Abstract
Five Vulcanian explosions were triggered by collapse of the Soufriere Hills Volcano lava dome in 2003. We report strainmeter data for three explosions, characterized by four stages: a short transition between the onset of disturbance and a pronounced change in strain; a quasi-linear ramp accounting for the majority of strain change; a more gradual continued decline of strain to a minimum value; and a strain recovery phase lasting hours. Remarkable similar to 800 s barometric gravity waves propagated at similar to 30 m s(-1). Eruption volumes estimated from plume height and strain data are 0.32-0.42 x 10(6), 0.26-0.49 x 10(6), and 0.81-0.84 x 10(6) m(3), for Explosions 3-5 respectively, consistent with quasi-cylindrical conduit drawdown
Translated title of the contribution | Unique strainmeter observations of Vulcanian explosions, Soufriere Hills Volcano, Montserrat, July 2003 |
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Original language | English |
Number of pages | 5 |
Journal | Geophysical Research Letters |
Volume | 37 |
Issue number | 19 |
DOIs | |
Publication status | Published - Jun 2010 |