The Cappadocia region is largely underlain by sedimentary rocks formed in lakes and streams, and ignimbrite deposits erupted from ancient volcanoes approximately 9 to 3 million years ago, during the late Miocene to Pliocene epochs. The rocks of Cappadocia near Goreme eroded into hundreds of spectacular pillars and minaret-like forms. The volcanic deposits are soft rocks that the people of the villages at the heart of the Cappadocia Region carved out to form houses, churches and monasteries. Goreme became a monastic center between 300-1200 AD.
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