The competing Carlow , Wabash , and Zook soils and the Coppock , Humeston , and Vesser soils are common landscape associates. Coppock soils lack a mollic epipedon and are fine-silty. Humeston soils have a distinct E horizon, dark colored, more clayey B horizon, and more contrast in texture between the A and B horizons. Vesser soils have a distinct E horizon and are fine-silty. Runoff is slow.
Permeability is moderately slow.
The soil floods commonly. Depth to an intermittent apparent water table is 0 to 1 foot at some time from November through July in most years. Most areas are cultivated. Corn, soybeans, small grains, and legume hays are the major crops. Some small areas are in woods and bluegrass pasture.