Současné trendy v zrnitostním složení sedimentů štěrkových lavic toků Moravskoslezských Beskyd – příkladová studie Sihelský potok

Jan Hradecký, Martin Děd

Abstrakt

Changes in sediment delivery to mountain stream channels are a typical feature of present-day geomorphological evolution of channel morphology. There is a high level of transport of coarse-grained sediments typical for Carpathian region built by flysch rocks. Evaluation of the effect of man-induced changes in the study area is focused on the quantification of this phenomenon through the use of automated sizing of coarse-grained sediments. Tendency in the composition of gravel bars is studied along the longitudinal profile and with regard to adjacent landforms.

Bibliografická citace

Hradecký, J., & Děd, M. (2016). Současné trendy v zrnitostním složení sedimentů štěrkových lavic toků Moravskoslezských Beskyd – příkladová studie Sihelský potok. Geologické výzkumy na Moravě a ve Slezsku, 15. Získáno z https://journals.muni.cz/gvms/article/view/4802

Klíčová slova

Silesian Unit; Moravskoslezské Beskydy Mts.; Sihelský potok Brook; automated particle-size analyses; gravel bars

Plný Text:

Reference

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