A View of Sir Isaac Newton's PhilosophyPemberton, Henry
Science
A View of Sir Isaac Newton's Philosophy
Pemberton, Henry
Newton, Isaac, 1642-1727. Principia
42. THIS figure of the earth has some effect on eclipses. It has been
observed above, that sometimes the nodes of the moon’s orbit lie in a
straight line drawn from the sun to the earth; in which case the moon
will cross the plane of the earth’s motion at the new and full. But
whenever the moon passes near the plane at the full, some part of the
earth will intercept the sun’s light, and the moon shining only with
light borrow’d from the sun, when that light is prevented from falling
on any part of the moon, so much of her body will be darkened. Also
when the moon at the new is near the plane of the earth’s motion, the
inhabitants on some part of the earth will see the moon come under
the sun, and the sun thereby be covered from them either wholly or in
part. Now the figure, which we have shewn to belong to the earth, will
occasion the shadow of the earth on the moon not to be perfectly round,
but cause the diameter from east to west to be somewhat longer than
the diameter from north to south. In eclipse of the sun this figure
of the earth will make some little difference in the place, where the
sun shall appear wholly or in any given part covered. Let A B C D (in
fig. 118.) represent the earth, A C the axis whereon it turns daily,
E the center. Let F A G C represent a perfect globe inscribed within
the earth. Let H I be a line drawn through the centers of the sun and
moon, crossing the surface of the earth in K, and the surface of the
globe inscribed in L. Draw E L, which will be perpendicular to the
surface of the globe in L: and draw likewise K M, so that it shall
be perpendicular to the surface of the earth in K. Now whereas the
eclipse would appear central at L, if the earth were the globe A G C
F, and does really appear so at K; I say, the latitude of the place K
on the real earth is different from the latitude of the place L on the
globe F A G C. What is called the latitude of any place is determined
by the angle which the line perpendicular to the surface of the earth
at that place makes with the axis; the difference between this angle,
and that made by a perpendicular line or square being called the
latitude of each place. But it might here be proved, that the angle
which K M makes with M C is less, than the angle made between L E and
E C: consequently the latitude of the place K is greater, than the
latitude, which the place L would have.
43. THE next effect, which follows from this figure of the earth,
is that gradual change in the distance of the fixed stars from the
equinoctial points, which astronomers observe. But before this can be
explained, it is necessary to say something more particular, than has
yet been done, concerning the manner of the earth’s motion round the
sun.
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