Le Alluvioni pedemontane dell'Argentiera (Sardegna nord-occidentale)

In this note are briefly described the pebbly continental alluvia that border the eastward Paleozoic complex of Argentiera area (North-Western Sardinia). These alluvia, defined like glacis probably würmian age, were originated from two different flows, which were divergent among themselfes, in metamorfic area that constitued its hinterland