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Black Sea coast of western Georgia, with the skyline of Batumi on the horizon Swallow's Nest in Crimea Coastline of Samsun in Turkey A sanatorium in Sochi, Russia. The Black Sea is a marginal mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia.
In the 1970s, marine dead zones were first noted in settled areas where intensive economic use stimulated scientific scrutiny: in the U.S. East Coast's Chesapeake Bay, in Scandinavia's strait called the Kattegat, which is the mouth of the Baltic Sea and in other important Baltic Sea fishing grounds, in the Black Sea, and in the northern ...
The Caucasian Riviera is located along the eastern shores of the Black Sea under the Caucasus Mountains. It runs from Novorossiysk, Russia to Sarpi, Georgia. The area is divided into five regions, of which four (Adjara, Guria, Samegrelo, and Abkhazia) are located in Georgia, and one (the Black Sea coast of Krasnodar Krai) is in Russia. The ...
Lake Assal is the most saline body of water on earth after Don Juan Pond with 34.8% average salt concentration [10] (up to 40% at 20 m (66 ft) depth); higher than the 33.7% level in the Dead Sea. [10] [16] The dissolved salts include NaCl, KCl, MgCl 2, CaCl 2, CaSO 4 and MgBr 2, with NaCl dominating in Lake Assal and MgCl 2 in the Dead Sea. The ...
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. [5] [6] 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).
The Black Sea Region is a coastal strip of land 20–60 kilometres (12–37 mi) wide that runs along the coasts of Romania, Bulgaria, and a broader coastal strip in northern Turkey and Georgia. The coastline has rocky bays and sea cliffs, but is dominated by long stretches of low sand dunes and beaches sloping into the Black Sea. [1]
The dried water strait between the Lisan and the western coast of the Dead Sea is named Lynch Strait, after William Francis Lynch who explored the Dead Sea area in 1848. Similarly to the nearby Mount Sodom (Jebel Usdum), the peninsula is largely made up of white calcareous sediment containing beds of salt and gypsum , rising to 600 feet (180 m ...
The Black Sea area has been isolated and reconnected many times during the last 500,000 years. [21] Opponents of the deluge hypothesis point to clues that water was flowing out of the Black Sea basin as late as 15,000 years ago. [22] In this alternative scenario, much depends on the evolution of the Bosphorus.