History, Ancient; Human beings -- Origin; Prehistoric peoples
The presence of the Nummulitic and other marine Eocene and Miocene
formations over such extensive areas, and at such great elevations,
is a conclusive proof that a great part of our existing continents
were then at the bottom of deep oceans. The Alps were certainly
10,000 feet lower than their present level, and the Himalayas more
so; and when this was the case a great part of Europe and Asia must
have been sea, in which only a few of the highest peaks and elevated
plateaux stood up as islands. The Pacific and Indian Oceans as well
as the Atlantic might then have poured their Gulf Streams into the
Polar basin, and prevalent southerly and westerly winds, blowing
over wide expanses of water, have deposited their vapour in genial
showers instead of in solid snow. The effect of such geographical
conditions in producing both heat and cold is admirably worked out
by Wallace in his _Island Life_, and few who read it can doubt
that Lyell was right in saying that they have been the principal
causes of the vicissitudes of climate. And here I may say a word to
express my admiration of the innate sagacity with which Lyell, many
years ago, and with comparatively few facts to work upon, sketched
out the leading lines of geology, which have been confirmed by
subsequent research. Details may have been corrected or added, but
his main theories have stood the fullest test of the survival of the
fittest. His law of the uniformity of natural causes, continued for
long intervals of time, holds the field unchallenged. These causes
may have operated a little more quickly or slowly in former ages
than at present, but they have been of the same order. The waste of
continents, instead, of averaging one foot in 4000 years, may have
averaged ten or twenty feet during certain periods, and certain
portions of the earth's crust may have been elevated or depressed at
a quicker rate than is now going on in Scandinavia; but no one any
longer believes in paroxysms throwing up mountain chains or sinking
continents below the ocean at a single blow.
In like manner later geologists have corrected details in the
distribution of land and sea suggested by Lyell to account for the
glacial period, but his main law has only received confirmation--viz.
that this distribution, and especially high land in high latitudes,
has been the principal cause of such periods.
At the same time there is a pretty general consensus of the best and
latest geologists, that, as Lyell himself suggested, elevation and
depression and other geographical changes, though the principal, are
not the sole causes of the glacial period. The main argument is, that
the phases of this period, though not exactly simultaneous over the
whole world, are too nearly so to be due to mere local movements,
and require the intervention of some general cosmic cause. We have
already seen that of such causes there is none which appears feasible
except Croll's theory of the effects of precession combined with high
eccentricity.
Public-domain text, read in full here on John Shaqi.
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