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Published February 22, 1996 | metadata_only
Journal Article

The origin of harmonic tremor at Old Faithful geyser


VOLCANIC eruptions are sometimes accompanied by a characteristic type of seismicity known as harmonic tremor, in which the signal is dominated by discrete vibration frequencies. This harmonic structure could reflect resonance behaviour in the excitation source or filtering of the seismic waves as they propagate through the surrounding rocks; but complexity and variability in the properties of volcanic systems make it difficult to discriminate between such mechanisms. To address this question, we have analysed the source and propagation characteristics of seismicity at Old Faithful geyser (Yellowstone National Park), the cyclic behaviour and accessibility of which make it an ideal natural laboratory for studying harmonic tremor associated with near-surface sources. We find that sharp pressure pulses inside the water column trigger distinct seismic events that give rise to a harmonic ground response whose frequency varies spatially but not temporally. A superposition of these seismic events creates the appearance of continuous harmonic tremor. The absence of resonance within the water column suggests that the harmonic motion must arise from the interaction of the seismic waves with heterogeneities in the surrounding elastic medium—most probably a near-surface soft layer.

Additional Information

© 1996 Nature Publishing Group. Received 20 July; Accepted 22 December 1995. We thank Yellowstone National Park Authorities, Science Office and park geologist R. Hutchinson for help in carrying out the experiments, J. Rineheart for sharing data, experiences and ideas, D. Dreger, B. Zajac, C. Scrivner, T. Melbourne, M. Jackson, J. Holt and A. Pino for work in the laboratory and in the field, J. Wetphal and J. Shepherd for shared expertise in the design of the probe, S. Smithson and the Seismic Exploration team of the University of Wyoming, Laramie, for their work in the 1992 experiment, S. Kieffer for help in planning and analysingthe 1991 experiment, and S. Cincera, D. Johnson, W. Miller, J. Nunez-Anzueto, V. Nenow and R. Taylor for technical support.

Additional details

August 22, 2023
August 22, 2023