The Tessina landslide is a large, seasonally active slope failure located on the southern slope of Mt. Teverone, in the Alpago valley of NE Italy, consisting of a complex system that has developed in the Tertiary Flysch deposit. In the paper analysis is presented of the movement of the landslide, concentrating on the EDM dataset, which provides a remarkable record of surface displacement patterns.

The use of surface monitoring data for the interpretation of landslide movement patterns.

MANTOVANI, Franco;
2005

Abstract

The Tessina landslide is a large, seasonally active slope failure located on the southern slope of Mt. Teverone, in the Alpago valley of NE Italy, consisting of a complex system that has developed in the Tertiary Flysch deposit. In the paper analysis is presented of the movement of the landslide, concentrating on the EDM dataset, which provides a remarkable record of surface displacement patterns.
2005
Petley, D. N.; Mantovani, Franco; F, ; BULMER M. H., AND ZANONI
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/1205409
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