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.