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rdf:type
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Description
| - The essence of the partial project 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, are analyzed. The partial project (in this article)deals with only one of them (block slide of sandstones sinking into claystones, whose bedrock is formed by undisturbed sandstones).
- The essence of the partial project 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, are analyzed. The partial project (in this article)deals with only one of them (block slide of sandstones sinking into claystones, whose bedrock is formed by undisturbed sandstones). (en)
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Title
| - One of Type Slope Deformation Model in Carpathian Flysch - Block Slide of Sandstones Sinking Into Claystones
- One of Type Slope Deformation Model in Carpathian Flysch - Block Slide of Sandstones Sinking Into Claystones (en)
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skos:prefLabel
| - One of Type Slope Deformation Model in Carpathian Flysch - Block Slide of Sandstones Sinking Into Claystones
- One of Type Slope Deformation Model in Carpathian Flysch - Block Slide of Sandstones Sinking Into Claystones (en)
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skos:notation
| - RIV/61989100:27350/03:00009246!RIV/2004/GA0/273504/N
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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...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/61989100:27350/03:00009246
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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...ontrolniKodProRIV
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http://linked.open...v/mistoKonaniAkce
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http://linked.open...i/riv/mistoVydani
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http://linked.open...i/riv/nazevZdroje
| - 35th International October Conference on Mining and Metallurgy
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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...ocetUcastnikuAkce
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http://linked.open...nichUcastnikuAkce
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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...iv/tvurceVysledku
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http://linked.open...vavai/riv/typAkce
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http://linked.open.../riv/zahajeniAkce
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number of pages
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http://purl.org/ne...btex#hasPublisher
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https://schema.org/isbn
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http://localhost/t...ganizacniJednotka
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