Rasgos generales del relieve en el sector suroriental de la Sierra Almijara (Málaga)

Abstract

The morphostructural landform o f this Betics coastal sector is conditioned by lithological, structural (Neotectonics) and geomorphologicai features. Tortonian planated relief was faulting during Mio-Pliocene age by a NW-SE oblique-slip and normal faults, like a stepped landscape, with a 700 m. of relative fall