These are the Amery , Haugen , Freeon , Magnor , Santiago , and Siouxcreek soils. The well drained Amery soils and the moderately well drained Haugen soils are in landscape positions similar to or slightly lower than those of Arland soils where the glacial till is more than 5 feet thick over the sandstone. The moderately well drained Freeon soils and the well drained Santiago soils are in similar or slightly lower landscape positions than Arland soils and the somewhat poorly drained Magnor soils are in lower landscape positions in drainageways and depressions. Freeon, Santiago, and Magnor soils are all in areas where there is a loess mantle 12 to 36 inches thick over till and there is no sandstone within a depth of 5 feet. The somewhat poorly drained Siouxcreek soils are in drainageways and depressions adjacent to Arland soils.
Surface runoff is slow to very rapid.
Permeability is moderate or moderately rapid in the silty and loamy mantle and moderately slow or moderate in the sandstone. Some pedons have sandy 2Bt or 2BC horizons with moderately rapid or rapid permeability. Corn, small grains, and hay are the principal crops. The more sloping areas are used for pastureland or woodland. Native vegetation is mixed hardwood forest.