Rose Canyon Fault: Difference between revisions
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Only in the 20th century has it become a concern, as mostly the region where the fault is located has not been significantly or substantially populated. The fault is capable of generating a 7.0 magnitude quake, with 8.0 magnitudes as it upper range. |
Only in the 20th century has it become a concern, as mostly the region where the fault is located has not been significantly or substantially populated. The fault is capable of generating a 7.0 magnitude quake, with 8.0 magnitudes as it upper range. |
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[[File:c:\users\mmaeder\desktop\Rose.png|thumbnail|Rose Canyon Fault (USGS)]] |
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== Extent == |
== Extent == |
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The Rose Canyon Fault is about {{convert|30|km|mi|abbr=on}} in length. It starts in the [[Mission Valley, San Diego|Mission Valley]] area and heads, past [[Mt. Soledad]] and [[La Jolla]], into the Pacific ocean, where it joins other faults, such as the [[Oceanside Fault]].<ref name="findingfaults">Monroe, Robert, "Finding Faults", 2002, "[http://explorations.ucsd.edu/faults/index.html]" March 2, 2010</ref> |
The Rose Canyon Fault is about {{convert|30|km|mi|abbr=on}} in length. It starts in the [[Mission Valley, San Diego|Mission Valley]] area and heads, past [[Mt. Soledad]] and [[La Jolla]], into the Pacific ocean, where it joins other faults, such as the [[Oceanside Fault]].<ref name="findingfaults">Monroe, Robert, "Finding Faults", 2002, "[http://explorations.ucsd.edu/faults/index.html]" March 2, 2010</ref> |
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Revision as of 20:26, 25 August 2014
Rose Canyon Fault is a right-lateral strike-slip fault running in a north-south direction through San Diego County, California.[1] Only in the 20th century has it become a concern, as mostly the region where the fault is located has not been significantly or substantially populated. The fault is capable of generating a 7.0 magnitude quake, with 8.0 magnitudes as it upper range.
Extent
The Rose Canyon Fault is about 30 km (19 mi) in length. It starts in the Mission Valley area and heads, past Mt. Soledad and La Jolla, into the Pacific ocean, where it joins other faults, such as the Oceanside Fault.[2]
Current state
Not much is known about the Rose Canyon fault at present,[when?] though its slip-rate is thought to be 1.1 mm/year.[1]
The Rose Canyon Fault has sustained at least one late Holocene rupture, with the date of the earthquake estimated to be after AD 1450 and most likely prior to construction of the San Diego Mission in 1769, as a large historical Rose Canyon earthquake would likely have destroyed that mission.[3]
The Rose Canyon Fault has recently[when?] garnered more attention because it runs through such highly populated areas, but is not thought to be much of a threat. However, some geophysicists, such as San Diego local Jeff Babcock, have hypothesized that a concentrated earthquake involving the Rose Canyon, Oceanside, and Newport-Inglewood faults could result in an earthquake up to magnitude 7.6 on the moment magnitude scale.[2]
References
- ^ a b Hart, E.W., Bryant, W.A., Wills, C.J., Treiman, J.A., and Kahle, J.E., "Summary Report: Fault Evaluation Program, 1987-1988, Southwestern Basin and Range Region and Supplemental Areas. Depart of Conservation, Division of Mines and Geology Open-File Report", 1989, "[1]" March 2, 2010
- ^ a b Monroe, Robert, "Finding Faults", 2002, "[2]" March 2, 2010
- ^ Southern California Edison, Paleoseismic Assessment of the Late Holocene Rupture History of the Rose Canyon Fault in San Diego, December, 2012 "[3]"