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The Dead Sea is a salt lake is bordered by Jordan to the east and Palestine's Israeli-occupied West Bank and Israel to the west. [5] [6] It is an endorheic lake, meaning there are no outlet streams. The Dead Sea lies in the Jordan Rift Valley, a geographic feature formed by the Dead Sea Transform (DST).
The Dead Sea is the largest body of water in Palestine, while the valley of Marj Sanur forms a seasonal lake. [5] A number of ephemeral streams, in Arabic called wadis, flow into the Jordan River or Dead Sea through the West Bank, including Wadi Og, Wadi Fa'rah and Wadi Qelt.
The dried water strait between the Lisan and the western coast of the Dead Sea is named Lynch Strait, after William Francis Lynch who explored the Dead Sea area in 1848. Similarly to the nearby Mount Sodom (Jebel Usdum), the peninsula is largely made up of white calcareous sediment containing beds of salt and gypsum , rising to 600 feet (180 m ...
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The stream originates on the crest of the Notza Ridge, which forms the watershed divide between the Dead Sea and the Red Sea, and from which all streams in the Arava desert flow either north to the Dead Sea or south to the Red Sea. The stream's prominent tributaries include: Nahal Paran, Nahal Barak, Nahal Tzin, Nahal Tzafit, and Nahal Nekorot. [1]
A general view shows the location of the accident where people were killed in a flash flood near the Dead Sea, Jordan, Thursday, Oct. 25, 2018. (AP Photo/Raad Adayleh) At least 21 people have died ...
Average precipitation. The characteristics of United States rainfall climatology differ significantly across the United States and those under United States sovereignty. . Summer and early fall bring brief, but frequent thundershowers and tropical cyclones which create a wet summer and drier winter in the eastern Gulf and lower Eas