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Mitchell, P. Chalmers (Peter Chalmers), 1864-1945

"Thomas Henry Huxley; A Sketch Of His Life And Work"

The continued progress of geology, and the
sturdy championship of it by men like Sedgwick, Chalmers, and Buckland,
who were at the same time reputable theologians and distinguished men of
science, had decided the battle in favour of the conclusions of science,
and it was accepted generally that the earth was almost indefinitely
old. At the same time, another and more strictly scientific dispute had
been in progress. The older school of geologists, looking on the face of
the world, and seeing it scarred by mighty fissures, displaying huge
distortions of the beds in the crust, had argued that geological change
had taken place by a series of mighty catastrophes. The tremendous
results which they saw seemed to them only possible on the theory that
unusual and gigantic displays of force had caused them. On the other
hand, Hutton and Lyell attempted to find adequate explanation of the
greatest changes in the slow forces which may be seen in operation at
the present time. Slow movements of upheaval and depression, amounting
at most to an inch or two in a century, may be shown to be actually in
existence now, and such slow changes acting for very many centuries
would account for the raising of continents above the sea, so that old
sea-bottoms became the surface of the land, and for the depression of
land areas so that new sedimentary rocks might be deposited upon them.


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