A shallow earthquake registered by the USGS as M5.0 hit the city of Cushing, Oklahoma at 01:44 UTC on November 7, 2016. The agency is reporting a depth of 5 km (3.1 miles). Today's quake hit just two months after M5.8, the strongest earthquake in Oklahoma's history, shook Pawnee and forced shutdowns of 37 oil wells.
The epicenter was located 2.8 km (1.9 miles) W of Cushing (population 7 826), 27.6 km (17.2 miles) ESE of Stillwater (population 45 668), 57.8 km (35.9 miles) ENE of Guthrie (population 10 191), 61.7 km (38.3 miles) W of Sapulpa (population 20 544), and 86.6 km (53.8 miles) NE of Oklahoma City (population 579 999), Oklahoma.
It was felt as far away as Iowa, Illinois and Texas.
In recent years, Oklahoma has had thousands of earthquakes. Nearly all have been traced to the underground injection of wastewater left over from oil and gas production.
According to media reports, it was a sharp earthquake near one of the world's key oil hubs which triggered fears it might have caused damage to key infrastructure.
A few minor injuries were reported.
City Manager Steve Spears questioned whether some of the community's century-old buildings might be unsafe. "Some damage was superficial, bricks falling off facades, but some older buildings might have damaged foundations that would be difficult to assess until daylight," Spears said.
The police warned people to stay out of downtown and cordoned off older parts of the town to keep away gawkers.
The Cushing Public School District has canceled classes Monday until they assess the potential damage.
One senior building was evacuated and provided shelter at a youth center gymnasium in Cushing.
Local media reported a temporary loss of power for about 2 hours.
Pipeline operators at the Cushing, Oklahoma, oil storage terminal said that there have been no immediate reports of any problems.
Cushing, Oklahoma – Damage after M5.0 earthquake on November 7, 2016. Credit: Kevin Stump
The USGS initially reported M5.3 but later downgraded it to M5.0.
USGS issued a green alert for shaking-related fatalities and economic losses.
Overall, the population in this region resides in structures that are resistant to earthquake shaking, though some vulnerable structures exist.
Estimated population exposure to earthquake shaking
Selected cities exposed
Oklahoma Geological Survey statement
This area has been an active zone of seismicity since 2015. The USGS estimates the maximum Modified Mercalli Intensity to be VI, in accord with reports of damage near the epicenter.
"We derived several focal plane solutions (FPS or beachball diagrams) from each event that indicate strike-slip displacement dominated the motion along the fault," OGS said.
The quake has already triggered several aftershocks of magnitudes less than 3. The likelihood of an aftershock being larger than this event is about 5%.
Aftershocks have the potential to create damage, just like the other earthquakes. They may be expected to continue and become less frequent with time.
In the case of further seismicity, OGS urged the public to protect themselves from falling objects: (1) drop to the ground; (2) cover your head and neck; and (3) hold on to any sturdy cover.
Earthquakes in the stable continental region
Natural occurring earthquake activity
Most of North America east of the Rocky Mountains has infrequent earthquakes. Here and there earthquakes are more numerous, for example in the New Madrid seismic zone centered on southeastern Missouri, in the Charlevoix-Kamouraska seismic zone of eastern Quebec, in New England, in the New York – Philadelphia – Wilmington urban corridor, and elsewhere. However, most of the enormous region from the Rockies to the Atlantic can go years without an earthquake large enough to be felt, and several U.S. states have never reported a damaging earthquake.
Earthquakes east of the Rocky Mountains, although less frequent than in the West, are typically felt over a much broader region than earthquakes of similar magnitude in the west. East of the Rockies, an earthquake can be felt over an area more than ten times larger than a similar magnitude earthquake on the west coast. It would not be unusual for a magnitude 4.0 earthquake in eastern or central North America to be felt by a significant percentage of the population in many communities more than 100 km (60 mi) from its source. A magnitude 5.5 earthquake in eastern or central North America might be felt by much of the population out to more than 500 km (300 mi) from its source. Earthquakes east of the Rockies that are centered in populated areas and large enough to cause damage are, similarly, likely to cause damage out to greater distances than earthquakes of the same magnitude centered in western North America.
Most earthquakes in North America east of the Rockies occur as faulting within bedrock, usually miles deep. Few earthquakes east of the Rockies, however, have been definitely linked to mapped geologic faults, in contrast to the situation at plate boundaries such as California's San Andreas fault system, where scientists can commonly use geologic evidence to identify a fault that has produced a large earthquake and that is likely to produce large future earthquakes. Scientists who study eastern and central North America earthquakes often work from the hypothesis that modern earthquakes occur as the result of slip on preexisting faults that were formed in earlier geologic eras and that have been reactivated under the current stress conditions. The bedrock of Eastern North America is, however, laced with faults that were active in earlier geologic eras, and few of these faults are known to have been active in the current geologic era. In most areas east of the Rockies, the likelihood of future damaging earthquakes is currently estimated from the frequencies and sizes of instrumentally recorded earthquakes or earthquakes documented in historical records.
As is the case elsewhere in the world, there is evidence that some central and eastern North America earthquakes have been triggered or caused by human activities that have altered the stress conditions in earth's crust sufficiently to induce faulting. Activities that have induced felt earthquakes in some geologic environments have included impoundment of water behind dams, injection of fluid into the earth's crust, extraction of fluid or gas, and removal of rock in mining or quarrying operations. In much of eastern and central North America, the number of earthquakes suspected of having been induced is much smaller than the number of natural earthquakes, but in some regions, such as the south-central states of the U.S., a significant majority of recent earthquakes are thought by many seismologists to have been human-induced. Even within areas with many human-induced earthquakes, however, the activity that seems to induce seismicity at one location may be taking place at many other locations without inducing felt earthquakes. In addition, regions with frequent induced earthquakes may also be subject to damaging earthquakes that would have occurred independently of human activity. Making a strong scientific case for a causative link between a particular human activity and a particular sequence of earthquakes typically involves special studies devoted specifically to the question. Such investigations usually address the process by which the suspected triggering activity might have significantly altered stresses in the bedrock at the earthquake source, and they commonly address the ways in which the characteristics of the suspected human-triggered earthquakes differ from the characteristics of natural earthquakes in the region. (USGS)
Featured image credit: Cushing damaged by M5.0 earthquake on November 7, 2016. Credit: Kevin Stump
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