Texture of the fine-earth of these horizons is loamy sand. Structure of the B horizon is granular or it is structureless. Consistence is very friable or loose. The BC horizon, where present, has hue of 10YR or 2.5Y, value of 4 or 5, and chroma of 3 to 6. Texture of the fine-earth is loamy sand.
Structure is granular or it is structureless.
Consistence is very friable or loose. The C horizon has hue of 10YR to 5Y, value of 3 to 5, and chroma of 2 to 4. Texture is sand or coarse sand in the fine-earth fraction and the horizon is normally stratified. These are the Bonaparte , Hinckley , Manchester , Mecosta , Multorpor , Otisville , and Riker series. Mecosta and Multorpor series are from outside LRR R and S. Bonaparte soils do not have allow loamy textures in the upper part and have carbonates within a depth of 40 inches.