How geomorphologic processes on slopes affect mid-mountain valley headwalls during the post-glacial history: a multi-methodical approach from the High Sudetes Mts

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F18%3A10374398" target="_blank" >RIV/00216208:11310/18:10374398 - isvavai.cz</a>

Výsledek na webu

<a href="https://meetingorganizer.copernicus.org/EGU2018/EGU2018-16117.pdf" target="_blank" >https://meetingorganizer.copernicus.org/EGU2018/EGU2018-16117.pdf</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

How geomorphologic processes on slopes affect mid-mountain valley headwalls during the post-glacial history: a multi-methodical approach from the High Sudetes Mts

Popis výsledku v původním jazyce

The present geomorphological state of mid-mountains reflects Cenozoic evolution containing tectonic, fluvial, glacial, periglacial and slope processes. The mountain valley headwalls are characterized by presence of all above-mentioned geomorphologic processes and they are one of the most dynamic parts of the landscape. The valleys also represent important corridors, in which the mass and energy is being transported from the upper parts of the mountains toward the foothills. Hence, the knowledge of their evolution is the key for complex understanding of geomorphological development of the mountains and their surroundings. The High Sudetes Mts. are suitable territory for geomorphic research of the upper parts of valleys, because there is a present insight about young tectonics, glacial, periglacial, fluvial and slope geomorphologic conditions during the Quaternary climate variations.

Název v anglickém jazyce

How geomorphologic processes on slopes affect mid-mountain valley headwalls during the post-glacial history: a multi-methodical approach from the High Sudetes Mts

Popis výsledku anglicky

The present geomorphological state of mid-mountains reflects Cenozoic evolution containing tectonic, fluvial, glacial, periglacial and slope processes. The mountain valley headwalls are characterized by presence of all above-mentioned geomorphologic processes and they are one of the most dynamic parts of the landscape. The valleys also represent important corridors, in which the mass and energy is being transported from the upper parts of the mountains toward the foothills. Hence, the knowledge of their evolution is the key for complex understanding of geomorphological development of the mountains and their surroundings. The High Sudetes Mts. are suitable territory for geomorphic research of the upper parts of valleys, because there is a present insight about young tectonics, glacial, periglacial, fluvial and slope geomorphologic conditions during the Quaternary climate variations.

Druh

O - Ostatní výsledky

CEP obor

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OECD FORD obor

10508 - Physical geography

Projekt

<a href="/cs/project/GA17-21612S" target="_blank" >GA17-21612S: Vývoj strukturních půd a jejich paleogeografický význam pro rekonstrukci přírodních podmínek střední Evropy v kvartéru</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2018

Kód důvěrnosti údajů

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