Conditions to Preserve the Sedimentary Record of Channel Planforms in Temperate Rivers of the Northern Hemisphere

Author:

Słowik Marcin1ORCID,Dezső József2,Kovács János34ORCID,Gałka Mariusz5,Sipos György6

Affiliation:

1. Adam Mickiewicz University Institute of Geology Geohazards Research Unit Poznań Poland

2. Department of Environmental and Physical Geography University of Pécs Institute of Geography and Earth Sciences Pécs Hungary

3. Department of Geology and Meteorology University of Pécs Pécs Hungary

4. University of Pécs Szentágothai Research Centre Environmental Analytical and Geoanalytical Research Group Pécs Hungary

5. Department of Biogeography, Paleoecology and Nature Conservation University of Lodz Faculty of Biology and Environmental Protection Lodz Poland

6. Department of Geoinformatics, Physical and Environmental Geography University of Szeged Szeged Hungary

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference94 articles.

1. Guide for selecting Manning’s roughness coefficients for natural channels and floodplains;Acrement G. J.;US Geological Survey Water‐Supply Paper,1989

2. Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar

3. Electrical resistivity imaging of anastomosing river subsurface stratigraphy and possible controls of fluvial style change in a graben-like basin, Czech Republic

4. An approach to the sediment transport problem from general physics;Bagnold R. A.,1966

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