AbstractThe magnitude of mass movements, which may be expressed by their dimension in terms of area or volume, is an important component of intensity together with velocity. In the case of slow-moving deep-seated landslides, the expected magnitude is the prevalent parameter for defining intensity when assessed as a spatially distributed variable in a given area. In particular, the frequency–volume statistics of past landslides may be used to understand and predict the magnitude of new landslides and reactivations. In this paper we study the spatial properties of volume frequency distributions in the Arno river basin (Central Italy, about 9100km2). The overall landslide inventory taken into account (around 27,500 events) shows a power-law sc...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
The influence of deep-seated gravitational slope deformations (DSGSDs) on the distribution of transl...
We have studied the frequency-area statistics of landslides in central Italy. We consider two data s...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
Discovering the physical explanations behind the power-law distribution of landslides can provide va...
A power‐law relation for the frequency‐area distribution (FAD) of medium and large landslides (e.g.,...
Linking landslide size and frequency is important at both human and geological timescales for quant...
Despite the availability of studies on the frequency density of landslide areas in mountainous regio...
Landslides are generally associated with a trigger, such as an earthquake, a rapid snowmelt or a lar...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
International audiencePower-law distributions of landslides and rockfalls observed under various con...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
International audienceDespite the idea that topography could control landslide size scaling law, the...
Ranging in size from very small to tremendous, landslides often cause loss of life and damage to inf...
For many geotechnical purposes, the proper estimation of shapes and dimensions of landslide rupture ...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
The influence of deep-seated gravitational slope deformations (DSGSDs) on the distribution of transl...
We have studied the frequency-area statistics of landslides in central Italy. We consider two data s...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
Discovering the physical explanations behind the power-law distribution of landslides can provide va...
A power‐law relation for the frequency‐area distribution (FAD) of medium and large landslides (e.g.,...
Linking landslide size and frequency is important at both human and geological timescales for quant...
Despite the availability of studies on the frequency density of landslide areas in mountainous regio...
Landslides are generally associated with a trigger, such as an earthquake, a rapid snowmelt or a lar...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
International audiencePower-law distributions of landslides and rockfalls observed under various con...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
International audienceDespite the idea that topography could control landslide size scaling law, the...
Ranging in size from very small to tremendous, landslides often cause loss of life and damage to inf...
For many geotechnical purposes, the proper estimation of shapes and dimensions of landslide rupture ...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
The influence of deep-seated gravitational slope deformations (DSGSDs) on the distribution of transl...
We have studied the frequency-area statistics of landslides in central Italy. We consider two data s...