Hydrogeology of the Olševa massif (Slovenia)
Olševa consists of highly pervious carbonates, forming a relatively big fractured and karstified aquifer. Due to its high-altitude mountainous nature, the aquifer is unpolluted and therefore has to be regarded as a potential source of drinking water for the future.The Olševa aquifer is tectonically...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Geological Survey of Slovenia
2002-12-01
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| Series: | Geologija |
| Subjects: | |
| Online Access: | http://www.geologija-revija.si/dokument.aspx?id=644 |