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The Ogallala Aquifer (oh-gə-LAH-lə) is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States. As one of the world's largest aquifers, it underlies an area of approximately 174,000 sq mi (450,000 km 2) in portions of eight states (South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas). [1]
The Barnsdall Main Street Well (also known as Indian Territory Illuminating Oil Company Well #20 Osage County) is a formerly active oil well in the middle of Main Street in the town of Barnsdall, Oklahoma. It is believed to be the only such oil well anywhere in the world.
In hydrology, a well test is conducted to evaluate the amount of water that can be pumped from a particular water well.More specifically, a well test will allow prediction of the maximum rate at which water can be pumped from a well, and the distance that the water level in the well will fall for a given pumping rate and duration of pumping.
The deepest natural gas well is 24,928 feet (7,598 m), in Beckham County, and the deepest producing oil well is 15,500 feet (4,700 m), in Comanche County. [4] Oil drillers active in Oklahoma include Fred M. Manning. [5] The first woman to drill a producing oil well on her own property, and the first female oil operator in Oklahoma was Lulu M ...
Location of the Spraberry Trend in Texas, showing major and nearby cities. Black lines are county boundaries. The Spraberry Trend (also known as the Spraberry Field, Spraberry Oil Field, and Spraberry Formation; sometimes erroneously written as Sprayberry) is a large oil field in the Permian Basin of West Texas, covering large parts of six counties, and having a total area of approximately ...
A non-exempt well is a well capable of producing more than 17.36 gallons per minute, and must submit semi-annual water well production reports to the District at a rate of $0.155 per 1,000 gallons.
The size and shape (slope) of the cone of depression depends on many factors. The pumping rate in the well will affect the size of the cone. Also, the type of aquifer material, such as whether the aquifer is sand, silt, fractured rocks, karst, etc., also will affect how far the cone extends.
Located in South Central Texas, the Edwards Aquifer encompasses an area of approximately 4,350 square miles (11,300 km 2) that extends into parts of 11 counties. [3] The aquifer's boundaries begin at the groundwater divide in Kinney County, East of Brackettville, and extend Eastward through the San Antonio area and then Northeast where the aquifer boundary ends at the Leon River in Bell County ...