Chenango and Tunkhannock soils have water-sorted sand and gravel within the series control section. Hazleton soils contain more than 40 percent sand in the A and B2 horizons. Itswoot soils have silty clay loam in the fine earth fraction of the B and C horizons. Lippitt soils have a paralithic contact at 20 to 40 inches and have fine sandy loam or sandy loam texture in their sola. Parker soils have coarse fragments dominated by granitic rocks and the sand fraction dominated by coarser sands.
Remote soils are in a more moist climate.
Warwick soils have water-sorted sand and gravel of slate and phyllite within the series control section. Watt soils have colors with chroma of 3 or less in the B horizon and bedrock between depths of 20 to 40 inches. Wyoming soils contain more than 50 percent coarser than very fine sand and contain rounded fragments from a number of kinds of rocks. Brownsville soils are on hillsides and summits of the dissected uplands in the Western Allegheny Plateau. Slopes have a plane or convex surface and have gradients of 2 to 70 percent.