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
The development of badlands in the Central Spanish Pyrenees is favoured by the presence of marls and a climate with a marked seasonality; the combination of these factors results in active hydrosedimentological processes. The study area was a small