As part of our work to better understand areas of induced earthquakes, the USGS installs seismometers in areas of increased seismicity, provides hazard estimations, and uses numerical models.
Increasing Rate of Earthquakes Beginning in 2009
The number of earthquakes in the central U.S. has increased dramatically over the past decade. Between the years 1973–2008, there was an average of 25 earthquakes of magnitude three and larger in the central and eastern United States. Since 2009, at least 58 earthquakes of this size have occurred each year, and at least 100 earthquakes of this size every year since 2013. The rate peaked in 2015 with 1010 M3+ earthquakes. Since 2015, earthquake rate has declined. In 2019, 130 M3+ earthquakes occurred in the same region. Nonetheless, this rate is far higher than the average of 25 earthquakes per year. Most of these earthquakes are in the magnitude 3–4 range — large enough to have been felt by many people—yet small enough to rarely cause damage. Damage has been caused by some of the larger events, including the M5.8 Pawnee and M5.0 Cushing Oklahoma earthquakes that occurred in 2016.
This increase in earthquakes prompts two important questions:
- Are they natural, or man-made?
- What should be done in the future as we address the causes and consequences of these events to reduce associated risks?
Delayed dynamic triggering of disposal-induced earthquakes observed by a dense array in Northern Oklahoma
Seismic hazard assessment at the Fallon, Nevada, Frontier Observatory for Research in Geothermal Energy site
Rupture model of the M5.8 Pawnee, Oklahoma earthquake from regional and teleseismic waveforms
Ground motions from induced earthquakes in Oklahoma and Kansas
Microseismic events associated with the Oroville Dam spillway
Earthquakes induced by hydraulic fracturing are pervasive in Oklahoma
Seismology with dark data: Image-based processing of analog records using machine learning for the rangely earthquake control experiment
Erratum to The 2013–2016 induced earthquakes in Harper and Sumner Counties, southern Kansas
Tidal response of groundwater in a leaky aquifer—Application to Oklahoma
Induced earthquake and liquefaction hazards in Oklahoma, USA: Constraints from InSAR
Induced earthquake families reveal distinctive evolutionary patterns near disposal wells
Injection-induced moment release can also be aseismic
As part of our work to better understand areas of induced earthquakes, the USGS installs seismometers in areas of increased seismicity, provides hazard estimations, and uses numerical models.
Increasing Rate of Earthquakes Beginning in 2009
The number of earthquakes in the central U.S. has increased dramatically over the past decade. Between the years 1973–2008, there was an average of 25 earthquakes of magnitude three and larger in the central and eastern United States. Since 2009, at least 58 earthquakes of this size have occurred each year, and at least 100 earthquakes of this size every year since 2013. The rate peaked in 2015 with 1010 M3+ earthquakes. Since 2015, earthquake rate has declined. In 2019, 130 M3+ earthquakes occurred in the same region. Nonetheless, this rate is far higher than the average of 25 earthquakes per year. Most of these earthquakes are in the magnitude 3–4 range — large enough to have been felt by many people—yet small enough to rarely cause damage. Damage has been caused by some of the larger events, including the M5.8 Pawnee and M5.0 Cushing Oklahoma earthquakes that occurred in 2016.
This increase in earthquakes prompts two important questions:
- Are they natural, or man-made?
- What should be done in the future as we address the causes and consequences of these events to reduce associated risks?