The Gilford and Hanska soils contain less fine and very fine sand in the solum and C horizon and lack the loamy strata. In addition, Gilford soils have a warmer more humid climate. The Jubilee soils have few to many mica flakes in the profile and formed in nonglacial sediments. The Lyles soils have less than 85 percent of the sand fraction in the fine and very fine and has up to 10 percent fine gravel. Toolesboro soils have redder hue and higher chroma in much of the Bg horizon and a lower proportion of fine and very fine sand.
Zadoc soils have an accumulation of iron oxides in the solum.
These soils have plane slopes with gradient of less than 2 percent. They commonly are on the deltaic portions of glacial lake plains and less commmonly on outwash plains, and stream terraces. They formed in loamy and sandy lacustrine or outwash sediments that are dominated by fine and very fine sand and that commonly are stratified. Loamy glacial till or silty lacustrine sediments underlie these sediments at depths below 50 inches in some pedons. These sediments are of the Des Moines lobe of the Late Wisconsinan glaciation.