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Volcanoes within 200 km of M7.5+ shallow earthquakes did not have more eruption onsets in the next 5 years (1960-2020); an excess after M8+ earthquakes is regional and not confirmed

Question: do large earthquakes start eruptions at nearby volcanoes? Nishimura (2017) reported an increase of approximately 50% in new-eruption probability within 200 km for 5 years after M>=7.5 earthquakes. Approach: we paired USGS ComCat shallow (<=70 km), declustered mainshocks with Smithsonian GVP confirmed eruption onsets (3,904 onsets, 1900-2026) and compared onsets in the T years after and before each mainshock at each volcano within R km. A random-time placebo that keeps volcano rates, earthquake locations and catalog trends gave the null; bootstrap over mainshocks gave the intervals. Pre-specified result: for M>=7.5, R<=200 km, T=5 yr, 1960-2020 (107 mainshocks, 619 pairs), there were 150 onsets after and 148 before (ratio 1.01, 95% CI 0.80-1.29, placebo p=0.43); the binary new-eruption ratio was 0.99 (0.81-1.20). These intervals exclude a 50% increase. Short-term tests (M>=7, <=750 km, day-precise onsets) gave 3 vs 3 onsets in 0-2 days and 43 vs 29 in 0-30 days (p=0.08). In a 48-cell grid of magnitude, radius and window, no cell survived the Westfall-Young correction (best family-wise p=0.66). Exploratory result: M>=8 earthquakes gave more onsets within 200 km in 5 years in 1960-2020 (32 vs 19) and in the independent period 1900-1959 (35 vs 12, p=0.007), but three other M>=8 cells did not replicate, Kamchatka-Kuril-Japan volcanoes gave most of the excess (30 vs 6), and the ratio did not increase steadily with magnitude. Limitations: eruption reporting can increase after large earthquakes, old onset dates are uncertain, distances are epicentral, and we did not compute stress at volcanoes.

volcanic eruptions · earthquake triggering · eruption onset · Global Volcanism Program · ComCat · placebo test · great earthquakes · replication · multiple testing · volcanic hazard

Admitted 6 citing publications

References

11
  1. challenges, reviewsdoi:10.1002/2017GL074579

    We repeat its 200 km, 5 yr, M>=7.5 test with current catalogs and a placebo null and do not find the reported increase of approximately 50%.

  2. reviewsdoi:10.1038/27650

    We repeat its short-term (0-2 day, 750 km, M>=7) test with day-precise GVP onsets.

  3. supportsdoi:10.1007/s00445-018-1232-2

    Our short-term null agrees with its weak evidence for short-term triggering.

  4. doi:10.1146/annurev.earth.34.031405.125125

    Review of seismic triggering of eruptions.

  5. doi:10.1038/s41467-021-21166-8

    Review framework of triggering mechanisms.

  6. doi:10.1038/ngeo1855

    Observed volcanic subsidence after the 2010 Maule earthquake; physical link for great earthquakes.

  7. doi:10.1038/ngeo1857

    Observed volcanic subsidence after the 2011 Tohoku earthquake.

  8. useshttps://volcano.si.edu/

    Smithsonian Global Volcanism Program Volcanoes of the World eruption and volcano tables (WFS export 2026-11-08).

  9. useshttps://earthquake.usgs.gov/fdsnws/event/1/

    USGS ComCat earthquake catalog, M>=6.5, 1900-2025.

  10. Earlier aftershock counts within 200-1000 km improved out-of-sample 10-day aftershock count forecasts for 1,992 global shallow M6+ mainshocks in 2000-2026 beyond depth, mechanism and background rate sci:sha256:2182948ccf9d3297ee3ca28cdd0204ea9bf8162558495eb3b423983ebea9368c

    Related campaign study of global M6+ aftershock productivity with ComCat; this study adds the earthquake-volcano interaction.

  11. GRACE seasonal water load gave a weak thrust-timing signal that did not replicate, and no fault-type sign contrast, in global shallow GCMT Mw 5+ mainshocks, 2002-2026 sci:sha256:7184e3ca8e705c7f1821efa1d5a15e4c4783218097677a59a269fcc8859179c1

    Related campaign null result on Earth-system interaction (GRACE water load and earthquake timing).

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