Agency overview | |
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Formed | May 29, 1908 |
Preceding agency |
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Jurisdiction | Oklahoma |
Headquarters | Norman, Oklahoma United States |
Employees | 42 (2016) [1] |
Agency executives |
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Website | ou.edu/ogs |
The Oklahoma Geological Survey is a state agency chartered in the Constitution of Oklahoma responsible for collecting and disseminating information about Oklahoma's natural resources, geological formations, and earthquakes. [2] [3] Shortly after Oklahoma became a state, its first legislature passed an enabling act on May 29, 1908 and Governor Charles Haskell signed it into law. The OGS was an offshoot of Oklahoma Territory's Territorial Survey, which was established in 1900. OGS remains the only state geological survey that was created by a provision in the state constitution. In 1924, jurisdiction of the OGS was officially put under the Oklahoma University Board of Regents, and has not been changed since. [4] In 2007, OGS became part of the Mewbourne College of Earth and Energy.
The Oklahoma Geological Society was established on the Oklahoma University campus under an agreement between OU geology professor, Charles N. Gould, and the OU Dean of Arts and Sciences, Professor James S. Buchanan. Gould had founded the Oklahoma Geological Survey in 1908 and became its first director until 1911, when he left to go into private practice as a geologist. [5] [lower-alpha 1]
In June, 1923, Governor Jack C. Walton, wanting to make major budget cuts to Oklahoma University, discontinued the Oklahoma Geological Survey. While Walton had been successful in removing the majority of the OU Board of Regents and replacing those members with his own supporters, his heavy handed approach toward the university had cost him much of his political support. He succeeded in having the former president, Stratton D. Brooks, resign, he was unable to bring in a high-quality president from outside before the start of the 1923-4 school year. In July, 1923, Walton appointed James S. Buchanan as Acting President. In his new role, Buchanan negotiated with Dr. Gould to revive the OGS on the OU campus in March, 1924. Moreover, Dr. Chester N. Gould returned to OU as director of the OGS. [6]
The main facilities of OGS are located at the OU main campus in Norman, Oklahoma. In 1965, OGS began operating a small geophysical laboratory near Tulsa. Its main function is to analyze earthquake activity in the state, based on data reported to this site from other seismographs scattered around the state. [4] The Oklahoma Petroleum Information Center, which opened in 2002, allowing the expansion of the core and sample library to house more than three hundred thousand cores from Oklahoma and elsewhere, preserving for future study and analysis earth samples acquired from wells drilled as far back as the 1920s. The building also houses the OGS publication sales office and an extensive library of petroleum data for Oklahoma. [4]
The mission of OGS is, "...to investigate the land, water, mineral, and energy resources of the state and to disseminate the results of those investigations to promote the wise use of Oklahoma's natural resources in a manner consistent with sound environmental practices." [4]
The mission is carried out through research and field work which the agency publishes in books, open files, maps, and internet documents. Particular attention is given to topics related to petroleum and coal, which have an especially large impact on the state's economy. However, OGS also studies of non-fuel mineral resources, such as: clays, shales, limestone and dolomites, crushed stone, copper, bentonite, salt, gypsum, uranium, helium, and iodine. [4] [lower-alpha 2]
OGS Interim Director Rick Andrews announced that the seismic observatory at Leonard, Oklahoma would close permanently during the summer of 2015. He said in a telephone interview with a reporter from the Tulsa World that the facility needed about $100,000 worth of maintenance and repairs in order to keep operating, but would still not be up-to-date. [7]
The article noted that the observatory, which had been built by a subsidiary of Standard Oil Company of New Jersey in 1961, had later been used by the U. S. Government to monitor nuclear tests, before it was acquired by OGS. Most recently it had been tasked to monitor and find the cause of earthquake swarms shaking central and northern Oklahoma. Andrews added that a slowdown in internet speeds near the remote location had also reduced the value of the observatory in performing the OGS mission, and that the activities would improve only by moving them to the main facility at Norman, Oklahoma. [7]
Oklahoma experienced swarms of minor earthquakes that attracted public attention in Oklahoma, starting after 2005 - 2006, when there was an increase in oil and gas exploration. [8] Most of these were low-magnitude (less than 3.0 on the moment magnitude scale), caused little physical damage and occurred in lightly populated rural areas of north central Oklahoma. The Oklahoma Geologic Survey believed that it had an obligation to perform scientific studies to determine why the phenomenon had suddenly occurred. The quakes continued, growing even more powerful, frequent and widespread.
By 2010-11, the number of quakes exceeding 5.0 in magnitude had become more significant. Some larger towns, such as Shawnee, Stillwater and Cushing had experienced more significant damage. In Shawnee, a tremor recorded as 5.9 knocked one of the four brick turrets off the top of the 100-year old main building. The other three identical turrets were still in place, but judged as so damaged that they had to be removed and completely rebuilt - with better earthquake reinforcement. [9]
As more earth scientists began exchanging information, suspicion grew that some of the new techniques that have been developed to recover the last traces of crude oil and natural gas from nearly exhausted formations. Many began to believe that the injection of very high pressure waste water into underground formations, a process called "fracking" might be at least partially responsible for many of the quakes. In mid-April 2015, the Oklahoma Geological Society posted a statement that it considered wastewater injections are "..very likely..." causing the majority of Oklahoma's earthquakes. [8] The Times article claimed that the OGS statement marked a distinct reversal of the state's previous position that the earthquakes were related to activities of the state's oil and gas industry. It noted that in the previous fall, the Republican governor had dismissed the idea in a public speech, stating that claims of such a relationship were only speculation and that more study was needed. [8] After the OGS issued its statement in April, 2015, the Oklahoma Oil and Gas Association (OOGA), again disputed its conclusions and repeated that more study is needed. OOGA's president, Chad Warmington, said that we," ... don’t know enough about how wastewater injection impacts Oklahoma’s underground faults"..."Nor is there any evidence that halting wastewater injection would slow or stop the earthquakes. [8]
An earthquake is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air and wreak destruction across entire cities. The seismicity, or seismic activity, of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The word tremor is also used for non-earthquake seismic rumbling.
Pawnee County is a county located in the U.S. state of Oklahoma. As of the 2010 census, the population was 16,577. Its county seat is Pawnee. The county is named after the Pawnee Nation, whose reservation used to encompass the county prior to allotment in 1893.
Cushing is a city in Payne County, Oklahoma, United States. The population was 7,826 at the time of the 2010 census, a decline of 6.5% since 8,371 in 2000. Cushing was established after the Land Run of 1891 by William "Billy Rae" Little. It was named for Marshall Cushing, private secretary to U.S. Postmaster General John Wanamaker.
The Alaska North Slope is the region of the U.S. state of Alaska located on the northern slope of the Brooks Range along the coast of two marginal seas of the Arctic Ocean, the Chukchi Sea being on the western side of Point Barrow, and the Beaufort Sea on the eastern.
Induced seismicity refers to typically minor earthquakes and tremors that are caused by human activity that alters the stresses and strains on Earth's crust. Most induced seismicity is of a low magnitude. A few sites regularly have larger quakes, such as The Geysers geothermal plant in California which averaged two M4 events and 15 M3 events every year from 2004 to 2009. The Human-Induced Earthquake Database (HiQuake) documents all reported cases of induced seismicity proposed on scientific grounds and is the most complete compilation of its kind.
The 1933 Long Beach earthquake took place on March 10 at 5:54 P.M. PST south of downtown Los Angeles. The epicenter was offshore, southeast of Long Beach, California, on the Newport–Inglewood Fault. The earthquake had a magnitude estimated at 6.4 Mw, and a maximum Mercalli intensity of VIII (Severe). Damage to buildings was widespread throughout Southern California. It resulted in 115 to 120 fatalities and an estimated forty million dollars' worth of property damage, equivalent to $837 million in 2021. The majority of the fatalities resulted from people running out of buildings exposing themselves to the falling debris.
Leonard is an unincorporated community in the southeastern corner of Tulsa County, Oklahoma, United States. The population at the 2020 U.S. Census was 262, compared to 200 in the 2010 census. It is located on U.S. Route 64 at the Wagoner County line. The town serves the surrounding farming area. It is notable for the presence of the nearby Leonard Geophysical Observatory.
James Shannon Buchanan, the fourth president of the University of Oklahoma, was born October 14, 1864, to Thomas and Rebecca Jane Shannon in Franklin, Tennessee. His grandfather, Major John Buchanan, was one of the founders of Nashville, Tennessee. His brother, John P. Buchanan was a governor of Tennessee. He attended public school and the academy at Murfreesboro, Tennessee. Then he attended and graduated from Cumberland University at Lebanon, Tennessee in 1885 with a Bachelor of Science degree. He did graduate work at both Vanderbilt University in 1893-4 and the University of Chicago in 1896. He received his LL.D. from Kingfisher College, Kingfisher, Oklahoma in 1917.
The Geysers is the world's largest geothermal field, containing a complex of 18 geothermal power plants, drawing steam from more than 350 wells, located in the Mayacamas Mountains approximately 72 miles (116 km) north of San Francisco, California.
An injection well is a device that places fluid deep underground into porous rock formations, such as sandstone or limestone, or into or below the shallow soil layer. The fluid may be water, wastewater, brine, or water mixed with industrial chemical waste.
An earthquake occurred with a magnitude 6.9 Mw on 24 March, 2011. It had an epicenter in the eastern part of Shan State in Myanmar with a hypocenter 10 km deep. It had two aftershocks, one of magnitude 4.8, another at magnitude 5.4, and two subsequent shocks at magnitude 5.0 and 6.2. The quake's epicentre was 70 miles (110 km) from the northern Thai city of Chiang Rai, north of Mae Sai and southeast of Kentung.
Hydraulic fracturing, also called fracking, hydrofracking, and hydrofracturing, is a well stimulation technique involving the fracturing of bedrock formations by a pressurized liquid. The process involves the high-pressure injection of "fracking fluid" into a wellbore to create cracks in the deep-rock formations through which natural gas, petroleum, and brine will flow more freely. When the hydraulic pressure is removed from the well, small grains of hydraulic fracturing proppants hold the fractures open.
The 2011 Colorado earthquake occurred on August 22 at 11:46 PM MDT with a moment magnitude of 5.3 and a maximum Mercalli intensity of VII. The epicenter of the intraplate earthquake was 10 mi (20 km) west northwest of Trinidad, Colorado, and 180 mi (290 km) south of Denver, according to the United States Geological Survey (USGS). It was the largest natural earthquake to affect Colorado for more than a hundred years.
The 2011 Oklahoma earthquake was a 5.7 magnitude intraplate earthquake which occurred near Prague, Oklahoma on November 5 at 10:53 p.m. CDT in the U.S. state of Oklahoma. The epicenter of the earthquake was in the vicinity of several active wastewater injection wells. According to the United States Geological Survey (USGS), it was the most powerful earthquake ever recorded in Oklahoma; this record was surpassed by the 2016 Oklahoma earthquake. The previous record was a 5.5 magnitude earthquake that struck near the town of El Reno in 1952. The quake's epicenter was approximately 44 miles (71 km) east-northeast of Oklahoma City, near the town of Sparks and was felt in the neighboring states of Texas, Arkansas, Kansas and Missouri and even as far away as Tennessee and Wisconsin. The quake followed several minor quakes earlier in the day, including a 4.7 magnitude foreshock. The quake had a maximum perceived intensity of VIII (Severe) on the Mercalli intensity scale in the area closest to the epicenter. Numerous aftershocks were detected after the main quake, with a few registering at 4.0 magnitude.
Environmental impact of hydraulic fracturing in the United States has been an issue of public concern, and includes the contamination of ground and surface water, methane emissions, air pollution, migration of gases and hydraulic fracturing chemicals and radionuclides to the surface, the potential mishandling of solid waste, drill cuttings, increased seismicity and associated effects on human and ecosystem health. Research has determined that human health is affected. A number of instances with groundwater contamination have been documented due to well casing failures and illegal disposal practices, including confirmation of chemical, physical, and psychosocial hazards such as pregnancy and birth outcomes, migraine headaches, chronic rhinosinusitis, severe fatigue, asthma exacerbations, and psychological stress. While opponents of water safety regulation claim hydraulic fracturing has never caused any drinking water contamination, adherence to regulation and safety procedures is required to avoid further negative impacts.
The environmental impact of hydraulic fracturing is related to land use and water consumption, air emissions, including methane emissions, brine and fracturing fluid leakage, water contamination, noise pollution, and health. Water and air pollution are the biggest risks to human health from hydraulic fracturing. Research has determined that hydraulic fracturing negatively affects human health and drives climate change.
The Oklahoma earthquake swarms are an ongoing series of human activity-induced earthquakes affecting central Oklahoma, southern Kansas, northern Texas since 2009. Beginning in 2009, the frequency of earthquakes in the U.S. state of Oklahoma rapidly increased from an average of fewer than two 3.0+ magnitude earthquakes per year since 1978 to hundreds each year in the 2014–17 period. Thousands of earthquakes have occurred in Oklahoma and surrounding areas in southern Kansas and North Texas since 2009. Scientific studies attribute the rise in earthquakes to the disposal of wastewater produced during oil extraction that has been injected more deeply into the ground.
The 2016 Oklahoma earthquake occurred on September 3, 2016 near Pawnee, Oklahoma. Measuring 5.8 on the moment magnitude scale, it is the strongest in state history. At 5.8 magnitude, this ties it with the 2011 Virginia earthquake, which was determined after it struck to be the most powerful quake in the eastern United States in the preceding 70 years.
With the development of both conventional and unconventional resources in Canada, induced seismicity caused by anthropological activities has been observed, documented, and studied.
On May 4, 2018, an earthquake with a magnitude of Mw 6.9 struck Hawaii island in the Hawaii archipelago at around 12:33 p.m. local time. The earthquake's epicenter was near the south flank of Kīlauea, which has been the site of seismic and volcanic activity since late April of that year. According to the United States Geological Survey the quake was related to the new lava outbreaks at the volcano, and it resulted in the Hilina Slump moving about two feet. It was the largest earthquake to affect Hawaii since the 1975 earthquake, which affected the same region, killing two people and injuring another 28.