I ciottoli di Verrucano dei depositi quaternari situati ad ovest del Monte Albano e le loro aree sorgenti
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Abstract
Sulla base delle caratteristiche litologiche e sedimentologiche dei depositi di conoide e fluviali dell’area, viene delineatauna possibile evoluzione dell’idrografia fra il Pliocene Superiore e l’Olocene.
The fan and fluvial deposits of the area are investigated, mostly referring to their lithologic and sedimentologic features,of in order to work out the hydrographic pattern evolution since Upper Pliocene times.
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