Lhota u Žiliny

General Characteristics

County (administration): Středočeský kraj
District (town): Kladno
Village: Lhota
Cadastre: Lhota u Kamenných Žehrovic
Map sheets: 12-23 Kladno, 12-233 Unhošť
Accessibility: access without footpath
ID: 3779


Geology

Short characteristics of the site: The locality is represented by morphologically prominent ridge with small surrounding outcrops. It belogs to the Barrandian area and stratigraphically to the Upper Cambrian of the Příbram-Jince Basin. A series of small abandoned quarries exposes subvolcanic massive grey up to pink rhyolite. Porphyric texture with some quartz phenocrysts is typical for this rock. Fine grained ground mass consists a a mixture of quartz feldspars, muscovite and sericite. This rhyolite was formerly quarried and utilized for buildng purposes.
Regional geologic unit: Bohemian Massif > Bohemicum > Barrandien > Příbram - Jince Basin
Stratigraphy: Upper Cambrian
Subject: geology, geomorphology, volcanology
Geological phenomenon: characteristic rock, rock bag
Genesis: volcanic
Rock: rhyolite


Territorial protection

Level of protection: Interesting geological localities in Protected landscape area
Part of LEPA (Large-size especially protected areas): Křivoklátsko
Conflicts of interests: forestry, vegetation


References
  • M.Stárková et al. (2014): Vysvětlivky ke geologické mapě 12-233 list Unhošť. - MS Archív ČGS Praha.
  • TOULA, J. (1969): Závěrečná zpráva kladensko, surovina: kámen. – MS Čes. geol. služba – Geofond. Praha.
  • Vidal et al. (1975):Radiometric age of volcanics of the Cambrian Křivoklát-Rokycany complex (Bohemian Massif). Geol. Rundsch. 64, 2, 563–570.
  • ŽÁK, J. – KRAFT, P. – HAJNÁ, J. (2013): Timing, styles, and kinematics of Cambro–Ordovician extension in the Teplá–Barrandian unit, Bohemian Massif, and its bearing on the opening of the Rheic Ocean. – International Journal of Earth Sciences, 102: 415–433.
  • Drost et al. (2004):New data on the Neoproterozoic–Cambrian geotectonic setting of the Teplá–Barrandian volcanosedimentary successions: geochemistry, U–Pb zircon ages, and provenance (Bohemian Massif, Czech Republic). – Int. J. Earth. Sci. 93: 742–757

Elaboration and Updating

Elaborated by: Marcela Stárková, 22.08.2014
Updated by: Gürtlerová Pavla, 21.10.2015


Citation

The database Important geological localities of the Czech Republic: 3779 [online]. Prague: Czech Geological Survey, 1998 [cit. 2023-06-16]. Available from: https:// lokality.geology.cz/3779.


Location in map:

Assessment

Scientifical assesment: medium
Educational assesment: middle
Significance: supraregional
Representativeness: middle
Geological importance: geo-historical value, geo-regional value (mapping)
Locality conditions: acceptable

You can send information about a change in the status of the site to lokality@geology.cz


© ČGS 2024, verze: 1.01 - 5.5.14 [21.02.2024]