Scree Slopes

Scree Slopes is a geomorphological landform characterized by an accumulation of loose, coarse rock fragments at the base of cliffs or steep rocky slopes, differentiated from other colluvial deposits by its origin through physical weathering and its typically unstable, conical profile shaped by gravity-driven particle movement.

99

Publications

4.5K

Citations

274

Authors

151

Institutions

Publications per year

2017–2026

12

Variants

Talus

Authors

274

  1. MZ
    Miloslav Zacharda

    Institute of Entomology, Czechia

    5 publications · 194 citations

    5

    h-index

  2. MR
    Michal Rendoš

    University of Pavol Jozef Šafárik, Slovakia

    5 publications · 117 citations

    5

    h-index

  3. AM
    Andrej Mock

    University of Pavol Jozef Šafárik, Slovakia

    5 publications · 117 citations

    5

    h-index

  4. BH
    Bernard Hétu

    Université du Québec à Rimouski, Canada

    4 publications · 297 citations

    4

    h-index

  5. VR
    Vlastimil Růžička

    University of Chemistry and Technology, Prague, Czechia

    3 publications · 112 citations

    3

    h-index

1–5 of 274

Venues

  1. Permafrost and Periglacial Processes

    6 publications · 800 citations

    6

    h-index

  2. Journal of Ecology

    4 publications · 82 citations

    4

    h-index

  3. Natural hazards and earth system sciences

    3 publications · 144 citations

    3

    h-index

  4. Geomorphology

    3 publications · 159 citations

    3

    h-index

  5. Earth Surface Processes and Landforms

    3 publications · 87 citations

    3

    h-index

1–5