loess deposits are formed far away from the desert
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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.
Loess is mostly created by wind, but can also be formed by glaciers. When glaciers grind rocks to a fine powder, loess can form. Streams carry the powder to the end of the glacier. This sediment becomes loess.
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