Author:
Kristianto ,Indrastuti N,Basuki A,Purnamasari H D,Adi S,Patria C,Haerani N
Abstract
Abstract
Anak Krakatau Volcano is located in the Sunda Strait known for its paroxysmal eruption in 1883. During the January - November 2019 period, seismicity was dominated by types of quakes which indicated the occurrence of magma supply (VA and VB), near-surface volcanic activity (LF, Hybrid, Harmonic Tremors), and volcanic activity above the volcanic surface (eruptions, emission, and continuous tremors). In the period December 2019 - July 2020, there was an increase in the types of quakes near the surface (LF, Hybrid) and the types of quakes on the surface (emission and continuous tremors). Volcanic deformation monitors changes in tilt over the 2019-2020 period associated with pressure releases before, during and after the eruption. The results of GPS data modeling, the shallow pressure source is at a depth of 0.22 km below sea level. Volcanic activity until July 2020 was dominated by activity near and above the volcanic surface associated with the growth of lava domes. The volcanic system of Anak Krakatau is currently an open system, with the potential for eruptions. Strengthening the early warning system for the eruption of Anak Krakatau is important in mitigating efforts and understanding its eruption potential
Reference24 articles.
1. Sistem pemantauan gunung Anak Krakatau;Basuki,2019
2. Real-time source deformation modeling through GNSS permanent stations at Merapi volcano (Indonesia);Beauducel,2014
3. Badan Geologi Kementerian Energi Dan Sumber Daya Mineral,2011
4. Geological map of Krakatau Volcanic Complex. Volcanological Survey of Indonesia;Effendi,1986
5. Real-time seismic amplitude measurement (RSAM): a volcano monitoring and prediction tool;Endo;Bulletin of Volcanology,1991
Cited by
1 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