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The karst springs of the Kanin massif = Kraški izviri pod Kaninskim pogorjemKomac, BlažIn this article the author summarizes the geographical, hydrological, and geological studies of the Kanin massif done to date and on the basis of physical and chemical analyses of the water describes ... the basic geographical characteristics of the karst springs below the mountains. Using recession curve analysis, the extent of the Glijun spring catchment area has been determined. Catchment areas, draining, and the location of a karst watershed depend on the quantity of water in the aquifer. Due to the overlapping of the catchment areas of various springs, the dumping of dangerous wasted in the high mountains can cause the pollution of many springs. Because the aquifers in the limestone and dolomite Kanin massif are closely linked to those in the Quaternary of the Bovec Basin, protecting the high mountain karst also protects the sources of potable water in the valley.Vir: Geografski zbornik [Elektronski vir] = Acta geographica. - ISSN 1408-8711 (Letn. 41, 2001, str. 7-43)Vrsta gradiva - e-članekLeto - 2001Jezik - angleškiCOBISS.SI-ID - 19490861
Avtor
Komac, Blaž
Teme
geografija |
fizična geografija |
krasoslovje |
kraška hidrologija |
kraški izviri |
visokogorski kras |
Julijske Alpe |
Bovška kotlina |
Kaninsko pogorje |
Slovenija |
geography |
physical geography |
karstology |
karst hydrology |
karst springs |
high mountain karst |
Julian Alps |
Bovec Basin |
Kanin massif |
Slovenia
Vnos na polico
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Komac, Blaž | 21464 |
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