The time and space evolution of large earth slides in weak and complex rockmasses, that characterize the northern Apennines, is depending on geological setting and past climate. At the present the reactivation of these landslides are due to mainly to hydrogeological and geotechnical features. Hydrogeological and geotechnical features of these landslides are to be taken into account. In this landslide some hydrogeological and geotechnical data have been collected from 2003 to date.
Hydrogeological study of large landslides reactivation mechanism: the Mt. Modino project (Northern Apennines)
GARGINI, Alessandro;PICCININI, Leonardo;
2005
Abstract
The time and space evolution of large earth slides in weak and complex rockmasses, that characterize the northern Apennines, is depending on geological setting and past climate. At the present the reactivation of these landslides are due to mainly to hydrogeological and geotechnical features. Hydrogeological and geotechnical features of these landslides are to be taken into account. In this landslide some hydrogeological and geotechnical data have been collected from 2003 to date.File in questo prodotto:
Non ci sono file associati a questo prodotto.
I documenti in SFERA sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
