Rose Canyon Fault: Difference between revisions

Rose Canyon Fault
Rose Canyon Fault
Rose Canyon Fault Zone, Newport Inglewood-Rose Canyon Fault Zone, Newport Inglewood-Rose Canyon-Vallecitos-San Miguel Fault Zone, Newport Inglewood-Rose Canyon-Descanso-Agua Blanca Fault Zone
	The Rose Canyon Fault is located at the bottom right of the map
Etymology	Rose Canyon
Standort	Onshore and offshore San Diego
Land	Vereinigte Staaten
State	California
Characteristics
Part of	California Continental Borderland
Length	~30–170 km (19–106 mi)
Tectonics
Earthquakes	1862 San Diego earthquake
Typ	Right-lateral strike-slip

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The Rose Canyon Fault is a right-lateral strike-slip fault that runs in a north–south direction off the coast of San Diego County, California until it comes ashore near downtown San Diego. The fault is linked to the Newport–Inglewood Fault (NIFZ) in the north and either the Agua Blanca Fault or San Miguel–Vallecitos Fault Zone in the south via en echelon step overs. Conservative estimates of the fault place the length around 30–50 km (19–31 mi), while interpretations including the NIFZ place the length at 170 km (110 mi). There are not many earthquakes associated with the fault, however a magnitude 6–6.5 may have struck on the fault in 1862. The fault runs very near to populated areas when offshore, hence there is high potential for infrequent large and damaging earthquakes.

Tectonic setting

Southern California lies along a transform boundary between the Pacific Plate and North American Plate. Faulting is taken up by three main groups of faults: the San Andreas Fault and linked faults, the Eastern California Shear Zone (ECSZ), and the California Continental Borderland (CCB). The San Andreas system and the ECSZ take up around 85% of the deformation, while the CCB accommodates the rest.^[1]^[2] The CCB is itself split into the Inner (ICB) and Outer Continental Borderlands. The ICB takes up ~6–8 mm (0.24–0.31 in) of the plate boundary's slip, with the Rose Canyon Fault being one of the most hazardous faults in the ICB system.^[1]^[3]

Fault characteristics

The right-lateral strike-slip fault extends for 30–50 km (19–31 mi) and slips at a rate of 1.1–2 mm (0.043–0.079 in)/yr.^{[note 1]}^[4]^[7] The fault begins in the San Diego Bay, then runs through La Jolla before turning offshore. It extends north paralleling the coastline before connecting with the Newport-Inglewood Fault via short en echelon step overs, and the two faults together extend for 170 km (110 mi).^[8]^[9]

Southern terminus

The southern terminus of the Rose Canyon Fault Zone has not been conclusively determined, and is considered to connect to the Descanso and Agua Blanca Faults and/or the San Miguel–Vallecitos Fault Zone.^[10]^[11] Researchers have suggested that both of these faults may transfer slip to the Rose Canyon Fault via San Diego Bay step overs, however no clear connection has been determined.^[12] Around the San Diego Bay, the fault splays out into many different strands, such as the Silver Strand and Spanish Bight faults.^[13]^[14] Some of these splay faults come very close to the Descanso Fault, which in turn links with the Agua Blanca Fault. This leads certain researchers to consider these faults interconnected as one major fault zone, the Newport Inglewood–Rose Canyon–Descanso–Agua Blanca Fault Zone.^[10]^[15]^[16] Others favor an interpretation which links the Rose Canyon to the San Miguel-Vallecitos Fault Zone, though just like with the Descanso and Agua Blanca faults, there are no visible faults connecting the two.^[12] Other researchers attempting to determine which of the two faults the Rose Canyon connects to in the south provide evidence for both faults having a potential link.^[17]^[18]^[19]

Seismic activity

The Rose Canyon Fault has little associated historic seismicity, however a magnitude 6–6.5 earthquake in 1862 is often attributed to it.^[20] The shock was assigned a Modified Mercalli intensity shaking of VII (Very strong). Shaking was widespread and felt in Los Angeles (over 100 mi (160 km) away). However, due to the lack of reports in the area, it is not possible to guarantee that this earthquake occurred on the Rose Canyon Fault.^[21] Trenching of the fault reveals multiple ruptures within the past 8,100 years, including a rupture that occurred between 300 years to shortly before the San Diego Mission was established.^[22] Some of these historic ruptures have an estimated magnitude of 7–7.3.^[23]

Future hazard

The Rose Canyon Fault Zone can produce large earthquakes which can be very destructive due to its proximity to major population centers in Southern California.^[8] On the fault, earthquakes nearing magnitude 7 have a recurrence interval between 700±400^[24] and 2,000 years.^[23] Scenarios modeling a magnitude 6.9 earthquake predict peak ground acceleration will reach 0.55 g in San Diego, and 0.35 g in Tijuana. Downtown San Diego and Mission Bay will experience liquefaction, while Mt. Soledad may experience landslides. Coastal areas such as La Jolla and Point Loma may experience localized coastal bluff failures, and submarine canyons may have landslides which trigger tsunami.^[25] Other studies link the Rose Canyon Fault with the Newport-Inglewood, and the combined fault zone can produce M7.3–7.4 earthquakes.^[8]

Notes

^ The Southern California Earthquake Center has the fault at 30km,^[4] A 2010 paper by Thomas Rockwell has it at 40km,^[5] and a 1997 book by Glenn Roquemore has the length at 50km.^[6]

References

^ ^a ^b Bormann & Kent, p. 2.
^ Liu, Wang & Li 2010, p. 1.
^ Maloney et al., p. 6.
^ ^a ^b "Rose Canyon Fault Zone". Southern California Earthquake Center. Southern California Earthquake Center. Archived from the original on 16 July 2011. Retrieved 31 December 2023.
^ Rockwell 2010, p. 9.
^ Roquemore 1997.
^ Lindvall & Rockwell 1995, p. 10.
^ ^a ^b ^c Sahakian et al. 2017.
^ Rockwell & Singleton 2018, p. 2.
^ ^a ^b SONGS 2012, p. 2.
^ Abbott & Elliott 1979, p. 29.
^ ^a ^b Maloney et al., p. 7.
^ Rockwell & Singleton 2018, p. 4.
^ Lindvall & Rockwell 1995, p. 1.
^ Rockwell & Singleton 2018, p. 3-4.
^ Grant & Rockwell 2002.
^ Abbott & Elliott 1979, p. 41.
^ Anderson, Rockwell & Agnew 1989, p. 10.
^ Roquemore 1997, p. 12.
^ De Wyze 2000, p. 6.
^ Roquemore 1997, p. 8.
^ Lindvall & Rockwell 1995, p. 9.
^ ^a ^b De Wyze 2000, p. 5.
^ Lin II 2020.
^ EERI 2020, p. 34.

Sources

Abbott, Patrick L.; Elliott, William J. (November 1979). "Faulting offshore San Diego and northern Baja California". In Legg, Mark R.; Kennedy, Michael P. (eds.). Earthquakes and other perils—San Diego region (PDF). San Diego Association of Geologists Guidebook. Retrieved 31 December 2023.
Anderson, John G.; Rockwell, Thomas K.; Agnew, Duncan Carr (May 1989). "Past and Possible Future Earthquakes of Significance to the San Diego Region". Earthquake Spectra. 5 (2): 299–335. doi:10.1193/1.1585524. Retrieved 1 January 2024.
Bormann, Jayne; Kent, Graham. Investigating recent deformation along the southern San Pedro Basin fault to assess evidence for connectivity between the San Pedro Basin and San Diego Trough fault systems (PDF) (Report). U.S. Geological Survey. Retrieved 27 December 2023.
De Wyze, Jeannete (2 March 2000). "Earthquake San Diego Danger Zones" (PDF). San Diego Reader. Retrieved 1 January 2024.
EERI (2020). San Diego Earthquake Planning Scenario (PDF) (Report). Retrieved 1 January 2024.
Grant, Lisa B.; Rockwell, Thomas K. (2002). "A Northward-propagating Earthquake Sequence in Coastal Southern California?". Seismological Research Letters. 73 (4). doi:10.1785/GSSRL.73.4.461. Retrieved 1 January 2024.
Lin II, Rong-Gong (4 March 2020). "San Diego faces critical earthquake danger from fault long believed to be inactive". LA Times. Retrieved 1 January 2024.
Lindvall, Scott C.; Rockwell, Thomas K. (10 December 1995). "Holocene activity of the Rose Canyon fault zone in San Diego, California". Journal of Geophysical Research: Solid Earth. 100 (B12): 24121–24132. doi:10.1029/95JB02627. Retrieved 31 December 2023.
Liu, Mian; Wang, Hui; Li, Qingsong (7 July 2010). "Inception of the eastern California shear zone and evolution of the Pacific-North American plate boundary: From kinematics to geodynamics". Journal of Geophysical Research. 115 (B7). Bibcode:2010JGRB..115.7401L. doi:10.1029/2009JB007055. Retrieved 30 December 2023.
Maloney, Jillian M.; Legg, Mark; Nicholson, Craig; Rockwell, Thomas K. "White Paper: The California continental borderland" (PDF). Southern California Earthquake Center. Retrieved 30 December 2023.
Rockwell, Thomas K.; Singleton, Drake (April 2018). Mid to Late Holocene Rupture History of the Rose Canyon Fault in San Diego, California (PDF) (Report). Retrieved 30 December 2023.
Rockwell, Thomas K. (28 May 2010). The Rose Canyon Fault Zone in San Diego. International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics. Retrieved 31 December 2023.
Roquemore, Glenn (1 April 1997). The Seismic Risk in the San Diego Region: Special Focus on the Rose Canyon Fault Systems: Workshop Proceedings. DIANE Publishing. ISBN 978-0-7881-4262-8.
Sahakian, Valerie; Bormann, Jayne; Driscoll, Neal; Harding, Alistair; Kent, Graham; Wesnousky, Steve (7 March 2017). "Seismic constraints on the architecture of the Newport-Inglewood/Rose Canyon fault: Implications for the length and magnitude of future earthquake ruptures". Journal of Geophysical Research: Solid Earth. 122: 2085–2105. doi:10.1002/2016JB013467. Retrieved 1 January 2024.
SONGS (December 2012). Paleoseismic Assessment of the Late Holocene Rupture History of the Rose Canyon Fault in San Diego (PDF) (Report). San Onofre Nuclear Generating Station. Archived from the original (PDF) on 15 September 2017. Retrieved 31 December 2023.

External links

Faults and Earthquakes in San Diego County – San Diego Natural History Museum

[7] The Southern California Earthquake Center has the fault at 30km,^[4] A 2010 paper by Thomas Rockwell has it at 40km,^[5] and a 1997 book by Glenn Roquemore has the length at 50km.^[6]

[FOOTNOTEBormannKent2-1] Bormann & Kent, p. 2.

[FOOTNOTELiuWangLi20101-2] Liu, Wang & Li 2010, p. 1.

[FOOTNOTEMaloneyLeggNicholsonRockwell6-3] Maloney et al., p. 6.

[SCEC-4] "Rose Canyon Fault Zone". Southern California Earthquake Center. Southern California Earthquake Center. Archived from the original on 16 July 2011. Retrieved 31 December 2023.

[FOOTNOTERockwell20109-5] Rockwell 2010, p. 9.

[FOOTNOTERoquemore1997-6] Roquemore 1997.

[FOOTNOTELindvallRockwell199510-8] Lindvall & Rockwell 1995, p. 10.

[FOOTNOTESahakianBormannDriscollHarding2017-9] Sahakian et al. 2017.

[FOOTNOTERockwellSingleton20182-10] Rockwell & Singleton 2018, p. 2.

[FOOTNOTESONGS20122-11] SONGS 2012, p. 2.

[FOOTNOTEAbbottElliott197929-12] Abbott & Elliott 1979, p. 29.

[FOOTNOTEMaloneyLeggNicholsonRockwell7-13] Maloney et al., p. 7.

[FOOTNOTERockwellSingleton20184-14] Rockwell & Singleton 2018, p. 4.

[FOOTNOTELindvallRockwell19951-15] Lindvall & Rockwell 1995, p. 1.

[FOOTNOTERockwellSingleton20183-4-16] Rockwell & Singleton 2018, p. 3-4.

[FOOTNOTEGrantRockwell2002-17] Grant & Rockwell 2002.

[FOOTNOTEAbbottElliott197941-18] Abbott & Elliott 1979, p. 41.

[FOOTNOTEAndersonRockwellAgnew198910-19] Anderson, Rockwell & Agnew 1989, p. 10.

[FOOTNOTERoquemore199712-20] Roquemore 1997, p. 12.

[FOOTNOTEDe_Wyze20006-21] De Wyze 2000, p. 6.

[FOOTNOTERoquemore19978-22] Roquemore 1997, p. 8.

[FOOTNOTELindvallRockwell19959-23] Lindvall & Rockwell 1995, p. 9.

[FOOTNOTEDe_Wyze20005-24] De Wyze 2000, p. 5.

[FOOTNOTELin_II2020-25] Lin II 2020.

[FOOTNOTEEERI202034-26] EERI 2020, p. 34.

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@@ Line 1: / Line 1: @@
+{{Short description|Seismic fault in Southern California}}
-'''Rose Canyon Fault''' is a right-lateral [[strike-slip fault]] running in a north-south direction through [[San Diego County]], California.<ref name="scec">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, "[http://www.data.scec.org/fault_index/rosecany.html]" March 2, 2010</ref> 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> Not much is known about this fault at present,{{When|date=August 2013}} though its slip-rate is thought to be 1.1&nbsp;mm/year.<ref name="scec" /> 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.<ref name="SONGSreport">Southern California Edison, Paleoseismic Assessment of the Late Holocene Rupture History of
+{{good article}}
-the Rose Canyon Fault in San Diego, December, 2012 "[http://www.songscommunity.com/docs/Paleoseismic_Trenching.pdf]"</ref> The Rose Canyon Fault has recently{{When|date=August 2013}} garnered more attention because it runs through such highly populated areas, but is not thought to be much of a threat. However, some [[geophysics|geophysicists]], such as San Diego local Jeff Babcock, have hypothesized that a concentrated [[earthquake]] involving the Rose Canyon, Oceanside, and [[Newport-Inglewood fault]]s could result in an earthquake up to magnitude 7.6 on the [[moment magnitude scale]].<ref name="findingfaults" />
+{{Infobox fault
+| name              = Rose Canyon Fault
+| other_name        = Rose Canyon Fault Zone, Newport Inglewood-Rose Canyon Fault Zone, Newport Inglewood-Rose Canyon-Vallecitos-San Miguel Fault Zone, Newport Inglewood-Rose Canyon-Descanso-Agua Blanca Fault Zone
+| namedfor          = Rose Canyon
+| namedby           =
+| yeardef           =
+| image             = Borderlands active faults page.jpg
+| image_size        =
+| image_alt         =
+| image_caption     = The Rose Canyon Fault is located at the bottom right of the map
+| pushpin_map       =
+| pushpin_map_width =
+| pushpin_map_caption =
+| pushpin_map_alt   =
+| pushpin_relief    =
+| pushpin_map_label =
+| pushpin_label_position =
+| pushpin_mark      =
+| pushpin_mark_size =
+| location          = Onshore and offshore San Diego
+| country           = United States
+| region            =
+| state             = California
+| cities            =
+| coordinates       =
+| elevation         =
+| elevation_m       =
+| elevation_ft      =
+| elevation_ref     =
+| topdepth_m        =
+| topdepth_ft       =
+| topdepth_ref      =
+| range             =
+| part_of           = [[California Continental Borderland]]
+| segments          =
+| length            = ~{{convert|30-170|km|abbr=on}}
+| width             =
+| depth             =
+| strike            =
+| dip               =
+| dip_angle         =
+| displacement      =
+| plate             =
+| status            =
+| earthquakes       = 1862 San Diego earthquake
+| type              = Right-lateral [[Fault (geology)#Strike-slip faults|strike-slip]]
+| movement          =
+| rockunit          =
+| age               =
+| orogeny           =
+| volcanic_arc/belt =
+| map_image         =
+| map_caption       =
+| embed             =
+}}
+[[File:Rose Canyon Fault.png|thumbnail|Rose Canyon Fault Map]]
+The '''Rose Canyon Fault''' is a right-lateral [[Fault (geology)#Strike-slip faults|strike-slip]] fault that runs in a north–south direction off the coast of [[San Diego County]], [[California]]  until it comes ashore near downtown [[San Diego]]. The fault is linked to the [[Newport–Inglewood Fault]] (NIFZ) in the north and either the [[Agua Blanca Fault]] or [[San Miguel–Vallecitos Fault Zone]] in the south via en echelon [[Strike-slip tectonics#Stepovers|step overs]]. Conservative estimates of the fault place the length around {{convert|30–50|km|abbr=on}}, while interpretations including the NIFZ place the length at {{convert|170|km|abbr=on}}. There are not many earthquakes associated with the fault, however a magnitude 6–6.5 may have struck on the fault in 1862. The fault runs very near to populated areas when offshore, hence there is high potential for infrequent large and damaging earthquakes.
+== Tectonic setting ==
+[[Southern California]] lies along a [[transform boundary]] between the [[Pacific Plate]] and [[North American Plate]]. Faulting is taken up by three main groups of faults: the [[San Andreas Fault]] and linked faults, the [[Eastern California Shear Zone]] (ECSZ), and the [[California Continental Borderland]] (CCB). The San Andreas system and the ECSZ take up around 85% of the deformation, while the CCB accommodates the rest.{{sfn|Bormann|Kent|p=2}}{{sfn|Liu|Wang|Li|2010|p=1}} The CCB is itself split into the Inner (ICB) and Outer Continental Borderlands. The ICB takes up ~{{convert|6-8|mm|abbr=on}} of the plate boundary's slip, with the Rose Canyon Fault being one of the most hazardous faults in the ICB system.{{sfn|Bormann|Kent|p=2}}{{sfn|Maloney|Legg|Nicholson|Rockwell|p=6}}
+== Fault characteristics ==
+The right-lateral [[Strike-slip tectonics|strike-slip]] fault extends for {{convert|30–50|km|abbr=on}} and slips at a rate of {{convert|1.1–2|mm|abbr=on}}/yr.{{refn|group=note|The Southern California Earthquake Center has the fault at 30km,<ref name="SCEC"/> A 2010 paper by Thomas Rockwell has it at 40km,{{sfn|Rockwell|2010|p=9}} and a 1997 book by Glenn Roquemore has the length at 50km.{{sfn|Roquemore|1997}}}}<ref name="SCEC"/>{{sfn|Lindvall|Rockwell|1995|p=10}} The fault begins in the [[San Diego Bay]], then runs through [[La Jolla]] before turning offshore. It extends north paralleling the coastline before connecting with the [[Newport-Inglewood Fault]] via short en echelon [[Strike-slip tectonics#Stepovers|step overs]], and the two faults together extend for {{convert|170|km|abbr=on}}.{{sfn|Sahakian|Bormann|Driscoll|Harding|2017}}{{sfn|Rockwell|Singleton|2018|p=2}}
+=== Southern terminus ===
+The southern terminus of the Rose Canyon Fault Zone has not been conclusively determined, and is considered to connect to the Descanso and Agua Blanca Faults and/or the San Miguel–Vallecitos Fault Zone.{{sfn|SONGS|2012|p=2}}{{sfn|Abbott|Elliott|1979|p=29}} Researchers have suggested that both of these faults may transfer slip to the Rose Canyon Fault via San Diego Bay step overs, however no clear connection has been determined.{{sfn|Maloney|Legg|Nicholson|Rockwell|p=7}} Around the San Diego Bay, the fault splays out into many different strands, such as the Silver Strand and Spanish Bight faults.{{sfn|Rockwell|Singleton|2018|p=4}}{{sfn|Lindvall|Rockwell|1995|p=1}} Some of these splay faults come very close to the Descanso Fault, which in turn links with the Agua Blanca Fault. This leads certain researchers to consider these faults interconnected as one major fault zone, the Newport Inglewood–Rose Canyon–Descanso–Agua Blanca Fault Zone.{{sfn|SONGS|2012|p=2}}{{sfn|Rockwell|Singleton|2018|p=3-4}}{{sfn|Grant|Rockwell|2002}} Others favor an interpretation which links the Rose Canyon to the San Miguel-Vallecitos Fault Zone, though just like with the Descanso and Agua Blanca faults, there are no visible faults connecting the two.{{sfn|Maloney|Legg|Nicholson|Rockwell|p=7}} Other researchers attempting to determine which of the two faults the Rose Canyon connects to in the south provide evidence for both faults having a potential link.{{sfn|Abbott|Elliott|1979|p=41}}{{sfn|Anderson|Rockwell|Agnew|1989|p=10}}{{sfn|Roquemore|1997|p=12}}
+== Seismic activity ==
+The Rose Canyon Fault has little associated historic seismicity, however a magnitude 6–6.5 earthquake in 1862 is often attributed to it.{{sfn|De Wyze|2000|p=6}} The shock was assigned a [[Modified Mercalli intensity scale|Modified Mercalli intensity]] shaking of VII (''Very strong''). Shaking was widespread and felt in [[Los Angeles]] (over {{cvt|100|mi|abbr=on}} away). However, due to the lack of reports in the area, it is not possible to guarantee that this earthquake occurred on the Rose Canyon Fault.{{sfn|Roquemore|1997|p=8}} [[Paleoseismology#Paleoseismic trenching|Trenching]] of the fault reveals multiple ruptures within the past 8,100 years, including a rupture that occurred between 300 years to shortly before the [[San Diego Mission]] was established.{{sfn|Lindvall|Rockwell|1995|p=9}} Some of these historic ruptures have an estimated magnitude of 7–7.3.{{sfn|De Wyze|2000|p=5}}
+== Future hazard ==
+The Rose Canyon Fault Zone can produce large earthquakes which can be very destructive due to its proximity to major population centers in [[Southern California]].{{sfn|Sahakian|Bormann|Driscoll|Harding|2017}} On the fault, earthquakes nearing magnitude 7 have a recurrence interval between 700±400{{sfn|Lin II|2020}} and 2,000 years.{{sfn|De Wyze|2000|p=5}} Scenarios modeling a magnitude 6.9 earthquake predict [[peak ground acceleration]] will reach 0.55 [[Spectral acceleration|''g'']] in San Diego, and 0.35 ''g'' in [[Tijuana]]. [[Downtown San Diego]] and [[Mission Bay (San Diego)|Mission Bay]] will experience [[liquefaction]], while [[Mt. Soledad]] may experience [[landslides]]. Coastal areas such as La Jolla and [[Point Loma]] may experience localized coastal bluff failures, and submarine canyons may have landslides which trigger [[tsunami]].{{sfn|EERI|2020|p=34}} Other studies link the Rose Canyon Fault with the Newport-Inglewood, and the combined fault zone can produce M7.3–7.4 earthquakes.{{sfn|Sahakian|Bormann|Driscoll|Harding|2017}}
+== Notes ==
+{{reflist|group=note}}
 == References ==
+{{Reflist|refs=
-<!--- See [[Wikipedia:Footnotes]] on how to create references using <ref></ref> tags which will then appear here automatically -->
+<ref name="SCEC">{{cite web |title=Rose Canyon Fault Zone |url=http://www.data.scec.org/fault_index/rosecany.html |website=Southern California Earthquake Center |publisher=Southern California Earthquake Center |access-date=31 December 2023 |archive-url=https://web.archive.org/web/20110716131700/http://www.data.scec.org/fault_index/rosecany.html |archive-date=16 July 2011 |url-status=dead}}</ref>
-{{Reflist}}
+}}
+'''Sources'''
+{{refbegin}}
+* {{cite book |last1=Abbott |first1=Patrick L. |last2=Elliott |first2=William J. |editor-last1=Legg |editor-first1=Mark R. |editor-last2=Kennedy |editor-first2=Michael P. |title=Earthquakes and other perils—San Diego region |date=November 1979 |publisher=San Diego Association of Geologists Guidebook |url=https://www.nrc.gov/docs/ML1929/ML19290D444.pdf |access-date=31 December 2023 |chapter=Faulting offshore San Diego and northern Baja California}}
+* {{cite journal |last1=Anderson |first1=John G. |last2=Rockwell |first2=Thomas K. |last3=Agnew |first3=Duncan Carr |title=Past and Possible Future Earthquakes of Significance to the San Diego Region |journal=Earthquake Spectra |date=May 1989 |volume=5 |issue=2 |pages=299–335 |doi=10.1193/1.1585524 |url=https://pubs.geoscienceworld.org/earthquake-spectra/article-abstract/5/2/299/584325/Past-and-Possible-Future-Earthquakes-of |access-date=1 January 2024}}
+* {{cite report |last1=Bormann |first1=Jayne |last2=Kent |first2=Graham |title=Investigating recent deformation along the southern San Pedro Basin fault to assess evidence for connectivity between the San Pedro Basin and San Diego Trough fault systems |publisher=U.S. Geological Survey |url=https://earthquake.usgs.gov/cfusion/external_grants/reports/G17AP00124.pdf |access-date=27 December 2023}}
+* {{cite news |last=De Wyze |first=Jeannete |date=2 March 2000 |title=Earthquake San Diego Danger Zones |url=http://webshaker.ucsd.edu/homework/EarthquakeSanDiegoDangerZones.pdf |newspaper=San Diego Reader |access-date=1 January 2024}}
+* {{Cite report |title=San Diego Earthquake Planning Scenario |date=2020 |url=https://sandiego.eeri.org/wp-content/uploads/2020/03/EERI-San-Diego-Scenario-2020.pdf |last=EERI |access-date=1 January 2024}}
+* {{cite journal |last1=Grant |first1=Lisa B. |last2=Rockwell |first2=Thomas K. |title=A Northward-propagating Earthquake Sequence in Coastal Southern California? |journal=Seismological Research Letters |date=2002 |volume=73 |issue=4 |doi=10.1785/GSSRL.73.4.461 |url=https://www.academia.edu/18351510/A_Northward_propagating_Earthquake_Sequence_in_Coastal_Southern_California |access-date=1 January 2024}}
+* {{cite news |last1=Lin II |first1=Rong-Gong |title=San Diego faces critical earthquake danger from fault long believed to be inactive |url=https://www.latimes.com/california/story/2020-03-04/san-diego-earthquake-fault-danger |access-date=1 January 2024 |work=LA Times |date=4 March 2020}}
+* {{cite journal |last1=Lindvall |first1=Scott C. |last2=Rockwell |first2=Thomas K. |title=Holocene activity of the Rose Canyon fault zone in San Diego, California |journal=Journal of Geophysical Research: Solid Earth |date=10 December 1995 |volume=100 |issue=B12 |pages=24121–24132 |doi=10.1029/95JB02627 |url=https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/95JB02627 |access-date=31 December 2023}}
+* {{cite journal |last1=Liu |first1=Mian |last2=Wang |first2=Hui |last3=Li |first3=Qingsong |title=Inception of the eastern California shear zone and evolution of the Pacific-North American plate boundary: From kinematics to geodynamics |journal=Journal of Geophysical Research |date=7 July 2010 |volume=115 |issue=B7 |doi=10.1029/2009JB007055 |bibcode=2010JGRB..115.7401L |url=https://doi.org/10.1029/2009JB007055 |access-date=30 December 2023}}
+* {{cite web |last1=Maloney |first1=Jillian M. |last2=Legg |first2=Mark |last3=Nicholson |first3=Craig |last4=Rockwell |first4=Thomas K. |title=White Paper: The California continental borderland |url=https://files.scec.org/s3fs-public/whitepapers/2020/Whitepaper_2020_Borderland.pdf?v=2 |website=Southern California Earthquake Center |access-date=30 December 2023}}
+* {{Cite report |title=Mid to Late Holocene Rupture History of the Rose Canyon Fault in San Diego, California |date=April 2018 |url=https://earthquake.usgs.gov/cfusion/external_grants/reports/G16AP00015.pdf |last=Rockwell |first=Thomas K. |access-date=30 December 2023 |last2=Singleton |first2=Drake}}
+* {{Cite conference |title=The Rose Canyon Fault Zone in San Diego |conference=International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics |url=https://scholarsmine.mst.edu/cgi/viewcontent.cgi?article=2907&context=icrageesd |last=Rockwell |first=Thomas K. |date=28 May 2010 |access-date=31 December 2023}}
+* {{cite book |last1=Roquemore |first1=Glenn |title=The Seismic Risk in the San Diego Region: Special Focus on the Rose Canyon Fault Systems: Workshop Proceedings|url=https://books.google.com/books?id=YjnXWTMc4eMC&pg=PA6|date=1 April 1997|publisher=DIANE Publishing|isbn=978-0-7881-4262-8}}
+* {{cite journal |last1=Sahakian |first1=Valerie |last2=Bormann |first2=Jayne |last3=Driscoll |first3=Neal |last4=Harding |first4=Alistair |last5=Kent |first5=Graham |last6=Wesnousky |first6=Steve |title=Seismic constraints on the architecture of the Newport-Inglewood/Rose Canyon fault: Implications for the length and magnitude of future earthquake ruptures |journal=Journal of Geophysical Research: Solid Earth |date=7 March 2017 |volume=122 |pages=2085–2105 |doi=10.1002/2016JB013467 |url=https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2016JB013467 |access-date=1 January 2024|doi-access=free }}
+* {{Cite report |title=Paleoseismic Assessment of the Late Holocene Rupture History of the Rose Canyon Fault in San Diego |date=December 2012 |url=http://www.songscommunity.com/docs/Paleoseismic_Trenching.pdf |last=SONGS |access-date=31 December 2023 |publisher=San Onofre Nuclear Generating Station |url-status=dead |archive-url=https://web.archive.org/web/20170915114713/http://www.songscommunity.com/docs/Paleoseismic_Trenching.pdf |archive-date=15 September 2017}}
+{{refend}}
+==Further reading==
+* {{cite book |last=Kennedy |first=Michael P. |date=1975 |title=Geology of the San Diego metropolitan area, California |url=https://archive.org/details/geologyofsandieg00kennrich |publisher=California Division of Mines and Geology }}
 == External links ==
-* [http://www.sdnhm.org/archive/research/paleontology/sdfaults.html Faults and Earthquakes in San Diego County]-
+* [http://www.sdnhm.org/archive/research/paleontology/sdfaults.html Faults and Earthquakes in San Diego County] – [[San Diego Natural History Museum]]
-{{-}}
 {{California Faults}}
 {{Faults}}
@@ Line 15: / Line 112: @@
 [[Category:Seismic faults of California]]
 [[Category:Geology of San Diego County, California]]
+[[Category:La Jolla, San Diego]]
+[[Category:Mission Valley, San Diego]]

v t e Seismically active fault zones and tectonic blocks of California
Statewide Faults	San Andreas Fault Salinian Block
Southern California	Brawley Seismic Zone Chino Fault Elsinore Fault Zone Elysian Park Fault Garlock Fault Hollywood fault Hosgri Fault Imperial Fault Zone Laguna Salada Fault Newport–Inglewood Fault Northridge Blind Thrust Fault Peninsular Ranges Puente Hills Fault Raymond Fault Rose Canyon Fault Salton Trough San Cayetano Fault San Diego Trough Fault Zone San Felipe Fault Zone San Gabriel Fault San Jacinto Fault Zone Santa Maria River Fault Santa Ynez Fault Shoreline Fault Sierra Madre Fault Zone Ventura Fault White Wolf Fault Whittier Fault Yorba Linda Fault
Northern California	Bartlett Springs Fault Calaveras Fault Clayton-Marsh Creek-Greenville Fault Concord Fault Hayward Fault Zone Healdsburg Fault Maacama Fault Mendocino Fracture Zone Mendocino Triple Junction Mount Diablo Thrust Fault Monta Vista Fault Nacimiento Fault Pleasanton Fault Rinconada Fault San Gregorio Fault San Pablo Fault Seal Cove Fault Serra Fault Silver Creek Fault Tesla Fault West Napa Fault
Sierra Nevada	Death Valley Fault Zone Furnace Creek Fault Zone Honey Lake Fault Zone Kern Canyon Fault Maria fold and thrust belt Owens Valley Fault Rescue Lineament-Bear Mountains fault zone Sierra Nevada Batholith Sierra Nevada Fault Sierra Nevada-Great Valley Block Smartville Block Walker Lane
Kategorie California Geological Survey Seismic Hazards Mapping Act Mexico (list)