Tectono-magmatic processes investigated at deep-water flanks of Hawaiian volcanoes
Eos, Transactions, American Geophysical Union
By: J. Naka, E Takahasi, D. Clague, Takeshi Hanyu, E. Herrero-Bervera, J. Ishibashi, Osamu Ishizuka, K. Johnson, T. Kanamatsu, I. Kaneoka, Peter W. Lipman, A. Malahoff, Gary M. McMurtry, B. Midson, Jeff Moore, J. Morgan, T. Naganuma, K Nakajima, T Oomori, Aaron Pietruszka, Satake Kenji, David R. Sherrod, Tsugio Shibata, K Shinozaki, Thomas W. Sisson, John R. Smith, S. Takarada, C. Thomber, Frank A. Trusdell, Nohiro Tsuboyama, T. Ui, Susumu Umino, K. Uto, and H. Yokose
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Abstract
Hawaiian volcanoes are exceptional examples of intraplate hotspot volcanism. Hotspot volcanoes, which frequently host large eruptions and related earthquakes, flank‐failure landslides, and associated tsunamis, can present severe hazards to populated regions. Many studies have focused on subaerial parts of Hawaiian volcanoes, but the deep‐water flanks of the edifices, which can reach 5700 m below sea level, remain poorly understood because they are so inaccessible. In 1998 a collaborative program between Japan and the United States was initiated to explore the evolution of Hawaiian volcanoes, including their growth and degradation
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Tectono-magmatic processes investigated at deep-water flanks of Hawaiian volcanoes |
| Series title | Eos, Transactions, American Geophysical Union |
| DOI | 10.1029/00EO00152 |
| Volume | 81 |
| Issue | 20 |
| Year Published | 2000 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 7 p. |
| First page | 221 |
| Last page | 226 |
| Country | United States |
| State | Hawaii |
| Google Analytic Metrics | Metrics page |