Some pedons have secondary carbonate accumulations, although most of these subhorizons have lower calcium carbonate equivalent than the parent material. Calcium carbonate equivalent is 0 to 30 percent. Those horizons that have 20 to 25 percent clay must also have 10 percent or more very fine sand. Sand content averages 35 to 60 percent. Silt content averages 35 to 45 percent.
Texture is loam or sandy loam.
Hue is 7.5YR or 10YR, value is 4 to 6, and chroma is 3 to 6. Some pedons have redoximorphic features. Many pedons have secondary carbonate accumulations in the upper part. The calcium carbonate equivalent is 25 to 40 percent. Belmont, Chenault, High Gap, Lumberton, Mandeville, Mifflin, Military, Nodine, Nollville, Norden, Whalan, and Woodbine soils have lithic or paralithic contacts within a depth of 60 inches.