle slope and is flanked by marshes extend- ing some miles to the east. Towards the south two or three rounded points are seen rising to a considerable elevation, 56 MANITOBA AND THE GREAT NORTH-WEST. but when the base is reached nothing to be called a hill is visible. On a westerly course we travelled twenty -one miles along the hills, about three miles from the green timber Having penetrated it nearly four miles, I am safe in stating that there are at least 100 square miles of good timber, nearly all balsam and aspen poplar. Occasionally a few small ash and ash-leaved maple appear, but these are of no value There is abundance of water in the hills, nearly one-fourth of the surface being covered by it, but the greater part of it is brackish, being in isolated ponds like those in the Touchwood Hills. Whenever the ponds are connected by an outflow they are invariably good. The others are not, unless fed directly by springs. The whole country to the north of the continu- ous wood consists of ridges, ponds, lakelets, and hay marshes, with very little level land, but the soil is always good, even on the tops of the ridges, which show gravel on the surface. Pits were frequently dug and the black loam was never less than nine inches in depth. Often with pebbles on the surface first-class soil was found for a depth of eighteen inches. From the top of the highest hill, at the northern end of the continuous green wood, a very extensive view of the whole country to the west and north was obtained. To the west the view was bounded by our powers of vision, while to the north numerous bluffs and ridges showed that some of the timber still remained, which had been seen by Palliser and Hind twenty years before. South westward of this region lies the western part of the great Souris Plain, which to the old explorers was a howl- ing wilderness destined to sterility, on account of its light rainfall, scarcity of water, and total absence of wood. This immense treeless expanse, extending from the Souris River, on the 101st Meridian, northwesterly to Moose Jaw Creek, in nearly the 106th Meridian, we crossed diagonally from Moose Mountain to the confluence of Moose Jaw and Thunder Creeks. CHARACTER OF COUNTRY BETWEEN LAT 49° AND 50°. 57 After leaving Moose Mountain, the country, for a few miles, is rather broken by occasional ponds of brackish water and ridges contaiaing a large percentage of gravel. Pro- ceeding westward, the country becomes more level, the soil better, but water scarcer; almost imperceptibly, the tra- veller enters upon a vast plaia, extending to the west and south into the Tiorizon, without a bush or mound to break its uniformity. At first, blue hills are seen to the north, but as days pass, these disappear, and that sense of utter lone- liness comes irresistibly upon him, that travellers crossing the " Great Plains " of the United States have noted. Numerous pits were dug into the soil each day, as we proceeded. As we passed west from Moose Mountain, the country became drier, the grass shorter, and the surface soil more difficult to penetrate. "We never failed to find first- class soil, but about eight inches of it was almost entirely roots and often very hard and dry, but beneath this, at a depth of two feet, it was quite soft. Roots penetrated much beyond this depth. Fire passes over the country every year, and, in 1879, in many places, burned the life so completely out of the roots of the various grasses which have a tendency to grow m clumps, that the following year, scarcely a blade was seen. Although the grass is short the rainfall is quite sufficient, as there is abundance of fresh water ponds, and yet not a shrub over six inches high exists in the country. I speak of the region east of the Qu'Ap- pelle trail, which we crossed in lat. 50° 03'. Before crossing the Qu'Appelle trail, the character of the soil changed. Instead of being a black loam on the surface, of varying depth, with a light colored clay sub-soil, it became more homogeneous, and was generally a strong friable clay with scarcely any water on the surface, but covered with a crop of tall, rich-looking grass, which was remarkably green and fresh. The soil was precisely the same as that I had noted on the great plain, south of Battleford, in 1879. For 58 MANITOBA AKD THE GREAT NORTH-WEST. forty -five miles, we passed over a region which was almost a dead level, and yet so rough, throughout the greater part of it, that our carts were nearly shaken to pieces. Patches of skin were jerked off the necks of the horses, by the twisting caused by the hummocks and hollows. By digging pits into the soil, we ascertained the reason of this extraor- dinary roughness. Although the ground appeared hard and dry, it was not so. In reality, about eighteen inches of the surface was quite soft, and so easily penetrated, that almost without an effort, a spade could be thrust into it up to the head. Beneath this, however, the clay was very hard and dry. All the spring and summer, rain enters the soil quite easily, by means of the cracks surrounding each hummock. These are well described by Dr, Robert Bell, when s[Deaking of another part of this region : — " The clayey ground, in this part of the country, is rendered hummocky and difl&cult to travel over by carts, owing to the fissures produced by dry- ing, in former years. These fissures divide the ground into spaces, usually five-sided, from one to two yards in width. The edges of the fissures, by falling in, have gradually con- verted the intervening spaces into dome-shaped mounds, which are hard and unyielding. These principal hummocks are again divided by minor fissures of more recent date. This kind of surface extends alike over the flat-bottomed hollows and low-swelling hills." The moisture descends almost at once into the soil, by means of these cracks, and owing to the imperviousness of the clay, is retained near the surface, or just below where the soil is friable. The win- ter's frosts expand this moist soil, and instead of these cracks being caused by the sun, they are frost cracks, produced by the heaving of the soil. Clay taken out at a depth of two feet, was generally in little cubes, and it was between the crevices of these that roots penetrated to an unknown depth. With all our exertions, water was obtained on the surface only four times in crossing this forty-five miles, and yet the CHARACTER OF COUNTRY BETWEEN LAT. 49° AND 50°. 59 whole air was odorous with roses which grow on bushes a few inches in height. The prevailing grass of the region was a species of wheat grass (Tnticum), closely related to the quick, quack or couch grass of Ontario, a grass known to be sweet and nutritious. Southwest of this tract, blue hills began to show themselves, but instead of water becoming more plentiful it became scarcer, and with our utmost exertions we could not obtain a drop, so that it was ultimately necessary to deviate from my instructions and proceed to the north. Before I was compelled to do this, however, I left the party encamped, at a water pool, and with two others went thirty miles to the south to locate the blue hills seen in that direc- tion. Ten miles over such a country as I have been describing, brought us to Moose Jaw Creek flowing to the northwest, with banks about ten feet m height^ and breadth about twelve feet The water was very muddy. After crossing it, we came upon another creek of pure sparkling water, which came from the Coteau and emptied into the first, a little to the west of our crossing. Nearly twenty miles over a perfectly level plam, which in places was covered with a profusion of cactus, brought us to the base of the Coteau, at a point near the Cactus HUls. The plain between the creek and the hills was principally Cretaceous clay, and occasional patches of it were without any vegetation, except that peculiar to arid soil. The ravines along the Coteau were filled with wood of small size. Ash, elm, maple, and poplar were the prominent species, but numerous shrubs were like- wise seen. Along the creeks, willow clumps were common but no trees. The lift from the plain to the top of the hills was about 400 feet, and seemed to be the " ruins of an escarpment," as the whole face consisted of a series of slides with the strata tilted at various angles. The plain crossed south of the 60 MANITOBA AND THE GKEAT NORTH-VEST. creek, appeared to be principally composed of the wasliings of the escarpraent, and was nearly level with a very slight dip towards the creek. Dr. Dawson, who carefully examined the Missouri Coteau, thus speaks of it : " One hundred and twenty miles west of Turtle Mountain, the second prairie plateau comes to an end against the foot of the great belt of drift deposits, known as the Missouri Coteau. " The Missouri Coteau is one of the most important features of the western plains, and is certainly the most remarkable monument of the glacial period now existing there. Though frequently mentioned in western reports, I cannot learn that its structure has yet been carefully studied. I have had the opportunity of examining more or less closely that portion of it which crosses the forty -ninth parallel, for a length of 100 miles. "Where cut somewhat obliquely by this parallel, the Coteau may be said to extend for a distance of forty -five miles. At right angles to its general course, however, its extreme width at this point cannot be more than thirty miles. On approaching it from the east, on the trail from Wood End, which, as already stated, is somewhat more elevated than the prairie lying east of it, a gradual ascent is made, till the edge of the Coteau is reached, amounting in a distance of twenty- five miles to about 150 feet. The country at the same time becomes more distinctly undulating — as on approaching Turtle Mountain from the east — till, almost before one is aware of the change, the road is winding among a confusion of abruptly rounded and tumultuous hills, which consist entirely of drift material, and in many cases seem to be formed almost altogether of boulders and gravel, the finer matter having been to a great extent washed down into the hollows. Where it appears, however, it is not unlike that of the drift of the lower prairies, being yellowish and sandy. Among the hills are basin-like valleys, round, or irregular m form, CHARACTER OF COUNTRY BETWEEN LAT. 49° AND 50°. 61 and without outlet, wMch are sometimes dry but generally hold swamps or small lakes, which have frequently been filled in with material washed from the hills so as to become flatbottomed. The hills and valleys have in general no very determinate direction, but a slight tendency to arrangement in north and south lines was observable in some parts of this region. The hills culminate on the line about the 305th mile point, and westward from this point they are neither so steep nor so stony. The country gradually subsides from its rough and broken character, to that of rather boldly undulating prairie, without, however, falling much in gene- ral elevation below the tops of the bolder hills further east. We have, in fact, passed up over the margin of the third great prairie steppe. " The whole of the Coteau belt is characterized by the absence of drainage valleys, and in consequence its pools and lakes are very often charged with salts, of which those most abundantly represented are sodic and magnesic sulphates. The saline lakes very generally dry up completely toward the end of the summer, and present wide expanses of white efflorescent crystals, which contrast in color with the crimson Salicornea with which they are often fringed. The crystal- line crust generally rests on a thick stratum of soft black mud. " The boulders and gravel of the Coteau were here observed to be chiefly of Laurentian origin, with, however, a good deal of the usual white limestone, and a slight admixture of quartzite drift. On the western margin some rather large disused stream valleys were seen, holding chains of saline lakes ; but their relation to the drift materials of the Goteau were not so clearly shown as in other localities further north, to be described. " In passing westward, from the last exposures of the ter- tiary rocks near "Wood End, to the locality of their first appearance within the Coteau, a distance of about seventy 62 MANITOBA AND THE GREAT NORTH-VEST. miles, we rise about 600 feet and attain an elevation of about 2,500 feet above the sea. The slope of the surface of the Lignite Tertiary then, assuming it to be uniform, is a little less than one hundred feet per mile ; and on and against this gently inclined plane, the immense drift deposits of the Coteau hills are piled. " Passing westward for about seventy miles, it is found to preserve much the same appearance. The prairie of the Coteau foot is rather undulating, and slightly raised above the general level, but the edge of the hilly country of the Coteau itself, is always from a distance well defined. To the northward and eastward, boundless level, treeless plains stretch to the horizon. The Traders' Road to Wood Moun- tain, after passmg along the base of the Coteau for the dis- tance above indicated, turns westward and crosses it, taking advantage of a deep bay in its edge, in which also rises a main tributary of the Souris River. The road then passes for about fifty miles through the Coteau belt, which must here be about thirty miles wide, and repeats almost exactly the physical features already described, though in this par- ticular locality neither quite so tumultuous nor so stony as on the line. " Following the Traders' Road westward for about twenty- five miles toward Wood Mountain, it passes for the most part between the southern edge of the Coteau proper, and the northern margin of the Tertiary plateau. Wherever from any hill, a view over the Coteau to the north can be obtained, it is seen to stretch away to the horizon in a suc- cession of wave-like mounds and ridges, which do not differ much in average altitude. " The intervening region, followed by the road on account of its facility, has characters of its own. Wide and deep valleys, often flat-bottomed, with systems of tributary coulees are found everywhere cut in the soft rocks of the foot of the Tertiary plateau. Some have small streams still flowino- in CHARACTER OF COUNTRY BETWEEN LAT. 49° AND 50°. 63 them, fed by the drainage of the plateau ; but for the most part these old valleys are dry or occupied by chains of small saliae lakes, the waters of many of which disappear early in the summer. The lakes usually have the long river-like forms of the valleys which contain them, and receive the waters of the brooks which still flow. One of the most im- portant, probably nine miles in length, forms the drainage basin for the streams of Wood Mountain ; its sides are abrupt and the water appears to be deep. These old valleys are evidently of pre-glacial age, and have formed a part of the original sculpture of the country. The heaping up of the great drift deposits of the Coteau along the foot of the Ter- tiary plateau, has blocked them up, and prevented the drain- age finding its way northward as before. Since the eleva- tion succeeding the glacial subsidence, the rainfall of the dis- trict has never been sufficiently great, in proportion to the evaporation, to enable the streams to cut through the barrier thus formed. The ex;istence of these valleys, and the arrangements of the drift deposits in this region, have impor- tant bearings on several problems connected with its general history." The Coteau resembles Turtle Mountain in its physical fea- tures and like that district would no doubt be thickly wooded but for the prairie fires, which have sometimes run hundreds of miles in the dry weather of autumn. As it is, the want of wood is one of the most serious drawbacks, and animals fed over these hills in summer would require to be wintered in some of the river valleys to the north, or in the wooded ravines of the Tertiary plateau to the south. The plateau of the Lignite Tertiary is for the most part adapted for pastoral purposes, and being covered with a good growth of grass, is well suited for this use. The strip of country between the plateau and the southern edge of the Coteau, partakes in some measure of its character, but has a less favorable appearance. 64 MANITOBA AND THE GREAT NORTH-WEST. One important advantage of this plateau is the existence along its edges of sheltered ravines and valleys, containing groves of poplars. Another is the presence beneath it of vast deposits of lignite coal. In one of these sheltered valleys the Half-breed settlement known as "Wood Mountain is situated. Here there has been stationed for a number of years a large detachment of the Mounted Police, and here too Sitting Bull made his headquarters after the slaughter of the American soldiers under Custer. In past time "Wood Moun- tain was a noted locality, as the buffalo roamed in countless thousands over the wide prairies on every hand, and the hunters had only to kill and eat, as game abounded. All this is changed, and now buffalo are becoming so scarce that in the vicinity of Wood Mountain they scarcely ever appear. V . -J* — — — - ^IPWf l!ii(Pi|p T^^'S vRBRS TSHRvWSr^TO'Wt'W^MS ^At^MWI^^MRkvHAi OF PART OF THE ^mw) #f CHAPTER IV. Character of Country between lat. 50° and 51° West of Mamiioba. Assiniboine below Brandon — Brandon — Assiniboine Rapid — Land near Brandon — Bran- don Hills— Land along the C.P.E.— Flat Creek— Gopher Creek— Land West of Gopher Creek — Pipestone Creek — Weedy and "Wolf Hills — Rich Country along the C. P. R. — Qu'Appelle River — Navigation of the Qu'Appelle — Country North of the Qu'AppeUe — Pheasant Plain, Leach Lake — Very rich Land in this Region — Long Lake — Fish in Long Lake — Waterfowl — Creeks at the Head of Long Lake — Country West of 102nd Meridian — Wood for House building and other Purposes — Country West of Touchwood Hills — Estimate of good Land in Qu'Appelle Valley — UnequaUed tract for Wheat — Early Ripening of Grain — Absence of Summer Frosts — Early Spring— Moose Jaw Creek — Dry Country in its Vicinity — Sand Hills West of it — The Coteau — Old Wives Lakes — Country West of Lakes — Excellent Pastures — Nutritious Grasses — ^Their Distribution — Sage Brush and Cactus no Proof of Aridity — Bullrush Lake — Strong Current Creek — Want of Wood — High broken Country — Appearance of Cypress Hills. The traveller ascending the Assiniboine finds that, after passing the mouth of the Souris, the eroding power of the river ceases ; its width sensibly diminishes and its tortuous- ness increases, while the banks become so low that from the hurricane deck of a steamer an extensive view, especially to the south and southwest, can be obtained. Owing to the crookedness of the river the ascent is slowly made, and an intelligent observer does not fail to notice that this is the reason that boats can ascend the river, for were it less crooked, and its waters not thus backed up, no boat could ascend the stream. The " Rapid," situated about eight miles above the mouth of the Souris, is caused by a ridge of boulders which here crosses the river, and which can be seen as a gravel and boulder ridge, extending back from the river on both sides. On the south side this line of boulders seems to extend in the direction of the " Hills of Brandon." The point on the Assiniboine which is now called Bran- don but formerly the " Grand Valley," was well named. The river banks at this point are very low, but some dis- 5 66 > MANITOBA AND THE GREAT NORTH-WEST. tance back on both sides, the country rises gradually until the general level of the prairie is attained. The vallfey lying between these elevations well deserves the name of " Grand." It is certainly destined to be a place of great importance both as regards its farming capabilities and railway and steamboat privileges. The soil, however, on the south side cannot be called first-class, as it contains much sand and gravel in the ridges back from the river, and many boulders on its surface. There is none of it, however, that will not be taken up, if indeed any of it has been left since the " boom " of last summer. About eight miles south of Brandon lie the " Brandon Hills," which are very picturesque on the east side, as they rise ridge over ridge from the level of the Souris, which here runs in a deep valley. Aspen is still found in some abundance along the slopes, but much of it is useless except for firewood. Standing 150 feet above the plain, on the most western ridge of the Brandon Hills, the traveller once looked over a vast grassy plain stretched out at his feet, without bush or mound to break its uniformity, except one solitary conical hill rising from the centre. Now, standing on the same point, he looks no longer on a solitary waste, but sees the plain dotted with the cabins of the settlers, and their cattle grazing peacefully in the little valleys or up their slopes. One short year more and stacks of grain will be grouped over every part of the plain, and what in the spring of 1880 was a vast prairie covered with waving grass, will, in the spring of 1882, be alive with settlers, and its solitude and loneliness gone for ever. Proceeding westward on the line of the C. P. R., the soil is a light sandy loam for a number of miles with many boulders near the railway. Beyond this, the country is first- class and comparatively level, but altogether without wood. About eleven miles out from Brandon, a patch of sand hills of about a square mile in extent is passed on the left, containing 2» 2 S -1 "1 i0 09 >if ?^ V ■ ' ■ is ^ > 01 M 1^ a S: «1 CD > o "^ II ii]0[z:[Z]D ■ II , II II II 11.1 r 1. izinann II mc^i^nn ZDC ^cijfiiic^n 1 l[ 1! IL J i[ IL II lU ncj ZDUJ II II II II 1 II 1 II II II II 1 =3c=:: II II II II 1 '1 ll l> ^H^'Q, ll lil 1 P, il III ll \'\ . [ i| |i| 1 o [ZD[Z] CDCZ G ZDCH. 1 is^ D II 1 D II 1 U II 1 D — ir-| D II 1 n IZllZIl 1 11 U ZDZZ] D 1 i; D L.L .11 1 ' II 1 □ CZ D IZICZ]' :=][= U II 1 cnnz U _JLJ __._ j_^j_ D 68 MANITOBA AND THE GREAT NORTH-WEST. some wood, consisting of oak and aspen of small size, fit onlj for fuel. These hills — like all sand hills — are flanked by marshes and hence protected from fire by water. Westward from this point to Flat Creek the railway keeps to the marshy plain, which extends all along the base of the high rolling country more to the north, and which lies between it and the Assiniboine. The tract lying between Flat Creek on the south and Gopher Creek on the north, is generally low and marshy, or consists of sand hills, altogether unfit for farming, but emi- nently suited for grazing purposes. In the marshes around the hills immense quantities of hay can be cut. There is good pasture, wood, and shelter in the hills themselves and permanent water abounds. After passing the last mentioned creek the land rises gradually and its character at once changes. An excellent farming country is entered upon, which extends with very little change to Moose Mountain, a distance of nearly sixty miles. For the whole distance the soil is rich and fertile, having a black sandy or clay loam surface soil, with the sub- soil varying from gravel coated with carbonate of lime in the ridges to a light ash-colored clay in the more level parts. All the water is good as far as the 102nd Meridian, but beyond that very little is found except in Moose Mountain itself. Pipestone Creek, flowing in a narrow valley about 190 feet deep, was, when I crossed it on the 26th of June, a rapid stream about twenty-one feet wide and thirty inches deep. It rises in the high country between the Qu' Appelle and Moose Mountain, and flows to the southeast into Oak Lake, described in a previous chapter. Near the lake the banks of the Pipe- stone are low and the valley not so confined, but as the stream is ascended the valley narrows and becomes much deeper, so that it is with extreme difficulty that carts can be taken across it. The summit of the valley slope is generally CHARACTER OF COUNTRT BETWEEN LAT. 50" AND 61°. 69 covered more or less with boulders, but this is no unusual occurrence, as the higher slopes of nearly all the river valleys of the plains are similarly covered. The upper part of the valley is filled with wood, which extends in clumps into the Wolf Hills, that were formerly covered with fine forests of aspen, but these have nearly all disappeared within the last thirty years. The "Weedy and Wolf Hills are a continuation of the Moose Mountain ridge, and are of the same general character. Many diverse opinions will be expressed regarding this region, as men of various temperaments view it. To one it will be a land of ponds, marshes, wUlow bushes, aspen clumps, and rolling hills, altogether unfit for farming on account of the broken character of the surface. Another see- ing these characteristics will consider each one an element of future good, and will say, this is a land destined to become the garden of the North-West. Both will notice that the soil is unsurpassed for richness, and as they examine the rich black clay loam, the croaker will declare that the soil is too rich, and that wheat would be sure to lodge owing to the length of straw. These objections have been urged to myself time and again, but they fall to the ground when fairly tested. The tract to which these remarks apply will be in the market the coming summer. That part of it west of the 102nd Meridian, included in Eanges from 1 to 10 west, and Townships 15, 16, 17, comprising about 2,000 square miles, will be found superior to any other locality yet opened for settlement. The Qu'Appelle Eiver joins the Assiniboine about three miles above Fort Ellice. At its mouth, and for twenty miles up to the mouth of the Big Cat Arm Creek, it averages seventy feet in width, with a depth of from eight to twelve. Cut Arm Creek comes in from the north and has a width of twenty-five feet, with an average depth of about three. Between Big Cut Arm Creek and the Pishing Lakes, the 70 MANITOBA AND THE GEEAT NORTH-WEST. river still retaras its size, being very little under seventy feet in breadth, but its depth varies from three to ten feet. Between the Second Fishing Lake and the Assiniboine, the distance in a straight line is about 110 miles, but by the winding of the river in its valley the distance is increased to 270 miles. Qn'Appelle Post and Mission are situated between the four Fishing Lakes, which are noted for their great depth and the abundance of white fish {Goregonus alhus) drawn from their waters. Above these lakes the river still retains a breadth of forty feet, but the depth decreases, so that at the Grand Forks, or outlet of Long Lake, it has become an insignificant stream. The total length of the valley is about 250 miles, but owing to its tortuousness the river cannot be less than 500 miles long. The valley for the whole distance averages fully a mile in width, and its depth varies from 200 to 300 feet. Small steamers can ascend to the Mission without difficulty when a few obstructions, caused by boulders, are taken out of the river's bed. The eastern end of the valley is of little value, as sand dunes and gravel hills choke up its northern side. Before Big Cut Arm Creek is reached the soil of the valley becomes very rich, and this is its general charac- ter for nearly 200 miles. general description of the country north of the qu'appelle. Extending from the Qu'Appelle, northwest by Pheasant^ File, and Touchwood Hills to Quill Lakes, eastward ta the vicinity of Livingstone, and southward, a little east of the 102nd Meridian, is a tract of country containing at least 7,000 square miles, or about four and a half million acres of excellent soil. It is true that the western side is almost devoid of wood, but to compensate, the hills,, extending all along its flank, are covered with trees. Pheasant Plain, which extends from the crossing of the Pelly CHAKACTER OF COUNTRY BETWEEN LAT. 50° AND 51°. 71 Eoad eastward for twenty-five miles, is altogether without wood, but the soil is exceedingly rich, and at no point is the wood to the southwest ten miles distant. Proceeding northward of the travelled road, the country becomes more broken, ponds and marshes are numerous, and wood increases both in size and quality, until it merges into continuous forest south of the present telegraph line. A rich black loam, about fifteen inches in depth, containing small grains of quartz or other rock, is the prevailing surface soil, but this imperceptibly passes into lighter colored sandy loam, as the timber becomes more continuous and of larger growth. The subsoil is generally a light colored marly clay, but this again, in the ridges, passes into gravel, which is generally gneiss covered with a coating of carbonate of lime. From a little west of the 102nd Meridian, boulders are numerous for about twenty miles, and occasionally after- wards, but no soil is seen too stony for successful cultiva- tion. At many points we dug into the subsoil, and found it as above. Tested with acid, it always gave indications of a very large percentage of carbonate of lime. The timber, on the tract passed over by me, is of very little value, but good poplar for building purposes will be found on the hills. Other explorers, who travelled the northern and eastern portion of this section, speak highly of its timber and of its being in considerable quantity. Spruce is also found in the northeastern corner of it. Good water seems to prevail throughout the whole region, although the running streams are few and quite small. Leach Lake, being fr3sh water, may contain fish. As there is abundance of timber in that section and good water, a large settlement will spring up in a year or two. The grass marshes so frequently spoken of, are abundant in this section, and are from the size of a flower plot up to a number of acres. 72 MANITOBA AND THE GEEAT NOKTH-WEST. Long or Last Mountain Lake lies in a depression that has a gentle descent from the east, extending over at least ten miles. It is forty miles long and has an average breadth of about one mile and a half. At its southern extremity a small stream, running in a deep but comparatively wide valley, discharges its surplus waters into the Qu'Appelle. This point is named the Grand Forks. Close to it must be the future city of the C. P R., as a branch line will be run before many years along the shores of Long Lake. Near the outlet of the Lake the banks are high but they gradually disappear, the high land on the one side passing into Last Mountain, and on the other forming an escarpment on the west side of the lake. The waters of the lake are sweet and pleasant to the taste, quite clear and of great depth. Multitudes of fish are caught here every fall by Indians who come down from the Touchwood Hills for the purpose of fishing. This lake and the four Fishing lakes in the valley of the Qu'Appelle are noted for their Whitefish that for many years have been a source of supply to all the Indians of the valley. Before many years steamboats will be plying on its waters, and the lovely land bordering on its shores will be dotted with farmhouses. Except on Last Mountain no wood is to be seen, but coal can be supplied by means of the lake and the C.P.R. One of the richest tracts in the Qu'Appelle valley lies east and north from Last Mountain and when known will be speedily taken up by farmers, as the much dreaded frosts of the Sas- katchewan valley are unknown. While encamped near the head of this lake, in 1879, we had ample opportunity to examine this portion of the country. We were particularly charmed with its soil, pro- ductions, and position. Multitudes of pelican, geese, ducks, avocets, phalaropes, water hens, and grebe, besides innu- merable snipe and plover were everywhere in the marshes CHARACTER OF COUNTRY BETWEEN LAT. 50° AND 51°. 73 at the head of the lake or along its shores, or on small islands lying to the south of the camp. This was early in July and experience tells me that not one-tenth was then seen of the bird life assembled in September and October. To the east of the head of the lake lay the rich country which produced the enormous mushrooms referred to in Chapter XI, when speaking of the lilies and other flowers which caused me to call this region the " Flower Garden of the Northwest " Passing roimd the head of Long Lake, from the east, we found a creek a few yards wide, with a sluggish current and a very miry bottom. Scarcely a mile from the first creek, we came to another of a totally different charac- ter. This creek had a gentle current of clear water, was nearly three feet in depth, and about eighteen wide. A fish weir was seen a short distance above our crossing, show- ing that fish ran up stream in the Spring. In half a mile, we crossed another creek, but this contained much less water. The middle creek, which is much the largest and which certainly contains fish in Spring, seems to be the stream which discharges Wolverine Creek. I believe the land on this stream will be found of unquestionable value, as the water in the creek was quite pure. The section lying west of the 102nd Meridian is bounded on the south by the Qu'Appelle, on the west by Long Lake, and by a line running northeasterly from the head of Long Lake to Quill Lakes. It may be said to have, both as regards surface and subsoil, a similarity of character, varying from deep black clay loam, with a light colored marly clay subsoil, to a light sandy or gravelly loam, with a gravelly subsoil. Some travellers taking the washed out subsoil thrown out by badgers, or found in cart ruts, as the real soil of the prairie, have characterized parts of this region as gravelly and sandy, but pits dug into the subsoil showed but a small percentage of either. 74 MANITOBA AND THE GREAT NOETH-WEST. Abundance of good water is found on every part of this tract for the greater part of the summer, and future settlers will find that good permanent wells can be obtained, at a reasonable depth, on any part of the prairie. Poplar wood for house-building, fencing, and firewood, can easily be pro- cured at Pheasant, File, and Touchwood Hills, which ex- tend from southeast to northwest through its whole extent. Almost continuous woods extend along the Carlton road, from twelve miles east of its western boundary to where the Qu' Appelle and Pelly road crosses it. Thence, eastward, extends the Pheasant Plain, a stretch of twenty-five miles long, without wood, but Pheasant Hills having abundance of it, are always in sight. East and northeast of this plain, copse wood is more or less abundant, until the Assiniboine is reached. West of the hills spoken of, no wood exists, but the soil is of the very best description. A depression, of which Long Lake partly fills the southern end, extends up to Quill Lakes. Although less than twelve miles wide where it crosses the travelled road from Carlton, the name of "Great Salt Plain" is given to a tract thirty miles from east to west. This valley contains many lakelets of brackish water. An alkaline creek, which crosses the road, seems to discharge the surplus waters of Quill Lakes into Long Lake. In this depression no wood is found. In fact, not a bush, so far as known, grows on a belt of country twenty-five miles wide, extending from the Qu' Appelle to Quill Lakes. I may here state that the appearance of the country just described, was altogether different from what I expect- ed. I had been led to believe that much of it was little else than desert. Having crosoed that part of i': north of the Qu' Appelle, in the summer of 1879, I can speak with certainty of the fertility of the immense plain sloping towards that river on both sides. Starting from the Qu' Appelle at its mouth, and pro- CHARACTER OF COUNTRY BETWEEN LAT. 50° AND 51°. 75 jecting a line nearly due west to the South Saskatchewan, a distance of over 250 miles, and including only the land south of the Touchwood Hills, a belt, with an average breadth of 100 miles, extends right up the Qu'Appelle. Here we have 25,000 square miles, or 16,000,000 acres of land lying in one block, that to my own knowledge, has over 90 per cent, fit for agricultural or pastoral purposes. The only poor soil in this extensive tract is that portion between Spy Hill and Fort Ellice, and two small groups of sand hills, lying at the sources of the Qu'Appelle. No alkaline soil is known on any part of it, except a narrow tract extending from the head of Long Lake toward Quill Lakes. Numerous small brooks are found on both sides of the river, and where there are no brooks, ponds of good water are seldom wanting. There will be no difficulty in obtaining first-class wheat crops throughout the greater part of it, as the soil is gener- ally a rich black loam, mixed with silica, and at times con- taining more or less gravel. The subsoil, in nearly every case, is a light colored clay, or clay intermixed with pebbles coated with carbonate of lime. Nearly the whole of the surface is a gently undulating plain easily drained, and over three-fourths of it sloping to the south. The crops at the Qu'Appelle Mission, about the centre of the area, ripen earlier than in any other part of the North-West ; barley having been cut, both in 1879 and 1880, during the last week in July. No summer frost has ever been reported from this region, and authentic reports say, that the spring is two weeks earlier than at "Winnipeg, Forty miles west of the File Hills, wood is no longer found, and from that to the Saskatchewan, not a bush of any description is seen. Moose Jaw Creek, about eight miles below its confluence with Thunder Creek takes a great bend to the east. At this point the sides of the valley are one hundred and forty feet deep. The breadth of the Creek is only sixteen feet, with about four inches of flowing water. Small clumps of maple and ash were observed, but no poplar. 76 MANITOBA AND THE GREAT NORTH-WEST. For the last twenty miles east of the Creek the country was very dry, and shewed signs of drought but the soil was rich and the grass tall. At our crossing, the creek flowed from the southeast, but a short distance lower down, it turned almost due east and then north, until it emptied into the Qu'appelle. West of Moose Jaw Creek the country changed at once, and four miles south of our crossing passed into sand hills which extended as low mounds from that point westward and northward. For thirty miles west from the creek the country was very dry, and frequently sand and gravel hills were seen with occasional patches of cactus, Opuntia Miasouriensis where the surface was sandy ; but much good soil covered with rich grass was also passed. To the south of our line of travel the country was more hilly than to the north. As we neared the base of the Coteau, alkaline plants became common, and small brackish lakes frequent, these being the usual harbingers of the approach to the Third Prairie Steppe, or Coteau. At every point where I have touched the Coteau I have noticed saline soil which has evidently been formed from the washing away of the face ■of the hills. A journey of twenty-eight miles, through a broken hilly country brought us to the head of Old Wives Lakes, which lie in a depression between the hills. The head of the north- ern Lake, is a series of detached alkaline ponds with mud margins and very brackish water. The waters of the Lakes are quite clear, but very salt. Strange to say, environed by the before mentioned salt pools a spring of excellent water was found not 100 yards from the head of the northern lake. This Lake is quite shallow for a long distance out, and the eastern side for many miles is much indented by points and bays. The western side is less broken, and is backed by higher hills than those which rise CHARACTER OF COUNTRY BETWEEN LAT. 50" AND 61°. 77 to the east. The twenty-eight miles of broken country passed through before reaching the lake, is well suited for pasturage, as there is abundance of water both fresh and brackish in the hills, and the soil is of varying character, sand or gravel prevailing. Passing west from Old Wives Lakes, the hills change their character and run in parallel ranges, from northeast to southwest with abundance of good pure water in ponds. Occasional swampy lakes varied the scenery. For about twenty-one miles west of the lakes, very little of the land could be claimed as agricultural, but all is excellent pasture. In the fifty-one miles referred to above, the leading grasses were all of the most valuable kinds for pas- ture. They were noted for their value in the fol- owing order. Stipa spartea (wild oats as named in Manitoba), took the lead, as indeed it does on all fairly dry and rich soils from Fort Ellice to the Rocky Mountains. This grass is preferred at all seasons by horses when travelling on the prairies, except late in July and August when its seeds are ripe. After the frosts come, horses always seek for this grass, and it is this species that constitutes the principal buffalo grass of the great plains. The other or more southern buffalo grass {Bouteloua oligostacliya), easily known by its curling leaves, and peculiar panicles of flowers was seen in some abundance on the drier knolls, but it is only found iu quantity where the soil is inclined to be arid, or much further to the southwest. JHticum repens (Couch or Quick grass), is always found where the soil is a strong clay, and wherever it is abundant, sand IS not to be found. Koderia cristata and Poa coesia grasses which have a tendency to grow in bunches, and are hence often classed as " bunch grasses," were comparatively common on the dry hills. These five species may be said to constitute the bulk of the western pastures, but more especially the three first mentioned. Artemisia cana 78 MANITOBA AND THE GREAT NORTH-WEST. (Canadian sage brusli), was met with, in some abundance on the clay plaia, twenty miles west of Old Wives Lakes, and is the same plant as that found by Palliser, nearly in the same longitude, at the Elbow of the South Saskatchewan, and called by him Artemisia tridentata, or the true American sage brush, which in reality never crosses our boundary east of the Eocky Mountains. This plant is no proof of aridity of climate as it is found only on Cretaceous clay, and wherever that crops out it is sure to be seen. At the present time it is growing at the base of the hill on the left bank of the Assiniboine, just opposite the mouth of the Qu'Appelle at Fort EUice, and as a proof that even the presence of the ■cactus does not always indicate aridity of climate, I may state that anyone may find cactus growing in the Qu'Appelle Valley, just south of where the Carlton road ascends out of it. Here then are the two plants, which former writers cited as proofs of the aridity of the climate of our western plains, found growing in the neighborhood of Fort Ellice where the rain-fall is known- to be abundant, because here they find a suitable soil — the first mentioned, clay, the latter clay and sand with a suitable amount of alkaline matter. Twenty-five miles west of Old "Wives Lakes, is a fine large fresh-water lake, called BuUrush Lake, which is at least eight miles long and five broad. Three creeks enter it from the north and west, and another discharges its sur- plus waters from the south end. Clay cliflfs over sixty feet high, are along the eastern side, and its waters, even at less than a rod from the shore, are very deep. At the north end of the lake, the trail from the Elbow joins the other coming from Qu'Appelle. Four miles east of the lake, good agricultural land was entered upon, which extended all around it. As we rounded the north end a sluggish stream was crossed, and beyond it another with water standing in deep pools. These streams come from the north. About two miles to the south another CHARACTER OF COUNTRY BETWEEN LAT. 50" AND 51°. 79 and larger stream was found coming from the hills and emptying into the head of the lake. Crossing the plain and a narrow range of hills with a rich, sandy loam surface soil, we descended into another valley and here found Strong Current Creek flowing to the east. Within a short dis- tance, it turns to the north and enters a range of hills which shuts in the valley on that side. The creek flowed down a valley from the west and meandered through it, having banks about ten feet high. Its bed was thirty yards wide, but there was flowing water only over part of it. A few willows grow in its bed, and these were the only brush seen in seventy-six miles, as not a bush exists around any of the lakes spoken of Nearly the whole of the tract lying between the Cypress Hills and Old Wives Lakes, has excellent soil, and at tiraes spreads out into wide, slightly undulating plains, covered with tall, rich grass. In other parts high rolling hills with deep valleys, having a northwest and south- east direction, are met with. Old Wives Creek receives the drainage of all these hills, but it is only in spring that any flow of water passes over its stony bed. The highest land is always to the north and west, and some of the ridges or narrow plateaux passed over, were found even higher than the eastern end of the Cypress Hills. Occasionally brackish lakes were seen, but water of any description was not abun- dant, although we never suffered from the want of it. The last twenty miles was over a gently undulating plain, with fair soil and but little water. As we approached the Cypress Hills, they rose before us bodily from the plain to the height of 400 feet, with the various ravines which penetrated the eastern face of the escarpment filled with wood. Along their base were the usual alkaline ponds and poor soil, but these were much restricted as Strong Current Creek was found flowing south along the base of the hills. After passing three miles south of our camp, it turns boldly to the 80 MANITOBA AND THE GREAT NOETH-WEST. north, so that before reaching the hills we were compelled to cross it twice in less than two miles. Blue hills shut in the horizon to the north ; twenty-five miles to the south- east lay the high ridges we had left the preceding day, and an interminable plain stretched away to the south, while in our front were the Cypress Hills themselves. CHAPTER V. Character of Country hetween lat. 51° and 52" West of Manitoha. Country West of the Assiniboine — Beaver and Touchwood Hills — Heavy Forest — Rich and Lovely Country — Great Salt Plain — Immense Plain to the South — Tract North of the Qu'Appelle — Rich Soil and Rank Grass — Last Mountain — Water Scarce en Sur- face — Broken Country, Twenty-two Miles Wide — Fine Pasture Lands — ITo Bad Soil in Eighty Miles — Lines of Boulders, near Humboldt — Cause of Wood at Certain Points — Extensive Plain Southwest of Touchwood Hills — Salt Marshes — Little Touch- wood Hills — Mission at this Point — File Hills — South Saskatchewan, Voyage Dowi^ It — Moose Woods — North of Moose Woods — Land East of River — Soil of Great Depth^- — Aroline, or Telegraph Crossing — Rich Land — Country West of River — Fine Level Tract— Eagle Creek— Eagle Hills, Fine Country for Stock. After passing above the mouth of Shell River the land on the right bank of the Assiniboine becomes exceedingly rich, and in every respect as good as that east of the river. All travellers and surveyors speak in the highest terms of the land west of Fort Pelly and south of the telegraph line, and although much of it is wet and generally covered with forest or brush it is a very desirable country. The Beaver and Touchwood Hills farther to the west are covered in part with heavy forest, and although not suitable for present set- tlement, owing to the forest and marsh which predominate in some places, yet there are large areas covered with a wealth of tall grass, pea vine, vetch, and lovely flowers that will tempt the pioneers of the next few years to locate in the park like country both north and south of these so-called hills. Extending west from the Touchwood Hills, is a level plain without wood for thirty miles on the line of the Carlton trail. This plain has been erroneously called the Great Salt Plain, whereas the part of it to which the term applies, is scarcely twelve miles wide on the trail. Stretching westerly 6 82 MANITOBA AND THE GREAT NORTH-WEST. from the hills, a plain over 120 roiles wide extends to the South Saskatchewan For nearly the whole distance, the surface is undulating or quite level with occasional waves a mile or two apart. Scarcely a twig exists on the whole plain. Fresh water and excellent soil are found every- where. In the southern part, near the head of Little Arm Creek, the country is broken into rolling hills, but the soil is very rich. The following description of this tract was written on the ground, and gives a general picture of this section The country described is generally on the 106th meridian from the Qu'Appelle River north. Our course was now due north for eighty mUes, so as to traverse the great plain, extending northward from the Qu'Appelle, in its greatest length. The soil of this plain was thought to be generally sandy, so I resolved to examine it every mile for the whole distance. We did not expect to find any wood and but very little water on the journey, so, after filling our kegs and piling a week's wood on our carts, we started north. Ascending out of the valley we found that the upper part of the slope and the outer margin of the plateau, were covered with boulders just as we had found them on the southern side. As we receded from the river, the plain crossed on September 11th began to assume the appearance of a range of hills, but we knew it was only the undulations rising slightly one over the other, and that no hills existed in that direction. This is the Eye Brow Hill Range of Hind's Report. For sixteen miles from the river, the plateau was almost level, with a slight rise to the north. The soil near the river was a light sandy loam with short grass, but this soon changed for the better and the grass became taller. From the crest of the plateau, spoken of above, we could see an immense distance to the west and north over a bound- CHARACTER OF COUNTRY BETWEEN LAT. 51" AND 52°. 83 less plain. Apparently about forty miles off, Last Mountain rose from the plain, standing alone being a very promi- nent object on the horizon in the northeast. Our course led us along the edge of the plateau, and occasionally "cut banks " could be seen in the distance, showing the course of Little Arm Creek. All day we travelled over a level prairie, covered with good grass, and having excellent soil but not a drop of water except at the creek. Another day, over the same level prairie, with Little Arm Creek flowing through it, brought us to the margin of a broken, h'^ly country which extended east and west as far as we could see, and was twenty-two miles from south to north. As we proceeded north, the soil constantly improved ; the grass was always tall, water abundant and good, and this tract although rough and much broken by lakelets, ponds, hay-marshes, and hills, had a rich soil and was well suited for pasture everywhere. Near the head of Little Arm Creek, clumps of bushes were observed nestling along the margin of some lakelets. These showed that, if fires could only be stopped, bushes suitable to shelter stock would soon grow up. A descent of 100 feet brought us to a plain, which extend- ed far to the north, while the hills we had just left, ran almost due east and west. Fifteen miles over the plain brought us to our most northern limit, latitude 51° 43' In travelling the eighty miles just described, I never observed bad soil. No sandy soil was seen except close to the Qu'Appelle. The greater part of the surface was level or gently rolling, and where it did rise into hills, the soil was always good. I constantly dug into the dry knolls and found excellent soil, although pebbles were on the surface and boulders were frequently seen. For the first thirty- five miles water was scarce, but after that it was always plentiful. Brackish water was never detected, except once, until we descended from the line of hills. After that 84 MANITOBA AND THE GREAT NORTH-WEST. occasional pools were seen in circular depressions or narrow valleys. For tlie last fifteen miles boulders on the knolls were of constant occurrence. Occasionally the country became more rolling and a few willows and small poplars about two years old were seen around the hollows, but not large enough to use as fiiel. Turning east we travelled for twenty-five miles over either a level or undulating prairie, with a clay loam surface soil, having numerous boulders at times scattered over it. The high ground left on Saturday, Sept. 11th, was seen in the south, but to the north a high undulating country alone was visible, with occasional patches of small wood. We now crossed a stony tract about five miles wide, running north and south, and afterwards entered on a level sandy loam plain, which extended to Wolverine Creek, a distance of six miles. This plain showed signs of alkali, and was the poorest land we had seen since leaving Strong Cur- rent Creek. After getting a supply of wood and communi- cating with Humboldt so as to fix our longitude, I turned south for the purpose of traversing what is known as the Great Salt Plain. Had the country in the vicinity of Hum- boldt continued as good as farther south, no wood would be found here either, but the stony tract referred to with jxumerous marshes, ponds and long narrow lakes, lying south of the woods, stops the tires and saves the wood. The soil near the margin of the woods was a dark colored sandy loam, containing a very large percentage of silica. This sandy and alkaline soil vanished as soon as we crossed Wolverine Creek, which is here nothing but a series of pools connected by sloughs. Proceeding south we entered upon a very level plain, which continued without change, except for the better, for thirty miles. Many clumps of small poplars of from one to six years growth were passed, and occasionally a narrow ridge or roll in the prairie, but nothing like a hill was seen for many miles. Near the CHARACTER OF COUNTRY BETWEEN LAT. 61° AND 52°. 85 centre of this tract we crossed a fine creek twenty feet wide, with two feet of flowing water in it, which is probably the discharge of Quill Lakes, and is the middle creek that enters the head of Long Lake. The creek merely runs in a slight depression, with banks nowhere more than four feet high, margin always dry and no signs of alkali. For many miles a higher tract could be seen to the west, with many prominences covered with trees or brushwood, but this dis- appeared or merged into the high country which lies to the southwest, and which is a continuation of the elevated region described as extending east and west from the head of Little Arm Creek. In the direction of the Touchwood Hills high rolling land could be seen, with occasional patches of wood. On this whole plain the greater part of the grass was tall enough for hay, water was abundant and always good, the soil invariably a rich sandy or clay loam, and no gravel except in the subsoil. The only poor land observed was a narrow strip on each side of Wolverine Creek. Crossing a small stream flowing nearly west we passed for six miles through a very fine country with rich soil, but all the depressions were alkaline and the marsh water gen- erally brackish. The country at this point seemed to be covered on the higher ground with a thia coating of drift, but this in the lower places gave place to Cretaceous clay, which here took the form of white mud swamps instead of the hard baked clay flats of the southern prairies, where- the rainfall was light. Having reached a small creek flowing to the west, and seeing Last Mountain lying southeast of us, we changed our course to the southeast before crossing the creek, and very soon entered on another part of the plain spoken of above, which was much more difficult to cross owing to numerous white mud swamps that lay in our course. Reach- ing the creek again, now flowing in a valley about half a mile wide, and crossing it with extreme difficulty, we entered on a fine undulating country of great extent. 86 MANITOBA AND THE GREAT NOETH-WEST. The tract described above is the only alkaline soU we saw on the " Great Salt Plain," which certainly is a misnomer, as I stated in my report of last year. That an extensive, treeless, and in some parts waterless plain, extends west and northwest from the Touchwood Hills I admit, but I do not admit, and am prepared to disprove that an alkalLue plain thirty miles wide extends either on the Carlton trail or any other line west or northwest from the Touchwood Hills. There is undoubtedly a saline depression extending from Quill Lakes to Long Lake, the worst parts of which are largely made up of white mud swamps or brackish marshes, but there are no data to show that it covers twenty per cent, of the area assigned to it. The country around the flanks of the Touchwood Hills is much broken or undulating, and has a good rich soil varying from dark colored clay loam to sandy loam. It is always covered with a certain amount of dark earth, and frequently, when gravel is seen on the surface, none is found by digging. The subsoil is usually a light colored clay loam, containing more or less gravel, which is generally covered with carbonate of lime. A line of broken country connects the Little Touchwood Hills and Last Mountain, and is more or less covered with small poplar copse. "Were the country level no wood could grow, as fires constantly sweep over the level ground without obstruction, and destroy all the young wood. I left my party when we reached the trail leading from Qu'Appelle to the Mission, and found the Missionary getting in his potatoes and other roots. His crops this year were very fine, the frost having done them no harm. He showed me over four hundred bushels of as fine potatoes as I ever saw, and told me all the Indians had abundance of them. Owing to the broken nature of the surface, farming by white men at this point would not be profitable, but it seems just the place for Indians. Patches of good arable land, interspersed with little lakes and hay marshes, were seen everywhere, and CHARACTER OF COUNTRT BETWEEN LAT. 51° AND 52°. 87 from the abundance of feathered game at this time (October 1st) it might be called the hunter's paradise. In three or four days any man with a breech loading shot-gun could have supplied himself with his winter's meat, as all lakes and ponds at that time were alive with ducks of many species. Indeed, from the middle of August until the lakes and ponds freeze up for the winter, water fowl are very plentiful everywhere. Multitudes breed in the country, and about the middle of September the sea ducks begin to arrive, and myriads of them crowd every pond. A ride of fifteen miles over a very rough trail brought me to Touchwood Post, on the Carlton Trail. The country between these two points — especially the western part — is very rough and much broken up by ponds and lakelets, with intervening ridges, but except on the western side near the Mission, nothing worthy of being called a hill was seen. What is generally denominated the Touchwood Hills by travellers is merely the broken country lying between the Little and Big Touchwood Hills, the one lying to the right of the trail, the other to the left. In the vicinity of the Mission, on the Indian Reserve, are fine groves of large-sized poplar, well suited for house building, and, excepting this, very little but second growth aspen and brush was seen. I may as well state in this connection that the Touch- wood Hills and File Hills as regards altitude can scarcely be considered hills at all. They are merely elevated plateaux, or more strictly speaking watersheds, protected from fire by innumerable ponds and marshes, which are scattered every- where over their surface, and in my estimation can never be first-clas: farming lands, though well suited for hay and stock farms. The Big Touchwood Hills extend eastward and merge into the Beaver Hills, and both are merely an elevated tract from which the small streams flowing to the Qu'Appelle on the south, or the White Sand River on the north receive their waters. Experience has taught me that 88 MANITOBA AND THE GREAT NORTH-WEST. ■wherever trees and brushwood are found, there we may look for a broken country, and one that contains too much water, while the open treeless prairie, generally condemned to sterility, is by far the best farming land. From the Elbow of the South Saskatchewan to its junction with the North Branch below Prince Albert, the river meanders through a valley of varying width, which cannot be better described than by reproducing the account written by Prof. Hind of his canoe voyage down the River from the Elbow in August, 1858. " The banks of the river slope gently from the prairie on the southwest side to an altitude of about 250 feet, they then become abrupt. On the northwest side the Sandstone cliff, varying from thirty to sixty feet in altitude, rises abruptly from the river, then follows a hilly slope to the prairie level. Trees, consisting chiefly of aspen, are found in patches on both sides. The river continues about half a mile broad, with numerous sand-bars and low alluvial islands. The drift above the sandstone is gravelly, and many small sand dunes occur on the hill bank sloping to the prairie, and have progressed beyond the prairie to a considerable dis- tance. A treeless prairie, boundless and green, except where the patches of drifting sand occur, is visible on either hand from the top of the bank ; below, the river glides with a strong current two and two and-a-half miles an hour, filling the broad trench or valley it has eroded. The June berry, La Poire, is very abundant ; shrubs or trees, eighteen to twenty feet high, loaded with this fruit, perfectly ripe and of excellent flavor, are numerous in every grove ; the ber- ries are of the size of large black currants, very juicy and sweet. This shrub is the La Poire of the Red River Voyar geurs. " About twelve miles from our camp, or sixty miles from the Elbow, forests of aspen begin to show themselves on the banks, after passing through a low country, which is an CHARACTER Or COUNTRY BETWEEN ,LAT. 51° AND 52". 89 expansion of the river valley. Ripple marks are numerous on the fresh mud, the furrows lying parallel to the course of the stream. They are quite recent and similar to those observ- ed on Red River in spring. The ash-leaved maple begins to show itself, but the aspen is the prevailing tree. The woods are not continuous, and the prairie on either side of the river remains bare ; it is fast regaining its former alti- tude. Sand hills are visible in the distance from the top of the bank La Poire is very abundant and fine flavored. The exposed cliffs consist of reddish loam, and the rock is no longer seen below them. At a point fifty -three miles from the Elbow, we made a careful section of the river, and found its breadth to be nearly one-third of a mile (28 chains) ; its greatest depth was ten feet on the east side, but on the west side there is another channel with nine feet of water. "As we approached the Moose Woods we passed for several hours between a series of low alluvial islands, from ten to twelve feet above the water. They sustain some fine elm, balsam, poplar, ash, ash-leaved maple, and a vast profusion of La Poire. The river valley is bounded by low hills lead- ing to the prairie plateau four to eight miles back. The country here furnishes an excellent district for the estab- lishment of a settlement. The spot where we camped for the night is an extensive, open, undulating meadow, with long rich grass, and on the low elevations rose-bushes, in bloom, grow in the greatest profusion. It is only ten feet from the water, yet it does not appear to be flooded in the spring ; water-marks and ice -marks are nowhere seen above four feet from the present level of the broad river. " The region called the Moose Woods, which we entered last evening, is a dilatation of the Saskatchewan flowing through an extensive alluvial flat six miles in breadth, and cut into numerous islands by the changing course of the stream. This flat is bounded by sand hills, some of which are nothing more than shifting dunes. The woods are in patches. 90 MANITOBA AND THB GREAT NORTH-WEST. and in the low land consist of balsam poplar, white wood, and aspen. Small aspen clumps cover the hills, but no liv- ing timber of importance has been seen as yet, although many fine dead trunks are visible, probably destroyed by fire. The river continues to flow through a broad alluvial flat for about twenty-five miles. Its water is very turbid like that of the Mississippi, holding much solid matter in mechanical suspension. " Beyond the Moose Woods the banks close upon the river^ and have an altitude not exceeding sixty feet. The breadth of the stream contracts to 250 yards, with a current fiilly three miles an hour. On the east bank the prairie is occasionally wooded with clumps of aspen, on the west side it is treeless, and shows many sand hills. During the afternoon we land- ed frequently to survey the surrounding country. Nothing but a treeless, slightly undulating prairie was visible ; many large fragments of limestone not much water-worn lie on the hill banks of the river, which is about 100 feet in altitude. The river continues very swift, and maintains a breadth of 250 yards. Frequent soundings during the day showed a depth of ten to twelve feet. A little timber dis- plays itself occasionally on the east bank below the level of the prairie. "At 8 A.M. we arrived at a part of the river where it showed an increase in breadth ; it is now about a quarter of a mile broad, still flowing through a treeless plain, in which only one low hill is visible. This character continues for many miles, the hill banks then begin to increase in altitude? and are about 100 feet high, but the river flows through a dreary treeless plain for thirty miles from our camp, after which " The Woods," as they are termed, begin ; they con- sist of a few clumps of aspen on the hill flanks of the deep valley of the river. The face of the country is changing fast, it is becoming more undulating, and patches of aspen woods appear on the prairie ; here and there, however, the r CHARACTER OF COUNTRY BETWEEN LAT. 51° AND 52°. 91 remains of a heavier growth are visible in clusters of black- ened trunks ten to fourteen inches in diameter. During the afternoon we anchored to measure the rate of the current. The river is 200 yards broad, and it flows three miles and a half an hour. Its average depth is seven and a half feet." . The land on the east side of the river was examined by Mr. George Simpson, D. L. S., during the past season all the way from the " Elbow " to the Middle Crossing (Batoche's) and pits were dug every twenty miles to the depth of four feet. Excepting a little in the neighborhood of the Elbow,, all land passed over and examined by him was first class. He reports that along the river the soil is rather sandy. These views are in accordance with my own. Later still a correspondent of the " Globe " reports that in this sandy belt, Mr. Clark, who keeps the ferry at the Telegraph Crossing,, informed him that, though the soil was not particularly promising in appearance, it was remarkably productive. " Everything in his garden grew and matured admirably this season, and he is very confident that grain would do well here. Large quantities of small timber are to be found along the banks of the South Saskatchewan within easy reach, and altogether ' Aroliue or the Telegraph Crossing' as it is called, promises to become a prosperous settlement in time." On the west side of the river the surface of the country is drier and less broken than on the east. Although the soil is sandy loam and contains some gravel and in places boulders on the surface, taken as a whole, the district be- tween the two rivers, south from Duck Lake, to the Moose "Woods, will make a fine agricultural settlement. I know that all manner of reports have been spread regarding it, but I still cling to my own opinions, corroborated as they are by the thorough examination of Mr. Simpson and the in- telligent correspondent of the " Globe " who remarks of the section west of the river : — 92 MANITOBA AND THE GREAT NORTH-WEST. " For the first few miles this morning the trail led along fine uplands, from which we were enabled to take our last look at the great discolored slopes away to the north of the river, where the purple bronze of the leafless bluffs contrast- ed richly with the limitless stretches of pale yellow prairie grass, a glorious boundless expanse that will some day be dotted over with countless farm houses, and be the home of a hardy, wealthy, and prosperous community, but which is now only pressed by the stealthy tread of the coyote as he chases the timorous hare, and where even the lonely moose is seldom disturbed by the prowling half-starved savage. " As we left the bank of the great prairie stream of the north, we passed through broad stretches of treeless plain, where the soil is both rich and dry, but the presence of many small boulders is likely to render it unpopular with farmers so long as the settler has so much choice country from which to select. " We have travelled some twenty -nine miles according to our own estimate of distances through open, treeless prairie, where the soil looks rather light and gravelly, but where the rich growth of buffalo grass would indicate that it is much more productive than it appears to be. Indeed it is rather difficult to judge fairly of a prairie country at this season' of the year, as everything looks parched and dried up with the severe frosts of early winter." Westward of this tract the country gradually merges into the broken ground along the southeastern part of the Eagle Hills. Before reaching these. Eagle Creek is crossed flowing through a valley covered with tall rich grass, and beyond, the hills rise in tumultuous masses without any order. Nearly all the land is good. In all the valleys the grass was of sufficient length for mowing. Excellent fresh water is found everywhere. Few localities could be found better adapted for stock raising than this part of the Eagle Hills. Should fire wood and shelter be wanted all that is necessary CHARACTER OF COUNTRY BET-WEEN LAT. 51° AND 52°. 93 is to move farther north towards the Saskatchewan, where there is abundance of both in the Eagle Hills. Numerous brooks of never failing water flow from the hills into the Saskatchewan. CHAPTEK VI. Character of Country between lat. 52° and 53° West of Manitoba. Porcupine Mountain — Country on Red Deer Eiver — Soil very Eioh — Exhaustless Fertility of the Carrot River Country — Prince Albert Settlement— Its Early History— Wonderful Progress in a few Years — Description of the Settlement — Many Houses in Course of Erection — Fall Sowed Wheat a Success — No injury from Frost — Duck Lake Settlement — Fort Carlton and its Vicinity — Country between the Rivers — Eagle Creek — The Bear and Eagle Hills — Land South of Them — Description of Battleford and Vicinity — Its Future Sketched Out — Land in the Neighborhood — Character of Soil — Police Farm at Battleford — The Government Farm — Remarkable Vitality of Seeds — Depth of Roots in the Soil — Plain South of Battleford — Coulees of the Plain — Their Origin — Country North of Bear HiUs — Splendid Pasture Land — Water Abundant — Grasses of the Plains — Cause of Absence of Wood — Constant Prairie Fires — Why the South side of a HiU is without Wood — What Causes Aridity — Description of Hand HiUs — Cactus not a Proof of Aridity of Climate — Fine Rich Land South of Battleford — Immense Area of Good Land — Manito Lake — Sounding Lake — Neutral Hills — Fine Pastoral Land to the Southwest — Land around Sullivan's Lake — Fine Land West of Sounding Lake — Rich Country at the Head of Battle River — Millions of Tons of Hay in This Re- gion — General View of the Country — Lakes Filled with Fish — Beaver still Numer- ous — AU Lakes and Ponds Filled with Birds in Spring and Fall — Bears and Wolves Numerous some Seasons, but Never Injurious Except to Small Stock. The Porcupine Mountain lies west of the Duck Mountain, and is separated from it by Swan River and its valley. It is bounded on the east and north by marshes, but on the south and west it passes by easy transitions into the more elevated plateau to the west. The " Mountain " itself is covered with a heavy forest of spruce and aspen. The trees, being preserved from fire by the surrounding marshes, attain a large size. Red Deer River, emptying into the northwestern corner of Lake Winnipegoosis, passes through a fine country. Its upper part possesses a soil only excelled by that of Carrot River, a fine stream which flows parallel to it and empties into the Saskatchewan, east of Cumberland House. All travellers and explorers unite in praising this extensive CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. 95 region, and settlers wlio went there two years since, have produced enormous crops on soil which is practically inex- haustible Marcus Smith, C. E., who travelled through this region in 1879, thus expresses himself regarding it : " We travelled southward from Fort a la Corne to Carrot Kiver, and up the banks of the latter to its outlet from Water Hen Lake. Here we found several fields of wheat with very heavy ■crops nearly ripe, and two farm homesteads. I examined the well at one of them and found a depth of six feet of black mould on the top, with sixteen feet of stiff clay loam to the bottom of the well. Mr. Robinson, the proprietor, in- formed me that this summer fourteen farms had been select- ed and a number of farmers were coming in next spring. " We started from the Lake on a course 30° east bearing for Little Quill Lake, and reached the summit of the range ■without difficulty, about nineteen miles from the Lake, in which the rise is less than 200 feet. The surface of the ground is very uniform, the soil of the richest quality, and several feet in depth. It is equal to the best parts of Manitoba — chiefly prairie with scattered clumps of poplar and willow, till near the summit of the ridge, which is nearly covered with a forest of poplar. Between Humboldt and Quill Lakes -the country is variable in some places, low and swampy where there is much willow brush, but eastward of this line, where the trail crosses the telegraph line, there are several miles of a beautiful park-like country, the trail wandering in open glades through groves of aspen. Before we reached the Quill Lake we came upon an alkaline pRiin extending northward to the telegraph line ; this continues eastward to near Fishing Lake, and probably also to some considerable distance north of these lakes." Prince Albert settlement, situated between the two bran- -ches of the Saskatchewan, was originall}'^ a Presbyterian Mission established about fourteen years ago by the Rev. 96 MANITOBA AND THE GREAT NORTH-WEST. Mr. Nesbitt. For some years after its location, it was thought that besides christianizing the Indians they could be taught farming, but buffalo being plenty they would not settle. In the summer of 1875 Captain Moore, an Irish gentleman of means, brought machinery for a steam saw mill on waggons from Winnipeg a distance of fully 700 miles by the road they had to travel. From that time the progress of the settlement was assured. Besides the saw mill a grist mill was erected, and flour at once fell to Winnipeg prices, but owing to the large amount required for the Indians it is much dearer at present. The progress of Prince Albert during the last six years has been astonishing, and at present it is the most important point west of Brandon. In 1877 there were about 500 people in the vicinity, and about 1,200 acres under cultiva- tion. Now report says there are 3,000 people in the neighborhood. The correspondent of the Toronto " Globe " writing from Prince Albert last August thus describes the settlement: — " The settlement, or rather the aggregation of settle- ments, including the Prince Albert District (extending from Fort Carlton down to the junction of the north and south branches of the Saskatchewan), includes a strip of territory about eighty miles from east to west, by fifty miles from north to south. This district contains a white and Half-breed popu- lation of about 3,000 souls. Here there are about 10,000 acres under crop, and fully 5,000 acres newly broken this year, the latter figure furnishing the reader with some idea of the rapidii^'' with which settlers have been flocking in within the last year. The town of Prince Albert may be designated as about four miles long by half a mile wide, along the south bank of the North Saskatchewan. The town is situated on a plateau considerably above high- water mark in the river, and is bounded on the south by a narrow and shallow ravine, beyond which rises another bench or CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. 97 bluff to the level of the surrounding prairie, which is con- siderably higher than the plateau upon which the town stands. The population of Prince Albert proper is about 800, but some idea of its rapid growth may be obtained from the fact that there are now no less than thirty-one buildings in course of erection in the town, and many parties intending to build are merely waiting to secure the services of carpenters, which are in great demand just now." Speaking of early frosts he says : '' Mr. Miller informed me that though he had been in the country eight years he had never lost anything by- early frosts. He does all his ploughing and sows his wheat late in the fall. In this way the wheat does not germinate till the following spring, but as soon as the frost is out of the surface of the ground, the wheat begins to grow, and is really well on the way before it could be put in the ground under the ordinary system of spring ploughing. Last year there was a pretty sharp frost about the 25th or 27th of August, but Mr. Miller sold his whole crop of wheat at $1.75 per bushel." Duck Lake Settlement is located half-way between Carl- ton on the North Saskatchewan and Batoche's Crossing of the South Saskatchewan. In the summer of 1875 Stobart, Eden & Co. started a store at this point, and the same year broke up a small piece of ground. That small piece has now become a large farm, and, other parties coming in, a fine set- tlement has been formed. Between Duck Lake and Prince Albert the country is generally a light sandy loam, but much of it would be considered very poor when compared with other sections. South from Duck Lake the land improves and is generally well suited for farming. Fort Carlton is situated on the right bank of the North Saskatchewan, and has been for some years the headquarters of the Hudson's Bay Company. Here every summer the Council meet and discuss the business of the Company, and receive the returns of the year's trading. Little farming is 7 98 MANITOBA AND THE GREAT NORTH-WEST. done close to the fort, but many fine farms are located between it and Duck Lake. To supply the settlers and themselves, Stobart, Eden & Co. have a portable flour mill, which does good work for the settlement. The tract of country lying southwest of this between the rivers has been described in the preceding chapter. Lying north of the river is a fine tract that may be seen from the heights above Eagle Creek, and which, when settlement crosses the river, will be very attractive. Eagle Creek, a fine stream of pure water, enters the Saskatchewan at the eastern end of the Eagle Hills. This stream seems to rise in a large coulee that extends many miles into the great plain south of Battleford. The Bear Hills pass gradually into the Eagle Hills, which, at first, turn to the northeast, but, as they approach the North Saskatchewan, they rend to the northwest and continue in that direction until they reach Battle River, some distance west of Battleford. At Battleford their base is about eight miles south. As they pass eastward they draw nearer to the Saskatchewan. Their northern slope is a continuous for- est of very good poplar {Pojpulus tremuloides and halsamifera), which breaks up and becomes interspersed with prairie as it approaches that river. Between Battleford and Eagle Creek no less than twenty-two small streams issue from the forest and make their way into the river. Owing to these streams, the country between the hills and river is very much cut up, and rendered well nigh impassable for loaded carts, when the kills are wet and slippery The land bordering on the river is generally a sandy loam, but many fine farms will yet be located there. In the hills themselves, and southward from them, the land is very rich, the soil being a black clay loam, changing as it gets drier (southward) into a sandy one, but with very little change in vegetation. Mr Wilkins, D L S , crossed diagon- ally through the hills, while I passed on both sides of them. CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. 99 and Hs report of tke land at the Mission and at the Govern- ment Farm agrees with my own observations. The land in the southern extension of the hills is very much broken and con- tains multitudes of ponds and fresh-water marshes, where immense quantities of natural hay of the best quality goes to waste every year. Although many people think the hills the best for settlement, I believe future settlers will prefer the prairie, as there is less broken land, less marsh and swamp, and less labor required to make a home. As the views of the " Globe's " correspondent regardirig Battleford are nearly in accord with my own, I give his description : — " This place is certainly one of the most beautiful and pic- turesque in the North-West, and if ever there was a spot which nature intended for the site of a city it is Battleford. The steamboat landing on the Saskatchewan is two or three miles west of where Battle River falls into the larger stream, but for a long way (several miles at least above this) the general direction of the two streams is parallel, though the strip of land between them is seldom above two miles and a half, and in places less than three-quarters of a mile, in width. This strip of land between the two rivers consists of a beau- tiful plateau of fine, smooth upland prairie. Its highest por- tion is along its centre, midway between the two streams, and it slopes away gently toward each. The lowest portion of this plateau is fifteen or twenty feet above the narrow strips of bottom land along both rivers, which latter in times of spring floods are sometimes partially submerged. On the other hand the highest portion of this plateau (which the reader will have already identified as the site of the future city of Battleford,) is considerably lower than the level of the prairie blufis, which rise beyond the Saskatchewan on the north and Battle River on the south. Here is a spot which could be easily drained by sewers falling each way from the central ridge ; the whole outer boundary would be 100 MANITOBA AND THE GREAT NORTH-WEST. river frontage, at ■which the Saskatchewan steamers could land at nearly all times, while the smaller craft, which would be required to navigate Battle River, could perform the service from the forks when the larger steamers could not ascend on the south side of the peninsula with safety. With a city located on this peninsular plateau ( which is now only occupied by the barracks of the Mounted Police), the south bank of Battle River and the north bank of the Sas- katchewan (about four miles apart) would afford the most charming situations for villa and suburban residences. " Regarding the country in the immediate vicmity of Battleford, I am quite aware that what I have to say flatly contradicts what appears to me to be the general impression concerning it. Before coming here I was told that Battleford was in the midst of a sterile, dreary waste of sand, but I wish we had a few hundred square miles of just such dreary wastes of sand in Ontario and Quebec. The soil is not the deep, black loam which I have seen m other portions of the Nortli- West, but at the same time that it is not unproductive 1 shall presently produce abundant proofs It is a rich and very friable soil, in which there is unquestionably some sand, but for all that it is deep, strong, warm and extremely productive. I should have stated before that the few houses (beyond the houses of Government officials, which are on the crest of the beautiful high bluff south of Battle River), are located on a narrow strip of bottom land south of the smaller stream, and the plateau to which I have already referred is the site of the future city." The police farm at Battleford was established in 1879. In the spring of that year Inspector Walker broke up the soil, and on my visit about the first of August I found every- thing well advanced and wrote in my journal, — " The police farm, situated on the point of land between Battle River and the Saskatchewan, is a sandy alluvium, and appears to be very dry and barren, but it certainly has produced good CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. lOl crops this year. Three months ago it was barren prairie^ now oats, barley, potatoes, and turnips, are growing luxuri- antly. In the garden, also broken up this spring, are cab- bages, cauliflowers, and other vegetables of the finest de- scription. Timothy and clover had been sown to form a grass plot, and these were now in flower and gave promise of producing abundance of seed. The Governor's farm, situated on the sand hills to the east of his residence, waa also visited. Here the soil, outside the fence, was covered with the short prairie sward indicative of dryness, and which would have been pronounced as unfit for cultivation by most people, yet within the fence were excellent oats, middling barley, short in the ear but grain fine, and first- class wheat, the latter standing thick on the ground, nearly five feet high, with correspondingly long ears, nearly ripe. " Besides the exuberant growth of most grains there is a remarkable vitality imparted to them in this region that astonishes a stranger. I am more and more convinced that it is not soil which is the cause of the astonishing crops pro- duced in the west, but the peculiar climate. When digging up the prairie soil, even in the hardest clays, I could never get below the roots of grass, and these were so numerous that they seemed to fill the soil. Owing to the severe win- ter's frost, and the light rainfall in spring, the young roots are enabled to penetrate the soil to a depth wholly beyond the belief of an eastern farmer. They seem to follow the pores opened by the frost right into the subsoil, and hence, instead of drawing their nourishment from four or five inches of soil, they draw it from eighteen to twenty-four inches." The great plain south of Battleford is not easily described, except in general terms, owing to its immense size and changing character. Coming from Battleford I found excel- lent grass, plenty of good water, and a rich loam or clay soil until I passed some distance south of lat. 52°, and west 102 MANITOBA AND THE GREAT NORTH-WEST. of the same Meridian. My assistant and myself noticed the change from a good strong clay, producing excellent pasture, to another clay covered with Artemisia and small Cactus, where the water was scarce and bad, and the pasture poor and dried up. On examination this clay proved to he the Creta- ceous St. Pierre beds of Dr. G. M. Dawson's Boundary Survey Report, and contains remains of Baculites and other fossils, together with nodules of brown iron ore. This tract of bad land is principally confined to the section between 111th and 112th meridians and between the 51st and 52nd par- allels. Except this region the Great Plain, as far as known, is not arid, but produces good grass, has generally abundance of water, and usually a good soil. This extensive tract is almost wholly without wood of any description. Not a shrub enlivens its surface, except occasional clumps of rose bushes {Rosa hlanda) a few inches high, the western snow- berry {Symjjhoricarpus occidentalis) , and the beautiful Silver berry {Elceagnus argentea). These could not be called bushes except on the ground of being woody. They are never seen more than three years old and hardly ever that. The coulee, in which Tramping Lake lies, is still partly wooded with poplar and maple, but except in this and a few other localities not seen by me, no wood exists. Coulees are quite a marked feature of the plains, but do not appear to be a part of the present natural system of drainage. They seem to be of an earlier geologic time, other than being dry water-courses of the present, and here the few creeks, which carry off the surplus water, originate. The Qu'Appelle Valley is a well known instance ; the val- ley in which the Red Deer Lakes lie is another. Crawling Valley between Red Deer and Bow Rivers is a third, and here on the Great Plains is a fourth, as Tramping Lake Coulee is said to be the head of Eagle Creek on the one side, and a stream emptying into Battle River on the other. As a rule, the lakes found in the coulees are salt, but this is easily CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. 103 accounted for, as their bottoms are always on the Cretaceous clay, and the springs near the bottom of the coulee are brackish likewise, while the springs nearer the prairie level contain good sweet water. All brooks found on the plains, although containing good water themselves, have saline soil along the sides of their valleys, and not unusually there are brackish lakes and marshes in these valleys. Extending northwards from the vicinity of the Bear Hills, is a tract of broken country with deep coulees, salt lakes, and occasional sand hills, which seem to extend westward to Tramping Lake. Much of the soil, however, is very rich, and there are large tracts of farming land intermixed with small areas of a broken and stony character. Captain Palliser's remark as to the barrenness of this country can only apply to the absence of wood, as he speaks again, on page 84 of his Eeport, thus : " The buffalo were seen in great numbers," and that " the country was entirely barren," and again, on the same page, he says, " we found only a swamp containing miserable herbage, which had been cropped by the buffaloes and afforded very scanty pasture for our horses." Here again I presume that the barrenness is not produced by natural causes, but by artificial ones. A perusal of my own journal and that of Mr. Wilkins shows that this region, although not everywhere suited for agriculture, possesses many fine tracts fit for the plough, and always good pasture. In the Pacific Railway Report of 1879, page 90, Col. MacLeod well describes the section he saw. He says : " The whole country is a high rolling prairie, with gravelly ridges running in every direction. Grass of vary- ing quality is to be found everywhere, and water varying with the season." Captain Dairy mple Clarke, in the same Report, says : " I should call the Great Plains a fine grazing country ; in many places the traveller comes across buffalo or bunch grass. This grass is most nutritious and always pre- ferred to other grass by both horses and cattle." With the 104 MANITOBA AND THE GREAT NORTH-WEST. statements of these gentlemen, I entirely agree, and, further- more affirm, that as this same region was the winter home of the buffalo, so in the near future it will be the winter home of immense herds of cattle, which can exist, as they did, by going on to the wind swept hill tops for nutritious food, when the poorer grass of the valleys lies covered by a mantle of snow. Water for cattle no more than for buffalo is needed in winter, as there is always snow enough among the grass to meet their wants. After the first of October our horses went to the hill tops for good grass, and I found on examin- ation that they always cropped the northern buffalo grass {Stipa spartea) or if the hill was very dry, the southern one {Bouteloua oUgostyclia). I must emphatically deny the statements made imputing barrenness to this region, but I admit that running streams or cool springs are extremely rare. Wood is absolutely absent, and even a bush a few in- ches high is seldom seen. The real cause of the absence of wood on every part of the region under consideration is undoubtedly prairie fires which sweep over almost every part of it year after year, des- troying the seedling trees as long as there are any seeds left to germinate, and year by year killing the bushes until the capacity of the root to send up shoots dies out, and then even willows cease to grow. Would any person affirm that wil- lows could not grow on the margin of the ponds where such plants as Polygonum aquaticu7n, Potamogeton perfoliatus and gramineit^, ZJtricularia vulgaris, Alisma Americana, and Sagittaria variabilis could grow and flourish ? And yet the first four of these were found in scores of ponds, and any botanist knows that these require permanent water. It was so moist on the plains that Cacti could not exist, but one could hardly walk through the Red Deer River Valley for them. While on the plains not a bush could be seen, yet in the valley, only a few yards from the Cacti, trees three feet in diameter stood. CHARACTER OF COUNTRY BETWEEN LAT. 52° AND 53°. 105 Palliser states that the southern sides of all valleys were much moister than the northern, and that the southern slopes of all hills were without wood, and deduces from this the aridity of the climate. I am inclined, with all respect, to differ from Captain Palliser in this conclusion. It only proves that a surface inclined to the sun will naturally become dry, while one inclined from it will retain its moisture. When fires come on the plains the dry side of the hill is soon de- nuded, while the moist side is left intact. The inference is plain. If aridity is the cause of the absence of wood, how is it that the sand hills at the head of the Qu' Appelle, where the ground is certainly dry, are covered with it? The Bad Hills to the northwest of Red Deer Lakes, have wood like- wise, while the Bear Hills to the north, which contain no sand, are without even a bush. The sand hills, observed by Mr. Wilkins and myself in the centre of the Great Plain, have brush in some quantity, while on good soil none exists. Finally, there is not a series of sand hills throughout the country, no matter how poor the soil, but what has either wood or brush, while immense tracts of first class soil is without a bush. The rich soil with its abundance of grass afibrds, when dry, fuel for the flame which destroys any seedling that may spring up; at the same time the sand hills, being unable to carry fire through their extreme poverty, keep it alive. Sand and aridity are popularly classed together ; but it should rather be sand and unfruitfulness. The impervious clays are arid throughout the regions explored by me. A comparatively small tract, commencing at Red Deer River, east of Blood Indian Creek, about the 111th Meridian, extend- ing northwesterly to ruear the 52nd parallel, and thence west to the Red Deer River, south of the Squirrels Head, is large- ly a region of impervious clays, and this was the worst tract seen by me or my assistant during the summer of 1879. Much of this tract is without drift, and the Cretaceous clays 106 MANITOBA AND THE GREAT NORTH-WEST. come to the surface, causing aridity, and producing alkaline swamps (white mud swamps), ponds, and lakes in abundance. The Hand Hills and their eastern extension are like an oasis in this unpromising region, for surrounding them on every side is the hard baked clay of the St. Pierre beds. The only soil throughout the region explored which would not naturally produce timber are these Cretaceous clays, well worthy the name " Bad Lands." I therefore maintain that the aridity, where it exists, is the result of soil and not of climate. Palliser, on page 11 of his Report when referring to this region, makes two statements corroborative of this. Describing the valley of the South Saskatchewan Palliser says : — " Even on the al- luvial points in the bottom of the valley, trees and shrubs only occur in a few isolated patches. The steep and lofty sides of the valley are composed of calcareous marls and clays that are baked into a compact mass under the heat of a parching sun. Sage and Cactus abound, and the whole of the vegetation bespeaks an arid climate." Eight lines below this on the same page he says : — " In the midst of the arid plain traversed by the South Saskatchewan, there are isolated patches of table land upon the surface of which the vegetation becomes luxuriant, and pasture of a fair quality may be found. The expedition spent two weeks at the Hand Hills, which form one of those patches, for the purpose of recruiting the horses." Here the natural order of things is reversed, and aridity is in the valley and luxuriance on the hill-tops. Why is this ? Not because of climate certainly, but on account of soil. All the arid spots, all the salt lakes, and the brackish marshes of the entire plain, were traced to one cause — the Cretaceous clay. Artemisia cana seems to be almost peculiar, on our plains, to the Cretaceous clay, and in the north the Cactus can only find on the clay the aridity of soil that is suited to its wants. CHARACTER OF COUNTRY BETWEEN LAT. 52" AND 53°. lOT The vegetation of these clays when dry outside of stream valleys, was characterized by numerous species of Artemisia,, and many Compositae, which in the north preferred salt lands. In Red Deer River Valley, Gacti, Artemisia, and various Ghenopodiacece vied with each other in luxuriance, while grass and the more useful herbaceous plants were almost entirely absent. Lying southwest from Battleford is a fine rich country which is reached about six miles from that " city " The country is almost a perfect level of good clay loam without a bush to break the monotony of the waving grass to the south. A fine rich country extends to the west from Battle- ford for at least eighty miles. It is generally level and often for many miles without a twig. In the vicinity of Manito Lake, there are large quantities of wood, and consequently there is broken country with numerous ponds and marshes. Sounding Lake is a sheet of brackish water about seven miles long and four miles wide, surrounded on its north, east, and south sides with wood, the poplar averaging about six inches in diameter. South of the lake, as far as could be seen, nothing met the eye but conical hills. Between Sounding Lake and the " Nose" the country is hilly', but contains good pasture, wood, and water. The hills generally have a black loamy soil, while the valleys are principally clay or clay loam. Along the north of the lake the country is sandy, extending about six miles to the east where heavy clay with rich grass is met with. The wood ceases as soon as the sand is left. South of this line of travel a series of hills was seen, doubtless a continuation of those over which we crossed before reaching Sounding Lake. The Neutral Hills lie northwest of Sounding Lake. Gen- erally they are mere ridges of broken, more or less wooded, country with clumps of small aspen scattered over their sur- face where protected from fire by either water or sand. Stretching southwest from this point and extending to Tail 108 MANITOBA AND THE GREAT NORTH-WEST. Creek is a wide tract of broken country well suited for stock raising and supplied with abundance of wood and water, both being found of excellent quality in the ravines and narrow valleys opening into Battle River. Sullivan's Lake, a large sheet of fresh water lying about the middle of this section, has much good land around it, but the greater part of this land is best suited for pasturage as it is much cut up by cou- lees and sharp or rolling hills. Lying still further west and between Battle and Red rivers is a tract of fine rich agricultural land that has no superior in the North-West. Still further west is a large district lying around the head of Battle River and south- west towards Red Deer River, where millions of tons of hay grow every year owing to the richness and moistness of the soil. This region though wet is well suited for stock, as the natural grasses are of the very best quality, and shelter is to be had close at hand. The region embraced in this chapter contains a large amount of prairie and forest lands all of the very best des- cription. Rivers and small streams are found in almost every part, and many lakes abounding in fish of excellent quality are dotted over the surface. "West of the Porcu- pine Mountain many beavers are yet trapped in winter. Little game, other than birds, of which there are myriads every spring and fall, is to be found in the country. Bears and wolves are occasionally met with, but no injury to either person or stock is ever done by them. CHAPTER VII. Description of the Govntry Drained hy the North Saskatche- wan and Athabasca Rivers. Extensive District Soutli of Nortli Saskatchewan— One Solid Block of 13,000,000 Acres — Large Area of Fertile Land North of River— Star Mission, its Success— Multitudes of Whitefish — Lac La Biche Mission— Fanning at the Lake— Wheat, Barley, &c. — —Victoria Mission— Small-poz Ravages- Rev. George McDougall his Death, the Edmonton Pioneer — Former Lawlessness at Edmonton — Change Caused by the Police — Edmonton, its Mills, Churches, Stores — Coal and Iron at Edmonton — Review of the Country— Ninty -six per Cent. Good Soil over a Vast Area— Lands for the Irish without Rent— St. Albert Mission, its History and Success— Catholic Mis- sionaries, their Work and Success— Bocky Mountain House, Fine Timber— Gold Washing— Beaver River, very Rich Laud— Green Lake, Abundance of Fish— Chipweyau Indians— Athabasca River and Country— Size of the River and its Tribu- taries — Little Slave River — Pembina River, Coal in its Banks — The McLeod — Baptiste's River— Jasper House and Valley— Climate of the Valley, Snow Fall very Light, Warm Winds, Dry Climate, Spring Weather— Horses Living out all Winter -Source of Warm Winds— Fertile Belt— Richness of It— Where Located— Prairie still Better — Wet Lands — Summer Frosts — Late Sowing — Fall Sowing, its Success. Northwest from Battleford, south of the North Saskat- chewan, the land is rather poor and sandy for fifty miles, but proceeding northwestward beyond this into the valley of the Vermilion River, the soil gets very rich and continues so all the way to Edmonton, a distance of over 200 miles. After leaving Battleford and reaching the meridian of Fort Pitt, the whole country between the North Saskatchewan on the north and Battle River on the south, and for thirty miles beyond Edmonton on the west, may be described as fertile and well suited for settlement. Much of it is so extremely rich, and the exuberance of its vegetation so great, that travellers have extolled it possibly beyond its merits, as large tracts of it are wet and bushy, and, probably, subject to summer frosts. Of that portion south of the telegraph line this cannot be said, as it is generally level, and for the most part with but little water on the surface. This tract is 110 MANITOBA AND THE GEEAT NORTH-WEST. unsurpassed in the North-West for its capacity to grow "wheat as the soil is rich, the surface is almost level, and what slope there is inclines to the south. The great area described above, containing not less than 13,000,000 acres, is yet with- out inhabitant, except the settlements in the vicinity of Edmonton. North of the Saskatchewan is a fine country, commencing a little east of Prince Albert, and extending westerly to Lac St. Ann's, fifty miles west of Edmonton. Owing to the southern bend of the river this tract varies in width from forty to one hundred miles. Throughout the whole of it the soil is warm, containing both sand and gravel, but, nevertheless, is generally rich and very fertile. It has likewise a southern aspect, and will therefore be free from frost in summer. About fifty miles north of Carlton the " Star Mission," in connection with the Church of England, is situated. This Mission was established in 1874, and placed in charge of the Rev. Mr. Hinds, who, besides being a minister, was a practi- cal farmer. He at once commenced to teach the old men farming and the children English, and in less than one year had a number of small farms commenced, and the children well advanced in the knowledge of English. Since then he has been very successful, and in 1879 Mr. O'Keefife, D.L.S., writes of the Mission : " At Sandy Lake the Indians under the supervision of the Rev. Mr. Hinds, Church of England Missionary, were cultivating successfully fine fields of grain and raising vegetables." Of the country in this vicinity the same writer says : " No finer country could be desired than the section above described. The water is pure and abundant, and the land extremely rich. Pea vine, vetches, grasses, and, in fact, all herbaceous plants were luxuriant. Very fine fish are in all the lakes and rivers of the section ; the whitefish being extremely abundant, large, and of fine quality. The timber on this section is not so good as that THE NORTH SASKATCHEWAN AND ATHABASCA COUNTRY. Ill eitlier east or west of it, but many groves were scattered through it. " In the northwestern part of it the land is very good, but the timber is not of large size, being nearly all second growth, as the old timber had been burnt down some years before. The whole section may be classed as level plain, or gently rolling land, no hill being seen higher than fifty feet, except in the vicinity of the Mission. The land generally is a rich loam, with a small percentage of gravel, which indeed is the prevailing character of the soil for many miles. Spring wheat at the Mission, the best I have seen, was fit to harvest August 20th, 1879." Two hundred and fifty miles northwest of the Star Mis- sion is Lac la Biche, where a Koman Catholic Mission has been established for many years. Long before railways were talked of, the Fathers at this Mission had brought in a grist mill, worked by horse power, and here in Lat. 55° wheat was being grown and ground, into flour long before the value of the Red River Valley becaine apparent to Canadians. Marcus Smith, C.E., thus speaks of the Mission : " Lac la Biche is 304 miles from Carlton. Mr. Trail, Hudson's Bay Company's officer at this post, stated that there were about forty families settled on this lake, principally Half-breeds and French Canadians. The Catholic Mission is on the lake shore, about nine miles northwest of the Post ; here I met Bishop Farand, from whom much valuable information was obtained concerning the country to the north and west. " Barley and wheat thrive well here, and also vegetables. There is a grist mill near the Mission. Abundance of white- fish are in this and the neighboring lakes. The timber of the country is spruce, poplar, and tamarac, all of good size. The divide between Beaver River and the Athabasca water- shed is not more than three miles from Lake la Biche." The Victoria and Whitefish Lake Missions are under the 112 MANITOBA AND THE GREAT NORTH-WEST. control of the Canada Methodists, and around each quite a settlement has been formed. In 1871 these Missions were in a very flourishing state, but an outbreak of small-pox devastated the settlement, and when the writer visited the country in 1872, only the chimneys of the houses remained standing. Their occupants were either dead or scattered to the four winds. The Rev. George McDougall, the pioneer Missionary to these parts, lost a daughter at this time, and he told me that the Blackfeet lay around for days waiting a chance to kill him or his wife, because they thought he had brought the calamity upon the country. God mercifully preserved him at that time, but in the winter of 1875 he perished miserably while visiting the Mission at Morleyville then in charge of his son John. On this Mission he had set his heart, and when the writer first saw him in 1872 he told of the wonders of the Bow River country, and prophesied its future greatness. In 1872 his house was the only one out- side the Fort at Edmonton, and lawlessness was so common, even amongst the semi-civilized Indians around the fort, that murders were of frequent occurrence. A month or two before my visit an Indian, from some unexplained cause, became angry with his wife and attempted to kill her with a knife, but she fled from him. He pursued and overtook her, and stabbed her to death a short distance from the fort. A relative of the woman when pointing out the spot where she died, asked with great earnestness when would law reach them, and I replied that it was then on its way m the person of Col. Robertson Ross, the Adjutant- General, who would set everything right. He came and the Mounted Police were sent out, and the murders then so frequent ceased. This is Edmonton society as it was in 1872. The state of farming was very little better. Fully one-half of the ripened wheat was smut, and doubt prevailed whether the THE NORTH SASKATCHEWAN AND ATHABASCA COUNTRY. 113 climate was at all suited for that grain. In 1881 Edmon- ton appears as a town and settlement of great importance. It has its regular agricultural shows, its balls, and its public exhibitions, where the inhabitants vie with each other in such matters as their exhibits, their agility, their personal attractions and refinement. Lawlessness has passed away, and although the stockade is still around the fort, the guns still in the bastions, and the great gate and wicket closed at night, the fear of Indians, like the buffalo, has passed away, and only the Hudson's Bay Company's officials recall the time, scarcely ten years since, when the Blackfeet and Sarcees made night hideous with their fearful yells and threatenings, on account of the cruel murder of two of their number under the very guns of the fort. Edmonton is a general term applied to a district, but still there is a concentration of houses and places of business called by that name. The village is some distance below the fort on the north side of the river. The Church of England and Canada Methodists have each a church, and a Presbyterian Mission having been established, a church will soon follow. There are several stores well stocked with goods suitable to the country, the chief being owned by J. H. McDougall, John Brown, and P. Heinwick, each carrying a stock of goods worth from $25,000 to $30,000, in- cluding freight, which swells the cost of goods in this distant part of the country. Three grist and saw-mills grind all the flour and saw all boards necessary for the settlement, and nothing is wanting now except railway communication, or better steamboat service upon the river. Abundance of coal can be dug out of the river bank, and less than a mile above the fort there is a deposit of bog iron ore, which may prove valuable when properly examined. We are now 890 miles by cart trail northwest from Winnipeg, and over this immense distance pits, four feet deep and twenty miles apart, have been dug, and a careful 8 114 MANITOBA AND THE GREAT NOETH-WEST. examination of the soils shows that only about five per cent, of the -whole distance is unfit for agriculture and classed as third class soils, when compared with those of Prince Edward County which is one of the most productive districts of Ontario. The extent of these fertile lands cannot be realized by any person reading the accounts published in newspapers or blue books, nor even in passing over the trails as these are only particular Imes. But having traversed the country in every direction I am enabled to grasp their immensity, without realising in any appreciable degree their influence upon the future of the civilized world. Seeing millions of acres of arable lands lying without inhabitants in one part of the British Dominions, and learning that in another part people on the brink of starvation are mur- dering each other for the privilege of renting a potato garden, causes one to exclaim against the shortsighted- ness of Governments, in not assisting emigration, and on the other hand against the foolishness of people remaining where their normal state for generations has been and will be one of poverty. Nine miles west of Edmonton is St. Albert Mission, the largest and most prosperous Mission settlement in the North- West. It is the seat of a Bishopric, having Bishop's palace, cathedral church, nunnery, and various other buildings, all of large size and well furnished. The Bishop's palace, as described by a late writer, is a magnificent building . " This is a handsome frame structure, eighty by thirty-two feet, three stories high, including a large attic, lighted by rows ^ of dormer windows, besides a large and well-lighted base- ment." Pere la Comb established the mission in 1858, when this was only an Indian and Half-breed camping ground. Nine years later he was succeeded by Pere la Due, Avho gave place to Bishop Grandm m 1871, and from that to the present time St. Albert has been the seat of a Bishopric, from which many eminent men have gone out to preach the glad THE NOETH SASKATCHEWAN AND ATHABASCA COUNTET. 115 tidings to the beniglited Indian women, that, in the sight of the "Great Spirit," the woman is equal to the man, and by this means to stamp out polygamy and make marriage more respected. Throughout the whole North-West there have been no men, of any Church, superior in any sense to the Fathers with whom the writer has met in his numerous journeys both east and west of the Rocky Mountains. He looks upon their labors as having produced due respect for the marriage relationship, a proper regard for the Sabbath, and an earnest for peaceable conduct and upright dealings one with another, in every part of the country he has visited. Lake St. Ann's may be said to be the present limit of available land on the old line of the C. P. R. Little farming is carried on. The whitefish fisheries constitute the most noteworthy industry. These were more highly valued in years gone by when people and dogs depended almost entire- ly on meat, but at present they receive little attention The Rocky Mountain House was formerly the frontier trading post on the borders of the Blackfeet country, and here the plain Indians came in all the splendor of their untutored savagary, and in days when Rum was king held their wild orgies in front of the fort. Since the advent of the police, and peace with the Crees, the Blackfeet roam and trade at will, and this fort has lost much of its impor- tance as a trading post. This post is about 150 miles south- west of Edmonton, within sight of the Rockies and on the margin of the Saskatchewan. It is 3,195 feet above the sea and the neighborhood is of very little value as a farming coun- try. Splendid groves of spruce and even forests of the same tree are on the upper Saskatchewan and its tributaries, and here in future will probably be the headquarters of the Rocky Mountain lumbering companies. Gold washing has been practised for many years in the vicinity of Edmonton, but in no case has success been 116 MANITOBA AND THE GREAT NORTH- WEST. SO marked as to cause any parties to leave off farming for the purpose of prosecuting it. That fine flour gold is de- posited on the bars each year is certain, but where it comes from, or whether it exists in large quantities, is still a matter of doubt. Beaver Eiver flows in a valley parallel to the North Sas- katchewan, from a point nearly north of Edmonton to the Meridian of Carlton, a distance in a straight line of nearly 300 miles. It turns north at Green Lake, 150 miles north of Carlton, apparently into a valley of which Green Lake is a part. When the Beaver river is high in spring, it fills Green Lake by means of a small stream connecting the two, but as its waters lower the current changes and the Lake begins to empty itself. The valley of Beaver River contains very rich land, but future experiments are necessary before wheat can be relied on as a sure crop. Green Lake is about eighteen miles long by from one to two wide. It is surrounded on all sides by a very fine poplar or aspen forest. The soil is rich and the climate suit- able for the growth of wheat. Beaver River and Green Lake, like all the northern rivers and lakes, are full of whitefish. Throughout all the northern forests the Chipweyan locates himself on the margin of a lake, builds himself a house, clears a potato patch, and sets his nets. A visit to these nets twice a day gives him his food the year round, and his potato patch in the fall, and a few bears furnish him with a change before winter sets in. When he retires to his win- ter hunting ground, near a lake, he sets his nets under the ice, and is still independent of four-footed game The Athabasca country is very little known, as it is all covered with forest and difl&cult of access. Much of it is wet, and that section through which the old C. P. R. line passes is very wet and marshy, and full of muskegs. These are veritable peat bogs being composed of the same material as the bogs of Ireland and Scotland. THE NOETH SASKATCHEWAN AND ATHABASCA COUNTRY. 117 The Athabasca at Fort Assiniboine, northwest of Edmon- ton, is fiilly 300 yards wide, being rather larger than the Saskatchewan at this point and flowing in a wider and deeper valley. About sixty miles northeastwards from this place it receives the discharge of Little Slave Lake from the west. The valley of this river is generally level and the soil on either side of the stream seems excellent sandy loam, and where free from timber abounds in rich grass and pea vine. Ascending the Athabasca from this point the first river met with is the Pembina, a stream about thirty yards wide, flowing from the southwest. This stream rises further out on the plain than any other belonging to the Arctic basin. It is known to show large exposures of coal in many parts of its course of a quality much superior to that of Edmonton. Proceeding still to the southwest we pass the mouth of the McLeod, a large stream one hundred yards wide. Here the banks of the Athabasca become 300 feet high. Below this stream a sandstone clifi" 100 feet high, having a coal seam five feet thick, is passed. Proceeding still up stream we reach Baptiste's Eiver, a tributary from the west which is ninety yards wide. On this stream there is abundance of fine timber of various species, the spru^se as on all other streams, proving to be the best. Jasper House is beautifully situated on an open plain, about six miles in extent within the first range of the Rocky Mountains. As the valley makes a bend above and below, it appears to be completely encircled by mountains which rise from 3000 to 4000 feet, with bold craggy outlines. The little group of buildings which form the "fort," has been constructed in harmony with the picturesqueness of the situation, after the Swiss style, with overhanging roofs and trellised porticoes. The dwelling house and two stores form three sides of a square, and these with a little detached hut constitute the whole of this remote establishment. The clim- ate of this valley is remarkable and is worthy of a passing 118 MANITOBA AND THE GREAT NOKTH-"WEST. notice. Mr. W. Moberly, C.E., who spent the winter of 1872-3 in the Jasper valley, twenty-two miles from the summit of the Rocky Mountains, says in his report to Mr. Fleming : — " The total fall of snow in the winter of 1872-3 at our depot in Jasper Valley, twenty-two miles east of the summit of the Yellow Head Pass, was two feet one and a half inches, and the greatest depth on the ground at one time was six and one-half inches. Jasper Valley from the Miette, and as far down the Eiver Athabasca as I have been, viz., about forty miles below Jasper House, has a dry climate. With the exception of a few occasional drops, I never saw any rain. There were some spells of frost in November, and a continuance of very cold weather in December ; it was cold in January, and four or five days in February ; at other times during the winter the weather was comparatively warm, frequently not even reaching the freezing point. The winds that blow with much violence render Jasper Valley unpleasant in the win- ter; the northeast wind always brought cold, and the southwest warm weather. " From the beginning of March to the 20th May, with the exception ot a little snow on the 26th and 27th April, the Weather was rdnarkably fine. This is the best season for field work as the flies do not make their appearance until the beginning of June. Comparatively speaking, the win- ter months in the district referred to are not as severe as at Toronto. To give an instance, I will mention that the pack animals (horses and mules) with the expedition, after an unusually hard season's work of about nine months duration, when they were very much worn out and nearly starved, after packing the supplies over the Rocky Mountains by the Athabasca Pass, the altitude of which is 6025 feet above the sea, and at a time when severe weather and snow storms were almost incessant, — the animals were turned out about the 20th January to shift for themselves, as we had no fod- der for them. Not a single one of them died and they were THE NORTH SASKATCHEWAN AND ATHABASCA COUNTRY. 119 all in fair condition when they resumed work the following March." This exceptional climate is only found along the base of the mountains, because when Mr. Moberly started east in March, he found a moister and cooler climate in the valley of the McLeod as he moved in the direction of Edmonton. It is extremely probable, as he states in another part of his report, that the warm currents of air that cause this dry and warm climate at the head of the Jasper Valley, come up the valley of the Columbia, from the " Great Columbian Desert " east of Walla Walla and pass through the mountains by the Athabasca and Yellow Head Passes. Although the country lying between Jasper Valley and Lac St. Ann's is supposed by many to be of little value on account of bog and marsh, later explorers show that this opinion is in part groundless, as Mr McLeod, C. E., speaks in high terms of certain tracts on the McLeod and Pembina rivers which were before thought to be marshy. The " Fertile Belt " of Palliser is that section of the arable lands which we have been describing in this and the pre- ceeding chapter. The opinions of Palliser were based on the vegetation alone, and where he met with prairie and short grass this he pronounced a desert, while he praised exceed- ingly the rich but moist lands lately denuded of forest. It is now known that the prairie lands are better suited for im- mediate settlement, and less subject to summer frosts, which prove so injurious to late sown grain on the more ele- vated and moister sections of the country. All the land on the Saskatchewan is not equally suited for agriculture, but there is no tract where there will not be continuous settlement, and when we speak of summer frosts and too much water and muskeg, and late harvests, we do not wish to be understood as being afraid of these, but only to state that these drawbacks exist. All the wet land in the country can be very easily 120 MANITOBA AND THE GREAT NORTH--WEST. drained, as there is plenty of fall. Even at present it is a question whether there is too much water in any part recently settled. There are summer frosts in some locali- ties, and late grain has heen injured, hut m the year 1880 none was damaged that was sown before the 10th June. Surely this is late enough when seeding commences over the whole country by April 20th. For the last three years I have been recommending fall sowing as a sure means of escaping injury from frost. By fall sowing I mean seeding so late that germenation will not take place before spring. This has been tried by Mr. Bannatine of Winnipeg, and he reaped his grain two weeks ahead of that sowed in the spring. CHAPTER VIII. Peace River. Position of the Lands Described — Area of the Eegion in Question — Character of Books and Soil — Its Composition and Disposition — Peace Eiver Prairie — ^Location of Prairie — Sandy Soils along Athabasca — Origin of Peace Eiver Prairie — 'Wonderful Vegetation — Climate of Peace Eiver — Summer of 1879 — All Sorts of Grain and Vege- tables Mature — Eipening of Grain at Dunvegan and other Points — Depth of Snow — Setting in of "Winter — Opening of Spring — Breaking up of the Ice — Difference in Climate of Valley and Plateau — Occurrence of Frost — Comparison of Temperatures — Peace Eiver Spring as Early as in Manitoba — Cause of Exceptional Climate — Chinook Winds — Length of Day and Increased Sunlight give Warm Summers — Immunity from Grasshoppers — Description of Little Slave Lake — Eipening of Grain at this Point — Whitefish in the Lake — Abundance of Beaver — Climate Unchanged to the North— Soil of the Northern Plain — Eipening of Grain at Vermilion — Summer Climate of that Region — Milder Climate Farther North at Little Eed Eiver — Vicinity of Fort Chipweyan — Extraordinary Wheat on Poor Soil — Crops at Fort Simpson on Mackenzie's Eiver — Climate and Crops at Fort Liard, Lat. 61° — Barley Eipens under the Arctic Circle — Farming on Peace Eiver a Success — Lakes Teeming with Fish — Birds in Countless Flocks — Eocks of Peace Eiver, Limestone, Gypsum — Abundance of Salt Bituminous Shales on Athabasca Eiver — Tar Springs — Descrip- tion of the Eiver — Appearance of its Banks — Land Between the Athabasca and the Peace Elvers. Dr. George M. Dawson, F. G. S., was sent out by the Dominion Government in company with one of the C. P. E. surveying parties in 1879, and spent the greater part of the summer in exploring the Peace River country, and the fol- lowing extract is taken from his official report. I prefer giving his report to my own as he takes up the whole subject : " The portion of the Peace River country, for which the exploration of last season enables pretty accurate general information to be given, may be considered as extending eastward from the Middle Forks of Pine River. West of this point, as already stated, the areas of fertile land are small, being confined to certain river valleys, which pene- trate the foot hills of the Rocky Mountains and high plateau 122 MANITOBA AND THE GEE AT NOETH-WEST. attached to them. With this western limit, the region now to be described may be considered as bounded on the north by the fifty-seventh parallel, to its intersection eastward with the Peace River. Thence the boundary may be assumed to follow the Peace River southward to the mouth of Heart Brook, near the confluence of the Smoky River. Thence to run southeastward to the extremity of Lesser Slave Lake, to follow the western border of the hilly region lying to the south of the lake to the Athabasca River ; thence to follow the Athabasca westward to the foot hills, and skirt- ing the foot hills to run northwestward to the first men- tioned point on Pine River. " The tract included within the limits above given has an area of about 31,550 square miles, and by far the larger part of this area may be classed as fertUe. Its average elevation may be stated as little over 2,000 feet, and this is maintained with considerable uniformity, for though the general surface slopes slightly from the north and south toward Peace River, the region as a whole may be consid- ered as a plateau through which the great gorge-like valley of the Peace has been excavated. This valley has in general a depth of 600 to 800 feet below that part of the plateau bordering it, with a width of two to three miles from rim to rim. Its tributary streams, at first nearly on the plateau level, flow in yalleys of continually increasing depth as they approach that of the Peace River. Those from the southeastern portion of the region rise either in the Rocky Mountains, or near the Athabasca, the tributaries received by the latter stream from the north and northwest being — with the exception of the Batiste — quite inconsiderable in this part of its course. " The ridges and hills by which this region is occasionally diversified, appear in all cases to be composed either of the generally soft rocks of the Cretaceous and Tertiary, or of arenaceous clays containing erratics, and representing the PEACE EIVER. 123 boulder clays of the glacial period. These elevations are generally slight, and with exceedingly light and gradual slopes, the scarped banks of the streams constituting much more important irregularities. These ridges, however, often resemble detached portions of a higher plateau, and spread widely enough to occupy in the aggregate a considerable area, of which the soil is not so uniform in character as else- where. With these exceptions, the soil of the district may be described as a fine silt, resembling the white silts of the Nechacco basin previously referred to, and not dissim- ilar from the loess-like material constituting the subsoil of the Eed Kiver Valley in Manitoba. This silt, at a short distance below the surface, is greyish or brownish in color, but becomes mixed superficially with a proportion of vege- table matter to a varying depth. It has evidently been deposited by a comparatively tranquil body of water not loaded with ice, probably toward the close of the glacial period, and has either never been laid down on the ridges and undulations above referred to, or has been since re- moved from them by natural processes of waste. As evi- denced by the natural vegetation its fertility is great. " West of the Smoky River, both to the south and north of Peace River, there are extensive areas of prairie country, either perfectly open and covered with a more or less luxuri- ant growth of grass, or dotted with patches of coppice and trees. " The northern banks of the Peace River Valley are also very generally open and grassed, and parts of the Valley of the Smoky and other rivers have a similar character. The total area of prairie land, west of the Smoky River, may be about 3,000 square miles. The remainder of the surface is generally occupied by second-growth forest, occasionally dense, but more often open and composed of aspen, birch, and Cottonwood, with a greater or less proportion of conif- erous trees. Some patches of the original forest, however, 124 MANITOBA AND THE GREAT NORTH-WEST. remain, particularly in the river valleys, and are composed of much, larger trees, chiefly coniferous, among which the black spruce is most abundant. Handsome groves of old and large cottonwoods are also to be found in some of the valleys. Where the soil becomes locally sandy and poor, and more particularly m some of the more elevated parts of the ridges before described, a thick growth of scrub pme and black spruce, in which the individual trees are small, is found ; and in swampy regions the tamarac is not want- ing, but grows generally intermixed with the black spruce. " East of the Smoky Kiver, and southward toward the Athabasca, the prairie country is quite insignificant in extent, the region being characterized by second growth woods of the character just described, which, on approaching the Athabasca, are replaced by extensive and well-nigh im- passable tracts of brul6 and wind-fall, in which second- growth forest IS only beginning to struggle up. " Though the prairies are most immediately available from an agricultural point of view, the regions now covered with second-growth and forest, where the soil itself is not inferior, will eventually be equally valuable. The largest tract of poor land is that bordering the valley of the Athabasca on the north. This rises to an elevation considerably greater than most of the region to the north and west, and appears during the submergence to which the superficial deposits are due, to have been exposed to stronger currents, which have prevented the deposition of the fine silt, causing it to be replaced by a coarser silt which passes m places with actual sand, and alternates with ridges of boulder clay. This region is also often very swampy, and for a width of twenty to twenty-five miles on the trail from Sturgeon Lake to the Athabasca is quite unsuited to agriculture, though still in many places capable of yielding good summer grazing when the forest has been completely removed by fire. To the northward, more particularly to the east of PEACE RIVEK. 125 Smoky River, peaty and mossy swamps occupy part of the surface, and these may be regarded as permanently unsuited to agriculture. " There is also a sandy tract, though of email width, along the lower part of the Elk River near its junction with the Smoky Deducting, as far as possible, all the areas known to be inferior or useless, with about 20 per cent, for the por- tions of the region under consideration, of which less is known, the total area of land, with soil suited to agricul- ture, may be estimated as at least 23,500 square miles. In the absence of complete maps, such an estimate cannot be otherwise than very rough, but may serve to give some idea of the fact. " Whatever theory be adopted, and may have been ad- vanced, to account for the wide prairies of the western por- tion of America further to the south, the origin of the prairies of the Peace River is sufficiently obvious. There can be no doubt that they have been produced and are main- tained by fires The country is naturally a wooded one, and where fires have not run for a few years, young trees begin rapidly to spring up. The fires are, of course, ulti- mately attributable to human agency, and it is probable that before the country was inhabited by the Indians it was everywhere densely forest-clad. That the date of origin of the chief prairie tracts now found is remote, is clearly evi- denced by their present appearance, and more particularly by the fact that they are everywhere scored and rutted with old bufialo tracks, while every suitable locality is pitted with the saucer-shaped " bufi"alo wallows." It is reported that a few buffaloes were seen last year near Pine River, but the animal has now become in the Peace River country practically extinct; an event which, according to the Indians, happened at a date not very remote, owing to a winter of exceptional severity, during which the snow ' reached to the buffaloes' backs.' 126 MANITOBA AND THE GREAT NORTH-WEST. " The luxuriance of the natural vegetation in these prai- ries is truly wonderful, and indicates, not alone the fertility of the soil, but the occurrence of a sufficient rain-fall. The service berry, or amalanchier, and the choke-cherry, are very abundant in some places, particularly on the so-called Grande Prairie, which constitutes the great berry gathering ground of the Indians. " With regard to the climate of the Peace Eiver country, we are without such accurate information as might be ob- tained from a careful meteorological record, embracing even a single year, and its character can at present be ascer- tained merely from notes and observations of a general character, and the appearance of the natural vegetation. " It may be stated at once that the ascertained facts leave no doubt on the subject of the sufficient length and warmth of the season to ripen wheat, oats, and barley, with all the ordinary root crops and vegetables, the only point which may admit of question being to what extent the occurrence of late and early frosts may interfere with growth. This remark is intended to apply to the whole district previ- ously defined, though it must be remembered, in consider- ing the subject, that the conditions of places situated in the bottom of the trough-like river valley, and 600 to 800 feet below the plateau, may be considerably different from those of its surface. " The summer season of 1879 was an unusual one, charac- terized by excessively heavy rain-fall, with cold raw weather in the early summer months. These conditions did not extend to the west of the Rocky Mountains, but appear to have been felt over the entire area of the plains to the Red River Valley. As a result of this, the crops generally throughout the North- West were later than usual, and the mean temperature of even the latter part of the summer appears to have been rather abnormally low. Not- withstanding this, on my arrival at Dunvegan, on the 16th PEACE RIVER. 127 of August, small patches of wheat and barley in the garden of the fort presented a remarkably fine appearance, and were beginning to turn yellow. On my return to the fort on August 31st these were being harvested, their com- plete ripening having been delayed by overcast and chilly weather which prevailed between these dates. At the first mentioned date potatoes were quite ripe, with the balls formed on the stalk, and the garden contained also fine cabbages, cauliflowers, beets, carrots, onions, lettuce, and tur- nips. Dwarf beans, cucumbers, and squashes, were also flourishing, and though these plants are particularly tender, showed no sign of frost. The two last named having been sown m the open ground did not appear likely to perfect their fruit. A few stalks of Indian Corn were also grow- ing, though it is improbable that this plant would ripen its seed m this district. " When this garden was again visited on the last day of August, the beans, cucumbers, and squashes had been 'cut down by a frost, but not completely killed. The potato tops were also slightly nipped. " Rev. M. Tessier, who has been at Dun vegan as a Mission- ary for some years, has always been able to ripen small, black butter-beans, but in some seasons not without difii- culty owing to frosts. He has also tried a few grains of oats which he procured accidentally, and obtained a return of astonishing adundance. About the date just referred to the potato plants at Smoky River post (The Porks) were badly cut down by frost, the tubers being, however, quite ripe, fine and large. " On the 15th September Mr. R McConnell, my assist- ant, found the potatoes in the garden of the fort at the west end of Lesser Slave Lake, and on the level of the plateau, little affected by frost, with tubers large and ripe. Mr. H. J. Gamble also ascertained that wheat thrives at this place. We found some rude attempt at cultivation also 128 MANITOBA AND THE GREAT NORTH-WEST. at the Cree Settlement, which consists of a few log houses built by Indians on the border of Sturgeon Lake, about seventy miles southwest of the west end of Lesser Slave Lake, and is at the average level of the country, with an elevation of about 2,000 feet. Here, on September 14th, the potato plants were slightly affected by frost, but not more so than observed with those at Dunvegan two weeks before. The tubers were quite ripe, but the Indians did not intend to dig them for about ten days. Turnips were very fine, and carrots, beets, and onions were good, though evi- dently cultivated with very little care. Two or three very small patches of barley had been almost completely destroyed by mice, but a few stalks remaining were quite ripe and with fine heads. The Indians here were very anxious to have a supply of garden seeds, which I have since been able to forward to them by the kindness of Messrs Stobart, Eden & Co., of Winnipeg. " At Fort St. John, ninety -five miles west of Dunvegan, and so much nearer the mountains, on July 26th, 1875, Professor Macoun states that potatoes, oats, barley and many varieties of vegetables were in a very flourishing state in -"Nigger Dan's" garden. The oats stood nearly five feet high and the barley had made nearly an equal growth. The barley and oats were both ripe about the 12th of August. Professor Macoun was informed by Charlette at Hudson's Hope, thirty miles still further west, that in 1874 there was no frost from the 1st of May until the 15th of Septem- ber. In 1875 sowing commenced the last week in April. There appears to have been a frost on June 28th, but the first autumn frost occurred on the 8th of September, and Mr. Selwyn found the potato tops still green in the middle of the month. Mr. H. J. Gamble saw wheat flourishing i here in July last, but on his return in September it had been cut down by frost. " Such are the notes that can be obtained on the growth of PEACE KIVER. 129 cereals and vegetables in the district in question, Erom information obtained at Dunvegan, it seems that the snow disappears about the middle of April, westerly winds sweep- ing it away fast. The river opens at about the same time. Cultivation begins at about the end of April or first of May. The river generally begins to freeze in November. The depth of snow, I was told, averages about two feet, an es- timate which agrees with Mr. Horetzky's statement. Mr. Horetzky was also told that the plains were often nearly bare up to the month of December, though the winter usually sets in with the month November. Sir Alexander Mackenzie remarked the same absence of snow in the early winter months of 1792. It was entirely gone on April 5th, 1793, and gnats and mosquitoes were troublesome on April 20th. Horses almost invariably winter out well without requiring to be fed. Hay should te provided for cattle, to ensure perfect safety, for a period of three or four months, though in some seasons it is necessary to feed the animals for a few weeks only. The Indians of the " Cree Settlement " on Sturgeon Lake, previously referred to, winter their horses "without any difficulty round the borders of a neighbouring lake, the shores of which are partly open. From Hudson'b Hope the horses are sent southward to Moberly's Lake to winter, and according to Mr. Selwyn, do well there. Lesser Slave Lake, with its wonderful natural meadows, has long been known as an excellent place for wintering stock, and is referred to as such by Sir J. Richardson. " Some general idea of the length and character of the seasons at Fort St. John may be gained by an examination of the extracts from the journals from 1866 to 1875, pub- lished by Mr. Salwyn. The dates of opening and closing of Peace River being an important clue to the mean tem- perature of the region, may be quoted as summarized by Professor Macoun in the same report (p. 156) : 130 MANITOBA AND THE GREAT NORTH-WEST. Ice breaking Ice drifting first time. 1867 , 2l6t November 8th. 1868 , , 20tii NoTcmber 7th. 1869 , , 23rd Norember 8th. 1870 , 26th No record. 1871 , , 18th November 10th. 1872 , ,- 19th. . November 8th. 1873 , 23rd November 4th. 1874 , 19th October 31st. 1875 , , 16th " The average date of the breaking up of the ice may thus be stated to be April 21st ; that on which ice is running on the river for the first time, November 7th. In 1792 and 1793, when wintering at the mouth of Smoky River, Sir Alexander Mackenzie observed the ice to be running for the first time on November 9th, while the river was clear of ice on the 25th April. I have been unable to find any precise records of the dates of closing and opening of the Saskatche- wan, biit Dr. Hector states these are usually the second week of November and the second week of April respectively. The Saskatchewan is a more rapid stream than the Peace. " With regard to the probable difference between the actu- al valley of the Peace and the plateau forming the general surface of the country, Professor Macoun observes, speaking of the vicinity of Fort St. John, that notwithstanding the difference m altitude the berries on the plateau ripened only about a week later than those near the river, while he was informed that there was about the same difference in the time of disappearance of the snow in spring. While at Dunvegan I ascertained that a similar difference was observed there, but it was added that this obtained chiefly with the wooded parts of the plateau, the snow disappearing on the prairies much about the same time as in the valley. In my diary, under date September 5th, I find the follow- ing entry : ' Aspens and berry bushes about the Peace River Valley now looking quite autumnal. On the plateau PEACE RIVER 131 800 or 900 feet higher, not nearly so much so. Slight tinge of yellow only on some aspen groves.' This difference, though not altogether constant and depending much on diversity of soil, appears to be actual. In October, 1872, Mr. Horetzky writes : ' We observed that, curiously enough, the vege- tation upon these uplands did not appear to have suffered so much from the effects of frost, this being probably due to the fact of the air in these upper regions being constantly in motion, while in the deep and capacious valley of the river the winds have often no effect.' " The difference between the valley and the plateau being thus very small, I have not treated separately the observa- tions for temperature taken by myself in the different situations. Most of the observations, however, refer to the plateau, and including the whole time spent in the country, from the Middle Forks of Pine River to the bank of the Athabasca, cover a period of nearly two months. The mean minimum temperature for the month of August, deduced from observations extending from the 6th to the 31st of the month, is 39' 9°. The mean of observations at 6 a.m. during the same period is 42-3° ; that of the observations at 6 p.m. 59-5°. In September the mean minimum tempera- ture was 28-1°. The mean of morning observations 34'3° ; of evening observations 51"5° I have endeavored to deduce from these observations mean temperatures for the months in question, by correcting them by the tables of hourly variations m temperature given by C. A. Schott in the Smithsonian Contributions to Knowledge (No. 277), but find it impossible to do so, as the daily range is here so much greater than that of any of the places represented by the tables, which refer chiefly to the eastern portion of the continent. It would appear that while in most places the mean temperature of the day is reached about 8 p.m., it is found in the Peace River country not far from 6 p.m., by reason of the increased rapidity of loss of heat by radiation 132 MANITOBA AND THE GREAT NORTH-WEST. due to greater elevation and drier atmosphere. The maxi- mum temperature was seldom observed, but the daily range was very great, and the maximum probably several times reached 80° in August, and often surpassed 70° in September. " From the 6th to the 31st August I registered two nights of frost, on the 13th and 20th of the month when the ther- mometer showed 32° and 26° respectively. Both of these were observed on the plateau, but one at least of them (that of the 20th) must have occurred also in the valley, from the effects produced at Dunvegan on tender vegetation. These frosts occurred m very fine weather, following a day of strong westerly wind, the result of which is to remove from the surface of the earth the whole of the lower heated layer of the atmosphere. This, succeeded by a calm and cloudless night with transparent sky, causes the ther- mometer to sink below the freezing point before morning When not preceded by strong wind, mere transparency of the atmosphere seems seldom or never to lead to frost m August m this district, as many beautifully starlight nights, without an approach of the mercury to freezing-point, were observed " Though in some cases such frosts as these may be general, and extend over a wide district of country, it is more usually found that they are quite local m character. A few floating clouds, or light wreaths of mist, may arrest radiation so far as to prevent frost over the greater part ol the country, while some spot accidentally exposed during the whole night under a clear sky experiences a tempera- ture below 33°. The contour and character of vegetation of the country also have much to do AVith the occurrence of I'rosts, and it is very frequently the case that river valleys are more subject to frosts than the upland districts. Dur- ing the month of September, in a region for the most part wooded, and often above the average altitude, between Dunvegan and the Athabasca, nineteen frosts were regis- PEACE EIVER. 133 tered, the actually lowest temperature being 20' on Septem- ber 18th. " Through the kindness of Colonel Jarvis, of the North- West Mounted Police, I have been able to secure a copy of records kept by Dr. Herkomer, of Port Saskatchewan, on the Saskatchewan River, about twenty miles northeast of Edmonton. For comparison with the observed tempera- tures m the portion of the Peace River country now dis- cussed, they are invaluable; for in the whole district sur- rounding Fort Saskatchewan and Edmonton, we now know from actual and repeated experiment that wheat and all other ordinary cereals and vegetables thrive, and yield most abundant crops. The climate in its great diurnal and annual range, corresponds exactly with that of the Peace River country. Fort Saskatchewan is situated on the brow of the Saskatchewan Valley, about seventy feet above the river, and therefore probably less liable to frosts than either the bottom of the river valley or extensive flat tracts of plain, where there is little circulation of air. This, with the position of the thermometers in regard to the buildings, leads to the belief that if at all in error, as representing the climate of the region generally, the indicated tempera- tures are slightly too great. The thermometer appears to have been read in all cases to the nearest degree only. " A comparison may be made between the temperature observed in the Peace River country duriug August and September, with those at Fort Saskatchewan, as follows : — Peace Eiver Country, mean of minima during August; 39-9°. II II " « « " September, 28-1°. .1 " " Frosts experienced during August, 3. II II « " " September, 19. Fort Saskatchewan, mean of minima during August, 39 '3°. 11 II « " " September, 31-1°. II " Frosts experienced during August, 0. II II II " " September, 15. II II mean of maxima for August, 77-8°. 11 II « « September, 6-81°. II II temperature of August, SS-S". II II " September, 49-6°. 134 MANITOBA AND THE GREAT NORTH-WEST. " The mean of maxima and actual mean temperature for the month cannot be stated for the Peace River country. The actual mean for Port Saskatchewan is obtained by adding the minima and maxima for each month together, and is probably very nearly correct. " While regretting that the data at disposal for the deter- mination of the agricultural value of the Peace Eiver country are not more ample, we may, I believe, arrive with consi- derable certainty at the general fact that it is great From such comparison as can be made, it would be premature to allow that the climate of the Peace River is inferior to that of the region about Edmonton or the Saskatchewan. It is true that in both the Saskatchewan and Peace River dis- tricts the season is none too long for the cultivation of wheat, but if the crop can be counted on as a sure one — and experience seems to indicate that it may — the occurrence of early and late frosts may be regarded with comparative indifference. The season is at least equally short through- out the whole fertile belt from the Peace River to Mani- toba, though early and late frosts are not so common m the low valley of the Red River. The almo t simultaneous advance of spring along the whole line of uhis fertile belt is indicated by the dates of the flowering of the various plants, a point referred to by me m some detail elsewhere. It is further unquestionable that the winter is less severe, and not subject to the same extremes in the Peace River and Upper Saskatchewan regions as in Manitoba. " We have already found reason to believe that the early and late frosts, and not the absence of a sufficient aggregate amount of heat, constitute the limiting condition of wheat culture in the North- West; but that neither the Saskatche- wan nor the Peace River countries he upon the actual verge of the profitable cultivation of wheat appears to be proved by the fact that oats succeed on the Saskatchewan, and also ■ — in so far as one or two seasons can be accepted as evidence PEACE RIVER. 135 — on the Peace River; while it is well known that this cereal is less tolerant of summer frost than wheat. This is further proved by the fact that at Fort Vermilion and Athabasca Lake, 180 and 300 miles respectively northeast of Dunvegan, Prof. Macoun found wheat and barley ripen- ing well ; but in this instance the fact is complicated by the circumstance of the decreasing altitude of the country which introduces a new condition. As no knowledge has been gained of this country on the Lower Peace in addition to that collected by Prof. Macoun in 1875, it is not included m the above discussion, though from it additional great areas might doubtless be added to the fertile tract. "Referring to the journals kept at Fort St. John, Mr. Selwyn, in the report already several times referred to, comes to the conclusion that the climate of the Peace River com- pares favorably with that of the Saskatchewan country, or Montreal. " It has often been stated in a general way that the cause of the exceptionally favorable climate of the Saskat- chewan and Peace River countries, as compared with those of the eastern portion of the American continent, is to be found in the prevalence of warm westerly winds from the Pacific. Sir Alexander Mackenzie speaks of these westerly winds in winter, writing : ' I had already observed at Athabasca that this wind never failed to bring us clear mild weather, whereas, when it blew from the opposite quarter, it produced snow. Here it is much more percep- tible, for if it blows hard southwest for four hours a thaw is the consequence, and if the wind is at northeast it brings sleet and snow. To this cause it may be attributed that there is so little snow in that part of the world. These warm winds come off the Pacific Ocean, which cannot, in a direct line, be very far from us, the distance being so short that, though they pass over mountains covered with snow, there is not time for them to cool.' 136 MAKITOBA AND THE GREAT NOETH-WEST " Farther south these southwesterly currents are known as ' Chinook Winds,' and similar consequences are observed to accompany their occurrence. Sir Alexander Mackenzie, however, in the summer of 1793, found the distance to the Pacific coast from his wintering place, at the mouth of Smoky River, greater than he appears to have imagined at the time he penned the above quoted remarks, and it is difficult indeed to understand how currents of air, blowing for at least 350 miles across a country which is for the most part mountainous, should retain enough warmth to temper effectually the climate of the plains to the east. This diffi- culty would appear to be particularly great in summer, when the mountains are largely snow-clad, and the mean temperature of the Peace and Saskatchewan Valleys, is pro- bably considerably in excess of that of the region interven- ing between them and the sea. " In addition to the favorable climatic conditions indicat- ed by the thermometer, the length of the day m summer in the higher northern latitudes favors the rapid and vigorous growth of vegetation, and takes the place, to a certain extent, of heat in this respect. This has been sup- posed to be the case from the luxuriant vegetation of some northern regions, but Alfonse de Candolle has put the matter beyond doubt by subjecting it to direct experiment. In latitude 56°, which may be taken as representing that of mucb. of the Peace River country, sunrise on 21st June occurs at 3h. 12m., sunset at 8h. 50m ; while six degrees further south in latitude 50°, which may be assumed to represent Manitoba, sunrise occurs on the same day at 3h. 49m., sunset at 8h. 13m. The duration of sunlight, in the first case, is 17h. 38m. ; in the second, 16h. 24m., or one hour and a quarter in excess in the northern locality. This excess of course decreases to zero at the spring and autumn equinoxes, and the difference is reversed in the winter. " A further circumstance giving to the Peace River country PEACE RIVER. 137 and that on the upper part of the Saskatchewan, other things being equal, a value as farming land acre for acre considerably greater than that of most parts of the North- West, is the immunity of this region from the visits of the devastating locust or grasshopper {Galaptenus sjpretus). I have elsewhere discussed the question of locust invasions, in several papers, and it has since been taken up by the United States Entomological Commission It must suffice to state here, that while a long series of years may pass with- out the occurrence of serious invasions, these must continue always, or at least for a very long time, to constitute a drawback to the whole territory lying south of a line drawn about sixty miles soath of Edmonton, and thence nearly following the border of the wooded country eastward and southward to Manitoba." Little Slave Lake lies nearly east and west. It is about seventy-five miles long, with an average breadth of about five miles. The south shore is low and marshy Extensive marshy meadows are around the southwestern extremity, but owing to willow thickets their extent is unknown. South of the lake the country is hilly, some of the hills even rising into mountains, but to the north the country becomes level and is said to pass into marsh some distance from the lake Vegetables in abundance are raised at the Post, and wheat and barley grow well but are seldom sown. Barley ripened here on August 12th, 1872, while at Edmon- ton the same year it did not mature until the 26th of that month. Large numbers of white fish are caught in the lake, and in the surrounding woods moose are quite common, being indeed the chief food of the people. Many beaver are still to be found in the neighbourhood, and the Rev. Mr. Gordon reports that as many as 8,000 were obtained in the winter of 1878. From the Rocky Mountains to very nearly Fort Simpson 138 MANITOBA AND THE GREAT NORTH-WEST. in latitude 62° there is scarcely any difference in soil or climate, except that the latter improves as we recede from the mountains. Near Fort Vermilion, in latitude 58° 24', I found both soil and climate everything I could desire. The soil here is of the very best description, evidently alluvial and of great depth. About half a mile from the river the land rises nearly fifty feet, with increased luxu- riance of vegetation, although two degrees north of St. John barley and vegetables grow much c[uicker and ripen earlier than at that Post. Barley sown on 8th May was cut August 6th, having been on the ground just ninety days. Turnips and early rose potatoes were large with indications of heavy crops. The whole country around this point is a plain, elevated from fifty to one hundred feet above the river. From frequent enquiries regarding the character of the soil at a distance from the river, it is believed to be exactly like that seen at Vermilion. The country intervening between this and the Caribou Mountains seemed level or to slope gradually up towards the mountains, and as far as the eye could see was covered with aspen forest interspersed with a few groves of spruce. No frosts occurred from early in May to September 8th, 1875. Often whole seasons pass without frost from early in May to October. Peace River at this point is 3,000 feet wide. At Little Red River, farther north, the climate seemed still milder, and if anything the soil richer. Cucumbers sown and ripened in the open air were seen August 15th, and all garden vegetables were ripe. Fort Chipweyan, at the west end of Lake Athabasca has comparatively poor soil in its vicinity, being largely composed of sand ; still here I obtained fine samples of wheat and barley that took the bronze medal at the Centennial Exhibition, held in Phila- delphia in the summer of 1876. The land is very low and swampy, being but little elevated above the Lake. Mr. Hardisty, Chief Factor in charge of Fort Simpson, PEACE RIYEK. 139 informed me that barley always ripened there, and that wheat was sure four times in five. Melons, if started under glass, ripen well. Frost seldom does much damage. Chief Trader McDougall says that Fort Liard, in latitude 61° north, has the warmest summer climate in the whole region. All kinds of grain and garden vegetables always come to maturity. He has been on the Youcan for twelve years, and says that in most seasons barley ripens under the Arctic circle in longitude 143° west. The localities mentioned were not chosen for their good soil, but for their facilities for carrying on the fur trade or for Mission purposes. Five-sixths of the land on Peace River is just as good as the points cited, and will produce as good crops in the future. The reason so little land is culti- vated is owing to the fact that the inhabitants — whites and Indians — dse flesh eaters. For three years the Rev. M. Garrioch has been farming at Vermilion, and has definitely settled the question of fertility and climate at that point. All kinds of grain ripen well and cattle winter as well there as anywhere else. The testimony of residents, and the meteorological obser- vations which have been taken at Fort Simpson for a series of years, show that wheat can be successfully grown as far north as lat. 61°, and barley up to the 66th parallel, or under the Arctic Circle. All the lakes of the north teem with fish of the very best quality, — whitefish and enormous trout are the principal. Geese, and ducks during the migrations are in countless thousands, and supply the whole population with food. At Fort Chipweyan many thousand geese are killed every fall and preserved for winter use. Not less than 25,000 dried white fish are required for the post every winter. Part of these is fed to the train dogs and the others serve as rations for the men when fresh fish are scarce. The seat of the fishery is at the Quatre Fourche River, a point where four 140 MANITOBA AND THE GREAT NORTH-WEST. rivers meet, about eight miles from the Fort. Here fish are caught every day in the year. So little is known of the country between the Athabasca and Peace Rivers that I have not attempted to describe it. Rich soil, however, is known to prevail, but much of the land is reported marshy on account of beaver. CHAPTER IX. Climate of the North-West. Koteg from Blodgett's Climatology — Its Great Value — Lake Superior Compared with North-West — Summer Heat Decisive of Climate — Thermal Lines Curve Northward — Spring opens Simultaneously on a Northwest line Between St. Paul's and Mackenzie Elvers — Deserts not Found North of Lat. 47° — Eain Sufficient on the Northern Plain — Buffalo more Abundant in the North — Peace River Compared with Germany and Russia — Canadian North-West the Better — A Prophecy Thirty Years Ago — Size of our North- West — Lord Selkirk's Opinions Seventy Years Ago — 500,000 Square Miles with a Mild Climate. The region to which the following remarks will mainly apply is bounded on the south by parallel of lat. 49° ; on the north by parallel of lat. 60° ; on the east by meridian 95°; on the west by the line of the Rocky Mountains. An area, in round numbers, of 667,600 square milps. For many years this vast region was almost a blank on our maps — little was known of it, either by Englishmen or Canadians, beyond the fact that furs were obtained there- from. More than twenty years ago, however, Americans recognized its value, and foretold its great future and even described it as the prospective granary of the world. In 1857 Capt. Palliser was commissioned by the British Government to examine the country south of the 54th parallel. Commencing his examination at the interna- tional boundary, in the vicinity of the Red River, he made a few traverses and reached Fort EUice late in the season. Proceeding up the right bank of the Qu'Appelle to its head, he crossed the South Saskatchewan and proceeded northward to Carlton, where he wintered. In June, 1858, he turned southwest and spent the summer on the Great Plains, wintering that year at Edmonton. In the follow- 142 MANITOBA AND THE GREAT NORTH-WEST ing spring he again proceeded south to the boundary, but afterwards passed to the west into British Columbia. He reported in very favorable terms of the northern portion of the country that he had traversed, but of the southern portion he spoke much less favorably — alleging that running water was very scarce ; that no wood was to be seen except in the river valleys ; and that, owing to the enormous herds of buffalo which covered the plains at that time, feed in many places was poor. As far as public opinion was concerned the only imme- diate result of this exploration was that a certain district in the north became known as the " Fertile Belt," and that the southern part, about which so little was said, was set down, or assumed to be, arid and of slight value ; an opinions till generally prevalent and mainly fostered hy writers whose views have been based on a misinterpreta- tion of Capt. Palliser's remarks. The survey of the International Boundary and the es- tablishment of the Mounted Police Force in 1874, tendered in some degree to dispel the cloud which hung over the south. Frequent journeys have done much since in the same direction, yet in the minds of the general public, and even of maiij' others who should be better informed, the old prejudice, in a measure, exists. In this case the past only repeated itself. How many are the instances of wealth unknown having remained for centuries under the eye of the dwellers on the spot, unap- preciated and untouched ? In our day the growth of the Dominion, demanding a through communication from east to west, and the exigen- cies of the over-populated countries of the old world, have been the means of enlightening the world as to the extent of the resources of the " Great North-West," thus fulfilling the beneficent intentions of the all- wise Creator. Explorers have traversed its length, settlers h;ive here CLIHATE OP THE NORTH-WEST. 143 and there dotted the new land, and the reports of one and the other only stimulate us to further research. Amongst those sent out to explore, I was first commis- sioned by Mr. Fleming in 1872, to examine the flora of the prairies between Winnipeg and Edmonton. The same year I was despatched in company with Mr. Charles Horetzki, to explore the Peace River and examine the country on its banks. The journeys resulted in the discovery of the low passes through the Rocky Mountains, and of an exten- sive tract of fertile country, since known as the Peace River District. In 1875, I accompanied Mr. Selwyn, Director of the Geological Survey, in the capacity of botanist, to British Columbia and from thence by the Peace River Pass to the east of the Rocky Mountains. Circumstances compelled me to descend the Peace River from the Rocky Mountains to Lake Athabasca, and 1 was thus enabled to see the country as far north as lat. 59°. Turning eastward at this point a journey of 1200 miles brought me to Winnipeg. The general conclusions which I arrived at from my ex- plorations of 1872 and 1875 were : 1st, That as there was but one flora common to the region extending from eight to twelve degrees of latitude, or as far north as 60°, and as that flora required a high summer temperature for its exist- ence, the thermometer would be found to show a corres- pondingly even distribution of heat throughout the whole district. 2nd, That exceptional or special conditions must exist to produce that high and even distribution of heat discovered as ranging over so great an area. These conclusions have since been established as facts by the recorded observations sent in from the Meteorological stations at Winnipeg, Fort McLeod, and Fort Calgarry in the south, and Fort Rae and Fort Simpson in the north. (See Meteorological Report for 1878.) In 1879 my attention was mainly directed to an investi- 144 MANITOBA AND THE GREAT NORTH-WEST. gatioii of the causes of the supposed aridity of the district lying to the south. I found a parched surface, dried and withered grasses, and in short every appearance of the ex- istence of such aridity ; but closer examination showed that these indications were illusory. At the point " Blackfoot Crossing " lat 50° 43' where the consequences of aridity appeared the strongest, I came upon ground broken up in the spring, bearing excellent crops of all kinds — oats being four feet high, while on the land outside the fence the grass was burnt up and all other vegetation withered. From this I argued that the rain-fall in the district was evidently ample for the requirements of vegetation, but that, until the baked crust was broken, it could not percolate the ground as rapidly as it fell and so a great portion was evaporated by the dry atmosphere and lost. Thus the apparent aridity vanishes before the first efforts of husbandry. Next to the question of aridity was that of the high and even temperature of climate. On this point I simply accumulated data bearing on the observations of former years, all of which tended to prove that the great plain to the northwestward, and north of lat. 49° extend- in 't alona; the Saskatchewan and other rivers between the 100th and 115th Meridians, and the narrow strip of coast north of Montery, California, present decided features of difference from other districts of the American continent. These differences and peculiarities I shall now deal with seriatim. TEMPERATURE, It was long ago asserted as a principle by Geologists that " land in quantity situated to the southward of lat 40° north, very materially raises the temperature of lands lying to the north of such parallel." (Sir C. Lyell). To the ex- pression '■ land in quantity," I would add, wJien its character i'j that of a desert or arid nature. Another maxim is thus laid down by a well known writer on American CLIMATE OF THE NORTH-WEST. 145 Climatology (Blodgett) " that high arid plains are indica- tive of great summer heat, of an arid atmosphere, and of little rain or snowfall." Now the conditions required to test the accuracy of both these propositions are presented in the position occupied by the North-West Territory. South of our boundary, within the United States, lies a vast tract of land, generally arid or desert, of which at least 500,000 square miles are embraced in a plateau which has a general level of COOO feet. At Laramie City in lat. 42° it is about 7000 feet above sea level, thence northward it rapidly falls off so that when it reaches our boundary in lat. 49° at Pembina, it is considerably under 1000 feet. At the base of the Rocky Mountains it is under 4000 feet. From the boundary the plain extends far to the north and only terminates at the Arctic Sea. In such a wide range of latitude it might well be expected that a considerable difference of temperature would be found. The following Table, however shows the temperature as being wonderfully uniform. (See Meteorological Report, 1878) : bTtI! A W OP Placb Lat. Long. W Jdne. Jdiy. Adgdst. „ j, Winnipeg 49. 53 97.07 59.2 65.8 63.3 62. 8 Fort M:cLeod...49.39 113.42 60.6 63.3 57.0 60.3 Norway House.. 54. 00 98.00 54.9 63.5 61 .2 59.9 Fort Simpson... 6 1. 52 121.25 58.8 63.4 63.2 61.8 In the same parallels of latitude in Europe the tempera- ture is recorded as follows. (See Blodgett) : Place. Lat. Jdne. Juli. Adgust. Penzance, S. W. England 50.08 59.5 62.1 61.1 60.9 Cracow, in Poland 50.04 64.0 65.8 64.9 64.9 Koeningsberg, in Prussia 54.42 57.4 62.6 61.7 60.6 St. Petersburg, in Bussia 59.56 58.2 62.7 60.8 60.6 We see that the summer temperature in the North-West Territories is exceptional. Believing, however, that in addition to the quoted causes, there are others which con- tribute to this result of exceptional temperature, I purpose for the present, to reserve the fact for further comment, 10 Mbad or Sum. Mog. 146 MANITOBA AND THE GREAT NORTH- WEST and pass on to the subject of isothermals. The recorded lines of equal temperature show that the various lines of heat, as they make westing from the eastern coast of the continent, tend in summer to curve upwards from the Gulf of Mexico in a northwesterly direction to a point in lat. SO'", long. 110° west. At this point the mean summer tempera- ture is 70° F., while at "Winnipeg, on the same parallel of lat., but 15° further east, the temperature is but 65°. Tra- cing these isothermals still further north, the line of great- est heat passes near Fort Vermilion in lat. 58° 24' and long. 116° 30' west. I may mention that at this point I found barley cut on August 6th, 1875, and wheat almost ripe. Still farther north and west the table shows that Fort Simp- son has a mean summer temperature of 61° 8' F. Turning to the west coast, the isothermal lines commence to turn northward from the Gulf of California, and for a time skirt the westerii side of the Rocky Mountains. On reaching the loAV point of the chain between lat 41° and 45° they turn to the east, cross the mountains, and strike the Dominion boundary on the 115th meridian. These westerly currents, named the " Chinooks " have been known to cause a rise in the temperature of 60° in a few hours. When in that country I enquired from a Half-breed about their effect on the snow. His reply was, " the Chinooks lick up snow, water and all." After crossing the Rocky Mountains the thermometric cur- rent of the west meets that of the east at or about the Hand Hills in lat. 51° 20', long. 112°. There, in 1879, I found that for days together, during August, the thei-mometer in the shade registered from 87° to 92° F. From the Hand Hills the united currents, following their resultant direc- tion, carry the temperature of latitudes extending almost to New Orleans over the North-West, and confer on it the blessings of a climate, not only exceptional as regards character, but productive of results to the agriculturist, CLIMATE OF THE NORTH-WEST. 147 which, I believe, are unsurpassed in any other part of the world. Returning to the course taken by the east and west cur- rents before their union at the Hand Hills, it is a matter for consideration, why that from the east departs from the natural law which would give to it an eastward, in place of a westward bend, while the western current follows the natural law and bends to the eastward. The answer to this question is the hey to almost every clrni- atological peculiarity of the North -West. The data which we have for the investigation of the question : " Why does the eastern current of heat proceed- ing northwestward from the Gulf of Mexico bend to the west ? " are : 1st. Recorded observations, which show that land of a desert character is heated to a greater degree than the land or water adjoining. 2nd. Recorded observations which show that currents of air are constantly on the move to where the land is most heated. 3rd. The fact that to the westward of the tract running northward from the Gulf of Mexico lies the " Great Ameri- can Desert." To my mind no argument is needed to show that the cause of the divergence of the eastern thermometric current to the westward is solely due to the position and effect pro- .duced by the American Desert. A confirmation of this inference is offered in the eastern hemisphere, where the Southeast Trade winds are drawn out of their course by the heated atmosphere of the Western Indies, and result in the Southwest Monsoon, and further by the northeastern trend of the isothermals in Northern Asia. In the transition from summer to winter we find the desert losing its tem- perature (terrestrial and atmospheric) and consequent attrac- tive influence on air currents warmer than its own. The first 148 MANITOBA AND THE GREAT NORTH-WEST. effect of this is that the isothermals pass away from their northern altitude and sink southward ; next, when freed from the desert influences, they no longer trend to the west- ward, but to the eastward. On the withdrawal of the southern warm currents, other currents from the north and from the west follow them up, particularly- on the east side of the Rockies, and establish the prevailing northwest win- ter winds, which being affected by the temperature of the Arctic regions on the one hand, and by the mountains on the other, bring the minimum line of cold far to the south. Were the American Desert an inland sea, the summers of our plains would lose their exceptional character, and our winters would be like those of Eastern Europe. In a book like the present, however, it would be out of place to discuss the climate of the eastern hemisphere ; but it could be shown that precisely similar causes to those which I have specified exist there, and are productive of the same results, HUMIDITV. The rainfall of the North-West offers as favorable a con- trast to that of other districts as the temperature. Rains usually come just when they are wanted and cease when vegetation no longer requires them, and when their con- tinuance would be detrimental to harvesting. Formerly the rainfall of a country was judged by the average for the whole year. Such a comparison, however, is misleading. What we want to know is the quantity that may be expected to fall :— (a) During the period of vegetation, and its distribution month by month. (6) During the harvest months. The period of vegetation in the North-West embraces May, June, July and August. The harvest months are Sep- tember and October. I append the following tabulary ar- ranged statements of rainfall : — CLIMATE OF THE NORTH-WEST. 149 Table I.— For the Four Months of Vegetation. POSITIO.N. Rainfall in Inche.s. Total for 4 Lat. Alt. May. .June. July Aug. Months. Winnipeg, Manitoba Toronto, Ontario Fort Riley, Kansas Rochester, New York 49.53 43.39 39.03 43.07 740 350 1300 506 2.17 2.98 4.14 3.04 3.42 3.04 3.08 2.68 3.72 l.OS 3.01 7.11 2.81 2.99 2.00 15.37 12.55 11.29 11.90 Table II. — For the Two Months of Harvest. PLA(!E Position. Rainfall in Inches. Total Lat Alt. Sept. Oct. 49.53 43 39 39.03 43.07 740 350 1300 506 0.73 4.45 4.18 3.05 0.03 2.96 0.02 3.39 0.76 Toronto. Ontario 7.41 Fort Riley, Kansas Rochester, New York 4.20 6.41 Having stated what the recorded facts as to rainfall are, I will give my reasons for asserting that these facts are the necessary consequences of the physical conditions existing m the west of the North American Continent. In the beginning of this chapter I referred to the posi- tion of the Great American Desert, and pointed out one of its effects on the air-currents rising northward from the Gulf of Mexico — viz., its power to attract and draw them to itself, and to the westward of their natural course. Another effect arises from the heat given off by radiation during the summer months. The Gulf air currents, laden with moisture, when drawn over the desert, are met by the rari- fied and heated air ascending from its surface, and the rain which in the ordinary course they would shower down, being prevented from falling, passes on and is wafted by the prevailing winds m the direction of our North-West. There their long borne and priceless load is given forth m the form of our summer rains. 150 MANITOBA AND THE GREAT NORTH-WEST. Having shown cause for the summer rains, I may now state that the simple " suspension of those desert effects which gave the summer rains," is the cause of the almost total absence of rain in the autumn and winter periods. It was shown when writing on the winter temperature, that as the desert cooled down the main air currents from the Gulf of Mexico no longer pursued a westward course, but passed to the eastward. This change of direction takes them over the region of the Canadian Lakes, where they deposit an abundant rainfall. AGRICULTURAL OPERATIONS. The progress of the seasons and the labors of the hus- bandman may be summarized as follows : — In April the hot and unclouded sun clears from the lands the last of its light snow covering, thaws, and at the same time dries the ground sufficiently to fit it for the plough, and almost simultaneously for seeding. Germination quickly follows and the young roots, moistened by the thawing of the subsoil, follow the pores opened out by the disintegrating power of the winter frosts, and penetrate to a depth inconceivable to those who have not put the matter to the test. By the time that the rains of May and June come, the roots have a firm hold of the ground, and growth is extraordinary. The July and early August rains nourish and swell the ear of the now ripening crops, and complete the promise of the early spring. Towards the end of August the winds change and the almost rainless period sets in and continues all winter. The farmer harvests his crop without loss and m the highest possil3le condition, stacking it in the open air, without even the necessity of thatching it for the winter. TO STOCK BREEDERS The advantages are equally great. Storms of sleet or wet snow are unknown on the western plains. The snow CLIMATE OF THE NORTH-WEST. 151 is always dry and light, hence cattle and horses may be left out the whole winter without suffering from wet. Intense cold they may experience, but stock-raisers know that where the cold is dry, cattle are not hurt. Hence cattle can be raised on the North-West Plains without buildings for win- tering them. Reference was made to Blodgett's Climatology in the foregoing remarks, and I now quote a part of his work bearing on the climate of our North-West, written by him over thirty years ago. A careful study of what he says will be necessary to the reading with profit of the succeeding chapter : " By reference to the illustration of the distribution of heat we see that the cold at the north of the great lakes does not represent the same latitude further west, and that beyond them the thermal lines rise as high in latitude, in most cases, as at the west of Europe. Central Russia, the Baltic districts and the British Islands, are all reproduced in the general structure, though the exceptions here fall against the advantage, while there they favor it through the influence of the Gulf Stream. " Climate is indisputably the decisive condition, and when we find the isothermal of 60° for the summer rising on the interior American plains to the 61st parallel, or fully as high as its average position for Europe, it is impossible to doubt the existence of favorable climates over vast areas now un- occupied. " This favorable comparison may be traced for the winter also, and m the average for the year. The exceptional cold for the mountain plateaux, and of the coast below the 43rd parallel, masks the advantage more or less to those who approach these areas from the western part of the Central States, and from the coast of California ; but though the distant mountain ranges remain high at the north, the width of their base, or of the plateau from which they rise, is much 152 MAN1T(JHA ANIJ THE GRKAT NOKTil-WEST. less than at the 42nd parallel. The elevated tracts are of less extent, and the proportion of cultivable surface is far greater. " It will be seen that the thermal lines for each season are thrown further northward on passing Lake Superior to the westward, in the charts of this work, than in those of the military report prepared by the author. At the time those were drawn the number of the observations beyond the limits of the United States were so small that the full ex- pression was not given to the statistics then used, in the fear that some correction would ultimately be found to apply to them, reducing the extreme northward curvatures they indicated. But a further collection and comparison warrants the position now given to the thermal lines, placing them further northward than before, and extending them in a course due northwest from Lake Superior to the 58th parallel. For the extreme seasons, whiter and summer, this accurate diagonal extension of the thermal lines across the arenas of latitude and longitude is very striking. The Buffalo winter on the upper Athabasca, at least as safely as in the latitude of St. Paul, Minnesota ; and the spring openn at nearly tlie same time along the immense line of -plains from St. Paul to Mackenzie River. '' The quantity of rain is not less important than the measure of heat to all purposes of occupation; and for the plains east of the Rocky Mountains there may reasonably be some doubt as to the sufficiency ; and doubts on this point whether the desert belt of lower latitudes is prolonged to the northern limit of the plains. If the lower deserts are due to the altitude and mass of the mountains simply, it would be natural to infer their existence along the whole line, where the Rocky Mountains run parallel and retain their altitude ; but the dry areas are evidently due to other causes prim- arily, and they are not found above the ilth parallel in fact. It is decivsive of the general question of the sufficiency of CLIMATE or THE NORTH-WEST. 153 rain, to find the entire surface of the upper plains either well grassed or well wooded ; and recent information on these points almost warrants the assertion that there are no barren tracts of consequence after we pass the bad lands, and the Coteau of the Missouri. Many portions of these plains are known to be peculiarly rich in grasses; and probably the finest tracts lie along the eastern base of the mountains, in positions corresponding to the most desert-like of the plains at the south. The higher latitudes certainly differ widely from the plains which stretch from the Platte southward to the Llano Estacado of Texas, and none of the references made to them by residents or travellers indicate desert characteristics. Buffalo are far more abundant on the north- ern plains, and they remain through the winter at their extreme border, taking shelter in the belts of woodland on the upper Athabasca and Peace Rivers. Grassy savannas like these necessarily imply an adequate supply of rain; and there can be no doubt that the correspondence with the European plains in like geographical position — those of East- ern Germany and Russia — is quite complete in this respect. If a difference exists it is in favor of the American plains, which have a greater proportion of surface waters, both as lakes and rivers. ******** " Next the area of the plains east of the Rocky Moun- tains, is not less remarkable than the first for the absence of attention heretofore given to its intrinsic value as a pro- ductive and cultivable region, within easy reach of emigra- tion. This is a wedge-shaped tract, ten degrees of longitude in width at its base along the 47th parallel, inclined north- westward to conform to the trend of the Rocky Mountains, and terminating not far from the 60th parallel in a narrow liae, which still extends along the Mackenzie for three or four degrees of latitude, in a climate barely tolerable. Lord Selkirk began his efforts at colonization in the neigh- 154 MANITOBA AND THE GREAT NORTH-WEST. bourhood of Winnipeg as early as 1815, and from personal knowledge he then claimed for this tract a capacity to sup- port thirty millions inhabitants. All the grains of the cool temperate latitudes are produced abundantly. Indian corn may be grown on both sides of the Saskatchewan, and the grass of the plains is singularly abundant and rich. Not only in the earliest exploration of these plains, but now they are the great resort for buffalo herds, which with the domestic herds, and the horses of the Indians and the colo- nists remain on them and at their woodland borders through- out the year. " The simple fact of the presence of these vast herds of wild cattle on plains at so high a latitude, is ample proof of the climatological and productive capacity of the country. Of these 'plains and their woodland borders the valuable surface measures fully. five hundred thausand square miles." CHAPTER X. Practical Remarks on Climate. Mr. Anderson, of Liatowel, Ireland, on Climate — Great Heat Causes no Inconvenience — Intense Cold Hardly Felt — Manitoba Winter Climate Better than that of Ontario — Snow Seldom over Twenty Inches in Depth — Seasons in Manitoba — Manitoba in the Middle of the Continent — Long Days of Summer — Autumn Weather —Snowfall — Heat and Humidity — Comparison of Summer Temperatures — Warm Summers and Dry Cold Winters — Table of Mean Temperatures— Summer Temperatures Compared — Peace RiTer Climate — Manitoba Climate — Hardness of Wheat —Grains in the Cluster— Min- nesota nowhere — Peace Eiver Wheat — Isothermal Lines — Corn and Wheat Zones — Temperature Necessary for Successful Wheat Culture — The Wheat Zones — Probably Three-fourths of the Wheat Lands of America in the New North- West— 200,000,000 Acres — Extent of the Territory — Lord Selkirk's Opinions Seventy Years Ago — Great American Desert— Its Effect on Climate — Changes Observed Passing North — How the Isothermal Lines Curve — Where the Heated Air comes From — Two Currents passing North— Summer Temperature the same over 300,000 Square Miles — Moisture in Sum- mer, its Absence in Winter — Eainfall of the Year — Progress of the Seasons — Fall Frosts not Injurious, Climate Unsurpassed for Farmers — Its Possibilities Unlimited — Depth of Winter Frost — Its Beneficial Effects on Soil — Table of Kaiufalls for 1879 and 1880 — Eainfall and Cloudlessness — Testimony of Settlers Regarding the Healthiness of the Climate. In the preceding chapter I have given the facts and deductions regarding the temperature and humidity of the atmosphere of the North-West as noticed by myself. I shall now give details of a more practical nature, and adduce other evidence just as conclusive as my own, regarding sum- mer and winter temperature, rainfall, and all other kindred subjects which naturally fall under the term climate. The following extract is from the report of Mr. R. H. B. P. Anderson, of Listowel, Co. Kerry, Ireland. In it he gives his views of the climate and seasons as observed by himself. These are worth more than a passing glance, as he touches with a master hand the most salient points of the subject. " The Climate of Manitoba and the North-West is one of the settler's most serious drawbacks, but we are inclined to look upon it as a much more serious affair than it really is. 156 MANITOBA AND THE GREAT NORTH-WEST. Description will do little to remove these impressions, it must be experienced to be understood. At home, exces- sive heat is generally accompanied by oppressiveness, with its attendant weariness and inertia; and cold, as a rule, with dampness, which makes it raw and piercing. Now this is not the case in Manitoba or the North-West. The lieat at 100° was undoubtedly very intense, but — and I speak from personal experience — without sultriness. I per- spired freely, but otherwise felt no inconvenience, and had energy enough for any amount of work. This was an unusual degree of heat; the summer mean is, I believe, about 70°. Usually during summer there is a pleasant breeze, and the higher the thermometer stands the more likely is there to be a breeze. No matter how hot the day, the night is sure to be cool. In winter the cold is very great, but nothing like what it is at home in proportion to the degrees of frost ; if it were, animal life would cease, for the thermometer sometimes sinks to 40° and 50° below zero — ^just imagine what that would mean in England ! but when it does so it is certain to be accompanied by a bright iind perfectly still atmosphere and a warm sun. However, as a rule, it stands at from 10° to 15°. As I had not an opportunity of experiencing it myself, I was not content with the testimony of the ordinary settler concerning it, but had that of such men as the Bishop of the Saskatche- wan and clergymen of various denominations, as well as bankers and others, on whose opinion I could rely. All agreed in saying that one feels no colder when the thermo- meter stands at 40° than when it is at 10° below zero, and that winter is a delightful part of the year. Numbers of people from Ontario said that the climate of Manitoba com- pared favorably with that of Ontario. There are, however, slight deviations which are intensely disagreeable. In the summer there are sometimes extremely high winds and hail- storms, and in the winter storms of wind and snow — PRACTICAL REMARKS ON CLIMATE. 157" ' blizzards ' as they are called. In spring and early autumn frosts sometimes occur, which do no good to the crops ; but all these things apply to the Western Statesof America just as much as they do to Manitoba. Indians camp out in their wretched canvas-covered tents during the most severe winters, and white men, when hunting, often do the same,. and think nothing of it. A curious fact is that Europeans, for the first two winters, bear the cold better than Cana- dians. Snow does not fall to any extent till the beginning of the year, and seldom exceeds an average of eighteen or twenty inches in depth. When the thaw comes it is unaccompanied by that abominable slushiness we have at home ; the snow evaporates leaving the ground dry. During spring and early summer an immense quantity of rain falls ; drought, which so often ruins the farmer in the United States, never occurs here. The dew is so heavy that one would imagine that there had been a fall of rain in the night. The seasons are as follows : Spring — April and May Summer — June, July, August, and part of September Autumn — ^part of September to the middle of November and then Winter. Of course in so extensive a country as Canada, there are slight differences in climate. In Ontario the harvest is ten days earlier than in Manitoba. All agree that as regards health the climate of the North- West cannot be surpassed." Another observer, Eev. ^Eneas McDonell Dawson, writes as follows : — " Manitoba is situated in the middle of the continent, nearly equally distant between the Pole and the Equator, and the Atlantic and Pacific Oceans. Its climate gives conditions of decided heat in summer, and decided cold in winter. The snow goes away and ploughing begins in April, which is about the same time as in the older Pro- vinces of Canada, the Northern United States on the At- lantic seaboard, and the North-Western States, Minnesota and Wisconsin. The crops are harvested in August and 158 MANITOBA AND THE GREAT NORTH-WEST. September. The long, sunny days of summer bring vegeta- tion of all sorts to rapid maturity. The days are warm and the nights cool. Autumn begins about the 20th September and last still November, when the regular frost sets in. The winter proper comprises the months of December, January, February and March. Spring comes in April. The summer months are part of May, June, July, August, and part of September. In winter the thermometer sinks to thirty and forty degrees below zero , but this degree of cold in the dry atmosphere of the North-West does not produce any un- pleasant sensations. The weather is not felt to be colder than that in the Province of Quebec, nor so cold as milder winters in climates where the frost, or even a less degree of cold than frost, is accompanied with dampness. In times of wind storms, however, the cold is found to be specially searching. The testimony of settlers is universal as to the fact that the winter is on the whole, both pleasant and healthy ; and former residents of both Ontario and Quebec state that they like it quite as well as that of those provinces. " Snow does not fall on the prairies to an average greater depth than eighteen inches, and buffaloes and horses graze out of doors all winter. They scratch the snow off the prairie grass, and grow fat upon it. Horned cattle graze out of doors part of the winter, but in some states of the weather they require to be brought in. Instances are, however, stated in which horned cattle have grazed out all winter. " Heat and humidity are the two chief elements of climate, and these two divisions of the North-west, the prairie and wooded, have high summer temperatures and heavy summer rains. South of the parallel of Manitoba, lie the regions of summer droughts and great heat — producing the immense deserts over the western territories of the United States, The abundance of rain in British America, with summer temperature sufficient to mature all the great staples of the temperate zones, makes it a good agricultural country. The PRACTICAL REMARKS ON CLIMATE. 159 absence of summer rains, with high temperatures, leaves vast areas of the interior of the United States barren wastes, especially those parts of the country westward from the 100th Meridian or west of the Missouri. The following table will serve for comparison between the summer tem- peratures of the Ked River and the countries south : — July. Augdst. Bommer Meam. Bed River 69.10 71.16 68.03 67. T6 Chicago 62.07 70.08 68.05 67.03 Iowa 66.04 70.05 68.09 68.06 Wisconsin 61.07 68.06 65.07 65.03 New York 64.02 68.05 66.07 66.05 Toronto 64.02 67.95 65.00 66.98 It will thus be seen that the summer is warmer than that of Northern Illinois, Western Wisconsin, Northern New York or Toronto. In relation to agriculture the intensity of winter cold is not injurious, but on the contrary it has advantages, and its effect upon physical comfort is mitigated as above stated, by a clear dry winter atmosphere," Mr. J. W. Taylor, the Consul of the United States at Winnipeg, who has a right to be considered an indisputable authority on account of his long residence in Winnipeg, and thorough knowledge of the subject matter in hand, wrote the letter, from which the following extracts are taken, to the Editor of the " Pioneer Press," St. Paul, Minnesota. Mr. J. A. Wheelock, Commissioner of Statistics to whom he alludes is the very man to whom he addresses his letter, as the Editor and Statician are one and the same person, and the present letter quotes the Editor against himself. COMPARATIVE TEMPERATURE. " A comparative statement of temperatures at St. Paul, Winnipeg, and Battleford, for the first months of the current year, including April, having been published by me and noticed in the " Pioneer Press," I assume that your readers will be interested in a similar statement for the year ending 160 MANITOBA AND THE GKEAT NORTH-WEST. July, 1879, to which I have added the monthly observations at Toronto : N. Lat , W. Long. Toronto 43.49 79.23. St. Paul 44.52 93 05. Winnipeg 49.50 96.20. Battleford 52.43 109.00. " It will be convenient to refer to latitudes as Toronto, 44° ; St. Paul, 45° ; Winnipeg, 50° ; Battleford, 53°. The place last named is situated on the Saskatchewan River, and is the capital of the North-West Territory of Canada, as the vast district west, of Manitoba (longitude 99°) to the Rocky Mountains is now known geographically and politically. Table of Mean Temperatures. Toronto. St. Paul. Winnipeg. Battlefokb. August 66.38 . . .... 72.00 .. 67.34 .. .... 67.79. September . . , . 58.18 .., .... 60.06 .. .... 52.18 .. .... 47.10. October 45.84 ... .... 46 03 .. .... 85.84 ,. .... 34.52. November . , . . 36.06 ... ... 38.03 .. .... 30.66 ... ,... 28.66. December 25.78 . . ... 19.03 .. .... 11.97 .. .... 7.43. January 22.80 ... . .. 16.03 .. 6.10 ... 0.45. Febniary 22.74 ... ... 15.02 .. .... 12.32 .., .... 10.25. March 28.93 .. .... 33.01 .. .... 14.14 ... .... 10.84. April 40 72 .. . ... 50.04 .. .... 39-10 .. .... 46.70. May 51.74 .., , ... 58.07 .. .... 53.13 ... .... 53.35. 61.85 ... 67.49 ... .... 67.09 .. ... 73.05 .. .... 63.20 ... .... 68.19 ... ,... 60.35. July ... 63.95. YlSAl'.LY MkANS. 44.04 ... ... 45.61 .. .... 36.67 ... .... 36.46. " A statement of mean temperature during the agricul- tural season, from April to August inclusive, exhibits the following proportions : — Toronto. St. Paui.. Winnipeg. Battleford. 57.65. 65.05. 58.19. 58.53 " Thus it will be seen that the climate, in relation to agri- culture, is warmer in Manitoba and over territory 700 miles to the northwest, than in the most central districts of On- tario, while St. Paul in lat. 45° is 7° 40' warmer than the vicinity of Toronto, in lat. 44°. PRACTICAL REMARKS ON CLIMATE. 161 " I hope soon to be in possession of similar statistics from Fort McMurray on the Athabasca River, and Fort Vermilion on Peace River, respectively 1,000 and 1,200 miles due north- west of "Winnipeg, and I have full confidence that the climate at these points will not be materially different from Battle- ford. The altitude of the Athabasca and Peace River dis- trict is less, and the trend of the Pacific winds through the Rocky Mountains is more marked than at Battleford. It was on the banks of the Peace River, well up in lat. 60°, that Sir Alexander McKenzie records, on the 10th of May, the grass so well grown that buflfalo, attended by their young, were cropping the uplands. " But I find my best illustration that the climate is not materially different west of Lake Athabasca, in lat. 60° from what we experience west of Lake Superior, in lat. 46°, in some personal observation of the northwestern extension of wheat cultivation. In 1871, Mr. Archibald, the well- known proprietor of the Dundas mills in southern Minnesota visited Manitoba. He remarked that the spring wheat in his vicinity was deteriorating^softening, — and he sought a change of seed, to restore its flinty texture. He timed his visit to "Winnipeg with the harvest and found the quality of grain he desired, but the yield astonished him. " Look," said he, with a head of wheat in his hand, " we have had an excellent harvest in Minnesota, but I never saw more than two well-formed grains in each group or cluster, forming a row, but here the rule is three grains in each cluster. That is the difference between twenty and thirty bushels per acre." More recently, Professor Macoun, the botanist of the Canadian Pacific Railway survey, has shown me two heads of wheat, one from Prince Albert, a settlement near the forks of the Saskatchewan, lat. 53°, long. 106° ; and another from Fort Vermilion on Peace River, lat. 59°, long. 116°, and from each cluster of the two I separated five well- formed grains, with a corresponding length of the head. 11 162 MANITOBA AND TIIK GREAT NORTH-WEST. Here was the perfection of the wheat plant, attained accord- ing to the well-known physicial law, near the most northern limit of its successful! growth. ISOTHERMAL LINES. " The line of equal mean temperature, especially for the season of vegetation between March and October, instead of following lines of latitude, bends from the Mississippi Valley far to the north, carrying the zone of wheat from Minnesota away to the 60th parallel in the valley of the Peace River, and reproducing the summer heats of New Jersey and southern Peinisylvania in Minnesota and Dakota, and those of northern Pennsylvania and Ohio in the valley of the Saskatchewan. * * # "Within the isothermal lines that inclose the zone west and northwest of Minnesota, which is being or is soon to be opened to cultivation, lies a vast area of fertile lands from which might easily be cut out a dozen new states of the size of New York. CORN AN-J) WHEAT ZONKS. " I assigned Ohio, Indiana, Illinois, Iowa, and even south- ern Minnesota to the zone specially adapted to corn, as the more southern states constitute a cotton zone ; and observing the imperative natural restrictions in the Mississippi Valley on the successful production of wheat, I hazarded the statement that three-fourths of the wheat producing belt of North America would be found north of the international boundary. This arithmetical division has since been ques- tioned by the " Pioneer Press." " I will venture to illustrate the climatic influences which control the problem under consideration, by some citations from ' Minnesota : Its place among the States ; by J. A. Wheelock, Commissioner of Statistics,' which, though pub- lished in 1860, is all the more an authority because of the confirmation of twenty years. The general law of limitation to the profitable cultivation of wheat is thus luminously PRACTICAL REMARKS ON CLIMATE. 163 stated. ' The wheat producing district of the United States is confined to about ten degrees of latitude and six degrees of longitude, terminating on the west at the 98th meridian. But the zone of its profitable culture occupies a comparatively narrow belt along the cool borders of the district defined for inland positions by the mean temperature of 55° on the north and 71° on the south, for the two months of July and August. This definition excludes all the country lying south of lat. 40", except western Virginia,, and north of that it excludes the southern districts of Pennsylvania, Ohio, Indiana, Illinois and Iowa, while it includes the northern part of these states, Canada, New York, Western Virginia, Michigan, Winconsin, Minnesota, and the Red River and Saskatchewan Valleys. In general terms it may be stated that the belt of maximum wheat production lies immediately north of the districts where the maximum of Indian corn is attained.' *4£j At, ^u* 4X^ 4t 41^ ^ ^ ^ ^ ^ "Tr 'rp TT •TT" "TT " "Will the great interior of the continent contribute to our exportations of wheat and its flour ? I refer to the terri- torial organizations of Montana, Idaho, Wyoming, Colorado, Utah and Nevada. Let us take the most favorable of all — Montana. Grand as are its resources, I am constrained to believe that only one-thirteenth of its surface is within reach of the unavoidable condition of irrigation, and that the mountains, with their mineral wealth, and the uplands as grazing grounds for cattle and sheep, will be the chief thea- tres of industrial activity. After careful inquiry in 1868, as United States Commissioner of mining statistics, I com- mitted myself to the following statement : — ' The area of the territory (Montana) is 146,689 square miles, equal to 93,881,184 acres — nearly the same as California, three times the area of New "York, two and a half that of New England, and yet no greater proportion is claimed by local authorities as susceptible of cultivation than one acre in thirty, or a 164 MANITOBA AND TPIE GREAT NORTH-WEST. total of 3,346,400 acres. Of course a far greater surface will afford sustenance to domestic animals. The limit to agri- culture, as in Colorado and New Mexico, is the possibility of irrigation.' * * * * It is the crowning feature of the ' fertile belt ' which broadens with reduced altitudes and constant air currents from the Pacific Coast, that the im- mense trapezoid, whose apex is bounded on the Mackenzie, has a sufficient quantity of summer rains for all the purposes of agriculture as organized in the Atlantic and Mississippi States. " I have no pride of opinion as to the accuracy of an impromptu estimate of proportions north or south of the boundary. I would cheerfully waive it, confessing to an arithmetical inaccuracy, if assured of a general acceptance of the opinion with which the article of the •' Pioneer Press " concludes, namely, that ' in Hudson's Bay Territory, outside of the old provmces, 200,000,000 acres are adapted to wheat raising.' That admission is more than enough to justify a railroad policy, which will push, within ten years, the loco- motive from Winnipeg fully 1,200 miles beyond its present bourne on Red River." The above extracts speak for themselves, and 1 have no diffidence in placing before the public the following summary of my own, after nine years study of the subject: — The region included in the following observations lies between the boundary (lat. 49°) and lat. 60° north, these parallels forming the southern and northern boundaries of the territory, while it extends from the 95th meridian to the Rocky Mountains, following their northwestern trend to lat. 60° north. For many years this vast extent of territory lay as a blank upon the maps, almost unknown to Englishmen and Canadians, and counted valueless except as a fur bearing country ; yet so long ago as 1812, Lord Selkirk said that the valley of the Red River alone would maintain a population PE ACTIO AL REMARKS ON CLIMATE. 160 of 30,000,000. The Americans were always alive to its true value, but, like true patriots, extolled their own country in preference to the land of the stranger. Over twenty years ago their writers called attention to it, and Wheelock spoke glowingly of it in his work on Minnesota. In 1872, I had the good fortune to spend a number of months in the territory, and travelled over its whole extent from east to west, and, being impressed with its importance as a field for immigration, I have since then taken every oppor- tunity to make myself acquainted with its climate and capa- bilities. In the following pages will be found my conclusions and the facts upon which they are based. Geologists are aware that high arid plains always amelio- rate the climate of countries north of them ; and Blodgett in his work on the Climatology of the United States, says that such plains are decisive of a high degree of summer heat with an arid atmosphere and little rain or snow. Within the United States there are at least 500,000 square miles of arid country, almost constantly receiving enormous ■ quantities of heat by day and giving it off at night by radia- tion. The general level of this plateau is fully 6,000 feet. At Laramie City it is about 7,000 feet above the sea, but from this point it rapidly falls off to the north, so that when it reaches the boundary at Pembina it is considerably less than 1,000 feet in altitude, and at the base of the Rocky Moun- tains under 4,000 feet. As the plain descends to the north the rainfall increases, the " cactus " and the " sage-brush " give place to bunch grass, and this, north of the line, soon passes into sward, quickly followed, as we proceed north- ward, by copsewood, which, north of the Saskatchewan, is re- placed by an aspen forest, or, on the watershed, by spruce. No appreciable alteration in temperature takes place, but only an increase of moisture as we pass to the north, and with this increase of humidity a more equable temperature is noticed. Less radiation takes place as we leave the high 166 MANITOBA AND THE GREAT NORTH-WEST. treeless plains, and, consequently, the variation of tempera- ture is less strongly marked between day and night. A careful examination of Blodgett's and Dove's charts shows that the isothermals curve upward from the Gulf of Mexico, and reach their northern bend in the United States, on the 110th meridian. Here in lat. 50° the mean summer temperature is placed at 70°, while at Winnipeg, 600 miles to the east, it is 65°. Following these lines 9° further north, we find that the isothermal of greatest heat passes Fort Ver- million, lat. 58° 24', on the Peace River, and Edmonton on the Saskatchewan, both points being noted for their pro- ductions. On the Pacific side the isothermals commence to curve north from the head of the Gulf of California, reaching our boundary at the 115th meridian, havmg actually crossed the Rocky Mountains before reaching this point, thus producing those warm dry winds of the southwest which are known in Montana and north of the boundary as " Chinook Winds." These winds are noticed more particularly in winter, and often raise the temperature over 60° in the course of an hour or two. They are noted for being both warm and dry, as they evaporate the snow as fast as they melt it. Their effects are not much felt north of lat. 52", and how lar east they extend is not known. Here, then, we have two currents of warm air flowing constantly into our territory, the one from the Gulf of Mexico, the other from the Gulf of California, and unitedly giving us heat and moisture which they have carried over the " Great American Desert " to leave on the lower plain to the north. Owing to the height and aridity of the " Desert," much heat is absorbed during the day, but it is constantly sent into the atmosphere at night, causing the air above the plain to be just as warm at night as during the day. Fort Laramie, in Wyoming Territory, is in the same latitude as Boston, and although 7,000 feet above the sea, has a summer temperature as high as Boston. A very little reflection will PRACTICAL REMAKKS ON CLIMATE. 167 show that, were the " Desert " an inland sea, the winters of our interior would be like those of Eastern Europe. "We would have a cooler summer and warmer winter. In an article like the present it would be out of place to discuss the climate of Eastern Europe, but the forces which enable the Russian to build his capital almost on the 60th parallel are precisely the same as those which send the warm air of the Gulfs to ameliorate the climate of our own North-West, and cause wheat and other cereals to be produced in the highest perfection. The following table of temperature is extracted from the Meteorological Report for i876 : — '^1 St •-3 i 3 < 1- IJ CD m CO Fort Calgarry, Lat. 51° Long. 114- Fort Simpson, Lat. 61= Long. 113° Toronto, Lat 44° Long. 79° Winnipeg, Lat. 50° Long. 97° Fort McLeod, Lat. 50° Long. US" 36.7 i's'.k 35.4 39.8 51.8 44.6 51.5 52.1 63.3 61.0 58.8 65.5 69.2 60.6 69.0 63.4 6J.ii 6.-;. 8 63.3 53.5 63.2 70.2 63.3 67.0 47.2 46.9 67.5 51.8 60.3 51.5 68.' 6 64.6 64.0 67.8 61.8 68.2 62.8 60.2 It will be seen by the above data that Fort McLeod and "Winnipeg, although 600 miles apart, have almost the same temperature, and, more surprising still, that Port Simpson, although 770 miles due north of Port McLeod, is warmer. Here we have a triangle with its three angles having almost the same summer temperature — its base being 600 miles in length, its perpendicular 770, and its hypothen- use 900. Purther records will probably increase this area but no continuous observations having been taken, we do not hazard an opinion. Captain Palliser, when in the Saskatchewan country in 1858-59, had pits sunk in the soil to see to what depth the frost penetrated, and at what time in the spring; the soil was free from it. On the level prairie in the vicinity of Edmon- ton, the frost penetrated to a depth of seven feet during the winter of 1858, while the next wmter it penetrated to a depth of six feet. The former year there was scarcely 168 MANITOBA AND THE GREAT NORTH-WEST. any snow, which accounts for the greater depth of frost. It may possibly remain in the ground all summer in a swamp but cannot remain m a fairly dry soil all the year round, except the mean annual temperature fall below freezing point. It is well known that a coating of moss or straw will keep the frost in the ground till June in Ontario, and I should not be surprised to hear of frozen soil in Mani- toba in July. Captain Palliser found that the ground, three feet below the surface, grew colder until about the 25th February, when the temperature began gradually to increase, but it was not until the 23rd of May that it had risen to .32°. I infer that the great depth to which the soil is frozen in winter is beneficial to the growing crops both as a fertilizer and as a retainer of moisture. After temperature the most important factor is humidity, and here, again, we have a remarkable example of a well known natural law As above stated, the winds are con- stantly drifting northward, and in winter, owing to their passage across the " American Desert," which is now very cold, they lose most of their moisture, and pass over our prairie as dry winds. In summer the very reverse of this takes place ; the dry, hot plains prevent deposition, and hence the winds come loaded with moisture, and give the summer rains which cause such astonishing growth in June and July. In most cases this dryness of the atmosphere is injurious to growing crops, but, owing to the situation of the ]3lains, in our case it is a positive good, the rains coming just when wanted, and ceasing when of no further use to the growing crop. The following data, taken from the Meteor- ological Report of 1876, illustrate this : — Winter. Spring. Summer. Autumn. Quarterly rainfall at Winnipeg 0.00 5.69 10.52 0.04 "Toronto 5.61 6.63 5.74 3.18 First Half Si;cond Half OF Year. of Year. Snowfall, in iucli' s, at Winuipig 28. 29.7 " " Toronto i7.7 45.7 PRACTICAL REMARKS ON CLIMATE. 169 It will be seen by the foregoing table that the rainfall at Winnipeg in sutnmer and spring is nearly equal to that of Toronto for winter, spring, and summer, and where Toronto has over three inches in autumn, Winnipeg has scarcely any. The absence of autumn rains in the west is a priceless boon, as it enables the farmer to thresh and harvest his grain without injury, and besides, gives him excellent roads when he needs them most. The progress of the seasons and the labors of the husband- man, throughout the North-West, may be summed up as follows : Early in April, the hot sun dissipates the slight covering of snow, and almost immediately, ploughing com- mences, as after the frost is out six inches, spring work may begin. Seeding and ploughing go on together, as the ground is quite dry, and in a few days the seed germinates, owing to the hot sunshine ; the roots receive an abundance of moist- ure from the thawing soil, and following the retreating frost through the minute pores opened in it, by its agency pene- trate to an astonishing depth (often two feet), all the time throwing out innumerable fibres. By the time the rains and heat of June have come, abundance of roots have formed, and the crop rushes to quick maturity. It is just as much owing to the opening power of the frost as to the fertility of the soil that the enormous crops of the North-West are due, and, as long as the present seasons continue, so long will the roots penetrate into the subsoil, and draw rich food from the inexhaustible reservoirs which I know are there. After the middle of August the rains almost cease, and for ten weeks scarcely a shower of rain falls, giving the far- mer time to do all necessary work before the long winter sets in. These general characteristics apply to the cli- mate of the whole North-West, and the same results are everywhere observed over tracts embracing 300,000 square miles of territory. One important result of this peculiar climate is the hardness and increased weight of the grain 170 MANITOBA AND THE GREAT NORTH-WEST. caused by it. Another, equally important, is the curing of the natural hay. Our experience of October and November has been that the horses and cattle do better to collect their own food on the prairie than to be fed with hay. All stock raisers know that it is not cold that injures horses or cattle, but those storms of sleet or soft snow which are so common in Ontario and the Eastern Provinces. Such storms are not seen in the North-West, and the cattle are never wet from November to April. Many intelligent persons are afraid of the winters of the North-West, as they measure the cold by the thermometer rather than by their own sensibilities. It is not by the thermometer that the cold should be measured, but by the humidity of the atmosphere. All through the fall my men never noticed a few degrees of frost, and it was no uncom- mon thing to see a man riding in a cart without his coat, when the thermometer was below freezing point. J. A. Wheelock, Commissioner of Statistics for Minnesota, wrote as follows concerning the atmosphere of that State, over twenty years ago : " The dryness of the air in Minnesota permits a lower range of temperature without frosts than in moist climates. The thermometer htus frequently been no- noticed at 20 degrees without material injury to vegetation. In the damp summer evenings of Illinois and Ohio, for example, the heat passes off rajsidly from the surface of the earth and from plants. Frosts develop under such circum- stances at a comparatively high temperature. The constant bath of moisture has softened the delicate coverins; and enfeebled the vitality of plants ; and thus a fall of the ther- mometer wbich in Minnesota would be as harmless as a summer dew, in Ohio would sweep the fields like a fire." What Wheelock says of Minnesota is equally true of the North-West Territories, and more so, as they are certainly drier. Dry air is a non-conductor of heat, and as the dryness increases with the lowering temperature, the in- PRACTICAL REMARKS ON CLIMATE. 171 creasing cold is not felt by either animals or plants, and we find a solution to the paradox, that although water may freeze, vegetation is not injured except when a humid atmosphere is in immediate contact with it. The increase of dryness in the air has the same effect as an increase of warm clothing for man and beast. "We suffered less from a temperature of 10° below zero, this winter, though lying in tents, without fire, than we would have done in Ontario with 10° degrees of frost. In conclusion, after nine years' study of all available ma- terial and constant observation, I can state that our peculiar climate is caused by the " Great American Desert," which commences at the 100th meridian, exactly south of our prairies, and extends with little interruption to the bound- ary of California. The winds passing over it descend on our interior plain, giving out heat and moisture in the summer, and in the winter wrapping the whole country in a mantle of dry air, which moderates the climate so much that without the aid of a thermometer no one would believe the cold was so intense. "We, have then, a dry, clear, cold winter ; a dry spring with bright sunshine ; a warm summer with an abundance of rain, but not necessarily a cloudy atmosphere, and a dry serene autumn, with possibly a snow storm about the equinox. An atmosphere like this, with a soil of abounding fertility extending over a region of almost boundless extent, causes me to feel that the words of Lord Beaconsfield were those of a far seeing statesman, and that our great North-"West is truly a land of " illimitable possibilities." During the summers of 1879 and 1880 I was on the plains the greater part of the season, and kept a record all the time, from which I make the following extracts : — 1879. June 19. Very heavy rain with severe thunderstonn. „ 20. Beautiful day. Cloudy in the morning. „ 21. Light showers in the forenoon. Thunder at night. 172 MANITOBA AND THE GREAT NOKTH-WEST. Ju July le 22. , 23. , 24. , 25. , 26. , 27. 28. 29. 30. 1. 2. 3. 4. 5. 6. 7-£ 10. 11. 12. 13. 14. 15. 16. IT. 18- 23. 24. 25- 31. Aug. 1, 4. 5. 6- 12. 13. 14. 15. 16. 17. 18- 20. 21- 23. 24. 25. 26. 27. Warm, pleasiint day. Terrible thunder storm this morning. Heavy rain all day. Showers in the afternoon. Rain as usual this morning. Lovely day. Dew heavy. Very beautiful day. Thunder storms passing to the south all day. Showers both north and south. No rain near ub. Slight showers after noon. Thunder storm with heavy rain in the evening. Very lovely day. Day very fine. Severe thunder storm with heavy rain. Slight showers in the afternoon. Tery fine days. Thunder storm with rain to the south. Very hot day. Thunder storm to the south. Gale from the west. Gale continued all day. Wind still strong. Light shower. Gentle wind. Lovely day. Thimder storm in the northwest. Lovelj' day. Very fine day. Thunder storm in the night. -2 2. Very beautiful days. Heavy rain this morning and nearly all day. Heavy showers in the afternoon. -30. Lovely days. Eain fell all the forenoon. Rain all night. Wet forenoon. Almost a frost this morning. Day very hot. Thunder storm to the southeast. Day very hot. Heavy rain in the night. Cool morning. •11. Weather intensely hot. Thunder in the distance. Slight shower. Very lovely day. Severe thunder storm at night. Very lovely day. Very hot day. 92° in shade. Very hot day. Strong gale without a cloud. Great change in the weather. Air qiiile cnnl. 19. Changes still continue. Clouds look veiy rough. 22. Weather very pleasant. Thunder after dark. Weather very jileasant. Terrific thunder storm in the night. Bain and a strong gale. Our tents blown away. Cool vrindy day. Pleasant day. Ruin threatening. PRACTICAL REMARKS ON CLIMATE. 173 Aug. 28. Rain threatening. Came at 6.00 p.m. Rained all night. „ 29. Rain this morning. „ 30 Lovely day. „ 31. Cold showers. During the month of September scarcely any rain fell, but there were a number of cloudy days and white frosts at night. The month closed with a thunder storm succeeded by a number of hot days. These were followed by strong winds which lowered the temperature, and on the 9th October a heavy snow storm was experienced over the whole country west of the Touchwood Hills. This snow soon dis- appeared and lovely weather with occasional low temper- atures continued till late in the season. Thunder storm with rain. Rain threatening all the morning. Heavy rain with thunder. !3. Very fine days. Slight showers in the north in the evening. Light local showers at noon. Terrific thunder at night. Evening cool. Slight rain after dinner. Thunder storm with heavy rain. Thunder storm with heavy rain in the afternoon. Lovely day. Thunder in the distance. Heavy rain in the night. Heavy rain at noon. Showers ahout noon, accompanied hy thunder. Lovely day. Light rain at night. Thunder storm in the afternoon. Thvmder storm at night Pleasant day. Showery in the aftemooiL Thunder storm in the night with heavy rain. Showers all around in the afternoon. Very fine day. High wind and heavy showers. Showers in the distance. Day very hot. Usual thunder and rain storm. Very hot day. Thermometer 87° in the shade. Lovely day. Lovely day. Strong wind all day. Thunder and rain in the afternoon. 1880. June 1 19. jj 20. » 21. )7 22- » 24. j; 25. » 26. » 27. J} 28. n 29. J) 30. July 1. )i 2. » 3. » 4. ji 5. » 6. n 7. » 8. » 9. » 10. » 11. » 12. » 13. J) 14. » 15. n 16. ji 17 n 18. » 19. » 20. 174 MANITOBA AND THE GREAT NORTH-WEST. Jiily 21. J? 22. ;j 23. » 24. V 25. n 26. 11 27. :? 28. 29. 30. If 31. Aug 1. ■) 2. )' 3. 11 4. V 5. 11 6. Jl 7. JJ 8. 1) 9. H 10. 11 11. Jl 12. 5? 13. 1? 14. 11 15. Day extremely hot. 89° in the shade. 95° in the shade. Thunder storms in the distance. Very -warm. 90° in the shade. Terrible thunder storm in the afternoon. Max. 92°. Usual thunder storm. Max. 93°. Pleasant day. Cloudy at night. Tory fine day. Light rain in the morning. Tliunder storm at noon. Pleasant day. Pleasant day. Wind strong from the south. Day warm. Tliunder storm with heavy rain. Thunder and rain all night. Very pleasant day. Ver3' warm all day. Sun's rays extremely hot. Max. 92°. Severe thunder storm in the afternoon. Cool day. Heavy rain in the afternoon. Very heavy rain with thunder all the forenoon. Pleasant day. Day very pleasant. Stormy day -vrith heavy rain. Cold rain, which continued all day. 16-17. Fine pleasant days. IS. Light showers, 19. Cool and pleasant. 20. Day very hot. 21-22. Thunder storm all niglit with torrents of rain. 23. Heavy rain all day. 24. Cold rain all day. 25. Temperature low. Clearing up. 20-27. Very pleasant days. 28. Cloudy with light showers. 29. Pleasant day. Wind strong from the west. 30. Fine, pleasant day. 31. Heavy rain storm all day with a fierce gale. September was much wetter than usual, with three very cold rain storms and low temperature accompanied with heavy gales. The early part of October was delightful with warm pleasant weather. About the 15th this changed to cold, and after this time the nights were more or less frosty. Although rain is frequent in summer, cloudy Aveather is uncommon, and many of the days on which rain is recorded PRACTICAL REMARKS ON CLIMATE. 175 were more than three-fourths cloudless. Heavy dew occur- red every night that the minimum thermometer fell to 50°. As the nights were nearly all cloudless the temperature during the summer had a great range, being often 92° at noon, and sinking to 55° in the night. A fall of temper- ature was always followed by rain without thunder. All severe thunder storms took place when the barometer was very low, but a light one might take place at any time. A rising barometer nearly always gave cloud, and very often rain, in summer ; in the autumn this was always so. The following notes on the healthiness of the climate are taken from the evidence of a great number, and are append- ed to show what settlers think of the country : — Testimony respecting Climate. Name. Post Office. Reuases. Hawaxdand Swain Moms We have never had any sickness. John Kelly „ The climate is very healthy. George Cadman High Bluff We have had very little sickness. William Jackson „ We have found the climate very healthy. A. J. Moore Nelsonville The climate is very healthy. Benj. J. Chubh „ Have had no sickness. Allan Bell Portage la Prairie . We have enjoyed excellent health. Jno. Brydon „ The climate is very healthy. James Airth Stonewall The climate is healthy. William Eagles „ The climate is healthy. Isaac Casson Emerson Have found the climate very healthy. F. T. Bradley ,, None of family suffered through climate. A. Macdonald Gladstone The climate is very healthy. Robert Fisher Cook's Creek Have had no sickness. J. G. Buit ,, I find the climate very healthy. George Taylor Poplar District This is a healthy climate. P. H. Brown „ Healthy. Proper clothing is necessary. J. S. Higginson Oakland No sickness in six years. W. Gresson Meadow Lea The climate is very healthy. James Stewart „ No case of sickness. E. "W. Johnston Springfield The climate is fairly healthy. William Corbitt „ My family have excellent health. J. W. Adshead St. Charles The climate is very healthy. Ben. Haitley « The climate is very healthy. Robert Black Bird's HiU The climate is very healthy. W. A. Mann » The climate is quite healthy. G. V. Fitzgerald Ridareville The climate is very healthy. D. F. Knight ^^ have had no sickness. 176 MANITOBA AND THE GREAT NORTH-WEST. Name. Post Office. Rf,makks. James Fleming West Lymie Have had no sickness. S. Ballantyne „ We have had perfect health here. J. Sutherland Kildonan The climate is exceedingly healthy. J. Geddis „ The climate is very healthy. William Green St. Agathe The climate is very healthy D. G. Low „ The climate is exceedingly healthy. John Smith Westhoume The climate is healthy. Rev. T. Scott „ The country is decidedly good for health. Andrew Dawson Headingly There is no sickness at all. W. B. Hall „ The climate is healthy. C. Begg Stone Fort Had forty-seven years of good health. T. B. Robinson Rockwood i cannot complain of the climate at all. Robert Bell „ rpi,g climate is very healthy. William Hill Woodlands There is no sickness. Neal McLeod Victoria The climate is quite healthy. John Currie „ The climate is quite healthy. Joseph Dobbs Sunnyside My family has never been sick. John Hourie St. Anne The climate is extremely healthy. CHAPTER XI. Natural Products of the Soil. Comparison of Floras— Peace Eiver Flora Compared with that of Ontario— Forest Flora —Flora of the Prairies— List of Species—" Sugar Maple"— Syrup from the Birch — Wild Plums — Cherries — Service Berries — Their Value — Berries in Pemmican — How Pemmican is Made — Berries for Breakfast — Strawberries — Currants and Gooseberries — Black Currants very "Valuable — High Bush Cranberries — Baspberries of Many Species — Jam from the Cloud Berry — Common Cranberries — Blueberries — Wild Sarsaparilla— Silver Berry- Buffalo Berry— Beautiful and Valuable Shrubs— Wild Hops — Hazel Nuts — Flowers and Shrubs at Brandon— Their Beauty and Utility — Strawberries at Brandon — Shnibs of the Prairie — Moose Mountain Flowers— Flowers at the Sand Hills and Flat Creek — Line of C. P. R.— Pipestone Creek — Flowers of the Plain — Great Souris Plain — Acres of Lilies — Gardens of the Prairie — Eoses Fill the Air with Perfume — Flowers at Moose Jaw Creek — Flowers of the Cypress Hills — Wild Lupines Covering Square Miles — Mushrooms, their Great Value and Enormous Size and Numbers — Mushrooms over 200 Miles of Country — Lyeoperdons (Puff- balls) not Poisonous — Flora at Long Lake, Lilies, Anemones, Pentstemons, Poten- tiUas and many Others — Common Poplar & Remedy for Intermittent Fever. Having spent a number of years in exploring the interior plains, and every season having made large collections of the flora, I am able to state what the actual products of the soil are. As every variety of soil and situation changes the flora, an enumeration of the species of each particular dis- trict would be necessary to enable a person capable of judging to form a proper estimate of the relation of that particular district, to another well-known one. In writing of the Peace River Flora in 1877, and calling the atten- tion to the climate of that district, I gave lists of the plants collected at certain points on that river, and compared them with those of Belleville, Ontario. The latter city being in Lat. 44°, while the most southern part of the Peace River country was north of Lat. 56°, or 840 miles north of Belleville. As the difference in Longitude is about 43°, the direct distance in a northwest line is close upon 2,250 miles. 12 178 MANITOBA AND THE GREAT NOETII-WEST. The collections referred to were made by myself in 1875, and were as exhaustive as time would permit. It is well- known, however, that the commoner plants are the typical ones of a district, and these were the species observed by me. The localities mentioned are Hudson's Hope, in Lat. 5G° 12' whence Peace River issues from the Rocky Mountains ; St. John's, 60 miles to the east ; Dunvegan, 120 miles lower down ; Fort Vermilion, 300 miles further down and in Lat. 58° 24'. The others were made at Little Red River, 100 miles to the east, and the last at the western end of Lake Athabasca, in Lat. 58° 42'. COMPARISON OF FLORAS. HudBon's Hope . . St. John's Dunvegan Vermilion Little Red River. Lake Athabasca Total. BULLEVILI.K. QljEBEC. West of Roc. MOHN. 211 130 7 17 248 161 3 6 246 IGO 2 5 159 112 2 1 128 S8 1 24:- 180 7 2 Great Plains'. 79 44 39 50 In the column under Quebec I place species not found at Belleville, but that belong to a cooler and possibly a moister region. The only species that show any .signs of a boreal tendency are those in this coluiim. Of all those obtained at Vermilion only two fell into this column namely, Yellow Rattle {lihinanthus Crl.Hta-yaUi), and the Northern High Bush CYsa\\>Qrxy {Yihurniun. ijauciflorum) . The features prominent in the whole region were a rich- ness in the soil, and a rankness in the vegetation, never seen in Ontario. Last summer I spent in the forest country west of Lake Winnipegoosis, and found about the same proportion of species which indicated coolness and moisture, and a larger percentage of eastern forms. NATURAL PRODUCTS OF THE SOIL. 179 The true prairie llora is altogether distinct from that of the forest, but along every stream, in the prairie, forest species are still numerous, so that an indiscriminate collec- tion from any part of the plains is no indication of its true character. A better knowledge of the southwest will show that large areas must remain permanent pasture, as there are tracts where the plants indicate not an arctic but a mountain flora, hence being too elevated for agriculture. The more prominent of these areas are the Cypress Hills, and the elevated coun- try that constitutes the foot hills of the Rocky Mountains, lying between Forts McLeod and Calgarry. As I purpose treating of the grasses when speaking of the great pastures, I shall now give a list of all other species of plants which have an economic value. Lint of Species. Vitis riparia, Mx. (Wild Grape) Negundo aceroides, Moench. (Ash-leaved Maple.) Prunus Virginiana, L. (Choke Cherry) " Americana, Marsh. (Wild Plum.) " Pennsylvanica, L. (Bird Cherry.) Fragaria Virginiana, Ehrh. (Wild Ijtrawberry.) " vesca, L. (Wood Strawberry.) Eubus Chamoemorus, L. (Cloud Berry.) " triflorus, Rich. (Dew Berry.) " arcticuB, L. (Arctic Raspberry.) " strigoBUS, Mx. (Raspberry) Amelanchier Canadensis var. Sascatoom of the Indian, La Poire of the French Half-breed, and the June BeiTy of the Canadian. Ribes hirtellum, Mx, 1 ^^^^-^ Gooseberries) " oxycanthoides. L. J " floridmn,L. I (Black Currants) " Hudsonianum, Rich. i " rubrum, L. (Red Currants) Heracleum lanatum, Mx. (Cow Parsnip) Aralia nudioaulis, L. (Wild Sarsaparilla) Viburnum pauciflorum, Pylaie. 1 ^.jjj^j^ ^^^^ Cranberry.) « OpuluB, L. ) " Lentago, L. (Pembina Berries) Vaccinium oxycoocus, L. 1 ^^ow Bush Cranberries) « macrocarpon, Ait. J J82 MANITOBA AND THE GREAT NORTH-WEST. Vaccinium Vitis Idoea. (Cow Berry) " Canadeuse, Kalru. \ " coespitosum, Mx. [-(Blue Berries) " myrtilloides, Hook. J Arctostaphylos XTva^ursi, Spreng. (Bear Berry) Ledum latifolium, Ait. Eloegnus argentea, Pursh. (Silver Beny) Shepherdia argentea, Nutt.. (Buffalo Berry) Corylus Americana, Walt, "t ^^^^^j ^^^^^^ " rostrata, Ait. J Betula papyracea. Ait. (Canoe Birch) Pinus contorta, Dougl. (Black or Sugar Pine) The Ash-leaved Maple or Box Elder has been referred to when speaking of the timber, and I will only further remark that wherever a grove of these trees is to be found there Indians have made sugar, and the bark pans in which they caught the sap are still lying around. Never having seen the sugar, nor heard of their mode of manufacturing it, I can give no information regarding it. Throughout the whole north a syrup is obtained from the sap of the Canoe Birch (Betula papyracea) which is very useful. Being a product of the northern forest it is a val- uable contribution to the culinary department of a Chip- weyan's household. Wild Plums are Yery common in many parts of Manitoba, and are simply delicious. In many localities this fruit can be gathered by the bushel, but like the Wild Grape it is local in its distribution, and does not extend beyond the boundaries of Manitoba. Choke Cherries, which in Ontario are extremely astringent, are in the North-West remarkably sweet, and pleasant to the taste. This species is very common on sand hills, and in thickets along the ravines or coulees entering the western rivers, and extends far to the north bearing as good fruit in the Peace Iliver Valley as it does further south. His Excellency the Governor-General spoke in very high terms of this berry when in conversation with the writer some time since in AVinnipeg. Other gentle- men have made the same remark, and all were surprised at NATURAL PRODUCTS OF THE SOIL. 183 its sweetness. It is a fact however that all fruits are sweeter on the great plains than eastward. This is doubtless caused by the cloudless skies and general dryness of the atmos- phere. La Poire, June, or Service Berry is the chief berry of the west. Though common throughout the great plain, forming thickets along the margin of all coulees where wood grows, it attains its highest perfection along Peace River. Below Dunvegan on the north side of the river the bank rises in a succession of terraces. These terraces and the slopes are covered with the Service Berry, and for many miles along the river the bushes are purple with ripe berries about the beginning of August. At this time, bears, Indians, and Half-breeds, live almost entirely upon them. It is no uncommon thing to see five or six bears in a morning breakfasting on the berries and eating them with the great- est relish. As bears are plentiful at this*time, their flesh and these berries are the general food of the camp. While visiting a berrying camp in 1875, on Peace River I was in- vited to breakfast. Our bill of fare consisted of boiled bear's flesh and Service Berries stewed in their fat. I need scarce- ly say that I ate a light breakfast. When on the Peace River Expedition in 1872, we had a quantity of pemmican made at St. John to enable us to cross the mountains. This pemmican consisted of one-third pounded meat (dried muscle) pounded to dust or shreds one-third grease (fine render- ed fat) and one-third Service Berries. Its manufacture was very simple. The dried meat was put in a large trough and the berries added, after which the grease melted, was poured over the meat and berries. All was now thorough- ly mixed with a wooden shovel, and put into skin bags made out of raw hide, with the hair side out. As it was shovelled into the bags a man pounded it solid. After these were filled they were sewed up and our food was ready. Strawberries are a very valuable crop, but more so in the 184 MANITOBA AND THE GREAT NORTH-WEST. middle regions, or northward than on the southern prairie. The true home of the strawberry is on the mixed prairie and forest lands, and here it bears heavy crops of fine delicious fruit that are highly prized by all residents in the country. While ascending the Assiniboine in June, 1879, a number of us left the steamer while she was " wooding up " a few miles above Brandon, and climbed the steep slope of the right bank (the coldest one) to the summit and there we obtained abundance of ripe strawberries on the 16th of June. At this date many are still planting their potatoes. Black Currants, Red Currants, and Gooseberries, are abun- dant in many localities. The Gooseberries are represented on the plains by Rihes oxycanthoides and in woods by Rihes hirtellum. Only occasionally will the bushes be found load- ed with ripe fruit, as some animal seems to live on the fruit in its semi-ripe state. Last season during August and a part of July we were in the alluvial valley of Red Deer River and its tributaries. On all the alluvial flats fine red and black currants were in the greatest profusion, and the men at meal-time gathered a dessert from the bushes close to them. Another Black Currant {Rihes Hudsonianum) ripened later, and like the Missouri Currant [Ribes aureum) instead of maturing altogether, as the common currant does, continued for a long time ; the lower berries on the raceme always ripening first. In many cases the crop of black currants, were settlers there to gather them, would be of great value. High Bush Cranberries are very abundant in the north- ern forest particularly Viburnum pauciflorum, which is the most northern form and which ripens before the first frosts. Viburnum Opulus is found principally in large clumps in river valleys, or on the borders of little ponds within the woods. Its fruit is not so acid as the other species, and is more abundant. The three species of dwarf Raspberry are valuable, espec- NATURAL PRODUCTS OF THE SOIL. 185 ially in the north where their fruit is in the greatest perfec- ■;ion. Ruhus triflorus is common in Ontario, but it is only in the cool damp forests north of Lat. 52" that it attains that juiciness and size which gives it value. Ruhus arcticus is first seen in the swampy district, west of the Lake of the Woods, but here its fruit is of little worth. Westward on the watershed of the Churchill about Isle La Crosse, and north- ward towards Portage la Loche, it is a fine and very pro- lific berry. Ruhus Cliamoemorus grows still farther north, and this and the preceeding are often found together in the muskegs. This species has a fine yellow fruit, and the pre- ceeding a bright red one. Both grow together in the same bog and often cover the surface with beautiful fruit. At Isle la Crosse and Lake Athabasca large quantities of these are collected by the Indian women, and made into jelly at the Hudson's Bay Company's posts. Red Raspberries are found everywhere in lately burnt forest, and seem to be larger and better fruit than we have in the east. Many writers speak as if this fruit wa,s every- where, but being a close attendant on burnt forest, it dies out when grass usurps its place. Low Bush Cranberries are common in all peat bogs, and tamarac swamps, but the fruit is not often gathered, as there is no demand for it. Vaccinium Vitis-Idcea grows in great profusion m all sandy or spruce woods, after the forest is reached. It is one of the most abundant fruits, and is easily .known by its bunches of bright scarlet fruit pendant on the ends of small stems covered with evergreen leaves. This fruit is common near Prince Albert. Although very acid it makes a fine jelly and is a first-class addition to an explorer's dessert. Blueberries are not common except in certain localities, and these are so far removed from where permanent settle- ment will be made, that it is only necessary to mention the sandy tracts where Banksian Pine flourishes to indicate 186 MANITOBA AND THE GREAT NOETH-WEST. where they may be obtained. The Dwarf Blueberry grows abundantly on the elevated country west of Edmonton, and here, as everywhere else, indicates a clima.te too cold for successful wheat culture. Wild Sarsaparilla forms the greater part of the vegetation under the tall aspens in many sections, and wherever dry forest is, or thick brush on the plains, there it is also. Labrador Tea grows in all muskegs and marshes, and, if half that is said of its virtues be true, it will yet be much sought after by speculators, and manufactured into a specific for many diseases. At present, when tea is scarce, the Indians and Half-breeds use it sparingly. Silver Berry is one of the commonest shrubs on the prairie, and deserves a place in all collections of hardy species. About the middle of June its small yellow flowers perfume the air. This perfume is wafted for miles on the light breezes of the prairie. Later its Silver Berries are attractive to the " Pra Trie Chickens," and amongst its stems in the fall coveys are sure, to be found. Even the leaves are beautiful, and shine like silver, and when laid under a lens lovely stellate hairs of great beauty are revealed. Buffalo Berry is generally found iu the river or stream valleys of the south. It has also been found on the Assini- boine below Brandon, and at Manitoba House on Lake Manitoba. This is another fine shrub with beautiful foliage shining like silver, and in the months of August and Septem- ber loaded with large clusters of bright red fruit. There is no other berry in the southwest comparable to it for the making of jelly. After we had been on bacon for months, a jelly of these berries was a luxury of the highest order. Grizzly bears are very fond of them, and are hunted where these grow. The only grizzly ever seen by me was in a thicket of these bushes. This shrub, if a quick grower, would be excellent for fencing, as it has a number of short and stiff thorny branches in every part. NATURAL PRODUCTS OF THE SOIL. 187 Wild Hops are common in every river bottom throughout Manitoba. The past summer I found them climbing over shrubbery and up trees, and forming festoons over the end of every dead stick in the valley of Bed Deer River, lat. 53°. No place in the Assiniboine valley is without them. At Fort Ellice the river bottom seems like a hop-yard after the leaves have fallen in autumn. Hops are in great pro- fusion in the Qu'Appelle Valley, and hang in larger bunches than are generally seen in hop-yards. Hazel nuts are found where there is brush. Many thick- ets of these bushes extend for miles, and being generally higher than a man's head, and growing in brul6 cause travellers to dread them as they would a quagmire. The fruit is gathered in great quantities by the Indians and stored for winter use. I purpose in the following pages to give a few notes on the flora of districts, knowledge of which is generally desired. A voyager on the Assiniboine in the ascent from Winnipeg to Brandon, cannot but remark the paucity of species in the river valley as regards trees. It is true he sees familiar forms but many eastern species are wanting, and he looks in vain for beech, maple, or pine, and only occasionally does he see oak or ash. Poplar and elm with willows, which sometimes attain to the size of trees, make up the bulk of the wood, while roses {Rosa blanda) and Pembina berries ( Vi- hurnum Lentago) form almost impassable thickets. The Ostrich fern (^Struthiopteris Germanica) is occasionally very abundant, and attains a great height, and all herbaceous vegetation is astonishingly luxuriant. Climbers too are not wanting, and Wild Hops {Humuhos Lupulus), Wild Balsam, Apple {Echinocystis lobata), Hedge Bindweed {Galystegia sepium), Wild Grapes ( Vitis riparia), and Virginia Creeper {Ampelopsis quinque folia) , are common or occasionally seen. Berry bearing shrubs are not rare, as thickets of Wild Plum {Primus Americana), Easpberrj^ {Ruhus strigosios). 188 HANITOBA AND THE GREAT NORTH-WEST. Service Berry (^Amelanchier Canadensis), High Bush Cranberry [Viburnum Opulus et pauciflorum) , Wild Cherry {Prunus Virginiana), and White Thorn (^Cratcegus cocci nea), are very common, and bear well flavored fruit; Goose- berries {Ribes oxycanthoides), Wild Black Currants {Ribes Jioridum), and Red Currants (^Ribes rubrum), are abundant in the valley, the two latter where the soil is wet, the former on the drier slopes. A beautiful western shrub, the Buffalo Berry [Shepherdia argeniea), is occasionally met with on the Assiniboine, but it is only on the Saskatchewan that it is seen in its beauty. A near con- gener, the Silver Berry {Elcegnus argentea), is abundant on the drier slopes, and throughout Manitoba is said to indicate good soil, but in reality it is only an occupant of a dry one. These two shrubs are well worthy of cultivation, being per- fectly hardy, and having beautiful silvery leaves, and sweet scented flowers — the blossoms of the latter about the middle of June loading the air with their fragrance. Later in the season, the former is borne down with its close clusters of bright red acid berries, which when made into jelly and sweetened we found to be an excellent corrective to salt pork. The berries of the latter are of the same color as the leaves, and are quite mealy. These with rose hips constituted the principal food of our so called Prairie Chicken, the sharp- tailed Grouse {Pedioecetes pJiasianellus), during the fall and winter. Besides the shrubs mentioned above, there are a few that should not be passed without notice, on account of their beauty. Foremost are the Lead Plant [AmorpJia canescens), which was abundant at Portage la Prairie in 1872, and a smaller species, Amorpha microphylla, which is found in some abundance at the Rapids on the Assiniboine. Both these species are worthy of a prominent place in any of our gardens. Wild Honeysuckle (Lonicera parvijlora) and two species ot Snow Berrj- {Symplwricarpus racemosvs et NATURAL PRODUCTS OF THE SOIL. 189 occidentalis) with wild Cornel [Gornus stolonifera) , and Downy Arrow-wood (Viburnum pubescens), are found in more or less abundance in the river valley. The Wild Cornel or "Western Kinnikinik is very abundant in the valleys of all streams, and it is from the inner bark of this shrub mixed with tobacco, that all the Indians of the plains, and the Half-breeds make the " Harouge " which they prefer to pure tobacco. The Kinnikinik of the east {^Arctostaphylos Uva-ursi,) and the Creeping Juniper {^Jun- iperus Sabina var. procumbens) are abundant on all sandy soil, and form the chief covering of the sand dunes and hills throughout the country. In the Grand Valley (Brandon) and west to the Moose Mountain on the 102nd meridian, 452 species of plants were noticed during the latter part of June, the majority of which were common in Ontario ; a few seemed to have a southern origin, while others were exclusively vrestern, and others again extended far to the north. At the time we crossed the extensive plain lying between the Grand Valley and Moose Mountain (the latter part of June), the whole country was gay with beautiful flowers. The air was loaded with the perfume of roses, and the Elae- gnus, and every little mound was bright with the tall purple spikes of Oxytropus splendens and Lamberti, while the level prairie was dotted with patches oi Arnica angustifolia looking like the Marigolds of our gardens. Even the marshes were beautiful with the nodding Plumes of the Cotton Grass {^Eriophorum polystachyon) , and their borders lined with Dodecatheon and the little yellow star grass {/Sisyrinchium Bermudiana). The Sand Hills at Flat Creek were covered in spots with a beautiful Cactus (Mamillaria vivipara) which grew in small compact clusters often not larger than a small apple with a beautiful pink flower rising from the centre. A lovely fern {Botrychium Lwnaria) was growing amongst 190 MANITOBA AND THE GREAT NORTH-WEST. the grass, and Lalhryus ve'iiosus — the western pea — formed thickets in the hollows between the hills. Around these hills were numerous marshes filled with various grasses, and sedges, while the hills themselves produced vetches and horse-tails {Equisetum). At Pipestone Creek the vegetation (June 27th) was won- derfully luxuriant, and pasture excellent. The leading grasses were Avena pratensis, Sporoholus heterolepis, Poa casia et serotina, Stipa spartea, Yilfa cuspidata, Galamagrostis stricta et Canadensis, and Phalaris arundinacea. The ponds contain Carex aristata in the centre where the water is deep and permanent, outside this line Garex lanuginosa and Carex marcida. The three species are found in this order all over the country, and wherever they exist water is abundant. When Carex aristata disappeared from the ponds, water was bad or merely rain water, and we had to be on the alert. The prominent flowers were three species of Penstemon, (P. gracilis, cristatus et confertus var.), Hedysarum horeale, Thermopsis rhombifolia, Gaura coccinea, Galium horeale, Sisy- rinchium Bermudiana, Arnica angustifolia, and four species of Astragalus (J. pectinatus, flexuosus, caryocarpus, et hisulca- tus). All of these would have been ornaments to any gar- den, and greAV in such profusion that they gave a marked character to the landscape. Passing westward towards Moose Mountain, Hedysarwm horeale covered square miles of plain, and being tall, over two feet high, its spikes of lovely pink flowers were exquisitely beautiful, as they nodded to the pleasant summer breeze. A handsome Primula (P. farinx)sa) was very conspicuous, and together with its congener the DodecatJieon made the margin of many a marsh a floral paradise with the profusion of their lovely and bright tinted flowers. The flora of Moose Mountain was in no respect dijfferent from that of many parts of Ontario, except in the absence of forest trees of which there were but few species. NATURAL PRODUCTS OF THE SOIL. 191 After passing out on to the " Souris Plain " a marked change took place in the flora, and the soil became much drier. Hedysarum Machenzii was occasionally seen in great patches, and being of a rich velvety purple, charmed the eye with its beauty. At this date (July 7th) many beautiful flowers were in their prime, and their peculiar habitats were worthy of more than a passing notice. Every species has its own habitat, and at one time in going through a rich hollow, lilies (Z. Philadelphicum) will cover acres with orange red flowers. Leaving there and ascending a slope, we will have to cross a carpet of the richest purple, for here Astragalus Jlexuosus is extremely abundant, and fills the air with its perfume. On yonder knoll Oxytropis splendens and Castilleia sessiliflora dispute possession with Astragalus pectinatus and Erigonum fiavum We pass the ridge and now there is more water and a new series of plants come in to view, and Zagadenus glaucus, PotentiUa gracilis, Anemone Pennsylvanica and Lysimachia cihata, mixed with various species of Astragali, are noted, and as hours pass into days this ever changing panorama glides past filling our hearts with delight as we contemplate this garden of nature. Days pass, and these lovely gardens are left behind, and now stretched out on every side, is a vast clay plain with an extremely rough surface. The flora has changed, birds have almost disappeared, and even the hills have gone out of sight, yet beauty is still around us on every hand, Koses {Rosa hlanda), scarcely six inches high, load the air with perfume. Lepachys columnaris enhances the beauty of the landscape with its yellow flowers, and the rich green of the grass is pleasing to the eye, yet over all this vast ex- panse not a bird wings its flight, and our utmost exertions could hardly obtain water for ourselves and horses. One hundred miles and upwards is crossed, and the only shrubs seen are the two snowberries (^Symphoricarpus racemosus 192 MANITOBA AND THE GREAT NORTH-WEST. et occidentalis) and the rose bushes, while Aster tnultiflorus, Lejjachys and Triticum repens, with various Potentillae, make up the bulk of the flora. Moose Jaw Creek, like all other streams throughout the country, had essentially an Eastern flora, and it was only on the gravel ridges and clay slopes bordering its valley, that the western forms were seen. Here the species were char- acteristic of the arid plains to the south, and partook largely of an alkaline character. The flora of the Cypress Hills is very remarkable, and differs in many respects from that of the plains. In the coulees which extend into the hills on the north and east sides, the vegetation is almost exclusively eastern, and con- tains numerous forest species, while that of the plateau above, and the upper slopes of the hills have the prairie features of the Rocky Mountain flora, and both Alpine and boreal species here find a home. In the upper part of the coulees amongst the spruce at the eastern end were Spircea hetulifolia, Geranium Richard- sonii, Ilahenaria rotundifolia, Phleum alpinum, Arenaria nar- difolia et verna, Delphinium azureum, and on the exposed gravel points and ridges that rose almost perpendicularly were Astragalus pauciflorus, Sedum stenopetalum, Cetraria nivalis, aculeata et Islandica, Polygonum, Paronychia, et Yesi- caria montana. In the deep coulees around springs of purest water, were large patches of Mimulus Jarnesii covered with a profusion of yellow flowers, and amongst the common sedges were Carex /estiva and capillaris. These, all mountain species, and numerous others known to dwell there, told a tale that the botanist alone could understand. Whether the Cypress Hills were an outlier of the Rocky Mountains or not, their flora indicated that their climate was that of the foot hills above Morleyville, and necessarily unfit to regu- larly mature cereals, although, in sheltered valleys, barley and potatoes could possibly be raised. NATURAL PRODUCTS OF THE SOIL. 193 The grasses of the plateau were of the real pasturage spe- cies, and produced abundance of leaves, and were so tall, that for miles at a time we had great difficulty in forcing our way through them. The chief were species of Festuca, Danthonia, Poa, Avena pratensis, Bromus, and Pfdeum alpin- um, and although their seeds were all ripe (August 4th) their leaves were quite green. As we proceeded westward over the plateau, it became more elevated and other species began to take prominence, notably Impinus argentea and Potentilla frwlicosa covered miles of country to the exclusion of other species, and as both grew about eighteen inches in height, and h ad a bushy habit, the whole country, for a day's travel, was either blue or yellow or both, as either species prevailed or were inter- mixed. In all my wanderings I never saw any spot equal in beauty to the central plateau of the Cypress Hills, After the middle of August, 1880, mushrooms became very abundant, and continued with us until the latter part of September, when the frosts became too severe, and prevent- ed their growth. There were three species all equally large and numerous, and although we consumed great quantities of them we never observed any ill effects from their use. There was one species, however, which was very large, and more abundant than the others, which I did not touch, as I did not like its appearance, yet the usual test indicated it to be nutritious. While crossing the great plains north of the QuAppelle in July, 1879, we found mushrooms by the cart- load, and the past season we used them every day for three weeks while travelling at least two hundred miles in an easterly direction. From the reports of other travellers, and my own observations, I am lead to believe that on nearly the whole prairie abundance of mushrooms will be obtained after any great rain fall during the summer. One species of Lycoperdon (Puff Ball) was seen that grew to a very large size, and numerous others were noticed during the whole 13 194 MANITOBA AND THE GREAT NORTH-WEST. season scattered over the plain in great profusion. No Lyco- ijerdoiL is poisonous, but if gathered young before the spores turn yellow, cut into thin slices, and fried, are highlj^ nutri- tious. Were it possible to teach the Indians to discriminate between the good and bad mushrooms, immense quantities could be collected every year, dried and stored away for future use as is done in Norway. The following notes from m}" journal will illustrate the flora in the vicinity of Long Lake as seen the first week in July, 1879. Flowers are a most conspicuous feature of the prairie. Hedysarum and various Astragali vieing with the liij' and the vetch in loveliness and luxuriance. Often whole acres would be red and purple with beautiful flowers, and the air laden with the perfume of roses. Sometimes lilies (^LUiinn l^hihidelplufinn) are so abundant that they covered an acre of ground bright red, at others they are mixed with another liliaceous plant {^Zagddenus glaturns) and form a ring around the willow thickets which we pass. At anoth- er time we come upon a pool of fine pure water, and within is Carex arisfata which the horses love so well, around it Avhere the water is neurlj" gone are Garex marcida and lanuginosa. Outside of these a ring of white anemones {Anemone Pennsi/luani<<() and growing Avhere it is slightly drier a yellow flower (Po/enHUa graclli'i). As the ground became still drier the Parf)le Pentstemons {Peidsteinon con- fertuft) would appear, and lastly the lilies would surround the whole. Mushrooms are extremely abundant, and attain a fabulous size. They grow in regular "fairy rings" often more than 40 feet in diameter. Some rings were found to contain so many, that taking all good and bad from one ring, we could almost load a cart. Other rings were devoted exclusively to a species of giant Puff-ball which Avere extremely numer- ous on almost ever}^ part of the plains. Amongst many others I measured one specimen of a mushroom that was 33| NATURAL PRODUCTS OF THE SOIL 195 inches in circumference, and 2| inches through the cap. The stem was over 2 inches in diameter and weight over three pounds. Dr. Loew, of the American Geological Survey, reports that the bark of the common Aspen (^Populus tremuloides) is used by the Indians in intermittent fever. His analysis of the bark gives salicin and populin. The former was long ago in common use in intermittents. "It has," says Dr. Rothrock, " long been more or less a domestic remedy, and, indeed, of a certaia class of practitioners, for this disease. It is not a little remarkable, however, that it should be used by the Indians, and we can only account for the fact that it does possess some remedial power in this direction, which a ' hit or miss' empiricism has led them to discover." CHAPTER XII. Raising Wheat. Red Eiver Prairie, Description of its Soil — An Old Countryman's Views — Extent of the Wheat Lands — 150,000,000 Acres of Wheat Lands — Manitoba Excluded from the Calculation — Good Land Continues for 100 Miles at a Time — Fixed Laws Regarding the Growth of Wheat — Northern Limits of Wheat Zone — Northern Wheat more Pro- lific — The Cause Explained — How Wheat Grows in Spring and Summer — Why Mani- toba Wheat is Hard — Roots Penetrate to a Great Depth — Analysis of Soil, far Supe- rior to the Best Wheat Land in Europe — Best Soil in the World in the North- West — Manitoba Formerly an old Lake Bottom — Soil of the Second Prairie Steppe — Soil of the Third Plateau — Gypsum very Abundant — Cactus no Proof of Aridity — Setter's Farm Described — Wheat Growing amongst Cactus — Appearance of the Land — Besults of 1880 — of 18S1 — Seed Bought in Minnesota in 1876 — Progress since Then — ^Mani- toba Wheat Admitted Duty Free into Minnesota — Opinions of Pioneer Press of St. Paul's, Minnesota, regarding North- West Wheat — Statements of Residents — Average Crop for Four Years — ^Average Yield of Canadian North-West Compared with the best States in the Union — Great Weight of the Grain — Qu'Appelle Region as a Wheat District — Prince Albert and Edmonton as Wheat Districts — Description of Edmon- ton — Gust's Farm at Edmonton — Country on Peace Eiver — Excellent Wheat Lands far to the North — Cucumbers Ripen in Lat. 60° — Wheat in Lat. 61° First-class — Spring Frosts not Hurtful— Fall Wheat not Suited for the North-West— Fall Sowing Recommended — No Doubt of its Success — Instances of Fall Sowing — Fall Sowing the True Policy of Settlers on the Prairie — Wheat Production of the Future beyond Cal- culation — England should Realise that we have the Greater part of the Wheat Lands of America — England's True Policy — Farmers Testimony Regarding the Soil. The Red River Prairie, or first Prairie Steppe, differs from the more western lands in being almost a dead level, except occasional ridges of gravel, which slightly change the uniformity of the surface. So much has been said and written regarding this prairie that I shall quote the opi- nions of only two individuals regarding it. One is noted for his scientific attainments, the other for his general in- telligence and close observation. Dr. George M. Dawson thus describes the Red River Prairie in 1874 : — "Of the alluvial prairie of the Red River, much has already been said, and the uniform fertility of the soil can- not be exaggerated. The surface for a depth of from two RAISING WHEAT 197 to four feet is a dark mould composed of the same material as the subsoil, but mingled with much vegetable matter. Its dark color is no doubt in part due to the gradual accumu- lation of the charred grasses left by the prairie fires. The soil may be said to lie ready for the plough, and in turning the tough prairie sod the first year, a crop of potatoes may be put in, though it is not efficiently broken up till it has been subjected to a winter's frost. When the sod has rotted, the soil appears as a light friable mould, easily worked, and most favorable for agriculture. The marly alluvium underlying the vegetable mould, would in most countries be considered a soil of the best quality, and the fertility of the ground may therefore be considered as practi- cally inexhaustible. The area of this lowest prairie has already been approxi- mately stated at 6,900 square miles, but of this the whole is not at present suited for agriculture. # # # * As a measure of the possible agricultural capacity of this great valley, take one-half of the entire area, or 3,400 square miles, equalling 2,176,000 acres, and for simplicity of cal- culation, let it be supposed to be sown entirely in wheat. Then at the rate of seventeen bushels (the average is ovef 25) per acre — which according to Prof. Thomas is the aver- age yield for Minnesota — the crop of the Red Eiver Valley would amount to 40,992,000 bushels." Our other quotation is from the report of Mr. R. H. B. P. Anderson, of County Kerry, Ireland. His description belongs partly to the Red River Prairie and partly to the Pembina Mountain district : — " The soil varies much, as it is natural to suppose over so large a tract of land, but as a rule it is rich, black, vegetable mould, working very like clay — rich beyond imagination and resting on a marly clay. The depth of the surface soil varies a good deal, in some places not more than ten or twelve inches, in others as many feet. I am informed that chemical analysis has 198 MANITOBA AND THE GREAT NORTH-WEST. proved the soil to be the best adapted of any in the world for the growth of wheat, and certainly practical experience bears this out. It is very easily worked, becoming as fine as powder. However, there are all descriptions of soil to be had here, from the heaviest clay to the lightest sandy loam." The above extracts will show that almost all observers class the land with the best in the world. Between Winni- peg and Edmonton, a distance by cart road of 980 miles, the various settlers affirm that where they are located is the best land in the country. Travel where you may the same story is told you, and proofs are shown of the astonishing fertility of the soil. At Fort Calgarry in the south wheat produces enormously, and in lat. 59", 600 miles due north of that point, I obtained wheat that took the Bronze Medal at the Centennial in Philadelphia, in 1876. In nineteen- twentieths of all this vast area there is a clay subsoil with a surface soil varying from black clay or clay loam to light sandy loam. It is difficult to give even an approximate estimate of the extent of cultivable lands in the North-West Territories. The following was made at the request of the Government' in 1877 : If a line be drawn from the boundary line where it is intersected by the 95th meridian, in a northwesterly direction to where the 122nd meridian intersects the 61st parallel, we shall have the base of an isoscles triangle, which has its apex on the 115th meridian, where it intersects the 49th parallel, one side being the boundary and the other the Rocky Mountains. This triangle encloses at least 300,000 square miles, or over 200,000,000 acres of land. In a rough classification I estimated 80,000,000 acres as arable land and 120,000,000 acres as pasture, swamps, and lakes. After two years further examination, I submitted another report to the Government, of which the following is a condensed summary. RAISING WHEAT. 199' Since the date of my last report I have had opportunities of gaining a much more extended personal knowledge of the region, and I have had access to the reports of all the recent explorations made by others, and had personal conversations with the several explorers. I am, therefore, in possession of much a dditional data and in a position to classify the areas of land with greater general accuracy. I now submit what I consider a tolerably correct estimate of the areas of the several descriptions of land between the Rocky Moun- tains and Manitoba, not including the latter province, and excluding also any available land that may exist north of lat. 57" in Peace River District. The total area of available land suitable for agriculture and pasture was 150,081,280 acres after 30,000,000 acres had been deducted for bad and wet lands. Within the whole area of 180,000,000 acres there are isolated patches of unavailable land, consisting of marshes and swamps, sand hills, barren clays and stony tracts. Possibly not one-third or 10,000,000 acres of the whole 48,000 square miles which I have deducted from the total area could be classed as sterile or irreclaimably wet. There can be no doubt that drainage will ultimately do much to contract the area of land now considered valueless. At present I consider that in the North-West of Canada, beyond Manitoba and within the western and northern limits defined, there are at least 150,000,000 acres of land suitable for agriculture and stock-raising, and of this area I feel confident that a higher percentage will be found avail- able for growing grain than in that portion of Ontario so well known for its productions — I refer to the peninsula lying between the Lakes Huron, Erie, and Ontario, and bounded on the north and east by a line drawn from Kings- ton to Lake Simcoe and the Georgian Bay. Many unacquainted with the country think that good land is in patches like most other districts. Often for 100 miles at a time no bad soil is seen in any direction, and the 200 MANITOBA AND THE GREAT NOKTH-WEST. only land not suited for grain would be tlie marshes or the steep slope of a coul6e. Much of the southern district now con- sidered fit only for pasture will yet be known as the best of wheat lands. Nothing is needed to prove this but the plough. There are certain laws applicable to wheat culture which are of the greatest importance when studied in reference to wheat growing in the North-West. Naturalists recognize the fact that there are certain limits within which each species of plant or animal attains its greatest development. I may mention here, that if the mean temperature of the two months, July and August, reaches 60°, wheat culture will be profitable. Now in the tables given in the chapter on climate, it is shown that in every part of the territory the temperature exceeds this. I might even state that this temperature is found over a far larger area. I believe that wheat culture will yet extend to within a short distance of Hudson's Bay and down the Mackenzie to lat. 65°. Another physical law fixes the greatest yield near the northern limit of successful growth. This was well exemplified by the wheat obtained in 1875 at Lake Athabasca, in lat. 58° 42'. In Ontario seldom more than two grains to the cluster are found, in Manitoba three is the usual number, at Edmonton four or five, and at Lake Athabasca five or six. Did the average yield of Ontario reach fifteen bushels, the yield in Manitoba would be twenty -three, at Edmonton over thirty, and at Peace Kiver forty bushels. This accounts for the large yields per acre reported from these places, and were only the same number of ears per acre harvested in the west the proportions would remain the same. But when an acre without either stump or stone is reaped we may expect to hear of thirty to forty bushels per acre being the average on well-tilled fields in Manitoba. There is no reason why sixty bushels to the acre should not be reaped. On another page I have stated in detail the growth of wheat froto seed time to harvest, and from that it will be RAISING WHEAT. 201 seen why the climate is so well suited for its growth. Cool- ness with moisture in spring gives root growth. The porous soil allows the roots to penetrate to an astonishing depth. During June and July there is abundance of rain and great heat, followed in August by still warmer weather and some rain, which completes the cycle of growth. As soon as the weather begins to cool, rain ceases and the air becomes very dry, hardening the grain and giving it that flintiness and weight for which all Manitoba wheat is noted. Two causes combine to produce the enormous crops reaped on those lands. The frosts of winter pulverise the ground to a depth of many feet. Summer rains, with almost constant sunlight, give a quick and vigorous growth. Owing to the looseness and porousness of the soil in spring the roots throw out many fibres, and when the rains come these openings are filled, and the growing crop feeds on eighteen inches of soil instead of three or four. Hence bad husbandry has little effect on the crop for many years. As long as the west is blessed with winter frosts and summer rains so long will teeming crops be the product of her soil. Were it necessary for the growth of the plant the small fibres could penetrate to a depth of over three feet. It will be remembered that the land is never wet when winter sets in. Only a few samples of the soil have been properly an- alyzed as far as I am aware. One I will give in the words and figures of the chemist who made the analysis, Professor Emmerling, Director of the Chemical Laboratory of the Agricultural Association of Kiel, in Holstein. He writes to Senator Emil Klotz : " The analysis of the Manitoba soil is now completed, and the result is in 100,000 parts : Potash 228.7 Sodinm 83.8 Phosphoric Acid 69.4 Lime 682.6 Magnesia 16.1 Nitrogen 486.1 (Signed) " V. Emmerling." 202 MANITOBA AND THE GREAT NORTH-WEST. Senator Klotz writes from Kiel, May 4th, 1872 : "After considerable delay I succeeded in obtaining the analysis of the Manitoba soil from Professor Emmerling, and hope it may be of service to you. Annexed I give you our analysis of the most productive soil in Holstein, Avhereby you will see how exceedingly rich the productive qualities of the Manitoba soil are, and which fully explains the fact that the land in Manitoba is so very fertile even without manure. " The chief nutrients are, first nitrogen, then potash and phosphoric acid, which predominates there ; but what is of particular importance is the lime contained in the soil, whereby the nitrogen is set free and ready to be absorbed in vegetable organisms. The latter property is defective in many soils, and when it is found defective recourse must be had to artificial means by putting lime or marl (a clay i^hich contains much lime) upon the same. According to the analy- sis of the Manitoba soil there is no doubt that, to the farmer who desires to select for his future home a country which has the most productive soil and promises the richest harvest, no country in the world offers greater attractions than the Province of Manitoba, in the Dominion of Canada." Analysis of Holstein soil and Manitoba soil compared : — HOLSTEIN son,. MANITOBA SOIL. EXCESS IN MANITOBA SOIL. Potash 30 228.7 198.7 Sodium 20 33.8 13.8 Phosphoric Acid.. 40 69.4 29.4 Lime 130 682.6 552.6 Magnesia 10 16.1 6.1 Nitrogen 4o 486.1 446.1 Manitoba or the first Prairie Steppe was originally with- out doubt an old lake bottom. Lake Winnipeg is the remains of the lake. It follows that nearly all Manitoba possesses an alluvial soil, chiefly derived from decaying vege- tation and the fine silts brought from the more elevated region to the west. Lying along the western margin of the Manitoba plain is a series of sand dunes, which gradually pass into the second Prairie Steppe, the soil of which is RAISING WHEAT. 203' diflferent from that of the plain below. The surface here is principally a dark-colored sandy loam, sometimes passing into clay, while at others it becomes quite light and sandy, more especially in the vicinity of the various rivers. The subsoil is very uniform and seems to be a light-colored marly clay, containing numerous pebbles coated with car- bonate of lime. As we approach the confines of the third plateau the soil gradually passes into clay and the surface and subsoil be- come more homogeneous. It is on this plateau where most of the pasture lands are situated. The greater part of it is altogether without wood. The second steppe contains much sand in certain localities and the third much gravel in the more elevated tracts. It is simply then a change from silt to sand and from sand to gravel. Only, however, about five per cent, of the soil can be called either sandy or grav- elly. The Second Steppe is composed of Cretaceous rocks overlaid with a thick coating of drift, while the Third Steppe is sometimes called the Lignite Tertiary Plateau, on account of it being composed of this group of rocks. One of the chief ingredients in this higher plateau is Gypsum, which can be gathered in a crystallized state wher- ever there is a slide in a river bank. The surface water of this plateau is often a mild solution of Epsom salts where the soil is not covered by drift and the clays obscured. When the underlying Cretaceous clays are exposed the water is equally bad and the soil shows signs of aridity, being cov- ered more or less with Cactus {Opuntia Missouriensis) and Artemisia {Artemisia cana). This is the "Sage Brush" of Palliser's Report, but not of the American Desert as he asserts. As it is generally supposed that these Cactus flats are too arid for the growth of wheat, I insert an extract from my report for 1880. The location referred to is on the north side of the Cypress Hills, and certainly had every appearance of sterility prior to being broken up. 204 MANITOBA AND THE GREAT NORTH--WEST. The creek upon -which the farm is located has on its banks some willows and maples, the former being the largest I have seen in the North-West, a few being three feet in diameter. There is no poplar on the creek, and all fence poles have to be brought from the hills. All the land broken up was in the flats along the creek, and consisted almost wholly of soil, which in my former reports I had pro- nounced worthless. The hills were composed of light or dark-colored sandy loam with numerous boulders and some gravel on the hill tops, and the flats along the creeks of Cretaceous clay and so arid that grass could not form a sward. The flats were covered with sage brush [Artemisia cana) and Cactus {Opuntia Missouriensis) and everything betokened aridity. This was how the country looked when I was there on August 13th, except the part under cul- tivation. Setter located the farm in April, set to work and broke up the artemisia and cactus flats, but got only a little sown before a drought set in, which continued all through June and caused some of the seed to lie in the ground over three weeks. Notwithstanding, I gathered ears of ripe wheat on August 14th, and have been informed since that the greater part of the crop ripened. At the time I gathered the ripe ears of wheat, Cactus was in flower for the second time, and both were flourishing together. The problem was solved, that the apparently arid soils were only so in appearance, and that all the land where not covered with sand or gravel would yet " blossom as the rose." The soil had been broken up only to the depth of a few inches and the change was astonishing. I could not penetrate the sun-baked clay, but not a yard away, where he had ploughed, I could dig to any depth. On the one hand was life, while on the other, the artemisia and cactus gave evidence of death or profound slumber, as all vegeta- tion was dried up by the great heat of the last month. RAISING -WHEAT. 205 My own observations and those of others who have care- fully examined many parts of the country, cause me to believe that actual settlement will show that fully eighty per cent, of the land is arable or will be located as farms. During the summer of 1875 the grasshoppers were very destructive in Manitoba, and scarcely any wheat was raised. The next spring nine-tenths of the seed had to be bought in Minnesota, yet in the fall of 1878, 1,100,000 bushels of wheat were harvested. In 1881 it had risen to millions of bushels, and now when railroads are open to take it to market, its production will go on at an ever increasing ratio, the capacity of the country being only limited by the means of transport. I place the testimony of residents in a tabulated form, to show the number of bushels raised by each per acre during the four years 1877 to 1880. As I give name and post-office address any person can verify the truth of the statement. One column is set apart for the average weight per bushel, so that parties may know that besides a large average of bushels there is a high average of weight. The number of bushels depends largely on soil, but the weight solely on climate, for no wheat can be heavy in a damp climate. Manitoba wheat is allowed to enter the United States free of duty when a guarantee is given that it is going to be manufactured for export. It has been found that a mixture of hard Manitoba wheat and the softer Min- nesota makes a far better flour than the Minnesota alone, and the shrewd Yankee takes advantage of this and gets the wheat admitted in bond. The following quotation from the "Pioneer Press" of St. Paul, Minnesota, certainly a disin- terested authority, will give point to the above statement. It says in its issue of November 8th, 1880 : — " It seems to be a settled fact that the further north wheat is grown, up to a certain limit, the better it is. * * * The future great wheat region of the world will, undoubt- 206 MANITOBA AND THE GREAT NOETH-WEST. edly be in the rich and far-famed valley of the Saskatchewan where this grain grows to perfection, not only in quality but in ever}^ other particular. The berry attains an amber color, rounds out into a fullness it does not attam here, and is rich in glutin, the life sustaining principle in flour. * * Some two or three years ago samples were jDrocured from several parts of the Province of Manitoba for trial. The best of these was placed in the hands of some of our leading wheat growers for cultivation. One variety, Scotch Fife, yielded the first year, at the rate of thirty-seven bushels to the acre, of a hard amber color, which the wheat inspector of the Millers' Association at Minneapolis pronounced the finest specimen he had seen since he had been connected with the Association. Straw stood up stiff and strong, some of it being over five feet high, the heads were long, while the color of the growing grain was superb." The above was scarcely in print when American buyers were in the country, and the whole surplus Avas bought up at a higher price than the Dakota wheat nearer home. The following returns are given by some of the most re- spectable and intelligent farmers in the North-West, and are reliable. Where the average is below twenty bushels it must be remembered that the cause is generally newly broken land, or some misfortune to the crop : — NAME. ADDRESS. YIELD PER ACRE. Aver'ge 1S77. 1878. 1879. 1880' Weight Ijerbhl. .Tohn Dilworth High Bluff 25 30 25 25 25 25 33 35 30 30 28 25 25 30 20 28 30 20 29 23 20 35 32 32 20 25 25 28 23 25 30 24 26 34 16 35 35 31 20 22 25 22 25 40 25 25 30 30 20 40 37 30 30 30 35 35 61 George Cadman William Jackson . . 60 62 William Eagles S. C. Higginson J Sutherland 65 Oakland 62J 63 Kildonan E B. E. Mitchell William Moss Cook's Creek High Bluff 66 60 64 John Ferguson John Airth 61 stonewall 63 Kobert Fisher Cook's Creek St. Charles 64 J W AdBhead 63 Robert Black Bird's Hill 62 EAISING WHEAT. 207 NAME. James Amisou . . William Corbett George Taylor . . John Brydon . . . E. J. Moore J. Geddes J. Macdouald . . . 0. Gillespie A. P. Stevenson . Ed-ward Scott . . P. Furguson Max. Wilton A. Dawson A. J. Hinker F. Ogletree T. H. Brown .... G. A. Tucker . . . A. V. Beckstead A. J. Nugent W. B. Hall Charles Begg . . . H. Grauby A. Poison, jr . . . . G. Tidsbury J. B. Robinson . . Neil Henderson . Thomas Sigsons. James Munroe . . James Taylor ... T. Dalzell William Hill . . . , J. Davidson John Fraser Alex. Adams . . . , John Hourie .... C. Stewart W. A. Farmer . . . E. Bumell Robert Bell John McKinnon. , J. W. Carlton . . . . E. P. Bradley ADDRESS. YIELD PER ACRE. Hig;h Bluff Springfield Poplar Point Portage la Prairie . . Nelsonville Kildonan Gladstone Plympton Nelsonville Portage la Prairie . . Gladstone High Bluff Headingly Green Ridge Portage la Prairie . . Poplar Point Portage la Prairie . . Emerson West Lynne Headingly Stone Fort High Bluff Kildonan High Bluff Rockwood Cook's Creek Portage la Prairie . . Kildonan Headingly High Bluff Woodland High Bluff Kildonan Clear Springs St. Anne Meadow Lea Headingly Nelsonville Burnside Portage la Prairie . . Clear Springs St. Pie 1877 35 35 26 31 27 20 30 10 33 25 30 30 30 25 25 30 25 30 20 20 35 27 25 23 24 30 25 30 15 26 15 25 24 38 20 28 27 30 27 30 25 30 1878. 34 30 25 33 24 30 30 28 30 27 29 34 30 17 38 20 27 35 20 30 30 25 30 25 28 30 28 30 16 25 20 25 25 35 34 2S 25 25 30 30 15 32 1879. 32 31 30 30 23 35 35 35 28 37 26 40 30 23 36 18 27 28 18 15 32 21 25 35 20 30 35 34 8- 33 15 30 22 30 18 15 20 30 30 30 10 40 1880. 35 50 36 30 28 35 30 25 30 33 30 35 30 26 30 27 23 35 25 40 35 30 30 20 36 36 30 34 15 20 26 26 25 40 30 20 25 30 27 30 20 25 Aver'ge Weight per bhl. 62 63 66 62 61 60 62 64 66 65 65 62 60 65 60 60 63 65 58 60 60 62 65 62 61 65 62 64 60 64 62 , 60 61 62 61 63 65 65 62 63 61 65 Average yield, according to the above, was over twenty- six bushels per acre. Taking twenty-six bushels as the average yield of the Canadian North-West, we will compare this with American States : — Canadian North-West 26 Bushels per Acre. Minnesota 17 „ Massaehusetts 16 ., Pennsylvania 15 „ Wisconsin 13 „ 208 MANITOBA AND THE GREAT NORTH-WEST. Iowa 10 Bushels per Acre Ohio 10 ,T Illinois 8 „ These facts show the superiority of the Canadian North- West as a wheat-growing country. The weight of the wheat grown is also remarkable. Taking the heaviest samples of each country we find : — Canadian North-West 66 lbs. per Bushel. Minnesota 65 „ Ohio 60 „ Pennsylvania 60 „ Illinois 58 „ The Qu' Appelle region, partly surveyed last year, will be opened up this year by means of the Canadian Pacific Rail- way, and here in one block are at least 10,000,000 acres of wheat lands which hitherto have been almost unknown to the general public. Late surveys show that on the line of the Canadian Pacific Railway, 100 miles west of Brandon, lies the finest tract yet opened up, and having the warmest summer climate in the North-West. At Prince Albert, 600 miles from "Winnipeg, there is a large settlement and abundance of wheat is grown. Two steam grist mills and one portable mill at Duck Lake grind the flour required for the surrounding country. Owing to the influx of settlers and the necessity of supplying the Indians, flour has been bringing a high price, and no diffi- culty is found in disposing of the surplus. Almost 1000 miles from Winnipeg is the Edmonton settle- ment, and here farming is carried on extensively. Two steam grist and saw mills are in operation, and at this distant point they have regular Agricultural shows, where the various products of the country are exhibited. The corres- pondent of the Toronto " Mail," writing of the settlement last October, thus speaks of its appearance and products : — " Edmonton is located on the north side of the Saskatche- wan River, 200 miles north of Calgarry, Bow River District, RAISING WHEAT. 209 and 300 miles west of Battleford, more or less — decidedly more over the bad state of the roads when I travelled them. The view of the river approaching from the south is very fine. A plateau — the original level of the country — ^extends from each side of the river, and it is only when near the edge of the bank that the traveller recognizes the deep channel which he has to cross to reach the town, apparently only a few chains distant. Approaching a little nearer, however, he perceives a large valley and a magnificent river sweeping rapidly eastward and northerly around a curve which forms a plateau large enough for a small farm, and then losing itself in a gorge some distance below, near where steam risiag from the smoke-stack of Edmonton Mills, gives evi- dence of progress and industry. The banks of the river at the ferry rise to nearly 200 feet, but the ascent is made by the benches and plateaux to the upper level, and so is toler- ably easy." After describing the town site, the Hudson's Bay Fort and remarking on gold and coal mining, he proceeds with his description and says : — "Two steam mills for sawing and grinding have been erected at Edmonton * * * * j^ ^jjj thus be seen that the rich agricultural country in this neighbourhood will have ample accommodation for having their wheat ground, as well as opportunity of obtaining supplies of lumber for build- ing purposes. But a short time since lumber had to be manufactured by hand labor, consequently was comparatively scarce. Now settlers can furnish their houses as economi- cally as those 500 miles farther east. Whilst referring to the surrounding country, I may mention that the most ex- tensive farmer in the district is Mr. Oust, whose farm is contiguous to the St. Albert's Mission. He is a native of the County Derry, Ireland, and has been on his present farm for five years. He had this year 180 acres of land under wheat, yielding thirty bushels to the acre ; thirty-six acres barley, yielding thirty-six bushels to the acre on new 14 210 MANITOBA AND THE GREAT NOKTH-WEST. & ground ; and twelve acres of oats yielding, twenty-five bushels to the acre. The grain crop this past season has been lighter than former years, owing to cold, wet weather, altogether exceptional in this district until the past two years. His oats this year are only twenty -five bushels to the acre, which he considered only half a crop. Mr. Oust had twelve ploughs engaged last fall (1880) to do up the ploughing for spring crop whilst the good weather lasted. He has forty -four head of cattle, sixty hogs — twelve of them fit to be slaughtered next week." Four hundred miles to the north crops are just as early as in the vicinity of Winnipeg, nine degrees or 650 liiiles farther south. While on Peace River, in 1875, I was enabled to collect information regarding the raising of grain along 770 miles of its course. Excellent potatoes were ob- tained on July 21st, in lat. 56°, and oats and barley ripened on the 12th August. Strange to say 400 miles to the north- east splendid barley was in the stock on the 6th of August, and wheat was ripe on the 12th. At Fort Ver- milion, in lat. 58° 24', I had a long conversation with old Mr. Shaw, who has had charge of the establishment for sixteen years. He said that frost never injured anything on that part of the river, and every kind of garden vegetables could be grown. Still farther to the north and east, at Little Red River, I found cucumbers, Windsor and pole beans ripe, and was told that their summers were always warm and frost did no harm. Chief Trader Macdougall says that Fort Liard, in lat. 61° N., has the warmest summer temperature of any place in the district, and that all kinds of grain come to maturity, and vegetables of every description could be raised with success. At Fort Chipweyan I obtained the wheat and barley which took the prize at the Centennial, and of the soil which pro- duced it I wrote : " Less than two miles from the Fort is the French Mission, where I obtained the barley and wheat. 212 MANITOBA AND THE GKEAT NORTH-WEST. The soil here is a mixture of humus and sand, and in any other locality would be considered valueless, but everything planted or sown around the Mission seems to flourish." There are no records to show that spring frosts ever did harm to the growing grain. It is a well-ascertained fact that as soon as spring does come, fine, warm weather is continuous, and the only danger from frost is after heavy rains in August. Fall wheat will never be a success on the prairie, but there is no reason why it should not in the moister country to the north. Usually September is too dry for a fall growth on the open prairie, and besides, the biting winds of winter, and the clear sunshine and light snow fall, would destroy the crop. For the last three years I have been advising settlers, both by public lectures and personal conversation, to sow their wheat and many garden seeds in the fall, say after the mid- dle of October, instead of in the spring as they now do. This is the true fall sowing, and it has only to be tried once to prove its success. I was led to think of this while at Battleford, in 1879, by seeing a field of self-sown barley almost ripe before the other had headed out. In the same field there had been a potato patch the preceding year, and now it was overrun with seedling potatoes. Every potato stalk had produced an abundance of fruit and now the seeds were scattered and growing. During the fall, owing to the dryness of the atmosphere, there is scarcely any growth, and my advice is to sow so late that the grain cannot germi- nate. Owing to the dryness of the seed and soil, it can- not absorb water enough to cause it to rot. When the first warm days of spring come the snow melts and passes into the soil, the starch of the seed by this time has changed to grape sugar, and germination taking place at the same time, the young plants get a start that no drouth can injure. We hope to see the day when nearly all the wheat shall be sown at this time, and then August frosts can destroy no RAISING WHEAT. 213 more. About the 20tli August there is a sudden lowering of the temperature, and all grain hard, at this time, is safe. Grain ripens slowly after this and is often injured by frost. Last season there were two notable instances of fall sowing chronicled in the newspapers. Mr. Bannatine, of the city of Winnipeg, sowed wheat and carrots early in the preced- ing November, just a few days after I had advised it from the public platform in that city. In July last the wheat was two weeks ahead of spring-sowed grain, and doubtless it ripened two weeks earlier. The other instance is related by a correspondent of the Toronto " Globe," who, while at Edmonton last October, got the facts from Mr. Oust. His words are — " Like many other pushing and intelligent agri- culturist in the North-West, Mr. Gust has come to the conclusion, that in future the safest and best plan of oper- ations will be to do as much fall sowing as possible, that is, putting in spring crops in the fall, so that they will germi- nate during the first warm days of spring, and mature for harvest long before the early frosts that are liable to visit this part of the country can possibly reach them. I am in- formed that Mr. Reid, down at Fort Saskatchewan, has tried the experiment of sowing spring wheat in the fall, and that the results have been most satisfactory." This is the true policy of settlers on the dry southern prai- rie where crops may suffer from a June drought, or those along the Saskatchewan where early frosts and cool winds are engendered by the proximity of forests or muskegs. As I have said fall wheat as sown in Ontario will never do on the prairie, but late fall sowing for spring growth will an- swer every purpose, and it requires no prophet to foresee it. Much might be written about the future and calculations made regarding the wheat production of years to come, but such speculations are needless. In a very few years the crop will be limited by the means of export, and just as the carrying capacity of the roads increases, so will the crop. 214 MANITOBA AND THE GREAT NORTH--WEST. No sane man can doubt this, for a glance at the map will tell him that there is actually no limit, but the want of a market, to the wheat crop of the North-West. When the rulers oi England awake, as they soon must, to the fact that within the Dominion of Canada exist to-day, as virgin soil, three- fourths of the wheat lands of North America, and that it is to her they must look for their future supplies of food, whether it be beef or flour, we will receive that amount oi attention and consideration which, as England's greatest colony, we deserve. What we want is men and money, and both these a judiciously framed emigrant policy on the part of Great Britain would give us. Year after year her people are passing by thousands into the United States, there to become alienated from the parent state, whilst one of her own colonies offers superior advantages, and reconciles every dissatisfied son to the old mother-land across the water. The hand writing is on the wall and few care to read it, but it stands there in flaming characters, — Give us land for it is the people's — it is ours. A few short years and the words change, and now they are — We take the land which is ours by our heritage of labor, — and we will get it. A few millions given now to assist emigration to the new North-West would relieve the pressure and convert re- bellious sons into loving grateful children. There is land enough for all, and there is no reason why we should not receive men for our offer of free land. Farmers' Testimony respecting the Soil. NAME. POST OFFICE. DEPTH OF SOIL. Ben Hartley St. Charles Black loam from 16 to 20 inches. John Dilworth High Bluff „ „ 18 to 24 inches. George Cadman „ „ „ about 1 5 inches. W. Jackson „ „ „ „ 18 inches. A. Gillespie Greenwood My farm is chiefly bush land. William Eades Stonewall Black loam 4 feet. J. C. Higginson Oakland „ 2 feet. J. Sutherland Kildonan Bast „ from 3 to 10 feet. Allan Bell Portr.go li Prairie. , „ „ 18 inches to 2 feet. RAISING "WHEAT. 215 NAME. POST OFFIOB DEPTH OF SOIL. James Sutton Nelsonville Black loam from 18 Inches to 2 feet, A D. Cadenhead Scratching Eiver . . I have dug 12ft.without reaching bottom. Adam Nelson Nelsonville Black loam 18 inches. A. J. Hinker Green Sidge Rev. T Cook Westbourne . . F. Ogletree . . Portage la Prairie.. T. Hy. Brown Poplar Point G. A. Tucker Portage ia Prairie A. V. Becksted Emerson A. C. Harvey Poplar Point .... G. C. Hall Portage la Prairie , P. McKay Portage la Prairie D. G. Lowe St. Agathe A. J. Nugent West Lynne ... W. B. Hall Headingly G. Turner Lower Fort J. G. Maley Morris A. Hepburn Emerson A. Poison Blildonan G. Tidsbury High Bluff James FuUerton Cook's Creek F. B. Robinson Rock Wood A. Nelson Stonewall W. Hill Woodlands N. McLeod Victoria H. Hodgson Springfield J. S. P. Carsley Ridgeville W. Alymer St. Leon Joseph Dodds Sunnyside John Hourie St. Anne P. Ferguson Gladstone C. Empson Whynne D. Gillespie Plympton W. Grierson Meadow Lea .... G. V. Fitzgerald Bigville from 2 to 4 feet about 1 foot. from 18 inches to 2 feet „ 18 inches to 2 feet. „ 12 to 18 inches. „ 3 to 4 feet. „ 18 to 24 inches. , 2 to 3 feet. „ 3 to 4 feet „ 3 to 4 feet. „ 4 to 5 feet „ 6 to 15 inches. ., 6 to 36 inches. „ 24 to 30 inches, about 3 feet, from 12 to 24 inches. „ 10 to 36 inches, about 20 inches, from 8 to 24 inches. „ 12 to 36 inches. „ 12 to 18 inches, about 18 inches. „ 4 feet, from 12 to 36 inches, about 18 inches, from 18 to 24 inches. „ 24 to 36 inches. „ 3 to 4 feet. about 18 inches. „ 4 feet, from 12 to 18 inches, about 18 inches. CHAPTER XIII. Gerenh, Root Crops, Seed Time and Harvest, Roads, doc. Barley — Us great Weight in the North — Bay of Quiute Bark'y — Additional 100,000,- 000 Acres Suited to Barley North of the Wheat Bel t — Uses of Barley in the West — Testimony Regarding its Culture in Manitoba — Average Yield for Four Years — Com- pared with the United States — Enormous Yield of Oats — Testimony of Residents is Manitoba — Average sixty Bushels per Acre — Nearly Three Times Greater than Ohio — 100 Bushels per Acre often Raised — Potatoes a sure Crop to the Arctic Circle — Kotteu ones Unknown — Chipweyans as Potato Cultivators — Remarkable size of Potatoes at Hay Lakes — Late Growth of Potatoes — Feeding Stock an Easy Matter — Pumpkins, Melons, and Cucumbers in the North — Melons Grow and Ripen North of St. Petersburg, or 1,200 Miles Northwest of Winnipeg and 900 Miles North of the Boundarj' — Extent and Capacity of the Country Beyond the Range of Average Com- prehension — Testimony of Residents Regarding the Productive Powers of the Soil — Timothy an Excellent Crop — Good Fall Pasture — Wild Hops — Clover — Flax — Hemp — Why all Crops Succeed so Well — Southern Russia a Parallel Case — Commencement of Spring — Setting iu of Winter — Seed-time in the North- West — Varies in Certain liccalities — Harvest Time — Earliest in the Qu'Appelle Valley — Always Free from Frost — Qu'Appelle Valley Compared with Saskatchewan — Time for Taking up Roots — ^Testimony Regarding Seed Time and Harvest — Roads of the West merely Cart Trails — No real Roads other than Railways in the Country — Description of Leading Trails — How Trails are Formed — Where they Lead to — No Attempts made to Improve them — Travellers Tell of their Own Incapacity — Experienced men Never get "Stuck" — How to Cross a "slew" with Loaded Carts — Trails or Roads of Ten Years Since — -How they were Formed — Indian Trails — Roads of the Future. Barley as a crop cannot be over-estimated when speaking or writing regarding the North-West. Doubts may be cast on the successful cultivation of wheat in many parts, but regarding barley there can be no question, as it ripens fifteen days earlier and resists fall frosts better. It is a northern grtiin and reaches its highest developement in the Mr North-West. Barley grown on Peace River weighs 58 lbs. to the bushel, and is so plump that it delights the eye of an Englishman when he sees it. Samples brought by myself from numerous points on the above river, were weighed in Winnipeg by the Inspector of Inland Revenue, and pronounced by him the finest in every sense he had ever examined. OEOPS, HARVESTS, AKD ROADS 217 It is well known to residents in Ontario that Bay of Quinte barley fetches a higher price in the United States than that raised south of the lakes. This ia not so much owing to soil as to climate. The great heat of the south causes it to ripen before maturity, and consequently the grain is shrivelled. In the north although the days are hot the nights are cool and ripening is a slower process. If 150,000,000 acres be given as the approximate number of acres suited to wheat culture, another 100,000,000 acres could be added if the raising of barley be taken into account. On the shores of Hudson's Bay it has been raised for many years. A round every post south of the Arctic Circle, the Hudson's Bay Go's employes cultivate it. On the Youcon it has been grown for many years within the Arctic Cirple. From every point the same report comes that the grain is in all cases plump and well filled up. As food for hogs ' and horses it cannot be beaten, and practical farmers seem to think it superior to oats for the one, and peas for the other. Within the settlements it is extensively sown, and outside of them it is the principal crop, as it can be used for food by both man and beast. That barley can be grown very successfully in Manitoba, will be shown by the following table. The quality of the grain is excellent, its color fine, and brewers pronounce it second to none for malting purposes. Average Yield for four Years. YIELD PKH AOKE. 1877. 1878. 1879. 1880. 30 35 30 30 42 40 36 35 40 40 40 35 60 66 70 — 40 46 62 40 25 20 25 30 50 50 50 50 42 39 45 45 AT'aee weignt per bushel. John Dilworth. . George Codman . W. Jackson A. Gillispie John Sutherland H. Bellenger. . . . William Moss. . , M. Owens HighBlufiF. tt tt tt tt Greenwood Kildonan Cumberland Hse.lat.54° High Bluff 50 48 48 50 62 56 50 50 218 MANITOBA AND THE GREAT NORTH-WEST. YIELD PER ACRE. 1877. 1879. 1880. 50 40 40 40 40 40 65 — 20 20 20 30 65 50 55 55 40 35 45 35 £i3 47 43 50 3S 38 40 50 50 40 45 50 40 40 4S 40 4S 45 50 60 30 30 30 30 50 50 60 55 40 40 30 40 40 30 50 40 30 30 30 35 35 33 36 30 52 30 20 40 30 32 36 28 40 40 40 45 50 50 40 45 75 40 48 60 50 40 20 30 34 31 20 40 40 36 42 50 30 25 25 25 60 50 25 30 42 39 45 45 40 30 20 30 50 50 60 50 Av'age weight per bushel. John Ferguson... James Airth J. W. Adshead. . J. Armson John Brydons. . . A. J. Moore. A. Macdonald . . . A. P. Stevenson. Max. Wilton. . . . A. J. Hinker F. Ogletree A. V. Beckstead Charles Begg . . . . G. Granby Alex. Poison, Jr. George Tidshury. T. B. Robinson.. Thomas Sigsons.. James Mnnroe... John Fraser Alex. Adams. . .. John Hourie. . . . W. A. Farmer. . , James Whimster, James Stewart. . , J. W. Carleton.. Matthew Owens. Nelson Brown. . . John MoKinnon. High Bluff Stonewall St. Charles High Bluff Portage La Pr.-n'i ' Nelsonville , Gladstone Nelsonville Hi-h Bluff. Green Ridge Portage La Prairie Emerson Stone Fort High Bluff. Kildonan High Bluff. Rockwood Portage La Prairie, Kildonan it Clear Springs St. Anne , Headingly High Bluff. Clear Springs High Bluff Portage La Prairie 50 56 50 48 50 50 50 50 52 57 50 50 50 52 62 50 50 50 50 50 50 52 51 52 50 50 50 48 50 Average yields according to the above, and many other instances for 1877 were 43, 1878, 38, 1879 39 and 1880, 41 bushels per acre. The following statement tells its own tale : — Canadian North-West, say 40 bushels per acre. Minnesota 25 " " •' Iowa 22 " " '• Wisconsin 20 " " " Ohio 19 " " " Indiana 19 " " " Illinois 17 " " " Throughout the North-West Territories barley is a sure crop, and the farther you proceed to the northwest, the plumper the grain and the greater the yield. For malting purposes no finer barley can be found in the world. Oats produce enormously, and are very plump. Their CROPS, HARVESTS. AND ROADS. 219 straw and that of wheat and barley ia wonderfully bright, tall, and stout. A look over a field of growing grain is all that is necessary to tell the practical man that here is a land with untold wealth in its soil, and as the life giving breeze fans his cheek, he feels that here life means an un- ending pleasure. The blood courses through his veins as it did when he was a boy, and he is young again in spirit if not in years. The sensation is irresistible, and all men feel never to be forgotten pleasures as they gaze on the waving fields of grain and prairie grass. It is not too much to say that everything is instinct with life. The following table will show that oats at any rate are very prolific : — Average Yield for four Years. AVEEAQE PER ACEE. 1877. 1S78. 1879. 1880 Aver'ge weight perbsh. John Dilworth.. . W. JackBon. . . . W.Eagles S. C. Higginson. . John Sutherland E. E. Mitchell. . Wm. Mobs. . .. M. Owens John FergviBon. . B.Fisher J. W. Adshead. . Robt. Black JameB AimiBon. . Wm. Corbett. . . J. G. Rent John Brydon . . . A. J. Moore ... . J. G-eddes A. McDonald.. . D. Gillespie .... A. P. Stevenson. . James Stewart . . . Ed. Scott P. Furgiison F. Ogletree T. H. Brown. . G. A. Tucker.... A. V. Becksted , A. J. Nugent. . . . H.B Hall G. Granby Alex. Poison, Jr. , Thomas Sigsons. James Munroe High Bluff. Stonewall. . . . Oakland Kildonan Cook's Creek. High Bluff.. Stonewall St. Charles .... Birds Hill High Bluff Springfield Cook's Creek Portage la Prairie . . Nelsonville Kildonan Gladstone Plympton Nelsonville Cook's Creek Portage la Prairie . . Gladstone Portage la Prairie . . Poplar Point Portage la Prairie . . Emerson West Lynne Headingly High Bluff Kildonan Portage la Prairie . . Kildonan 60 75 40 55 54 30 60 70 75 62J 100 52 80 75 30 75 60 40 40 15 100 37 60 60 75 60 60 75 50 80 65 40 60 90 75 75 35 50 57 35 60 60 70 45 45 85 60 30 80 56 35 40 60 100 37 55 70 60 40 40 100 50 80 70 50 62 75 60 80 35 60 58 50 60 60 65 45 85 60 75 65 55 68 60 40 40 80 80 40 60 90 60 40 50 90 60 80 73 50 52 70 60 40 60 50 60 70 57 65 50 80 65 75 65 40 70 50 40 40 60 75 50 65 75 50 60 60 60 60 100 65 50 65 60 40 35 35 39 38 38 36 42 36 38 33 42 42 38 38 38 36 34 36 40 40 40 35 36 38 34 37 40 34 40 38 38 38 40 220 MANITOBA AND THE GREAT N0RTH-WES1 ADDRESS. ATERAQE PEE ACHE. Aver'ge weight per bsh. 1877. 1878, 1879. 1880. John. Taylor Headingly 25J 95 60 50 40 70 52 65 75 54 50 35 70 80 60 50 85 30 80 80 '!^ 60 60 51 75 75 50 45 40 40 80 80 50 80 25 75 75 65 40 60 50 75 75 50 50 45 60 60 90 50 85 30 80 80 70 40 20 60 75 75 55 40 35 57 50 70 60 80 35 Thomas Dalzell High Bluff 40J J. Davidson . . « 36 Alex. Adams Clear Springs 38 38 36 W. A. Farmer Headingly Hie-h Bluff 40 J. Stewart . , 41 Kobt. Bell Bumside 36 40 M. Ferris . . . Burnside 40 J. W. Carlton 36 TMT, OwPTiR High Bluff 42 u 34 K. P. Bradley St Pie 40 John McKirmon John Winster . . Portage la Prairie High Bluff 38 The average yield for the four years ranges from 58 to 62 bushels per acre. The comparison between the Cana- dian North-West and some of the American States as res- pects the yield of oats is as follows : — Canadian North-West, say average 60 bushels per acre. Minnesota 37 „ Iowa 28 „ Ohio 23 „ The oats grown are very superior in qual.ty, being plump and heavy, averaging in weight about 381bs. to the bushel. The yield per acre is simply enormous, an average of over eight}^ bushels to the acre being no uncommon thing, and in a few exceptional cases even one hundred bushels have been realized. For newly broken ground, I am of opinion that oats will be found the most remunerative crop, and there is alwaj^s a ready home market for all that can be raised. Evidence is at hand to show the enormous crops of pota- toes that are raised. Some specimens have been obtained weighing over five pounds each, and it is no unfrequent occurrence to have 600 bushels to the acre. When it is con- sidered that potatoes range in price from 80 cents to $1.50 per bushel, it is no exaggeration for a Manitoba farmer to say that he could make more with a potato patch in the CROPS, HARVESTS, AND ROADS. 221 North-West than he could with a large farm in Ontario. The average yield of over 100 instances for 1877-80 inclu- sive was 318 bushels to the acre. Potatoes in every part of the country are a sure crop, growing along the shores of Hudson's Bay, and producing a fair average at Fort Good Hope, on the Mackenzie River, north of the Arctic Circle. In my travels up and down the country I never saw a rotten one, and never came on a tract where they would not succeed. In the forest country north of the Saskatchewan, the Chipweyans locate themselves on the banks of the various rivers and lakes, erect houses, put in a small patch of potatoes, carrots, and turnips, and during the latter part of the summer and fall, revel in luxuries, having the finest whitefish for the taking and lovely pota- toes for the gathering. Everywhere it is the same, and whether the soil is clay, loam, or sand, crops beyond descrip- tion are taken off without costing the cultivator one tithe of the labor required in the east. In 1879, while at Hay Lakes, 800 miles west of Winni- peg, I went into a potato field and measured two specimens of two varieties. The white variety measured on an average 17J inches and the purple variety 15| inches, in circumference. Two measurements were taken in each case, and the length was only an inch greater than the breadth. This was on the 26th September and many of the leaves were still green. At Isle La Crosse Lake, in lat. 57° north, I found potatoes still growing on September 22nd, 1875, and I had the pleasure of eating new potatoes in the shadow of the Rocky Mountains, in lat. 56° 12' north, on the 21st of June of the same year. Feeding stock with roots will be an easy matter, as the crops of turnips and carrots are simply amazing. These grow everywhere in the north, and always give large re- turns. Governor Morris told me that he saw fine pumpkins and melons growing at the north end of Lake Winnipeg. & 222 MANITOBA AND THE GREAT NORTH-WEST, I found quantities of ripe cucumbers at Little Red River, grown from English seed, in lat. 58° 30', on the 14th August, 187-5. At Fort Simpson, Mr. Hardisty informed me that they grew melons every year, and had no difficulty with them when started under glass. This Fort is situated at the confluence of the Liard and Mackenzie Rivers, north of Great Slave Lake, and is situated in lat. 62°, or two degrees further north than St. Petersburg. The great extent of country under discussion may be realized when I state that the above locality (Fort Simpson) is over 1200 miles, as the crow flies, northwesterly from Winnipeg, and is due north of the American boundary over 900 miles. It is extremely difficult for one unacquainted with the subject to grasp the extent and capacity of the country. It is practically boundless as far as this generation is concerned, and long after our bones are mouldered into dust there will still be millions of acres untrodden by the foot of the hus- bandman. Pages could l^e written at this point filled with what would seem highly-colored and extravagant adjectives, and yet these would not reach the reality. The potential powers of the soil can be best illustrated by letting the residents speak for themselves : — W. H. J. Swain, of Morris, Has produced 800 to 1000 bushels of turnips to the acre, and sixty bushels of beans have also been raised 1 >y him per acre. S. C. Higginson, of Oakland, Has produced cabbages weighing 17 J, lbs. each. Allan Bell, of Portage la Prairie, Has had cabbages forty-five inches in circumference, and turnips weighing 25 lbs. each. Thomas B. Patterson, Has realized forty tons of turnips to the acre, some of them weighing as much as 20 lbs. each. Robert E. Mitchell, of Cook's Creek, Raised a squash of six weeks growth, measuring five feet six inches around the centre. CROPS, HARVESTS, AND ROADS. 223 William Moss, of High Blufc, Has produced carrots -weighing ] 1 lbs. eacli, and turnips measuring tliirty- six inches in circumference. James Airth, of Stonewall, states that the common weight of tuinii)S is 1 2 lbs. each, and some of them have gone as high as 32J lbs. Isaac Casson, of Green Ridge, Has raised 270 bushels of onions to the aero. John Geddis, of Kildonan, states he has raised 300 bushels of carrots and 800 bushels of turnips per acre. John Kelly, of Morris, Has produced 800 to 1000 bushels of turnips to the acre. Joshua Appleyard, of Stonewall, Also states his crop of turnips to have been 1000 bushels per acre, the com- mon weight being 12 lbs. each. Edward Scott, of Portage la Prairie, Raised 400 bushels of turnips from half an acre of land. W. H. J. Swain, of Morris, Had citrons weighing 18 lbs. each. Francis Ogletree, of Portage la Prairie, Produced onions measuring 4| inches through the centre. A. V. Beckstead, of Emerson, Gives his experience as follows: — Mangle Wurzels weighing 27 lbs. each. Beets 23 lbs., Cabbages 49 lbs., Onions each IJ lbs. in weight. W. B. Hall, of Headingly, Has raised carrots three inches in diameter, beets weighing 20 lbs. each, and gives the weight of his turnips generally at 1 2 lbs. each. Philip McKay, of Portage la Prairie, Took 200 bushels of turnips from one quarter of an acre of land, some of them weighing 25 lbs. each. He has produced carrots four inches in diameter and fourteen inches long, has had cabbages measuring twenty-six inches in diameter, solid head, and four feet with the leaves on. His onions have meas- ured 16 inches in circumference, and cauliflower heads nineteen inches in diameter. James Laurie & Bro., of Morris, Have produced turnips thirty inches in circumference, onions fourteen inches and melons thirty inches. He had one squash which measured about the same size as an ordinary flour barrel. James Owens, of Point du Ch^ne, Had turnips 30 lbs. each, onions fourteen inches around, and cuctunbers eighteen inches long. 224 MANITOBA AND THE GREAT NORTH-WEST. Neil Henderson, of Cook's Creek, Has raised 1000 bushels of turnips to the acre, carrots five inches in diameter and eighteen inches long, while his onions have frequently measured five inches through . James Bedford, of Emerson, Has raised 1000 hushels of turnips to the acre. It must be remembered, that none of the farmers men- tioned above used any special cultivation to produce the results described, and out of nearly 200 reports which we have received from settlers concerning the growth of roots and vegetables in the North-West, not one has been unfa- vorable. Timothy has been grown for many years by farmers in the older settled parts of the country, and all with one accord speak highly of it as a crop. Thomas Dalzell, of High Bluff, has grown timothy for eight years, and says he has had from two to three tons to the acre. It is often seen growing alongside the track on the prairie, and unlike the wild grasses the root leaves are always green. In the fall of 1880 this was notably so between Rat Creek and Portage la Prairie, where cattle were out on the timothy stubble eating the green leaves in the beginning of November. In the latter part of the same month, the preceding year, white clover and timothy were quite green along the roadside east of Portage la Prairie. Red clover must produce enormously, as many species of plants closely related to it grow every- where in the country. "Wild hops are known to produce large quantities, said to be equal if not superior to any seen in cultivation. Flax and hemp were formerly cultivated, and produced large crops. Hemp has been grown twelve feet high. In the future, large areas will be sown with these plants, as their fibre will be utilized for many purposes, and flax seed will be required for making oilcake for fattening stock. The reason why all manner of vegetables succeed in the North-AVest is not far to seek. As has been shown in the CROPS, HAEVESTS, AND KOADS 225 preceding chapter, the soil is the best in the world. The light rainfall prevents the land from becoming sour, and the severe and continued frost pulverizes the soil deeper than any other subsoiling process could possibly do. A rich soil, an unequalled seed-bed, a superior seed time, plenty of rain in the growing season, long sunny days, and clear dewy nights combine to produce crops of all sorts that cannot be equalled. Southern Russia has long been noted for the richness of its soil and its extraordinary crops of wheat. Our North- West is under the same parallels of latitude, is known to be a country of summer rains, and to have every peculiar- ity of the Russian Plain. Russia in past years has been famous for its wheat, shipped from Odessa. Riga is the port from which hides and tallow, hemp, flax, oilcake, lin- seed oil, and many other products have come, and it is not claiming too much to expect that our North-West will supply all these in coming years We have all the natural facilities, but we want men to till the soil. The questions put to people acquainted with the country are — When does spring commence ? When does winter set in ? When do you sow your seed ? What time does harvest commence ? When do you take up your roots ? From Winnipeg to Peace River, points fully 1300 miles apart, spring commences about the same time. Taking one year with another, the first spring flowers make their, ap- pearance about April 15th. Captain Butler found the whole hillside covered with beautiful Anemones {Anemone patens) on April 22nd, in lat 56" north. The same year spring commenced in the neighborhood of Winnipeg at the same date. Red River, in lat. 48°, does not break up earlier than the middle of April, and Peace Rivpr, eight degrees further north, is not later. Winter sets in, as far as the closing of Red River is con- cerned, some time during the first ten days of November. 15 22G MANITOBA AND THE GREAT NORTH-WEST. Peace River closes much later, as it is only at this date that the livst ice is seen in the river. Often very cold weather conies in October, and snow lies on the ground for eight or ten days, but it passes away and usually a beautiful season commences which lasts far into December. At this time the nights are more or less frosty, with clear, calm and most delightful days. The latter part of December aud January are generally very cold, and during this period the ther- mometer falls very low. Seed time in the North-West continues from the first of April to the middle of June, that is from the very earliest time when seeding can take place to the latest period when it is wise to sow At Battleford seeding has been done in March, but this is so exceptional that it should only be noticed. After talking Avith many fiirmers, I found that M;i,y is the general time for all spring work, but that wheat sowed as late as June lOtli generally escapes the frost, and til at barley will produce a crop ten days later. All good farmers say that grain should not be sown later than June first, On Peace Pdver, in lat 50", work commences about April 20th, and after this time potatoes are planted, and grain sown. Still farther north, at Vermilion, there is little gardening until after the first of May. At Fort Chipweyan, on Lake Athabasca, scarcely anything is done until May 10th. About 90 days are required on Peace River to ripen barley, but earl}' sown weed takes less time. Harvest depends altogether on the time of .sowing Early sown gram ripens in fewer daj's than late sown, as it has all the hot weather to juature in. A great and permanent fall of temperature alvyays takes place about the middle of August, and after this grain is slow to ripen. Throughout the whole valley of the Qu'Appelle. spring lime and harvest time are earlier than in Manitoba. This is partly caused hy the -^varmcr soil and drier atmosphere of that region. In 1879 strawberries were in abundance "O-^ CROPS, HARYESTS, AND ROADS. 227 by the middle of June at Fort Ellice. The spring was fully ten days earlier than at Winnipeg. At Qu'Appelle 130 miles west of Port Ellice, Mr. Marcus Smith, C. E., found "barley cut and stored by July 27th" in the same year. Prom time immemorial Indian corn has been grown in the valley, and all kinds of garden vegetables are cultivated by the Missionaries. Mr. Sette the English Church Missionary on the Little Touchwood Hills, says that in that section crops are always cut early and never injured by frost. At Prince Albert, wheat ripened the same year about the mid- dle of August, and at Battleford a few days earlier. Edmon- ton was later, and it seems a settled matter that there are from twelve to twenty days difference in the ripening of grain between the valley of the Qu'Appelle and that of the Saskatchewan. Potatoes are stored by careful people before the 10th October, as after this date there may come a few days of hard frost, and do much injury to them. Beets require to be cared for at the same time, but carrots and turnips can be left till November. Root cellars are easily cons- tructed and there is no difficulty in saving all kinds of roots. Many farmers in the west take up their potatoes in the latter part of September, and experience shows that this is the safest plan. I subjoin a few statements from settlers regarding seed time and harvest. These all refer to Manitoba. John McKinnon, Three Creeks, Portage la Prairie, says : — " The usual time of sowing wheat, oats, and peas is from the beginning- of April to the middle of May, barley from middle of May till the beginning of June. The weather during seeding and harvest is generally dry. The usual time to harvest is from the middle of August till September." John W. Carlton, of Clear Springs, says : — " Land ought to be ploughed in the fall, and sown as early as possible in the spring. Seeding is from 1 tli to 1 5th of April, and harvest from 1 0th of August to 15th Sejjtember. The Mennonites here grow all their tobacco, and it stands about four feet high." 228 MANITOBA AND THE GREAT NORTH-WEST. James Sinclair, of Greenwood, says: — " The month of May is generally fair ; June wet, August and September fair weather. All kinds of roots and vegetables should be sown as early as the ground is in iit condition, and will be fit for gathering about the middle of October." Henry West, of Clear Springs, says : — " I have been in the country six years, and have found the driest summers to give the best crops, even though there was no rain except an odd thunder storm." H. C. Graham, of Stonewall, says : — " Spring weather, at time of seeding, is generally bright, with some warm showers of rain. In harvesting we rarely have rain ; usually clear fine days." Arthur J. Moore, of Nelsonville, says : — " The weather in April and May is usually dry and clear. A good deal of rain in June, is followed by a very dry and fine harvest, which usually commences in the second week in August. Have grown buckwheat success- fully. Have seen good crops of flax amongst the Mermonites. Timothy and clover d® well. Planted twenty apple trees two years ago which are doing well." F. T. Bradley, of Emerson, sa}^s : — "I cultivate wheat, seldom raising other grain. This season (1880) I commenced seeding April icth, SLiison being backward did not finish seeding till 5th of May, and then had eighty acres under crop; Commenced harvest on August 9th, expect an average of thirty bushels to the acre." Thomas Henry Brown, of Poplar Point, says : — " Plough as much land as you can in the fall, and sow as early as the frost is out of the ground, just enough for the harrow to cover the seed. As far as my experience goes the ordinary vegetables, such as turnips, carrots, cabbage, onions, beets, peas, beans, &c., grow well here. I have raised as good vegeta,bles since I have been here, with comparatively but little cultivation, as I have seen raised in my native place. County Kent, England, where market gardening is carried on to perfection." Questions are constantly asked about roads, and most writers speak of the roads in anything but complimentary terms. The truth is there are no roads in the country. What are familiarly called roads are merely the trails used by buffalo hunters and Hudson's Bay Company's employes when traversing the country from point to point. As settlers came into the country they used these trails and began to locate in their vicinity. While the prairie remained un- CROPS, HARVESTS, AND ROADS. 229 inclosed the roads were excellent except at a creek crossing or a low marshy spot, in the language of the country termed a " Slough" or " Slew." The brigades of Red Eiver carts, often one hundred in number, travel in single file, each cart drawn by one horse or ox, and carrying from eight to ten hundred weight. A road, then, originally consisted of two rut-marks on the prairie sod and a path between. As traffic increased these ruts would wear deep into the soil and one or more new ruts would be formed by keeping one wheel in the former track. On the main trail to Battleford and Edmonton twenty such ruts can now be counted running parallel to each other. Within the settlements, road allowances are now more or less inclosed, and by constant travel the prairie sod has been cut completely away, This makes the roads almost impass- able in the wet weather in June and July. Some attempts have been made to improve them by building bridges over the creeks and in some cases making a " turnpike" by dig- ging a ditch on either side of the road and throwing the earth into the centre. This, when levelled, makes a capital road in dry weather, but when rain falls it is simply indescribable. Outside of Manitoba no attempts whatever have been made to either bridge a creek or drain a slough so that each traveller does the best he can. Travellers seem to delight in recording their difficulties and give astounding details of how many times they got "stuck" in a quagmire or floundered through a creek, and relate these incidents with great unction. To an ex- perienced traveller all this is merely a record of their own ignorance and inexperience, for the man who has his wits about him never gets " stuck" in these places but avoids them by not trying to pass one without examination. We, who are accustomed to prairie travelling, laugh at the woe- begone looks of the green horns who get into a " slew" and spend hours getting out again. The proper way to pass one 230 MANITOBA AND THE GREAT NORTH-WEST. of these places, in tlie wet season, is to get to one side of the usual trail and have a man to lead the horse through with his feet on the broken grass and uncut sod and at least one wheel on a new track. Should the first horse break through a little grass thrown into his tracks will carry the next one across. Besides the man leading the horse another should be on each side of the cart ready to assist. Having travelled many thousand miles on the prairie hy compass and passed every obstruction, even rivers nearly half a mile wide without any assistance other than our own ingenuity, I can say that prairie travelling is an exceed- ingly simple matter when a few grains of common sense are included in the process. Ten years ago there were very few trails in the country other than those made by the Indians. The main trail for the west started from Winnipeg and at Portage la Prairie forked. One branch went by the White Mud past West- bourne, Palestine, Gladstone, and Odanah and met the other a few miles east of Salt Lake. The other road, called the South Trail, continued to the west, crossed Rat Creek and McKinnon's, and passed on to the " Big Plain " beyond Pine Creek. Here a branch left the trail and going still farther south crossed tlie Assiniboine at Brandon and passed up the right bank of the river to Fort Ellice. At Brandon a branch went still farther south and lost itself on the Souris Plain. From the " Big Plain" the road continued westward joining the north trail at the above mentioned point. Passing Shoal Lake and Birtle it struck the Assiniboine above the mouth of the Qu'Appelle. Crossing the river it continued on northwesterly to the Touchwood Hills and thence to the South Saskatchewan. Crossing it at Batoche's ferry, the trail passed by Duck Lake to Carlton. Here it again forked, and one branch crossed the north Saskatchewan and con- tinued up to Edmonton. The other passed in the direction of Battleford and on to Edmonton. This southern road was CROPS, HARVESTS, AND ROADS. 231 seldom travelled ten years ago, as fears were entertained of Indian raids. From Edmonton the trail continued 90 miles farther to Fort Assiniboine on the Athabasca River. Fort Ellice was a central point, and trails passed from it to every point. One went up the right bank of the Assiniboine to Fort Pelly, 140 miles to the north. Another passed to the west and threw off a branch when opposite Qu'Appelle, which passed through Qu'Apppelle and north to the Touchwood Hills. The main trail passed westward to Moose Jaw Creek and from thence to the Cypress Hills where it ceased or merged into another which followed the right bank of the South Saskatchewan from Batoche's ferry to the country on the Milk River. From Fort Ellice another led to the southwest, by Moose Mountain to Wood Mountain, and was the usvial route taken by the Half-breeds when going out to hunt the buffalo. Of late years many cross trails have been added to these, but with the exception of the above, and a trail leading south from each of the Hudson's Bay Company's forts on the Saskatchewan to the buffalo plains, scarcely any others existed. These trails were seldom direct. Travellers had to mean- der from side to side according as wood and water could be found. Indian trails on the contrary led from hill top to hill top and anywhere on the buffalo plains a high hill has an Indian trail passing over or near it. Often, when travelling without a trail, we have been able to strike one almost par- allel to our line by studying the topography of the country, and deducing the direction in which they should run. On the prairie west of the Red River Valley, roads such as we have in Ontario will never be needed as the soil is naturally dry and only during the month of June is the rainfall great. In the fall, winter, and spring, all roads are in good order and will remain so when the mud holes are ditched and drained. The future traffic roads are iron ones and all others will be built with local labor as the country roads of Ontario are constructed CHAPTER XIV. Grasses of the Plains, Forests, and Mountains. Pastures of the Prairies — Their Value in Various Sections — Design of the Chapter — List of Grasses, their Habitats — List of Cyperaces, their Habitats — List of Rushes — List of Leguminosse (Pea Family) — Why Certain Grasses have Various Names — Effects of Burning the Grass — "Wild Oat" of Southwestern Manitoba a Bugbear — Sheep Killing by its Awns a Myth — Description of the Grass — How it Injures Man or Beast — Hay made of this Grass — Its Effects on Horses — Really the best Grass on the Plains — Hay Grasses — Manitoba Hay — Practical Remarks on Manitoba Hay — Testi- mony of Residents Regarding the Hay Crop — Sand Hill Grasses — Bunch Grasses — ■ Buffalo Grasses — "Grama-grass" — Grasses of the Alkali Lands — Valuable Grasses — Grasses of the Bow River Country — Spring Food of Horses — Summer Food — Winter Grass of the Prairie — Winter Pasture in the'Forost — Only one Poor Grass' in ISTinety- six — Value of the Pea Family — Artemisia Frigida as a Forage Plant — Eurota lanata — Analyses of Grasses. All the prairie is pasture land, but all is not equally good pasture. The pastures that are exceptionally good this year will be poor the next. The pasture on burnt prairie is good all summer. But this cannot be said of tha which is unburnt. The same species of grass extend through 20° of longitude and sometimes 10° of latitude, and a grass spoken of very highly in one locality may be condemned in another. The pastures of Bow River are highly praised while those farther east with the same specie^ are despised, because public opinion has not been roused in their favor. I purpose in the following list to give all the grasses of the plains, so that Both scientific and practical men may recognize the value of those wonderful pastures, extending for nearly 1,000 miles from east to west. Follow- ing the true grasses I shall give the Cyperaceas or sedges which constitute much of the hay and the greater part of the vegetation of the ponds, and lastly a list of the LeguminosaB, which include the vetches, peas, and all other plants of the order looked upon in all lands as of the most nutritious character. As so little is known GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 233 of the real value of the grasses and other plants of the region I shall collect analyses of a number of the grasses and show their comparative value for feeding purposes. If space permit, either in this chapter or those devoted to stock-raising, I shall more particularly describe a few of the prominent grasses. Table I. List of Orasses. BOTANICAL NAME. Leersia oryzoides. Zizania aquatica. Alopecurus aristulatus . Phleum alpinum. Vilfa cuspidata. Sporobolus lieterolepis. " cryptandrus . " asperifolus. Agrostis scabra. Cinna arundinacea. Muhlenbergia glomerata. " sylvatica. Calamagros tis striata. " lojigifolia. " Canadensis. " Langsdorfifii. " sylvatica. " Porteri. Ericoma cuspidata. Oryzopsis Canadensis. " asperifolia. Stipa spartea. " viridula. " Richardsonii. " comata. Spartina gracilis. " glabra. " cynosuroides. Bouteloua oligostachya. Graphephorum melicoides. " festuoaceum. Koeleria cristata. Eatonia obtusata. " Pennsylvanica. MelicaHallii. Glyceria airoides. " tenuiflora, COMMON NAME. Rice Grass. Wild Rice. Wild Water Foxtail. Wild Timothy. Rush Grass. Brop-seed Grass. Hidden Drop-seed. Rough Leaved Drop-seed. Tickle Grass. Wood Reed Grass. Drop-seed Grass. Sylvan Muhlenbergia. Reed Bent Grass. Blue Joint Grass. Canada Rice Grass. Rough Leaved Rice Grass. " Wild Oat," Buffalo Grass, Feather Grass. Graceful Salt Marsh Grass. Salt Marsh Grass. Fresh Water Cord Grass. Buffalo Grass. Hall's Melic Grass. Narrow Leaved Spear Grass. Meadow Spear Grass. PLACE or GROWTH. Wet places, eastward. Lake of the M'^oods. In wet places near ponds. Cypr. and Porcupine Hills. Damp prairies. Abundant eastward. Sand hills. Rich dry soil. River banks. Cool moist woods. Boggy and rich soil. Eastern Manitoba. Very common, moist ground. Sandy soil. Water pools and forest. Forest marshes. Rocky Mountains. Rocky Mountains. Sand hills, in bunches. Cypress Hills. Northern forest. Very abundant. Very common. Foot Hills, Rocky Mount. Rather scarce. Abundant, salt marshes. Rare, western plains. Manitoba, very common. Southern or dry plains. Cypress Hills. Fresh water pools. Dry hills and river banks. By pools. Moist woods. Brandon and westward. Salt marshes. Salt marshes. 234 MANITOBA AND THE GREAT NOETH-AVEST. BOTANIl'AL NAMK. Glyoeria iiervata. ** aquatica. " fluitans. " distans. " paucifiora. Brizopyi'um spicatum. Catabrosa aquatica. Munroa squarrosa. Poa annua. " pratensis. " tenuifolia. " alpina " serotina. " laxa. " Andina, " ccBsia . " nemoralis. " Eatoni. Festuoa ovina. " Thurberi. " tenella. Bronius ciliatiis. " Kalmii. " brevi-aristatus. Phragmites communis. LopturiLS punieulatus. Triticimi rcpuns, " dasystachyum. " violaceum. " caniniim. " strigosnm. Hordeiim jxibatum. " pratense. Elymus Canadensis. " Sibiricus. " mollis. " condensatns. " striatns. " Tirgiuic-us, " dasy^tachgum. " parviflorum. Dantlionia spicata. '• intermedia. " Californica. " sericea. Aira ca3spitosa, Avena striata. Avena pratensis. CO-MJtON NAME. Water Spear Grass. Common Manna Grass. Spike Grass. Annual Spear Grass. June Grass. Slender leaved Poa. B'oul Meadow, Wavy Meadow Grass. Wood Meadow Grass. Sheep's Fescue. Tliurber's Fescue. Small Fescue Grass, Fringed Brome Grass. Wild Chest, Common Reed Grass. Couch Grass, Soft Wheat Grass, Squirrel Tail Grass. Canadian Lyme Grass. Siberian Lyme Grass. Smooth Lyme Grass. Slender Hairy Lyme. Lyme Grass. Soft Lyme Grass. Wild Oat Grass. Prairie Oat Grass. Californian Oat Grass, Silky Oat Grass. Hassock Grass, Wood Oat Grass. Meadow Oat Grass. PLACE OP GROWTH. Damp pastures and pools. In pools. In standing water. Salt marshes. Northern river bottoms. Salt marshes. In spring rivulets. Red Deer Valley. Near Winnipeg. Very common. Fine pasture grass. Cypress Hills, Abundant in w'et places. Manitoba prairies. Western prairies. Prairies, many forms. Cypreiss Hills. a il Sandy soil, Brandon and westward. Cyioress Plills. Damp prairies and thickets. Thicket and prairie. Cypress Hills. Bogs and Marshes. Dry hillsides. Salt mar.shes. Forest openings Manitoba plain Thickets, river iianks. Cypress Hills Salt marshes. Salt marshes, rare, Plivcr banks and tliickete. Cypress Hills, Lake Winnipegoosis. Southern Plains, Thickets. Moist river liottoms. Mountain Woods. Rich prairies. Forest openings. Rich prairies. Cypress Hills. Bow River. River banks. Thickets, Brandon and wes.v.-ard. GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 235 BOTANICAL NAME. Trisetum Biibspioatum. Hierochloa borealis. Phalaris aruudinacea. Beckmannia erucEeformis. Panicmn virgatum. " xanthophysum. " depauperatmn. " dichotommn. " pauciflormn. Andropogon furcatus. " Bcoparius. COMMON NAME. Seneca G-raes. Reed Canary Grass. Beckmann's Grass. Tall Smooth Panic. Finger Spiked WoodUYaBB, Purple "Wood Grass. PLACE OP GROWTH. Rocky Mountains. Prairies, very common. BogB and marshes. Wet places, northward. Sand Hills. Thickets. Manitoba prairies. I' II South-Western Manitoba. River valleys northward. Rich or sandy slopes. Tahle II. Oyperacece BOTANICAL NAME. Cyperus Bchweinitzii. Eleocharis palustris. '• acicularis. " tennuis. Sciripus cfespitosus " pauciflorus. " maritimus. " pungens. " atrovirens. " validus. " fluviatilis. " microcarpus. Eriophorum alpinum. " vaginatum. " polystachyon. " gracile. Carex adusta. « aperta. " alpina. « aquatilis. " arctata. " arida, « aristata. '■ aurea. « Backii. " canescens. « capillaris. « concinna. " Crawei. " debilis. " cristata. « Deweyana. COMMON NAME. Schweintiz's Gallingall. Common Spike Rush. Hair Club Rush. Slender Club Rush. Scaby stalked Club Rush. Sea Bulrush. Chair Bottom Rush. Bulrush. River Rush. Wood Rush. Cotton Grass. Harestail. Broad leaved Cotton Grass. Narrow leaved Cotton Grass. Alpine Sedge. Water Sedge. Short beaked Wood Sedge. Dry Sedge. Awned Sedge. Golden-fruited Sedge. Back's Sedge. White Ci-.rex. Hair-like Sedge. Crawe's Sedge. Weak Sedge. Crested Sedge. Dewey's Sedge. PLACE OF GROWTH. Sand Hills. Marshes. Soft boggy ground. Shores of lakes. Peat bogs, northward. Shores of lakes. Salt lakes. Lake shores. Stream valleys. Bogs and marshes. Water marshes, north. Streams and creeks Peat bogs, north. II II CI Grass marshes. II .. Thickets. Manitoba. North woods. Borders of marshes. Woods, eastward. Manitoba i^rairie. Common in marshes Boggy ground. Dry thickets. Damp woods, north. II II II Dry woods. Lake shores. Thickets. Prairies. Thickets and prairies. 236 MANITOBA AND THE GREAT NORTH-WEST. BOTAinOAL NAME. Carex disticha. " Douglasii. " ebumea. " feetiva. « filifolia " filiformis. " granulans. " gynocrates: " Houghtouii. " irrigua. " lanuginosa. " laxiflora. " Liddoni. " limosa. « pulla. " livida. " longirostriB. marcida. monile. Meadii. Novse-Angliffi. (Ederi. oligosperma. obtusata. panicea. Pariyana. Pennsylvanica. polytrichoides. prairea. retrorsa. Richardsonii. riparia. scirpoid«a. scoparia. siccata. stellulata. stipata. straminea. stenophylla. sychnocephala. tenella. tenuiflora trispei-ma. teretiuscula. Torreyi. utriculata. COlfHON NAUE. Douglas' Sedge. Bristle-leaved White Sedge. Slender Sedge. Slender-leaved Sedge. Granular Spiked Sedge. Houghton's Sedge. Spring Sedge. Woolly-fruited Sedge. Loose-flowered Sedge. Liddou's Sedge. Mud Sedge. Livid Sedge. Long-beaked Sedge. Mead's Sedge. New England Sedge. CEder's Sedge. Few-fruited Sedge. Parry's Sedge. Pennsylvania Sedge. Bristle Stalked Sedge. Prairie Sedge. Late-fruited Sedge. Richardson's Sedge. Lake Sedge. Brown-spike Sedge. Dry-spiked Sedge. Little Prickley Sedge. Awl-fruited Sedge. Straw-colored Sedge. Two-seeded Sedge. Slender cluster Spike Sedge. Three-seeded Sedge. Lesser-panicled Sedge. Torrey's Sedge. Bladder-fruited Sedge. PLACE OF GEOWTH. Marshy meadows. Dry gravel hills. River banks. Rich damp slopes. Dry gravel prairie. Peat bogs. Manitoba prairie. Boggy prairie. Peat bogs, north. Sandy woods. Peat bogs. Damp prairies. Damp woods. Gravelly ridges. Peat bogs. Bow River Valley. Peat bogs. Thickets. Open prairies. River margins. Damp prairie. Rocky woods. Lake margins. Peat bogs. Dry prairies. Damp prairies. il u Dry thickets. Wet woods. Marshy prairie. Wet woods. Dry thickets. Marshes. Damp prairies Dry prairie. Dry sandy thickets. Wet woods and marshes. Wet woods. Dry prairies. Dry gravel ridges. Alluvial soil. Wet woods. Marshes. Wet prairies. Marshes. GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 237 BOTANICAL NAMK. COMMON NAME. I'LACE or GKOWTH. Carex vaginata. Wet -woods. " varia. Dry ravines. " vulgaris. Nortborn meadows. " vulpinoidea. Fox Sedge. Eastern' prairie. " Willdenovii. Willdenow's Sedge. Lake of tho Woods. » vesicaria. Bow River. « ampuUacea. Ponds in the south. Table III. List of Rushes. BOTANICAL NAME. COMMON NAME. PLACE OF GEOWTH. Lnzula paiviflora. Small-flowered Wood Eush. Rocky Mountains. Juncus alpimis. Alpine Rush. River margins. « Balticus. Baltic Rush. Common on prairie. « bufonius. Toad Rush. Muddy places. " Canadensis. Canadian Rush. Low places. " filiformis. Slender Rush. North woods. " longistylis. Long-styled Rush. Moist ravines. « nodosus. Eound-headed Rush. Marshes and Springs. " tenuis. Slender Rush. Open prairie. « xipMoides. Western prairie. « Vaseyi. Vasey's Rush. Manitoba prairie. Table IV. LeguminosoB. [Pea Family.) BOTANICAL NAME. COMMON NAME. PLACE OP GEOWTH- LnpinuB argenteus. SUvery Lupine Cypress Hills. " Kingii. King's Lupine. Sand Hills. Psoralea argophylla. Silvery Psoralea. Prairies. " esculenta. Cree Potato. Sandy Prairies. « lanceolata. Sand Hills. Petalostomum violaceus. Purple Prairie Glovei Prairies. " candidus. White Prairie Clover, Gravelly Soil. Amorpha canescens. Lead Plant. Manitoba Prairie. " microphylla. Small-leaved Indigo Plant . Assiniboine River, Astragalus caryocarpus. Ground Plum. Prairies. « Canadensis. Woods and thickets. « hypoglottis. Damp prairies. « pectinatus. Dry prairies. « adsurgens. g u it " aboriginum. ^ Gravelly Hills. « triphyllus. g" Dry prairies. " pauciflorus. 1 Cypress Hills. « flexuosus. P Prairies. " frigiduB. Rocky Mountains. « microcystis North Woods. Astragalus bisulcatus Prairies. 238 MANITOBA AND THE GREAT NORTH-WEST. EOTAKICAL NAME. COMMON NAME. PLACE OF OROWTH. Astragalus multiflorus. Prairies. « Drummondii. Dry Prairies. " racemosus. g (( a « Missouriensis. ^ Alkaline soil. " Kentrophyta. ^ Dry sand. Oxytropus campestris. Rich prairies. " Lamberti. a> U il « deflexa. t£ a " splendens. Dry knolls. " podocarpa. Rocky Mountains Glycynhiza lepidota. Wild Liquorice. Rich soil. Hedysarum Mackenzii. Dry slopes. " borealu. Ricli prairie. Vicia Americana. AVild Vetcli. Woods and thickets. Lathyras venosus. Prairie Pea a u " ochroleucus. ti u " palustris. Marsh Vetchling. Wet meadows. " maritimiTS. Beacli Pea. Lake shores. Thermopsis rhombifolia. Wild Bean. Rich prairies. Amphicarpoea monoica. Hog Pea Nut. Thickets. In Table 1 I have enumerated 96 species of true grasses found by myself growing wild in the North-West. These include many species which are of little value as pasture grasses on our prairies, yet in other lands are highly prized. Numerous species which on our prairies become tall enough to be cut for hay, in the drier country south of the boun- dary, seldom attain the height of a few inches. Indians in past time burnt the grass over wide areas every fall, so that the young and tender grass of the burnt dis- tricts might tempt the buffalo to migrate. On the dry southern plain few of the grasses bear seed the year after a fire, as the surface of the ground being bare of any covering to act as a mulch, the Avarm sun begins to change the grass to hay before seed has been formed. Where the rainfall is greater this is not noticed and heavy crops of grass loaded with seed may be seen every year. Hence certain grasses obtain local names. A grass may be cut for hay in one locality, in another it may bear no seed and be merely short pasture. By burning the gj:ass, good pasture for the GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 239 season is assured, but this should always be done in spring after the cattle have roamed over it all winter. Should the grass not be burned the young shoots grow up amongst the old grass, and cattle and horses wander off to where there is less of this mixture. In Southern Manitoba many people speak against Stipa spartea, and call it " Wild Oat." Terrible stories are told of its effects on cattle, sheep, and horses, and even on men, but most of the tales are exaggerations or without one grain of truth. Further to the west, this grass, where the soil is dry and parched, scarcely ever produces more than five or six seeds in a season. Owing to the dryness of the climate it here has a tendency to form tufts, and is called " buffalo grass." This is the famous grass of the hills in the Bow Kiver country, and forms the bulk of the winter pasture of the great plains. I speak from a thorough knowledge of both the grass and its distribution, and do not fear contra- diction. An illustration of the stories told about this grass may be of interest. In conversation with a gentleman last win- ter, he said, that no sheep could live a summer in Southern Manitoba owing to the " wild oat," and in proof he related the following anecdote : Many years ago the Hudson's Bay Company brought up a large number of sheep from St. Cloud, and pastured them on the plains. During the summer the sheep began to die, and an examination being made of two of them, their livers were found filled with the seeds and long awns of this grass. I asked him if any had been found in any other part of the sheep's body, and he said they had not. I asked him if he believed such nonsense and he at once answered, yes. I hinted that witches might have had a hand in the death of the sheep, as it was by filling the livers of their victims with pins and needles, in the good level old times, that they compassed their death. He became indignant and the conversation dropped. Sheep, horses, 240 MANITOBA AND THE GREAT NORTH-WEST. and cattle fatten on these pastures. After a few years prac- tical experience those myths will pass into oblivion. The genus of grasses to which Stipa spartea belongs is represented on our plains by four species. All these species have remarkably awned seeds, and the one in question has one often seven inches long. It is not the awn, however, in this case, which does the mischief. The spikelets are one- flowered, and the seed always falls away at maturity. At the base of the seed is a callus (a hard and extremely sharp point) which will penetrate anything it is pushed against. This point is much smaller than the seed, and is no part of it. All travellers on the plains in July are tormented with these seeds penetrating their moccasins, or entering their socks, or forming a fringe around their ankles, and even the callus getting into their shirts, but no ill efiects other than the above are ever noticed. In the seven years I have travelled the plains, I never knew a horse to be injured by this grass, nor did I ever see a horse which did not prefer it to every other. Colonel Irvine, Commissioner of the North-West Mounted Police, told me when at Fort Walsh in 1880, that this grass, cut m a green state and dried for hay, was rather dangerous. While in charge of Wood Mountain a quantity of it had been cut for hay, and the horses got the seeds fast- ened in their mouths, so that after eating it their mouths had to be examined. After a time the horses began to eat it without injury to their mouths, and no other injurious results were observed. This is the only grass against which an outcry has been raised, but in reality it is the one most highly spoken of, and deservedly so. It is the most plentiful and widely distribu- ted grass on the plains, and is always found on soil which is comparatively dry. Owing to its preference for dry soils it is seldom tall enough for hay, and as its seeds ripen early and fall away amongst the grass, the ill effects if any arising from it will be short lived. GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 241 The grasses naturally fall into groups as regarjds their habitats, some preferring one place and some another. Those of the thickets, forest glades or prairies, stream valleys, coulees or ravines are hay grasses. Mixing with these in the vicinity of wood, are wild peas and vetches, and various species of Rosacese and Compositge that make excellent hay. Approaching the marshy spots or growing in the water in June and July, are various Carices and other sedges, and amongst these in great quantities Juncus Balticus. It will be seen that hay varies with the locality, and while one farmer may have a coarse poor hay his next neighbor may have a superior article. In that part of Mani- toba northwest from Portage la Prairie the hay is very coarse, containing large quantities of Fresh Water Cord-Grass, mixed with Blue Joint and Foul Meadow. A western horse accustomed to a finer quality of hay will scarcely touch this, while the ponies of the neighborhood eat it with avidity. On the drier prairie this kind of hay is not seen, and all other varieties are abundant. Where there are many ponds much of the hay will be composed of various sedges and certain Poas and Calamagrostis. If the soil be rich and not too moist, the Carices disappear, and besides the above grasses species of Danthonia, Bromus, Triticum, Elymus, Hierochloa and Vilfa, with numerous Rosacese and Legumi- nosse appear in great profusion. Should the hay be cut in a river valley it is almost wholly composed of Garex aristata Foul Meadow, and Blue Joint. This is the hay of the mixed forest and prairie country. Men accustomed to see the finer kinds of cultivated hay would be apt to say that this coarse stuff could have very little fattening power, but I reply by stating that owing to the extraordinary richness of the soil all grasses are nutritive, but all are not alike pala- table. Manitoba horses fatten on their hay. A horse brought from west of Fort Ellice would hardly live upon it. The one has been accustomed to a superior article as regards taste, 16 242 MANITOBA AND THE GREAT NOKTH-WEST. the other kno^s no difference. When I speak of Manitoba in this connection I mean that part which lies east of Pembina Mountain. A late writer speaking of western or Manitoba hay makes the following practical remarks : " The first point a farmer would note about them is the abundance of the foliage of nearly all the species, while the grasses of Eastern Canada are nearly all culm or stem, having most of them only one, two, or three leaves ; most of the North-Western grasses have ten or twenty leaves. Of course this is an extremely valuable feature in grass, as the leaves are more easily di- gested than the culms. " The calms are esceediiigly fine in the prairie grass, and this again would strike a farmer as indicating a good quality of grass, add to this that there are in some species such an abundance of seeds as to make the fodder partake of the na- ture of a feed of grain, and it will be seen that the tales about the readiness with which stock will fatten on prairie hay are not overdrawn." The testimony of residents regarding the hay crop in the older settlements will be of interest, as these men speak from actual experience. The assertion that the native hay is superior to that made from cultivated species, should be taken as a doubtful one. It is not on account of the species, but on account of soil and climate, that the hay is so good. Why every fruit and succulent stem should be so sweet, I cannot say, but that they are so I know by experience. To the causes which produce this result we must ascribe the fat tening powers of the hay, and not to the species themselves. Testimony of Settlers regarding Grasses and Hay. Only t. a few are given. NAME. POST OFPICB. EEMAEKS. B. Hartley. St Charles Hay plentiful almost equal to Timothy. J. W. Adshead " I have hay in any quantity. GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 243 NAME POST OFFICE. REUABE8 Jas Sturton Nelsonville I have 20 acres which will yield 20 tons. A. J. Moore " I have plenty of good hay. Fifty hun- dred weight to the acre. Geo Tidsberry . . , High Bluff. Hay is plentiful. Very best quality. Eoht Adams. " There is plenty of hay on my farm. Eev. Thomas Cook Westboume There is any amount of good hay. Jno. Smith " I have abundance of hay of differen kinds. Jas. FuUerton Cook's Creek Best quality of ravine hay. W. E. Mitchell " Large quantities of hay Quality good. Jas Airth Stonewall I have thousands of tons of the best hay. A. McDonald " I have plenty of good hay. T. H. Brown Poplar Point There is abundance of hay. Quality good. A. C. Harvey Poplar Point Therels abundance of hay. Quality good. W. B. Hall Headingly I can get any quantity f good hay. W. A. Farmer " There is more wild hay than we need. Jas. MathewBon Emerson There is plenty of the best of hay. Louis Dinsing " Hay is plentiful, and very good. Wm. A. Mann Bird's Hill Have more hay than I can cut. E. Black " I have hay of the best quality. Wm. Corbett ... Springfield Hay is in abundance. Quality good. S. J. Parsons " Hay is in abundance. Quality good. Eobt. Bell; Bumside We can get good hay close to us. Another group prefers the sand hills and dry arid soils. These are highly spoken of in the United States, and con- stitute most of their pasture grasses. Group of Sandhill Orasses. Sporobolus cryptandrus. Calamagrostis longifolia. Festuca ovina. Panicum virgatnm. Andropogon scoparins. Koeleria cristata. These are the inhabitants of the sands, though other species may be frequently seen in company with them. Ericoma cuspidata is a most lovely grass, growing in bunches on almost pure sand, and down in Arizona is considered a valuable pasture grass. The greater number of these grow in bunches and are hence called " bunch grass," but this is true of all species which grow on dry ground or Avhere the rainfall is light, except they have running root stocks. Fes- 244 MANITOBA AND THE GREAT NORTH-WEST. tuca, Andropogon, and Koeleria are all valuable grasses, and owing to their great production of leaves make excellent and continuous pasture. It is the " Buffalo Grasses," however, that attract the attention of most people, and of these we may say a few words. The true Buffalo Grass is unknown on our prairies, but is common in Kansas and Colorado. Its name is BucJiloe dactyloides. In habit it is quite different from any species we have, as it throws out runners, like those of the straw- berry, which take root and so form new plants. Our buffalo grasses are two in number. One of which {Bouteloua oligos- tacliya) I call the southern buffalo grass. The other {Stipa spartea) is the northern one Of the latter I have spoken at some length, and shall now call attention to its distri- bution. This species is co-extensive with the prairies in the North-West and is most abundant on the " Buffalo Plains," the old winter haunts of the buffalo. The former is our representative of the "Grama grasses'^ of the United States. These constitute the bulk of the pas- tures in the southwestern states. The latter is represented by numerous species of the same genus farther to the south^ and are all considered excellent pasture grasses. It is note- worthy that within the limits of these two species the buffalo has had its home from time immemorial, and on our central plains the latter has its greatest development, and here in former times millions of buffalo found food in the winte Another valuable group which gives us many species, suited, both for pasture and hay, is found aiound salt ponds and in alkaline flats. Of this group the more prominent species are : — Spartina gracilis. „ glabra. Glyceria airoides. „ distans. ,, tenuiflora. GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 245 Biizopymm spicatum. Triticum repens (many forms). Hordeum jubatum. „ pratense. Poa tenuifolia. The most valuable of these are Poa, Triticum, and Spar- dna. These four grasses are valuable, and are greedily eaten by both horses and oxen wherever found. In my opinion no pastures are more valuable in summer than those of the salt marshes. Every summer when travelling on the plains our horses, when let out of harness, make straight for the salt marsh, if there is one in the neighborhood. At Morleyville in the Bow River country I noticed that wher- ever there was a patch of salt marsh plants these were cropped to the ground and tall grasses left standing. Many condemn the salt marshes as being sterile, but to my own knowledge they are preferred both by horses and cows to the pastures of the uplands. Almost all maritime countries have extensive marshes along their coasts, reclaimed from the sea, which are accounted valuable both for hay and pasture. In fact they are noted for their value. In our North-West we have narrow tracts which contain much saline or alkaline matter, and these are condemned as worthless by the same individuals who praise the others. In early spring horses eat indiscriminately on the prairie. As the grasses harden they begin to show a preference and now repair to the salt marsh or the pond. Here they find Triticum repens (Quick or Quack grass), which is an invalu- able grass on all clay and alkaline soils. Should the camp be pitched where this grass is abundant the horses begin to gain flesh at once, and three days will set them up. When this grass is old or not to be had horses repair to the round depressions in the prairie, where water stands nearly all summer, and crop the succulent tops of Garex aristata which produces very little seed, but abundance of stems and leaves. This species is preferred until the first severe frost, when 246 MANITOBA AND THE GREAT NORTH-WEST. they abandon the marsh and take to the hill top. Their food now is the Buffalo grass, which during the month of August had passed from grass into well cured hay, with still a little green grass amongst it. As hay it is equally as good as grass, and having produced next to no seed, the whole of the nutriment is laid up in the leaves. It is not true of our Buffalo grass that the seed is among the leaves as it is in Kansas. Owing to the annual fires, it matures little seed but a profusion of leaves, which contain all the nutriment of seeds. It is this ripening of the leaves by the great heat of August, and the light rainfall afterwards which does not rot the leaves, that cause our prairie pastures to be so fattening in winter. The winter pastures of the forest are quite different. In early summer and even often as late as July the ponds in the forest and the alluvial valleys of rivers are covered with water, which prevents rapid growth. The principal vege- tation of these ponds and flats are Carices, Poas, and Blue Joint. These all produce many leaves, but scarcely any seed, and are quite green when tlie fi'ost comes. This kills their upper leaves, but does not injure what is below, and in a few of these ponds or marshes a band of horses will find food for the whole winter. Should thu snow be ever so deep the ponies will paw it away and get all the food they need but if a crust should come and not a pea vine or vetch to be had, they would necessarily succumb. A thaw in the North. West, that does not clear the ground of snow, is more to be dreaded than a temperature of 50° below zero. In the enumeration of species at the beginning of this chapter I gave ninety -six as growing wild on the plains and in the woods. Of this number forty-four sjoecies are made into hay, and only one accounted injurious — Brizopyrum gpicatum The Cyperaceae number eighty-five species, and of these not one is accounted injurious, though many are of little use for either pasture or hay. Still, of these I know GRASSES OF THE PLAINS, FORESTS, AND MOUNTAINS. 247 that forty -six species are either cut for hay or eaten as green pasture. All writers speak of the pea pine and vetch, and know the value of clover and the Leguminosae generally, but few are prepared to hear that in Ontario we have only twenty-six species of this order, while in the North-West we have forty-two. So numerous are some species in indi- viduals that they completely obscure the ground and prevent any other species from competing with them. Another fodder plant, " Pasture Sage," of Nevada {Arte- misia frigida), is worthy of mention. In many of the states, notably in Nevada and Utah, this species is almost wholly the winter pasture. After passing on to the treeless plains of the south this species becomes quite common, and in many localities is fully one-third of the vegetation. Not being recognized by our people as a forage plant, I mention it so that attention may be drawn to it as the best of winter pasture. It is this species that grows in such quantities at Ashcroft and other places in British Columbia, and always takes the place of bunch grass when the latter is destroyed by cattle. In general appearance it is extremely like wormwood, and I am sure that much of its value depends on the bitter principle it contains in common with all the Artemisias. Another plant well worthy of mention is the White Sage {Eurota lanata), which is found abundantly on the tops of the dry hills on the southern plain. Dr. Rothrock in the botany of the 100th meridian says of this plant : — " White Sage is widely diffused throughout the Western territories, and held m high respect as a winter forage ; stock feeding on it actually gaining flesh when living on this plant, so unpromising in its appearance It is noteworthy that most animals do not eat it from choice." I give the analysis of a few of the native western grasses taken from the Report of the United States Commissioner of Agriculture, in 1879. By placing the well known Timothy :^48 .MANITOBA AND THE GREAT NORTH-ATEST. (Phleum j)f' -2 . Duc/s.) 4. Vulpes fulvus var. fulvus. (Eed Fox.) 6. II '! " decussatue. (Cross Fox.) 6. ■ '■ " argenteus. (Silver and Black Fox.) 7. " macrourus, Baird. (Prairie Fox.) 8. " velox, And. and Bach. (Kit Fox.) 9. " lagopus, Eich. (Arctic Fox.) 10. Canis lupus, L. (White and Gray Wolf.) 11. « latrans. Say. (Coyote or Prairie Wolf.) Family III Mustelidm.<^, Sr/. >>l>izcl(/tay>/.-iJ''Trt/f/f/if'i/.s, Swain. " •'tianocephaLv-% Cah. <^hii}irulax pt/rp'/rt'as, Lickt. I 'nrvns car7iivoru:i, Bert. ,, .imfricanus., Atid. Pinir.orvtis Columhianus, B<>n. Pica Hud.'innica. Covets. t'l/a 7111 r }/.•,- cr/.ttalfi.Sj .'^wain.s pp.Tt^ormiH ' ''//;«r/e;i.sv'K Bnn. It is not ueceSBary to enter into details regiirding the species singly, but a few remarks on the various groups may be interesting to not a few. The Thrushes are represented by seven species^ whict BIRDS OF THE NORTH-WEST. 357 have their homes either in the thick forest or in the thick- ets bordering on the prairie. The Catbird, Robin, and Hermit Thrush are very common and are found everywhere. The Shore Lark and Lapland Longspur are very common on the prairies in September and October, and are frequently taken for Snow Buntings. While passing along the trail the traveller will see these birds running before him in the ruts, and when he approaches too near they rise up and fly some distance ahead, keeping this up for miles. Of the seventeen warblers none belong exclusively to the prairie All are birds of the thickets, and being very shy are not often seen except by the collector, who follows them to their haunts and occasionally gets a glimpse of their bright colors as they retire to the thickest coverts on his approach. When going up or down a river the Bank and Cliff Swallows are often seen in myriads circling around. The former, where the bank xs alluvium often perforates it to the depth of two or three feet, while the latter will cover the hard face of a clay cliff with thousands of nests, and as you glide past, from every nest one or more heads are pro- truded to gaze on the passing stranger. The Red Eyed Vireo fills the forest with its song, and were it not carefully watched would be taken for a variety of birds, as it has quite a variety of notes in its song. The Pinches as usual are well represented both by forest and prairie species. Many of these birds are very beautiful, especially the Evening and Rose-breasted Grosbeaks. These birds live in the thick forests, and the song of the latter is often heard answering that of the Baltimore Oriole, which breeds m the same localities. On the plains near Old Wives Lakes the White Winged Blackbird and the Missouri Skylark are common, and will at once attract the attention. The former by its uncommon plumage, and the latter by its peculiar flight which might be correctly termed luidulating . 358 MANITOBA AND THE GREAT NORTH-WEST. Of all the birds on the prairie none will attract more attention than the Cow-birds. As they build no nests they are great travellers, often keeping with a train of carts crossing the trackless plains for weeks together. Both in 1879 and 1880, while travelling without a trail, these birds have kept with us for weeks. When on the march they would fly alongside the carts and light in the grass, and immediatel}^ pounce on any grasshopper which lit near them. In July when Bull-dogs (^Qad-flies) were troublesome these birds would sit on the horses' backs and pick them off. Often one would take up its position on the horse's rump and catch every fly that dared approach. At night they would some- times sit in the grass, on the carts, or even perch on the horses, if no bushes were in the vicinity. No birds to-day, are such nuisances in the North-West as the various species of Blackbirds. These birds, in many parts of Manitoba, are a heavy tax at present on farmers, but as settlements increase, their power to injure will de- crease, as they w ill have more fields to attack and possibly be fewer in number. Meadow Larks and Bob-o-Links are very beautiful birds, and are found on almost everj^ part of the prairie. The Magpie is very common to the west of the Touchwood Hills, but seems never to come east of the As- siniboine River, at Fort Ellice. The Whiskey Jack or Canada Jay is the first to greet the lonely traveller, when he stops for the night in any part of the forest, and in the morning, it salutes him with the first streak of dawn, and bids him good-bye Avhen he leaves. The Cow-bird, the Whiskey •Tack, and the Indian are all alike sociable, and wherever the white man stops, there these congregate — for food. The next sub-order is the Clannitores, or Flycatchers. They are represented by one Family, five Genera, and eight Species enumerated below : — Kingbird, Ti/raiinii^s Carolmenj^ia, TcTm. Arkansas Fly-catcher. " verlicahis, Say. Say's Fly-catclier, Saiioriiiis Suyus, Buird. Phebe Bird, " fiisciix, linird. BIRDS OF THE NORTH-WEST 359 Olive-eided Fly-catcher, Conoiopus borealis, JSaird. "Western Wood Pewee, " Richardsoni, Baird. Traill's Fly-catcher, Empidonax TraiUii, Baird. Least Fly-catcher, " minimus, Baird. The Kingbird is common throughout the territory, and well deserves his name of "tyrant," as he guards carefully his own domain, and chases away every bird that would in- jure either his mate or her young. On and around the Cypress Hills, the Arkansas Fly-catcher is quite common^ but seems to extend no farther north. The Least Fly- catcher is very abundant in the damp northern forest, and often in a tall tree is indistinguishable from the Red-Eyed Vireo, which, however, is a much larger bird. Order II. Picurin'. This order has few representatives in the North-West, but they are interesting though few. In our limits, it is represented by six Families, eleven Genersi, and fourteen Species, as follows : — Whip-poor-Will, Antrosiomiis vocifervs, Bon. Night Hawk, Chonleiles Viryinianiis, Bon Chimney Swift, Chalvrapelagicu, Baird Humming Bird, Trochilus eoluhrin, L. Kingfisher, Ceryle Aicyoii, Bon. Black-billed Cuckoo, Coccygim erythrojihthalmus, Bon. Pileated Woodpecker Hylotoimis pikatus, Baird. Hairy Woodpecker, Pjc ws villosus, L Downy Woodpecker, „ .jnibescens, L Three-toed Woodpecker, Picoides arcticus, Gray. Banded Three-toed Woodpecker, „ Amfricamis, Breh. Yellow-hilled Woodpecker, Sphyrapicus varius, Baird. Brown-headed Woodpecker, " thyroideus, Baird. High-holder, Colaptes auraius, Swains. All of these are birds of the thicket or forest, though they may be seen on the prairie when in pursuit of food. I have noticed the Humming bird as far north as lat. 59°, in the vicinity of Lake Athabasca. Sir John Richardson places its northern limit in lat. 57° All the Wood-peckers, as their name indicates, live in the woods. None were observed in the south, except the Hairy Wood-pecker and High-holdtr, which were met with on the Cypress Hills. 360 MANITOIiA AND THE GREAT NORTH-WEST. Order III. Raptores. Numerous species of this order have their homes on the plains or m the forests, and live on mice, moles, frogs, and birds. It is principally represented by the two Familes the Strigidoe or Owls, and the Falconidce or Hawks. Of the three Families, we have eighteen Genera and twenty-four Species which are as below : — Great Horned Owl, Arctic Owl, Screech Owl, Long-eared Owl, Short-eared Ow], Great Grey Owl, Great While or Snowy Owl, Hawk Owl, Richardson's Owl, Marsh Harrier, Sharp-iihinned Hawk, Gos Hawk, Peregrine Falcon, Pigeon Hawk, American Merlin. Sparrow Hawk, Red-tailed Hawk, Swainfion's Buzzard, Kough-legffed Hawk. C.ilifomian Squirrel Hawk, Fish Hawk Osprev, (Jolden Eaglf. Bald EaglK. Turkey Buzzard. Bubo Virginianus, Bon " arcticus, Swains Scops asio, Bon. Otus Wilsonianus, Les>i Brachyolus palustris, Gould. Symium cmereum^ Aud Nyciea Scandiaca, Newi Sumia ulula, Bon Nyctale Richardsoni, Bon Circus Hudsonius, Vieill AccipUer fiucus, Oray Astur atricapillus, JarJ Falco anatum, Bon " columbarius, L '' Ricliardsoni, Ridtj " sparverius, L. Buteo boTealis, Gond. " Swain.soni, Bon. Archibuteo Sancti-Johanms, Gond " ferrugiTieus, Ch-ay Pand.ion haMcctus, Cab Aquila chryssetus, L Halicetus leucocephalus, Sav. CatJiaries aura. Jll The only Owl observed on the plains is the Marsh Owl, which has been noticed to make many short flights by day. All the other Owls are found in the thickets or forests bor- dering the great plains. Four species of the smaller falcons are found m the river bottoms throughout the jirairie. Owing to the different color of the plumage at various ages, i\iey are hard to distinguish, except by comparing a large number of skins. These hawks are all very beautiful, but the Sparrow Hawk in full or adult plumage is the most beautiful BIRDS (IF TJIE NORTll-WKST 361 No hawk is more abundant than the Marsh Harrier, which is conptantly on the move, gliding over the marshes or the prairie, looking for mice or small birds. Swainson's Hawks are generally seen follownig each otluT, in quick succession along the top of the high bluffs Avliich shut in a river val- ley. Or, at another time, they ni&y be seen sitting on the \evy edge of a " cut bank," gazing down into the valley, or perched on the top of a knoll, watching the train as it moves past Eagles are seldom seen away from the moun- tains or the rocky shores of the interior lakes. It is seldom that the Turkey Buzzard is seen, except in the spring, when it comes to finish what the Raven has left of the winter's dead Order IV. (Johvmhidce. This order is represented by only one species, the Wild Pigeon {Ectopistes migratoria) of Swains. Few pigeons are seen on the plains, but m the latter part of August and the first half of September, they are abundant in the northern river valleys, feeding on the berries of the Wild Cornel {Corniis stolonifera). Order Y. Oaliinoe. The Gallinaceous birds, though few in number as regards species, are of great value on account of their size. All being winter residents, they furnish many a meal to the starving Indian or other wanderer, when other game is not to be had. In the following enumeration I include all the species of Ptarmigan, although some of them live most of the time very far north : — Spruce Partridg •, Telrao Canadensis, J, Franklin's Grousi " Franklini, Doiii/I Blue or Dusky Grouse, " obscurus, Say Black-tailed Grouse, " Ricluirdsoni, Couex Sage Cock Centrocerciis urophasianui, Ln Sharp-tailed Grouse, T'ediceceles phasianellus, Kll Prairie Hen. Cupidonia cupido, Baird. ■*' Partridge " Jionana vmbelhiK, Sleph <3jey-;-uffed Gn.use, " umbelloides, Dougl. 362 MANITOBA AND THE GREAT NORTH--WEST. White Tailed Ptarmigan, Lagopus leucurus, Swaint. White Ptarmigan, " albtis, Aud. Book Grouse, '• rupestris, Leack. Of the above twelve species all belong to the forest, ex- cept three : Sage Cock, Prairie Hen, and Sharp-tailed Grouse or " Prairie Chicken." The two first are only found along a part of the southern boundary, so that the Prairie Chicken is really the only Gallinaceous bird found on the prairie In the woods and thickets we have the Partridge or Ruffed Grouse, and the Spruce Partridge. These birds are very numerous m the poplar woods to the north of Fort Pelly. During the past season, while they were feeding on the black currants which abounded in the low woods, I shot large numbers of them, and supplied ourselves with fresh pro- visions when our stock was running low. All the other species, except the last two, which have their home to the north, are natives of the rocky mountains. The Black- tailed Grouse is a fine large bird, and frequents the timber on the higher slopes of the mountains. Order VI. Grallatores, or Waders. This order is represented by three sub-orders, and numer- ous species. For the sake of brevity, I shall give the species of the three in succession, and only introduce those in this and the succeeding orders which, at some time of the year, are found on the great prairie or the forests along its border : — /. Sub-Order. Limicolce [VieilV) Black-billed Plover, Squatarola Helvetica, Vieill. Golden Plover, Charadriiis marmoratus, Wag Kill-deer Plover, Aegialiiis vocifera, Bon Semipalmated Plover, " semipalmatus, Cab Piping Plover, " Tnelodia, Coues. American Avocet, Recurmrostra Americana, Om. Wilson's Phalarope, Sieganopsus Wilsoni, Couei Northern Phalarope, Lobipes hyperboreus, Cuv. American Snipe, Gallinago Wilsoni, Bon. Red-breasted Snipe, Macrorhumpkus griseus, I/each. Stilt Sandpiper, Micropalama himaniopus, Bd. BIRDS OF THE NORTH-WEST. 363 Semipalmated Sandpiper, Ijeaet Sandpiper, Baird's Sandpiper, Jack Snipe, White-mmped Sandpiper, Sanderling, Great Marbled Godwit, Black-tailed Godwit, Semipalmated Tattler, Greater Yellow Shanks, Lesser Yellow Shanks, Solitary Tattler, Spotted Sandpiper, Prairie Plover, Long-billed Curlew, Hudsonian Curlew, Esquimaux Curlew, Ereunetes pmillus, Cass. Tringa minulilla, Vieill. " Bairdii. Co-uet. " maculata, Vieill. " fuscicollis, Vieill. Calidris arenaria, III. LiTnosafedoa, Ord. " Hudsonica, Swains. Tolanus aemipalmatus, T. " melanoleucus, Vieill. '' flavipes, Vieill. " solitarius, And Tnngoides maculariua, Gray. Actiturus Bartramius, Bon. Numenms longirostris, Wils. " Hudsonicus, Lath. " borealis, Lath. Great Blue Heron, Green Heron, Bittern, //. Sub-Order. Herodiones. Ardea herodias, L. " virescens, L. Botaurus minor, Bote. III. Sub-Order. Alectorides. White or Whooping Crane, Sandhill or Brown Crane, Virginia Rail, Carolina Rail, Coot Mud Hen, Grus Americana, Tern. Grus Canadensis, Tern. Rallus Virginianus, L. Porzana Carolina, Cab. Fulica Americana, 0ms. The Plover first come to our notice. Late or early in September, the Golden Plover descend to the plains, and here they may be seen in large flocks, feeding on the open prairie or along the borders of a marsh. Killdeer and Semipalmated Plover breed in the country, and can be shot at any time. On the borders of brackish ponds or wading in the shallow water, the beautiful Avocet and Great Marbled Godwit may be found all summer. Around every pond and on every saline marsh are various species of Sand- piper and Snipe. As the month of August draws to a close, these appear in countless numbers and fill the air with their various calls, and a sportsman, if no better game were near, 'Would consider himself in paradise. 364 MANITOBA AND THE GREAT NORTH-WEST. Bitterns are very common in the grass marshes at all seasons. The Great Blue Heron frequents river margins, and often surprises the belated voyager when seen standing on the upper limbs of a dead tree, peering down at him as he silently glides underneath. Cranes are seldom seen in flocks, except in September, when they congregate prior to their southern flight. They are always the first to migrate, and long lines of them will be seen high up moving south- ward in the latter part of September. Order VII. Lamellirostres . Trumpeter Swan, Whistling Swan, Snow Goose Wavy, Canada Goose, Mallard or Stock Duck, Pintail Duck, Gadwell. Grey Duck, American Widgeon, Green Winged Teal. Blue Winged Teal, Cinnamon Te^al, Shoveller. Spoon Bill, Wood Duck, Blue Bill, Broad Bill, Little Black Head, Eing Necked Duck, Ked Head, Canvass-back Duck. Golden Eye, Barrow's Golden Eye, Buffle-head, Spirit Duck, American Scoter, Euddy Duck, Merganser, Sheldrake, Ked Breasted Merganser, Hooded Merganser. Cygnus buccinator, Hick. " Americanus, Sharp Anser hyperboreus, F'all. Branta Canadensis,' Gray. Anas boschas, L. Dafila acuta, L. Ckaulelasmus streperus, Gray. Mereca Americana, Steph. Querquedula Carolinensis, St. " discors, Steph. " cyanoptera, Cass Spatula clypeata, Boie. Aix sponsa, Boie. Fuligula marila, Steph. '■ affinis, Eyton. '' coUaris, Bon. '• ferina, Bon. " vallisneria. Step. Bucephala clangula, Coues, " Islandica, Baird. " aZbeola, Baird. Anas nigra, Wilson. Erismatura rubida, Bon. Mergus Merganser, L " serrator, L. " cucullatus, L. In the foregoing list, I have included no species which I have not seen in the North-West, and have no doubt but that many of the " Sea Ducks," not enumerated here, will be shot by others. Both the Swans and the Wavy breed in the north, and are only seen in the migrations. The BIRDS OF THE NORTH-WEST. SSo- Canada Goose still breeds around the larger lakes, and on islands in them. So late as June, 1879, I have seen the Canada Goose and a flock of young ones on the Assiniboine where the town of Brandon now stands, and at present they still breed on the river, above Port Ellice. Of all the prairie ducks none is more plentiful than the Mallard. This species is always found in the grass marshes, and during the month of September, their loud " quack- quack" is heard continually rising from them. It is true sport to obtain them, as they always lie close amongst the grass and have to be taken on the wing. I have never noticed the Black Duck in any part of the North-West, nor do I know that others have. Teal are in great numbers, and these with the Spoon-bill make up the greater part of the ducks, south of the Touchwood Hills, prior to the migra- tions. It is scarcely credible the myriads of ducks that fill every pond and marsh in September and October, and no description could give an adequate picture of the astonishing sight. On the margin of a pond, the Tattlers are running backwards and forwards, making all manner of discordant noises. Killdeer Plover, Ring-necked Plover, and eight or ten species of Sandpipers are just as busy. Red-breasted Snipe are in hundreds, and very busy thrusting their long bills into the mud. Outside the line of waders are the Spoonbills and Teal, and still farther out, the Widgeon and Butter Ball, but we want none of these — they are too small and not worth shooting for food. Behind a tuft of sedges, we hear the " Quack " of the Mallard, and we still lie close though sorely tempted. Sailing majestically from behind the sedge, comes a fine drake, followed by three ducks. They are in line, and a good shot will fetch them all. Aim- ing ^at their heads, the gun is fired, and with loud cries all the life of the pond rises with a roar like thunder, and darkens the air with their numbers. Four ducks, each larger than a very fine tame duck, are struggling in the 36G MANITOBA AND THE GREAT NORTH-WEST. pond, they are picked up, and a supper for six is soon in the little camp behind the ridge. The Mergansers, or, as we call them, " Saw-bills," are river ducks, and often during the month of August, will keep before a boat for days, as it passes up or dowu a river. They are beautiful ducks Ijut poor food, except men are on short allowance, when they are considered valuable. By their aid, I was enabled, lust summer, to accomplish my work when food grew scarce, and it was only when full supplies of food were ol)tained that we discovered they were _ii-^litj. Order Vni. Steganopodes . White Felicaii, Pelecanvs irachyrhynchus. Lulh. Itouljle-crested Cormorant, Gracuhis dilophux. Oray. Pelicans are numerous on Long Lake, Old Wives Lakes, ■and Gull Lake, north of Cypress Hills. These are their breeding places on the plains. They are very abundant, as well as the Cormorants on Lake Winnipegoosis, and doubt- less many of the large northern lakes. On many of the rivers are Pelican Rapids, because here, they sit on the boulders, watching for the fish which are ascending the rapids. In 1875, when ascending Beaver River, we came to the Pelican Rapids on that river. Numerous Pelicans were sitting on the large boulders in mid stream, and all but one flew at our approach. At first, I was amused at the contortions this one was making, but it was only when the bow Indian seized a pole, and the others put all their energy in the paddle, that I realized that the bird could not rise. When we were almost within striking distance he made a greater effort than before, heaved his load of fish into the river, and sailed away. We only remembered the guns when the shooting was out of our power. Lying be- side me, as I write, is a Pelican's pouch, sixteen inches long and nine inches deep, so it can easily be seen that they have space for a considerable load. BIRDS OF THE NORTH-WEST. 367 Order IX. Longipennes. Herring Gull, Ring-billed Gull, American Mew Gull, Franklin's Rosy Gull, Bonaparte's Gull, Forster's Tern, Common Tern, Black Tern, White-Winged Black Tern, Larus argentatus, Bniiin. " Delawarensis, Ord. " brachyrhynchus, Rich. " FranhUniy Rich. " Philadelphia, Gray. Sterna Forsteri, Null. *' JTirundo, Auct. Ilydroclielidon lariformis, Cuues. " nigra, Gray. All the gulls and terns, except the last one, are abundant on Lakes Manitoba and Winnipegoosis. On the lakes of the prauie, Franklin's Gull, Bonaparte's Gull, and the Ring-billed Gull are quite common. As they vary much in immature states, an amateur may be led to believe he has many species when he has only three. The Black Tern is very common in all marshy tracts on the prairie, and seems more like a large species of Swallow than a Tern. On a small lake, at the head of Swan River, a few of the White-Winged Black Tern were observed, and one was shot This is an extremely rare bird. Forster's and the Common Tern are very plentiful on the larger lakes in the forest country, and enliven many a sand bar and group of bare rocks heaped up by ice in the shallow of a northern lake. Order X. Pygopodes. Colymbus torquatus, Briinn. " sepientrionalis, L. Podiceps occidetitalisj Coues. " cristatus, Lath. " rubricoUis, Bon. " comutus, Lath. " auritus, Nutt. Podilynibus podiceps, Lawr. Great Northern Diver, Loon, Red Throated Diver, Western Grebe, Crested Grebe, Red-necked Grebe, Homed Grebe, American Eared Grebe, Dab-Chick, The two latter aie quite common on the deep pools which are found on some parts of the prairie, and occasionally a loon may be seen in the larger bodies of water. On Water Hen River and Lake, the Western and Red-necked Grebe breed in great numbers. Their nests are built on the old 368 MANITOBA AND THE GREAT NORTH-WEST. Hedges, and rise and fall with the water. Here, the In- dians collect large numbers of eggs in the proper season, and one old fellow, last season, astonished me by the remark that he cmild have fresh eggs all summer. On enquiry, I learned that he went regularly' to the same nests, and never took all the eggs, so that- he kept the poor bird laying all summer. The various species of Grebe, the Coot, and Bittern are all called W;iter Hens hy Indians, but more especially the ^a'st mentioiied . The Western Grebe is a very beautiful and graceful bird. Its length averages nearly thirty inches, including the bill which is very narrow and sharp-pointed. Underneath it is a pure glussj^ white, from the base of the hill to its other extremitj'. The upper part of tlie head and neck are .sooty black, back and wing coverts greyish-black becoming lighter nn the lower part of the back. This bird seems to ho altogether miknowii in tlie interior, and yet it has brud in tliousands, at Water Hen River, from time im- memorial, l^p to the present, it has oidv \>vn known From the Pacific Coast. I place the whol<.' scries of birds in tlie ff)llowing table, merely giviua', ]i()we\-ei'. the Orders. Families. Genera. arianiiida5 1 I 1 IT -^ Friiiffillidai IrturidiH Coi-vida^. ... Tymiiiiiida' ■_'l) 1 .,., 10 8 BIRDS OF THE NORTH-WEST. 369 ORDER. FAMILY. SENERA. SPECIES. Ficariae Cypselidag 1 2 1 1 1 5 8 9 1 1 6 3 1 2 11 2 1 3 14 1 1 3 1 2 1 Caprimuligidas .... 2 Trochilidie 1 Alcedinid^e 1 1 Picidse 8 Raptores it StrigidsB 9 FaloonidsB 14 11 Cathartidse 1 ColumbEe Columbidffi Tetraonidae 1 12 Grallatores.. Charadriidae 5 II 1 li Phalaropodidas 2 I Scolopacidae 20 u ArdeidsB 3 a u Eallidas 3 TiATTipl HrnstrfiR Anatidse "6 1 u Phalacrocoracidaa ] CoIymbidEe 2 H 6 OEDEES. PassereE Picariae Recapitulation. FAMILIES. 1 17 1 6 1 3 1 1 1 1 1 7 1 1 1 2 1 1 1 2 GENEHA 65 11 18 1 6 23 U 2 3 3 SI >ECIES- 103 14 24 Columbae GallinEe Giallatores Steganopodes LongipenneB Pygopodes 1 12 36 26 2 9 8 10 41 146 235 I have been careful to introduce no species into the fore- going catalogue of which I had not seen specimens east of the Rocky Mountains and west of Winnipeg. "When a better knowledge is obtained of the country a few species will be added, so that we may say the Avi-fauna of the territory, leaving out the Arctic birds, is about 250 species. The few notes appended will be read with interest by many parties settling in the country, as they were written on the ground. 24 370 MANITOBA AND THE GREAT NORTH-WEST. While encamped at Grand Valley (now Brandon) on the Assiniboine, numerous birds, common in Ontario, were ob- served, such as Meadow Larks, Robins, Blackbirds, Cow Birds, Bob-o-links, Bitterns, and numerous finches, which were breeding either on the prairie or in the bush along the river. On the prairie the Kill Deer Plover was noticed, and on the drier upland the " Prairie Plover" or Bartram's Tatt- ler was occasionally seen. Farther west these birds were quite common, the latter on the prairie and the former along the lakes or ponds throughout the country. One evening in July we pitched our camp close to the nest of a Kill Deer Plover, at this time one little bird being hatched out and the other emerging from the shell. In our presence she assisted the chick out of the shell, and as soon as both were able to stand she coaxed them away from the nest, and before dark had them safely hidden away in the sedges bordering the pond from which we obtained our water. On the sand hills at Flat Creek two fine specimens of the Long Billed Curlew were obtained. One or two others were shot near the Cypress Hills, but it was a very rare bird and seldom seen. In the marshes east of Moose Mountain both the Sand Hill Crane and the White Crane were breeding, together with the Phalaropes. These beautiful and interest- ing birds were quite numerous near Moose Mountain. The Shoveller or Spoonbill Duck, the American Widgeon, the Green Winged Teal, the Blue Winged Teal, and the Mal- lard were breeding in or near the marshes, and their eggs were occasionally obtained. Skimming over these eastern marshes, and occasionally darting down to the surface, was the beautiful Black Tern. On the great plain west of Moose Mountain few birds were met with, but on the eastern side flocks of the Yellow Headed Blackbirds were seen around ponds, and on the western part near Moose Jaw Creek, the rare and interest- ing White Winged Blackbird was met with. The common- BIRDS OF THE NORTH-WEST. 371 est bird on this prairie was the Chestnut Collared Bunting, although never recognized after this. In the vicinity of the Coteau we reached a few salt water ponds, and here obtained numerous specimens of the beauti- ful Avocet, which were very plentiful around all the salt lakes on the western plains, and so fearless that we had no difficulty in shooting all the specimens we desired. On the same pools were the Marbled Godwit and the Willet or Stone Snipe, both large and beautiful birds. Numerous sand- pipers and many of the smaller snipe were abundant, and during the months of August and September could have been shot by the hundred as they waded or swam in the various pools or lakes we passed. After the middle of August we began to shoot ducks, and besides the species mentioned above, the Gadwell or Grey Duck and Red-breasted Merganser bred in numbers on the plains. Coots or Mud IJens and Pied Billed Grebe were in great numbers, and afforded fine sport, as we had to wade almost up to our neck to obtain our specimens, as they were very difficult to kill owing to their diving power. After the middle of September the sea ducks began to arrive, and it is no figure of speech to say that the ponds and lakelets were alive with them. For the following six weeks feathered game of every kind were so abundant that any person in a week could have shot enough ducks and geese to have lasted a family all winter. The abundance of water fowl in the interior is of such importance at this time when Indians are being fed by the Government, that they should be compelled to lay in a stock of food for themselves during the winter. To see hunters perishing of hunger, or living on supplies furnished by the Government, and at the same time surrounded by millions of birds is, a paradox ; but these men carry rifles, and bird shooting to them is a small business after buffalo hunting. Within a day's journey of the Cree Reserve on the north side of the Cypress Hills, is i>iZ MANITOBA AND THE GREAT NORTH-WEST. a large lake named by me Gull Lake, which during the last da}'s of August was literallj' alive with birds, and when one siiot was enough to supply six of us with a dinner, yet these Indians were largely depending on the Government rations at this time, and Colonel McDonald could scarcely persuade some young men to go and kill a few ducks by liberal offers of powder and shot. At the Assinilwine Reserve it was just the same, plenty of birds in the neighborhood but scarce!}' any attempt made to shoot them, as the men pre- ferred Government rations to independence. Rifles to-day are of little value to the plain Indians, and they should be equired to exchange these for shot guns at an early da}'. Geese, ducks, and prairie chickens are taking to the stubble fields in the fall, so that no difficulty will be found by in- coming settlers to lay up a supply of fat fowl for the winter. About forty species of game birds were either shot or seen on the prairie, and it is vciy proljabie that many species A\'e-re not observed as we were far east of the main migrating lines. All birds shot were fat, and soup made from the various species of snipe and plover was considered a great dainty. Tlie value of the bird crop after the railroad is built will be enormous, but the destruction of eggs in the spring by Indians must cense . None but those who reside in the interior or have been there in the autumn can realiz'' the number of birds living there or passing through at thar, season. Hawks were numei'ous, and various species were shot both on the prairie and in the ri\'er valleys. The sparrow hawk was always found in tlie vicinity of wood, and frequented all the stream valleys throu<;h()ut the country Along the prairie and over ponds and marshes tlie Marsh Harrier was constantly gliding, and frequently paid the death penalty for his inquisltiveness. Many fine specimens of Swainsou's Hawk were shot, and it was only liy obtaining the skins that we were able to decide on tiie species, owing to the BIRDS OF THE NORTH-WEST. 373 daxk color of the plumage. This hawk delighted to sail close along the top of the cliffs bordering a stream, and pick up any living thing observed. Occasional specimens of the Rough Legged Hawk were obtained, but it was very wary, and always soared at a great height. Other species were in more or less abundance, and one young specimen of the Bald Headed Eagle was obtained where it was evidently catching snakes at the margin of a lake. Owls were not common on the prairie, and only one species the Short Eared or Marsh Owl, was seen with any degree of frequency. Along the margin of the woods the Greater Horned Owl and the Lesser Horned Owl were occasionally noticed but were apparently rare. Of the Gull family many fine specimens were obtained at some of the larger lakes. On the 28th August five species were shot on Gull Lake, a large sheet of water north of the Cypress Hills. Franklin's Rosy Gull was secured in fine plumage, and many of the others in various states and different ages, so that in twenty specimens one would be led to believe there were at least ten species. CHATTER XXII. Notes on Reptiles, Fishes, and Iiisects. List of RcptilcK — Snaki's in Hpriug and Autumn — Gathering of Snakes at Livingstone — SnakoK in BuUrusli Lake — Fisliing for Hiredons — Rattlesnakes — Lizardfc Toads and FrogR — List of Fishes — Tlie Perclies — The " Dore " — Carp Family — The\> .jlreat Numbers — Not Considered Good Food — Dried for Dogs and Bait — The Pike or Jaick Fish — Its Habits — The Cat Fish — Salmon Family — Arctic Salmon — Mountain Trout — Arctic Trout — Anecdotes — Bow River Trout — White Fish — Their gre^t Value — White Fish in the Pi-airie Region — In the Forest Region — West of the Mountains — The little White Fish or HeiTing — Th(^ Gold-eye — Fishing for Gold-eyes in the -Rivers of the Prairie — Western Pickerel — Its Value — The Loclie or Biu-bot — The Sturgeon — Fish Supply of the Saskatchewan Valley and Prairie Country — Qu'Appclle and Long Lake Fisheries — Notes on Insects — Butterflies of the Prairie — Myriads in June — Absence of Moths — Coleoptera or Beetles — Grasshoppers and their Allies — Grasshopper Plague — Its Causes and Prevention — Conclusion. Reptiles are far from numerous in the North- West, yet wonderful stories are told of the immense numbers of Garter Snakes {Eutcenia slrtalis) in some localities. At Stony Mountain, sixteen miles from Winnipeg, they are seen in myriads in early spring and in September. During these periods they lie in the sun and coil into terrible look- ing objects, but are perfectly harmless. Last autumn they were gathering for their winter sleep when T was at Livingstone (Swan River Barracks), and as they were said to be numerous I went to see them. All accounts I had ever read fell far short of the reality. They were congregated in and around three basin shaped hol- lows, which were partly filled with very large boulders, ;ind bordered by a few clumps of bushes. The grass for rods around was filled with them, and the stones completely covered. As we approached, a hiss that caused a shudder to pass through me, greeted us from all sides. A few hurried steps and Inspector Griesbach, of the Mounted Police and I, stood on the great boulder, in the centre NOTES ON REPTILES, FISHES, AND INSECTS. 375 of the hollow, from which the snakes slid as we took pos- session. As soon as my excited nerves allowed me to look intelligently around, I saw a sight never to be forgotten. Coiled on every bush and forming cables from the size of a hawser up to writhing masses three feet in diameter, were snakes from one to five feet in length. Around the hollow, but more particularly on the sunny side, they lay in great heaps, so closely packed together that nothing but heads could be seen. It was terrible to look upon the glittering eyes that were fixed upon us by thou- sands, and see the forked tongues thrust out and withdrawn as the perpetual hiss unceasingly fell upon our ears. After a few minutes we became more accustomed to each other's society, and now instead of being disgusted with the writh- ing masses, we saw beauty in every fold. The rays of the western sun falling on their bodies at every angle, caused a mingling of color that none but a master pen could depict. At Bullrush Lake, on the prairie west of Old Wives Lakes, during the month of July, Bald Headed Eagles and Eough Legged Hawks were feasting on snakes. The snakes were catching their food in the lake. I cut one open and discovered the remains of an animal like a lizard. Having abundance of fishing lines with us, we set some lines baited with pork, and next morning hauled out a strange looking animal. Having seen the Menobranchus {Necturus lateralis) of the Great Lakes, I took this animal to be a species of Siredon, possibly Siredon lichenodes, which has been ob- tained south of the boundary. The specimen looked very much like an overgrown lizard, but the prominent gills showed it to be a denizen of the water. It is extremely probable that many, if not all the Lizard Lakes in the North-West, get their names from this animal. Between the Forks of the Bow and Red Deer Rivers, a species of rattle snake is said to find a home, but I have never seen it. 376 MANITOBA AND THE GREAT NORTH-WEST. I have heard many stories about the number of lizards ill certain localities, but must confess to a disbelief in the number. While passing through the Touchwood Hills witlt Half-breeds, I have always heard of multitudes of lizards, but never saw one. During the many summers I have spent on the. prairies. I have observed not more than half a dozen, and these were very small, seldom attaining a length. of six inches. Archbishop Tache, in his work on the North- West, speaking of lizards, says : — ■' Our lizards are of two species— one, rather larger thaji. the other, is marked with green ; the other is altogether grey. These animals are very harmless, and are chiefly found in the centre of the prairie region. They are most numerous in the small lakes, and in the neighborhood of the Touchwood Hills. Their only unpleasant points ai'e their appearance, and desire to approach travellers. Wheii camping, at certain seasons of the year, it is necessary to surround one's tent with a small ditch, of which the inner side is cut vertically, as these lizards climb up only gentle slopes. Unless this precaution is taken, they come into the tents in every direction ; and there are many who would dislike to be either awake, or asleep, on a bed covered with lizards." Toads and frogs a)-e aljundant, (^specially the latter. it is probable that there are at least half a dozen species of small frogs on the southern prairies. Man\- of them are very beautiful, and their bright colors were much ad- mired as we marched across the monotonous plains of the south. A large frog was seldom seen, except in the woods or along the rivers of the plains. The only troublesome animal met with is the leach, which infests all running streams and most of the lakes. They are of two species, — one from three to four inches, the other quite small. While wading around in the ponds, collecting aquatic plants, my legs havc^ often been covered NOTES ON REPTILES, FISHES, AND INSECTS. 377 with the smaller species, but these were easily taken oflF by scraping with a knife. Last season, when ascending Red Deer River, the men were much troubled with the larger species, which infested the mud and other debris found in the river bed. Usually, the men wore old shoes, without socks, and the leeches would get into the shoes, and then attach themselves to the ankles or feet. Often they crawled between the toes, and caused great incon- venience, as it was extremely difficult to get them off. When taken off, the blood would flow freely for some time, but no ill effects followed. In the enumeration of the fishes, I shall be as accurate as possible, where no authorities on the subject are attainable, Richardson's work being so rare, that it is practically beyond my reach. The value of the fishes of the northern rivers and lakes is so little known to the world, that some of the statements regarding their numbers may be looked upoa with suspicion. CATAL©GUE OF WESTERN FISHES. Order. Teleocephali. (The Typical Fishes.) I. Sub-Order. Acanthopteri. (The Spiny-rayed Fishes.) family I. Percidse. {Tlie Perches.) \ . Perca Americana, Schrank. (Common Yellow Perch.) 2. Stizostethium vitreum, Jorden & Copeland. (Wall-eyed Pike. Dory Pickerel.) Family II. Centrarchidse. {The Sun Fishes.) :;. Eupomotis, Gill & .Jordon, (Common Sun Fish.) Family III. Sciamidie. (The Maigres.) 4. Haploidonotue grannlens, Eaf. (Bubblers. Drum. White Perch.) Family IV. C'ottidie. (The Scidpins.) 5. Cottus cognatus, Rich. (Northern Sculpin.) //. Sub-Order. Anacanthini. {The Jugular Fishes.) Family V. Oadidse. (The Cod Fishes.) 6. Lota maculosus, Less. (Methy Burbot.) 7. " compressa, Less. (Ling or Eel-Pout.) 378 MANITOBA AND THE GREAT NORTH-WEST. ///. Sub-Order. Hemibranchi. {The Half-Gilled Fishes.) Family VI. Gasierosteidsc. (The Sticklebacks.) 8. Gasterosteus concinnus, Rich. (The Stickleback.) IV. Siib-Order. Haplovii. (The Toothed Minnoios.) Family VII. Escoidcc. {The Pikes.) 9. Esox nobilior, Thomp. (Muskalhinge. ) 10. " lucius, Linn. (Pike or Jack-Fish.) F. Sub-Order. Isospondyli. {The Trout-like Fishes.) Family VIII. Salmonidsc. (The Trout.) 1 1 . Halmo salar, L. (Great Sea Salmon.) 12. " quinnat, Rich. (The Columbia River Salmon.) 13. " Scouleri, Rich. (The Ekewan or British Columbia Salmon.) 14. ■' Rossii, Rich. (Roes'b Arctic Salmon.) 15. " Hearnii, Rich. (Coppermine River Salmon.) 16. •' namaycush, Block. (Great Lake Trout. ) 1 7. siscowet, Agassiz. (Lake Superior Trout.) 18. Mackenzii, Rich. (The Inconnu.) in. Lewisi, Grd. (Large Rocky Mountain Tmul.) 30. " tsuppitch, Rich. (Western Salmon Trout.) 'il. " Gairdneri, Rich. (Columbia River Trout.; 22. Clarkii, Rich. (Clark's Western Trout.) 23. ' fontinalis, Mitchell. (Common Brook TroiiL; 24. " etellatus, Grd. (Reeky Mountain Brook Tniut.) 3.5. " Hoodii, Rich. (Hood's Northern Trout.) 26. Thymallus signifer. Rich. (Bach's Grayling.) 37. " thymalloides. Rich. (Lesser Grayling.) 28. Coregonus albus, Le Seur. (White Pish.) 39. " Couesii, Milner. (Chief Mountain White Fish.) 30. " quadrilateralis, Rich. (Round Fish.) .^1. " lucidus, Rich. (Bear Lake White Fish.) 32. " artedi, Le Seur. (Lake Herring.) Family IX. Hyodontidx. (The M'hiii Ey<.) :;:; Hyodon chrysopsis, Rich. (Golden Eye.) 3-1. " tergisus, Le Seur. (Silver Bas.s. Mijon Eye > (T. Sab-Order. Eventognathi. {The Carp-like Fishe-s.) Family X. Cyprinidse. (The Minnows.) 35. Lii.xiliis cornutus, Jordon. (Common Shiner.) 36. Xui nmis biguttatus, Kirt. (Horned Chub.) Family XI. Catoslomidse. (The Suckers.) 37. Catostorms longirostrum, Le Seur. (Red Sucking Carp.) 38. " Forstcrianus, Agas. (Grey Sucking Carp.) 19. ' Sueurii, Rich. (Le Scur's Carp.) NOTES ON REPTILES, FISHES, AND INSECTS. 379 Order. Neinatognathi. ( The Sheat FisJies. ) Family XII. SiluridK. 4e. Sllurus borealis, Rich. (Large Cat-Fish.) Order. Ghondrostel. {The Cartilaginous Ganoids.) Family XIII. Acipenseridse. ( The Sturgeons.) il. Aiipenser rubicuuduB, Le yuer. (Lake Sturgeon.) 42. " Rupertianiis, Rich. (Western Sturgeon.) In the preceding catalogue I have enumerated only those species which I have been able to identify from the writings of various travellers and my own observations. The com- mon Yellow Perch seems to be abundant in all the large lakes, but is seldom caught, as few fish with a hook and line, and the nets in use have too large meshes. I obtained this fish last summer in Lake Winnipegoosis, Swan Lake, and in small lakes at the head of Red Deer River. The Pickerel stands next to the white fish as food and is much valued by the Indians who live on Lakes Winnipeg, Manitoba, and Winnipegoosis. During the sum- mer the White Fish seems to retire into deep water, and at this season the Pickerel is taken in great numbers, either with the hook and line or by means of short nets set on the shallows or bars in the lakes. Last summer while exploring these lakes and Red Deer River, we scarcely ever failed to catch all the fish we wanted by setting our net on a shoal in the lake or across an eddy in the river. The Ling or Burbot is common in all the lakes on both sides of the mountains, but is seldom if ever used for food. Sir John Richardson refers to this fish in the following words : — " The Methy Lake and Portage are named from the Cree designation of the Burbot {Lota maculosa— La loche of the Canadians), which abounds in these waters, and often supplies a poor and watery food to voyageurs whose provisions are exhausted. Though the fish is less prized than any other in the country, its roe is one of the best, and with a small addition of flour, makes a palatable and very 380 MANITOBA AND THE GREAT NORTH-WEST. nourishing bread." Another writer says of it : — " Gorged with food or full of roe its naturally short body becomes in- ordinately enlarged ; and its tail, very much like an eel, matches very badly with the thick body. The Methy has scales, but they are so small and so deeply imbedded in gelatinous epidermis that they can barely be distinguished in very many specimens. This fish is a cause of a great annoyance to fishermen in winter ; it fixes itself with fishing lines in the most wonderful way. and entangles them most jierfectly. When taken out of the wn.ter it alternately wrisiales and .straiahtens itself so as to make it a difficult task to unhook. Its smooth and sticky skin is so much colder than that of other inhabitants of the water, that the fisherman who shivers for hours together in the intensest cold on the lakes, is not very happy when he finds a Methy on the line he draws from under the ice. They are gener- ally thrown away to feed crows ; only the roe and liver are retained. At the posts in the interior, the roe is pounded and made into a kind of biscuit, to which whatever name strikes the fancy is given. The liver, which is rich and delicate, is also made into food, unless it becomes necessary to extract the oil for use in lamjjs, by which one can only half see. and which have, besides, anything but an agreeable ,'5mell."' While at Fort McLeod, in the northern part of British Columbia, in November, 1S72, numbers of these fishes were caught in a large wicker basket placed in the stream. In almost every case, they were found with the small western white-fish in their mouth and stomach, the tail only being- visible. It is possible that they gorged themselves when caught in the trap with the others. Carp are taken in great numbers in every part of the North-West, but in all cases, they are looked upon as the next step to actual starvation. Wherever I have been, I have noticed that they are always selected for the dogs, NOTES ON REPTILES, FISHES, AND INSECTS. 381 and never eaten by the Indians or Half-breeds, except in cases of actual hunger. In the fall, these fish are dried by themselves, and kept for bait for Marten traps or for the dogs. Last year, we caught great numbers of the Red Finned Sucker, but after the first attempt at eating them, we always let them go again, as their flesh was far from being pleasant to the taste, after eating Pickerel and Jack- fish. All the streams are filled with them in spring, and some of the smaller brooks are apparently blocked with them. Archbishop Tache, who has travelled so extensively in the west, thus writes of them :— " At the mentioia of Carp, the people of other countries figure to themselves a good and fine fish, but here the impression is quite of another character. When I first came into the country, I talked with gusto, about ' Soupe a la Carpe.' An old man, who had never tasted ' Soupe a la Carpe,' but who considered he had, m his time, eaten rather too much of the fish, could not agree with me, and said significantly : " It is useless to talk about it ; carp is but carp.' I did not at first under- stand the reason for his dislike ; later, I had the opportunity and leisure to appreciate the correctness of his opinion. When one has but one kind of food to eat, when, for ex- ample, it is necessary to be satisfied with carp, — boiled, perhaps, in the water it was born in, without sauce or salt, or addition of any kind, — one quickly tires of the fish, and when this is frequently repeated, the simple name of the animal suffices to excite repulsion. The head of the carp is, beyond comj)arison, preferable to the body ; but many heads would be required to satisfy an appetite excited by work and fatigue, and one soon tires of sucking these small bones. All the species abound in this country, and par- ticularly the Red and Grey Suckers. This fish spawns in the month of June, and, several weeks previous, they are seen and killed m great numbers. When spawning is over. 382 MANITOBA AND THE GREAT NORTH-WEST. particularly in shallows or stony river beds, they assemble in such numbers that their crowded dorsal fins, showing above the water, make it appear as if all the fish were artificially attached to one another, and they can then be killed with a stick. It is easy to understand that, in such circumstances as these, Indians cannot absolutely starve, but they invariably look upon the necessity for feeding on Carp as starvation. The vitality of the Carp is so great, that many true tales about it would be regarded as fabulous. A Carp may be frozen, thawed and then decapitated, and yet not die immediately ; and they are seen to strike with their tails, and jump about for a long time after they have suffered such mutilation as would be apparently most likely to quiet them, and to cause immediate death." Pike or Jack Fish are found in every river and small stream throughout the country, and although not par- ticularly disliked by the Indians and Half-breeds, yet are considered only second rate food. When fresh caught and cooked until they are crisp, they are, in my opinion, excellent food. Last summer, we ate them almost every day, and relished them. No difficulty was experienced in catching them upon a hook baited with a small bit of pork. When in camp, at Fort Calgarry, in 1879, numbers were caught in Bow River by merely throwing the trawl into the river and drawing it out again. For a couple of days, we fed two families of Sarcies by means of one line, yet when we gave the line to them, they could not catch a fish. Small Pike, eight or ten inches long, were noticed in all the small brooks crossed on the plains, and in many marshes they were frequently observed amongst the grass. It is a curious fact that certain fish are caught in nets at one time of the day, and other species are caught at other times, in the same place. During the six days I was in camp on Swan Lake, last summer, I paid particular attention to the fisheries. The Indians and Half-breeds had many NOTES ON REPTILES, PISHES, AND INSECTS. 383' nets set in the lake, which they examined night and morning. The nets were quite short, and set with one end towards the beach and the other towards the lake. Stakes were driven into the gravel, never in more than eight feet of water, and to these the nets were attached. Stones were employed for sinkers, and pieces of spruce for floats. Every evening, large numbers of Pike were found in the nets, but not another fish of any kind. In the morning, Gold Eyes, Carp, and occasionally White-fish were found, but no Pike. Seeing this occur day after day, I was led to watch the habits of the lake fish, and found that Pike, and the various species of Trout were day feeders, and retired to the depths at night, while the other fish came into the shallows at that time. By this, it would appear that carnivorous fish, un- like carnivorous mammals, feed in the day time, while the other and less voracious fish come out at night. If all fed at the same time, in a very few years the largest carnivor- ous species would utterly devour the smaller. During certain seasons, great numbers of Pike are caught in Lake Winnipeg. Many have been taken which weighed over thirty pounds, but the usual weight is between six and ten pounds. They vary much in color, but those obtained in Peace River seemed to be exactly the same species as those drawn from the rivers of the plain. In the northern lakes they are particularly abundant, and from the number of lakes named after this fish, I am quite sure that it is the predom- inant species. The Catfish is found in some abundance in the Saskatch- ewan, below the forks, but is not common in the upper part of the stream. It is quite common in Lake Winnipeg, and the smaller lakes connected with it, but is seldom caught except by lines set at night. It is the Salmon Family, however, that are most highly valued by the natives of the interior. I am well aware that there are species in many of the lakes, which have never 384 MANITOBA AND THE GREAT NORTH-WEST. been described. By casting the eye over any map of the country north of the prairie region, it will be seen that lakes are a very marked feature of the surface. Now, if it be understood that there is scarcely a lake throughout the vast interior, far north of the Arctic Circle, which does not teem with White-fish, a proximate idea may be formed of the vast food resources of the country. I have never seen a lake in tlie forest regif)n that did not teem with magnifi- cent fish, and of .such excellent flavcjr that they are never distasteful to the appetite. In the \'alley of Qu'Appelle, are the four Fi.sliing Lakes. Crooked Lake, and E,ound Lake, making in all a continuous lake over thirty miles Imig and nearly a mile wide, with water in many places over fifty feet deep. Long Lake, forty miles long, and averaging one and a half miles in width, may be said to be part of the same i'i\an\ These seven lakes are filled with White-fish of the very best quality, and are taken, in the latter lake, in great numbers by the Touchwood Indians, every fall. In 1879, I picked up fish skeletons on the shores of Long Lake, that measured seven and three-fourths inches across the eyes, and nine and a half inches from the intersection of the neck to the end of the jaw. At various times, I have seen multitudes caught in Lakes Manitoba, Winnipegoosis, Little Slave Lake, Lake St. Ann's, Lac la Biche, Green Lake, Isle la Crosse Lake, Clear Water Lake, Buffalo Lake, Methy Lake, Lake Athabasca, and many other small lakes. I have seen Methy River so full of White-fish, that we killed them with common poles, and, finally^ I may say I never heard of a lake, in- the forest region, which did not contain them in myriads. Others have spoken of them in connection with their explorations, and these I will quote as confirmatory of my statements. H. J. Cambio. C. E,, when speaking of the fish at Little Slave Lake, says : "We were presented with a supply of White Fish, weighing from three to four pounds each, similar in NOTES ON REPTILES, FISHES, AND INSECTS. 385 CTery respect to those found in the great North American Lakes." At Moberly Lake, in lat. 46°, close to the Rocky Mountains he found the White Fish very abundant in Sep- tember, 1879. They varied from four to six pounds each in weight, were very fat and seemed quite equal to the far- famed White Fish of Lake Huron. Archbishop Tach^, so often quoted, speaking of this fish says : " Without exception, it is incontestably the most pala- table of all our fishes, and is the only one which is tolerable as a sole food. The Attihawmeg is found throughout the country ; the lakes, large and small, are nearly all frequent- ed by them, and they providentially swarm in some of the little lakes, otherwise, without this resource, many parts of the country would be uninhabitable. I am entitled to speak on the subject, for I have lived for whole years on White Fish as a principal food, and frequently the only one. It is not to be understood that living wholly upon one kind of food is not tiring, but this particular fish does not pall, nor does it excite the aversion generally caused by all other kinds. " The White Fish generally weighs only three or four pounds ; but they are occasionally caught weighing as much as fourteen pounds, and in this case their flesh would delight the most experienced judges of this kind of food. Without dressing or sauce of any kind, these fine fish are much superior to any I have tasted elsewhere, even when most artistically cooked. The White Fish spawns in autumn, and this is also the season for great fishing expeditions, although the fish is in its worst condition. The Attihawmeg, caught in autumn, are preserved in a very peculiar but simple man- ner : a frame work is set up, and on its top strong poles are laid three feet apart. Small rods, rather longer than the space intervening between the poles, are next prepared. As the fish are thrown on to the bank, a hole is cut through their tail-ends, and using this, ten are threaded on to each 25 386 MANITOBA AKD THE GREAT NORTH-WEST. rod, thus forming what is called a broche (a sj)it) the ends of which are placed on two of the poles. The fish, now hang- ing head downwards, have their throats cut with a slash of a knife, to free the blood, and to allow water to escape readily. " The sharp nights at the end of October, assist to harden the fish, and to preserve them. When the season is not ex- ceptionally warm, hung fish (a la pente) is excellent. Of course the flavor is injured by prolonged heat, and naturally it is only in autumn that this process can be adopted." Sir John Richardson thus describes the mode of fishing practised by the Northern Indians : " The nets, formed like those used in the herring fishery, measure, before mounting, one hundred and twenty yards in length, but are gathered in to eighty yards by the intro- duction of the backing-line along the upper edge. The depth of the net varies with that of the waters in which it is to be employed, from two to four yards. For the capture of White Fish, of the ordinary size of three or four pounds, the mesh is five and a half inches long, and where these fish are very large it is increased to six. For taking the Bear Lake herring, and the small coregoni of other localities, the meshes vary from two inches to two and three-quarters. In open waters the nets are short, as in the herring fishery; the upper margin being buoyed with cedar or fir floats, and the lower one depressed by stones. The fish hang them- selves in the meshes, being unable, from the form of the gill-plates, to withdraw their heads after having once passed them through. Trout of 15 lbs. weight may be taken in ^ the White Fish nets, and also inconnu {Salmo mackenzii) weighing 20 lbs. ; but the meshes will not admit the heads of the larger trouts (namay-cush), which weigh from 30 to 50 lbs. These are caught with Cod-hooks. " In winter the nets are set under the ice. The first step is to make a series of holes, about fifteen feet apart. A pole NOTES ON REPTILES, FISHES, AND INSECTS. 387 is then introduced, and conducted along the surface of the water from hole to hole, carrying with it a line, which serves to haul in a string of nets, properly buoyed and loaded but seldom exceeding five in number. The rope is then detached, and each end of the net is fastened to a piece of wood, laid across its respective hole, or to a stake driven into the ice. On visiting the nets next day only the extreme holes are opened, the rope is attached anew at one end, and is veered away as the nets are withdrawn by the opposite hole. The fish that have been caught being removed, the nets are drawn back to their places by the line. A line of nets reaches about 400 yards, and the fisherman generally endeavors to carry it entirely across a strait or pass in the lake which fish are known to frequent. " Every second or third day, fishermen who are careful take their nets out of the water to dry and repair them. If this be not attended to, the threads swell and rot and few fish enter the meshes ; the floats also become water-logged if not often dried. In severe weather, the fisherman erects a canvas or skin screen to windward, to shelter him while he overhauls his nets. Esquimo snow barricades are much more effective, but pride will not permit the Orkney or Canadian fisherman to turn the useful expedients of the Esquimaux to account." On the west side of the Rocky Mountains, families of Indians may be found, both in winter and summer, living where a small stream leaves or enters a lake. They use no nets. The stream is staked from both sides towards the centre, sloping with the water. In the centre is placed a wicker basket, which is often of a large size. One that was placed in the river, at Port Macleod, was oblong in form, eight feet long and four feet in diameter. The open end was placed down stream, as the fish were now (November) running up stream. From the rim of the open end, a cone of wicker work extended 388 MANITOBA AND THE GREAT NORTH-WEST. inwards about four feet This cone tapered to an opening about six inches in diameter, and through this the fish passed into the basket. There being no egress, but by the way they came, they remain in the basket. When the basket is lifted into a boat or taken on shore, a lid is opened in the top, and the fish turned out. The proceeds of one day and night were 177 very nice fish, and although none of them were large, the majority were fit for the table. Fresh water Herring were most numerous, then Suckers, three or four Chub, and one Ling or Burbot. Later in the season, the large fish were caught. In summer, Trout were the principal fish ; at this time, they were always running down stream. East of the mountains I have never seen the basket used, but fish wiers are common. Last season, two families of Indians were catching large numbers of Pike and other fish, at the forks of the Red Deer and Etoimomi Rivers, by means of one. They had constructed a dam about three feet high, all the way across the river, except in one spot. Below this opening, they had hammered in sharp- ened stakes and woven willows around them, so that a complete paddock was formed. At pleasure, they could run the water off and take out the fish. After White-fish, Trout are reckoned the best, and, cer- tainly, they are the most sought after. Both east and west of the Rocky Mountains, they are in great numbers, and are easily caught by the fly or a piece of pork on a common hook. In northern British Columbia, they are in multi- tudes in every stream, are fine flavored and quite large. Their flesh is generally salmon-colored and very firm. Within the Rocky Mountains, we caught numbers of a beau- tiful trout, which was called by the Half-breeds, the " Arctic Trout." Its flesh, however, was white and soft, and far inferior to the commoner species. In all the mountain streams, which unite to form the South Saskatchewan, there are multitudes of beautiful trout NOTES ON KEPTILES, FISHES, AND INSECTS. 389 Three species are very common, and easily taken by means of a small piece of pork on a hook. One species is very common in the small brooks, and may be regarded as a large sized brook trout. Another species, rather larger, has soft white flesh, and is not so palatable as the other. In the larger streams, and in the mountain lakes and tarns is a third species, which may be looked upon as the Mountain salmon, on account of its size and flesh, and the sport it gives the angler before its capture. This is the fish for sportsmen, as its size and agility make it a difficult fish to capture, and as it is from five to thirty pounds in weight, it requires more than common ability in the angler to land it. Our mode of catching these, in Bow River, was to wade into the stream and fish for them in the rapids. When one was hooked, it required all our dexterity to land it, and very often, a souse in the water, on account of the slippery stones, was all we received for our arduous labor. On one occasion, one of the men was standing on a log close to the margin of the river, when an enormous fish took the hook, and before he was aware of it, he was sprawling in the water. He had been using the trawling line which we use for pike, and although he was considerably startled by the plunge in the ice cold water, he held on to the line, and three of us shortly after landed a noble fish about twenty- five pounds weight. To the sportsman, and the lover of picturesque and sub- lime scenery, there is no place on the American Continent that holds out inducements equal to those to be found in the Bow River country. Hunting or fishing, as he turns his gaze to the west, he will see towering up to the skies, peak over peak, the everlasting hills. If he watch the clouds forming around the snowy peaks, and dispersing as they float towards the plain, he will see beautifully exemplified the great laws of condensation and evaporation. Should he be an artist, the various bits of color, as the clouds come and 390 MANITOBA AND THE GREAT NORTH-WEST. go, will fill his heart with delight, and he will desire to live under their shadows for ever. And should the mountains become tiresome, he has only to turn to the east, and look over the swelling prairie, until in the distance the grassy mounds melt into the limitless horizon. Still looking east- ward, the hum of the busy multitude 1,000 miles away, will fall upon the ear of the mind, and the dreamer can spend hours, thinking of the time when all the intervening plains will be alive with teeming millions, and the mountain barrier at his back be the gateway to the " Golden West." Within the mountains besides fishing, hunting the Big Horn and the Rocky Mountain Goat will give exciting sport. Should the student of nature desire to examine the recesses of the mountains he can easily do so, as any of the beds of shingle will lead him into narrow canyons or beside tiny waterfalls, which come from giddy heights or far up the slopes where he will see the power' that frost and rain exert in pulling down the mountains. A few short years and this hitherto unknown region will be the shrine to which many weary pilgrims will turn their faces and gain that health and vigor denied to many of the devotees of the more fashionable resorts of the East. When the iron horse goes snorting up the Pass, much of the wildness of the present will have passed away for ever, but the ever varying beauty of the mountains will remain, and the heart will be cold indeed that does not glow with pleasure as the eye roams over the unrivalled beauty of the ever changing panorama. The Gold Eye is a beautiful fish, and if other and better fish could not be obtained it would be more highly prized than it is. It is generally about fourteen inches long, rather flattened and with white and delicate flesh. Its large and shining scales give it a silvered appearance, and its extremely large eye, with a yellow iris has won its English name "Gold Eye." This fish is abundant in all the rivers of the plains and was the only fish taken with NOTES ON REPTILES, FISHES, AND INSECTS. 391 bait except the Pike. No matter how muddy the water we could always reckon on Gold Eyes. Sturgeon are often caught in great numbers in the Sas- katchewan, Red, and Assiniboine Rivers. There are two species of this fish in the Saskatchewan. Sir John Richardson places its northern limit in about 54^ degrees north latitude. The smaller species {Accipenser Rupertianus) has a tapering snout. It seldom exceeds ten or fifteen pounds weight. The other is the Nameyu of the Crees, and often weighs ninety pounds and sometimes even attains the weight of one hundred and thirty. Its snout is short and blunt, being only one third as long as the entire head. This species ascends the Winnipeg River and enters the Lake of the Woods and sometimes ascends Rainy River to Fort Francis. Many fine sturgeon are speared in the Assiniboine and Red Rivers by Indians but there is no systematic attempt made to make a business of their capture. I append Archbishop Tache's account of this fish :— " There are Sturgeon in North America as well as in Northern Asia. Not only does the Pacific Ocean send them in crowded shoals into the rivers flowing from this country, but our lakes are not without them. This large fish delights in a part of this territory ; it willingly frequents Lake Win- nipeg, and nearly all the important rivers flowing into and out of it ; there are some in the lower part of English River, but they do not ascend beyond the fall at Frog Port- age, and they try in vain to get over Carp Rapids in Rapid River, a tributary of the Saskatchewan ; so that the neigh- borhood of Frog Portage is the northern limit to which they reach in the interior of the country. Nor are they found to the west of this point in the same latitude ; but to the south and east they are generally distributed. In our great central basin they are found in abundance. There are very fine sturgeon in Lake Winnipeg; I have seen them seven 392 MANITOBA AND THE GREAT NORTH--WEST. feet long and one hundred and fifty pounds in weight. The fish is excellent to eat ; it furnishes a great deal of oil, and its air-bladder, simply dried, supplies the very useful isinglass of commerce. " Salt provisions are as yet not much used here, and salt is so dear that salting Sturgeon has not hitherto been thought of; but such a method of preserving them would be more profitable than the plan adopted by the Indians of merely drying some pieces.' ' In the future the fisheries of Lake Winnipeg, Manitoba and Winnipegoosis will be developed to such an extent that fish will be a large article of diet and pay a remunerative price to the regular fishermen. The communities settled in the vicinity of the Qu' Appelle and Long Lakes will have abundance of the finest White Fish at their doors, and should their lakes become exhausted, they can very easily be restocked as the artificial breeding of fish in the Dominion has become a regular branch of business. Dr. G. M. Dawson when naturalist to the Boundary Sur- vey collected twenty-two species of butterflies, many of which were very beautiful and sometimes in great numbers. During the month of June in the partially wooded country, small blue butterflies are very common and at the same time many of the commoner species of Ontario are seen flitting about in myriads. Later in the season numerous active species of small size are seen on the prairie sucking the nectar of the various Compositae which cover the plain with their showy flowers. Towards the end of October large numbers of a species of Golias congregate on the damp mud along the trail or are seen lazily sitting on the late flower- ing Astus Scarcely any moths were noticed at any time and during all the summers spent on the plains a large one was never seen. It is true that owing to the attacks of the mosquitoes we were seldom out of our tents after sundown and may not have been abroad when they flew. NOTES ON REPTILES, FISHES, AND INSECTS. 393 Many species of beautiful Coleoptera were obtained on the " Great Plains" which on investigation proved to be a part of the insect fauna of the South-Western States. It is a curious fact that in both fauna and flora the south-western part of the North-West Territories contains many species common in California, and further investigations will likely add many other species as every year new forms are being added to the list. This fact is one more link in the chain of proof regarding the source of the warm winds of the South-West and tends to show the permanency of the mild climate. In the past the plague of grasshoppers has been on the land more than once and in the future may reasonably be expected again. Dr. G. M. Dawson, from whom I have quoted so often, has paid a great deal of attention to this subject and thus deals with it in his Keport on the Interna- tional Boundary Survey : — " The grasshoppers forming des- tructive swarms in the region of the plains east of the Rocky Mountains, appear to belong to a single species, which has been called Galoptenus spretus. This insect much resem- bles the Galoptenus femuir-^uhrvm, or red-legged grasshopper, which an exceptional years has been destructive to crops in various parts of the Eastern States. Spretus differs, how- ever, from femur^ubrvm specifically, and can not only be distinguished from it in form, but possesses a far higher degree of instinct and power of migration, circumstances suiting it to the almost boundless plains which it inhabits. " Locusts are not natives of the eastern region of the plains, where their devastations are most severely felt. They come from the far west as a winged swarm, and where they happen to be when they are mature, their eggs are deposited. From these eggs, in the ensuing spring, the young come forth, and cause often more complete des- truction of crops than the wuiged adults ; for they attack the young grain, eatmg it down as fast as it grows. The 394 MANITOBA AND THE GREAT NORTH-WEST. young so produced, however, appear not to have so much vitality as those coming fresh from the west. A great part of them may reach maturity and migrate some distance, but their progeny in the third season seems rarely to give much trouble. " The range of the insect (meaning by that term not only their chief breeding places, but the whole area known at one time or other to be overrun by them) is not bounded to the west by the Rocky Mountains, except where these con- stitute, as in British America, the unbroken front of the western region of forest. They spread across the watershed in Colorado and Utah, and appear to have been observed by Mr. Byers, in the valley of the South Pork of the Columbia River, near Fort Hall. Southward, according to Prof. Thomas, they extend as far as the Raton Mountains and into Texas; while to the east they have spread to the prairie country of the Mississippi, and have been known, on more than one occasion, to penetrate far into Iowa. The entire Province of Manitoba is liable to their incursions, and they have penetrated in swarms as far east as the Lake of the Woods. Northward, they are probably only limited by the line of the coniferous forest, which approximately fol- low the North Saskatchewan River. " The eggs of the Locust are not deposited promiscuously, or uniformly distributed over the surface ; whether in their native breeding places or in their eastern colonies. High and dry situations, with hard soil, are preferred. Thus, when the young are hatched, from this original deposition of the eggs — and no doubt also from a natural gregarious tendency — they form colonies, which are often widely sep- arated. These I have seen on the third prairie plateau in 1874, and the young insects are also noticed to be thus dis- tributed in the Red River Country this year, and elsewhere, wherever they have been carefully observed. The insects do not seem to travel far from their hatching place for some KOTES ON REPTILES, FISHES, AND INSECTS. 895 days ; but when they have increased somewhat in size, they begin to move forward together, and in a determinate direc- tion, though not by any means invariably from northwest to southeast. Prof, Studley of Kansas, has experimented on the unfledged grasshoppers, by sifting flour on them in the morning, and measuring the distance travelled over by the insects so marked at night, and finds that their rate of prog- ress is from one-fourth to one-half mile per diem. In the last week of July, 1873, I met the grasshoppers hatched out in the northern part of the Red River Country, travel- ling southward down the valley. They were in the pupa stage, and appeared to be advancing more rapidly than the above measurement would indicate. Their fixed determina- tion to travel southward was remarkable. " On obtaining their wings, the grasshoppers prepare for flight, and only wait the advent of a favoring breeze, to set out in the direction which their instinct leads them to pursue. On July 12th of last year, I observed swarms ready for flight on the high plains of the third plateau, west of White Mud River (long. 107° 35). The day was hot and calm,, and though many of the insects were on the wing at all altitudes in the atmosphere, they were following no de- terminate direction, but sailing in circles, and crossing each other in flight. The greater number were hovering over the swamps and spots of luxuriant grass, or resting on the prairie. A slight breath of air would induce them all to take wing, causing a noise like that of the distant sound . of surf, or a gentle breeze among pine trees. They appeared ill at ease, and anxiously waiting a favorable wind. " The grasshopper has not intrinsic powers of swift flight. It can bear itself upon the wing for a long time, but depends chiefly on the wind for propulsion, and travels fast or slow according to its motion. It flies only in the sunlight and during the warmer hours of the day, coming to the ground about 4 p.m., if the day be fine ; or at any time when a 396 MANITOBA AND THE GREAT NORTH-WEST. heavy cloud covers the sun, or on the approach of a storm. Nor does it fly in any direction the wind may happen to blow, but has the extraordinary instinct to travel only on those days when the wind may favor it in its appointed course. This, as already mentioned, is generally south-east- ward, from its high-land breeding grounds to the lower and more fertile eastern regions. It is not by any means in- variably so, however ; and some of the broods hatched this spring are already showing a similar persistent desire to move northward, while in their full strength and vigor. When the locust reaches nearly its eastern or southern limit, the organization of the swarms appears in great measure to fail, they move in almost any direction with the wind, or remain long on the ground where food is abundant. After the deposit of eggs, which in the normal sequence of events next happens, the insects are much exhausted, and soon die, though often making a short fickle flight. " Such is the life-history of the insect. The causes which fortunately prevent its increase and continued abode in the eastern prairie region, appear to be chiefly climatic. It would seem that the locust requires, to bring it to healthy maturity, the dry warm climate of the higher plains. In the eastern colonies the young are sometimes hatched in considerable numbers by a mild autumn, and perish in the succeeding winter. A relapse of cold and damp weather after their hatching in spring, causes the death of great numbers. The eastern brood is a weaker one, and is ac- cordingly more subject to the attacks of diseases, and para- sites. Mr. Riley catalogues four of the latter. The two first ( Tromhidium sericeum and Astoma gryllaria) are mites ; the two latter {Tachina anonyma and Sarcophaga carnovria) flies, the larvae of which feed on the grasshopper and live within it. All these seem to have appeared in connection with the swarm of 1874, and their progeny of this spring, in Manitoba. The Tromhidium, or silky white, attacks the NOTES OK REPTILES, FISHES AND INSECTS. 39V egg. The Astoma attaches itself to the mature insect, generally under the wings. The first appearance of the locusts in formidable numbers in the Red River Valley, seems to have been in the year 1818, six years after the foundation of Lord Selkirk's colony. They then arrived on the wing in the last week of July, and destroyed nearly everything but the wheat crop, which partly escaped, being nearly ripe. Eggs were deposited, and in the following spring, the wheat and all other crops were destroyed as fast as they appeared above ground. Eggs seem again to have been deposited in 1819, and in 1820 the crops are said once more to have suffered greatly. The next recorded incursion is that of 1857, from which it would seem that for 36 years the insect had not appeared. In 1857, the crops are said to have been so far advanced as to escape great damage, but eggs were deposited, and in 1858 all the young grain was devoured. In 1864, they again appeared, and left their eggs, but neither the adults, nor the young of 1865 were sufficiently numerous or wide-spread to do much damage. In 1867, numerous swarms poured in, but did little injury, the crops being too far ad- vanced; their progeny in the ensuing Spring, however, devoured everything, causing a famine. They again ap- peared in 1869, the young in 1870 doing much harm. In 1872, fresh swarms arrived, but as usual, too late to do much damage to wheat. Eggs were left in abundance in the northern part of the Province, and in the following Spring the farmers over considerable districts did not sow. In 1874, winged swarms came in from the west, arriving earlier than usual, and inflicting great injury on the crops in some districts. Eggs were deposited in almost all parts of the Province, and the result has yet to be seen." During the fall and winter of 1875 they all died, and since then Manitoba and the North-West have not been visited by them. 398 MANITOBA AND THE GREAT NORTH-WEST. Mosquitoes are a real plague and cause more irritation to man and beast than all other plagues together. Little need be written about them as like the summer's heat and winter's cold they are of periodic occurrence. Another insect, named by the Half-breed the " Bull-dog," is a terrible pest during ihe month of July. He is only troublesome however about the middle of the day and seldom remains more than a few days at a time. Flying ants are troublesome in August but they seldom remain many days, and only fly when the day is very warm and sultry. CHAPTER XXIII. Minerals of the North- West. Boundary of the Laurentian Series— Lower Silurian Rooks— Limestone at the Stone Fort near Winnipeg— Building Stone of Winnipeg— Devonian Series along Lakes Manitoba and Winnipegoosis— Salt Deposits in these Rocks— Pure Salt Collected in 1881 — Description of the Manufacture of Salt on Lake Winnipegoosis — Devonian Rocks on Peace River — Gypsum, Salt, and Petroleum — Gypsum on Peace River Salt Springs of Salt River — Tar Springs on the Athabasca — Cretaceous Series — Its Extension — Limestone and other Boulders — Gravel and Sand— Niobrara Limestone Souris Coal Field— Coal in the Peace River Country— Lignite Tertiary— Its Probable Extension — Coal Deposits of Immense Extent — Pure Hematite in connection with the Coal — In the Saskatchewan Country — At Edmonton — Along Peace River Its Probable Value — Gold on the Saskatchewan — On Peace River — Gold Washing Seldom Remunerative — Brick Clays — Their Great Value and Probable Extent — Concluding Remark*:. Geological Formations represented in the North-West are very few, and a glance at a map will suffice to explain fully the following notes. On the east side of Lake "Winni- peg, the Laurentian series extend from the shore line, for the greater part of the length of the lake. Striking north- westerly from the head of the Lake they appear at the western end of Lake Athabasca as a series of glaciated rocks, glistening in the sunlight like polished silver. Along the northwest shore of Lake Winnipeg, the rock exposures are Lower Silurian and those at the stone Fort are described as the Hudson Eiver Group of the same series. On Pine Island Lake near Cumberland House, and at the Grand Rapids of the Saskatchewan are many fine exposures of the Silurian series. The rocks of the Hudson River Group furnish the build- ing stone for the "Stone Fort," Fort Garry, all the old churches in the vicinity of Winnipeg, and all the stone for the foundations of the massive structures which have been and are now being erected in Winnipeg. Stoney Mountain will be a mine of wealth to future speculators, from which 400 MANITOBA AND THE GREAT NORTH-WEST. lime, stone, and gravel will be procured for the wants of the city. Lying farther south and possibly underlying the greater part of the western side of the Manitoba Plain are the Devonian Series. These rocks are known to be largely developed on both sides of Lakes Manitoba and Winni- pegoosis. Numerous salt springs are found in connection with them, and during the last summer the writer saw salt springs and brooks of strong brine flowing from them in various localities at the head of Lake Winnipegoosis. The subjoined list of salt springs known to occur on Lakes Man- itoba and Winnipegoosis may tend to excite interest in these extensive deposits: — 1. Crane River, Lake Manitoba. 2. Water Hen River, Dickson's Landing. 3. Salt Point, east side of Lake Winnipegoosis. 4. Salt Springs, ) 5. Pine River, v Winnipegoosis. 6. Rivers near Duck Bay, ) 7. Turtle River, Lake Dauphin. 8. Swan or Shoal, two localities. 9. Salt River flowing into Dawson's Bay. 10. Numerous salt springs and bare saturated tracts of many acres in extent on Red Deer River, which flows into the head of Dawson Bay, Lake Winnipegoosis. For ten miles up this river salt springs are quite frequent, and excel- lent salt was collected in three places where it formed a crust on the surface of the ground. Some springs were ex- amined where a respectable rivulet of strong brine issued from them clear as crystal and evidently quite pure. All the springs and marshes seen were bordered with seaside plants, and one of them, which has never been found from the sea coast before in America, was found in abundance. The plant referred to is Sea Side Plan tarn {Plantago Maritima.) MINERALS OF THE UTORTH-WEST. 401 From time immemorial, salt has been manufactured along the west sides of Lakes Manitoba and Winnipegoosis, and at Salt Springs the manufacture was carried on by John Monk- man, in 1859, when the works were visited by Professor Henry Y. Hind. The manufacture had been carried on for forty years prior to that time by Jas. Monkman, his father. Professor Hind thus describes the springs and the manufac- ture of salt at the time of his visit : — " The soil at the Salt Springs is a very retentive yellow- ish-white clay, containing small limestone boulders and pebbles, with boulders of the unfossiliferous rocks. The wells, for obtaining a supply of brine, are sunk wherever a small bubbling spring is observed to issue from this reten- tive clay. The springs are constantly changing their povsition, and as the wells become exhausted from time to time, a fresh excavation is made where a new spring is observed to issue. No doubt boring, or deeper wells, would prevent these changes, and not only secure a larger flow of brine, but insure its permanency. The wells at present are twenty -five in number; but some of them appear to have been lately abandoned, and others have long since ceased to yield brine. They are situated four hundred yards from the lake shore, and were first worked forty years since, by James Monkman. He has made salt at both Swan and Duck Rivers. The manufacture is now carried on with profit for the Hudson's Bay Company, at Swan River, and at Winnipegoosis Lake by Monkman' s sons. " At the ' Works ' there are two small log-houses and three evaporating furnaces. The kettles of English con- struction, are well-made rectangular vessels of iron, five feet long, two feet broad, and one foot deep. They are laid upon two rough stone walls, about twenty inches apart, which form the furnace. At one extremity is a low chimney. The whole construction is of the rudest descrip- tion ; and at the close of the season the kettles are removed, 26 402 MANITOBA AND THE GREAT NORTH-WEST. turned over, and the furnace permitted to go to ruin, to be rebuilt the following spring. " The process of making salt is as follows . When a pring is found a well five feet broad and five feet deep is excavated, and near this an evaporating furnace is erected. The brine from the wells is ladled into the kettles, and the salt scooped out as it forms, and allowed to remain for a short time to drain, before it is packed in birch bark roggins for transportation to Eed River, where it commands twelve shillings sterling a bushel, or one hundred weight of flour, or a corresponding quantity of fish, pemican, or buffalo meat, according to circumstances." While on the subject of salt I cannot do better than speak of that which is obtained on Salt River, an affluent of Slave River. Salt obtained here is used throughout the north. In September, 1875, during my visit to Fort Chipweyan at the western end of Lake Athabasca, a boat load of excellent salt was brought up from Salt River. It differed from common coarse salt in consisting of large cubical crystals, which were very hard when placed under the teeth. Sir John Richardson, in his narrative of the Arctic Search- ing Expedition under his command, thus speaks of the salt deposits on Salt River: — "In 1820, I ascended the very tortuous Salt River, for twenty miles, for the purpose of visiting the salt springs, which give it its name. Seven or eight copious springs issue from the base of a long even ridge, some hundreds of feet high, and, spreading their waters over a clayey plain, deposit much pure common salt in large cubical crystals. The mother water, flowing off in small rivulets into the Salt River, communicates to it a very bitter taste ; but before the united streams join the Slave River, the accession of various fresh-water rivulets dilutes the water so much that it remains only slightly brackish. A few slabs of greyish compact gypsum protrude MINERALS OF THE NORTH-WEST. 403 from the side of the ridge above mentioned, and a pure white gypsum is said to be found at Peace Point on Peace River, distant about sixty or seventy miles in a southwest direction, whence we may conjecture that these springs may belong to the Onondago salt group of the Helderberg division of the New York system. The Athabasca and Mackenzie River districts are supplied from hence -with abundance of good salt. We obtained some bags of this useful article from Beaulieu, who was guide and hunter to Sir John Franklin on his second overland journey, and who has built a house at the mouth of Salt River. This is a well chosen locality for his residence. His sons procure abundance of deer and bison meat on the salt plains, which these animals frequent in numbers, from their predilection for that mineral ; and Slave River yields plenty of good fish at certain seasons." The Devonian rocks crop out on Peace River, below Fort Vermillion, and show very fine sections at the falls on Peace River near Little Red River, and at ether points. All the rock at the falls is a blueish limestone, which, when fully exposed to the influence of the weather, breaks up into thin layers. On the right bank, immediately below the falls, it forms cliffs from twenty to thirty feet high. The River at this point is nearly a mile wide, and presents a series of little falls all the way across. The many small rocky islands and isolated rocks that rise out of the river, and on the brink of the fall, all the way to the other side, form a beau- tiful panorama of rushing and falling water, with wooded or rocky islets, succeeded below the falls by placid river and sylvan scene. At present (August 15) the fall is about fifteen feet, but at high water it cannot be half as much. A couple of fossils were obtained here, which were identical with others collected from a different locality. The islands in the river below the falls are rocky ; rocks are also ex- posed on the right bank for about two miles, and are then 404 MANITOBA AND THE GREAT NORTH-WEST. concealed. About three miles below the falls Little Red River comes in on the right bank, and, at its outlet, a dif- ferent rock formation presents itself The beds are composed almost altogether of many species of corals. There is a good exposure, and, as we took a day here to rest, I made a large collection. The lower layers are of fine texture, thin bedded, and without fossils. These are followed by beds almost wholly made up of those branching corals {Alveolites) so common in Devonian rocks, intermixed with a species of Zaplirentis in great abundance, some of the higher strata being largely made up of these, but occasionally associated with others of a rounded form. Above the latter there are, at least, six feet of rock holding large corals, in which the fine structure was nearly obliterated by the crystallization of the mass. Others were observed in concentric layers ; < and some, when broken, fell apart as if formed in successive laminae. Another outcrop occurs about a quarter of a mile up Red River. No fossils were observed here, but the rock, which is heavy -bedded and in a nearly horizontal position, appears to overlie those just described, and adds a few feet to the total thickness exposed. The rock at this point seems to overlie that at the chuttes. Approaching " Rapid Bouille " the banks of the river begin to attain some elevation, but no rocks are exposed until the head of the rapid is passed ; then limestone crops out, but so much broken and contorted that its dip is not apparent. Many fossils were found at this point, both loose and in the rock. A few yards below this, fine white gypsum crops out, and continues as the lowest rock in the section for the next twenty miles. This is overlaid by a light grey granular rock, largely made up of gypsum ; perhaps a limestone was observed in it, but there were no fossils. Descending the rapid the rock rises higher and higher along the shore, and by the time the lower end is reached. MINERALS OF THE NORTH-WEST. 405 it has attained a height of at least fifty feet above the water. At the foot of the rapid the river is divided into two channels by a high rocky island, which stands almost m the centre of the river. In many places the gypsum attains a thickness of from ten to fifteen feet, and is as clear and white as snow. The banks of the river and the islands from here to Peace Point, a distance of fifteen miles, show this rock generally much contorted, but seldom broken. At one point on the high bank the beds have been upheaved without being broken, to the height of at least forty feet, and show a very fine example of curved strata. On the Athabasca there are large deposits of bituminous shale, which are the source of the petroleum or mineral tar so frequently spoken of in connection with that river. I passed up the river in September^ 1875, and noted down what I saw. After entering the river from Lake Athabasca we gradually passed from mud to sand, but we went fully fifty miles before we saw anything like a pebble . The first indications of "tar" were in the shape of pebbles composed of sand and tar, formed above and carried down by ice About two miles below Echo's home we came upon the first gravel beach, and at Echo's the true bank showed for the first time on the left, but it was noticed about a mile above Embarras River on the right, and many times after- wards, showing that the river was eroding its right bank, while forming new land on the left. At this point the soil on both sides of the river is good, and the banks have the reddish tinge observed at Vermillion. Later in the day Birch Mountain showed blue in the distance, bearing about southwest. As we ascended, the river banks kept increasing in height, and the country began to assume the appearance of a good agricultural region. No rock was seen, but the " tar conglomerate " became very abundant, often being in beds two feet thick. Early on the afternoon of September 406 MANITOBA AND THE GREAT NORTH-WEST. 7th we came upon the shale beds which produce the tarry matter. After passing along them for about two miles, we stopped to trade for some dried meat, when I had an oppor- tunity of examining them. I found below a light grey sand- stone, partly saturated with tar, and overlying this there was at least fifteen feet of it completely saturated, and over this again shaleJargely charged with alkaline matter. This was the sequence all the way, although at times there was much more exposed. Where we landed, the ooze from the bank had flowed down the slope into the water and formed a tarred surface extending along the beach over one hun- dred yards, and as hard as iron ; but in bright sunshine the surface is quite soft, and the men when tracking along shore often sink in it up to their ankles. During the remain- der of the afternoon we sailed past other rock exposures, but observed no change in their aspect or mode of occur- rence, though very often they were much higher. Next morning we had travelled about two hours when we stopped at a tar spring to procure the tar which was obtained last winter. The rock here was just the same as that seen yesterday. Instead of getting the tar on the beach, as I expected, I was led up the hill until we attained the height of forty feet ; here we found a small pool of water, and underneath it the pure tar. I noticed a little stream of water flowing into the pool, which was coated with an oily scum, and under the stream there was an abundance of tar. Along the beach it was seen oozing out in many places, and by gathering and washing the sand saturated with it, we obtained just as '"ure tar as we brought from the spring on the hill-side. Bluish concretionary limestone, in appearance like that at Little Red River, crops out on both sides of the river at Point of Rocks, forming cliffs twenty-five feet high. The upper beds are thick and withstand the weather, but about six feet from the top, these gave place to rock which MINERALS OF THE NORTH-WEST. 407 crumbles exactly like that containing the large corals at Red River. For more than twenty miles this rock was observed, and it was from it that the fossils were obtained, labelled " thirty miles below the forks." After about twenty miles, we again came on the tar shale, and passed the place where the Hudson's Bay Company get their sup- ply for the boats. All the limestone passed to-day was cream colored or light grey, and was heavily bedded on top, but had much the appearance of shale below. The frost disintegrates the latter, and it separates into fragments suitable for road-making. Nearly all the strata show graceful curves, the folds never rising higher than ten feet. The dip is about north and south, the strike crossing the river at nearly right angles. Within ten miles of the forks, a very fine section of the rock is exposed, showing the limestone, and then about ten feet of yellowish cla.y, followed by at least 100 feet of black shale, which looked like sandstone, and in the dis- tance resembled the shale between Dunvegan and Smoky River. Alkaline springs were observed oozing out of these strata, but there was no tar. I have no doubt but that the shale, out of which the tar comes, overlies the coral formation observed at Red River. Exactly at the forks, the latter rises out of the water, capped by at least 150 feet of black shale, from which the tar oozes, and these are surmounted by a few beds producing an alkaline efflorescence. Mr. Moberly told me that the tar beds extended up the Athabasca to near the mouth of Lac la Biche River, and I found that they still continued up the Clearwater, but eventually sank beneath the soil. About ten miles up the Clearwater, the men pointed out a tar spring in the stream, from which tar was very often obtained. Before passing the Pembina River, we came upon sand- stone which is suitable for making grindstones. This rock was occasionally seen for about two miles, when signs of' 408 MANITOBA AND THE GREAT NORTH--WEST. tar again appeared. These passed away, and limestone was occasionally seen, and towards evening, I procured those fine fossils which were so much admired. For nearly a day after this, no rock exposures appeared, but when we came upon the rocks again, they differed from any I had yet observed. They were cream-colored, shaly, non-fossilif- erous limestones. After passing these, we came to the sulphur springs. Pour little creeks discharge these springs. They are said to be very bitter, and their margins are lined with sulphur. Sir John Robinson, in his narrative, says : " At eight, we came to a sulphurous spring, which issues from the limestone on the bank of the river. Its channel is lined with a snow-white incrustation, the taste of the water is moderately saline and sulphurous, and, from its coolness, rather agreeable than otherwise. It has a slight odor of sulphurated hydrogen." Speaking of the bitumen. Sir John says : " About thirty miles below the Clearwater River, the limestone beds are covered by a bituminous deposit upwards of one hundred feet thick, whose lower member is a conglomerate, having an earthy basis much stained with iron, and colored by bitumen. Many small grains and angular fragments of transparent and translucent quartz compose a large part of the conglomerate, which also contains water-worn pebbles of white, green, and otherwise colored quartz, from a minute size up to that of a hen's egg or larger. Pieces of green-stone and nodules of clay-ironstone also enter into the composition of this rock, which, in some places, is rather friable, and in others, possesses much hardness and tenacity. Some of the beds above this stone are nearly plastic, from the quantity of the mineral pitch they con- tain. Roots of living trees and herbaceous plants push themselves deep into beds highly impregnated with bit- umen ; and the forest where that mineral is most abundant does not suffer in its growth. MINERALS OF THE NORTH-WEST. 409 The shale banks are discontinued for a space, in the neighborhood of Beren's House, where thin beds of lime- stone come to the surface, and form cliffs twenty or thirty feet high at the water's edge. Still farther down the river, or about three miles below the Red River, where there was once a trading establish- ment, now remembered as Le vieux Fort cle la Rimere Rouge, a copious spring of mineral pitch issues from a cre- vice in a cliff composed of sand and bitumen. It lies a few hundred yards back from the river, in the middle of a thick wood. Several small birds were found suffocated in the pitch. At the deserted post, named Pierre au Gal/met, cream- colored and white limestone cliffs are covered by thick beds of bituminous sand. Below this, there is a bituminous cliff, in the middle of which lies a thick bed of the same white earth, which I had seen higher up the river in con- tact with the limestone, and following the undulations of its surface. A few miles farther on, the cliffs for some distance are sandy, and the different beds contain variable quantities of bitumen. Some of the lower layers were so full of that mineral as to soften in the hand, while the upper strata, containing less, were so cemented by iron as to form a .firm dark-brown sandstone of much hardness. The cliff is, in most places, capped by sand containing boulders of lime- stone. Every bituminous bed, carefully examined with the microscope, was found to consist, in addition to the bitumen, of small grains of transparent quartz, unmixed with other rock, but enclosing a few minute fragments of the pearly lining of a shell. A similar bed in another locality contained, besides the quartz, many scales of mica. The whole country, for many miles, is so full of bitumen that it flows readily into a pit dug a few feet below the surface. 410 MANITOBA AND THE GREAT NORTH-WEST. Dr. George M. Dawson, Assistant Director of the Geolog- ical Survey of Canada, in his report on the geology of the 49th parallel, thus speaks of the distribution of the Creta- ceous Rocks in the North-West Territories : — " The Cretaceous rocks, corresponding in age with the great chalk formations of Europe, though very different from them in mineral character, are those which spread over by far the greatest surface. Except in a few localities, and those chiefly in proximity to the Rocky Mountain region of uplift, they are still almost as perfectly horizontal as when originally deposited. The eastern edge of this formation partly overlaps the underlying Silurian and Devonian beds, and runs nearly parallel with the base of the Laurentian range, at a distance of about one hundred and thirty miles, from the fifty-third to the fiftieth parallel of latitude. Southward, it tends to the east, and probably crosses the forty -ninth parallel east of Red River ; while in south-western Minnesota, Cretaceous rocks repose directly in some places on granites, which are no doubt Laurentian. " The general course of the eastern outcrop is consequently about north-north-east ; and it is marked broadly, by a series of escarpments and elevations, including — from south to north — Pembina, Riding, Duck, Porcupine, and Basquia Mountains. All these appear to be composed for the most part, if not entirely, of Cretaceous rocks, though the ex- treme edge of the formation may often stretch beyond them. These so-called " mountains " are, more correctly speaking, — as already shown — salient points of the edge of the second plateau, and the generally horizontal position of the beds thus suddenly cut off to the east, attests the immense denudation which must have taken place in com- paratively modern times. " North of the Basquia Mountain, from the very scanty information we at present possess, the edge of the Cretaceous would appear to run westward, and cross the Saskatchewan MINERALS OF THE NOKTll-WEST. 411 River, near Fort a la Come, where at Cole's Falls a dark- colored shale which has been referred to the lowest mem- ber of the series, occurh. It may very probably be nearly conterminous with the edge of the second plateau, which, according to Dr. Selwyn, crosses the river forty-five miles below the Fort. The western border of the Cretaceous seems, in some places, to follow closely along the base of the Rocky Mountain Range, but many circumstances arise to complicate the question in that region, and it will only be after the accumulation of much more information than is at present in our possession, that the line can be laid down with any accuracy. In some parts of the range, Cre- taceous rocks have been included among the mountains themselves, and considerably altered ; but the greater part of the newer strata, which must have covered the palae- ozoic rocks of this region when the uplift first took place, have been removed by denudation. " The Cretaceous rocks thus defined in breadth, north of the boundary line, have been noted by Professor Hind, Dr. Hector, Dr. Selwyn, and Prof. Bell, in many localities on the second prairie level, some of which are more par- ticularly referred to in the sequel, and are known to extend in a broad zone from the North Saskatchewan to the Mexican frontier and southward. " Our knowledge of the Cretaceous beds ueyond the North Saskatchewan, is as yet very limited, and depends almost entirely on the observations of Sir J. Richardson, aided by chance notes of other explorers not professed geol- ogists. It IS likely, however, that a trough or series of more or less isolated basins of lignite and coal-bearing strata, follows near the eastern base of the mountains the whole way to the Arctic Sea. A part of these beds is known to represent the Lignite Tertiary of the south, but judging from their association elsewhere, they will probably be found to rest on Cretaceous rocks throughout. Indeed, 412 MANITOBA AND THE GKEAT NORTH-WEST. from the fragmentary nature of the information concerning the great northern region, and the unsettled questions with regard to the age of the coal series of the analogous region, near the mountains and south of the North Saskatche- wan, it is impossible to decide whether some of the coals and lignites described, may not belong to the Cretaceous formation itself. The existence of Cretaceous beds has, however, only been determined with certainty at a single locality, on the Bear Lake River, near its junction with the Mackenzie. Sir J. Richardson, here, discovered an Ammonite among sandstones and shales which he states resembles those of the coal measures." The subdivision of the Cretaceous, as it occurs in Mani- toba and the North-West Territories, will require dis- cussion after the systematic description of the localities in which it has been examined. From its close general re- semblance, however, to that which has been studied in the western part of the United States, it will be useful to have the Upper Missouri Section of Meek and Hayden, which has now become typical, as a standard of comparison. The formation is there composed as follows in descending order : — Later Cretaceous. No 5. Fox Hill Beds. —Grey, ferruginous and yellowish sanastones and arenaceous clays. Marine Shells 500 feet No. 4 Fort Pieree Gkodp. — Dark grey and blueish plastic clays Marine shells, gypsum and fish remains 700 feet Earlier Cretaceous. No. 3. NioBRARi Geohp. — Calcareous marls, Marine shells, fieli remains, For- aminifera, &c 200 feet. No. 2. Fort Benton Group. — Dark grey laminated clays with some limestone. Marine shells 800 feet. No. 1 , Dakota Group. — Yellowish, reddish, and whitish sandstones, and clay, with occasional lignites. Marine and some fresh water shells and Angiospermous leaves 400 feet Giving as an approximate thickness of the formation in that region, 2600 feet. MINERALS OF THE NORTH-WEST. 413- The Lignite Tertiary rocks north of the line are not bounded by any great physical features of the country, but adhere closely to the upper members of the Cretaceous, and behave as an upper member of that formation might be expected to do. Though no doubt originally deposited in extensive basin-like depressions of the Cretaceous strata, these are now generally found forming slightly elevated plateaux. Denudation must have acted on these rocks on a vast scale, but they still cover an immense area and con- tain the greatest stores of mineral fuel known to occur in the vicinity of the forty-ninth parallel. The line of their eastern edge crosses the parallel near the 102nd meridian, and thence appears to pursue a northwestward course, remaining for some distance nearly parallel with the edge of the third plateau. Beyond the Elbow of the South Saskatchewan, though the same physical feature continues to the north, it is not known what relation it may bear to the outcrop of this formation, nor has its northern limit been ascertained. Between the North and South branches of the Saskatchewan River there is a great tract of country, the geological features of which are still very imperfectly known, but where it is highly probable, outlyers, if not direct extensions of this Lignite formation will be met with. To the west, it appears to extend,, at least in some places, nearly to the base of the Rocky Mountains. " A thick mantle of sands and clays, referable to the glacial period, and to former great lakes, covers almost the entire surface of the plains. A geologist may often travel a hundred miles without once being able to observe a section of the underlying Creatceous or Tertiary rocks, and but for their great uniformity and simplicity of structure, it would be a very difficult task to unravel the geology of so vast a region. The very monotony of the plains is, however, tO' a great extent, a corollary of the attitude of the strata 414 MANITOBA AND THE GREAT NORTH-WEST. between them, and of their unconsolidated and homogeneous character." In many parts of the country particularly along the upper slopes of the coulees and river banks there are numerous boulders of various kinds of rock. About one- third are white limestone and the remainder various kinds of metamorphic rocks particularly gniess. Lines of bould- ers are to be found along the Little Saskatchewan in the vicinity of Rapid City, and much of the land is very seri- ously encumbered by them. The same complaint is made at Birtle on Bird Tail Creek and westward in the direction of Fort Ellice. Brandon has its share, and when the excite- ment, which is now at fever heat, begins to die out many will complain of the multitudes of stones which encumber their lots. Port Ellice and almost every town or village laid out on the bank of a river is in the same category. Boulders are found in ridges on many parts of the Second Prairie Steppe and often extend for miles in almost straight lines. When the country is more thoroughly examined these ridges will be found to indicate the margins of great depressions, possibly of lake basins of a former period. In the valley that stretches from the source of the Qu' Appelle to the South Saskatchewan there are multitudes of en- ormous boulders. One of these was measured by Prof. Hind, and was found to be 78 feet in circumference and at least 14 feet in altitude. The next largest was one of limestone, seen on the prairie below the Moose Woods. It is about 16 feet high and at least 60 feet in circumference. In the valley of the Souris near the boundary they are in immense numbers and all appear to lie on the surface. At Livingstone, Swan River, and Banicks they lie so close that no cultivation of the soil could be effected. Scores of places might be enumerated where they lie thickly on the ground and extensive tracts where not one can be seen in a day's journey. MINERALS OF THE NORTH-WEST. 415 All the interior lakes be they large or small are margined by a wall of boulders which are pressed into position as perfectly as if they had been placed there by man. Ice is certainly the cause of this in every case and a careful observer cannot fail to be struck with the uniformity with which it acts. While encamped on the shores of Long Lake in July, 1879, my attention was called to a point of rocks which extended into the Lake near its northern end. Two large boulders lay at the base of the heap and between them and the lake were two deep grooves which they had made in the spring when being shoved out of the Lake by ice. Each stone had been forced by ice out of the depths of the lake and left its record behind A careful measure- ment was made, and it was found that the stones had been shoved 47 yards or more. We traced the drove into water three feet in depth but how much farther it extended we could not determine. Gravel and sand are not wanting in any part of the country, although there are wide areas where none appears on the surface. All water obtained from gravel is excellent, and many ponds fed by springs are found where gravel mounds predominate. Nearly all the gravel on the Second Prairie Steppe is coated with carbonate of lime, but on the Third Plateau the character of the gravel changes and is a quartzite with the pebbles so smooth that it seems but as yesterday when it was an old sea beach. In many places, notably the Cypress Hills and elevations over 2000 feet above the sea, along the eastern base of the Rocky Moun- tains, this gravel is spread as a thin sheet over the surface. I have often noticed it less than three inches in depth, and covering the surface conformably to the undulations. This is the gravel that prevents much of the land south of lat. 50° and in the Bow River District from being fit for agriculture. Sand is another feature of the plains, and may be said to be a characteristic of the whole country west of Red River 416 MANITOBA AND THE GREAT NORTH-WEST. Plain. Sand dunes are found in front of the Second Prraiie Steppe, between the Pembina Mountain and Riding Moun- tain, and are well developed on the line of the Canadian Pacific Railway east of De Winton. By means of these dunes the Railway is carried from the lower to the upper plain, and all travellers must notice the striking resemblance that these hills bear to those along our great lakes on the Ocean itself. Along the Souris, especially southwest of Brandon, there are numerous sand hills which in many places are little else than moving masses of sand. At Flat Creek, on the line of the Canadian Pacific Railway and southwesterly in the direction of Oak Lake, sand hills are largely developed and are a characteristic feature of the country. At the head of the Qu'Appelle are three groups of sand hills which are gradually shifting eastward by the action of the wind- Along the east and northern faces of the group on the north side of the Qu'Appelle are a series of shallow pools or salt lakes which are dry or nearly so in summer, and from which when the wind blows the saline encrustations rise like smoke and disappoint the weary traveller as he looks anxiously around for a pool of good water. Enticed by the vapor he hastens on, and instead of a camp fire by a pool of refreshing water, he finds a dried up lake and its surface covered with saline crystals. My party became entangled in these sandy wastes on the 11th July, 1879, and before we could extricate ourselves and find water both men and horses suffered severely. Inside the line of ponds spoken of above the sand begins to rise into hills, which are being constantly blown away to form others. The movement is constantly from west to east, and the hollows and little hills with their trees and bushes are being continually filled up by the eastward move- ment of the sand. The second group of hills crosses the South Saskatchewan about three miles south of the Elbow, MINERALS OP THE NORTH-WEST. 417 and shortly after develops into an extensive sandy tract with sand hills 100 feet high towering up on every hand. The hills were without a partical of vegetation, and were very steep except on the western face where they were furrowed by the wind. Another extensive group lies north of the Cypress Hills near Gull Lake, and are of the same general character. On their southern side surrounded by sand, and in many cases standing in it is a grove of large Cottonwood trees These are probably the last remains of the former forrest, yet at present neither tree nor shrub exists within many miles of them. Other groups of sand hills are to be met with, but in general they are all alike, and seem to have been produced by the same cause — currents and eddies when the land was submerged after the close of the glacial period. The sandy country in all cases is above the general level of the district where they exist. About twenty-five miles north of the Boundary, where the Boyne Kiver cuts through the Pembina escarpment, limestone beds are seen, which Dr. G. M. Dawson refers to is the Niobrara division of the cretaceous rocks. The rock a cream-colored or nearly white limestone, breaking easily along horizontal planes, parallel to the surfaces of the shells of Ostrea and Inocerarmts, of which it is in great part com- posed. The same rock seems to crop out on the Assiniboine, about ten miles below the mouth of the Souris, where it shows fine exposures of nearly horizontal strata. Above Brandon, beds of apparently the same character have been observed, but owing to slides in the river bank, the ex- posures cannot be properly examined. In the chapter on fuel, will be found a full account of the coal as it occurs in the North-West, and, therefore, we will only give in this place the extent of the Lignite Tertiary, as shown by Dr. Dawson, in his exhaustive report. 27 418 MANITOBA AND THE GKEAT NORTH-WEST. " The total area of the western part of the Prairie region, between the forty-ninth and fifty-fourth parallels, now known by more or less connected lines of observation, to be underlaid by the lignite and coal-bearing formation or formations, does not fall short of 80,000 square miles ; and should future investigation result iu affixing some of the fuels to the lower cretaceous, it must be much greater. The importance of these great deposits of fuel, in a country naturally so destitute of wood over great areas, cannot be exaggerated." Since this was written, our knowledge has increased, borings have been made in the Souris Coal Field, and work- able seams are now known to exist there. Peace River has been further explored, and here, likewise, excellent coal has been obtained. In both cases, these coals belong to the lower cretaceous, and hence the remark in the pre- ceding paragraph, about the extension of the coal fields, is more than carried out, and it is now probable that the area will be nearly doubled. Brown hematite, in more or less abundance, is known to exist over a very wide extent of the prairie section, and has been observed by myself cropping out in many places on the Saskatchewan and its tributaries, and in numerous places on Peace River It is generally in thin layers or slightly connected nodular masses, and from the appended analyses, it may be considered a valuable and rich ore. Dr. Dawson thus speaks of its occurrence and value : — • '' The ironstones of the Lignite Tertiary formation, to which frequent reference has been made, though occurring very often in the same sections and in close proximity tu the lignites, have not been observed in any part of the area examined to occur in considerable thickness. They gener- ally appear in nodular sheets or scattered nodules, follow- ing certain horizons in the clays and argillaceous sands, and are found in greater or less abundance in nearly all the MIKERALS OF THE NORTH-WEST. 419 sections examined. Externally they weather to various shades of chocolate-brown and reddish-brown, but are hard and compact in structure, and within preserve their bluish- grey or yellowish-grey color. " The subjoined partial analyses of specimens collected in 1873, were published in the "Report of Progress" for that year. I regret that the time at my disposal prevents the examination of other specimens subsequently obtained : — /. Glay Ironstone. (Souris Valley.) Protoxide of Iron 49.00 Water lost at 115° C 121 Carbonic Acid lost on ignition 28.57 Siliceous matter insol. in H. CI 1 7.04 Phosphorus Trace. Uetallic Iron per cent, in raw ore 30 11 Metallic Iron, in calcined ore 54.27 //. Clay Ironstone. (Great Valley.) Protoxide of Iron 46.72 Water lost at 115° C 3 57 Carbonic Acid lost on ignition 21.23 Siliceous matter insol. in H. CI 8 72 Sulphuric Acid 0.30 Phosphorus 0.03 Metallic Iron, in raw ore 36.34 Metallic Iron, in calcined ore 49.90 " A small quantity of iron is present as peroxide, in each ore, but I have not thought it necessary to make a separate estimation of this. " It would appear that the iron ores of this formation rank high in the class to which they belong, and that if occurring in sufficient quantity, they might eventually be- come of great economic importance. I have not seen, however, in the vicinity of the Line, any place in which they are so abundant as to warrant the hope of the profit- able production of iron. In some localities, great surfaces are more or less thickly covered with nodules which have 420 MANITOBA AND THE GREAT NORTH-WEST. "been left behind by the erosion of the containing rocks ;. and it is, of course, possible that further search may lead to the discovery of sections in which so many bands occur, as to render it profitable to work over the entire bank for their extraction. If the manufacture of iron is ever to be carried on on a large scale, for the supply of the interior region of the conti- nent, it will naturally be conducted towards the base of the Rocky Mountains. There the fuels are better suited for this purpose, and ironstone probably occurs quite as abundantly in the formation. There, too, it may be confidently ex- pected that search will bring to light deposits of the richer classes of ores, among the palaeozoic rocks of the mountains. Gold, in small quantities, has been obtained, both above and below Edmonton, on the North Saskatchewan. It is found amongst the sand and gravel of the river bed, at the lowest stage of the water. Experienced miners make fair wages for a few weeks, before the setting in of winter, but, in no case, has a sufiicient amount been realized to warrant the belief that large deposits exist. The gold is exceed- ingly fine, and seems to be deposited every season, as the same bars will produce a small quantity of it each year. That found on Peace River is of the same character, and occurs in the same situations, but in much greater quantities. This remark applies only to that part of the river west of the Rocky Mountains. Without gold in greater quantities and in more accessible situations can be obtained by those who seek for it, this industry will never be profitable in the North- West. Up to 1873 brickiuaking was never attempted in Manitoba. During the summer of that year a beginning was made to manufacture them, but the success of the experiment was very indifferent and many prophesied the failure of the enterprise. Other attempts were made next year with the most gratifying success, and since then no difficulty has been MINERALS OF THE NORTH-WEST. 421 experienced in producing not only a good but very superior article. At Emerson, Portage la Prairie, Rapid City, and all other points good brick have been produced, and now it is a well ascertained fact that in every district brick clays abound. Besides its superior soil the North-West contains enor- mous deposits of coal underlying at least 150,000 square miles of surface. Immense deposits of salt exist on Lakes Manitoba and Winnipegoosis, and on Salt River in the vicinity of Great Slave Lake. Numerous petroleum springs are seen for many miles along the Athabasca ; and gold and iron in some abundance in certain parts of the country, so that, altogether, we are safe in saying that our vast interior is rich in those minerals which add most to the comfort and •wealth of civilized man. CHAPTER XXIV. Hiiiory of the Norfli -West, from tlie discorery of Ameri/ia /o tlie year 1821. First Voyage of Jacques Cartier — What he Intended Doing— Second Voyage — The Dis- f oveiy of the St. Lawrence — Montreal Reached— Roberval's Attempt at Settlement — His ^^'ant of Success — Champlain Founds Quebec, in 1608 — Interferes in Indian Qu.arrels — Lake Superior heard of, in lfil5 — Missionaries Traverse its Shores, 1641 — Frejir.hmen Cross hy the Dawson Route and Lake Winnipeg to Hudson Bay, in 1666— Offers of Service to the Quebec Merchants, Renewed in Pans, Accepted in liiigland — Gillam's Voyage — Formation of Hudson's Bay Company, in 1670 — Establishment of Forts on the Bay — Quarrels with the French — English Left in Possession of the Bay- French Trade Extended Westward — Duluth on Lake Superior — Bed River Reached and Forts Erected, 1732 — Fort a la Corne Reached, before 1763 — Cession of the Coun- try — Canadian Traders in the West — Hudson's Bay Company move Inland, in 1774 — Canadians in the Interior Nearly 100 years Before them — The Athabasca Reached by the Canadians — Hudson's Bay Company Beach E,ed Eiver, in 1793 — The Trade open to all Parties — Formation of the North- West Company, 1783 — Fort William, on Lake .Superior, their Head-quarters — Quarrels with the Hudson's Bay Company — Lord Sel- kirk Buys Shares, gets Control of the Concern, Obtains a Grant of Land, and Attempts Settlement — The North-West Company Deny his Right to the Land, and Claim Prior Rights — They publicly state their Determination to Fight — Counter Preparations by the Hudson's Bay Company — Settlers Leave for Canada, in 1S15 — Arrival of Governor Semple — Preparations to Expel the North-West Company — Both Sides Prepare for War — Forts Gibraltar and Pembina Taken by .Semple — North-West Property Confiscated — Red River Blockaded — Attempt to Provision the Boats — Governor Semple Interferes and Loses his Life — Hudson's Bay Company Account of the Fight — Opposite Account — Apathy of the British Government before the Fight — Warned Repeatedly by the North- Westers — Lord .Selkirk's Preparations — Takes Possession of Fort William — The Colony Re-established m 1817 — Troubles with tlie Grasshoppers — Union of the Companies, in 1821. In the spring of 1534 Jacques Cartier, an able and experienced seaman of St. Malo, wa.s sent out by Francis I of France to explore the northeast coast of America, and if possible find a route to India, which at that time attracted the attention of the mercantile world. In the latter part of the preceeding century Columbus and Cabot had made their celebrated voyages, and Spanish adventurers were now engaged in overthrowing the old empires of the southern HISTORY OF THE NORTH-WEST, TO 1821. 423 part of the continent. Unlike the Spanish, the English made no attempt to follow up the discoveries of Cabot, and at the time of Cartier's voyage still reposed on their laurels as the discoverers of the American continent. Prior to his voyage, in the year 1534, he had sailed along the coast from Carolina to the northern part of Nova Scotia. Cartier's intention seems to have been either to strike the coast north of this, or find the passage so anxiously sought for. Entermg the Gulf of St. Lawrence he passed between the Magdalen Isles and crossed to the Bay of Chaleurs. Landing on its shores he took possession of the surrounding country in the name of the King of France. While at Gasp^ he took on board two Indians and sailed for France. Although close to the entrance of the St. Lawrence he does not seem to have recognized the existence of the river, but learned it from the Indians he carried away. In May, 1535, he again set sail and crossed the Gulf of St Lawrence, piloted by natives of the country, possibly those he had taken away the proceeding year. After a voyage of some length he reached the Island of Orleans, where he got supplies of Indian corn, fish, and fruits He next visited Stadicona (now Quebec), and pushed on with part of his men to Hochelaga, on the same island where Montreal now stands. After ascending to the summit of the mountain on the island, and viewing thence a great extent of country, he gave the hill the nanie of Mount Royal, which has now become Montreal. Returning to the mouth of the St. Charles, where he had left his men, he prepared to winter at that point During the winter, scurvy in its most malig- nant form broke out amongst them, and one-quarter of his ships' companies died. On the return of spring Cartier sailed for France, taking with him Danacona the king of the country. The Sieur de Roberval, a nobleman of Picardy, having obtained a commission from the king and liberty to establish 424 MANITOBA AND THE GREAT NORTH-WEST. a permanent colony in the country, sent out Cartier with the colonists in 1541. He attempted to get up the Lachine Rapids, but failed, and then turned his attention to wintering in the country. In the spring he embarked his colonists for France, and meeting Roberval coming out with a larger band the two disagreed, Cartier going on to France and Roberval proceeding on his voyage. Various causes pre- vented the complete establishment of the colony, and Canada seems to have been almost forgotten for over fifty years. Acadia (Nova Scotia) had been attracting some attention during this time, but in the year 1607 the Sieur de Monts abandoned Acadia and turned his attention to Canada. The next year his Lieutenant, Champlain, laid the foundation of Quebec and the first permanent settlement was formed. At this time the Algonquins were engaged in a deadly struggle with the Iroquois confederacy. The former applied to Champlain for assistance, which was readily granted, and in 1609 the French and their allies had their first fight with the Iroquois. Firearms settled the question, and the red man fell before the murderous weapon. This one act of Cham- plain brought untold woes upon the French colonists in future years During the summer of 1615 Champlain ascended the Ottawa and crossing to Lake Nipissing, passed down French River to Lake Huron. While on this expedition he heard of Lake Superior ; but it was twenty-six years after this before a Frenchman launched his canoe on the Great Lake. Twv^' missionaries of the Society of Jesus reached the lake in 1641, or just 100 years after the first attempt at settlement Twenty-five years later, or in 1666, two French gentle- men, De Grosselier and Raddison, passed around Lake Superior, ascended the Kaministiqua, and crossed to the waters of Rainy River, down which they floated to the Lake of the Woods Following Winnipeg river to its outlet ia HISTORY OF THE NORTH-WEST, TO 1821. 425 the lake of the same name, they turned north and descending the Nelson from Lake Winnipeg to Hudson's Bay, demonstrated the existence of a water route from Lake Superior to Hudson's Bay. Before this there is no doubt but that traders had penetrated far to the north by the Ottawa and other streams, and possibly had reached the Bay. The Assiniboines seem to have been well acquainted with the route, for history informs us that they conducted >these gentlemen from Lake Superior to the sea, and brought them back in safety. On their return to Quebec they offered to conduct ships into Hudson's Bay, and by this means reach the heart of the " Pur Countries" by water, and save the canoe route by Lake Superior. Their proposal was rejected, and a subse- quent one to the French Government met the same fate. While in Paris they met the British Ambassador, who advised them to go to London. Here they were favorably received Vjy a number of merchants and persons of standing, and a Mr. Gillam, connected with the Newfoundland trade, was commissioned to prosecute the discovery Mr. Gillam sailed in the Nonsiich, ketch, in 1667, into Baffin's Bay, to the height of 75° north, and from thence southward to 51", whence he entered a river, to which he gave the name of Prince Rupert's, and, finding the Indians friendly, he erected a small fort. The persons interested in this vessel, upon the return of Gillam, applied to Charles Second for a Patent, who granted them the Hudson's Bay Company's Charter, dated the 2nd May, 1670. In the same year a Mr. Bailey was sent out as Governor and established Forts Rupert and Nelson. By the year 1686 the Hudson's Bay Company had increased their establishments to five, viz., Albany, Moose, Rupert, Nelson, and Severn. Already the French disputed their claim to sovereignty. In 1682 the Hudson's Bay Company took possession of Nelson River, and shortly after the French reached St. Therese 426 MANITOBA AND THE GREAT NORTH-WEST. or Hayes River. During the next four years there were constant disputes, and in 1686 the Chevalier de Troyes, in time of peace, took possession of the forts on James' Ba}' viz., Rupert, Moose, and Albany Factories. All the forts were captured and retaken in succeeding years. The treaty of Ryswick was signed in 1697, and left the French in possession of all forts on James' Bay, except Albany. During the next seventeen years an inconsiderable trade was carried on by the English. By the Treaty of Utrecht all the territories on the Bay were ceded to them. The tenth article of the treaty ceded all the lands and forts on the Bay to Queen Anne, but expressly sti- pulated that the " Company of Quebec and all other subjects of the Most Christian King whatsoever, could go by land or by sea, whithersoever they pleased." A wooden fort was erected at the mouth of the Churchill in 1718, and named Fort Prince of Wales Twenty-four years later we find the English ascending the Albany River and building a trad- ing post 150 miles from the coast to serve as a check to the Indians who were in the habit of ascending that river to meet the French traders. Daniel Greysolon du Luth, in the year 1678, built a small house at the mouth of the Kaministiqua and traded with both the Dacotahs and Assiniboines, and deservedly the first city at the head of the lake was named in his honor. Some Montreal merchants formed a company in the year 1731 and sent M. Verendrys and P^re Messager as their agents to Lake Superior. They were instructed to explore the coun- try, and try if possible to connect Canada with Louisiana by the Mississippi route. Pushing west by what we now call the Dawson route we find them building Fort St. Charles on the Lake of the Woods in 1732. Following down the Winnipeg River they erected Fort Maurepas on that stream in 1734, and Fort Rouge at the forks of the Assiniboine and • Red Rivers. They now ascended the Assiniboine River to HISTORY OF THE NORTH-WEST, TO 1821. 42T Portage la Prairie and crossed over to Lake Manitoba, where they erected two forts, Fort Dauphin at the head of Lake Manitoba and Fort de la Reine at its foot. Proceeding west- ward they discovered the Swan and Red Deer Rivers, and erected a fort at the head of Cedar Lake, which they named Fort Bourbon. They now entered the Saskatchewan and proceeded up the River to the forks, below which they built their last fort, which they named Fort a la Corne. This was the most western point reached by the French prior to 1763. Four years after the cession of Canada to England, numbers of British born subjects entered into the fur trade, and estab- lished their headquarters at the mouth of Pigeon River on Lake Superior. Thomas Currie wintered at the west end of Cedar Lake, in 1767-68. In 1775, Mr. Frobisher, by pushing north from Cumberland House, intercepted the Indians on their way to Churchill to trade with the Hudson's Bay Com- pany, and obtained all their furs, by the one venture clearing $50,000. Next year, his brother penetrated to Isle la Crosse, and met the Indians still nearer their winter quarters. In the spring of 1778, a number of the Saskatchewan traders put their goods into a common stock, and placed Mr. Peter Pond in charge of them, directing him to proceed to the Atha- basca and trade with the Indians He took the present Hudson's Bay Company's route, by Cumberland House, Frog Portage, Isle la Crosse, and on to the Methy Portage and down the Clearwater River to the Forks of the Athabasca. Here he built a house, and in the spring of 1779, planted garden seeds. Ninety-six years after, I visited the same neighborhood, and Pond's location was pointed out to me. As soon as the Hudson's Bay Company found that the Cana- dians were cutting off their trade from Churchill, they set about to restore it. They were compelled to carry the goods to the Indians, instead of seeing the Indians coming to the goods In 1774, Mr. Heme, the discoverer of the Copper- naine River, was sent inland to establish a trade with the 428 MANITOBA ANU THE GKEAT NORTH-WKST. Indians. lie located on Pine I.sland Lake and built Cumber- land House, from Avhicli point all supplies were passed into the north for the next hundred years. It was only in 179P> that the Hudson's Bay Company's servants reached Red River. Pushing up the Assiniboine, they built their first 'brt at the mouth of the Souris. After the cession of the country, in the year 1763, large ibrtinies were made by individuals, who penetrated the In- \lian country for the purpose of trade. Large number.s engaged in the traffic, and their mutual bickerings caused so much ill feeling, that many of the leading merchants refused to supply any more goods. During the winter of 1783-84, Lhese merchants formed a company under the name of the North -West Company. One of the leading articles of the agreement was, that the small capital of each should be thrown into a common fund, and each should share the pro- tit,« according to the amount invested. After a few years, a large number of traders .receded from the North-West Com- jiany, and formed a new one, known in Canada as the X. Y. Company. In the year 1805, a coalition was formed, and these two became one strong Company. It was now divided into 100 shares, partly held by capitalists in Montreal and London, and partly by men in the trade, called " Wintering Partners." Fort William, near Thunder Bay, was considered th(,^ seat of power, and here the partners met every year to consider the affairs of the Company. Atter the formation of the new Company, the trouble be- tween them and the Hudson's Ba}'' Company broke out into open violence, and murder and robbery were of frequent occurrence. At this time. Lord Selkirk visited Montreal, and there learned enough to satisfy him, that rich and fertile lands existed on the banks of the Red River. On his return to England, he had some conversation with Sir Alexander Mackenzie, and they both decided to buy Hudson's Bay Company's stock, which had fallen from 250 to about 60. HISTORY OF THE NOETH-WEST, TO 1821. 429 No dividend had been paid for a number of years, and every- thing was falling into decay. Shortly after this, Lord Selkirk bought out Sir Alexander, and thus became possessed of forty per cent, of the stock. The next step was the placing of a number of Lord Selkirk's friends on the Direc- torate. In May, 1811, a " General Court " was convened by public notice, aiid the " Proprietors were informed that the Governor and Committee considered it beneficial to their interests to grant in fee simple, about 116,000 square miles of what was supposed to be their territory, on condition that he should establish a colony on the grant." All present, except Lord Selkirk and the Committee, objected to this and signed a protest, but notwithstanding the grant was confirmed, and Lord Selkirk became the " ideal proprietor " of an immense territory. The North-West Company promptly " denied the right, either of the Hudson's Bay Company or Lord Selkirk, to any part of the territory ceded to him," claiming that they and their predecessors had been in occupancy for at least a cen- tury. This claim is undoubtedly true, as it was a well ascertained fact that the French colonists formed the " Beaver Company," in 1630 and traded in the country before the grant was made by Charles II, in 1670. Even the terms of the grant denied the pretensions now set up, for it ex- plicitly stated that : — " The grant only applied to countries not occupied or discovered by the subjects of any other Christian Prince or State." The Canadians to a man were opposed to the grant, on the ground of its illegality as a matter of law, and further, that the Grantors could not give what they did not possess. To us, at this date, it is simply ridiculous to read that the land granted extended from the southern end of Lake Winnipeg, as far south as lat. 46°, fully 200 miles into the United States. Furthermore, the North- .West Company stated that they would not recognize in any sense the exclusive right of trade, or jurisdiction claimed 430 MANITOBA AND THE GREAT NORTH-WEST. by the Hudson's Bay Company, and that they would resist all attempts to seize either their persons or property, or to dispossess them of their trade. Lord Selkirk was not to be deterred by these threats, but in the spring of 1811 the first instalment of twenty-five families was sent out in the Hudson's Bay Company's ships. This company passed the winter at York Factory and in the spring of 1812 started for Red River, which they reached too late in the season to do much. In the spring of the next year some farming was attempted, but seed was scarce and little was raised. Early in the winter, a large accession oi' immigrants arrived and the prospects of the settlement began to brighten. Other settlers came in during the summer of 1814 and Mr. Miles Macdonell, Lord Selkirk's deputy, who had previously trained his men to the use of arms, issued the following proclamation. — : •' District of Ossiniboia. To Mr. DunfMu Cameron, acting for the North-West Company at the Forks of Red River. Take notice, that by the authority and on behalf of your landlord, the Right Honorable Thomas, Earl of Selkirk, I do hereby warn you, and all your associates of the Nortii- West Company, to quit the post and premises you now occupy- at the Porks of Red River, within six calendar months from date hereof. Given under my hand at Red R,iver Settlement, this twenty-first day of October, 1814. (Signed) Miles Macdonell." Proclamations similar to the above were posted throughout the country, and it became abundantly evident that the Hudson's Bay Company were in earnest During the winter dissatisfaction began to show itself in the colony and numbers of settlers applied to the North-West Company HISTORY OF THE NORTH-WEST, TO 1821. 431 for assistance to leave the country . It is extremely probable, that Mr. Cameron, if not the originator of this movement, assisted the malcontents very much. In the spring of 1814 a large quantity of provisions had been taken by force from a fort of the North-West Company at the mouth of the Souris, and for this a warrant was issued against Messrs. Macdonell and Spencer his Sheriff. The one was indicted for issuing a warrant and the other for executing it. Mr. Spencer was arrested early in the winter and sent to Rainy Lake. On the approach of spring, 1815, the settlers took refuge in the North-West Company's Fort, taking with them the cannon and ammunition of the Hudson's Bay Company at the same time. The " Free Canadians " and Half-breeds were now aroused, and Mr. Macdonell quietly gave himself up. After the surrender of Mr. Macdonell the settlers came in a body to Mr. Cameron and asked to be taken out of the country. He acceded to their wishes, and fifty families were brought to Little York (Toronto). About two-thirds of the settlers having left for Canada, the other third left the Forks and proceeded north to Lake Winnipeg for the purpose of leaving the country by Hudson's Bay. During the preceding winter (1814-15), Lord Selkirk had not been idle and had sent out two expeditions, one by way of Montreal, and the other under Governor Semple by Hudson's Bay. Mr. Robertson, who came by Montreal, arrived first at Red River and remained with the settlers whom he found near Lake Winnipeg. Mr. Semple, with another contingent of settlers, arrived at Red River in September, 1815, and re-established the colony. In order to force the North-West Company to leave the country, or acknowledge Lord Selkirk's supremacy, a regular attack by armed men was made on Fort Gibraltar on the night of the 17th of March, 1816. The fort was taken, and Mr. Cameron and his people were made pri- i'-j'I MANITOBA AND THE GEEAT NORTH-WEST. soners. Three days after, the fort at the mouth of the Pembina was attacked and taken, and all the occupants made prisoners. Every thing in the shape of goods, furs, papers, and ammunition was confiscated for the use of Lord Selkirk. The two forts were levelled to the ground. An attack was made on Fort Qu'Appelle near where Fort Ellice now stands, which proved unsuccessful, Mr. Alex- ander Mackenzie, the gentleman in charge, beating off ttie attacking party. A large stock of provisions was laid up here for the use of the North canoes, and had these fallen into Governor Semple's hands, tlic North-West Gompav / would have been starved out. As tJie North canoes '. jre daily expected, iMv. Scuiplc took measun^s to prever.t them fuscending R.('d River l)y building batteries on the ■ .mks and stationing a small gunboat on Lalce Winnipe,"- The North-Westers had not been idle, I)u' liad retaliated wlien they had oppoi'tunity. An attempt was made to carry provisions from Fort Qu'Appelle to Lake Winnipeg, and an escort of (ll'ty Indiana and Half-breeds was sent with the provi,sious. Tliey were instructed to keep away on the prairie so as to pass Mr. Semple's Fort (Fort Douglas), with- out being seen, Ai"ter they had passed the Fort, Gover- nor Semple, seeing, l)y means of a telescope from a lookout on the top of his fort, the circuit made by the Indians and Half-breeds, determined to intercept them. The following is Mr. Pritchard's account oj" the tight, and it may be considered the Hudson'.s Bay Company's version ; — '' On the afternoon of the 19th .Tune, a man in the watch- house, called out that the Half-breeds were coming. The Governor, some gentlemen, and myself looked through spy- glasses and saw distinctly some armed people passing along the plains. A man then called out, " they " (meaning the Half-breeds), ''are making for the settlers;" on which the Governor said, " we must go out and meet these people, let twenty men follow me." We proceeded by the old road HISTORY OF THE NORTH-'WEST, TO 1821. 433 leading down to the settlement. As we were going along we met many of the settlers running to the fort, crying " the Half-breeds, the Half-breeds." When we were ad- vanced about three quarters of a mile along the settlement, we saw some people on horseback behind a point of woods. On a nearer approach the party appeared to be more numer- ous, on which the Governor made a halt and sent for a field piece, which, delaying to arrive, he ordered us to advance. We had not proceeded far before the Half-breeds on horse- back, with their faces painted in the most hideous manner, and in the dress of Indian warriors, came forward and sur- rounded us in the form of a half-moon. We then extended our line and moved more into the plain, and as they advanced, we retreated a few steps backwards and then saw a Canadian named Bouchier ride up to us waving his hand, and calling out, " What do you want ? " The Governor replied, " What do you want ? ' ' To which Bouchier answered, " We want our Fort," to which the Governor said, " Go to your Fort." They were by this time near each other and consequently spoke too low for me to hear. Being at some little distance to the right of the Governor, I saw him take hold of Bouchier' s gun and in a moment a discharge of fire-arms took place ; but whether it bi'^^an on our side or by the enemy it was impossible to distinguish. My attention was then directed towards my personal defence. In a few moments, almost all our people were killed or wounded. Captain Rogers having fallen, rose up again and came towards me, when, not seeing one of our party that was not either killed or wounded, I called to him, " For God's sake give yourself up." He ran towards the enemy for that pur- pose, myself following him. He raised up his hands, and in English and broken- French, called out for mercy ; a Half- breed, son of Colonel William McKay, shot him through the head, and another ripped open his belly with a knife while uttering the most horrid imprecations. Fortunately for me, 28 434 MANITOBA AND THE GREAT NORTH-WEST. A Canadian named Lavigne joined his entreaties with mine and saved me, though with the greatest difficulty, from sharing the fate of my friend at that moment. I was rescued from death, in the most providential manner, no less than six times, on my road to and at the Frog Plain, the head-quarters of these cruel murderers. No quarter was given to any of the party, except to myself. The knife, the axe, or the ball put a period to the existence of the wounded ; and such horrible barbarities were practiced on the bodies of the dead as characterize the inhuman heart of the savage. The mild and amiable Mr. Semple, lying on his side, his thigh broken, and supporting his head on his hand, addressed the chief commander of our enemies by in- quiring if he was Mr, Grant, and being answered in the affirmative, said, " I am not mortally wounded, and if you could get me conveyed to the Port, I think I would live." Grant promised to do so ; and immediately left him in the care of a Canadian, who afterwards told me that an Indian of their party came up and shot Mr. Semple in the breast. I entreated Mr. Grant to procure for me Mr. Semple's watch or seal for the purpose of transmitting them to his friends, but I did not succeed. " Our force amounted to twenty -eight men, of whom twen- ty-one were killed and one wounded. These were Governor Semple, Captain Rogers, Mr. James White, Surgeon ; Mr. Wilkinson, private Secretary to the Governor ; Lieutenant Holt, of the Swedish navy, and Mr. Alexander McLean, a settler, with fifteen laboring men. J. J. Bourke was wound- ed in his retreat to the Fort. The enemy, I am told, were sixty-two in number, the greater part of Avhom were the regularly engaged clerks and servants of the North- West Company. They had one man killed and another wounded. On the field I saw six of the North-West Company's Cana- dian servants, viz. : Bouchier, Morin, Deschamp, Joseph Hesse, Magian, and Lavigne." HISTORY OF THE NORTH-WEST, TO 1821. 435 We shall now give the North-West Company 'a version of the affair at the Seven Oaks, which is corroborated in almost every particular by the settlers who were in the colony at the time. This version states, that on meeting the Hud- son's Bay men, the Half-breeds sent one of their number, a Canadian named Bouchier, who spoke English, to enquire of the Governor, his object in pursuing them in a hostile man- ner. Bouchier rode up to the Governor, and some words passed between them, upon which Mr. Semple took hold of Bouchier' s horse by the bridle, disarmed him and ordered him to be taken prisoner. Bouchier attempting to es- cape, the Governor ordered his men to fire immediately at him ; and when his people hesitated, because of the danger they would inchr in such a conflict, he was more peremptory in his commands, accusing them of cowardice for not imme- diately obeying him. His orders were at last obeyed by some of his party, and of the shots fired, one grazed Bouchier's ear in his flight, and another passed through the blanket of an Indian advancing in the attitude and with the lan- guage of friendship. Seeing himself thus treacherously assaulted, the Indian levelled his guu and fired in return, which example his party followed, and the melancholy result of the conflict was that the Indians rushing in, Mr. Semple and about twenty of his people lost their lives. One Haljf-breed and an Indian were killed on the other side. Both parties seemed to feel that a crisis was approaching in 1816. Lord Selkirk arrived in Montreal, in the fall of 1815, and at once commenced to enlist men for service in the interior, but to the world generally he referred to them as settlers on his Red River Lands. The war had ended between the United States and England, and the two .regi- ments, De Meuron's and De Watteville's, were disbanded. A-bout 140 men belonging to these regiments were enlisted, and with all the pomp and circumstance of war they started in canoes from Lachine. 436 MANITOBA AND THE GREAT NORTH-WEST. During the winter, the North-West Company oiFered to enter into terms of union with Lord Selkirk, but he paid no attention to them. Feeling assured that his intention was to crush them, they appealed to the Government, and in a letter written to the Secretary of State, on February 1st, 1816, occurs this passage : — " We do not presume to point out the particular proceed- ing which, in this case, would be satisfactory to ourselves. Our sole object is to put an end to violence and bloodshed, and we are perfectly satisfied that, in the discussion to which such proceedings must give rise, the interests of His Majes- ty's Canadian subjects will, at least, meet with as favorable consideration as those of their opponents." Again we find them applying to the same official, in a letter dated March 1st, 1816, in which they say : — " We do not venture to suggest the remedy it may be in their power, or may appear eligible to His Majesty's Gov- ernment to provide in this case, but we are certain if some measure be not adopted to define, without delay, the limits, power, and authority of the Hudson's Bay Company, a con- test will ensue in the interior, the results of which will be dreadful with respect to loss of lives and property." They also enclosed the correspondence which passed the preceeding winter between their agents and Lord Selkirk. The Government were slow to act, and paid no heed to their appeals. In the meantime, his Lordship had got himself appointed a Justice of the Peace for the Indian Ter- ritories and Upper Canada. A military escort, under the name of a body-guard, consisting of a Sergeant and detach- ment of the 37th Regiment, were also given him. In the instructions to this guard, it was distinctly stated that they were to interfere with neither party in their quarrels, as both parties had equal rights in the country. After a careful examination of all the material at hand, I can only come to the conclusion — that both parties were HISTORY OF THE NORTH-WEST, TO 1821. 437 lawless, that each of them was deteripined to wipe out the other, and that each was willing to use the Indians and Half-breeds to carry out its purposes. Lord Selkirk, who was not a fur-trader, wished to settle the country and en- courage agriculture, while the North-West Company desired to preserve the fur-trade. Miles Macdonell, who had gone up to Red River in the spring, reached there a few days after the fight, and at once returned with the news to Lord Selkirk, whom he met at the entrance to Lake Superior. On receipt of the news, Lord Selkirk immediately headed for Fort "William, the headquarters of the North-West Company, where he seized everything in the Fort, and converted it to his own use. Besides appropriating the goods, he took all the officers pri- soners, and in every way conducted himself as a conqueror. During the winter the Fort, on Point Douglas, was sur- prised, and again Lord Selkirk reigned at Red River After the fight, in June, the settlers retreated to Jack River at the foot of Lake Winnipeg. They remained there until the spring of 1817, when an express arrived with the news that the fort was taken and they were invited to return. In hopes that peace might finally be established, they retraced their steps and commenced work anew, but there was not a plough in the colony, and all the work had to be done with the hoe. His Lordship now set to work to consolidate the colony, and in August, 1817, each of the settlers obtained his land. The settlement was named Kildonan, after their old parish in Scotland. Peace had now been ratified by the Imperial Commissioners, and the people thought their troubles at an end ; but on the 18th of July, 1818, clouds of grasshoppers settled down on the colony and ate up every green thing. Again they had to retreat to Pembina where they had lived^ the proceeding winter, and to hunt the buffalo for their subsistence. Farming was tried in the spring of 1819. 438 MANITOBA AND THE GREAT NORTH-WEST. but again the crops were eaten up by grasshoppers. Many of the young men had now become good hunters, and no fears were felt when they saw their hopes blasted for another season. Retreating once more to Pembina, they subsisted by the chase all winter and laid up a store of food for the coming summer. The country still being alive with grasshoppers no land was cultivated in 1820, and all lived on the products of the chase, or upon fish caught in the rivers or lakes. In February 1821, a party started for Prairie du Chien, under the command of a Mr. Laidlaw, and purchased 250 bushels of wheat. This they loaded on fiat boats, and when the ice left the Red River in spring, floated it down to the colony. This was sown and a good crop followed, and the food troubles of the Red River settlements were at an end. Both parties now began to see the error of their ways, and negotiations were entered into which terminated with the amalgamation of the two companies in the year 1821. Up to the time of the union the greater part of the exploring and mapping out of the country was done by the North- West Company, and no matter what may be said to the con- trary, the honor of exploring this country to the Pacific belongs to Canadians. Thompson, the geographer of the Company, named and laid down many rivers, and gave as our first knowledge of British Columbia. Others navigated the Fraser and Columbia, established posts on both rivers, traded with Japan and China, and sent vessels round Cape Horn. By the co-partnership entered into (March 26th, 1821,) it was agreed that forty shares of the one hundred, into which the company was divided, should belong to the North- West Company, and sixty to the Hudson's Bay Company. This agreement was to continue for twenty -one years. In 1834 this agreement was re-affirmed and it was decided to continue it for an unlimited period. CHAPTER XXV. History from 1821 to 1870. Arrival of the Swisu— Settlement of the old Hudson's Bay Company's Servants— Terri- ble Winter of 1825— Disastrous Flood of 1826— Emigration of the Swiss— Red River Colony Prosperous — Sir George Simpson's Policy — Attempts at Various Industries — Sheep Farming— Cause of Failure— Lord Selkirk's Title to the Land Reverts to the Hudson's Bay Company— Farming Tried on a large Scale— Schools Established- Everything Done to Prevent Successful Farming— Half-breeds Frighten the Com- pany — The Council of Assiniboia Formed — Duty Imposed on Imports and Exports Regulars Sent into the Colony— People Petition for then- Rights— They take the Law into their Own Hands and Trade becomes Free- Red River Flood of 1852 — Captain Palliser's Expedition — Expedition under Dawson and Hind — Arrival of Dr. Schultz The i^'br- Wester Established — Hudson's Bay Company's Opposition — The Dominion Established — A Demand made for the North-West Territories — Country Systemati- cally Be-littled — Bishop Tache's Book — He sees no Good in the Country — Purchase of the Territory — Steamboat on Red River — Dr. Schultz Imprisoned — The Power of the Company Broken — Portage la Prairie — Grasshopper Plagues — Canada Takes Steps to Acquire Possession of the Country — Conflicting Interests — Mutteringsof the Stoi-m in the Fall of 1869— The Claims of the French Half-breeds — Sui-veyors Stopped by Louis Riel — Hudson's Bay Company and Roman Catholic Fathers Decline to Interfere — An attempt at Independence — Fort Garry given up to Riel — Governor McTavish's Explanation — His Evident Complicity with the Rebels Almost Admitted — His Child- like Simplicity — O'Donohue Joins the Rebels — He Introduces the Fenian Element — His Letter to the Canadian Government — Bill of Rights drawn Up — The Movement is seen in its proper Aspect — Canadians Attempt to break Riel's Power — Their Imprison- ment — Murder of Scott — Arrival of Bishop Tache — Riel changes from a Wolf to a Lamb — Fenian Flag Pulled Down — Arrival of Colonel Wolseley with his Troops, and Flight of Riel and Lepiue — Conclusion. A NUMBER of poor Swiss were brought to the colony in the fall of 1821, but these being altogether unacquainted with manual labor sujffered severely. Before they reached the colony winter had set in and they suffered frightful hard- ships while on Lake Winnipeg. When they arrived food was very scarce, and in December a move was made to join the hunter's camp beyond Pembina. Being without either horses or dogs they harnessed themselves to the sleds and drew their children and household effects the whole distance. Spring found all at work and a larger 442 MANITOBA AND THE GREAT NORTH-WEST. area "was planted than ever before. Good crops followed and all had abundance of food. After the union of the two companies a number of the old servants either left the service or were dismissed. Most of these men had wives and families, and therefore resolved to settle in the country. A survey of the " River Lots " had been made in 1822 by a Mr. Kemp, and at this time all lots were reduced to eight chains frontage and extended back 160 chains to the rear, each lot containing 128 acres. Laborers were entitled to one lot each, and other servants according to their standing. By this influx of settlers the colony was more than doubled and the area of the settlements widely extended. " The Swiss, in 1821, settled among the De Meurons, on the Riviere la Seine, which takes its rise in the forests to the east, and falls into the Red River about a mile below the confluence of the Assiniboine River with the latter. Others of the Swiss had settled on the Red River above the Forks. The refugees from Pembina squatted down near the Swiss. The Scotch occupied what is now divided into the Parishes of St. John and Kildonan. The Protes- tants arriving in the settlement extended down along the Red River, and occupied the Parishes of St. Paul and St. Andrew" * As time passed the French Half-breeds came in from the Saskatchewan, and settled on the Lower Red River and at White Horse Plains. The fall of 1825 was ushered in by a cold and wet Sep- tember, followed in October by heavy snow, which covered the plains to a great depth. In December a terrible snow storm came on, which lasted three days and four nights, and drove the buffalo far to the south. The plain hunters prior to this had been in great distress, owing to the depth of snow and the weakness of their horses. This storm deprived them of food, and they at once commenced to make their way to Pembina. Rumors reached the post * Guim's History. HISTORY FROM 1821 TO 1870. 443 that the hunters were starving, and steps were immediate- ly taken to render assistance. Men were despatched with provisions over the snow covered plains, and many were rescued when at the last extremity. Before assistance could be rendered to all, not less than thirty men, women,, and children perished in the snow from hunger and cold. As soon as the weather turned warm, the river began to rise, and by the 2nd of May, the accumulated waters had overflowed the banks and began to submerge the surround- ing country. Before the day closed, the entire district was changed into a huge lake, and most of the settlers had deserted their homes. At the Forks of the Assiniboine and Red River (Fort Garry), the river rose nine feet in twenty-four hours. By the 21st of May, the waters were sixteen feet above high water mark, and the Red River Plain was a vast lake. The flood, after this date, began to subside, and by the middle of the month of June, the waters had left the land, and the inhabitants returned to their desolated homes. In too many instances the sites only remained, as the houses had disappeared in the flood. Scarcely allowing the land to dry, the settlers went to work with a will, and sowed wheat and barley, and planted potatoes, all of which came to maturity, though planted after the 20th of June. The Swiss and De Meurons, having become disgusted with the country, determined to go to Fort Snelling, in the United States. On the 24th of June, the emigrating party to the number of 243 started on their arduous journey. They reached their destination in safety, and the Swiss set- tled down on the Upper Mississippi and became prosperous. The Red River Colony prospered during the next few years, and far more grain was produced than was required in the country. Up to 1832, the Hudson's Bay Company brought in all the goods, but about this time, a few private gentlemen began to bring in goods, which they sold to the 444 MANITOBA AND THE GREAT NORTH-WEST. settlers at a handsome profit. Seeing this, the Company changed their tactics and encouraged agriculture, promising a market for everything produced. At first, land was sold for five shillings per acre, but now it was increased to seven shillings and six pence, and was difficult to obtain. In a short time, the settlers had a large surplus on hand, and Sir George Simpson saw it was time to put a price on farm produce. Convening a mercenary and subservient Council, he had his regulations passed, and at one sweep prices fell from 100 to 300 per cent. All the articles required by the settlers remained as they were, and the people grumbled long and loudly over the change, but had to acquiesce. Various attempts were made to establish industries other than farming, but from one cause or another they failed. The growing of flax and hemp was tried and succeeded re- markably well, but the settlers being ignorant of its after management very little of it was utilized. A cattle farm on a large scale was next attempted, but this too proved a failure, as the severe weather, want of proper care, but prin- cipally the wolves, which then abounded, decimated the herd, and that business was given up. Sheep farming on an extensive scale was next attempted, and as the experiment is one that has been spoken of to prove the unsuitableness of the country for such occupations, I give it in the words of a late author. The sheep were purchased in Kentucky, and what follows took place on their way to the Red River Settlement. It will be seen that the reference to the grass with " barbed spines" wholly refers to Dakota, as it was in passing through that State the sheep died. The story with many embellshments has been transferred to our North- West, and is used by many as a reason why sheep farming will not pay. It is quite evident that the grass was made to do duty to cover the brutality of the parties in charge who condemned every sheep to death when it showed any signs of exhaustion. HISTORY FROM 1821 TO 1870. 445 " After a variety of adventures and loss of time the party reached Kentucky, and found that the price of sheep there differed very little from what they could have bought them at in Missouri, being from five shillings to seven shillings a head. Here the number acquired were, 1,475, but on the way back they began to meet with the difficulties that the sagacious Bourke foresaw and foretold. They had to pay for pasture every night and whenever they halted during the day, besides many sheep died from the effects of hard driving. On their way up the Mississippi they gave another instance of the wisdom of their management ; they saw that the sheep were suffering from the burden and heat of their fleeces, and at a certain place they halted to clip them, and agreed with a certain individual to let him have all the wool at a fixed price. The following day the wool was to be delivered and the money paid, but the indi- vidual not being able to raise the full amount, could not get wool to the value of the cash he had. At the same time a number of poor people had collected about the place and made several offers, according to their means, for portions of the wool ; but their united offers falling short of the original valuation they were rejected with contempt, and the wool was ordered to be burnt on the spot, which indi- cated neither wisdom nor humanity. The former would say, sell the wool for what the people are able to give for it, which in all probability would have amounted to a few hundred dollars ; the latter would say, if the people be too poor to buy, better that it should clothe the needy than that it should be burnt. Giving it away might answer a good object; it could not fail to enlist in their behalf the friend- ship of those among whom they were travelling, which, no doubt, would be of some value. Had the sheep been pur- chased in Missouri they might have been in Red River before the excessive heats of July and August had come on, and before the tall coarse grass on the plains had come to its full height. 446 MANITOBA AND THE GREAT NOETH-WEST. " Many localities on those plains produce a species of plant which, in its native state, is armed with sharp barbed spines, which penetrated the sheeps' skins as they walked through the grass, and finally caused death, which with over-driving killed the helpless creatures by tens and by twenties every day. It was currently reported and believed that 1,200 of these over-driven and helpless animals perished from the cause already referred to, or by the knife, between St. Peter's and Pembina. It is distressing to relate that every sheep that failed to keep up with the flock was doomed to have its throat cut by order of the men who had so un- fortunately been trusted with their safety. The agents in these butcheries did not hesitate to inform the writer that in one morning only, while at breakfast, the bloody knife deprived no less a number than forty-four of life. The leaders, as became men in their positions, rode in advance of their chai-ge, and every now and then the men would have to ride up to them with the news that so many of the sheep could not be made to move on. ' Cut their throats and drive on,' was the invariable order. A few days' rest, say one iu seven, would have enabled these worn out animals to recruit their strength, or even a few hours each alternate day allowed them to rest and feed, might have enabled many of those whose lives had been cut short by the knife to perform the journey. On their arrival at the top waters of Red River they came to a camp of Sioux, or met with a party of that nation, who received them kindly. These Indians were headed by the great war chief Wanata, who, with a number of his braves, escorted them and hunted for theJn until they arrived at Pembina; yet such was the intensity of their longing for home that even while protected and provided for by the Great Chief, they drove on without stop or stay, heedless of the wanton and barbarous butchery of many of their charge every day, which so disgusted the drivers that they refused to use the HISTORY FROM 1821 TO 1870. 447 knife any longer in shedding innocent blood, leaving the business in the hands of their superiors. However, they arrived in the settlement in the latter end of September, with 251 sheep, a few of which died afterwards in con- sequence of the hardships they had undergone by the way." In 1835, the Hudson's Bay Company purchased, from the young Earl of Selkirk, all right and title to the grant made to Thomas, Earl of Selkirk, in 1811, for the sum of =684,000. This was done to give the Companj' undivided control 01 the land and government of the country. Not satisfied with their repeated failures, the Company, in the year 1836, made another attempt at farming and this year imported a tew lamilies from the Old Country. Wonders were now to be performed, and in the spring of 1838, about twenty acres were ploughed and put under crop, but from this little more was reaped than fed the experimenters. The home market still remained open, and farmers had the privilege of selling eight bushels a year to the Company, if they had no other way of earning a shilling. " Hunters and trip men were tavored with a market for four bushels from each, at three and six pence per bushel. Importers and mechanics could sell no grain at the Company's stores, which state of things shows conclusively that the settlers raised abundance of grain for their own use, and in the aggregate ten times more than the market demanded. Yet, as soon as Chief Factor McMillan had left his establishment. Captain Gary was on nis way to form another — and all for the benefit of the Colony." " We may ask here, was such a project calculated to benefit the settlers ? We do not hesitate to say that it was not ; but that its success would have closed against them the limited market that they had hitherto, and might have been the means of sending numbers of industrious men to seek homes in other lands. 448 MANITOBA AND THE GREAT NORTH-WEST. " The Company, we believe, was favorable to the Colony. while it existed on a small scale, as it supplied that body with provisions and men in the heart of their trading dis- tricts, and helped to give a tone to its proceedings at home, which edat that politic body knew well how to turn to serve its own purposes, as is to be seen by the reports sub- mitted to the Colonial Office, in 1836 and 1837, by Gover- nors Simpson and Pelly, when soliciting the renewal of license. These gentlemen did not scruple to claim the merit of having some Catholic and two Protestant Mission- aries, with thirteen schools in Red River. We know that the late Bishop of Juliopolis received a salary from the Company, and so did, as we have said, the two Missionaries of the Church of England. The High School at St. John's was patronized by the wintering partners, whose children were the only pupils that were admitted, and on it the fur trade Council bestowed an annual grant of .£100 ; but the unfortunate twelve schools, where the plebeian multitude received all the education that fell to their lot, were unen- dowed, and even unknown to the nabobs of the fur trade ; yet, the two Governors dragged them in to do duty on the above occasion, as well as the experimental farms." During the year 1835, the Half-breeds, on account of one of their friends being ill-treated, made a demonstration against the Hudson's Bay Company, and so frightened the Officers that they yielded to most of their demands, and as a consequence, they became more over-bearing than ever. " In the following spring, another physical demonstration took place before the gates of the Fort. A number of demands were made, as follows : 1st. The prices of pro- visions were to be raised. 2nd. An export was demanded for tallow, robes, and other articles procured by the chase. " They loudly protested against any import duty being levied on goods imported from the United States, for many HISTORY FROM 1821 TO 1870. 449 French Canadians and Half-breeds, both French and Eng- lish, had already made several trips to the Mississippi, exporting horned-cattle, horses, furs, and some articles of Colonial industry, and, on their return, bringing home cotton goods, groceries, ammunition, tobacco, etc., etc. " These bold adventurers considered themselves entitled to exemption from import duty on two grounds : 1st. On account of their having established commercial intercourse with the neighboring States. 2nd. On account of the great danger incurred on their journey to and fro. Their demand fell on deaf ears, the Colonial Governor and his Council were exclusionists and all interested to defeat every at- tempt to export the produce of the country, or to introduce foreign manufactured goods, except via Hudson's Bay. Yet these hostile demonstrations and demands were not unpro- ductive of some advantage, especially to intending settlers, as the salutary fear which they impressed on our men in power, was the cause of reducing the price of land from twelve shillings and sixpence to seven shillings and six- pence. And at the same time, to please the native youth, it was decided by the land agents, that each young man on settling on land should receive twenty-five acres gratis." The population of the country had increased so much at this time, that Sir George Simpson, who was then Governor, decided on forming a Council of the leading men of the settlement. None were chosen except those who were either in the pay of the Hudson's Bay Company or had been at some time connected with them. This circumstance caused the settlers to look upon it, if not with suspicion, with very little confidence. At this meeting, it was de- cided to raise a volunteer force, to divide the country into districts, tO appoint Magistrates, to organize Civil and Criminal Courts, and to erect public buildings. At the close of the session. Sir George Simpson announced the grant of £300 by the Company, in aid of public works at Red River. 29 450 MANITOBA AND THE GREAT NORTH-WEST. This gift came at a very opportune time, as it enabled the authorities to build a Court House and Goal. It was also decided to charge a duty of Tg per cent on all goods of foreign manufacture imported into the Colony whether for sale or for use, and still worse they decided to charge an export duty of Yg per cent on all goods, provisions or live stock, being the growth, produce, or manufacture of the Red Eiver Colony. The impartial reader at this date sees in whose interests these laws were made and the ardent desire the Company had to encourage home production. Before this time (1836) considerable trade had taken place between St. Paul in Minnesota and the Red River colonists, and they saw or thought they saw the destruction of their trade aimed at by the late enactments. The French Half- breeds and Canadians had never taken kindly to the rights or assumptions of the H. B. Co'y, and they writhed under the export duty and took every opportunity of evading it. Fearing that an outbreak might take place a large force of regulars was sent out and quartered in the colony in the Autumn of 1864. After remaining two years they were ordered home and 140 pensioners sent up to take their place. The coming of the soldiers gave new life to the colony and almost for the first time money circulated in the neighbor- hood of the future Winnipeg. Mr. Isbester of London, who was a native of the colony commenced at this time an agitation in favor of the country and interested a large number of the British House of Com- mons in its favor. Petition after petition had been sent home craving the right of trading with the Indians, but no redress could be obtained. Tired of quiet submission they waited for a chance of asserting their rights by force and it came, and, as in 1816, the Company and the Government awoke. "In the spring of 1849 William Say re, a French Half- breed, had been arrested and imprisoned for trading furs. HISTOEY FROM 1821 TO 1870. 451 Three other Metis — McGinnis, Laronde and Guillette — had been arrested on the same charge, but held to bail to stand their trial at the first criminal court. The charge against them, namely, their accepting furs from the Indians in ex- change for goods, was considered as contrary to the rules of the Company's charter, wherein it is stated the Hudson's Bay Company shall have the sole trade and commerce of all the territories within Rupert's Land. For some time it had been rumored that the party to which the culprits in question belonged were preparing to resist any attempt at the punishment of these men by an armed force, and on the 17th May, on the day appointed to sit upon this celebrated case, the Metis were seen collecting in armed bands from all parts of the country. This movement took place about half-past ten o'clock. Those in command of these armed parties simply stated the object of the gathering to be to resist the infliction of any punishment, whether fine or imprisonment, upon the offenders. They conducted them- selves in the most orderly manner, merely surrounding the Court House, and by their presence showing their intentions. It is to be noticed that there was no attempt on their part to interfere with the trial, now about to be in progress; nor was there any attempt made to rescue the prisoners from the hands of the Authorities. When the trial proceeded, Sayre confessed that he had traded furs with the Indians. A verdict of "Guilty" was found against him, and there- upon Sayre proved that one of the ofl&cers of the Hudson's Bay Company had given him permission to trafi&c ; and on this pretext he was discharged. The cases of McGinnis, Laronde, and Guillette were not proceeded with and they all left the court together, greeted with great applause. " It was perfectly patent to the Half-breeds who were directly interested in the trial of this suit, as well as the white settlers, who looked with very considerable interest upon it, that the Hudson's Bay Company fearing to provoke 452 MANITOBA AND THE GREAT NORTH-WEST. a collision, which they knew must inevitably occur, had made use of a subterfuge to quietly get Sayre out of the scrape, with at least the semblance of the dignity of the law ; and so firmly were all convinced that at least this arbitrary in- justice of right was forever broken that the cries of " Vive la liberte" and "Trade is free " were heard from all sides. Guns were discharged, hands were shaken, and three volleys given in testimony of the victory." In 1851 Governor Ramsey, of Minnesota, visited Pembina and made a treaty with the Sioux for the extinction of their claims to the land. On his return to St. Paul he re- ported that the Red River settlers were raising so much and had such a limited market that they were metaphorically speaking " smothering in their own fat." The year 1852 was another black-letter year. Early in May the river began to rise and by the 7th it was eight feet above the usual high-water mark. It continued to rise until the 22nd when it reached within eighteen inches of the flood of 1826. Again the people had to leave their homes and wide-spread ruin met them on every hand, but by the 12th of June many were back to their fields and at work putting in a little crop. By the end of the year it had almost passed from the minds of the people and all things went on as usual. A census of the colony was taken in 1849, which showed it to contain 5,391 inhabitants of all ages and nationalities. Of live stock there was 2,085 horses and mares, 6,014 cattle of all ages, 1,565 pigs, and 3,096 sheep. There were likewise 6,329 acres of land under cultivation. These figures show that the colony had made very material pro- gress, and was not as many yet believe, a land where live stock could not thrive owing to the severity of its Arctic winters. Although 3,000 sheep were in the colony thirty- two years ago, many say in our day that the country is un- guited for them, and they cannot survive the long winters. HISTORY FROM 1821 TO 1870. 453 The fullness of time arrived in 1857, and the Imperial Government sent out an expedition under Captain Palliser, which explored the greater part of the interior, and during three years gathered sufficient material to warrant him to report favourably on the country, and through his as- sistants Doctor Hector and Mons Bourgeau to give the outside world a knowledge of its geology and botany. He reported highly on the Saskatchewan country, and since his day it has been called the " Fertile Belt." In the same year (1857) the Legislature of Canada fitted out an expedition, and placed it under the command of S. J. Dawson, C.E., and Professor Henry Y. Hind. During the succeeding two years these gentlemen examined the country between Lake Superior and the South Saskatchewan. Their report, which was published in^ 1859, -attracted much atten- tion, and a number of Canadians were induced to settle in the country. Among others who went there at this time was Dr. Schultz, then a student of Queen's College, Kingston. Being at that time under the tuition of Dr. George Lawson, now of Dalhousie College, Nova Scotia, he had imbibed an ardent love of botany, which was the favorite pursuit of that gentleman. While crossing the, plains from Crow Wing to Pembina he made a collection of plants which attracted my attention and led me to study the geographical distribution of plants. The result of this investigation showed me that the summer climate of the Red River country was suitable for the growth of all cereals. In after years I had the opportunity of proving this. The same year that Dr. Schultz came to Red River two Canadians — Mr. W. Buckingham and Mr. Caldwell — brought in a printing press. The end was now approaching rapidly, and the ever astute Hudson's Bay Company saw it, and at once set to work to counteract the effects of d newspaper. Efforts were made to induce the people not to patronize the " Nor' -Wester," the name given to the newspaper, but 454 MANITOBA AND THE GREAT NOETH--WEST. these failed. While the printing press was doing its work another power was rising which soon swept down the bar- riers that interest and ignorance had raised against a better acquaintance with the west. In 1867 Canadian patriots established the Dominion of Canada, and at once a cry was raised for our rights in the west. A determined stand was now made, and most extraordinary stories were told in England before a Committee of the House of Commons,^ showing that the country was little better than an iceberg. In 1868 Bishop Tach6 published his sketch of the North- West, and he, too, like the Hudson's Bay Company, looked upon the country as scarcely suited for civilized man. Its rivers were unsuited for navigation, and its climate hyper- borean. Not one section is spoken of as being suited to a farming community. Indeed on page sixty-three, when discussing the probabilities as to who the future owners of the country would be, he says : — " For my own part, as there are extremely great difficulties in the way of colonizing the few points in this vast territory capable of cultivation, I acknowledge frankly that I would as soon — perhaps prefer- ably — see the country remain as it is as see it change, if the changes are to be such, as it appears to me, they would inevitably be." The italics are mine. The Bishop had lived many years in the country, had seen more of it than any other man, and in 1868 he writes as above, yet he had read Lord Selkirk's statement made fifty-five years before that the country was capable of supporting 30,000,000 of people. Neither the avowed desire of the Bishop nor the representations of the Hudson's Bay Company could prevail on Canadians to relinquish the desire to obtain this useless region, so the Imperial Government took the matter up, and the Hudson's Bay Company's rights were purchased for £300,000 sterling. Although the country was of no value for farming purposes, according to their own showing, they took care to reserve one twentieth of the HISTORY FROM 1821 TO 1870. 455 " Fertile Belt," when they disposed of the remaining terri- tory, and now advertise 7,000,000 acres of land for sale as their share of it. But to resume, the advent of a few Canadians and the establishment of a newspaper began to work wonders. In 1862 a light draft steamboat was placed upon the river, but the Sioux massacre taking place a little later so unsettled everything that it was not a success as a commercial venture. Public opinion was constantly becoming more opposed to the rule of the Hudson's Bay Company, and measures had to be adopted to counteract this. Dr. Schultz having got control of the " Nor' -Wester," became very out-spoken against the monopoly, and measures at once were taken to silence him. In February of the year 1866 he was brought before the Quarterly Court on an action of indebtedness for £300 sterling, but in the absence of the prosecution the case was deferred. The case was brought on again in May, but Dr. Schultz desiring to plead his own cause, and the court not allowing it, judgment was given against him without trial. In the spring of 1867 a large and influential petition was sent in to the Hudson's Bay Company's authorities asking to have Dr. Schultz appointed on the Council instead of Mr. Caairs, a councillor lately deceased. " So strong was the petition in question that it was felt that this man must be got rid of in some way or another." History is said to re- peat itself, and now after a lapse of fifty years the l^orth- West Company (Canada), as represented by Dr. Schultz, stands face to face with the Hudson's Bay Company. The sheriff, with a posse, proceeded to the trading post of Dr. Schultz in February, 1868, for the purpose of putting in force the judgment of the court recorded against him in May, 1867. A scuffle ensued and the sheriff and his men were ejected, but shortly after the Doctor gave himself up, and asked to be tried by the authorities. Tuttle, in his history of Manitoba, thus describes the sequel : — 456 MANITOBA AND THE GREAT NOKTH-WEST. " The authorities, believing him'to be a dangerous subject, bound him securely with ropes and conveyed him in a cari- ole to the Hudson's Bay Justice of the Peace, before whom he was charged with having assaulted the sheriff in the dis- charge of his duty. He admitted that he had defended his property in the absence of any legal method of protection to resist the judgment of the court given against him with- out the intervention of a jury, and in which he had no opportunity to plead his case ; and stated that he was willing to abide by the result of a new trial, if a new trial before a jury of the inhabitants was granted. The Hudson's Bay Company, however, finding their dangerous enemy in their power, forthwith consigned him to prison. This occurred early in the day, and before night the inhabitants in the neighborhood, to whom Dr. Schultz had been endeared by his steadfast advocacy of their rights, and his intrepid con- duct under oppression, immediately collected, and after an imprisonment of four hours he was released by them, after they had torn down the jail walls and battered in the prison door. The large number who had collected for this purpose were thoroughljf excited, and proposed to visit in a body the Hudson's Bay Company authorities, who, from the walls of their fort had witnessed the breaking in of the jail, which was only a few yards distant. The Doctor, however, calmed their feeling by proposing to go alone and unattended, to visit within the fort walls the magistrate who had submitted him to such ignominious procedure. This he did, and stated distinctly that he was still willing to undergo a trial on the charge brought against him, and to give bonds for the pay- ment of the amount if judgment should be rendered against him. No attempt was made to recapture him or any of his friends on this occasion, but later, in the month of January, the General Council was held to consider the critical position of the Hudson's Bay Company's rule in the country ; a reso- lution was arrived at to embody a force of 100 special con- HISTORY FROM 1821 TO 1870. 457 stables, to be organized into a permanent force. Once raised, however, the authorities felt that public opinion was so strong against them in the Schultz matter, that they re- frained from using their newly acquired power, and on the 10th of the following month, thought it better to accede to the Doctor's request and grant him a new trial. At this trial, which was conducted in the ordinary form of jury trials, he was allowed to plead his own case, and received, amidst the unanimous acclamations of the spectators, a ver- dict in his favor without one dissenting voice ; it having been distinctly proven that the claim made of £300 against him was entirely without foundation." Assiniboia, as it was called, extended in every direction for fifty miles from Fort Garry. Outside of this limit, the settlement of Portage la Prairie had been formed by the Venerable Archdeacon Cochrane, who objected to the rule of the Hudson's Bay Company. Matters went well for a while, but disturbances taking place, it was thought ad- visable to set up a government of their own, which was organized by Mr. Thomas Spence. No other end was sought in this organization than mutual protection. As soon as the Imperial Government was made aware of what the people had done, it notified Mr. Spence how far he could go without breaking the law. The people now demanded with one voice the privilege of electing Councillors to fill the vacancies caused by death or resignation in the Council of Assiniboia. For two or three years, grasshoppers had ravaged the Colony, but m 1868, they entirely destroyed the crop, and starvation stared the inhabitants in the face. An appeal was made to the outside world for aid, England sending £3,000, Canada, £3,600, and the United States, £900 Wheat and flour were brought on sleds from St. Paul, Min- nesota, and death from starvation averted. Late in the autumn, the Canadian Government sent out engineers and surveyors to commence the construction of 458 MANITOBA AND THE GREAT NORTH-WEST. the road between the Red River Settlement and the Lake of the Woods. This undertaking was looked upon by the Hudson's Bay Company and other parties in the Colony, as the beginning of the end, and during this winter, the sub- ject was much discussed, both in Canada and the Red River Colony. As usual, at this time, there were many in Canada, who thought we were unable to purchase such a vast domain as the Hudson's Bay Territories, and many elaborate calcula- tions were made to show the foolishness of such a step. After along discussion, the Resolutions introduced into the Dominion Parliament by the Hon. W. Macdougall, were car- ried by a large majority. Dire results were to follow, as the land was considered by those gentlemen to be dear at any price. In October, 1868, the Canadian Commissioners sailed for England, but it was not until March 9th, 1869, that the negotiations between the Canadian Commissioners and the Hudson's Bay Company terminated by the former agreeing that the Dominion Government would pay the Hudson's Bay Company £300,000 on the surrender of their rights to the Imperial Government, and that the Imperial Govern- ment should, within one month of such transfer, re-transfer the same to Canada. Early in 1869, an Act was passed by the Dominion Par- 'liament, providing a Territorial Government for the country to be acquired from the Hudson's Bay Company. All the preliminaries being arranged, a number of surveyors were sent up in the summer for the purpose of inaugurating the survey of the Red River Valley. Many conflicting interests were at work at this time. The French party desired to be left as they were, or if an- nexation had to take place, let it be with the United States. It was evident to their leaders that few years would inter- vene before they would be only a mere handfull, and their HISTORY FROM 1821 TO 1870 459 power gone forever. The Hudson's Bay Company's officers knew that the English partners dared little for them and less for the country, so long as they could make a profit on their investments. They received $1,500,000 for their rights in the country, one-twentieth of the land and the fur trade remaining practically as it was. The change benefitted the English partners, but would it help the traders ? The few Canadians in the country certainly did not keep still, but talked much of what was coming, and long before win- ter set in, threatenings were heard of what might take place. It will be remembered that in the early stages of the settlement, the French Half-breeds lived entirely by hunt- ing, and had their headquarters at Pembina. Gradually they settled down in various parts of the Red River and Assiniboine valleys, and all apparently as squatters. In 1861, Governor Ramsey, of Minnesota, bought the land in the vicinity of Pembina from the Sioux, and never paid any attention to the claims of the residents. Our people com- menced to survey the very lands these people claimed as their own, and when Colonel Dennis intimated that some arrangement should be made with the Half-breeds, his report was laid aside, and he was ordered to commence work. Mr. Macdougall does not appear to have considered seriously the probability of trouble referred to in Colonel Dennis' report, and never submitted his letters on the sub- ject to the Council with any recommendation. On the 11th October, a survey party, under Mr. Webb, was stopped by a party of French Half-breeds, under Louis Kiel. No violence was used, Riel and some of his followers simply stepping on the chain, and ordering Mr. Webb to cease work. The reason he gave was that the land be- longed to the French Half-breeds, and they would not allow it to be surveyed, until some arrangement was made with them. No arms were seen on any of the party, and only 460 MANITOBA AND THE GREAT NORTH-WEST. threats were used, but Mr. Webb thought it most prudent to retire as ordered. A meeting was shortly after held by the disaffected French Half-breeds, at the house of one of their number, when it was determined to resist the entrance of Mr. Mac- dougall into the country, by force if necessary. Colonel Dennis now applied to the Hudson's Bay authorities, and Governor McTavish and Dr. Cowan had interviews with Riel, and pointed out the irnpyopriety of his conduct. Riel answered, as usual, the French Half-breeds should have been consulted with first. Application was now made to the Church, but Father Superior Lestang, who was in charge of the Diocese during the absence of Bishop Tache at Rome, declined to interfere, on the ground that he might lessen his influence with his people in so doing. The Half-breeds were not slow to see that the authorities in the country were at one with them or would not inter- fere, so their next step was to take up arms, and stop further proceedings by force. Mr. Macdougall was ordered to leave the North- West Territories in twenty-four hours, and was compelled to do so by a party of armed men. It now became apparent that what had been talked of for some time was about to be attempted, and that an indepen- dent organization was about to be established. In 1868 Bishop Tach^ in his sketch of the North-West hinted broadly what the people — his people — wanted. He felt that were Canadians allowed to come in like a flood, there was no hope for his people, and he naturally underrated the country for the purpose of deterring them. His hints had not been understood, and now the country was transferred and his people turned over to new governors without any guarantee that they would be honestly dealt with. We ask not who advised the rebellion, but this we do say that from their experience of the dealings of the Hudson's Bay Company with them the Half-breeds acted wisely from. their stand- HISTORY FROM 1821 TO 1870. 461 point. They lost their lands at Pembina in 1851 ; in the late transfer their rights were never recognized, and now as free men they decided to look out for themselves. In conversation with a Canadian two years after the event he told me that it was sending up a " cut and dried " Govern- ment from Canada, before explaining to the people, that caused all the difficulty. It may have been the excuse for the rising, but the apathy or something worse of the Hud- son's Bay Company and the plain advice of Bishop Tach6, were evidences of a something which lay deeper than that. "Warning after warning having been given to the Hudson's Bay Company that Fort Garry would be taken possession of, they paid no heed to them but just went on as before. As it is not my purpose to write a detailed account of the " Rebellion," but merely to show the causes that led to it. I will give in the words of a late writer the taking of Fort Garry hy the rebels, and Governor McTavish's explanation regarding it. " About the same time that Hon. Mr. Macdougall was driven back to Pembina by Riel and his followers, it began to be rumored that the insurgents intended to take possession of the Fort, and the authorities were duly informed of the fact in ample time to have made preparations for its defence, had they felt so disposed, but they paid no attention to the warning. Sergeant James Mulligan, at the time chief of police at Fort Garry, states in an afl&davit taken subse- quently, that he ' urged upon Dr. Cowan, the chief factor in charge of Fort Garry, the danger in which the Fort stood, from the intention of the insurgents to seize it ; and re- quested him to call upon a portion of the 300 special con- stables and the pensioners to defend it.' Fort Garry was a strong stone fort, bastioned and defended by thirteen six- pounder guns, was amply supplied with ammunition and provisions, and had in it also 390 Enfield rifles, so that if Governor McTavish had only closed the gates, he could, at 462 MANITOBA AND THE GREAT NORTH-WEST. least, have held the place against any force that the insur- gents could possibly have brought against him, if he was afraid to do more ; but even this he failed to do, although he and Dr. Cowan were warned by other parties than Mulligan that the place would be taken possession of. Not the slightest precaution was taken, the gates were not closed, cannon were not in position, and yet the Governor and chief factor knew that a body of men had been in possession of the Pembina Road for ten days, and had threatened to occupy the Fort. On the afternoon of the second of November, Riel, with about 100 men, came down the road from Riviere Sal, entered the open gates, and immediately proceeded to billet themselves in the various houses within. Dr. Cowan, the officer in charge of the Fort said ' What do you want here with all these armed men ? ' Riel replied, •' We have come to guard the Fort.' ' Against whom ? ' asked Dr. Cowan. ' Against a danger,' Riel answered. This was all the explanation given, and seemed to satisfy the chief factor ; and Riel and his followers were left in unconditional possession. " The force being housed, next fed, proceeded to arm themselves with Enfield rifles in place of their own shot guns, closed the gates, set a guard, placed the cannon in position, and for the first time since its inception the re- bellion became formidable. The insurgents had now pos- session of nearly all the cannon in the settlement ; were abundantly supplied with small arms and ammunition ; had all the provisions and other stores of the Hudson's Bay Company, more than enough to last them all winter, and it became evident that if they pleased to hold possession of the Fort until spring they could do so, for there was no force m the settlement able to dislodge them, and it would be summer or perhaps later before any force could arrive from Canada. In short, the insurgents were now 'masters of the situation,' and held the position which ought to have HISTORY FROM 1821 TO 1870 403 been occupied by the loyal party, and which they would have occupied but for the supineness — to use no harder term — of the officers of the Hudson's Bay Company. Governor McTavish's explanation of the capture of Fort Garry, as conveyed to the Hon. Mr. Macdougall in a letter dated 9th November, is certainly a remarkable production when we consider that the Hudson's Bay Company was still the de facto government, and that he, as the chief officer, was supposed to protect the property of the Company if nothing more. He says: 'Excepting in one respect — but that, I am sorry to say, a serious if not in a formidable sense — little change as far as we can learn has, since my last, come over the arrangements or the spirit of these people. * * * "jiie occurrence to which I have alluded in the preceding paragraph is this, that on the afternoon of Tuesday, the 2nd inst., a number of these daring people suddenly, and without the least intimation of their inten- tion to make such a move, took possession of the gates of Fort Garry, where they placed themselves inside and out- side the gates, to the number in all of about one hundred and twenty, and where, night and day, they have con- stantly kept a pretty strong armed guard. Oii being asked what they meant by such a movement upon the Fort, they said their object was to protect it. Protect it from what ? they were asked. Their answer was — danger. Against what danger ? they were asked. To this question, they replied that they could not specify the danger, but that they would do so hereafter, and obstinately took up the positions they have since kept, in spite of all our protests and remonstrances at such a bold and high-handed proceed- ing. On coming into the Fort, they earnestly disclaimed all inter tion of injuring either person or property within it, and must be allowed that in that respect they have kept their word ; but it is an inconvenience and a danger .aext to intolerable, to have a body of armed men, even 464 MANITOBA AND THE GREAT NORTH--WEST. with professions of peace towards ourselves, forcibly billeted upon an establishment such as this. Their intentions in coming to the Fort they have never definitely expressed, nor have they yet specified the danger from which their presence was meant to protect the place. We are, there- fore, left in some measure to conjectures, and by these we are strongly led to believe that you were expected to come to the Fort, and that by thus having previous possession of the gates, they felt that they would be sure of keeping you out.' The extreme simplicity of the Governor of Hudson's Bay Company in being led to believe that the object of Riel, in taking possession of the Fort, was to keep Mr. Macdougall out, is certainly refreshing — especially as he had been informed ten days before, that the capture of the Fort was intended for that very purpose." Shortly after this letter was written, W- B. O'Donohue, an Irishman, joined the movement and assumed the duties of Treasurer, collecting the import duty of four per cent, on all merchandise not imported by the Hudson's Bay Com- pany. This man, after the rebellion was crushed, being banished from the country, wrote the following letter to the Speaker of the Dominion Parliament, on the 26th February, 1875. What gives point to his statements is the fact that he was private tutor to Governor McTavish's children, and, therefore, intimate with him. He writes : " I make the following statement of facts, which I can prove most con- clusively : — " The insurrection was advised by Governor McTavish, who, with other ofiicers of the Hudson's Bay Company, also aided and abetted it from its inception up to the very hour it ceased to exist. That Riel was in constant com- munication with Governor McTavish, and on many occa- sions under his instructions. That he. Governor McTavish, fully recognized the Provisional Government. That Donald A. Smith, on arriving at Fort Garry, recognized the Gov- HISTORY FROM 1821 TO 1870. 465 ernment also in my own hearing, and, with Governor McTavish, was Kiel's adviser during his stay at the Fort, and after the departure of both of these from the couutiy, Kiel continued to hold counsel with John McTavish, who then represented the Hudson's Bay Company." After December 1st, " The Bill of Rights " was drawn up smd sanctioned by the French party and their adherents. This Bill was evidently what Bishop Tach6 had in his mind before the trouble commenced, and when too late, the Hudson's Bay Company saw they were playing into the hands of men opposed to their pretensions as well as to those of the Canadians. "When the " Bill of Rights " was passed, it became apparent to the most oblivious that wiser heads than a few French Half-breeds were guiding the movement, and the people of Canada woke up to a right understanding of the matter. During the winter Riel carried matters with a high hand, and attempts were made to break or modify his power, but without avail. The Canadians were taken prisoners and lodged in Fort Garry, the Fenian flag was hoisted, and all connection with Canada declared at an end. The few Americans in the country used their influence to have an annexation movement begun, and a newspaper was started to promulgate these views. In the meantime Bishop Tach6 was on his way from Rome, and strong hopes were enter- tained that on his arrival quietness would reign. One of the Canadians named Thomas Scott had made himself ob- noxious to Riel by his outspoken loyalty, and this man Riel determined to put to death. Without a show of a trial he was condemned to be shot, and on the 4th of March at noon he was taken outside of the Fort and brutally murdered. On the 9th of March Bishop Tach6 reached Fort Garry, and at once poured oil on the troubled waters. Riel offered to give up all the Hudson's Bay Company's property on the 28th of the same month, and about that date the annexation 30 466 MANITOBA AND THE GREAT NORTH-WEST. sheet ceased to appear. Acting under Bishop Tach^'s advice the "Fenian Flag" was hauled down and the Union Jack was hoisted in its stead. Riel now became very loyal, and " God save the Queen" was played by his band The regulars and Canadian militia were now mustering on the west end of Lake Superior, and shortly after started on their long and arduous expedition through the wilderness. On the 24th of August Colonel Wolseley's troops arrived at Port Garry, and the same morning Riel and his valiant band disappeared. CHAPTER XXYI. Ten Years Remmis(^ences and Notes on the Various Settlements and Villages. Purport of the Chapter — Manitoba and Winnipeg as They Were in 1872 — Grasshopper Plague^Crop of 1875 — Stage Bide in the Winter of 1875 — Disappearance of the GraBshoppers — Settlements Extend to the Second Plateau — Nelsonville Founded — Wet Seasons Conunence — Many Observers Condemn the Country — Bapid City Com- menced in 1878 — Land in the Neighborhood Rapidly Settled — The Assiniboine Ascended to Fort Ellice in May, 1879 — Crowds enter the Country East of Fort Ellice — Birtle Founded — Bock Lake Settlement — Winter of 1879-80 — Odanah and Minnedosa the Bage In the Spring of 1880 — Grand Valley Comes into Notice — Stiff-necked and Soft-hearted Immigrants — Mosquitoes Prove too Much for Them — English Ideas of Canadian Kindness — Canadian Notions Begarding Englishmen's Inability to Fall in with the Ways of the Country — No Stealing on the Plains — Settlements North of Birtle — Formation of the "Syndicate" — The "Boom" at Portage la Prairie — ^Winnipeg and Emerson take the Fever — Boute of the C.P.B. Changed in the Spring of 1881 — Brandon Founded on the Assiniboine — Vigor of the Syndicate — Railway Opened to Brandon — Speculation at Fever Heat — Conflict- ing Statements Regarding the Country — Short Notices of Selkirk, Emerson, Portage la Prairie, Morris, Brandon, Bapid City, Minnedosa, Odanah, Birtle, etc., etc. It is not the purpose of this Chapter to give a history of the last ten years, but merely to indicate the successive steps by which the country was opened up and the various villages laid out. In the chapters on the History and Pro- gress of Winnipeg, Education and Religion, Steamboats and Navigation, Railways and their development much of the history will be introduced, so that this chapter will be merely complimentary to them. During 1872 numerous settlers came to the country by the Dawson route via Lake Superior, while others came on the Northern Pacific to Fargo and either descended the Red River in boats or drove their own horses over the prairie to Manitoba. The preceding year the smallpox had raged on the plains and many Indians had died near Edmonton of th«^ disease. Captain Butler had just pub- 468 MANITOBA AND THE GREAT NORTH-WEST. lished his " Great Lone Land" and with the volume in my hand I entered for the first time the portals of the great plains. Winnipeg was a small village near Point Douglas and half a mile of prairie intervened between it and Fort Garry. Eastern Portage la Prairie consisted of one house and the western end could boast of one or two small houses around the Hudson's Bay Company's store. Grant and Mackenzie had settled on Eat Creek, nine miles to the west, but no settler had crossed the creek except the former. This season a few settlers took the road to the White Mud and laid the foundation of the settlements that sprang up there during the next year or two. For the next three years the grasshopper plague was upon the whole province and no wheat or next to none was raised in 1875. Many got a crop of potatoes, but the country was on the verge of starvation, and all the seed wheat had to be brought from Minnesota. DufFerin had been laid out on the boundary in 1873, but no progress was made. West Lynne on the west side of the Red River was a place of some importance as the high road to St. Paul passed near it. Stage-coaches were not infrequent in their transit through the village carrying their loads of shivering passengers to or from the bleak prairies of Dakota. A winter stage-coach ride of fifty-eight conse- cutive hours from Winnipeg to Fargo made the most lasting impression. Night and day we kept on, and enjoy- ing a nap in a stage coach with the temperature at zero was the greatest luxury we had. Our waking moments were full of torture, but sleep, such as it was, made us oblivious to suffering. The very marrow in our bones seemed to freeze, and as I write I shudder at the recollection. A new era dawned in 1876. The grasshoppers disap- peared, a large immigration took place, heavy crops were produced and the land rejoiced. This year settlement extended beyond the Pembina Mountains, Nelsonville was TEN years' reminiscences AND NOTES. 469 founded, the people learned that the upper plain was as fertile as the .lower, and the land along the boundary be- came thickly settled. A series of wet years now set in. Man J- parts of Manitoba were little better than a bog or a lake and numerous individuals, who had gone out to take up land, returned with evil reports. In 1877, settlement reached the " Big Plain" beyond Pine Creek, and the next year Rapid City, on the Little Saskatchewan, was founded by J. C. Whqlhems. The summer of 1878 saw a large immigration to the country around Rapid City, and to meet the demands of trade an attempt was made to ascend the Assiniboine to a point whence goods could be taken to the settlements on both sides of the river. The boats ascended without difficulty to a point about eight miles above the mouth of the Souris and discharged their cargoes at the foot of the " Rapid." This location obtained the name of " Rapid City Landing" as all goods destined for that point were landed here. Captain Webber, of the steamboat " Manitoba," examined the " Rapid," and pronounced his determiuation of taking freight and passengers to Fort Ellice. This was in May, 1879. His attempt was successful, although the wise ones at once condemned the whole undertaking. "While he was getting his cargo I reached "Winnipeg, and learned that the roads were in a terrible state for at least 150 miles. He promised to wait a day for me, and in the meantime I bought all my outfit for the plains, and we started at the appointed time. We reached Fort Ellice all right, and a high- way was opened to the interior. The attention of both specu- lators and farmers was now turned to the river, and a large number settled a little east of Port Ellice, and Birtle was founded by a gentleman, named Chambers, from St. Catherines. The Souris Plain was a great point of attrac- tion, and many settlers took up claims and began farming around Rock Lake. 470 MANITOBA AND THE GREAT NORTH-WEST. During the winter of 1879-80, interested parties got up some excitement about Odanah and Minnedosa, two embryo cities, located where the " North Trail " crosses the Little Saskatchewan. In the spring, a rush took place, and the boats on the Assiniboine River were loaded with freight and crowded with passengers, destined for those two " cities." Instead of using " Rapid City Landing," as in the spring of the preceding year, the boats now ascended the river to " Grand Valley," six miles above the rapid, and here the nucleus of a new city was established. Hundreds of tons of freight came up the river in t'le spring of 1880,, numerous immigrants arrived, and things looked lively. While in camp a week, at the " Grand Valley," I had ample opportunity of studying the peculiarities of the people. Camped by themselves were a number of English families, the members of which kept themselves apart from all others, and seemed to court seclusion. No attempt was made to gain information, and as a natural result, none was proffered. One day, two young men with their outfit started off for Rapid City. Owing to the heavy rain which had been falling for some days, the trail {Boad) was very bad in many places. Lacking experience, and being unaccus- tomed either to ask or take advice, they made little pro- gress and camped less than a mile from the " Landing," after having loaded and unloaded their waggon four times. Scarcely any progress was made the next day, and the second night they camped at a water-hole in a little hollow. A Canadian passing by told them to pitch their tent on an adjoining hill, as the mosquitoes would be bad that night. In response he was informed that they knew their own business. How they passed the night is not known, but early the next forenoon they reached the "Landing" again, sold their outfit for what they could get and were off for more congenial companionship in Winnipeg. On the same boat which took them back we cheered a number of TEN years' REMriTISCENCES AND NOTES. 471 others who, through ignorance, self-will or cowardice, had given up the attempt at settlement and had left in disgust. My camp was on the south side of the river and late one evening three young Englishmen crossed the river with two heavy loads of goods in two poor carts. While we were remarking on their foolishness for starting so late they passed us without a word and proceeded on their way towards the Brandon Hills to which they were bound. They had not gone two hundred yards when an axle broke and their load fell to the ground. We went up to see what was the matter, and as soon as I learned the nature of the accident I offered to lend them a cart and had my met assist them to load up, but advised them either to stop all night where they were or leave part of their loads. The leader of the party now asked me my charge for the cart and assistance, and as I only laughed at him, he said they had been told before they left England to hold no communication with Canadians as they would charge an exhorbitant price for everything they sold and do nothing without pay. We became more confidential, and 1 told him what we thought of them and how we looked on their proceedings. As I advised him to leave potatoes and flour, and a large trunk in his broken cart till the next day, he asked, would it not be stolen ? I informed him that only white men stole, and that Indians and Half-breeds, no matter what was said to the contrary, were strictly honest and as a matter of principle did not appropriate anything found on the prairie. I relate the above incidents as specimens of certain classes of occurrences that are constantly taking place, and a little less reserve on the one hand and much less contemptuous criticism on the other, would wonderfully assist in smoothing over the difficulties and privations incidental to settling in a new country. Acting on advice given by me, many Englishmen settled to the northwest of " Grand Valley " in the spring of 1880. Owing to the surveys that were now 472 MANITOBA AND THE GREAT NORTH-WEST. being prosecuted with vigor, many settlers "went northwest from Birtle to Shell River and located there. In the summer of 1880 Sir John Macdonald went to England with the avowed purpose of making arrangements with capitalists for the building of the Canada Pacifi'Vyinnipeg'T7^imii- peg in 1870 — Railway Surveys — Pembina Branch — Winnipeg ±he Outlet of the Jnter- lor Trade — The "Boom " in 1881— 'Statistics of the Trade of Winaipeg—Enumeratioa •* the Chief Buildings — Present Area of th« City^The Business Corporations-r-City Schools — Former . Trade with Winnipeg — Klontrasted with the . Present — Railway Grounds and Offices — Postal Facilities Past and Present — Leading Societies — The Press of Winnipeg — Agricultural Society — ^Extracts From Lord Dufferin's Speeches — ..Geographical Position — Rivers and. Lakes of Canada — Mennonites and Icelanders — The Future of the City — ^Appearance of Winnipeg to a New- Comer — Hoiy .Business is Transacted — Preponderance of Males — Occupation and thence to T^te Jaune Cache at the summit of the Rocky Mountains. In the spring of 1880, 127 miles of this section wa3 placed under contract, and up to the present considerable progress has been made. By the route above given the distance from Lake Nipis- sing to Burrard Inlet is 2,500 miles. In surveying the various lines 12,000 miles were actually chained, and over 40,001) miles of lines examined at a cost to the country of not less than $3,000,000. The various reports form a small library ia themselves, and the surveys although costing so much leave a country which was purchased for $1,500,000 in 1869, worth at least $250,000,000 in 1881. Had the Canadian Pacific Railway never been mooted very little improvement would have taken place, and to-day no American Railway would be near the frontier. The bargain with the " Syndicate " was scarcely con- cluded, when they showed their determination to carry the road still farther south. Acting on my report of the pre- ceding year, they sent Engineers south of the Assiniboine, and examined the country westward. Brandon was located, and their examination of the country was so satisfactory, that they sent engineers into the Rocky Mountains to ex- amine the Bow River Pass, or as it is called in the reports, the Kicking Horse Pass. These engineers have reported, and it is believed that the road may be carried through the mountains at that point. At present, the road is located from Winnipeg to Moose Jaw Creek, a distance of 404 miles. From this point they can go west to Calgarry, or turn to the northwest in the direction of Battleford. A branch extends southwesterly from Winnipeg, passing to the vicinity of Turtle Mountain, and thence westward to the Souris coal fields. This line is located 220 miles, and construction is far advanced on eighty -nine miles. From Brandon, another branch leads out southwesterly, for a dis- tance of 195 miles. In all, since the Company got posses- 616 MANITOBA AND THE GREAT NOETH-WEST. sion, on the first of May, 1881, they have located 819 miles, constructed about 300 miles, and have regular trains on 161 miles. During the coming summer, they are going to push on the work still more rapidly, so that by the fall of 1883, they may reach the base of the Rocky Mountains. As soon as the Syndicate obtained control, last spring, they set to work with an energy which astonished many, and before winter, had regular trains running from Winni- peg to Brandon, a distance of 145 miles. This place had no exist3nce last spring, and, at present, has a population of over 1,000. Churches have been built, schools have been organized, and all the machinery of civilization has been put in force in the comparatively short space of six months. Grading has been pushed on with great vigor beyond Bran- don, and it is confidently expected that the line will be opened to Qu'Appelle by the first of June, which point is at least 200 miles west of Brandon, and in the heart of a rich cultivated region. With the opening of the Lake Superior Branch, and only that part of their lines which are graded, this one Company will have, before the end of next summer, not less than 1,000 miles of railway in operation in the Canadian North- West. These lines are built in the very best manner, the ties are nearly all larch (tamarac), the rails are all steel of the best quality, and furnished with fish plates, bolts, and spikes of superior make. For some years, the South Western Railway Company has held a charter, to build a road from Winnipeg to the Souris coal field, southwest of Manitoba. Acting on their charter, they built or assisted to build the magnificent Louisa iron bridge, across the Red River, within the limits of the city of Winnipeg. Over this bridge, the whole railway traffic, both east and west, passes. It may be mentioned here, that Winnipeg is on the left or west bank of the Red River, and that St. Boniface is exactly opposite, on the east HISTOEY, AND FUTURE OF OUR RAILWAYS. 617 pr right bank. Owing to financial difl&culties, the road made little progress until last summer, when it passed under a new management, and this, with the aid of unlimited cash, has pushed the grading of the road rapidly to the south. Last spring, another railway was projected to run from Portage la Prairie to the western boundary of Manitoba. It was named the Westbourne and Rocky Mountain Rail- way, and is intended to pass by Westbourne, Gladstone, Odanah, and westward to Prince Albert, on the Saskatch- ewan. Part of this line has been placed under construction, and as the whole line for 600 miles has been projected through a rich and, to my knowledge, fertile country, there can be no doubt of its ultimate success. In view of future possibilities, a charter was obtained, two years since, to run a railway from Hudson's Bay to Lake Winnipeg. This road is called the Nelson River Railway, and explorations carried on last summer, show that the road can be easily built. This is not the only pro- jected road, as numerous others are chartered or will be chartered this winter, and with the branch lines that the Syndicate are permitted to build under their charter, the country will be filled with a complete network of roads. At present, there are only two outlets in contemplation : one to the south leading to St. Paul, 480 miles distant from Winnipeg ; the other to the east, which will be completed during the present year, leading to Prince Arthur's Landing, 430 miles from Winnipeg. A charter was granted last year by the Local Legislature of Manitoba, to a company to build a road called the Winnipeg and South Eastern Rail- way. The termini of this road are Winnipeg and Duluth. As this road was altogether in the interests of the Amer- icans, and intended to draw the trade of our North-West to Chicago and New York, it was very properly disallowed by the Governor in Council. Sooner or later this road will be built, and not it alone, but others not yet thought of. If 618 MANITOBA AND THE GREAT NORTH-TVEST. the trade of the interior is going to require so many branch lines to fulfill its requirements, it follows, as a matter of course, that two roads are not enough to carry the products of the interior to eastern markets. There being no wood nor very great manufacturing facilities in the North-West, the western bound freight will be very nearly equal to that going east, for many years to come. All manufactured articles having to be brought into the country, would it not be well for the people of Ontario to awake to this fact, and make preparations to supply them? Ten years will not elapse when the wheat, barley, and oats of the West, will come pouring into this Province, and whether prepared or unprepared, the farmers must take the consequences. Tariff or no tariff, manufactured articles must be sent West, and the sooner the Ontario people wake up to the fact that their supremacy, as a farming people, is in danger of passing away, the better it will be for them. While there is time, then put more money in factories and other industries, and be prepared to reap the golden harvest which is already at your doors ! The northern outlet, at present, engages the attention of many far-seeing men, but, up to the present time, nothing certain is known regarding the navigation of Hudson's Bay. Dr. Robert Bell, of the Geological Survey, in his coming report, is expected to throw considerable light on the sub- ject, but the report not being published, it is not available at present. In the preceding chapter will be found the latest published notices of the navigation, and other mat- ters pertaining to that great inland sea. Two years since, a charter was obtained from the Dominion Government, for the purpose of connecting the navigable waters of Hud- son's Bay with those of Lake Winnipeg, by a railway up the valley of the Nelson River. Careful examination has shown that the route is practicable, but the harbor of Port Nelson, at the mouth of the Nelson River, is far from being HISTORY, AND FUTURE OF OUR RAILWAYS. 619 as good as reported. The promoters of the route are still sanguine of its ultimate success, but later explorations point to the Churchill as the real outlet of the interior plains. In view of the adoption of the Churchill route, a charter has been obtained to run a railway from the mouth of that river to some point on the Saskatchewan. From various articles which have appeared from time to time, in our leading papers, it seems that the intention is to strike the Saskatchewan at some point east of' Cumberland House. Should this be attempted, it will result in failure, as east of that point, the country is very low on both sides of the river for many miles. The true route is to ascend the right bank of the Churchill to the mouth of the Little Churchill, and then strike southwest almost in a straight line to Fort k la Come. From information I have picked up from various sources, there will be no diflficulty in find- ing a suitable route, as there is a tract of rather sandy country which stretches almost continuously from near Fort k la Corne to the southern bend of the Churchill, on the 100th Meridian. The proposed line would keep north of the chain of lakes which form the Burntwood River, a tributary of the Nelson. A short distance above Fort a la Corne, there is an excel- lent crossing of the Saskatchewan, to which many lines will converge in the future, as no attempt will be made to bridge the South Saskatchewan nearer than the Moose "Woods, one hundred miles to the south. All roads intended to pass to the northwest or north of the Saskatchewan, must start from this point. This being the case, and I speak from a full knowledge of the subject, the future dis- tributing centre of the North-west, will be located below the Forks of the Saskatchewan, close to or above Fort a la Come. Granting the successful navigation of Hudson's Bay, of which there can be no reasonable doubt, it follows^ as a natural consequence, that the mouth of the Churchill .620 MANITOBA AND THE GREAT NORTH-WEST. will be selected as the terminus for the railway which will shortly follow. My other point, below the Forks of the Saskatchewan, of necessity must be the next objective as here the country is high and dry, and there is a good crossing Of the main river. Many parties, who have only a partial idea of the subject, point to Prince Albert as the real objective point for the terminus on the Saskatchewan, but its claims for this distinction pass away, when the sub- ject is only partially understood. Prince Albert, being on the North Saskatchewan, is cut off from all participation in the eastern or southern railway trafl&c and the trade of the ■South Saskatchewan. The more that is known of the country, the greater will appear the engineering difficulties in regard to river crossings west of the 106th Meridian, and fewer will be the points selected by practical men for that purpose. In conclusion, I desire to call the attention of thinking men to the prospective future of our interior Plains. Skept- icism regarding the capabilities of the country has nearly passed away, and the future lines of trade are being studied and examined with a critical eye. Englishmen are awaking to an appreciation of the evident future of our country, and it were well that amongst other less momentous matters, the value of the North-west, as a store-house for meat and grain, -obtain greater consideration. In case of a war between England and Kussia, it is scarcely a remote possibility that the United States might be tempted to stop the supply of Eng- land with food, and in that event, two years would scarcely be necessary to bring the people of the islands to the verge of starvation. Such a contingency could not happen were the Hudson's Bay proved to be navigable, as the whole of the resources of our vast interior would be at the disposal of Britain, and cattle and grain under convoy could be carried -thither in a very few days. This is only a prospective matter, but there is another that is a reality, and one which, in a year or two, will attract much attention. Let any person HISTORY, AND FUTURE OF OUR RAILWAYS. 621 take a map of North America, and look at the situation of San Francisco. By following the line of the Union Pacific Railway eastward, he will see Ogden over 900 miles east of San Francisco, and 1,000 miles farther east, Omaha, on the Missouri. Chicago is about 2,500 miles by rail from San Francisco, and five days continuous travel is necessary be- tween the two points. This is the present short line to the east, and when the Canada Pacific is opened, we know that it will be much shorter, as it crosses the Meridians where they have less breadth. The route of the future is much shorter. From Ogden a branch line has been built northward and has now reached Helena the capital of Montana, and is ex- pected to reach Fort Benton during the coming year where it will intersect the Northern Pacific. Between Benton and the Canada Pacific Railway as now projected there is only about 200 miles, which in a very few years will be open for traffic. By keeping the Canada Pacific for over 100 miles to the eastward and building a branch line from near Old Wives Lakes to Fort k la Corne, direct communication will be obtained with the line leading to Hudson's Bay, and by the time a passenger or freight going east reaches Chicago either one or the other going north will be close to Hudson's Bay. The construction of the two short lines spoken of will be extremely easy as there are no water courses to cross nor hills to ascend. It is so self-evident that this is the future line of traffic that nothing further need be said in its favor except to note that this line will tap the Union Pacific^ the Northern Pacific, and the Canada Pacific, and carry for a certainty all freight destined for the European market. "When this line is opened our stockmen -will kill their own cattle and send the meat to Europe as the northern route will be colder and the meat not subject to a high tempera- ture in transit. The above is the main line of the future, and Saskatchewan City will be the capital of the North- west, and Fort Churchill the New Archangel of Canada. CHAPTER XXXIII. Admce to Immigrants both as Regards Reaching the Country a/nd What to do when They get there. Where Information can be Obtained — Fare to Canada — Articles Eequired on the Voyage — From Whom to get Information — A Government Officer at each Ship- ping Port — How to Label Bonded and other Goods — How to Act on Board Ship — Articles Needed for the Voyage — Household Articles to be Bought — Mechanics' Pools — Farmers Should bring no Furniture — Warm Clothing to be Brought — Routes from Quebec to Manitoba — Agent at Duluth — Agents in Manitoba — Fare from Quebec to Manitoba — Carrying Heavy Freight a Mistake — Agents' Duties — Dominion Land Offices — Correspondence with Officials — How to Address Letters — Points to be Noted — Cautions to Immigrants — No Purchase of Homestead Land Valid until Title is Obtained — All Titles or Assignments should be Registered at Ottawa — Bounty War- rants and Land Scrip — Duties of Homesteaders — Make Entry of Homestead as soon as Possible — See that no One has any Claim to the Land Selected — Titles to all Lands Purchased should be Examined into — Land Guides will Assist at Selections of Lands — How to Select Good Land^How to get Good Sweet Water — Hay and Wood Secon- dary to Good Soil and Water — Spring best Time to Emigrate — Good Crops Raised on Spring Ploughing — New Plan of Sowing in Spring — Old Country People should fall into the Ways of the Country — Deep Ploughing in Manitoba a Mistake — How to Bring Money and Where to Place it —Illustrations of How much can be Saved in Five Years — Success Depends on the Settler — Canadian North-west Compared with Dakota and Minnesota — Opening of Canadian Pacific Railway — Statements of Settlers Regarding Outfit — Mode of Proce lure — Prices — Amount of Money Necessary Success — inFarming — Climate — Wintering Cattle, Oxen, and Horses — The Kind of Settlers Needed. How to reach the North-west is a question constantly asked by emigrants, and one not easily answered in their own country, but very easily answered in Canada. Should the questioner live in Great Britain or Ireland the necessary information can be obtained by writing to any one of the following gentlemen, who are the accredited agents of the Dominion Government in the mother countries : — London. — Sir A. T. Galt, G. C. M. G., &c., High Commis- sioner for the Dominion, 10 Victoria Chambers, London, S.W. Mr. J. Colmer, Private Secretary (same address). Liverpool. — Mr. John Dyke, 25 Water street. Glasgow. — Mr. Thomas Grahame, 40 Enoch Square. ADVICE TO I.UMIGRANTS. 623 Belfast. — Mr. Charles Foy, 29 Victoria Plaoe. Dublin. — Mr. Thomas Connolly, Northumberland House. Reliable information having been obtained on the points desired, the next step is to purchase a ticket if possible before leaving home. Always take your ticket, if in sum- mer, to Quebec or Montreal, not to Halifax, or St. John's, and never to any point in the United States, because should you do so you have a long railway route ahead of you. The better plan if going to Manitoba direct is to book right through, but never go faster thcvn your lug- gage. The greater part of the following instructions taken from recently issued publications, may be relied on for their accuracy : — When it has been decided to go to Canada, one of the Canadian steamship lines, whose advertisements can be found in the newspapers, should be written to, so as to secure a berth. There are vessels sailing from Liverpool, London, Bristol, Glasgow, Londonderry, and Cork. The fare from any of the places named to Quebec, depends upon the class of passage taken. The saloon fare ranges from ,£10 to £18 ; the intermediate is £8 8s. ; and the ordinary steerage passage is £6 6s., but agricul- turists and domestic servants have the benefit of a lower rate. This can be ascertained from the steamship offices, and they will also supply the necessary forms to be filled up ; children under ten years are charged half fare, and infants under one year a nominal sum. The fares include a plentiful supply of food, and good sleeping accommoda- tionon board. To Manitoba through tickets are issued by the steamship companies. The fare from London or Liverpool to Winni- peg ranges from £9 5s. assisted steerage, to £28 the saloon passage. Passengers are advised to take advantage of these tickets. 624 MANITOBA AND THE GREAT NORTH-WEST. To secure a berth, in the steamer it is necessary to send a deposit of <£5 for a saloon passage ; £1 for an intermediate or a steerage passage. Twenty culpic feet of luggage are allowed to each saloon passenger, ten to each intermediate, and ten to each steerage. Any information or advice as to the most useful things to take to Canada, or upon any other subject, may be obtained at the offices of the Steamship Companies, or at any of the Canadian Government offices. Steerage passengers have to provide bedding and certain utensils for use on board, which are enumerated in the bills of the Steamship Companies. They can be purchased at the port of embarkation, or hired for the voyage, from some lines — for a few shillings — leaving bed-covering only (a rug or blanket) to be provided by the passenger. Government agents are stationed at the principal places in Canada, and they should be enquired for on arrival. They will furnish information as to free grant and other lands open for settlement in their respective provinces and dis- tricts, farms for sale, demand for labor, rates of wages, route to travel, distances, expenses of conveyance ; receive and forward letters and remittances for settlers, and give any other information that may be required. Persons with capital should not be in a hurry to invest their money. They can get good interest for it by deposit- ing it in the banks, and can give themselves time to look around before settling. There is good banking accommo- dation in most of the towns, and letters of credit can be obtained from any of the English banks. An officer of the Canadian Government, at Liverpool, will see the emigrants on board the ocean steamers in pondition to ensure their comfort and safety during the passage to America He will render them any advice and assistance in his power. The name and address of this officer is — John Dyke, 15, Water Street, Liverpool. ADVICE TO IMMIGRANTS. 625 This officer may be written to for any desired information respecting removal to Canada. Intending settlers in the Canadian North-west will be met on their arrival, either at Quebec or Halifax, by a re- gular authorized officer of the Dominion Government, who will at once take them in charge, have their luggage properly looked after, and will see them safely on board the railway train for the West. Settlers effects, in use, will be passed free through the Custom House, and any necessary bonding arrangements will be made which will thus prevent any delay, inconve- nience, or loss occurring. Each passenger, before his de- parture from the port in Great Britain, should be provided with address cards as follows : — Mr of England, Passenger to Winnipeg, Manitoba, Canada. In Bond and he should see that one is pasted on each of his packages of luggage. As soon as the passenger gets on board he should read the rules he is expected to obey whilst at sea. He will find them hung up in the steerage, and should do his best to carry them out, and to be well-behaved and keep himself clean, as this will add much to his own comfort and health, as also to the comfort and health of others. If he have any grievance or real cause of complaint during the passage, he should go and make it known at once to the Captain. The arrangements, are, however, now so perfect for securing comfort and speed on the great ocean steam lines, that complaints are seldom or never heard. All boxes and luggage should be plainly marked with the passenger's name and the place he is going to. They will be stowed away in the hold of the vessel, so whatever is wanted on the voyage should be put into a trunk, carpet 40 626 MANITOBA AND THE GREAT NORTH-WEST. bag, or small box, which the passenger will take with him into his berth. Emigrants are often induced to make a clean sweep and part with everything they have before leaving the Old Country, because it is said the charge;.; for extra luggage are so large that they woiild come to more than the things are worth. Now there are many little household necessaries Avhich when sold would not bring much, but these same things if kept would be exceedingly valuable in the new country or the bush, and prove a great comfort to the family as well. It is not, therefore, always advisable to leave them behind ; they would not take up much room, and the cost of freight would be little compared to the comfort they will bring. The personal effects of emigrants are not liable to custom duty in Canada. Extra luggage (unless very bulky) is seldom charged for on the Canadian railways. Lay in as good a stock of clothes before leaving home as you possibly can. Woollen clothing and other kinds of wearing apparel, blankets, household linen, etc., are cheaper in the United Kingdom than in Canada. The emigrant's bedding, if it is good, should be brought ; and if he has an old pea jacket or great coat he should keei3 it by him, for he will find it most useful on board ship. Agricultural laborers need not bring their tools with them, as these can be easily got in Canada, of the best des- cription, and suited to the needs of the country. Mechanics are advised to bring such tools as they have, particularly if specially adapted to their trades. Both classes must, however, bear in mind that there is no difficulty in bujing any ordinary tools in the principal towns at reasonable prices, and that it is better to have the means of purchasing what they want after reaching their destinations, than to be hampered with a heavy lot of lug- gage on their journey through the countrj-. It must also be borne in mind that the tools bought in Canada will likely be specially adapted to the use of the country. ADVICE TO IMMIGRANTS. 627 Farmers and others with means, going out as saloon pas- sengers, sometimes take with them the greater portion of their household furniture, bedsteads, tables, pianos, and other heavy and cumbersome articles. Nothing could be more absurd than this. The cost is very great, the articles are liable to be damaged on the voyage ; and even should they reach Canada uninjured, many of them will be found to be out of place and next to useless. All heavy household furniture should be sold off; it is much better to make a clean sweep of it and to go out, so to speak, " in high march- ing order." Furniture of all kinds can be bought in Canada as cheaply as in England. The pianos made in Canada are second to none. Everything in the way of house furnishing is to be had at reasonable prices, and much better suited to the country than the English-made articles. By following out the advice given above, one may go to Canada with ease and comfort. The voyage is a short one, from eight to ten days 5 the steamships are of the very best class, and the wants and welfare of the passengers are care- fully and constantly looked after. In fact it is little else than a pleasure trip on a large scale. It may be mentioned that there are two routes by which an intending settler can reach Manitoba from Quebec, or any other Canadian port, namely : the " all rail route," via Detroit, Chicago, and St. Paul to Winnipeg, or by what is called the Lake Route, that is by railway to Sarnia or Collingwood on Lake Huron, thence by steamer to Duluth on Lake Superior, and by rail from Duluth to Winnipeg. The journey by the former route is quicker by about a day, but the latter is more economical. By either of these routes the settler will be met by the agents of American land and railway companies, who will endeavor to persuade settle- ment in the United States as preferable to Canada ; but the settler is advised to proceed direct to his intended destina- tion, and decide upon his location after personal inspection. 628 MANITOBA AND THE GREAT NORTH-WEST. In 1882, a line of railway will be completed from Thun- der Bay (Lake Superior) to Winnipeg, and westward. It will pass entirely through Canadian Territory, and its benefits both to new and old settlers will be very great. It may be added that most of the rivers and lakes in Man- itoba and the North-west are navigable, and that steamers now ply during the season on the River Saskatchewan, be- tween Winnipeg and Edmonton, a distance by water of about 1,200 miles, with passengers and freight, calling at Prince Albert, Carlton, Battleford, and other places on the way. Steamers also run regularly between Winnipeg, St. Vincent, and other places on the Red River. There is also steam communication on the river Assiniboine, between Fort Ellice and Winnipeg. At Duluth, during the season of navigation, a special agent is placed, Mr. W. C. B. Grahame. He will be in at- tendance on the arrival of all steamers, to assist emigrants in the bonding of their baggage, and otherwise to give them information. All emigrants should be implicitly guided by his disinterested official advice, in preference to listening to persons whom they do not know, who may have interest to deceive them. Agents in Manitoba. Emerson J. E. Tetu Winnipeg W. Hespeler. These agents will give emigrants all possible information and advice. The emigrant, or second class fare, in 1880, from Quebec to Winnipeg via Duluth was $25.50, and by the rail route via Chicago and St. Paul, $30.50. Pirst-class tickets are from 152.00 to $59.25. Children under thirteen are taken at half price, and 150 pounds of luggage is allowed to each adult. There will probably be very little, if any, differ- ence in the above rates, in 1882. In the case of a colony going together, the settlers might hire a railway car for the ADVICE TO IMMIGRANTS. 629 carriage of their eflfects, other than their luggage, to the point of the steamboat port, or continuously, and by this means, get a cheaper rate of freight. Many of the settlers from the older parts of Canada do this. It is not recommended to the settler who is travelling to Manitoba, to burden himself with heavy furniture and lug- gage, as the freight of these would probably cost him aS much as they are worth. As a rule, the emigrants should be advised not to take with them either furniture or agri- cultural implements. The latter particularly, specially adapted to the country, can be cheaply purchased at Emer- son or Winnipeg ; but a plentiful supply of clothing and bedding should be taken, together with such articles of general use as can be conveniently and easily packed. Of course, artizans who go will take their own special tools with them ; but they must remember that this may be expensive if they are heavy. The emigrants will be met at Winnipeg by Mr. Hespeler, the Government Agent, who will give them every possible information and assistance, and give them directions how to proceed to their lands ; or if they take Emerson, as the point in the Province from which they start, they will find a shed at the Railway Station, and buildings at Dufferin at which they can rest, while Mr. Tetu, the Government agent, will give them information. Dominion Lands Offices. The following is a list of the official names of the Loca Districts, together with the Post-Office address of the Local Agent : Wiimipeg Winnipeg. Gladstone Gladstone. Birtle Birtle. Dufferin Nelsonville. Turtle Mountain Turtle Mountain. Souris Souris-Mouth. Little Saskatchewan Odanah. Prince Albert Prince Albert, N. W. T. 630 MANITOBA AND THE GREAT NORTH-WEST. The Head-Offices of the Dominion Lands is at "Winnipeg, being a branch of the Department of the Interior. Correspondence with Officials. Observance of the following hints for conducting cor- respondence with officers connected with the Department of the Interior, will save time and trouble to the official staflf, facilitate the submission of applications for decision, and, consequently, tend to diminish the period in which replies may be looked for : — I. Address no letters on official business by name to the Minister, or any one else connected with the department, .e letters to person illy addressed may be deemed private coiTespcndence, and, in the poss.ble absence of the person to whom they are directed, remain unopened till his return. II. All letters to the Authorities at Ottawa on land matters should be addressed, in a plain hand, to The Hon. the Minister, Department of the Interior, Ottawa. Dominion Land Branch. No stamp is required for letters directed to the official head of the Department, such communications being " free." III. In correspondence with any of the local Officers, a letter should be addressed as follows Three-Cent The Locai. Agent, Stamp. Dominion Lands Office, In this case the ordinary postage rules apply. IV. Write in a concise and courteous manner, upon foolscap paper, on one side of the paper only, leaving a margin of at least an inch on left-hand side. V. In the right-hand top corner of the first page write distinctly the official name of the post office to which a reply is to be addressed, together with the date of your letter. If the matter occupies more than one page, see that the pages are numbered ; and be sure that your signature is legible. VI. Never deal with more than one subject in a single communication ; but write a separate letter for each. VII. On receiving a reply, if you respond to it, do not fail to quote the reference number of the official file, which you will observe on the left-hand top comer of the first page (i. c, at the head of your letter put In reply to No ) VIII. Keep copies of all your correspondence with the Department or Local Offices. IX. All remittances to pay for Dominion Lands should be made in lawful money of Canada, by registered letter. A Local Agent is not bound to accept any person's cheque. ADYICE TO IMMIGRANTS. 631 Useful Hints to Emigrants. Strangers going to the North-west, should be extremely cautious in purchasing the abandonment of any one's home- stead claim, as all assignments and transfers of the home- stead right (until recommended for patent) are absolutely invalid, though, so far as the party assigning is concerned, such assignment may be deemed by the Dominion Lands Authorities as evidence of voluntary abandonments. Any person, however, whose homestead has been recom- mended by the local Agent for letters patent (proofs of fulfilment of conditions having, of course, been filed with ' him) may legally convey, assign, and transfer his right and title therein. There is a book kept in the Department of the Interior for the registration, at the option of the parties interested, on payment of a fee of $2.50, of any such assignment of legally assignable rights (proof of which must accompany the application to register), and the law holds every assignment so registered as valid against any other assignment unregistered or subsequently registered, even if previously made. Every assignment must, for the purpose of registration, be entirely unconditional. Bounty Land Warrants, whether issued to men who have served in the North-west Mounted Police or the Militia force formerly performing duty in Manitoba, are accepted in payment of all lands for the amount they represent, viz ; 160 acres ; but purchasers of warrants should be careful to see that the assignment to themselves, as well as all pre- vious assignments, are duly registered at Ottawa. It is essential to its validity that the first assignment of a war- rant should be endorsed on the document itself. Land scrip, whether that issued to Half-breed heads of families or of the kind granted to " old settlers " in the Settlement Belts, to extinguish certain claims, is of the same value as cash, to the hearer, in any purchase of Dom- inion Lands, for the amount represented on its face. 632 MANITOBA AND THE GREAT NOETH-"WEST. Settlers who take up homesteads are required to become actual residents and improvers of their claims, within six months from date of entry. In the case, however, of im- migrants applying to the Minister of the Interior for leave ' to settle in a community, and showing good cause, the Governor General in Council has power to extend the period to twelve months. It is important, in every case, to make a homestead entry as soon as possible, because no patent can issue (as a free grant) until three years from the date of entry have ex- pired ; and it is essential to reside on the homestead and cultivate the same continuously, in order that no delay may be occasioned at the expiration of the above period. Fur- ther, it is important, because, should circumstances require the settler to reside elsewhere, a continuous fulfilment of the homestead conditions for twelve months would give him the right, ander a special clause of the Act, to purchase such homestead at the current price of the adjacent Govern- ment lands. The Department holds residence to have been " continuous " in the legal sense, notwithstanding the settler may have been absent from his homestead for a period not exceeding six months altogether in any one year of his occupation ; cultivation must, however, have been carried on each season by himself or his representatives. In the case, however, when a certain number of home- stead settlers, embracing not less than twenty families, with a view to greater convenience in the establishment of schools, churches, &c., ask to be allowed to settle together in a hamlet or village, the Minister may vary the require- ment as to residence on, but not as to the cultivation of, each separate quarter-section. Immigrants will act wisely in making sure that the land for which they propose to enter is not already claimed in any way by a prior occupant. As a general rule, it will be found safer to take up land to which no legal or equitable claim is ADVICE TO IMMIGRANTS. 633 likely to be asserted, than to go into disputed possession of a superior location. In the one case, the settler can con- fidently proceed with his improvements ; in the other, he will be hindered by the delay and uncertainty involved in obtaining a decision. Purchasers of land in Manitoba and the North-west Ter- ritories that has been already patented from the Crown, should never pay any portion of the price agreed upon, without first satisfying themselves, by obtaining an abstract of title from the Registry Ofiice for the Registration Dis- trict in which the lands are situated, that no agreements, mortgages, judgments, or other incumbrances are recorded against it; also, that no arrears of taxes are due upon such property. It should also be remembered that, as the law attaches the greatest possib.e importance to priority of registration, no delay should be allowed to in. ervene be- tween the signing of the deed and seeing that it is duly registered. A Registrar's fee, in Manitoba, for registering an ordinary conveyance is $2.20 ; he charges fifty cents for a search, and for an abstract, according to the number of the entries of documents affecting the property. Persons travelling in the North-west are required to be particularly careful to extinguish their camp-fires before leaving them, so that the destructive consequences of a prairie fire may be prevented. Both in Manitoba and the Territories, legislation has provided adequate penalties for the punishment of criminal negligence in this respect. Should it happen, however, that a party of immigrants are threatened by a prairie-fire approaching them, and no other means of escape are available, the danger may be efiectually overcome by setting fire to the prairie to leeward of the party, and moving the travellers, with their outfit, into the ground so burnt over. When one or more persons have reached a district where they purpose looking for land, the better plan is to go at 634 MANITOBA AND THE GREAT NOETH-WEST. once to the Agent and ask for the numbers of vacant sections in the various townships. Attached to each agency is a " Land Guide," whose duty is to take charge of strangers and show them where the vacant lands are, and give them infor- mation as to the quality of the soil, the presence of water, and any other matter about which he may be questioned. As most people prefer to select lands for themselves^ advice on this point may seem out of place, still a few hints may benefit some. The first requisite is a dry level or gently rolling surface free from brush on at least two-thirds of the lot. The next necessity is permanent and pure water. Should there ue ponds on the lot an examination is abso- lutely necessary, to see whether the water is pure or saline. The best and simplest test is to wash with soap in the water. If it forms a suds the water is good, if curds in the dry season, the water is bad. I speak of ponds in this con- nection, as brooks and rivers contain hard water in nearly every case. Another test is the grass. Should grass in the middle of a pond be green at the latter part of September the water is permanently good, if rotted the water is unfit for use at that time. Wood and hay lands are really secondary objects, as it is much better for a farmer to have a good wheat farm which he can at once break up and from which he can begin to make money, than to clear the land of brush and young wood, and waste time in draining. As is shown in another place any party taking a prairie lot is entitled to twenty acres of wood land. Few lots are without hay lands, as all hollows con- tain more or less hay. Now, when railways are extending into the country, it is much better to come out in early spring if a crop is desired the first year. Any party reaching their land by the middle of May can have potatoes, wheat, and garden vegetables that same season. All that is necessary is to procure the laud, pitch a tent, and set to work. ADVICK TO IMMIGRANTS. 635 Recently it has been discovered by successful experiments, that seeds sown on the prairie grass and then ploughed lightly, will yield good crops the same season. This is a most important discovery, as it shows that an immigrant arriving on his claim in the spring can begin to realize a return from his labors almost as quickly as if the land had already been cultivated and improved. The following is an account of the experiments made in this respect, and they will be found worthy the consideration of every farmer con- templating the "breaking" of new lands. An experiment in raising grain on fresh sod has been tried in the vicinity of Big Stone Lake for the past two sea- sons with such marked success, that it is worthy of exten- sive trials. We are not informed who the first experimenter was, but at any rate, in the vicinity of Big Stone City, there are farmers so confident of success that they have put in considerable quantities of small grain in the ficesh sod dur- ing the past season, and in every case, so far as we could learn, with the most beneficial result. The novelty of the operation is that the grain is first sown on the prairie grass, and then the "breaking" is done. A rather light sod is turned, and the buried grain quickly finds its way through. In a few weeks the sod is as rotten as need be, and can be kicked to pieces easily with the foot. Now for an illustration : A Mr. Daly, near Big Stone City, in the vicinity of Big Stone Lake, sowed ten acres of oats this last year. He put two bushels and a peck to the acre, and broke his land. Last fall, from ten acres he harvested 420 bushels of oats which were worth sufficient to pay for the breaking, and leave him some seventy -five dollars besides. This year he sowed forty- five acres in this way with equally good success, the yield, according to estimate, as he had not threshed when we got there, not being less than 1,000 bushels on the piece. An- other gentleman near him sowed buckwheat in the latter part of May in the same way, and he has every promise of 636 MANITOBA AND THE GREAT NORTH-WEST. a magnificent crop. Another tried corn, dropping a few ker- nels in every fourth furrow. Wheat has not been tried, but will be another year. It has been found that grain can be sowed on the prairie early and the sod rotted as readily as if sowed in June, as the growing crop shades it and but little grass starts. This is a valuable discovery and will be worth much to new beginners who, thus far, with the exception of potatoes, have not expected anything before the second year. It will be of value also to larger farmers who are obliged to go to a heavy outlay each year for breaking, for the oat crop not only pays for the labor, but leaves a good margin besides. It is an experiment certainly worth a trial. The immigrant settling in a new country will understand the value of this discovery which will enable him to realize sufficient for his expenses the first year, and perhaps will enable him to place a sum of money aside for future use. The new settler when he arrives in the country ought to locate his farm with as little delay as possible, and then set to work to break as much land as he can for the ensuing year's seeding. If he should be in time to sow on the sod as already described, by all means let him do so, but if not he should break as much as possible for cultivation the following year. He and his family can very well camp out in tents during the summer, and in the fall there will be plenty of time to erect a warm house and stables for the winter. It is of the greatest importance that old countrymen should fall into the methods of old settlers on the prairie Too often they allow their prejudices to lead them into practices which the experience of practical men show to be altogether unsuitable to a prairie country. For instance, with respect to ploughing, or as it is called, "breaking" the prairie, the method, in Manitoba, is quite difierent from that in an old country. The prairie is cov- ered with a rank vegetable growth, and the question is how ADVICE TO IMMIGRANTS. 637 to subdue this, and so make the land available for farming purposes. Experience has proved that the best way is to plough not deeper than two inches, and turn over a furrow from twelve to sixteen inches wide. This is well done during the months of June and July. It is found that the sod is effectually killed when turned over during these two months. It has happened that some farmers from older countries, in love at home with deep ploughing, have de- spised the methods of the country, and tried deep ploughing in Manitoba. These men have come to learn wisdom from practical disappointment, but this is an unnecessarih" ex- pensive lesson. We have already advised intending settlers to avoid bur- dening themselves with an unnecessary amount of luggage. We would, however, recommend them to bring with them as much of their clothing as they conveniently can, as it packs in small compass, and saves outlay in the new land. Be sure, however, to bring your money, or that portion of it which you will not require to use on the way, in the form of a draft or bill-of-exchange. If you lose the draft or bill, you can always have it replaced. If you bring gold, silver, or bank notes, and lose it, you will probably never recover your loss. There are four large banking institu- tions in Winnipeg, any one of which will be able to cash your draft or bill on your arrival. As soon as you reach Winnipeg, by placing yourself in the hands of the Govern- ment guides, you will be able to make your purchases at reasonable prices, and will be secure from any imposition in that respect. The following figures may prove of interest to intending settlers, as showing what can be done in the Canadian North-west. Farms can be purchased at almost any price from one dollar per acre upwards, and one hundred and sixty acres can be secured as a homestead free, on payment of ten dollars entry fee. We will, however, base our cal- 638 MANITOBA AND THE GREAT NORTH-WEST. culations on the Government price for pre-emptions of one dollar, and we will illustrate a term of five years occupancy : First Year. Expenditure of settler with family of say five, for provisions, &c., one year $250.00 One yoke of oxen 125.00 One cow 35.00 Breaking plough and harrow 35.00 Waggon 80.00 Implements, &o 25.00 Cook stove, &c., complete 25.00 Furniture 25.00 Tent 10.00 Sundries, say 50.00 Outlay for First Year $660.00 At the end of the year, he will have a comfortable log- house, barn, &c., cattle implements, and say twenty acres of land broken, ready for seed. Second Year. Will realize from twenty acres — 600 bushels of grain at 60c., which is a low figure $360.00 Expenditure, say 300.00 To the good $60.00 And he will have an additional twenty acres of land broken. Third Year. Forty acres will give him 1,200 bushels of grain, at 60c $720.00 Will pay for land $160.00 Expenditure, including additional stock and implements. . 600.00 660.00 To the good $60.00 And he will, with his increased stock and other facilities, be able to break at least thirty acres. Fourth Year. Seventy acres will give him 2,700 bushels of grain, at 60c $1,260.00 Less expenditure for further stock, implements, and other neces- saries 600.00 To the good $660,00 And another thirty acres broken. ADVICE TO IMMIGRANTS. 639 Fifth Year. 100 acres will give him 3,000 bushels of grain, at 60c $1,800.00 Less, same expenditure as previous year 600.00 To the good $1,200.00 At the end of the fifth year, he will stand as follows : — Cash, or its equivalent on hand $1,980.00 160 acres of land increased in value to at least $5 per acre 800.00 House and barn, low appraisal 250.00 Stock, including cattle and horses 600.00 Machinery and farm implements, 50 per cent, of cost, say 200.00 Furniture, &e 150 00 $3,980.00 Less — outlay fii-st year , . . . : 660.00 To credit of ferm $3,320.00 In these calculations, we have endeavored to be as near the truth as possible. We have increased the number of acres broken during the three years, because with an increase f>f stock and other facilities for breaking, the settler can break more. This has been the experience of farmers here. Then we have placed the expenditure high, while the price \uoted for the grain is much lower than is paid at present by buyers. We show a profit of $3,000, after paying for everything, in five years ; but we can cite numerous cases m which settlers have cleared more than $4,000 and $5,000 in the same time, and in which in many instances they had not $100 to commence with. The whole success of the new settler depends upon his economical management perseverance, and untiring industry. If he pays more than $1 per acre for his land, he may be sure it will rise corres- pondingly in value as the country progresses. The intend- ing settler, however, must never forget that he can always obtain 160 acres of land free, from the Government, in addition to that which he purchases. There is one point we desire to impress upon intending settlers, and that is the large yield of grain in the Canadian 640 MANITOBA AND THE GEEAT NORTH-WEST. North-west. From this time, no immigrant need settle at any great distance from railway communication unless he desires to do so, so that he can always be within easy reach of a steady market. We may safely place the average yield per acre, at thirty bushels of wheat after the second year, and can also safely say that grain will fetch as high prices as in Minnesota or Dakota. In the Canadian North-west, however, allowing prices to be equal, how does the settler stand, as compared with those south of the boundary line. Average yield, per acre, in the Canadian North-west, 30 bushels, say at 80c $24.00 Average yield in Minnesota, 17 bushels, say at 80c 13.60 In favor of Canadian settler. . . $10.40 This is a considerable difference which is borne out by facts, and when it is considered that the cost of living is less than in the United States, the difference becomes still greater. It simply resolves itself into this, that settlers in the Canadian North-west can afford to sell their grain, owing to their large returns at fully 50 per cent, lower than those in the United States, and still be as well off, or they can (prices being equal) realize the same percentage more than their neighbors south of the boundary line. The opening of the Canadian Pacific Railway to Lake Superior, next year, will give the North-west equal ship- ping facilities with the Western States. What more can we say for the information of those who are looking for new homes to guide them to this " Land of Promise," but a simple word in conclusion. The Canadian Pacific Rail- way is to be pushed forward at a rapid rate during the next few years, and will give employment to thousands of men. A very large amount of grain and other supplies will be required to carry on the extensive public works of the Canadian North-west, and farmers will be kept busy in order to supply this home demand for years to come. ADVICE TO IMMIGRANTS. 641 In addition to this, immigrants will be able to find plenty of work for themselves and their teams, during their spare time, so that the sooner settlers make up their minds to come here, the better it will be for themselves. The next ten years in the Canadian North-west will assuredly be a time of great progress and prosperity. In conclusion, we submit the following evidence of set- tlers on certain points connected with outfit and farming : Statements of Actual Settlers. Nelson Brown of High Bluflf, says : — "In my opinion the month of September is the most favorable for settlers to come here, and in no case should they come earlier than May. Let them bring good medium-sized close-made horses with them. Have been here eight years and know the requirements pretty well." Henry "West of Clear Springs, says : — "I have been in the country six years and have found the driest summer to give the best crops, even though there was no rain except an odd thunder- shower. New settlers should come in May and break their land till July, then, after cutting and saving plenty of hay for all the cattle, they can pre- pare their buildings for the winter." James Stewart of High Bluff, says : — " I would suggest that intending settlers in the North-west who come to settle down on prairie land should break up an acre or two around where they build, on the West, North and East and plant with maple seeds. Plant in rows four feet apart, the seeds to be planted one foot apart ; they afterwards can be turned out and transplanted. I have them 12 feet high from the seed planted four years ago, and they will form a good shelter. I find, after a residence of nine years, that this North-west country is well calculated for raising the different kinds of grain sown by farmers. Market prices are very good. Wheat, 85c. to $1.15 ; Oats, 50c. to 60c., and Barley, 60c." James McEwan of Meadow Lea, says : — " Farmers should have Canadian horses and get oxen and cows, and purchase young cattle. By doing so they will double their money every year. I am in the business and know by experience." George Ferris of St. Agathe, says : — " I would advise immigrants to fetch all the cash they can. They can suit themselves better by buying here about as cheap, and they will only get just what they need." Jno. George of Nelsonville, says : — " I consider this country the place to come to, providing any man wants to make a home and knows something of &,rming, that has about $400 to $500 to begin with." 41 642 MANITOBA AND THE GREAT NORTH-WEST. John A. Lee of High Bluff, says : — " Now that we have the locomotive, we shall be able to compare with anything in the Dominion, and take the lead with roots-'and I defy the United States for samples of grain of all kinds. They have only the start of us iu fruits, hut we are progressing well in that respect. If folks would work four months in the year they might be independent in this country. I came here in 1873 with only thirty dollars in my pocket, ten of which I paid for my homestead of 160 acres. It is going on two years since I began to cultivate the place I am now living on, and have 74 acres under cultivation, with a suitable house and other fixtures, and I could get $3,000 for one of my quarter sections. Icaube found in High Bluff at any time with $50 to back my words." Geo. C. Hall of Portage la Prairie, says : — '■ My claim is situated on the banks of the Assiniboine and we therefore enjoy direct steamboat communication with Winnipeg. The land is not fiat but rolling prairie, no need of drainage, but still it is well watered by running springs. All crops look well. I planted potatoes on 1st June, and In eight weeks we had our first meal of them. 1 expect about 300 bushels to the acre. The climate of the country is all that can be desired. Any man who wishes to furnish a home for himself should try and locate in this country, and if he be a man of any energy he will not be long in making a comfortable and profitable home for himself and family. It was a happy day that I first lauded on this soil." D. H. Knight of Ridgeville, says : — " I would recommend settlers to get oxen for breaking the sod. Horses cost much more to keep as they require grain. Oxen can be worked on the grass. I am more in the stock line, and I can say the country is well adapted for stock-raising. The pasturage could not be better. Abundance of hay can be had for the cutting, and with a little care cattle winter well, and come through in good condition." James D. Stewart of Cooks Creek, says :^— " Would advise new settlers to buy oxen instead of horses as they can be fed cheaper and will do more work if well treated and fed on grass and good hay." Joshua Appleyard of Stonewall, says : — "I would advise any young man with good heart and $300 to come to this country, for in five years he can be independent." Jno. Ferguson of High Bluff, says : — "I would advise settlers in a general way to start with oxen as they are less expensive in cost and keep the first year at a less risk than horses. 1 would advise them not to bring any implements with them but procure the best of all classes here, as they are especially adapted for this country." Thos. H. Ellison of Scratching River, says : — "Any man with a family of boys such as I have, that intends living by farming and raising his boys to farm, is only fooling away his time in other places when he can average a hundred per cent, more each year with his labor here as I have done. I have farmed iu Europe, State of New York, and Ontario, aud I can say tliis safely.'' ADVICE TO IMMIGRANTS. 643 Geo. Fidsbury of High Bluff", says : — " I would not advise any man coming out here to farm to bring any more luggage witli him tliau he can actually help. 1 have sometimes weighed roots here and found them to surpass any I ever grew in Canada. I do not think there is any use telling the immigrants the weights as they will hardly believe it. It is enough for them to know that this coimtry can produce mare to the acrt with less cultivation than any part of Canada." CHAPTER XXXIV. Advice to Settlers and Travellers. Protection against Sudden Storms in Winter — Thunder, Rain, or Wind Storms in Sum. mer — How to Protect Horses and Cattle from Flies — Smudges — Keeping the Tent Clear of Mosquitoes — Care of Horses when Travelling — How to Find Lost Horses — Precautions to be Used — Where to Pitch a Camp in Summer — In Winter — How to Find Water — How to Know Sweet Water — Protection against Prairie Fires — Saving Hay and Fences — How to Travel Over the Prairie With or Without a Koad — White Mud Swamps — Carelessness of Travellers as Regards their Personal Comfort — How to Pre- vent a Prairie Fire — Penalty for Starting One — Crossing Streams with Bridges — How to Cross, &c., &c. Occasionally notices appear in the public prints of travellers and others who have lost their lives by being caught on an exposed prairie in a winter storm or blizzard. Should old travellers be caught in one of these storms no attempt is made to proceed to their destination, but an immediate halt is called or an effort is made to reach the nearest shelter. Should none be near, the nearest ravine or vouleS is entered and the banks of snow made to do duty for a house. Instances have been known where Half- breeds have lain comfortably in the drifts for days and saved themselves and horses, when if they had proceeded they would have been frozen to death. In the win- ter of 1875 I was travelling with a company of Half-breeds when a terrible snow-storm came on accompanied with a fierce gale, which drove the icy particles into our eyes with such force that they scarcely left us the power to see. We were sixteen miles from wood, and it was decided to attempt to reach it. Failing in this, we were to make a break wind of our carts, and camp in a favorable hollow. Knowing what we intended to do we pushed on, our leader merely taking the direction of the wind on his cheek! Beaching the wood and penetrating it some distance we ADVICE TO SETTLERS AND TBAVELLERS. 645 discovered a little pond where we unharnessed our horses, built a roaring fire and thawed the ice out of our beards and hair. We now built booths of poles and willows, and thatched them over with the long grass of the pond, and for the next thirty-six hours enjoyed ourselves amazingly. A few visits to the edge of the wood showed the storm still raging on the prairie, and for two nights and a day we were snow-bound. We obtained abundance of food for our horses in the grassy glades, and scarcely gave a thought to the blizzard that swept the prairie a quarter of a mile away. All travellers should carry matches summer and winter. These should always be placed in an inner breast pocket so as to be dry and handy. Inexperience says they are not necessary, or, we know a friend who has them. Wisdom says, carry them yourself. In winter, besides matches, dried grass, or the outer bark of the canoe birch, should always be carried so that not an instant need be lost in lighting a fire if the necessity for it should arise. In the winter of 1872 when travelling in Northern British Columbia, the weather was intensely cold and the lakes were frozen over, but in some places the rivers discharging them were covered with only a thin film of ice. We reached a small river, discharging Carrier Lake, which I crossed in safety. An old Indian following me broke through, and by the time he was out he was like an icicle. In an instant every pack was on the ground, a fire was lit and while he changed his clothes, a cup of hot tea was got ready and scarcely fifteen minutes elapsed before we were again on the way. The cause of settlers and others losing their lives in win- ter can always be shown to arise from their desire to reach home or from persistently fighting the storm, until their vitality and animal heat are so far exhausted that they sink down and fall into a deep sleep and never awake. On the 646 MANITOBA AND THE GREAT NORTH-WEST. other hand, if a man lies down and gets cold when asleep, he will surely wake up with a change of temperature. All parties caught in a severe storm should conserve their powers, instead of weakening them by persistent efforts, and this can be done by at once fleeing to shelter, and if no fire can be lighted, wrapping the body up in warm clothing, and remaining passive until the storm ceases. During the past winter, a number of individuals lost their lives by not fully recognizing the danger they ran in exposing them- selves on the prairie, when a severe wind storm (Blizzard) was in progress. Owing to its force and the icy particles that fill the air, it is next to impossible to make progress, except before the wind, and too often this is in the wrong direction. It is, therefore, absolutely necessary for all parties travelling in a thinly settled part of the country, any time after the beginning of October, to carry matches with them, and if caught in a storm, to retreat at once to a thicket, and build a fire and remain there quietly until the storm is past. Summer storms are often very severe, and frequently accompanied by terrific thunder and wind. I consider a prairie thunder storm as one of the most appalling occur- rences which a traveller on the plain has to encounter, and one which he has no means to escape. There are few days in June and July, when thunder is not heard from some point of the compass. Most of the storms are merely local, and last but a short time. They generally take place after three o'clock in the afternoon, and no matter how severe the night storm may be, the air is clear and calm in the morning. Should a series of storms take place, the tempera- ture is considerably lowered, and a cloudy and windy day will likely follow. All travellers should have a strong cover for each waggon or cart, and see that it is securely fastened every night before retiring to his tent. Very frequently, the traveller ADVICE TO SETTLERS AND TRAVELLERS. 647 may retire to rest witli not a speck of cloud anywhere above the horizon, and wake up a little after midnight, with the incessant roll of thunder in his ears, ard his eyes blinded with the vivid lightning. It is now that the un- wary traveller pays the penalty for being ignorant. Care- lessly pitched tents are blown down, or the rain pours through, and everything is thoroughly soaked. Morning breaks, and the goods are found injured by the rain, and to complete the disaster, the horses have stampeded and are nowhere to be found. Nearly all travellers relate such occurrences as happening to themselves, and seem to see no way of preventing the disaster. Prevention is very easy, and the careful traveller is never caught unprepared. When seeking a camping place for the night, any time during the summer, an elevated spot, near a pool of water, should be chosen, so that comparative freedom from mos- quitoes may be secured if there should be a little wind. Feed and shelter for the horses are absolutely necessary, as both may be needed any night. All the conveyances should be placed west of the tents, and each tent securely tied to a cart by a guy rope passing over the end of the ridge-pole. The rear of the tents should be next to the carts, so that should a storm arise in the night, there would be no danger of the tents being blown down. By taking these precautions, no storm can do much damage, and men fall into the habit of doing this as a matter of routine. In the latter part of June, 1879, I encamped on the prairie, just west of Qu'Appelle, but on the plateau above the river valley. About three hundred yards distant, another exploring party stopped for the night. We ar- ranged our camp in our usual manner, and retired to rest. About two o'clock, a.m., a terrific rain, thunder, and wind storm broke over us, and for five hours we lay and listened to the terrific uproar. After the rain ceased we attempted to make a fire, but could not succeed for some time owing to 648 MANITOBA AND THE GREAT NORTH-WEST. the force of the wind and wetness of the wood. Our tents had withstood the tempest's power and kept us perfectly dry. Not so with our friends in the other camp. Their tent had been blown down at the commencement of the storm, and there was not a man in the camp that had a dry rag. Of course, in letters to their friends, they omitted to state that their wretchedness was the result of their own carelessness. I visited their camp and found that the storm was altogether unexpected and had caught them un- prepared, and their tents tumbled^about their ears in a few minutes. Horses will not face a severe rain and wind storm on the prairie, so that it is absolutely necessary to stop if the storm is meeting you. On the approach of a thunder storm in the day time, which may be of short duration, it is only necessary to turn the horses heads away from the storm, and they will stand perfectly quiet. The men can get under the carts or stand out in the rain, as it suits them_ Care must be taken that horses do not stampede in a storm, as many travellers through the carelessness of their team- sters lose much time through this cause. All through the summer, mosquitoes are very trouble, some at night, and often put the horses almost wild. Ever}' evening, it is necessary to make a " smudge " to keep off the flies and enable the horses to eat a little during the night. It is made by lighting a fire with a little dry wood, and then putting on green sticks and covering all up with sods, so as to make a continuous smoke. When flies are troublesome and a little wind stirring, horses always feed head to wind, and it is necessary to note the direction of the wind before retiring to rest, as it is nothing unusual to find that the horses have gone off miles during the night. By noting how the wind blows in the evening and how it is in the morning, a man of some experience will always go straight to the horses, even if they are miles ADVICES TO SETTLERS AND TRAYELLERS. 649 awaj. Many parties think it cruel to hobble horses every night after having been in harness all day, but experience proves that horses eat more and wander less by adopting thia practice. My practice was always to make a smudge, hobble my horses in good pasture, and trust to their being all right in the morning. By following this practice I never lost a horse, and during two summers, travelled 4,300 miles up and down the prairie chiefly by compass. Besides looking to the comfort of our horses, we should "be careful of ourselves and always take pains to make our- selves comfortable. The chief trouble of the North-West is the mosquito, and to a sensitive person, they are a source of constant torture. I have seen men so punished by them, that their eyes were closed, their necks swollen, and they suffered great agony. There -S no use in disguising the fact of their constant presence, and of their being a : eal plague. Settlers on the prairie must expect them for years to come, but with the progress of settlement they will in a great measure disappear. Tents can be kept clear of mosquitoes only by closing every aperture by which they can enter, as one small hole will often admit more flies than two men can dispose of. They enter tents just in the same way that bees enter a hive, and should one make its way in it will be followed by hundreds in a short time. After closing the tent so that none could enter, a man, with a lighted candle, soon singed the wings of those within, and for the evening and night we had immunity from their attacks. On account of the flies the rule is to pitch the tent in summer always on a knoll, but in winter or after the flies have disappeared in a low sheltered spot. In the depth of winter, tents are not used by travellers except they are supplied with a small stove. A winter camping place is chosen in a thicket or grove where wood is abundant. Should the party be travelling where there is spruce or any coniferous trees, one section of the party gets vsrood while 650 MANITOBA AND THE GREAT NORTH-WEST. the other clears away the snow from where the sleeping place and fire are to be. Brush is strewn thickly for a bed and in the direction of the wind it is piled up to make a wind-break. The fire is built in front and along the back a piece of canvas is stretched which keeps out the wind and reflects the heat. Buffalo robes and blankets are now spread on the boughs, and although the temperature of the air may be far below zero, comfort and genuine pleasure reign in the bivouac, and no thought of discomfort enters the mind of any one. I have lain in such camps when the temperature was very low, and never experienced any real discomfort. White men always lie with their feet to the fire, but very frequently the Indians lie with their side to it, and when one side gets cold they get up, put on a fresh log, and lie down in the opposite direction. Some years since it was rather difficult to obtain good water on many of the trails, and few ventured to leave them in search of it. A Half-breed's plan of getting good water is to taste it, and if it is no worse than a weak in- fusion of Epsom salts he will pronounce it very good for tea. After some experience and close observation I discovered that where a certain species of sedge ( Garen aristata) grew in profusion there I might look for good water at any season if the grass remained green. Late in the fall many pools that contained good water in the summer become brackish. This was formerly the case in and around the Touchwood Hills, and much difficulty was experienced in obtaining sweet water. In the fall of 1879 I noticed every pond that con- tained green sedge had sweet water. On the other hand those where the sedge was rotting and apparently dying invariably had brackish or very poor water. Since then I have carefully noted the water pools, and in all cases the sedge gave the same results. When the seasons become, drier than they are at present many pools in Moose Moun- tai and the Touchwood Hills and other localities, which at ADVICE TO SETTLERS AND TRAVELLERS. 651 present have comparatively pure water, become brackish in the autumn. Prairie fires are dangerous both to settlers and travellers, but especially to the former. During the month of August the grass begins to dry up owing to the great heat and the dryness of the atmosphere. September completes what August commenced, and by the first week in October all the grass is dry, and for hundreds of miles a continuous hay meadow extends without a break. At this time scarcely a shower falls, and in the middle of the day it is very warm and often the wind is strong. A party of travellers stop for dinner, and without due precaution light a fire, or a smoker throws down a lighted match. In an instant the grass is in a blaze, and before a person has time to think the fire is rods away and speeding over the prairie as fast as a horse can gallop. Numerous fires started as above have been known to run over 100 miles without stopping. Should the fire reach a trail in the night it will scarcely ever cross it as the ruts stop it most efiectually. A fire on our buffalo plains is not the formidable affair that novelists and many travel- lers make it. The grass is generally short, seldom over a foot high, and on this account the fire never attains much volume. Although many times quite close to fires, in only one in- stance did I have to protect myself from them. While lying in camp on the plain nearly 100 miles southwest of Battle- ford on the first Sabbath of October, 1879, my assistant noticed huge volumes of smoke rising in the southwest, but a great distance off". He and I were travelling alone, and naturally felt some fear of the fire reaching us. Without any hesitation he ran for the horses, and besides hobbling them we fastened a long line to each of them and tied them to the carts. We at once took down our tent and packed everything up, putting all our stuff" in the carts. We saw that the fire was coming straight for us, and that a very 652 MANITOBA AND THE GREAT NORTH-WEST. short time would elapse before it would be upon us. The sun was setting and before dark we harnessed the horses and placed them in the carts and moved to a small patch of sandy ground where the grass was quite thin and waited for the enemy. The lurid glare in the heavens kept increas- ing as the shadows of evening fell, and darkness had not settled over the prairie before we saw long tongues of flame thrown up against the sky from a distant ridge ; these dis- appeared and the bright glare only remained. A few min- utes pass and a nearer ridge is reached and a long line of fire is seen to cross it and disappear. Horses and men are now aroused, and I try if the grass where we are will carry fire and find it will not. We at once move to its outer edge and securely fasten our horses, so that they may not break loose and leave us. A few minutes more and the fire has passed the last ridge, and with the speed of a fast horse it bears down upon us. As it came near us the whirling smoke and leaping flames seemed to take the forms of living things that were in terrible agony and added largely to the sublimity of the spectacle. When it reached our oasis it swept past on either side, and a few gulps of smoke, accompanied with a strong hot wind, were the only discomforts it caused us. When it was past we saw that it kept an even front, and wherever the grass was long and thick the flame continued for some time after the first rush had passed. A stiff" gale had been blowing all day and continued throjigh the night, and before the next evening, this fire reached the Eagle Hills, and burnt up all the hay cut by Red Pheasant's band. Where it burnt the hay, it was fully 130 miles to the northeast of us. This same fire swept up between the two Saskatchewans the next night, and burnt up the tent of a party of the Mounted Police who barely escaped with their lives, as the fire came upon them when they were asleep. Ten days after, I crossed the same tract, and for twenty-four miles our horses never obtained a mouthful of food, as the fire had licked it all up. ADVICE TO SETTLERS AND TRAVELLERS. 653 Settlers can easily protect their houses, barns, and stocks by ploughing a few furrows around them, and without this or something else is done there is no safety. Burning a ring of grass, in the evening, outside of the ploughing is more effectual, but this should be done during a calm even- ing, and the fire stopped after it has burned the required breadth. Many new comers think these precautions are unnecessary, and hence the doleful accounts of the loss of hay and even houses, which we read of from time to time. "While travelling on the prairie, in September and Octo- ber, no fire should be lit in the middle of the day, without two or three persons are standing ready to extinguish the grass when sufficient ground is burnt over, for safety. No fire should be left uncovered when the party moves away, and it is the duty of the leader to see personally that all fire is either extinguished or covered up. There is a pen- alty of $200 for the starting of a prairie fire, and as the informer gets half the fine, Indians and Half-breeds are constantly on the alert, during the dangerous season, to pounce on any delinquent. Many people blame the Indians for setting the prairie on fire, but my experience leads me to lay the blame on white men, especially the young bloods who go shooting in the fall. A stump of a cigar dropped on the prairie is much more dangerous than an Indian fire. Travelling on the prairie is an easy matter with or with- out a road. Experience combined with intelligence, how- ever, are necessary to ensure success. My plan is never to combat a difficulty without seeing my way to overcome it. Most people, when travelling, take a guide or a man who has been over the country before, and who knows or pro- fesses to know where the water-pools are. As a rule, these men have not a high order of intelligence, and dare not venture off the beaten track. They know nothing of the use of the compass, and laugh at any person thinking to cross the country by the aid of one. Should these parties 654 MANITOBA AND THE GEEAT NORTH-WEST. get into a region not visited by tliem before they are per- fectly helpless, and will do more barm than good. When the Mounted Police first entered the country, they always took a guide when moving from point to point. On one occasion, when Colonel Irvine and party were passing frjm Fort Walsh to the Saskatchewan, in the direction of Battleford, they camped on the open plain. In the morning, when they started off, the atmosphere was cloudy and the sun obscured. After travelling steadily all day, they reached their old camping place in the evening, although they thought they were forty miles away from it. When ques- tioned, the old guide explained that he had travelled with the wind on his right hand all day, and could not be blamed if it changed. Numerous instances of a like nature could be related, each instance showing that guides are mere en- cumberances when in an unknown district. Should any per- son be travelling in the surveyed districts. Captain Allen's Prospector's Manual will be found invaluable, as it is supe- rior to a whole army of unlettered guides, and will never lead any one astray. Outside of the surveys, a map and pocket compass are necessary, and these should be studied constantly until the mind takes in the whole country, and a traverse of an unknown region becomes only a pleasurable excitement. Owing to the absence of woods and the rolling character of the country, parties may cross it in any direc- tion, provided they take the risk of finding water at con- venient distances. White mud swamps are the terror of both Indians and Half-breeds. Should a person incautiously attempt to cross one or even lead a horse to the margin to drink, he will find it a difficult matter to get on firm ground again. In the south, where the rainfall is light, these swamps, in the dry season, are hard baked clay flats, covered with a sprink- ling of saline plants. Proceeding northward, these gradu- ally change their character, and pass into the much dreaded ADVICE TO SETTLERS AND TRAVELLEBS. 655 swamp. One of the worst kind has a dry surface which will not bear the weight of ^ horse, and into which he sinks deeper at every step, until he lies down from sheer exhaus- tion. The much dreaded salt plain west of the Touchwood HUls, contains a number of swamps of the very worst de- scription. Southwest of the hills we became entangled in a series of these, in the autumn of 1880, and it was only by hard work and much ingenuity that we saved our horses. When we entered on the clay flat it seemed quite hard, but first, one horse went down and then another, until nine were lying panting on the yielding surface. By the time we got across, both men and horses were almost worn out, as all the carts had to be taken over by hand, and the men had to assist the poor horses when they sunk down com- pletely exhausted. Nearly all the " sloughs " spoken of by travellers are embryo white mud swamps. In every case, they are merely saturated Cretaceous clay, and pass from liquid " white " mud in the north to hard baked clay flats in the south. These constitute the " bad lands " of the south, and the saline swamps and " sloughs " of the north. As a rule, creature comforts are provided in abundance by all travellers, and yet very few know how to make them- selves comfortable under all circumstances. Tea and suffi- cient food of any kind will suit on the plains as all parties are blessed with a good appetite. Food, however, is not all that is necessary. In no case should a tent be pitched care- lessly or with the door to the west. Many storms come up suddenly from that quarter in the night, and a carelessly pitched tent admits the rain or what is much worse the tent is blown down in the midst of the storm and every possession is sent to the four winds or is thoroughly soaked. No careful traveller will retire except he feels assured that he is secure for the night. When the camping place is 656 MANITOBA AND THE GREAT NORTH-WEST. reached the evening may be beautiful and a gentle wind blowing, so that the mosquito is not abroad and the tired and possibly lazy travellers may decide to sleep under the canopy of heaven. After they get asleep the wind falls and they are awakened by the myriads of flies which cause them such discomfort that ever after when they think of that terrible night they shudder involuntarily. Flies and storms should always be expected in summer and always guarded against. No person need have any fear of catching cold on the plains by exposure to the night air, as such a thing never happens. "When preparing the tent for the night a water- proof blanket should always be placed next the ground and over that a bufialo robe with the hair side up. After this any kind of covering will do. Care must be taken on the return to civilization that the traveller does not catch cold by sleeping in a close room, as experience teaches that such rooms are extremely dangerous. It is wise to open the window and door of the room even if the temperature of the air is at zero, so that you may escape a severe cold. After the first season I always did this and by so doing es. caped the colds that all surveyors complain of when they return to civilization. Travellers should always have a five or ten gallon keg with them, and see that this is filled with good water at least once a day. When travelling without a guide this is absolutely necessary, as water may be extremely scarce in the district where a person may chance to be and great suffering may result. In July, 1880, myself and party were thirty hours without water owing to the carelessness of the men whose business it was to see that a supply was on hand. We were never without water again, and I gave no instruc- tions regarding it. The above incident happened on the western part of the Great Souris Plain. The plain for sixty miles east of the Canadian Pacific Railway crossing Moose ADVICE TO SETTLERS AND TRAVELLERS. 657 Jaw Creek is almost waterless, and great caution is necessary when traversing it. Many other localities where water is scarce might be cited, but it is unnecessary to mention them as wise men will be prepared for all such while fools will run to their own destruction, or like my party suffer for their neglect of known duty. Water suited for horses is generally obtainable at least once a day, but that for culi- nary purposes is much more scarce than many imagine. I speak of surface water. It is not necessary to enumerate all the little things travellers should carry, but axes, a saw, an augur, a drawing knife, a spade, rope, and twine are absolutely required, wire of two sizes, a hammer, and clout nails or tacks should always be taken. Medicines are seldom needed, but salve and plaister for cuts should never be dispensed with as the traveller is liable at any moment to meet with an accident. The cooking utensils should be in charge of one man even if only for a day at a time, and should be counted after every meal. Knives, forks, spoons, and many other small articles get into the grass and without constant watchful- ness and extreme care get lost. Axes, whetstones, and knives are left lying around by most travellers, and are just the things most required on a long journey. In every well- organized party one man is detailed to go over every part of the camping ground after the others have started and pick up all the odds and ends that may have been left. The chief difficulty experienced in traversing the country is the crossing of rivers and small streams. Besides the crossing there is the descent into the valley and the ascent out of it. With loaded carts and too often baulky horses this is no easy matter. At this time the spade is always useful to dig down the bank so that the water may be reached. Sometimes the stream may only be a few feet wide but have a quagmire on either side and not a bush for miles. 42 G58 MANITOBA AND THE GREAT NOKTIf-WEST. In a case of this kind long grass or sedge is cut and a track made for the horse to walk on, and although he may tremble in every limb on account of the shaking of the bog he takes his load across. The others follow and that difficulty is sur- mounted. Another time a creek is reached that is quite narrow but running in a deep trench. The horses are taken from the carts, the ridge poles of the tents are stretched across the creek and the carts drawn across bv hand. In August, 1880, Ave reached the dry bed of a creek on the north side of the Cypress Hills, and after examining it for miles, found it apparently impassable. The banks of the creek were perpendicular, and the bed a quicksand. So soft was the sand that the man who tried it had to cross on his hands and knees. A brief consultation was held, and while one party cut down willows to bridge the quicksand, another dug down the banks. In an hour we were across and ready for our next difficulty which soon came. The day was extremely warm, men and horses were thirsty, and as it drew on towards noon, I climbed a hill and saw scarcely a mile away, a beautiful lake glistening in the sun. With joyful hearts we hurried on, and unhitched close to the lake. The horses naturally went to the water, but to our astonisfment would not touch it. An examina- tion showed that Oi'.r beautiful lake was liquid inud, with scarcely an inch of water on the surface. We had our din- ner, as we carried our own supply, but it was sundown before our utmost endeavors could find any for the horses. On the loth July, 1879, we reached the elbow of the South Saskatchewan, at the head of the Qu'Appelle valley. At this point, the river was 770 yards wide, and flowing with a steady current. Sixty miles to the north, there was a ferry, and forty miles to the south, Palliser had crossed, twenty-three years before, but witli the loss of a waggon. After examining the river carefully, both above and below the Elbow, we decided to cross at that point. The means ADVICE TO SETTLERS AND TRAVELLERS. 659 "was the next consideration. There was no timber to con- struct a raft, so we decided to build a boat. We had no boards, but we had a large tent, water proof blankets, and cart covers. John Matheson, of Winnipeg, who had charge of the horses and outfit generally, made a wooden frame about nine feet long and four and a half feet wide at the stern, shaped like the letter A, and interlaced it with willows. Over this we put the tent, and over all we nailed the water-proof blankets. By means of this frail boat, we purposed taking across a river nearly half a mile wide, four months provisions, all our camp equipage, four carts, and two buckboards, besides risking our own lives. The night before we undertook to cross was an anxious one, and shortly after sunrise we were ready to make the attempt. Our boat was found to leak considerably, but one man bailing could keep it afloat. A small load was put on board, and one man pulling two small oars and another bailing, they started. After crossing a small branch close to us, they drew the boat for a long distance up the river by walking on a sand bar. When they thought they had ascended far enough, they attempted to cross the main channel, but the width (over 500 yards) being much greater than they expected, tliey were unable to make the shore, and landed the stuff on an island near the further side. In coming back, they were carried over half a mile below our camp, and had to haul the boat up. They were in good spirits, however, as the boat was quite safe, and by going further up the bar they were sure they couid make the land. Another load was soon on board and hauled far up the sand bar, and was easily taken across. All working with a will, the greater part of the provisions and baggage were across before night. Much time was lost in getting the horses across, as they frequently turned back when almost half across. One or two were nearly drowned, be- 660 MANITOBA AND THE GREAT NORTH-WEST. ing unable to stem the current for 500 yards on a stretch. These, after resting a while on a bar some distance below us, finally reached the shore. The next forenoon, we brought over the remainder of our outfit, and by sundown camped on the crest of the valley, with the mighty river sweeping in graceful curves at our feet. Behind us lay the river, and in our front those illimitable plains which on our maps were shown as a waterless and treeless desert. On the morrow, we entered on the great plain which we eventually traversed in every direction, and lifted the veil which had enshrouded it for many years. This jyiagram is intended to illustrate the uni- form disposition of Free Grant and Pre-emption Lands, also of Railway or Public Lands as the case may he, in each Township in Manitoba and the North- West Territories. '■ — n — "^ 1 ■ \ -^;i- - 1 ^ I 1 ■ 1 1 __^2-_- 1 1 1 1 1 1 I 1 1 --34- - 1 _ 1 1 1 — 3|5 --- 1 1 1 i ( 1 „ 1 \ \ 1 1 ■ 1 . ! -19 — 1 1, i 1 1 Sch'ool - 29- 1 La^ds 1 1 ; 1 i 1 —27— 1 1 HBiCas __ 26 ~ Lands 1 1 1 ■ - 1 ■ 1 1 2,Q — 1 r 1 L — 4- - - 1 1 ■ 1 1 ---22.-- \ 1 1 1 \ 1 1 1 1 1 1 i 1 1 1 1 1 1 ■ --lie- 1 1 1 1 1 - -1'5-- 1 \ i - 1 1 1 - 14 — 1 1 1 1 1 1 r 1 1 7—- 1 1 H.BiCos 8 LAHtXS 1 1 9 1 1 1 - -10- 1 1 1 1 1 SCHJOOL -11 LaMos 1 1 ' 1 - 12 - ) 1 1 1 _.L_ 6 i 1 5- - 1 1 1 4—- 1 1 1 1 5 ' [ 1 1 1 1 -—-2 - 1 1 ' i 1 - 1 - Homestead and Fre-emption Lands. Railway or Fuilic Lands, as the casemay he. CHAPTER XXXV. North-West Land Regulations and Mode of Survey. Inauguration of the Surreys — The International Boundary — Principal Meridians — Size of Townships — Numhering of Ranges and Townships-^Base Lines — Correction Lines- Size of Townships — Eoad Allowances — How Sufyey Lines are Marked on the Ground Dominion Land Regulations — Diagram showing the Division of a Township into Sections General Regulations — Homesteads and Pre-emptions — Colonization Plan Number One Plan Number Two — Timber for Settlers — Pasturage Lands— General Provisions— Canadian Pacific Railway Lands — Conditions of Sale — Liberality of Canadian Land Regulations —Hudson's Bay Company's Lands — School Lands — Lands at Private Sale. Immediately after the preliminaries for tlie transfer of the North-West Territories had been arranged between the Imperial and Dominion Governments, Colonel J. S. Dennis, D.L.S. (late Deputy Minister of the Interior), was, on the 10th July, 1869, directed by the Hon. William Macdougall, Minister of Public Works, to repair to the Red River and prepare a plan for laying out the country into Townships. After visiting the country and consulting with the Crown Lands Department of the Dominion and the Public Lands Department of the United States, a plan of survey was drawn up and adopted by the Minister of the Interior. During the summer of 1873 the International Boundary, lat. 49°, was established by the Boundary Commission ap- pointed by the Imperial and United States Governments. This line was fixed upon as the base of the surveys, and was thereafter known as the " First Base." From this line others were run at right angles northward and named Principal Meridians. The First Principal Meridian runs northward from a point on the International Boundary, about eleven miles west of the town of Emerson. The Second Principal Meridian is established upon the 102nd meridian of west longitude, passing about thirty miles west 662 MANITOBA AND Tll£ GREAT NORTH-AVEST. of Fort Ellice. The Third, Fourth, and Fifth Principal Meridians are identical with the 106th, 110th and 114th Meridians respectively. The latter passes close to Forts Calgarry and Edmonton. After mature deliberation it was decided to lay out the country in four-sided townships of almost a square form. Each township measures on its east and west sides from centre to centre of the road allowances, which form its actual boundaries, exactly 483 chains, and on its north and south sides 486 chains more or less, subject to the deficiency or surplus resulting from the convergence or diverge .nee of the meridians, as the case may be, caused by the curvature of the surface of the earth. In numbering these townships certain terms were adopted which gave precision to each township no matter where situated. Starting at the First Principal Meridian on the International Boundary, the first township west of the Meridian was termed Range I, the next west. Range II, and so on till the Second Princi- pal Meridian was reached, when the numbering commenced again. It will thus be seen that the first township west of any Principal Meridian is in Range I west, and so on in regular order. The next step was to give position, and the first township was numbered Township 1, the next north Township 2, and so on as far as the surveys extend to the north. After establishing the First Base, or International Boundary, other lines were run twenty-four miles apart, parallel to this one and numbered Second,Third, Fourth, and Fifth Base as far as the surveys extend to the north. The country is afterwards laid out into blocks twenty -four miles square, or nearly that, each block containing sixteen town- ships. These blocks are contained between four straight lines, having a Base Line at the north and at the south. Exactly twelve miles from either Base a line is run east and west, named a " Correction Line," and on this line all correc- A ! ; J, ; 1 : 1 I : 1 '. I ^ I A ; 1 a 2! .... ^...A---i--y — i---?--f— *"' -----. — ] — J — .; ill. Ml ■ -3 — 1 j..._,j,...J— ^..„ ; ' ! 1 life H K) a 30 i-i Q t> S 2 i 1 i. i ^ I ' ' ' ■ A ■ < m jVo. 2. G A TOWNS ND LINKS. — . • r r--.-^---T >■ Jj»--i--j-- — ^ . J r '--■5^--;--R— ■ r 1 1 1 1-14-1- , r - - i 5 "I r— 1 ',-■■■[ •' i :• i !■—••—■—?—■ > 1 ! < ! 1 A J . ;-i-i-4- r- • 1 1 r— 1 3 s 1 -., r-rrri r— r— -r-'-B--' ;-"■] r — . i-4--f-f-- 1— o ■=9 "- .'-■!— r—.-"^ If-T- i-r— 1 r — -.-— r—y—-, r- | NORTII-AVEST LAND REGULATIONS. 665 tions occasioned by the convergence of meridians or any- other caus? are made. East of the First Principal Meridian the Ranges are numbered edst of that meridian and the townships numbered as usual. Every township is sub-divided into thirty-six " sections," each containing one square mile or 640 acres, more or less. All townships are subject to the conveyance and divergence of meridians, together with certain road allowances having a width of one chain on each section line running north and south, and on every alternate section line running east and west. Under the old system of survey all road allowances were one chain and a half (110 feet) wide, but a new system was inaugurated last year by which all are now reduced to one chain (66 feet). Diagram No. 1 gives a township as laid out under the old system of survey, and No. 2, one under the new system. The following extracts are taken from an excellent little work published by Captain C. W. Allen, of Winnipeg, en- titled the Land Prospector's Manual and Field Book : — " Survey lines are marked on the ground by the planting or erecting of such posts, stones, mounds, or other monu- ments as will serve the temporary purpose of guiding Prospectors through the country, and which also constitute permanent landmarks to establish the legal boundaries of farms held by different proprietors. " Only a single row of posts (or other monuments) to in- dicate the corners of townships, sections, or quarter-sections is placed on the ground to show the line surveyed, except in the case of correction lines. Such posts are invariably planted along the wesiei-n limit of the road allowance on all lines running north and south, and in the southern limit of the road allowance on all lines running east and west. It follows, accordingly, that such corner posts always stand on the northeast corner of the township, section, or quarter- sections to which they belong ; also, that these single lines 666 MANITOBA AND THE GREAT NORTH-WEST. of posts govern the relative position of the corners on the opposite sides of the road allowance (or road allowances) on which they stand, whether the same may be those of adjacent townships, sections, or quarter sections. (See dia- gram No. 2.") On correction lines, however, the boundaries on both sides of the road allowance are planted with monuments indicat- ing the township, section, and quarter-section corners. " The kind of monument employed varies somewhat, according to the material available in the locality surveyed ; but the position in which all such are placed is governed by unalterable rules, and the inscriptions or marks are all in conformity. " In a timbered country, a post, three inches square, and showing two feet above ground is firmly planted at the township or section corner to be indicated, and it bears marks as hereafter described. The post distinguishing a quarter-section corner in such a region is three inches wide, being flattened on two sides, and it stands eighteen inches only above the surface, with the flattened sides at right angles to the line on which it standi. In a wooded region where stone abounds, corners are sometimes defined by simple stones correctly planted and properly marked. The position of all such corners are indicated by simple monuments, such as a post or stone, and further defined by the astronomical bearing, and dis- tance therefrom being marked in red chalk upon some ad- jacent tree, the side of which nearest to the monument ig also inscribed with the letters " B. T." cut into the trunk." " In a prairie country, the posts stand in the centre of mounds, generally of earth, thrown up in the form of right- angled pyramids. At the corners of townships, these mounds are three feet high, their bases being six feet square ; at the corners of sections or quarter-sections the mounds stand at two feet and six inches high, and their NORTH-WEST LAND REGULATIONS. 667 bases are five feet square. In the formation of these mounds, the earth is taken from four square pits, each being opposite one of the four sides of the mound. In a prairie country, that is also stony, the mounds are often built of stones, piled up around the posts, so as to conform, as nearly as possible, to the earth mounds in size and shape. " If a township or other corner fall in a ravine, the bed of a stream, or some similar situation where it would be im- possible to erect a monument of a permanent character, and should a " bearing tree" not be obtainable the surveyor in- dicates the position of such corner by erecting at the nearest suitable spot a " witness mound." In this case the mound is in the form of a cone 2ft. 6in. high, its base having a dia- meter of 6ft. The post in the centre is marked " W. M." and also inscribed, in red cbalk, with the bearing and dis- tance to such corner. " The posts in all mounds show at least ten inches above the apex of the same, whether the latter have been built of earth or stones. " On ordinary surveyed lines the posts and mounds are so placed that their angles rest upon the line on which they stand. " On correction lines, however, the post and mounds are erected square with the line, which passes through the centre of two sides of the mound. " Iron posts, which are placed at every tovmship corner,, consist of either iron bars or tubes, driven into the ground with a sledge, and inscribed, by means of a cold chisel, with the necessary marks. The mounds in connection with such monuments form an exception to the general rule, in that they are so placed that the iron post stands at the northern angle thereof There is, however, with iron posts, the usual difference in respect to monuments on correction lines, the mounds in connection with which are built with their bases facing the cardinal points of the compass, the iron post 668 MANITOBA AND THE GREAT NORTH-WEST. being established in the centre of the base of the mound fronting the road allowance. '"' The letters, marks, and figures on posts and trees are distinctly cut in with a knife or scribing iron ; those on iron posts and stone corners with a cold chisel. " Quarter-section corner posts are simply marked with the conventional sign " j " to indicate their character, and bear no inscription showing to what township or range they belong. "Posts or stone monuments indicating all other corners bear sufficient marks to thoroughl}- indicate the position they are intended to legally establish; and must always be read from the top of the post downwards. " On township corners the upper figure on either side of the post indicates the number of the township which that side of the post faces, and the next figure indicates the range. " On all other section corners, whether on township lines or in the interior of a township, the numbers of the sections only are to be found on the corresponding faces of three sides of the post ; but in addition to the section number, the number of the township and that of the range appear on the fourth face, which is invariably the south-west one. " The posts planted along the correction lines simply ex- hibit luarks to show the number of the townships and sections the boundaries of which they form respectively. Township corners have the number of the section shown on the west side of the post, and the numbers of the township and range on its north side. In cases where the posts stand in the nortliern limit of the road allowance, the letter " E " for road alone is marked on the other two sides. A correspond- ingly opposite plan will be found to have been adopted in marking the township corner posts in the southern limit of the road allowance on correction lines. Section corner posts on correction lines have the numbers of the sections on NORTH-WEST LAND REGULATIONS. 669 their east and west sides, the letter " R " on the side facing the roadway, and on the fourth side the number of the township and range. " In ranges numbered from the First Principal Meridian the letters " E " or " W " are marked on the post after the number of the range, to denote that it is east or west of that meridian." The settler from the United Kingdom will at first find the nomenclature of this system of survey a little new and strange ; but he will, on slight acquaintance with it, be- come charmed with its simplicity and accuracy. The surveys are marked on the prairie itself by iron and other kinds of monuments and posts at the corners of the divisions and subdivisions ; and so soon as the settler makes himself acquainted with these, he will instantly understand the position and extent of his own farm on the prairie, or of any other in the country ; or when travelling in any part of the country these posts will tell him at a glance exactly where he is. A settler may obtain a grant of 160 acres of land free, or even numhered sections, on the condition of three years con- tinued residence, and payment of the ofl&ce fees amounting to ten dollars, and he may purchase on reasonable terms adjoining portions of sections. A settler should obtain from the Government Agents general information as to lands open for settlement. All even numhered sections (except 8 and 26, which are Hudson's Bay Company's Lands) belong to the Government, and are open, being specially reserved, for free homesteads and pre-emptions. Odd numbered sections (with exception of 11 and 29, which are School Lands) for twenty-four miles on each side of the Canadian Pacific Railway, may be generally stated to be railway lands, purchasable from the Company, and not open to homestead and pre-emptions. 670 MANITOBA AND THE GREAT NORTH-WEST. DOMINION LAND REGULATIONS. Diagram shewing the division of a Township into sections. Each section — a square mile- is subdivided into quarter sections of 160 acres. Those shaded green are reserved for Free G-rant Homesteads and their att;iched Pre-emptions. The following Regulations for the sale and settlement of Dominion Lands in the Province of Manitoba and the North-West Territories shall, on and after the first day of January, 1882, be substituted for the Regulations now in force, bearing date the twenty-fifth day of May, 1881 : — 1. The surveyed lands in Manitoba and the North-West Territories shall, for the purposes of these Regulations, he classified as follows : Cla^u A. — Lands within twenty-four miles of the main line or any branch line of the Canadian Pacific Railway, on either side thereof. Class B — Lands within twenty miles, on eitlier side, of any projected line of railway {other than the Canadian Pacific Railway) approved by Order in Council published in the " Canada Gazette." Class C. — Lauds south of the main line of the Canadian Paciiic Railway not included in Class A or B. Class D. — Lands other than those in Classes A, B, and C. 2. The even-mmibored sections in all the foi-egoing classes are to be held exclusively for homesteads and pre-emptions. a. Except in Class D, where they may be affected by colonization agreements as hereinafter provided ; b. Except where it may be necessary, out of them, to provide wood lots for settlers ; c. Except in cases where the Minister of the Interior, under provisions of the Dominion Land Acts, may deem it expedient to withdraw certain lands, and sell them at public auction or otherwise deal with them as the Governor in Council may direct. .3. The odd-uiimbereil sectious in Class A are reserved for the Canadian Paciiic Rail- way Company. 4. The odd-numbered sections in Classes B and C shall be for sale at $2.50 per acra payable at time of sale ; a. Exrept where they have been or may be dealt with otherwise by the Governor General in Council. 5. The odd-numbered sections in Class D shall be for sale at $2 per acre, payable at time of sale, C. Except where they have been or may bo dealt with otherwise by the Governor in Council. b. Except lands affected by colonization agreements, as hereinafter provided 6. Persons who, subsequent to survey, but before the issue of the Order in Council of 9th October, 1S79, excluding odd-numbered sections from homestead entry, took posses- sion of land in odd- numbered sections by residing on and cultivating the same, .shall, if continuing so to occupy them, be permitted to obtain homestead and pre-emption entries as if they were on even-numbered sections. NOKTH-WEST LAND REGULATIONS. 671 PRE-EMPTIONS. 7. The prices for pre-emption lots shall be as follows : For lands in Classes A, B and C, $2.50 per acre. For lands in Class D, $2.00 per acre. Payments shall be made in one sum at the end of three years from the date of entry, or at such earlier date as a settler may, under the provisions of the Dominion Land Acts, obtain a patent for the homestead to which such pre- emption lot belongs. COLONIZATION. Plan Number One. 8. Agreements may be entered into with any company or person (hereinafter called the party) to colonize and settle tracts of land on the following conditions : a. The party applying must satisfy the Government of its good faith and ability to fulfil the stipulations contained in these regulations. b. The tract of land granted to any party shall he in Class D. 9. The odd-numbered sections within such tract may be sold to the party at %% per acre, payable, one-fifth in cash at the time of entering into the contract, and the balance in fom- equal annual instahneuts from and after that time. The party shall also pay to the Government five cents per acre for the survey of the land purchased by it, the same to be payable in four equal annual instalments at the same times as the instalments of the purchase money. Interest, at the rate of six per cent, per annum shall be charged on all past due instalments. a. The party shall, within five years from the date of the contract, coloniae its tract. 1>. Such colonization shall consist in placing two settlers on homesteads on each even-numbered section, and also two settlers on each odd-numbered section. C. The party may be secured for advances made to settlers on homesteads according to the provisions of the 10th section of the Act 44 Victoria, Cap. 16 (the Act passed in 1881, to amend the Dominion Lands Acts). d. The homestead of 160 acres shall be the property of the settler, and ho shall have the right to purchase the pre-emption lot belonging to hig homestead at $2 per acre, payable in one sum at the end of three years from the date of entry, or at such earlier date as he may, under the pro- visions of the Dominion Lands Acts, obtain a patent for his homestead. e. When the settler on a homestead does not take entry for the pre-emption lot to which he has a right, the party may within three months after the settler's right has elapsed purchase the same at $2 per acre, payable in cash at the time of purchase. 10. In con.'iideration of having colonized its tract of land in the manner set forth in sub-section Ij of the last preceding clause, the party shall be allowed a rebate of one- half the original purchase-money of the odd-numbered sections in its tract. a. During each of the five years covered by the contract an enumeration shall be made of the settlers placed by the party in its tract, in accordance with sub-section b of clause 9 of these regulations, and for each bon& fide settler so found therein a rebate of one hundred and twenty dollars shall be credited to the party ; but the sums so credited shall not, in the aggre- 672 MANITOBA AND THE GREAT NORTH-WEST. gate, at any time exceed one hundred and twenty dollars for each bond fide settler found within the tract, in accordance with the said sub-section, at the time of the latest enumeration. b. On the expiration of the five years, an enumeration shall be made of the bona fide settlers on the tract, and if they are found to be as many in num- ber and placed in the manner stipulated for in sub-section b of clause 9 of these regulations, a lurther and final rebate of forty dollars per settler shall be credited to the party, which sum, when added to those previously credited, will amount to one-half of the purchase money of the odd-num- bered sections and reduce the price thereof to one dollar per acre. But if it should be found that the full number of settlers required by these regula- tions are not placed in conformity with sub-section b of clause 9 of these regulations, then for each settler fewer than the required number, or not placed in conformity with the said sub-section, the party shall forfeit one hundred and sixty dollars of rebate. C. If at any time during the existence of the contract the party shall have failed to perform any of the conditions thereof, the Governor in Council may cancel the sale of the land purchased by it, and deal with the party as may seem meet under the circumstances. d. To be entitled to rebate, the party shall furnish to the Minister of the Interior evidence that will satisfy him that the tract has been colonized and settled in accordance with sub-section 1) of clause 9 of these regfu- lations. Plan Number Two. \\. To encourage settlement by capitalists who may desire to cultivate larger farms than can be purchased where the regulations provide that two settlers shall be placed- on each section, agreements may be entered into with any company or person (herein- after called the party) to colonize and settle tracts of land on the following conditions : a. The party applying must satisfy the (ioverument of its good faith and ability to fulfil the stipulations contained in these regulations. b. The tract of land granted to p.ny party shall be in class D. C. All the land within the tract may be sold to the party at two dollars per acre, payable in cash, at the time of entering into the contract. The party shall, at the same time, pay to the Government five cents per acre for the survey of the land purchased by it. cl. The party shall, within five years from the date of the contract, colonize the township or townships comprised within its tract. e. Such colonization shall consist in placing one hundred and twenty-eight bonct fide settlers within each township. 12. In consideration of having colonized its tract of land in the manner set forth in sub-section e of the last preceding clause, the party shall he allowed ^ rebate of one- half of the original purchase money of its tract. a. During each of the five years covered by the contract, an enumeration shall be made of the settlers placed by the party in its tract, in accordance with sub-section e of clause 11 of these regulations, and for each bond fide settler so found therein a rebate of one hundred and twenty dollars shall be repaid to the party ; but the sums so repaid shall not, in the aggregate, at any time exceed one hundred and twenty dollars for each NOBTH-WEST LAND REGULATIONS. 673 bond fide settler found within the tract, in accordance with the said sub- section at the time of the latest enumeration. b. On the expiration of the five years, an enulneration shall be made of the bond fide settlers placed by the party in its tract, and if they are found to be as many in number and placed in the manner stipulated for in sub- section e of clause 11 of these regulations, a further and fii:r.! rebate of forty dollars per settler shall be repaid, which sum when added to those previously repaid to the party will amount to one-hj.if of the purchase money of its tract and reduce the price thereof i ) one dollar per acre. But if it should be found that the full number of settlers required by these regulations are not on the tract, or are not placed in conformity with the said sub-section, then, for each settler fewer than the required number or not settled in conformity with the said sub-section, the party shall forfeit one hundred and sixty dollars of rebate. C. To be entitled to rebate, the party shall furnish to the Minister of the Interior evidence that will satisfy him that the tract has been colonized and settled in accordance with sub-section e of clause 11 of these regula<- tions. Official Notice. 13. The Government shall give notice in the Canada Oazette of all agreements" en- tered into for the colonization and settlement of tracts of land under the foregoing plans, in order that the public may respect the rights of the purchasers. TIMBER FOR SETTLERS. 14. The Minister of the Interior may direct the reservation of any odd or even- numbered section having timber upon it, to provide wood for homestead settlers on sections without it ; and each such settler may, where the opportunity for so doing exists, purchase a wood lot, not exceeding twenty acres, at the price of $5 per acre in cash. 15. The Minister of the Interior may grant, under the provisions of the Dominion Lands Acts, licenses to cut timber on lands within surveyed townships. The lands covered by such licenses are thereby withdrawn from homestead and pre-emption entry and from sale. PASTURAGE LANDS. 16. Underthe authority of the Act 44 Tic, Cap. 16, leases of tracts for grazing pur- poses may be granted on the following conditions : — a. Such leases to be for a period of not exceeding twenty-one years, and no single lease shall cover a greater area than 100,000 acres. b. In surveyed territory, the land embraced by the lease shall be described in townships and sections. In unsurveyed territory, the party to whom a lease may be promised shall, before the issue of the lease, cause a survey of the tract to be made, at his own expense, by a Dominion Lauds Surveyor, tmder instructions from the Surveyor-General ; and the plan and field notes of such survey shall be deposited on record in the Department of the Interior. C. The lessee shall pay an annual rental at the rate of $10 for every 1,000 acres embraced by his lease, and shall within three years from the granting of the lease, place on the tract one head of cattle for every ten acres of land embraced by the lease, and shall during its term maintain cattle in at least that proportion. 43 674 MANITOBA AND THE GREAT NORTH-WEST. d. After placing the prescribed number of cattle upon the tract leased, the lessee may purchase land within his leasehold for a home farm and corral, paying therefor $2.00 per acre in cash. e. Failure to fulfil any of the conditions of his lease shall subject the lessee to forfeiture thereof. 1 7. When two or more parties apply for a grazing lease of the same land, tenders shall be invited, and the lease shall be granted to the party offering the highest pre- mium therefor in addition to the rental. The said premium to be paid before the issue of the lease. GENERAL PROVISIONS. 18. Payments for land may be in cash, scrip, or police or military bounty warrants. 19. These regulations shall not apply to lands valuable for town plots, or to coal or other mineral lands, or to stone or marble quarries, or to lands having water power thereon ; or to sections 11 and 29 in each Township, which are School Lands, or Sections 8 and 26, which belong to the Hudson's Bay Company. By order, Depabtmbnt of the Intekiob, LINDSAY RUSSELL, Ottawa, 23rd December, 1881. Surveyor Oeneral. CANADIAN PACIFIC RAILWAY LANDS. The land subsidy to the Canadian Pacific Railway Com- pany consisting of 25,000,000 acres, the odd numbered sec- tions are set aside for the purpose of this grant, for twenty- ibur miles on each side of the Canadian Pacific Railway (see Clause 2 of the Ofl&cial Land Regulations). As thes6 sections everywhere alternate with the even numbered ones held by the Government for free grants and pre-emp- tions, it is advisable to give here the regulations of the Pacific Railway for the sale and disposal of their lands. The following is a copy : — The Canadian Pacific Railway Company, Montreal, Canada, Nov. 2ith, 1881. The Company are prepared, until further notice, to sell lands for agricultural pur- poses, at the price of $2.50 per acre, one-sixth payable in cash, and the balance in five annual instalments, with interest at six per cent., a rebate for actual cultivation being made as hereafter described. The genera] conditions of sale are :— 1. That all improvements placed upon land purchased shall remain thereon until final payment for the laud has been made. 2. That all taxes and assessments lawfully imposed upon the land or improvements, shall be paid by the purchaser. 3. The Company reserve all mineral, cool or wood-lands, lands with water power thereon, or tracts for town sites and railway purposes ; but as regards wood NORTH-WEST LAND REGULATIONS. 676 lands, the purchaser will be permitted to cut a sufficient 0[uantity for fuel, fencing, and for the erection of buildings on his land. 4. The purchaser will be required within four years from the date of the contract for the purchase of the land, to bring under cultivation, and sow and reap a crop on three-fourths of the said land ; but if he shall erect buildings thereon satisfactory to the Company, and shall reside thereon continuously for three years, then the quantity to be cultivated shall be reduced to one half. Dairy farming or mixed grain and dairy farming to an extent to be agreed upon, will be accepted as the equivalent of cultivation, entitling the settler to rebate. 5. A credit of $1.25 per acre will be allowed for all land so cultivated during four years ; an extension of the time being granted in consideration of the erection of buildings and other improvements. 6. A reservation of 200ft, in width for right of way or other railroad purposes wi]l be made in all cases. 7 . If the purchaser fails to carry out strictly the conditions of his contract within the specified time, the Company reserve the right to cancel the contract, whereupon the lands would become forfeited and revested in the Company. But in case of forfeiture the Company would take into consideration an appli- cation for a new sale to the original purchaser at a revaluation. 8. Special contracts will be made with Companies for large tracts of land for settle- ment purposes or for cattle raising. 9. Liberal rates for settlers and their effects will be granted by the Company over its railway. For further information apply at the office of the Company, Bartholomew Place, London, England ; to John McTavish, Land Commissioner, Winnipeg, Manitoba, or to the Secretary of the Company, at Montreal, Canada. GEORGE STEPHEN, President- CHARLES DRINKWATER, Secretary. It will appear from a comparison of these conditions of sale by the Pacific Railway Company with the Dominion Government Land regulations, that if a family of four adults desire to settle together they may obtain a really large estate on very moderate terms. For instance, each of the four members of the family may settle on the four free homesteads, of 160 acres each, in any even numbered un- occupied section, each may then purchase another 160 acres at $2.50 (10s. stg.) per acre from the Pacific Railway Com- pany in the adjoining odd numbered sections. This is the same price as that offered by the Government pre-emption in the Railway Belt, with the exception that the Pacific Railway Company offer a rebate of |1. 25 (5s. stg.) per acre, within three to five years following the date of purchase, on condition of cultivation. The settlers while building on 676 MANITOBA AND THE GREAT NOETH-WEST. the homes'^eads and making cultivation thereon, would be able, within the time mentioned, also to cultivate the whole or the greater part of the Pacific Railway lands. The office fees for the Government Homesteads are $10 (£2 stg.). A family of four could, in this way, in three years obtain a. large estate of 1,280 acres of probably the richest wheat growing land in the world, at a merely nominal price, and thus secure a position not only of comparative but of sub- stantial wealth. Farmers with sons can with great advan- tage avail themselves of these conditions, and have the advantages of neighborhood in settling together. In cases where it is an object for families with means to take up and farm more extensive tracts of land, the regula- tions would also admit of this. For instance, two brothers might take up free homesteads and two quarter sections of any Government lands and pre-empt the remaining two quarter sections, thus obtaining a whole section or 640 acres for their homesteads and pre-emptions. They could then purchase the whole of each of the four adjoining odd num- bered sections of Railway lands, and thus obtain between them a large estate of 3,200 acres. By cultivating the odd sections and getting the rebate, this estate could be pur- chased on exceedingly moderate terms ; while the rule of the Pacific, Railway Company to insist on double the price of lands not cultivated, would act as a powerful dissuasive to acquiring lands for mere speculation, for the reason that the cultivation rebate is always open to the actual settler who, for some years to come, will have large tracts of land to choose from. The arrangement we have indicated is es- pecially desirable for settlers from England with means. It will be noticed that the price of the Pacific Railway lands is the same as that of the Government pre-emption in the Railway Belt. The terms of credit are also liberal. The land policy of the Government of Canada, combined ■with the advantages offered by the Pacific Railway Com- NOETH--WEST LAND REGULATIONS. 677 pany, is the most liberal of any on the Continent of North America. Liberality of Canadian Land Regulations. The Canadian Land Regulations having been very gen- erally represented to be more onerous and less liberal than those of the United States, it is proper to point out for in- tending settlers that ten dollars ($10) covers the whole of the ofl&ce fees in Canada, either for a pre-emption or a home- stead ; but in the Western States there are three fees, one of eight dollars, payable on entry, another of eight dollars for a commission, and another of ten dollars when the patent is issued, making twenty -six dollars ($26.00). In some of the States the fees are thirty-four dollars ($34.00). The lands are sold at $2.35 and $1.25 per acre. These prices are nearly the same, but the difference is favorable to Canada. In fact it is repeated that not on the Continent of America, and it is believed not elsewhere are the Land Regulations so favorable as in Canada. It is provided by the Canadian Naturalization Act, that aliens may acquire and hold real and personal property of every description, in the same manner and in all respects, as a natural born British subject. The only disqualification of aliens is, that they are not qualified to hold office under the Government, or to vote at parliamentary or municipal elections. The oath of allegiance required of aliens who desire to become British subjects simply expresses fidelity to the Queen and Constitution, without any discrimination against the nation from which the aliens come. To take up the United States Government land the fol- lowing oath is required to be taken : — DlSTEICr COUET, , Judicial District, ( State of County of ) J do swear tliat I will support the Constitutiou 678 MANITOBA AND THE GREAT NORTH-"WEST. of the United States of America, ard tliat I do absolutely and entirely "Renounce and Abjure for ever all Allegiance and Fidelity to every Foreign Power, Prince, Potentate, State or Sovereignty whatever, and particularly to the Queen of Great Britain and Ireland, whose subject I was. And further, that I never have borne any hereditary title, or been of any of the degrees of Nobility of the country whereof I have been a subject, and that I have resided within the United States for five years last past, and in this State for one year last past. Subscribed and sworn to in open Court I this day of 18.... ' Clerk. Hudson's Bay Company's Lands. Sections No. 8 and No. 26 in every township are Hudson's Bay Company's lands, and all settlers must be careful not to enter upon them before they have acquired them from the Company. The prices vary according to locality. Mr. C. J. Brydges is the Land Commissioner of the Company. His official residence is at Winnipeg, Manitoba, and applications may be made to him. Under agreement with the Crown the Hudson Bay Company are entitled to one-twentieth of the lands in the fertile belt, estimated at about seven million of acres. School Lands. Sections No. 11 and 29 in every township are School Lands. That is, the proceeds from their sale are to be ap- plied to the support of education. They are not attainable at private sale. When disposed of it will be at public com- petition by auction. All squatters on those lands, therefore, will have to pay for them the price they bring by auction when sold, or they will pass by that sale out of their hands. Lands at Private Sale. The settler may sometimes find it convenient to buy lands, partially improved, with buildings and fences upon them at private sale. It very frequently happens that Half- breed or other lands may be obtained on moderate terms. CHAPTER XXXVI. StatiMics. Population of the Dominion in 1881 as Compared with that of 1871 — Population of the Cities and Towns — Place of Birth — Religious Belief. — Areas of the Provinces, etc. The purpose of the following chapter is to give in an epitomised form the statistics of the Dominion, commencing with the population, showing the nationalities and religions of the inhabitants, as well as the areas of the different provinces J together with a table of all cities and towms having a populalion of over 5,000, and such other infor- mation as could be put into the limited number of pages at our disposal. TOTAL POPULATION OF THE DOMINION. Census of 1861 3,090,561 « 1871 3,485,761 " 1881 4,324,810 POPULATION BY PROVINCES. 1881 1871. Ontario 1,923,228 1,620,851 Quebec 1,359,027 1,191,516 New Brunswick 321,233 285,594 Nova Scotia 440,572 387,800 Prince Edward Island 108,891 94,021 Manitoba 65,954 , 12,228 British Columbia 49,459 . 10,586 The North-West Territories 56,446 . 680 MANITOBA AND THE GREAT NORTH-WEST. POPULATION OF CITIES AND TOWNS HAVING OVER 5,000 INHABITANTS IN 1881 COMPARED. 1871. 1881. Montreal Quebec Toronto Halifax St. John Hamilton Ottawa London Kingston Brantford St. Catherines . . . Thi-ee Rivers . . . Belleville Guelph Levis Fredericton Chatham , Sorel Port Hope Brockville Peterborough . . . St. Jean Baptiste Stratford Windsor Lindsay Woodstock Gait St. Hyacinthe . . . St Thomas Hull (city) Moncton (town) . Winnipeg (city) . Victoria (city) . . . Portland Charlottetown . . Sherbrooke St Henri Quebec. Ontario. Nova Scotia. New Brunswick. Ontario. Quebec. Ontario u Quebec. New Brunswick. Ontario. Quebec. Ontario. Quebec. Ontario. Quebec Ontario Quebec. New Brunswick Manitoba. British Columbia. New Brunswick. Prince Edward Islnd Quebec. 107,225 59,699 56,092 29,582 28,805 26,716 21,545 15,826 12,407 8,107 7,864 7,570 7,305 6,878 6,691 6,006 6,873 5,636 5,114 5,102 4,611 4,408 4,313 4,253 4,049 3,982 3,827 3,746 2,197 241 3,270 12,520 8,807 4,432 140,747 62,446 86,415 36,100 26,127 35,961 27,412 19,746 14,091 9,616 9,631 9,296 9,516 9,890 7,597 6,218 7,873 5,791 5,585 7,609 6,812 5,874 8,239 6,561 5,080 5,373 5,187 5,321 8,367 6,890 5,321 7,985 5,925 15,226 11,485 7,227 6,415 Table I. — origins of the people. In this table will be found only those claiming origin from English, Scotch, Irish, Trench, German, or Indian parentage. All others will be excluded as not necessary to our present purpose. STATISTICS. 681 POPULATION BY PROVINCES. PROVmOES. ENGLISH. aOOTOH. IRISH. FRENCH. GERMAN. INDIAN. Ontario 535,835 81,515 93,387 128,986 21,414 11,503 7,297 1,374 378,536 54,923 49,829 146,027 48,933 16,506 3,892 1,217 627,262 123,749 101,284 66,067 25,415 10,173 3,172 281 102,743 1,073,820 56,635 41,219 10,751 9,949 916 2,896 210,557 9,719 10,683 42,262 1,368 9,158 952 32 15 325 Quebec 7,515 1401 2 125 New BninBwick Nova Scotia Prince Edward Island. Manitoba 281 6,767 25,661 49,472 British Colvunbia TheN.W. Territories. Totals 881,311 699,863 957,403 1,298,929 284,731 108,547 POPULATION OF CITIES AND TOWNS OVER 5,000. CITIES. ENGLISH. SCOTCH. IRISH. FRENCH. GERMAN. NEGROES. TOTAL. Montreal 16,407 12,531 28,995 78,684 1,476 71 140,747 Quebec 3,437 1,683 10,224 46,444 263 7 62,446 Toronto 34,608 13,754 32,177 1,230 2,212 593 86,415 Halifax 11,707 6,540 12,814 936 2,292 1,039 36,100 St John 8,499 3,343 12,863 239 503 315 26,127 Hamilton 13,559 7,716 10,787 500 2,306 505 35,916 Ottawa 4,895 2.922 9,593 9,384 353 14 27,412 Loudon 8,617 3,543 6,062 223 439 261 19,746 Portland 3,679 . 2,077 8,448 124 370 84 15,226 Kingston 4,039 1,932 7,069 480 377 73 14,091 Charlottetown 3,716 3,166 4,059 215 441 83 11,485 Brantford 4,081 1,668 2,658 133 584 175 9,616 St. Catherines. . . 2,934 1,342 3,804 189 829 336 9,631 Three Rivers 288 256 182 8,537 46 8,670 Belleville 3,482 1,136 3,384 545 868 8 9,516 Gnelph 3,866 2,434 2,810 82 517 107 9,890 L6vis 290 1,934 147 987 431 2,690 6,681 82 10 226 9 162 7,597 Fredericton 6,218 Chatham 2,594 1,256 1,607 583 361 781 7,873 Sorel 163 2,606 82 564 90 2,146 5,427 94 9 162 .... 5,791 Port Hope 5,585 Brockville . 1,842 987 3,635 456 269 . .. 7,609 Peterborough . . . 1,948 1,156 2,952 624 100 1 6,812 Sherbrooke . . 1,774 612 799 3,957 17 2 7,227 St JeanBaptiste. 178 114 193 5,334 35 5,874 Stratford. . 2,954 1,849 2,773 64 436 26 8,239 Windsor 2.066 884 1,261 811 413 995 6,561 Lindsay 1,174 599 2,749 316 202 9 5,080 Woodstock 2,544 1,768 671 52 205 42 6,373 Gait . 1,294 2,634 764 28 423 13 5,187 St Hyacinthe 64 41 58 5,089 8 5,321 St. Thomas . 3,798 1,723 1,972 128 503 58 8,367 Hull 257 259 371 5,933 49 6,890 Moncton. 2,251 1,169 967 363 158 8 5,032 Winnipeg 2,352 2,470 1,864 450 191 4 7,985 Victoria . .... 2,318 917 831 145 332 137 5,925 St Henri 326 174 346 5,519 22 1 6,415 682 MANITOBA AND THE GREAT NORTH-WEST. >-} Ph O Ph a &< O M 3 « o Tt< m 1:- t- T*< CO Ol 00 1^- o CO 1 OiOOrHOCSlr-tO-^O'^COiMi-lCDJr-OO-^aOO • CO M "^«.'35_« 0_10 -^Oq^CO C<^- oo CO ^ ■ OOOWC^C^JCOC-IO-^t-OJCq CO^ • CO CO CD CO • •^ C^ OS OO iM ■^j^ "^ ■aouisnaaa jiaK r^ ' Tf €6" CO -C0CT>iA01W5t-«C^Oe0l:-OOQ0l0r-< «J .OiOO-— (CDC- t)< l^i-(cqTf< .r-iTt<"^COO"*(Mt— iCjiriMO r-( t- iCi^QO Oi • m C- t- CO CO «> OS^-— ' C<) CO c- -^ ■oaaanb r-Tco^oir 't-^co* -^ -^ 00 It- • P5 lO lr-(MC0iOC0-*i^iClC^t--«#W'-i'U3»OClt-C0Q0 Oicqcoco-*asiOMcoco»fla)P5coooooa>i- 1 STATISTICS 683 Table II. — religions of the people. In this Table I group together all Baptists, Methodists, and Presbyterians, and take a column for each. Pagans and those of no religion I place in the sixth column. HELIGIOKS BY PROVINCES. PROVINOKS. Ontario Quebec New Brunswick . . Nova Scotia Prince Edward Isla'd Manitoba British Colimibia. N. W. Territories. English. Presby'ians Methodists. R.Catholios Baptists. No B^lierioa 366,639 417,749 592,103 320,839 106,680 3,225 68,797 •50,287 39,221 1,170,718 8,853 438 46,768 42,888 34,544 109,091 81,092 116 60,255 122,488 50,811 117,483 83,761 121 587 8,395 1,686 13,794 1,713 14 14,297 14,262 9,470 12,246 9,449 2,189 7,804 4,016 3,516 10,043 434 617 3,166 531 461 4,443 20 362 RELIGIONS OF CITIES AND TOWNS OVER 5,000. KAHES. English. Presby'ians Methodists. R Catholics Baptists. No Religion! Montreal 14,338 3,328 30,913 9,332 5,980 9,605 4,825 6,502 3,756 3,815 1,670 2,023 2,439 101 2,343 1,901 230 1,555 1,804 130 1,891 2,175 1,375 1,270 89 2,354 1,635 1,207 1,303 781 46 1,995 263 637 2,373 1,720 179 11,597 1,344 14,612 4,992 3,554 7,879 3,059 3,257 1,872 2,600 2,197 1,467 1,474 209 1,490 2,422 98 822 1,181 49 972 1,382 1,431 482 103 2,087 693 674 1,680 2,632 68 1,466 155 1,038 2,365 908 169 5,327 883 16,357 3,711 3,287 8,317 2.173 4,952 1,795 2,398 2,604 2,481 2,217 68 3,229 2,442 71 993 2,498 17 1,765 1,591 1,845 481 42 1,394 1,746 1,273 1,388 862 3 2,431 118 875 1,370 705 86 103,679 66,255 15,716 14,705 8,701 7,134 15,901 3,284 4,600 4,451 4,384 1,471 2,582 8,831 2,164 1,895 7,185 1,621 1,506 6,526 603 1,954 1,887 4,511 5,596 1,549 1,878 1,643 302 528 5,165 952 6,234 976 1,020 866 5,920 1,402 174 3,667 2,704 3,737 1,066 461 885 1,856 200 472 1,570 627 115 482 7 1,189 729 '330 360 256 63 9 417 364 215 647 236 11 1,065 79 1,357 349 114 28 39 5 Toronto Halifex 59 8 St. John 3 TTamiltriTi , , , , 69 Ottawa 30 London 2 Portland 1 3 Charlottetown '2 St. Catherines Three Rivers Belleville 23 1 Guelph 1 Fredericton Chatham 2 1 Sorel Port Hope 3 BrockviUe 16 Peterborough Sherbrooke St. Jean Baptiste . . . Stratford. 1 Lindsay 15 2 Gait 15 St. Hyacinthe St. Thomas Hull 7 3 Moncton. .. Winninesr 1 Victoria 179 St. Henri === €84 MANITOBA AND THE GEEAT NORTH-WEST. hi O w O CO 12; o I— ( cs Pi CDiri'*pH(MC0OC0CDC0OC0CMCDOO00<=>-^JHl0C001C0C0Jr^0i'.C0C0C0t-*00KJ'^Oi-(iriC^i-(CDC0i© i4 C10001i-HlOl«rH10tNCOt^ ^^irr«^r-rco'i--r'*"cD*0*C^C^'^«rfff CO't^lcTcO*"^ Ol C^Tc^ »— ISDCDC^'^-^OflCD' CSl W CM OS t^ tN CN '^l' OO O (M (M Cq CO rH r-H 00 (N t-^ m W rH -CO'*iOCOCO'*i-(«OCO'*OOlOt^OOOi-HeOCMCO-*OiooOi-4| i-H »r-l COOOCO»OCSC3JrHir5d< 000 m»-(-^-* 't^-^COCq M ,_JrHi-( 0"^ CO CO (M oT Hsiiiaa t-( I— I 00Q0lOCD05aDl>-C0CMi-HC0^00r-ir^-tf ■COOOCOi>--*10COOOOCOCDi>. COCOl^CM'^Oi-^O COCOO-*u:i?D X^CMtOC-.C<1-^"*CM CDi— ((M (Ct^CqCMCOi-l OiOCOCM .i-HOJ^CM CO •yaoxi^YM r-T t>r cm" -*" CO 1 (M CO CsT CO OC rH T-l . >-l CO .t--iac^o-^co .-^(Mp-tCO -Oi ■'*-<*CO"CDCOi-H r-lJ>«CO.— 10 •aKVisi ITS CO • i-H r-l m ^ • CO T-l CO r-t ■!-< icT t 1^^ t^ i-T CM*^ '. C^^ a(A\.aH:-a. iNiH J -<*< CM oooico .-ThrHoocMCDooio^G^ioqcoosoocqcr^^^eci-^Oi-Homi-H-^o COOOr-* .<©0>COl^>-l^lOCMOXn-Tti CZ?CMC0(MiOCM^i>-i-li-'5O •HOiALSKnaff i>."*CO-r-lOi">.CO'*--* COCOi-H T— (CDi-( i-HCOCOi— ((M oTr-T ; Ca-^r^i-^ -^ OiTHO^ .-T AvaN "* CO . O "* CO CO 1-i COOlCq .00i>-lCCO'a:5OiOsOi-^.00CDCq»-( .C^t-OrHlOt^OOCOirii— 'OO CC-*rH .r-iOOiOO(MOSr-(COi— ('^CO r-l •COCOIO»— ti-lt>-<©t^ir5rcrcoi-r ioct i^'^^iurrcM' rn" i->» I— 1 , rH 1:0 10 . Oi ,-H '^ OOOIO .CM001-^'*rHC0Cr)C0i;001l>.CMl>-«>i-H'»"*— ICMOOCOO (M Oi 00 -(D JT^t^ tM^i-l '^ Oi i:^ CO CO CN O CO -* CD O CN '^ SD ■oaaanb -TjricTcM ; o'oOii^' j-TocT incvTr-T Cf t?r CM* i,-^ CD CO -I** 1—1 CDQO-Tjioo-* OJOiO^-lOSCOr-l^~u:i■r'lOOO^cq-*(M»HOOl>•COcOCO«5U:5 crj^jr^iciwcocO'*»ocoa>oooocqiocoosi>-coi-iof"^OTHCOoomcD cD03cq"*i>-coincooosi— lososirsiN.icit^'^iraojojcooscotMcoait^cn •orarxNo 00 -<*^ CO t-* CD CD CO tH I>- CO r-( CO « CO i-l Cq J>. CO r-lr-l CO CO ^1-1 >* 1 ^ ^ DD 1 A m K - CD .Xj % % . 1=1 o T? CO • ^( m s -s fl 2^^-S « *43 m ca M -S ^ CO -ils Ph 3 f^i-r- c5 holi Eng nal. Congregational Episcopal Bible Christian! Primitive Meth Other Methodis fl K K>1 ^ ■r-l 1 a < (/ PC 1 ""c c i= a 1 C C 1 C c ■■c El C c .Z R a F a 1-^ Congregatio: Church of S Eeformed P Other Presb t .t^ viawmoo hsixihs •vaoiiiivw ^lO-^C00i-*<:O(M"^u:S'«*i-HC0'^00Cr C^-^ t^»000-*Or-*\OlOOWcq(M^OC0T-lpH'— (Mi-lt^cq '<* 00 00 I-I 00 OT O .-( O ■* (M CO r-( t^ X^ ,_( '<* 00 00 CO i-Tof ■aNVTSi 'a 'J QO»r5irs-«!Ht^tt>t>-io Wi-HtMCOO-^t^O t^OS"*CNU:SC0rH»H r-T M CO lOl^r th" •VIXOOS VAON eooQOO»r--i-(«DrHCO "^ Gr CO I-I 1-^ CI •oaaan?) osoJ^-^ocoG<^'^oo>coosoooosccr- 1.— (Ooousuraows Ot^C000rHt-.t-^i>>C0r-l'^O>C0MC0C0»0i0T-(-^e050 aaflocMkooO(MOCO "^c^oeicq co-*kn to ■-_! 4-» W^ Ul^ 1— > 4.-* •.— ~ ~ aaeocMU3CO(MOCO !_>« b'^ V.-<« |. "* c^ o (N cq tHT|( CO«D5D^r--l^01(MOOCDOiOOO-*COCq"*OOeOrH cooir-coooo'^eO"*wiO'^r^t>-'*ou3moiiOi— I oorHeDi>.oo-*co j-f^ouacqco-^i-Hoo-^c^iNcq I -^fp a ee a ^ o cqPh O V t4 09 O <1» « C -H 'm ^ boa 5 § - - O OJ M 'C f) am o acs O-O !^ PQ !zi O N S H 04 02 OQ b O <1 >zi 686 MANITOBA AND THE GREAT NORTH-WEST. Talle IV. — Areas of Provinces. PKOVINOES. SQUARE MILES. ACKES. Ontario 101,733 188,688 20,907 27,174 2,133 123,200 341,305 2,665,252 65,111,463 Quebec..... 120,764,651 Nova Scotia 13,382,003 17,393,410 Prince Edward Island 1,365,400 78,848,040 British Columbia 218,435,200 North-West Territories 1,706,761,280 Total 3,470,392 2,221,061,447 Table V. — dwellings. TEMPORARY. . HOUSES. TOTAL NAMES. VESSELS. ANTIE S. IN- ABITED UN- INHABITED BEING BUILT. OCCUPIED. Ontario Quebec 43 6 33 11 4 2 16 1 1,216 314 385 199 35 401 2,785 9,357 358,034 216,112 73,736 50,956 17,685 12,400 6,992 2,294 19,649 18,469 2,897 2,397 607 796 1,738 30 3,145 2,887 1,234 901 328 1,136 151 100 359,293 216,432 Nova Scotia New Brunswick Prince Edward Island. 74,154 51,196 17,724 12,803 9,793 11,662 British Columbia North-West Territories Total 116 14,692 738,209 46,683 9,882 753,017 STATISTICS. 687 O o O o 1-5 o oT CO o h-t P Ph O Ph ^ «o o -* to ^ o '^ lO CO o ■^ (M „ 1 ^ CO r-l vn U3 "^ ■«*< 00 OS o CO iH 00 OS 1 T-H 00 00 O) ia la o OO^ "^ CO -* Oi CO (N -r ccT ''iJ' 1 o IH ~ rH- ^" cq-- 55 CO CO CO ^ N CO cq Oi .— ( o c CO CO lO CO T-H -* *^ I-H ■* CO !>. 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ITS o t^ OC CO oc o o 00 Oi 00 O o a- " o O o l>^ ir^ ur ■-t CO oc t^ oo CD t* -* (N cq CO cc cc rH ^ CO oo 03 ■* C9 cq I-H 1-t r-i G^ ^ 1-. la cq -* OS cc irs -<* OS ''t CO o> la CO CO cq PC] oc o I-H oc w t^ K cr en c» CO o !>. 1 f? -^ c 00 o a ^« cc cc I-H oo cq I-H CO 1 H ir IT !>. oo CO CO -* -* CO t* P C^ cr •:o CO c< cq -^ '^ '"tt oo G? ' d -<* 00 o oc iH cc *^ a CO Ift O CO CD 'tf (N !>. iC CO 1>- c^ OO CO cq cq ■* CD s "^ cq -* l> \a '^ o I-H CO t^ I-H oo 1 K •> n *k 1 -^l to CO CO CD a- Oi O- Cfl OS 1- -* oo cq 1 «c (N 1^ ■^ o c cq '^ X>. -^ op CO 1 K o- a 03 CO CO cc CD U3 cq o i-T 1-^ 1 9I1I1 !nin£^ pUB •s ax9g •pau iBH ■ )9M0 PJAV uaipiiqo 1 c Ph a: 1 i E 1 oi 2 1 1 'I ci IS I 1 3 o AGENTS WANTED ! AGENTS WANTED BY The ¥orM PuMisEing Co. GUELPH, ONTARIO. 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