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

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Mara Reed
https://orcid.org/0000-0003-4185-2843
Anna Barth
Taka'aki Taira
https://orcid.org/0000-0002-6170-797X
Jamie Farrell
https://orcid.org/0000-0003-0620-6168
Michael Manga
https://orcid.org/0000-0003-3286-4682

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.

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How to Cite
Reed, M., Barth, A., Taira, T., Farrell, J. and Manga, M. (2024) “A shake and a surge: Assessing the possibility of an earthquake-triggered eruption at Steamboat Geyser”, Volcanica, 7(2), pp. 733–748. doi: 10.30909/vol.07.02.733748.
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Dates
Received 2024-01-03
Accepted 2024-07-08
Published 2024-10-17
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