Evolución geomorfológica del cañón del río Guadalhorce en el Trías de Antequera (Archidona, Málaga)
AbstractThe 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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Durán Valsero JJ. Evolución geomorfológica del cañón del río Guadalhorce en el Trías de Antequera (Archidona, Málaga). CIG [Internet]. 2013 May 21 [cited 2023 Jun. 11];10:43-54. Available from: https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/923
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