Canfield , Rittman , and Wooster soils which have fragipan horizons are adjacent where Wisconsinan till deposits are more than 40 inches thick. Chagrin , Holly , Lobdell , and Orrville soils are on nearby flood plains. Chili , Conotton , and Wheeling soils which do not have a lithic contact are on adjacent glacial outwash and terraces. Hanover and Titusville soils which have fragipan horizons are adjacent where Illinoian till is more than 40 inches thick. The potential for surface runoff is very low to high depending on slope.
Permeability is moderate.
Most areas on slopes less than 18 percent are cleared and used for cultivated crops. Corn, small grains, and mixed hay are principal crops. Some areas are pastured. Orchards are common, especially in areas within a few miles of Lake Erie. Many areas are in nonagricultural uses.