Lava Cooling is a geological process in which molten rock undergoes thermal dissipation and solidification upon exposure to the atmosphere or hydrosphere, distinguished by the progressive reduction in temperature and resultant crystallization of volcanic materials at the Earth's surface.
110
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6.8K
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254
Authors
131
Institutions
Publications per year
2017–2026
13
Parents
Publications
110
R. W. Griffiths · Annual Review of Fluid Mechanics · 2000 · 391 citations
Emplacement and cooling of komatiite lavas
Herbert E. Huppert, R. S. J. Sparks, J. S. Turner et al. · Nature · 1984 · 262 citations
Komatiites I: Eruption and Flow
HE Huppert, R. S. J. Sparks · Journal of Petrology · 1985 · 242 citations
1–5 of 110
Authors
254
- AH
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- AG
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- LK
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1–5 of 254
Institutions
131
Lancaster University
Lancaster, United Kingdom
10 h-index
13 publications
356 citations
Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
8 h-index
18 publications
769 citations
University of Alaska Fairbanks
Fairbanks, United States
5 h-index
9 publications
414 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
5 h-index
5 publications
193 citations
University of Turin
Turin, Italy
5 h-index
9 publications
779 citations
The Open University
Milton Keynes, United Kingdom
4 h-index
13 publications
362 citations
United States Geological Survey
Reston, United States
4 h-index
4 publications
188 citations
University of Hawaii System
Honolulu, United States
4 h-index
9 publications
313 citations
1–8 of 131
Venues
- Journal of Geophysical Research Atmospheres
JGR · 26 publications · 2K citations
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- Journal of Volcanology and Geothermal Research
14 publications · 714 citations
13
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- Geophysical Research Letters
11 publications · 380 citations
11
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- Bulletin of Volcanology
10 publications · 614 citations
10
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- Journal of Petrology
5 publications · 693 citations
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