We investigated movement kinematics of the Montaguto earth flow and dynamic of its most active sector using data from GPS surveys and an instrumentation station. Residual movement of the flow was concentrated where the basal slip-surface form risers, where deep drainages are not installed and/or where springs fed man-made earth-flow creeks. Movement within the most active sector of the earth flow, the Body, was characterized by short-lived acceleration and deceleration driven by water-table-level variation during the spring, and by a slow-persistent movement interrupted by small surges, triggered by rapid rises of the water table caused by heavy rainfall during the winter. Our results improve the knowledge of the behavior of the Montaguto e...
Active earthflows commonly exhibit seasonal movements controlled by rainfall, snowmelt, and in some ...
Surface mapping, GPS surveys, T-Lidar surveys, boreholes, seismic profiles, and HVSR measurements we...
The Mount Pizzuto earth flow has been periodically active in recent decades. Early in 2006, it surge...
We investigated movement kinematics of the Montaguto earth flow and dynamic of its most active secto...
This paper summarizes the methods, results, and interpretation of analyses carried out between 2006 ...
This paper aims to define the control exerted by geological setting on the evolution and segmentatio...
This paper aims to define the control exerted by geological setting on the evolution and segmentatio...
Historical movement of the Montaguto earth flow in southern Italy has periodically destroyed residen...
We reconstruct the deformational pattern of the Mount Pizzuto earth flow using displacement data der...
We investigated relations between slip-surface geometry and deformational structures and hydrologic ...
Surface mapping, GPS surveys, T-Lidar surveys, boreholes, seismic profiles, and HVSR measurements we...
The morphodynamic evolution of the Costa Gaveta slope and landslides is strongly influenced by syste...
We used aerial photos and field observations to produce multitemporal maps of the Caforchio earth fl...
Active earthflows commonly exhibit seasonal movements controlled by rainfall, snowmelt, and in some ...
Surface mapping, GPS surveys, T-Lidar surveys, boreholes, seismic profiles, and HVSR measurements we...
The Mount Pizzuto earth flow has been periodically active in recent decades. Early in 2006, it surge...
We investigated movement kinematics of the Montaguto earth flow and dynamic of its most active secto...
This paper summarizes the methods, results, and interpretation of analyses carried out between 2006 ...
This paper aims to define the control exerted by geological setting on the evolution and segmentatio...
This paper aims to define the control exerted by geological setting on the evolution and segmentatio...
Historical movement of the Montaguto earth flow in southern Italy has periodically destroyed residen...
We reconstruct the deformational pattern of the Mount Pizzuto earth flow using displacement data der...
We investigated relations between slip-surface geometry and deformational structures and hydrologic ...
Surface mapping, GPS surveys, T-Lidar surveys, boreholes, seismic profiles, and HVSR measurements we...
The morphodynamic evolution of the Costa Gaveta slope and landslides is strongly influenced by syste...
We used aerial photos and field observations to produce multitemporal maps of the Caforchio earth fl...
Active earthflows commonly exhibit seasonal movements controlled by rainfall, snowmelt, and in some ...
Surface mapping, GPS surveys, T-Lidar surveys, boreholes, seismic profiles, and HVSR measurements we...
The Mount Pizzuto earth flow has been periodically active in recent decades. Early in 2006, it surge...