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Field and laboratory analysis of the runout characteristics of hillslope debris flows in Switzerland

Autor
Hurlimann, M.; McArdell, B.W.; Rickli, C.
Tipus d'activitat
Article en revista
Revista
Geomorphology
Data de publicació
2015-01-01
Volum
232
Pàgina inicial
20
Pàgina final
32
DOI
https://doi.org/10.1016/j.geomorph.2014.11.030 Obrir en finestra nova
Projecte finançador
Análisis de los mecanismos de rotura de deslizamientos superficiales y corrientes de derrubios desencadenados por lluvias
Repositori
http://hdl.handle.net/2117/77265 Obrir en finestra nova
Resum
Hillslope debris flows are unconfined flows that originate by shallow failures in unconsolidated material at steep slopes. In spite of their significant hazard for persons and infrastructure in mountainous regions, research on hillslope debris flows is rather scarce in comparison to other landslide types. This study focusses on the runout characteristics of hillslope debris flows applying two different approaches. First, detailed landslide inventories, which include field measurements of 548 slo...
Citació
Hurlimann, M., McArdell, B.W., Rickli, C. Field and laboratory analysis of the runout characteristics of hillslope debris flows in Switzerland. "Geomorphology", Març 2015, vol. 232, p. 20-32.
Paraules clau
Hillslope debris flow, Laboratory experiment, Landslide inventory, Runout distance, Switzerland
Grup de recerca
EnGeoModels - Monitoring and Modelling in Engineering Geology

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