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

Authors

734

  1. DJ
    Daniel J. Fornari

    Woods Hole Oceanographic Institution, United States

    20 publications · 1K citations

    17

    h-index

  2. DA
    David A. Clague

    Monterey Bay Aquarium Research Institute, United States

    10 publications · 684 citations

    10

    h-index

  3. RW
    R. W. Embley

    NOAA Pacific Marine Environmental Laboratory, United States

    10 publications · 599 citations

    10

    h-index

  4. WW
    William W. Chadwick

    Oregon State University, United States

    10 publications · 615 citations

    10

    h-index

  5. JG
    James G. Moore

    United States Geological Survey, United States

    9 publications · 967 citations

    9

    h-index

1–5 of 734

Venues

  1. Geochemistry Geophysics Geosystems

    33 publications · 1.8K citations

    26

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 25 publications · 1.9K citations

    22

    h-index

  3. Bulletin of Volcanology

    22 publications · 1.2K citations

    20

    h-index

  4. Journal of Volcanology and Geothermal Research

    17 publications · 650 citations

    16

    h-index

  5. Earth and Planetary Science Letters

    15 publications · 1K citations

    15

    h-index

1–5