Pagés Valcarlos, J. L.Vidal Romani, J. R.2015-04-292015-04-291997http://hdl.handle.net/10272/10468This 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 CalidaspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Geomorphological evolutionFluvial CapturesRíasGaliciajournal articleopen access