A shake and a surge: Assessing the possibility of an earthquake-triggered eruption at Steamboat Geyser

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.30909/vol.07.02.733748. This is version 2 of this Preprint.

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Authors

Mara H. Reed , Anna Barth, Taka'aki Taira, Jamie Farrell, Michael Manga

Abstract

When and why earthquakes trigger volcano and geyser eruptions remains unclear. In September 2022, Steamboat Geyser in Yellowstone, USA erupted 8.25 hours after a local M3.9 earthquake—an improbable coincidence based on the geyser’s eruption intervals. We leverage monitoring data from the surrounding geyser basin to determine if the earthquake triggered this eruption. We calculate a peak ground velocity of 1.2 cm s−1, which is the largest ground motion in the area since Steamboat reactivated in March 2018 and exceeds a threshold associated with past earthquake-triggered geyser eruptions in Yellowstone. Despite no changes in other surface hydrothermal activity, we found abrupt, short-lived shifts in ambient seismic noise amplitude and relative seismic velocity in narrow frequency bands related to the subsurface hydrothermal system. Our analysis indicates that Steamboat’s eruption was likely earthquake-triggered. The hours-long delay suggests that dynamic strains from seismic waves altered subsurface permeability and flow which enabled eruption.

DOI

https://doi.org/10.31223/X58M37

Subjects

Earth Sciences, Physical Sciences and Mathematics, Volcanology

Keywords

geyser, Hydrothermal, eruption triggering, dynamic stress

Dates

Published: 2024-01-03 07:03

Last Updated: 2024-10-17 07:47

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License

CC BY Attribution 4.0 International