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Triggering of volcanic eruptions

Author

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  • Alan T. Linde

    (Carnegie Institution of Washington)

  • I. Selwyn Sacks

    (Carnegie Institution of Washington)

Abstract

Although earthquakes and volcanic eruptions are each manifestations of large-scale tectonic plate and mantle motions, it is usually thought that the occurrences of these events are not directly related. There have been some studies, however, in which triggering of volcanic eruptions by earthquakes (remote from the volcano) has been proposed1,2. The 1992 Landers (southern California) earthquake caused triggered seismicity at very large distances3, including the magmatically active4 Long Valley caldera region which also experienced a significant coincident deformation transient5. Motivated by this demonstration of the ability of a distant earthquake to disturb a volcanic system, and the earlier studies of specific cases of eruption triggering, we examine here the historical record of eruptions and earthquakes to see if there are indeed significantly more eruptions immediately following large earthquakes. We find that within a day or two of large earthquakes there are many more eruptions within a range of 750 km than would otherwise be expected. Additionally, it is well known6 that volcanoes separated by hundreds of kilometres frequently erupt in unison; the characteristics of such eruption pairs are also consistent with the hypothesis that the second eruption is triggered by earthquakes associated with the first.

Suggested Citation

  • Alan T. Linde & I. Selwyn Sacks, 1998. "Triggering of volcanic eruptions," Nature, Nature, vol. 395(6705), pages 888-890, October.
    • Handle: RePEc:nat:nature:v:395:y:1998:i:6705:d:10.1038_27650
    DOI: 10.1038/27650
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    Cited by:

    1. G. Surve & G. Mohan, 2012. "Possible evidence of remotely triggered and delayed seismicity due to the 2001 Bhuj earthquake (Mw = 7.6) in western India," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 64(1), pages 299-310, October.
    2. Howard Roscoe, 2001. "The Risk of Large Volcanic Eruptions and the Impact of this Risk on Future Ozone Depletion," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 23(2), pages 231-246, March.
    3. G. Babayev & A. Tibaldi & F. Bonali & F. Kadirov, 2014. "Evaluation of earthquake-induced strain in promoting mud eruptions: the case of Shamakhi–Gobustan–Absheron areas, Azerbaijan," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 72(2), pages 789-808, June.
    4. O. Mishra & D. Zhao & Chandan Ghosh & Z. Wang & O. Singh & Biman Ghosh & K. Mukherjee & D. Saha & G. Chakrabortty & S. Gaonkar, 2011. "Role of crustal heterogeneity beneath Andaman–Nicobar Islands and its implications for coastal hazard," Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, Springer;International Society for the Prevention and Mitigation of Natural Hazards, vol. 57(1), pages 51-64, April.

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