Vertical Accretion

Vertical Accretion is the process of sediment deposition that occurs incrementally upward on a floodplain surface during overbank flow events, distinguishing it from lateral accretion by involving vertical build-up of alluvial material perpendicular to the flow direction rather than lateral migration of channel-derived deposits.

181

Publications

14.2K

Citations

501

Authors

230

Institutions

Publications per year

2017–2026

51

Authors

501

  1. ML
    Matthew L. Kirwan

    William & Mary, United States

    8 publications · 1.1K citations

    8

    h-index

  2. DR
    Donald R. Cahoon

    United States Geological Survey, United States

    7 publications · 1.1K citations

    7

    h-index

  3. JW
    John W. Day

    Louisiana State University, United States

    6 publications · 528 citations

    6

    h-index

  4. AD
    Andrea D’Alpaos

    University of Padua, Italy

    5 publications · 113 citations

    5

    h-index

  5. WH
    W. H. Patrick

    Louisiana State University, United States

    5 publications · 544 citations

    5

    h-index

1–5 of 501

Venues

  1. Earth Surface Processes and Landforms

    11 publications · 717 citations

    11

    h-index

  2. Journal of Coastal Research

    JCR · 10 publications · 697 citations

    10

    h-index

  3. Estuarine Coastal and Shelf Science

    10 publications · 1.2K citations

    10

    h-index

  4. Journal of Sedimentary Research

    JSR · 7 publications · 732 citations

    7

    h-index

  5. Limnology and Oceanography

    7 publications · 1K citations

    7

    h-index

1–5