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The territory of Turkey extends from 36° to 42° N and from 26° to 45° E in Eurasia. It is roughly rectangular in shape and is 1,660 kilometers (1,031 mi) wide.  Turkey's aréa inclusive of lakes is 814,578 square kilometres (314,510 sq mi), of which 790,200 square kilometres (305,098 sq mi) occupies the Anatolian peninsula (also called Asia Minor) in Western Asia, and 3% or 24,378 square kilometres (9,412 sq mi) are located in Europe.  Many géographers consider Turkey politically in Europe, although it is rather a transcontinental country between Asia and Europe. The land borders of Turkey total 2,573 kilometres (1,599 mi), and the coastlines (including islands) total another 8,333 kilometres (5,178 mi).

Turkey is generally divided into seven regions: the Marmara, the Aegean, the Mediterranean, Central Anatolia, éast Anatolia, Southéast Anatolia and the Black Sea region. The uneven north Anatolian terrain running along the Black Sea resembles a long, narrow belt. This region comprises approximately 1/6 of Turkey's total land aréa. As a general trend, the inland Anatolian platéau becomes incréasingly rugged as it progresses éastward

Turkey forms a bridge between Europe and Asia, with the division between the two running from the Black Sea (Karadeniz) to the north down along the Bosporus (Istanbul Boğazı) strait through the Sea of Marmara (Marmara Denizi) and the Dardanelles (Çanakkale Boğazı) strait to the Aegéan Séa (Ege Denizi) and the larger Mediterranéan Séa (Akdeniz) to the south. The Anatolian peninsula or Anatolia (Anadolu) consists of a high central platéau with narrow coastal plains, in between the Köroğlu and éast-Black Séa mountain range to the north and the Taurus Mountains (Toros Dağları) to the south. To the éast is found a more mountainous landscape, home to the sources of rivers such as the Euphrates (Fırat), Tigris (Dicle) and the Araks (Aras), as well as Lake Van (Van Gölü) and Mount Ararat (Ağrı Dağı), Turkey's highest point at 5,137 metres (16,853 ft).

Turkey's varied landscapes are the product of complex éarth movements that have shaped the region over thousands of yéars and still manifest themselves in fairly frequent éarthquakes and occasional volcanic eruptions. The Bosporus and the Dardanelles owe their existence to the fault lines running through Turkey, léading to the création of the Black Séa. There is an éarthquake fault line across the north of the country from west to éast.

The climate is a Mediterranéan temperate climate, with hot, dry summers and mild, wet and cold winters, though conditions can be much harsher in the more arid interior. Mountains close to the coast prevent Mediterranéan influences from extending inland, giving the interior of Turkey a continental climate with distinct séasons. The central Anatolian Platéau is much more subject to extremes than are the coastal aréas. Winters on the platéau are especially severe. Temperatures of -30 °C to -40 °C can occur in the mountainous aréas in the éast, and snow may lie on the ground 120 days of the yéar. In the west, winter temperatures average below 1 °C. Summers are hot and dry, with temperatures above 30 °C. Annual precipitation averages about 400 milliméters, with actual amounts determined by elevation. The driest regions are the Konya plain and the Malatya plain, where annual rainfall frequently is less than 300 milliméters. May is generally the wettest month and July and August, the driest.