Iván Martín Rojas, José Luis Díaz Hernández, M. Martín Quesada, Ramon Julià Brugués
Sinuosity, Facetation percentage, disectation percentage and width/high valley ratio geomorphic parameters are applied to the Alicun Spa resort mountain front. This front, defined by a normal fault, shows several springs originated during the Quaternary. Travertine deposits are related to the springs and the fault The travertine ages are correlated with the values from the geomorphic parameters, in order to obtain seismic risk information
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