Recent Landform Evolution in the Moravian-Silesian Carpathians (Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61988987%3A17310%2F12%3AA13017FG" target="_blank" >RIV/61988987:17310/12:A13017FG - 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

Recent Landform Evolution in the Moravian-Silesian Carpathians (Czech Republic)

Popis výsledku v původním jazyce

Topographic changes in the Moravian-Silesian Carpathians have been due to variations of natural conditions (climatic changes, accelerated rates of exogenic geomorphic processes during the Little Ice Age), but mainly to the growing intensity of human activities (tillage, deforestation, accelerated soil erosion, urban sprawl). In this geomorphologically highly sensitive region, land-use changes exerted a great influence on the intensity and type of exogenic geomorphological processes in the last millennium. Their impact is studied on archive maps. The density of slope deformations (like deep-seated slope failures, lateral spreading, toppling, sackung, translational and rotational landslides, earthflows, debris flows, and rockfalls) in the study area is the highest in the Czech Republic.Other geomorphic processes presented in this overview are erosion by water on the surface and underground (piping), wind erosion, and a range of anthropogenic processes.

Název v anglickém jazyce

Recent Landform Evolution in the Moravian-Silesian Carpathians (Czech Republic)

Popis výsledku anglicky

Topographic changes in the Moravian-Silesian Carpathians have been due to variations of natural conditions (climatic changes, accelerated rates of exogenic geomorphic processes during the Little Ice Age), but mainly to the growing intensity of human activities (tillage, deforestation, accelerated soil erosion, urban sprawl). In this geomorphologically highly sensitive region, land-use changes exerted a great influence on the intensity and type of exogenic geomorphological processes in the last millennium. Their impact is studied on archive maps. The density of slope deformations (like deep-seated slope failures, lateral spreading, toppling, sackung, translational and rotational landslides, earthflows, debris flows, and rockfalls) in the study area is the highest in the Czech Republic.Other geomorphic processes presented in this overview are erosion by water on the surface and underground (piping), wind erosion, and a range of anthropogenic processes.

Druh

C - Kapitola v odborné knize

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

2012

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Recent Landform Evolution. The Carpatho-Balkan-Dinaric Region

ISBN

978-94-007-2447-1

Počet stran výsledku

37

Strana od-do

103-139

Počet stran knihy

460

Název nakladatele

Springer

Místo vydání

Heidelberg

Kód UT WoS kapitoly

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