"Geomorfologick\u00FD v\u00FDvoj dolnomoravsk\u00FDch niv" . . . . . "6"^^ . . "[84737390931B]" . . "Biosferick\u00E1 rezervace Doln\u00ED Morava/Lesy \u010CR, s. p." . "\u010Cupa, P., et al.: Lu\u017En\u00ED les v niv\u011B Moravy a Dyje" . "14410" . "RIV/00216224:14410/10:00040579!RIV11-MSM-14410___" . "Kolejka, Jarom\u00EDr" . . "Geomorfologick\u00FD v\u00FDvoj dolnomoravsk\u00FDch niv"@cs . "Geomorfologick\u00FD v\u00FDvoj dolnomoravsk\u00FDch niv" . . . "RIV/00216224:14410/10:00040579" . . . "260680" . "Z krajin\u00E1\u0159sk\u00E9ho hlediska v\u016Fbec syst\u00E9m \u00FAdoln\u00EDch niv p\u0159edstavuje jistou kostru dan\u00E9 krajiny, hmotou a komunika\u010Dn\u011B propojuj\u00EDc\u00ED jej\u00ED jednotliv\u00E9 \u010D\u00E1sti. Vzhled sou\u010Dasn\u00FDch niv je produktem kvart\u00E9ru, a\u010Dkoliv jejich v\u00FDvoj byl predisponov\u00E1n situac\u00ED v posledn\u00ED f\u00E1z\u00EDch t\u0159etihor. P\u0159edkvart\u00E9rn\u00ED geologick\u00E9 podlo\u017E\u00ED ovliv\u0148uje konfiguraci nivy p\u0159\u00EDmo p\u0159\u00EDtomnost\u00ED hornin a zemin - prahy v z\u00FA\u017Een\u00FDch m\u00EDstech v \u00FAdol\u00ED Dyje, neckovit\u00E9 \u00FAdol\u00ED Moravy. Od po\u010D\u00E1tku holoc\u00E9nu doch\u00E1z\u00ED b\u011Bhem velk\u00FDch inundac\u00ED k resedimentaci pleistoc\u00E9nn\u00EDch fluvi\u00E1ln\u00EDch \u0161t\u011Brk\u016F a p\u00EDsk\u016F. Od st\u0159edn\u00EDho holoc\u00E9nu se p\u0159ipojuje ukl\u00E1d\u00E1n\u00ED povod\u0148ov\u00FDch hl\u00EDn a jemn\u00FDch p\u00EDsk\u016F. P\u0159es nivy Dyje a Moravy vedly cesty a stezky, \u010Dasto po agrada\u010Dn\u00EDch valech. Intenzita antropick\u00FDch aktivit v niv\u011B radik\u00E1ln\u011B narostla s n\u00E1stupem pr\u016Fmyslov\u00E9 revoluce po polovin\u011B 19. stolet\u00ED. P\u0159edev\u0161\u00EDm se zv\u00FD\u0161il tlak na intenzivn\u011Bj\u0161\u00ED vyu\u017E\u00EDv\u00E1n\u00ED pozemk\u016F, co\u017E vedlo k n\u00E1sledn\u00E9 pot\u0159eb\u011B ochrany majetku a \u017Eivot\u016F, ale tak\u00E9 ochrany p\u0159\u00EDrodov\u011Bdn\u011B a historicky cenn\u00FDch lokalit."@cs . "P(IAA300860903), S, V" . "flood plain; land forms; Morava; March; Dyje; Thaya; development"@en . "100"^^ . . "Geomorphological development of Lower Morava River floodplain"@en . . "Z krajin\u00E1\u0159sk\u00E9ho hlediska v\u016Fbec syst\u00E9m \u00FAdoln\u00EDch niv p\u0159edstavuje jistou kostru dan\u00E9 krajiny, hmotou a komunika\u010Dn\u011B propojuj\u00EDc\u00ED jej\u00ED jednotliv\u00E9 \u010D\u00E1sti. Vzhled sou\u010Dasn\u00FDch niv je produktem kvart\u00E9ru, a\u010Dkoliv jejich v\u00FDvoj byl predisponov\u00E1n situac\u00ED v posledn\u00ED f\u00E1z\u00EDch t\u0159etihor. P\u0159edkvart\u00E9rn\u00ED geologick\u00E9 podlo\u017E\u00ED ovliv\u0148uje konfiguraci nivy p\u0159\u00EDmo p\u0159\u00EDtomnost\u00ED hornin a zemin - prahy v z\u00FA\u017Een\u00FDch m\u00EDstech v \u00FAdol\u00ED Dyje, neckovit\u00E9 \u00FAdol\u00ED Moravy. Od po\u010D\u00E1tku holoc\u00E9nu doch\u00E1z\u00ED b\u011Bhem velk\u00FDch inundac\u00ED k resedimentaci pleistoc\u00E9nn\u00EDch fluvi\u00E1ln\u00EDch \u0161t\u011Brk\u016F a p\u00EDsk\u016F. Od st\u0159edn\u00EDho holoc\u00E9nu se p\u0159ipojuje ukl\u00E1d\u00E1n\u00ED povod\u0148ov\u00FDch hl\u00EDn a jemn\u00FDch p\u00EDsk\u016F. P\u0159es nivy Dyje a Moravy vedly cesty a stezky, \u010Dasto po agrada\u010Dn\u00EDch valech. Intenzita antropick\u00FDch aktivit v niv\u011B radik\u00E1ln\u011B narostla s n\u00E1stupem pr\u016Fmyslov\u00E9 revoluce po polovin\u011B 19. stolet\u00ED. P\u0159edev\u0161\u00EDm se zv\u00FD\u0161il tlak na intenzivn\u011Bj\u0161\u00ED vyu\u017E\u00EDv\u00E1n\u00ED pozemk\u016F, co\u017E vedlo k n\u00E1sledn\u00E9 pot\u0159eb\u011B ochrany majetku a \u017Eivot\u016F, ale tak\u00E9 ochrany p\u0159\u00EDrodov\u011Bdn\u011B a historicky cenn\u00FDch lokalit." . . "978-80-254-5753-5" . "B\u0159eclav" . . . . "Geomorphological development of Lower Morava River floodplain"@en . . . . "1"^^ . "Geomorfologick\u00FD v\u00FDvoj dolnomoravsk\u00FDch niv"@cs . . "1"^^ . "Lu\u017En\u00ED les v niv\u011B Moravy a Dyje" . "The system of alluvial plains represent some kind skeleton of given landscape connecting its individual segments by the matter exchange and transportation. Present landscape view is resulted by its development in Quaternary period, but there are some evidences of impacts inherited from Tertiary here. Pre-Quaternary geological environment influences the present-day alluvium directly by rocks and deposits - narrower Dyje valley segments, strait Morava valley. Since the Holocene beginning, the re-deposition of Pleistocene gravel and sand run continously, at the time of Middle Holocene the accummulation of loamy flood deposits was added. Merchant roads and paths crossed the alluvium usually following the course of agradation dykes. Intense human impact started in the second half of the 19th century. More intensive land utilizing was followed with flood dykes construction, and later ignited the nature protection and preservation of historically important sites."@en .