The paper deals with the interpretation of slow slide mechanisms involving detrital covers, whose movements, being related to the current shear stress level, are essentially due to variations of pore water pressure regimen. The interpretation has been carried out through a simple mechanical model whose movements, on the sliding surface, are assumed of visco-plastic type. Results of computations show a satisfactory agreement with the observed behaviour of the well monitored Fosso S. Martino landslide (Italian Apennines).

A simple mechanical model for the interpretation of translational active landslides involving detrital covers.

FERLISI, Settimio
2004

Abstract

The paper deals with the interpretation of slow slide mechanisms involving detrital covers, whose movements, being related to the current shear stress level, are essentially due to variations of pore water pressure regimen. The interpretation has been carried out through a simple mechanical model whose movements, on the sliding surface, are assumed of visco-plastic type. Results of computations show a satisfactory agreement with the observed behaviour of the well monitored Fosso S. Martino landslide (Italian Apennines).
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11386/1068667
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