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Ramón Blanco-Chao, Manuela Costa-Casais, Daniel Cajade-Pascual and Gonzalo Gómez-Rey
During the last glaciation, thick nival and periglacial sediments buried large sectors of the NW coast of Spain. The sediments were mostly eroded by the rising sea level during the Holocene, but in several places they remain, forming sedimentary cliffs. ...
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