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.
Hinckley soils have rock fragments dominated by granite, gneiss, and schist.
Manchester soils have hue of 5YR or redder. Multorpor soils have hue OF 10YR and chroma of 1 or 2 throughout. Otisville soils have rock fragments dominated by siltstone and shale. Riker soils formed in a mixture of unburned coal and coal ash and have carboliths, pieces of coal or coal slag in the soil. Quonset soils are on nearly level to very steep slopes on terraces, outwash plains, deltas, eskers, and kames.