These are the Council , Elevasil , Gale , Hixton , and Tarr soils. The well drained Council soils are nearby where there is a loamy colluvial or eolian mantle more than 60 inches thick. The well drained Elevasil and Hixton soils are nearby where there is a loamy mantle 20 to 40 inches thick over the sandstone. Gale soils are nearby where there is a loess mantle 18 to 34 inches thick over the sandstone. Tarr soils are on adjacent side slopes and foot slopes below the Boone soils where the sandy deposits are more than 60 inches thick.
Surface runoff is slow to very rapid.
Permeability is rapid in the sandy mantle and moderately slow or moderate in the sandstone. Many areas are used for woodland. Common trees are northern pin oak or black oak, jack pine, and eastern white pine. Some areas are cleared and used for cropland. Common crops are corn, small grain, and hay.