Ripples in the Barrika flysch on the Spanish Basque coast. Flysch formed at the end of the Mesozoic era, in the Cretaceous - flysch is formed by the accumulation of sediments following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular strata of sandstone and limestone, here straightened by the Pyrenean orogeny and cleared by erosion - Biscay- Basque Country - Spain
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Image Number: 4413-68462422Rights ManagedCredit Line:Jean-Philippe Delobelle/Biosphoto/SuperStockCollection:Biosphoto Contributor:Jean-Philippe Delobelle Model Release:NoProperty Release:NoResolution:7861×5240
