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The geomorphological and geoarchaeological study made on the Paleolithic sites of Monforte de Lemosbasin (Lugo, Galicia), along with the available OSL datings, allowed us to correlate the Pleistocenedeposits found in the basin with erosion phases previously detected in the glacial and coastal sequencesof NW Iberia as well as in other Galician Paleolithic sites. Some of these phases may be attributed toHeinrich events. In this sense, the colluvial layers identified at Monforte de Lemos show the key roleplayed by morphogenetic processes in the configuration of the continental deposits during the H4 eventat the site of As Lamas and, probably, by H6 at the site of O Regueiral. These sites can be regarded asgood examples of the role played by erosion phases on site formation and post-depositional processes inNW Iberia archaeological sites. El estudio geomorfologico y geoarqueologico de los yacimientos Paleoliticos de la depresion de Monfortede Lemos (Lugo, Galicia), asi como las dataciones OSL nos permiten correlacionar los depositos coluvialesPleistocenos de la cuenca terciaria con los procesos erosivos identificados en depositos glaciares y costerosdel NW de la peninsula Iberica, asi como en otros yacimientos gallegos del Paleolitico. Algunas de estasfases pueden relacionarse con los episodios Heinrich. En este sentido, los niveles coluviales de Monfortede Lemos nos muestran la alta incidencia de los procesos morfogeneticos en los depositos continentalesdurante el H4, en el caso del yacimiento de As Lamas y, probablemente, del H6, en el yacimiento de ORegueiral. Son una muestra del papel desempenado por los episodios erosivos en la formacion de losyacimientos y efectos post-deposicionales identificados en los yacimientos arqueologicos del NW Peninsular.

estudos do quaternário

Geomorphological and geoarchaeological evolution of the Monforte de Lemos basin (Galicia , Spain). Erosion phases and post-depositional processes in NW Iberia