Belgian Caverns.—The relics discovered by Dr. Schmerling, in the caves of Belgium, must be referred to the time of the retreat of the glaciers. The glaciers were still in existence, but their receding had freed immense tracts of land, and the space they now covered was small in proportion to their former extent. Whether it be considered or not, that vegetation greatly nourished and the great wild beasts were rapidly increasing, one thing must be noticed, and that is, floods must have succeeded or followed closely upon the retreat of the ice. Many remains, referred to the glacial epoch, may in reality, have occupied the time of the floods occurring just previous to the commencement of the inter-glacial. The Belgian Caverns, near LiÉge, either belong exactly to the ice, or else to a period not far removed. Lyell considers the older monuments of the palÆolithic period to be the rude implements found in ancient river gravel and in the mud and stalagmite caves. The caverns of the province of LiÉge were not the dens of wild beasts, but their contents had been swept in by the action of water. The bones of man "were of the same color, and in the same condition as to the amount of animal matter contained in them, as those of the accompanying animals, some of which, like the cave-bear, hyena, elephant, and rhinoceros, were extinct; others, like the wild-cat, beaver, wild boar, roe-deer, wolf, and hedgehog, still extant. The fossils The floors of these caverns were incrusted with stalagmite. FOSSIL SKULL OF THE ENGIS CAVE NEAR LIEGE. The fossil skull from the cavern of Engis was deposited at a depth of about five feet, under an osseous breccia containing a tusk of the rhinoceros, the teeth of the horse, and the remains of small animals. The breccia was about three and one-fourth feet wide, and rose to the height of about five feet above the floor of the cavern. In the earth which contained the skull there was found, surrounding it on all sides, the teeth of the rhinoceros, horse, hyena, and bear, and with no marks of the earth having been disturbed. There was also found the cranium of a young person, in the floor of the cavern, besides an elephant's tooth. When first observed, the skull was entire, but fell to pieces when removed from its position. Besides these there were found a fragment of a superior maxillary bone, with the molar teeth worn down to the roots, indicating that of an old man; two vertebrÆ, a first and last dorsal; a clavicle of the left side, belonging to a young individual of great stature; two fragments of the radius, indicating a man of ordinary height; a fragment of an ulna: some metacarpal bones; six metatarsal, three phalanges of the hand and one of the foot. Dr. Schmerling found in this cave a pointed bone implement incrusted with stalagmite and joined to a stone. Of the Engis skull Professor Huxley has remarked, "As Professor Schmerling observes, the base of the skull is destroyed, and the facial bones are entirely absent; but the roof of the cranium, consisting of the frontal, parietal, and the greater part of the occipital bones, as far as the middle of the occipital foramen, is entire, or nearly so. The left temporal bone is wanting. Of the right temporal, the parts in the immediate neighborhood of the auditory foramen, the mastoid process, and a considerable portion of the squamous element of the temporal, are well preserved." A piece of the occipital bone, which Schmerling seems to have missed, has since been fitted on to the rest of the cranium by Dr. Spring, the accomplished anatomist of LiÉge. "The skull is that of an adult, if not middle-aged man. The extreme length of the skull is 7.7 inches. Its extreme breadth, which corresponds very nearly with the interval between the parietal protuberances, is not more than 5.4 inches. The proportion of the length to the breadth is therefore very nearly as 100 to 70. If a line be drawn from the point at which the brow curves in towards the root of the nose, and which is called the 'glabella' (a, Fig. 8), to the occipital protuberance (d), and the distance to the highest point of the arch of the skull be measured perpendicularly Fig. 7. Fig. 8. a. Superciliary ridge and glabella. "The front view shows that the roof of the skull was very regularly and elegantly arched in the transverse direction, and that the transverse diameter was a little less below the parietal protuberances, than above them. The forehead cannot be called narrow in relation to the rest of the skull, nor can it be called a retreating forehead; on the contrary, the antero-posterior contour of the skull is well arched, so that the distance along that contour, from the nasal depres Some of the views expressed by Professor Huxley are at variance with those of other eminent scientists. Lubbock reports him as saying, "There is no mark of degradation about any part of its structure. It is, in fact, a fair average human skull, which might have belonged to a philosopher, or might have contained the thoughtless brains of a savage." Dr. Schmerling, Buchner, and Vogt are arrayed against Huxley. The first says, "I hold it to be demonstrated that this cranium has belonged to a person of limited intellectual faculties, and we conclude thence that it belonged to a man of a low degree of civilization." The cause of this wide difference of opinion may arise from the failure to observe the fact that the older the formation in which a skull is found, the lower is the type. The ordinary observer, judging by the cast of the skull, would see nothing ape-like about it, and certainly would fail to see any indications of a philosopher. NEANDERTHAL SKULL. The Neanderthal skull was taken from a small cave or grotto in-the valley of the DÜssel, near DÜsseldorf, situated about seventy miles north-east of the region of the LiÉge caverns. The grotto is in a deep ravine sixty feet above the river, one hundred feet below the surface of the country, and at a distance of about ten feet from the DÜssel River. It is fifteen feet deep from the entrance (f), which is seven or eight feet wide. Before the cavern had been injured, it opened upon a narrow plateau lying in front. The floor of the cave was covered four or five feet in thickness with a deposit of mud or loam, and containing some rounded fragments of chert. Two laborers, in removing this deposit, first noticed the skull, placed near the entrance, and further in met with the other bones. As the bones were not regarded as of any importance, at the time of their discovery, only the larger ones have been preserved. Fig. 9. a. Cavern sixty feet above the DÜssel, and one hundred feet below the surface of the country at c. Some discussion has arisen in respect to the geological time of these bones. There was no stalagmite overlying the mud or loam in which the skeleton was found, and no other bones met with save the tusk of a bear. There is no certain data given whereby its position may be known. Professor Huxley declares that the bones "indicate a very high antiquity." The diluvial or glacial origin of the Neanderthal skull is still further confirmed by the discoveries made, in the summer of 1865, in the Teufelskammer. This cavern is situated one hundred and thirty paces from the one in which the human bones were found, and on the same side of the river.. In the loam-deposit of this cave were found numerous fossil bones and teeth of the rhinoceros, cave-bear, cave-hyena, and other extinct animals. "A great part of these bones, especially those of the cave-bears, agree in color, weight, density, and the preservation of their microscopic structure, with the human bones found in the Feldhofner Cave (in which the Neanderthal man was found), and both are covered with the same dendrites, or tree-like markings." Before entering into a description and discussion of this remarkable skull, an enumeration of the other bones will be given. All the bones are characterized by their unusual thickness, and the great development of all the elevations and depressions for the attachment of muscles. The two thigh bones were in a perfect state, also the right humerus and radius; the upper third of the right ulna; the left ulna complete, though pathologically deformed, the coronoid process being so much enlarged by bony growth that flexure of the elbow beyond a right angle was impossible; the left humerus is much slenderer than the right, and the upper third is wanting. Its anterior fossa for the reception of the coronoid process is filled up with a bony growth, and, at the same time, the olecranon process is curved strongly downwards. The indications are that an injury sustained during life was the cause of this defect. There was an ilium, almost perfect; a fragment of the right scapula; the anterior extremity of a rib of the right side, and two hinder portions and one middle portion of ribs resembling more the ribs of a carnivorous animal than those of man. This Fig. 10. a. The superciliary ridge and glabella. The cranium is thus described by Professor Huxley. "It has an extreme length of 8 inches, while its breadth is only 5¾ inches, or in other words, its length is to its breadth as 100 is to 72. It is exceedingly depressed, measuring only about 3.4 inches from the glabello-occipital line to the vertex. The longitudinal arc, measured in the same way as in the Engis skull, is 12 inches; the transverse arc cannot be exactly ascertained, in consequence of the absence of the temporal bones, but was probably about the same, and certainly exceeded 10¼ inches. The horizontal circumference is 23 inches. But this great circumference arises largely from the vast development of the superciliary ridges, though the Professor Huxley describes this skull to be the most ape-like of all the human skulls he has ever seen, and in its examination ape-like characters are met with in all its parts. Professor Schaaffhausen and Dr. Buchner regarded this skull as a race-type, and Professor Huxley has said "that it truly forms only the extreme member of a series leading by slow degrees to the highest and best developed forms of human skulls." That this skull is a race-type is evident from the fact that it is not an isolated case. The fragment of the skull from the loess of the Rhine (Alsace), by its depressed forehead and strongly projecting superciliary arches, greatly resembles the Neanderthal skull. The skull from the calcareous tuff of Constatt, in its low, narrow forehead and strong superciliary arches, resembles the Neanderthal. Professor Huxley considers that the Borreby skulls, belonging to the stone age of Denmark, "show a great resemblance to the Neanderthal skull, a resemblance which is manifested in the depression of the cranium, the receding forehead, the contracted occiput and the prominent superciliary ridges." Human Skull of Arno.—The human skull, found by Professor Cocchi in the valley of the Arno, near Florence, in diluvial clay, together with various bones of extinct species of animals, is considered by Carl Vogt to be of like antiquity with the Engis and Neanderthal skulls. |