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
a compression of the earth towards the poles.
Mean-while, Bouguer and his party were prosecuting a similar work in
Peru, under extraordinary difficulties. These were caused, partly by the
localities, and partly by the ill-will and indolence of the inhabitants.
The place selected for their operations was in an elevated valley
between two principal chains of the Andes. The lowest point of their arc
was at an elevation of a mile and a half above the level of the sea;
and, in some instances, the heights of two neighboring signals differed
more than a mile. Encamped upon lofty mountains, they had to struggle
against storms, cold, and privations of every description, while the
invincible indifference of the Indians, they were forced to employ, was
not to be shaken by the fear of punishment or the hope of reward. Yet,
by patience and ingenuity, they overcame all obstacles, and executed
with great accuracy one of the most important operations, of this
nature, ever undertaken. To accomplish this, however, took them nine
years; of which, three were occupied in determining the latitudes
alone.[5]
I have recited the foregoing facts, in order to give you some idea of
the unwearied pains which astronomers have taken to ascertain the exact
figure of the earth. You will find, indeed, that all their labors are
characterized by the same love of accuracy. Years of toilsome watchings,
and incredible labor of computation, have been undergone, for the sake
of arriving only a few seconds nearer to the truth.
The length of a degree of the meridian, as measured in Peru, was less
than that before determined in France, and of course less than that of
Lapland; so that the spheroidal figure of the earth appeared now to be
ascertained by actual measurement. Still, these measures were too few in
number, and covered too small a portion of the whole quadrant from the
equator to the pole, to enable astronomers to ascertain the exact law of
curvature of the meridian, and therefore similar measurements have since
been prosecuted with great zeal by different nations, particularly by
the French and English. In 1764, two English mathematicians of great
eminence, Mason and Dixon, undertook the measurement of an arc in
Pennsylvania, extending more than one hundred miles.
[Illustration Fig. 12.]
[Illustration Fig. 13.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account