12 - Clallam gravelly sandy loam, 0 to 15 percent slopes. (CmC) This moderately deep, moderately well drained soil is on hills. It formed in compact glacial till. The native vegetation is mainly conifers and shrubs. Elevation is 40 to 1,800 feet. The average annual precipitation is 16 to 30 inches, the average annual air temperature is about 48 degrees F, the average frost-free period is 160 to 200 days, and the average growing season (at 28 degrees) is 210 to 260 days. Typically, the surface is covered with a mat of organic material 2.5 inches thick. The surface layer, where mixed to a depth of 6 inches, is dark brown gravelly sandy loam. The upper part of the subsoil is brown gravelly sandy loam about 4 inches thick, and the lower part is brown very gravelly sandy loam about 18 inches thick. Compact glacial till is at a depth of 28 inches. Depth to impact glacial till ranges from 20 to 40 inches. In some areas of similar included soils, the surface layer is sandy loam or very gravelly sandy loam. Included in this unit are small areas of Catla, Dick, Elwha, Hoypus, McKenna, Mukilteo, and Yeary soils. Also included are small areas of Clallam soils that have slopes of more than 15 percent and soils that are more than 40 inches deep to compact glacial till. Included areas make up about 25 percent of the total acreage. The percentage varies from one area to another. Permeability of this Clallam soil is moderate to the compact glacial till and very slow through it. Available water capacity is low. Effective rooting depth is 20 to 40 inches. Runoff is medium, and the hazard of water erosion is slight. Water is perched above the compact glacial till from January through April. The effect of the layer of compact glacial till on use and management is similar to that of a hardpan. This unit is used mainly as woodland. It is also used as hayland, pastureland, cropland, and homesites. This unit is suited to year-round harvesting operations. Logging roads require suitable surfacing. Rock for road construction is not available in areas of this unit. Seedling establishment and the hazard of windthrow are the main concerns in the production of timber. The low precipitation during the growing season and low available water capacity contribute to seedling mortality. Reforestation can be accomplished by planting Douglasfir seedlings. If seed trees are present, natural reforestation of cutover areas by Douglas-fir occurs periodically. When openings are made in the canopy, invading brushy plants can delay the establishment of seedlings. Because the rooting depth is restricted by the compact glacial till, trees occasionally are subject to windthrow. If this unit is used for homesite development, the main limitation is wetness. Excavation for roads and buildings increases the risk of erosion. Use of this unit for septic tank absorption fields is limited by wetness and depth to the compact glacial till. Because of the depth to glacial till, onsite sewage disposal systems often fail to function properly during periods of high rainfall. Use of heavy equipment during construction compacts the soil and reduces permeability, particularly during periods when the soil moisture content is high. Absorption lines should be installed on the contour to prevent surfacing of effluent in downslope areas. 12 - Clallam gravelly sandy loam, 0 to 15 percent slopes. (CmC) (con’t) Table 10 – Sanitary Facilities Soil name and map symbol Clallam gravelly sandy loam, 0 to 15 percent slopes Septic tank absorption fields Severe: cement pan, wetness Sewage lagoon Severe: cemented pan, slope, wetness Table 14 – Physical and Chemical Properties of Soils Soil name and map symbol Clallam gravelly sandy loam, 0 to 15 percent slopes Depth (In) Clay (%) Permeability (In/hr) 0-10 3-8 0.6-2.0 10-28 3-12 0.6-2.0 28 --- --- Table 15 – Water Features Soil name and map symbol Hydrologic group Clallam gravelly sandy loam, 0 to 15 percent slopes C High Water Table Depth (ft) Kind Months 1.5-3.0 Perched Jan-Apr Clallam County Critical Area Code Application Geologic Hazard Soil Type Landslide (1.a.ii) Compact Glacial Till SCS Erosion Hazard Potential ESA Trigger No Landslide (1.a.iv) <Moderate No Erosion (1.b.v) <Moderate No Seismic (1.c.iii) Note: 1. Landslide hazard (1.a.ii) is defined as glaciolacustrine silt and clays on terraces. 2. Seismic soils 1.c.iii) are defined as beaches, Mukilteo muck, Lummi silt loam, Sequim- McKenna-Mukilteo complex, and Tealwhit silt loam No