The Story of the Earth and ManDawson, John William, Sir
Science
The Story of the Earth and Man
Dawson, John William, Sir
Human beings -- Origin; Paleontology
It may be stated with certainty that the Pliocene period of geology
affords no trace of human remains or implements; and the same may I
think be affirmed of the period of glaciation and subsidence which
constitutes the earlier Post-pliocene. With the rise of the land out
of the Glacial sea indications of man are believed to appear, along
with remains of several mammalian species now his contemporaries.
Archæology and geology thus meet somewhere in the pre-historic period
of the former, and in the Post-glacial of the latter. Wherever,
therefore, human history extends farthest back, and geological
formations of the most modern periods exist and have been explored, we
may expect best to define their junctions. Unfortunately it happens
that our information on these points is still very incomplete and
locally limited. In many extensive regions, like America and
Australia, while the geological record is somewhat complete, the
historic record extends back at most a few centuries, and the
pre-historic monuments are of uncertain date. In other countries, as
in Western Asia and Egypt, where the historic record extends very far
back, the geology is less perfectly known. At the present moment,
therefore, the main battle-field of these controversies is in Western
Europe, where, though history scarce extends farther back then the
time of the Roman Republic, the geologic record is very complete, and
has been explored with some thoroughness. It is obvious, however, that
we thus have to face the question at a point where the pre-historic
gap is necessarily very wide.
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