Recent landforms evolution in the Moravian-Silesian Carpathians (Czech Republic).
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F12%3A33142269" target="_blank" >RIV/61989592:15310/12:33142269 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/68145535:_____/12:00383036
Výsledek na webu
<a href="http://dx.doi.org/10.1007/978-94-007-2448-8_6" target="_blank" >http://dx.doi.org/10.1007/978-94-007-2448-8_6</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-94-007-2448-8_6" target="_blank" >10.1007/978-94-007-2448-8_6</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Recent landforms 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 landforms 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.
Klasifikace
Druh
C - Kapitola v odborné knize
CEP obor
DE - Zemský magnetismus, geodesie, geografie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2012
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název knihy nebo sborníku
Recent landform evolution. The Carpatho-Balcan-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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