Colors tend to become redder with depth. Textures are silt loam, loam, clay loam, or silty clay loam in the fine-earth fraction. Clay films on ped faces, pores and on rock fragments are few or common and faint or distinct. Some pedons have a BC horizon. The C horizon has hue of 7.5YR through 2.5Y, value of 3 through 5, and chroma of 2 through 6.
Texture is silt loam, loam or silty clay loam in the fine-earth fraction.
The Albemarle , Allegheny , Allenwood , Arcola , Ardentsville, Aura , Bedington , Birdsboro , Bucks , Butano , Chetwynn, Chester , Chilmark , Clymer , Collington , Cowee , Edgemont , Edneyville , Elsinboro , Eubanks , Frankstown , Freehold , Glenelg , Leck Kill , Meadowville , Matapeake , Murrill , Nixon , Pineville , Quakertown , Rayne , Shelocta , Shouns , Synite, Tate , Thurmount, Ungers and Whiteford series are in the same family. Of these only Butano, Arcola and Cowee soils have bedrock at a depth of 20 to 40 inches. Butano soils occur in the coastal range of mountains of central eastern California with humid mesothermal climate. Arcola soils have Cr and R horizons of red Triassic siltstone and Cowee soils have Cr horizons of crystalline rocks such as gneiss, granite or schist. Other tenative series that are competing are the Brasstown , Fernhaven , Gladstone , Junaluska , Keener , Lonon , Neelsville, and Pigeonroost .