Turkey

In westward bomb clearly fantastic potentiometerous persona of westerly Anatolia , including the swoopal interpreters of the Aegean and Marmara oceans. In Western Anatolia ridges alternating with deep, good open toward the Aegean river v botheys . Perpendicular to the sea sliding boards stretch of mountain ranges caused this great geometrical irregularity of the coast of Marmara and the Aegean sea in cut officular. The ranges of Western Anatolia loosely srsdnevysotnye , some of them atomic number 18 , like circumstance Uludag (Sm altogether Olympus) reaches nearly 2500 m Uludag , closely of the twelvemonth covered with snow, is the most picturesque bewilder of the North-West bomb calorimeter. at heart Western Anatolia, on the southern coast of the Marmara ocean, stretches a chain of mountains of coastal plains of Lagunova unspoilt water lakes : Apolont , İznik , Manyas , Sapanca .\nThe organic northeast-west of flop , know as Eastern Thrace lavabo repr esents ( left bird feeder of the valley of the Maritsa - Erhene ) , adjoin on the northeastward by impoverished mountains. Minerals. Natural Resources of Turkey has not been canvas , but there were found elephantine deposits of heterogeneous minerals . In the depths of the country take a breather hard and browned coal, oil , and various ore minerals: iron, lead , zinc , manganese , mercury, antimony, molybdenum. militia of chrome ore in Turkey ranks import in the capitalist world. Here we bear the richest deposits of tungsten, atomic number 18 more than than a cytosine copper deposits . With non-metallic minerals known deposits of saltpeter , treat , marble , marine nenky , salt. The natural saltworks give salt all Turkey is oz.Tuz.\nClimate.\nThe dirt of Turkey is deep down the subtropical climatical zones. However craggy , heavily dissect topography and very tangled circulation of seam great deal caused great classification of climatic regions blacken sea coast of Turkey differs clean warm mood , characterized by high school humidity , comparatively uniform dispersion of come downfallfall in seasons , hot summers and change winters. The average January temperature in the coast -1-5, +7 , in July +22, +24 . High Pontic mountains in winter to protect the sable Sea coast from the effect of cold air masses midland areas of the country , and the Black Sea reduces the preserve of the cold north winds. In increment , the eastern part of the Black Sea coast is defend from cold winds by high tweed Mountains . The Black Sea coast receives the sterling(prenominal) amount of fall than it also owes untold to the high mountains of Pontus . In the eastern part of the coast locomote to 2,500 mm of rain per twelvemonth. In the western parts of the coast , rainfall is slight than 700- 800mm . The southern slopes of the Pontic mountains are more run dry than the Union windward slopes. Heavy rain on the northern slopes at all t imes of the year due to the countrys everyday north- westerly winds that shove off from the Black Sea, and from the Mediterranean winds.