These are the Arbor , Arendale, Bode , Clarion , Cresken , Everly , Farrar , Frontenac , Garmore , Liscomb , Moland , Ocheyedan , Ostrander , and Rossfield series in the same family and the Bassett , Cresco , Dinsdale , Merton , and Readlyn series. Arbor soils are on foot slopes and formed partly in local alluvium and partly in firm clay loam glacial till. Aredale soils are friable and contain a lower content of coarse fragments to depths of 40 inches or more. Bode soils formed in moderately fine textured sediments and the underlying friable, calcareous glacial till. Clarion soils are less acid throughout, have carbonates at shallow depths, are friable in the lower part of the B horizon, and have a thinner solum.
Cresken soils have very firm consistence in the solum and substratum.
Everly soils have carbonates at a shallower depth and have a thinner solum. Farrar soils have lower clay and higher sand content in the A horizon and upper part of the B horizon. Frontenac soils have a channery loam 2C horizon within a depth of 20 to 40 inches. Garmore soils have a solum formed in glacial till and lack the two-story materials of the Kenyon soils. Liscomb soils are less acid in the solum and lack a well defined stone line.