Cyclic lava effusion during the 2018 eruption of Kīlauea Volcano

Author:

Patrick M. R.1ORCID,Dietterich H. R.2ORCID,Lyons J. J.2ORCID,Diefenbach A. K.3ORCID,Parcheta C.1ORCID,Anderson K. R.4ORCID,Namiki A.5ORCID,Sumita I.6ORCID,Shiro B.1ORCID,Kauahikaua J. P.1ORCID

Affiliation:

1. U.S. Geological Survey, Hawaiian Volcano Observatory, Hilo, HI 96720, USA.

2. U.S. Geological Survey, Alaska Volcano Observatory, Anchorage, AK 99508, USA.

3. U.S. Geological Survey, Cascades Volcano Observatory, Vancouver, WA 98683, USA.

4. U.S. Geological Survey, California Volcano Observatory, Menlo Park, CA 94025, USA.

5. School of Integrated Arts and Sciences, Hiroshima University, Higashi Hiroshima, Hiroshima 739-8521, Japan.

6. Graduate School of Natural Science and Technology, Kanazawa University, Kakuma, Kanazawa, 920-1192, Japan.

Abstract

Caldera collapse and flank eruption Real-time monitoring of volcanic eruptions involving caldera-forming events are rare (see the Perspective by Sigmundsson). Anderson et al. used several types of geophysical observations to track the caldera-forming collapse at the top of Kīlauea Volcano, Hawai'i, during the 2018 eruption. Gansecki et al. used near–real-time lava composition analysis to determine when magma shifted from highly viscous, slow-moving lava to low-viscosity, fast-moving lava. Patrick et al. used a range of geophysical tools to connect processes at the summit to lava rates coming out of far-away fissures. Together, the three studies improve caldera-collapse models and may help improve real-time hazard responses. Science , this issue p. eaaz0147 , p. eaay9070 ; p. eaaz1822 ; see also p. 1200

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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