The Prehistoric World; Or, Vanished RacesAllen, Emory Adams
History
The Prehistoric World; Or, Vanished Races
Allen, Emory Adams
Archaeology; Indians; Prehistoric peoples
In view of these facts, it is not strange that no advance in
culture is noticeable; and the grounds just mentioned may go far
to explain why we catch sight, here and there, of bits of
customs, habits, and manners of life which strangely remind us of
widely distant people—though it will not explain the presence of
words of Malay or Chinese origin which are claimed to exist.30
What is known as the Eskimo trace is quite marked in the physical
characters and in the arts of the Californians.31 It is,
probably, the continuance of the type of the primitive American
race.
It would naturally be interesting to know whether any date can be
given for the Pliocene Age, and so give us some ideas as to the
antiquity of man, if he were really here during that epoch. This,
however, is one of the most difficult questions to answer, and in
the present state of our knowledge incapable of solution.
Approximations have, of course, been made, and, as might be
expected, vary greatly in results. When it was acknowledged on
all hands that on geological grounds the age of the earth was
certainly very great, many times the few thousand years hitherto
relied on, it is not strange that popular thought swung to the
other extreme, and hundreds of millions of years were thought
necessary to explain the series of changes which the geologists
unfolded. This demand for a greatly extended time was
strengthened when the law of the gradual evolution of life was
expounded by the modern school of naturalists, and as great a
lapse of time as five hundred millions of years was not deemed an
extravagant estimate. Sir William Thompson has, however,
demonstrated that the time that has elapsed since the crust of
the earth became solidified can not be far from one hundred
millions of years, and consequently we know the time since the
appearance of life must be greatly less than that number of
years.
Attempts have been made to estimate the length of time required
to form the sedimentary crust of the earth. The results are so
divergent on this point that it is best not to adopt any standard
at present. Our views on this matter are also dependent on the
time that has elapsed since the close of the Glacial Age, which,
as we have seen, is not yet a settled point. If it be true that
the islands of the Pacific commenced to sink during late Tertiary
times, then we have a measure of that time in the growth of
coral, which has required at least four hundred thousand years to
form reefs the thickness of some that are known to exist.32
Public-domain text, read in full here on John Shaqi.
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