Redoximorphic accumulations and depletions are in shades of brown or gray. Texture is silt loam or silt. Redoximorphic accumulations and depletions are in shades of brown or gray. Texture is silt loam or silty clay loam. Redoximorphic accumulations and depletions are in shades of yellow, brown or gray.
Texture is silt loam or silty clay loam.
Redoximorphic accumulations and depletions are in shades of yellow, brown and gray. These iclude the Adaton , Amagon and Dundee series in this family. Adaton, Amagon, and Dundee soils have A and E horizons with a combined thickness of less than 24 inches. Amagon soils have more than 15 percent sand coarser than very fine in the upper 20 inches of the argillic horizon. Adaton and Dundee soils typically do not have E horizons.