Structure is weak fine or medium subangular blocky. Consistency is friable. The Bx horizon has hue of 2.5Y through 7.5YR, value of 4 or 5, chroma of 3 through 6, and it is mottled. It is sandy loam, loam, or silt loam in the fine earth. Structure is weak very coarse prismatic parting to weak medium or thick platy.
Consistency is firm and brittle.
Some pedons have thin BC horizons. It is usually gravelly loamy sand or sandy loam and includes stratified layers of sand, gravel, sandy loam, loam, or silt loam. Bath , Broadalbin , Ira , Lackawanna , Mardin , Rushford , Sodus , Swartswood , Wellsboro , and Wurtsboro soils are in the same family. All of the listed series lack stratified materials within the series control section, do not have C horizons that have loamy sand textures or have Cd horizons. Montauk soils lack Bx horizons and lack mottles above a depth of 30 inches.