All have lower base saturation. In addition, Culleoka and Ryder soils are moderately deep to bedrock. Duffield soils are very deep to bedrock. Westmoreland soils have higher mean annual precipitation. Nollville soils are on gently sloping to moderately steep convex upland ridges of low relief.
Ridges are usually long and narrow and have a general north-south orientation.
Relief is usually less than 100 feet. Slopes range from 3 to 35 percent. These soils formed in residuum from argillaceous limestone. Hagerstown soils have hue redder than 7.5YR in the Bt horizon and average more than 35 percent clay in the control section. Runoff is medium to very rapid.