Remarkable flysch formations of Deba, Basque Coast Geopark, Basque Country, Spain. Flysch formed at the end of the Mesozoic era in the Cretaceous - flyschs are formed by sediment accumulation following repeated submarine avalanches, due to earthquakes, and producing after compaction and crystallization very regular layers of sandstone and limestone here recovered by Pyrenean orogeny and released by erosion.

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Image size: 5504x8256 pixels (18.3"x27.5" @300dpi)

Keywords

Environment / Hazard / Natural hazard / Seism

Area / Marine area / Sea bottom / Sedimentary bottom

World sea and ocean / Atlantic Ocean / North Atlantic Ocean / Bay of Biscay

Matter (substance) / Water (matter) / Water surface

July

Atmosphere / Meteorological phenomenon / Sky / blue sky

Earth's crust / Geological formation / Geologic stratum

Europe / European Union / Basque country

Atmosphere / Meteorological phenomenon / Tide / Low tide

Earth's crust / Erosion

Area / Strand / Rock shore

Earth's crust / Landform / Cliff

Leisure / Journey / Tourism

World mountain and summit / Pyrenees (Range)

Shot / Overview

Earth's crust / Rock

Earth's crust / Geological formation

Earth's crust / Rock / Sedimentary rock / Derivate rock / Flysch

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