GEOMORPHOLOGICAL INVENTORY OF ROCK LANDFORMS ONMT. KAMENEC IN THE NOVOHRADSKÉ HORYMTS. (THE CZECH REPUBLIC)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12410%2F14%3A43887282" target="_blank" >RIV/60076658:12410/14:43887282 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68145535:_____/14:00431722

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

GEOMORPHOLOGICAL INVENTORY OF ROCK LANDFORMS ONMT. KAMENEC IN THE NOVOHRADSKÉ HORYMTS. (THE CZECH REPUBLIC)

Popis výsledku v původním jazyce

For the investigated area, located in the Novohradské hory Mts. (South Bohemia), cryogenic forms built by granite are characterize and are forming a unique relief in the Czech Republic. Study site Mt. Kamenec (1 072 m a.s.l.) is distinguished by high density of manifold cryogenic forms. Detailed geomorphological mapping with using GPS instrument was utilized for research and geomorphological inventory, the geomorphological map of the study lokality was elaborated. Within cryogenic forms, basic destructive and accumulative forms were mapped - tors (9), fros cliffs (10), peak kastle coppies, rock wall, blockfield, debris heap and small weathering forms (rock ledges, rock basins ). Main destructive granite forms are conditioned by activities of cryogenicweathering and structural-tectonic character (jointing and foliation) of granite. One hundred sixty-six joint measurements were performed in the interested area. It was found, that prevailing orientations of joints are ENE-WSW and NW-SE,

Název v anglickém jazyce

GEOMORPHOLOGICAL INVENTORY OF ROCK LANDFORMS ONMT. KAMENEC IN THE NOVOHRADSKÉ HORYMTS. (THE CZECH REPUBLIC)

Popis výsledku anglicky

For the investigated area, located in the Novohradské hory Mts. (South Bohemia), cryogenic forms built by granite are characterize and are forming a unique relief in the Czech Republic. Study site Mt. Kamenec (1 072 m a.s.l.) is distinguished by high density of manifold cryogenic forms. Detailed geomorphological mapping with using GPS instrument was utilized for research and geomorphological inventory, the geomorphological map of the study lokality was elaborated. Within cryogenic forms, basic destructive and accumulative forms were mapped - tors (9), fros cliffs (10), peak kastle coppies, rock wall, blockfield, debris heap and small weathering forms (rock ledges, rock basins ). Main destructive granite forms are conditioned by activities of cryogenicweathering and structural-tectonic character (jointing and foliation) of granite. One hundred sixty-six joint measurements were performed in the interested area. It was found, that prevailing orientations of joints are ENE-WSW and NW-SE,

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DO - Ochrana krajinných území

OECD FORD obor

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Projekt

<a href="/cs/project/KJB300460501" target="_blank" >KJB300460501: Porovnání kvartérního vývoje Novohradských hor a vybraných částí Šumavy</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Carpathian Journal of Earth and Environmental Sciences

ISSN

1842-4090

e-ISSN

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Svazek periodika

9

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

RO - Rumunsko

Počet stran výsledku

8

Strana od-do

253-260

Kód UT WoS článku

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EID výsledku v databázi Scopus

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