A History of Science — Volume 1Williams, Henry Smith
History
A History of Science — Volume 1
Williams, Henry Smith
Science -- History
With the aid of this implement, Eratosthenes carefully noted the longest
and the shortest shadows cast by the gnomon--that is to say, the shadows
cast on the days of the solstices. He found that the distance between
the tropics thus measured represented 47 degrees 42' 39" of arc.
One-half of this, or 23 degrees 5,' 19.5", represented the obliquity of
the ecliptic--that is to say, the angle by which the earth's axis dipped
from the perpendicular with reference to its orbit. This was a most
important observation, and because of its accuracy it has served modern
astronomers well for comparison in measuring the trifling change due to
our earth's slow, swinging wobble. For the earth, be it understood, like
a great top spinning through space, holds its position with relative but
not quite absolute fixity. It must not be supposed, however, that
the experiment in question was quite new with Eratosthenes. His merit
consists rather in the accuracy with which he made his observation than
in the novelty of the conception; for it is recorded that Eudoxus, a
full century earlier, had remarked the obliquity of the ecliptic. That
observer had said that the obliquity corresponded to the side of a
pentadecagon, or fifteen-sided figure, which is equivalent in modern
phraseology to twenty-four degrees of arc. But so little is known
regarding the way in which Eudoxus reached his estimate that the
measurement of Eratosthenes is usually spoken of as if it were the first
effort of the kind.
Much more striking, at least in its appeal to the popular imagination,
was that other great feat which Eratosthenes performed with the aid
of his perfected gnomon--the measurement of the earth itself. When we
reflect that at this period the portion of the earth open to observation
extended only from the Straits of Gibraltar on the west to India on
the east, and from the North Sea to Upper Egypt, it certainly seems
enigmatical--at first thought almost miraculous--that an observer
should have been able to measure the entire globe. That he should have
accomplished this through observation of nothing more than a tiny bit of
Egyptian territory and a glimpse of the sun's shadow makes it seem but
the more wonderful. Yet the method of Eratosthenes, like many another
enigma, seems simple enough once it is explained. It required but the
application of a very elementary knowledge of the geometry of circles,
combined with the use of a fact or two from local geography--which
detracts nothing from the genius of the man who could reason from such
simple premises to so wonderful a conclusion.
Public-domain text, read in full here on John Shaqi.
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