Man and the Glacial PeriodWright, G. Frederick (George Frederick)
History
Man and the Glacial Period
Wright, G. Frederick (George Frederick)
Glacial epoch; Prehistoric peoples
[Footnote BH: American Journal of Science, vol. cxxxii, 1886, p. 77.]
When, now, we attentively consider the combination of causes necessary to
produce the climatic conditions of the great Ice age of North America, we
shall be prepared to find far more extensive variations in the progress
of the continental glacier, both during its advance and during its
retreat, than are to be observed in any existing local glaciers.
With respect to the arguments adduced in favor of a succession of glacial
epochs in America the following criticisms are pertinent:
1. So far as we can estimate, a temporary retreat of the front, lasting
a few centuries, would be sufficient to account for the vegetable
accumulations that are found buried beneath the glacial deposits in
southern Ohio, Indiana, central Illinois, and Iowa, while a temporary
readvance of the ice would be sufficient to bury the vegetable remains
beneath a freshly accumulated mass of till. Thus, as Dr. Bell suggested,
the interglacial vegetal deposits do not necessarily indicate anything
more than a temporary oscillation of the ice-front, and do not carry
with them the necessity of supposing a disappearance of the ice from the
whole glaciated area. Thus the introduction of a whole Glacial period to
account for such limited phenomena is a violation of the well-known law
of parsimony, which requires us in our explanations of phenomena to be
content with the least cause which is sufficient to produce them. In the
present instance a series of comparatively slight oscillations of the
ice-front during a single glacial period would seem to be sufficient to
account for all the buried forests and masses of vegetal _débris_ that
occur either in the United States or in the Dominion of Canada.
Public-domain text, read in full here on John Shaqi.
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