Dolomitic landscapes are characterized by vertical rock cliffs and soil-mantled hillslopes originated from glacial or colluvial deposits, which hide a complex subsurface aquifer due to the permeability of the dolomitic rocks. To improve the understanding of the hydrological functioning of such complex hydrogeological systems, the hydrology group of the Department of Land, Environment, Agriculture ...[Read More]
Featured catchment series: The Rio Vauz catchment – long-term hydrologic observations in the Dolomites
