Camelback soils are loamy-skeletal, have mollic epipedons thicker than 16 inches, and have frigid soil temperatures. Lanoak soils have mollic epipedons thicker than 16 inches, lack argillic horizons, and have frigid soil temperatures. Pavohroo soils have mollic epipedons thicker than 16 inches and are fine-loamy. Rin soils are coarse-silty, lack argillic horizons and have mollic epipedons thicker than 16 inches. Robin soils have mollic epipedons thicker than 16 inches and are greater than 20 inches to the top of the argillic horizon.
Sedgway soils are loamy-skeletal.
Turnerville soils lack mollic epipedons. Camelback soils are on convex south slopes. Lanark, Lanoak and Rin soils are on south slopes. Pavohroo soils are on concave north slopes. Robin soils are on stable south slopes.