Aspects of nature, in different lands and different climates (Vol. 1 of 2): with scientific elucidationsHumboldt, Alexander von
Science
Aspects of nature, in different lands and different climates (Vol. 1 of 2): with scientific elucidations
Humboldt, Alexander von
Physical geography; Plant morphology; Science; South America -- Description and travel
Volcanoes are quiescent for centuries before they burst forth anew;
and the idea that in the so-called older countries, a certain peace
must prevail in nature, is founded on a mere play of the imagination.
There exists no reason for assuming one entire side of our planet to
be older or newer than the other. Islands are indeed raised from the
bed of the ocean by volcanic action, and gradually heightened by coral
animals, as the Azores and many low flat islands of the Pacific; and
these may indeed be said to be newer than many Plutonic formations of
the European central chain. A small district of the earth, surrounded,
like Bohemia and Kashmeer, (and like many of the vallies in the Moon),
by annular mountains, may, by partial inundations, be long covered
with water; and after the flowing off of this lake or inland sea,
the ground on which vegetation begins gradually to establish itself
might be said, figuratively, to be of recent origin. Islands have
become connected with each other by the elevation of fresh masses of
land; and parts of the previously dry land have been submerged by the
subsidence of the oscillating ground; but submersions so general as
to embrace a hemisphere, can, from hydrostatic laws, only be imagined
as extending at the same time over all parts of the earth. The sea
cannot permanently overflow the boundless plains of the Orinoco and the
Amazons, without also overwhelming the plains adjoining the Baltic. The
sequence and identity of the sedimentary strata, and of the organic
remains of plants and animals belonging to the ancient world enclosed
in those strata, shew that several great depositions have taken place
almost simultaneously over the entire globe.” (For the fossil vegetable
remains in the coal formation in North America and in Europe, compare
Adolph Brongniart, Prodrome d’une Hist. des Végétaux Fossiles, p. 179;
and Charles Lyell’s Travels in North America, vol. ii. p. 20).
[20] p. 10.--“_The Southern Hemisphere is cooler and moister than our
Northern half of the globe._”
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