Grigsby soils have coarse-loamy control sections. Sensabaugh soils have fine-loamy control sections. Skidmore soils are in a loamy-skeletal particle size class. The remaining associated soils are on stream terraces or on uplands and have argillic horizons. The surface runoff is negligible to low on nearly level slopes and ranges to rapid on steeper banks of streams and rivers.
Permeability is moderate.
Depth to a seasonal water table is greater than 6 feet. The soil is subject to rare to frequent flooding or ponding in depressions for variable duration. Most areas are used for growing corn, tobacco, soybeans, and hay. Forested areas are bottomland hardwoods, such as river birch, yellow-poplar, sycamore, elm, willow, boxelder, oak, hickory, and red maple. Many stream banks and narrow flood plains consist of native canebrakes.