Pyroclastic Flows

Pyroclastic Flows is a highly mobile, ground-hugging suspension of volcanic particles and hot gases that results from explosive volcanic eruptions and is distinguished from other volcanic mass movements by its high temperature, turbulence, and rapid, destructive flow dynamics.

928

Publications

55K

Citations

2.2K

Authors

735

Institutions

Publications per year

2017–2026

131

Authors

2.2K

  1. RS
    R. S. J. Sparks

    University of Bristol, United Kingdom

    39 publications · 4.9K citations

    34

    h-index

  2. ES
    Eliza S. Calder

    University of Edinburgh, United Kingdom

    20 publications · 2K citations

    19

    h-index

  3. TH
    T. H. Druitt

    Centre National de la Recherche Scientifique, France

    21 publications · 2.1K citations

    19

    h-index

  4. OR
    Olivier Roche

    Laboratoire Magmas et Volcans, France

    24 publications · 1.2K citations

    19

    h-index

  5. PD
    Pierfrancesco Dellino

    University of Bari Aldo Moro, Italy

    15 publications · 879 citations

    14

    h-index

1–5 of 2.2K

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 81 publications · 7.6K citations

    52

    h-index

  2. Journal of Volcanology and Geothermal Research

    121 publications · 7.3K citations

    51

    h-index

  3. Bulletin of Volcanology

    85 publications · 6.1K citations

    44

    h-index

  4. Geophysical Research Letters

    32 publications · 1.8K citations

    24

    h-index

  5. Canadian Journal of Earth Sciences

    25 publications · 905 citations

    18

    h-index

1–5