The Galabre site is part of Draix-Bleone observatory, located in the French South Alps, upstream of Digne, on the right side of the Bleone river.
The hydrosedimentary station of La Robine-sur-Galabre was created in 2008 to measure water of sediment fluxes from the Galabre catchment, 20 km2. This catchment integrates a diversity of lithologies and land use that are characteristic of the Pre-Alps. The climate is mountainous and Mediterranean. The site is characterized by intense erosion and intermittent sediment fluxes.
The variables that are monitored on the long-term include rainfall and meteorology, high-frequency water discharge and suspended sediment concentration (10 minutes), some physico-chemical properties of stream water and sediments.