"2002-06-10+02:00"^^ . . "RIV/61988987:17310/02:00000070" . . . . "fluvial geomorphology; morphodynamic changes; dynamic equilibrium; aerial images; man-induced river bed changes"@en . . . . "[836A92846263]" . "Contribution to the morphodynamic chronology of Beskydian rivers (Mor\u00E1vka River 1780-1997)"@en . "In the case of Beskydian water streams we are concentrating on the morphodynamics in the historic period (1780 ? 1997). We have chosen the Mor\u00E1vka River as an example locality. It represents ideal object of study from the point of geomorphologic regime and types of changes influenced by a man. The studied locality itself is the length between the weir in Vy\u0161n\u00ED Lhoty and the confluence of the Mor\u00E1vka and the Ostravice Rivers in Fr\u00FDdek-M\u00EDstek (see Fig. 1). The impacts caused transformation of the dynami c mechanisms of geomorphologic processes that can be explained through theory of stability, theory of dynamic equilibrium and theory of geomorphic thresholds. Water streams with geomorphologic braiding channel pattern are marked with frequent anabranchi ng in thickly gravelled beds as a consequence of unbalanced flows (pre-glacier zone) or as a consequence of periodic (or, as the case may be, episodic) flooding. The last example is typical for the Beskydian region." . "RIV/61988987:17310/02:00000070!RIV/2004/MSM/173104/N" . . "641701" . "Contribution to the morphodynamic chronology of Beskydian rivers (Mor\u00E1vka River 1780-1997)"@en . "In the case of Beskydian water streams we are concentrating on the morphodynamics in the historic period (1780 ? 1997). We have chosen the Mor\u00E1vka River as an example locality. It represents ideal object of study from the point of geomorphologic regime and types of changes influenced by a man. The studied locality itself is the length between the weir in Vy\u0161n\u00ED Lhoty and the confluence of the Mor\u00E1vka and the Ostravice Rivers in Fr\u00FDdek-M\u00EDstek (see Fig. 1). The impacts caused transformation of the dynami c mechanisms of geomorphologic processes that can be explained through theory of stability, theory of dynamic equilibrium and theory of geomorphic thresholds. Water streams with geomorphologic braiding channel pattern are marked with frequent anabranchi ng in thickly gravelled beds as a consequence of unbalanced flows (pre-glacier zone) or as a consequence of periodic (or, as the case may be, episodic) flooding. The last example is typical for the Beskydian region."@en . "17310" . "Hradeck\u00FD, Jan" . "1"^^ . "0"^^ . "1"^^ . "0"^^ . "7"^^ . . "Contribution to the morphodynamic chronology of Beskydian rivers (Mor\u00E1vka River 1780-1997)" . . "Masarykova univerzita. P\u0159\u00EDrodov\u011Bdeck\u00E1 fakulta; \u010CAG" . . "Z(MSM 173100002)" . "80-210-2974-9" . . . "Brno" . . . . "Brno" . . "Contribution to the morphodynamic chronology of Beskydian rivers (Mor\u00E1vka River 1780-1997)" . "50-56" . . "Kirchner, K., Ro\u0161t\u00EDnsk\u00FD, P. : Geomorfologick\u00FD Sborn\u00EDk" .