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Saturday, August 1, 2009
The Dead Sea is one of the most saline lakes in the world. It is fed mainly by River Jordan in the north and by perennial springs and streams from the east and west. Having no outlet, the Dead sea is a "terminal lake" which loses huge amounts of water by evaporation into the hot dry air. This results in high concentrations of salts and minerals in a unique composition that is particularly rich in chloride salts of magnesium, sodium, potassium, calcium, bromine and various others. The Dead Sea brine's chemical composition reflects erosion, as well as the recycling of older deposits.
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