CRADLE OF CIVILIZATION
Cappadocia is one of the flowers of world with history, geography, and culture it has. Hence this extraordinary feature has drawn attention of the world and has been included into World Heritage List by UNESCO in 1985. Turkey is one of the nine countries taking place in World Heritage List.
Cappadocia Region located in the center of the Anatolian Peninsula, in the center of what is now Turkey, with its valley, canyon, hills and unusual rock formations. It is surrounded with Aksaray, Kayseri, Kırşehir, Nigde and Nevşehir city where formations are widespread as to the others. The relief consists of a high plateau over 1000m in altitude that is pierced by volcanic peaks, with Mount Erciyes (ancient Argaeus) near Kayseri (ancient Caesarea) 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 (250 mi) east–west and 250 km (160 mi) 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 to arid.
FORMATION OF CAPPADOCIA
60 million years ago Taurus Mountains rised up in 3rd geologic age. Volcanos started erupting with the compression of North Anatolian plateau. Mount Erciyes, Hasandag and Göllüdag, between two of them, spumed forth lava to the region. Ashes collected in the plateau formed a soft ash layer. Upper side of ash layer was covered with a thin lava layer consisted of basalt in some areas. Basalt cracked and fell apart. Rains started eroding soft tufa by weeping through the cracks. Winds also took part in the formation. Consequently, cones with hard basalt hat came into existence. Local people gave a name to these interesting and different kinds of rocks : “Fairy Chimneys”.