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Torcal de Antequera | Karst landforms

WI_e5080.jpg

This rugged landscape at approx. 1100-1400 m asl. is the result of millions of years of chemical and mechanical weathering of the prevailing limestone. The often regular arrangement of fractures, where both types of weathering are most intense, and the largely horizontal bedding of the rock layers, have led to spectacular landforms.

Location
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Created
on Sunday 9 February 2020 by Martin Mergili
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2756 visits, CC BY-NC-SA 4.0 DEED license