Rodríguez Vidal, JoaquínCáceres Puro, Luis Miguel2017-08-212017-08-211993http://hdl.handle.net/10272/14058The 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 fallspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/GeomorphologyNeotectonicsBetic Rangejournal articleopen access