Articles | Volume 25, issue 9
https://doi.org/10.5194/nhess-25-3455-2025
https://doi.org/10.5194/nhess-25-3455-2025
Brief communication
 | 
16 Sep 2025
Brief communication |  | 16 Sep 2025

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

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

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Cited articles

Bebbington, M. S.: Incorporating the eruptive history in a stochastic model for volcanic eruptions, J. Volc. Geotherm. Res., 175, 325–333, https://doi.org/10.1016/j.jvolgeores.2008.03.013, 2008. 
Bebbington, M. S.: Assessing spatio-temporal eruption forecasts in a monogenetic volcanic field, J. Volc. Geotherm. Res., 252, 14–28, https://doi.org/10.1016/j.jvolgeores.2012.11.010, 2013. 
Bebbington, M. S.: Spatio-volumetric hazard estimation in the Auckland volcanic field, Bull. Volc., 77, 39, https://doi.org/10.1007/s00445-015-0921-3, 2015. 
Bebbington, M.: Brief communication: A magma depletion alternative for vent distribution in volcanic fields – MATLAB/OCTAVE code, Zenodo [data set] and [code], https://doi.org/10.5281/zenodo.15299975, 2025. 
Bebbington, M. S. and Cronin, S. J.: Spatio-temporal hazard estimation in the Auckland Volcanic Field, New Zealand, with a new event-order model, Bull. Volc., 73, 55–72, https://doi.org/10.1007/s00445-010-0403-6, 2011. 
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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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