Engineering Geology for Society and Territory - Volume 3 2014
DOI: 10.1007/978-3-319-09054-2_65
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Sediment Dynamics and Channel Adjustments Following Torrential Floods in an Upper Alpine Valley (Guil River, Southern French Alps)

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“…Due to some predisposing (schist bedrock supplying abundant debris, structural opposite slopes, strong hillslope channel connectivity) and triggering (summer and winter Mediterranean rainstorms) factors, the Upper Guil catchment is particularly prone to hydrogeomorphic hazards such as torrential floods, debris flows, landslides, rockfalls or avalanches (Fort et al, 2002(Fort et al, , 2014Arnaud-Fassetta et al, 2004. These hazards frequently impact the local population (fatalities, destruction of buildings and in-frastructure, loss of agricultural land, road closures) causing difficulties for local managers, who also have to cope with the legislation and management procedures of the Parc Naturel Régional du Queyras (PNRQ) (Arnaud-Fassetta et al, 2004.…”
Section: Physical Contextmentioning
confidence: 99%
“…Due to some predisposing (schist bedrock supplying abundant debris, structural opposite slopes, strong hillslope channel connectivity) and triggering (summer and winter Mediterranean rainstorms) factors, the Upper Guil catchment is particularly prone to hydrogeomorphic hazards such as torrential floods, debris flows, landslides, rockfalls or avalanches (Fort et al, 2002(Fort et al, , 2014Arnaud-Fassetta et al, 2004. These hazards frequently impact the local population (fatalities, destruction of buildings and in-frastructure, loss of agricultural land, road closures) causing difficulties for local managers, who also have to cope with the legislation and management procedures of the Parc Naturel Régional du Queyras (PNRQ) (Arnaud-Fassetta et al, 2004.…”
Section: Physical Contextmentioning
confidence: 99%