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https://doi.org/10.5194/egusphere-2025-2010
https://doi.org/10.5194/egusphere-2025-2010
15 May 2025
 | 15 May 2025
Status: this preprint is open for discussion and under review for Natural Hazards and Earth System Sciences (NHESS).

Brief communication: A magma depletion alternative for vent distribution in volcanic fields

Mark S. Bebbington, Melody G. Whitehead, and Gabor Kereszturi

Abstract. The location of a volcanic vent controls an eruption's hazards, intensities, and impact. Current kernel density estimation methods of future vent locations in volcanic fields assume that locations with more past-vents are more likely to produce future-vents. We examine an alternative hypothesis that an eruption depletes the magma source, causing holes or dips in the spatial density estimate for future vent locations. This is illustrated with the Auckland Volcanic Field, Aotearoa-New Zealand, where both magmatic and phreatomagmatic eruptions have occurred, according to the vent location, with the latter resulting in more explosive eruptions and hence hazard.

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Mark S. Bebbington, Melody G. Whitehead, and Gabor Kereszturi

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Mark S. Bebbington, Melody G. Whitehead, and Gabor Kereszturi
Mark S. Bebbington, Melody G. Whitehead, and Gabor Kereszturi

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Short summary
In volcanic fields, the location of an eruptive vent controls the hazards, their intensities, and ultimately the impact of the eruption. Estimates of where future eruptions are likely to occur inform evacuation plans, the (re)location of vital infrastructure, and the placement of early-warning monitoring equipment. Current estimates assume that locations with more past-vents are more likely to produce future-vents. We provide the formulae for an alternative hypothesis of magma depletion.
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