Connectivity of the coarsest fraction in headwater channels: imprints of fluvial processes and debris-flow activity

Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F15%3AA1601EOY" target="_blank" >RIV/61988987:17310/15:A1601EOY - 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
Connectivity of the coarsest fraction in headwater channels: imprints of fluvial processes and debris-flow activity
Popis výsledku v původním jazyce
Some steep headwater streams of the midmountains landscape of the flysch belt of the Western Carpathians are affected by debris flows. Connectivity of the largest boulder and cobble fractions has been evaluated in steep streams found in the transitionalzones between the hillslopes and alluvial cones of similar lithology and watershed morphometry. Two longitudinal profiles affected by past debris-flow activity and two longitudinal profiles void of such processes were selected.
Název v anglickém jazyce
Connectivity of the coarsest fraction in headwater channels: imprints of fluvial processes and debris-flow activity
Popis výsledku anglicky
Some steep headwater streams of the midmountains landscape of the flysch belt of the Western Carpathians are affected by debris flows. Connectivity of the largest boulder and cobble fractions has been evaluated in steep streams found in the transitionalzones between the hillslopes and alluvial cones of similar lithology and watershed morphometry. Two longitudinal profiles affected by past debris-flow activity and two longitudinal profiles void of such processes were selected.

Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DE - Zemský magnetismus, geodesie, geografie
OECD FORD obor
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Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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