It has weak to strong, thin to thick platy or weak to strong very coarse prismatic structure which in some pedons parts to weak to strong, thin to thick platy, or the horizon is massive. All structure in the Cd horizon is considered inherited from the parent material. Consistence is firm or very firm. These are the Chesuncook , Crary , Dixfield , Dixmont , Mundal , Peru , Skerry , Sunapee , Telos , and Worden series in the same family. Chesuncook and Telos soils have more than 10 percent clay in the particle-size control section.
Crary soils have a thin aeolian or water deposited mantle.
Dixmont and Sunapee soils do not have dense basal till. Mundal soils have a spodic horizon greater than 18 inches thick. Peru and Skerry soils have redoximorphic features at greater depths and are moderately well drained. Worden soils have a spodic horizon greater than 18 inches thick or a Bh horizon greater than 4 inches thick. Colonel soils are on glaciated uplands.