WFS service provides access to basic information related to the mining operations (both abandoned or operating continuously or intermittently) and minerals occurrences of industrial minerals and rocks. Service was created in the framework of the Minerals4EU project and its harmonizated according to the INSPIRE requeriments-

Geological map of the Iberian Peninsula, Balearic and Canary Islands at 1M scale. It includes the chronolithostratigraphic units and the representation of the tectonic structure by means of faults and thrusts.

The service consists of two layers of dots symbolising the position of mineral occurrences for the entire national territory. Depending on the scale of visualisation, two layers of information have been created. Indications I: Only the location of the points is represented. Visible from scales smaller than 1:200.000. Indications II: The points are represented with a symbolisation according to different attributes. Visible from scales larger than 1:200,000. The reference systems offered by this service are:CRS:84, EPSG:4326, EPSG:4258, EPSG:4230, EPSG:23028, EPSG:23029, EPSG:23030, EPSG:23031, EPSG:25828, EPSG:25829, EPSG:25830, EPSG:25831

The geological age map of the units at a scale of 1:1,000,000 has been generated from the information in the chronolithostratigraphic column of the map. In all units the System has been specified, the Series has only been covered in about half of the units and the Floor is occasional. In cases where it has not been possible to establish a chronostratigraphic section, the value "undetermined" has been assigned.

Map showing the chronolithostratigraphic units of the area covered by the sheet separated by different types of contacts: normal or concordant, discordant, intrusive and other. The tectonic structure is represented by the cartographic traces of folds, the orientation and dip of planar and linear elements contained in the rocks, as well as by the structural relationship - through faults and thrusts - between the cartographically differentiated rock assemblages. Unique features of the igneous rocks as well as the degree of migmatisation of the metamorphic rocks are also depicted. The map is accompanied by the lithostratigraphic legend and conventional signs.

Map with the geographical distribution of the areas where similar expansivity is assumed for the clays, which have been classified into four groups: none to low, low to moderate, moderate to high and high to very high. The different mapped units have been assigned age (4 possible) and lithology (7 different types). The map also shows the surface formations without distinction.

The Neotectonic Map expresses those structural, morphological, stratigraphic and other features that show relatively recent movements (from the period considered neotectonic), as well as the type of stress to which the peninsula is subjected. Its objectives are to identify deformations from the Middle Miocene - Upper Miocene boundary to the present day. The materials have been classified into six categories, two for volcanic materials differentiated by age; and four for the rest of the materials, with four subdivisions according to age. It also includes tectonic structures, stress and deformation directions, diapiric structures and other related phenomena, all with age expression. The map contains information on the Spanish continental shelf.

This map shows deposits dated as Plio-Pleistocene to contemporary, classified in 10 geochronological intervals and separated according to their genesis. Glacial, volcanic, karstic, aeolian, littoral, edaphic, palaeontological and prehistoric entities are included.

The lithological map at a scale of 1:1,000,000 has been obtained by assigning the most representative lithology or lithological association to each cartographic unit on the map. It has been based on the original classification of the edited map, which has been subsequently revised, giving rise to the current classification.

Map showing the geographical distribution of ground movements classified into four main groups: horizontal component in continental areas, vertical component in continental areas, unstable areas linked to coastal areas and movements related to mining operations. Also included are continental areas with important erosive processes.