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θερμότατος κτλ. This passage, as to the climate of India, well illustrates H.'s mistaken views of the earth's shape. As he supposes it to be flat, the Indians on the extreme east have the sun nearest to them, and so hottest, in the early morning; this lasts till the time of the ‘market's breaking-up’ (i.e. about 10 a.m.); as the sun goes west, the day gets cooler. Rawlinson, however, thinks that H. may be reproducing inaccurately a real account of the contrast between the hot mornings and the cool afternoons, when the sun is behind the hills, of the high Indian valleys. For ἀγορῆς διαλύσιος cf. ii. 173. 1 and iv. 181. 3.
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