The importance of seismic methods application for geological reconstruction of rockslide threatened open pit

Kondela, Julián; Prekopová, Marta; Budinský, Vladimír; Pandula, B.; Ďuriška, Igor

doi:10.1016/j.jappgeo.2018.09.005

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Conditions and Causes Of Rockslide Development1

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Cited by 4 publications

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“…There is a tectonic thrust fault in the given area, where Mesozoic sedimentary rocks of mainly dolostones and broken limestone were pushed over granites. The carbonate complex as well as the rockslide is significantly disrupted tectonically, karstificated and divided into blocks of differing extent [4].…”

Section: Conditions and Causes Of Rockslide Developmentmentioning

confidence: 99%

Change of a Highway Route Caused by a Rockslide

Kopecký

Brcek

Frankovská

et al. 2021

APP

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During the spring of 2013, a relatively large rockslide with a total area of 96,952 m2 occurred in the eastern part of the Malá Fatra mountains. The anticipated depth of the slip surfaces was from 30 to 40 metres and the volume of moving mass was estimated to be 2,000,000 m3. The maximum movement of the rockslide on the first day in March 2013 was estimated to be 43 m. The front of the rockslide interfered with the projected D1 highway route. The paper presented here offers an analysis of the causes of the rockslide and its activity in association with the potential threat to the proposed highway.

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Section: Conditions and Causes Of Rockslide Developmentmentioning

confidence: 99%