Debris Flows

Debris Flow is a type of rapid mass wasting characterized by a saturated, heterogeneous mixture of water, rock fragments, soil, and organic material that moves downslope under gravity as a cohesive, viscous fluid, distinguished from other slope failures by its high density, mobility, and ability to transport large solid particles en masse.

2.7K

Publications

170.4K

Citations

5.9K

Authors

1.6K

Institutions

Publications per year

2017–2026

823

Authors

5.9K

  1. BW
    Brian W. McArdell

    Swiss Federal Institute for Forest, Snow and Landscape Research, Switzerland

    42 publications · 3.8K citations

    33

    h-index

  2. JW
    Jason W. Kean

    United States Geological Survey, United States

    38 publications · 3.9K citations

    31

    h-index

  3. PC
    Peng Cui

    Chinese Academy of Sciences, China

    48 publications · 2.6K citations

    28

    h-index

  4. MS
    Markus Stoffel

    University of Geneva, Switzerland

    37 publications · 3.6K citations

    27

    h-index

  5. RM
    Richard M. Iverson

    United States Geological Survey, United States

    32 publications · 9K citations

    26

    h-index

1–5 of 5.9K

Venues

  1. Geomorphology

    121 publications · 10.8K citations

    63

    h-index

  2. Engineering Geology

    100 publications · 8.5K citations

    54

    h-index

  3. Natural hazards and earth system sciences

    122 publications · 8.9K citations

    54

    h-index

  4. Landslides

    127 publications · 9.3K citations

    48

    h-index

  5. Earth Surface Processes and Landforms

    88 publications · 6.4K citations

    46

    h-index

1–5