DescriptionWithout 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|
|Event title||AGU Fall Conference 2010|
|Location||San Francisco, United States|
|Degree of Recognition||International|