We study processes that form and modify volcanoes in the sea |
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Volcanic eruptions and flank collapses are significant geologic hazards. Our goal is to better understand these and other volcanic processes in the deep sea environment. Through this research we hope to gain insight into potentially destructive eruptions on land or in shallow water. We are studying:
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Our research is highlighted in these web pages, presented through abstracts of our publications
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Hot spots: Hawaiian Islands and Loihi Seamount |
To study these processes, our research takes us to places such as Hawaii, the Gorda Ridge, and the seamounts off California. These places are characterized by different types of volcanism: hot spots, mid-ocean ridges, and intraplate seamounts. We also work off the West Coast studying geologic processes unrelated to volcanoes.
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Our most recent papers are listed at the top of the Publication List page. Our publications | Collaborators' pubs | News and videos
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Related MBARI YouTube videos:
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| High-tech robots reveal details of the deep | "Snow-blower" hydrothermal vents | Davidson Seamount | Hawaii highlights |
Submarine Volcanism project team
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Current projects
- The Submarine Volcanism project (this site; see also Marine Geology Research at MBARI)
- Endeavour Segment Integrated Study Site, and Fine-scale Crustal Accretion Processes (see MBARI benthic projects for descriptions)
- Seafloor Mapping AUV project
Why is this research important?
Submarine volcanoes may impact us, even though they are underwater. How?
Submarine eruptions are poorly understood.
Why?
There are many advantages to studying samples erupted under water.
What are they?
Here is an interview with Dr. Clague
What is it like to explore the deep sea?
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Latest cruise logs: Gulf of California, Leg 7 |
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How do we explore the deep sea? Here is information about the equipment we use.
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| Hot spots | Mid-ocean ridges | Seamounts | Margin |
| Publication list | Cruise logs | FAQ, resources | Site map |
Questions? Comments? Please contact Jenny Paduan


















