Dynamics of the December 2002 flank failure and tsunami at Stromboli volcano inferred by volcanological and geophysical observations

Dynamics of the December 2002 flank failure and tsunami at Stromboli volcano inferred by volcanological and geophysical observations
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根据火山学和地球物理观测推断的 2002 年 12 月斯特龙博利火山侧翼崩塌和海啸的动力学

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发表时间:
2003
期刊:
影响因子:
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通讯作者:
Domenico Patanè
Domenico Patanè
中科院分区:
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文献类型:
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作者:
A. Bonaccorso;S. Calvari;G. Garfi;L. Lodato;Domenico Patanè

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2002年斯特龙博利火山的侧面喷发开始于12月28日,经过几个月的强烈爆炸活动在山顶火山口。12月30日,地震网络记录到两次大的侧翼故障和相关的海啸波。这是首次通过多学科监测系统记录到侧翼坍塌和海啸及其相关现象。火山学和地球物理学监测,以及在故障之前和之后立即进行的热调查,使我们能够定义和解释事件的顺序。这场仍在持续的喷发首次提供了一个机会,让人们有机会了解斯特龙博利火山喷发的动力学、侧翼破坏和滑坡的形成及其潜在的危险。
The 2002 effusive flank eruption at Stromboli volcano started on December 28, after several months of strong explosive activity at the summit craters. On December 30, the seismic network recorded two large flank failures and associated tsunami waves. This is the first time that a flank collapse and tsunami, and their associated phenomena, have been recorded by a multi‐disciplinary monitoring system. Volcanological and geophysical monitoring, as well as thermal surveys performed immediately before and after the failure, allowed us to define and interpret the sequence of events. The still on‐going eruption has provided, for the first time, the opportunity to look into the dynamics of Stromboli's effusive eruptions, flank failure and landslide formation, and their potential hazard.