DiscountsLast MinuteColorful Turkey

July 18, 2018by Emma Churchill0
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Turkey , is a transcontinental country located mainly on the Anatolian Peninsula in Western Asia, with a smaller portion on the Balkan Peninsula in Southeastern Europe. Turkey is bordered on its northwest by Greece and Bulgaria; north by the Black Sea; northeast by Georgia; east by Armenia, Azerbaijan, and Iran; southeast by Iraq; south by Syria and the Mediterranean Sea; and west by the Aegean Sea.

 

One of the world’s earliest permanently settled regions, present-day Turkey was home to important Neolithic sites, and was inhabited by various civilisations. Hellenization started in the area during the era of Alexander the Great and continued into the Byzantine era.

 

Turkey is a predominantly mountainous country, and true lowland is confined to the coastal fringes. About one-fourth of the surface has an elevation above 4,000 feet (1,200 metres), and less than two-fifths lies below 1,500 feet (460 metres). Mountain crests exceed 7,500 feet (2,300 metres) in many places, particularly in the east, where Turkey’s highest mountain, Mount Ararat, reaches 16,945 feet (5,165 metres) close to the borders with Armenia and Iran.

In the southeast the Uludoruk Peak reaches 15,563 feet (4,744 metres); though further west, the Demirkazık Peak (12,320 feet [3,755 metres]) and Mount Aydos (11,414 feet [3,479 metres]) are also significant peaks. Steep slopes are common throughout the country, and flat or gently sloping land makes up barely one-sixth of the total area.

These relief features affect other aspects of the physical environment, producing climates often much harsher than might be expected for a country of Turkey’s latitude and reducing the availability and productivity of agricultural land. Structurally, the country lies within the geologically young folded-mountain zone of Eurasia, which in Turkey trends predominantly east to west. The geology of Turkey is complex, with sedimentary rocks ranging from Paleozoic to Quaternary, numerous intrusions, and extensive areas of volcanic material. Four main regions can be identified: the northern folded zone, the southern folded zone, the central massif, and the Arabian platform.

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Emma Churchill

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