Metadata 1823
Historical seismograms from Prague seismic station. Non-continuous data stored on paper records since 1927 to the 1990s.
The Faculty of Mathematics and Physics of Charles University, in cooperation with the University of Patras, operates since 1997 a network of seismographs in western Greece, which are the part of the Greek seismic network (HUSN).
This dataset contains information on the location of seismic surveys acquired offshore Malta
The Seismotectonic Map of the Republic of Srpska 1:300 000 represents an integration of geological, tectonic, seismotectonic and geophysical data on possible earthquake sources. The map is a compilation of all available data and the results of the previous basic and regional geological, seismological and geophysical research and explorations in the teritory of the Republic of Srpska, Bosnia and Herzegovina and the region. The knowledge of seismotectonic characteristics of the region enables the characteriz...
Iso-content maps of Selenium (Se), 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...
The Danish, French, Italian, Maltese and Polish sentinel springs studied in the SentinelSprings project, further described on website: https://sentinelsprings.eu The location of the springs are visable in the EGDI mapviewer, link below
This series contains 3D Geological Models of different areas in Hungary
This series contains geological maps of Hungary in different scale
The service presents a map overview of models in EGDI3D Geological Model Database. From each mapped area, a link is provided to a preview of the model.
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.