The Araguás Catchment of the Central Spanish Pyrenees has been monitored since 2004 to study weathering erosion, as well as the hydrological and sediment responses to rainfall in order to understand the dynamics of a badland area in a relatively
Morphological analysis and erosion rate evaluation in badlands of Radicofani area (southern Tuscany - Italy)
Argile ; Badland ; Bassin-versant ; Erosion des sols ; Erosion hydrique ; Italie ; Modèle numérique de terrain ; Mouvement de masse ; Photogrammétrie ; Toscana ; Vitesse d'érosion
Badland ; Clay ; Digital elevation model ; Erosion rate ; Italy ; Mass movement ; Photogrammetry ; Soil erosion ; Toscana ; Water erosion ; Watershed
station located on slopes, identify gravity as the main morphogenic process responsible for slope shaping. The calanchi badland areas are characterised by constant and rapid shrinking of their edges resulting from landslides which occur in autumn
The dispersive nature of the highly sodic silts of the Triassic-rich unit of the Góchar formation plays a fundamental role in the erosion of the Mocatán catchment badlands in Almería, where a rejuvenating pipe and incised channel network is rapidly
This study aims to quantify flood-based sediment yields in 2 highly active headwater catchments in the upper Isábena River : Villacardi and Cabecera. The results are compared with the sediment delivery from a zero-order badland catchment
This paper examines the changes from 1955 to 2002 in soil erosion and deposition due to changes in land-use patterns in the semi-arid territory of Craco, which is characterised by landsliding and badland erosion. This analysis integrates the Unit