Detailed geological study of the western part of a new road leading to Lanjarón (Betic Cordillera) has revealed the existence of natural instabilities in metapelitic rock masses of the Alpurride Units. We have analysed the stability of the future slopes in the Cerro de la Escolta based on detailed geological mapping and measurement of structural data and mechanical discontinuities.
© 2001-2024 Fundación Dialnet · Todos los derechos reservados