Evolución geomorfológica del cañón del río Guadalhorce en el Trías de Antequera (Archidona, Málaga)

Abstract

The geomorphological evolution of Guadalhorce River Canyon and aside are as is the result of the interaction of erosive processes ( on the surface and underground) and the Trias lifting ( due do the appearance, in depth, of gypsum and/or rock salt), since Pliocene, in such a way that superficial and suhtcrranean drainage and gypsiferous massifs karstification are closely joincd nowadays