The human skeleton from the undisturbed loess of the Rhine, near Lahr, was found in nearly a horizontal position, but in such a manner as to forbid the idea of sepulchre. These bones were exhumed from a perpendicular cliff of solid loess, about five feet high. The town of Lahr is situated four miles from, and about one hundred feet above, the Rhine, and not far from the tributary valley drained by the Schutter, flowing from the Black Forest.

In the alluvial plain into which the Schutter flows the the loess is two hundred feet thick. The loess rises eighty feet above the Schutter. At Lahr it has been denuded so as to form a succession of terraces on the right bank. It was in the lowest of these from which the skeleton was taken. Immediately below this bed there were found pebbles, and still lower down was a bed of gravel containing rounded stones of sandstone and gneiss from the Black Forest.

There are several interesting facts connected with this discovery. M. Boué considers that the loess of the Lahr is continuous with that of the Rhine, and before the loess had been denuded there was not less than eighty feet of loamy deposit above the human skeleton. The glaciers had deposited their great gravel beds, and had began to melt. The melting of them had formed a mixture of loam and gravel. Then when the torrents poured forth from the glaciers the loam was formed without the pebbles. The unfortunate man, whose remains were found, was buried far beneath the surface, during the very first part of the course of the violent streams pouring forth from the field of ice. The glaciers were then on the retreat, and the incautious man probably fell a victim while on the chase.[20]

The cave of La Naulette, Belgium, afforded a jaw-bone similar to the Moulin-Quignon. The bone came from a river deposit of loam covered with a layer of stalagmite, and at a depth of thirteen feet from the surface. Associated with it were the remains of the mammoth, woolly-haired rhinoceros, and flint implements. These implements present the same type as those of St. Acheul. With this jaw were also found a human ulna, two human teeth, and a fragment of a worked reindeer born. This jaw-bone is very thick, round in form, and the projection of the chin is almost entirely absent. The chin is said to hold an intermediate position between that of the animals and those of the present race of men. The cavities for the reception of the canine teeth are very wide, and one of the most remarkable things is that the three molars are reversed, that is the first true molar is the smallest, and the last the largest. The inner surface of the jaw at the point of the suture or symphysis, forms a line obliquely directed upwards. Taking the jaw all in all, it is the most ape-like human jaw ever discovered.[21]

The flint implements from Hoxne were found under three different layers or beds. The first, vegetable, a foot and a half in depth. The second was clay, seven and a half feet thick. The third, a bed of sand, with shells one foot in thickness. The fourth layer, containing the implements was a bed of gravel two feet in depth. The number of these flints was so great that they were carried out by the baskets-full, and thrown into the ruts of the adjoining road. On account of the great number, this spot might have been the place where they were manufactured. Their date is not coeval with the bowlder clay, but undoubtedly belong, to the last of this epoch.

The human bones found in the loess of the Rhine, near Colmar, were two fossilized fragments of the skull. They were found in undisturbed soil along with the fossil bones of the extinct species of mammoth, horse, gigantic deer, aurochs, and other mammalia. The fragment of the skull "showed a depressed forehead, strongly projecting superciliary arches, and a type, on the whole, approaching the so-called dolichocephalic, or long-headed form."[22] These remains date so near the end of the glacial as to almost enter the inter-glacial.


CHAPTER III.

GLACIAL EPOCH—CONTINUED.