The Philosophy of History, Vol. 1 of 2Schlegel, Friedrich von
Philosophy
The Philosophy of History, Vol. 1 of 2
Schlegel, Friedrich von
History; History -- Philosophy
and of never exceeding those limits.
Thus to explain the fact that the habitable earth has not, as
originally, so warm a temperature as the north, we need not have
recourse to any supposition of a central fire suddenly extinguished,
like an oven that becomes cold, or to any other violent hypothesis of
the same kind; for this fact may be sufficiently accounted for by the
last great revolution of Nature--the general deluge, which as may be
assumed with great probability, produced a change in the heretofore much
purer, balmier, and more genial atmosphere. That, towards the equator,
the position of the earth's axis has undergone a change, and that
thereby this great revolution in the earth's climate was occasioned, is
indeed a bare possibility; but until further proof, this must be
regarded as a purely gratuitous hypothesis. But without subscribing to
these fanciful suppositions, and mathematical theories, and without
wishing to penetrate, with some geologists, into the hidden depths of
the earth in quest of an imagined central fire, we shall find on the
inhabited surface of the globe, or very near it, many proofs and
indications of the once superior energy of the principle of fire--a
principle whereof volcanoes whether subsisting or extinct, and the
kindred phenomena of earthquakes, may be considered the last feeble,
surviving effects; for not basalt only, but porphyry, granite, and in
general all the primary rocks, and those which, according to the
classifications of geologists, are more immediately akin to them, can be
proved to be of a volcanic nature with as much certainty, as we can
trace, in the horizontal secondary formations, the destructive influence
and operation of the element of water. Hence this layer of
subterraneous, though now in general slumbering fire, with all its
volcanic arteries and veins of earthquakes, may once have been as widely
diffused over the surface of the globe as the element of water, now
occupying so large a portion of that surface. As volcanic rocks exist in
the ocean, or rather at its bottom, and as their eruptions burst through
the body of waters up to the surface of the sea; as their volcanic
agency gives birth to earthquakes, and not unfrequently raises and
heaves up new islands from the depths of the ocean; naturalists have
concluded, with reason from these various facts, that the volcanic basis
of the earth's surface though tolerably near, must still be somewhat
deeper than the bottom of the sea. And without stopping to examine the
hypothesis relative to the immeasurable depth of the ocean, the opinion
which fixes the earth's basis at about 30,000 feet, or one geographical
mile and a half below the surface of the sea, does not exceed the modest
limits of a well-considered probability. In the present period of the
globe, water is the predominant element on the earth's surface. But if
that volcanic power which lies deeper in the bosom of the earth, and the
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