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The water table is the upper surface of the zone of saturation. The zone of saturation is where the pores and fractures of the ground are saturated with groundwater, [1] which may be fresh, saline, or brackish, depending on the locality. It can also be simply explained as the depth below which the ground is saturated.
Watertable control. In geotechnical engineering, watertable control is the practice of controlling the height of the water table by drainage. Its main applications are in agricultural land (to improve the crop yield using agricultural drainage systems) and in cities to manage the extensive underground infrastructure that includes the ...
Jonesboro (/ ˈ dʒ oʊ n z b ʌ r ə /) is a city located on Crowley's Ridge in the northeastern corner of the U.S. State of Arkansas. Jonesboro is one of two county seats of Craighead County . In 2023, the city had an estimated population of 80,560, [ 4 ] making it the fifth-most populous city in Arkansas .
An aquifer is an underground layer of water -bearing material, consisting of permeable or fractured rock, or of unconsolidated materials (gravel, sand, or silt). Aquifers vary greatly in their characteristics. The study of water flow in aquifers and the characterization of aquifers is called hydrogeology. Related terms include aquitard, which ...
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Type. Building. Designated. June 11, 1992. Reference no. 92000617. Mammoth Spring State Park is a 62.5-acre (25.3 ha) Arkansas state park in Fulton County, Arkansas in the United States. The park is located surrounding National Natural Landmark of the same name to provide recreation and interpretation for visitors. [2]
Beaver Lake, Bull Shoals Lake, and Table Rock Lake are man-made lakes or reservoirs created by the U.S. Army Corps of Engineers under the authority of the Flood Control Act of 1938. [11] Bull Shoals Dam near Mountain Home, Arkansas was constructed from 1947 to 1951 at a cost of $86 million [12] and is the 5th largest concrete dam in the United ...
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]