Karst Denudation

Karst Denudation is a geomorphic process, distinguished from other denudational phenomena by its reliance on the chemical dissolution of soluble rocks—particularly limestone, dolomite, and gypsum—through karstification, leading to the progressive lowering and shaping of land surfaces in karst terrains.

29

Publications

985

Citations

71

Authors

43

Institutions

Publications per year

2017–2026

2

Authors

71

  1. FG
    Franci Gabrovšek

    Karst Research Institute, Slovenia

    2 publications · 69 citations

    2

    h-index

  2. WB
    William B. White

    Pennsylvania State University, United States

    2 publications · 41 citations

    2

    h-index

  3. US
    Uroš Stepišnik

    University of Ljubljana, Slovenia

    2 publications · 68 citations

    2

    h-index

  4. LM
    Ludovic Mocochain

    Centre de Recherche et d’Enseignement de Géosciences de l’Environnement, France

    1 publications · 44 citations

    1

    h-index

  5. VV
    Veerle Vandeginste

    KU Leuven, Belgium

    1 publications · 25 citations

    1

    h-index

1–5 of 71

Venues

  1. Acta Carsologica

    3 publications · 52 citations

    3

    h-index

  2. Earth Surface Processes and Landforms

    3 publications · 151 citations

    3

    h-index

  3. Geomorphology

    3 publications · 139 citations

    3

    h-index

  4. Sedimentary Geology

    2 publications · 69 citations

    2

    h-index

  5. Australian Geographer

    1 publications · 16 citations

    1

    h-index

1–5