El acantilado de El Asperillo: Cuaternario reciente y fases históricas en el litoral de Huelva

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Two kinds of formations are present in the stratigraphic chronosecuence of the El Asperillo cliffs (Huelva coastline, Spain): Late Pleistocene-Holocene (22.000-11.000 BP) organic-rich horizons, and Holocene-Recent (<5.000 BP) sand dunes systems

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Atribución-NoComercial-SinDerivadas 3.0 España
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España