refers to a low-lying plain or basin.

Geology

The filling of this depression occurred simultaneously with its uplift. At its base there are bioclastic calcarenites from the Upper Miocene. These materials are typical marine deposits in areas close to the coast. Marine marl was deposited on top of these rocks. On top of them there are essentially detrital materials from continental fluvial environments (clays, silts, sands, conglomerates and rocks typical of lacustrine

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