The Meeting-Place of Geology and HistoryDawson, John William, Sir
Religion
The Meeting-Place of Geology and History
Dawson, John William, Sir
Deluge; Prehistoric peoples
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.
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