WMS service for visualization of the topographic map 1:1.000.000.

WMS service for visualization of the subdivision of the municipalities of Catalonia into districts and census sections. The service provides the layers of census sections that have been published since 2002 until the revision date of this metadata.

WMS service for visualization of Cartographic Orientation System (SOC) grids, 1x1 and 5x5 km of resolution, with their identifiers.

WMS service for visualization of the cartography of the study of the residential areas of the province of Barcelona, made in 2012 at scale 1:5,000.

WMS service for visualization of the ecosystem services cartography of the province of Barcelona.

WMS service for visualization of the Local Topographic Reference (RTL), which constitutes the reference topographic geoinformation with total or partial coverage of municipal management areas or geographic areas of specific themes that require detailed topographic information, and it includes information regarding relief, hydrography, road network and other transport networks; buildings, constructions and facilities; land cover, toponymy and municipal inventories.

WMS service for visualization of information related to deep geothermal, such as heat flow, geothermal gradient and thermal conductivity isolines, isotherms at different depths, temperatures at different depths, wells and boreholes, and areas of geothermal potential. The data are only displayed between zoom levels equivalent to 25,000 and 10,000,000 scale denominators.

WMS service for visualization of the industrial establishments that handle dangerous substances that are included in the Plaseqcat emergency plan and the theoretical affectation areas in the event of a serious accident.

WMS service for visualization of the nuclear emergency planning zones and the nuclear urban planning zones.

WMS service for visualization of the Structural map of Catalonia 1:250,000. It includes information about the main tectonic structures of Catalonia, which have a very important role in geothermics. On the one hand, larger structures are related to the thickness of the crust and lithospheric mantle, which also affect the distribution of temperatures in depth. Moreover, the relief topographic and the hydraulic gradient are conditioned by them, therefore, the principal directions of groundwater flow.