The boreholes database is an inventory of subsurface data in Catalonia through the collection of available geological and geotechnical survey information. The surveys are classified into three groups: surveys, penetrometers and trial pits.

3D model of geological surfaces that contains the main stratigraphic surfaces and geological structures of Catalonia, the location of the main exploration drillings and the topographic and bathymetric surface of the model area.

3D model of Port del Comte aquifers, developed as part of the assessment of underground water resources available in Catalonia. More specifically, this model contains the lithological-hydrogeological units, the main geological structures, the topographic surface of the project area, the location of the main karst springs and the saturated rock volumes of the water reservoirs associated with each of the springs

3D model of aquifers in the urban and peri-urban areas of Girona and surrounding municipalities, developed within the framework of the MUSE project (Management Urban Shallow geothermal Energy, 2018-2021). More specifically, this model contains the lithological-hydrogeological units, the main geological structures and the topographic and piezometric surfaces of the project area.

Location and characteristics of the geotechnical surveys of the subsoil carried out (boreholes, penetrometers and test pits).

WMS service for visualization of information related to local surface geothermal, such as geothermal stations, aquifer thicknesses, isolines and temperatures at different depths, and geothermal potential. Some data are only displayed between zoom levels equivalent to 10,000 and 100,000 scale denominators.

WMS service for visualization of seismical information until 2019.

WMS service of visualization of the territorial geology that groups together different sets of information on the geological characteristics of the territory.

WMS service for visualization of terrain deformations. It includes information from different studies about vertical deformation of the ground made ​​by topographic surveys, GPS and differential interferometry.

Magnetic anomaly measurements and zoning of the territory according to this at a scale of 1:250,000.