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
5. The absolute date of the first appearance of man cannot perhaps be
fixed within a few years or centuries, either by human chronology or by
the science of the earth. It would seem, however, that the Bible
history, as well as such hints as we can gather from the history of
other nations, limits us to two or three thousand years before the
Deluge of Noah, while some estimates of the antiquity of man, based on
physical changes or ancient history, or on philology, greatly exceed
this limit. If the earliest men were those of the river gravels and
caves, men of the 'mammoth age,' or of the 'palæolithic' or palæocosmic
period, we can form some definite ideas as to their possible antiquity.
They colonised the continents immediately after the elevation of the
land from the great subsidence which closed the pleistocene or glacial
period, in what has been called the 'continental' period of the
post-glacial age, because the new lands then raised out of the sea
exceeded in extent those which we have now. We have, as stated in a
previous chapter, some measures of the date of this great continental
elevation, and know that its distance from our time must fall within
about eight thousand years. Many indications, both in Europe and
America, lead to the belief that it is physically impossible that man
could have colonised the northern hemisphere at an earlier date than
this geologically recent continental period.
6. There is but one species of man, though many races and varieties; and
these races or varieties seem to have developed themselves at a very
early time and have shown a remarkable fixity in their later history.
There is reason to believe, however, from various physiological facts,
that this is a very general law of varietal forms, which are observed to
appear rapidly or suddenly, and then in favourable circumstances to be
propagated continuously. It would seem also to apply to the introduction
of forms regarded as species, since it is not unusual to find a genus at
or near its origin represented by its maximum number of specific forms.
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