A Preliminary Dissertation on the Mechanisms of the HeavensSomerville, Mary
Science
A Preliminary Dissertation on the Mechanisms of the Heavens
Somerville, Mary
Celestial mechanics
The height to which the tides rise is much greater in narrow channels
than in the open sea, on account of the obstructions they meet with. In
high latitudes where the ocean is less directly under the influence of
the luminaries, the rise and fall of the sea is inconsiderable, so that,
in all probability, there is no tide at the poles, or only a small
annual and monthly one. The ebb and flow of the sea are perceptible in
rivers to a very great distance from their estuaries. In the straits of
Pauxis, in the river of the Amazons, more than five hundred miles from
the sea, the tides are evident. It requires so many days for the tide to
ascend this mighty stream, that the returning tides meet a succession of
those which are coming up; so that every possible variety occurs in some
part or other of its shores, both as to magnitude and time. It requires
a very wide expanse of water to accumulate the impulse of the sun and
moon, so as to render their influence sensible; on that account the
tides in the Mediterranean and Black Sea are scarcely perceptible.
These perpetual commotions in the waters of the ocean are occasioned by
forces that bear a very small proportion to terrestrial gravitation: the
sun's action in raising the ocean is only the 1/38448000 of gravitation
at the earth's surface, and the action of the moon is little more than
twice as much these forces being in the ratio of 1 to 2.35333. From this
ratio the mass of the moon is found to be only 1/15 part of that of the
earth. The initial state of the ocean has no influence on the tides;
for whatever its primitive conditions may have been, they must soon have
vanished by the friction and mobility of the fluid. One of the most
remarkable circumstances in the theory of the tides is the assurance
that in consequence of the density of the sea being only one-fifth of
the mean density of the earth, the stability of the equilibrium of the
ocean never can be subverted by any physical cause whatever. A general
inundation arising from the mere instability of the ocean is therefore
impossible.
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