Flow Slides

Flow Slide is a type of slope failure mechanism characterized by the rapid, fluid-like deformation and downslope movement of saturated, fine-grained soils or weak rock masses, distinguished from other slope failures by its low resistance to shear stress and continuous, viscous flow behavior.

63

Publications

3.1K

Citations

165

Authors

72

Institutions

Publications per year

2017–2026

18

Authors

165

  1. YH
    Yu Huang

    Tongji University, China

    5 publications · 148 citations

    5

    h-index

  2. OH
    Oldrich Hungr

    University of British Columbia, Canada

    3 publications · 157 citations

    3

    h-index

  3. GB
    Giuseppe Buscarnera

    Northwestern University, United States

    3 publications · 143 citations

    3

    h-index

  4. XW
    Xiaobo Wang

    Albert Einstein College of Medicine, United States

    2 publications · 34 citations

    2

    h-index

  5. ZD
    Zili Dai

    Tongji University, China

    2 publications · 58 citations

    2

    h-index

1–5 of 165

Venues

  1. Canadian Geotechnical Journal

    13 publications · 719 citations

    13

    h-index

  2. Landslides

    4 publications · 355 citations

    4

    h-index

  3. Engineering Geology

    4 publications · 114 citations

    4

    h-index

  4. Journal of Marine Science and Engineering

    3 publications · 46 citations

    3

    h-index

  5. Environmental Earth Sciences

    2 publications · 128 citations

    2

    h-index

1–5