. . . "2"^^ . "Kirchner, Karel" . . . "Blokov\u00E1 svahov\u00E1 deformace v krystalick\u00FDch hornin\u00E1ch v \u00FAdol\u00ED Svratky severoz\u00E1padn\u011B od Ti\u0161nova"@cs . "Sborn\u00EDk \u010Cesk\u00E9 geografick\u00E9 spole\u010Dnosti" . "217;220" . "CZ - \u010Cesk\u00E1 republika" . . "Blokov\u00E1 svahov\u00E1 deformace v krystalick\u00FDch hornin\u00E1ch v \u00FAdol\u00ED Svratky severoz\u00E1padn\u011B od Ti\u0161nova" . "Svratka river valley; slope deformations; crystalline rocks; tectonics; pseudokarst forms"@en . "Deep-seated block deformation in crystalline rocks in the Svratka river valley north-west of Ti\u0161nov town"@en . "1210-115X" . "V hlubok\u00E9m, tektonicky zalo\u017Een\u00E9m \u00FAdol\u00ED Svratky jihov\u00FDchodn\u011B od obce Bora\u010D byly zji\u0161t\u011Bny 3 svahov\u00E9 deformace situovan\u00E9 do kr\u00E1tk\u00FDch svahov\u00FDch depres\u00ED zahlouben\u00FDch do p\u0159\u00EDkr\u00E9ho lev\u00E9ho svahu. Jsou vyvinuty v oblasti budovan\u00FDmi krystalick\u00FDmi horninami (b\u00EDte\u0161sk\u00E1 ortorula) a na v\u011Bt\u0161in\u011B plochy maj\u00ED star\u00FD charakter bez ostr\u00FDch morfologick\u00FDch projev\u016F. Prvn\u00ED \u2013 nejv\u011Bt\u0161\u00ED \u2013 lokalita dosahuje d\u00E9lky t\u00E9m\u011B\u0159 1 km a \u0161\u00ED\u0159ky 200 m. Jej\u00ED nejspodn\u011Bj\u0161\u00ED \u010D\u00E1st prota\u017Een\u00E1 pod\u00E9l ost\u0159e zahlouben\u00E9 erozn\u00ED r\u00FDhy byla aktivov\u00E1na v podob\u011B blokov\u00E9ho proudov\u00E9ho sesuvu o d\u00E9lce 320 m a \u0161\u00ED\u0159ce 80 m, poru\u0161uj\u00EDc\u00EDho hluboce skaln\u00ED podlo\u017E\u00ED. Z povrchov\u00FDch tvar\u016F se krom\u011B n\u011Bkolika odlu\u010Dn\u00FDch st\u011Bn a v\u00FDrazn\u00E9ho \u010Dela balvanit\u00E9 akumulace vyskytuj\u00ED \u010Detn\u00E9 tahov\u00E9 rozsedliny a pukliny a n\u011Bkolik hlub\u0161\u00EDch pseudokrasov\u00FDch dutin. Na z\u00E1klad\u011B morfologie bylo ve svahov\u00E9m \u00FAdol\u00ED rozli\u0161eno 5 r\u016Fzn\u011B star\u00FDch f\u00E1z\u00ED sesouv\u00E1n\u00ED. Ostatn\u00ED dv\u011B m\u00E9n\u011B rozs\u00E1hl\u00E9 svahov\u00E9 deformace se projevuj\u00ED akumulacemi na dnech dal\u0161\u00EDch dvou depres\u00ED, je\u017E jsou tvo\u0159eny pouze kamenit\u00FDmi de..." . . . "Altogether, 3 slope deformations were newly found out in the tectonically predisposed valley of the Svratka river south-east of the Bora\u010D village, all situated in short slope depressions within steep left valleyside. They evolved in the area build up of crystalline rocks (b\u00EDte\u0161 orthogneiss of the Moravicum) and they possess an old character without sharp morphological features within major part of its area. First \u2013 the largest \u2013 locality reaches length of 1 km and width of 200 m. Its lowest part extended along sharply cut erosion rill was activated in a form of deep-seated elongated landslide with a length of 320 m and width of 80 m, disturbing largely the bedrock. Several detachment walls, distinctive head of blocky accumulation, frequent tensile cracks and several deeper pseudokarst caverns are occuring on the surface within meso-forms. Altogether, 5 phases of landsliding were distinguished in the slope valley. The other two less extensive slope deformations display by accumulatio..."@en . . . "[C41B5BED8CAB]" . "Blokov\u00E1 svahov\u00E1 deformace v krystalick\u00FDch hornin\u00E1ch v \u00FAdol\u00ED Svratky severoz\u00E1padn\u011B od Ti\u0161nova" . "Ro\u0161t\u00EDnsk\u00FD, Pavel" . "V hlubok\u00E9m, tektonicky zalo\u017Een\u00E9m \u00FAdol\u00ED Svratky jihov\u00FDchodn\u011B od obce Bora\u010D byly zji\u0161t\u011Bny 3 svahov\u00E9 deformace situovan\u00E9 do kr\u00E1tk\u00FDch svahov\u00FDch depres\u00ED zahlouben\u00FDch do p\u0159\u00EDkr\u00E9ho lev\u00E9ho svahu. Jsou vyvinuty v oblasti budovan\u00FDmi krystalick\u00FDmi horninami (b\u00EDte\u0161sk\u00E1 ortorula) a na v\u011Bt\u0161in\u011B plochy maj\u00ED star\u00FD charakter bez ostr\u00FDch morfologick\u00FDch projev\u016F. Prvn\u00ED \u2013 nejv\u011Bt\u0161\u00ED \u2013 lokalita dosahuje d\u00E9lky t\u00E9m\u011B\u0159 1 km a \u0161\u00ED\u0159ky 200 m. Jej\u00ED nejspodn\u011Bj\u0161\u00ED \u010D\u00E1st prota\u017Een\u00E1 pod\u00E9l ost\u0159e zahlouben\u00E9 erozn\u00ED r\u00FDhy byla aktivov\u00E1na v podob\u011B blokov\u00E9ho proudov\u00E9ho sesuvu o d\u00E9lce 320 m a \u0161\u00ED\u0159ce 80 m, poru\u0161uj\u00EDc\u00EDho hluboce skaln\u00ED podlo\u017E\u00ED. Z povrchov\u00FDch tvar\u016F se krom\u011B n\u011Bkolika odlu\u010Dn\u00FDch st\u011Bn a v\u00FDrazn\u00E9ho \u010Dela balvanit\u00E9 akumulace vyskytuj\u00ED \u010Detn\u00E9 tahov\u00E9 rozsedliny a pukliny a n\u011Bkolik hlub\u0161\u00EDch pseudokrasov\u00FDch dutin. Na z\u00E1klad\u011B morfologie bylo ve svahov\u00E9m \u00FAdol\u00ED rozli\u0161eno 5 r\u016Fzn\u011B star\u00FDch f\u00E1z\u00ED sesouv\u00E1n\u00ED. Ostatn\u00ED dv\u011B m\u00E9n\u011B rozs\u00E1hl\u00E9 svahov\u00E9 deformace se projevuj\u00ED akumulacemi na dnech dal\u0161\u00EDch dvou depres\u00ED, je\u017E jsou tvo\u0159eny pouze kamenit\u00FDmi de..."@cs . "P(GA205/03/0211)" . . . . "Deep-seated block deformation in crystalline rocks in the Svratka river valley north-west of Ti\u0161nov town"@en . "2" . . "4"^^ . "RIV/68145535:_____/06:00078936" . "111" . . "467197" . "RIV/68145535:_____/06:00078936!RIV07-GA0-68145535" . "2"^^ . . "Blokov\u00E1 svahov\u00E1 deformace v krystalick\u00FDch hornin\u00E1ch v \u00FAdol\u00ED Svratky severoz\u00E1padn\u011B od Ti\u0161nova"@cs . . .