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Custom Soil Resource Report <br /> Across-slope shape: Linear <br /> Parent material: Alluvium derived from igneous, metamorphic and sedimentary <br /> rock <br /> Typical profile <br /> Ap-0 to 2 inches: clay loam <br /> BAt-2 to 14 inches: clay loam <br /> BCt- 14 to 18 inches: clay loam <br /> C1 - 18 to 40 inches. sandy clay loam <br /> C2-40 to 60 inches: sandy clay loam <br /> Properties and qualities <br /> Slope: 0 to 2 percent <br /> Depth to restrictive feature: More than 80 inches <br /> Natural drainage class: Well drained <br /> Capacity of the most limiting layer to transmit water(Ksat): Moderately high (0.21 <br /> to 0.71 in/hr) <br /> Depth to water table: More than 80 inches <br /> Frequency of flooding: None <br /> Frequency of ponding: None <br /> Calcium carbonate, maximum in profile: 14 percent <br /> Gypsum, maximum in profile: 1 percent <br /> Salinity, maximum in profile: Nonsaline to very slightly saline (0.0 to 2.0 <br /> mmhos/cm) <br /> Sodium adsorption ratio, maximum in profile: 2.0 <br /> Available water storage in profile: High (about 10.9 inches) <br /> Interpretive groups <br /> Land capability classification(irrigated): 2e <br /> Land capability classification(nonirrigated). 7c <br /> Hydrologic Soil Group: C <br /> Ecological site: Loamy Saltdesert(R034BY401 CO) <br /> Hydric soil rating: No <br /> Minor Components <br /> Stagie <br /> Percent of map unit: 10 percent <br /> Landform: Stream terraces <br /> Landform position (three-dimensional): Tread <br /> Down-slope shape: Linear <br /> Across-slope shape: Linear <br /> Ecological site: Loamy Saltdesert(R034BY401 CO) <br /> Hydric soil rating: No <br /> Fruitland <br /> Percent of map unit. 5 percent <br /> Landform: Stream terraces <br /> Landform position (three-dimensional): Tread <br /> Down-slope shape: Linear <br /> Across-slope shape: Linear <br /> Ecological site: Sandy Saltdesert(R034BY402CO) <br /> Hydric soil rating: No <br /> Mesa <br /> Percent of map unit: 5 percent <br /> Landform: Stream terraces <br /> 18 <br />