This study investigates relationships between climate changes and hillslope evolution in the Dolomites (eastern Alps, Italy), during the Late Quaternary, with particular attention paid to landslide processes. The basic premise is that modifications in landslide frequency may be interpreted as changes in the hydrological conditions of slopes, which are in turn controlled by climate. After the statistical analysis of a data set composed of 73 conventional radiocarbon ages, obtained from 24 landslides, four periods of enhanced landsliding have been identified: I. from 10,700 to 8400 cal BP, between Younger Dryas and the Preboreal; II. from 8200 to 6900 cal BP, during the older Atlantic; III. from 5800 to 4500 cal BP, between Atlantic and Subbo...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
Landslide chronologies are essential both for understanding the causes of mass movements and for the...
Landslides and in particular the temporal concentrations of instability events in different periods ...
This study investigates relationships between climate changes and hillslope evolution in the Dolomit...
This study concerns the relationships between climate changes and hillslope evolution during the Lat...
This study concerns the relationships between climate changes and hillslope evolution during the Lat...
none2This study concerns the relationships between climate changes and hillslope evolution during th...
The paper deals with the relationship between the temporal occurrence of landslides and climatic cha...
Since 1991, investigation on the relationships between landslide occurrence and climatic change from...
This paper deals with the use of records of past landslide events in the study of climate changes. T...
Landslides and in particular the temporal concentrations of instability events in different periods ...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
The area of Corvara in Badia, located in the Dolomites (NE Italy), is characterised by mountain grou...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
The paper first introduces the main geological and geomorphological features of the Italian Dolomite...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
Landslide chronologies are essential both for understanding the causes of mass movements and for the...
Landslides and in particular the temporal concentrations of instability events in different periods ...
This study investigates relationships between climate changes and hillslope evolution in the Dolomit...
This study concerns the relationships between climate changes and hillslope evolution during the Lat...
This study concerns the relationships between climate changes and hillslope evolution during the Lat...
none2This study concerns the relationships between climate changes and hillslope evolution during th...
The paper deals with the relationship between the temporal occurrence of landslides and climatic cha...
Since 1991, investigation on the relationships between landslide occurrence and climatic change from...
This paper deals with the use of records of past landslide events in the study of climate changes. T...
Landslides and in particular the temporal concentrations of instability events in different periods ...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
The area of Corvara in Badia, located in the Dolomites (NE Italy), is characterised by mountain grou...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
The paper first introduces the main geological and geomorphological features of the Italian Dolomite...
This paper deals with the use of landslide records in the analysis of landscape sensitivity, with pa...
Landslide chronologies are essential both for understanding the causes of mass movements and for the...
Landslides and in particular the temporal concentrations of instability events in different periods ...