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[6] Dryopithecus and Mesopithecus.

There are, however, in France two localities, one in the upper and the other in the middle miocene, which have afforded what are supposed to be worked flints. [7] The geological age of the deposits seems in both cases beyond question, but doubts have been cast, and this seemingly with some reason, on the artificial character of the flint flakes, while in the case of some examples which appear to be scrapers and borers, like those in use long afterward by semi-civilised peoples for working in bone and skin, there are grave doubts whether they actually came from the miocene beds. Lastly, it has even been suggested that these flints may be the handiwork of miocene apes, a suggestion not so unreasonable as at first sight it appears, when taken in connection with the working instincts of beavers and other animals. Monkeys, however, seem to have less of this gift as artificers than most other creatures. On the whole, we must regard the existence of miocene man as not proven, though, if it should prove to be a fact, it may be useful to some of the scoffers of these days to know that it would not be so irreconcilable with the Biblical account of creation as they seem to suppose. It might, however, prove a serious stumbling-block to orthodox Darwinians, and might raise some difficulties respecting antediluvian genealogies.

[7] Puy, Courny and Thenay.

In the pliocene of Europe there are alleged to be instances of the occurrence of human bones. One of these is that of the skull now in the museum of Florence, supposed to have been found in the pliocene of the Val d'Arno. It is, however, a skull of modern type, and may have been brought down from the surface by a landslip. But this explanation does not seem to apply to the human remains found in lower pliocene beds at Castelnedolo, near Brescia. They include a nearly entire human skeleton, and are said by good observers to have been imbedded in undisturbed pliocene beds. M. Quatrefages, who has described them, and whose testimony should be considered as that of an expert, was satisfied that the remains had not been interred, but were part of the original deposit. Unfortunately the skull of the only perfect skeleton is said to have been of fair proportions and superior to those of the ruder types of post-glacial men. This has cast a shade of suspicion on the discovery, especially on the part of evolutionists, who think it is not in accordance with theory that man should retrograde between the pliocene and the early modern period, instead of advancing. Still we may ask, why not? If men existed in the fine climates of the miocene and early pliocene, why should they not have been a noble race, suited to their environment; and when the cold of the glacial period intervened, with its scarcity and hardships, might they not have deteriorated, to be subsequently improved when better conditions supervened? This would certainly not be contradictory to experience in the case of varieties of other animals, however at variance with a hypothetical idea of necessarily progressive improvement. Let us hope that the existence of European pliocene man will be established, and that he will be found to have been not of low and bestial type, but, as the discoveries above referred to if genuine would indicate, a worthy progenitor of modern races of men.

It still remains to inquire whether man may have made his appearance at the close of the pliocene or in the early stages of the pleistocene, before the full development of the glacial conditions of that period. Perhaps the most important indications of this kind are those adduced by Dr. Mourlon, of the Geological Survey of Belgium, [8] from which it would appear that worked flints and broken bones of animals occur in deposits, the relations of which would indicate that they belong either to the base of the pleistocene or close of the pliocene. They are imbedded in sands derived from eocene and pliocene beds, and supposed to have been remanié by wind action. With the modesty of a true man of science, Mourlon presents his facts, and does not insist too strongly on the important conclusion to which they seem to tend, but he has certainly established the strongest case yet on record for the existence of tertiary man. With this should, however, be placed the facts adduced in a similar sense by Prestwich in his paper on the worked flints of Ightham. [9]

[8] Bulletin de l'Académie Royale de Belgique, 1889.

[9] Journal of the Geological Society, London, May 1889.

Should this be established, the curious result will follow that man must have been the witness of two great continental subsidences, or deluges, that of the early pleistocene and the early modern, the former of which, and perhaps the latter also, must have been accompanied with a great access of cold in the northern hemisphere. It seems, however, more likely that the facts will be found to admit of a different explanation.

Every reader of the scientific journals of the United States must be aware of the numerous finds of 'palæolithic' implements in 'glacial' gravels, indicating a far greater antiquity of man in America than on other grounds we have a right to imagine. I have endeavoured to show, in a work published several years ago, [10] how much doubt on geological grounds attaches to the reports of these discoveries, and how uncertain is the reference of the supposed implements to undisturbed glacial deposits, and how much such of the 'palæoliths' as appear to be the work of man resemble the rougher tools and rejectamenta of the modern Indians. But since the publication of that work, so great a number of 'finds' have been recorded, that despite their individual improbability, one was almost overwhelmed by the coincidence of so many witnesses. Now the bubble seems to have been effectually pricked by Mr. W. H. Holmes, of the American Geological Survey, who has published his observations in the American Journal of Anthology and elsewhere. [11]

[10] Fossil Man, London, 1880.

[11] Science, November 1892; Journal of Geology, 1893.

SECTION AT TRENTON, ON THE DELAWARE, SHOWING THE RELATION OF THE STONE IMPLEMENTS TO THE GLACIAL (?) GRAVELS (after Holmes)

One of the most widely-known examples was that of Trenton, on the Delaware, where there was a bed of gravel alleged to be pleistocene, and which seemed to contain enough of 'palæolithic' implements to stock all the museums in the world. The evidence of age was not satisfactory from a geological point of view, and Holmes, with the aid of a deep excavation made for a city sewer, has shown that the supposed implements do not belong to the undisturbed gravel, but merely to a talus of loose débris lying against it, and to which modern Indians resorted to find material for implements, and left behind them rejected or unfinished pieces. This alleged discovery has therefore no geological or anthropological significance. The same acute and industrious observer has inquired into a number of similar cases in different parts of the United States, and finds all liable to objections on similar grounds, except in a few cases in which the alleged implements are probably not artificial. These observations not only dispose, for the present at least, of palæolithic man in America, but they suggest the propriety of a revision of the whole doctrine of 'palæolithic' and 'neolithic' implements as held in Great Britain and elsewhere. Such distinctions are often founded on forms which may quite as well represent merely local or temporary exigencies, or the débris of old work-shops, as any difference of time or culture.

CHIPPED QUARTZITES, MODERN AMERICAN (after Holmes)

Upper line (1 to 6), unfinished and rejected pieces.

Lower line (7 to 18), progress of development from the unfinished oval form to finished lance and arrow-heads.

For the present, therefore, we may afford to pass over with this slight notice the alleged occurrence of miocene and pliocene man, and this the rather since, if such men ever existed in the northern hemisphere, the cold and submergence of the pleistocene must have cut them off from their more modern successors in such a way that man must practically have made a new beginning at the close of the glacial age.

I do not refer here to the finds of skulls and implements in the auriferous gravels of Western America. Some of these, if genuine, might go back to the pliocene age, but in so far as the evidence now available indicates, they all belong to the modern races of Indians, and, in one way or another, by fraud or error, have had assigned to them a fabulous antiquity.

There still seems reason to believe that remains of man and his works exist in beds which are overlaid by boulders and gravel, implying a cold climate. These may indicate the last portion of the glacial period proper, in which case the beds with human remains may be called inter-glacial, or they may indicate a partial relapse to the cold conditions occurring after the glacial age had passed away, and in the early part of the modern period. My own view is, that it is most natural to draw the boundary line of the pleistocene and anthropic or modern at the point where the earliest certain evidences of man appear, and that the anthropic age will be found to include not only an early period of mild climate succeeding the glacial age, but a little later a return of cold, not comparable with that of the extreme glacial period, but sufficient seriously to affect human interests, and which almost immediately preceded those physical changes which carried away palæocosmic man, or the man of the earliest period, and many of his companion animals, and introduced the neanthropic or later human age. We shall find facts bearing on this in the sequel.

In the meantime, we may consider it as established beyond cavil that man was already in Europe immediately after the close of the glacial period, and was contemporary with the species of animals, many of them large and formidable, which at that time occupied the land. He must have entered on the possession of a world more ample and richer in resources than that which remains to us. The early post-glacial age was, like the preceding pliocene, a time of continental elevation, in which the dry land spread itself widely over the now submerged margins of the sea basins. In Europe, the British Islands were connected with the mainland, and Ireland was united to England. The Rhine flowed northward to the Orkneys, through a wide plain probably wooded and swarming with great quadrupeds, now extinct or strange to Europe. The Thames and the Humber were tributaries of the Rhine. The land of France and Spain extended out to the hundred-fathom line. The shallower parts of the Mediterranean were dry land, and that sea was divided into two parts by land connecting Italy with Africa. Possibly portions of the shallower areas of the Atlantic were so elevated as to connect Europe and America more closely than at present.

Connected with this elevation of the continents out of the sea was a great change of climate, whereby the cold of the pleistocene age passed away and a milder climate overspread the northern hemisphere, while the newly-raised land and that vacated by snow and ice became clothed with vegetation, and were occupied by a rich quadrupedal fauna, including even in the northern parts of Europe, Asia, and America, species of elephant, rhinoceros, and other genera now confined to the warmer climates. This new and noble world was the rich heritage of primeval man.

Pictet has estimated the number of species of mammals inhabiting Europe in the palanthropic period at ninety-eight, [12] of which only fifty-seven now live there, the remainder being either wholly or locally extinct—that is, they are either not now existing in any part of the world, or are found only beyond the limits of Central, Western, and Southern Europe. The extinct species also include the largest and noblest of all. It has been remarked that the assemblage of palanthropic species in Europe and Western Asia is so great and varied that with our present experience we can scarcely imagine them to have existed contemporaneously in the same region. For example, the association of species of elephant and rhinoceros, the musk-sheep, the reindeer, the Cape hyena, and the hippopotamus seems to be incongruous.

[12] Zittel, in a recent paper (1893), gives 110 species of mammals in the pleistocene and early modern. Of these about twenty of the largest and most important are extinct.

Various theories have been proposed to remove the difficulty. Modern analogies will allow us to believe in such astounding facts if we take into account the probability of a warm climate, especially in summer, along with a wooded state of the country providing much shelter, and wide continental plains affording facilities for seasonal migrations. There were no doubt also climatal changes in the course of the age, which may have tended to the remarkable mixture of animal types in its deposits. In connection with this there is now every reason to believe that while, in its earlier part, the palanthropic age was distinguished by a warm climate, in its later portion a colder and more inclement atmosphere crept over the northern hemisphere. As an illustration of this, it is known that in the earlier part of the period a noble species of elephant named Elephas antiquus, and a rhinoceros (R. Merkii), abounded in Europe; but as the age advanced these species disappeared, and were replaced by the mammoth (E. primigenius) and the woolly rhinoceros (R. tichorhinus), animals clothed like the musk-ox in dense wool and hair, and evidently intended for a rigorous climate. With and succeeding these last species, the reindeer becomes characteristic and abundant. It is, as we shall see, a point of much importance in what may be called the prehistoric history of man, that he was introduced in a period of genial temperature as well as of wide continental extension, and survived to find his physical environment gradually becoming less favourable, and the age ending in that great cataclysm which swept so many species of animals and tribes of men out of existence, and reduced the dry land of our continents to its present comparatively limited area.

I should, perhaps, have noticed here the worked flints found so abundantly in some parts of the south of England, which have long attracted the attention of collectors, and have in some cases been referred to glacial or pre-glacial times. I believe, however, they are all really post-glacial, though in some cases belonging to the earliest portion of that period. [13]

[13] Prestwich on 'Ightham Beds,' Journ. Geol. Soc., 1893; Dawkins, Journ. Anthrop. Soc., 1894.

We may close the present chapter by presenting to the eye in a tabular form the series of events included in the pleistocene and modern periods of the great cenozoic time.

LATER CENOZOIC, OR TERTIARY PERIOD

(In Ascending Order, or from the Older to the Newer)

Newer Pliocene.—A continental period of long duration, elevated land, much erosion, much volcanic action.

Pleistocene.—Irregular elevation and depression of the land, ending in wide submergence with cold climate. Glaciers on all mountains near to coasts and ice-drift over submerged plains. Glacial period, with an inter-glacial mild period in the middle and great submergence of the continents toward the close.

Anthropic.—Palanthropic, or post-glacial, in which the land emerges and attains a very wide extension, and is inhabited by a varied mammalian fauna. Man appears in Europe, Asia, and North Africa. Terminated by a recurrence of cold and great subsidence, deluging all the lower lands. Neanthropic.—Area of continents smaller than in the previous period. Surviving races of men and species of animals repeople the world. Modern races of men and modern animals.

CHAPTER IV

THE PALANTHROPIC AGE [14]

[14] Called by some 'Palæolithic,' from the use of implements like that figured on p. 41.

We have now to inquire more particularly what we can learn as to the earliest men known to us, those who appeared in Western Asia and Europe at the close of the glacial period, when the cold had passed away and a genial climate had succeeded, and when the continents of the northern hemisphere had attained to their largest dimensions, were clothed with a rich vegetation and tenanted by an abundant mammalian fauna, including many large and important creatures now extinct.

We may first notice here a necessary limitation to our knowledge. The dry land of this age was of greater dimensions than at present. A large portion of what then was land is consequently now under the sea or deeply buried in alluvial deposits. Hence if any men of this age lived near the borders of the ocean, their remains must now be inaccessible, and the relics which we find must be those of inland tribes or of those who were driven inland by the encroachments of the waters. Our means of information are thus limited, and we must be prepared to admit that there may have been in this age great and populous communities of which we can have no record, at least of a geological character. Hence if we should find remains of only rude races of men, we should not be justified in assuming that all the peoples of the palanthropic age were of this character, more especially if we can find any indications that the men whose remains are accessible to us, though rude themselves, may have belonged to more advanced races.

FLINT HACHE OF THE ANCIENT OR CHELLEAN TYPE, AURILLAC (after Carthaillac)

The bones, implements and weapons, and débris of the feasts of these primitive peoples are to be found principally in caves of residence or of sepulture, [15] and in the alluvia deposited by rivers, and in a few cases in rock fissures or marine gravels, into which remains were drifted, or in which they were deposited by water. Here, again, we have another limitation, for it is possible that large populations may have lived on plains or in forests in perishable structures, and, like some modern savages, may have disposed of their dead in such a way that their bones could not have been preserved. In such cases we can hope to obtain, and then very rarely, only stone implements and other imperishable relics.

[15] Caverns, in relation to this subject, may be divided into those of residence, in which early men have lived and have left therein the débris of their food, the ashes and cinders of their fires, and implements, &c.; those of sepulture, in which the bodies of the dead have been deposited; and those of inundation, into which the bodies of animals or men have been drifted by floods. The same cave may, however, exhibit these different conditions in the deposits on its successive floors. Thus men may have inhabited a cave for a time; it may next have been invaded by river floods depositing mud, and it may subsequently have been used for burial.

Notwithstanding these limitations, however, it is wonderful that so much has been recovered from the ground by the diligence of collectors, and that the material thus obtained has proved so fertile in information respecting our long-perished ancestors.

Supposing, then, that we search for remains of palæocosmic men in river alluvia, or in caves of residence or burial, or in similar repositories, the question next arises, by what means can we distinguish their bones from those of later times? The following criteria are available:

(1) The remains were in their present condition at least as long ago as the date of the earliest history or tradition. This evidence is of course of greatest value in those regions in which history extends farthest back. Thus the remains of early men in the Lebanon caves, which we know date much farther back than the arrival of the first Phœnicians and Canaanites in Syria, are in a different position, in so far as history is concerned, from those occurring in countries whose written history goes back only a few centuries.

(2) The deposits containing these remains may underlie those holding relics of historic times, or may indicate different physical conditions of the districts in which they occur from those known within historic periods. This is the case with some river beds, as those of Grenelle, near Paris, and with the successive deposits in old caves of residence.

(3) They may be accompanied by remains of animals now extinct in the regions in question, and whose disappearance and replacement by the modern fauna implies great lapse of time and physical changes; as, for instance, when we find that men have left remains of their feasts holding bones of the extinct woolly rhinoceros and his contemporaries, or in now temperate climates, those of the reindeer.

(4) The remains themselves may indicate a race or races of men and a condition of the arts of life different from any known in the region in historic times. Thus we may have skulls and skeletons indicating men racially distinct from any now extant, and implements and weapons different from those in use in the times of history or tradition.

We have now to consider what evidence of this kind vindicates the assertion that man existed on our continents in the second continental or post-glacial age, or, as others will have it, in the closing period of the glacial age, and was contemporary with the mammoth and other great beasts now extinct. This evidence, which has been accumulating with great rapidity and relates to many parts of the northern hemisphere, is too voluminous to be reproduced here. [16] But a few examples of it may be given, more especially from parts of the old world whose history extends farthest back and where explorations have been most extensive.

[16] Reference may be made to Christy and Lartet, Reliquiæ Aquitanicæ; Quatrefages, Homme Fossile; Dupont, L'Homme pendant les Ages de Pierre; Carthaillac, La France Préhistorique; Dawkins, Cave Hunting and Early Man in Britain; Fossil Men and Modern Science in Bible Lands, by the author.

My first instance shall be one originally described by Canon Tristram, and which I had an opportunity to examine in 1884—the caverns or rock shelters in the face of the limestone cliff of the pass of Nahr-el-Kelb, north of Beyrout. At this place, in old caverns partly cut away in the forming of the Roman road round the cliff, there is a hard stalagmite, or modern limestone, produced by the calcareous drippings from the rock. This is filled with broken bones intermixed with flint flakes suitable for use as knives or spears or darts, and occasional fragments of charcoal. The bones are those of large animals, and have been broken for the extraction of the marrow; and the whole is evidently the remnants of the cuisine of some primitive tribe of hunters, now cemented into a somewhat hard stone by stalagmitic matter. The bones are not those of the present animals of Syria, but principally of an extinct species of rhinoceros (R. tichorhinus), a species of bison, and other large mammals which inhabited the region in the pleistocene and post-glacial periods. It is farther known that these animals had been extinct long before the early Phœnicians penetrated into this country, perhaps 3000 B.C., and that the deposits existed in their present state when the early Egyptian conquerors passed this way, at least 1500 B.C., on their march to encounter the Hittites. It is also known that the earliest historic aborigines of the Lebanon, certain rude tribes which seem to have existed there before the migration of the Phœnicians, subsisted on the modern animals of the district, and used flint implements and weapons somewhat differing from those of the earlier cave men of the region. [17] What, then, were these earlier cave men? Certainly no people known to history, unless those whom we know as antediluvians. [18]

[17] See the illustration on p. 97.

[18] For more detailed description see Modern Science in Bible Lands; also Egypt and Syria, in the Bypaths of Bible Knowledge, by the author.

From the Lebanon we may pass to the west of Europe, where in France and Belgium a vast number of interesting relics of palæocosmic man have been discovered, and have been scientifically examined.

We may take as an illustration the cave of Goyet, on the cliffs bounding the ravine of the Samson, a tributary of the Meuse. This cavern is about forty-five feet above the present ordinary level of the river, but in post-glacial times seems to have been invaded by inundations, as it shows on its floor five distinct ossiferous surfaces, separated by layers of river-mud. These successive surfaces have been carefully examined by M. Dupont, and their contents noted.

On the lowest of these, or the first in order of age, were found numerous skeletons and detached bones of the cave lion and the cave bear; the former a possible ancestor of the lion of Western Asia, the latter closely allied to the grizzly bear of North America, but both entirely extinct in Europe. One of the skeletons of the lion was of unusually large size, and so complete that when set up it forms the principal ornament of the cave collection in the Brussels Museum.

CAVE OF GOYET, BELGIUM (section after Dupont)

1 to 5, layers of clay deposited in the mammoth ages

The next surface, the second in order of time, had a greater variety of animal remains. The lion had disappeared, and instead hyenas haunted the cave, and had dragged in animal bones to be gnawed. These included remains of the cave bear, wolf, rhinoceros, mammoth, wild horse, wapiti, Irish stag, chamois, reindeer, wild ox, besides several smaller animals. The above animals are now all unknown in the fauna of modern Europe, except the reindeer, the chamois, and the wolf. But the most remarkable discovery on this surface was that of a few human bones, gnawed like the others by the hyenas. Man was thus already in the country, and contemporary with all these animals. How the hyena obtained his bones, whether from some neglected corpse or from some badly-constructed grave, will never be known; but the discovery introduces us to a tribe or family of men coming as immigrants into a region already stocked with many great quadrupeds. They probably did not yet dwell in caves, which, at a later and perhaps more inclement period, formed their homes. Dupont concludes from the condition of the bones that on both the older surfaces the cave bear was the later tenant, and had replaced the lion on the first and the hyena on the second.

The remaining surfaces introduce us to man as a cave-dweller. On the oldest of them are found not only abundance of débris of food, but worked flints and bones, objects of ornament, and evidences of the use of fire. The two higher layers show works of art in more varied and improved forms, as if a certain progress in the arts of life had taken place during the occupancy of the cave. Among the objects in the upper layers were red oxide of iron, showing the use of colouring matter for the skin or garments, bone needles, proving the manufacture of clothing by sewing, bone points for darts, skilfully-barbed bone harpoons, ornaments made of perforated teeth of animals, and fragments of bone, and a remarkable necklace of a hundred and twenty-four silicified shells of the genus Turritella, looking like spirals of agate, with a pendant made of another and larger shell. These shells are not known to occur nearer to the cave than Rheims, in Champagne. It is scarcely too much to say that this necklace might be worn by any lady of the present day. A certain amount of imitative art is also shown in the carving of animal and plant forms and fancy devices on pieces of reindeer antler, which may have served for handles of weapons or implements. But objects of much more elaborate design have been found in caverns of this age in France. (See illustrations on pp. 59 and 68.)

LANCE-HEAD FORMED OF A FLINT FLAKE (CAVE OF MOUSTIER)

Similar to weapons found in the Goyet cave. The flat face shows a bulb of percussion (after Falsan)

The food of these people, in so far as it was of an animal nature, may be learned from the broken bones, which show that here as elsewhere they carried into their caves only the legs and skulls of the larger animals they killed, leaving the carcases; though it is quite possible that, like North American hunting Indians, they may have stripped off portions of flesh from the back, and preserved the heart, liver, &c., which would of course leave no remains.

Dupont gives lists of the animals in each layer. Those in the lower of the anthropic layers consist of twenty-three species of quadrupeds and some bones of birds. Among the former were the mammoth, the rhinoceros, two species of bear, the horse, the reindeer, two other species of deer and two bovine animals. Even the lion, the hyena and the wolf were eaten by these people. It is interesting to note that the numerical preponderance was in favour of the reindeer and the wild horse, though remains were found indicating seven individuals of the mammoth, and four of the rhinoceros, as having fallen a prey to the old hunters. In the highest bed the number of species and the proportions of each one are nearly the same, so that no material change in the fauna had occurred during the occupancy of this cave. It may also be noted that while Dupont calls this a cave of the mammoth age, the French archæologists are in the habit of naming similar deposits those of the reindeer age. The age of both animals was in reality the same, except that in France the reindeer seems to have survived the mammoth, and indeed we know this to be the fact from its continuing in the forests of Germany till the Roman times.

This cave may serve as an example of the manner in which the men of the palanthropic age make their appearance. Let it be observed also that this is only one instance selected from many giving similar testimony, and that Dupont adduces evidence to show that there may have been a contemporary plain-dwelling people, of whom less is known than of the troglodytes. Let it also be noted that there are other caves in Belgium, to which we shall return later, which show how the neocosmic men contemporary with the present fauna succeeded the men of the mammoth age.

We may now inquire as to the physical characters of the men of this period. It may be stated in answer to this question that two races of men are known in the palanthropic age, both somewhat different from any existing peoples, and known respectively as the Canstadt and Cro-magnon races. As the latter is the most important and best known, we may take it first, though the former may locally at least have been the older.

The valley of the little river Vezère, a tributary of the Dordogne, in the south of France, abounding in overhanging rock-shelters, seems to have been a favourite abode of the men of the mammoth and reindeer age. The rock-shelter of Cro-magnon explored by Lartet is one of these, and that of Laugerie Basse is on the opposite side of the same stream.

The former is a shelter or hollow under an overhanging ledge of limestone, and excavated originally by the action of the weather on a softer bed. It fronts the south-west, and, having originally been about eight feet high and nearly twenty deep, must have formed a comfortable shelter from rain or cold or summer sun, and with a pleasant outlook from its front. Being nearly fifty feet wide, it was capacious enough to accommodate several families, and when in use it no doubt had trees or shrubs in front, and may have been further completed by stones, poles, or bark placed across the opening. It seems, however, in the first instance to have been used only at intervals, and to have been left vacant for considerable portions of time. Perhaps it was visited only by hunting or war-parties. But subsequently it was permanently occupied, and this for so long a time that in some places a foot and a half of ashes and carbonaceous matter, with bones, implements, &c., was accumulated. All of these, it may be remarked, belong to the palanthropic age. By this time the height of the cavern had been much diminished, and, instead of clearing it out for future use, it was made a place of burial, in which five individuals were interred. Of these, three were men, one of great age, the other two probably in the prime of life. The fourth and fifth were a woman of about thirty or forty years of age, and the remains of a fœtus.

These bones, with others to be mentioned in connection with them, unquestionably belong to some of the oldest human inhabitants known in Western Europe. They have been most carefully examined by several competent anatomists and archæologists, and the results have been published with excellent figures in the Reliquiæ Aquitanicæ, where will also be found details of their characters and accompaniments, among which last were about three hundred small shells of different species pierced for stringing or attachment to garments. These men are, therefore, of the utmost interest for our present purpose, and I shall try so to divest the descriptions of anatomical details as to give a clear notion of their character. The doubts at one time cast on the age of these skeletons have been removed by the discovery of others at Laugerie Basse, Mentone, &c. They are no doubt palanthropic, though not of the earliest part of the period. The 'Old Man of Cro-magnon' was of great stature, being nearly six feet high. More than this, his bones show that he was of the strongest and most athletic muscular development; and the bones of the limbs have the peculiar form which is characteristic of athletic men habituated to rough walking, climbing, and running; for this is, I believe, the real meaning of the enormous strength of the thigh-bone and the flattened condition of the leg in this and other old skeletons. It occurs to some extent, though much less than in this old man, in American skeletons. His skull presents all the characters of advanced age, though the teeth had been worn down to the sockets without being lost; which, again, is a character often observed in rude peoples of modern times. The skull proper, or brain-case, is very long—more so than in ordinary modern skulls—and this length is accompanied with a great breadth; so that the brain was of greater size than in average modern men, and the frontal region was largely and well developed. The face, however, presented very peculiar characters. It was extremely broad, with projecting cheek-bones and heavy jaw, in this resembling the coarse types of the American face, and the eye-orbits were square and elongated laterally in a manner peculiar to the skulls of this age. The nose was large and prominent, and the jaws projected somewhat forward. This man, therefore, had, as to his features, some resemblance to the harsher type of American physiognomy, with overhanging brows, small and transverse eyes, high cheek-bones, and coarse mouth. He had not lived to so great an age without some rubs, for his thigh-bone showed a depression which must have resulted from a severe wound—perhaps from the horn of some wild animal or the spear of an enemy.

OUTLINE OF THE SKULL OF THE 'OLD MAN OF CRO-MAGNON' (after Christy and Lartet)

The woman presented similar characters of stature and cranial form modified by her sex, and in form and visage closely resembled her sisters of the American wilderness in the pre-Columbian times. If her hair and complexion were suitable, she would have passed at once for an American-Indian woman, but one of unusual size and development. Her head bears sad testimony to the violence of her age and people. She died from the effects of a blow from a stone-headed pogamogan or spear, which has penetrated the right side of the forehead with so clean a fracture as to indicate the extreme rapidity and force of its blow. It is inferred from the condition of the edges of this wound that she may have survived its infliction for two weeks or more. If, as is most likely, the wound was received in some sudden attack by a hostile tribe, they must have been driven off or have retired, leaving the wounded woman in the hands of her friends to be tended for a time, and then buried, either with other members of her family or with others who had perished in the same skirmish. Unless the wound was inflicted in sleep, during a night attack, she must have fallen, not in flight, but with her face to the foe, perhaps aiding the resistance of her friends or shielding her little ones from destruction. With the people of Cro-magnon, as with the American Indians, the care of the wounded was probably a sacred duty, not to be neglected without incurring the greatest disgrace and the vengeance of the guardian spirits of the sufferers.

Unreasonable doubts have been cast on the burial of the dead by palæocosmic men. The burial of men of the Cro-magnon race at that place and at Laugerie Basse and Mentone is established by the most unequivocal evidence; and interments of men of the Canstadt race have been found at Spy, in Belgium. Of course, even if interment proper had not been practised, there might have been cremation, as among the Tasmanians, or burial on stages or in huts, as among some American Indians. Still, that interment was practised we know, and this carries with it the certainty that our palæocosmic men must have had some simple ideas of religion.

THE FIRST SKELETON FOUND IN THE MENTONE CAVES (after Rivière)

The skulls of these people have been compared to those of the modern Esthonians or Lithuanians; but on the authority of M. Quatrefages it is stated that, while this applies to the probably later race of smaller men found in some of the Belgian caves, it does not apply so well to the people of Cro-magnon. Are, then, these people the types of any ancient, or of the most ancient, European race? The answer is that they are types of the cave men of the mammoth age in Europe. Another example is the remarkable skeleton of Mentone, in the south of France, found under circumstances equally suggestive of great antiquity. Dr. Rivière, in a memoir on this skeleton, illustrated by two beautiful photographs, shows that the characters of the skull and of the bones of the limbs are similar to those of the Cro-magnon skeleton, indicating a perfect identity of race, while the objects found with the skeleton are similar in character. I had an opportunity of verifying his description by an examination of the skeleton in the Museum of the Jardin des Plantes, in 1883; and more recent discoveries at Mentone have confirmed the conclusion that this man really represents a race of giants, some of them seven feet high, who inhabited Southern Europe in the palanthropic age. A similar skeleton found by Carthaillac, at Laugerie Basse, was buried under a great thickness of accumulated débris of cookery, as well as of large stones fallen from above. This skeleton had its shell ornaments in place on the forehead, arms, legs and feet, in a manner which would induce the belief that they had been attached to a head-dress, sleeves, leggings, and shoes or moccasins. (See illustration on p. 79.)