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
For the generalization of cosmical views, corresponding with the plan we
have proposed to follow in giving a delineation of nature or of the
universe, the solar system to which the Earth belongs may be considered in a
two-fold relation: first, with respect to the different classes of
individually agglomerated matter, and the relative size, conformation,
density, and distance of the heavenly bodies of this system; and secondly,
with reference to other portions of our starry cluster, and of the changes
of position of its central body, the Sun.
The solar system, that is to say, the variously-formed matter circling round
the Sun, consists, according to the present state of our knowledge of
'eleven primary planets',* eighteen satellites
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or secondary planets, and myriads of comets, three of which, known as the
"planetary comets," do not pass beyond the narrow limits of the orbits
described by the principal planets.
[footnote] * (Since the publication of Baron Humboldt's work in 1845,
several other planets have been discovered, making the number of those
belonging to our planetary system 'sixteen' instead of 'eleven'. Of these,
Astrea, Hebe, Flora, and Iris are members of the remarkable group of
asteroids between Mars and Jupiter. Astrea and Hebe were discovered by
Hencke at Driesen, the one in 1846 and the other in 1847; Flora and Iris
were both discovered in 1847 by Mr. Hind, at the South Villa Observatory,
Regent's Park. It would appear from the latest determinations of their
elements, that the small planets have the following order with respect to
mean distance from the Sun: Flora, Iris, Vesta, Hebe, Astrea, Juno, Ceres,
Pallas. Of these, Flora has the shortest period (about 3 1/4 years). The
planet Neptune, which, after having been predicted by several astronomers,
was actually observed on the 25th of September, 1846, is situated on the
confines of our planetary system beyond Uranus. The discovery of this
planet is not only highly interesting from the importance attached to it as
a question of science, but also from the evidence it affords of the care and
unremitting labor evinced by modern astronomers in the investigation and
comparison of the older calculations, and the ingenious application of the
results thus obtained to the observation of new facts. The merit of having
paved the way for the discovery of the planet Neptune is due to M. Bouvard,
who, in his persevering and assiduous efforts to deduce the entire orbit of
Uranus from observations made during the forty years that succeeded the
discovery of that planet in 1781, found the results yielded by theory to be
at variance with fact, in a degree that had no parallel in the history of
astronomy. This startling discrepancy, which seemed only to gain additional
weight from every attempt made by M. Bouvard to correct his calculations,
led Leverrier, after a careful modification of the tables of Bouvard, to
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