Strippings and iron accumulations in shades of red, brown, yellow, gray, or pink range from none to many . Some horizons are variegated in these colors. Up to 5 percent iron-manganese concretions are in the Bt horizon in some pedons. Few skeletans, brittle masses, weathered glauconitic material, or shale fragments are in the lower parts of the Bt horizon in some pedons. A 2Bt horizon is recognized in some pedons below a depth of 20 inches that has hue of 2.5YR to 10R, value of 3 or 4, and chroma of 2 to 8.
Texture is loam, clay loam, or sandy clay loam.
Strippings and iron accumulations in shades of red, brown, yellow, gray, or pink range from none to many. These are the Addielou , Allen , Avilla , Bama , Dubach , Etowah , Holston , Ironcity , Leesburg , Minvale , Nella , Noboco , Octavia , Pikeville , Ruston , and Warnock series in the same family. Addielou soils have an ochric epipedon more than 20 inches thick and the upper Bt horizons have a more yellow hue. Avilla and Pikeville soils have more than 15 percent coarse fragments in the lower part of the solum. Allen soils formed in alluvium or colluvium from mountain geologies.