Česká geologická služba
Geological localities
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Lom pod Červeným vrchem

General Characteristics

County (administration): Central Bohemia Region
District (town): Příbram
Cadastre: Věšín v Brdech
Map 1 : 50 000 (sheet No): 2212, 22121
Geological region: Barrandien Palaeozoic; Blanice Furrow
Accessibility: - entry permit for car necessary
Technical object: guarry
Excursion locality: yes
ID : 4172

Geology

Short characteristics of the site: THIS DATABASE RECORD IS BEING CURRENTLY TRANSLATED
Regional geologic unit: Bohemian Massif - crystalline complex and pre-Variscian Palaeozoic - Bohemicum (Central Bohemian region) - Barrandien
Stratigraphy: paleozoikum - kambrium - spodní kambrium
Subject: geology, lithology, sedimentology, economic geology, history
Geological phenomenon: characteristic rock
Genesis: sedimentary, metamorphic (contact metamorphism), hydrothermal mineralization
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) - Brdy
Part of the Geopark: Barrandien
Conflicts of interests: open cast mining

References

Stárková et al. 2019 - Vyvětlivky ke geologické mapě 1 : 25 000, list 22-121 Mirošov; SLAVÍK, F. (1915): Chiastolitické břidlice v okolí rožmitálském (Chiastolithic shales in surroundings of Rožmitál). Rozpr Čes Akad Vědy Slovesn Umění, Tř II 24: 1 –15.

Elaboration and Updating

Elaborated by: Vorel Tomáš, 06.11.19

Citation

The database Significant geological localities of the Czech Republic: 4172 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-05-04]. Available from: http:// lokality.geology.cz/4172.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Železitá alterace kambrických pískovců, Tomáš Vorel, 2016


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