which by land would have taken us eighty-eight hours, in three and one-half days. The river, therefore, must flow with an average velocity of almost four miles per hour. In places it is much swifter, and in others decidedly slower. The Tigris leaves the mountains near Argana-Maaden, and flows past the walls of Diarbekir, where it is apt to cause slight inundations in summer time. It then receives the Battman river flowing in a southerly direction from the high Karsann-Mountains and carrying more water into the Tigris than this river contained before. Immediately after the union of these two rivers the Tigris enters another mountainous territory formed of sandstone. The gentle curves of the broad and shallow river are transformed into the sharp criss-cross angles of a ravine. The banks are abrupt, often vertical on both sides; and on top of some steep, rocky slopes your eye may discover groves of dark-green palms, and in their shadows the settlements of tribes of Kurds, who in this region are mostly cave-dwellers. The town of Hassn-Kejfa (Hossu-Keifa), situated on a high rock whence a narrow staircase descends to the river, offers a most unusual aspect. The old city below has been destroyed, and only a few minarets still pointing to the sky indicate that mosques and houses once stood here. The inhabitants were obliged to retreat to the top of the cliff, where they built a wall of defence on the only accessible side. In the narrow ravine I discovered huge blocks which had rolled down from above. People have hollowed them and are using them as dwelling places. These "huts" today make up a small, very irregular town, which, however, possesses even a bazaar. By far the most noteworthy remains are the ruins of a bridge which used to cross the Tigris. There was one gigantic arch with a span of between eighty and one hundred feet. I do not know whether the credit for such a daring structure should be given to the Armenian kings or the Greek emperors, or perhaps even to the califs.