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Malá Pleš

General Characteristics

County (administration): Central Bohemia Region
District (town): Rakovník
Cadastre: Branov
Map 1 : 50 000 (sheet No): 1232, 12321
Geological region: Barrandien Palaeozoic; Blanice Furrow
Accessibility: - access without footpath
ID : 3292

Geology

Short characteristics of the site: Barrandian, Middle Cambrian. Outcrop of conglomerates on the relief promontory. They stratigraphically belong to the Vosnik Conglomerate, youngest member of the Skryje-Týřovice Cambrian. Medium- up to coarse grained conglomerate is of petromictic character, contains quartz, lydite, spilite and greywacke clasts. Contact with overlying Upper Cambrian andesite is also exposed.
Regional geologic unit: Bohemian Massif - crystalline complex and pre-Variscian Palaeozoic - Bohemicum (Central Bohemian region) - Barrandien
Stratigraphy: paleozoikum - kambrium - střední kambrium, paleozoikum - kambrium - svrchní kambrium
Subject: stratigraphy, sedimentology, volcanology
Geological phenomenon: lithological boundary, lava flow
Genesis: sedimentary, volcanic
Rock: conglomerate, slate, schist, andesite

Territorial conservation

Level of protection: National nature reserve in Protected landscape area
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 and Biological Locality)
Part of LEPA (Large-size especially protected areas): CHKO (Protected landscape area) - Křivoklátsko
Part of the Geopark: Barrandien
Conflicts of interests: without conflicts

References

Horák, L. (1962): Nové poznatky o stavbě skryjsko-týřovického kambria. – Čas. Mineral. Geol., roč. 7., č. 4., 404 – 406. Praha.; Kettner, R. (1923): Kambrium skrejsko-tejřovické a jeho okolí. – Sbor. St. geol. Úst. Čs. Republ., 3, 5–63. Praha.

Elaboration and Updating

Elaborated by: Vorel Tomáš, 14.01.11
Updated by: Kukal Zdeněk 01.10.12

Citation

The database Significant geological localities of the Czech Republic: 3292 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-05-02]. Available from: http:// lokality.geology.cz/3292.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Andezity svrchního kambria díky své větší tvrdosti vytvářejí vlastní ostroh při ústí potoka od vrchu Malá Pleš do Berounky., Motyčková Kamila - Šír Jiří, 2015


(C) 2003-2012 ČGS, verse aplikace 1.21 [3.2.2016]