The geological and geomorphological survey of the southern slope of the M. S.Bartolomeo (568 m a.s.l.) led to the identification of a lanslide on which Salò was built. A detailed geomorphological map is here presented. The landslide is referreble to the Early Holocene (older than 7100 +/- 150 14C yr BP). The causes of the landslide are mainly connected to the geological structure of the area: the southern slope of the M. S.Bartolomeo slumped on the plastic Oligocene marl outcropping at the base.
Geomorphological map of the Landslide of Salò (Brescia)
BARONI, CARLO
1992-01-01
Abstract
The geological and geomorphological survey of the southern slope of the M. S.Bartolomeo (568 m a.s.l.) led to the identification of a lanslide on which Salò was built. A detailed geomorphological map is here presented. The landslide is referreble to the Early Holocene (older than 7100 +/- 150 14C yr BP). The causes of the landslide are mainly connected to the geological structure of the area: the southern slope of the M. S.Bartolomeo slumped on the plastic Oligocene marl outcropping at the base.File in questo prodotto:
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