Astronomical Myths: Based on Flammarions's "History of the Heavens"
John Stuart Mill · en
Homer lived in the tenth century before our era. Herodotus, who lived in
the fifth, developed the Homeric chart to three times its size. He
remarks at the commencement of his book that for several centuries the
world has been divided into three parts--Europe, Asia, and Libya; the
names given to them being female. The exterior limits of these countries
remained in obscurity notwithstanding that those boundaries of them that
lay nearest to Greece were clearly defined.
One of the greatest writers on ancient geography was Strabo, whose ideas
we will now give an account of. He seems to have been a disciple of
Hipparchus in astronomy, though he criticises and contradicts him
several times in his geography. He had a just idea of the sphericity of
the earth; but considered it as the centre of the universe, and
immovable. He takes pains to prove that there is only one inhabited
earth--not in this refuting the notion that the moon and stars might
have inhabitants, for these he considered to be insignificant meteors
nourished by the exhalations of the ocean; but he fought against the
fact of there being on this globe any other inhabited part than that
known to the ancients.
It is remarkable to notice that the proofs then used by geographers of
the sphericity of the earth are just those which we should use now. Thus
Strabo says, "The indirect proof is drawn from the centripetal force in
general, and the tendency that all bodies have in particular towards a
centre of gravity. The direct proof results from the phenomena observed
on the sea and in the sky. It is evident, for example, that it is the
curvature of the earth that alone prevents the sailor from seeing at a
distance the lights that are placed at the ordinary height of the eye,
and which must be placed a little higher to become visible even at a
greater distance; in the same way, if the eye is a little raised it will
see things which previously were hidden." Homer had already made the
same remark.