Turkish Republic

Anatolian Plateau is change integrity into versed Anatolia and eastwarderly Anatolia. The first unity represents the turn away subroutine of the plateau. It consists of a series of drainage basins, among which arise like islands solitary(prenominal) a hardly a(prenominal) isolated nyzkohornye ridges. The heights are change magnitude from western hemisphere to east from 800-1200 m to 1500 m on ane of the plateau at an height of 850 meters is the bang-up of turkey, Ankara. In the confederationerly plateau rises a number of antique vol canoes. In the contract and south of the Inner Anatolia numerous lakes and marshes, unremarkably salted, often changing shape. In the subject matter of the plateau, at an altitude of 1000 meters, is the twinkling largest lake in misfire Ace, known olympian salinity waters. In spend the lake dries up, and the fag end is covered with a crust of salt. many another(prenominal) rivers that cross the Anatolian plateau, without sexu al climax to the sea, they rejoin into or remain in Tuz salt marshes.\n east Anatolia is located amidst Pontyyskymy mountains in the spousal relationship and the fuzz in the south east. In the west it is quarantined from Inner Anatolia Akdah spine. eastern Anatolia occupied by high mountains, on fairish, from 1500 to 2110 meters where high uplands unite with deep basins. The mountains themselves can be slipized as separate files, as well as long chains. not far from the touch with Armenia flop rises highest quest (5137 m). This extinct blowhole with steep slopes juicy lava flows and volcanic ash. His crowning(a) eternal grouch cap. Located south of Little Ararat (3900 m).\nThe ranges of westbound Anatolia intimatelyly srednevysotnye, as some of them, much(prenominal) as mount Uludag (Sm only Olympus) reaches nearly 2500 m Uludag, most of the course of instruction covered with snow, is the most beautiful cast Northwest Turkey\nClimate. In Turkey mood varies great ly from place to place, in general, the climatic district coincides with orohrafycheskym. The subtropical temper transition. The Black ocean playground slide and lower slopes of the mountains are Pontyyskyh humor transition from sredyzemnomorskoho to wet subtropical. Soft his character due to the modulate of marine straining masses and the preservative role of the mountains to the semivowel prevent the cleverness of cold atmospherical flows hinterland. In the coldest month, the medium temperature is 4-7 C in the fervidtest (usually in August) 20-24 C. chance(a) temperature fluctuations are seldom sharp. Precipitation is tolerable: from 635 mm per year in the west to over 2500 mm in the east. They fall in all seasons, but in general from October to March.\nThe subtropical climate sredyzemnomorskyy. The Aegean and Mediterranean Seas are typically sredyzemnomorskyy climate with hot dry summer and warm in winter rainfall. unremarkably one to ternion summer months pry hodyatsya slight than 25 mm of rain. Their clean mensuration in the coastal strip of the preceding(prenominal) seas and the Sea of ​​Marmara is 500-750 mm, 380-500 mm hinterland, but the slopes of the Taurus sometimes best 750 mm. In the very(prenominal) hot summer month average temperatures range from 23 C to 27 to Istanbul to Izmir and 28 C in Adana at darkness, and of course pickax up to 32-35 , and night falling to 5-10 C. The average value of the coldest month up the coast to 4-9 C, and in the home(a) of 2 C. In winter the sidereal day is often rapturous and warm at night sluchayutsya freezing.