General Characteristics
County (administration): Pardubice Region
District (town): Chrudim
Cadastre: Štěnec
Map 1 : 50 000 (sheet No): 1431, 14313
Geological region: Czech Cretaceous Basin - E-Bohemian and W-Moravian Cretaceous; Chrudim Cretaceous; Králíky Furrow; Police Basin
Accessibility: - no traffic restriction ( by car)
ID : 3617
Geology
Short characteristics of the site: The hydrogeological drilling, water outflow in a brook. The area consists of the Cretaceous sediments. Their section includes basal sandstones of the Peruc-Korycany Formation and overlying finer grained sediments of the Bílá Hora Formation. The vertical alternation of sediments with different porosity makes also possible the alternation of collectors and isolators. Detailed hydrogeological studies were carried out in this area. This locality belongs to the National Geopart "Železné hory - the Iron Mountains".
Regional geologic unit: Bohemian Massif - superficial deposits and post-Variscian magmatites - Cretaceous - Czech Cretaceous Basin
Stratigraphy: mezozoikum - křída - svrchní křída - turon - střední turon
Subject: hydrogeology
Geological phenomenon: spring, river source
Genesis: sedimentary
Rock: marlstone
Territorial conservation
Level of protection: Registered interesting geological localities
Protection of a geol. phenomenon: C - Geological phenomenon is the reason for a registration in the database of CGS
Part of the Geopark: Železné hory
Conflicts of interests: private property
References
DOUCEK, Jan (2012): Národní Geopark Železné hory - mapování. Závěrečná zpráva, MS Vodní zdroje Chrudim, spol. s r. o. Elaboration and Updating
Elaborated by: Králová Anna, 05.11.12
Updated by: Kukal Zdeněk 21.09.17, Kukal Zdeněk 26.09.17 Citation
The database Significant geological localities of the Czech Republic: 3617 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-05-06]. Available from: http:// lokality.geology.cz/3617. Location in map:
Links to neighbouring localities within 2 km radius are available on mouse click in the map window. |