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bezeichnete
Abfolge besteht aus einer Wechsellagerung von Sand- und Tonsteinschichten und bildet den jüngsten Abschnitt der alpidischen (Unterkreide bis Paläogen) Flyschabfolge zwischen Deba und Zumaia (Geopark Baskische
333:– You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
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Part of the Eocene flysch sequence cropping out at Playa de
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Alpidische Flysch-Abfolge eozänen Alters an der Playa de
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Juan
Ignacio Baceta Caballero, Xabier Orue-Etxebarria, Estíbaliz Apellaniz Ingunza:
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Enseñanza de las
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43° 18′ 05.15″ N, 2° 15′ 37.45″ W
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
