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Coordinates: 33°53′N 117°35′W / 33.883°N 117.583°W / 33.883; -117.583
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The '''Chino Fault''' is a [[Fault (geology)|fault]] that extends along the eastern [[Chino Hills|Chino Hills range]] region, from [[Corona, California|Corona]] in [[Riverside County, California|Riverside County]] to the [[Los Serranos, Chino Hills, California|Los Serranos, Chino Hills]] area of [[San Bernardino County, California|San Bernardino County]] in [[Southern California]].
The '''Chino Fault''' extends along the eastern [[Chino Hills|Chino Hills range]] region, from [[Corona, California|Corona]] in [[Riverside County, California|Riverside County]] to the [[Los Serranos, Chino Hills, California|Los Serranos, Chino Hills]] area of [[San Bernardino County, California|San Bernardino County]] in [[Southern California]].<ref>{{cite web | url = https://earthquake.usgs.gov/research/external/reports/02HQGR0046.pdf | archive-url = https://web.archive.org/web/20160303221545/https://earthquake.usgs.gov/research/external/reports/02HQGR0046.pdf | url-status = dead | archive-date = 2016-03-03 | title = The Chino Fault and Its Relation to Slip on the Elsinore and Whittier Faults and Blind Thrusts in the Puente Hills | publisher = United States Geological Survey|author= Robert S. Yeats}}</ref>


==Geology==
==Geology==
The Chino Fault and [[Whittier Fault]] are the two upper branches of the [[Elsinore Fault Zone]], which is part of the trilateral split of the [[San Andreas fault]] system. The right-lateral strike-slip fault has a slip rate of 1.0 millimeter/year and is capable of producing anywhere from a [[Moment magnitude scale|M<sub>W</sub>]]6.0 to a M<sub>W</sub>7.0 earthquake.
The Chino Fault and [[Whittier Fault]] are the two upper branches of the [[Elsinore Fault Zone]],<ref>{{Cite Q|Q66372720}}</ref> which is part of the trilateral split of the [[San Andreas Fault]] system. The right-lateral strike-slip [[Fault (geology)|fault]] has a slip rate of 1.0 millimeter/year and is capable of producing anywhere from a {{M|w|link=y}} 6.0 to a {{M|w|link=y}} 7.0 earthquake.<ref>{{cite web | url = http://www.data.scec.org/fault_index/chino.html | title = Chino Fault | publisher = Southern California Earthquake Data Center | access-date = 2008-11-12 | archive-url = https://web.archive.org/web/20090313185209/http://www.data.scec.org/fault_index/chino.html | archive-date = 2009-03-13 | url-status = dead}}</ref>


==See also==
==See also==
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==References==
==References==
{{Reflist}}
* {{cite web | url = http://www.data.scec.org/fault_index/chino.html | title = Chino Fault | work = Southern California Earthquake Data Center}}
* {{cite web | url = http://earthquake.usgs.gov/research/external/reports/02HQGR0046.pdf | title = The Chino Fault and Its Relation to Slip on the Elsinore and Whittier Faults and Blind Thrusts in the Puente Hills | work = U.S.G.S.}}


{{coord|33|53|N|117|35|W|region:US-CA_type:landmark|display=title}}
{{coord|33|53|N|117|35|W|region:US-CA_type:landmark|display=title}}


{{California Faults}}
{{California Faults}}

[[Category:Seismic faults of California]]
[[Category:Seismic faults of California]]
[[Category:Strike-slip faults]]
[[Category:Strike-slip faults]]
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[[Category:Geology of San Bernardino County, California]]
[[Category:Geology of San Bernardino County, California]]
[[Category:Geography of Corona, California]]
[[Category:Geography of Corona, California]]



{{RiversideCountyCA-geo-stub}}
{{RiversideCountyCA-geo-stub}}

Latest revision as of 19:42, 24 November 2024

The Chino Fault extends along the eastern Chino Hills range region, from Corona in Riverside County to the Los Serranos, Chino Hills area of San Bernardino County in Southern California.[1]

Geology

[edit]

The Chino Fault and Whittier Fault are the two upper branches of the Elsinore Fault Zone,[2] which is part of the trilateral split of the San Andreas Fault system. The right-lateral strike-slip fault has a slip rate of 1.0 millimeter/year and is capable of producing anywhere from a Mw 6.0 to a Mw 7.0 earthquake.[3]

See also

[edit]

References

[edit]
  1. ^ Robert S. Yeats. "The Chino Fault and Its Relation to Slip on the Elsinore and Whittier Faults and Blind Thrusts in the Puente Hills" (PDF). United States Geological Survey. Archived from the original (PDF) on 2016-03-03.
  2. ^ D.L. Lamar; S.C. Swanson (1981). "Study of seismic activity by selective trenching along the Elsinore fault zone, Southern California". Open-File Report. 81–882. doi:10.3133/OFR81882. ISSN 0196-1497. Wikidata Q66372720.
  3. ^ "Chino Fault". Southern California Earthquake Data Center. Archived from the original on 2009-03-13. Retrieved 2008-11-12.

33°53′N 117°35′W / 33.883°N 117.583°W / 33.883; -117.583