Žďárské Vrchy Highland - Geomorphological Landscape in the Top Part of the Bohemian-Moravian Highland with the Unique Crystalline Rocks Forms

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F16%3A00460827" target="_blank" >RIV/68145535:_____/16:00460827 - 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_18" target="_blank" >10.1007/978-3-319-27537-6_18</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Žďárské Vrchy Highland - Geomorphological Landscape in the Top Part of the Bohemian-Moravian Highland with the Unique Crystalline Rocks Forms

Popis výsledku v původním jazyce

Žďárské vrchy Highland is built by metamorphic rocks and is situated in the upper part of Bohemian-Moravian Highlands. A typical feature of Žďárské vrchy is the occurrence of isolated groups of rocks or rock formations (walls, towers, small rock cities), which dominate on flat upland ridges. These ridges are separated by open valleys with flat headwaters. Rock formations are limited by vertical walls and often significantly protrude above the surrounding landscape, occasionally reaching heights well above 30 m, although 15 m is the typical height value. The Žďárské vrchy Highland is a part of the Protected Landscape Area Žďárské vrchy and many rock formations were declared as natural monuments. Landforms of the Žďárské vrchy Highland have originated through polygenetic development since the Cretaceous and are in many ways unique within the highlands in the Hercynian Europe.

Název v anglickém jazyce

Žďárské Vrchy Highland - Geomorphological Landscape in the Top Part of the Bohemian-Moravian Highland with the Unique Crystalline Rocks Forms

Popis výsledku anglicky

Žďárské vrchy Highland is built by metamorphic rocks and is situated in the upper part of Bohemian-Moravian Highlands. A typical feature of Žďárské vrchy is the occurrence of isolated groups of rocks or rock formations (walls, towers, small rock cities), which dominate on flat upland ridges. These ridges are separated by open valleys with flat headwaters. Rock formations are limited by vertical walls and often significantly protrude above the surrounding landscape, occasionally reaching heights well above 30 m, although 15 m is the typical height value. The Žďárské vrchy Highland is a part of the Protected Landscape Area Žďárské vrchy and many rock formations were declared as natural monuments. Landforms of the Žďárské vrchy Highland have originated through polygenetic development since the Cretaceous and are in many ways unique within the highlands in the Hercynian Europe.

Druh

C - Kapitola v odborné knize

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

Landscapes and Landforms of the Czech Republic

ISBN

978-3-319-27536-9

Počet stran výsledku

10

Strana od-do

221-231

Počet stran knihy

422

Název nakladatele

Springer

Místo vydání

Cham

Kód UT WoS kapitoly

000376577900019