The Bt horizons have hue of 10YR or 7.5YR, value of 5 or 6 and chroma of 6 or 8. Texture is loam, clay loam, or sandy clay loam in the fine earth fraction. The C horizon has hue of 10YR or 7.5YR value of 5 or 6 and chroma of 6 or 8. Texture is loam, fine sandy loam, or sandy loam in the fine earth fraction. Some pedons have a discontinuity below the control section with hue of 7.5YR, 5YR, or 2.5YR, value of 4 or 5 and chroma of 5 to 8.
Texture is loam, clay loam, or clay in the fine earth fraction.
Transitional horizons occur between major horizons in many pedons. They have properties and features similar to adjacent horizons. Additionally, series that were formerly in the same family, but have not been updated to the latest editions of Keys to Soil Taxonomy include Alonzville , Bailegap , Beersheba , Gunstock , Harmiller , Marr , Shinbone and Sunnyside series. Alonzville soils formed in alluvium. Bailgap, Lonewood, Riney and Sunnyside soils have hue of 7.5YR or redder in some part of the Bt horizon.