Mountain resources and valorisation database — permeable hydrogeological complexes of the mountain sector, aquifer site

Vector-type geo-referenced database, composed of multiple information layers, which are described below. The hydrogeological complexes permeable by fracturing (in rock) of the Emilia Romagna Apennines are the premises of the mountainous aquifers; In the tabular content, they are differentiated into: ‘store rock’ means the location of significant densities of sources and thus of the main aquifers; ‘Deployment areas’ means hydrogeological complexes in rock, potentially permeable, location of minor aquifers. A particular type of permeable hydrogeological complexes, those of morenic origin, have been differentiated. Permeable hydrogeological complexes corresponding to the negative side coverings are differentiated when related to rock aquifers, or when isolated. The permeable hydrogeological complexes of terraced alluvial deposits (in the Apennine valleys) are the place of underground water circulation, governed by relations with water courses. Finally, a distinction is made between the permeable hydrogeological complexes corresponding to the evaporites of the Apennines and Milian-Magnician Apennines. The variants to the Provincial Coordination Regional Plans (PTCP), during the phase of adaptation to the Regional Water Protection Plan (PTA, 2005), in the period from 2006 to 2012.