Clemente Irigaray, E. Romero Cordón, José Chacón Montero
On 12 January 1970 a large slide took place on the old main Malaga-Granada road, characte rized initially by a rock fall with rotational sliding at the main scarp, followed by a widespread gra- vitational flow. The hidrogeological regime at a limestone-mar/ boundary, the lithology, the structural complexity and the high slope-angles result in a high susceptibility area to landsliding; the triggering factor on that occasion was high rainfall
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