what are loess plains
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Loess is an aeolian sediment formed by the accumulation of wind-blown silt, typically in the 20–50 micrometer size range, twenty percent or less clay and the balance equal parts sand and silt that are loosely cemented by calcium carbonate
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Dissected Loess Plains. Dissected Loess Plains contains loess (wind blown silt) deposits that are among the thickest (200+ feet) in North America. Eroded canyons and deep valleys that occur at this site reveal the geological history of the Loess Plains better than any other place in the Great Plains.
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