About: Contribution to the morphodynamic chronology of Beskydian rivers (Morávka River 1780-1997)     Goto   Sponge   NotDistinct   Permalink

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Description
  • In the case of Beskydian water streams we are concentrating on the morphodynamics in the historic period (1780 ? 1997). We have chosen the Morávka 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 Vyšní Lhoty and the confluence of the Morávka and the Ostravice Rivers in Frýdek-Místek (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.
  • In the case of Beskydian water streams we are concentrating on the morphodynamics in the historic period (1780 ? 1997). We have chosen the Morávka 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 Vyšní Lhoty and the confluence of the Morávka and the Ostravice Rivers in Frýdek-Místek (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)
Title
  • Contribution to the morphodynamic chronology of Beskydian rivers (Morávka River 1780-1997)
  • Contribution to the morphodynamic chronology of Beskydian rivers (Morávka River 1780-1997) (en)
skos:prefLabel
  • Contribution to the morphodynamic chronology of Beskydian rivers (Morávka River 1780-1997)
  • Contribution to the morphodynamic chronology of Beskydian rivers (Morávka River 1780-1997) (en)
skos:notation
  • RIV/61988987:17310/02:00000070!RIV/2004/MSM/173104/N
http://linked.open.../vavai/riv/strany
  • 50-56
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • Z(MSM 173100002)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...dnocenehoVysledku
  • 641701
http://linked.open...ai/riv/idVysledku
  • RIV/61988987:17310/02:00000070
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • fluvial geomorphology; morphodynamic changes; dynamic equilibrium; aerial images; man-induced river bed changes (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...ontrolniKodProRIV
  • [836A92846263]
http://linked.open...v/mistoKonaniAkce
  • Brno
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  • Brno
http://linked.open...i/riv/nazevZdroje
  • Kirchner, K., Roštínský, P. : Geomorfologický Sborník
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...ocetUcastnikuAkce
http://linked.open...nichUcastnikuAkce
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Hradecký, Jan
http://linked.open...vavai/riv/typAkce
http://linked.open.../riv/zahajeniAkce
http://linked.open...n/vavai/riv/zamer
number of pages
http://purl.org/ne...btex#hasPublisher
  • Masarykova univerzita. Přírodovědecká fakulta; ČAG
https://schema.org/isbn
  • 80-210-2974-9
http://localhost/t...ganizacniJednotka
  • 17310
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