El acantilado de El Asperillo: Cuaternario reciente y fases históricas en el litoral de Huelva
Loading...
Publication date
Advisors
Department
Research group
Center
Abstract
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














