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Science 3 March 1995:
Vol. 267. no. 5202, pp. 1328 - 1332
DOI: 10.1126/science.267.5202.1328

Articles

Rapid Deformation of the South Flank of Kilauea Volcano, Hawaii

Susan Owen 1, Paul Segall 1, Jeff Freymueller 1, Asta Mikijus 1, Roger Denlinger 1, Thora Árnadóttir 1, Maurice Sako 1, and Roland Bürgmann 2

1 Geophysics Department, Stanford University, Stanford, CA 94305, USA.
2 U.S. Geological Survey, Hawaiian Volcano Observatory, HI 96718, USA.

The south flank of Kilauea volcano has experienced two large [magnitude (M) 7.2 and M 6.1] earthquakes in the past two decades. Global Positioning System measurements conducted between 1990 and 1993 reveal seaward displacements of Kilauea's central south flank at rates of up to about 10 centimeters per year. In contrast, the northern side of the volcano and the distal ends of the south flank did not displace significantly. The observations can be explained by slip on a low-angle fault beneath the south flank combined with dilation deep within Kilauea's rift system, both at rates of at least 15 centimeters per year.

Submitted on September 9, 1994
Accepted on December 1, 1994


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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Seismic Velocity and Attenuation Structure of the East Rift Zone and South Flank of Kilauea Volcano, Hawaii.
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Shallow Normal Faulting and Block Rotation Associated with the 1975 Kalapana Earthquake, Kilauea Volcano, Hawaii.
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Bulletin of the Seismological Society of America 91, 1553-1562
Overthrusting and sediment accretion along Kilauea's mobile south flank, Hawaii: Evidence for volcanic spreading from marine seismic reflection data.
J. K. Morgan, G. F. Moore, D. J. Hills, and S. Leslie (2000)
Geology 28, 667-670
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High Magma Storage Rates Before the 1983 Eruption of Kilauea, Hawaii.
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