Cave Hunting: Researches on the evidence of caves respecting the early inhabitants of EuropeDawkins, William Boyd
History
Cave Hunting: Researches on the evidence of caves respecting the early inhabitants of Europe
Dawkins, William Boyd
Antiquities, Prehistoric -- Europe; Caves -- Europe; Europe -- Antiquities; Prehistoric peoples -- Europe
The discovery of a rudely chipped implement of quartzite, of the
pointed oval shape common in the gravels of Britain and France,
published by Mr. Medlicott in 1873, in the “Records of the Geological
Survey of India,” proves further that man was a member of the
remarkable fauna which inhabited the valley of the Narbadá in ancient
times. It was dug out of reddish unstratified clay by Mr. Hacket at a
depth of three feet from the upper surface, which was covered by twenty
feet of ossiferous gravel, on the left bank of the Narbadá near the
valley of Bhutra. The clay belongs to the same fluviatile series as
that from which the mammalia were obtained and named by Dr. Falconer in
1828. Both clay and gravel are shown to be of fluviatile origin, by the
presence of fresh-water mussels of the varieties still living in the
adjacent river.
The fossil bones belong to extinct and living animals. Among the
former are two kinds of elephant (_E. namadicus_) and (_E. stegodon
insignis_), one of which is closely allied to the European _E.
antiquus_, two species of hippopotamus, one (_H. palæindicus_) with
four incisors in front of the jaws like the African, and a second with
six incisors belonging to the extinct division of hexaprotodon, a
large ox (_Bos namadicus_), a deer and a bear. The living forms are
represented by the buffalo (_Bubalus namadicus_), which is identical
with the wild arnee from which the Indian domestic buffaloes have
descended, and the gavial, or long-snouted Gangetic crocodile. This
imperfect list, borrowed from Dr. Falconer,[272] shows that there is
the same mixture of extinct with living forms in the valley of the
Ganges, while the clays and gravels were being accumulated, as we
have observed in the pleistocene deposits of Europe, and the fauna
may therefore be referred to the pleistocene age, and probably, as
Mr. Medlicott proposes, to the late division of that age. The exact
correspondence of the quartzite implements with those which are so
abundant in the European river-strata of the same age, adds additional
weight to this conclusion.
_Are the Palæolithic Aborigines of India related to those of Europe?_
It is not a little remarkable that Dr. Falconer, writing in 1865 of the
peculiar fauna of the Narbadá, should have held the view that man was
living in India at that time, and that the memory of the hippopotamus
was handed down in Aryan traditions, under the striking name of the
water elephant. “After reflecting,” he writes, “on the question during
many years in its palæontological and ethnological bearings, my leaning
is to the view that _Hippopotamus namadicus_ was extinct in India long
before the Aryan invasion, but that it was familiar to the earlier
indigenous races.” (ii. p. 644.) This inference is proved to be
literally true by the discovery of the palæolithic implements in the
ossiferous strata of the Narbadá, which must have required long ages
for their accumulation and subsequent erosion.
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