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Photographer’s Note

Volcanic eruptions began in Cappadocia in the Upper Miocene about 70 million years ago. The lava flew from volcanoes submerged in lakes. The plateau of tuff formed from the materials discharged by the main volcanoes was then continuously altered by the eruptions of smaller and less violent volcanoes. From the Upper Pliocene onwards, these layers of tuff were exposed to erosion by rain and the waters of lakes and rivers, paticularly the Kizilirmak, resulting in what we see today. Foodwater pouring down the sides of valleys combined with strong winds tore away the softer volcanic rock exposing the harder parts and resulting in the formations known an "fairy chimneys" of which there are several types in Cappadocia - conical pointed, columnar, or mushroom-shaped. Here in the very spectacular "Love Valley".

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Additional Photos by JM Hullot (vincz) Gold Star Critiquer/Gold Star Workshop Editor/Gold Note Writer [C: 2907 W: 85 N: 5445] (19039)
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