The Dyje Canyon-like Valley: Geomorphological Landscape of Deep Valley at the Eastern Part of the Marginal Slope of Bohemian Massif
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F16%3A00460829" target="_blank" >RIV/68145535:_____/16:00460829 - isvavai.cz</a>
Výsledek na webu
<a href="http://www.springer.com/us/book/9783319275369" target="_blank" >http://www.springer.com/us/book/9783319275369</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-3-319-27537-6_19" target="_blank" >10.1007/978-3-319-27537-6_19</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The Dyje Canyon-like Valley: Geomorphological Landscape of Deep Valley at the Eastern Part of the Marginal Slope of Bohemian Massif
Popis výsledku v původním jazyce
Southeastern margin of the Bohemian-Moravian Highland is cut by deep river valleys with incised meanders. The canyon-like valley of the Dyje River belongs to the most important and attractive of them. The valley is embedded into the Paleogene regional planation surface (etchplain) within the hilly land relief, creating sharp morphological contrast, unique in the Bohemian Highland and in the adjacent part of Austria. In the period of the Cold War the area was closed to the public for more than 40 years as it was a part of the “iron curtain. After political changes in the Czech Republic Europe in 1989, the border area was open to the public. Due to rare landscape phenomenon (including landforms) the Dyje valley with its surroundings was declared the Podyjí National Park in 1991. Three basic relief types have been defined in the study area. Special attention is devoted to site with Ice caves the longest pseudokarst cave system in crystalline rocks in the Czech Republic.
Název v anglickém jazyce
The Dyje Canyon-like Valley: Geomorphological Landscape of Deep Valley at the Eastern Part of the Marginal Slope of Bohemian Massif
Popis výsledku anglicky
Southeastern margin of the Bohemian-Moravian Highland is cut by deep river valleys with incised meanders. The canyon-like valley of the Dyje River belongs to the most important and attractive of them. The valley is embedded into the Paleogene regional planation surface (etchplain) within the hilly land relief, creating sharp morphological contrast, unique in the Bohemian Highland and in the adjacent part of Austria. In the period of the Cold War the area was closed to the public for more than 40 years as it was a part of the “iron curtain. After political changes in the Czech Republic Europe in 1989, the border area was open to the public. Due to rare landscape phenomenon (including landforms) the Dyje valley with its surroundings was declared the Podyjí National Park in 1991. Three basic relief types have been defined in the study area. Special attention is devoted to site with Ice caves the longest pseudokarst cave system in crystalline rocks in the Czech Republic.
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
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2016
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
Landscapes and Landforms of the Czech Republic
ISBN
978-3-319-27536-9
Počet stran výsledku
15
Strana od-do
233-247
Počet stran knihy
422
Název nakladatele
Springer
Místo vydání
Cham
Kód UT WoS kapitoly
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