La disolución de rocas evaporíticas : un importante factor geomorfológico en el Valle del Ebro

J. Mandado, J. Rodríguez Vidal, J. M. Tena

Abstract


The analysis of different physical-chemical factors for the solubilitation of the system gypsum-anhydrite remark the significance of textures and contents of NaCl in solutíon. Geomorphologíc processes such as the escarp and the dome of Remolinos or the depressions in El Castellar are effects of disolution phenomena for evaporitic materials in the Ebro Valley.



DOI: https://doi.org/10.18172/cig.931

Copyright (c) 2013 J. Mandado, J. Rodríguez Vidal, J. M. Tena

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

© Universidad de La Rioja, 2013

ISSN 0211-6820

EISSN 1697-9540