The English works of Thomas Hobbes of Malmesbury, Volume 01 (of 11) — Thomas Hobbes — John Shaqi
The English works of Thomas Hobbes of Malmesbury, Volume 01 (of 11)
Thomas Hobbes · en
As for the spring tides which happen at the time of the new and full
moons, they are caused by that simple motion, which at the beginning I
supposed to be always in the moon. For as, when I showed the cause of
the eccentricity of the earth, I derived the elevation of the waters
from the simple motion of the sun; so the same may here be derived from
the simple motion of the moon. For though from the generation of clouds,
there appear in the sun a more manifest power of elevating the waters
than in the moon; yet the power of increasing moisture in vegetables and
living creatures appears more manifestly in the moon than in the sun;
which may perhaps proceed from this, that the sun raiseth up greater,
and the moon lesser drops of water. Nevertheless, it is more likely, and
more agreeable to common observation, that rain is raised not only by
the sun, but also by the moon; for almost all men expect change of
weather at the time of the conjunctions of the sun and moon with one
another and with the earth, more than in the time of their quarters.
In the last place, the cause why the spring tides are greater at the
time of the equinoxes hath been already sufficiently declared in this
article, where I have demonstrated, that the two motions of the earth,
namely, its simple motion in the little circle _l b k c_, and its
diurnal motion in _l d k e_, cause necessarily a greater elevation of
waters when the sun is about the equinoxes, than when he is in other
places. I have therefore given possible causes of the phenomenon of the
flowing and ebbing of the ocean.
[Sidenote: Cause of the precession of the equinoxes.]
11. As for the explication of the yearly _precession of the equinoctial
points_, we must remember that, as I have already shown, the annual
motion of the earth is not in the circumference of a circle, but of an
ellipsis, or a line not considerably different from that of an ellipsis.
In the first place, therefore, this elliptical line is to be described.