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A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps)
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A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps)
A Limestone Pavement with well developed Clints (blocks) and Grykes (gaps). This is Carboniferous age limestone, part of a large area of Karst above Austwick, Yorkshire, UK. Slightly acidic rainfall, erodes and enlarges naturally occurring joints in the limestone leaving a characteristic pavement surface. February 2018
naturepl.com / : Graham Eaton
Media ID 18284898
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Erosion Geology Geomorphology Karst Limestone Limestone Pavement Rock Yorkshire
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