Redox depletions with chroma of 2 or less are below 30 inches. Texture is silt loam or silty clay loam. The 2Bt and 3Bt horizons have hue of 2.5YR or 5YR, value of 4 or 5, and chroma of 4 to 8, or hue of 2.5YR, value of 3, and chroma of 4 or 6. Mottles, or redox concentrations and depletions are in shades of brown, red and gray. Some subhorizons, have no dominant hue and are mottled in shades of red, brown, yellow and gray.
Texture is clay loam, silty clay loam, silty clay, clay and their gravelly or very gravelly analogs.
These are the Baylis , Crider , Hootentown , Ryker , Stinesville , and Winnipeg series. Baylis, Crider, Ryker, Stinesville, and Winnipeg soils soils formed in loess over residuum or glacial drift. These soils typically contain less sand above the discontinuity. In addition, they have hues of 7.5YR or browner in the upper part of the argillic horizon. Hootentown soils formed in alluvium.