Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dome du Barrot

Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dome du Barrot
SuperStock offers millions of photos, videos, and stock assets to creatives around the world. This image of Mudcracks in the Permian pelites of the Cians Gorges, Alpes Maritimes, France. Permian pelites aged 250 Ma: clays of volcanic and detrital origin were oxidised under a tropical climate and slowly transformed into rocks, over a thickness of 1000 metres. Mudcracks were formed on the surface of sedimentation lagoons during dry periods in a tropical climate. Gorges du Cians, Dome du Barrot by Jean-Philippe Delobelle/Biosphoto is available for licensing today.
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Image Number:  4413-18973563Rights ManagedCredit Line:Jean-Philippe Delobelle/Biosphoto/SuperStockCollection:Contributor:Model Release:NoProperty Release:NoResolution:8256×5504
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