General Characteristics

County (administration): Zlín Region
District (town): Vsetín
Cadastre: Prostřední Bečva
Map 1 : 50 000 (sheet No): 2523, 25232
Geological region: Subsilesian & Silesian units
Accessibility: - no traffic restriction ( by car)
ID : 885

Geology

Short characteristics of the site: Rocky hill slope with outcrops of the sediments of the Godula Beds. They consists of massive beds of glauconitic sandstones with interlayers of fissile claystones and conglomerates (Cretaceous age). Movement of sandstone blocks formed largest pseudokarst cave system in the Beskydy Mts.
Regional geologic unit: Carpathian - Flysch belt - Outer (Menilit-Krosněny) group of nappes
Stratigraphy: mezozoikum - křída
Subject: geomorphology
Geological phenomenon: pseudocrast cave
Genesis: gravitational
Rock: sandstone

Territorial conservation

Level of protection: Interesting geological localities in Protected landscape area
Protection of a geol. phenomenon: C - Geological phenomenon is the reason for a registration in the database of CGS
Part of LEPA (Large-size especially protected areas): CHKO (Protected landscape area) - Beskydy
Conflicts of interests: tourism, sports

References

Wagner, J. et al. (1990): Jeskyně Moravskoslezských Beskyd a okolí.

Elaboration and Updating

Elaborated by: Šulgan František, 22.11.93

Citation

The database Significant geological localities of the Czech Republic: 885 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-04-25]. Available from: http:// lokality.geology.cz/885.

Location in map: