Alluvial Fans

Alluvial Fan is a sedimentary landform composed of unconsolidated clastic material deposited by gravity-driven, distributive fluvial processes radiating from a confined source point, typically at a mountain front, distinguished from other fluvial depositional systems by its characteristic conical topography and proximal-to-distal grain size diminution.

814

Publications

44.2K

Citations

2K

Authors

774

Institutions

Publications per year

2017–2026

119

Authors

2K

  1. AH
    Adrian Harvey

    University of Liverpool, United Kingdom

    14 publications · 1.2K citations

    13

    h-index

  2. LA
    Lewis A. Owen

    University of Cincinnati, United States

    12 publications · 647 citations

    11

    h-index

  3. AE
    Anne E. Mather

    University of Plymouth, United Kingdom

    7 publications · 481 citations

    7

    h-index

  4. RC
    Robert C. Finkel

    Lawrence Livermore National Laboratory, United States

    7 publications · 442 citations

    7

    h-index

  5. DB
    Didier Bourlès

    Centre National de la Recherche Scientifique, France

    6 publications · 423 citations

    6

    h-index

1–5 of 2K

Venues

  1. Geomorphology

    56 publications · 3.1K citations

    35

    h-index

  2. Sedimentary Geology

    42 publications · 2K citations

    27

    h-index

  3. Journal of Sedimentary Research

    JSR · 30 publications · 3.3K citations

    24

    h-index

  4. Earth Surface Processes and Landforms

    25 publications · 1.8K citations

    22

    h-index

  5. Geological Society London Special Publications

    30 publications · 1.3K citations

    21

    h-index

1–5