Meteoric astronomy: A treatise on shooting-stars, fire-balls, and aerolitesKirkwood, Daniel
Science
Meteoric astronomy: A treatise on shooting-stars, fire-balls, and aerolites
Kirkwood, Daniel
Meteors
In regard to the physical history of those meteoric masses which,
in such infinite numbers, traverse the interplanetary spaces, our
knowledge is exceedingly limited. Such as have reached the earth's
surface consist of various elements in a state of combination. It
has been remarked, however, by a distinguished scientist[32] that
"the character of the constituent particles of meteorites, and their
general microscopical structure, differ so much from what is seen
in terrestrial volcanic rocks, that it appears extremely improbable
that they were ever portions of the moon, or of a planet, which
differed from a large meteorite in having been the seat of a more or
less modified volcanic action." As the celebrated nebular hypothesis
seems to afford a very probable explanation of the origin of those
bodies, whether in the form of rings or sporadic masses, its brief
consideration may not be destitute of interest. We will merely premise
that the existence of true nebulæ in the heavens--that is, of matter
consisting of luminous gas--has been placed beyond doubt by the
revelations of the spectroscope.
As a group, our solar system is comparatively isolated in space; the
distance of the nearest fixed star being at least seven thousand times
that of Neptune, the most remote known planet. Besides the central or
controlling orb, it contains, so far as known at present, ninety-nine
primary planets, eighteen satellites, three planetary rings, and nearly
eight hundred comets. In taking the most cursory view of this system we
cannot fail to notice the following interesting facts in regard to the
motions of its various members:
1. The sun rotates on his axis from west to east.
2. The primary planets all move nearly in the plane of the sun's
equator.
3. The orbital motions of all the planets, primary and secondary,
except the satellites of Uranus and Neptune, are in the same
_direction_ with the sun's rotation.
4. The direction of the rotary motions of all the planets, primary and
secondary, in so far as has been observed, is identical with that of
their orbital revolutions; viz., from west to east.
5. The rings of Saturn revolve about the planet in the same direction.
6. The planetary orbits are all nearly circular.
7. The _cometary_ is distinguished from the _planetary_ portion of the
system by several striking characteristics: the orbits of comets are
very eccentric and inclined to each other, and to the ecliptic at all
possible angles. The motions of a large proportion of comets are _from
east to west_. The physical constitution of the latter class of bodies
is also very different from that of the former; the matter of which
comets are composed being so exceedingly attenuated, at least in some
instances, that fixed stars have been distinctly visible through what
appeared to be the densest portion of their substance.
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