Landslide landscape of the Moravskoslezské Beskydy Mountains and their surroundings

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F16%3AA1701M50" target="_blank" >RIV/61988987:17310/16:A1701M50 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Jazyk výsledku
angličtina
Název v původním jazyce
Landslide landscape of the Moravskoslezské Beskydy Mountains and their surroundings
Popis výsledku v původním jazyce
Moravskoslezské Beskydy Mts represent the highest part of the Western Carpathians in theCzech Republic and could serve as an archetype of elevated flysch landscape that originated within the Alpine thrust-and-fold belt. Major landforms of the area originated as a consequence of Miocene thrusting, rock control (alternation of sandstone and shale layers of different rock strength), fluvial processes and mass movements. Of major importance are ancient and active landslides that play a crucial role in increasing geodiversity of themountain slopes.
Název v anglickém jazyce
Landslide landscape of the Moravskoslezské Beskydy Mountains and their surroundings
Popis výsledku anglicky
Moravskoslezské Beskydy Mts represent the highest part of the Western Carpathians in theCzech Republic and could serve as an archetype of elevated flysch landscape that originated within the Alpine thrust-and-fold belt. Major landforms of the area originated as a consequence of Miocene thrusting, rock control (alternation of sandstone and shale layers of different rock strength), fluvial processes and mass movements. Of major importance are ancient and active landslides that play a crucial role in increasing geodiversity of themountain slopes.

Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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