Loess is a fine-grained deposit that has been windblown to it's location. It has the constancy of clay. It is often found in the Mississippi Valley.
Loess is an aeolian sediment formed by the accumulation of wind-blown silt, typically in the 20–50 micrometre size range, twenty percent or less clay and the balance equal parts sand and silt2 that are loosely cemented by calcium carbonate.It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs.
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