| Rapid deformation of the South flank of kilauea volcano, hawaii. | |
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MedLine Citation:
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PMID: 17812606 Owner: NLM Status: PubMed-not-MEDLINE |
Abstract/OtherAbstract:
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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. |
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Authors:
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S Owen; P Segall; J Freymueller; A Mikijus; R Denlinger; T Arnadóttir; M Sako; R Bürgmann |
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Publication Detail:
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Type: Journal Article |
Journal Detail:
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Title: Science (New York, N.Y.) Volume: 267 ISSN: 0036-8075 ISO Abbreviation: Science Publication Date: 1995 Mar |
Date Detail:
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Created Date: 2010-06-08 Completed Date: 2010-07-02 Revised Date: - |
Medline Journal Info:
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Nlm Unique ID: 0404511 Medline TA: Science Country: United States |
Other Details:
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Languages: eng Pagination: 1328-32 Citation Subset: - |
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From MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine
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