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Caplan-Auerbach et al. 2001
Caplan-Auerbach, J., Fox, C.G. and Duennebier, F.K. (2001). Hydroacoustic detection of submarine landslides on Kilauea Volcano. Geophysical Research Letters 28: doi: 10.1029/2000GL012545. issn: 0094-8276.

Landslides produced at the site where lava flows into the ocean at Kilauea volcano have been detected hydroacoustically. Up to 10 landslides per day were detected by a hydrophone on the Hawaii Undersea Geo-Observatory (HUGO), located 50 km south of the entry site. The largest of these landslides, partly subaerial events known as bench collapses, were detected by a network of hydrophones in the eastern Pacific, 5000--7000 km away from the source. The landslides display a characteristic spectral signature easily recognizable among other signals such as earthquake T-phases and anthropogenic noises. The fact that signals are detected at great distances suggests that hydroacoustic detection of landslides could be a powerful tool in tsunami monitoring and modeling efforts. ¿ 2001 American Geophysical Union

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Abstract

Keywords
Marine Geology and Geophysics, Instruments and techniques, Oceanography, General, Ocean acoustics, Oceanography, Physical, Tsunamis and storm surges
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
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