dead sea hotels are places to stay when you are at the Dea Sea. Lots of peoplecome her to see this place mentioned in senses in the Bible, and also for medicinal resons. You can float on it. The Dead Sea (Hebrew: Ya-m Ha-Melah., " Sea of Salt "; Arabic: al-Bah.r l-Mayyit, " Dead Sea ") is a salt lake between Israel and the West Bank to the west, and Jordan to the east. It is 422 metres (1,385 ft) below sea level, and its shores are the lowest point on the surface of Earth 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 as salty as the ocean. 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. In Arabic the Dead Sea is calledArDeadSea.ogg al-Bahr al-Mayyit (help·info) ("the Dead Sea"), or less commonly bah.r^(u) lu-t. "the Sea of Lot"). Another historic name in Arabic was the "Sea of Zo?ar", after a nearby town. In Hebrew, the Dead Sea is He-Dead Sea.ogg Ya-m ha-Melah. (help·info), meaning "sea of salt," or Ya-m ha-Ma-vet (?? ?????, "sea of death"). In antiquity it was sometimes referred to as Ya-m ha-Mizrah.î "the Eastern sea") or Ya-m ha-‘A(ra-vâ "Sea of the Arabah"). The Greeks called it Lake Asphaltites (Attic Greek he- Thálatta asphalti~te-s, "the Asphaltite" sea.
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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 Fault zone 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 (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 Judean Hills. The highlands east of the Dead Sea receive more rainfall than the Dead Sea itself. There are two contending hypotheses about the origin of the low elevation of the Dead Sea. The older hypothesis is that it lies in a true rift zone, an extension of the Red Sea Rift, or even of the Great Rift Valley of eastern Africa. A more recent hypothesis is that the Dead Sea basin is a consequence of a "step-over" discontinuity along the Dead Sea Transform, creating extension of the crust with consequent subsidence.
Around three million years ago what is now the valley of the Jordan River, Dead Sea, and Wadi Arabah was repeatedly inundated by waters from the Mediterranean Sea. The waters formed in a narrow, crooked bay which was connected to the sea through what is now the Jezreel Valley. The floods of the valley came and went depending on long scale climate change. The lake that occupied the Dead Sea Rift, named "Lake Sodom", deposited beds of salt, eventually coming to be 3 km (2 miles) thick.
According to geological theory, approximately two million years ago the land between the Rift Valley and the Mediterranean Sea rose to such an extent that the ocean could no longer flood the area. Thus, the long bay became a lake.
The first such prehistoric lake is named "Lake
Gomorrah." Lake Gomorrah was a freshwater or brackish lake that extended
at least 80 km (50 mi) south of the current southern end of the Dead Sea and 100
km (60 mi) north, well above the present Hula Depression. As the climate became
more arid, Lake Gomorrah shrank and became saltier. The large, saltwater predecessor
of the Dead Sea is called "Lake Lisan."
Near Ein Gedi, salt builds
up along the shores of the Dead Sea.
Cobble encrusted with halite evaporated
from the Dead Sea near Ein Gedi.
Pebbles cemented with halite on the western
shore of the Dead Sea near Ein Gedi.
In prehistoric times great amounts of sediment collected on the floor of Lake Gomorrah. The sediment was heavier than the salt deposits and squeezed the salt deposits upwards into what are now the Lisan Peninsula and Mount Sodom (on the southwest side of the lake). Geologists explain the effect in terms of a bucket of mud into which a large flat stone is placed, forcing the mud to creep up the sides of the pail. When the floor of the Dead Sea dropped further due to tectonic forces, the salt mounts of Lisan and Mount Sodom stayed in place as high cliffs. (see salt domes)
From 70 000 to 12 000 years ago the lake level was 100 m (328 ft) to 250 m (820 ft) higher than its current level. This lake, called "Lake Lisan", fluctuated dramatically, rising to its highest level around 26,000 years ago, indicating very wet climate in the Near East. Sometime around 10 000 years ago the lake level dropped dramatically, probably to levels even lower than today. During the last several thousand years the lake has fluctuated approximately 400 m (1,310 ft) with some significant drops and rises. Current theories as to the cause of this dramatic drop in levels rule out volcanic activity, therefore it may have been a seismic event. Until the winter of 1978-79, when a major mixing event took place,[8] the Dead Sea was composed of two stratified layers of water that differed in temperature, density, age, and salinity. The topmost 35 metres (115 ft) or so of the Dead Sea had a salinity that ranged between 300 and 400 parts per thousand and a temperature that swung between 19 °C (66.2 °F) and 37 °C (98.6 °F). Underneath a zone of transition, the lowest level of the Dead Sea had waters of a consistent 22 °C (71.6 °F) temperature and complete saturation of sodium chloride (NaCl).[citations needed] Since the water near the bottom is saturated, the salt precipitates out of solution onto the sea floor.
Beginning in the 1960s water inflow to the Dead Sea from the Jordan River was reduced as a result of large-scale irrigation and generally low rainfall. By 1975 the upper water layer of the Dead Sea was saltier than the lower layer. Nevertheless, the upper layer remained suspended above the lower layer because its waters were warmer and thus less dense. When the upper layer finally cooled down so that its density was greater than the lower layer the waters of the Dead Sea mixed (1978-79). For the first time in centuries the lake was a homogeneous body of water. Since then stratification has begun to redevelop. The Dead Sea area has become a major centre for health research and treatment for several reasons. The mineral content of the water, the very low content of pollens and other allergens in the atmosphere, the reduced ultraviolet component of solar radiation, and the higher atmospheric pressure at this great depth each have specific health effects. For example, persons suffering reduced respiratory function from diseases such as cystic fibrosis seem to benefit from the increased atmospheric pressure.[10]
Sufferers of the skin disorder psoriasis also benefit from the ability to sunbathe for long periods in the area due to its position below sea level and subsequent result that many of the sun's harmful UV rays are reduced.[11]
Thus, the region's climate and low elevation have made it a popular center for several types of therapies:
* Climatotherapy:
Treatment which exploits local climatic features such as temperature, humidity,
sunshine, barometric pressure and special atmospheric constituents.
* Heliotherapy:
Treatment that exploits the biological effects of the sun's radiation.
*
Thalassotherapy: Treatment that exploits bathing in Dead Sea water. The sea is
called "dead" because its high salinity prevents macroscopic aquatic
organisms, such as fish and aquatic plants, from living in it, though minuscule
quantities of bacteria and microbial fungi are present.
In times of flood, the salt content of the Dead Sea can drop from its usual 35% salinity to 30% or lower. The Dead Sea temporarily comes to life in the wake of rainy winters. In 1980, after one such rainy winter, the normally dark blue Dead Sea turned red. Researchers from Hebrew University found the Dead Sea to be teeming with a type of algae called Dunaliella. The Dunaliella in turn nourished carotenoid-containing (red-pigmented) halobacteria whose presence caused the color change. Since 1980, the Dead Sea basin has been dry and the algae and the bacteria have not returned in measurable numbers.
Many animal species live in the mountains surrounding the Dead Sea. Hikers can see camels, ibex, hares, hyraxes, jackals, foxes, and even leopards. Hundreds of bird species inhabit the zone as well. Both Jordan and Israel have established nature reserves around the Dead Sea.
The delta of the Jordan river was formerly a veritable jungle of papyrus and palm trees. Flavius Josephus described Jericho as "the most fertile spot in Judea". In Roman and Byzantine times sugarcane, henna, and sycamore fig all made the lower Jordan valley quite wealthy. One of the most valuable products produced by Jericho was the sap of the balsam tree, which could be made into perfume. But by the 19th century Jericho's fertility had disappeared.
There are several small communities near the Dead Sea. These include the West Bank Israeli settlements in the Megilot Regional Council: Vered Yeriho, Kalya, Almog, Beit Ha'arava, Mitzpe Shalem and Avnat. There is a beautiful nature preserve at Ein Gedi, and the Dead Sea hotels are located on the southwest end at Ein Bokek near Neve Zohar. Highway 90 runs north-south on the Israeli side.Potash City is a small community on the Jordanian side of the Dead Sea. Highway 65 runs north-south on the Jordanian side.
In Ezekiel 47:8-9 there is a specific prophecy that the sea will ".. be healed and made fresh", becoming a normal lake capable of supporting marine life. A similar prophecy is stated in Zechariah 14:8, which says that "Living waters will go out from Jerusalem, half of them to the eastern sea (likely the Dead Sea) and half to the western sea (the Mediterranean)..." The remoteness of the region attracted Greek Orthodox monks since the Byzantine era. Their monasteries such as Saint George in Wadi Kelt and Mar Saba in the Judean Desert are places of pilgrimage. like hotels in a way. More recently, explorers and scientists arrived in the area to analyze the minerals and research the unique climate. Tourism in the region has been developed since the 1960s.The Dead Sea Scrolls were found in caves at Qumran at the Dead Sea. The world's lowest road, Highway 90, runs along the Israeli and West Bank shores of the Dead Sea at 393 m (1,289 ft) below sea level.
The Dead Sea canal is a proposed project of building a canal from either the Mediterranean Sea (MDSC) or the Red Sea to the Dead Sea (RSDSC), taking advantage of the 400-meter difference in water levels between the seas. The water flowing through the canal may help redress the drop in the level of the Dead Sea observed in recent years. The canal can also be used to generate hydroelectric power because of surface difference and maybe by salinity gradient power, and desalinate water by reverse osmosis.Find a Cottage in Britain or Ireland
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There are several small communities near the Dead Sea. These include the West Bank Israeli settlements in the Megilot Regional Council: Vered Yeriho, Kalya, Almog, Beit Ha'arava, Mitzpe Shalem and Avnat. There is a beautiful nature preserve at Ein Gedi, and the Dead Sea hotels are located on the southwest end at Ein Bokek near Neve Zohar. Highway 90 runs north-south on the Israeli side.
Potash City is a small community on the Jordanian side of the Dead Sea. Highway 65 runs north-south on the Jordanian side.
More recently, explorers and scientists arrived in the area to analyze the minerals and research the unique climate. Tourism in the region has been developed since the 1960s.
The Dead Sea Scrolls were found in caves at Qumran at the Dead Sea. The world's lowest road, Highway 90, runs along the Israeli and West Bank shores of the Dead Sea at 393 m (1,289 ft) below sea level.
There are also health spas and hot springs along the shore, besides the unique water of the Dead Sea itself. A golf course named for Sodom and Gomorrah was built by the British at Kalia on the northern shore. The first major hotels were built in Israel, first at nearby Arad, and since the 1960s at the Neve Zohar resort complex. The Jordanian side has seen increasing development in recent years. For example, three international franchises have opened seaside resort hotels near the King Hussein Bin Talal Convention Center along the eastern coast of the Dead Sea.
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