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• Exhibit Page 33 • Unit 014 Name Dalmatian loam Description The Dalmatian soil is formed in alluvium derived from mixed sources. The Dalmatian soil is moderately well drained. Typically, the surface layer is dark grayish brown loam about 13 inches thick. The subsoil is dark grayish brown loam about 12 inches thick. The upper 14 inches of the underlying material is dark brown loam. The next 10 inches is dark grayish brown to dark gray sandy clay loam. The lower part to a depth of 60 inches is dark gray gravelly sandy loam. Permeability of the Dalmatian soil is moderate. Available water capacity is high. The hydrologic group is B. Effective rooting depth is 60 inches or more. Runoff is slow, and the hazard of water erosion is slight. A seasonal high water table is at a depth of 36 to 72 inches in the spring. This soil is subject to brief periods of flooding in the spring. Shrink-swell potential is low. Unit 014 Name Apmay loam Description The Apmay soil is somewhat poorly drained. It formed in alluvium derived from mixed sources. Typically, the surface layer is brown loam about 4 inches thick. The subsurface layer is brown clay loam about 6 inches thick. The upper 8 inches of the subsoil is brown clay loam. The lower 4 inches is dark yellowish brown sandy loam. The substratum to a depth of 60 inches or more is brown extremely gravelly loamy sand and sandy loam. Permeability of the Apmay soil is moderately slow to a depth of 20 to 40 inches and moderately rapid below this depth. Available water capacity is moderate. The hydrologic group is B. Effective rooting depth is 20 to 40 inches. Runoff is slow, and the hazard of water erosion is slight. A seasonal high water table is at a depth of 12 to 24 inches in the spring. This soil is subject to brief periods of flooding in the spring. Shrink-swell potential is low. Unit 014 Name Schrader loam Description The Schrader soil is poorly drained. The Schrader soil formed in alluvium derived from mixed sources. Typically, the surface layer is dark grayish brown loam about 13 inches thick. The subsurface layer is brown fine sandy loam about 4 inches thick. The next layer is brown sandy clay loam about 7 inches thick. The substratum to a depth of 60 inches or more is brown fine sandy loam. Permeability of the Schrader soil is moderate. Available water capacity is moderate. The hydrologic group is D. Effective rooting depth is 60 inches or more. Runoff is slow, and the hazard of water erosion is slight. A seasonal high water table is at a depth of 12 to 24 inches in the spring. This soil is subject to brief periods of floodi~in the spring. Shrink-swell potential is low. Four States Aggregates, LLC 30 DEC 2000 Application for Permit: Line Camp Pit FSA-LCP-D1-001