2009–16 Oklahoma earthquake swarms
Seismicity map for Oklahoma and nearby areas – Dark blue circles indicate earthquakes from pre-2009 while circles of other colors indicate earthquakes since 2009. | |
Date | 2009–present |
---|---|
Duration | About seven years |
Type | Intraplate earthquakes |
Areas affected |
Central and North-Central Oklahoma South-Central Kansas Dallas–Fort Worth metroplex |
Total damage | Unknown |
Max. intensity | VIII (Severe) (November 5, 2011 Oklahoma earthquake) |
Casualties | Minor injuries associated with November 5, 2011 Oklahoma earthquake |
Greatest magnitude |
|
Mean depth | 5.43 km (3.37 mi) in 2014[1][lower-alpha 1] |
Total events |
>6,810 in OK since January 1, 2009 (USGS)[2] >12,900 in OK since January 2, 2008 (OGS)[3][lower-alpha 2] ≥2,300 in KS since January 1, 2013 (USGS)[4] |
Beginning in 2009, the frequency of earthquakes in the U.S. State of Oklahoma rapidly increased from an average of less than two 3.0+ Mw earthquakes per year to hundreds in 2014 and 2015. Thousands of earthquakes have occurred in Oklahoma and surrounding areas in southern Kansas and North Texas since 2009.[6] Scientific studies attribute the rise in earthquakes to the disposal of salt water produced during oil extraction that has been injected more deeply into the ground.[7][8]
One of the most significant earthquakes of this swarm was a 5.6 magnitude earthquake east of the Oklahoma City area which was the strongest earthquake in the history of Oklahoma.[9] Multiple seismologists advised local residents of an even greater risk of earthquakes in 2014 when the number of earthquakes increased to a dangerously high level. In response to the major increase in earthquakes in the Central United States, the United States Geological Survey began developing a new seismic hazard model to account for risk associated with induced seismicity. To date, no fewer than six individual earthquake sequences in Oklahoma have been identified and named by the Oklahoma Geological Survey.[10] Other swarms have been observed in south-central Kansas and North Texas.
According to data from the United States Geological Survey, there have been approximately 1,971 earthquakes in Oklahoma with moment magnitudes greater than or equal to 3.0,[11] about 65 earthquakes with magnitudes greater than or equal to 4.0, and two earthquakes with magnitudes greater than 5.0 associated with the earthquake swarms from the beginning of 2009 through April 2, 2016.[12]
In March 2013, a peer-reviewed paper published by a research team led by seismologist Katie Keranen at the University of Oklahoma in the scientific journal Geology reported that "the volume of fluid injected into the subsurface related to the production of unconventional resources continues to rise" and that there was a link between the "zone of injection and the seismicity" potentially triggering the November 5, 2011 Prague earthquake.[13][14] In March 28, 2016 the USGS released the USGS National Seismic Hazard Map which concluded that the primary cause of the earthquake in Oklahoma in 2011 was pressure on fault lines from cumulative effects of injecting oil drilling wastewater under high pressure into the underground.[13][15][16] Although the 2011 earthquake was the largest on record, the USGS reported that the central and eastern U.S. (CEUS) has undergone the most dramatic increase in seismic activity in the United States since 2009 with an average of 318 earthquakes of magnitude 3.0 a year up from 24 a year from 1973 to 2008. In 2015 there were 1,010 earthquakes in the CEUS region. By mid-March, 2016 there were already 226 earthquakes of magnitude 3.0 and larger in the CEUS.[16] The oil industry pressured the OGS to release a statement saying "The interpretation that best fits current data is that the Prague earthquake sequence was the result of natural causes" which they later recanted.[17]
Background
The first earthquake known to have occurred within the boundaries of Oklahoma occurred in September 1918 when a series of shocks was felt in El Reno, Oklahoma, the strongest of which was an estimated intensity V on September 10. On September 27, 1929, another tremor of intensity VI was centered in the same area and was felt in central and western Oklahoma; minor damage occurred in nearby areas and one chimney fell. The total affected area was approximately 20,000 km2 (7,700 sq mi).[18]
A magnitude 5.5 earthquake occurred near El Reno on April 9, 1952 at 10:29 a.m. CST (16:29 UTC), and at the time, it was the strongest earthquake ever recorded in Oklahoma. Most of Oklahoma was affected, as were parts of Arkansas, Iowa, Kansas, Missouri, Nebraska, and Texas. Damage was not extensive, but local residents were alarmed, and several thousands of dollars in damages occurred. Chimneys were toppled, walls were cracked, windows were broken, and bricks were loosened from buildings. In Oklahoma City, a crack measuring 15 meters (49 ft) was found in the State Capitol following the earthquake. The earthquake, which occurred along the Nemaha Fault, had a maximum intensity of VII near the epicenter.[18][19]
Scattered earthquakes occurred in Oklahoma between 1952 and 1969 with intensities as high as VII.[18] Between 1978 and 2008, the average long-term rate of earthquakes was approximately two earthquakes of magnitude 3.0 or greater per year.[6] However, in 2009, this number jumped to 20 with the beginning of several swarms of earthquakes in Oklahoma.[20] Research suggests that most of the significant earthquakes in Oklahoma since the 1930s may have been induced by oil production activities.[21]
Earthquakes
2011–12
A rise in seismicity in Oklahoma was observed in 2011. Early on the morning of November 5, 2011, an earthquake with a magnitude of 4.8 struck an area east of Oklahoma City roughly centered between Sparks and Prague. At the time, it was the strongest earthquake associated with the rise in Oklahoma's seismicity. Less than a day later at 10:53 p.m., a 5.6 Mw earthquake occurred near the location of the preceding 4.8 magnitude earthquake, becoming the strongest earthquake observed with any of the swarms as well as the strongest earthquake in the history of Oklahoma. This also resulted in the reclassification of the magnitude 4.8 earthquake as a foreshock and the 5.6 magnitude earthquake as the mainshock.[22] The earthquake received over 66,000 "Did You Feel It?" responses nationwide sent to the United States Geological Survey.[23] It was believed that the earthquake had occurred along the Wilzetta Fault, also known as the Seminole Uplift. Following this earthquake, several portable seismograph stations were established by the USGS, OGS, and University of Oklahoma School of Geology and Geophysics to aid with detection of future earthquakes in the area.[9] The 5.6 Mw mainshock was followed by a magnitude 4.8 aftershock slightly under two days later, and numerous other aftershocks occurred in the following months.[24][25] Through the end of 2011, 64 earthquakes were recorded, nearly double the number recorded for 2010.[20]
2012 saw a decrease in seismic activity in Oklahoma when compared to 2011, with a recorded annual total of 35 earthquakes magnitude 3.0 or greater, 29 less than recorded in the previous year.[20]
2013–14
On December 7, 2013, an earthquake occurred within the city limits of Oklahoma City in an area south of Lake Arcadia with a magnitude of 4.5 Mw. This was the strongest earthquake to occur in Oklahoma since the November 5, 2011 earthquake near the Prague–Sparks area east of Oklahoma City.[26] For 2013, an estimated 109 earthquakes occurred according to the Oklahoma Geological Survey, a number substantially higher than in any previous year going back to 1978.[20]
The 2014 total of 3.0+ magnitude earthquakes by May 2 was higher than the entire yearly total for 2013, at over 140 earthquakes. The number of earthquakes in Oklahoma increased by about 50% from October 2013 to May 2, 2014, prompting the United States Geological Survey to issue an uncommon "Earthquake Advisory" for Central Oklahoma warning of the elevated possibility of damaging, 5.5+ magnitude earthquakes. This was the first advisory in the United States ever issued east of the Rocky Mountains and remains effective.[6]
On July 17, 2014, the United States Geological Survey released an updated map identifying seismic hazard for the continental United States.[27] However, the earthquakes occurring in much of Oklahoma were not included in the creation of the map, for it is believed by the USGS that some degree of the earthquakes may have been induced by wastewater injection, and the map is meant to represent natural seismicity alone due to the unpredictable nature of earthquakes created by human industrial activities. Austin Holland of the OGS voiced concerns about the removal of the earthquakes in the map's creation, and he said "By removing them, we are underestimating the potential of serious seismic hazard in Oklahoma." William Ellsworth of the USGS responded by mentioning that the USGS was working on a new hazard model; "Everyone here thinks quakes, regardless of origin, need to be accounted for in our hazard model," he said.[28]
The swarms, while initially located primarily further south, traveled northward from Central Oklahoma into Logan County in early 2014. Additional earthquake swarms initiated in north-central Oklahoma, including areas near Medford, Oklahoma. The latter swarms crossed into southern Kansas in 2013. Many earthquakes have also occurred in the southernmost part of Kansas since they began, with the most significant being a magnitude 4.9 earthquake on November 12, 2014, the strongest earthquake produced by the swarms since a magnitude 4.5 earthquake struck in Northeast Oklahoma City on December 7, 2013 almost a year earlier.[26][29]
2015–16
By the end of 2014, 567 earthquakes of at least magnitude 3.0 were recorded in Oklahoma, more than the number of 3.0+ magnitude earthquakes from the previous 30 years combined.[30] In 2014, there were over twice as many earthquakes recorded in Oklahoma as in California, making Oklahoma the most seismically active state in the contiguous United States by a substantial margin. A review by EnergyWire examined earthquakes of greater than or equal to magnitude 3.0, and found that seismic activity in Oklahoma had been spreading northward into Kansas, which experienced a major jump in earthquakes from 2013 to 2014.[31] As in southern Kansas, earthquakes increased in frequency in North Texas, with over 130 earthquakes occurring there from 2009 to early 2015.[32]
For the first time, the United States Geological Survey would include earthquakes believed to have connections to industrial activities in its National Seismic Hazard Map which sets standards for construction and insurance rates.[33] According to USGS National Seismic Hazard Project head Mark Petersen, an updated version of the map will become available before the end of 2015. This marks a deviation from the past, with the USGS updating the National Seismic Hazard Map annually instead of every six years.[34]
The United States Geological Survey updated its National Seismic Hazard Map in 2014; however, potentially induced earthquakes were intentionally not considered in this analysis as geologists were uncertain how to incorporate non-tectonic earthquakes. Several months later in April 2015, a comprehensive assessment was released analyzing the link between the increase in seismic activity in the Central United States and oil and gas operations. Seventeen induced seismicity zones for earthquakes over the past 50 years were delineated in this assessment, including one region encompassing northern Oklahoma and parts of southern Kansas, a second region covering central Oklahoma down to the Oklahoma–Texas border, and a third region encompassing the Dallas–Fort Worth area of Texas.[35][36]
On April 21, 2015, the Oklahoma Geological Survey abandoned its skepticism of the possible link between earthquakes and industrial activities and said in official statement that it "considers it very likely that the majority of recent earthquakes, particularly those in central and north-central Oklahoma, are triggered by the injection of produced water in disposal wells." In 2013, the seismicity rate was "70 times greater than the background seismicity rate observed in Oklahoma prior to 2008", potentially although unlikely explainable by natural variations in seismicity, but the seismicity rate by the time of the statement was "about 600 times greater than the background seismicity rate" and was "very unlikely the result of a natural process."[37][38][39]
Late on August 16, the number of earthquakes in Oklahoma with moment magnitudes of ≥3.0 for the year of 2015 surpassed the yearly total for 2014 of 585 such earthquakes with over six times as many MW 3.0+ earthquakes as California. Through August 19, Oklahoma average 2.5 MW 3.0+ earthquakes a day in 2015; if earthquakes were to continue to occur at this rate through the remainder of 2015, Oklahoma would total over 912 such earthquakes, an increase of over 55% as compared to 2014.[40]
On December 29, a magnitude 4.3 earthquake struck in northeastern Oklahoma County near the town of Edmond. The quake caused structural damage to at least one home and caused power outages to over four thousand residents.[41] This was followed by a 4.2 magnitude earthquake on the morning of January 1, 2016, again in northeastern Oklahoma County in a nearby area.[42] Then on January 6, two earthquakes - one of magnitude 4.4 and one of magnitude 4.8 - struck near Fairview in northwest Oklahoma within just 30 seconds of each other. On February 13, slightly over five weeks later, an earthquake with an estimated magnitude of 5.1 struck 28 kilometers (17 miles) northwest of Fairview.[43] It was the third-strongest earthquake ever recorded in Oklahoma.[44]
Cause
Researchers have correlated the increase in earthquakes in central and north-central Oklahoma to injection disposal of produced water from two actively drilled stratigraphic intervals: the Mississippi Lime play, in north-central Oklahoma and extending into Kansas, which uses hydraulic fracturing; and the Hunton dewatering play, in central Oklahoma, which does not use hydraulic fracturing.[46] Both Mississippi Lime and Hunton plays produce large volumes of produced water; frac flowback makes up less than 5 percent of the injected wastewater.[47] More than 70 percent of the produced water from both plays is disposed through permitted Class II injection wells into the Arbuckle Group where it rests on Precambrian basement. The increase in pore pressure can release pre-existing stresses along faults in the basement rock.[48]
Between 2011 and 2014, the percentage of earthquakes spatiotemporally associated with injection wells has increased sharply by 87%.[49] A study of historic earthquakes has concluded that "much of the earthquake activity in the 1950s and 1980–1990s was induced" by injection of wastewater in deep disposal wells and the cluster of activity since 2009 is not consistent with the natural rate of fluctuations seen in the past.[50]
Governmental response
In September 2014, in response to the swarms of earthquakes, Oklahoma Governor Mary Fallin announced the creation of a "Coordinating Council on Seismic Activity" to help promote further understanding of the increase in seismicity. Fallin added, "We believe that by linking scientists and energy experts, we can develop sound regulatory practices and policies in our state while also alleviating any questions our citizens might have." The council, led by Michael Teague, is expected to include input from multiple areas, including "the Oklahoma Geologic Survey, the Oklahoma Corporation Commission, the Oklahoma Energy Resources Board, the University of Oklahoma, Oklahoma State University, the Oklahoma Independent Petroleum Association, the Oklahoma Oil and Gas Association, and various state legislators".[51] However, some criticized the council, saying it included too many representatives from the oil and gas industry; additional critics pointed out the fact that Michael Teague was the Oklahoma Secretary of Energy. Teague replied by saying that he was also concerned with environment, and he followed by adding, "We are talking to environmental groups and industry folks and academic folks and state agencies and how do you bring them all together?"[52]
After EnergyWire obtained Oklahoma Geological Survey email correspondence through an Oklahoma Open Records Act request in 2015, it was found that after the OGS acknowledged a link between oil and gas operations and the ongoing earthquakes in the latter part of 2013, state seismologist Austin Holland was called into a meeting with University of Oklahoma President David L. Boren and oil executives. Holland had previously spoken with a senior official of the United States Geological Survey discussing the connection between a swarm of earthquakes near and east of Oklahoma City. Holland wrote to USGS science advisor Bill Leith in 2013 "Since early 2010 we have recognized the potential for the Jones earthquake swarm to be due to the Hunton dewatering," but he followed by saying "But until we can demonstrate that scientifically or not we were not going to discuss that publicly." In October 2013, a joint statement between the OGS and the USGS announced that "activities such as wastewater disposal" may be a "contributing factor to the increase in earthquakes." Holland was requested a week later to come to Oklahoma Corporation Commission headquarters by then-Commissioner Patrice Douglas for a meeting. Also sent for was then-president of exploration at Continental Resources, Jack Stark. As Holland recounted in a later email, Stark and Douglas were "concerned" by the joint statement.[17] This precedes the Oklahoma Geological Survey's April 2015 change in position where the agency acknowledged that the earthquakes were "very unlikely the result of a natural process."[37]
In April 2015, after the Oklahoma Geological Survey acknowledged that the tremendous increase in the frequency of earthquake occurrence is likely due to the injection of produced water in disposal wells,[37] the State of Oklahoma launched a website providing information about earthquakes in the state, including an interactive map where both earthquakes and disposal wells can be plotted.[38][39]
"Traffic light" system
The Oklahoma Geological Survey has developed a "traffic light" system, which assigns "yellow light" status to some disposal wells, imposing limits on injection rates and pressures, and "red light" status to some injection wells, requiring them to shut down.[53] Injection wells are regulated by the Oklahoma Corporation Commission, which regulates oil and gas in the state. The Corporation Commission has also required more than 50 disposal wells drilled down to the basement to be plugged back.
Following earthquake activity in Alfalfa County, Oklahoma near the Kansas–Oklahoma border in late-January 2015, the Oklahoma Corporation Commission ordered SandRidge Energy to shut down an injection well it was operating. This was the second wastewater injection well directed to "shut in" or halt operations by the agency since a new monitoring system was established in 2013. According to Matt Skinner, a spokesman from the commission, the directive was issued on February 3 in response to a magnitude 4.1 earthquake recorded in the area four days earlier. According to Skinner, "They were operating under a 'yellow light' permit with language that said shut in if there's any seismic activity."[54]
Potential damage
As a result of the magnitude 5.6 earthquake on November 5, 2011, an estimated one million dollars in damage occurred in and around the Prague area.[55] So far, there has not been a significant amount of damage reported from other earthquakes, but in April 2014, the United States Geological Survey released an analysis indicating that "the likelihood of future, damaging earthquakes [in central and north-central Oklahoma] has increased as a result of the increased number of small and moderate shocks."[6]
In light of the greatly increased earthquake activity, about 15% of Oklahomans had purchased earthquake insurance by early 2015 according to Oklahoma Insurance Commissioner John D. Doak.[56]
On June 30, 2015, the Oklahoma Supreme Court ruled that homeowners who had suffered injuries or property damage as a result of frequent earthquakes believed to be caused by industrial activities could legally sue for damages in trial courts. This ruling was issued in spite of efforts by the industry to prevent such lawsuits from being accepted. The case, originally brought before a state court by Sandra Ladra, who had sustained injuries during the 2011 Oklahoma earthquake, named the Spess Oil Company and New Dominion, two oil and gas companies, as defendants in the case. The case was initially dismissed by a state court under the premise that such cases must go before the Oklahoma Corporation Commission as required by state law. After Ladra's lawyer appealed to state supreme court, the 7-to-0 ruling on June 30 was made.[57]
See also
Notes
- ↑ This mean depth figure is for Oklahoma only.
- ↑ Earthquakes included in this total have a minimum magnitude of 2.0 and are complete above a magnitude of 3.0. The total from the United States Geological Survey is significantly lower than that from the Oklahoma Geological Survey as the USGS does not report events as small as the OGS; information from the USGS is still included as its information is updated more frequently. This data is valid through February 29, 2016.
References
- ↑ Darold, Amberlee P.; Holland, Austin A.; Morris, Jennifer K.; Gibson, Amie R. (February 19, 2015). Oklahoma Earthquake Summary Report 2014 (PDF). Oklahoma Geological Survey (Report) (Norman, Oklahoma: University of Oklahoma). Archived from the original on March 16, 2015. Retrieved March 15, 2015.
- ↑ "USGS Map of Earthquakes (Oklahoma: 2009-01-01–2016-04-02)". Earthquake Hazards Program. United States Geological Survey. April 2, 2016. Retrieved April 2, 2016.
- ↑ "Animation of Oklahoma Seismicity: January 2, 2008–February 14, 2016". Earthquake Hazards Program. United States Geological Survey. February 14, 2016. Retrieved February 29, 2016.
- ↑ "USGS Map of Earthquakes (Kansas: 2009-01-01–2016-04-02)". Earthquake Hazards Program. United States Geological Survey. April 2, 2016. Retrieved April 2, 2016.
- ↑ "USGS Map of Earthquakes (North Texas: 2009-01-01–2016-04-02)". Earthquake Hazards Program. United States Geological Survey. April 2, 2016. Retrieved April 2, 2016.
- 1 2 3 4 "Record Number of Oklahoma Tremors Raises Possibility of Damaging Earthquakes". United States Geological Survey, Oklahoma Geological Survey. May 2, 2014. Retrieved July 2, 2014.
- ↑ Francis, Mathew (June 18, 2015). "This Oil Extraction Process Is Causing Earthquakes In Oklahoma". Forbes. Retrieved 8 November 2015.
- ↑ Fracking-Linked Earthquakes May Strike Far from Wells, Live Science, Becky Oskin, May 2, 2014. Retrieved 19 January 2016.
- 1 2 "Magnitude 5.6 – Oklahoma". Earthquake Hazards Program. United States Geological Survey. November 6, 2011. Retrieved July 2, 2014.
- ↑ "Recent Earthquakes: Town Hall Meeting, June 26, 2014" (PDF). Oklahoma Geological Survey. University of Oklahoma. June 26, 2014. Retrieved July 13, 2014.
- ↑ "USGS Map of 3.0+ Magnitude Earthquakes (Oklahoma: 2009-01-01–2016-04-02)". Earthquake Hazards Program. United States Geological Survey. April 2, 2016. Retrieved April 2, 2016.
- ↑ "USGS Map of 4.0+ Magnitude Earthquakes (Oklahoma: 2009-01-01–2016-04-02)". Earthquake Hazards Program. United States Geological Survey. April 2, 2016. Retrieved April 2, 2016.
- 1 2 Keranen, Katie M.; Savage, Heather M.; Abers, Geoffrey A.; Cochran, Elizabeth S. (2013). "Potentially induced earthquakes in Oklahoma, USA: Links between wastewater injection and the 2011 Mw 5.7 earthquake sequence". Geology. doi:10.1130/G34045.1. Retrieved April 28, 2016.via EBSCO
- ↑ Sumy, Danielle F.; Cochran, Elizabeth S.; Keranen, Katie M.; Wei, Maya; Abers, Geoffrey A. (March 7, 2014). "Observations of static Coulomb stress triggering of the November 2011 M5.7 Oklahoma earthquake sequence". Solid Earth. Journal of Geophysical Research 119 (3): 1904–1923. doi:10.1002/2013JB010612. Retrieved 2015-04-30.
- ↑ Achenbach, Joel (March 28, 2016), "7 million Americans at risk of man-made earthquakes, USGS says", Washington Post
- 1 2 Fitzpatrick, Jessica; Petersen, Mark (March 28, 2016), "Induced Earthquakes Raise Chances of Damaging Shaking in 2016", USGS, retrieved April 28, 2016
- 1 2 Soraghan, Mike (March 5, 2015). "Oklahoma agency linked quakes to oil in 2010, but kept mum amid industry pressure". EnergyWire (Environment & Energy Publishing, LLC). Retrieved March 9, 2015.
- 1 2 3 "Oklahoma Earthquake History". United States Geological Survey. n.d. Retrieved April 18, 2015.
- ↑ "Historic Earthquakes — El Reno, Oklahoma — 1952 04 09 16:29:28.4 UTC". United States Geological Survey. n.d. Retrieved April 18, 2015.
- 1 2 3 4 "Earthquakes in Oklahoma of M3+" (PNG). Earthquake Hazards Program. United States Geological Survey. September 24, 2014. Retrieved March 17, 2015.
- ↑ Hough, Susan E.; Page, Morgan. "A Century of Induced Earthquakes in Oklahoma?". 10/20/2015. U.S. Geological Survey. Retrieved November 8, 2015.
Several lines of evidence further suggest that most of the significant earthquakes in Oklahoma during the 20th century may also have been induced by oil production activities. Deep injection of waste water, now recognized to potentially induce earthquakes, in fact began in the state in the 1930s.
- ↑ "M4.8 – Oklahoma". Earthquake Hazards Program. United States Geological Survey. November 5, 2011. Retrieved March 18, 2015.
- ↑ "M5.6 – Oklahoma (BETA)". Earthquake Hazards Program. United States Geological Survey. November 6, 2011. Retrieved July 4, 2014.
- ↑ "M4.8 – Oklahoma". Earthquake Hazards Program. United States Geological Survey. November 7, 2011. Retrieved April 9, 2015.
- ↑ "Nov. 6, 2011 M5.6 Oklahoma Earthquake Foreshocks and Aftershocks". Earthquake Hazards Program. United States Geological Survey. July 31, 2012. Retrieved March 18, 2015.
- 1 2 "M4.5 – 9km ESE of Edmond, Oklahoma". Earthquake Hazards Program. United States Geological Survey. December 7, 2013. Retrieved January 27, 2015.
- ↑ Robertson, Jessica; Petersen, Mark (July 17, 2014). "New Insight on the Nation’s Earthquake Hazards". Earthquake Hazards Program (United States Geological Survey). Retrieved August 11, 2014.
- ↑ Eaton, Joe (July 31, 2014). "Oklahoma Grapples With Earthquake Spike—And Evidence of Industry's Role". National Geographic Daily News (National Geographic Society). Retrieved August 11, 2014.
- ↑ "M4.9 – 13km S of Conway Springs, Kansas". United States Geological Survey. November 12, 2014. Retrieved February 4, 2015.
- ↑ Branstetter, Ziva (January 27, 2015). "Prague earthquake suit before Supreme Court could set precedent". Tulsa World. Retrieved February 9, 2015.
- ↑ Soraghan, Mike (January 5, 2015). "Earthquakes: Shaken more than 560 times, Okla. is top state for quakes in 2014". EnergyWire (Environment & Energy Publishing, LLC). Retrieved February 4, 2015.
- ↑ Kuchment, Anna; Loftis, Randy Lee; Osborne, James; Selk, Avi (January 11, 2015). "What’s at fault? Scientists seek cause of Irving earthquakes". The Dallas Morning News. Retrieved February 3, 2015.
- ↑ Oskin, Becky (February 12, 2015). "Hidden Faults Explain Earthquakes in Fracking Zones". LiveScience (Purch, Inc.). Retrieved February 21, 2015.
- ↑ Kuchment, Anna (January 31, 2015). "USGS likely to upgrade North Texas’ quake risk level". The Dallas Morning News. Retrieved February 7, 2015.
- ↑ Peterson, Mark D.; Mueller, Charles S.; Moschetti, Morgan P.; Hoover, Susan M.; Rubinstein, Justin L.; Llenos, Andrea L.; Michael, Andrew J.; Ellsworth, William L.; McGarr, Arthur F.; Holland, Austin A.; Anderson, John G. (April 23, 2015). Incorporating Induced Seismicity in the 2014 United States National Seismic Hazard Model—Results of 2014 Workshop and Sensitivity Studies (USGS Open-File Report 2015–1070) (PDF) (Report). United States Geological Survey. doi:10.3133/ofr20151070. ISSN 2331-1258. OCLC 38116130. Retrieved April 23, 2015.
- ↑ Pérez-Peña, Richard (April 23, 2015). "U.S. Maps Pinpoint Earthquakes Linked to Quest for Oil and Gas". The New York Times. Retrieved April 24, 2015.
- 1 2 3 Andrews, Richard D.; Holland, Austin A. (April 21, 2015). Statement on Oklahoma Seismicity (PDF). Oklahoma Geoogical Survey (Report) (University of Oklahoma). Retrieved April 23, 2015.
- 1 2 Wines, Michael (April 21, 2015). "Oklahoma Recognizes Role of Drilling in Earthquakes". The New York Times. Retrieved April 23, 2015.
- 1 2 "Earthquakes in Oklahoma". Office of the Oklahoma Secretary of Energy and Environment. Oklahoma City, Oklahoma: Government of Oklahoma. April 21, 2015. Retrieved April 23, 2015.
- ↑ Soraghan, Mike (August 19, 2015). "Earthquakes: Oft-shaken Okla. tops last year's quake record". EnergyWire (Environment & Energy Publishing, LLC). Retrieved August 29, 2015.
- ↑ "4.3 Magnitude Earthquake Causes Damage, Power Outage Near Edmond". Oklahoma City, Oklahoma: KWTV-DT News 9. December 29, 2015.
- ↑ "Another Strong Earthquake Shakes Oklahoma". Oklahoma City, Oklahoma: KWTV-DT News 9. January 1, 2016.
- ↑ "M5.1 - 28km NW of Fairview, Oklahoma". Earthquake Hazards Program. United States Geological Survey. February 13, 2016. Retrieved February 13, 2016.
- ↑ "Oklahoma hit by its third-strongest earthquake ever: USGS". Reuters. February 13, 2016. Retrieved February 13, 2016.
- ↑ Justin Rubinstein (August 27, 2015). Yes, Humans Really Are Causing Earthquakes. U.S. Geological Survey. Event occurs at 15:22.
- ↑ David Brown, "Dispelling myths about seismicity," AAPG Explorer, Oct. 2015.
- ↑ "Oklahoma earthquakes linked to oil and gas drilling," AAAS, 18 June 2015.
- ↑ K. M. Keranen and others, Science, .
- ↑ Ge, S.; et al. (19 June 2015). "High-rate injection is associated with the increase in U.S. mid-continent seismicity". Science (AAAS) 348 (6241): 1336–1340. doi:10.1126/science.aab1345.
The yearly percent-age of associated earthquakes has risen sharply to ~87% from 2011 to 2014
- ↑ Hough, Susan E.; Page, Morgan. "A Century of Induced Earthquakes in Oklahoma?". 10/20/2015. U.S. Geological Survey. Retrieved November 8, 2015.
...we conclude that it is possible that earthquakes were induced by oil production activities in Oklahoma as early as the 1920s, and several lines of evidence support our conclusion that much of the earthquake activity in the 1950s and 1980–1990s was induced.
- ↑ Wilmoth, Adam (September 4, 2014). "Oklahoma Gov. Mary Fallin creates seismic activity council". The Oklahoman (NewsOK.com). Retrieved September 11, 2014.
- ↑ Stewart, Sarah (September 9, 2014). "Council to study Oklahoma earthquakes criticized for members’ professions". KFOR-TV (KFOR.com). Retrieved October 1, 2014.
- ↑ Wertz, Joe (February 11, 2015). "Mapped: ‘Traffic Light’ Wells in Oklahoma’s Earthquake Country". StateImpact Oklahoma (Oklahoma Public Media Exchange). Retrieved October 11, 2015.
- ↑ Branstetter, Ziva (February 4, 2015). "State orders injection well shut down after northwestern Oklahoma earthquake". Tulsa World. Retrieved February 7, 2015.
- ↑ Gallucci, Maria (April 22, 2015). "Oklahoma Earthquake Swarm 2015: In Sharp Turnaround, Oklahoma Officials Confirm The Link Between Fracking Wastewater And Earthquakes". International Business Times. Retrieved May 19, 2015.
- ↑ Wertz, Joe (January 14, 2015). "Oklahoma Earthquake Rate is High, But Holding Steady". StateImpact Oklahoma (Oklahoma Public Media Exchange). Retrieved February 4, 2015.
- ↑ Oppel Jr., Richard A. (June 30, 2015). "Oklahoma Court Rules Homeowners Can Sue Oil Companies Over Quakes". The New York Times.
External links
Wikimedia Commons has media related to Earthquakes in Oklahoma. |
- Official State of Oklahoma Website for Earthquakes
- Oklahoma Geological Survey Leonard Geophysical Observatory
- Incorporated Research Institutions for Seismology Earthquake Browser – Vicinity of Oklahoma
- USGS Kansas Earthquake Information
- USGS Oklahoma Earthquake Information
- Kansas Geological Survey: Kansas Earthquakes
- StateImpact Oklahoma: Exploring the Link Between Earthquakes and Oil and Gas Disposal Wells
- StateImpact Texas: How Oil and Gas Disposal Wells Can Cause Earthquakes
- Oklahoma Earthquake Summary Report 2014
- Reawakened Oklahoma Faults Could Produce Larger Future Events
- Oklahoma Geological Survey Statement on Oklahoma Seismicity – April 21, 2015
- USGS: Induced Earthquakes