Slovenski INSPIRE metapodatkovni sistem
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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 harmonized geological map of Slovenia is a simplified version of the 1:250 000 scale Geological Map of Slovenia (Buser, 2009), which was compiled using the Basic Geological Map of Slovenia at a scale of 1: 100.000 (compiled by various authors during the 1960's to 1980's) with the addition of new information by Buser. It is primarily a lithostratigraphic map.The faults were selected for portrayal 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 temperatures at a depth of 100 m and is made with data from 398 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. 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 100 m a stronger positive anomaly is in the northeastern part of Slovenia, and in a smaller eastern part of the Krka basin. 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.
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Taxi stops are reserved parking areas intended for stopping or parking taxis during taxi services. Taxi stops are marked with prescribed traffic signals (traffic signs and floor markings).
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For the needs of spatial planning and for implementing the policy of Land Registry, the Spatial Management Act (hereinafter: ZUreP-3) introduces a new record, called the Register of building land. It contains information on built-up land and non-built-up building land. - Built-up land is divided into associated building land, the associated land of construction engineering facilities and construction lots. The difference between the associated building land and the associated land of construction engineering facilities is that the associated building land will be determined in a process of mass capture, while the building lots are determined in the administrative procedure. The associated building land is therefore the first approximation of the building lot. - Non-built-up building land is classified into development stages which are determined by ZUreP-2 according to their equipment with public infrastructure, the status of the legal regime on land and the regulation of land with spatial planning documents. The Register of building land is in accordance with the ZUreP-3 intended for the planning of usage land or new building land in the process of preparation of municipal spatial planning documents, planning of utility equipment, implementation of Land Registry policy, rehabilitation and ensuring adequate parcel and ownership structure, ensuring affordable land for residence and work, management of land in the public interest and for the assessment of duties on building land and evaluation of building land. Register of building land is also the basis for providing information on developmental stages and other properties of building land for interested investors. The Register of building land will enable the implementation of Land Registry policy, increase the awareness of investors, and thus significantly contribute to a more successful development.
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In the Remote Sensing Database the remote sensing data, ortophoto and remote sensing technical data are being managed.
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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 isotherms at a depth of 2000 m and is derived from Geothermal map - Expected temperatures at a depth of 2000 m, which is made with data from 240 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 2000 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 the anomaly is not so much visible 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.