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The Rainwater Basin wetland region is a 4,200 sq mi (11,000 km 2) loess plain located south of the Platte River in south-central Nebraska. [1] 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 ...
Fillmore County lies within the eastern portion of Nebraska's loess plain, a region of soil deposited by the wind between 25,000 and 13,000 years ago, forming a plain that slopes to the southeast. The Big Blue and its tributaries have incised channels into the loess surface in places, but in much of the county the original plain remains.
English: Fillmore County Minnesota 42 % Savanna Soils. Sourced-from Web Soil Survey (WSS), Natural Resources Conservation Service, United States Department of Agriculture. Sourced-from Web Soil Survey (WSS), Natural Resources Conservation Service, United States Department of Agriculture.
The county has a total area of 862 square miles (2,230 km 2), of which 861 square miles (2,230 km 2) is land and 0.8 square miles (2.1 km 2) (0.09%) is water. [8] The county is part of the Driftless Area or Paleozoic plateau. This part of Minnesota was ice-free during the last ice age. Fillmore County also displays a karst topography.
Spring Valley Township is a township in Fillmore County, Minnesota, United States. The population was 590 at the 2000 census. The population was 590 at the 2000 census. Spring Valley Township was organized in 1858, and named for several springs within its borders.
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The creek was named for the rush plants lining its banks. [2]Rush Creek suffered severe flooding in the Southeast Minnesota floods of August 18–20, 2007. [3]According to the Minnesota Department of Natural Resources, fish species present in Rush Creek include: brown trout, brook trout, rainbow trout, white sucker, American brook lamprey, creek chub, northern hog sucker, golden redhorse ...