Talus Formation

Talus Formation is a geomorphological process characterized by the accumulation of rock debris at the base of cliffs or slopes, resulting from the weathering and gravitational displacement of rock fragments.

99

Publications

3.7K

Citations

218

Authors

134

Institutions

Publications per year

2017–2026

9

Authors

218

  1. CK
    Colin K. Ballantyne

    University of St Andrews, United Kingdom

    6 publications · 194 citations

    6

    h-index

  2. LS
    Lennart Strömquist

    Uppsala University, Sweden

    5 publications · 141 citations

    4

    h-index

  3. HT
    H. T. U. Smith

    University of Stirling, United Kingdom

    3 publications · 54 citations

    3

    h-index

  4. AK
    Adam Kotarba

    Institute of Geography and Spatial Organization, Polish Academy of Sciences, Poland

    3 publications · 119 citations

    3

    h-index

  5. FA
    Francis A. Macdonald

    Planetary Science Institute, United States

    2 publications · 64 citations

    2

    h-index

1–5 of 218

Venues

  1. Geomorphology

    10 publications · 391 citations

    10

    h-index

  2. 8

    h-index

  3. Permafrost and Periglacial Processes

    5 publications · 246 citations

    5

    h-index

  4. Earth Surface Processes and Landforms

    5 publications · 121 citations

    5

    h-index

  5. Arctic and Alpine Research

    4 publications · 143 citations

    4

    h-index

1–5