General Characteristics

County (administration): Zlín Region
District (town): Vsetín
Cadastre: Malá Bystřice
Map 1 : 50 000 (sheet No): 2523, 25233
Geological region: Fore-Magura, Rača (E from the Napajedla gateway), Bystrica & Bílé Karpaty units
Accessibility: - no traffic restriction ( by car)
Excursion locality: yes
ID : 1056

Geology

Short characteristics of the site: Active landslide Vaculov – Sedlo is complex slope failure on the area of 2.5 km2, with removed volume about 123 millions m3. The rockground is built of Eocene Beloveža Formation (Rača Unit of the Magura Group of Nappes). The main body of the landslide represents the block slide 40 to 70 m thick. Gravity movements formed or predisposed variety of features like frontal folds, landslide lakes, pseudokarst forms, rockfalls, growth response of trees etc. The landslide is important open-air laboratory for geotechnical study and monitoring. This locality is situated in the Protected Landscape Area Beskydy.
Regional geologic unit: Carpathian - Flysch belt - Magurian group of nappes
Stratigraphy: kenozoikum - kvartér, kenozoikum - paleogén - eocén
Subject: engineering geology, geomorphology
Geological phenomenon: pseudocrast cave, landslide, sinkhole, swallow hole, scree
Genesis: gravitational
Rock: claystone, sandstone

Territorial conservation

Level of protection: Registred geological localities suggested to protection 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) - Beskydy
Conflicts of interests: forestry, ground instability

References

Pesl, V. et al. (1990): Vysvětlivky k základní geologické mapě 1 : 25 000, list 25-233 Valašská Bystřice. - MS ČGÚ Praha.; Sloboda, J. - Sekyra, Z. - Kujal, R. - Trávníčková, E. (1998a): Malá Bystřice - tábor Tatry. Geotechnický průzkum sesuvu. – MS, S.G.-Geotechnika, 35 str. Ostrava.; Baroň, I. et al. (2003): Svahové deformace v ČR: Výzkum modelových lokalit na Vsetínsku v roce 2002 a 2003, Etapová závěrečná zpráva. - MS ČGS, Praha.; Baroň, I. (2004): Structure, dynamics and history of deep-seated slope failures in the rača Unit, Magura Nappes, Outer Western Carpathians (Czech Republic). - MS Masarykova univerzita, Brno, 98 pp.; Baroň, I. (2005): Stručný popis registrovaných sesuvných jevů na listu mapy 1:10 000 25-23-22. - MS ČGS, Praha.; Bubík, M. - Švábenická, L. (2006): Výsledky mikropaleontologického studia vrtů vyhloubených v rámci výzkumu sesuvů v magurském flyši. Geol. výzk. Mor. Slez. v roce 2005, 36-40. Brno.; Bubík, M. et al. (2007): Vysvětlivky k základní geologické mapě ČR 1 : 25 000, 25-233 Valašská Bystřice. MS Česká geologická služba, 75 s. Praha.

Elaboration and Updating

Elaborated by: Kirchner Karel, 10.11.94
Updated by: Gürtlerová Pavla 22.02.12, Bubík Miroslav 27.02.12, Kukal Zdeněk 27.12.17

Citation

The database Significant geological localities of the Czech Republic: 1056 [online]. Prague: Czech Geological Survey, 1998 [cit. 2024-05-02]. Available from: http:// lokality.geology.cz/1056.

Location in map: