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.
Saturday, August 1, 2009
Alive
Although called the "Dead Sea", this sea and the whole region on its shore is very much alive. The Dead Sea region is also an ideal base for touring Israel. Travel distances are short, with Jerusalem only in hour's drive, and Tel Aviv and Tiberias only 2 hours away.
Thursday, July 30, 2009
Beginnings of The Dead Sea as a Spa
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.
Thursday, July 30, 2009
The Dead Sea
The Dead Sea is the lowest place on earth, roughly 1,300 feet (400 meters) below sea level. It is 34 miles (55 km.) long and varies between 11 miles (18 km.) and 2 miles (3 km.) in width. The Sea is 1,400 feet (430 m.) deep. This unique sea is fed by the Jordan River. There is no outflow; and the exceptionally high rate of evaporation (high temperatures, low humidity) produces large quantities of raw chemicals. These are extracted and exported throughout the world for use in medicine, agriculture and industry.
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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