Spatial (GIS) analysis of relief and lithology of the Vsetinske Vrchy mountains (Outer West Carpathians, Czech Republic)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F03%3A00001550" target="_blank" >RIV/61989592:15310/03:00001550 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

čeština

Název v původním jazyce

Spatial (GIS) analysis of relief and lithology of the Vsetinske Vrchy mountains (Outer West Carpathians, Czech Republic)

Popis výsledku v původním jazyce

By combination of digital elevation model (DEM) with digital geological maps within GIS environment one is able to detect manifestations of neotectonic movements. This technique is demonstrated on Vsetínské vrchy Mountains, a 367 km2 large area in the Outer West Carpathians, Czech Republic. The results show that steeper hillslopes, higher local relief (LR) and greater Strahler's hypsometric integrals (SHI) correlate well with regions of hard bedrock geology. Contrary to less resistant bedrock geology which is correlated with predominantly gentle slopes, lower LR and smaller SHIs. These facts do not support former opinions on significant neotectonic block faulting of the Vsetínské vrchy Mountains during "neotectonic period". The relief topography is concordant with underlying variously resistant rocks. Thus it seems probable that the youngest evolution of overall study area proceeded steadily. The topographic relief have experienced the state of dynamic equilibrium, which have been caus

Název v anglickém jazyce

KAVES - the catalog of extensions and scripts for ArcView GIS 3.1

Popis výsledku anglicky

By combination of digital elevation model (DEM) with digital geological maps within GIS environment one is able to detect manifestations of neotectonic movements. This technique is demonstrated on Vsetínské vrchy Mountains, a 367 km2 large area in the Outer West Carpathians, Czech Republic. The results show that steeper hillslopes, higher local relief (LR) and greater Strahler's hypsometric integrals (SHI) correlate well with regions of hard bedrock geology. Contrary to less resistant bedrock geology which is correlated with predominantly gentle slopes, lower LR and smaller SHIs. These facts do not support former opinions on significant neotectonic block faulting of the Vsetínské vrchy Mountains during "neotectonic period". The relief topography is concordant with underlying variously resistant rocks. Thus it seems probable that the youngest evolution of overall study area proceeded steadily. The topographic relief have experienced the state of dynamic equilibrium, which have been caus

Druh

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

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

<a href="/cs/project/GA205%2F03%2F0211" target="_blank" >GA205/03/0211: Geografie vybraných přírodních extrémů, jejich dopady a kartografická vizualizace na Moravě a ve Slezsku</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2003

Kód důvěrnosti údajů

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

Název periodika

Annales Societatis Geologorum Poloniae

ISSN

0208-9068

e-ISSN

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Svazek periodika

73

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

12

Strana od-do

55-66

Kód UT WoS článku

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EID výsledku v databázi Scopus

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