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| rdf:type
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| Description
| - 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 the first 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 with only 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 gradient of slopes
- 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 the first 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 with only 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 gradient of slopes (en)
- 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 the first 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 with only 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 gradient of slopes (cs)
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| Title
| - 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
- 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 (en)
- 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 (cs)
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| skos:prefLabel
| - 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
- 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 (en)
- 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 (cs)
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| skos:notation
| - RIV/61989100:27350/06:00016742!RIV08-GA0-27350___
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| http://linked.open.../vavai/riv/strany
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| http://linked.open...avai/riv/aktivita
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| http://linked.open...avai/riv/aktivity
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| http://linked.open...iv/cisloPeriodika
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| http://linked.open...vai/riv/dodaniDat
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| http://linked.open...aciTvurceVysledku
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| http://linked.open.../riv/druhVysledku
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| http://linked.open...iv/duvernostUdaju
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| http://linked.open...titaPredkladatele
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| http://linked.open...dnocenehoVysledku
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| http://linked.open...ai/riv/idVysledku
| - RIV/61989100:27350/06:00016742
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| http://linked.open...riv/jazykVysledku
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| http://linked.open.../riv/klicovaSlova
| - slope deformation; engineering geology; flysch zone (en)
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| http://linked.open.../riv/klicoveSlovo
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| http://linked.open...odStatuVydavatele
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| http://linked.open...ontrolniKodProRIV
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| http://linked.open...i/riv/nazevZdroje
| - Sborník vědeckých prací Vysoké školy báňské-Technické univerzity Ostrava, Řada hornicko-geologická
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| http://linked.open...in/vavai/riv/obor
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| http://linked.open...ichTvurcuVysledku
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| http://linked.open...cetTvurcuVysledku
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| http://linked.open...vavai/riv/projekt
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| http://linked.open...UplatneniVysledku
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| http://linked.open...v/svazekPeriodika
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| http://linked.open...iv/tvurceVysledku
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| issn
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| number of pages
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| http://localhost/t...ganizacniJednotka
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| is http://linked.open...avai/riv/vysledek
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