The Bt commonly is loam, silt loam, silty clay loam, clay loam, or channery analogues of these textures. It is extremely acid to medium acid in the upper part and very strongly acid to slightly acid in the lower part. Some pedons have a 2Bt horizon up to 24 inches thick. They are very strongly acid to slightly acid except for the C horizon that ranges to neutral. Thin strata of coarser textures from weathered sandstone are in some pedons.
Bedrock is interbedded, fractured siltstone or fine-grained sandstone and soft, red clay shale.
These are the Amanda , Belmont , Belmore , Chenault , Chili , Coggon , Conestoga , Douds , El Dara , Gallman , Grellton , Hayden , Hebron , Hickory , High Gap , Hollinger , Kalamazoo , Kanawha , Kendallville , Kidder , Kosciusko , Leroy , Letort , Lindley , Mandeville , Martinsville , McHenry , Miami , Mifflin , Military , Nodine , Norden , Ockley , Owosso , Pecatonica , Princeton , Rawson , Relay , Renova , Richland , Riddles , Roseville, Sisson , Skelton , Strawn , Theresa , Wawasee , Westville , Whalan , Woodbine , and Wykoff series. Amanda, Coggon, Hayden, Hickory, Kendallville, Kidder, Leroy, Lindley, McHenry, Miami, Owosso, Pecatonica, Renova, Riddles, Roseville, Strawn, Theresa, Wawasee, Westville, Woodbine, and Wykoff soils have glacial drift within a depth of 40 inches and have coarse fragments of mixed lithology including some crystalline rocks. Belmont soils commonly are not as acid in the lower part of the solum and have coarse fragments mainly of limestone and are underlain by a lithic contact at a depth of 40 to 60 inches. Belmore, Chenault, Chili, Douds, El Dara, Gallman, Kalamazoo, Kanawha, Kosciusko, Martinsville, Nodine, Ockley, and Sisson soils have evidence of stratification or have rounded coarse fragments. Conestoga, Hollinger, and Letort soils have a significant mica content.