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
(8) Reference has already been made, in connection with the
distribution of plants, to the possibility that the primeval atmosphere
was richer in carbon than that of more modern times, and that this
might operate to produce diminution of radiation, and consequent
uniformity of temperature; but this cause could not have been efficient
in the later geological periods.
There may thus be said to remain two theories of those enumerated
by Wood, to which more detailed consideration may be given, namely,
numbers four and seven, which may be named respectively those of Croll
and Lyell, or the astronomical and geographical theories.
The late Mr. Croll has, in his valuable work "Climate and Time," and
in various memoirs, brought forward an ingenious astronomical theory
to account for changes of climate. This theory, as stated by himself,
is that when the eccentricity of the earth's orbit is at a high value,
and the northern winter solstice is in perihelion, agencies are
brought into operation which make the south-east trade winds stronger
than the north-east, and compel them to blow over upon the northern
hemisphere as far as the Tropic of Cancer. The result is that all the
great equatorial currents of the ocean are impelled into the northern
hemisphere, which thus, in consequence of the immense accumulation of
warm water, has its temperature raised, so that ice and snow must, to a
great extent, disappear from the Arctic regions. In the prevalence of
the converse conditions the Arctic zone becomes clad in ice, and the
southern has its temperature raised.
At the same time, according to Croll's calculations, the accumulation
of ice on either pole would tend, by shifting the earth's centre of
gravity, to raise the level of the ocean and submerge the land on the
colder hemisphere. Thus a submergence of land would coincide with a
cold condition, and emergence with increasing warmth. Facts already
referred to, however, show that this has not always been the case, but
that in many cases submergence was accompanied with the influx of warm
equatorial waters and a raised temperature, this apparently depending
on the question of local distribution of land and water; and this, in
its turn, being regulated not always by mere shifting of the centre
of gravity, but by foldings occasioned by contraction, by equatorial
subsidences resulting from the retardation of the earth's rotation, and
by the excess of material abstracted by ice and frost from the Arctic
regions, and drifted southward along the lines of arctic currents. This
drifting must in all geological times have greatly exceeded, as it
certainly does at present, the denudation caused by atmospheric action
at the equator, and must have tended to increase the disposition to
equatorial collapse occasioned by retardation of rotation.[178]
Public-domain text, read in full here on John Shaqi.
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