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This study analyses the slope debris of the Maigmo mountain (Alicante), forms which are in charge of regulating these slopes. The relation between the morpho-structure is studied making a distinction between two different types of slopes. There is a clear difference between the present day screes or these belonging to a near past and more ancient deposits (Pleistocene). Amongst the first, apart from distinguishing several types depending on the perimetral morphology, we analyse the section in order to determinate the nature; on the other hand the deposits which lie underneath complete the morphology of these slopes.

Notas sobre las acumulaciones de ladera en el Macizo del Maigmó