Submarine Lava Flows
Submarine Lava Flows is a geological phenomenon characterized by the extrusion and movement of molten rock onto the ocean floor, distinguished from subaerial lava flows by its formation under high-pressure aqueous conditions that influence cooling rates, morphology, and emplacement dynamics.
245
Publications
14.8K
Citations
734
Authors
318
Institutions
Publications per year
2017–2026
28
Parents
245
A POSSIBLE ORIGIN OF THE HAWAIIAN ISLANDS
J. Tuzo Wilson · Canadian Journal of Physics · 1963 · 1.2K citations
Petrology of deep sea basalt near Hawaii
James G. Moore · American Journal of Science · 1965 · 282 citations · Full text
1–5 of 245
734
17
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Monterey Bay Aquarium Research Institute, United States
10 publications · 684 citations
10
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NOAA Pacific Marine Environmental Laboratory, United States
10 publications · 599 citations
10
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10
h-index
9
h-index
1–5 of 734
318
United States Geological Survey
Reston, United States
24 h-index
49 publications
4.1K citations

University of Hawaii System
Honolulu, United States
22 h-index
36 publications
2.9K citations
Woods Hole Oceanographic Institution
Falmouth, United States
18 h-index
46 publications
3.1K citations
Oregon State University
Corvallis, United States
15 h-index
27 publications
1.8K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
61 publications
1.4K citations

University of Hawaiʻi at Mānoa
Honolulu, United States
11 h-index
22 publications
1.3K citations
NOAA Pacific Marine Environmental Laboratory
Seattle, United States
9 h-index
17 publications
647 citations
Hawaiian Volcano Observatory
Ocean View, United States
9 h-index
12 publications
1.2K citations
1–8 of 318
33 publications · 1.8K citations
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JGR · 25 publications · 1.9K citations
22
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22 publications · 1.2K citations
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17 publications · 650 citations
16
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15 publications · 1K citations
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