INTERACTION OF THE HILLSLOPES AND VALLEY BOTTOMS ON THE NW SLOPE OF THE LYSA HORA MT., THE HIGHEST PEAK OF THE WESTERN BESKIDS

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10318688" target="_blank" >RIV/00216208:11310/15:10318688 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/49777513:23420/15:43925201

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

INTERACTION OF THE HILLSLOPES AND VALLEY BOTTOMS ON THE NW SLOPE OF THE LYSA HORA MT., THE HIGHEST PEAK OF THE WESTERN BESKIDS

Popis výsledku v původním jazyce

To reveal the slope-channel interaction in the highest parts of the Western Beskids, we studied the valley floor, colluvial accumulations and slope deformations in the Satina River valley (Outer Western Carpathians, Czech Republic). In the uppermost partof the valley the gradual change from the U-shaped to the V-shaped valley is distinctive. The river channel is vertically cut in the middle part of the valley (ca 19 m into the sediments and further 3 m into the bedrock formed by thinly laminated claystones). Colluvial layers formed by multigenerational debris flows with fluvial intercalations form the sedimentary infill in this stretch. The method of electrical resistivity tomography has confirmed deep-seated disintegration of the Luksinec ridge and the occurrence of several generations of rockslides and rather shallow debris slides on the slopes above the studied site. Accumulations of the landslides are considered to be the source area of a large volume of colluvial sediments in the

Název v anglickém jazyce

INTERACTION OF THE HILLSLOPES AND VALLEY BOTTOMS ON THE NW SLOPE OF THE LYSA HORA MT., THE HIGHEST PEAK OF THE WESTERN BESKIDS

Popis výsledku anglicky

To reveal the slope-channel interaction in the highest parts of the Western Beskids, we studied the valley floor, colluvial accumulations and slope deformations in the Satina River valley (Outer Western Carpathians, Czech Republic). In the uppermost partof the valley the gradual change from the U-shaped to the V-shaped valley is distinctive. The river channel is vertically cut in the middle part of the valley (ca 19 m into the sediments and further 3 m into the bedrock formed by thinly laminated claystones). Colluvial layers formed by multigenerational debris flows with fluvial intercalations form the sedimentary infill in this stretch. The method of electrical resistivity tomography has confirmed deep-seated disintegration of the Luksinec ridge and the occurrence of several generations of rockslides and rather shallow debris slides on the slopes above the studied site. Accumulations of the landslides are considered to be the source area of a large volume of colluvial sediments in the

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2015

Kód důvěrnosti údajů

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

Název periodika

Carpathian Journal of Earth and Environmental Sciences

ISSN

1842-4090

e-ISSN

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Svazek periodika

10

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

RO - Rumunsko

Počet stran výsledku

16

Strana od-do

159-174

Kód UT WoS článku

000355385400014

EID výsledku v databázi Scopus

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