Document Type
Article
Publication Date
2001
Keywords
Earthquake swarm, Loihi submarine volcano, Seismic activity
Abstract
The largest earthquake swarm yet recorded on Loihi submarine volcano took place in July and August of 1996. The swarm consisted of two phases of seismic activity and was associated with the formation of a pit crater and additional faulting of Loihi’s summit platform. The first phase of activity was comprised of predominantly high-frequency events scattered over the southern flanks of the volcano. Following a day of seismic quiescence, the second phase of activity began, consisting of lower-frequency earthquakes with strong T-phases. The phase 2 events took place beneath Loihi’s summit, presumably marking the formation of the pit crater, Pele’s Pit. Data obtained by an ocean-bottom seismometer (OBS) on Loihi during the swarm help constrain a new velocity model for Loihi. The relocated earthquakes, combined with other characteristics of the swarm, enabled us to develop a model for the events leading up to the formation of Pele’s Pit that includes (1) a prolonged eruption, (2) a tectonic event beneath Loihi’s south flank, and (3) the drainage of a shallow magma chamber.
Publication Title
Bulletin of the Seismological Society of America
Volume
91
Issue
2
First Page
178
Last Page
190
Required Publisher's Statement
© 2001 by the Seismological Society of America
DOI: 10.1785/0119990170
Recommended Citation
Caplan-Auerbach, Jacqueline and Duennebier, F. K., "Seismicity and Velocity Structure of Loihi Seamount from the 1996 Earthquake Swarm" (2001). Geology Faculty Publications. 47.
https://cedar.wwu.edu/geology_facpubs/47
Subjects - Topical (LCSH)
Earthquake swarms--Hawaii; Volcanoes--Hawaii; Seismic waves--Speed--Measurement
Geographic Coverage
Hawaii
Genre/Form
articles
Type
Text
Language
English
Format
application/pdf