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Brawley Seismic Zone

January 01, 1970

The Brawley Seismic Zone (BSZ), also known as the Brawley fault zone, is a predominantly extensional tectonic zone that connects the southern terminus of the San Andreas Fault with the Imperial Fault in Southern California.[1] The BSZ is named for the nearby town of Brawley in Imperial County, California, and the seismicity there is characterized by earthquake swarms.

class=notpageimage|
Brawley Seismic Zone and surrounding area. The red lines are simplified faults. Right-lateral direction of motion of the transform fault is shown (pink arrows). The red rhombs are pull-apart basins; the northern one is the site of the Niland geothermal field, the southern the Cerro Prieto geothermal field.

Geology edit

See also: Extensional tectonics

The Brawley Seismic Zone represents the northernmost extension of the spreading center axis associated with the East Pacific Rise which runs up the axis of the Gulf of California and is in the process of rifting the Baja California Peninsula away from the mainland of Mexico, with significant subsidence taking place at southern California's Salton Sea and at Laguna Salada in Baja California. Other major locations along the axis include the Cerro Prieto spreading center located south of Mexicali, and Wagner Basin (a submarine depression in the Gulf of California).[2]

The Salton Buttes on the south shore of the Salton Sea are on the north margin of the Brawley Seismic Zone and are linked to volcanic and geothermal activity within the zone. The Brawley Seismic Zone has been interpreted as an "onshore spreading center" which runs diagonally across the Salton Trough.[1]

Earthquake swarms edit

On August 26, 2012 near Brawley, a swarm of more than 300 small to moderate earthquakes occurred with the largest two reaching a maximum of 5.3 and 5.5. Some light cosmetic damage was found on some older buildings in downtown Brawley. Earthquake swarms are not unusual for the area. In 2005, also near Brawley, there was a swarm with a peak magnitude of 5.1, while in 1981 a swarm included one quake which was measured at 5.8. The swarm activity is not understood completely, but the new restlessness could generate data that will help scientists to gain a better understanding of the region.[3] According to a geologist at the United States Geological Survey (USGS), such swarms are typical for the Brawley zone: "The area sees lots of events at once, with many close to the largest magnitude, rather than one main shock with several much smaller aftershocks."[4]

Other activity edit

See also: List of earthquakes in California

The Imperial Valley of southern California experiences high rates of seismicity with a pronounced portion of the activity occurring within the Brawley Seismic Zone that separates the San Andreas fault to the north and the Imperial fault to the south. The Imperial fault was the source of the 1940 El Centro earthquake and the 1979 Imperial Valley earthquake. There was more than 30 km (19 mi) of surface rupture associated with the 1979 event along the northwest trending Imperial fault from just north of the Mexico–United States border to an area south of Brawley and the BSZ was found to have ruptured, with surface cracks, for a length of 13 km (8.1 mi).[5] The 1940 and 1979 mainshocks were of similar size and both were followed by damaging aftershocks near Brawley.[6]

References edit

  1. ^ a b Fuis, Gary S.; Mooney, Walter D. (1990), "Lithospheric structure and tectonics from seismic-refraction and other data", The San Andreas Fault System, California, Geological Survey Professional Paper 1515, United States Geological Survey, pp. 207–236
  2. ^ David L. Alles (2011). "Geology of the Salton Trough" (PDF). Western Washington University. Retrieved September 30, 2012.
  3. ^ Sewell, Abby (August 26, 2012). ""Earthquake storm" continues to rattle Imperial County, surrounding areas". Los Angeles Times. Retrieved August 26, 2012.
  4. ^ Associated Press (August 26, 2012). "Series of earthquakes rattle Southern California" The Oklahoman
  5. ^ Larsen, Shawn; Reilinger, Robert (1991). "Age constraints for the present fault configuration in the Imperial Valley, California – Evidence for northwestward propagation of the Gulf of California rift system". Journal of Geophysical Research. 96 (B6). American Geophysical Union: 10, 339–10, 340. Bibcode:1991JGR....9610339L. doi:10.1029/91jb00618. hdl:2060/19900012177.
  6. ^ Bolt, Bruce (August 2005), Earthquakes: 2006 Centennial Update – The 1906 Big One (Fifth ed.), W. H. Freeman and Company, p. 61, ISBN 978-0716775485

Sources

  • Hauksson, E.; Stock, J.; Bilham, R.; Boese, M.; Chen, X.; Fielding, E. J.; Galetzka, J.; Hudnut, K. W.; Hutton, K.; Jones, L. M.; Kanamori, H.; Shearer, P. M.; Steidl, J.; Treiman, J.; Weia, S.; Yang, W. (March–April 2013), "Report on the August 2012 Brawley Earthquake Swarm in Imperial Valley, Southern California" (PDF), Seismological Research Letters, 84 (2), Seismological Society of America: 177–189, doi:10.1785/0220120169
  • Meltzner, A J.; Rockwell, T. K.; Owen, L. A. (2006), "Recent and long-term behavior of the Brawley Fault Zone, Imperial Valley, California: An escalation of slip rate?" (PDF), Bulletin of the Seismological Society of America, 96 (6), Seismological Society of America: 2304–2328, Bibcode:2006BuSSA..96.2304M, doi:10.1785/0120050233

External links edit

January 01, 1970
brawley, seismic, zone, also, known, brawley, fault, zone, predominantly, extensional, tectonic, zone, that, connects, southern, terminus, andreas, fault, with, imperial, fault, southern, california, named, nearby, town, brawley, imperial, county, california, . The Brawley Seismic Zone BSZ also known as the Brawley fault zone is a predominantly extensional tectonic zone that connects the southern terminus of the San Andreas Fault with the Imperial Fault in Southern California 1 The BSZ is named for the nearby town of Brawley in Imperial County California and the seismicity there is characterized by earthquake swarms Los AngelesSan DiegoMexicaliSalton SeaTijuanaAlamo River mouthColorado River mouthLaguna SaladaYumaGulf of CaliforniaColorado River ValleyCerro Prieto volcanoclass notpageimage Brawley Seismic Zone and surrounding area The red lines are simplified faults Right lateral direction of motion of the transform fault is shown pink arrows The red rhombs are pull apart basins the northern one is the site of the Niland geothermal field the southern the Cerro Prieto geothermal field Contents 1 Geology 2 Earthquake swarms 3 Other activity 4 References 5 External linksGeology editSee also Extensional tectonics The Brawley Seismic Zone represents the northernmost extension of the spreading center axis associated with the East Pacific Rise which runs up the axis of the Gulf of California and is in the process of rifting the Baja California Peninsula away from the mainland of Mexico with significant subsidence taking place at southern California s Salton Sea and at Laguna Salada in Baja California Other major locations along the axis include the Cerro Prieto spreading center located south of Mexicali and Wagner Basin a submarine depression in the Gulf of California 2 The Salton Buttes on the south shore of the Salton Sea are on the north margin of the Brawley Seismic Zone and are linked to volcanic and geothermal activity within the zone The Brawley Seismic Zone has been interpreted as an onshore spreading center which runs diagonally across the Salton Trough 1 Earthquake swarms editOn August 26 2012 near Brawley a swarm of more than 300 small to moderate earthquakes occurred with the largest two reaching a maximum of 5 3 and 5 5 Some light cosmetic damage was found on some older buildings in downtown Brawley Earthquake swarms are not unusual for the area In 2005 also near Brawley there was a swarm with a peak magnitude of 5 1 while in 1981 a swarm included one quake which was measured at 5 8 The swarm activity is not understood completely but the new restlessness could generate data that will help scientists to gain a better understanding of the region 3 According to a geologist at the United States Geological Survey USGS such swarms are typical for the Brawley zone The area sees lots of events at once with many close to the largest magnitude rather than one main shock with several much smaller aftershocks 4 Other activity editSee also List of earthquakes in California The Imperial Valley of southern California experiences high rates of seismicity with a pronounced portion of the activity occurring within the Brawley Seismic Zone that separates the San Andreas fault to the north and the Imperial fault to the south The Imperial fault was the source of the 1940 El Centro earthquake and the 1979 Imperial Valley earthquake There was more than 30 km 19 mi of surface rupture associated with the 1979 event along the northwest trending Imperial fault from just north of the Mexico United States border to an area south of Brawley and the BSZ was found to have ruptured with surface cracks for a length of 13 km 8 1 mi 5 The 1940 and 1979 mainshocks were of similar size and both were followed by damaging aftershocks near Brawley 6 References edit a b Fuis Gary S Mooney Walter D 1990 Lithospheric structure and tectonics from seismic refraction and other data The San Andreas Fault System California Geological Survey Professional Paper 1515 United States Geological Survey pp 207 236 David L Alles 2011 Geology of the Salton Trough PDF Western Washington University Retrieved September 30 2012 Sewell Abby August 26 2012 Earthquake storm continues to rattle Imperial County surrounding areas Los Angeles Times Retrieved August 26 2012 Associated Press August 26 2012 Series of earthquakes rattle Southern California The Oklahoman Larsen Shawn Reilinger Robert 1991 Age constraints for the present fault configuration in the Imperial Valley California Evidence for northwestward propagation of the Gulf of California rift system Journal of Geophysical Research 96 B6 American Geophysical Union 10 339 10 340 Bibcode 1991JGR 9610339L doi 10 1029 91jb00618 hdl 2060 19900012177 Bolt Bruce August 2005 Earthquakes 2006 Centennial Update The 1906 Big One Fifth ed W H Freeman and Company p 61 ISBN 978 0716775485 Sources Hauksson E Stock J Bilham R Boese M Chen X Fielding E J Galetzka J Hudnut K W Hutton K Jones L M Kanamori H Shearer P M Steidl J Treiman J Weia S Yang W March April 2013 Report on the August 2012 Brawley Earthquake Swarm in Imperial Valley Southern California PDF Seismological Research Letters 84 2 Seismological Society of America 177 189 doi 10 1785 0220120169 Meltzner A J Rockwell T K Owen L A 2006 Recent and long term behavior of the Brawley Fault Zone Imperial Valley California An escalation of slip rate PDF Bulletin of the Seismological Society of America 96 6 Seismological Society of America 2304 2328 Bibcode 2006BuSSA 96 2304M doi 10 1785 0120050233External links editFault History and Architecture of the Southernmost San Andreas Fault and Brawley Seismic Zone New Constraints from CHIRP Data Acquired in the Salton Sea American Geophysical Union Fall Meeting 2006 List of all events for Brawley Swarm Southern California Seismic Network August 2012 Brawley California Earthquake Swarm United States Geological Survey Retrieved from https en wikipedia org w index php title Brawley Seismic Zone amp oldid 1154267135, wikipedia, wiki, book, books, library,

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