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Lake Stanley Draper is a reservoir in southeast Oklahoma City, United States. It is one of three municipal reservoirs in the city. [a] Principal construction on the reservoir occurred between 1962-1963. Upon completion it was named after the long-time director of the Oklahoma City Chamber of Commerce, Stanley Draper. [3]
A water level device showing both ends at the same height. A water level (Greek: Aλφαδολάστιχο or (υδροστάθμη) [Alfadolasticho]) is a siphon utilizing two or more parts of the liquid water surface to establish a local horizontal line or plane of reference.
The river held at that level for two hours, but by then the level at the east end of the dam failed, sending the downstream river level 2 feet (0.61 m) higher in a matter of minutes. [8] By the time the crisis had passed, Jones, Oklahoma and Spencer, Oklahoma, two towns downstream of Oklahoma City, had been surrounded by water. The official ...
Lake Hefner is a reservoir in northwestern Oklahoma City, Oklahoma.It was built in the 1940s to expand the water supply for the city of Oklahoma City, [2]. It is named after Robert A. Hefner, who served as mayor of Oklahoma City from April 11, 1939, to April 8, 1947, but was originally named the "Bluff Creek Reservoir."
In Oklahoma, streamwater is defined to include “water in ponds, lakes, reservoirs, and playa lakes” [2] (or dry lakes). Streamwater is considered to be publicly owned; the Oklahoma Water Resources board is responsible for appropriation for all areas of the State of Oklahoma except the Grand River basin, where the Grand River Dam Authority (GRDA) has responsibility for allocation on a use ...
Underwater construction is industrial construction in an underwater environment. It is a part of the marine construction industry. [1] It can involve the use of a variety of building materials, mainly concrete and steel. There is often, but not necessarily, a significant component of commercial diving involved.
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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]