Síntesis de la evolución geomorfológica de Galicia Occidental

Abstract

This paper presents an actualization of the ideas about the geodinámicaI and geomorphological setting of Western Galicia, as well as the cenozoic evolution, and a model were the evolutionary sequence is proposed. The present relief seems to be a response to the fluvial action (incision and processes of captures), as a consequence of the base level changes along the Cenozoic. The Rías were formed in that way, together with widespread entrenchment of the drainage net of western Calida