Notas sobre las acumulaciones de ladera en el Macizo del Maigmó

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.