Deodorant for Men Lord Dr Nona BioOrganic Dead Sea 95ml

 The Dead Sea (Arabic: البَحْر  المَيّت‎, al-Baḥr  El-Mayyit, Hebrew: יָם  הַ‏‏מֶּ‏‏לַ‏ח‎, Yām  Ha-Melaḥ; "Dead Sea" ,  "Sea of Salt"), also      called    the Salt  Sea, is a salt  lake bordering Israel and  the West  Bankto the west, and Jordan to  the east. Its surface and shores   are  422 metres (1,385 ft) below sea  level,^[2] the  lowest elevation on the Earth's  surface on dry land. The Dead Sea is 378 m (1,240 ft) deep, the deepest hypersaline  lake in the world. It is also  one of the world's saltiest bodies  of water, with 33.7% salinity.  Only Lake  Assal (Djibouti), Garabogazköl and  some hypersaline lakes of the McMurdo  Dry Valleys in Antarctica (such  as Don  Juan Pond and perhaps Lake  Vanda) have a higher salinity. It is 8.6 times more salty than the  ocean.^[3] This  salinity makes for a harsh environment where animals cannot flourish, hence  its name. The Dead Sea is 67 kilometres (42 mi) long and 18 kilometres  (11 mi) wide at its widest point. It lies in the Jordan  Rift Valley, and its main tributary is  the Jordan  River.

The Dead Sea has attracted visitors from around the Mediterranean  basin for thousands of years.  Biblically, it was a place of refuge for King  David. It was one of the world's first health resorts (for Herod the Great), and it has been the supplier of a wide variety of  products, from balms for Egyptian mummification to potash for fertilizers.  People also use the salt and the minerals from the Dead Sea to create cosmetics and  herbal sachets.

The Dead Sea is an endorheic  lake located 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 Faultzone in Turkey and  the northern end of the Red  Sea Rift offshore of the  southern tip of Sinai.

The Jordan  River is the only major water  source flowing into the Dead Sea, although there are small perennial springs  under and around the Dead Sea, creating pools and quicksand pits  along the edges.^[6] There  are no outlet streams.

Rainfall is scarcely 100 mm (3.9 in) per year in the northern part of the  Dead Sea and barely 50 mm (2.0 in) in the southern part. The Dead Sea zone's  aridity is due to the rainshadow effect  of theJudean  Hills. The highlands east of the Dead Sea receive more rainfall than the  Dead Sea itself.

To the west of the Dead Sea, the Judean Hills rise less steeply, and are  much lower, than the mountains to the east. Along the southwestern side of  the lake is a 210 m (690 ft) tall haliteformation  called "Mount  Sodom".