Scientific American Supplement, No. 841, February 13, 1892Various
Science
Scientific American Supplement, No. 841, February 13, 1892
Various
Science -- Periodicals
That which has deceived the adherents of the glacial theory, as
understood in its absolute sense, is, they have generally placed a too
high estimate on its extent and intensity. It needs but a little
effort of the reasoning powers to come to the conclusion that the
earth had cooled to the degree that all animal and vegetable life
could exist upon it, and that a portion of the earth's surface
permanently covered with snow and ice was absolutely indispensable to
the existence, perpetuity, and well-being of animal and vegetable
life. Again, they have attributed to the glaciers the rocks, gravels,
and other material which they have found spread here and there long
distances from the mountains. The transportation of the so-called
erratic rocks has appeared inexplicable in any other way, and the
piles of rock and gravel have been considered so many _moraines_, that
is, deposits of diverse material transported by the glaciers. They do
not regard the probability of other agents taking the place of
glaciers, and undervalue the moving power of water. Water in liquid
state has often produced analogous effects, and it has often been the
error of the glacialists to confound the one with the other. The
erratic rocks and the moraines are undoubtedly the ordinary
indications of the ancient gravels, but, taken isolatedly, they are
not sufficient proof. In order to convince they should be accompanied
with a third indication, which is the presence of striated rocks which
we find in the neighborhood of our actual glaciers. When all these
signs are together then there is hardly a possibility of error, but
one alone is not sufficient, because it can be the effect of another
cause.
Public-domain text, read in full here on John Shaqi.
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