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Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallization

Arzilli, F; La Spina, G; Burton, MR; Polacci, M; Le Gall, N; Hartley, ME; Di Genova, D; ... Lee, PD; + view all (2019) Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallization. Nature Geoscience , 12 pp. 1023-1028. 10.1038/s41561-019-0468-6. Green open access

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Abstract

Basaltic eruptions are the most common form of volcanism on Earth and planetary bodies. The low viscosity of basaltic magmas inhibits fragmentation, which favours effusive and lava-fountaining activity, yet highly explosive, hazardous basaltic eruptions occur. The processes that promote fragmentation of basaltic magma remain unclear and are subject to debate. Here we used a numerical conduit model to show that a rapid magma ascent during explosive eruptions produces a large undercooling. In situ experiments revealed that undercooling drives exceptionally rapid (in minutes) crystallization, which induces a step change in viscosity that triggers magma fragmentation. The experimentally produced textures are consistent with basaltic Plinian eruption products. We applied a numerical model to investigate basaltic magma fragmentation over a wide parameter space and found that all basaltic volcanoes have the potential to produce highly explosive eruptions. The critical requirements are initial magma temperatures lower than 1,100 °C to reach a syn-eruptive crystal content of over 30 vol%, and thus a magma viscosity around 105 Pa s, which our results suggest is the minimum viscosity required for the fragmentation of fast ascending basaltic magmas. These temperature, crystal content and viscosity requirements reveal how typically effusive basaltic volcanoes can produce unexpected highly explosive and hazardous eruptions.

Type: Article
Title: Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallization
Open access status: An open access version is available from UCL Discovery
DOI: 10.1038/s41561-019-0468-6
Publisher version: https://doi.org/10.1038/s41561-019-0468-6
Language: English
Additional information: This version is the author accepted manuscript. For information on re-use, please refer to the publisher’s terms and conditions.
Keywords: Petrology, Volcanology
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Engineering Science
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Engineering Science > Dept of Mechanical Engineering
URI: https://discovery.ucl.ac.uk/id/eprint/10086851
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