Reevaluating the 2008-2009 Yellowstone Lake swarm with deep learning

Woodrich, Hayley G

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https://hdl.handle.net/2142/129954 Copy

Description

Title

Reevaluating the 2008-2009 Yellowstone Lake swarm with deep learning

Author(s)

Woodrich, Hayley G

Issue Date

2025-07-23

Director of Research (if dissertation) or Advisor (if thesis)

• Maguire, Ross
• Gregg, Trish

Department of Study

Earth Sci & Environmental Chng

Discipline

Geology

Degree Granting Institution

University of Illinois Urbana-Champaign

Degree Name

M.S.

Degree Level

Thesis

Keyword(s)

geophysics, machine learning, geology, volcanology, Yellowstone

Abstract

The 2008-09 Yellowstone Lake seismic swarm was one of the most energetic in the last several decades with >800 earthquakes recorded between December 26, 2008 and January 8, 2009 (ANSS Comprehensive Earthquake Catalog, ComCat). While the cause of the swarm is uncertain, its location and coinciding extensional surface deformation hints at magma migration. Recent tomographic imaging suggests that the hypocenters occurred within an area of shear wave speed anomalies of up to 25% slow, suggesting that the swarm was located within a warm magma mush zone. In this study, we investigate the spatial and temporal evolution of the 2008-09 Yellowstone Lake swarm, as well as the spatial relationship between swarm activity and magma storage. We produced an updated seismicity catalog for the Yellowstone region between December 1, 2008, and January 31, 2009, using a combination of deep learning-based phase pickers (PhaseNet and EQTransformer) and GaMMA for phase association. Compared to ComCat, our catalog increases the number of events during the swarm period from 811 to 2297 and the number of events during the full cataloged period from 1217 to 3316. Earthquake hypocenters were relocated using HypoDD, a double-difference algorithm that minimizes the difference observed and calculated travel times. Updated hypocenter locations confirm that the Yellowstone Lake swarm occurred within the seismic slow zone, primarily in a region where wave speeds are 15-20% slow, consistent with a magma mush or partial melt.

Graduation Semester

2025-08

Type of Resource

Thesis

Handle URL

https://hdl.handle.net/2142/129954

Copyright and License Information

Copyright 2025 Hayley Woodrich

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