Structure ranges from moderate or strong, very fine to medium granular. Base saturation of the A1 horizon is less than 50 percent. Color of the B2 horizons include hues of 10YR or 7.5YR, values of 6 or 7 dry and 3 to 5 moist, and chromas of 2 to 4. They are massive, or range from weak, fine to coarse subangular blocky or granular. C horizons may occur in areas having bedrock below 30 inches.
Bedrock consists primarily of basalt, andesite or basaltic tuffs.
Boze , Chiquito and Suttler soils have been classified in the same family. Boze soils differ by having bedrock at depths ranging from 48 to 100 inches and decreasing pH values in the soil profile ranging from 5.6 to 5.3. Suttler soils differ by being dominantly 40 to 55 inches to schist or gneiss bedrock and being medium acid decreasing to very strongly acid. Chiquito soils differ by having formed in granitic colluvium and alluvium, very coarse sandy loam control sections, very strongly acid A1 horizons, and being excessively drained. Goodfellow and Windy soils are also similar, but differ by having more than 50 percent coarse fragments in their control sections.