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

Juan José Durán Valsero

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



DOI: https://doi.org/10.18172/cig.923

Copyright (c) 2013 Juan José Durán Valsero

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This work is licensed under a Creative Commons Attribution 4.0 International License.

© Universidad de La Rioja, 2013

ISSN 0211-6820

EISSN 1697-9540