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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]
Aquifers of the United States Withdrawal rates from the Ogallala Aquifer.. This is a list of some aquifers in the United States.. Map of major US aquifers by rock type. An aquifer is a geologic formation, a group of formations, or a part of a formation that contains sufficient saturated permeable material to yield significant quantities of water to groundwater wells and springs.
The greatest threat to the Blue River is the withdrawal of water for human use from the Arbuckle-Simpson Aquifer. Withdrawal exceeds recharge which reduces the flow of the river. In 2011, to help protect the aquifer and the land, the Nature Conservancy purchased 490 acres of land along the river near Connerville.
The Ogallala aquifer is the principal source of water for agriculture in western Kansas. It’s not an underground lake as some believe but saturated sediments that have been deposited over the ...
Aquifers of the United States are organized by national principal aquifer codes and names assigned by the National Water Information System (NWIS). Aquifers are identified by a geohydrologic unit code (a three-digit number related to the age of the formation) followed by a 4 or 5 character abbreviation for the geologic unit or aquifer name. [10]
A geological expert tells a legislative committee that Oklahoma needs to work harder to conserve water for future needs. Oklahoma is using more water than ever, but not replenishing underground ...
The Oklahoma Water Resources Board is paying for numerous studies to forecast water supply through 2075.
The Garber Sandstone is a geologic formation from the Permian Period in Oklahoma. It serves as an important aquifer, the Garber-Wellington Aquifer, in Logan, Oklahoma, and Cleveland counties of central Oklahoma. [2] The upper portion of the Garber is associated with extensive baryte mineralization associated with desert rose occurrences in the ...