Numerous mass movements of different typology characterize both mountainous and piedmont sectors of the Emilia-Romagna Region (Apennine chain, North Italy). Although a less spatially frequent landslide typology within the region, rock falls represent severe threats to buildings, roads and persons due to their high propagation velocity. This paper presents an extract of the Emilia-Romagna regional map of the rock fall runout areas at a scale of 1:25,000. The analysis of rock fall runout areas was based upon a three-dimensional morphological method (TDM). The zone presented in the Main Map encompasses the area surrounding Mount Cimone, in the Emilia-Romagna Region. The proposed regional map of rockfall runout is noteworthy for plannin...
Many types of thematic maps dealing with slope movements have been proposed in the scientific litera...
In the mountainous areas, rockfalls are a common type of massmovements that represents a major cause...
Landslide dams are a particular kind of natural dams which form when an earth or rock mass reaches a...
<p>Numerous mass movements of different typology characterize both mountainous and piedmont sectors ...
A map derived by rockfall analysis at Mount Pellegrino is presented herein. The study area is affect...
A landslide hazard zonation is a division of the land surface into areas, and the relative ranking...
The Monte Gallo area is a carbonate relief that develops a significant nature reserve and highly att...
The long-lasting earthquake sequence of Central Italy in 2016 triggered around 1370 landslides, most...
A hazard assessment has been performed on rock slopes impending over a segment of the Taorminese Roa...
Rockfalls are common in the steep and vertical slopes of the Campania carbonate massifs and ridges,...
In the last 20 years the natural oriented reserve of Monte Pellegrino is affected by several rockfal...
Determining landslide hazard at the national scale remains a difficult task. However, such a complex...
In the context of slope instability phenomena, the detachment of blocks from steep walls account for...
Extensive landslide occurrences affected the Emilia-Romagna Region (north Apennines, Italy) during M...
The extent of the study area is about 20 km2 and its elevation ranges from about 1300 m a.s.l. to 21...
Many types of thematic maps dealing with slope movements have been proposed in the scientific litera...
In the mountainous areas, rockfalls are a common type of massmovements that represents a major cause...
Landslide dams are a particular kind of natural dams which form when an earth or rock mass reaches a...
<p>Numerous mass movements of different typology characterize both mountainous and piedmont sectors ...
A map derived by rockfall analysis at Mount Pellegrino is presented herein. The study area is affect...
A landslide hazard zonation is a division of the land surface into areas, and the relative ranking...
The Monte Gallo area is a carbonate relief that develops a significant nature reserve and highly att...
The long-lasting earthquake sequence of Central Italy in 2016 triggered around 1370 landslides, most...
A hazard assessment has been performed on rock slopes impending over a segment of the Taorminese Roa...
Rockfalls are common in the steep and vertical slopes of the Campania carbonate massifs and ridges,...
In the last 20 years the natural oriented reserve of Monte Pellegrino is affected by several rockfal...
Determining landslide hazard at the national scale remains a difficult task. However, such a complex...
In the context of slope instability phenomena, the detachment of blocks from steep walls account for...
Extensive landslide occurrences affected the Emilia-Romagna Region (north Apennines, Italy) during M...
The extent of the study area is about 20 km2 and its elevation ranges from about 1300 m a.s.l. to 21...
Many types of thematic maps dealing with slope movements have been proposed in the scientific litera...
In the mountainous areas, rockfalls are a common type of massmovements that represents a major cause...
Landslide dams are a particular kind of natural dams which form when an earth or rock mass reaches a...