Abstract The reconstruction of triggering conditions, geomorphic effects, and damage produced by historical floods and debris flows significantly contributes to hazard assessment, allowing improved risk mitigation measures to be defined. Methods for the analysis of historical floods and debris flows vary greatly according to the type and quality of available data, which in turn are influenced by the time the events occurred. For floods and debris flows occurring in the Alps a few decades ago (between about 1950 and 1980), the documentation is usually better than for previous periods but, unlike events of most recent years, quantitative data are usually scanty and the description of the events does not aim to identify processes according to ...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; their for...
The estimation of debris flow magnitude is essential for the assessment of debris flow hazard. Histo...
The estimation of debris flow magnitude is essential for the assessment of debris flow hazard. Histo...
The estimation of debris-flow magnitude is an essential step in the assessment of debris-flow hazard...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; their form...
Abstract. Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; ...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
Abstract. The knowledge of past events is important for the assessment of debris-flow hazard. Amongs...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; their for...
The estimation of debris flow magnitude is essential for the assessment of debris flow hazard. Histo...
The estimation of debris flow magnitude is essential for the assessment of debris flow hazard. Histo...
The estimation of debris-flow magnitude is an essential step in the assessment of debris-flow hazard...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
The estimation of debris flow volumes is a basic requirement for the assessment of debris flow hazar...
Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; their form...
Abstract. Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; ...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
Abstract. The knowledge of past events is important for the assessment of debris-flow hazard. Amongs...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
In this work, a multidisciplinary study is presented in which potential debris flow events are studi...
Alluvial fans are often present at the outlet of small drainage basins in alpine valleys; their for...