The Barada, or river of Damascus, rises in the plain of Zebdany--the very centre of the Antilibanus. It has its real permanent source in a small nameless lake in the lower part of the plain, about lat. 33° 41’; but in winter it is fed by streams flowing from the valley above, especially by one which rises in lat. 33° 46’, near the small hamlet of Ain Hawar. The course of the Barada from the small lake is at first towards the east; but it soon sweeps round and flows-southward for about four miles to the lower end of the plain, after which it again turns to the east and enters a romantic glen, running between high cliffs, and cutting through the main ridge of the Antilibanus between the Zebdany plain and Suk, the Abila of the ancients. From Suk the river flows through a narrow but lovely valley, in a course which has a general direction of south-east, past Ain Fijoh (where its waters are greatly increased), through a series of gorges and glens, to the point where the roots of the Antilibanus sink down upon the plain, when it bursts forth from the mountains and scatters. Channels are drawn from it on either side, and its waters are spread far and wide over the Merj, which it covers with fine trees and splendid herbage. One branch passes right through the city, cutting it in half. Others irrigate the gardens and orchards both to the north and to the south. Beyond the town the tendency to division still continues. The river, weakened greatly through the irrigation, separates into three main channels, which flow with divergent courses towards the east, and terminate in two large swamps or lakes, the Bahret-esh-Shurkiyeh and the Bahret-el-Kibli-yeh, at a distance of sixteen or seventeen miles from the city. The Barada is a short stream, its entire course from the plain of Zebdany not much exceeding forty miles.