Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
The late Dr. Newmayr, of Vienna, a veteran physical geographer, in
an able discussion of the climates of past ages, one of his last
scientific papers, has fallen back on the hypothesis of a change in
the position of the poles.[181] His failure to account for ancient
climates by other causes evidently, however, depends on an inadequate
conception of the effects of geographical changes, along with serious
misconceptions as to the distribution of plants and the characters of
vegetation at different periods. These points we shall have to discuss
in subsequent pages.
[181] _Society for Dissemination of Natural Science._ Vienna, January,
1889.
In an address before the American Association, in 1886, Dr.
Chamberlain, one of the ablest American authorities on the Glacial
period, makes the following remarks as to the causes of the Pleistocene
cold:--
"If we turn to the broader speculations respecting the origin of the
Glacial epoch, we find our wealth little increased. We have on hand
practically the same old stock of hypotheses, all badly damaged by
the deluge of recent facts. The earlier theory of northern elevation
has been rendered practically valueless; and the various astronomical
hypotheses seem to be the worse for the increased knowledge of the
distribution of the ancient ice sheet. Even the ingenious theory
of Croll becomes increasingly unsatisfactory as the phenomena are
developed into fuller appreciation. The more we consider the asymmetry
of the ice distribution in latitude and longitude, and its disparity
in elevation, the more difficult it becomes to explain the phenomena
upon any astronomical basis. If we were at liberty to disregard the
considerations forced upon us by physicists and astronomers, and
permit ourselves simply to follow freely the apparent leadings of the
phenomena, it appears at this hour as though we should be led upon an
old and forbidden trail,--the hypothesis of a wandering pole. It is
admitted that there is a _vera causa_ in elevations and depressions of
the earth's crust, but it is held inadequate. It is admitted that the
apparent changes of latitude shown by the determinations of European
and American observatories are remarkable, but their trustworthiness
is challenged. Were there no barriers against free hypotheses in
this direction, glacial phenomena could apparently find adequate
explanation; but debarred--as we doubtless should consider ourselves to
be at present--from this resource, our hypotheses remain inharmonious
with the facts, and the riddle remains unsolved."
It should be observed here that the unsolved "riddle" is that of a
continental ice sheet. This, as we have already seen, is probably
insoluble in any way, but fortunately needs no solution, being merely
imaginary. If we adopt a moderate view as to the actual conditions of
the Pleistocene, the geographical theory will be found quite sufficient
to account for the facts.
Public-domain text, read in full here on John Shaqi.
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