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Sedimentary texture of crevasse splays formed by present-day and palaeofloods against the background of floodplain geomorphology and lithofacies exposed in channel cut banks (in the Vistula River valley between Warsaw and Płock, Poland)

Grzegorz Wierzbicki

Grzegorz Wierzbicki

Department of Water Engineering and Applied Geology, Institute of Environmental Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life SciencesWarsaw, Poland
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Wierzbicki, Grzegorz
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Marcin Górka

Marcin Górka

Department of Sedimentary Basins, Faculty of Geology, University of WarsawWarsaw, Poland
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Górka, Marcin
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Piotr Ostrowski

Piotr Ostrowski

Department of Water Engineering and Applied Geology, Institute of Environmental Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life SciencesWarsaw, Poland
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Ostrowski, Piotr
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Agnieszka Kałmykow-Piwińska

Agnieszka Kałmykow-Piwińska

Department of Environmental Protection and Natural Resources, Faculty of Geology, University of WarsawWarsaw, Poland
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Kałmykow-Piwińska, Agnieszka
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Tomasz Falkowski

Tomasz Falkowski

Department of Water Engineering and Applied Geology, Institute of Environmental Engineering, Faculty of Civil and Environmental Engineering, Warsaw University of Life SciencesWarsaw, Poland
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Falkowski, Tomasz
  
31. Okt. 2023
Sedimentary texture of crevasse splays formed by present-day and palaeofloods against the background of floodplain geomorphology and lithofacies exposed in channel cut banks (in the Vistula River valley between Warsaw and Płock, Poland)'s Cover Image
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Online veröffentlicht: 31. Okt. 2023
Seitenbereich: 180 - 196
Eingereicht: 29. Sept. 2023
Akzeptiert: 31. Okt. 2023
DOI: https://doi.org/10.2478/mgrsd-2023-0030
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© 2023 Grzegorz Wierzbicki et al., published by Sciendo
This work is licensed under the Creative Commons Attribution 4.0 International License.

Figure 1.

Model of floodplain geomorphology (type of meandering river), including distribution of particular lithofacies (see supplemental information for description of abbreviations)Source: own study based on Bridge 2003, Ostrowski et al. 2021 and Szmańda 2011
Model of floodplain geomorphology (type of meandering river), including distribution of particular lithofacies (see supplemental information for description of abbreviations)Source: own study based on Bridge 2003, Ostrowski et al. 2021 and Szmańda 2011

Figure 2.

Geomorphological map of the study area and locator map with simplified landscape typology of Poland based on Kondracki & Richling 1994Source of the main map: own study adopted from Wierzbicki, Ostrowski & Falkowski 2020 and modified
Geomorphological map of the study area and locator map with simplified landscape typology of Poland based on Kondracki & Richling 1994Source of the main map: own study adopted from Wierzbicki, Ostrowski & Falkowski 2020 and modified

Figure 3.

Aerial orthophotomap taken shortly after levee breachSource of the image: KZGW by courtesy of Łukasz Sławik (MGGP Aero); see Wierzbicki et al. 2013
Aerial orthophotomap taken shortly after levee breachSource of the image: KZGW by courtesy of Łukasz Sławik (MGGP Aero); see Wierzbicki et al. 2013

Figure 4.

Particle size distribution graph of deposits taken from the study areaSource: own study
Particle size distribution graph of deposits taken from the study areaSource: own study

Figure 5.

Grain size statistical parameters (Folk & Ward 1957) of deposits taken from the study areaSource: own study
Grain size statistical parameters (Folk & Ward 1957) of deposits taken from the study areaSource: own study

Figure 6.

Sections No. 1 and No. 15. See supplemental informationSource: own study
Sections No. 1 and No. 15. See supplemental informationSource: own study
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