Landslide of Sandstone Blocks with the Surface of Sliding Running on the Layer of Underlying Claystones - One of Type Slope Deformation Model in Carpathian Flysch

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F06%3A00016742" target="_blank" >RIV/61989100:27350/06:00016742 - 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

Landslide of Sandstone Blocks with the Surface of Sliding Running on the Layer of Underlying Claystones - One of Type Slope Deformation Model in Carpathian Flysch

Popis výsledku v původním jazyce

The essence of the study is the knowledge broadening concerning various stability processes in the slopes of the Carpathian flysch, which is one of the most active geological unites in the Czech and Slovak Republic as far as slope deformations are concerned. The aim of the grant is the qualification of the factors essential in the landslide type gravitational movement in the slopes of the Carpathian flysch. For this purpose, several basic type models of the slope geological structure were chosen in thefirst phase. In the following phases, the relationships between the degree of stability on one side and internal friction angle, cohesion, saturation, slope gradient and the on the other side, were analyzed. The partial study (in this article) deals withonly one of them (Landslide of sandstone blocks with the surface of sliding running on the layer of underlying claystones). From analysing the results it follows that it is the saturation of the slope, the saturation of layers and the gr

Název v anglickém jazyce

Landslide of Sandstone Blocks with the Surface of Sliding Running on the Layer of Underlying Claystones - One of Type Slope Deformation Model in Carpathian Flysch

Popis výsledku anglicky

The essence of the study is the knowledge broadening concerning various stability processes in the slopes of the Carpathian flysch, which is one of the most active geological unites in the Czech and Slovak Republic as far as slope deformations are concerned. The aim of the grant is the qualification of the factors essential in the landslide type gravitational movement in the slopes of the Carpathian flysch. For this purpose, several basic type models of the slope geological structure were chosen in thefirst phase. In the following phases, the relationships between the degree of stability on one side and internal friction angle, cohesion, saturation, slope gradient and the on the other side, were analyzed. The partial study (in this article) deals withonly one of them (Landslide of sandstone blocks with the surface of sliding running on the layer of underlying claystones). From analysing the results it follows that it is the saturation of the slope, the saturation of layers and the gr

Druh

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

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GP205%2F02%2FD144" target="_blank" >GP205/02/D144: Analýza vlivu geologické stavby a základních geotechnických parametrů na stabilitu svahů v typových modelech vněkarpatského flyše</a><br>

Návaznosti

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

Rok uplatnění

2006

Kód důvěrnosti údajů

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

Název periodika

Sborník vědeckých prací Vysoké školy báňské-Technické univerzity Ostrava, Řada hornicko-geologická

ISSN

0474-8476

e-ISSN

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Svazek periodika

LII

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

10

Strana od-do

57-66

Kód UT WoS článku

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EID výsledku v databázi Scopus

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