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Rainwater Basin

1963 establishments in NebraskaIUCN Category IVLandforms of Adams County, NebraskaLandforms of Clay County, NebraskaLandforms of Fillmore County, Nebraska
Landforms of Franklin County, NebraskaLandforms of Gosper County, NebraskaLandforms of Hall County, NebraskaLandforms of Hamilton County, NebraskaLandforms of Kearney County, NebraskaLandforms of Phelps County, NebraskaLandforms of Saline County, NebraskaLandforms of Seward County, NebraskaLandforms of York County, NebraskaNational Wildlife Refuges in NebraskaProtected areas established in 1963Protected areas of Adams County, NebraskaProtected areas of Clay County, NebraskaProtected areas of Fillmore County, NebraskaProtected areas of Franklin County, NebraskaProtected areas of Gosper County, NebraskaProtected areas of Hall County, NebraskaProtected areas of Hamilton County, NebraskaProtected areas of Kearney County, NebraskaProtected areas of Phelps County, NebraskaProtected areas of Saline County, NebraskaProtected areas of Seward County, NebraskaProtected areas of York County, NebraskaRegions of NebraskaWetlands of Nebraska

The Rainwater Basin wetland region is a 4,200 sq mi (11,000 km2) loess plain located south of the Platte River in south-central Nebraska. It lies principally in Adams, Butler, Clay, Fillmore, Hamilton, Kearney, Phelps, Polk, Saline, Seward, and York counties and extends into adjacent areas of southeastern Hall, northern Franklin, northern Nuckolls, western Saline, northern Thayer and northwestern Webster counties. Before European settlement, this plain was covered by prairie grasslands interspersed with thousands of ephemeral playa wetlands, called Rainwater Basins. Informally and locally, individual Nebraska Rainwater Basins are referred to as rainbasins, basins, lagoons, lakes, ponds, marshes, hay marshes, and lakes marshes. To the west, a tallgrass prairie in the east once gradually transitioned into mixed grass prairie. Currently, the Rainwater Basin wetland region is covered by farms, mainly growing corn and soybeans. Several, interspersed, stream courses, of which largest is the Big Blue River and its tributaries, drain this region. Riparian woodlands and upland slopes possessing oak woodlands are associated with these streams. In the spring and fall months, millions of migratory birds pass through the region to feed and rest. Along with riparian habitats associated Platte River, Big Blue River, its tributaries, and smaller streams, Rainwater Basins are a major component of the Central Flyway of North America.Prior to its agricultural development in historic times, the Rainwater Basin wetland region was characterized by numerous playa wetlands, Rainwater Basins, numbering in the thousands. The shallow depressions, in which these wetlands occur are lined with a nearly impervious layer of clayey soil, a claypan, that prohibits surface water from penetrating the subsoil. As a result, Rainwater Basins are not naturally influenced by the water table and the sole source of water is run-off in the form of rain, snow and, currently, drainage from crop irrigation. Because the primary source of water for these wetlands is precipitation, they annually vary in depth, expanse and seasonality due to changes in precipitation regimes and are called Rainwater Basins.

Excerpt from the Wikipedia article Rainwater Basin (License: CC BY-SA 3.0, Authors).

Rainwater Basin
East 31st Street, Kearney

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N 40.708333333333 ° E -99.081111111111 °
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CHI Health Good Samaritan

East 31st Street 10
68847 Kearney
Nebraska, United States
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Catholic Health Initiatives

call+13088657100

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chihealthgoodsamaritan.org

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