On the Connexion of the Physical SciencesSomerville, Mary
Science
On the Connexion of the Physical Sciences
Somerville, Mary
Physical sciences; Science
The moon is flattened at her poles from her centrifugal force, therefore
her polar axis is the least. The other two are in the plane of her
equator, but that directed towards the earth is the greatest (N. 142).
The attraction of the earth, as if it had drawn out that part of the
moon’s equator, constantly brings the greatest axis, and consequently
the same hemisphere, towards us, which makes her rotation participate in
the secular variations of her mean motion of revolution. Even if the
angular velocities of rotation and revolution had not been nicely
balanced in the beginning of the moon’s motion, the attraction of the
earth would have recalled the greatest axis to the direction of the line
joining the centres of the moon and earth; so that it would have
vibrated on each side of that line in the same manner as a pendulum
oscillates on each side of the vertical from the influence of
gravitation. No such libration is perceptible; and, as the smallest
disturbance would make it evident, it is clear that, if the moon has
ever been touched by a comet, the mass of the latter must have been
extremely small. If it had been only the hundred thousandth part of that
of the earth, it would have rendered the libration sensible. According
to analysis, a similar libration exists in the motions of Jupiter’s
satellites, which still remains insensible to observation, and yet the
comet of 1770 passed twice through the midst of them.
The moon, it is true, is liable to librations depending upon the
position of the spectator. At her rising, part of the western edge of
her disc is visible, which is invisible at her setting, and the contrary
takes place with regard to her eastern edge. There are also librations
arising from the relative positions of the earth and moon in their
respective orbits; but, as they are only optical appearances, one
hemisphere will be eternally concealed from the earth. For the same
reason the earth, which must be so splendid an object to one lunar
hemisphere, will be for ever veiled from the other. On account of these
circumstances, the remoter hemisphere of the moon has its day a
fortnight long, and a night of the same duration, not even enlightened
by a moon, while the favoured side is illuminated by the reflection of
the earth during its long night. A planet exhibiting a surface thirteen
times larger than that of the moon, with all the varieties of clouds,
land, and water, coming successively into view, must be a splendid
object to a lunar traveller in a journey to his antipodes. The great
height of the lunar mountains probably has a considerable influence on
the phenomena of her motion, the more so as her compression is small,
and her mass considerable. In the curve passing through the poles, and
that diameter of the moon which always points to the earth, nature has
furnished a permanent meridian, to which the different spots on her
surface have been referred, and their positions are determined with as
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