La evolución de las laderas de la Sierra de Alhama (provincias de Granada y Málaga). Influencia de la estructura geológica y la paleosismicidad
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Abstract
La Sierra de Alhama presenta una muy diferente evolución de
sus laderas N y S. En la ladera sur hay un importante desarrollo de
deslizamientos de masas coherentes que están ausentes en la norte.
Estos se han producido por la diferente estructura de esa sierra en
cada ladera, combinada con la erosión, y probablemente por la acción de importantes paleoterremoto
The Sierra de Alhama presents a very different evolution of its N and S slopes. On its southern slope there is an important development of coherent landslides that are absent on the north slope. These have been produced by the different structure of that mountain on each slope, combined with erosion, and the probable action of important paleoearthquakes
The Sierra de Alhama presents a very different evolution of its N and S slopes. On its southern slope there is an important development of coherent landslides that are absent on the north slope. These have been produced by the different structure of that mountain on each slope, combined with erosion, and the probable action of important paleoearthquakes
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