No spreading across the Southern Juan de Fuca Ridge axial cleft during 1994-1996

Direct‐path acoustic measurements between seafloor transponders observed no significant extension (−10±14 mm/yr) from August 1994 to September 1996 at the southern Juan de Fuca Ridge (44°40′ N and 130°20′ W). The acoustic path for the measurement is a 691‐m baseline straddling the axial cleft, which...

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Bibliographic Details
Published in:Geophysical research letters Vol. 26; no. 16; pp. 2525 - 2528
Main Authors: Chadwell, C. David, Hildebrand, John A., Spiess, Fred N., Morton, Janet L., Normark, William R., Reiss, Carol A.
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 15-08-1999
American Geophysical Union
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Summary:Direct‐path acoustic measurements between seafloor transponders observed no significant extension (−10±14 mm/yr) from August 1994 to September 1996 at the southern Juan de Fuca Ridge (44°40′ N and 130°20′ W). The acoustic path for the measurement is a 691‐m baseline straddling the axial cleft, which bounds the Pacific and Juan de Fuca plates. Given an expected full‐spreading rate of 56 mm/yr, these data suggest that extension across this plate boundary occurs episodically within the narrow (∼ 1 km) region of the axial valley floor, and that active deformation is occurring between the axial cleft and the plate interior. A cleft‐parallel 714‐m baseline located 300 m to the west of the cleft on the Pacific plate monitored system performance and, as expected, observed no motion (+5±7 mm/yr) between the 1994 and 1996 surveys.
Bibliography:istex:EDC84D1F96CE38A007749AEBD8D9A0B9A7818872
ArticleID:1999GL900570
ark:/67375/WNG-CMQHJ2Q6-9
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/1999GL900570