The Geography of Strabo, Volume 1 (of 3): Literally Translated, with NotesStrabo
History
The Geography of Strabo, Volume 1 (of 3): Literally Translated, with Notes
Strabo
Geography -- Early works to 1800
geography, and in mathematics a geographer; and so lies open to the
attacks of both parties. In this third book, both he and Timosthenes get
such severe justice, that there seems nothing left for us to do;
Hipparchus is quite enough.
CHAPTER II.
1. We will now proceed to examine the statements made by Posidonius in
his Treatise on the Ocean. This Treatise contains much geographical
information, sometimes given in a manner conformable to the subject, at
others too mathematical. It will not, therefore, be amiss to look into
some of his statements, both now and afterwards, as opportunity occurs,
taking care to confine ourselves within bounds. He deals simply with
geography, when he tells us that the earth is spheroidal and the
universe too, and admits the necessary consequences of this hypothesis,
one of which is, that the earth contains five zones.
2. Posidonius informs us that Parmenides was the first to make this
division of the earth into five zones, but that he almost doubled the
size of the torrid zone, which is situated between the tropics, by
bringing it beyond these into the temperate zones.[626] But according to
Aristotle the torrid zone is contained between the tropics, the
temperate zones occupying the whole space between the tropics and the
arctic circles.[627] Both of these divisions Posidonius justly condemns,
for the torrid zone is properly the space rendered uninhabitable by the
heat. Whereas more than half of the space between the tropics is
inhabited, as we may judge by the Ethiopians who dwell above Egypt. The
equator divides the whole of this space into two equal parts. Now from
Syene, which is the limit of the summer tropic, to Meroe, there are
5000 stadia, and thence to the parallel of the Cinnamon region, where
the torrid zone commences, 3000 stadia. The whole of this distance has
been measured, and it may be gone over either by sea or land; the
remaining portion to the equator is, if we adopt the measure of the
earth supplied by Eratosthenes, 8800 stadia. Therefore, as 16,800 is to
8800, so is the space comprised between the tropics to the breadth of
the torrid zone.
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