Page:The geography of Strabo (1854) Volume 1.djvu/157

 CHAP. ii. 1, 2. INTRODUCTION. 143 CHAPTER II. 1. WE will now proceed to examine the statements made by Posidonius in his Treatise on the Ocean. ThFs Treatise contains much geographical info7rniatTon7^olnetimes given in a manner conformable to the subject, at others too mathematical. It will not, therefore, be amiss to look into some of his state- ments, both now and afterwards, as opportunity occurs, taking care to confine ourselves within bounds. Pie deals simply with geography, when he tg.lla ns, t.hqt the ear {.h is spheroidal and the universe too, and admits the necessary consequences ot this hypothesis^ one of which is, that the earth contains five zone's. 2. Posidonius informs us that Parmenides was the first to make this division of the earth into five zones, but tEaT he almost doubled the size of the torrid zone, which is situated between the_ tropics, by bringing it beyond these into the temperate zones. 1 But according to Aristotle the torrid zone is contained between the tropics, the temperate zones occupy- ing the whole space between the tropics and the arctic cir- cles. 2 Both of these divisions Posidonius justly condemns, for the torrid zone is properly the space rendered uninhabit- able by the heat. Whereas more than half of the space be- tween 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, 1 According to Plutarch, both Thales and Pythagoras had divided the earth into five zones. Since Parmenides lived one hundred and fifty years after the first of these philosophers, lie cannot be considered the author of this division. As Posidonius and Strabo estimated the breadth of the torrid zone at 8800 stadia, and Parmenides is said to have nearly doubled it, this would give 17,600 stadia, or 25 &' 34", taking this at 25 it would appear that Parmenides extended the torrid zone one degree beyond the tropics. 2 The Arctic Circles of the ancients were not the same as ours, but varied for every latitude. Aristotle limited the temperate zone to those countries which had the constellation of the crown in their Arctic Circle, the brilliant star of that constellation in his time had a northern declina- tion of about 36 30', consequently he did not reckon that the temperate zone reached farther north or south than 53 and a half. We shall see that Strabo adopted much the same opinion, fixing the northern bounds of the habitable earth at 54 25' 42". Gosselin.