Freissinières catchment is particularly prone to catastrophic floods. Floods are characterized by the influence of temporal dams : the removal of such dams imply massive supply of water and sediments downstream. Dams are due to the large amount of sediments provided from the hill slopes by paraglacial and glacial sediment sources.La vallée de Freissinières est propice au déclenchement de crues torrentielles. Ces crues torrentielles sont caractérisées par un fonctionnement en embâcle / débâcle. Ce fonctionnement s 'explique par l 'importante fourniture de débris depuis les versants, plus particulièrement par la disponibilité des sources de sédiments glaciaires et paraglaciaires.Cossart Étienne, Szuba Perrine. L'influence paraglaciaire dans l...
Abstract The alpine catchment of l'Eglise (Montagne des Arcs, left bank of Isère river, Tarentaise) ...
For the last 150 years, the Haut Arc glaciers (Savoie, France) follow a quite constant generalized r...
Abstract. - The silty loamy plateaux of the north of France have been affected since many years by f...
Freissinières catchment is particularly prone to catastrophic floods. Floods are characterized by th...
Freissinières catchment is particularly prone to catastrophic floods. Floods are characterized by th...
National audienceLa vallée de Freissinières est propice au déclenchement de crues torrentielles. Ces...
In Alpine high mountain area like the Mont Blanc massif the paraglacial period is the time which is ...
Les recherches géomorphologiques et géoarchéologiques, appliquées à l’étude des fonds de vallée, per...
Dans le bassin versant de la Semoigne, les glissements de terrain anciens connaissent des réactivati...
The current retreat of the glacier fronts induces changes of both discharge and sediment availabilit...
National audienceThe current retreat of the glacier fronts induces changes of both discharge and sed...
Downstream middle Garonne : geomorphology and flood dynamics. When it is a question of floods, fluvi...
La géomorphologie paraglaciaire permet de comprendre l'évolution des milieux ayant été englacés soum...
La géomorphologie paraglaciaire permet de comprendre l'évolution des milieux ayant été englacés soum...
Abstract The alpine catchment of l'Eglise (Montagne des Arcs, left bank of Isère river, Tarentaise) ...
For the last 150 years, the Haut Arc glaciers (Savoie, France) follow a quite constant generalized r...
Abstract. - The silty loamy plateaux of the north of France have been affected since many years by f...
Freissinières catchment is particularly prone to catastrophic floods. Floods are characterized by th...
Freissinières catchment is particularly prone to catastrophic floods. Floods are characterized by th...
National audienceLa vallée de Freissinières est propice au déclenchement de crues torrentielles. Ces...
In Alpine high mountain area like the Mont Blanc massif the paraglacial period is the time which is ...
Les recherches géomorphologiques et géoarchéologiques, appliquées à l’étude des fonds de vallée, per...
Dans le bassin versant de la Semoigne, les glissements de terrain anciens connaissent des réactivati...
The current retreat of the glacier fronts induces changes of both discharge and sediment availabilit...
National audienceThe current retreat of the glacier fronts induces changes of both discharge and sed...
Downstream middle Garonne : geomorphology and flood dynamics. When it is a question of floods, fluvi...
La géomorphologie paraglaciaire permet de comprendre l'évolution des milieux ayant été englacés soum...
La géomorphologie paraglaciaire permet de comprendre l'évolution des milieux ayant été englacés soum...
Abstract The alpine catchment of l'Eglise (Montagne des Arcs, left bank of Isère river, Tarentaise) ...
For the last 150 years, the Haut Arc glaciers (Savoie, France) follow a quite constant generalized r...
Abstract. - The silty loamy plateaux of the north of France have been affected since many years by f...