Prasinites of the Marine de Scalo, Cap Corse. The rocks are green schists or prasinites, derived from the metamorphism of hydrated basalts under conditions of low pressure and temperature (ophiolitic complexes) - Pinu - Cap Corse - Corisca

Prasinites of the Marine de Scalo, Cap Corse. The rocks are green schists or prasinites, derived from the metamorphism of hydrated basalts under conditions of low pressure and temperature (ophiolitic complexes) - Pinu - Cap Corse - Corisca
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DETAILS
Image Number: 4413-35535907Rights ManagedCredit Line:Jean-Philippe Delobelle/Biosphoto/SuperStockCollection:BiosphotoContributor:Jean-Philippe DelobelleModel Release:NoProperty Release:NoResolution:5504×8256
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