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Intraplate earthquake

October 22, 2023

The term intraplate earthquake refers to a variety of earthquake that occurs within the interior of a tectonic plate; this stands in contrast to an interplate earthquake, which occurs at the boundary of a tectonic plate. Intraplate earthquakes are often called "intraslab earthquakes," especially when occurring in microplates.[1][2]

Distribution of seismicity associated with the New Madrid Seismic Zone (since 1974). This zone of intense earthquake activity is located deep within the interior of the North American plate.

Intraplate earthquakes are relatively rare compared to the more familiar boundary-located interplate earthquakes. Structures far from plate boundaries tend to lack seismic retrofitting, so large intraplate earthquakes can inflict heavy damage. Examples of damaging intraplate earthquakes are the devastating Gujarat earthquake in 2001, the 2012 Indian Ocean earthquakes, the 2017 Puebla earthquake, the 1811–1812 earthquakes in New Madrid, Missouri, and the 1886 earthquake in Charleston, South Carolina.[3]

Fault zones within tectonic plates Edit

The surface of the Earth is made up of seven primary and eight secondary tectonic plates, plus dozens of tertiary microplates. The large plates move very slowly, owing to convection currents within the mantle below the crust. Because they do not all move in the same direction, plates often directly collide or move laterally along each other, a tectonic environment that makes earthquakes frequent. Relatively few earthquakes occur in intraplate environments; most occur on faults near plate margins.

By definition, intraplate earthquakes do not occur near plate boundaries, but along faults in the normally stable interior of plates.[4] These earthquakes often occur at the location of ancient failed rifts, because such old structures may present a weakness in the crust where it can easily slip to accommodate regional tectonic strain.

Compared to earthquakes near plate boundaries (megathrust earthquakes), intraslab earthquakes at a similar magnitude radiate more seismic energy. Thus "seismic energy" is considered a better measure for the potential macroseismic effects of an earthquake as compared to the seismic moment used to calculate M w."[5]

Examples Edit

Examples of intraplate earthquakes include those in Mineral, Virginia in 2011 (estimated magnitude 5.8), Newcastle, New South Wales in 1989, New Madrid in 1811 and 1812 (estimated magnitude as high as 8.6),[6] the Boston (Cape Ann) earthquake of 1755 (estimated magnitude 6.0 to 6.3), earthquakes felt in New York City in 1737 and 1884 (both quakes estimated at about 5.5 magnitude), and the Charleston earthquake in South Carolina in 1886 (estimated magnitude 6.5 to 7.3). The Charleston quake was particularly surprising because, unlike Boston and New York, the area had almost no history of even minor earthquakes.

In 2001, a large intraplate earthquake devastated the region of Gujarat, India. The earthquake occurred far from any plate boundaries, which meant the region above the epicenter was unprepared for earthquakes. In particular, the Kutch district suffered tremendous damage, where the death toll was over 12,000 and the total death toll was higher than 20,000.

In 2017, the 24–29 km deep magnitude 6.5 Botswana earthquake that shook eastern Botswana occurred at over 300 km from the nearest active plate boundary.[7] The event occurred in an underpopulated area of Botswana.

The 1888 earthquake in Río de la Plata was an intraplate quake,[8] from reactivated faults in the Quilmes Trough, far from the boundaries of the South American Plate. With a magnitude greater than 5.0 it was felt "in the cities of Buenos Aires, La Plata and other small towns and villages along the Rio de Plata coastal regions."[9] The towns of Punta del Este and Maldonado in Uruguay were hit by a tsunami generated by the quake.[9]

Causes Edit

Many cities live with the seismic risk of a rare, large intraplate earthquake. The cause of these earthquakes is often uncertain. In many cases, the causative fault is deeply buried,[7] and sometimes cannot even be found. Some studies have shown that it can be caused by fluids moving up the crust along ancient fault zones.[7][10] In such circumstances, it is difficult to calculate the exact seismic hazard for a given city, especially if there was only one earthquake in historical times. Some progress is being made in understanding the fault mechanics driving these earthquakes.

Intraplate earthquakes may be unrelated to ancient fault zones and instead caused by deglaciation or erosion.[11]

Prediction Edit

Scientists continue to search for the causes of these earthquakes, and especially for some indication of how often they recur. The best success has come with detailed micro-seismic monitoring, involving dense arrays of seismometers. In this manner, very small earthquakes associated with a causative fault can be located with great accuracy, and in most cases these line up in patterns consistent with faulting. Cryoseisms can sometimes be mistaken for intraplate earthquakes.

See also Edit

References Edit

  1. ^ Iwata, Tomotaka; Asano, Kimiyuki (2011). "Characterization of the Heterogeneous Source Model of Intraslab Earthquakes Toward Strong Ground Motion Prediction". Pure and Applied Geophysics. 168 (1–2): 117–124. doi:10.1007/s00024-010-0128-7. S2CID 140602323.
  2. ^ Senoa, Tetsuzo; Yoshida, Masaki (2004). "Where and why do large shallow intraslab earthquakes occur?". Physics of the Earth and Planetary Interiors. 141 (3): 183–206. doi:10.1016/j.pepi.2003.11.002.
  3. ^ Hough, Susan E.; Seeber, Leonardo; Armbruster, John G. (October 2003). "Intraplate Triggered Earthquakes: Observations and Interpretation". Bulletin of the Seismological Society of America. Seismological Society of America. 101 (3): 2212–2221. Bibcode:2003BuSSA..93.2212H. CiteSeerX 10.1.1.189.5055. doi:10.1785/0120020055.
  4. ^ Yang, Xiaotao (2014). "Seismicity of the Ste. Genevieve Seismic Zone based on Observations from the EarthScope OIINK Flexible Array". Seismological Research Letters. 85 (6): 1285–1294. doi:10.1785/0220140079.
  5. ^ Leyton, Felipe; Ruiz, Javier A.; Camposa, Jaime; Kausel, Edgar (2009). "Intraplate and interplate earthquakes in Chilean subduction zone: A theoretical and observational comparison". Physics of the Earth and Planetary Interiors. 175 (1): 37–46. doi:10.1016/j.pepi.2008.03.017. citing Choy, G.L.; Boatwright, J.; Kirby, S., 2002. The radiated seismic energy and apparent stress of interplate and intraslab earthquakes at subduction-zone environments: Implications for seismic hazard estimation, in The Cascadia subduction zone and related subduction systems–Seismic structure, intraslab earthquakes and processes, and earthquake hazards, Open-File Report 02–328, pp. 107–114, eds Kirby, S.H.; Wang, K.; Dunlop, S., US Geological Survey, Menlo Park, CA.
  6. ^ Penick, James L. The New Madrid Earthquakes. Columbia, MO: University of Missouri Press, 1981. ISBN 0-8262-0344-2
  7. ^ a b c Kolawole, F.; Atekwana, E. A.; Malloy, S.; Stamps, D. S.; Grandin, R.; Abdelsalam, M. G.; Leseane, K.; Shemang, E. M. (2017-09-09). "Aeromagnetic, gravity, and Differential Interferometric Synthetic Aperture Radar analyses reveal the causative fault of the 3 April 2017 Mw6.5 Moiyabana, Botswana, earthquake". Geophysical Research Letters. 44 (17): 8837–8846. Bibcode:2017GeoRL..44.8837K. doi:10.1002/2017gl074620. ISSN 0094-8276. S2CID 134584787.
  8. ^ Benavídes Sosa, Alberto (1998). "Seismicidad y seismotectónica en Uruguay". Física de la Tierra (in Spanish) (10): 167–186.
  9. ^ a b Rossello, Eduardo Antonio; Heit, Benjamín; Bianchi, Marcelo (2020). "Shallow intraplate seismicity in the Buenos Aires province (Argentina) and surrounding areas: is it related to the Quilmes Trough?". Boletín de Geología. 42 (2): 31–48. doi:10.18273/revbol.v42n2-2020002. S2CID 219934403. from the original on 4 August 2022.
  10. ^ Gardonio, B.; Jolivet, R.; Calais, E.; Leclère, H. (2018-07-13). "The April 2017 Mw6.5 Botswana Earthquake: An Intraplate Event Triggered by Deep Fluids" (PDF). Geophysical Research Letters. 45 (17): 8886–8896. Bibcode:2018GeoRL..45.8886G. doi:10.1029/2018gl078297. ISSN 0094-8276. S2CID 134667492.
  11. ^ Shobe, Charlie (18 December 2018). "Can Rivers Cause Earthquakes?". Scientific American. Retrieved 26 December 2018.

Further reading Edit

  • Stein, S., and S. Mazzotti (2007). "Continental Intraplate Earthquakes: Science and Policy Issues", Geological Society of America, Special Paper 425.

External links Edit

  • Intraplate Earthquakes: Possible Mechanisms for the New Madrid and Charleston Earthquakes
  • Symptomatic Features of Intraplate Earthquakes – PDF
  • Earthquake Hazards Program, USGS

October 22, 2023
intraplate, earthquake, this, article, includes, list, general, references, lacks, sufficient, corresponding, inline, citations, please, help, improve, this, article, introducing, more, precise, citations, august, 2011, learn, when, remove, this, template, mes. This article includes a list of general references but it lacks sufficient corresponding inline citations Please help to improve this article by introducing more precise citations August 2011 Learn how and when to remove this template message The term intraplate earthquake refers to a variety of earthquake that occurs within the interior of a tectonic plate this stands in contrast to an interplate earthquake which occurs at the boundary of a tectonic plate Intraplate earthquakes are often called intraslab earthquakes especially when occurring in microplates 1 2 Distribution of seismicity associated with the New Madrid Seismic Zone since 1974 This zone of intense earthquake activity is located deep within the interior of the North American plate Intraplate earthquakes are relatively rare compared to the more familiar boundary located interplate earthquakes Structures far from plate boundaries tend to lack seismic retrofitting so large intraplate earthquakes can inflict heavy damage Examples of damaging intraplate earthquakes are the devastating Gujarat earthquake in 2001 the 2012 Indian Ocean earthquakes the 2017 Puebla earthquake the 1811 1812 earthquakes in New Madrid Missouri and the 1886 earthquake in Charleston South Carolina 3 Contents 1 Fault zones within tectonic plates 2 Examples 3 Causes 4 Prediction 5 See also 6 References 7 Further reading 8 External linksFault zones within tectonic plates EditThe surface of the Earth is made up of seven primary and eight secondary tectonic plates plus dozens of tertiary microplates The large plates move very slowly owing to convection currents within the mantle below the crust Because they do not all move in the same direction plates often directly collide or move laterally along each other a tectonic environment that makes earthquakes frequent Relatively few earthquakes occur in intraplate environments most occur on faults near plate margins By definition intraplate earthquakes do not occur near plate boundaries but along faults in the normally stable interior of plates 4 These earthquakes often occur at the location of ancient failed rifts because such old structures may present a weakness in the crust where it can easily slip to accommodate regional tectonic strain Compared to earthquakes near plate boundaries megathrust earthquakes intraslab earthquakes at a similar magnitude radiate more seismic energy Thus seismic energy is considered a better measure for the potential macroseismic effects of an earthquake as compared to the seismic moment used to calculate M w 5 Examples EditExamples of intraplate earthquakes include those in Mineral Virginia in 2011 estimated magnitude 5 8 Newcastle New South Wales in 1989 New Madrid in 1811 and 1812 estimated magnitude as high as 8 6 6 the Boston Cape Ann earthquake of 1755 estimated magnitude 6 0 to 6 3 earthquakes felt in New York City in 1737 and 1884 both quakes estimated at about 5 5 magnitude and the Charleston earthquake in South Carolina in 1886 estimated magnitude 6 5 to 7 3 The Charleston quake was particularly surprising because unlike Boston and New York the area had almost no history of even minor earthquakes In 2001 a large intraplate earthquake devastated the region of Gujarat India The earthquake occurred far from any plate boundaries which meant the region above the epicenter was unprepared for earthquakes In particular the Kutch district suffered tremendous damage where the death toll was over 12 000 and the total death toll was higher than 20 000 In 2017 the 24 29 km deep magnitude 6 5 Botswana earthquake that shook eastern Botswana occurred at over 300 km from the nearest active plate boundary 7 The event occurred in an underpopulated area of Botswana The 1888 earthquake in Rio de la Plata was an intraplate quake 8 from reactivated faults in the Quilmes Trough far from the boundaries of the South American Plate With a magnitude greater than 5 0 it was felt in the cities of Buenos Aires La Plata and other small towns and villages along the Rio de Plata coastal regions 9 The towns of Punta del Este and Maldonado in Uruguay were hit by a tsunami generated by the quake 9 Causes EditMany cities live with the seismic risk of a rare large intraplate earthquake The cause of these earthquakes is often uncertain In many cases the causative fault is deeply buried 7 and sometimes cannot even be found Some studies have shown that it can be caused by fluids moving up the crust along ancient fault zones 7 10 In such circumstances it is difficult to calculate the exact seismic hazard for a given city especially if there was only one earthquake in historical times Some progress is being made in understanding the fault mechanics driving these earthquakes Intraplate earthquakes may be unrelated to ancient fault zones and instead caused by deglaciation or erosion 11 Prediction EditScientists continue to search for the causes of these earthquakes and especially for some indication of how often they recur The best success has come with detailed micro seismic monitoring involving dense arrays of seismometers In this manner very small earthquakes associated with a causative fault can be located with great accuracy and in most cases these line up in patterns consistent with faulting Cryoseisms can sometimes be mistaken for intraplate earthquakes See also EditNew Madrid Seismic Zone Major seismic zone in the southern and midwestern United States Wabash Valley Seismic Zone major sesmic zone in Lower Ohio Valley along Wabash River in Illinois and IndianaPages displaying wikidata descriptions as a fallback Saint Lawrence rift system Seismically active zone paralleling the Saint Lawrence RiverReferences Edit Iwata Tomotaka Asano Kimiyuki 2011 Characterization of the Heterogeneous Source Model of Intraslab Earthquakes Toward Strong Ground Motion Prediction Pure and Applied Geophysics 168 1 2 117 124 doi 10 1007 s00024 010 0128 7 S2CID 140602323 Senoa Tetsuzo Yoshida Masaki 2004 Where and why do large shallow intraslab earthquakes occur Physics of the Earth and Planetary Interiors 141 3 183 206 doi 10 1016 j pepi 2003 11 002 Hough Susan E Seeber Leonardo Armbruster John G October 2003 Intraplate Triggered Earthquakes Observations and Interpretation Bulletin of the Seismological Society of America Seismological Society of America 101 3 2212 2221 Bibcode 2003BuSSA 93 2212H CiteSeerX 10 1 1 189 5055 doi 10 1785 0120020055 Yang Xiaotao 2014 Seismicity of the Ste Genevieve Seismic Zone based on Observations from the EarthScope OIINK Flexible Array Seismological Research Letters 85 6 1285 1294 doi 10 1785 0220140079 Leyton Felipe Ruiz Javier A Camposa Jaime Kausel Edgar 2009 Intraplate and interplate earthquakes in Chilean subduction zone A theoretical and observational comparison Physics of the Earth and Planetary Interiors 175 1 37 46 doi 10 1016 j pepi 2008 03 017 citing Choy G L Boatwright J Kirby S 2002 The radiated seismic energy and apparent stress of interplate and intraslab earthquakes at subduction zone environments Implications for seismic hazard estimation in The Cascadia subduction zone and related subduction systems Seismic structure intraslab earthquakes and processes and earthquake hazards Open File Report 02 328 pp 107 114 eds Kirby S H Wang K Dunlop S US Geological Survey Menlo Park CA Penick James L The New Madrid Earthquakes Columbia MO University of Missouri Press 1981 ISBN 0 8262 0344 2 a b c Kolawole F Atekwana E A Malloy S Stamps D S Grandin R Abdelsalam M G Leseane K Shemang E M 2017 09 09 Aeromagnetic gravity and Differential Interferometric Synthetic Aperture Radar analyses reveal the causative fault of the 3 April 2017 Mw6 5 Moiyabana Botswana earthquake Geophysical Research Letters 44 17 8837 8846 Bibcode 2017GeoRL 44 8837K doi 10 1002 2017gl074620 ISSN 0094 8276 S2CID 134584787 Benavides Sosa Alberto 1998 Seismicidad y seismotectonica en Uruguay Fisica de la Tierra in Spanish 10 167 186 a b Rossello Eduardo Antonio Heit Benjamin Bianchi Marcelo 2020 Shallow intraplate seismicity in the Buenos Aires province Argentina and surrounding areas is it related to the Quilmes Trough Boletin de Geologia 42 2 31 48 doi 10 18273 revbol v42n2 2020002 S2CID 219934403 Archived from the original on 4 August 2022 Gardonio B Jolivet R Calais E Leclere H 2018 07 13 The April 2017 Mw6 5 Botswana Earthquake An Intraplate Event Triggered by Deep Fluids PDF Geophysical Research Letters 45 17 8886 8896 Bibcode 2018GeoRL 45 8886G doi 10 1029 2018gl078297 ISSN 0094 8276 S2CID 134667492 Shobe Charlie 18 December 2018 Can Rivers Cause Earthquakes Scientific American Retrieved 26 December 2018 Further reading EditStein S and S Mazzotti 2007 Continental Intraplate Earthquakes Science and Policy Issues Geological Society of America Special Paper 425 External links EditIntraplate Earthquakes Possible Mechanisms for the New Madrid and Charleston Earthquakes Symptomatic Features of Intraplate Earthquakes PDF A physical understanding of large intraplate earthquakes PDF Earthquake Hazards Program USGS Retrieved from https en wikipedia org w index php title Intraplate earthquake amp oldid 1172983084, wikipedia, wiki, book, books, library,

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