Turkey
History
Antiquity
The Anatolian peninsula, comprising most of modern Turkey, is one of the oldest continuously inhabited regions in the world. The earliest Neolithic settlements such as Çatalhöyük (Pottery Neolithic), Çayönü (Pre-Pottery Neolithic A to Pottery Neolithic), Nevalı Çori (Pre-Pottery Neolithic B), Hacılar (Pottery Neolithic), Göbekli Tepe (Pre-Pottery Neolithic A) and Mersin are considered to be among the earliest human settlements in the world.[23]
The settlement of Troy started in the Neolithic and continued into the Iron Age. Through recorded history, Anatolians have spoken Indo-European, Semitic and Kartvelian 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 radiated.[24] The Hattians were an ancient people who inhabited the southeastern part of Anatolia, noted at least as early as ca. 2300. Indo-European Hittites came to Anatolia and gradually absorbed Hattians ca. 2000–1700 BC. The first major empire in the area was founded by the Hittites, from the eighteenth through the 13th century BC. The Assyrians colonized parts of southeastern Turkey as far back as 1950 BC until the year 612 BC, when the Assyrian Empire was conquered by the Chaldean dynasty in Babylon.[25][26] Following the Hittite collapse, the Phrygians, an Indo-European people, achieved ascendancy until their kingdom was destroyed by the Cimmerians in the 7th century BC.[27] The most powerful of Phrygia’s successor states were Lydia, Caria and Lycia. The Lydians and Lycians spoke languages that were fundamentally Indo-European, but both languages had acquired non-Indo-European elements prior to the Hittite and Hellenistic periods.
Starting around 1200 BC, the coast of Anatolia was heavily settled by Aeolian and Ionian Greeks. Numerous important cities were founded by these colonists, such as Miletus, Ephesus, Smyrna (modern Ä°zmir), and Byzantium (later Constantinople and Istanbul). The first state established in Anatolia that was called Armenia by neighboring peoples (Hecataeus of Miletus and Behistun Inscription) was the state of the Armenian Orontid dynasty. Anatolia was conquered by the Persian Achaemenid Empire during the 6th and 5th centuries BC and later fell to Alexander the Great in 334 BC.[28] Anatolia was subsequently divided into a number of small Hellenistic kingdoms (including Bithynia, Cappadocia, Pergamum, and Pontus), all of which had succumbed to the Roman Republic by the mid-1st century BC.[29] Arsacid Armenia, the first state to accept Christianity as official religion had lands in Anatolia.
Geography
Turkey is a transcontinental[81] Eurasian country. Asian Turkey (made up largely of Anatolia), which includes 97% of the country, is separated from European Turkey by the Bosphorus, the Sea of Marmara, and the Dardanelles (which together form a water link between the Black Sea and the Mediterranean). European Turkey (eastern Thrace or Rumelia in the Balkan peninsula) comprises 3% of the country.[82]
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.[79] It lies between latitudes 35° and 43° N, and longitudes 25° and 45° E. Turkey’s area, including lakes, occupies 783,562[83] square kilometres (300,948 sq mi), of which 755,688 square kilometres (291,773 sq mi) are in Southwest Asia and 23,764 square kilometres (9,174 sq mi) in Europe.[79] Turkey is the world’s 37th-largest country in terms of area. The country is encircled by seas on three sides: the Aegean Sea to the west, the Black Sea to the north and the Mediterranean to the south. Turkey also contains the Sea of Marmara in the northwest.[84]
The European section of Turkey, East Thrace, forms the borders of Turkey with Greece and Bulgaria. The Asian part of the country, Anatolia, consists of a high central plateau with narrow coastal plains, between the KöroÄŸlu and Pontic mountain ranges 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 (16,946 ft).[84][85] Lake Tuz, Turkey’s third-largest lake, is a macroscopically visible feature in the middle of the country.
Turkey is divided into seven census regions: Marmara, Aegean, Black Sea, Central Anatolia, Eastern Anatolia, Southeastern Anatolia and the Mediterranean. The uneven north Anatolian terrain running along the Black Sea resembles a long, narrow belt. This region comprises approximately one-sixth of Turkey’s total land area. As a general trend, the inland Anatolian plateau becomes increasingly rugged as it progresses eastward.[84]
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. There is an earthquake fault line across the north of the country from west to east, which caused a major earthquake in 1999.[86]
Climate
The coastal areas of Turkey bordering the Aegean Sea and the Mediterranean Sea have a temperate Mediterranean climate, with hot, dry summers and mild to cool, wet winters. The coastal areas of Turkey bordering the Black Sea have a temperate Oceanic climate with warm, wet summers and cool to cold, wet winters. The Turkish Black Sea coast receives the greatest amount of precipitation and is the only region of Turkey that receives high precipitation throughout the year. The eastern part of that coast averages 2,500 millimeters annually which is the highest precipitation in the country.
The coastal areas of Turkey bordering the Sea of Marmara (including Istanbul), which connects the Aegean Sea and the Black Sea, have a transitional climate between a temperate Mediterranean climate and a temperate Oceanic climate with warm to hot, moderately dry summers and cool to cold, wet winters. Snow does occur on the coastal areas of the Sea of Marmara and the Black Sea almost every winter, but it usually lies no more than a few days. Snow on the other hand is rare in the coastal areas of the Aegean Sea and very rare in the coastal areas of the Mediterranean Sea.
Conditions can be much harsher in the more arid interior. Mountains close to the coast prevent Mediterranean influences from extending inland, giving the central Anatolian plateau of the interior of Turkey a continental climate with sharply contrasting seasons.
Winters on the plateau are especially severe. Temperatures of −30 °C to −40 °C (−22 °F to −40 °F) can occur in eastern Anatolia, and snow may lie on the ground at least 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 driest.[87]
Economy
Turkey has the world’s 15th largest GDP-PPP[5] and 17th largest Nominal GDP.[7] The country is a founding member of the OECD and the G-20 major economies. During the first six decades of the republic, between 1923 and 1983, Turkey has mostly adhered to a quasi-statist approach with strict government planning of the budget and government-imposed limitations over private sector participation, foreign trade, flow of foreign currency, and foreign direct investment. However in 1983 Prime Minister Turgut Özal initiated a series of reforms designed to shift the economy from a statist, insulated system to a more private-sector, market-based model.[47]
The reforms spurred rapid growth, but this growth was punctuated by sharp recessions and financial crises in 1994, 1999 (following the earthquake of that year),[88] and 2001,[89] resulting in an average of 4% GDP growth per annum between 1981 and 2003.[90] Lack of additional fiscal reforms, combined with large and growing public sector deficits and widespread corruption, resulted in high inflation, a weak banking sector and increased macroeconomic volatility.[91] Since the economic crisis of 2001 and the reforms initiated by the finance minister of the time, Kemal DerviÅŸ, inflation has fallen to single-digit numbers, investor confidence and foreign investment have soared, and unemployment has fallen. The International Monetary Fund forecasts a 6% inflation rate for Turkey in 2008.
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