Aa Lava Flows is a type of basaltic lava flow characterized by a rough, clinkery surface texture formed by the brittle fracturing of the cooling lava crust during slow, non-uniform movement, distinguishing it from the smooth, ropy surface of pahoehoe lava flows.
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2.9K
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92
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54
Institutions
Publications per year
2017–2026
0
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Publications
43
1–5 of 43
Authors
92
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1–5 of 92
Institutions
54
University of Hawaii System
Honolulu, United States
3 h-index
5 publications
1K citations
Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
3 h-index
3 publications
133 citations
United States Geological Survey
Reston, United States
3 h-index
6 publications
537 citations
Arizona State University
Tempe, United States
2 h-index
3 publications
64 citations
Ghent University
Ghent, Belgium
2 h-index
6 publications
142 citations
Royal Observatory
Edinburgh, United Kingdom
2 h-index
2 publications
104 citations
Lancaster University
Lancaster, United Kingdom
2 h-index
6 publications
150 citations
University of Buea
Buea, Cameroon
2 h-index
5 publications
113 citations
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Venues
- Journal of Volcanology and Geothermal Research
6 publications · 503 citations
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- Journal of Geophysical Research Atmospheres
JGR · 6 publications · 584 citations
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- Bulletin of Volcanology
5 publications · 625 citations
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- American Journal of Science
4 publications · 384 citations
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- Geophysical Research Letters
3 publications · 99 citations
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