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
Scientific superstitions, understanding by this name the reception
of hypotheses of prominent men, and using these as fetishes to be
worshipped and to be employed in miraculous works, are scarcely less
common in our time than superstitions of another kind were in darker
ages. One of these which has been dominant for a long time in geology,
and has scarcely yet run its course, is that of the Great Ice Age,
with its accompaniments of Continental Glaciers and Polar Ice Cap.
The cause of this it is not difficult to discern. The covering of
till, gravel and travelled boulders which encumbers the surface of the
northern hemisphere from the Arctic regions more than half way to the
equator, had long been a puzzle to geologists, and this was increased
rather than diminished when the doctrine of appeal to recent causes on
the principle of uniformity became current. It was seen that it was
necessary to invoke the action of ice in some form to account for these
deposits, and it was at the same time perceived that there was much
evidence to prove that between the warm climate of the early Tertiary
and the more subdued mildness of the modern time there had intervened a
period of unusual and extreme cold. In this state of affairs attention
was attracted to the Alpine glaciers. Their movement, their erosion
of surfaces, their heaping up of moraines bearing some resemblance to
the widely extended boulder deposits, their former greater extension,
as indicated by old moraines at lower levels than those in process of
formation, were noted. Here was a modern cause capable of explaining
all the phenomena. Men's minds were taken by storm, and as always
happens in the case of new and important discoveries, the agency of
glaciers was pushed at once far beyond the possibilities of their
action under any known physical or climatal laws. This exaggerated idea
of the action of land ice in the form of glaciers is not yet exploded,
more especially in the United States, where official sanction has been
given to it by the Geological Survey, and where it has been introduced
even into school and college text-books. It affords also a telling
bit of scientific sensationalism, which can scarcely be resisted by a
certain class of popular writers. America has also afforded greater
facilities for extreme theories of this kind, owing to the wide and
uninterrupted distribution of glacial deposits, and the more simple
and less broken character of its great internal plateau, while the
influence of great leading minds, like those of the elder Agassiz and
of Dana, naturally held sway over the younger geologists. Fortunately
Canada, which possesses the larger and more northern half of the
North American continent; though numerically inferior, and therefore
overborne in the discussion, has, in the main, remained steadfast to
facts rather than to specious theories, and has been confirmed in this
position by the clearer testimony of nature in a region where many of
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