Slope deformations of the central ridge of the Kysucké Beskydy Mts (Slovakia)

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F09%3AA1100ZWP" target="_blank" >RIV/61988987:17310/09:A1100ZWP - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

Slope deformations of the central ridge of the Kysucké Beskydy Mts (Slovakia)

Original language description

The Veľká Rača massif is a part of the Kysucké Beskydy Mts. and it belongs to the Magura Unit in the Outer Western Carpathians. Nappe-type flysch structure of the Outer Western Carpathians represents environment that is favourable for the occurrence of large slope deformations. Tectonic faults with NE-SW direction predisposed the initiation of these deformations in the studied area. In the case of the Veľká Rača Mt. we speak about a gravitational disintegration of the mountain ridge and contiguous slopes.

Czech name

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Czech description

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Type

D - Article in proceedings

CEP classification

DE - Earth magnetism, geodesy, geography

OECD FORD branch

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Project

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Continuities

S - Specificky vyzkum na vysokych skolach

Publication year

2009

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Article name in the collection

Geomorfologický sborník 8

ISBN

978-80-7399-746-5

ISSN

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e-ISSN

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Number of pages

2

Pages from-to

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Publisher name

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Place of publication

Brno

Event location

Kašperské hory

Event date

Apr 15, 2009

Type of event by nationality

EUR - Evropská akce

UT code for WoS article

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