Learn more about Anatolia
Anatolia is a peninsula of Western Asia which forms the greater part of the Asian portion of Turkey, as opposed to the European portion (Thrace, or traditionally Rumelia). It is also often called by the Latin name of Asia Minor, which comes from the Greek Mikra Asia.
The name comes from the Greek Aνατολή (Αnatolē) or Ανατολία (Anatolía), which means "rising of the sun" or "east". The Turkish form Anadolu derives from the original Greek version and is often associated with ana ("mother") by popular etymology.
- See also: Geography of Turkey
The Anatolian peninsula is bounded by the Black Sea to the north, the Mediterranean Sea to the south, the Aegean Sea (itself an arm of the Mediterranean) to the west, and the bulk of the Asian mainland to the east. The peninsula is delineated by an indefinite line from the Black Sea to the Gulf of İskenderun, thereby covering about 60% of modern-day Turkey. The Anatolian Plateau is the large and semiarid central plateau, which is rimmed by hills and mountains that in many places limit the access to the fertile, densely settled coastal regions.
Anatolia's terrain is structurally complex. A central massif composed of uplifted blocks and downfolded troughs, covered by recent deposits and giving the appearance of a plateau with rough terrain, is wedged between two folded mountain ranges that converge in the east. True lowland is confined to a few narrow coastal strips along the Black Sea and Mediterranean Sea coasts. Flat or gently sloping land is rare and largely confined to the deltas of the Halys River, the coastal plains of Cilicia, and the valley floors of the Gediz River and the Büyükmenderes River, and some interior high plains in Anatolia, mainly around Tuz Gölü (Salt Lake) and Konya Ovasi (Konya Basin).
The Black Sea region, loosely called Pontus by various scholars, has a steep, rocky coast with rivers that cascade through the gorges of the coastal ranges. A few larger rivers, those cutting back through the Pontic Mountains (Doğu Karadeniz Dağları), have tributaries that flow in broad, elevated basins. Access inland from the coast is limited to a few narrow valleys because mountain ridges, with elevations of 1,525 to 1,800 m in the west and 3,000 to 4,000 m in the east in Kaçkar Mountains, form an almost unbroken wall separating the coast from the interior. The higher slopes facing southwest tend to be densely wet. Because of these natural conditions, the Black Sea coast historically has been isolated from Anatolia.
The North Anatolian Mountains in the north are an interrupted chain of folded highlands that generally parallel the Black Sea coast. In the west, the mountains tend to be low, with elevations rarely exceeding 1,500 m, but they rise in an easterly direction to heights greater than 3,000 m south of Rize. Lengthy, troughlike valleys and basins characterize the mountains. Rivers flow from the mountains toward the Black Sea. The southern slopes—facing the Anatolian Plateau—are mostly unwooded, but the northern slopes contain dense growths of both deciduous and evergreen trees.
The narrow coastal plains of the Mediterranean region, separated from the Anatolian plateau by the Taurus Mountains, which reach elevations of 2,000 to 2,750 m, are cultivated intensively. Fertile soils and a warm climate make the Mediterranean coast ideal for growing citrus fruits, grapes, figs, bananas, various vegetables, barley, wheat, and, in irrigated areas, rice and cotton. The Çukurova in the east is a plain that is the most developed agricultural area of the Mediterranean region.
Stretching inland from the Aegean coastal plain, the Central Anatolian occupies the area between the two zones of the folded mountains, extending east to the point where the two ranges converge. The plateau-like, semiarid highlands of Anatolia are considered the heartland of the country. The region varies in elevation from 600 to 1,200 m from west to east. The two largest basins on the plateau are the Konya Ovasi and the basin occupied by the large salt lake, Tuz Gölü. Both basins are characterized by inland drainage. Wooded areas are confined to the northwest and northeast of the plateau.
Eastern Anatolia, where the Pontus and Taurus mountain ranges converge, is rugged country with higher elevations, a more severe climate, and greater precipitation than are found on the Anatolian Plateau. The region is known as the Anti-Taurus, and the average elevation of its peaks exceeds 3,000 m. Mount Ararat, at 5,137 m the highest point in Turkey, is located in the Anti-Taurus. Lake Van is situated in the mountains at an elevation of 1,546 m. The headwaters of three major rivers arise in the Anti-Taurus: the east-flowing Aras, which empties into the Caspian Sea; the south-flowing Euphrates; and the south-flowing Tigris, which eventually joins the Euphrates in Iraq before emptying into the Persian Gulf. Several small streams that empty into the Black Sea or landlocked Lake Van also originate in these mountains.
Southeast Anatolia south of the Anti-Taurus Mountains. It is a region of rolling hills and a broad plateau surface that extends into Syria. Elevations decrease gradually, from about 800 m in the north to about 500 m in the south. Traditionally, wheat and barley were the main crops of the region, but the inauguration of major new irrigation projects in the 1980s has led to greater agricultural diversity and development.
Temperatures of Anatolia
Ankara (central Anatolia)
Antalya (southern Anatolia)
Mountains close to the coast prevent Mediterranean influences from extending inland, giving the interior of Turkey a continental climate with distinct seasons. The Anatolian Plateau is much more subject to extremes than are the coastal areas. Winters on the plateau are especially severe. Temperatures of -30°C to -40°C 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. Summers are hot and dry, with temperatures above 30°C. Annual precipitation averages about 400 mm, with actual amounts determined by elevation. The driest regions are the Konya Ovasi and the Malatya Ovasi, where annual rainfall frequently is less than 300 mm. May is generally the wettest month and July and August the driest.
 Ecoregions of Anatolia
Anatolia's diverse topography and climate has encouraged a similar diversity of plant and animal communities. The mountains and coastal plain of northern Anatolia, with its humid and mild climate, is home to temperate broadleaf, mixed, and coniferous forests. The central and eastern plateau, with its drier continental climate, is home to deciduous forests and forest steppes. Western and southern Anatolia, which have a Mediterranean climate, are home to Mediterranean forests, woodlands, and shrub ecoregions.
Because of its strategic location at the intersection of Asia and Europe, Anatolia has been a cradle for several civilizations since prehistoric ages, with Neolithic settlements such as Çatalhöyük (Pottery Neolithic), Çayönü (Pre-Pottery Neolithic A to pottery Neolithic), Nevali Cori (Pre-Pottery Neolithic B), Hacilar (Pottery Neolithic), Göbekli Tepe (Pre-Pottery Neolithic A) and Mersin. The settlement of Troy starts in the Neolithic and continues forward into the Iron Age. Major civilizations and peoples that have settled in or conquered Anatolia include the Colchians, Hattians, Luwians, Hittites, Phrygians, Cimmerians, Lydians, Persians, Celts, Tabals, Meshechs, Greeks, Pelasgians, Armenians, Romans, Goths, Kurds, Byzantines, Seljuk Turks, and Ottomans. These peoples belonged to many varied ethnic and linguistic traditions. Through recorded history, Anatolians have spoken both Indo-European and Semitic languages, as well as many languages of uncertain affiliation. In fact, given the antiquity of the Indo-European Hittite and Luwian languages, some scholars have proposed Anatolia as the hypothetical center from which the Indo-European languages have radiated. Other authors have proposed an Anatolian origin for the Etruscans of ancient Italy and the Elymians of Sicily.
Today the inhabitants of Anatolia are mostly native speakers of the Turkish language, which was introduced with the conquest of Anatolia by Turkic peoples and the rise of the Seljuk Empire in the 11th century. However, Anatolia remained multi-ethnic until the early 20th century (see Rise of Nationalism under the Ottoman Empire). The last population exchange, occurring as result of the Treaty of Lausanne between Turkey and Greece, eliminated most of the Turks in Greece and most of the Greeks in Turkey. A significant Kurdish ethnic and linguistic minority exists in the south eastern regions, while Armenians and Georgians used to have a presence in the northeast.
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|States that ruled over Anatolia|
|Old Kingdom||Ionia||Byzantine Empire|
|New Kingdom||Hellenistic Greece||Nicaean Empire|
|Urartu||Persian Empire||Roman Greece|
|Republic of Turkey|
 See also
- Saint Anatolia, Roman Catholic Saint
- Administrative structures during the Ottoman Period; the article Subdivisions of the Ottoman Empire.
- Ancient Greece
- Hayastan (Greater Armenia)
- Cilicia (Lesser Armenia)
- Western Armenia (Ottoman Armenia)
- List of ethnic groups
- Ancient Near East
- Middle East
- History of Ottoman Armenia
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