The Prehistoric World; Or, Vanished RacesAllen, Emory Adams
History
The Prehistoric World; Or, Vanished Races
Allen, Emory Adams
Archaeology; Indians; Prehistoric peoples
Mr. Skertchly, of the Geological Survey of England, has furnished
still another estimate, based on the growth of the Fen-beds on
the east coast of England. It is sufficient to state that he also
arrives at an estimate of about seven thousand years for the
Neolithic period.21 Now these results are interesting, and their
substantial agreement is, to say the least, striking. We must
remember, however, that none of them are free from error. They
may serve to clear up our thoughts on this subject, but we notice
they tell us nothing as to the beginning of the Neolithic Age.
Abandoning the effort to obtain dates for the various ages,
attempts have been made to calculate the entire interval that has
elapsed since the close of the Glacial times, and thus set bounds
to the first appearance of Neolithic man. We briefly touched on
this question in determining the antiquity of the Paleolithic
Age, and we say, as far as this country was concerned, it was
comparatively a recent thing, but as for Europe, it must be at a
very remote time. M. Quatrefages has called our attention to two
investigations in Europe, which, in order to understand this
question, we will now glance at. The waters of the Rhone carry
into Lake Geneva every year quantities of sediment. In other
words, from this and other sources, the lake is gradually being
filled up. Carefully calculating the amount carried into the lake
in a year, estimates have been made of the length of time it has
taken the river to fill up the lake as much as it has.
But in making this calculation the date arrived at was a maximum
one—that is, a point beyond which it is not reasonable to suppose
the time extended. These calculations gave as a result one
hundred thousand years. The meaning of this is that the time
elapsed since the close of the Glacial Age was something less
than the number just stated. On the other hand, a minimum date
for this time has been obtained by estimating the amount of
erosion in the valley of the River Saone, in France. From this we
know that the time can not be less than seven thousand years.22
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