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North Fork Yellow Bank River
The Yellow Bank River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed October 5, 2012 tributary of the Minnesota River in western Minnesota in the United States. It is formed by the confluence of two longer streams, the North Fork Yellow Bank River and the South Fork Yellow Bank River, which also flow in northeastern South Dakota. Via the Minnesota River, the Yellow Bank River is part of the drainage basin, watershed of the Mississippi River, draining an area of approximately in an agricultural region. The river was named for yellowish drift (geology), glacial drift in bluffs along the river. Its name was translated from the Sioux language as "Spirit Mountain Creek" by William H. Keating, William Keating in his account of Stephen Harriman Long's expedition to the region in 1823. It was labelled as "Yellow Earth River" on an 1860 map of Minnesota. Geography The river's north and south forks each rise in South Dak ...
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United States
The United States of America (USA), also known as the United States (U.S.) or America, is a country primarily located in North America. It is a federal republic of 50 U.S. state, states and a federal capital district, Washington, D.C. The 48 contiguous states border Canada to the north and Mexico to the south, with the semi-exclave of Alaska in the northwest and the archipelago of Hawaii in the Pacific Ocean. The United States asserts sovereignty over five Territories of the United States, major island territories and United States Minor Outlying Islands, various uninhabited islands in Oceania and the Caribbean. It is a megadiverse country, with the world's List of countries and dependencies by area, third-largest land area and List of countries and dependencies by population, third-largest population, exceeding 340 million. Its three Metropolitan statistical areas by population, largest metropolitan areas are New York metropolitan area, New York, Greater Los Angeles, Los Angel ...
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Sioux Language
Sioux is a Siouan language spoken by over 30,000 Sioux in the United States and Canada, making it the fifth most spoken Indigenous languages of the Americas, Indigenous language in the United States or Canada, behind Navajo language, Navajo, Cree language, Cree, Inuit languages, and Anishinaabe language, Ojibwe.Statistics Canada: 2006 Census
Since 2019, "the language of the Great Sioux Nation, three dialects, Dakota, Lakota, and Nakota" is the official Indigenous language of South Dakota.South Dakota Legislature (2019)

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American Elm
''Ulmus americana'', generally known as the American elm or, less commonly, as the white elm or water elm, is a species of elm native to eastern North America. The trees can live for several hundred years. It is a very hardy species that can withstand low winter temperatures, but it is affected by Dutch elm disease. The wood was seldom utilized until the advent of mechanical sawing. It is the state tree of Massachusetts and North Dakota. Description The American elm is a deciduous tree which, under ideal conditions, can grow to heights of . The trunk may have a diameter at breast height (dbh) of more than , supporting a high, spreading umbrella-like canopy. The leaves are alternate, long, with double-serrate margins and an oblique base. The leaves turn yellow in the fall. The perfect flowers are small, purple-brown and, being wind-pollinated, apetalous. The flowers are also protogynous, the female parts maturing before the male, thus reducing, but not eliminating, self-f ...
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Odessa, Minnesota
Odessa ( ) is a city in Big Stone County, Minnesota, United States. The population was 103 at the 2020 census. History Odessa was platted in 1879 when the railroad was extended to that point. It was named after Odesa, Ukraine. Geography According to the United States Census Bureau, the city has a total area of , all land. U.S. Route 75 and Minnesota State Highway 7 ( co-signed) serves as a main route in the community. Demographics 2010 census As of the census of 2010, there were 135 people, 58 households, and 39 families living in the city. The population density was . There were 68 housing units at an average density of . The racial makeup of the city was 100.0% White. Hispanic or Latino (U.S. Census), Latino of any race were 3.0% of the population. There were 58 households, of which 20.7% had children under the age of 18 living with them, 56.9% were Marriage, married couples living together, 5.2% had a female householder with no husband present, 5.2% had a male househo ...
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Big Stone National Wildlife Refuge
Straddling the headwaters of the Minnesota River in west-central Minnesota, Big Stone National Wildlife Refuge is within the heart of the tallgrass prairie's historic range. Today, less than one-percent of tallgrass prairie remains. Big Stone Refuge serves as the "keeper of the prairie" by working to maintain and restore native prairie habitat while providing optimum nesting cover for waterfowl and other grassland nesting birds. The refuge contains : 1,028 acres in Big Stone County and in Lac qui Parle County. The refuge is located in Minnesota's 7th congressional district. The primary refuge purposes stated in authorizing documents are flood control, recreation, and fish and wildlife conservation. The refuge's principal objective is to provide optimum nesting cover for ground-nesting waterfowl production. Geography and geology The park is located at the headwaters of the Minnesota River, near the border of South Dakota and Minnesota. Big Stone Lake lies a mile north of th ...
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Nassau, Minnesota
Nassau ( ) is a city in Lac qui Parle County, Minnesota, United States. The population was 72 at the 2010 census. History A post office called Nassau was established in 1888, and remained in operation until it was discontinued in 1998. Nassau was platted in 1893. Geography According to the United States Census Bureau, the city has a total area of , all land. Demographics 2010 census As of the census of 2010, there were 72 people, 35 households, and 19 families living in the city. The population density was . There were 42 housing units at an average density of . The racial makeup of the city was 100.0% White. There were 35 households, of which 20.0% had children under the age of 18 living with them, 51.4% were married couples living together, 2.9% had a female householder with no husband present, and 45.7% were non-families. 40.0% of all households were made up of individuals, and 20% had someone living alone who was 65 years of age or older. The average household size wa ...
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Strandburg, South Dakota
Strandburg is a town in southern Grant County, South Dakota, United States. The population was 63 at the 2020 census. Its name is derived from the town's founder, the Swedish John Strandburg. __TOC__ Geography According to the United States Census Bureau, the town has a total area of , all land. Demographics 2010 census As of the census of 2010, there were 72 people, 27 households, and 17 families residing in the town. The population density was . There were 36 housing units at an average density of . The racial makeup of the town was 95.8% White and 4.2% Native American. There were 27 households, of which 29.6% had children under the age of 18 living with them, 51.9% were married couples living together, 3.7% had a female householder with no husband present, 7.4% had a male householder with no wife present, and 37.0% were non-families. 37.0% of all households were made up of individuals, and 14.8% had someone living alone who was 65 years of age or older. The average hou ...
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Grant County, South Dakota
Grant County is a County (United States), county in the U.S. state of South Dakota. As of the 2020 United States census, 2020 census, the population was 7,556. The county seat is Milbank, South Dakota, Milbank. The county was founded in 1873 and organized in 1878. It is named for Ulysses S. Grant, 18th President of the United States. Geography Grant County lies on the east side of South Dakota. Its east boundary line abuts the west boundary line of the state of Minnesota. The terrain consists of rolling hills, sloping to the northeast. The area is largely devoted to agriculture. The highest point of the terrain is on the county's south boundary line, towards its southwest corner, at ASL. Grant County has a total area of , of which is land and (0.9%) is water. The List of U.S. states by elevation, lowest point in the state of South Dakota is located on Big Stone Lake at Big Stone City, South Dakota, Big Stone City in Grant County, adjacent to Ortonville, Minnesota, where th ...
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South Shore, South Dakota
South Shore is a town in Codington County, South Dakota, United States. The population was 189 at the 2020 census. It is part of the Watertown, South Dakota Micropolitan Statistical Area. Geography According to the United States Census Bureau, the town has a total area of , all land. The town takes its name from its location on Punished Woman Lake. Demographics 2010 census As of the census of 2010, there were 225 people, 99 households, and 56 families residing in the town. The population density was . There were 122 housing units at an average density of . The racial makeup of the town was 95.1% White, 0.4% African American, 1.8% Native American, and 2.7% from two or more races. Hispanic or Latino of any race were 1.8% of the population. There were 99 households, of which 29.3% had children under the age of 18 living with them, 44.4% were married couples living together, 6.1% had a female householder with no husband present, 6.1% had a male householder with no wife pres ...
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Till Plain
Till plains are an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed with melts out of the glacier in irregular heaps, forming rolling hills. Till plains are common in areas such as the Midwestern United States, due to multiple glaciation events that occurred in the Holocene epoch. During this period, the Laurentide Ice Sheet advanced and retreated during the Pleistocene epoch. Till plains formed by the Wisconsin glaciation cover much of the Midwest, including North Dakota, South Dakota, Indiana, Minnesota, Wisconsin, Iowa, Illinois, and northern Ohio (see Glacial till plains (Ohio)). Characteristics Till plains are large flat or gently sloping areas of land on which glacial till has been deposited from a melted glacier. In some areas, these depositions can be up to hundreds of feet thick. The morphology of the till plain is ge ...
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Missouri River
The Missouri River is a river in the Central United States, Central and Mountain states, Mountain West regions of the United States. The nation's longest, it rises in the eastern Centennial Mountains of the Bitterroot Range of the Rocky Mountains of southwestern Montana, then flows east and south for before entering the Mississippi River north of St. Louis, Missouri. The river drains Semi-arid climate, semi-arid Drainage basin, watershed of more than 500,000 square miles (1,300,000 km2), which includes parts of ten U.S. states and two Canadian provinces. Although a tributary of the Mississippi, the Missouri River is slightly longer and carries a comparable volume of water, though a fellow tributary (Ohio River) carries more water. When combined with the lower Mississippi River, it forms the List of rivers by length, world's fourth-longest river system. For over 12,000 years, people have depended on the Missouri River and its Tributary, tributaries as a source of sustena ...
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Plateau
In geology and physical geography, a plateau (; ; : plateaus or plateaux), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wider ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, plate tectonics movements, and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. They may be formed by upwelling of volcanic magma or extrusion of lava. The underlining mechanism in forming p ...
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