Open AccessEvolución geomorfológica del cañón del río Guadalhorce en el Trías de Antequera (Archidona, Málaga)
Author(s) -
Juan José Durán Valsero
Publication year - 2013
Publication title -
cuadernos de investigación geográfica
Language(s) - English
Resource type - Journals
eISSN - 1697-9540
pISSN - 0211-6820
DOI - 10.18172/cig.923
Subject(s) - geology , canyon , gypsum , geomorphology , trias , geochemistry , paleontology , phanerozoic , structural basin , cenozoic
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
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