Evolución geomorfológica del cañón del río Guadalhorce en el Trías de Antequera (Archidona, Málaga)
Juan José Durán Valsero
Cuadernos de Investigación Geográfica · 2013
doi:10.18172/cig.923 (opens in a new tab)
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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
Abstract licence: CC BY
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