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led beard. [The chlanis was a light summer-mantle, worn especially by the more elegant Athenians, and generally made of expensive materials. The simpler cloak, the himation, was worn by the Doric Greeks, and principally by the Spartans.] The boat had left Naukratis, at that time the only Hellenic port in Egypt, about half an hour before. [This town, which will form the scene of a part of our tale, lies in the northwest of the Nile Delta, in the Saitic Nomos or district, on the left bank of the Canopic mouth of the river. According to Strabo and Eusebius it was founded by Milesians, and Bunsen reckons 749 B. C. It seems that in the earliest times Greek ships were only allowed to enter this mouth of the Nile in case of necessity. The entire intercourse of the Egyptians with the hated strangers was, at that time, restricted to the little island of Pharos lying opposite to the town of Thonis.] During their journey, the grey-haired, moody man had not spoken one word, and the other had left him to his meditations. But now, as the boat neared the shore, the restless traveller, rising from his couch, called to his companion: "We are just at our destination, Aristomachus! That pleasant house to the left yonder, in the garden of palms which you can see rising above the waters, is the dwelling of my friend Rhodopis. It was built by her husband Charaxus, and all her friends, not excepting the king himself, vie with one another in adding new beauties to it year by year. A useless effort! Let them adorn that house with all the treasures in the world, the woman who lives within will still remain its best ornament!" [We are writing of the month of October, when the Nile begins to sink. The inundations can now be accurately accounted for, especially since the important and laborious synoptical work of H. Barth and S. Baker. They are occasioned by the tropical rains, and the melting of the snows on the high mountain-ranges at the Equator. In the beginning of June a gradual rising of the Nile waters can be perceived; between the 15th and 20th June, this changes to a rapid increase; in the beginning of October the waters reach their highest elevation, a point, which, even after having begun their retreat, they once more attempt to attain; then, at first gradually, and afterwards with ever increasing rapidity, they continue to sink. In January, February an
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