Slovenski INSPIRE metapodatkovni sistem
Keyword
geologija
23 record(s)
Type of resources
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INSPIRE themes
Keywords
Contact for the resource
Formats
Representation types
Scale
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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 Basic Geological Map of Slovenia as a part of joint Basic Geological Map of SFR Yugoslavia presents lithological and stratigraphic characteristics of rocks, their relationships, age and other. It is a key to the understanding of the geology of Slovenia. It consists of 23 sheets at a scale of 1: 100,000.
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Basic geological map of Yugoslavia presents lithological and stratigraphic characteristics of rocks, their relationships, age and other. It is a key to the understanding of the geology of Slovenia. It consists of 23 sheets, scale 1: 100.000.
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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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Karte prostorske porazdelitve vrednosti spremenljivk vezanih na temperaturo zraka so narejene na osnovi meritev klimatoloških meteoroloških postaj, ki so v obravnavanem obdobju neprekinjeno delovale vsaj deset let. Za računanje vrednosti spremenljivk vezanih na temperaturo zraka v pravilni mreži z ločljivostjo 100 m x 100 m je bila uporabljena metoda optimalne prostorske interpolacije, ki upošteva povezanost obravnavane spremenljivke z nadmorsko višino in preko izbrane okolice upošteva tudi vpliv mikrolokacije. Zaradi majhne gostote mreže opazovanj, je vpliv mikrolokacije možno upoštevati le v manjši meri.
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Geological Units are polygons, defined by equal composition (lithology) and age.
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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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Naravni hidrogeološki objekti, kjer podzemna voda po naravni poti pride na površje.
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Layer shows discontinuities in the geological structure, and characterizes them according to their type and observation method.
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The underground geothermal conditions can be presented, irrespective of the aquifers' position, with the appropriate geothermal maps. These maps represent the expected isoterms at a depths and are derived from Geothermal maps - Expected temperatures , which are made with data from 302 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.