Obruk Plateau Geoway
Kızören Sinkhole
Medium
Neojen-Kuvaterner
Kızören Sinkhole is a huge sinkhole structure formed as a result of karst collapse. This structure, which is the product of hundreds of years of geological processes, is one of the most striking examples of the Konya Obrukları Plateau.
How Was It Formed?
Formed by dissolution of underground limestone and ceiling collapse. Depth can exceed 100 meters.
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