The Kendallville series consists of very deep, well drained soils formed in loamy Wisconsinan till and the overlying mantle of outwash, and in a thin layer of loess in most areas on moraines, kames and eskers.
Permeability is moderate in the solum and moderately slow in the substratum.
Slope ranges from 0 to 40 percent. Kendallville silt loam, on an undulating 4 percent slope in a timothy meadow on the Cable moraine at an elevation of about 1210 feet above mean sea level. 40 degrees 05 minutes 29 seconds N. and long. 83 degrees 37 minutes 42 seconds W., NAD 27. The depth to carbonates is 20 to 40 inches.