The de La Flecha river basin is located to the southwest of San Juan Province at around 31°50′ S, 68°57′ W. In this area a total of twenty debris-rock slides, in the Cordón de las Osamentas, were mapped and studied. The mode of failure of each was determined to be a rotational slide. The areal extent of the smallest observable landslide body is approximately 0.58 km2 and the largest is 367.76 km2. The slides were detected through high resolution satellite imagery interpretation, digital elevation models and field surveys, by identifying both the landslide detachment zones and landslide bodies based on the Geographic Information System (GIS). The slides have varying controlling factors, including lithology and slope, which seem to be the mai...
A megalandslide has been identified on the western hillslope of Cerro Uritorco peak (1.949 m a.s.l.)...
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de ...
The main objective of this paper is to consider the influence of Quaternary faults as likely trigger...
The distribution of late Pleistocene to Holocene rockslides in the western flank of the eastern moun...
As one of the main environmental effects of earthquakes, the distribution of landslides could reflec...
A large (>0.1 km2) and complex mass movement in the Central Andes of Argentina (final portion of Cor...
The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and nor...
In the Central Andean region of Argentina, we found gravimetric andgeomorphological evidence of an u...
This paper presents an inventory of landslides and hazard and risk zonation mapping along the Río Gr...
Landslides are downslope mass movements, which implies the combination of natural complex processes ...
A geomorphologic description of the Du´dar landslide (Granada, S Spain) has been carried out using a...
Drawing on historical documents and a detailed field study, we have been able to characterize the Gü...
The Fuegian Andes, in the southernmost part of South America, are characterized by a relatively youn...
En este trabajo se describe una avalancha de rocas muy bien preservada situada en el área de Las Maj...
Between 2001 and 2005, a large debris rock slide occurred on the western slope of the Cordillera de ...
A megalandslide has been identified on the western hillslope of Cerro Uritorco peak (1.949 m a.s.l.)...
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de ...
The main objective of this paper is to consider the influence of Quaternary faults as likely trigger...
The distribution of late Pleistocene to Holocene rockslides in the western flank of the eastern moun...
As one of the main environmental effects of earthquakes, the distribution of landslides could reflec...
A large (>0.1 km2) and complex mass movement in the Central Andes of Argentina (final portion of Cor...
The eastern foothills of the Central Andes, known as the Subandean Ranges, in Peru, Bolivia, and nor...
In the Central Andean region of Argentina, we found gravimetric andgeomorphological evidence of an u...
This paper presents an inventory of landslides and hazard and risk zonation mapping along the Río Gr...
Landslides are downslope mass movements, which implies the combination of natural complex processes ...
A geomorphologic description of the Du´dar landslide (Granada, S Spain) has been carried out using a...
Drawing on historical documents and a detailed field study, we have been able to characterize the Gü...
The Fuegian Andes, in the southernmost part of South America, are characterized by a relatively youn...
En este trabajo se describe una avalancha de rocas muy bien preservada situada en el área de Las Maj...
Between 2001 and 2005, a large debris rock slide occurred on the western slope of the Cordillera de ...
A megalandslide has been identified on the western hillslope of Cerro Uritorco peak (1.949 m a.s.l.)...
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de ...
The main objective of this paper is to consider the influence of Quaternary faults as likely trigger...