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Abstract
In paper the development of Val Gardena Formation NW of Ljubljana is described. Almost all members of formation are exposed, but nowhere in continuous profiles. Detailed subdivision of Palaeozoic beds permitted a better idea also of tectonic structure of area, especially in the environs of Sv. Jakob, Sv. Katarina and abandoned Knapovže Pb, Zn, Hg deposit.
Highlights
In paper the development of Val Gardena Formation NW of Ljubljana is described
The Val Gardena Formation is completely developed on @irovski vrh
This is the area of popular tourist localities of Sv
Summary
V prispevku je prikazan razvoj Grödenske formacije na obmo~ju severozahodno od Ljubljane, kjer najdemo skoraj vse ~lene formacije, vendar nikjer v sklenjenih profilih. Katarine v sose{~ini starega, opu{~enega Pb, Zn, Hg rudi{~a Knapove
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