Island Life; Or, The Phenomena and Causes of Insular Faunas and FlorasWallace, Alfred Russel
Science
Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras
Wallace, Alfred Russel
Biogeography; Glacial epoch; Island ecology
than under-estimate the possible rate of deposit.[42]
Now a coast line of 100,000 miles with a width of 30 gives an area of
3,000,000 square miles, on which the denuded matter of the whole land-area
of 57,000,000 square {112} miles is deposited. As these two areas are as 1
to 19, it follows that deposition, as measured by _maximum_ thickness, goes
on at least nineteen times as fast as denudation--probably very much
faster. But the mean rate of denudation over the whole earth is about one
foot in three thousand years; therefore the rate of maximum deposition will
be at least 19 feet in the same time; and as the total maximum thickness of
all the stratified rocks of the globe is, according to Professor Haughton,
177,200 feet, the time required to produce this thickness of rock, at the
present rate of denudation and deposition, is only 28,000,000 years.[43]
_The Rate of Geological Change Probably Greater in very Remote Times._--The
opinion that denudation and deposition went on more rapidly in earlier
times owing to the frequent occurrence of vast convulsions and cataclysms
was strenuously opposed by Sir Charles Lyell, who so well showed that
causes of the very same nature as those now in action were sufficient to
account for all the phenomena presented by the rocks throughout the whole
series of geological formations. But while upholding the soundness of the
views of the "uniformitarians" as opposed to the "convulsionists," we must
yet admit that there is reason for believing in a gradually increasing
intensity of all telluric action as we go back into past time. This subject
has been well treated by Mr. W. J. Sollas,[44] who shows that, if, as all
physicists maintain, the sun gave out perceptibly more heat in past ages
than now, this alone would cause an increase in almost all the forces that
have brought about geological phenomena. With greater heat there would be a
more extensive aqueous atmosphere, and, perhaps, a greater difference
between equatorial and polar temperatures; hence more violent winds,
heavier rains and snows, {113} and more powerful oceanic currents, all
producing more rapid denudation. At the same time, the internal heat of the
earth being greater, it would be cooling more rapidly, and thus the forces
of contraction--which cause the upheaving of mountains, the eruption of
volcanoes, and the subsidence of extensive areas--would be more powerful
and would still further aid the process of denudation. Yet again, the
earth's rotation was certainly more rapid in very remote times, and this
would cause more impetuous tides and still further add to the denuding
power of the ocean. It thus appears that, as we go back into the past,
_all_ the forces tending to the continued destruction and renewal of the
earth's surface would be in more powerful action, and must therefore tend
to reduce the time required for the deposition and upheaval of the various
geological formations. It may be true, as many geologists assert, that the
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