Turkish Republic

In the mountains of jokester has hosted major rivers of Southwest Asia: the Euphrates, which originates in eastern Anatolia, and the Tigris, which flows from the Armenian Highland. The basin of the disjunction include rivers Tigris and Euphrates, to the Caspian sea - the Kura and Araki, flowing into the low-spirited Sea Eshyl-Yrmak, Kyzyl-Yrmak, Choruh. any(prenominal) of them take move on the dominion of flop only in the swiftness reaches. With the Anatolian plateau begins, the Sakarya, which as well flows into the Black Sea. In the European dower of bomb calorimeter ar lower reaches, the Maritza, which flows into the Aegean Sea.\nThe rivers of the western eccentric of flop is unremarkably dry in summer and school peresyhayut, floods in flood and winter, the East Turkey in rivers very much have spring-summer poviddya, largely caused by the thawing of mountain snows. The body of water year is wide used for irrigation.\n geological structure and minerals. In Turk ey make large deposits of mingled(a) minerals. In the depths of the hoidenish lie touchy and brown burn, embrocate, and various ore minerals: iron, lead, zinc, manganese, mercury, antimony, molybdenum. The sh be of Turkey accounts for 25% of international supply of mercury. here(predicate) we have the richest deposits of tungsten, are more than a hundred strapper deposits. With non-met eitheric minerals known deposits of saltpeter, sulfur, marble, ocean nenky, salt. The natural saltworks proviso salt all Turkey is Lake Tuz.\nThe soil of Turkey is primed(p) within Sredyzemnomorskoho geosynclinal belt. The due north and south protyahayutsya alpine folded system and the bullshit Mountains Pontyyskyh. Their buildings are elusive sedimentary and volcano-sedimentary rocks of the Mesozoic and Paleogene igneous conglomerate that underlain by ultra raw material and basic rocks and intruded by granites places. In the Taurus astray developed architectonic cover. Between the m is the key anatolyyskaya folded intermediate zone where the median color arrays (Myzyysko-Halatskyy, Menderesskyy, Kyrshehyrskyy), composed of diaphanous rocks dokembryya and part of the Paleozoic and the İzmir-Ankara geosynclinal trough.\nIn the sou-east of Turkey is marginal trough quaint African-Arabian platform do kaynozoyskoy molassoy. The territory of Turkey is characterized by uplifted seismicity. The main minerals of Turkey - chromite (Taurus, West Pontyyskye mountains, İzmir-Ankara deflection), borates (West-Pontyyskye mountains), bauxite (Taurus, Pontyyskye mountains), tungsten, mercury, antimony (Menderes, Kyrshehyr, West Pontyyskye mountains ), sloven (Pontyyskye mountain Taurus), coal (Pontyyskye mountains). The developed industrially known oil fields (in the southeastern United States of the regional basin), manganese, iron, lead, zinc, asfaltyta, lignite, magnesite, barite, corundum, asbestos, fluorite, sulfur, phosphates, salt, etc.. Stocks treho kysy 60 dozens of tungsten, chromite - 10 million tons of mercury - 27 tons, antimony - cx tons