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 orthoimages related to wildfires.

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

WMS service for viewing information related to Theme 9 - Protected sites, of Annex I of the INSPIRE Directive, in the geographical area of Catalonia. The service allows viewing the dataset of Protected sites Natura 2000 of Catalonia, according the Directive requirements, derived from the data set Natura 2000 network sites.

WMS service for visualization of the maritime space management, published by the Generalitat de Catalunya (Government of Catalonia). It includes information such as grasslands.

WMS service for viewing information related to Theme 2 - Buildings, of Annex III of the INSPIRE Directive, in the geographical area of Catalonia. The service allows viewing the dataset of Buildings of Catalonia, according the Directive requirements, derived from 1:1,000 topographic cartography of some municipalities of Catalonia.

WMS service for visualization of the columns of boreholes, trial pits and penetrometers available in Catalonia.

WMS service for viewing information related to Theme 9 - Protected sites, of Annex I of the INSPIRE Directive, in the geographical area of Catalonia. The service allows viewing the dataset of Protected sites PEIN of Catalonia, according the Directive requirements, derived from the data set Plan of Areas of Natural Interest (PEIN).

WMS service for visualization of the agrological capacity of soils.

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.