These are the Conser , Kokomo , Konert , Lippincott , Millsdale , Pewamo , and Rowe soils in the same family and the Ashkum , Bono , Hoytville , Lorain , Montgomery , Peotone , and Ragsdale soils. Millsdale soils have a lithic contact at depths less than 40 inches. Ashkum, Bono, Montgomery, and Peotone soils do not have argillic horizons. In addition, Ashkum and Peotone soils have 2C horizons formed in glacial drift. Hoytville and Lorain soils do not have mollic epipedons.
Ragsdale soils are fine-silty.
Calamine soils typically are on broad nearly level areas, in slightly depressed areas and swales, on foot slopes, where seepage occurs, and in nearly level basins of old flood plains. Slopes are typically 0 to 3 percent, but on foot slopes, where seepage occurs, slopes range to 12 percent. They formed in 15 to 30 inches of loess, or other silty deposits, and in the underlying residuum weathered from calcareous shale of Ordovician age. Mean annual temperature is about 45 to 53 degrees F, and mean annual precipitation ranges between 25 and 35 inches. These are the Ashdale , Derinda , Dodgeville , Keltner , Schapville , and Shullsburg soils.