The 2018 Rift Eruption And Summit Collapse Of Kilauea Volcano

C A Neal, S R Brantley, L Antolik, J Babb, M Burgess, K Calles, M Cappos,J C Chang, S Conway,L Desmither, P Dotray,T Elias, P Fukunaga, S Fuke,I A Johanson, K Kamibayashi, J Kauahikaua,R L Lee, S Pekalib, A Miklius, W Million, C J Moniz,P A Nadeau, P Okubo,C Parcheta, M P Patrick,B Shiro, D A Swanson, W Tollett, F Trusdell,E F Younger, M H Zoeller,E K Montgomery-Brown,K R Anderson,M P Poland,J Ball, J Bard,M Coombs,H R Dietterich,C Kern,W A Thelen, P F Cervelli,T Orr,B F Houghton, C Gansecki, R Hazlett,P Lundgren, A K Diefenbach,A H Lerner,G Waite,P Kelly,L Clor, C Werner, K Mulliken, G Fisher

SCIENCE(2019)

引用 423|浏览6
暂无评分
摘要
In 2018, Klauea Volcano experienced its largest lower East Rift Zone *(LERZ) eruption and caldera collapse in at least 200 years. After collapse of the Pu'u 'O' O vent on 30 April, magma propagated downrift. Eruptive fissures opened in the LERZ on 3 May, eventually extending -6.8 kilometers. A 4 May earthquake [moment magnitude *(Mw) 6.9] produced -5 meters of fault slip. Lava erupted at rates exceeding 100 cubic meters per second, eventually covering 35.5 square kilometers. The summit magma system partially drained, producing minor explosions and near-daily collapses releasing energy equivalent to Mw 4.7 to 5.4 earthquakes. Activity declined rapidly on 4 August. Summit collapse and lava flow volume estimates are roughly equivalent-about 0.8 cubic kilometers. Careful historical observation and monitoring of Kilauea enabled successful forecasting of hazardous events.
更多
查看译文
AI 理解论文
溯源树
样例
生成溯源树,研究论文发展脉络
Chat Paper
正在生成论文摘要