The Bt horizon has hue of 2.5YR through 7.5YR value of 4 or 5 and chroma of 3 or 4. Texture is silty clay loam, silt loam, or clay loam, with or without thin subhorizons of silty clay in the fine-earth fraction. The B horizon has moderate or strong fine to coarse subangular or angular blocky structure. BC horizons with similar colors and textures are in some pedons. The C horizon has colors that are similar to that of the B horizon.
Texture is silty clay loam, clay loam, sandy clay loam, or silty clay in the fine-earth fraction.
These are the Amanda, 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, Rainsville, Rawson, Relay, Renova, Riddles, Richardville, Richland, Sisson, Skelton, Strawn, Summitville, Theresa, Wawasee, Westville, Whalan, Woodbine, and Wykoff series in the same family, and Culleoka, Peabody, Upshur and Westmoreland series in related families. Amanda, Kosciusko, Rainsville, Richardville, Wawasee, and Wykoff soils sola formed in glacial till or outwash. The Belmore, Chili, and Kendalville soils have waterworn gravels throughout Chenault soils do not allow B horizons with 5YR colors. Coggon, Gallman, Pectonica, Richland, Skelton and Westville soils have thicker sola. Conestoga and Hollinger soils have coarse fragments of quartz, chert and schist and have a significant mica content.