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Country update of Slovak Republic

Marian Fendek and Juraj Franko

Key words
hydrogeothermal structures
Location
Slovakia
Conference
World Geothermal Congress
Year
2000
Session
Country Updates
Language
English
Paper number
R0852

Full text

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Abstract

Geothermal energy in the territory of the Slovak Republic is related to geothermal waters which largely over in Triassiv carbonates of Inner Western Varpathian nappes and, to a lesser extent in Neogene sand, sandstones and conglomerates or in Neogene andesites and related pyroclastics. The distribution of aquifers with geothermal waters and the thermal manifestation of hydrogeothermal structures have enabled the definition of 26 prospective areas and structures with potentially exploitable geothermal energy resources. These aquifers lie at depth of 200-500 m (except in spring areas) and the reservoir temperatures of their geothermal waters range from 20-240oC. The total amount of thermal energy potential of geothermal waters in prospective areas represents 5538 MWt.

Copyright 2000, International Geothermal Association. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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