Česká geologická služba
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Oblík

General Characteristics

County (administration): Plzeň Region
District (town): Klatovy
Cadastre: Prášily
Map 1 : 50 000 (sheet No): 2233, 22333
Geological region: Šumava Moldanubicum - district KT; Moldanubicum of the Český les Mts.; Domažlice crystalline complex; W-Bohemian Pluton; W-Bohemian basic magmatites
Accessibility: - passable footpath
ID : 2618

Geology

Short characteristics of the site: Isolated rocky elevation which can be called "tor". The tor summit offers magnificent view. Its rock consists of so called stromatitic migmatite. This means that it is clearly banded. First bands are of quartz-feldspar composition, second ones of biotite and sillimanite. The rocks is intensively folded. This locality belongs to the National Park Šumava.
Regional geologic unit: Bohemian Massif - crystalline complex and pre-Variscian Palaeozoic - Moldanubicum - Metamorphic units in Moldanubicum
Stratigraphy: proterozoikum
Subject: geomorphology, geology
Geological phenomenon: characteristic rock, tor
Genesis: metamorphic (general metamorphism)
Rock: migmatite

Territorial conservation

Level of protection: Interesting geological localities in National park
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): NP (National park) - Šumava
Part of the Geopark: Královská Šumava
Conflicts of interests: without conflicts

References

Babůrek J. et al. (2007): Vysvětlivky k základní geologické mapě ČR 1:25 000, list 22-333 Srní, MS, ČGS

Elaboration and Updating

Elaborated by: Babůrek Jiří, 16.01.07

Citation

The database Significant geological localities of the Czech Republic: 2618 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-03-29]. Available from: http:// lokality.geology.cz/2618.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Skalnaté vrcholové partie kóty Oblík (1225 m)tvořené stromatitickým migmatitem., Pavla Gürtlerová, 2009
Skalnaté vrcholové partie kóty Oblík (1225 m)s výhledem na Srní., Pavla Gürtlerová, 2009
Skalnatý vrcholý kóty Oblík (1225 m)tvořený stromatitickým migmatitem., Pavla Gürtlerová, 2009


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