Metadata 1674
This is PSI data for Riga, Latvia. It has been provided by CGG NPA Satellite Mapping as part of the ESA funded Terrafirma project.
This is PSI data for Rio-Antirio, Greece. It has been provided by Harokopio University as part of the ESA funded Terrafirma project.
The Geological Survey Ireland (GSI), as partner and Work Package 7 (Minerals) leader of EMODnet Geology Phase III, are compiling information on rock peg vein deposits. EMODnet partners are submitting the spatial extent of mapped deposits and established information; here you can view data collated thus far. Need abstract information here.....
The Geological Survey Ireland (GSI), as partner and Work Package 7 (Minerals) leader of EMODnet Geology Phase III, are compiling information on rock peg vein deposits. EMODnet partners are submitting the spatial extent of mapped deposits and established information; here you can view data collated thus far. Need abstract information here.....
This is PSI data for Rome, Italy. It has been provided by TRE as part of the ESA funded Terrafirma project.
This is PSI data for Rome, Italy. It has been provided by TRE as part of the ESA funded Terrafirma project.
Iso-content maps of Rubidium (Rb), 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...
This is PSI data for Rybnik_Ostrava, Poland. It has been provided by GAMMA Remote Sensing as part of the ESA funded Terrafirma project.
S layer represents soil media with direct assignment of S index values (Soil Map of Greece 1:500.000)
S layer represents soil media with direct assignment of S index values for each pedological unit and information from pedological profiles and litho-geochemical map (where no profiles were available). The highest values correspond to lithologies that don't constitute soils or at least very shallow ones (< 30 cm). The lowest values are significant for areas with deeper soil layers (sedimentary rocks).