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EnglishThe 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.
| Titolo: | Geomorphological map of the Landslide of Salò (Brescia) |
| Autori interni: | |
| Anno del prodotto: | 1992 |
| Rivista: | |
| 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. |
| Handle: | http://hdl.handle.net/11568/232141 |
| Appare nelle tipologie: | 4.1 Contributo in Atti di convegno |
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