The BC horizon has colors similar to the Bt horizon. It is fine sandy loam, silt loam, loamy fine sand, loamy very fine sand or very fine sandy loam. Thin strata of sand, silty clay loam or silty clay are in some pedons. Some pedons have a Bk horizon with colors and textures similar to the BC which contain soft accumulations of calcium carbonate. The Ck horizon has 10YR or 7.5YR hue, value of 5 or 6 and chroma of 1 to 4.
Redoximorphic features range from few to many.
It is stratified with layers of silt loam, fine sandy loam, very fine sandy loam, loamy very fine sand, fine sand, or very fine sand or is dominated by one of these textures. Some pedons have thin strata of sand, silty clay loam, or silty clay. These are the Brady , Budd , Oakton and Wasepi series. These soils do not have stratified material within a depth of 40 inches. Dixboro soils are on lake plains, outwash plains, and deltas.