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Changes in Seismic Anisotropy After Volcanic Eruptions: Evidence from Mount Ruapehu

Miller, Vicki, Savage, Martha·2001·Science
DOI 10.1126/science.1063463
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Abstract

The eruptions of andesite volcanoes are explosively catastrophic and notoriously difficult to predict. Yet changes in shear waveforms observed after an eruption of Mount Ruapehu, New Zealand, suggest that forces generated by such volcanoes are powerful and dynamic enough to locally overprint the regional stress regime, which suggests a new method of monitoring volcanoes for future eruptions. These results show a change in shear-wave polarization with time and are interpreted as being due to a localized stress regime caused by the volcano, with a release in pressure after the eruption.

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Metadata

Authors
Miller, V., & Savage, M.
Affiliations
Institute of Geophysics, Victoria University of Wellington, Wellington, New Zealand.
Venue
Science
Publisher
American Association for the Advancement of Science (AAAS)
Published
2001-09-21
Volume
293
Issue
5538
Pages
2231-2233
ISSN
  • 0036-8075
  • 1095-9203
DOI
10.1126/science.1063463
Cited by
104
References
0
Language
en

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CoChat. (2026). Citation check: Changes in Seismic Anisotropy After Volcanic Eruptions: Evidence from Mount Ruapehu. https://app.cochat.ai/papers/10.1126/science.1063463
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Miller, V., & Savage, M. (2001). Changes in Seismic Anisotropy After Volcanic Eruptions: Evidence from Mount Ruapehu. Science. https://doi.org/10.1126/science.1063463