Gully Headcut Migration

Gully Headcut Migration is a geomorphological process in which the upstream advance of a vertical or steeply sloping erosion front at the head of a gully occurs due to hydraulic undercutting and mass failure, distinguishing it from other forms of channel erosion by its localized, stepwise progression driven by detachment and collapse at the headcut face.

35

Publications

2.2K

Citations

141

Authors

72

Institutions

Publications per year

2017–2026

14

Authors

141

  1. JP
    Jean Poesen

    KU Leuven, Belgium

    5 publications · 814 citations

    5

    h-index

  2. SJ
    Sean J. Bennett

    University at Buffalo, State University of New York, United States

    5 publications · 241 citations

    5

    h-index

  3. MG
    Mingming Guo

    Chinese Academy of Sciences, China

    4 publications · 155 citations

    4

    h-index

  4. NK
    Narges Kariminejad

    Shiraz University, Iran

    4 publications · 195 citations

    4

    h-index

  5. HR
    Hamid Reza Pourghasemi

    Shiraz University, Iran

    4 publications · 195 citations

    4

    h-index

1–5 of 141

Venues

  1. Geomorphology

    6 publications · 475 citations

    6

    h-index

  2. CATENA

    6 publications · 400 citations

    6

    h-index

  3. Earth Surface Processes and Landforms

    5 publications · 319 citations

    5

    h-index

  4. Land Degradation and Development

    4 publications · 220 citations

    4

    h-index

  5. Water Resources Research

    2 publications · 95 citations

    2

    h-index

1–5