Cappadocia

Geography and climate Cappadocia lies in eastern Anatolia, in the center of what is now Turkey. The relief consists of a high plateau over 1000 m in altitude that is pierced by volcanic peaks, with Mount Erciyes near Kayseri being the tallest at 3916 m. The boundaries of historical Cappadocia are vague, particularly towards the west. To the south, the Taurus Mountains form the boundary with Cilicia and separate Cappadocia from the Mediterranean Sea. To the west, Cappadocia is bounded by the historical regions of Lycaonia to the southwest, and Galatia to the northwest. The Black Sea coastal ranges separate Cappadocia from Pontus and the Black Sea, while to the east Cappadocia is bounded by the upper Euphrates, before that river bends to the southeast to flow into Mesopotamia, and the Armenian Highland.This results in an area approximately 400 km east–west and 250 km north– south. Due to its inland location and high altitude, Cappadocia has a markedly continental climate, with hot dry summers and cold snowy winters.Rainfall is sparse and the region is largely semi-arid.

History Cappadocia was known as Hatti in the late Bronze Age, and was the homeland of the Hittite power centred at Hattusa. After the fall of the Hittite Empire, with the decline of the Syro-Cappadocians after their defeat by the Lydian king Croesus in the 6th century, Cappadocia was ruled by a sort of feudal aristocracy, dwelling in strong castles and keeping the peasants in a servile condition, which later made them apt for foreign slavery. It was included in the third Persian satrapy in the division established by Darius, but continued to be governed by rulers of its own, none apparently supreme over the whole country and all more or less tributaries of the Great King.

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