Dead Sea
Geography

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. 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). This left lateral-moving transform fault lies along the tectonic plate boundary between the African Plate and the Arabian Plate. It runs between the East Anatolian Fault zone in Turkey and the northern end of the Red Sea Rift offshore of the southern tip of Sinai.

Water feeds into the Dead Sea from various sources, many small or intermittent, including:

(Wadi is the Arabic term for a river valley with a small or intermittent stream; Nahal is the equivalent in Hebrew. The two terms are often used interchangeably in English names for the same body of water.)

The water of Wadi Hassa is now completely consumed in Jordan. The Jordan River, which passes through the Sea of Galilee, has been substantially diverted. It currently only contributes about one-sixth of the inflow to the Dead Sea, less than direct rainfall.

There are also small perennial springs under and around the Dead Sea, forming pools and quicksand pits along the edges.

The Wadi Mujib valley, 420 m below the sea level in the southern part of the Jordan valley, is a biosphere reserve, with an area of 212 km (82 sq mi). Rainfall is scarcely 100 mm (4 in) per year in the northern part of the Dead Sea and barely 50 mm (2 in) in the southern part. The Dead Sea zone's aridity is due to the rainshadow effect of the Judaean Mountains. The highlands east of the Dead Sea receive more rainfall than the Dead Sea itself.

To the west of the Dead Sea, the Judaean mountains rise less steeply and are much lower than the mountains to the east. Along the southwestern side of the lake is a 210 m (700 ft) tall halite mineral formation called Mount Sodom.
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