Česká geologická služba
Geological localities
Home  > Search > Nové Bránice - úvoz

Search

Nové Bránice - úvoz

General Characteristics

County (administration): South Moravia Region
District (town): Brno-venkov
Cadastre: Nové Bránice, Trboušany
Map 1 : 50 000 (sheet No): 2434, 24343
Geological region: Neogene of the Carpathian foredeep
Accessibility: - passable footpath
ID : 4299

Geology

Short characteristics of the site: THIS DATABASE RECORD IS BEING CURRENTLY TRANSLATED
Regional geologic unit: Carpathian - Carpathian foredeep - Southern part of Carpathian foredeep
Stratigraphy: kenozoikum - neogén - miocén - spodní miocén - ottnang
Subject: lithology, sedimentology
Geological phenomenon: characteristic rock, ripple marks, lithological boundary
Genesis: sedimentary
Rock: sand, clay

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
Conflicts of interests: without conflicts

References

Papp, A. - Rogl, F. - Seneš, J. et al. (1973): M2 Ottangien. Die Innviertler, Salgotarjaner, Bantapustaer Schichtengruppe und die Rzehakia Schichten. - Chronostratigraphie und Neostratotypen, 3. Bratislava.

Elaboration and Updating

Elaborated by: Tomanová Petrová Pavla, 11.04.22

Citation

The database Significant geological localities of the Czech Republic: 4299 [online]. Prague: Czech Geological Survey, 1998 [cit. 2022-12-08]. Available from: http:// lokality.geology.cz/4299.

Location in map:

Links to neighbouring localities within 2 km radius are available on mouse click in the map window.
Sedimenty ottnangu, subhorizontálně a korytovitě uložené písky, Pavla Tomanová Petrová, 2022
Sedimenty ottnangu, písky s polohami štěrčíků, Pavla Tomanová Petrová, 2022
Sedimenty ottnangu v úvozové cestě, Pavla Tomanová Petrová, 2022
Sedimenty ottnangu v úvozové cestě mezi obcemi Jezeřany-Maršovice a Nové Bránice, Pavla Tomanová Petrová, 2022


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