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Ruiniform chaos of Rajol
Description
About 240 years, the Causses (limestone plateau*) were formed by the accumulation of marine sediments. The errection of the Pyrenees and the Alps provoked an uprising of the region and formed numerous cracks on the surface area. The streaming infiltrates there, sculping rocks by dissolution of limestone. The erosion is more or less active according to the resistance of rocks, that's why we observe ruiniform sculptures today.
Technical Information
Lat, Lng
44.13263.23071
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Altitude
0 m
Point of Interest updated on 08/05/2024
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Parc naturel régional des Grands Causses
71 Boulevard de l'Ayrolle 12100 MILLAU France
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