Document Type
Article
Publication Date
5-1-2001
Keywords
Kilauea volcano, HUGO, Hydroacoustic detection, Submarine landslides
Abstract
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.
Publication Title
Geophysical Research Letters
Volume
28
Issue
9
First Page
1811
Last Page
1813
Required Publisher's Statement
© 2001 American Geophysical Union
DOI: 10.1029/2000GL012545
http://onlinelibrary.wiley.com/doi/10.1029/2000GL012545/abstract
Recommended Citation
Caplan-Auerbach, J., C. G. Fox and F. Duennebier, Hydroacoustic Detection of Submarine Landslides on Kilauea Volcano, Geophys. Res. Lett., 28(9), 1811-1814, 2001
Subjects - Topical (LCSH)
Submarine volcanoes--Hawaii--Kilauea; Underwater acoustics--Hawaii--Kilauea; Landslides--Hawaii--Kilauea
Geographic Coverage
Kilauea (Hawaii)
Genre/Form
articles
Type
Text
Language
English
Format
application/pdf