[p.273]and Wady Sheriat. In Djebel Adjeloun, Moerad, and Beni Obeid, none of the basalt or black stone is met with; but in some parts of El Kefarat, in our way from Hebras to Om Keis, I saw alternate layers of calcareous and basaltic rock, with thin strata of flint. The habitations of Om Keis are, for the greater part, caverns. There is no water but what is collected in reservoirs during rains; these were quite dried up, which was the occasion, perhaps, of the place having been abandoned, for we found not a single inhabitant. My guide being ignorant of the road to Feik, wished to return to Hebras; and I was hesitating what to do, when we were met by some peasants of Remtha, in the Haouran, who were in their way to the Ghor, to purchase new barley, of which grain the harvest had already begun in the hot climate of that valley. I joined their little caravan. We continued, for about half an hour from Om Keis, upon the high plain, and then descended the mountains, the western declivity of which is entirely basaltic. At the end of two hours from Om Keis, we reached the banks of the Sheriat el Mandhour, or Sheriat el Menadhere (Arabic] or Arabic) which we passed at a ford. This river takes the additional name of the Arabs who live upon its banks, to distinguish it from the Sheriat el Kebir (Great Sheriat), by which the Jordan is known. The Sheriat el Menadhere is formed by the united streams of the Nahr Rokad [Arabic], which flows from near Ain Shakhab, through the eastern parts of Djolan; of the Hereir, whose source is in the swampy ground near Tel Dilly, on the Hadj route, between Shemskein and El Szannamein: of the Budje, which comes from Mezareib, and after its junction with the Hereir, is called Aweired [Arabic], and of the Wady Hamy Sakkar, besides several other smaller Wadys. The name of Sheriat, is first applied to the united streams near Szamme. From thence it flows in a deep bed of tufwacke; and its banks are cultivated by the Arabs Menadhere (sing. Mandhour), who live under VALLEY OF THE GHOR.