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SEISMIC TRIGGERING OF ERUPTIONS IN THE FAR FIELD: Volcanoes and Geysers
Abstract
Approximately 0.4% of explosive volcanic eruptions occur within a few days of large, distant earthquakes. This many “triggered” eruptions is much greater than expected by chance. Several mechanisms have been proposed to explain triggering through changes in magma overpressure, including the growth of bubbles, the advection of large pressures by rising bubbles, and overturn of magma chambers. Alternatively, triggered eruptions may occur through failure of rocks surrounding stored magma. All these mechanisms require a process that enhances small static stress changes caused by earthquakes or that can convert (the larger) transient, dynamic strains into permanent changes in pressure. All proposed processes, in addition to viscoelastic relaxation of stresses, can result in delayed triggering of eruptions, although quantifying the connection between earthquakes and delayed, triggered eruptions is much more challenging. Mud volcanoes and geysers also respond to distant earthquakes. Mud volcanoes that discharge mud from depths greater than many hundreds of meters may be triggered by liquefaction caused by shaking, and may thus be similar to small mud volcanoes that originate within a few meters of the surface. Changes in permeability of the matrix surrounding main geyser conduits, by opening or creating new fractures, may explain the observed changes in their eruption frequency.
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“The mechanisms by which earthquakes infl uence magmatic volcanoes and hydrologic systems are unknown, and debated, but owing to the large distances between the earthquakes and the sites where the responses occur, the dynamic stresses produced by passing seismic waves are usually implicated in the triggering mechanisms (Manga and Brodsky, 2006).”
From Triggering of the largest Deccan eruptions by the Chicxulub impact (2015) · cites this paper as Manga and Brodsky, 2006
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“About 0.4% of explosive volcanic eruptions occur within a few days of distant earthquakes, an eruption frequency that is ~10 times greater than background rates (Manga and Brodsky, 2006).”
From Triggering of the largest Deccan eruptions by the Chicxulub impact (2015) · cites this paper as Manga and Brodsky, 2006
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Cited by
State shift in Deccan volcanism at the Cretaceous-Paleogene boundary, possibly induced by impact
Renne, P. R., Sprain, C. J., Richards, M. A., Self, S., Vanderkluysen, L., & Pande, K. (2015) · Science · doi:10.1126/science.aac7549 · Cited by 431
Triggering of the largest Deccan eruptions by the Chicxulub impact
Richards, M. A., Alvarez, W., Self, S., Karlstrom, L., Renne, P. R., Manga, M., Sprain, C. J., Smit, J., Vanderkluysen, L., & Gibson, S. A. (2015) · Geological Society of America Bulletin · doi:10.1130/b31167.1 · Cited by 210
Self-citation
Metadata
- Authors
- Manga, M., & Brodsky, E.
- Affiliations
- Department of Earth and Planetary Science, University of California, Berkeley, California 94720-4767;
- Department of Earth Sciences, University of California, Santa Cruz, California 95060
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 2006-05-01
- Volume
- 34
- Issue
- 1
- Pages
- 263-291
- ISSN
- 0084-6597
- 1545-4495
- Cited by
- 434
- References
- 0
- Language
- en
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- Manga, M., & Brodsky, E. (2006). SEISMIC TRIGGERING OF ERUPTIONS IN THE FAR FIELD: Volcanoes and Geysers. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.34.031405.125125