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Tracking Secondary Lahar Flow Paths and Characterizing Pulses and Surges Using Infrasound Array Networks at Volcán de Fuego, Guatemala
Volcanica
  • Ashley R. Bosa, Boise State University
  • Jeffrey B. Johnson, Boise State University
  • Silvio De Angelis, University of Liverpool
  • John J. Lyons, U.S. Geological Survey
  • Amilcar Roca, Instituto Nacional de Sismologia, Vulcanologia, Meteorologia e Hidrologia (INSIVUMEH)
  • Jacob F. Anderson, Boise State University
  • Amando Pineda
Document Type
Article
Publication Date
10-25-2021
Abstract

Lahars are one of the greatest hazards at many volcanoes, including Volcán de Fuego (Guatemala). On 1 December 2018 at 8:00 pm local Guatemala time (~2:06:00 UTC), an hour-long lahar event was detected at Volcán de Fuego by two permanent seismo-acoustic stations along the Las Lajas drainage on the southeast side. To establish the timing, duration, and speed of the lahar, infrasound array records were examined to identify both the source direction(s) and the correlated energy fluctuations at the two stations. Co-located seismic and acoustic signals were also examined, which indicated at least five distinct energy pulses within the lahar record. We infer that varying sediment load and/or changes in flow speed is shown by clear fluctuations in the acoustic and seismic power recorded at one of the stations. This particular event studied with infrasound provides insight into how lahars occur around Volcán de Fuego.

Creative Commons License
Creative Commons Attribution 4.0 International
Citation Information
Ashley R. Bosa, Jeffrey B. Johnson, Silvio De Angelis, John J. Lyons, et al.. "Tracking Secondary Lahar Flow Paths and Characterizing Pulses and Surges Using Infrasound Array Networks at Volcán de Fuego, Guatemala" Volcanica (2021)
Available at: http://works.bepress.com/jeffrey_johnson/59/