Lava Flow Cooling is a geophysical process representing the gradual thermal dissipation and solidification of molten rock as it extrudes onto the Earth's surface, distinguished by the conductive and convective heat transfer mechanisms that govern the transformation of active lava into solidified crust within the context of volcanic effusion dynamics.
91
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120
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2017–2026
11
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Publications
91
Komatiites I: Eruption and Flow
HE Huppert, R. S. J. Sparks · Journal of Petrology · 1985 · 242 citations
1–5 of 91
Authors
227
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120
Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
6 h-index
12 publications
675 citations
University of Alaska Fairbanks
Fairbanks, United States
5 h-index
9 publications
414 citations
University of Hawaii System
Honolulu, United States
4 h-index
9 publications
462 citations
United States Geological Survey
Reston, United States
4 h-index
4 publications
170 citations
Centre National de la Recherche Scientifique
Paris, France
4 h-index
8 publications
220 citations
Universidad Nacional Autónoma de México
Mexico City, Mexico
4 h-index
16 publications
308 citations
Alaska Volcano Observatory
Fairbanks, United States
4 h-index
8 publications
389 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
4 h-index
6 publications
290 citations
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- Journal of Geophysical Research Atmospheres
JGR · 25 publications · 2.1K citations
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- Journal of Volcanology and Geothermal Research
8 publications · 511 citations
8
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- Geophysical Research Letters
7 publications · 314 citations
7
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- Bulletin of Volcanology
5 publications · 412 citations
5
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- American Journal of Science
4 publications · 284 citations
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