Magnitude 5.0 Earthquake in Payne County, Oklahoma.

The United States Geological Survey recorded a Magnitude 5.0 Earthquake at a depth of 5.0 km about 2 km to the west of the city of Cushing in Payne County, Oklahoma, slightly before 7.45 pm local time on Sunday 6 November 2016 (slightly before 1.45 am on Monday 7 December GMT). No fatalities or major damage have been reported, but a number of minor injuries and damaged buildings have been reported in the Cushing area, and people have reported feeling the event across much of Oklahoma as well as parts of Kansas, Missouri, Arkansas and Texas.

Damage in Cushing, Oklahoma, following the 6 November 2016 Earthquake. AN24.

Oklahoma is naturally prone to Earthquakes, particularly in the southwest of the state, near the Meers Fault Zone, but since 2009 has suffered a sharp increase in the number of small quakes in the central and northeast parts of the state. While most of these quakes have been quite small, a few have been large enough to potentially cause problems, and any unexplained increase in seismic activity is a cause for concern.

In a paper published in the journal Geology on 26 March 2013, a team of geologists led by Katie Keranen of the ConocoPhillips School of Geology and Geophysics at the University of Oklahoma linked one of the largest of these quakes, a Magnitude 5.7 event in November 2011 which caused damage locally and was felt across 17 states, to the practice of pumping liquids (usually brine) into injection wells, which is common in the hydrocarbons industry and used to displace oil or gas, which can then be extracted from nearby extraction wells (where this is done in bursts at pressure to intentionally break up rock it is called hydraulic fracturing, or fracking). Significantly they suggested that the practice could lead to quakes years or even decades after the actual injection.

Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.

See also...

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Magnitude 3.2 Earthquake in Payne County, Oklahoma.

The United States Geological Survey recorded a Magnitude 3.2 Earthquake at a depth of 4.5 km in northeast Payne County, Oklahoma, slightly before 5.20 pm local time (Slightly before 10.20 pm GMT) on Sunday 27 July 2014. There are no reports of any damage or injuries associated with this event, though it was felt locally.

The approximate location of the 27 June 2014 Payne County Earthquake. Google Maps.

Oklahoma is naturally prone to Earthquakes, particularly in the southwest of the state, near the Meers Fault Zone, but since 2009 has suffered a sharp increase in the number of small quakes in the central and northeast parts of the state. While most of these quakes have been quite small, a few have been large enough to potentially cause problems, and any unexplained increase in seismic activity is a cause for concern. 

In a paper published in the journal Geology on 26 March 2013, a team of geologists led by Katie Keranen of the ConocoPhillips School of Geology and Geophysics at the University of Oklahoma linked one of the largest of these quakes, a Magnitude 5.7 event in November 2011 which caused damage locally and was felt across 17 states, to the practice of pumping liquids (usually brine) into injection wells, which is common in the hydrocarbons industry and used to displace oil or gas, which can then be extracted from nearby extraction wells (where this is done in bursts at pressure to intentionally break up rock it is called hydraulic fracturing, or fracking). Significantly they suggested that the practice could lead to quakes years or even decades after the actual injection.

Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.

See also...

 Magnitude 3.1 Earthquake in Grant County, Oklahoma.

The United States Geological Survey recorded a Magnitude 3.1 Earthquake at a depth of 2.4 km in southern Grant County...

 Magnitude 3.3 Earthquake in Grant County, Oklahoma.

The United States Geological Survey recorded a Magnitude 3.3 Earthquake at a depth of 4.4 km in southwest Grant County...

 Magnitude 3.6 Earthquake in Lincoln County, Oklahoma.

The United States Geological Survey recorded a Magnitude 3.6 Earthquake at a depth of 5.0 km in northern Lincoln County...

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Magnitude 2.9 Earthquake in Payne County Oklahoma.

The United States Geological Survey recorded a Magnitude 2.9 Earthquake at a depth of 5.0 km roughly 2 km to the northeast of the town of Ripley in Payne County, Oklahoma, slightly after 11.35 pm local time on Saturday 21 September 2013 (slightly after 4.35 am on Sunday 22 September GMT). This is not a large quake, and is highly unlikely to have caused any damage or injuries, though a number of people reported feeling it in the north of Payne County.

The approximate location of the 21 September 2013 Payne County Earthquake. Google Maps.

Oklahoma is naturally prone to Earthquakes, particularly in the southwest of the state, near the Meers Fault Zone, but since 2009 has suffered a sharp increase in the number of small quakes in the central and northeast parts of the state. While most of these quakes have been quite small, a few have been large enough to potentially cause problems, and any unexplained increase in seismic activity is a cause for concern. 

In a paper published in the journal Geology on 26 March 2013, a team of geologists led by Katie Keranen of the ConocoPhillips School of Geology and Geophysics at the University of Oklahoma linked one of the largest of these quakes, a Magnitude 5.7 event in November 2011 which caused damage locally and was felt across 17 states, to the practice of pumping liquids (usually brine) into injection wells, which is common in the hydrocarbons industry and used to displace oil or gas, which can then be extracted from nearby extraction wells (where this is done in bursts at pressure to intentionally break up rock it is called hydraulic fracturing, or fracking). Significantly they suggested that the practice could lead to quakes years or even decades after the actual injection.

Witness accounts of quakes can help geologists to understand these events and the rock structures that cause them. If you felt this quake (or if you were in the area but did not, which is also useful information) you can report it to the USGS here.

See also Magnitude 4.9 Earthquake in the Wind River Mountains of Wyoming, Magnitude 5.3 Earthquake in Chihuahua State, Mexico, Magnitude 3.1 Earthquake in west Okfuskee County, Oklahoma, Magnitude 2.5 Earthquake in Van Buren County, Arkansas and Magnitude 4.2 Earthquake in Chihuahua State, Mexico.

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