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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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    Hydrogeological map of Slovenia 1:250.000 represent hydrogeological characteristics of overlaying strata. The identification and classification of strata is based on LAWA classification. Hydrogeological units of LAWA classification are defined on type of porosity and basic petrographical composition. Geological strata with kartic porosity were additionaly classified after karstification stage.

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    Vodonosni sistem je ozemlje z geološko zgradbo, v kateri nastopata vsaj dva različna vodonosnika, z ali brez medsebojne hidravlične povezave. Na obravnavanem območju so bile meje vodonosnih sistemov prilagojene na merilo karte 1:25.000. Namenjena so zanesljivemu ugotavljanju stanja celotne pomembne prostornine podzemnih voda v državi in doseganja okoljskih ciljev, ki jih predpisuje Vodna direktiva.

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    Map represents the calculated (surface) heat-flow density (HFD) in mW/m2 with topographic correction. It is made with data from 119 boreholes from the measured temperatures in the available boreholes and measured thermal conductivity on cored rock samples from the same boreholes. The pattern of the HFD isolines is affected by numerous parameters, particularly the thermal conductivity of rocks, rock permeability and fracturing, fluid content of the rocks, and all are reflected in the measured temperature gradient in the boreholes.

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    Mineral deposits and resources

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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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    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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    Karta podaja potencialna plazovita območja za območje celotne Slovenije v šestih razredih verjetnosti pojavljanja plazov; ni verjetnosti, zelo majhna verjetnost, majhna verjetnost, srednja verjetnost, velika verjetnost, zelo velika verjetnost. Zanesljivost napovedi je približno 0,88.