Morfologie říčního koryta Křížového potoka ve východních Krkonoších

This master thesis deals with the morphology of mountain river channels - with structures, patterns and shapes resulting from fluvial processes. The findings are documented on the Křížový potok river channel in the Eastern Krkonoše mountains. There are several specifics which influence the evolution...

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Bibliographic Details
Main Author: Dvořáková, Magdalena
Other Authors: Kliment, Zdeněk
Format: Dissertation
Language:Czech
Published: 2010
Online Access:http://www.nusl.cz/ntk/nusl-286306
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spelling ndltd-nusl.cz-oai-invenio.nusl.cz-2863062017-06-27T04:41:11Z Morfologie říčního koryta Křížového potoka ve východních Krkonoších Morphology of the Křížový potok river channel in the Eastern Krkonoše Mountains Kliment, Zdeněk Dvořáková, Magdalena Engel, Zbyněk This master thesis deals with the morphology of mountain river channels - with structures, patterns and shapes resulting from fluvial processes. The findings are documented on the Křížový potok river channel in the Eastern Krkonoše mountains. There are several specifics which influence the evolution of mountain river channels. The first one is high elevation change and big slope of the river, which determinate the formation of typical structures, such as waterfalls, cascades and steps, often related with pools. Plane bed, riffle-pool and dune-ripple also represent typical structures of mountain river channels. Specific microstructures are represented by potholes. River channels in forested mountain basins are affected by logs and wood debris, which create local barriers where fine-grained material accumulates. In the Křížový potok river channel, a high diversity of the channel structures can be seen. The most common structures are step-pools and cascades. The stream is influenced by large accumulation of delluvial sediments and wood debris which create obstacles to the flow. 2010 info:eu-repo/semantics/masterThesis http://www.nusl.cz/ntk/nusl-286306 cze info:eu-repo/semantics/restrictedAccess
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language Czech
format Dissertation
sources NDLTD
description This master thesis deals with the morphology of mountain river channels - with structures, patterns and shapes resulting from fluvial processes. The findings are documented on the Křížový potok river channel in the Eastern Krkonoše mountains. There are several specifics which influence the evolution of mountain river channels. The first one is high elevation change and big slope of the river, which determinate the formation of typical structures, such as waterfalls, cascades and steps, often related with pools. Plane bed, riffle-pool and dune-ripple also represent typical structures of mountain river channels. Specific microstructures are represented by potholes. River channels in forested mountain basins are affected by logs and wood debris, which create local barriers where fine-grained material accumulates. In the Křížový potok river channel, a high diversity of the channel structures can be seen. The most common structures are step-pools and cascades. The stream is influenced by large accumulation of delluvial sediments and wood debris which create obstacles to the flow.
author2 Kliment, Zdeněk
author_facet Kliment, Zdeněk
Dvořáková, Magdalena
author Dvořáková, Magdalena
spellingShingle Dvořáková, Magdalena
Morfologie říčního koryta Křížového potoka ve východních Krkonoších
author_sort Dvořáková, Magdalena
title Morfologie říčního koryta Křížového potoka ve východních Krkonoších
title_short Morfologie říčního koryta Křížového potoka ve východních Krkonoších
title_full Morfologie říčního koryta Křížového potoka ve východních Krkonoších
title_fullStr Morfologie říčního koryta Křížového potoka ve východních Krkonoších
title_full_unstemmed Morfologie říčního koryta Křížového potoka ve východních Krkonoších
title_sort morfologie říčního koryta křížového potoka ve východních krkonoších
publishDate 2010
url http://www.nusl.cz/ntk/nusl-286306
work_keys_str_mv AT dvorakovamagdalena morfologiericnihokorytakrizovehopotokavevychodnichkrkonosich
AT dvorakovamagdalena morphologyofthekrizovypotokriverchannelintheeasternkrkonosemountains
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