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  • A channel-reach morphology of mountain headwater streams results from the balance between ?uvial and hill- slope processes. A large dataset (n = 102) of channel-reaches coming out from ?ysch mid-mountains was evaluated and compared with streams occurring in other environments. Two new channel-reach morphologies were distinguished with respect to their differences in the ratio of sediment supply to transport capacity: bedrock-cascades and step-rapids. The chaining of channel-reach morphologies by gradient criteria and the parameters of channel gradient and bankfull width related to the basin area show similar trends, when compared to other recent studies. By contrast, bankfull depth indicates its independence on increasing basin area. Signi?cant downstream coarsening of bed material occurs only in alluvial stepped-bed morphologies (cascades, step-pools and step-rapids) mainly due to strong slope-channel coupling processes.
  • A channel-reach morphology of mountain headwater streams results from the balance between ?uvial and hill- slope processes. A large dataset (n = 102) of channel-reaches coming out from ?ysch mid-mountains was evaluated and compared with streams occurring in other environments. Two new channel-reach morphologies were distinguished with respect to their differences in the ratio of sediment supply to transport capacity: bedrock-cascades and step-rapids. The chaining of channel-reach morphologies by gradient criteria and the parameters of channel gradient and bankfull width related to the basin area show similar trends, when compared to other recent studies. By contrast, bankfull depth indicates its independence on increasing basin area. Signi?cant downstream coarsening of bed material occurs only in alluvial stepped-bed morphologies (cascades, step-pools and step-rapids) mainly due to strong slope-channel coupling processes. (en)
Title
  • Morphological patterns of headwater streams based in flysch bedrock: Examples from the Outer Western Carpathians
  • Morphological patterns of headwater streams based in flysch bedrock: Examples from the Outer Western Carpathians (en)
skos:prefLabel
  • Morphological patterns of headwater streams based in flysch bedrock: Examples from the Outer Western Carpathians
  • Morphological patterns of headwater streams based in flysch bedrock: Examples from the Outer Western Carpathians (en)
skos:notation
  • RIV/61988987:17310/14:A1501AZQ!RIV15-GA0-17310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GAP209/10/0309)
http://linked.open...iv/cisloPeriodika
  • 8/2014
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 30554
http://linked.open...ai/riv/idVysledku
  • RIV/61988987:17310/14:A1501AZQ
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • High-gradient stream; Channel-reach morphology; Bankfull geometry; Flysch; Western Carpathians (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [C1A545D6334B]
http://linked.open...i/riv/nazevZdroje
  • CATENA
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 119
http://linked.open...iv/tvurceVysledku
  • Hradecký, Jan
  • Galia, Tomáš
issn
  • 0341-8162
number of pages
http://localhost/t...ganizacniJednotka
  • 17310
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