Channel Avulsion

Channel avulsion is a fluvial geomorphology process wherein a river or stream abruptly abandons its established channel in favor of a new course, typically due to sediment aggradation reaching a threshold that destabilizes flow continuity.

109

Publications

9.2K

Citations

293

Authors

165

Institutions

Publications per year

2017–2026

29

Authors

293

  1. RS
    Rudy Slingerland

    Pennsylvania State University, United States

    5 publications · 1.1K citations

    5

    h-index

  2. ND
    Norman D. Smith

    University of Nebraska–Lincoln, United States

    5 publications · 1.1K citations

    5

    h-index

  3. DA
    Douglas A. Edmonds

    Indiana University Bloomington, United States

    5 publications · 211 citations

    5

    h-index

  4. MG
    Maarten G. Kleinhans

    Utrecht University, Netherlands

    4 publications · 612 citations

    4

    h-index

  5. CP
    Chris Paola

    University of Minnesota, United States

    4 publications · 714 citations

    4

    h-index

1–5 of 293

Venues

  1. Journal of Sedimentary Research

    JSR · 12 publications · 1.1K citations

    12

    h-index

  2. Earth Surface Processes and Landforms

    10 publications · 1.3K citations

    10

    h-index

  3. Sedimentology

    8 publications · 1.2K citations

    8

    h-index

  4. Geology

    8 publications · 901 citations

    8

    h-index

  5. Geomorphology

    6 publications · 580 citations

    6

    h-index

1–5