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
Setting aside, then, these assumptions, which proceed from incorrect or
insufficient information, we may now refer to a consideration of the
utmost importance, and which Mr. Croll himself, though he adduces it
only in aid of the astronomical theory of glacial periods, has treated
in so masterly a manner, as really to give it the first place as an
efficient cause. This is the varying distribution of ocean currents,
in connection with the differences in the elevation and distribution
of land. The great equatorial current, produced by the action of the
solar heat on the atmosphere and the water, along with the earth's
rotation, is thrown, by opposing continental shores, northward into
the Atlantic and Pacific in the Gulf Stream and Japan current, giving
us a hot-water apparatus which effectually raises the temperature of
the whole northern hemisphere, and especially of the western sides of
the continents. Mr. Croll imagined that if his astronomical causes
could, to ever so small an extent, intensify the action of these
currents, or their determination to the north, we should have a period
of warmth, while a similar advantage given to the southern hemisphere
would produce a glacial age in the north. But this requires us to
assume what ought to be proved; namely, that the position of aphelion,
and the increase or decrease of eccentricity, would actually so swing
the equatorial current to the north or south. It further requires us
to assume--and this is the most important defect of the theory--that
no change occurs in the distribution of land and water; because
any important change of this kind might obviously exert a dominant
influence on the currents. Let us take two examples in illustration of
this.
Public-domain text, read in full here on John Shaqi.
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