Laski Ravnik

The area studied by Mihevc and his colleagues, included large, horizontal, epiphreatic caves. In contrast, all of the features currently accessible on the surface of Laski Ravnik were originally deep phreatic, oblique (reflecting the dip of the enclosing strata), and relatively small. All of the denuded channels in the area are filled with a variety of clastic sediments, and localized flowstone deposits also occur. Where visible and washed clean, the channel walls are seen to be modified to some extent by small-scale spalling. 

Gersl., M., Stepisnik, U., and Sustersic, S., 1999, Brezstropa jama pri bunkerju (La ki Ravnik) [The unroofed cave near the bunker (Laski Ravnik) in Slovene, English summary], Acta carsologica, 28 pp. 77-90. 

Sustersid, F., 1998b, Interaction between a cave system and the lowering karst surface Case study Laski Ravnik, Acta carsologica, 27 pp. 115-138. 

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