The Linden and Pope series are in the same family. The Linden and Pope soils do not contain mica and in addition, the Linden soils have B horizons with dominant hues of 5YR or redder. Pope soils developed in sediments derived from sandstons and shales. The Barbour , Bermudian , Clifty , Craigsville , Gladden , Hadley and Ondawa series are similar soils in related families. Clifty soils have more than 18 percent clay in the particle-size control section.
Gladden soils are very cherty in the lower part of the solum and have siliceous mineralogy.
Hadley soils have less than 15 percent coarser than very fine sand in the particle size control section. Ondawa soils are frigid. Comus soils are on floodplains in the northern Atlantic Coastal Plain and the mesic Southern Piedmont. Slopes range from 0 to 8 percent. Comus soils formed in recent alluvium containing moderate to large amounts of mica.