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 extends as far as the southern extremity of the Dead Sea, while on the east it merges into the desert-steppe. This tableland is divided into three main sections: (1) From the Yarmuk to Wadi Hesbun, which empties into the Jordan near its mouth. This region comprises the hill masses of Jebel Ajlun and of the northern Belka. A considerable part of the latter is well wooded. (2) From the Hesbun to Wadi el-Hasa, the latter river falling into the Dead Sea at its southern end. This consists of the districts of southern Belka and ElKerak, which form an open and high plateau sometimes known as the Mountains of Moab. The highest summit is Jebel Shihan (3,470 ft.). The region contains various perennial streams, and there are large tracts of the best wheat-growing land in Syria. (3) From the Hasa to the Gulf of Akaba. Here the mountains continue for the most part as a narrow and sterile plateau, terminating further south just east of the Gulf of Akaba.

Coast

The coast-line of Syria from the Gulf of Alexan dretta to the Egyptian frontier runs in general from north to south. In northern Syria naturally good harbours are few, except in the Gulf of Alexandretta, where secure anchorage may be found at all seasons. Latakia and Tripoli are comparatively open and exposed, and Beirut depends largely on artificial protection. With the exception of the stretches of plain (see above, p. 4), the whole extent of coastline to a short distance beyond the Litani is in the main abrupt and in parts lofty.

In southern Syria, beyond Akka (Acre) the shore is conspicuously uniform and low, mainly consisting of long shallow curves of low, sandy beach. With the exception of the headland of Carmel there are no strongly marked prominences producing sheltered bays, and Athlit, Tantura. Abu Zabu Jaffa (Yafe), and Askalon provide the only possibilities of natural har bourage. The small estuaries of the coastal streams [2947]