the plains called by the des position of loess are called
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Loess
Encyclopedic entry. In some parts of the world, windblown dust and silt blanket the land. This layer of fine, mineral-rich material is called loess.
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When the climate warmed up, the warm temperatures melted the glaciers creating tremendous flows of water down into a valley or river, and exposing vast plains of mud. ... Often several loess deposits are stacked on top of each other, because each individual glacier produced new loess deposits.
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