General Characteristics
County (administration): Plzeň Region
District (town): Rokycany
Cadastre: Stupno, Kříše
Map 1 : 50 000 (sheet No): 1233, 12332
Geological region: Permo-Carboniferous and Tertiary of the Central Bohemian & Western Bohemian limnic regions
Accessibility: - no traffic restriction ( by car)
Excursion locality: yes
ID : 995
Geology
Short characteristics of the site: Part of the Upper Radnice Coal Seam, formerly mined in the Kliment Mine. This seam belongs stratigraphically toi the Westphalian C (Radnice Beds, Kladno Formation). In the banded coal tuffitic interlayers can be observed. Typical example of a development of the coal seam.
Regional geologic unit: Bohemian Massif - superficial deposits and post-Variscian magmatites - Upper Carboniferous and Permian - Central and Western Bohemian Late Palaeozoicum
Stratigraphy: paleozoikum - karbon - svrchní karbon - siles
Subject: mining and mining impacts, geology, sedimentology, economic geology, paleontology
Geological phenomenon: fossils-flora, bed, characteristic rock
Genesis: organogenic (activity of organisms)
Rock: coal
Territorial conservation
Level of protection: Nature monument
Additional information: See the Digital register of the Agency for Nature Conservation and Landscape Protection of the Czech Republic AOPK ČR
Protection of a geol. phenomenon: A - Protected Area (declared as Geological Locality)
Part of the Geopark: Barrandien
Conflicts of interests: without conflicts
References
Pašek, J. (1968): Geologické a uhelně petrografické poměry v dole Matylda IV. v břaské pánvi. - MS PŘF UK Praha. Elaboration and Updating
Elaborated by: Drábková Jana, Pašek Jaroslav, 11.02.94
Updated by: Lojka Richard 10.07.10, Lojka Richard 10.07.10 Citation
The database Significant geological localities of the Czech Republic: 995 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-04-19]. Available from: http:// lokality.geology.cz/995. Location in map:
Links to neighbouring localities within 2 km radius are available on mouse click in the map window. |