SULL'ORIGINE DELLA VAL TROMPIA A SUD DI INZINO

The Autor describes the results of a research on the possible continuation of the Inzino faultdown to the lower Val Trompia.In his opinion its origin is probably not later than the middle Miocene.Italso gave rise to an overcut valley which widened during the Mcssinian.The dcep thickness of the alluvialconglomerates,as verified by the wells recently drilled north of Brescia,is ascribed to a strong subsidenceof the area south of the Nave-Gussago fault during the Pleistocene.