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οἰκότα: the view is consistent and reasonable (cf. iii. 111. 1; vii. 167. 1), but H. leaves the intervention of the Deity an open question, he does not himself adopt the opinion of the pious believers in Poseidon (cf. Introduction, §§ 26, 32). τὴν γῆν σείειν. Hence the Homeric titles ἐνοσιχθών, ἐννοσίγαιος, &c., and in Thessaly πετραῖος (Pind. Pyth. iv. 138). Philostratus (Imag. ii. 17) finds the best proof that the cleft was made by an earthquake in the zigzag shape of the cliffs. The ups and downs on either side the valley correspond closely to each other, and the rocks are of the same kind and appearance. Modern geologists would agree with H., except that they might substitute a series of volcanic movements for a single earthquake. H. is at his best in such questions of geology and physical geography (cf. ii. 10-12).
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