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Ogallala Changes In Feet 1980-1995 USGS
Ogallala may refer to: *Ogallala, Nebraska *Ogallala Aquifer The Ogallala Aquifer () is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States. One of the world's largest aquifers, it underlies an area of approximately in porti ... * Ogallala Commons * Ogallala Formation * Oglala Lakota (Sioux) {{geodis ...
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Ogallala, Nebraska
Ogallala is a city in and the county seat of Keith County, Nebraska, United States. The population was 4,737 at the 2010 census. In the days of the Nebraska Territory, the city was a stop on the Pony Express and later along the transcontinental railroad. The Ogallala Aquifer was named after the city. History Ogallala first gained fame as a terminus for cattle drives that traveled from Texas to the Union Pacific railhead located there. These trails are known as the Western or Great Western trails. The Union Pacific Railroad reached Ogallala on May 24, 1867. The city itself was not laid out until 1875 and not incorporated until 1884 The town's name comes from the Oglala Sioux tribe. Geography Ogallala is located at (41.128806, -101.719460). According to the United States Census Bureau, the city has a total area of , of which is land and is water. Ogallala is in the US Mountain Time Zone (UTC−7/-6). Ogallala is close to Lake McConaughy, a large man-made lake and a state ...
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Ogallala Aquifer
The Ogallala Aquifer () is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States. One of the world's largest aquifers, it underlies an area of approximately in portions of eight states (South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas). It was named in 1898 by geologist N. H. Darton from its type locality near the town of Ogallala, Nebraska. The aquifer is part of the High Plains Aquifer System, and resides in the Ogallala Formation, which is the principal geologic unit underlying 80% of the High Plains. Large-scale extraction for agricultural purposes started after World War II due partially to center pivot irrigation and to the adaptation of automotive engines for groundwater wells. Today about 27% of the irrigated land in the entire United States lies over the aquifer, which yields about 30% of the ground water used for irrigation in the United States. The aquif ...
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Ogallala Commons
The Ogallala Aquifer () is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States. One of the world's largest aquifers, it underlies an area of approximately in portions of eight states (South Dakota, Nebraska, Wyoming, Colorado, Kansas, Oklahoma, New Mexico, and Texas). It was named in 1898 by geologist N. H. Darton from its type locality near the town of Ogallala, Nebraska. The aquifer is part of the High Plains Aquifer System, and resides in the Ogallala Formation, which is the principal geologic unit underlying 80% of the High Plains. Large-scale extraction for agricultural purposes started after World War II due partially to center pivot irrigation and to the adaptation of automotive engines for groundwater wells. Today about 27% of the irrigated land in the entire United States lies over the aquifer, which yields about 30% of the ground water used for irrigation in the United States. The aquife ...
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Ogallala Formation
The Ogallala Formation is a Miocene to early Pliocene geologic formation in the central High Plains of the western United States and the location of the Ogallala Aquifer. In Nebraska and South Dakota it is also classified as the Ogallala Group. Notably, it records the North American Land Mammal Ages (NALMAs) Hemphillian, Clarendonian, and Barstovian. It also includes an excellent record of grass seeds and other plant seeds, which can be used for biostratigraphic dating within the formation. The Ogallala Formation outcrops of Lake Meredith National Recreation Area preserve fish fossils. Similar specimens from the same unit are found at Alibates Flint Quarries National Monument in Texas. Development At the beginning of the Rocky Mountains uplift, the final floor of the Western Interior Seaway was elevated several thousand feet (thousands of meters) above sea level. The previous pattern of erosion of material from the northeast into the midcontinent was largely reversed so that m ...
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