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Limestone pavement

Limestone pavement

E415/0184

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Credit

ASTRID & HANNS-FRIEDER MICHLER / SCIENCE PHOTO LIBRARY ASTRID & HANNS-FRIEDER MICHLER / SCIENCE PHOTO LIBRARY

Caption

Limestone pavement. The joints have been enlarged by chemical weathering to form a pattern of clints (ridges) and grykes (clefts). Limestone pavements are typical of karst scenery, a type of limestone topography produced by percolating ground waters and underground streams, named after the Karst region in Slovenia. Photographed in the Austrian Alps.

Release details

Model release not required. Property release not required.

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