Mid-channel Bars

Mid-Channel Bars is a fluvial landform characterized as a longitudinal, elongated deposit of sediment within the river channel, distinguished by its central or near-central position relative to the thalweg and its formation through flow separation and sediment deposition in response to channel width variations or bedform interactions.

36

Publications

1.5K

Citations

108

Authors

64

Institutions

Publications per year

2017–2026

16

Authors

108

  1. JH
    Janet Hooke

    University of Liverpool, United Kingdom

    3 publications · 203 citations

    3

    h-index

  2. GH
    Gregory H. Sambrook Smith

    University of Birmingham, United Kingdom

    2 publications · 191 citations

    2

    h-index

  3. MP
    Manish Pandey

    National Institute of Technology Warangal, India

    2 publications · 28 citations

    2

    h-index

  4. ZW
    Zhaofei Wen

    Chongqing Institute of Green and Intelligent Technology, China

    2 publications · 61 citations

    2

    h-index

  5. JK
    Judith K. Maizels

    University of Aberdeen, United Kingdom

    2 publications · 111 citations

    2

    h-index

1–5 of 108

Venues

  1. Earth Surface Processes and Landforms

    6 publications · 469 citations

    6

    h-index

  2. Geomorphology

    4 publications · 186 citations

    4

    h-index

  3. Journal of Sedimentary Research

    JSR · 3 publications · 105 citations

    3

    h-index

  4. Current Science

    2 publications · 29 citations

    2

    h-index

  5. Water

    2 publications · 31 citations

    2

    h-index

1–5