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Vlčí skála u Hertvíkovic

General Characteristics

County (administration): Hradec Králové Region
District (town): Trutnov
Cadastre: Mladé Buky - Hertvíkovice
Map 1 : 50 000 (sheet No): 0342, 03423
Geological region: Permo-Carboniferous of the Krkonoše-piedmont and Lower Silesian basins
Accessibility: - access without footpath
ID : 3471

Geology

Short characteristics of the site: Krkonoše Piedmont Basin, Permian, Upper Rotliegend (Saxonian). Conglomerate of the Horní Město Beds of the Trutnov Formation. It is of petromictic character, with subangular pebbles up to 30 cm large, with matrix consisting of coarse-grained carbonatic sandstone. Conglomerate is massive, locally with cross bedding and low-angle cross bedding.
Regional geologic unit: Bohemian Massif - superficial deposits and post-Variscian magmatites - Upper Carboniferous and Permian - Lugic Late Palaeozoicum (including Triassic deposits)
Stratigraphy: paleozoikum - perm - spodní perm - saxon
Subject: stratigraphy, sedimentology, petrology, geology
Geological phenomenon: horizontal section, selective erosion, bedding
Genesis: sedimentary
Rock: breccia, conglomerate

Territorial conservation

Level of protection: Registered geological localities suggested for protection
Protection of a geol. phenomenon: B - Geological phenomenon is the reason for a recommendation to the protection
Conflicts of interests: without conflicts

References

Martínek, K. ed. (2012): Vysvětlivky k základní geologické mapě České republiky 1:25 000, list Svoboda nad Úpou 03-423. ;Burliga S., Martínek K. and Wojewoda J. (2008): Perm Karkonoskiego basenu piedmontowego i basenu Nachodu. Wycieczka C, POKOS 3, Baseny srodgórskie: kontekst regionalny srodowisk i procesów sedymentacji. Kudowa Zdrój, 15 – 21 Sep, 2008, pp. 84 – 110, ISBN 978-83-922330-2-2.

Elaboration and Updating

Elaborated by: Martínek Karel, 08.03.12
Updated by: Kukal Zdeněk 26.11.12, Martínek Karel 14.02.13

Citation

The database Significant geological localities of the Czech Republic: 3471 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-04-26]. Available from: http:// lokality.geology.cz/3471.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Brekciovité slepence hornoměstských vrstev trutnovského souvrství. Polymiktní charakter slepenců s valouny kvarcitů, mramorů, svorů , slicitů. Výrazné subvertikální puklinové systémy mají směry sz.-jv. a sv.-jz. často jsou paralelní se sz. orientovanými zlomy., Karel Martínek, 2008


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