Paxton (soil)

The Paxton series consists of deep, well-drained soils formed in glacial till derived mainly from schist, gneiss, and granite. They are characterized as coarse-loamy, mixed, active, mesic Oxyaquic Dystrudepts. These soils are typically found on upland landforms such as ridges, hills, and drumlins.

Paxton soils generally have a dark brown or brown surface layer (A horizon) consisting of loam or silt loam. The subsoil (B horizon) is typically a yellowish brown or strong brown, coarse-loamy material, often with a higher clay content than the surface horizon. Mottles are often present in the lower part of the subsoil, indicating seasonal wetness. The substratum (C horizon) consists of unweathered glacial till.

These soils are moderately acidic to strongly acidic. Permeability is moderate in the surface and subsoil and slow to moderate in the substratum. Available water capacity is moderate. Paxton soils are commonly used for woodland, hay, and pasture. Some areas are also used for cultivated crops where slopes are gentle. The seasonal high water table and slow permeability in some areas can limit certain uses.