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Gravitational deformations in mesozoic rocks of the carpathian mountain ranges

Nemĉok, A. / Baliak, F.

Summary The authors deal with gravitational deformations in areas built of Mesozoic rocks, included in the area of high mountain ranges of the West Carpathians. These areas are affected by slope movements of all the four principal groups in the sense of the classification by A. Nemčok, J. Pašek, J. Rybář (1972). In total 410 deformations have been recorded. Most frequent are ceep slope deformations with the character of disintegration of mountain ridges and of slopes with a system of rock rifts and blocks distributed over the alpinotypically folded soft bedrock. An example of such deformations is the deformation on Sivý vrch hill and Radové skaly in the Západné Tatry moúntains, which is described in detail.

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Gravitational deformations in mesozoic rocks of the carpathian mountain ranges

Nemĉok, A. / Baliak, F.

Summary The authors deal with gravitational deformations in areas built of Mesozoic rocks, included in the area of high mountain ranges of the West Carpathians. These areas are affected by slope movements of all the four principal groups in the sense of the classification by A. Nemčok, J. Pašek, J. Rybář (1972). In total 410 deformations have been recorded. Most frequent are ceep slope deformations with the character of disintegration of mountain ridges and of slopes with a system of rock rifts and blocks distributed over the alpinotypically folded soft bedrock. An example of such deformations is the deformation on Sivý vrch hill and Radové skaly in the Západné Tatry moúntains, which is described in detail.

Gravitational deformations in mesozoic rocks of the carpathian mountain ranges

Nemĉok, A. / Baliak, F.

Summary The authors deal with gravitational deformations in areas built of Mesozoic rocks, included in the area of high mountain ranges of the West Carpathians. These areas are affected by slope movements of all the four principal groups in the sense of the classification by A. Nemčok, J. Pašek, J. Rybář (1972). In total 410 deformations have been recorded. Most frequent are ceep slope deformations with the character of disintegration of mountain ridges and of slopes with a system of rock rifts and blocks distributed over the alpinotypically folded soft bedrock. An example of such deformations is the deformation on Sivý vrch hill and Radové skaly in the Západné Tatry moúntains, which is described in detail.

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Title:

Gravitational deformations in mesozoic rocks of the carpathian mountain ranges

Contributors:

Nemĉok, A. (author) / Baliak, F. (author)

Published in:

Bulletin of the International Association of Engineering Geology - Bulletin de l'Association Internationale de Géologie de l'Ingénieur ; 16

Publication date:

1977

ISSN:

DOI:

https://doi.org/10.1007/BF02591463

Type of media:

Article (Journal)

Type of material:

Electronic Resource

Language:

English

Keywords:

Zeitschrift , Online-Ressource , Ingenieurgeologie

Classification:

BKL: 56.00$jBauwesen: Allgemeines / 38.58 Geomechanik / 38.58$jGeomechanik / 56.20 Ingenieurgeologie, Bodenmechanik / 56.00 Bauwesen: Allgemeines / 56.20$jIngenieurgeologie$jBodenmechanik
RVK: ELIB18

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