They have weak to strong, fine or medium granular, or subangular blocky structure, and friable or very friable consistence. The E horizon, when present, has hue of 7.5YR through 5Y, value of 5 or 6, and chroma of 2 or 3, and is faintly mottled in some pedons. It is very fine sandy loam, loam, silt loam or silty clay loam in the fine-earth fraction. The E horizon has weak or moderate subangular blocky or platy structure, and very friable to firm consistence. The albic material constitutes less than 15 percent by volume of the horizon.
Redoximorphic features are few through many and faint, or they are absent.
The Bt horizon has hue of 7.5YR through 5Y, value of 3 through 6, and chroma of 2 through 4. The horizon has both low and high chroma redoximorphic features. In pedons with matrix colors in chroma of 2, the color is lithochromic and not evidence of an aquic moisture regime. The Bt horizon has silty clay loam or silty clay textures with subhorizons in some pedons ranging from silt loam to clay. They have moderate or strong, medium or coarse angular or subangular blocky structure with or without coarse or very coarse prisms.