Physical Weathering

Physical Weathering is a geological process whereby rocks and minerals are broken down into smaller fragments without altering their chemical composition, distinguished from chemical and biological weathering by the absence of chemical transformation and the predominance of mechanical forces such as freeze-thaw cycles, thermal expansion, and abrasion.

170

Publications

9.5K

Citations

529

Authors

278

Institutions

Publications per year

2017–2026

40

Authors

529

  1. SS
    Siegfried Siegesmund

    University of Göttingen, Germany

    4 publications · 626 citations

    4

    h-index

  2. FP
    Francesco Perri

    University of Calabria, Italy

    3 publications · 114 citations

    3

    h-index

  3. IM
    Ian Meiklejohn

    University of Pretoria, South Africa

    3 publications · 75 citations

    3

    h-index

  4. SC
    Salvatore Critelli

    University of Calabria, Italy

    3 publications · 174 citations

    3

    h-index

  5. CS
    C. S. Riebe

    University of Wyoming, United States

    3 publications · 274 citations

    3

    h-index

1–5 of 529

Venues

  1. Earth Surface Processes and Landforms

    8 publications · 408 citations

    8

    h-index

  2. Geomorphology

    5 publications · 247 citations

    5

    h-index

  3. Geophysical Research Letters

    5 publications · 219 citations

    5

    h-index

  4. The Journal of Geology

    JG · 5 publications · 384 citations

    5

    h-index

  5. New Zealand Journal of Geology and Geophysics

    NZJG · 4 publications · 219 citations

    4

    h-index

1–5