Channelized Pyroclastic Flows

Channelized Pyroclastic Flows is a type of pyroclastic density current characterized by confinement and directional movement within pre-existing topographic valleys or volcanic channels, distinguishing it from unconfined or radially spreading pyroclastic flows.

33

Publications

2.2K

Citations

97

Authors

59

Institutions

Publications per year

2017–2026

5

Authors

97

  1. RS
    R. S. J. Sparks

    University of Bristol, United Kingdom

    7 publications · 876 citations

    7

    h-index

  2. OR
    Olivier Roche

    Laboratoire Magmas et Volcans, France

    4 publications · 168 citations

    4

    h-index

  3. TH
    T. H. Druitt

    Centre National de la Recherche Scientifique, France

    3 publications · 267 citations

    3

    h-index

  4. JC
    Jeremy C. Phillips

    University of Bristol, United Kingdom

    2 publications · 120 citations

    2

    h-index

  5. TF
    Toshitsugu Fujii

    The University of Tokyo, Japan

    2 publications · 305 citations

    2

    h-index

1–5 of 97

Venues

  1. Journal of Volcanology and Geothermal Research

    8 publications · 473 citations

    8

    h-index

  2. Bulletin of Volcanology

    6 publications · 566 citations

    6

    h-index

  3. Journal of Geophysical Research Solid Earth

    3 publications · 80 citations

    3

    h-index

  4. Geological Society London Memoirs

    2 publications · 257 citations

    2

    h-index

  5. Earth and Planetary Science Letters

    2 publications · 149 citations

    2

    h-index

1–5