Metadata 1667
The GSI, as partner and Work Package 7 Minerals leader of EMODnet Geology Phase II, are compiling information on Polymetallic sulphides PMS. EMODnet partners are submitting mapped PMS locations and existing information, here you can view data collated thus far. The PMS information presented here are of mapped PMS locations. Also known as Volcanogenic Massive Sulfides (VMS), Seafloor Massive Sulfides (SMS) and Black Smokers, PMS are base metal sulfur-rich mineral deposits. They occur along the earth’s major...
The Portuguese HydroGeological Resources Database provides geological and hydrogeological information for drill holes, wells, springs and boreholes.
This view service provides access to geological and hydrogeological information for drill holes, wells, springs and boreholes
The Portuguese Mineral Occurrences and Resources Information System (SIORMINP) provides access to geoscientific, technical and economic information on occurrences, reserves and resources, associated commodities, geology, mines, mining activities, mining wastes and areas with mining potential known in mainland Portugal.
This download service provides access to information related to the mineral occurrences, reserves and resources, associated commodities, geology, mines, mining activities, wastes and areas with mining potential of Portugal mainland. Moreover, this information is the result, improvement and adaptation of SIORMINP to the data structure model and vocabularies used in European projects, namely Eurogeosource, Promine, Minerals4EU, ProSUM and Mintell4EU, according to INSPIRE Directive requirements.
This view service provides access to information related to the mineral occurrences, reserves and resources, associated commodities, geology, mines, mining activities, wastes and areas with mining potential of Portugal mainland. Moreover, this information is the result, improvement and adaptation of SIORMINP to the data structure model and vocabularies used in European projects, namely Eurogeosource, Promine, Minerals4EU, ProSUM and Mintell4EU, according to INSPIRE Directive requirements.
The thickness maps of the Post-LGM deposits can be used to identify areas where i) pre-Holocene submerged landscapes are exposed at or close to the seabed, or, ii) where there is high potential for preservation of early Holocene landscape features such as submerged river valleys or coasts. Contours are presented as depth (metres) below the present seafloor or the base of the post-LGM sedimentary cover. In glaciated regions, the thickness of the Holocene is used.
Thickness of the Last Glacial Maximum (LGM) deposit. Contours are presented as depth (metres) below present seafloor or the base of the post LGM sedimentary cover. LGM is defined on average at 18,000 years BP. In glaciated regions the thickness of the Holocene is used. Confidence is defined as follows: 1. High: Sampled feature with good age and palaeoenvironmental control. 2. Sampled feature with poor or none age and palaeoenvironmental control. 3. Constructed by remote sensing data only, 4. Low: Reasonabl...
Iso-content maps of Potassium (K), one of the chemical elements.obtained in the Geochemical Atlas of Spain Project, distributed in stream sediments (14,864 samples), superficial soils (0-20 cm.) (13,505 samples) and deeper soils (20-40 cm.) (7,682 samples). The results of the chemical analysis are shown in two types: total dissolution of the sample with 4 acids and partial dissolution with aqua regia. With the analytical results of all the sampled points, an isocontent map is made with adjustment to a squa...
Long term average (LTA) Potential Groundwater Recharge (GWRpot) for the European domain at 1 km spatial resolution for the period 1981-2010. The LTA GWRpot data set i part of a series of gridded datasets established in the TACTIC project for estimating Potential Groundwater Recharge (GWRpot). The data available are AET, Effective precipitation (Peff=Precipitation-AET), Groundwater Recharge coefficient (Rcoef defined as the ratio: Peff / GWRpot ) The Potential Groundwater Recharge GWRpot = (Precipitation-AE...