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
Parents
928
A vesicularity index for pyroclastic deposits
B. F. Houghton, Colin Wilson · Bulletin of Volcanology · 1989 · 583 citations
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735

Centre National de la Recherche Scientifique
Paris, France
42 h-index
189 publications
12.4K citations
Laboratoire Magmas et Volcans
Clermont-Ferrand, France
35 h-index
90 publications
6.7K citations

University of Bristol
Bristol, United Kingdom
34 h-index
109 publications
9.5K citations

Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
32 h-index
157 publications
8.5K citations
United States Geological Survey
Reston, United States
30 h-index
81 publications
5.3K citations
Institut de Recherche pour le Développement
Marseille, France
30 h-index
77 publications
3.9K citations

Université Clermont Auvergne
Clermont-Ferrand, France
27 h-index
70 publications
5.6K citations
Cascades Volcano Observatory
Vancouver, United States
22 h-index
34 publications
2.1K citations
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JGR · 81 publications · 7.6K citations
52
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121 publications · 7.3K citations
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85 publications · 6.1K citations
44
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32 publications · 1.8K citations
24
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25 publications · 905 citations
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