These are the Brookston , Crosier , Martinsville , and Whitaker soils. The poorly drained Brookston soils are in depressions similar to Rensselaer. The well drained Martinsville and somewhat poorly drained Crosier and Whitaker soils are on swells and knolls on till plains, stream terraces, outwash terraces, or outwash plains. Poorly and very poorly drained. The potential for surface runoff is negligible.
Permeability is moderate.
An intermittent apparent high water table is at a depth of 2 feet above the soil surface to 0.5 feet below during the winter and spring in undrained phases. Most of these soils are used to grow corn, soybeans, and small grain. Native vegetation is swamp grasses and deciduous hardwood forest. In Indiana, Illinois, and Michigan. Newton County, Indiana, 1948.