The physical characteristics and behaviour of a small-magnitude debris flow are reported for an event at Col du Sabot, France. The event occurred on a high alpine meadow. Entrainment and deposition took place along the path, which yielded a relatively small peak cumulative flow volume of nearly 200 m3 and a travel distance of 344 m to the point of terminal deposition. Volume change along the event path, from point of origin, was simulated using the model UBCDFLOW. The model determines travel distance as the point along the path of movement where the cumulative flow volume diminishes to zero. A comparison of the modelled travel distance with the actual distance from field observations shows excellent agreement
The estimation of runout distances on fans has a major role in assessing debris-flow hazards. Differ...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
Debris flows are common phenomena in mountainous, steep and prone-to-intense-erosion catchments. The...
Assessment of debris flow travel distance is an essential part of landslide risk management. Confide...
Debris flows are a well known geomorphic process all over the World, as can be seen in the map prese...
Debris flows can occur on both forested (natural) and clearcut (logged) hillslopes in coastal Briti...
Debris flows can occur on both forested (natural) and clearcut (logged) hillslopes in coastal Briti...
Two current approaches for the analysis of debris flows exist; semiempirical and empirical approache...
Two current approaches for the analysis of debris flows exist; semiempirical and empirical approache...
This research aims to improve our knowledge of debris flow occurrence and behaviour in New Zealand. ...
The estimation of runout distances on fans has a major role in assessing debris-flow hazards. Differ...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
The physical characteristics and behaviour of a small-magnitude debris flow are reported for an even...
Debris flows are common phenomena in mountainous, steep and prone-to-intense-erosion catchments. The...
Assessment of debris flow travel distance is an essential part of landslide risk management. Confide...
Debris flows are a well known geomorphic process all over the World, as can be seen in the map prese...
Debris flows can occur on both forested (natural) and clearcut (logged) hillslopes in coastal Briti...
Debris flows can occur on both forested (natural) and clearcut (logged) hillslopes in coastal Briti...
Two current approaches for the analysis of debris flows exist; semiempirical and empirical approache...
Two current approaches for the analysis of debris flows exist; semiempirical and empirical approache...
This research aims to improve our knowledge of debris flow occurrence and behaviour in New Zealand. ...
The estimation of runout distances on fans has a major role in assessing debris-flow hazards. Differ...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...
International audienceDebris flows are among the most dangerous processes in mountainous areas due t...