Abstract
AbstractThe 2018 summit and flank eruption of Kīlauea Volcano was one of the largest volcanic events in Hawaiʻi in 200 years. Data suggest that a backup in the magma plumbing system at the long-lived Puʻu ʻŌʻō eruption site caused widespread pressurization in the volcano, driving magma into the lower flank. The eruption evolved, and its impact expanded, as a sequence of cascading events, allowing relatively minor changes at Puʻu ʻŌʻō to cause major destruction and historic changes across the volcano. Eruption forecasting is inherently challenging in cascading scenarios where magmatic systems may prime gradually and trigger on small events.
Publisher
Springer Science and Business Media LLC
Subject
General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry
Reference100 articles.
1. Neal, C. A. et al. The 2018 rift eruption and summit collapse of Kīlauea Volcano. Science 363, 367–374 (2019).
2. Dietterich, H. R. et al. Lava effusion rates and channel dynamics during the 2018 Kilauea lower East Rift Zone eruption. AGU Fall Meet. Abstr. V43C–V40215 (2019).
3. Anderson, K. R. et al. Magma reservoir failure and the onset of caldera collapse at Kīlauea Volcano in 2018. Science 366, eaaz1822 (2019).
4. Tilling, R. I., Kauahikaua, J. P., Brantley, S. R. & Neal, C. A. The Hawaiian Volcano Observatory—a natural laboratory for studying basaltic volcanism. U. S. Geol. Surv. Prof. Pap. 1801, 1–64 (2014).
5. Moore, R. B. Volcanic geology and eruption frequency, lower east rift zone of Kilauea volcano, Hawaii. Bull. Volcanol. 54, 475–483 (1992).
Cited by
63 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献