Česká geologická služba
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Kapradinec (1083.1m)

General Characteristics

County (administration): South Bohemia Region
District (town): Český Krumlov
Cadastre: Maňávka u Českého Krumlova
Map 1 : 50 000 (sheet No): 3223, 32231
Geological region: Šumava Moldanubicum - districts ST, PT, CK, CB, PI
Accessibility: - special entry permit necessary (military area, quarry, private land)
ID : 3724

Geology

Short characteristics of the site: The small rocky outcrops exposing penetration of amphibole-biotite melagranite (durbachite) into a secondary foliation of the felsitic granulite. This rock complex is also transected by a dyke of pegmatite several dozens of centimetres thick. This locality belongs to the southeastern part of the Šumava Mts. area.
Regional geologic unit: Bohemian Massif - crystalline complex and pre-Variscian Palaeozoic - Moldanubicum - Magmatites in Moldanubicum
Stratigraphy: variské (hercynské) stáří vyvřelin
Subject: geology, structural geology
Geological phenomenon: horizontal section
Genesis: magmatic, metamorphic (general metamorphism)
Rock: durbachite, pegmatite, gneiss

Territorial conservation

Level of protection: Interesting geological localities in Protected landscape area
Protection of a geol. phenomenon: B - Geological phenomenon is the reason for a recommendation to the protection
Part of LEPA (Large-size especially protected areas): CHKO (Protected landscape area) - Šumava
Conflicts of interests: warfare

References

Pertoldová J., Nahodilová R. eds (2013): Vysvětlivky k základní geologické mapě 1:25 000 list 32-231 Horní Planá. - MS, ČGS Praha

Elaboration and Updating

Elaborated by: Doláková Eva, 09.10.13
Updated by: Pertoldová Jaroslava 16.10.13, Kukal Zdeněk 29.09.17

Citation

The database Significant geological localities of the Czech Republic: 3724 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-05-05]. Available from: http:// lokality.geology.cz/3724.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Intruzivní kontakt durbachitů plutonu Knížecího stolce a retrográdně metamorfovaných granulitů křišťanovského masivu definovaný orientací sekundární magmatické foliace. Délka spodní hrany je 40 cm., Kryštof Verner, 2013
Výchoz granulitové ruly ve vyšším stupni přeměny, SN037., Jaroslava Pertoldová, 2012


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