LANGUAGE

Historically, Turkic people have lived and left their influence throughout many parts of Eurasia. Turkish political history began with the creation of the powerful Hunnic State, which was able to expand its borders from Eastern Turkestan and Central Asia to Central and Western Europe under the command of Attila.

After the Huns, until 1040 a series of states founded by various Turkic tribes rose to prominence and consequently collapsed due to invasions from other Turkic tribes. One group in particular was the House of Seljuk, a branch of the Kınık Oğuz Turks who, in the 9th century, resided on the periphery of the Muslim world, north of the Caspian and Aral Seas in the Yabghu Khaganate of the Oğuz confederacy. In the 10th century, the Seljuks migrated from their homelands in Central Asia into the eastern Anatolian regions.

Following their victory over the Byzantine Empire in the Battle of Manzikert in 1071, the Turks permanently settled in Anatolia, giving rise to the Anatolian Seljuk State which developed as a separate branch of the larger Seljuk Empire. During the time of the Seljuk dominance, there were two other prominent Turkish states, the Karahanids and Ghaznavids who became unified under Seljuk rule. In 1243, the Seljuk armies were defeated by the Mongols and the power of the empire slowly disintegrated. In its wake, one of the Turkish principalities governed by Osman I was to evolve into the Ottoman Empire, thus filling the void left by the collapsed Seljuks and Byzantines.

The Ottoman Empire interacted with both Eastern and Western cultures throughout its 623-year history. In the 16th and 17th centuries, it was among the world's most powerful political entities, often locking horns with the powers of eastern Europe in its steady advance through the Balkans and the southern part of the Polish-Lithuanian Commonwealth. Following years of decline, the Ottoman Empire entered World War I through the Ottoman-German Alliance in 1914, and was ultimately defeated. After the war, the victorious Allied Powers sought the dismemberment of the Ottoman state through the Treaty of Sèvres.

Republican era

The occupation of Istanbul and İzmir by the Allies in the aftermath of World War I prompted the establishment of the Turkish national movement. Under the leadership of Mustafa Kemal Pasha, a military commander who had distinguished himself during the Battle of Gallipoli, the Turkish War of Independence was waged with the aim of revoking the terms of the Treaty of Sèvres. By September 18, 1922, the occupying armies were repelled and the country saw the birth of the new Turkish state. On November 1, the newly founded parliament formally abolished the Sultanate, thus ending 623 years of Ottoman rule. The Treaty of Lausanne of 1923 led to the international recognition of the sovereignty of the newly formed "Republic of Turkey" as the successor state of the Ottoman Empire, and the republic was officially proclaimed on October 29, 1923, in the new capital Ankara.

Mustafa Kemal became the republic's first president and subsequently introduced many radical reforms with the aim of founding a new secular republic from the remnants of its Ottoman past. The Turkish parliament presented Mustafa Kemal with the honorific name "Atatürk" (Father of the Turks) in 1934.

GEOGRAPHY AND CLIMATE

The territory of Turkey is more than 1,600 kilometres (1,000 mi) long and 800 km (500 mi) wide, with a roughly rectangular shape. Turkey's area, inclusive of lakes, occupies 783,562 square kilometres.

The European section of Turkey, in the northwest, is Eastern Thrace, and forms the borders of Turkey with Greece and Bulgaria. The Asian part of the country, Anatolia (also called Asia Minor), consists of a high central plateau with narrow coastal plains, between the East-Black Sea mountain range to the north and the Taurus Mountains to the south. Eastern Turkey has a more mountainous landscape, and is home to the sources of rivers such as the Euphrates, Tigris and Aras, and contains Lake Van and Mount Ararat, Turkey's highest point at 5,165 metres (16,944 ft).

Turkey's varied landscapes are the product of complex earth movements that have shaped the region over thousands of years and still manifest themselves in fairly frequent earthquakes and occasional volcanic eruptions. The Bosporus and the Dardanelles owe their existence to the fault lines running through Turkey that led to the creation of the Black Sea.

Turkey has a Mediterranean 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 Mediterranean influences from extending inland, giving the interior of Turkey a continental climate with distinct seasons. The central Anatolian Plateau is much more subject to extremes than coastal areas. Winters on the plateau are especially severe. Temperatures of −30 °C to −40 °C (−22 °F to -40 °F) can occur in the mountainous areas in the east, and snow may lie on the ground 120 days of the year. In the west, winter temperatures average below 1 °C (34 °F). Summers are hot and dry, with temperatures generally above 30 °C (86 °F) in the day. Annual precipitation averages about 400 millimetres (15 in), 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 millimetres (12 in). May is generally the wettest month, whereas July and August are the most dry.

CULTURE