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Home | Submarine Volcanoes

Plate Tectonic Setting

Map of the Earth's tectonic plates.

Based on a map prepared by the U.S. Geological Survey.

 

Like continental volcanoes, submarine volcanoes are most common where tectonic plates move towards or away from each other. In the case of divergent plate boundaries, where plates are spreading away from each other, the rate of plate movement plays an important role in determining the type of volcano that forms and the rate of eruptive activity. Submarine volcanoes at convergent plate boundaries (subduction zones) are much like their subaerial ("under air" or continental) counterparts except that the weight of the overlying water modifies their eruption style. Hot spots leave linear "tracks" of seamounts across the ocean basins and build some of Earth's largest volcanoes.

 

  • Hot Spot Volcanism
  • Submarine Volcanoes at Convergent Plate Boundaries
  • Submarine Volcanoes at Divergent Plate Boundaries
‹ Submarine Volcanoes up Hot Spot Volcanism ›
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  • Plate Tectonic Setting
    • Hot Spot Volcanism
    • Submarine Volcanoes at Convergent Plate Boundaries
    • Submarine Volcanoes at Divergent Plate Boundaries
  • Submarine Eruptions
  • Features and Deposits
  • Submarine Volcanic Ecosystems
  • For More Information
VW is a higher education, k-12, and public outreach project of the Oregon Space Grant Consortium
administered through the Department of Geosciences at Oregon State University.

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