i I w r mniiWj k !iwpwiw i » w»m i w I I iw < >i>' i iiWI»W»llll l'.WI > lLW >l W ' *« THE ^^5»fo|, SCIENTIFIC SERIES! ^^^•c niif'iiiiTiiinmii i i i[i ii a i rii i < i ii «itii ^i iiii i» i"iii fHi ri ^' *« ' i « » « »i u i . i -•Mtimll^Md^^^SIMM^^^I**" AHeMMMWEUiW v''**»v.'^«*<.,;**c^^ '--^S**"-- I MI II 1 l >l lll l l«lliy«iaM 1 il lWlWl l llMMt iiiM i»tf» MWiW a jMli a . ^ ^^ 'aiia** Cornell University Library The original of tliis bool< is in tine Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924031174661 arV1871 Man before metals. Cornell University Library 3 1924 031 174 661 olln.anx THE INTERNATIONAL SCIENTIFIC SERIES VOLUME XLV. THE INTERNATIONAL SCIENTIFIC SERIES. Each book complete in One Volume, 12mo, aitd bound in Cloth. I. FORMS OF WATEE: a Familiar ExpoBition of the Origin and Phenomena of Glaciers. By J. Ttndall, LL. D., F. E. S. With 25 lUuMrations. $1.50. n. 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ANTS, BEES, AND WASPS. A Eecord of Observations on the Habits of the Social Hymenoptera. By Sir John Lub- bock, Bart., F. E. S., D. C. L., LL. D., etc. $2.00. XLHI. SCIENCE OF POLITICS. By Sheldon Amos, author of " Science of Law." $1.75. XLIV. ANaMAL INTELLIGENCE. By Geoege J. Eom^ujes. $1.75. New York: D. APPLETON & CO., 1, 3, & 5 Bond Street. THE INTERNATIONAL SCIENTIFIC SERIES. MAN BEFORE METALS. BY N. JOLY, PH0FE8S0R AT THE SCTENOE FAODLTT OF TOTTLOITBE; OOBBBSPONDENT OF THE DtSTITITTE. WITB ONE BTTNDRED AND FORTY-EiatlT ILLVSTBATIONS. NEW YORK: D. APPLETON AND COMPANY, 1, S, AHB 6 BOND STEEET. 1883, /l/i^l> ^/ tlCRNELL- UNIVEBSITYj LIBRARY CONTENTS. FAOB INTRODUCTION . 1 PAET I. THE ANTIQUITY OF THE HUMAN RACE. CBAP. I. The Pebhistorio Ages (I.) General notions of the structure of the earth. (II.) The meaning of the word ' fossil ' as applied to man and other organised beings. (III.) Prehistoric ages. (IV.) The great antiquity of man proved by Egyptian monuments. II. The Work op Boucher db Perthes . . . .35 (I.) The splintered flints of Abbeville. (II.) Discovery of the jawbone of Moulin-Quignon. III. The Bone Caves 48 (I.) History of the question. (II.) Description of the bone caves. (III.) Age of the caverns. (IV.) Quaternary fauna; inhabitants of the bone caves. (V.) Bones of wounded animals found in the cavea. (VI.) Entire human skeletons found in the caves. Wounded human bones. Fractured skulls. (VII.) Proofs furnished by the condition of the bones, and their chemical composition. iv. The Peat Mosses and the Kitchen Middens . . 91 (I.) The Danish peat mosses. (II.) The peat mosses of Swit- zerland. Leaf-marked coal of Morchweill, of Wetzikon, of Utznach, and of Durnten. (III.) The kitchen middens or shell mounds. VI CONTENTS. CHAP. PAQB V. The Lake Dwellings and the Nueaghi . . . 105 (I.) The lake dwellings of Switzerland. (11.) Implements of Stone age found in the Swiss lakes. (HI.) The in- habitants of the lake dwellings. The Swiss epoch of the lake dwellings. Manners and customs of their inhabi- tants. (IV.) The flora of the Swiss lake dwellings. (V.) Ancient and modern constructions similar to the lake dwellings. (VI.) The Nuraghi of Sardinia. VI. BuEiAL Places 130 (I.) Various methods of sepulture. (II.) Burial in caves. (III.) Eemarks upon the burial places found in the caves. (IV.) The dolmens. (V.) The giant tombs of Sardinia. VII. Pebhistoeic Man in Ameeica 162 (I.) The Chulpas of Peru and Bolivia. (II.) The mounds and the mound_ builders. VIII. Man of the Teetiaet Epoch 175 (I.) The human bones of the Volcano of la Denise. The striated bones of the elephant of Saint Prest. The Meiocene flints of Thenay, IX The Gebat Antiquitt of Man 181 PART II. PRIMITIVE CIVILISATION. I. Domestic Life 188 (I.) The origin of the use of fire. (IT.) Food and cooking. (III.) Clothing. (IV.) Ornaments and jewels. II. INDUSTBY 211 (I.) Methods employed in the manufacture of stone imple- ments. (II.) Religious and superstitious uses of the flints. (III.) Weapons of war and of the chase. (IV.) Fishing implements. (V.) Tools. (VI.) Weaving and sewing. CONTENTS. vii CHAP. PAOB in. AGBICUIiTUEB 252 (I.) Primitive agriculture. (II.) Tlie domestication of animals. (III.) Origin and home of our principal domestic animals. (IV.) Origin of our cultivated plants. IV. Navigation and Commbecb 280 (I.) Navigation. (II.) Commerce. V. The Fine Aets 287 (I.) The arts of design in the oaves. (II.) Painting and music. (Ilfc) Pottery. VI. Language and Weiting 312 (I.) The origin of speech. (II.) Supposed characteristics of primitive tongues. (III.) Origin of writing. VII. Kbligion 327 (I.) Religious ideas of primitive man. (II.) Worship and amulets. (III.) Cannibalism and human sacritice. (IV.) Transformation of human sacrifice into modern religious dogma. VIII. The Portrait or Quatebnary Man .... 362 MAN BEFORE METALS. INTRODUCTION. The only trustworthy annals of primitive humanity aj-e written in the Book of JN^ature ; to it, therefore, we should have recourse. Unfortunately many leaves have disap- peared, or have been effaced from this great book, written by the hand of God, and those which remain are for the most part hard to interpret. Hence, in spite of the pre- cept of ancient philosophers {yv&Oi asavrov), that which man knows least well is himself. For in fact neither his body, his affections, nor his mind, nor the vital principle which animates him, are entirely known to him; he is ignorant of his origin, his cradle, his history. But on the other hand, man has measured the heavens, and calculated the weight of the earth and the distance of the stars. He has converted Jove, the Thunderer of old, into a mere messenger, who instantaneously trans- mits the thought, and even the voice of man from one end of the world to the other. He is able, moreover, by another unlooked for wonder, to recall the voice of the dead. He has taught golden-haired Phoebus and pale Diana to paint their image, his own, or that of anj^thing he wishes, on the lens of a camera-obscura, and has even reduced them to the humble rdle of copyists of ouj ancient manuscripts. He has dethroned Neptune, and laughs at his terrors. He can outstrip the bird on the wing, and 2 INTEODUCTION. machines made by him can travel without fatigue ten times as fast as the swiftest horse. Man has conquered the elements ; the winds obey him as his slaves, and soon, perhaps, ships of a new kind will cut their way through the regions of the air as safely as vessels now traverse the vast extent of the ocean. Fire has become a liquid in his hands.' The earth, subjected to an universal analysis, reveals her secrets one by one. In short his genius daily invents wonders, which, surprising as they are, now appear so natural that the bare mention here made of them may appear common-place to the reader. Man, I repeat, knows not his own nature nor his own history. Yet nothing of greater moment could be presented ' as the object of his study, of his active curiosity, and of his eager desire to learn the origin and nature of things. Wrapped in a thick veil, buried in the remote past, the first records of the human race have long been con- cealed from the eyes of seekers, who did not even suspect their existence, or at any rate their deep significance. The rare concurrence of fortunate circumstances, the wisdom, ingenuity, and courageous perseverance of a man imbued at once with courage and the true scientific spirit, have been necessary to the complete interpretation of the mys- terious language of these splintered stones, of these bones dug out of the bowels of the earth and given back to the light of day after so many thousands of years, perhaps of centuries! Archaeology, greeted at first with ironical sneers or the contempt of incredulity, has by an inevitable reaction given rise to extravagant enthusiasm, and to ill- considered systems, which have more than once injured its cause and obstructed its real progress. With equal disre- gard for over-eager enthusiasts and systematic detractors, we must concern ourselves solely with the results obtained. Beyond all question the most important, the most unex- ' Under the well-chosen name of liquid fire, the learned and la- borious Nickl6s has defined a, substance of which the important dis- covery cost him his life. May I be allowed to lay the tribute of my affectionate and sincere sorrow on the grave, which closed so prematurely over this savant, who was as honourable ae he was learned 1 INTEODUCTION, 3 pected, and at the same time one of the most assured of these results, is the establishment of the great antiquity of prehistoric man. The name itself indicates that history, as it has been hitherto understood and taught, is unable to give us any precise information concerning this antiquity. Neither the tables of Manetho, nor the Bible itself, can help us here. Many learned men and theologians admit that their chronology is imcertain, full of gaps, and corrupted by copyists and commentators. Sylvestre de Sacy, a Christian of undoubted orthodoxy admitted that there was no Bible chronology. One of our most learned ecclesiastics has owned, with a sincerity which does him credit, that 'the chronology of the Old Testament has i never been accepted by the Church.' He declared it to be the result of the combination of certain dates, of the interpretation of certain passages, which concern neither faith nor morals, and which may be corrupt; it is even certain that there are breaks ; and the cosmogonies of the different authorised versions do not agree with each other, &c. &c. ' Nothing therefore,' continues the learned theo- logian, 'need prevent the addition of a greater or less number of years to the generally accepted figure touching the first appearance of man on the earth, if science were able to fix the date with certainty. But this certain result is far from being attained.' ' On this last point we entirely agree with the learned Abbe Duilhe de Saint-Projet. But the concession which he makes regarding the uncertainty of Bible chronology is in our eyes far more important than his own, since it shelters us from the reproach of impiety so often cast upon unoffending science by those who know nothing of her spirit and misconceive her aims. Moreover, science replies by facts, and often by benefits, to those conclusions, rashly formed a priori, by which some men attempt to annul her discoveries, to accusations as unjust ' See the Semaine oafholique de Touhvse, March 28, 1869, and espe- cially the MineroB de Toulouse, in which the Conferences of M. I'AbbS Duilh6 de Saint-Projet are reviewed in a spirit of impartiality which does credit both to the able critic and the learned theologian. 4 rSTEODUCTION. as they are malicious, which are too often and too lightly brought against her. Some of the following facts, revealed by learned men, confirm in all essentials the statements of the purest orthodoxy. ' No date,' says the eminent palaeontologist, M. Ed. Lartet, ' is to be found in Genesis which assigns a time for the birth of primitive humanity ; but chronologists have for fifteen centuries endeavoured to force the Bible facts into agreement with their systems. Thus, no less than one hundred and forty different opinions have been formed about the single date of the Creation, and between the extreme variations there is a discrepancy of 3,194 years in the reckoning of the period between the beginning of the world and the birth of Christ. The chief disagree- ment is with respect to the interval of time nearest to the Creation. From the moment therefore that it becomes a recognised fact that the question of human origin owes no allegiance to dogma, it will become, as it ought to become, a scientific thesis open to discussion, to be con- sidered from every point of view, and capable of receiving that solution which tallies best with fact and with ex- perimental proof.' Such is our own scientific profession of faith upon this delicate question. It would have been far better to move onward with Gralileo than to force an unworthy recantation from him, especially as we have seen in our own day one of the most famous of his countrymen. Father Secchi, Director of the Eoman Observatory, and Corresponding Member of the French Institute, proclaim the superiority of the philosophy of this same Gralileo, once condemned and imprisoned by the Inquisition. ' Let science take her course,' we repeat with M. Duruy, ' let her do her work ; the soul is at the end of it.' ^ We pass on to the consideration of the means by which the new science of archaeology is enabled to establish, not ' Ed. Lartet, Nouvelles reoherohes siir la ooexistence de Vlwmme et del grands mamimifercs fosdles, reputes caraoteristiqiies de la derniere •pirwde geologiqiis {Armales des Sciences NatureUei, i' Serie, t. xv. p. 256.) 2 V. Duruy, Discours an Senat, INTRODUCTION. 5 the precise date of the appearance of man on the earth, since this result has not been and perhaps will never be attained, but to determine an approximate date which is certainly prior to that indicated by any cosmogony. Flints are found scattered over the surface of the soil, or buried in its depths ; in the heart of gloomy caves, or beneath the ruins of the most ancient monuments ; some rudely shaped, others finely polished and fashioned into forms similar to those of our axes, knives, and tools of every kind. These flints had been observed by the ancients, who gave them the names of lapides fulrnvn/is, ceraunice gemmoB, &c., and in later times they were called lightning atones, thunderbolts, stones fallen from heaven. They were employed in certain sacred rites by the Egyptians, the Komans, and perhaps also by the Scandinavians, the worshippers of Odin and Thor. Even in our day, in the nineteenth century, so slow is progress in any direction, these stones, said to be fallen from heaven, are the object of superstitious veneration in remote country districts, and they may not unfrequently be found in the cottages or cowsheds of peasants, who firmly believe that they can thereby preserve their dwell- ings from lightning, themselves from witchcraft, and their cattle from disease. But what are these strange stones, which, since they have attracted the notice of antiquaries, have been found in almost every part of the world : at Paris and at the Cape of Good Hope, at Toulouse and Christiania ; In the dilu- vium of the valleys of the Somme and of the Thames, and in the ossiferous clay of the caves of Languedoc and Peri- ^ gord ; in the dolmens of Brittany, of Algeria, and of Pal- , estine; beneath;^the ruins of Nineveh aad Babylon; in the Malay peninsula and in Japan ; and even on the banks of the Ohio and the Mississippi? This question was difficult to answer. According to some, these splintered flints were ' freaks of nature,' others held that they were of volcanic origin ; others again, that they were stones split off by winter frosts. Some sagacious 6 INTRODUCTION. men maintained that they were gun-flints, and moreover of recent fabrication. A learned antiquary of Abbeville, struck by the singular form of some of these flints, which abound in Pieardy, collected a great number of them, and examined and com- pared them with anxious and loving study. ' "Were it only a question of pin-making, this is the price of success,' are the words of some philosopher. Unfortunately, the heated imagination of the antiquary, unconsciously in- fluenced by a deceitful illusion, discovered on these flints the figures of men, of animals, of plants, carved with a definite intention, and even graphic signs, true hiero- glyphs. Here he was mistaken : but while the dream of the archaeologist soon vanished, the reality remained. These flints were, indeed, works of art, a rude and primitive art it must be confessed ; but as real and full of meaning in its simple expression as the Venus of Melos or the friezes of the Parthenon. They were evidently man's handiwork ; he had shaped these flints, had given them definite forms, and had made them into weapons or tools. And as these instruments of war, of the chase, or of handicraft were found buried at great depths, along with bones of extinct species, in strata undisturbed since their original formation, the logical, necessary, irrefutable con- clusion is that Dieu e3fc ^ternel, mais I'homme est bien vieux. Old in truth, for he was the contemporary of the mam- moth or woolly elephant, of the Rhinoceros tichorhinus, of the unwieldy hippopotamus, the bear, and the great cat of the caverns, of the Irish elk, and of other animals of extinct species, of which our natmral history museums possess complete and magnificent specimens. But M. Boucher de Perthes underwent infinite trouble, annoyance, I had almost said humiliation, before he ob- tained the recognition of this conclusion, upon which all the otters really depended. Etienne Greofiroy Saint- Hilaire has said, and he speaks with authority, 'the INTEODUCTION. 7 crown of the innovator is a crown of thorns.' The famous antiquary wreathed his brows with such a crown, which wounded him more than once. The idea was suggested, however, and since it was true, nothing could prevent its ultimate triumph, which is now complete. More than twenty years elapsed before the discovery of M. Boucher de Perthes was allowed to come before the areopagus of the Institute. It is said that Cuvier refused to accept it ; and this may easily be believed of a savant who had laid' down the principle that man, the last born of creation, could never have been contemporary with those lost species whose remains lie buried in the most ancient quaternary beds. MM. Brongniart, Flourens, and Dumas, to their praise be it spoken, were the first to encourage the researches of Boucher de Perthes, and to show themselves open to conviction. The cautious and the timid, those who feared to be involved in some heresy or imposture, held aloof, and maintained that, even admitting the flints of Abbeville and of Saint-Acheul to be of human workmanship, their great antiquity would still remain a matter for dispute, so long as the precise age of the beds in which they were discovered was unde- termined, so long as the virgin condition of these beds was unproven, and lastly, until not only the bones of extinct species, but also those of the human race, should be found buried with these stone tools. These will certainly be found, was the confident reply of the courageous author of the book on Antediluvian Antiquities, and it was not long before the event justified his prophetic words. Many such discoveries have been made, and at the present day nothing seems more surely proved than the great antiquity of the human race. How- ever, some belated or cautious minds are still in doubt, and it is precisely those whom we seek to convince. In order to accomplish this end, modern science has neglected no means of information, has left no ground unexplored. Cyclopean monuments, cities buried under layers of five or six forests, the frozen soil of Siberia and Greenland, the 8 INTEODUCTION. tumuli of Ohio and Scandinavia, burial caves, dolmens, and menhirs, the lake dwellings of Switzerland and Italy, the nuraghi of Sardinia, the lava and volcanoes of Au- vergne, the dUuvium of plains and valleys, bone caves and fossil beds, have all been investigated by the science of our day, even to the rubbish heaps formed by the refuse of the primitive kitchens of the Scandinavians, known to Danish archaeologists as ' kjokkenrndddinger,' and in Eng- land as ' kitchen middens.' Our aim in publishing this book has been to bring before the reader the numerous proofs hitherto collected of the great age of the human race, together with the details which confirm them. This forms the subject of the first part. In the second, we shall treat of the customs, the industry, the moral and religious ideas of man, such as Jie was before the use of metals was known to him, and we shall endeavour to trace his portrait with fidelity. PAET L THE ANTIQUITY OF THE HUMAN RACE. CHAPTEE I. TKE PMEHISTORIC AGES. I. GEITEBAL BTOTIONS OP THE STKUOTUHE OP THE EAKTH. It seems necessary, for the better understanding of the following chapters, to give to those of our readers who are unfamiliar with geological terms, a general idea of the various stages through which our globe has passed before arriving at the condition which it now presents to our view. The immense majority of geologists hold that the earth was originally a mass of incandescent and fluid matter. As it gradually cooled an outer crust was formed, and the vapours dispersed in the atmosphere were con- densed upon the surface of the globe, and formed the seas. At the bottom of these original seas the primary rocks and those of the transition period were deposited. These were followed by those of the tertiary period, which Lyell has divided into eocene, meiocene, and pleiocene ; * ' The beds of the tertiary period have been thus divided by Lyell according to the number of recent shells contained in them as compared to the fossil ones. The lowest layer, the eocene beds (?a>s, dawn, and Kaii/is, recent), that is, the most ancient deposit of the tertiary epoch, contains only 3J species per cent, similar to those which now exist. The meiocene, or middle layer (fieTo;/, less, and Kaifds, recent) is that in which the recent shells, less numerous than in the pleiocene, are in the proportion of 17 or 20 per cent, as compared to the extinct species. The proportion increases to 40 or 50 per cent, in the upper layer, the pleiocene beds (irAeioi', more, and Kaiii6s, recent). An important remark 10 THE ANTIQUITY OF THE HUMAN EACE. lastly the beds of the quaternary epoch, improperly styled diluvian.' The oldest rocks, those which were formed by the action of fire, and which have therefore received the name of plutonic, are not stratified, that is, disposed in layers, and contain no organic remains. The sedimentary or aqueous rocks contain, on the other hand, numerous remains of vital organisms, belonging to creatures more or less complex, and bearing more or less resemblance to the plants and animals of the present day as they are nearer to or farther removed from our own time. The geologist is thus enabled to determine the relative age of a given rock by means of the fossil species of which it bears the impression or retains the dSbris, just as an antiquary can judge of the age of a monument by the coin he has found beneath its ruins. But we cannot enter into the history, full of interest as it is, of the successive phases of life on the surface of the earth ; suflfice it to say that birds ^ and mammalia are rare in the beds of the secondary epoch, at least in Europe, and are first found in great abundance in the tertiary for- mations ; that certain marsupials and pachydermata now completely extinct (pterodon, palceotherium, acerothe- has been made by Mr. Marsh, namely that the three layers of beds of the tertiary epoch, as they exist in America, ' are not the exact equivalents of the eocene, meiocene, and pleiocene of Europe, although usually so considered and known by the same names ; but, in general, the fauna of each appears to be older than that of ii s corresponding representative in the other hemisphere ; an important fact not hitherto recognised.' (Marsh, Introduction and Succession of Vertebrate Life in America, p. 24. An address delivered before the American Association for the Advance- ment of Science at Nashville, Tenn., August 30, 1877.) ' The words diluviiim, diluvian strata, since they sometimes convey the impression that the biblical deluge created these beds, should be abandoned along with the error which has given rise to these mis- leading terms. The names of rocks of the fourth epoch, or post-pleiocene, have rightly been substituted for the latter, as more in harmony with the facts of geological chronology. The beds known under these names are far anterior to the historical deluge of Noah or of Deucalion. 2 Birds are already numerous in the secondary rocks in America. It was in the chalk beds of the Kansas that Marsh discovered the remark- able odontm-nithes, or toothed birds, which seem to establish one link between birds and reptiles, as the pterosaurians without teeth (genus ptiyranodelonytoixa the passage from reptiles to birds. QUATEENAKY EOCKS. 11 rium, &c. &c. ), are the first to appear ; that these are succeeded by other often colossal and extinct forms, such as the megatherium, the di/notherium,, the nmacroiherium,, the Tnastodon, and even monkeys (dryopithecus) ; finally, that later on, and in the uppermost or pleiocene beds, elephants, oxen, horses, carnivorous and quadrumanous animals begin to appear, which show much analogy with extant genera and species. As Professor Albert Gaudry justly observes : ' The pachyderms flourished on the earth during the earlier half of the tePtiary period, and only isolated examples of them are to be seen at the present day; the ruminants on the other hand lived during the second half of the tertiary period, and their order is still extremely numerous in our own time.' ' The quaternary or diluvian beds follow the pleiocene, and their latest formations may be considered as belonging to the present epoch. We will therefore devote a few moments to the study of these beds, which are the more important to us, since they alone, as far as we yet know, are almost incontestably proved to contain the most ancient traces of the existence of man upon the earth. QUATERNARY OR DILUVIAN ROCKS. The diluvium of geologists. — The quaternary beds, also called diluvian, pleistocene, or still better, post-plei- ocene, are composed of a series of layers or depositions of very various nature (marine, fluviatile, torrential, or glacial), formed between the end of the pleiocene period and the dawn of history. Sometimes stratified, sometimes mixed or incoherent, they contain the remains of numerous mammals, some of which of colossal size have slowly and gradually become extinct, while others, usually smaller, have survived to our own day. The stratified deposits of which these beds are partly composed are very similar to those of the tertiary period. ' Albert Gaudry, Zes eneJiaiitements du monde anvmal dams les temps gSologiques, p. 77, Paris, 1878. 12 THE ANTIQUITY OP THE HUMAN RACE. The great marine formation of the coasts of Sicily, the pampas of South America, the sands of Sahara, the steppes of Eastern Eussia, the travertine of Tuscany, are well- known examples of quaternary deposits. But in addition to these, other much less regular deposits have been formed under circumstances very characteristic of the epoch in question. These characteristic phenomena are as follows : — (1) Erratic deposits of the Alps, and of the north of Europe. (2) Diluvium of the valleys. (3^ Filling of the caves and osseous breccia. (4) Certain appearance of man upon the earth. Glacial, Period. Erratic Phenomena. — It seems proved beyond a doubt that towards the close of the tertiary, or at the beginning of the quaternary epoch, the temperature of the northern hemisphere was sensibly lowered. As the atmosphere became moister and colder, the watery vapour was condensed, and frequent falls of snow, in the form of n4ve, covered the mountains, plains, and valleys of northern and central Europe with glaciers. This is known as the glacial period.^ The Alpine traveller ' This term is perhaps incorrect, as it leads to the belief that there was but one glacial period. Many geologists, however, and notably M. Ch. Martins, reckon two glacial epochs, the first belonging to the older plei- ocene period, the second to the more recent, that is, towards the beginning of the quaternary epoch. Certain geologists go so far as to maintain, that these glacial phenomena recurred periodically from the time of the most ancient fossiliferous strata down to that of the diluvian rocks properly so called. M. Julien, who has specially devoted himself to the study of glaciers, also admits two glacial epochs ; the one beginning ' after the development of the mastodon, which became extinct in Europe at the end of the tertiary period, while it continued to live in America throughout quaternary times. This first glacial epoch was followed by the diluvian period, a consequence of the melting of these first glaciers, to which magnificent phenomenon the formation of valleys, the erosion of the soil, the transport of boulders, &o., must also be attributed. The glacial phenomena were repeated at the epoch of the EleiJJias primigenius, and have left their traces in the Vosge.s, the Alps, and the Pyrenees, as the first had done in Switzerland and in northern Europe. The inter- glacial epoch, that is, the intervening period, is represented by the sub- merged forest of Cromer, the leaf -impressed coal of Dumteu and of Utznaoh (canton of Zurich), the deposits of the Val d' Arno, &o. M. Julien considers the Alpine diluvium to be a re-formation of the sedi- EEKATIC PHENOMENA. 13 is surprised to see blocks of granite or porphyry lying on the eastern flank of the Jura, or dispersed in the Swiss valleys ; they are often of enormous size, and their mine- ralogic constituents differ completely from that of the calcareous beds or Jurassic marl upon which they lie. Striated, grooved, and poUshed surfaces may be observed on these detached blocks, and upon the undisturbed rocks which shut in on either side the Alpine valleys. The transport of these colossal masses of rock to the heights where they may now be seen, and the scratching, grooving, and*partial polish which may be observed upon them, are now generally admitted to be the work of ex- tinct glaciers, which in their slow progress, and by means of the stones imbedded in their mass, have polished, and as it were, engraved the rocks with which their movement brought them in contact. The erratic blocks lying upon peaks often very far from their original site were also brought thither by the glaciers of that period. At some definite period a rise in the temperature of the surrounding atmosphere brought about the melting of the ice, and as a natural consequence all the foreign bodies which were borne along by the glacier were deposited on the sides of the mountains or in the valleys. The action of the floods, caused by the melting of the same ice, sufficiently explains also the presence of glacial mud, the fragments of rock, the gravel and waterwom pebbles which are to be found at the foot of the Alps, and in the neigh- bouring valleys (moraines). The erratic phenomena in the north, more complex and more extensive than those of the Alps, are evidently due to analogous causes. In this case the floating ice from the arctic regions transported immense blocks, of which the mineralogic constituents sufficiently prove their foreign ment of the first period, to which he also attributes the upper grey and red diluvium, and the lower grey diluvium, or diluvium of the plains. He attributes to the second period the diluvium of the Vosges, and he connects the heas with the melting of the glaciers of the Bhine which belong to this period, and which still subsisted when those of the Vosges had completely disappeared. {Mate/rioAuc pow wrmr h Vhigtmre primitive et natv/relle de Vhomme, t. v. p. 374.) 2 14 THE ANTIQUITY OF THE HUMAN EACE. origin, to a great distance from the place of their forma- tion. These blocks, known in Germany under the name of Fwndlinge (foim.dlings), are scattered abundantly over the plains of Eussia, Poland, Prussia, and even of England. Nearly similar phenomena took place in North America. Deposits of sand, gravel, and sea shells, known under the name of drift, are to be found in the neighbourhood of these blocks, which are for the most part angular. Everything seems to prove that these deposits, which ex- tend over a great part of Northern Eiuope, starting from the Scandinavian peninsula, were formed at the bottom of the sea, by which, during or immediately after the first glacial epoch, the greater part of North America, the British Isles, and Scandinavia was covered. Diluvium, of the Valleys.— The ordinary erratic pheno- mena, we are told by M. Leymerie, took place principally among mountains and in their immediate neighbourhood, and the glaciers were the principal agents, or at least took a direct part in their production. The various phenomena which are known collectively as diluviuTn, are on the con- trary chiefly to be observed in the plains, and they owe their existence to river-floods. Two distinct and contrary effects are produced by these phenomena — the formation of those valleys known as valleys of erosion, and the partial filling of these same valleys by the diluvian waters bearing along in their current the debris from the moun- tains (gravel, waterworn pebbles, sediment of mud and sand, usually impregnated with oxide of iron or calcareous matter), which they deposit upon the plain. The two sorts of diluvium are generally distinguished as the grey and the red diluvium, the latter more recent than the former. Lastly, an important deposit of an homogeneous greyish-yellow sediment, known in Alsace under the name of lehTTt, (loam) and on the other side of the Ehine as loess, covers the stony deposit which constitutes the true diluvium to a depth of sixty or eighty yards. M. Favre has established between the diluvian beds of the north-west of France, and those of the valley of the Ehine, a parallel which it may be useful to reproduce QUATERNAJIY EOCKB. 15 here. If, as we have no reason to doubt, this parallel be exact, it foUows that the remains of human industry found in the valleys of the Somme, of the Seine, and of the Mame, correspond to the lower diluvium of the Ehine valley, a deposit far more- ancient than the glaciers of the Vosges, since it is separated from the latter by the mean diluvium of the Ehine, or red diluvium of the Seine valley.' Quaternary Beds. In the North-icest of France. Upper Dbposit. — Zehm or loess. Mean Deposit. — Sand and gravel, known as red diluvium (valleys of the Somme, Seine and Maine). Lower Deposit. — Gravel trans- ported from a distance, contain- ing flints of human workmanship, and fossil remains of Elephas primigenius, rhinoceros, stag, horse, ox, &o. In the R/tine Vatley. Zehm or loess in the plain, moraines in the monntains. Gravel composed of materials not transported from a distance : an earlier deposit than the ancient glaciers. Gravel, pebbles, composed ex- clusively of rooks of Alpine origin, of earlier date than the glaciers. The diluvian, or quaternary, epoch, is further charac- terised, as we have before remarked, by the deposits in the caves, by the formation of osseous breccia,* and by the certain appearance of man upon the earth. The cir- cumstantial details into which we shall shortly enter allow and even constrain us to confine ourselves for the moment to these general outlines. With the exception of a few species, extinct or migrated,' the quaternary fauna and flora offer the most striking analogies, or more strictly speaking, the most complete identity, with the fauna and flora of the present day. ' A. Favre, Bur Vexistenoe de I'lumme s^ir la terre anteriewement a Vapvarition des anciens glaciers. (^BibliotJiique universelle de Genifoe ; Archives, t. viii. p. 200, 1860.) * The osseous breccia are heaps composed of angular fragments of rock and various fossil bones, cemented together by calcareous or ferru- ginous mud. These osseous breccia occur in the bone caves, and in the numerous holes or fissures which abound on the coasts of the Mediter- ranean (Cette, Antibes, Nice, Gibraltar, &o.). • The principal species of the quaternary beds which are extinct at the present day are the mammoth, the Rhinoceros tioliorhinus, the great bear, the great cat, the cave hyena, and the Irish elk. 16 THE ANTIQUITY OF THE HUMAN EACE. Gheonoiogical Table Jl. — ^Aqueous rocks formed at the bottom Modem Bocks , , . , Quaternary or post- pleiooene rocks Tertiary Kooks Secondary Eooks Transition Eooks Primary Eocks ( Pleiocene Meiooene Eocene . Cretaceous Jurassic . Trias /■Permian . Carboniferous . Devonian Silurian . Cambrian OF THE PeINCIPAIi EOCKS. of seas, and stratified, or disposed in layers. J Lacustrine and fluTiatile deposits. \ Sand hUls Eed diluvium, and upper lehm or loess Grey diluvium Ehine loess of glacial origin Sand pits of Saint-Prest Freshwater strata Sands of the Orleannais FaXwns of Tonraine Limestone of Beauce ■Gypsum and marl of Paris and Aix Paris limestone beds London clay Chalk of Champagne Lithographic limestone of Solen- hofen Variegated marl, muscTwVkalk Sandstone of the Vosges Coal fields, new and old red sand- stone, schistose rocks of the Pyrenees B. — ^TJnstratifled or Plutonic rocks. CrystaUine schists Gneiss, mica-schist Metamorphic limestone Eruptive MooJcs Granite Trachyte Serpentine Protogine Basalt Diorite Porphyry Lava Ophite II. THE MEABTIITG OP THE ■WOBD FOSSIL AS APPLIED TO MAN AND OTHER OBGANISED BEINGS. The species of man •whom ■we propose to study is commonly kno'wn as fossil^ man, priTrdtive man, pre- ' JPreJiistorio man is frequently but -wrongly designated fossil man. This last epithet suggests the idea of an extinct species ; applied to FOSSIL SPECIES 17 historic man : he has even been sometimes called man- monlcey, or pithecanthrope. The first of these denomi- nations needs comment; tha second rests upon a bold hypothesis, which needs proof. What then is a fossil being ? The various definitions which this word has re- ceived necessarily bear the stamp of the opinions prevalent at the time when they were given. Thus, when geologists explained all phenomena by tremendous cataclysms, when Alcide d'Orbigny supposed that the Sovereign Architect, filling the ungrateful rdle of Penelope, created and destroyed his still incomplete work twenty-seven times, the word fossil was understood to mean any organic remains naturally buried in the strata of the earth previous to the last catastrophe which over- whelmed it, that is, before the appearance of man upon its surface. Now, this first appearance, placed after the dilu- vian or post-pleiocene epoch, properly so called, apparently formed a natural boundary between geological ages and the present time. Every animal or vegetable species of which the remains were found buried in the diluvian, ter- tiary, or yet older strata, were reputed to be fossil, and therefore necessarily extinct. All species buried at a later date than the diluvian deposit were to be considered merely humatile or sub-fossil. The words fossil species were, therefore, synonymous with extinct species, as if any organised being might not be individually fossil, without the extinction of the entire species to which it belonged. Thus the urus was only fossil in Caesar's time ; at the present day the whole species is fossil and extinct. But the aurochs, whose remains are found in the diluvian beds with those of the cave bear and of the mammoth, is at once fossil and living, since it is still to be found, in small numbers it is true, in the forests of Lithuania, where it continues to breed under the special protection of the Czar of Eussia. Moreover, a certain number of animals of which the man it signifies merely that he has been contemporary with lost species, for bis own still exists. 18 THE ANTIQUITY OF THE HUMAN EACE. remains are found in strata of a later date than the first appearance of man, have become extinct at a time very near our own. No one will deny that these species are at once fossil and extinct. The dodo of the Isle of France, the dinomis of New Zealand, and the epyornis of Mada- gascar are cases in point. We therefore apply the word fossil to all species really extinct, even though its extinc- tion was not prior to the present geological period, and took place under conditions similar to those now existing. For us every extinct species, such as mammoth or dodo, is fossil, although every fossil species is not necessarily extinct, such as reindeer and musk ox. As it is essential in the discussion of every important subject to arrive at a distinct understanding as to the meaning of the terms employed, we assert that, in our opinion, the term fossil as applied to man does not repre- sent the idea of extinction (for we hold that primitive man still exists in the person of his descendants), but that of synchronism with those great animals (mammoth, Rhinoceros tichorhinus, &c.) which, after leaving more or less numerous traces in the pleiocene rocks, have ended by becoming extinct at difierent ages of the quaternary epoch, and of which some few have survived even to our own day, as the reindeer, musk ox, &e. Fossil man, as we understand the words, does not belong to the present geological age, to that which directly follows the quaternary epoch. His actions are not within the domain of history, since they are far earlier. The study of primitive man belongs to the province of palaeon- tology, on the same grounds as that of his contemporaries, the great cave bear and the mammoth. The human species is fossil but not exti/nct. III. PREHISTOKIC AGES. ' It is with humanity as with the successive individuals of which it is composed; memory only begins at a some- what advanced stage of the development of the race ; it has no consciousness of earlier conditions. The first mani- festations of essential activity have left no traces in the PREHISTORIC AGES. 19 memory of mankind.' ' But, as is invariably the case, at the point where history ceases, fable begins. Classical antiquity tells us of four successive ages — the ages of gold, silver, bronze, and iron. Under the reign of Saturn, that is during the golden age,' men enjoyed a long life, which they spent in the midst of happiness, peace, and plenty. But the horrors of war were soon let loose among them ; iron took the place of gold ; a rapid de- cadence began, and man retains at the present day only faint traces oj his primitive perfection and happiness. Another myth of later date, and more in harmony with the facts observed, tells us that the earth was originally inhabited by a race of giants, and by a subsequent creation of a race of dwarfs. The giants dwelt among the rocks, and built there walls of cyclopean masonry ; they carried stone clubs, and were ignorant of the use of metals. The dwarfs, far weaker, but at the same time far more in- dustrious than the giants, inaugurated the age of bronze.' They sought this metal in the bowels of the earth, and with the help of fire forged precious ornaments and shining arms, which they gave to men. Finally, giants and dwarfs gave place to the men of the iron age, and were forced to abandon the land. It is curious to see poetry thus fore- stall history, and mention distinctly tJie series of epochs which are generally admitted by modern science. Lucre- tius has these lines in his poem, ' De natura rerum ' : — Arma antiqua, manns, migues, denteaque f uertmt, Et lapides, et item sylvarum fragmlna rami : Posterlus f erri vis est, serisque reperta, Sed prior seris erat, quam f erri cognitus usas. The researches undertaken, and the discoveries given to the world in these days in Denmark, England, France, Switzerland, Italy, and, indeed, in almost every part of the world, show that the facts are very nearly in agreement with the fable. Archaeology combines with geology to show that human civilisation has passed through three more or less distinct stages, in Europe at least, for which the names of stone, ' Lamennaia, Esquisse d'wne PhiloiopMe, t. iii. p. 42. 20 THE ANTiaUITY OF THE HUMAN RACE. bronze, and iron ages have been retained, although they may be, perhaps, rather too suggestive of the myth. We ought, probably, to reckon that a copper age intervened between the stone and bronze ages, if not in Europe,' where it has left few traces, at least in certain districts of the New World. For instance, the mound builders, an ancient and long extinct race, whose earthworks excite the astonishment and admiration of the traveller in the valleys of the Ohio and Mississippi, wrought the native copper of Lake Supe- rior with stone hammers and without the aid of iire, long before the day when the Mexicans and Peruvians cast bronze statues, weapons, and ornaments of every kind. It is certain that Europe, whose advanced intellectual culture is justly the object of our admiration, was first inhabited by tribes to whom the use of metals was entirely unknown. Flints more or less skilfully fashioned, and other very hard materials, such as serpentine, quartz, and diorite, bones, horn, and wood were the only tools used in the manufac- ture of their weapons and of the implements of their rude industry. These tribes belonged, then, to the stone age, the first stage of civilisation. But it has been thought expedient to divide this age into two periods, according to the dif- ferent degrees of perfection to which the workmanship of the implements had attained in each subdivision; the earlier of these two periods has received the name of archseolithic or palaeolithic (the age of rough hewn stone), ' Several urns and instruments of pure copper have, however, been found in the British Isles, in Hungary, Savoy, Switzerland, and Spain, where, according to M. de Prad, the copper age preceded the bronze age. According to M. Bougemont, the Bussian Tschoudes also had their age of pure copper. Lastly, implements both of pure copper and of bronze have been taken from Egyptian tombs which date from the time of Suphis, the builder of the great pyramid. We cannot hitherto decide with certainty whether or no a copper age existed in France or in America. But it is a fact that ornaments of red copper (necklace beads, rings, and bracelets) have lately been found in the burial caves of Saint Jean d'Alcas and of Durfort, and even in the dolmens of AvejTon (Cazalis de Fondouce, Cartailhac). In this there is nothing surprising, since copper is far easier to work than bronze : it is therefore natural that the former should have preceded the latter, especially in districts where copper in a pure state is more or less abundant. THE STONE AGES. 21 the more recent that of neolithic (age of polished stone).' (See figs. 1, 2, and 3.) The cave bear, the mammoth, the Rhinoceros ticho- Fio. 1, 2. Carved flints (Dbsmark). Specimens of STONE IMPLEMENTS. (After Lubbock.) Fig. 3. Specimen of polished STONE (Irish axe). rhi/nus, &c. belong to the first of these periods ; they had become extinct in the neolithic period. At this last ' The archseo- oi palseolithio age is anterior to, the neolithic age posterior to, the second glacial epoch. 22 THE ANTIQUITY OF THE HUlffiAIJ EACE. epoch even the reindeer had disappeared from our lands and had migrated northwards, whither the musk ox (Ovibos moschatus) soon followed it. The age of polished stone is further characterised by the construction of the dolmens, the dawn of agriculture, and the complete domestication of several animals, which have since become the faithful companions or the useful servants of man. The neolithic age was succeeded by that of bronze, an alloy of about nine parts of copper to one of tin, which is inferior in hardness to steel, but usually harder than iron.' After the lapse of a period of time whose duration is yet undetermined, iron, which is far more diflScult of ex- traction and fusion than copper, replaced bronze ; at which point the third period or stage of European civilisation began. It is sometimes rather diflScult to draw the line sharply between the various ages which we have just enumerated ; the work of one is often carried on into another. Thus for instance in a single cave of the island of Zeeland, flints simply splintered, and those which are polished or at least carefully fashioned, have both been discovered ; and again during the age of bronze, even during that of iron, stone was stiU frequently used concurrently with metal. The discovery of one or more implements of stone in any given spot is, therefore, not a suflScient groimd for asserting that these implements belong, actually and exclusively, to one or other of the palaeolithic or neolithic periods established by Lubbock.^ In Uke manner, the use of bronze was not discontinued immediately after the dawn of the iron age ; witness the tombs of Hallstadt in Austria, where bronze swords were ' It is supposed to be satisfactorily proved, that the iron age in Denmark extends back about as far as the Christian era ; the age of bronze is supposed to have lasted about 2,000 years ; lastly, the stone age, which includes the indefinite time previous to the bronze epoch, lasted for a thousand years, during which man occupied that country. 2 In North America, for instance, implements of rough hewn stone are commonly found mixed with polished flints. It is therefore im- possible to establish any chronological order. THE IRON AND BRONZE PERIOD. 23 found with axes and knives of iron. At Hallstadt the passage from one age to another was evidently slow and gradual. But elsewhere, in Switzerland for instance, at the time of the invasion of the Helvetians, the transition appears to have been violent, like social revolutions or the great disturbances of the earth's crust. In short it is easy to understand that in a given country, among a given people, a thousand circumstances may have influenced the successive or simultaneous use of stone and of metals. Hence arises a more or less pronounced inequality in the march of civilisation ; the use of iron, for example, being known to one people, whilst another had only stone and bronze at its disposal. Thus in Liguria, no trace of the use of , metal previous to Eoman times has been discovered ; the age of stone lasted in that country until the beginning of history ; and finally, it was not until the early years of the present century that the Lapps abandoned the use of stone tools. Even in our day groups of men exist who are still in their lithic age, and who are nevertheless in intimate and daily relations with peoples who have attained an advanced stage of civilisation. Such are the Australians, who cling persistently to their savage life, and continue to use weapons and tools of stone in presence of the metals of every kind introduced by the English. The modem Papuans remain stationary, while under the influence of British civilisation the fauna and flora of their native land are undergoing a change as radical and complete as that which might be produced by a sudden disturbance of the earth's crust. The New Caledonians of the present day employ iron implements concurrently with axes of well polished stone. Sir Samuel Baker assures us that the inhabitants of Illuria (Northern Africa) use extremely primitive tools, such as anvils and hammers of stone, and yet at the same time they show remarkable skill in ironwork. Similar facts have been observed among the Kafiirs and the inhabitants of Polynesia. According to Charles Smart, surgeon in the United States army, the Lacaudones of Chiquis, the last 24 THE ANTiaUITY OF THE HUMAN EACE. remains of a people whom the conquerors were unable to subdue, live in huts buUt of palm leaves, and hunt with stone-headed arrows, though they cultivate the sugar-cane and fruit trees. We should, however, be drawing a false inference from these facts, in concluding that the tribes of which we have just spoken are still in the Etone age properly so called. A slight examination will prove this conclusion to be erroneous, and will show that the simultaneous use of stone and metal is no rarer in our own day than it was before and during the Trojan war. A sufficient proof is furnished us by the example of the smiths and tinkers of Ireland, who until a comparatively recent period used in their daily work hammers and anvils of stone. M. Emile Bumouf assures us that in certain districts of the Levant pieces of flint fixed in a triangular piece of wood drawn by a horse are still used to chop straw for fodder. If, therefore, as far as Europe is concerned, the ex- clusive use of stone may serve to characterise an extremely remote period, the case is different when instruments of metal are found in company with stone implements. Thus, when M. Moura, who represented the French interests at the court of the King of Camboja, discovered axes of polished stone among the strata of that country, the pre- sence of wrought copper permitted our learned colleague Dr. Noulet to consider these implements as marking the transition between the neolithic and bronze ages.* The same inferences are naturally drawn on the several oc- casions when the simultaneous use of stone and metal has been found in Europe. It is therefore indispensable, before pronouncing an opinion as to the real age of a flint implement, to be thoroughly acquainted not only with the place where it was found, but also with all the circumstancjes which attended its discovery. Moreover, the use of iron is not " Dr. Noulet, VAge de la pierre poUe au Camhodge, d'aprea les d4oomiertm de M. Mowa, Uevtenant de vaisseau, Toulouse, 1877. DURATION OF THE STONE AND BRONZE EPOCHS. 25 necessarily preceded by that of bronze and copper (Northern Tartary, and Finland, are cases in point), and similarly copper and bronze may have been long in use among a people (such as the Mexicans and Peruvians), to the almost total exclusion of iron. As for the use of stone, unless it be exclusive, it does not, as we have just seen, imply any very marked social inferiority, stiU less any definite degree of antiqvuty. Nevertheless some authors have attempted to establish precise dates, assigning 5,000, or 7,000 years, as the most remote limit of the stone age ; 3,000, or 4,000 years, as that of the age of bronze ; while the iron age would only have a duration of 2,000 years.' It is needless to point out that, so far, no proofs are forthcoming in support of these assertions, and that every well-balanced mind should be on its guard against such precision, not to say audacity, of statement, since in the present state of science it is absolutely impossible that it can be trustworthy. We will therefore continue to employ this entirely relative or mineralogic chronology, until a better one is satisfactorily determined ; taking especial care not to neglect the valuable data which palaeontology, stratigraphy, and all industrial progress may furnish us. We must also remember that all the divi- sions we have established, of which the rigorous application is hardly admissible, even as far as Europe is concerned, cannot be appHed with any certainty to America, Africa, or AustraHa. Indeed numerous facts which have been observed in America, tend to prove that it is not necessary for the complete social development of a people that it should pass successively through the three ages of stone, bronze, and iron. As a summary of the preceding remarks, we may present them in a synoptic form. ' According to Count Gozzadini, it appears nearly certain that, if the use of iron only began in Scandinavia cowards the beginning of the Christian era, the metal was employed at YUlanova and Marzabotto at least as early as 1600 B.C. 26 THE ANTIQUITY OF THE HUMAN EACE. a MiNBBALOGIC CHKONOLOGY. Ages. - /Flints simply chipped (palseo- or arohseolithic age of Stone. \ Lubbock '). t Polished Flints (neolithic age, id.) /Completely transitory, and apparently accidental in Copper. J Europe. i More real and permanent in America. Bronze. Common to the two continents, but at different epochs. , Comparatively recent in America and Scandinavia, more ■( remote in Italy and the rest of Europe. Iron. Saint-Acheui. Type. Axe, carved on both sides. FiQ. 4. Front view. Fio. 5. Side view. M. de Mortillet has proposed to substitute for this chronology, which is altogether mineralogic, another founded solely upon the relative skill shown in the work- manship of the flints. Setting aside for the moment the flints of Saint-Prest and of the calcareous beds of Beauce, of which we shall speak presently, we give the following chronology, which we may call industrial : 1. The Saint,- Acheul epoch, the oldest of the qua- ternary beds, characterised by its amygdaloid or almond shaped axes (figs. 4 and 5). ' Evans subdivides the neolithic age into two periods ; that of nver gravel, and that of the caves. CAEVED FLINTS. 27 2. The Moustier epoch, with its scrapers, and triangular lance heads, worked only on one side (figs. 6, 7, and 8). Moustier Ttpb. Lance head, carved only on one side. Fis. 6. Uncut surface. Fio. 7. Side view. Fia. 8. Carved surface. 3i The Solutre epoch, with its beautiful arrow-heads cut in the form of laurel leaves (fig. 9). Fig. 9. SoLtTTR^ Type. Lance bead. 4. The Madeleine epoch, in which bone implements and weapons are found with those of stone. 6. The Eobenhausen epoch, or that of polished stone. 28 THE ANTIQUITY OF THE HUMAN EACE. These divisions are wortli consulting, for they are use- ful landmarks in this long series of centuries which must have elapsed between the earliest traces of human industry and the age of bronze properly so called. Unfortunately, in this case also, the authors who have paid most attention to this subject are far from being agreed ; and the determination of the limits and nature of prehistoric epochs is at present characterised by a certain vagueness which future discoveries and comparisons wiU doubtless help to dissipate. Professor Broca, by turning to account the data fur- nished at once by stratigraphy, palaeontology, and archaeo- logy, has already been able to establish among the data in question a certain agreement or concordance, of which the following table may serve to show the importance and appropriateness. Pbbhistoric Chronology of the Quateenaet Epoch. Stratigraphical Sata V Arohseolithic period Low levels of undis- tvirbed val- leys Mean levels High levels Neolithic period Eeoent beds Metallic period \ " Falseontological Data Age of the mammoth Id. interme- diate Id. of the rein- deer Modern fauna Archseological Sata. Age of carved stone or archseolithic age: axe of Saint- Acheul. Arrow head of Moustier Id. of Solutr^ Polished axe Age of bronze Age of iron It was for some time generally believed that the age of stone was confined to northern Europe. It is now es- tablished beyond dispute that every part of this continent at one time employed carved flints to the exclusion of all metal, and that the age in question has been more or less fully represented, at diiferent times, not only in Scandinavia, but also in Finland, Germany, France, Italy, England PALEOLITHIC AND NEOLITHIC AGES. 29 Belgium, Syria, Palestine, in Egypt, China, Japan, in India, and even in America. Finally, it must be remembered that all we have said respecting the succession of the different ages applies almost exclusively to Europe, some- times exclusively to France. Certain authors, among others MM. de Mortillet, Car- taiUiac, and Forel, of Lausanne, have asserted that there exists an immense interval between the palseoUthic and neolithic ages, considered from the three points of view of ethnology, palseqptology, and workmanship. But M. Cazalis de P^ondouce maintains that no such interval exists.' He holds first, with M. de Quatrefages, that there was a con- tinuity of race during the two epochs, and that a great part of the present population of Europe is descended from those prehistoric men whom we are now considering ; and he maintains that, in the quaternary fauna, between the ages of carved and of polished stone, there is the same continuity. Successive extinctions have taken place, clear- ances brought about gradually in the lapse of time, from the disappearance of the cave bear and of the mammoth to the migration of the reindeer and of the musk ox to- wards colder cUmates than our own ; but the animals of the neolithic period, and even those of modem times, are the survivors of that ancient fauna in the midst of which dwelt the men of Abbeville and Cro-Magnon. The quaternary flora, as we shall presently see, leads us to precisely the same conclusions. In short, everything tends to show that there is direct filiation between the rude workmanship of the flint of Saint-Acheul, and the skilled workmanship of the flint of the neolithic age. But a still better proof that this gap, assumed to exist by certain archseologists, is purely imaginative, is to be found in the recent discovery of a deposit which presents the manifest transition between the ages of splintered and of polished stone. I allude to the cave of Duruthy, situated near Sorde (Basses Pyrenees), where MM. Lartet and Chaplain-Duparc have observed ' a human race, associated in Perigord with the mammoth, ' See Cazalis de Fondouoe, Pierre tmlUt et Pierre poUe, laeime qui aurait existi entre ces deux ages ; Remie d'Anthr&pologie, 1874, p. 631. 30 THE ANTIQUITY OF THE HUMAN RACE. the lion, and the reindeer,' first in the age of triangulai bone arrow-heads (Cro-Magnon), then in that characterised by the barbed bone arrow-heads, and representations of animals (La Madelaine, Laugerie Basse), and which, after manifesting itself in the fully developed artistic phase at the bottom of the cave discovered at Sorde, is found again towards the upper part of the same cave, with flint weapons, which from their finished form, and rudimentary pohsh might almost be classed in the age of polished stone.' In conclusion ; the three ages of stone, bronze, and iron have not been in all places and at all times successive, but very often simultaneous. Though they mark three stages in the civilisation of nations, it does not follow that aU have passed through them at the same periods. The chronological value of these ages is not always therefore absolute and general, but sometimes purely local and relative. Finally, flint implements are so far from being themselves, and in all cases, the distinctive marks of a very remote epoch, that many tribes, even among those to whom the use of iron is known, often employ stone in preference to metal. On the continent of Europe the general series of facts has everywhere been the same, but the details, the particular characters, have varied accord- ing to a great number of local circumstances. Though they resemble each other, there is not always perfect synchronism. It is not therefore to be wondered at, if we are stiU, as regards many points, reduced to mere con- jecture and hypothesis. The important point is the establishment of the principal landmarks ; this has been ^ already done more or less successfully ; the future wiU decide whether it is necessary to displace them. IV. THE QBEAT AITTIQTTITY OP MAW PROVED BT EGYPTIAM- MONUMElfTS. Formerly learned men regarded the famous lists of the kings of Egypt, drawn up by Manetho, as apocryphal and false, lists whkih ascribed an extremely remote date • Loiiis Lartet et Chaplain Dnparo, Uhe sepvltii/re des anoiens troglo- dytes des Pyrenees, Paris, 1874, ANCIENT EGYPTIAN CIVILIZATION. 31 to the most ancient dynasties. At the present day the curious monuments brought to light by the excavations of M. de Mariette have shown that far from having gone beyond the facts of history, and ' over-crowded his picture with imaginary Pharaohs' (as M. Maury has happily expressed it), Manetho has omitted several whose inscrip- tions and devices modem Egyptian scholars can read almost as easily as the inscription on the Pantheon may be read in Paris. It is no long^ disputed that ' on the banks of the Nile art and civilisation date from a time anterior to all history ; that Egypt was from the beginning cast in a mould which has hardly changed with ages, and which the foreign con- querors who succeeded in establishing their rule in the land were forced to respect.' ' The development of this idea, which strongly supports our own theory, forms the subject of a learned paper by this weU-known Academician, with which the readers of the ' Eevue des deux Mondes ' are doubtless acquainted. In order to dissipate every legitimate doubt as to the great antiquity of the Egyptian people, and of their civilisation and their arts, it is not necessary to cross the sea, to go to Karnac and to penetrate into its temple, four times as large as Notre Dame in Paris, although it was reserved exclusively for the devotions of the king. It was enough to visit the little temple of Philse in the Champ de Mars, where the rich treasures of the Egyptian exhibition (1867) were displayed to the eyes of all nations. Their artistic beauty and richness, and above all the art displayed in the adorning of the sepulchres, were very remarkable. This is due to the fact that the inhabitants of the Nile, ever pre- occupied with the idea of a future Hfe, looked upon the tombs ' as their true abodes throughout eternity ' (Alfred Maury). Here were exposed coflSns in the form of mum- mies, entirely covered with symbolic figures whose colours have resisted the ravages' of time, and two statues, the one of diorite, the other of green basalt, representing the king • Alfred Maxixy, Vancienne Egypte d^aprh Us dernieres decouvertes ; Jtevue dos deux Mondes, Sept. 1, 1867, p. 183. 32 THE ANTiauiTY OF THE HUMAN RACE. Chafra or Chephren (the fourth king of the fourth dynasty, and the builder of the second of the great pyrainids); statues so well preserved, one of them especially, that fihey appear to be ' fresh from the hands of the able sculpt6r,'by whom they were carved more than 5,000 years ago.' Art does not attain at once to that grace of line and truth of expression of which the face of Pharaoh, son of Ea, the sun-god (Chafra), offers us an example. Side by side with these statues of the king Chafra or Schaffra we may'place the wooden statue of one named Ea-em-ke, • feiriarkable for its wonderful state of preservation, and also for its beauty as a work of art, unsurpassed by any of the Greeks, as we are told by a competent judge.' This Ea-em-ke was the governor of a province during the fifth dynasty, that is to say, about a century later than king Schaffra. Lastly, the door of the great pyramid of Sakkara, now one of the most precious treasures of the Berlin Museum, formed part of a monument, which, if it were really built, as it is generally believed, under the first dynasty,'' has withstood for nearly sixty-eight centuries the destroying hand of man and of time. ' Such figures terrify the imagination. Forty-niae cen- turies before the birth of Christ is a great age for a work of human hands, and above all, for a true work of- art. Neither India, Asia, nor Assyria have any relics Of a time which approaches so nearly to the origin of humanity. But that which is really overwhelming to the mind is to find at that date, not savage tribes, but a powerfully con- stituted society, of which the formation must have required the lapse of centuries; a civilised people advanced in science and art, and in the knowledge of mechanics, capable of raising monuments of immense size and of indestructible solidity.' ^ I shall only mention the jewels found at Thebes on the mummy of the queen Aah-hotep, mother of king Amosis, • M. Fr. Lenormant. ^ Under King Onennephes, 4895 B.C. ' r. Lenormant, L'AnUguUe d, Vllxiposition wniverselle : Gazette dei Beaux-Arts, Sept. 1, 1867. EGYPTIAN ART. 33 jewels of unequalled finish aoad beauty, although they date from the time when Joseph became the minister of the then reigning Pharaoh. Necklaces, bracelets, mirrors, and sacred axes of bronze, carved and gilt, a richly worked dagger, enamelled earthen vases, &c., all these works of antique art excite our surprise and admiration. ' Neither Greece nor Etruria,' we are told by M. Lenormant, ' has produced any jewels which surpass those of the queen Aah-hotep in grandeur of conception, in elegance and purity of form, or in beauty of workmanship. But imagi- nation is confounded at the thought that these ornaments, which reveal such a high degree of artistic culture, such wonderful manual skill in the workmen, are the product of a time of civil trouble and of war, when Egypt was pain- fully emerging from a long-continued struggle with a horde of barbarians (hyhsos or shepherd kings) whose invasion had covered her land with ruins.' It is time to conclude, but I cannot refrain from no- ticing two other objects in a wonderful state of preservation which were exposed in the collection of M. Maxiette. Here again M. Lenormant shall speak for us. ' The graceful wooden spoon, which represents a young Nubian girl swim- ming and pushing an oval basin before her on the surface of the water, is of the time of Moses. With a little imagination we might almost believe that it lay on the table of Pharaoh's daughter. This charming little basket, with a cover woven of parti-coloured cane, and admirably preserved, which one of our own ladies might use as a work-basket, was found at Thebes in a tomb of the eleventh dynasty. It is therefore two centuries older than Abraham. Many centuries must have elapsed before such a degree of perfection was attained, and we are, indeed, far removed from the first attempts at sculpture which have been dug out of the caverns of Languedoc and Perigord. Yet there can be no doubt that Egyptian art, so perfect under the reign of Chephren and his successors, began by equally rude attempts. But from what remote age they date, or what were the names of those earlier artists, we know as 34 THE ANTIQUITY OF THE HUMAN EACE. little as we know who were the sculptors whose chisel created the sphinx and the statues of the kings.' We must add that in the remote epochs of which we are speaking, the Egyptian tongue was already formed, I and possessed a written character. The greater number ' of our domestic animals were bred by the Egyptians, and distinct and .long established breeds were known to them i (greyhounds, lop-eared goats, &c.). No one can tell with certainty the number of centuries they must have passed through before attaining to so complex a civUisatiou. The whole history of Egypt confirms our belief in the immense antiquity of the human race. We pass on now to compare the remains of primitive industry preserved in the diluvian gravel. of the vaUeys or the sediment of the bone caves with the works of Egyptian art. We must study the flints and the lesson to be drawn from them. CHAPTER II. TSE WORK OF BOUCSES. DE PERTHES. I. THE SPLIITTEKED FLIBTTS OE ABBEVILLE. To the history of the diluvium a discovery belongs which, though insignificant in appearance, is in reality of the utmost importance from its bearing upon primitive in- dustry : I allude to the flints, sometimes merely chipped into shape, sometimes carefully polished, found in such abundance and in such widely distant parts of the earth, from Paris to Nineveh, from China to Camboja, &om Grreenland to the Cape of Good Hope. Although the true nature of these flints has not been made known to us for more than forty years, the ancients knew of their existence, and, at least to those that were polished, they gave the strange names of lapides fuhninis, ceraunice gemmcE, which expressed the strange notion that they had fallen from the skies with the thunderclap, or were formed in the earth by the fire of Jove. They afterwards came to be looked upon as ' freaks of nature ' (lusus naturce) : as early as 1734, Mahudel, and after him Mercati, ventured to say that they were the weapons of antediluvian man, but this bold assertion was received with ridicule and incredulity. Buffon in 1778, in his ' Epoques.de la Nature,' aflBrmed again that the first men began by sharpening into the form of axes these hard flints, jades, or thunder-bolts, which were believed to have fallen from the clouds and to be formed by the thunder, but which, said he, ' are merely the first monuments of the art of man in a state of nature.' This just theory passed unnoticed at the time, but all scientific men are now agreed upon its truth. But it 36 THE ANTIQUITY OF THE HUMAN EACE. is to M. Boucher de Perthes that the honour belongs of having dispersed all doubts and inspired conviction. From the year 1836 to 1841 he made researches, pickaxe in hand, among the ancient tombs, the caves, the peat mosses, the diluvium of the valleys and of the bone caves, and collected thence flints of a remarkable form, more or less sharpened at the edges, presenting a number of unequal facets, and shaped like axes or knives. The origin of these chipped stones and the strata to which they rightly belong form the subject of a series of in- genious inductions, and of prophetic remarks which the event soon justified. I leave the author to speak for himself: ' The yellowish tinge of some of these chipped stones of the diluvium was a first indication. This tinge was not that of the flint itself, but was entirely superficial, whence I concluded it was due to the ferruginous nature of the soil with which the stone had come in contact. A certain layer of the diluvium fulfilled this condition ; the shade of colour was precisely that of my axes. They had been imbedded in it, but the question remained whether their presence there was the effect of a recent revolution, and later displacement, or if it dated from the formation of the bed. If the axe was in the bed from its beginning the problem was solved ; the man who had made the implement was anterior to the cataclysm to which the deposit owed its formation. In this case there is no possibility for doubt ; for the diluvian deposits do not, like the peat-bogs, present an elastic and permeable mass, nor a gaping chasm Mke the bone caves, open to every comer, and which have for centuries served as a shelter, and then as a tomb, to so many different creatures ; in such a mixture of all ages, in this neutral bed, a species of caravanserai for past generations, it is impossible to characterise the different epochs. ' In the diluvian formations, on the contrary, each period is sharply defined. The horizontally disposed layers, the strata differing in colour and substance, show us the history of the past in clear characters : the DISCOVERIES OF BOUCHEB DE PERTHES. 37 great convulsions of nature seem to be traced upon them by the finger of God. ' Here the proofs begin ; and they cannot be gain- said, if this work of human hands, of which I said, " It is there," has remained there from the first. As irremovable as the bed itself, it came with it, and has there remained, and since it has aided in its formation, it had a prior existence.' ' This work of human hands, to which M. Boucher de Perthes was devoting all his efforts, was ' those rude stones which in their imperfection prove the existence of man no less surely than such a building as the Louvre itself could have done.' He had found the proofs which he sought so eagerly, and in 1839 he brought them from Abbeville to Paris : but the axes and knives of the dUuvium excited the ridicule of geologists, and inspired them with doubts as to the sanity of the man of genius who came with a candour which does him honour, to submit his discoveries to those who could not understand him. They were afraid of these stones, whose language, as interpreted by M. Boucher de Perthes, concealed, as they thought, some heresy or mysti- fication ; and for a time the flints of Abbeville were con- demned to ridicule or oblivion. But fortunately, as it nearly always happens, truth, long unrecognised, ended by overcoming the systematic resistance, the absurd preju- dices, and the presumptuous incredulity of its opponents. They consented at last to examine the discoveries, and thenceforward doubt became impossible. They had under their eyes the manifest proof of human workmanship of a much earlier date than the earliest traditions, or than the monuments which the most remote antiquity has left us. In spite of the evidence of proofs, the question was not generally considered to be resolved; objections poured in from every quarter. Some maintained that these fractured flints were not of human workmanship ; that they were of volcanic origin ; melted by intense heat, and ' Boucher de Perthes, De Vliomme a/idedilv/ricn et de ses ceimres, p. 3, Paris, I860. 3 38 THE ANTIQUITY OF THE HUMAN RACE. thrown up into space from the crater, they fell back into the water in the form of a vitrified glass. Others attributed them to the action of frost, which had split the flints so adroitly as to cause them to take the form of axes and knives. The means by which they were introduced into the diluvian beds was easily explained by the assertion that the workmen employed in the excavations had placed them there. Some even went so far as to maintain that these axes had penetrated the upper layers in virtue of their own weight, as if the beds in which they are found were sufficiently permeable ever to have allowed of such infiltration. Some well-known geologists asserted that these de- posits were of recent origin, or at least but little earUer than the arrival of the Eomans in Gaul. Others, considering them to belong to the quaternary epoch, that is, to a pre- historic period, have maintained the opinion, unsupported by any adequate proof, that these strata have been dis- turbed by man ; that is, that their original position has been changed long after their formation. Others again asserted that these chipped stones were merely gunflints : ' a remarkable statement,' said a critic, with a spice of malice, ' which proves that its authors were very certainly not the inventors of gunpowder.' Indeed these objections are not serious, and it seems astonishing that they can have been seriously made by their authors. The first, which attributes the origin of the flints to volcanic action, may be classed with the ancient notion which attributed to Jove the origin of the Iwpides fulmvais, of the ceraunice gemmcB. The second, which explains the origin of these same flints by the action of frost, is no explanation at all. To admit the third, we must admit also the most complete under- standing among the workmen of every country, and these are not a few, where artificially shaped stones have been found in the diluvium. The fourth objection, asserting that the stones deposited on the surfaces of the diluvian beds have by their own weight buried themselves in them, is sufficiently refuted by its own absurdity. ANTIQUITY OF THE BONES. 39 There remains, then, only the assertion of those who hold that the diluvian strata, displaced after their forma- tion, received at a comparatively recent epoch the axes and knives which they contain. But as M. Boucher de Perthes reasonably demands, by whom were they dis- placed ? Not by man, for the whole population of Gaul would not have sufficed for the task, even if the diluvium of Abbeville were alone in question. The utter im- possibility of such a displacement is made manifest when we consider that the same phenomenon, that is, the pre- sence of hewn mnts, has been observed in the same situations and in identical circumstances in aU quarters of the globe. Moreover, the bones of extinct animals, of fossil ani- mals in the sense which Cuvier himself attached to the word, are nearly always found with the flints in question. Such are the Mephas primigenius, the Rhinoceros ticho- rhinus, &c. Again, a whole limb of the Rhmoceros haymi- toechus was found at Menchecourt, of which the different bones were still, as it were, articulated and placed each in the position which they had occupied during life. Cer- tainly, if, as it must be admitted, this Hmb had occupied undisturbed for thousands of years its original position in the gravelly bed where it was found, it is impossible still to deny that the hewn flints lying beside it were contempo- raneous with it. Many other similar or analogous facts have been observed. However, it must be owned that we cannot conclude with absolute certainty that they are of the same date from the fact that the flints are frequently found in company with the bones of extinct species. It is just possible that violent currents had borne along in their course and mingled together the d&hris of very different epochs. But doubt would be no longer possible if unequi- vocal traces of human workmanship were discovered upon the bones found buried in the same beds with the flints. Our learned colleague, however, M. Ed. Laxtet saw, and many others have since seen, incisions. made by a sharp instrument, probably a flint knife, upon the bones of the 40 THE ANTiaUITY OF THE HUMAK EACE. rhinoceros, and upon the antlers of stags of extinct species which were found in all the diluvian beds of the valley of the Somme. Similar examples have since been repeatedly remarked, and there is no tolerably complete collection which does not contain flint implements found in company with the antlers and bones of extinct animals, bearing the marks of the teeth of saws or of incisions made in order to detach the skin from them, to separate them from the skull, or to divide them into fragments of a convenient size. We may conclude then, that the flints of the diluvium of Picardy are the productions of human art, proving that the man of Abbeville lived at the same time as the mam- moth and the Rhinoceros hcemitcechus, that is to say, at an altogether prehistoric period, At that time the bed of the Somme was 60 ft. higher than its present level ; the river had not then hollowed out the valley in which it now flows. England was not separated from France by the Straits of Dover at the epoch of which we are speak- ing; and supposing London and Abbeville to have been then in existence, the traveller might have gone from one town to the other on foot. The Ehine valley stretched away to the northward across the plains not yet sub- merged beneath the German Ocean, and received the tributary waters of the Humber, the Tweed, and the Thames, whose streams were fuller and more rapid than they are in our day. The Ehine and the Ehone, abun- dantly fed from the same source, hollowed their vast beds, bearing along in their currents the dSbris of the con- temporary fauna, and burying with them the stone im- plements of our European ancestors in the fresh deposits which they formed. Nevertheless, in spite of the important results ob- tained by the patient researches of M. Boucher de Per- thes, the Institute, for more than fifteen years, regarded with the most complete indifference the discoveries of the learned antiquary of the Somme. Finally, however, its members were obliged by the force of circumstances to cast a more or less contemptuous glance upon these dis- CONTROVERSY RESPECTING THE ST.-ACHEUL FLINTS. 41 coveries. A paper * written by Dr. EigoUot, at first the declared adversary, but afterwards the warm partisan of the theories of Boucher de Perthes, drew the attention of the first, scientific body in France to the 'Antiquites Dilu- viennes,' a book which contains, it is true, many daring conjectures, but at the same time a number of convincing facts, ingenious theories, and unanswerable arguments. As the author says, ' this attention was not kindly. A purely geological question was made the subject of religious controvgrsy. Those who threw no doubt upon my religion accused me of rashness : an unknown archeeolo- gist, a geologist without a diploma, I was aspiring, they said, to overthrow a whole system confirmed by long experience and adopted by so many distinguished men. They declared that this was a strange presumption on my part. Strange, indeed ; but I had not then, and I never have had, any such intentions. I revealed a fact; consequences were deduced from it, but I had not made them. Truth is no man's work ; she was created before us and is older than the world itself; often sought, more often repulsed, we find, but do not invent her. Sometimes too we seek her wrongly, for truth is to be found not only in books ; she is everywhere ; in the water, in the air, on the earth ; we cannot make a step without meeting her, and when we do not perceive her it is because we shut our eyes or turn away our head. It is our prejudices or our ignorance which prevent us from seeing her, from touching her. If we do not see her to-day, we shall see her to-morrow ; for strive as we may to avoid her, she will appear when the time is ripe. Happy the man who is prepared to greet her, and to say to the passers-by, Behold her ! ' ^ As the Institute of France had so long refused to Listen or to believe, it is not astonishing that the public re- mained indifferent or incredulous, and that as late as 1853 M. Boucher de Perthes was still asked how it was that ' Dr. Eigollot, Memoire smr les indruments en silex trouves a Saint- Acheul, Amiens, 1851. ' Boucher de Perthes, De Vhomme antedilumcn et de scs anivres, p. 13, Paris, 1860. 42 THE ANTiaUITY OF THE HUMAN EACE. his pretended" antedihivian axes and knives were only to be found in the gravel beds of the valley of the Somme ; how it happened that he alone had found any such? Numerous facts gave a prompt reply to these questions, of which the contempt and incredulity were ill-disguised. Others were sought for and were found, indeed, had already been almost unconsciously found. In fact, without going back to the precise details which antiquity has furnished us respecting the flints called thunder-bolts, there is in the British Museum a stone weapon, found by Conyers, as the label tells us, more than a centiiry and' a" hafl;' ago, with an elephant's tooth, near Grruyes. This weapon, which, according to Evans, is rudely sketched in a letter on the antiquities of London, dated 1715, is the exact reproduction of the flint lance heads so common in the diluvian beds of Abbe- ville and Saint-Acheul. A century later than Conyers, in 1800, John Frere found in a gravel quarry at Hoxne, in Suffolk, flint tools of the same type as those since found in the valley of the Somme, and like them, intermixed with bones of extinct elephants and rhinoceros. Similar discoveries have since been made in every quarter of the globe. Thus in this case also, truth, long denied and banished, has overcome systematic and contemptuous incredulity, and, at the moment I write these lines, there is no scientific man who is not convinced that the most rudely shaped flints show human workman- ship as clearly as the axes of the Eoman lictors : for ' the flints speak,' says Lubbock. We have heard and have still more to hear of what they have to tell us. II. DISCOVERT OF THE JA'CTTBOITE OF MOUIiIlf- • aUIGKOW. On March 23, 1863 (we are careful to give this me- morable date), M. Boucher de Perthes was gratified by the discovery, at Moulin-Quignon, of the famous jaw- bone, or rather the part of a human jawbone, which became the subject of so much controversy. It lay im- bedded about five yards deep in dark sandy gravel, the JAWBONE OF MOULIN-QUIGNON. 43 colour of which was due to an admixture of manganese and oxide of iron, and which was in immediate contact with the subjacent chalk. The same bed contained carved flint, axes of the Saint-Acheul type, and teeth of the mammoth (Elephas primigenius). On April 24, in the same year, M. de Quatrefages made known this discovery in the author's name to the members of the Institute, proclaiming it to be ' one of the most important which could be made in natural science.' (See fig. 1 0.) All the newi^papers, not only the scientific journals, but also the political organs, vied with each other in spreading the news of the discovery ; and it was indeed Fig. 10. Jawbose of Mol'lik-Quignon. a memorable event. Following the example of M. de Quatrefages, who had been one of the first to visit Abbe- ville to inspect the place of this important discovery, and to enquire into all the accompanying circumstances, several English savants, whose names are justly cele- brated (Evans, Falconer, Prestwich, all members of the Koyal Society, who had already visited Abbeville in 1859), again visited France, and having entered at once upon a strict and conscientious enquiry into the alleged facts, they began to entertain doubts as to the authen- ticity of the jawbone, and to suspect that it might have been fraudulently introduced by the workmen into the bed where it was foimd. Far from denying in a general way the great antiquity of the human race, these men of science had more than once brought proofs in its favour 44 THE ANTiaUITY OF THE HUMAN EACE. but in the present case they did not feel absolutely con- vinced, and they said so honestly. Their doubts were principally due to the close resem- blance which this jawbone bears, physically and anato- mically, to other inferior maxillaries belonging to members of races now in existence. Prompted by the desire of dis- pelling such doubts, and of resolving at once and for all the important question in debate, M. de Quatrefages proposed that a kind of congress should be held, at which, after having seen and handled the subject of dis- pute, English and French men of science should discuss together the difficult or disputed points and then draw their conclusions. In accordance with this suggestion, Messrs. Busk, Carpenter, Falconer, and Prestwich went to Abbeville. Among the French savants were MM. Milne-Edwards, de Quatrefages, Desnoyers, Delesse, Lartet, Daubree, Delafosse, Hebert, Albert Gaudry, P. Bert, Alph. Milne- Edwards, de Vibraye, Dr. Vaillant, I'Abbe Bourgeois, Dr. Garrigou, &c. M. H. Milne-Edwards was chosen president of the congress. After the facts had been examined and discussed, it was unanimously agreed that the axes and the jawbone of MouUn-Quignon were really authentic, and that fraud had had no part in their burial. However, Messrs. Busk and Falconer still desired to make some reservations, and the latter requested that the following declaration should be annexed to the report. 'My opinion is that the discovery of the human jaw- bone is authentic, but that neither its characteristics nor the conditions under which it was found, sufficiently prove that the aforesaid jawbone is of very great antiquity.' Messrs. H. Milne-Edwards, de Quatrefages, Lartet, Prestwich, and Carpenter, on the other hand, remained firm in the belief that this human relic belonged to an extremely remote date. M. Pictet of Geneva, and the immense majority of geologists, both French and foreign, embraced this opinion, and declared that the man of Moulin-Quignon had witnessed the geological phenomenon which had deposited the beds of diluvian gravel. CONGRESS OF SAVANTS AT ABBEVILLE. 45 Messrs. Falconer and Busk did not remain long uncon- vinced. One dissentient voice was raised, however, in the midst of the general concord, and affirmed in the Academy of Sciences at Paris, that neither the axes of Moulin- Quignon, nor those of Menchecourt, and of Abbeville, nor even those of Grrenelle and Clichy, should be considered as diluvian. Subsequent causes had imbedded them in these strata, which had been disturbed and were even comparatively modem. Therefore, added the same Aca- demician, a great authority in geological questions, it is a mistake or a chimera to believe that man was the con- temporary of the mammoth or the diluvian rhinoceros. This incredulous, or at least exceedingly cautious Acade- mician, was M. Elie de Beaumont. On the other hand, we can oppose to this well-known name those of MM. Prestwich, Lyell, Lartet, Des- noyers, Gaudry, and others, who all maintained that the beds of Abbeville and of Moulin-Quignon belonged to the quaternary epoch, and had remained undisturbed from the day of their formation. This was the state of affairs, and the ' trial of the jaw- bone' seemed to be at an end, when on July 18, 1864, M. de Quatrefages communicated to the Academy a new Note, in which he announced that M. Boucher de Perthes had just found, in the district of Moulin-Quignon, already so famous, a second jawbone, a skull, and other human bones. The author of the memorandum insisted upon the identity of the spot, upon the precautions taken to avoid deception, and he declared himself to be as before, abso- lutely convinced of the authenticity of these remains. The learned Academician left it to geologists to determine the age of the beds whence they were taken, and also the antiquity of the human race buried therein. The question now appeared to be definitively settled, for so many minute precautions, such a careful examina- tion, such learned consultations, with names so justly re- spected, seemed to be a guarantee of the truth which was above the least suspicion. Yet it was whispered, and even audibly spoken in certain circles which profess to be well 46 THE ANTIQUITY OF THE HUMAN RACE. informed, that the members of the Congress of Abbeville were the victims of a monstrous fraud, and Evans himself repeats that ' I do not of course allude to the too cele- brated Mouhn-Quignon jaw, over which I have already pronounced a Requiescat in pace,' ' Even granting that this deception was really practised, no one can deny that the skuUs of Grenelle and of CUchy, of which we shall soon have occasion to speak, were taken from an undisturbed bed of grey diluvium, as ancient as that of MouHn-Quignon. The skulls of Neanderthal, of Engis, &c., and the jawbones of Naulette (figs. 1 1 and 12), Fig. 11. jAWBONii of Naulette. Fig. 12. Jawbone of chimpanzee. of Aurignac, and of Arcy, found in the bone caves of the palaeolithic age, also bear strong testimony in favour of the great antiquity of the human race. It is in the caves therefore that we will now seek our proofs. But here, more than anywhere else, we must surround ourselves with ' See Evans, The Ancient Stone Implements, Weapons, and Orna- ments of Great Britain, p. 617. Although human bones have not yet been found in the diluvium of English valleys, the author whom we have just quoted admits that the human race is contemporaneous with the extinct animals of which the remains are found abundantly in Franee in the same diluvium, or in a number of bone caves. SKULLS OF NEANDERTHAL. 47 minute precautions. We shall have to examine the bones and other objects which are found there, and determine whether they are buried in a virgin soil which has never been disturbed ; since it is on this condition only that we can draw certain conclusions from the facts which have been observed. CHAPTER III. THE BONE CAVES. I. HISTOKT OP THE QUESTIOIT. Every important discovery is generally preceded by partial discoveries which herald or foreshadow its approach. Some fact attracts the attention of an observant mind ; another similar fact appears, perhaps simultaneously, perhaps after an interval of greater or less duration ; other phe- nomena of like nature group themselves around the first ; and this assemblage of scattered gleams produces a ray of light which at length strikes the eyes of all beholders. But the new idea which shines out brilliantly from the surrounding obscurity is nearly always opposed to the reigning opinion which has become, so to speak, an article of scientific, often even of reUgious faith. Hence arise a strenuous opposition, a more or less passionate strife, until at last the human mind can enjoy its new conquest in peace. Such is the approximate history of every question which has been the subject of human dispute. That which concerns the synchronism of our species with the great extinct mammals could form no exception to the general law. Proofs of this fact are now abundant ; and the bone caves have furnished a contingent which is by no means to be despised. As early as 1828, Toumal of Narbonne announced to the scientific world the discovery of human remains,' and of things fashioned by the hand of man, in the cave of Bize (Aude) intermixed with bones of animals which ' A fragment of the superior maxillary. MAN AND EXTINCT SPECIES CONTEMPOEARY. 49 Cuvier himself considered as fossil in every acceptation of the word. This discovery, important in every point of view, was received with a caution which was almost exces- sive, even on the part of the Institute. It is true that the proof is not absolutely complete, since the cave of Bize was at one time beUeved to date only from the time of the reindeer, and, as it was said, con- tained no remains of the cave bear, nor of the cave hyena, nor of the mammoth, nor of the Rhinoceros tichorhinus, &c., in a word, of none of the great characteristic mam- malia of the beginning of the quaternary epoch. But at the present day every serious objection disappears in face of the fa^ts attested by Grervais, that the cave bear and cave hyena do occur at Bize, that he has himself found them there, and that consequently the cave is of more ancient date than was originally believed. We cite the words of the learned professor of the museum, who is known to be as a rule opposed to the theory of the great antiquity of man. ' I maintain that the Ursus spelcsua and the Hyaena spelcea are buried in the same place as man ; and that the cave of Bize may be cited as a proof in support of the opinion that our species was the contemporary of these two great carnivora.' ' Every doubt as to the contemporary existence of man and of extinct species should have disappeared, when on June 29, 1829, M. de Christol, then secretary of the Societe d'Histoire Naturelle of MontpeUier, submitted to the Institute a paper entitled, ' Notice sur les ossements fossiles des cavemes du departement du Gard.' The author of this work, which received at the time less notice than it deserved, after having carefully examined the caves of Pondres and of Souvignargues (Gard), adduced new and conclusive facts in support of those already cited by M. Toumal. He proved incontestably, as we think, that the cave of Pondres, being entirely filled by the diluvium at the time when he visited it, could not have ' Gervais, Reoherches swr Vaneiennete de Vlwmme et de la periode quaternaire, p. 64. 50 THE ANTIQUITY OF THE HUMAN EACE. received any substance of modern or foreign origin, which has sometimes happened with certain hollows more easy of access. He showed further that the bones of hyenas and the fragments of pottery which occur there are found at every depth, and that the human remains are ' in precisely the same geological conditions as all the other bones with which they are associated.' At Souvignargues M. de Christol dug out of the deepest part of the undisturbed diluvium a humerus, a radius, a fibula, a sacrum, and two vertebrae, which had formed part of the skeleton of an adult of sniall size, perhaps of a woman, as Professor DubreuU thinks. In 1833 Dr. Schmerling explored the numerous caves of Belgium, and in several of them, notably at Engis and at Engihoul, near Liege, he ascertained the existence of skulls and of portions of the human skeleton, together with those of bears, hyenas, elephants, rhinoceroses, &c., lying in the diluvian deposits, sometimes above and some- times below the remains of these species which are already universally recognised as fossil. Bones and flints shaped by human hands, extracted from the same beds, served to confirm Schmerling in the belief that man was the con- temporary of the extinct animal population whose remains he had found. The conclusion was no doubt logical, and yet it was opposed by several geologists of great authority. Lyell himself did not at first admit it (1833) ; but more than a quarter of a century later (1860), on the occasion of a visit to the Schmerling collection, and to several of the places whence the specimens it contains were extracted, the famous author of the ' Principles of Greology ' frankly acknowledged and retracted his error, in terms which are still more creditable to his character than to his judgment. This brings us to 1835, the date at which I, an un- known disciple of science, ventured to maintain that man was perhaps the contemporary of the bears whose remains I had lately found at Nabrigas (Loz^re) together with a fragment of pottery of early workmanship, which was EELiaUIiE DILUVIAN^. 51 judged worthy by M. Christy to be cast at Toiilouse for the purpose of enriching the principal museums of France.' My paper, which was published in the ' Bibliotheque Universelle ' of Greneva, being the work of an unknown author, attracted very little notice in France, and in spite of the new proofs which it brought forward in support of the theory of the co-existence of man and extinct species, was perhaps for that very reason, forgotten or ranked with those rash assumptions then called juvenile, of which my learned predecessors MM. Tournal and Christol had given me the example. I hope the reader will pardon me this personal allusion, this return towards an already distant past, which recalls to me my early beginnings in science, to which I have with disinterested devotion consecrated the greater part of my life. In 1838 a work appeared entitled ' Essais sur les cavemes a ossements et sur les causes qui les y out accu- mules.' After enumerating the different places where either human remains or fragments of human industry have been found, the author, M. Marcel de Serres, con- cludes by saying : ' It appears then an established fact .... that man was the contemporary of the extinct species whose remains are found scattered in certain of the bone caves of Europe' (p. 198). It is true that, in 1860, Marcel de Serres expressed a very different opinion. ' It appears,' he says, ' that the true beds of diluvian deposit, also called diluvium, do not contain the least trace of bones, nor of human industry and remains.' ^ At the present day few, if indeed any, geologists share this later opinion of the MontpelUer professor. In England the bone caves had also been eagerly ex- plored, but often without method, and with preconceived ideas. The important work of Dr. Buckland, published in 1823, under the title of 'Eeliquise Diluvianse,' had ' I presented one of these casts to the Museum of Natural History at Toulouse. ^ Marcel de Serres : ' Ses espeoes perdueg, et des rOfCes qui ont disparu des lieux gu'elles haHtaient primitivement ' {Annal. Seient. Natwrel., t. xiii. p. 300, 1860). 52 THE ANTIQUITY OF THE HUMAN EACE. attracted considerable attention among scientific men ; but it maintained that man was not contemporary with the extinct species. The discoveries made in 1842 in Kent's Cavern, near Torquay, Devonshire, by Mr. Grodwin Austen, clearly disproved these conclusions, but without convincing geologists or palseontologists. The year 1858 marks the beginning of an important era. A reaction against the too absolute opinions of Dr. Buckland set in in England, and this opposition originated in the Royal Society. Several of its most eminent mem- bers, among others Falconer and Prestwich, were com- naissioned by the Eoyal Society to explore with the greatest care the recently discovered cave of Brixham (Devon- shire), and to draw up a report on the subject. Among a quantity of caxved flints and bones of extinct species, an entire left hind leg of Ursus spelceus was found lying above the incrustation of stalagmite which covered the bones of other extinct species and the carved flints. The bear had therefore lived after the manufacture of these flint knives, consequently after the men who fashioned them. These men were therefore more ancient than the cave bear. Such were the conclusions of the Eoyal Society, and they were shortly afterwards confirmed by discoveries similar to those made at Brixham, notably by those of the cave of Long Hole (Grlamorganshire), where Colonel Wood, in 1861, found imbedded in the same stratum flint tools of the type of those of Amiens, together with bones of the Rhinoceros hcemitcBchus, which is of yet earlier date than the tichorhinus. From all these facts we gather that the theory of the co-existence of man and extinct species is no new one, and that proofs in support of it are not wanting ; but it has only been supported by incontestable evidence, at least as far as France is concerned, since the publication of the valuable works of M. Lartet on the bone caves of Perigord and upon the burial cave of Aurignac (Haute Garonne). It may even be said that the last remarkable monograph of this savant has become the starting point of all the DESCRIPTION OF THE BONE CAVES. 53 researches which have since been undertaken in France, in England, in Belgium, in Italy, and in Spain. I am far from wishing to underrate the value and importance of the work which has been done in the bone caves of neigh- bouring countries ; but the caves of France, and especially those of southern France and of Perigord, have supplied the most convincing proofs in support of this theory of synchronism, which acquires every day a greater number of partisans. This is an important fact, which Lyell him- self seems to h^ive somewhat forgotten, but M. d'Archiac has taken care to claim the recognition of its great im- portance. II. DESCBIPTIOIT OP THE BONE CAVES. The name of bone caves is given to the more or less extensive natural cavities which occur in Ihe sedimentary rocks of almost every epoch, but especially in those of the cretaceous beds of the Jurassic Mountains, and which contain a variable number of bones of men or of animals, intermixed, as a rule, with articles of human workman- ship. These cavities, usually complex, and very irregular in form, communicate with each other, sornetimes by wide galleries, sometimes by winding passages^ so narrow and so low that they can only be traversed on hands and knees. Varying considerably in length and height, they extend sometimes a distance of some miles in the interior of the strata in which they are concealed. Situated for the most part at a much higher level than existing watercourses, they communicate with the outer air by openings in the side of the mountain, by holes in the vaulted roof, or by a species of natural wells, into which in many cases those torrents fell which formerly bore along in their current the various matters now found in the caves. Hence come the evident marks of erosion which are almost always to . be observed on their walls.' As they hollowed out the valleys and gradually deepened their beds, the great rivers of the quaternary ' The care of Duruthy, recently described by M. Louis Lartet, is hollowed in a bed of nummulitic chalk. 54 THE ANTIQUITY OF THE HXTMAN EACE. epoch, often swollen by heavy rains, bore away the rocks which closed the entrance of the caverns, and deposited within them the ossiferous sediment and the waterworn stones which are found there ; we must therefore admit, with M. Ed. Dupont, first, that the openings of the caverns found on the slopes of the valleys took place at a date corresponding to their greater or less height above the present level of the river ; secondly, that the fluviatile de- posits with which they are partly filled are the more ancient, the higher they are raised above this same level. These deposits usually consist of a reddish, or some- times black sediment of sand or mud, containing bones of different kinds intermixed with sand, gravel, and water- worn pebbles, or with angular fragments broken off firom the roof or walls of the cavity. The ossiferous sediment is usually disposed in layers ; sometimes it forms a hard crust, intermixed with fragments of bone imbedded firmly in its mass, and it is then termed a bone breccia. Breccia of this nature nearly always occupy the lower part of the caverns and fill up their fissures. A stalagmitic crust of varying thickness covers in many cases the sediment and the remains imbedded in it. Sometimes even the successive ossiferous deposits are separated from each other by as many layers of stalagmite as there are layers of sediment.' Other calcareous incrust- ations, known as stalactites and stalagmites, presenting the most varied and whimsical forms, often cover the floor, the walls, and the roof of the caverns, and give them that fantastic appearance which caused them formerly to be considered as the abode of fairies. Occurring, as we have said, in the most various beds (chalk of the transition period, Jurassic, cretaceous, nummu- Utic, and upper marine tertiary rocks), and in every country ' In certain Brazilian caves Lund has counted seven layers of ossi- ferous sediment, separated by as many layers of stalagmite ; a certain proof that the bones therein contained were deposited at different and successive epochs. The same phenomenon was observed in a gallery of the cave of Brixham, near Torquay, and in certain caverns of France and Belgium. This clearly shows that the waters were introduced and with- drawn several times, and in the intervals the stalagmite was deposited. CONTENTS OF THE BONE CAVES. 55 on the earth, the bone caves present nearly everywhere the same general characters, but not the same contents. Thus while the most ancient caverns of the European con- tinent contain in more or less abundance the bones of the Ursus spelcBus, the Hycena spelcea, the Mephas primige- nius, the Rhinoceros tichorhinus, the Cervus tarandus, the Megaceros hibemicus, the Bison europceus or aurochs, &c., those of America contain, besides the monkeys peculiar to that continent, the remains of animals which recall, but in colossal proportions, certain species of edentata stiU living in the country. Such are the megatheriuTn, the mylodon, the Tnegalonyx, the glyptodon, &c. Finally, in Australia, where the only indigenous mam- mals belong exclusively to the family of marsupials or pouched animals, we find marsupials of gigantic size in the bone caves {Diprotodon australis, Macropus atlas, Phascolomys gigas, &c.). The condition of the bones imbedded in the sediment of the caves shows that they have undergone considerable changes in their chemical composition. They have gene- rally lost the greater part of their organic matter. They are fragile, resonant, more or less friable, cracked, and stick to the tongue when they are touched with it. Many of them are irregularly broken across, or else intentionally split lengthways. As a rule, they are scattered without any order in the sediment of the caves, but sometimes they have retained their natural positions. This was" the case with a femur, tibia, fibula, patella, and an astragalus of Ursus spelceus, found by Dr. Falconer in the cave of Brix- ham. The skeletons of the great mammalia (elephant, horse, ox, &c.) are very rarely found entire' in the ossifer- ous grottoes, while all the pieces of the skeleton of the reindeer and of animals of small or middling size are very often, indeed nearly always, to be found. This is owing to the fact that the troglodyte savages of our lands carried ' Among the rare examples of which we are speaking, we may instance the al rost entire skeleton of a rhinoceros found in the ossiferous s.jdi- ment of Dream Cave, in Derbyshire, an evident proof that when intro- duced into this subterranean cavern, it was still clothed with flesh, or at least that the bones were still connected by ligaments. 56 THE ANTIQUITY OF THE HUMAN EACE. away entire to their subterraneous dwellings those victims of the chase whose weight was not too great, while they cut up on the hunting ground the larger booty, contenting themselves with bearing away the head and limbs to eat in the cavern. So many different opiaions have been put forward with respect to the means by which the bone caves were filled, that it appears impossible to reconcile them with each other. The supposition that all bone caves have been filled by watercourses in flood, which at different times have borne thither, in company with gravel, mud, and pebbles, the immense quantity of bones which they encountered on the surface of the soil, is, we think, a too absolute assertion, and one which observation has shown to be false. For often even the youngest and most fragile bones present no trace of a violent or prolonged removal ; their sharpest edges, their most acute angles, are intact, which would certainly not be the case had they been carried any dis- tance by the current. Now this is precisely what has been observed in those caverns which contain only the remains of Ursus spelceus. We are therefore justified in ascribing the accumulation of these remains to the prolonged habitation of the bears in these caves, until the moment when they were over- whelmed by the waters, diluvian or other, and buried then and there in the sediment which they bore along with them. Again, when we find in company with these bones of bears, and imbedded in the same sediment, those of herbi- vorous animals intermixed with those of the great Felidm or of Hyaena spelcea, we ought to admit with the author of ' Eeliquise Diluvianae,' that these great carnivora may have carried their prey into these subterranean hollows, to devour it there at their leisure. The marks of the teeth of the carnivora still to be seen on the bones of the herbivora crushed by their powerful jaws ; the presence of their excrement (^coprolithes) in the very place of de- posit; the heaps formed by these ejecta, still placed one over the other, and as if articulated together ; are so many proofs which testify against the th.eory which assigns the ACCIDENTAL DISTXTHBANCES IN THE CAVES. 57 action of diluvian currents as the sole agent in the trans- port of organic remains into the bone caves. The action of man himself should be seriously taken into consideration in seeking to determine the causes which have brought about the filling of the caves. For in many cases ' they have served as dwellings, as refuges, as the rendezvous of hunters, as meeting places or tombs to the earliest populations of these districts. It is there- fore not surprising that they should have left in them their mortal remains, the fragments of their daily meals, their weapons, their tools, in a word the still simple pro- ducts of their dawning industry. Unfortunately, we cannot always be sure that these objects are of the same date as the bones of extinct species with which they are found. Accidental disturbances of the soil, occurring at widely separated periods, may have mixed the productions of human industry with bones of a very different date. This is evidently the case in the cave of Fausan (Herault), where Marcel de Serres found a fragment of enamelled glass embedded in a skull of Ursus spelcBUS ; specimens of fire-baked pottery, relatively quite modern, were found at Bize by the same naturalist, side by side with other vessels of unbaked clay, and of far ruder workmanship. Similar facts, which may have occasioned many mistakes, have been observed in several other caves, among which it is suflScient for the moment to cite those of Herm and Aurignac. We cannot therefore always, and as a matter of course, conclude that the human bones found in company with the remains of extinct animals were contemporary with each other. But doubt is no longer reasonable when the bones of animals and those of our own species, uniformly mixed, imbedded in the same sediment, and which have undergone the same alterations, are moreover covered by a thick layer of stalagmite ; when objects of a completely primitive industry occupy the same bed with bones be- longing to extinct species ; when the latter bear the ' Some Italian caves were inhabited in the time of the Etruscans, and a few are still used in modern days. 58 THE ANTIQUITY OF THE HUMAIJ EACE. evident marks of human workmanship ; finally, when we find in the dUuvian strata of the valleys, manufactured objects and bones exactly like those discovered in caves of the same date. Now aU these circumstances occur together in the valleys of the Somme, the Ehine, the Thames, &c. ; as well as in certain caves of France, Eng- land, Belgium, Italy, Sicily, &c. All these bone caves cannot and must not, as we shall presently show, be referred to the same epoch. There are many far less ancient than those of which we have just spoken. A considerable number of caves belong to the age of polished stone, among which those in the departments of Ariege, of Aveyron, of Lozere, of Grard, and of Marne, have acquired a certain notoriety. In most of these, especially in those which have been used as places of burial, human bones have been found in company with objects made by man, and with remains of animals belonging to species which are analogous to, or altogether the same as those of our time. MM. Grarrigou and Filhol, who have care- fully studied the caves in Ariege {Niaux, Bedeilhac, Mas-d'Azil, &c.) are of opinion that they are of the same date as the oldest lake dwellings of Switzerland.' "We shall have occasion to recur to several of these eaves in the course of this work. * In' spite of the opinion of certain geologists who are somewhat behind the age, the researches ma;de in the caves, and likewise those of which the ancient alluvial deposits have been the theatre, clearly prove that man is prior to the events of which the diluvium was the product and the witness. Before that hour his foot pressed the soil which in the far distant future, now for us an obscure past, was to become the land of Gaul. He was the contemporary of the great annihilated quadrupeds. He saw, in our latitude, the primitive elephants wandering in virgin forests, the hippopotamus disporting itself in the rivers, the rhinoceros wallowing in the mud of the • See F. Garrigou and H. Filhol, Age de la 2>ierre poUe dams Us cavernes des Pyrenees ariegeoises. AGE OF THE CAVERNS. 59 marshes ; he heard the roaring of the Hon, and disputed his life with the terrible cave hear, and hunted those primitive oxen and stags the species of which are extinct.' ('Cosmos,' Journal Scientifique, 1867, p. 199.) III. AGE OP THE CAVEBlirS. M. Lartet is the author of the idea, at once natural and ingenious, that a kind of palseontologic chronology founded upon the gradual and successive disappearance of the great characteristic species of the quaternary epoch might be established f(Sr the bone caves of Europe. In following out this suggestion we find four principal divisions in the long period to which the bone caves belong, namely : 1. The age of the great cave bear {Ursits spelceua). 2. The age of the mammoth elephant (^Elephas pHmi- genius), and of the rhinoceros with partitioned nostrils {Rhinoceros tichorhinus). 3. The age of the reindeer (Gervus tarandus). 4. The age of the aurochs {Bison Europceus). The first of these ages is characterised by the presence of the bear, usually accompanied by the hyena, and the great cat or cave lion; the Ursus spelceus did not, accord- ing to M. Lartet, smvive this first period. The second epoch is distinguished by the disappearance of the mam- moth, which became extinct, after having long had as almost inseparable companions the Rhinoceros tichorhinus, the great hippopotamus, and Gervus megaceros. In the third period the reindeer, which at first predominates, disappeared from central Europe and migrated further north. Lastly, in the fourth age, the aurochs, which still live among tte Caucasus mountains and in the Lithu- anian forests, is at the present day, with the reindeer, emigrated towards the North, the sole remaining repre- sentative in temperate Europe of those species which are reckoned characteristic of the quaternary period. M. Dupont has proposed a classification of the caves which differs from that of M. Lartet. He holds that the oldest caves should be characterised by the presence of such animals as are completely extinct {Mammoth, Ursus 60 THE ANTIQUITY OF THE HUMAN RACE. spelcBus, Felis spelcea). To the second class would belong those caves in which are found the hones of those animals which have migrated (reindeer, chamois), but which survive to our own day. In a third and last group he would include those caves which contain the bones of species still living, or which have been destroyed by man. But as it nearly always happens in such cases, subsequent observations soon showed that these divisions were far too definite, the same cave often belonging to two and even to three consecutive ages. For instance, Garrigou and Martin proved that the cave of Lourdes (Hautes Pyrenees),^ ranked by Milne- Edwards and Lartet in the age of the aurochs, should be ascribed to an earlier epoch, for it contains a quantity of reindeer bones, a species which disappeared, as we have already shown, considerably earlier than that of the aurochs." In several caves of Sologne, the Marquis de Vibraye observed in the lowest layer of the diluvium (grey diluvium) bones of extinct species contemporary with the mammoth, together with flint tools of rude workmanship ; the upper layer (red diluvium) contained, on the other hand, abundant remains of the reindeer inter- mixed with flints wrought with a degree of skiU which testifies to the existence of a civilisation equal to that of the lake dwellers of Switzerland. Four successive ages have also been observed in the cave of Mas-d'Azil (Ariege).^ The age of the reindeer and that of polished stone are equally represented in the cave of la Vache.' ' Thus we have,' says M. d'Archiac, ' in this single valley of Ariege, the elements of a human chronology which is nowhere else to be found in so complete a form in so limited a space.* The Cave of the Fairies (Yonne), explored by M. de ' Comptes rendia de Vlmtitut, Mar. 2, 1864. Age de Vavirochs et dge dvi renne dans la grutte de Lourdes. 2 Garrigou and Filhol, Age de la pierre polie dans les eavernes del Pyrinees anegeaises. » Dr. Garrigou, Age du renne dans la gratte de la VaeTie, pres de Tarascon {Ariege). Memoire Soo. Sist. Nat. de Taultmse, 1867, p, 58. * D'Archiac, Faune quaternoAre, p. 106, Paris, 1865. KENT'S CAVERN. 61 Vibraye, is likewise an example of a cave where several successive ages are well represented. In the lowest layer are contained the remains of the great characteristic species of the diluvium ( ITrsus spelceus, Hycena spelcea, &G.) ; in the middle layer are those of the reindeer ; lastly, in the upper layer (loess) bones of animals stiU living in the district (fox, badger). Analogous facts have been remarked in the department of Herault (cave of Pontil) by M. Grervais ; in that of Aude (at SallMes-Cabardes) by M. Filhol ; in Poitou by MM. Brouillet and Meilles, &c. Kent's Cavefn, near Torquay, is another example which proves incontestably that the same bone cave may have been inhabited by man at different epochs. In a layer of red loam overlying the original soil of this cave are found bones of extinct or migrated animals {Machai- rodus latidens, Ursus spelceus, ffycena spelcea, Gervus tarandus, &c.), intermixed with carved flints (some of the Saint-Acheul type, others resembling those of Aurignac, of Moustier, and of Laugerie Haute), and with implements of reindeer bone (harpoons and barbed arrows, awls, pins and needles), which resemble the delicate work of the troglodytes of la Madelaine (Dordogne).' The bed of red loam which contains these various objects is itself covered by a layer of stalagmite from one to three feet thick, and a third layer of dark muddy soil, from four to fifteen inches in depth, overlies the stalagmite. ' Above the stalagmite, and principally in the black mould, a number of relics have been found belonging to different periods, such as socketed celts, and a socketed knife of bronze, and some small fragments of roughly- smelted copper, about four hundred flint flakes, cores, and chips, a polishing stone, a ring of stone already described, numerous spindle-whorls, bone instruments terminating in comb-like ends, pottery, marine shells, numerous mam- ' Among the flint instrnments discovered in Kent's Cavern are several ■which have the form of long splinters, similar to the splinters of obsidian with which the inhabitants of New Caledonia tip their javelins, and which those of Terra del Fuego use both for arrow heads and knives. Tho English flint knives in question are very like those of Laugerie HautOj but the workmanship is not so good. 4 62 THE ANTIQUITY OF THE HUMAN RACE. malian bones of existing species, and some human bones, on which it has been thought there are traces indicative of cannibalism. Some of the pottery is distinctly Eoman in character, but many of the objects belong, no doubt, to pre-Roman times.' ' We cannot hesitate to conclude from this list, that subsequent to the deposit of the stratujn of dark soil, Kent's Cavern was frequented by men of the age of bronze and of polished stone, without counting those of the Roman epoch who have left in the cave the traces of their in- dustry. But it is equally incontestable that Kent's Cavern long served as a dwelling to the primseval inhabitants of the country, that they had their meals in it, and worked in i3int and bone there, &c., until the day when the thick layer of stalagmite which covers the ossiferous sediment was formed. No other explanation would account for this strange admixture of bones of extinct species, of flints of the Saint-Acheul and Moustier types, of artistically wrought bone implements, contained in the same sediment. Here then is a cave which contains incontestably in situ, according to the scientific men who have explored it, objects belonging to all ages, and which it is consequently impossible to rank in either of the too exclusive categories admitted or proposed by palaeontologists. The caves of Hohefels in Wurtemberg and of Thayngen in Switzerland offer analogous and perhaps even more remarkable facts ; for in the last especially were found an essentially northern fauna, and animals whose contemporaneity was far from being suspected. The palaeontological classification of caves is therefore liable to lead us into serious mistakes ; and moreover it is often entirely local. Thus Louis Lartet himself was obliged to modify in almost every respect the chronology of his illustrious father, in determining the age of the Spanish caves which he had been exploring. Therefore ' ETans, The Ancient Stone Implements, Weapons, and Ornaments uf Great Britain, p. 445, 1872. In certain Italian caves (Grotta dell' Onda, Grotta de' Goti e della Giovannina) bones of Ursus spelieui have been found as well as tools of the neolithic age. CLASSIFICATION OF THE CAVES. 63 in 1867 Dr. Garrigou proposed to the Societe d'Histoire Naturelle of Toulouse a new classification, which is gene- rally adopted at the present day. It is as follows : — 1. The age of the TJraus spelceus, with which the author connects also the period of the mammoth. 2. The age of the Cervus tarandus (reiadeer), com- prising also that of the aurochs, and characterised in its latter half by the almost complete disappearance of the species of the first age indicated above. 3. The age pf poUshed stone. Like those which it was intended to reform, the classi fication of Dr. Garrigou is somewhat arbitrary ; for we do not know with certainty the precise epoch at which the animals which characterise any given period ap- peared in our lands or disappeared from them. More- over, these epochs sometimes overlap one another, like those of stone, bronze, and iron. • "We know, for instance, that the great cave bear and the mammoth often accom- pany the reindeer, even in those caves where the bones of the latter are far more numerous ; that in certain caves (Solutre) the bones of the last-named animal were dis- covered along with those of the horse, predominant in its turn and perhaps already domesticated ; finally that M. L. Lartet found carved and engraved reindeer bones in the cave of Duruthy, together with objects of industry which announced the dawn of the age of polished stone. While recognising the defects we have mentioned, and taking as his point of departure the comparative degree of skill attained in the workmanship of the artificial pro- ducts taken from the bone caves, M. de MortUlet proposed to class these implements as follows : — 1. The epoch of Saint-Acheul (Somme), distinguished by the almond-shaped axe, the axe in the form of a cat's tongue, and by the absence of bone implements. 2. The epoch of Moustier (Dordogne), distinguished by scrapers and triangular lance heads, cut only on one side. 3. The epoch of Solutre (Sa6ne-el>-Loire). The almond-shaped axes disappear j the flint spear heads are 64 THE ANTIQUITY OF THE HUMAN EACK more skilfully wrought. The principal weapon is an angular mace, which reappears in the following epoch. 4. The epoch of Aurignac (Haute Garonne). Bone implements are more frequent. The angular mace per- sists. The arrow and spear heads, instead of being flint, are fashioned in bone or from the antlers of the reindeer. 5. The fifth epoch is that of la Madelaine (Dordogne), distinguished from the preceding by the presence of numerous works of art carved or engraved upon stone or bone. The arrow and lance heads in bone or reindeer horn are, as at Aurignac, bevelled or pointed at their lower extremity so as to penetrate the shaft which is destined to carry them. The above classification would be doubtless convenient, if it were in entire agreement with the facts. Unfor- tunately the testimony of facts tends to lessen its value. Thus the workmanship of Cro-Magnon, for instance, seems less advanced than that of la Madelaine, and yet M. de Mortillet confounds the two epochs. Moreover, judging from its tombs, its carved flints, and rude sculpture, we are inclined to place Solutre in an epoch intermediate between the ages of the reindeer and of polished stone. This cave would thus be more recent than la Madelaine, although it is ranked long before it by M. de Mortillet, However, on receipt of further informa- tion, M. de MortiUet subsequently modified his original classification, and we here reproduce an abridged form of his new table of the geological ages. Ages Periods Neolithic, or of polished stone I ^^ Epbenhausen. The lake dwellings ' ^ [ and dolmens. Palseolithio, or of chipped stone /Of la Madelaine. The majority of the bone oaves ; almost the whole of the reindeer epoch. Of Solutrfi. The reindeer and the mam- moth. Of Moustier. The great cave bear. Of Saint- Aohenl. The mammoth. Eoltthic, or of stone splintered f „« mi, m i- by the action of fire jOf Thenay. Tertiary period. CLASSIFICATION Of M. HAMY. 65 However ingenioug and convenient the industrial classi- fication of M. de Mortillet may be, it is not even a purely artificial one, and more than one objection has already been raised against it on this head. For whatever he may maintain, the progress of industry is not sufficiently evident nor the differences sufficiently marked, between the types of Moustier and Saint-Acheul, to allow us to admit their regular succession in space and time. Nume- rous and precise observations made on the spot by M. d'Acy prove thjt one type is not placed above the other, and that the flints of the Moustier type are as abundant in the lower strata as in the upper, although, according to the theory of M. de Mortillet, they do not occur in the former and only appear higher up. Taking into account at once the stratigraphical, palae- ontological, and archaeological characters, and especially desirous to remove the doubts which some people still retain with respect to the authenticity or to the great age of the bones and works of art found in the caves, M. Hamy has endeavoured to establish, between the caves and the quaternary alluvium, a parallel which shows them to be often identical. Indeed it could hardly be otherwise, since in a great number of cases, the filling of the caves took place at the same time as the deposition of the allu- vium in the valleys. There is therefore an agreement, and even synchronism, between these two series of facts, and the organic remains, as well as the products of human industry, are generally identical in the two kinds of de- posit in question. If then the fauna of the alluvium of the valleys and that of the sediment of the bone caves are similar,-^the proofs furnished by the one corroborate those given by the others, and by establishing a comparison we can draw our conclusions with certainty. Starting from these pre- mises, which are undoubtedly correct, and always subor- dinating, as he says, the history of the caves to that of the alluvium, M. Hamy has divided the bone caves into five groups corresponding to as many places which serve as types of stratified alluvium. 66 THE ANTiaUITY OF THE HUMAIJ EACE. The first group belongs to the period of transition be- tween the upper pleiocene and quaternary strata. It com- prises, on the one hand, the shelly and sandy beds (crag) of the counties of Norfolk and Suffolk, the submerged forests of England, and the caves of which Montreuil is the type ; on the other, the caves of Wookey, Gower, Syracuse, of San Teodoro, &c., which were fiUed up at a date ante- rior to the second glacial period. The pleiocene and quaternary species here co-exist, but the latter become more and more abundant, while the former gradually disappear.' Flint implements exist, but they are more rudely fashioned than those of Abbeville. The caves of the second group, of which Moustier, Herm, and Nabrigas may be considered as the principal types, belong to the age of the mammoth. This group is characterised palseontologically by the simultaneous pre- sence of extinct animals (cave bear, mammoth, &c.), those which have migrated (reindeer and hippopotamus), and those stiU extant in the country (horse, ox, &c.). Geologically it corresponds to the grey diluvium of Paris, that is, to the lowest layers of the fluviatUe alluvium, to which M. Belgrand has given the name of lower levels. The corresponding typical beds are those of Hoxne, Saint- Acheul, Abbeville, Levallois, the valley of the Ehine, Clermont-sur-Ariege, Denise, &c. The skulls of Neander- thal, Lahr, Egnisheim, and of the Olmo ; the jawbones of MouUn-Quignon, of Naulette, and of Arcy, belong to this age of the mammoth. The third group forms a link between the ages of the mammoth and reindeer. The typical caves are those of Aurignac, Bize, Cro-Magnon, Engis, and the Trou du Sureau in Belgium. The stratified alluvium comprised ' An ElepTias meridionaUs was fotmd at San Teodoro ; and in the cave of Baume (Jura), which chronologically corresponds to the strati- fied deposits of Cromer and Montreuil, a Maelimrodus latidens, a plei- ocene species of great hear, with long flattened canine teeth, serrated at the edges and curved backwards like a scimitar, was found in company with the Hyama spelcea and the ElepTiat primigenkm, animals which distinctly belong to the quaternary epoch. DIVISIONS OF THE QUATERNAEY EPOCH. 67 in this group belongs to the mean levels of the Seine and to the deposits of which those of Grenelle and Var are types. The work in bone improves, and the shaping of the flint tools is simplified. The fourth group includes the types of Eyzies, of la Madelaine, of Laugerie Haute ; to which must be added the other caves of Perigord (excepting that of Cro-Mag- non) as well as la Vache, Massat, Bruniquel, Trou Magrite, Pont a Lesse, and Solutre. M. Hamy ranks in this sub- division the beds of Boulonnais, of Schiissenried, and the high levels of Qie Seine (red diluvium and loess). This group corresponds to the first age of the reindeer. The grotto of Chaleux and other caves of the valley of the Lesse {trou du Frontal, trou des Nutons), belonging 1.0 the second age of the reindeer, are comprised in the fifth group. With these are reckoned in France the caves of Lourdes, and those of la Balme and Bethenas in Dauphine. The skulls of Furfooz belong to this epoch, which is distinguished from the preceding ones by a marked decadence in the work in flint and bone, which in the preceding epoch had shown a steady improvement. At Eyzies and at Massat the first attempts at engrav- ing on stone were discovered. At la Madelaine carving in bone begins, and at Laugerie Basse and at Bruniquel it attains its highest degree of perfection. A specimen of carving on stone was found at Solutre. The data furnished at once by stratigraphy, palseon- tology, and prehistoric archaeology, form the bases of the divisions proposed by M. Broea for the quaternary epoch, divisions which he has himself drawn up in the following table, which we have already given, p. 28. 68 THE ANTIQUITY OF THE HUMAN EACE. StratigrapMcal Data Palaeontologioal Data ArcbffiOloglcal Data Quater- nary - epoch Modem epoch Low levels of undis- turbed valleys Mean levels High levels Recent beds ' Age of the lhammoth Intermediate age Age of the reindeer Modern fauna The axe of Saint- Acheul (fig. 13-14"; Airo-whead of Mous- tier (fig. 15-17) Arrow head of So- lutr6 (fig. 18) The polished axe (fig. 19) Hence we see that M. Broca adopts the stratigraphi- cal data established by M. Belgrand, and, that in deter- mining the palseontological data, he admits, with M, Hamy, an intermediate age between that of the mammoth and of the reindeer, that is, an age corresponding to the middle of the quaternary epoch. At this period, several species contemporary with the mammoth had already dis- appeared; others were nearly extinct; while the reindeer, on the contrary, was becoming more common, since it was altogether predominant in the following age, to which it gives its name. • As for the data founded upon archseology, that is on the greater or less degree of perfection attained by the workmanship of stone during the archseolithic period, M. Broca reduces them to three principal ones, and cha- racterises each representative type nearly in the same way as M. de Mortillet has done. Finally, applying this classification to the caves of Perigord, he ranges them in the following chronological order : — ■ 1 . Moustier, the earliest of the caves in Dordogne. 2. Cro-Magnon, more recent than the preceding, but belonging equally to the intermediate age. 3. Laugerie Haute and Grorge-d'Enfer, on the right bank of the Vez^re, already form part of the reindeer age. ' M. Broca justly remarks chat though they are called recent as compared to the quaternary beds proper, the epithet is unsuited to them from the point of view of our modern chronology, since the lapse of ssveral centuries was required for the formation of some of them. — \Bevue Soieatifique, Nov. 16, 1872.) Saint-Acheul Typk. Iio. 13. Front view. Axe, carved on both sides. FiQ. 14. SideTiew. MouSTi 1 __B. Via. 15. Uncut surface. Lanob head carved oitlt on one side. Fia. 16. Side view. FiQ. 17, Carved surface; 70 THE ANTiaUITY OF THE HUMAN KACE. 4. Laugerie Basse, Eyzies, and la Madelaine form a group which brings us down to the total disappearance of the reindeer from France, and consequently to the end of the quaternary epoch, succeeded by the modern or neo- lithic period.' Fig. 18. Solctee Type. Lance head. Fig. ]9. Polished stone axe. (AJEter Lubbock. * Prehistoric man.') All these are doubtless laudable attempts, and they throw some light on a subject which still remains somewhat obscure ; but each author has his own distinct system, and ' Some facts observed at Bruniquel, at Solutr6, and in the cave of Duruthy, seem to indicate that the reindeer became extinct in France towards the beginning of the neolithic period. QUATEENAEY FAUNA. 71 it is difficult to decide to which to give the preference, not as being the most convenient, but the most correct. However, it is undeniable that these essays are useful, since they connect the abundant facts of past ages, deter- mine their chronological sequence, and in a word illustrate the history of quaternary man. Unfortunately, the classi- fication drawn up by the authors of these various attempts, ingenious as they are, cannot always be pronounced strictly accurate, and they do not present that concord and har- mony which is one of the distinguishing marks of truth. They may nevertheless be adopted provisionally until the progress of science, or the chances of the future, furnish us with a better guide. IV. dUATEBNABT FATTIJ-A. HSTHABITAITTS OF THE BONE CAVES. At the beginning of the quaternary epoch the mastodon existed no longer, at least in Europe,' nor the Mephas meridionalis of the sand-pits of Saint-Prest. The Hippo- potamus major and the iJAinoceros Merkii and leptorhinus of the pleiocene period were still living. But the quater- nary fauna properly so called, is chiefly represented among us by the mammoth, the Rhinoceros tichorhinus, the cave bear, cave hyena, great cave lion, the Irish elk, &c., which ended by yielding place to the reindeer, to the glutton, the musk ox, the Saiga antelope, the chamois, the wild goat, and the marmoset, which at a later date migrated to other districts. We may add to this list nearly all the animals living at the present day, and which appear to be the more or less modified descendants of quaternary species. Of these then some are extinct; such as Ursus spelcBUs, Hyaena spelcea, Felis spelcea, Elephas primi- genius. Rhinoceros tichorhinus, Megaceros hibemicus, to which we must add the Machairodus cultridens and latideins (R. Owen) found in certain caves of France and England. Other species still living; lemming, lagomys, glutton, arctic fox, reindeer, musk ox, have migrated towards the north of Europe, and even to America. Others, ' This animal lived in America during tide quaternary period. 72 THE ANTIQUITY OF THE HUMAN BACE. on the contrary have gained the east (Saiga antelope, hamster), or the south, or have no longer any kindred species except in the hottest regions of Africa and Asia (hippopotamus, elephant, lion, hyena). Others have taken refuge on the summits of the Alps and Pyrenees (chamois, wild goat, marmoset) or have dis- appeared from our countries since the beginning of history ; such for example is the urus {Bos prmdgenius), which in the time of Caesar still inhabited the Hercynian forest and even the great woods of the Vosges and other parts of Lorraine (Godron). Others have fled before man, their improvident de- stroyer. Of these are the aurochs {Bison europceus), restricted at the present day to the forests of Lithuania, ■ with the exception, however, of a few scattered individuals recently found wild in the neighbourhood of the Caucasus ; the lynx, which, according to Cuvier, has almost entirely disappeared from inhabited districts, but which is still to be found in the Pyrenees and even in Africa ; the beaver, formerly very common among us, and now banished to the banks of the Ehine and the Danube, where it is only to be found in small numbers ; the mouflon, which M. Bour- guignat says he found in the cave of Vence in Provence, and which now exists only in the islands of Sardinia and Corsica. Others, finally, have remained in those same districts where we find at the present day the bones of their earliest ancestors : the wolf, the dog, the fox, the badger, the otter, the mole, the hedgehog, the common stag, the ox, the wild boar, the horse, &c. Birds, reptiles, fishes, and molluscs, of similar or analo- gous species to those now existing, are also to be found in the caves of Europe ; but these are in small number as com- pared to mammalia. With regard to fishes, M. Ed. Lartet has made an important observation : they are rare or common in proportion to the remote or recent date of the bone caves. For instance, in the caves of Aurignac (Haute Ga- ronne), of Moustier, of Gorge d'Enfer (Dordogne), and of la Chaise (Charente), they are distinguished by the presence of the unbarbed arrow, and where not a single fishbone has BIRDS RECENTLY EXTINCT. 73 been hitherto discovered. We are left in uncertainty as to whether the earliest inhabitants of our lands were possessed of tackle sufficiently perfect to procure them- selves an abundance of iish, or whether, as is highly improbable, they were in the habit of eating on the banks of the river the raw fish they had just caught. On the other hand, fish abound in caves of more recent date, where barbed arrows and harpoons are found, in la Made- laine, at Eyzies, at Bruniquel, &c. The same remarks apply to birds, which are also less abundant where arrow heads with a double range of barbed points are wanting. This fact had been already noticed by M. Brun, before M. Ed. Lartet called attention to it. With regard to birds, only two species have become ex- tinct in Europe since the quaternary epoch, and nearly in our own time, the grouse {Tetrao urogallus) and the great penguin (^Alca impennis), which are no longer found in Denmark. But cases are numerous among the birds of the Isles of Bourbon and Matu"itiu8, of Madagascar and New Zealand.' No species, either among reptiles, fish, or invertebrate animals, has lately become extinct excepting the Cyrena fluminalis, which lived formerly in the Somme and the Thames, and which is now confined to the waters of the Nile and certain rivers of Asia.' ' The dinomis and the epyornis are two gigantic birds, something like the ostrich; the one found in the most recent strata oJE New Zealand, the other in the modem alluvium of the Isle of Madagascar. The height of the latter was about 16 feet, its eggs were equal in capacity to six ostrich eggs, to 148 hens' eggs, to 60,000 humming birds' eggs. One of them which I was enabled to see and measure at Toulouse had the following dimensions : — m. Great diameter 1 ft. 8 in. Little diameter 9 in. Thickness of the shell . . . . 1 to 2 lines. Finally, it could contain nearly 2 gallons of water. One of the eggs of the epyornis described by Saint-Hilaire was still larger. Hence we readily conceive that the Malagasy use them as provision vessels, and even, it is said, as saucepans. It is not quite certain that these birds are completely extinct. The dodo, nearly akin to our gallinaceous birds, was still extant in Mauritius in 1626. ^ Certain Crustacea (^Qamma/rus loricatvi and Mysis reUcta), whose 74 THE ANTIQUITY OF THE HUMAN KACE. All the species of mammalia which we have already named as occurring in the eaves of Europe are not equally and uniformly distributed among them. In some the pachydermata and the great camivora are predominant, especially the hyenas (^e.g. Kirkdale in Lancashire, Lunel- viel in Herault). Elsewhere (in the caves of Franconia, of Osselles, of Nabrigas, of Herm, &c.) the bears are more abundant, sometimes to the exclusion of all other species. In a great many districts (Bize, Bruniquel, la Madelaine, Eyzies), the reindeer predominates, nearly always accom- panied by other ruminants of the genera bos, cervus, and ovibos, and even by the cave bear and other great pachy- dermata then gradually disappearing. It was for a long time believed that the reindeer was only to be found in the bone caves. Eecently discovered facts have proved this to be a mistake which it is im- portant to correct. In a diluvian bed in the Thames valley, that of Acton, which resembles in all particulars that of the valley of the Somme, Colonel Lane Fox found the bones of Cervus tarandus intermixed with those of Hippopotamus major, of Elepha^ prvmigenius, of Rhino- ceros hoiinitcechus, of Bos primigenius, and of Bison 'prisons, in company with flint implements of the rudest workmanship. Some months after this discovery by Colonel Lane Fox, M. Chantre observed in the sediment of the Ehone basin a curious assemblage of species of the quaternary fauna, among which figured the Cervus tarandus. Finally, the bones of the reindeer were found at Schiissenried in Suabia on a moraine of an ancient Rhine glacier ; ^ a new proof that this animal lived in origin dates from the glacial period, are still extant in Sweden, in Lakes Wenner and Wetter. Moreover, recent soundings made on the coasts of Europe and America hare raised from the bottom of the sea tereiratulce and sea urchins similar to those found in the chalk of the hill of Meudon, of the cliffs of the coast of England, and of the plains of Champagne. > At Schiissenried reindeer bones were found on the moraine of an ancient Rhine glacier, in company with those of the glutton and of the arctic fox, with remains of mosses which are now only found in the most northern regions of Europe. The bones of this animal were so abundant in the above mentioned place that Professor Fraas was enabled, by making an anatomical selection among them, to reconstruct an entire akeleton, now in the museum at Stuttgard, Reindeer bones were also DISTRIBUTION OF QUATERNARY FAUNA. 75 Suabia during the glacial period, perhaps even during the interval which elapsed between the two glacial periods which have left their traces in Switzerland. Its existence in France long after the extinction of the great pachyder- mata, of which event moreover the exact date is entirely unknown to us, is rendered more than probable by the discovery of its bones intermixed with those of the horse and the ox in the caves of Bethenas and of la Balme in Dauphine, and further by implements of the neolithic age, perhaps ev^ of the age of bronze, found with these same bones at Bruniquel. As for the Saiga, M. Albert Gaudry has lately shown that this species of antelope lived in the reindeer age not only in Perigord but also in Angoumois, and that our ancestors fed upon the flesh of this beautiful animal. In short, the quaternary faima resembles our modern fauna, which is merely the continuation of it ; but the former is richer, more varied, better nourished, and conse- quently more vigorous than ours. However, in spite of their greater size, the diluvian mammalia, like those of the tertiary rocks, had, it seems, a relatively small brain, and perhaps a shorter life than those of modern times. "We are struck by the strange association, especially in the quaternary fauna, often in an extremely narrow circle, of species so numerous and so distinct either in their habits or with regard to the geographical distribution of kindred species now extant. We shall shortly examine the cause of this phenomenon, which has long perplexed palaeontologists, and which has lately found a satisfactory so lution in the knowledge of the distribution of land and water in Europe at the time when these animals lived in Europe. As an example of the singular assemblage of species of which we are speaking, we shall presently quote the list of those which, according to M. Merk, were found together in the Kesslerloch, in the neighbourhood of Thayngen. See p. 78. found in abundance at Thayngen, and in the cave of Pont-du-Gard. This animal advanced, therefore, further towards the east of Europe than it was originally believed. — (_Revue Soi»n,tiflque, Jan. 11 and 25, 1873, pp. 665 and 712.) 76 THE ANTIQUITY OF THE HUMAN RACE. Principal Mammalia op the Caves of Feancb, or of THE Diluvium. Extant in the districts Extinct or highly modified Migrated where they are now found in a fossil state Hyiena spelsea Cape hyena Bat (several species) Felis spelsea Aurochs Shrew mouse Blephas primigenius Eeindeer Hedgehog Ursus spelaeus Elk Dormouse Machairodus cultridens Canadian stag Water rat Rhinoceros tichorhinus Virginian stag Common bear Ehinooeros hsemitseohus Lagomys Badger Equus lartetianus Lemming Wolf Megaoeros hibernicus Spermophilus Urus 1 Domestic Animals Dog Marmoset Fox Horse Chamois Polecat Ox Wild goat Weasel Goat Beaver Marten Sheep Musk ox Babbit Pig Saiga Hare Fallow deer Eoe deer Bed deer Fauna of the Bnolish Caves. We think it desirable to give for the sake of comparison the list of animals and of the products of art found in Kent's Cavern, near Torquay. The following list, drawn up by Evans, is the enumeration of the species whose bones were found in the red loam underlying a thick layer of stalagmite. Maehairodus latidens very rare Mlis leo, var. spelcsa, cave lion . . . abundant Hycena orooicta, var. spelaa, cave hyasna . very abundant Camis Vapus, wolf ..... rare Cmiis imlpes, var. spelaus, large fox . . „ Oulo luicus, glutton very rare X/rius spelceus, cave-bear .... abundant Ursus prisons— ferox, grizzly bear . . „ Vrsits a/rcios, brown bear .... scarce Mephas primigenitcs, mammoth . . . not very common OBJECTS FOUND IN THE OSSIFEROUS SEDIMENT. 77 Bhiiwcero! tieTwrTiirmg, woolly rhinoceros , JSquus eaballug, horse Bos primigenim, urus Sison priseus, bison . Cervus megaoeros, Irish elk Cervws elaphvs (Strongyloceroi spdieun, Owen), stag . Ce-rvus taraadus, reindeer . Lepiis timidus (var. cUhimanus ?) Lagomys spelams, cave pika Arvicola ampMbius, water vole . A. agrestis, field vole . A. pratensu, bank vole Ccutor fiber, be^er . hare abundant very abundant scarce abundant not uncommon abundant rare very rare rare »» very rare scajToe ' Animals wTwse remains merefovmd in the bed of black vuntld above tlie stalagmite. Dog X Short-horn ox {Bos longifrons) Boe deer Sheep Goat Pig Babbit That is, the fauna of the present day, accompanied by instruments of the polished stone and bronze ages. In other bone caves of Great Britain, the following species have been found : Rhinoceros hcemitcechus. Mhi/noceros megarhinus. Elephas antiquus. Cervus Guettardi (a variety of the reindeer). Lemming'. In the diluvian gravel beds two molluscs occur which no longer exist in England (Hydrohia marginata, and Go7-bicula fiuminalis). Objects of Human Industbt found in the Ossiferous Sediment. Flint implements of the types of Saint-Acheul, of Aurignac, of Moustier, of Laugerie Haute ; barbed har- ' Note the absence of Ovibos mosahatus, or musk ox, both in the oaves and diluvian gravel beds of England. The birds and fish found in Kent's Hole have not yet been determined. See Evans, Ancient Stone Implements and Weapons of Great Britain, pp. 462, 463. 78 THE AJSTTIQXriTY OF THE HXMAN EACE. poons and arrows, fish hooks, pins and needles of bone, nearly resembling similar objects found at la Madelaine (Dordogne). Fauna of the Cave op Kbssleeloch, nbae Thayngen (Switzer- land), ACOOEDINe TO THE LIST OF M. MBKK. f 1- Number of Specimens Cave lion ... 3 Extinct animals . 2. 3. Mammoth . Ehinoceros 4-6 1-2 [ i. Bear . 1 ■ 1 5. Reindeer . 250 Towards the north . 6. Glutton 4 7. Arctic fox . 3 ■ 8. Chamois 1 "3 Towards the Alps . 9. 10. 11. Wild goat Alpine hare Marmoset . 1 500 1 1 1 Towards America . Towards the Alps 12. 13. 14. ri5. Wapiti Canis lagopus Lagoped . Aurochs 1 40-60 80 6 1 16. Eed deer . 6 § 17. Bear . 2 3 To neighbouring countries- 18. 19. 20. Lynx . Wild cat . Wolf . 3 1 17 21. Swan . 1 22. 23. Wild goose . Osprey 2 1 '3 Still in the land . f24. 25. European fox Hare . 2-3 2 a ■ 26. Crow . 3 'a < Domesticated . 27. 28. Dog J Horse . 1 20 V. BOITES OF WOUNDED AWIMALS POTTlfD IW THE CAVES. If it be true that the wrought flints are works ' which no freak of nature, no agency but a human hand, guided by a human mind, could have produced ' (A. Graudry), we may say the same with still more certainty of the bones of extinct or migrated species which bear the unmistake- able marks of wounds made by man, or the no less evident trace of an industry which reveals an art, doubtless rude, but already animated by a lively sense of nature. We will consider the former in the first instance. BONES OF WOUNDED ANIMALS. 79 In his ' Eecherches sur les Ossements Fossiles,' vol. iv. p. 396, Cuvier speaks of a head of cave hyena (of Gailen- reuth) whose occiput had been fractured, and which had recovered from the wound; Marcel de Serres has observed a similar fracture on the skull of an Hyceifia speloea (of Lunel-viel), whose left parietal bone was cleft through the whole thickness of the bone, a wound produced, he thought, by the tooth of some other carnivorous animal.' But it seems more natural to attribute these wounds to some weapon (flint javeUn, or arrow) thrown by man, for since the time at which these observations were made by the authors whom I have quoted, several authentic examples of this kind of wound have been noted by trustworthy observers. I myself excavated from the cave of Nabrigas,^ in Loz^re, a skull of Vraus spelceus, which presented a marked depression on the right frontal bone, and in the centre of this depression a circular hole, whose smooth and polished edges indicate that a wound made by some sharp projectile had begun to cicatrise. Supposing tbat-a combat had taken place between this bear and one of its own kind, it is more than doubtful, in my opinion, that one of the canine teeth of the latter could have thus pierced and fractured one of the frontal bones, while the other left not the slightest trace upon the skull. The wound in ques- tion seems to me therefore to have been made by some missile thrown by a human hand. Admiral Wauchope affirms that he has seen a stone hammer imbedded in the skull of an Irish elk (^Cervus megaaeros), and even several heads of other animals of the same species wounded in like manner. On an entire skeleton of Bos urus (the urus of Csesar) dug in the presence of Nilsson from out a deep peat moss of Southern Scandinavia, he observed the first lumbar vertebra pierced from in front by a javelin armed with a flint head, which had been thrown with such force that the point had pene- ' Maroel de Serres, Essai stir Us cavernes a ossements, p. 165. Paris, ] 838. ^ See N. Joly, Note swr uns notmelle caveme a ossements {Lozire'), in the BibHothegue Unirerselle de Geneve (1835.) 80 THE ANTIQUITY OF THE HUMAN EACE. trated into the next vertebra, in which it remained im- bedded.' Professor Steenstrup possessed, in his collection, fossil skulls of stags found in the kitchen middens, con- taining, incrusted in the bone, splinters of flint, doubtless broken off from some missile thrown by the hunter. Lastly, MM. Lartet and Christy have given an illustration in their interesting work on the caves of Perigord, of the vertebra of a young reindeer pierced by a flint arrow, which had remained in the wound (fig. 20). The Toulouse Museum of Natural History possesses the lower maxillary of an Ursus spelceus, of which one Fig. 20. Vkrtebra of a reindeeIi, with flint arrow head imbedded in the bone. (After Ed. Lartet and Christy.) branch, violently broken in two, resumed its functions after a complete cicatrisation. In what manner and on what food the animal lived during the necessarily very slow formation of the bone, it is impossible to say. That the wound in question was made by man seems extremely probable, we cannot say it is certain, since it is just pos- sible that the animal may have broken its jawbone by falling from a rock. As for the bones which bear the marks of regular in- cisions more or less deep, although they have sometimes ' Sven Nilsson, The Primitive Inhabitcmts of Scandinavia, p. 169, London, 1868. HUMAN BONES IN THE CAVES. 81 given rise to strange mistakes, the bones of haUtherium found at Pouance for instance,' it is known that palaeon- tologists set a high value on those of the pleiocene beds of Saint-Prest {Elephas Tneridionalis), of the quaternary deposits of the Somme valley (Rhvnoceroa 7neridionali8\ or of the channel of the Oureq (^Megaceros hibernicus), not to mention the incisions made vdth a flint tool on a quantity of reindeer bones, with the evident purpose of cutting the tendons near to their root, in order to use them for sewing. All these facts prove nothing less than the certain existence of man at an epoch far anterior to all historical tradition. We must not close this chapter without saying a few words about the fractured jawbones of the cave bear and lion, which M. Garrigou believes to have been used by man as defensive weapons. It seems more natural to attribute these fractures to a simpler cause than that which has been assigned. The dental canal of these maxillaries is enormous, and the disappearance of the dental nerve after they have been buried for a short time leaves a con- •siderable hollow, and age and damp render the slightest shock sufiBcient to break the bone at its weakest point. This may account for the fracture, which is always in the same place, observed on the numerous jawbones of Ursus spelcBUS in the Natural History Museum of Toulouse. We give this explanation with the more confidence that our opinion on this point was shared at the session of the Congress of Bologna by Professor Steenstrup, of Copen- hagen, a savant whose weight as an authority will certainly not be denied. VI. EWTIBE HTTMABT SKBLBTOWS FOUND IM" THE CAVES. WOUNDED HUMAIT BONES. TEAOTUKED SKUIiIiS. Although the caves have at every epoch served as dwellings, and frequently also as burial places, entire ' It is now generally known that Sir Charles Lyell and many other palaeontologists attribute to the teeth of the dog-fish (pa/rehm-odori) the supposed human incisions which have been observed by certain scien- tific men on the bones of the halUherirum found in the shell marl of Pouanofi.. 82 THE AKTiaTJITY OF THE HUMAN EACE. human skeletons are rarely found in them. "When this does occur, it generally shows that the corpse was buried in the fossil-bearing stratum long after its formation. M. Cartailhac, indeed, asserts that all the researches he has made justify him in declaring that every complete human skeleton found in the caves may be considered, a 'priori, as of later date than the fluviatile deposit in which it is contained. This is, perhaps, too sweeping an assertion, but it should be remembered by those palaeontologists who wish to avoid such mistakes as have been made, especially with regard to the human remains of Herm and Aurignac. Schmerling,who has explored forty-eight Belgian caves, found human bones in only two or three of them. Lund, out of 800 Brazilian caves, which he examined, found only six containing human remains. These bones are always rather rare in the ossiferous caves belonging to the oldest stone age, but they become fairly common in the reindeer epoch, and still more so in the neolithic age. If I am not mistaken, we possess hitherto only four or five authentic examples of the complete human skeleton, belonging undoubtedly to a very ancient epoch, the true palaeoUthic age. The first was discovered at Laugerie Basse (Dordogne) by MM. Massenat, Lalapde, and Car- tailhac, in a layer containing carved reindeer bones, an evidently undisturbed stratum, for it was covered with enormous blocks, detached from the rock which formed the vaulted roof of the shelter which served as a refuge to the troglodytes of the reindeer age, and which was pre- ferred by them to other homes. The authors of this dis- covery rightly judged from these facts that they beheld the victim of a landsUp, which occasionally took place at that remote epoch, as in our own day, and of which the traces still exist. The skeleton of Laugerie Basse was lying on its side, and appeared to have originally been in a crouching posture. The left hand lay under the left parietal bone, the right upon the neck. The elbows fell nearly to the knees ; one foot was close to the pelvis. The vertebral column had been ENTIEE SKELETONS. 83 crushed by the corner of a great block, and the pelvis was broken ; but all the bones retained their natural positions or were little removed from them. In a word, this skele- ton presented exactly the appearance of a startled man, raising his hands to his head, and making himself suddenly as small as possible. Near the skeleton, and scattered in pairs, lay shells {Oyprceapyi^um and Cyprom lurida) which had no doubt served to adorn some garment. Two pairs of these shells lay on the forehead, one pair nearly touching each humerus, four for the knees, and two at each foot. The skeleton of Laugerie Basse is then a well authen- ticated example of human remains contemporary with the reindeer. Unfortunately, the authors of this important discovery have given us no detailed account of character- istics of the skeleton in question, which is so much the more to be regretted that it would have been of great interest to compare its skull with those of Bruniquel, of Furfooz, of Cro-Magnon, and with all those of the reindeer age, and even of earlier epochs. Another entire skeleton, buried in the caves of the arehseolithic epoch, was found on March 26, 1872, by M. Eivi^re, in one of the bone caves of Mentone,' at a depth of about twenty-one feet, along with numerous flint and bone implements,^ marine and land shells, and bones of mammalia, among others of Ursus spelceus, HycBna spelcea, Felis antiqua, &c. This skeleton was lying on the left side, in the attitude of a man whom death had overtaken during sleep. A number of perforated shells of Nassa neritea, and a few stag's teeth, also perforated, were scattered here and there upon the skull, and it is probable that these teeth and shells were formerly part of some head ornament ; other shells of the same species, symmetrically ' In the cave of Cavillon, the fourth bone cave of the bamisse roussS (a patois word for red rocks). ' These instruments belong to three . different types, those of Mous- tier, of la Madelaine, and of polished stone. There is therefore reason to suppose that several epochs at once are represented in these caves. In spite of several fractures the skull had preserved its form : it was dolichocephalous. The vertebral column, the ribs, and the bones of the limbs were nearly intact, and lay in their natural positions. 84 THE ANTIQUITY OF THE HUMAN RACE. arranged, were probably also the ornaments of the dress. M. Eiviere at the end of his report calls attention to the fact that the skeleton in question ' offers no characteristics which in any way proves it to be akin to monkeys, and that the human skulls which it most nearly resembles are those found at Cro-Magnon ' (Perigord). Three other skeletons presenting the same characters as the above have since been found at Mentone. If entire skeletons are rare in the caves of the palaeo- lithic age, they are on the other hand fairly common in the burial caves of the neolithic period. As we shall have Fig. 21. Female skull of Cro-Magnok, wounded in the forehead. (After Louis Lartet.) occasion to speak of these caves where we treat of the burial grounds, we need only mention this fact in passing. When isolated human bones, more or less entire, are intermixed with the remains of extinct species, when it is certain that the stratum in which they are found has not been disturbed, we may assume with certainty that these bones are really contemporary with the deposit in which they are imbedded. But these cases of indisputable syn- chronism are rare (jawbones of Arcy, of la Naulette, &c.). Another criterion of the great age of human remains WOUNDED HUMAN BONES. 85 is furnished by the wounds made by stone weapons, of which some among them bear the marks or contain the fragments. Of this number is a human tibia found in the dolmen of Font Kial in Aveyron, which is pierced by a flint-headed arrow which had remained in the wound and had produced considerable exostosis. We may also cite as an example, a female skull, discovered several years ago by M. Louis Lartet in the cave of Cro-Magnon, and of which the frontal bone showed a wound in process of healing, which was probably produced by a flint weapon (fig. 21). The elder M. Lartet, in his remarkable work, ' Sur la coexistence de I'homme et des grands mammif^res fossiles,' speaks of a Danish dolichocephalous skull of the stone age perforated by a lance-headed piece of the antler of an elk. Beside this skull lay thirty or forty skeletons also of a dolichocephalous race, and near them the stone weapons which the conquerors had used to slay their enemies. Spring saw in the cave of Chauvaux, in Belgium, a human parietal bone in which the flint axe which had broken the victim's skull remained fixed. Nilsson, cited by Lubbock, says that in a tomb of the neolithic age attributed to Albus McGaldus, king of Scotland, a skele- ton of extraordinary size was found in 1807, of which one arm had been almost separated from the trimk by a blow from an axe of diorite, of which a fragment still remained in the bone. Lastly, M. Pruni^res discovered, in the caves of Baumes- Chaudes in Loz^re, still more convincing proofs.' These are human bones which still contain the flint heads of the arrows which wounded them. Often too these flint arrow- heads are encased in a newly formed bony tissue, a clear proof that they had pierced the bone of the living subject and that the wounds had subsequently healed. M. Pruni^res has observed, moreover, that these flint arrow heads were not like those made by the inhabitants of the caves, but resembled those of the inhabitants of the ' See the Bulletin de la SooiHl d'Anthropologie de Paris, p. 215, May 16, 1878. 5 86 THE ANTiaUITY OF THE HUMAJ* EACE. neighbouring dolmens, to whom therefore these wounds must be attributed. Undoubtedly one of the most curious discoveries which has been made of late years, is that of pierced or rather Fig. 22. TEEPAifNED skull taken from a dolmen, and presented by M. Peunieees to the Museum of the Institut Anthkopologique. (Half natural £ize.) A B, Median line of the stull, passing the root of the nose at A, the crown of the head at c, the lamhdoid suture at D, and the occiput at B ; E, bone of the left eyebrow ; P, bone of the right, fractured ; a 6, sickle-shap^ edge of the surgical trepanning jfractised in childhood on the upper edge of the left pariei^bone; dc, 6d, edges of the posthumous trepanning. The suture, instead of following the median line CD, has been drawn considerably to the left. TEEPANNED SKULLS. 87 trepanned human skulls, found by Dr. Pruni^res in the cave of Homme-mort in Lozere ' and in several dolmens in the same department. Discs of bone, equal in size to the holes in the skulls have been found, sometimes within them, sometimes separately, lying beside them or at some distance. Many of these are pierced by one or two holes, so as to allow them to be strung upon a cord. Their diameter varies from that of a shilling to that of a crown- piece (see fig. 22). Some of them, more or less elliptical in shape, measure seven inches in length and five in their greatest width. M. Broca has made an exhaustive study of the subject,'' which is, thanks to his labours, now very well known. The trepanning was effected sometimes on the living subject, sometimes after death. An incision in the form of a X was first made on the skin under the hair, then the bone was scraped with a flint knife, until sooner or later the disc or discs of bone were detached from the skull ; for sometimes two or three were taken from one indi- vidual even while living. It is a remarkable fact that the cases in which the operation, which is especially dangerous when we consider the poverty of the surgical apparatus of our ancestors of the stone age, proved fatal, are so rare that out of twenty skulls in the possession of Dr. Pruni^res, he has only observed one instance. AU the others present unmistakeable traces of a complete recovery. The motive of this operation has of course been sought, and the use of these discs found in the interior of the cranium or in the soil where the corpses had been buried. "We shall return to this subject in the chapter on Eeligion. We shall see that the practice of trepanning persisted throughout the neolithic period, and that the use of these discs is the earUest proof of a beUef in a future life. The instances of human bones in the caves which were ' Artificially perforated skulls have also been found in the burial caves of la Marne, of Sordes, in the neighbourhood of Pan, in the ancient tombs of the Canary Isles, in the dolmens of Algeria, and even in Mexico and Peru. ' See the Revue d' Amtlwopologie, t. ii. p. 18, 1873, and t. vi. pp. 1 an;! 193, 1877. 88 THE ANTIQUITY OF THE HUMAN KACE. undoubtedly contemporary with extinct species are rare ; we purposely repeat this fact, and the greatest circum- spection is required before pronouncing on this kind of synchronism. Nothing is easier than to make the greatest mistakes on this point ; the cautious M. Ed. Lartet him- self assumed that the human bones of Aurignac were contemporary with those of Ursus spelceus and of the mammoth which he had himself found in the true archaeo- lithic stratum of this cave, whereas, imbedded in a far more recent layer, overlying the former, they dated in reality from the neolithic age. VII. PBOOFS FTJENISHED BT THE COBTDITIOIT OP THE BOlfES, AND THEIB CHEMICAL COMPOSITIOIJ". When human bones are found buried in the same strata with those of extinct species, and when it is certain that the bed which contains them both is virgin and undis- turbed soil, we may logically conclude, as we have said, that these remains of men and animals date from the same epoch. The similarity of appearance, and especially the equal quantity of animal matter which they still contain, duly considering, of co.urse, the age and nature of the animal, give new weight to this conclusion. Now the quantity of ossein is easily deduced from that of the nitrogen discovered by chemical analysis. In this manner M. Delesse found that the proportion of nitrogen con- tained in the human bones found at Aurignac was very nearly the same as that in the bones of the bear, reindeer, and rhinoceros with which the remains of our own species were found associated in this burial cave. The numerous analyses of M. Scheurer-Kestner produced similar results, and led their author to believe with M. Delesse in the co-existence of man and the extinct species whose remains were under examination. The nature of the bones, that of the soil, its dryness or humidity, its permeability by air and water, the more or less ancient date of burial, the depth at which they lie, &c., have a considerable effect on the condition of the bones, so that those most recently buried are not always CHEMICAL COMPOSITION OF POSSIL BONES. 89 the best preserved. Hence M. Fremy has had no diffi- culty in proving that nothing is more variable ' than the quantity of organic matter contained in fossil bones; some of them no longer contain any at all, others have a proportion of 8, 10, and even 20 per cent. Some strata have such a preserving power that M. Gimbernat was able to make an edible jelly from some bones of Elephas primigenius, and M. Bibra made a strong paste from the bones of Ursus spelceus. Mr. A. Milne-Edwards has seen a tooth of the last-^amed fossil species, found in the diluvium of the-neighbourhood of Compi^gne, which still contained sufficient ossein to retain its shape, after its calcareous substance had been expelled by the action of hydrochloric acid. Lastly, some bones of the mastodon found at New York, in 1845, still contained 27 to 30 per cent, of ani- mal matter. With bones so well preserved it would then be possible to prepare an antediluvian broth, a real soup oi pre-adamite gelatine. Who knows if this strange notion may not one day be realised by the unceasing progress of chemistry, which every day displays wonders far more sur- prising and of greater interest.^ The impossibility of determining by analysis the precise age of any bone, ancient or recent, will be easily seen from the foregoing statements. On the other hand, if the bones under examination, belonging partly to the human race, partly to extinct species, occupy the same bed and contain the same proportion of nitrogenous matter, we may admit with some degree of certainty the synchro- nism of the analysed remains. In this way M. Scheurer- Kestner satisfied himself that the skull of Eguisheim, for example, was of the same date as the bones of the mam- moth and of the cave bear found along with it.' ' Marrel de Serres had long since observed that the chemical composition of the bones of the caves and that of the remains contained in the tertiary beds are sometimes absolutely identical. ' This strange idea, of which we have just spoken, was put in execu- tion by German naturalist s at the congress of Tubingen. ' They had th e pleasure,' M. Babinet tells us, ' of eating, not a beefsteak, but a soup of mammoth gelatine.' See Revue Soientijique, 1866. Conference by M. Babinet on the Glacial Period. ' Scheurer-Kestner, Reeherohes C7dmiqiies snr les Ossements trnuvea 90 THE ANTIQUITY OF THE HUMAN RACE. From all these facts we must conclude that if the chemical analysis of bones can, in certain cases, and by comparison, furnish useful data with respect to their rela- tive ages, it cannot tell us anything about their absolute age. Hence again it results that if the doubts recently put forward with regard to the human bones of Aurignac have a real foundation, that is, if these bones are much less ancient than those of the cave bear, mammoth, and rhinoceros, considered as contemporaneous by M. Ed. Lartet, we must also conclude that the analysis of these bones made by M. Delesse does not prove all that which he wished it to show. dans le Ichm cHEgvJiiTieim,. AnnaUs des Sciencei Natwrelleg, t. vii. p. 1 65, 1867 91 CHAPTER IV. THE PEAT MOSSES AND THE KITCHEN MIDDENS. I. THE DAWISH PEAT MOSSES. It is well known that in certain regions (chiefly at the bottom of gently sloping valleys), and under the influence of certain conditions, aquatic plants, the hypnum, the sphagnum, &c., herbaceous land plants, heaths, and even forest trees, heaped up in shallow waters, become inter- laced and partly decomposed, and produce a combustible of no great value. This combustible is peat. Denmark is especially rich in various kinds of peat beds, known in that country as engmose (meadow marshes), lyngmose (heath marshes), and skovmose (forest marshes). The last alone deserve a few moments' attention, since they show that very different vegetations succeeded each other at different epochs in the soil of Denmark. Professor Steenstrup, who has made a special study of the subject, tells us that a layer of peat, composed of perfectly recog- nisable aquatic plants [hypnum), is placed above the amor- phous, almost felt-like peat, which occupies the centre and bottom of the funnel-shaped basins in which it was formed. Stunted pines, heaped one over the other, still occupy the place in the marsh where they grew in the remote past. Then the sphagnum, takes the place of the hypnum, and the heath appears, along with whortle- berries, birches, hazels, and elders. Lastly, the Scotch fir,, which once grew along the borders of 'the moss, but which has long since disappeared from the land, appears in great abundance, and principally on the outer belt. These trees now lie overturned in such a way that their roots are turned towards the edge of the basin and their tops towards the 92 THE ANTIQUITY OF THE HUMAIJ RACE. centre; they are heaped upon each other and overlap with such regularity, that they present the appearance of piles of timber artificially arranged. By degrees they disappear and are replaced by the sessile-leaved oak (Qwercus robur sessilifolia of Smith), which in its turn gives place to the pedunculate leaved oak {Quercus pedunculata, Eberhard), almost the only one now existing in Denmark. Finally the beech appears {Fagus sylvestris), which at the present day grows so luxuriantly in this part of Scandinavia, that these forests are reckoned the finest in the world. What causes brought about these changes in the vegetation ? Judging from the shells of the peat mosses, whose species are identical with those actually existing in that region, the climate does not appear to have under- gone any great modifications of temperature. Hence Steenstrup has been led to beUeve that the succession of the fir, the sessile-leaved oak, and the beech is simply due to a gradual desiccation and improvement of the soil, the fir thriving in poor and marshy, while the beech grows only in dry and fertile districts. The series of layers of peat which we have just de- scribed extends to a depth of not less than 15 to 20 ft., and this argues the lapse of a great period of time between their origin and the moment at which their formation ceased. Ten to twelve thousand years perhaps, according to Steenstrup, went to the accumulation and transformation of these remains of a vegetation which has partly or wholly disappeared from the district. The traces of fire still to be seen upon some of the pine trunks, and the presence of carved flints in the layer of peat formed by the same substance, are facts brought forward by the famous professor of Copenhagen in support of his assertion, that man existed at the period when dense pine forests covered Denmark with their sombre but rich vegeta- tion. Other facts, not less convincing, corroborate the deductions of the learned Danish professor. He drew out, with his own hands, an iixe which had been violently driven into the trunk of a Scotch fir {Pinus sylvestris). Now EEMAINS FOUND IN PEAT MOSSES. 93 this tree is no longer, and has never been since historic times, indigenous to the Danish isles, and has not thriven when the attempt has been made to re-introduce it. It has also been proved by Steenstrup in a most in- genious and conclusive way that the Bos primigenius was contemporary with the ancient Danish forests. In a forest peat moss of the island of Moen, he discovered an entire skeleton of this primitive ox, buried, so to speak, in a shroud of the needles of the Scotch fir. Needles of the same trees, slightly crushed, and in small fragments, con- stituted a blackish mass, placed within the space occupied by the skeleton, which mass is nothing else than the perfectly recognisable excrements of the ruminant, which lived and browsed in the Danish forests together with the blackcock, which has long since disappeared from them. Two bones of the stag, found in the peat mosses of Jutland and Finland, where the Scotch fir is very abun- dant, have led the Danish savant to the same conclu- sion with regard to the animals to which these bones belonged. Steenstrup has further, concluded from the presence of flint arrow heads in these bones, and arrow heads which had during the life of the animal been covered by a new formation of bone, that man had pursued and wounded the stags, but had not been able to kill them. He was therefore contemporary with them, and conse- quently with the pine forests of Denmark. The stone age terminates with these forests. That of bronze saw the birth of the first oak of the peat mosses (^Quercus rohur sessiUfolia) ; for it is in a layer of this oak that the magnificent bronze shields which now adorn the Museum at Copenhagen were found. Lastly, the historic, or iron age, belongs essentially to the epoch of the beech. No human bones have as yet been found in the Danish peat mosses. ' Who will tell us,' exclaims Virchow, ' how long this calendar of trees, if I may be allowed the expression, has been established ; how many centuries have elapsed since the pine forests ceased to spread their dark verdure over the surface of these marshes ? We do not know, but we know that with the 94 THE ANTIQUITY OF THE HUMAN EACE. disappearance of the pines the blackcock also was forced to quit Denmark, for it fed upon their young shoots in the spring. If doubt were still entertained as to the coincidence of the age of the pines and the stone age, the discovery of a flint implement in the peat at the foot of such a pine would be a conclusive fact.' ' We must not leave the peat mosses of Denmark with- out mentioning the numerous necklace beads and ear- rings of amber which were dug out of those of Jutland. One of them furnished, it is said, more than 4,000 such beads, enclosed in a wooden casket, which has suggested the idea that this was the stock in trade of some jeweller of the neolithic age. The Irish bogs have furnished palaeontology with remains of the Megaceros hibernicus in a perfect state of preservation, and several museums, especially that of Toulouse, possess a complete and well mounted skeleton of this animal, which was the contemporary of the mam- moth and the cave bear. Among the French peat mosses we may mention in particular those situated near the mouth of the Somme, from some of which M. Boucher de Perthes extracted rough-hewn axes, and bones of the Irish elk, and from others a quantity of bone and flint implements (stag's horn axes with wooden handles, flint knives, bone fish- hooks, necklaces, &c.), which undoubtedly_belong to the age of polished stone. The proofs of the great antiquity of man furnished by the peat mosses of the Somme valley are less striking than those of the Danish bogs, but they have their value. Boucher de Perthes tells us moreover that in several districts in the neighbourhood of Abbeville, where an immense forest formerly stood, alders and oaks twelve feet in diameter may be laid bare by digging through the layer of peat formed subsequently above them. Some of these are still standing, others are uprooted and lie with their heads towards the source of the river. The renowned antiquary surmises that these ■ Tirchow, Zes tumuli et les Jialitations lacuHres (Revue des court scientifiques, i' ann^e, 1866, p. 7). PEAT MOSSES NEAB PAEIS. 95 trees were overthrown by a gust of wind from the sea, or by a tidal wave of more than ordinary force, the same perhaps which swept away the isthmus which formerly united Grreat Britain and the Continent.' Whatever we may think of this last hypothesis, it is certainly true that these trees have fallen on the very spot where they grew, and that since they fell, great beds of peat not less than 5 or 6 yards in. depth, have been formed above them. This peat is covered by a bed of waterworn pebbles to a dept|i of 12 or 16 inches. Now in the lowest layer, half-polished axes, along with bones of oxen, boars, roebucks, and stags, have been found. The conclusion is easy to draw. The peat mosses of the neighbourhood of Paris belong for the most part to the same epoch. Some few among them seem, however, to date from the reindeer age. In the latter, which are formed of a fibrous peat, MM. Eoujou and Julien found hearthstones, flint imple- ments, and even pottery, which they believe to be of later date than the period of the mammoth, but more ancient than the age of polished stone. However, we must not forget that, by reason of their greater per- meability, especially when they are in a soft condition, the peat mosses may have received and covered bones and products of human industry which it would be a mistake to regard in every case as contemporaries, merely from the fact that they occupy the same level. Many mistakes have been committed in this respect, and it is impossible to be too cautious in pronouncing upon the real age of any object found in the peat. But when Boucher de Perthes and Steenstrup have searched these bogs with the attention and care for which they are so justly celebrated, the results have great value, and give the most convincing' evidence in favour of the thesis which we are endeavouring to establish ; namely, the great antiquity of the human race. ' Boucher de Perthes, De Vhonime Antidilwcien, p. 18. 96 THE ANTiaUITY OP THE HUMAN EACE. II. THE PEAT MOSSES OE STWITZEKLABTD. LEAE- MAEKED COAL OF MOBCH"VrEIIiI,, OE 'WETZIKOM', OE UTZNACH, AND OE DUKUTEIT. We cannot leave unnoticed tlie peat mosses containing leaf-impressed coal wliicli occur in various parts of Switzer- land, notably at Wetzikon in the east of Switzerland, at Morchweill near Saint Gall, at TJtznach, and at Diirnten in Oberberg. These masses of carbon, of which the mean thickness is a yard, and which in certain districts attain to a depth of 4J yards, are traversed by veins of clay, and they rest upon a bed subsequently formed of dirty white or yellowish clay. The shells of freshwater molluscs still existing in the country have been found imbedded in this layer {Anodonta, valvata depressa, obtusa, &c.). The trunks of pines are also abundant, overthrown in every direction, with their roots, their bark, and fibrous tissue with its concentric layers, show- ing that some of them were more than a century old, in a perfect state of preservation. These trees are much flattened, and encased in a blackish or brownish substance produced by the decaying of herbaceous plants. The trees are rarer in the upper layers, which are principally com- posed of compressed masses of carbon interlaced with roots and reeds. Twenty-four species of plants, of which eight are trees or shrubs, have been discovered by Heer in these peat- bogs of the ancient world. We give the list of them : — Common fir (^Pinus abies). Scotoli fir QPinus syhiestris). Mountain pine {Finns montamd). Larch {Pvrvui Im-ix). Tew (taxus hacoata). Birch (^Betula alba). Oak {Querous robv/r). Maple (^Acer pseudoplatan'us). Hazel (^CoryVus avellana). Herbaceous Plants Marsh trefoil (Jlenyanthes trifo- Uata). Common reed (Phragmites eom- mtmis). Raspberry (Puius idism). Perforated myrtle ( Vaociniwm vitis idced). Lake scirpns (^Sovrpvs laovstrW). Several species of sphagnwm. Mosses, among others Mypnum di- Imiii, found at Thonou by M. Morlot among other glacial re- mains. ANIMAL EEMAINS IN PEAT MOSSES. 97 Only one plant of this epoch seems to have disappeared, namely, a species of nuphar, of which M. Gaspary has made a separate genus, under the name of holopleura. Animals which occuk in the Lbaf-maeked Coal. Hammolia Insects Elephas antiquus ) JRMnooeros etnisous [ Extinct Bob prim^enmt \ species Ur»ui 8pel(sus } Molluscs Anodonta Vahata depressa Valvata oMusa Iridium oiliquv/m , Donaoia discolor 1 Existing D. sencea ] species Existirg species At Diirnten and at Utznach we find trunks of firs and birches a foot in diameter, with well preserved cones. At Morchweill an acorn still retaining its cup was found, and two varieties of hazel nut, of which one resembled the modern kind. Lastly, among the animals whose remains have been found in these beds, the most ancient species of the diluvium of the valleys occur, such as Mephas an- tiquus, Rhinoceros etruscus, Bos primigenius, and Ursus spelcBus, contemporaries of the man of the caves. We find with these species, long since extinct, the elytra of insects belonging to species identical with those which still exist on the shores of the Swiss lakes {Donacia dis- color and D. sericed). According to Oswald Heer, one of these peat mosses, that of Morchweill, and perhaps that of Wetzikon, is placed between two beds containing striated erratic blocks, which seems to show that they were formed in the interval which separates the two glacial periods admitted by some geologists and rejected by others. Whichever opinion is adopted, it is at any rate true and incontestible that these masses of leaf-impressed carbon are covered by a glacial deposit. They belong therefore to an extremely remote epoch, and are at least contemporary with the ancient Ehine alluvium, above which the lehm or loess was deposited at the epoch of the great extension of the glaciers of the 98 THE ANTIQUITY OF THE HUMAN EACE. Swiss Alps and of the Vosges, now extinct. JN'ow, it is in this loess, at Eguisheim in Alsace, and at Lahr in Baden, that MM. Faudel and Ami Bone found human bones of which we shall soon have occasion to speak, a conclusive proof that man existed during the glacial period, that is, at an epoch when the woolly elephant, the rhinoceros, and the reindeer existed in our land. III. THE KITCHEM- MIDDENS OB SHELL MOUNDS. The remains of prehistoric cookery, which are found in considerable heaps on the seashore, are known as kitchen middens to Scandinavian archaeologists. These heaps are principally composed of oyster shells (Ostrea edulis), of mussel shells {Mytilus edulis), of limpets (Garditi'm edulp), and of periwinkles (Littorina littorea). Bones of mammalia, of birds and fishes, are found together with these molluscs, and other similar refuse. The principal mammalia are the st;ag {Gervus elephas), the wild goat (C. capreolus), and the wild boar [Sus scrofa). The reindeer is rarely found; but according to Steenstrup, it does occur in the kitchen middens, though its presence was long disputed. We must add to these about fifteen other species which are far less com- mon than those already mentioned. These are the brown bear, the dog, the wolf, the fox, the cat, the lynx, the marten, the otter, the seal, the walrus, the beaver, the water rat, and the mouse. Birds are represented by the wild swan {Gygnus musicus'), the blackcock (Tetrao urogallus), and the great penguin {Alca impennis), now nearly extinct. The fishes which occur most frequently are the herring (Ghipea harengus), the cod {Gadus cellarius), the dab {Pleuronectes liTnanda), and the eel {^Murcena anguilla). It is worthy of remark that none of these animals belong to an extinct fauna. As for the kitchen debris themselves, they form heaps from 1 to 3 yards in height, by 100 to 350 yards long and 50 to 70 wide, and there are more than fifty of them, all situated a short distance from the shores of the Baltic, and seldom raised more than three yards above the level KITCHEN MIDDENS. 99 of the sea. Among the refuse still remain the coal cinders of ancient hearths, rude pottery, numerous flint imple- ments, and some few traces of stag's horn. But there is no vestige of metals, nor of cereals, nor, consequently, of agriculture. The dog was, however, already domesticated, as Professor Steenstrup has proved in a most ingenious way. He had observed that nearly all the long bones of mammalia and birds taken from the refuse heaps were reduced to their shaft or diaphysis. The heads or extre- mities had disappeared or were very irregularly broken. Moreover, Steenstrup remarked that the long bones were from twenty to twenty-five times more numerous than the short bones. Struck by these two facts, he shut up several dogs and gave them bones to gnaw. They devoured the short bones, gnawed the heads of the long bones, and left the shafts in precisely the same condition as those of Copenhagen. Hence the learned professor concluded that the Danish aborigines were in possession of a do- mestic animal, the dog, which accompanied them every- where, shared their repasts, and served itself as food to these still barbarous tribes. As for the bones of the other mammalia, they bear evident traces of having been purposely fractured by man, who broke them in order to extract the marrow which they contained for food. As zoological museums of ancient times, and as links between the past and the present, the kitchen middens furnish Danish men of science with valuable data respecting the fauna of the coimtry which their labours have rendered famous. Thus at the time when the use of metals was still unknown to their ancestors but when they were already in possession of better flint tools than those found in the diluvium of Abbeville and in certain caves of prehistoric times, the mammoth, the woolly .rhinoceros, the musk ox, &c., no longer existed in Denmark. The oyster, at that time very common on the shores of the Baltic, has in several districts completely disappeared, and in the places where it is still found it is comparatively small and stunted. This is. also the case 100 THE ANTiaUlTY OF THE HUMAN EACE. with the other edible molluscs before mentioned. This result is attributed to a perceptible decrease of saltness which has taken place in the waters of the Baltic, owing Figs. 23, 24. Lamce heads from .the kitchen middens. vAfter Lubbodk.) to the great quantity of fresh water poured into this inland sea by the rivers of the present day, and to the obstruction of the channel of communication between the North Sea and the Kattegat caused by the formation' of the land added to Jutland. REMAINS FOUND IN KITCHEN MIDDENS. 101 The presence of the bones of the blackcock in these refuse heaps proves that this bird, now extinct in Denmark, found the resinous buds which form its favourite food in the pine forests which grew near the coast. The great penguin (^Alca, im'pennis, Linnaeus), now, according to some authorities, confined to the most inaccessible rocks of Iceland and Greenland, or, as others say, entirely extinct, was then common upon these shores. Its oily flesh was not despised ; its fat was used at once for food, fuel, and light.' The refuse heaps contain no remains of the do- mestic fowl. As a sporting, and especially as a fishing people, the ancient Danes have left in their kitchen middens a quan- tity of the remains of eels, cod, flounders, and herrings ; all deep sea fish, in search of which they were obliged to venture far out to sea in boats formed of the trunk of a tree hollowed by flints and fire : a terrible struggle for existence, in which many human victims fell, but in which dangerous school many bold spirits were formed. Human remains have hitherto been sought in vain in the kitchen middens ; but as we have already said, a number of flint implements have been found there, some of which are rudely fashioned and resemble those of the diluvium (figs. 23 and 24) ; others, less common than the former, are of better workmanship and are even polished by the grindstone, for example some axes of a peculiar character, flat on one side and more or less convex on the other, and of which the object is confessedly unknown to M. Steenstrup (figs. 25, 26, and 27). Certain savage tribes of modern times make similar axes (figs. 28, 29, 30), According to calculations of which we do not guarantee the accuracy, the kitchen middens of Denmark are about 7,000 years old, and are contemporary with the earliest lake dwellings. Steenstrup believes them to be of the same age as the dolmens, and believes that the people ' By placing a wick of any kind, moss for instance, in the stomach of a penguin, an economical lamp was obtained. In the middle ages the fat of this bird was used as fuel in the place of wood on the coasts of Newfoundland. 102 THE ANTIQUITY OF THE HUMAN EACE. Fia. 25. Convex taoe. Axe of the kitches jiidden's (after Lubbock). Fio. 26. Side Tiew. Pig. 27. Ilat &oe. 'lis ^ MoDEKN New Zealand axe lit the British Museom. (After Lubbock ' Prehistoric Man.') Fio. 28. ConveK face. Fio. 29. Side view. FiQ. 30. Flat face. CARVED BONES AND HOEN. 103 ■who raised these great stone monuments, and those who have left the refuse of their meals in the kitchen middens, are one and the same. Worsae, de Quatrefages, and Desor do not share this opinion. According to the famous Danish archaeologist, the refuse heaps represent in the north the beginning of the age of splintered stone, while the dolmens belong to the end of it. M. de Quatrefages, again grounding his belief upon the fact that the remains of the industry of the people who formed the shell mounds are never found wj.th the remains of Elephas primigenius, nor even with those of the reindeer (although, as we have seen, Stoenstrup affirms that the latter do occur in the refuse heaps), concludes that the construction of the kitchen middens is of a much later date than the race of Aurignac and of Moulin- Quignon ; he adds that, ' between the stone age of our earliest ancestors and that of the primitive Danes a whole, geological period intervenes.' M, Desor, for his part also, denies the identity of the people of the kitchen middens with that of the dolmens, for, independently of the numerous domestic animals to be met with in the latter, objects in bronze and even in iron occur also, which are never found in the kitchen middens. It is therefore more than doubtful whether these two kinds of monuments date from the same epoch ; we may even go so far as to say that the problem is now solved ; the dolmens, and especially those in which iron and bronze occur, being proved to be far more recent than the kitchen middens of Denmark. Blackish ashes have been found in the latter, which chemical analysis has shown to contain a considerable pro- portion of manganese ; these ashes were produced by the combustion of a species of sea-weed {Zostera marina) sprinkled with sea-water. This double process resulted in a sort of saline efflorescence (the sal nigrum of Pliny). Bones and antlers of the stag carved into fish-hooks, chisels, axe blades, &c,, have been found among the debris. A sort of bone comb was discovered at Meilgaard, destined probably to split the tendons then used as thread and cordage. The remains of Danish cooking seem to show 104 THE ANTiaUITY OF THE HUMAN EACE. that the tribes who formed one layer after another in such a way that they bear a certain resemblance to geological strata, Hved under the shelter of tents, and practised hunting and fishing, eating their spoils on the spot. Eefuse heaps of still earlier date than those of Den- mark have been observed in Suabia at Schiissenried. Others occur in certain caves of France, Belgium, in the Orkney Isles, in Scotland, England, &c. We may mention among others the cave at Brixham, where, associated with fragments of rude pottery and bones of extinct species, heaps of oyster shells and other saltwater molluscs occur, as well as fishbones of the genus scarus. Cook observed debris of a similar character at Cape Leveque, in Australia. Lastly, Darwin and Lyell men- tion others in Guinea, and on the coasts of New Finland. They have even been found in America ; in the States of Maine, Florida, Massachusetts, &c. Those of America are of two kinds, some containing marine shells in abundance, the others, situated in the interior of the continent, espe- cially on the banks of the Mississippi and the St. John rivers, contain only freshwater molluscs (unio, paludina, aTnpullaria). In all of them occur axes, arrow heads and flint knives simply splintered, rude pottery, but never metal. The fauna excavated from them differs in no respect from that of the present day. Everything in these refuse heaps indicates a civilisation similar to that of the people who formed the Danish shell mounds, but not perhaps of such remote antiquity. 105 CHAPTEE V. TEE LAKE DWELLINGS AND THE NUBAGBL I. THE IiAEi: DWELLIiras OF S'WITZEELAITD. It was during the winter of 1853-54, at an epoch when the waters of the lake of Zurich had fallen to the lowest level they are ever known to have attained, that Keller observed near Obermeilen the first piles, which led to so many important discoveries and such remarkable strides in the science of archaeology. Anyone may have observed in the Paris Exhibition of 1867, in the galleries devoted to Natural Science, those curious specimens which displayed before our eyes the dawning arts, industry, agricultural labours, and domestic life of the first inhabitants of Helvetia. If we read the successive reports communicated by Keller to the Antiquarian Society of Zurich; Troyon's book on the lake dwellings, which Carl Vogt styles some- what severely an historical romance, a •pious fancy ; lastly, the work on the lake dwellings of Neufchatel, published by M. Desor, in 1865 ; if we add to these works the general views of Morlot on archaeology, several critical articles of Pictet on fossil man, independently of what he has said in his great treatise on palaeontology ; the ' Crania Helve- tica ' of His, the studies of Eiitimeyer on the fossil fauna of Switzerland, the ' Crania Grermanise Meridionalis Ori- entalis ' of Ecker, the ' Vorlesungen iiber den Menschen, seine Stellung in der Schopfung und in der Greschichte der Erde,' by Carl Vogt, the ' Pfahlbaualterthiimer von Moosseedorf,' by Jahn and Uhlmann, &c., we shaU be convinced that love of science, allied to the noblest patriotism, could alone have brought to light so many 106 THE ANTiaUITY OF THE HUMAN RACE. interesting discoveries in so short a time and in so limited a space of ground. The following details are taken from these original sources and from personal recollection. It has been justly remarked that the lake dwellings of Switzerland are at the same time monuments of prehistoric architecture, a zoological museum, and a gallery of anthro- pology. Framework and piles, remains of wild and domes- tic animals, various forms of human skulls, implements of Fig. 31. Ancient Swiss lake dwellings, in part restored by com-' PAKISON WITH THE LAKE HUTS OF MODERN SAVAGES IN Nkw GuINEA. every description in bone, flint, bronze, and iron, pottery of more or less artistic workmanship, objects of art and ornament, woven stuffs, grinding stones, millstones for crushing, grains, bread, fruits, ashes, coal, &c., all these are found therein, or at least were found there in a state of confusion, which the science of antiquaries and palaeonto- logists has reduced to the most perfect order (fig. 31). Long known to the fishermen, who often entangled their nets in them, the piles of the Swiss lakes only at- CONSTRUCTION OF LAKE DWELLINGS. 107 tracted the attention of scientific men about 1853. Keller was one of the first to understand, their importance, and the reports whch from that time (1854) he continually laid before the Antiquarian Society of Zurich bear witness to the zeal, conscientiousness, and power of observation which he has displayed in the production of a work worthy of his country and of himself. By the help of the ruins which remain beneath the waters, let us endeavour to reconstruct in imagination these ancient dijellings, which a well-known savant, for once mistaken, asserted to have been built and inhabited by beavers. Imagine a number of piles,' fifteen to thirty feet long, with a diameter of three to nine inches, standing about four to six feet above the surface of the water when it is still. The distance between these piles varies ; some of them are arranged at right angles to the shore, others are parallel to it, and form altogether a rectangle or a circle. Usually fixed in the mud of the lake above the surface of which they are raised, they are sometimes supported (when the nature of the soil does not allow them to be imbedded in it) by heaps of stones, or Stemhergen, arranged round their base. Suppose these piles to be joined by transverse beams, held in their places by wooden pins. It then only remains to establish a kind of platform des- tined to support the hut and constructed of thick planks or of split trunks of trees roughly squared, and bound together by strong cords, wooden pins, or even by cross pieces of wood and by dovetailing. Finally, suppose that oval, circular, or rectangular huts are built upon this plat^ form, ten, fifteen, or even twenty-seven feet in diameter, of which the walls are formed of perpendicular posts, bound together by wattled branches lined with a cement of clay. Each hut is covered by a roof of bark, thatch, cane, reed, fern, or moss ; a door is left for the entrance, and a trapdoor within communicates with the lake. The trunk of a tree serves for seat and table, a heap of moss ' More than 40,000 were counted at Wangen, and about 100,000 at Eobenhausen. 108 THE ANTiaUITY OF THE HUMAN RACE. for a bed. Lastly, suppose each hut surrounded by a ring of piles, of which the upper end touches the surface of the water, to prevent the approach of hostile canoes, and united to the shore by a drawbridge, and a sufficiently exact idea will be obtained of the lake dwellings which in prehistoric times existed in Switzerland and elsewhere. The number of these habitations at present known in this country exceeds 200. The lake of Neufchatel alone has furnished forty. Each village was composed on the aver- age of about 300 huts.' It is no easy task to decide the precise motive for the construction of these lake dwellings. It is scarcely likely, us some authors have maintained, that they were simply huts, used temporarily for fishing, or magazines for food and other stores, if we take into consideration the im- mense labour it must have cost to build them. Moreover, it is impossible by this hypothesis to account for the number and diversity of the objects found among the piles if we deny that these places were lake villages or cities, inhabited by a population already so dense that certain districts contained from twelve to fourteen hundred souls. Again it has been said, but there are absolutely no grounds for the assertion, tha,t these houses on piles were places of temporary meeting, and even temples consecrated to the worship of the waters. Everything seems to show that the oldest lake dwellings of Switzerland do not go bsick beyond the neolithic age, and that they ceased to exist quite at the beginning of the iron age, that is, shortly after the Eoman invasion. The huts of Moosseedorf, Wangen, Eobenhausen, Meilen, Concise, Saint Aubain, &c., belong to the age of polished stone. None of the lake cities of the bronze age which have been hitherto discovered are situated in the east of Switzerland. To this age belong those of Greneva, Bienne, Sempach, Morat, CortaiUod, Auvernier, Neufchatel. Those At Wangen, near Lucerne, and in the lakes of Zurich, of Pfeffikon, and of Constance, floors or platforms placed one above the other were remarked, bearing circular huts with a conical roof thatched with straw and bark. These platforms, though much damaged, still measured forty-two feet in length by fifty in width. DATE OF LAKE DWELLINGS. lO'J of BienDe and Neufchatel witnessed the earliest days of the iron age and come very near to historic times. At la T^ne a Eoman coin bearing the efiSgy of Claudius was discovered, which would seem to prove that this settle- ment existed as late as the middle of the first century of our era. Moreover, a vase bearing a Latin inscription was discovered in the lake of Bourget, and some Eoman swords at Bienne. Some of these settlements contain remains belonging to two or three di^erent ages. For instance the ages of stone and bronze are represented at Estavayer, and those of stone, bronze, and iron at Neufchatel and Nidau, In the east of Switzerland the lake cities disappear with the age of stone ; in the west they last until the iron age. Some few even seem to have lasted to the beginnings of history, but to fix the precise date of their first appearance seems to be too bold an attempt. Certain authors, however, assign an age of 5,000, and even of 7,000 years to the oldest lake cities, whose construction would thus be anterior to that of Nineveh and Babylon. Troyon makes them date from 2,000 years before our era, that is, eight to ten centuries before the Trojan war, and M. Gervais himself adopts this calculation, which probably falls considerably short of the truth. Finally M. Eiitimeyer believes that the lake cities form in Switzerland the earliest stage in the history of the human race, a conclusion which is inadmissible since the discovery at Verrier,' at the foot of Mont Sal^ve, of human constructions of the reindeer age," which M. Ed. Lartet, an authority on such questions, ' The hill of Verrier, at the foot of Mont Salfeve, near Geneva, was formed by a landslip of the almost vertical strata of this mountain after the glacial epoch. The cavities left between the great blocks of which it is formed afterwards served as shelter to man. But the presence of carved reindeer bones in this place, and especially those of Thayngen, and the total absence, or at least the extreme rarity of such remains in the lake cities, incoutestably prove that the arrival of man in Switzerland is anterior to the lake dwellings. ' Reindeer bones, carved or otherwise, had, before these discoveries, already been observed in different parts of Switzerland, notably in the neighbourhood of Geneva, on the lake at Meilen, and at Windisch on the banks of the Keuss. All these bones were found in the alluvium of 6 110 THE ANTIQUITY OF THE HUMAU EACE. believes, judging from the workmanship, to be contem- porary with several settlements of Perigord of the so- called second epoch (reindeer age). The recent discovery of the cave of Thayngen, near Schafif hausen, confirms the theory of the learned palaeontologist. The inhabitants of the lake dwellings were therefore preceded in Switzerland by the dwellers in the caves, who date from the archseo- lithic epoch, and perhaps even they are not the earliest representatives of the human race in that country. It is generally admitted that the lake cities were more than once, by accident or design, destroyed by fire. The ruins found at the bottom of the lakes are a clear proof of this fact. A terrible conflagration seems to have marked the limit of each historical period. The confused and vague ideas which are all that we hitherto possess, will not allow us to give a definite reply to the question as to who these strange people were that built and inhabited these lake cities. Here, as in many other cases, there is an immense field for conjecture, and adventurous minds may give the rein to their im- agination. If we consult the archasologists of the north — M. Worsae, for instance — ^they tell us that the first inhabi- tants of the lake cities were aborigines of the west and north of Europe, of Keltic origin. . Their race endured as long as the lake dwellings, and perfected itself in arts and manufactures on the spot they inhabited. Keller, Dessor, and Virchow share this opinion. The almost complete identity of plan in the lake buildings of different epochs ; the great resemblance of certain objects in common use, made of stone, bronze, iron, and clay ; the similarity of the way in which fruits and other provisions of various kinds were preserved ; all this seems to refute the opinion held by M. Troyon and others, that peoples of different races and degrees of civilisation successively invaded and occu- pied the lake dwellings, the conqueror imposing his customs, industry, and way of life upon the conquered. the terraces which succeeded the glacial epoch, and at a height of con- siderably more than twenty-five or thirty yards above the actual level of the rivers and lakes of Switzerland. IMPLEMENTS IN SWISS LAKES. Ill From the fact that certain practised in Switzerland during the epoch of polished stone somewhat resembled those which the ancient Egyptians had adopted about iifty cen- turies before the Etruscan pe- riod, Carl Vogt concludes that the bidlders of the lake cities came from the laanks of the Nile long before the first Aryan migrations, and before the use of metals was known in Egypt. Unfortunately the data upon which so original an opinion is based do not appear to us suf- ficient to place it beyond dis- pute. IL IMPLEMEITTS OP STONE AGE I-OUBTD IN THE S-WISS IiAKES. The objects found in the Swiss lakes, under the peat, and among the ruins of the lake dwellings of the stone age, , are, as was to be expected, very similar to those found in the caves ofthe neolithic age. Buta harvest richer in many respects is gathered from the lake dwell- ings, since, independently of the weapons and utensils of every kind in stone, bone, and clay, the remains of a fauna and flora almost completely similar to our modern fauna and flora have been discovered in them. The stone axes, hammers, and agricultural processes Fig. 32. Axe, with hoen socket and wooden handle, found AT RoBENHAUSEN. (After Lub- book.) chisels are always 112 THE ANTIQUITY OF THE HUMAN RACE. highly polished, and usually fixed in a handle carved from the antler of a stag (fig. 32). Stones for polishing pur- poses, grindstones, stones for crushing corn, and stone hearths, are not rare in the lake cities. Paring knives, or polishers, of which some are a species of jade highly polished, are usually fixed in a stag's-horn handle. Lance and arrow heads and knives of flint are not uncommon, and, as usual, represent the types universally adopted. The same holds good of the weapons. The flint saw (fig. 33), usually only two or three inches long, is fixed in the groove of a wooden blade and is held firmly in its place by a dark-coloured cement of which the composition is un- FiG. 33. Flint SAW. (After Lubbock, ^nown. Utensils and tools ' Prehistoric Man.') of bone and hom have also been found, such as knives, scissors, axes, hammers, arrows, harpoons, bodkins, fish- hooks, straight and curved needles, pierced by one or two holes, and sometimes even grooved to prevent the thread from interfering with the firee play of the implement. Some needles are sharpened at both ends, and the eye is then in the middle. The bone hairpins present the closest resemblance to the metal ones of modern days. The innate taste for ornament shows itself in the rings and bracelets of bone or stone, in the necklace beads made of Baltic amber, of stags' antlers sawn into fragments more or less small, and even of nuts pierced through and through. Horn drinking cups of varied forms, and naturally of small size, have been found at Concise and Moosseedorf. One of these, hollowed from a stag's antler, was furnished with a wooden bottom attached by means of three pins, of which the holes are to be seen near the lower edge. A quantity of fragments of rude pottery, like that of the caves of the neolithic age, sometimes blackened by plumbago, not thrown on the wheel, and but very slightly ornamented, have been taken from a number of these lake settlements (fig. 34). Some vases are intact, but rather small, with flat and rounded bottoms, while in the PRAGMENTS OF POTTEEY. 113 succeeding age vases of a similar nature ended in a conical point and were supported on stands or rings of clay. Fig. 34. Feagmknt of pottery found in the lake of Zueich. (After Lubbock.) Several of those found at Concise bear two lumps or knobs pierced with a hole to allow of their being sus- pended by a cord. Fig. 35. Pieof, of woven stuff found at Eobenhausen. (After Lubbock.) The weaver's shuttle, the spindle, the weights destined to aid in the rotatory movement of the spinning wheel, the loom itself, with its spools for stretching the thread. 114 THE ANTIQUITY OF THE HUMAN EACE. already existed. Cords made from the bark fibre of cer- tain trees, thread made from flax (not hemp), woven and plaited stuffs, had been discovered at the bottom of the lakes of Constance and PfefiSkon, at "Wangen and Roben- hausen (fig. 35). Twigs of willow, interlaced with straw, were even found at Wangen, probably the remains of a basket even more ancient than that used by queen Aah- Hotep (see p. 33). The preserving property of peat explains, in part at least, the preservation for such a length of time of all these tissues, as well as that of the half-carbonised cereals, seeds, and fruits, of which Heer discovered the existence in the lakes of Constance and Pfeffikon (see p. 120). Lastly, in one of the oldest settlements of the lake of Bienne, that of Locras (age of polished stone), M. Grass discovered wooden bowls and platters, and even little birch-bark boxes, furnished with lids and made to open and shut at will by means of a string hinge. Ob- jects made of stag's horn or bone are not uncommon at Locras. Several of great historic interest have been discovered in that place : among others a comb pierced with a hole by which it might be suspended, maces, or battle axes, which still retain a part of their handle, and a sort of wand of office. The bone objects include fish- hooks, daggers, and a sort of comb for carding flax, formed of three ribs split lengthways, pointed at one end, and joined together by fine string. Lastly, a flat rectangular piece of bone pierced with a hole at one end, was probably used for making nets. Few tissues occur at Locras ; but, on the other hand, several balls of thread, string, and cord have been found there. At Grerafin (lake of Bienne, stone age), a spoon was found made of yew wood beautifully wrought, and at 'V\''eyeregg, Austria (age of polished stone), a bone fork. The lake dwellings of the stone age have also furnished a great number of bones of animals, of which a list will be found on p. 119, There are no entire skele- tons, and the bones are generally split lengthways, in order to extract the marrow, a very ancient and per- LAKE CITIES IS OTHEE LANDS. 115 sistent custom, since it dates from the earliest stone age, from the epoch even of the cave bear and mam- moth, and it is still practised by the Lapps and other peoples of the Finn race who inhabit the north of Europe. To their praise be it spoken, no trace of cannibalism has been observed among the inhabitants of the Swiss lake dwellings. Switzerland is not the only country in which lake cities occur. Italy, Austria, Hungary, Pomerania, France, and Savoy possess huts built on piles after the manner of those of Switzerland, but they are generally smaller, and nearly all belong to the age of polished stone. Occasionally, how- ever, metal objects occur in them, probably of foreign origin, which were imbedded in the mud of the lake at a date subsequent to the construction of the huts. Paolo Lioy has described those of Lake Fimon (Italy), and he maintains that they belong to the reindeer age.' Those of Savoy are far less ancient, since some of them, that of Grresine for instance on the lake of Bourget, are, accord- ing to M. Rabut, not more than 3,000 years old. Those of Lake Paladru in Is^re are yet more recent ; for M. Chantry, who explored them with so much care, found in them a quantity of iron objects and even a Carlovingian coin. However, history makes no mention of this lake city. The local tradition that the ruins of an ancient city which had been destroyed by divine vengeance existed at the bottom of the lake, led to the discovery 6f the ruins of a lake village occupying in point of fact the spot indicated. A recent author ^ has even asserted that Toulouse was once a lake city ; but M. de Mortillet has refuted this opinion in a manner which appears to us conclusive. It is worthy of remark, however, that according to Strabo, Cicero, and Justinian, a sacred lake existed formerly in the neighbourhood of Toulouse where the neighbouring tribes offered gold and silver to their gods. • See Paolo Lioy, Ze abitazioni Icuiustre delta eta della jAetra nel Vicentino. Yicenza, 1866. ' See Revue wroheologigue du Midi de la France, 1866-1867, pp. 170 and 196. 116 THE ANTiaUITY OF THE HUMAN EACE. HI. THE INHABITANTS OF THB LAKE DASrELLINGS. THE SWISS EPOCH OP THE LAKE II"WrBLLIlirGS. MANNEBS AND CUSTOMS OF THEIB INHABITANTS. At the epoch of the lake cities, immense forest's, already peopled by our modern fauna, covered the slopes of the Swiss mountains, and descended sometimes to the very shores of the lakes. Here the urus, the aurochs, the red deer, the roebuck, the wild goat, the wild boar, the wolf, the fox, roamed at liberty. The otter disported himself in the clear waters the beaver constructed its dams, the brown bear crouched in his cave, while the IdmTner-geyer (lamb-slayer vidture), watching his prey, hovered in the £dr. The dog, already the companion and help-mate of man, hunted with him the denizens of the forests whose flesh served as food for both of them. Besides the dog, the dwellers on the lake had brought under their sway the greater number of the animals which are now domesti- cated : the ox, the goat, the sheep, the pig, and perhaps even the horse — an immense step in advance, which even rendered agricultiu-al labour possible. In effect they cul- tivated most of our cereals. The spoils of hunting, and of fishing with net and line, milk, and fruits of all kinds, also served for nourishment. To judge from certain of their works of art and orna- ments (coral necklaces, amber beads, jade, &c.), it would appear that they carried on a commerce by barter with the peoples of the Mediterranean, of the Baltic, of the Scilly Isles, perhaps even of the 'East. But these asser- tions are possibly rash, and are still the subject of serious doubts. They were clothed in skins, sewn or unsewn, and in hempen, or linen stuffs skilfully woven. Woollen stuffs were unknown to them ; at least no trace of them has hitherto been found. The arts of making baskets,' ropes, and lace, had already reached a comparatively advanced stage of development. Their pottery, not made upon the wheel, is not wanting in a certain elegance. But the arts of design were in an extremely backward > Baskets closely resembling those taken from Egyptian tombs have been found in Switzerland. INHABITANTS OF LAKE CITIES. 11 V condition, compared to their development in the reindeer age among the inhabitants of the caves of Perigord and Languedoc. Their architecture was of the simplest de- scription; but their carpenters had invented ingenious methods of joining, mortising, dovetailing, &c., of remark- able size and solidity, which are in no respect inferior to several of those adopted in our own day. Finally, with the aid of fire and of flint tools, the lake dwellers of the age of stone constructed boats of astonishing size and soHdity. • In our present social conditions it is difficult for us to understand the motives which led the early inhabitants of Switzerland to expend so much labour in constructing dwellings above the surface of the water. But if we con- sider that at that remote epoch Switzerland was almost covered by impenetrable ■virgin forests, inhabited by innumerable wild beasts, we shall understand these super- human efforts to defend themselves from their attacks, and to avail themselves of the protection of water against the attacks of an enemy of superior strength. With regard to the moral Ufe of the lake dwellers of Switzer- land we are reduced as in so many other cases to mere conjecture. Those of the neolithic age probably worshipped nature, but they did not stain their religious rites by bloody sacrifices. It is said that the erratic blocks, scattered in such profusion in all mountainous districts where glaciers occiu", served them for altars.' Until quite lately it was not known where and in what manner the lake dwellers buried their dead, or even if they did so at all. A recent and quite unforeseen discovery has thrown light upon this doubtful question ; I allude to the discovery made at Auvernier, not far from the shores of Lake Neufchatel, of a burial cave containing at least a dozen corpses of every age and sex, which had been interred in stone coffins. This stone coffin, like those ' Some antiquaries consider that this use was made of, 1st, the Cowrt Stone, still to be seen in the lake near Lausanne; 2nd, the Nodding Stones; situated near Geneva ; and 3rd, the Wedding Stone (lake of Neufchatel), where, a few years ago, betrothed couples still swore eternal love and fidelity to each other. 118 THE ANTIQUITY OF THE HUMAN ILi.CE. found in England, was barely six feet long by three and a half wide, and five deep. It was formed of great slabs of granite placed upright and covered by other stones, like the dolmens, with this difference, however, that the tombs of Auvernier were hollowed in the ground and enclosed by granite slabs. Moreover, on the southern side there was a sort of narrow passage, with no stone roof, communi- cating with the principal division or tomb. Another accessory chamber, constructed on the northern side, en- closed two skuUs and a few bones. Although some bronze objects (evidently of more recent importation) were found in this new kind of dolmen, M. Desor attributes the tomb of Auvernier to the end of the neolithic age. It therefore appears that the lake dwellers committed their dead to the earth and surrounded them, with stone slabs in the form of a coffin, thus suggesting a comparison with the gigantic monuments which we shall describe under the name of dolmens. The objects interred with the dead, although few in number, also bear a close re- semblance to those of the dolmens (serpentine axes per- forated for suspension, teeth of bears and wild boars, and bone discs also pierced, &c.). The anatomical characteristics of the lake dwellers of Switzerland are scarcely better known than their moral and religious ideas. However, M. His, upon insufficient data as we think, has undertaken to class them according to the form of the skull. He distinguishes f jur principal types :— 1. That of Sion, where the dolichocephalous' character is strongly marked. 2. That of Hohlberg 1 -0 xi. j i- i. 1,1 3. That of Bel-Air j ^°^^ dohchocephalous. 4. That of Dissentis. the only brachycephalous t3rpe. But we place little faith in these sharply defined racial characters. ' The dolichocephalous skulls (or long-heads) are those of which the form is comparatively long and narrow ; the brachycephalous (or short- heads) are distinguished by their relatively greater transverse diameter, as compared to the longitudinal section ; the mesocephalou (or mean- heads) hold the middle place between the two above-mentioned forms. FAUNA OF SWISS T-AKK CITIES. 119 To judge from the bones, unfortunately few in number, found in the Swiss lakes, their inhabitants were of small size and possessed of no grace of limb. ,But we cannot decide with certainty the ethnic origin of these strange tribes, which is enveloped in obscurity, so that we can only wander with uncertain steps in the region of con- jecture. Nevertheless, these unknown people, be they whom they may, have left to us beneath the clear waters of their lakes, records whose meaning is as clear as that of the pyramids, tjie statues, and the sphinx of Egypt. Modern science has already cleared up unexpectedly some points of the history of this people ; but there is no written record of its origin or its end, and the bones which remain are too few in number to allow us to decide with certainty to what race it belonged. Fauna op the Swiss Lake Dwellings. (After Kutimeyer.) Vrsits arctos Moles intlgarii Sfvftelafoina „ martcs „ putorUi^ „ ermiuca J.vtra vulgaris CaiiU lujms „ famiUarU „ miJpet Felis catvs liriiiaceiis ewopania (Jastor fiber Sciiirus ewropiBus jVus sylvatictts Xepui timidiis Sus scrofaferui „ paliiMris „ domesticus Eqmis caballus Cermu aloes „ elaphus „ cajveolus Oris aries Antilope nipieapra Bos primigenius „ bison Taurus primigeni'ia „ brachyceros „ frontosus Capra ibex „ hirous To this list we must add about twenty birds and ten species of reptiles or of fish which are still extant. Out of the thirty-two species of mammalia mentioned above, six were domesticated, namely, the dog, the horse, the pig, the goat, the sheep, and the ox, of which last there were several varieties. The hare is extremely rare, and the mouse, the rat, the cat, the ass, and the fowl are entirely absent. It will be seen that this fauna also dififers from the present fauna of Switzerland by the possession of the 120 THE ANTIQUITY OF THE HUMAN EACE. urus, of the aurochs or European bison, the elk, the stag, and the wild boar. IV. THE PLOBA OF THE SWISS LAKE D'WELLIITaS. Like the fauna of the same epoch, this flora offers the closest analogy with that of our day. However, a plant then very common in Switzerland (Trapa Tiatans) seems to have completely disappeared, though Lubbock affirms that it is still occasionally to be met with. Some few have only changed their altitude ; such are the Pinus fnughon and the NwpJiar pumilum, or dwarf water lily. For the rest, this flora, in its two principal elements, the plain and the mountain, has its root in the lignites of Diirnten and TJtznach, where larches, pines, and maples of similar species to the modern ones occur. We subjoin a list drawn up by Professor Heer, and borrowed from the work 'Habitations Lacustres,' of M. Troy on, of the seeds and fruits of the stone age found in the Swiss lakes. I. Cereals. Wheat . German wheat Six-ranked Barley . Double-ranked Barley Tritiown vuZ^ore, Will. Eobenhausen. Wangen ' „ dweoctnim, Schw. „ „ monocoocum, L. „ Sordewm Iwxasticlwn, L. „ „ „ distichwm, L. „ n. Fbuits. Apple tree (two varieties, wild and cultivated) . Pyrus malus, L. . Robenhausen. Wangen Pear tree . . . Pyrus commwnis, L. . „ „ Cherry tree . . . Prwnus avium, L. . „ Plum tree insitioia, L. . „ III. Textile Plants. Flax . . . Linum usUatissimum, L. Eobenhansen. Wangen ' At Wangen several bushels of wheat were found heaped up in one place. This was evidently the provision of some family or tribe. The preservation of seeds, fruits, and even bread, found at Eobenhausen and Wangen, is a most unexpected phenomenon, but it can be explained by the more or less complete carbonisation which they have undergone, and by the preserving virtue of the peat in which they are found. What are the antiquities of Herculaneum and Pompeii compared to those of Wangen and Robenhausen 1 ANCIENT P^ONIANS. 121 Hazel nut ' Beech nut . Blackberry Kaspberry Strawberry Sloe IV. Edible Wild Fruits. . Corylus miellana, L. . Bobenhausen . Fctg-us syhatiea, L. . „ . Mubus idcBus, L. . „ Wangen „ fructicoms, L. „ . Fraga/ria msoa, L. . „ . Smims spinosa, L. . „ V. Othek Seeds and Fhttits 'which mat have been used Bird cherry . Water chestnut Yew . Common Gomel wood) Water lily Yellow water lily Dwarf water lily Lake soirpus . Scotch fir Marsh fir (Dog- FOB Food. Pnmus padus, L. Trapa natcms, L. Taxus baccata, L. Eobenhausen. Wangon Comits tanguinea, L. . NyiivphcBa alba, L. . Nuphav Uttevm, L. . . Nuplmr pumilum, L. . Soirpus lacvMris, L. . , Pimm sylveitris, L. . . Pinu) uligiTwta, L. . We must add to this list the Sambucus nigra or com- mon elder, of which the fruit is edible, and is used to make a preserve ; the Triticum turgidwrn (Egyptian wheat), Triticum, spelta, Secale cereale, Avena sativa, Panioum miliaceum, Setaria italica, Silene cretica, Faba vulgaris, Fisum sativum, Ervum lens, Linum angusti- folium. Hemp appears to have been unknown to the lake dwellers of Switzerland. V. AWOIEITT AliTD MODEHW COWSTETTCTIOIirS SIMILAK TO THE LAKE D-WTELLIlfOS. All the authors who have studied the huts built on piles have mentioned those of Lake Prasias, in Thrace, as presenting a remarkable analogy with the lake cities of Switzerland. Professor Virchow of Berlin, one of the last to treat of them, gives from Herodotus (fifth century before Christ) the following description of the aquatic dwellings of the ancient Pseonians : — ' The people of the Pseonians dwelt in Thrace. Several of these tribes had settled on dry land. But one of them. inhabited a city built on piles, in the middle of the lake • Some of these have a hole bored through them, as if they had been used for necklace-beads or children's toys. 122 THE ANTIQUITY OP THE HUMAN RACE. of Prasias, wliose only cominunicatioii with the shore was a narrow bridge. The town, of which the piles had been set up in the first instance by the common labour of the citizens, continually increased in size ; for each citizen who took a wife was bound to bring three posts from the neighbouring forest of Orbelos, and to fix them in the lake; the number of wives was not limited. On these piles a common flooring of beams was placed, and each man built thereon his hut, communicating with the water by a trapdoor. They fastened the little children by a cord that they might not fall into the water. Horses and cattle were fed upon fish, which were so abundant in the lake that it was only necessary to open the trapdoor and let down a net, which was soon filled.' Hippocrates, in his treatise on Air, Water, and Places, tells us that the people settled on the banks of the Phasis (the river rendered famous by the Golden Fleece and the Expedition of the Argonauts) built houses of wood and reeds on piles in the middle of the marshes ; their health, he adds, is much impaired by this way of life. Even to this day, and in the same place, the inhabit- ants build their dwellings as in the time of Hippocrates. Virchow further informs us, on the authority of the traveller Maurice Wagner, ' that the town of Eedout-Kaleh, on the Chopi, is composed of two long rows of wooden huts. These huts, which are hardly larger and more spacious than the booths at Frankfort fair, rest on piles raised a foot above the marshy soil. The same is true of Novo- Tscherkask, the capital of the Cossacks of the Don.' (Virchow, ' Eevue des cours scientifiques,' 1866, vol. iv. p. 10.) In modern times we know of a number of places where habitations are constructed more or less resembling the lake cities of ancient Helvetia. Without speaking of the Papuans of New Gruinea, who at the present day build their houses precisely after the fashion of the Pseonians, the persistence of this same mode of construction among the inhabitants of the banks of the Phasis, and even among the Cossacks of the Don, is worthy of remark. Very LAKE HUTS IN COCHIN CHINA. 123 similar habitations occur also in various parts of Oceania, in Borneo, in the Islands of Ceram and Mindanao, &c. Dumont d'Urville saw at Tondano, in the Island of Celebes, a town now almost entirely destroyed, private dwellings supported on piles artistically carved, and representing men and animals. He tells us that Tondano is a compound word, signifying tnan of the water, and that the houses of Fig. 36. Modekn lake TywexAssas of tite inhabitants of New Guinea. (After Dumont d' UivUle.) this town bore a striking resemblance to the reed huts and marsh dwellings of la Vendee, his native country. In the port of Dorei in New Guinea certain houses, or sanctuaries consecrated to the gods, are raised on piles representing naked human figures. In many tribes the ordinary houses are also built in like manner (fig. 36). The interior of Africa is still too little known to enable us to mention many lake dwellings in that country. The practice of building above the surface of the water seems however to have taken root there, at least along the banks of the Niger, the Zambesi, and the Tsadda. 124 THE AlfTIQUITY OF THE HUMAN EACE. In Cochin China, the present inhabitants of Camboja (placed under the protectorate of France in 1864), ' live,' Dr. Noulet tells us, ' in bamboo huts supported on piles, not only along the banks of the rivers, but also on land, and even in the vast forests which cover the interior of the country, and in places where there can be no risk of floods.' • With regard to America, we know that in order more surely to avoid hostile attacks, the Aztecs raised their houses of cane and reed on piles, planted among a group of low and marshy islands, which they afterwards con- nected by dikes protected by palisades. Such was the origin of Mexico, which resembles at once, as we see, the FiQ. 37. Tbaksveese section ok an Irish okannoge. (After Lubbock.) crannoges of Ireland (fig. 37) and the lake dwellings of Switzerland. Lastly, on their arrival in the New World, the Spaniards saw on the lagoon of Maracaibo a kind of village entirely built on piles, ' a little wooden Venice,' says Elisee Eeclus, to which one of the republics of Columbia owes at the present day its name Venezuela. In the 'same way the floating islands ^ of the ancient Assyrians and Chinese had, or have still, their parallels ia Mexico, in those floating gardens which the first historians of the conquest describe with enthusiasm, and which were a species of raft covered ' Dr. Noulet, Z'dge de la pierre polie et du bronze au Ca/nibodge, tHapres les dicoimertes de M. J. Mowra, lieutenant de vauseau, repre- sentant du proteetarat franqais au Cambodge, in the archives of the Natural History Museum of Toulouse, 1879, p. 6, first report. ^ On the Assyrian bas-reliefs are to be seen artificial islands formed of great reeds, interlaced with one another, and which served as dwellings to the wealthy men of the time of Nineveh and Babylon. THE NUEAGHI OF SAEDINLl. 125 with soil, bearing houses surrounded by the fairest flowers and the richest vegetation. According to M. Desor, the Isle of Roses, in the lake of Starnberg in Bavaria, is only an artificial island dating from the stone age, and inhabited from that time down to our own day. At this very day a castle rises in the midst of its cool shade.' VI. THE KUKAQHI OI" SARDIiriA. The Nuraghi are perhaps the most curious monuments of the stone age. 'Those cyclopean constructions, which have withstood the wear of centuries, a,nd which, scattered almost in profusion throughout Sardinia (the Abbate Spano has counted more than 40,000 of them), still rear their imposing mass before the wondering eyes of the traveller and of the archaeologist. There is no doubt that they were the cradle and home of the primitive races who settled in the island in the remote past. The labours of the learned Abbate Giovanni Spano ^ have proved beyond dispute that we have here one of the earliest examples of the natural formation of a society by men after they have abandoned the nomadic life of hunters. Here, as Mante- gazza has happily expressed it, ' We may read a page of history written by an ancient people over the whole face of Sardinia.' "What this people was, we do not know. Spano sup- poses them to have come from the plains of Shinar at the time of the great emigration which dispersed the tribes of Chaldea through Persia, Palestine, Greece, Italy, and Northern Europe. The first comers grouped their dwellings in the most favourable sites for combined resist- ance in case of a hostile invasion. By degrees, as the chiefs of the tribes grew more powerful, as the family increased, the dwelHngs became more numerous. New comers built others ; and here we find the explanation of the fact that all the Nuraghi are not equally well built, ' E. Desor, Zes Palafittes ou ocmstmctions laoustres da lao de Neuf- chatel, p. 11. Paris, 1865. " See Giovanni Spano, Paleontologia siM-da, ogaia Vetci, preMstorioa segnata rwi monumenti o7ie si trovanc in Sa/rdegna. CagUari, 1871. 126 THE ANTiaUITY OF THE HUMAN EACE. Fig. A Sardinian nuraghi of the earliest EPOCH. the earliest being constructed simply of natural masses, which had been detached from the neighbouring rocks and lay scattered upon the ground, while those of a later date are built of hewn stone, al- though the ma- sonry stiU re- mains rude. The former belong to the stone age, the latter to that of bronze. They are all in the form of a truncated cone. Some have only one room ; others two, and sometimes even three, one above the other. In the interior of these there is a winding stair made of enormous blocks placed at an acute angle in the thickness of the wall, leading to the upper chamber. Others again have an outer wall enclosing a triangular or polygonal space, with an apartment of the same form as the Nuraghi at each angle. These rooms communicate with each other by vaulted passages of which the roof is almost always pointed. Each layer of stone is laid without mortar (figs. 38 and 39). The interior consists sometimes of a great room with a conical roof, and capable of containing forty or fifty people.' The vaulted roof is built of uniform Fig. 39. Vertical section of the SAME, showing THE NICHES AND THE WINDING STAIK. ' The Nuraghi tetirola of the land of Botolana serves as a shelter in POTTERY IN THE NUEAGHI. 127 stones, disposed like those of our modern buildings, pre- senting, that is to say, their larger end to the outer, and their smaller to the inner surface of the wall. The most ancient Nuraghi have but one room, without niches or hiding-places constructed in the thickness of the wall, and terminated in a pointed arch. Three such niches usually occur in the dwellings of a later age, one opposite the door, and one on either side. Another niche to the right of the door was intended as a lurking-place for the defender of J;he entrance in case of attack. The soil which has been formed round the earliest Nuraghi since their construction is no less than two or three yards in thickness. In the lowest layer we find remains of rude hand-made pottery, coal and bones crumbled to dust, but never bones of species extinct in the island, except stag's antlers and boar's tusks, inter- mixed with accumulations of the remains of birds. Pieces of flint and of obsidian occur also, axes of black basalt and porphyry of the archseolithic type, fragments of pottery, &c.,_ some of which appear to belong to the earliest stone age.' In the succeeding layers, we come to polished axes, arrow heads, knives, stones for slinging, fossilised teeth of the dogfish, pottery which has been partially baked by winter to about 500 pigs, driven down from the mountains by the swineherds. ' Many French archaeologists maintain that pottery dates only from the age of polished stone. We know, however, that M. de Serres found at Bize in Aude, and M. de Christol at Souvignaiguea in Gaide, fragments of pottery which it is scarcely possible not to consider contemporary with the reindeer, perhaps even with the bear, in company with whose remains they were found. I myself extracted some from a bear cave at Nabrigas (Lozfere), M. Perry at Vergisson, near M^oon, and M. Dupont in several bone oaves of Belgium has observed specimens of still earlier date. Lastly, the Abbate Giovanni Spano assures us that he found in the different layers of soil which surround the Nuraghi of Sardinia, earthen vases (entire or in pieces) belonging to all the ages, ' gtmiiglie che in se portano il carattcre di un' eta la jn& rimota,' says the learned abbate. He calls attention also to the fact that the rudest specimens occur in the lowest layer. Those which are found in the second or middle layer are less rude, and so on until we arrive at the uppermost strata, where they are smooth and polished. Some few even appear to belong to the fioman epoch. On the other hand, in the giant tombs in the neighbourhood of the Nuraghi, we only find ill-formed pottery of the rudest description. 128 THE ANTIQUITY OF THE HUMAN EACE. fire, with teeth of the wild boar and other animals, and shells of several species of molluscs, which appear to be the kitchen refuse of these primitive tribes. Lastly, smooth black fragments of pottery have been extracted from the upper layers, as well as pieces of bronze, which indicate the age of transition between stone and this metal. The Abbate Spano has not been able to find any iron objects : he accounts for the absence of iron by the destructive effect of damp ground and the influence of the atmo- sphere upon this metal. The same savant attributes the construction of the Fig. 40. Burgh of Moussa, Shisilanu Isles. (After Lubbock.) Nuraghi to the first immigrants who came from the East into Europe. Orientals or aborigines, archseolithic or neo- Hthic, these peoples have in any case left us monuments of real and great value to the history of humanity, and although we do not adopt all the Abbate's theories without reserve, we recognise with gratitude the zeal which their discoverer has displayed in dispelling, to some extent, the obscurity which still envelopes them. Similar monuments have been found in the Balearic isles, where they are known by the name of Talayoti ; in the Island of Pantelleria, where they are called Sesi ; SIMILAR CONSTRUCTIONS IN IRELAND. 129 and even in France, in the department of Herault, ac- cording to M. Cazalis of Fondouce. But they are especially numerous in Scotland and the neighbouring islands. They are there known as burghs or brocks, and we give an illustration of one of the most celebrated, the burgh of Moussa, one of the Shetland Isles (fig. 40). It will be seen that these monuments resemble in every respect the Nuraghi of Sardinia, and the existence of an identical type in so distant a country renders the truth of the bypotiesis of the Abbate Spano with regard i^»^/f