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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 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]
Optima Lake was built to be a reservoir in Texas County, Oklahoma.The site is just north of Hardesty and east of Guymon in the Oklahoma Panhandle. [2]The earthen Optima Lake Dam (National ID # OK20510) was completed in 1978 (47 years ago) () by the United States Army Corps of Engineers, with a height of 120 feet (37 m), and a length at its crest of 16,875 feet (5,144 m). [3]
Edwards and Trinity Aquifers map. The Edwards Aquifer is one of the most prolific artesian aquifers in the world. [2] Located on the eastern edge of the Edwards Plateau in the U.S. state of Texas, it is the source of drinking water for two million people, and is the primary water supply for agriculture and industry in the aquifer's region.
This is a list of artesian wells in the United States.. Artesian, South Dakota wells; Artesian, Washington wells; Artesian Commons, Olympia, Washington; The Artesian Hotel, Sulphur, Oklahoma
Lake Overholser is a reservoir within the city limits of Oklahoma City, Oklahoma. [ a ] Lake Overholser is formed by Overholser Dam on the North Canadian River in Oklahoma County, Oklahoma . [ b ] The lake is 2.9 miles (4.7 km) west of Bethany [ 2 ] and 4.4 mi (7.1 km) from Yukon .
The Texas and Oklahoma red beds are sedimentary rocks, mostly consisting of sandstone and red mudstone. [8] The red color of the rocks is due to the presence of ferric oxide . [ 9 ] The rocks were deposited during the early Permian in a warm, moist climate, [ 10 ] with seasonal periods of dry conditions.
The Deep Fork begins in and around northern Oklahoma City and flows eastward through Oklahoma County where five miles of the river is impounded by Arcadia Lake.Below the lake the river crosses into Lincoln County, winds back and forth across the Creek–Okfuskee county lines, crosses into Okmulgee County, meanders through the 9,600-acre (39 km 2) Deep Fork National Wildlife Refuge near the ...