Blocky Lava Flows is a type of lava flow characterized by a rigid, polygonal crust composed of large, angular fragments that form as a result of highly viscous, slow-moving basaltic to andesitic lava undergoing brittle deformation during cooling and solidification.
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2.2K
Citations
187
Authors
116
Institutions
Publications per year
2017–2026
6
Variants
Block Lava
Parents
Publications
48
Graeme A. Macdonald · American Journal of Science · 1953 · 257 citations
Miocene-Pliocene glaciations in southern Alaska
George H. Denton, R. L. Armstrong · American Journal of Science · 1969 · 107 citations · Full text
1–5 of 48
Authors
187
- RS
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1–5 of 187
Institutions
116
University of Bristol
Bristol, United Kingdom
4 h-index
7 publications
510 citations
Australian National University
Canberra, Australia
3 h-index
4 publications
113 citations
Planetary Science Institute
Tucson, United States
3 h-index
3 publications
127 citations
University of Hawaiʻi at Mānoa
Honolulu, United States
3 h-index
3 publications
178 citations
Centre National de la Recherche Scientifique
Paris, France
3 h-index
4 publications
197 citations
Arizona State University
Tempe, United States
3 h-index
7 publications
458 citations
University of Hawaii System
Honolulu, United States
3 h-index
4 publications
261 citations
Goddard Space Flight Center
Greenbelt, United States
2 h-index
3 publications
189 citations
1–8 of 116
Venues
- Journal of Geophysical Research Atmospheres
JGR · 6 publications · 278 citations
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- Bulletin of Volcanology
4 publications · 114 citations
4
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- American Journal of Science
3 publications · 378 citations
3
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- Journal of the Geological Society
JGS · 3 publications · 57 citations
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- Journal of Volcanology and Geothermal Research
3 publications · 147 citations
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