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
Even the celebrated Halley, at the end of the seventeenth century, hollowed
out the Earth in his magnetic speculations. Men were invited to believe
that a subterranean freely-rotating nucleus occasions by its position the
diurnal and annual changes of magnetic declination. It has thus been
attempted in our own day, with tedious solemnity, to clothe in a scientific
garb the quaintly-devised fiction of the humorous Holbert.*
[footnote] *[The work referred to, one of the wittiest productions of the
learned Norwegian satirist and dramatist Holberg, was written in Latin, and
first appeared under the following title: 'Nicolai Klimii iter subterraneum
novam telluris theoriam ac historiam quintae monarchi Nicolai Klimii iter
subterraneum novam telluris theoriam ac historiam quintae monarchi ad huc
nobis incognitae exhibens e bibliotheca b. Abelini. Hafniae et Lipsiae sunt.
Jac. Preuss', 1741. An admirable Danish translation of this learned but
severe satire on the institutions, morals, and manners of the inhabitants of
the upper Earth, appeared at Copenhagen in 1789, and was entitled 'Niels
Klim's underjordiske reise ocd Ludwig Holberg, oversal after den Latinske
original of Jens Baggesen'. Holberg, who studied for a time at Oxford, was
born at Bergen in 1685, and died in 1754 as Rector of the University of
Copenhagen.] -- Tr.
p 172
The figure of the Earth and the amount of solidification (density) which it
has acquired are intimately connected with the forces by which it is
animated, in so far, at least, as they have been excited or awakened from
without, through its planetry position with reference to a luminous central
body. Compression, when considered as a consequence of centrifugal force
acting on a rotating mass, explains the earlier condition of fluidity of our
planet. During the solidification of this fluid, which is commonly
conjectured to have been gaseous and primordially heated to a very high
temperature, an enormous quantity of latent heat must have been liberated.
If the process of solidification began as Fourier conjectures, by radiation
from the cooling surface exposed to the atmosphere, the particles near the
center would have continued fluid and hot. As, after long emanation of heat
from the center toward the exterior, a stable condition of the temperature
of the Earth would at length be established, it has been assumed that with
increasing depth the subterranean heat likewise uninterruptedly increases.
The heat of the water which flows from deep borings (Artesian wells), direct
experiments regarding the temperature of rocks in mines, but, above all, the
volcanic activity of the Earth, shown by the flow of molten masses from open
fissures, afford unquestionable evidence of this increase for very
considerable depths from the upper strata. According to conclusions based
certainly upon mere analogies, this increase is probably much greater toward
the center.
Public-domain text, read in full here on John Shaqi.
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