This study deals with clast morphological analysis from Pleistocene-Holocene alluvial fan deposits attending to their shape and roundness. These deposits infill the low area of nine coastal small basins located between cala Tirant and Fornells, at Northern Menorca (Balearic Islands). Clast morphology and shape analysis show that differences in basement lithology of each basin controls the clast abundance as well as bed thickness and joint style controls the clast form. Additionally, clast shape does not reflect evidences of transport mechanisms and agents due to the short distances of transport from the basin head.
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