Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent AstronomersOlmsted, Denison
Science
Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent Astronomers
Olmsted, Denison
Astronomy
The _precession of the equinoxes_ is a slow but continual shifting of
the equinoctial points, from east to west. Suppose that we mark the
exact place in the heavens where, during the present year, the sun
crosses the equator, and that this point is close to a certain star;
next year, the sun will cross the equator a little way westward of that
star, and so every year, a little further westward, until, in a long
course of ages, the place of the equinox will occupy successively every
part of the ecliptic, until we come round to the same star again. As,
therefore, the sun revolving from west to east, in his apparent orbit,
comes round to the point where it left the equinox, it meets the equinox
before it reaches that point. The appearance is as though the equinox
_goes forward_ to meet the sun, and hence the phenomenon is called the
_precession_ of the equinoxes; and the fact is expressed by saying, that
the equinoxes retrograde on the ecliptic, until the line of the
equinoxes (a straight line drawn from one equinox to the other) makes a
complete revolution, from east to west. This is of course a retrograde
motion, since it is contrary to the order of the signs. The equator is
conceived as _sliding_ westward on the ecliptic, always preserving the
same inclination to it, as a ring, placed at a small angle with another
of nearly the same size which remains fixed, may be slid quite around
it, giving a corresponding motion to the two points of intersection. It
must be observed, however, that this mode of conceiving of the
precession of the equinoxes is purely imaginary, and is employed merely
for the convenience of representation.
The amount of precession annually is fifty seconds and one tenth;
whence, since there are thirty-six hundred seconds in a degree, and
three hundred and sixty degrees in the whole circumference of the
ecliptic, and consequently one million two hundred and ninety-six
thousand seconds, this sum, divided by fifty seconds and one tenth,
gives twenty-five thousand eight hundred and sixty-eight years for the
period of a complete revolution of the equinoxes.
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