Cosmos: A Sketch of the Physical Description of the Universe, Vol. 1Humboldt, Alexander von
History
Cosmos: A Sketch of the Physical Description of the Universe, Vol. 1
Humboldt, Alexander von
Astronomy; Cosmography; Physical geography; Science -- History
In a general view of nature, all these phenomena are fused together in one
sole idea of the reaction of the interior of a planet on its external
surface. We thus recognize in the depths of the earth, and in the increase
of temperature with the increase of depth from the surface, not only the
germ of disturbing movements, but also of the gradual elevation of whole
continents (as mountain chains on long fissures), of volcanic eruptions, and
of the manifold production of mountains and mineral masses. The influence
of this reaction of the interior on the exterior is not, however, limited to
inorganic nature alone. It is highly probable that, in an earlier world,
more powerful emanations of carbonic acid gas, blended with the atmosphere,
must have increased the assimilation of carbon in vegetables, and that an
inexhaustible supply of combustible matter (lignites and carboniferous
formations) must have been thus buried in the upper strata of the earth by
the revolutions attending the destruction of vast tracts of forest. We
likewise perceive that the destiny of mankind is in part dependent on the
formation of the external surface of the earth, the direction of mountain
tracts and high lands, and on the distribution of elevated continents. It
is thus granted to the inquiring mind to pass from link to link along the
chain of phenomena until it reaches the period when, in the solidifying
process of our planet, and in its first transition from the gaseous form to
the agglomeration of matter, that portion of the inner heat of the Earth was
developed, which does not belong to the action of the Sun.
This material taken from pages 204-248
COSMOS: A Sketch of the Physical Description of the Universe, Vol. 1
by Alexander von Humboldt
Translated by E C Otte
from the 1858 Harper & Brothers edition of Cosmos, volume 1
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p 204
In order to give a general delineation of the causal connection of
geognostical phenomena, we will begin with those whose chief characteristic
is dynamic, consisting in motion and in change in space. Earthquakes
manifest themselves by quick and successive vertical, or horizontal, or
rotatory vibrations.*
[footnote] *[See Daubeney 'On Volcanoes', 2d ed., 1848, p. 509.] -- Tr.
Public-domain text, read in full here on John Shaqi.
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