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Thales of Miletus (Athen. ii. 87) attributed the rise of the Nile to its being held back by the Etesian winds. H.'s refutation is sensible; the winds blow from the north-west, and so would have affected equally the rivers of Africa and of Syria. But it must be admitted that neither land has ‘many rivers’, and of the Syrian ones, the Orontes flows south-west, and so would not have been affected. In Africa H. knew of the Cinyps and the Triton (iv. 175, 178 nn.).
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