Add to ORKGIt is well known that a large part of the landslides which every year occur in the world are triggered by rainfalls. However, the mechanics of slope movements due to pore pressure change is not completely clarified. Such a topic is the subject of this report where either the case of first-time slides or that of landslide reactivation are examined. It is shown that simple models can reproduce both processes of slope failure, and may help in predicting the slope behaviour, with particular reference to the rate of induced movement
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
Earthflows are typical landslides in tectonized clay shales. In the long-term stage after triggering...
It is well known that a large part of the landslides which every year occur in the world are trigge...
It is well known that many landslides, which occur every year in the world, are triggered by rainfal...
The rate of slope movement has major socio-economic implications on the rapid global urbanization, w...
Forecasting the possibility of flow-type failures within a slow-moving landslide mass is rarely take...
Reactivated landslides in stiff clays and shales typically move on a pre-existing shear surface and ...
The analysis of the behaviour of natural slopes is generally performed in the assumption of fully dr...
Landslides triggered by hydraulic perturbations are initiated by a decrease in the effective stress,...
Risk management for natural terrain landslides requires understanding of the complex underlying proc...
One of the factors causing the acceleration of landslides is the loss of strength of the soil involv...
The paper discusses the field investigations, geotechnical characterization and time evolution of hor...
Experience shows that slope movements occurring in similar geomorphogical contexts may display very ...
Earthflows are typical landslides in tectonized clay shales. In the long-term stage after triggering...
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
Earthflows are typical landslides in tectonized clay shales. In the long-term stage after triggering...
It is well known that a large part of the landslides which every year occur in the world are trigge...
It is well known that many landslides, which occur every year in the world, are triggered by rainfal...
The rate of slope movement has major socio-economic implications on the rapid global urbanization, w...
Forecasting the possibility of flow-type failures within a slow-moving landslide mass is rarely take...
Reactivated landslides in stiff clays and shales typically move on a pre-existing shear surface and ...
The analysis of the behaviour of natural slopes is generally performed in the assumption of fully dr...
Landslides triggered by hydraulic perturbations are initiated by a decrease in the effective stress,...
Risk management for natural terrain landslides requires understanding of the complex underlying proc...
One of the factors causing the acceleration of landslides is the loss of strength of the soil involv...
The paper discusses the field investigations, geotechnical characterization and time evolution of hor...
Experience shows that slope movements occurring in similar geomorphogical contexts may display very ...
Earthflows are typical landslides in tectonized clay shales. In the long-term stage after triggering...
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
The development of progressive failure in slopes is a poorly understood process, and relatively few ...
Earthflows are typical landslides in tectonized clay shales. In the long-term stage after triggering...