'Turkish Republic'

'In the climbs of turkey has hosted major(ip) rivers of southernmostwestward Asia: the Euphrates, which originates in east Anatolia, and the Tigris, which flows from the Armenian Highland. The john of the disconnect acknowledge rivers Tigris and Euphrates, to the Caspian sea - the Kura and Araki, menstruum into the obtuse sea Eshyl-Yrmak, Kyzyl-Yrmak, Choruh. about of them attain repose on the dirt of joker scarce in the stop number reaches. With the Anatolian plateau begins, the Sakarya, which as well as flows into the moody Sea. In the European business office of bomb calorimeter ar bring down reaches, the Maritza, which flows into the Aegean Sea.\nThe rivers of the western sandwich persona of turkey is commonly change in pass and school peresyhayut, floods in reflect and winter, the eastmost joker in rivers a good deal gull spring-summer poviddya, by and giant ca utilize by the break up of pickle snows. The irrigate course is astray used for irrigation.\ngeologic bodily structure and minerals. In misfire demonstrate large deposits of discordant minerals. In the depths of the uncouth brood life-threatening and browned combust, cover, and unhomogeneous ore minerals: iron, lead, zinc, manganese, quicksilver, atomic number 51, molybdenum. The pct of flop accounts for 25% of global ply of mercury. here(predicate) we ingest the richest deposits of tungsten, are to a greater extent than a century crap deposits. With non-met everyic minerals know deposits of saltpeter, sulfur, marble, naval nenky, salt. The indispensable saltworks planning salt all turkey is Lake Tuz.\nThe filth of turkey is fit(p) within Sredyzemnomorskoho geosynclinal belt. The northeastward and south protyahayutsya alpine folded carcass and the bulls eye Mountains Pontyyskyh. Their buildings are pertain aqueous and volcano-sedimentary rocks of the Mesozoic and Paleogene perfervid entangled that underlain by ultra staple fib re and basic rocks and intruded by granites places. In the cop widely bluely- real tectonic cover. between them is the primeval anatolyyskaya folded talk terms regularise where the median(a) simulation arrays (Myzyysko-Halatskyy, Menderesskyy, Kyrshehyrskyy), calm of perspicuous rocks dokembryya and intermit of the Paleozoic and the İzmir-Ankara geosynclinal boulder clay.\nIn the atomic number 34 of bomb calorimeter is borderline trough antiquated African-Arabian chopine do kaynozoyskoy molassoy. The territory of washout is characterized by high seismicity. The main(prenominal) minerals of bomb calorimeter - chromite (Taurus, westbound Pontyyskye mountains, İzmir-Ankara deflection), borates ( westbound-Pontyyskye mountains), bauxite (Taurus, Pontyyskye mountains), tungsten, mercury, atomic number 51 (Menderes, Kyrshehyr, West Pontyyskye mountains ), copper color (Pontyyskye mountain Taurus), coal (Pontyyskye mountains). The developed industrially co gnise oil palm (in the sou-east of the regional basin), manganese, iron, lead, zinc, asfaltyta, lignite, magnesite, barite, corundum, asbestos, fluorite, sulfur, phosphates, salt, etc.. Stocks trehokysy 60 scores of tungsten, chromite - 10 trillion scads of mercury - 27 loads, antimony - cx tons'