Slovenski INSPIRE metapodatkovni sistem
Type of resources
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INSPIRE themes
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The harmonized geological map of Slovenia at a scale of 1:1,000,000 is a simplified version of the 1:250,000 scale Geological Map of Slovenia (Buser, 2009). The latter was compiled from the Basic Geological Map of Slovenia at a scale of 1: 100,000 (contributed by various authors between 1960's and 1980's and updated with new information gathered by S. Buser). The map is basically lithostratigraphic. The two layers incorporated in the map are lithostratigraphic units and major faults. The faults depicted on the map were selected using two criteria; regional extent and tectonic importance. The map presented here was edited specifically for the purpose of the OneGeology-Europe project by M. Bavec, M. Novak, M. Poljak, M. Trajanova and D. Skaberne.
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The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. This map represents the expected temperature lines at a depth of 3000 m and is derived from Geothermal map - Expected temperatures at a depth of 3000 m, which is made with data from 214 boreholes. It is made on the basis of measured temperatures in accessible boreholes throughout the country. However, since the temperature field depends on the geological structure in the depths and tectonic characteristics, the course of the isotherms is a result of many influences, such as thermal conductivity of rocks, permeability and fracturing of rocks, all of which are reflected in the measured temperatures in boreholes. In this depth also a radiogenic heat production in the rocks has smaller influence. The distribution of boreholes, which were useful for the measurement of temperature, is very uneven and different as regard the depths. Following the expected temperatures at a depth of 3000 m a stronger positive anomaly is in the northeastern part of Slovenia, from the line Maribor-Rogatec to the east, while in the eastern part of the Krka basin there is no anomaly any more. In the northeastern part of the country the anomaly is the result of the thinning of the Earth's crust and greater conductive heat flow from the Earth's mantle. Elsewhere temperatures are much lower.
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The vector data collection DPK 1000V is an object-oriented cartographic database at 1 : 1 000 000 scale. Elements on the map are divided into eight objects groups: mathematical elements, settlements and objects, communications, relief, hydrography, land cover, boundaries and dividing line, geographical names. The data set is used for "rough" orientation in the space and for the needs of large scale and thematic displaying.
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Product by the Pangeo project: http://www.pangeoproject.eu/ PanGeo provides information about the stability of the ground on which we live, work and play. Ground instability, or "geohazards", affect us all. They can be dangerous and costly, yet information on these phenomena can be difficult if not impossible to obtain. The PanGeo service provides entirely free access to geohazard information for many of the largest cities in Europe . The PanGeo service is aimed at local authorities, civil protection agencies, geological surveys, the public, insurers and businesses providing environmental and land reporting services. The service and products available are entirely free to use, even for commercial gain, providing appropriate credits are given (see licence terms). Information in PanGeo is derived from detailed analysis of local geological data combined with satellite measurements of ground movement.
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Mineral deposits and resources INSPIRE compliant WFS services for Minerals4EU
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Layer Geomorphologic Features shows the location of various types of geomorphological phenomena. Only point data are included.
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The register of addresses is a record of address information. It consists of entered address data that is stored permanently. The register of addresses takes information about the address number, settlement, street, house number and number of the apartment or business premises from the real estate cadastre and the register of spatial units. Data on the spatial units in the area of which the centroid of the address is located are taken from the register of spatial units by the intersection of the centroid of the address and the areas of the spatial units. The register of addresses data is determined by the cadastre information system when a new address number is determined, data taken from the real estate cadastre changes, or the borders, names or codes of spatial units in the area of which the address is located are changed. In case of changes to the address number, the cadastre information system forwards the change to the central population register.
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The layer keeps data on parking spaces intended exclusively for electric vehicles. Data covers the entire municipality, although the parking spaces are mostly located in the urban part.