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
41. HENCE it follows, that as we stand, our bodies are perpendicular
to the surface of the earth. Therefore in going from north to south
our bodies do not keep in a parallel direction. Now in all distances
from the pole the same length gone on the earth will not make the same
change in the position of our bodies, but the nearer we are to the
poles, we must go greater length to cause the same variation herein.
Let M I L K (in fig. 117) represent the figure of the earth, M, L the
poles, I, K two opposite points in the middle between these poles. Let
T V and P O be two arches, T V being most remote from the pole L; draw
T W, V X, P Q, O R, each perpendicular to the surface of the earth,
and let T W, V X meet in Y, and P Q, O R in S. Here it is evident,
that in passing from V to T the position of a man’s body would be
changed by the angle under T Y V, for at V he would stand in the line
Y V continued upward, and at T in the line Y T; but in passing from O
to P the position of his body would be changed by the angle under O
S P. Now I say, if these two angles are equal the arch O P is longer
than T V: for the figure M I L K being oblong, and I K longer than M L,
the figure will be more incurvated toward I than toward L; so that the
lines T W and V X will meet in Y before they are drawn out to so great
a length as the lines P Q and O R must be continued to, before they
will meet in S. Since therefore Y T and Y V are shorter than P S and S
V, T V must be less than O P. If these angles under T Y V and O S P are
each 1/90 part of the angle made by a perpendicular line, they are said
each to contain one degree. And the unequal length of these arches O P
and V T gives occasion to the assertion, that in passing from north to
south the degrees on the earth’s surface are not of an equal length,
but those near the pole longer than those toward the equator. For the
length of the arch on the earth lying between the two perpendiculars,
which make an angle of a degree with each other, is called the length
of a degree on the earth’s surface.
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