Description
Without warning, a new eruption of Volcano 0403-091 (30 km NW of Vava’u, northern Tonga) occurred on the 7th August 2019 producing a >200 km2 pumice raft. Pumice raft formation and evolution is poorly understood, yet rafts pose a range of potential hazards for marine traffic and infrastructure. The 7th August raft was imaged by satellites almost daily, so its source and path are well-constrained. This eruption therefore provides a unique opportunity to sample both rafted pumice with known float times and sunken pumice at the vent, as well as a rare chance to study vent structure, hydrothermal activity and marine life interactions immediately following an explosive, shallow eruption. Here we present the first results from a rapid response survey of the submarine vent site, conducted 6 months post eruption. We discuss the textural and geochemical charcateristics of the samples collected at the vent and compare them with floating pumice collected by a boat that intersected the raft (floated for 1 week), and from the shores of two Fijian Islands (floated for > 1 month). Physical, geochemical and textural (including high resolution X-ray computed tomography) analyses of these different pumice types from a single well-constrained eruption help to determine the controls on pumice raft formation and their potential hazards for marine shipping and infrastructure.Period | 16 Dec 2020 |
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Event title | American Geophysical Union Fall Meeting 2010 |
Event type | Conference |
Location | San Francisco, United StatesShow on map |
Degree of Recognition | International |
Related content
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Activities
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NERC Urgent Grant
Activity: Other activity types › Other
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Research output
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The 2019–2020 volcanic eruption of Late’iki (Metis Shoal), Tonga
Research output: Contribution to journal › Article › peer-review