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Custom Soil Resource Report <br /> Very low: Less than 0.5 percent <br /> Low: 0.5 to 1.0 percent <br /> Moderately low: 1.0 to 2.0 percent <br /> Moderate:2.0 to 4.0 percent <br /> High:4.0 to 8.0 percent <br /> Very high: More than 8.0 percent <br /> Outwash <br /> Stratified and sorted sediments (chiefly sand and gravel) removed or"washed <br /> out"from a glacier by meltwater streams and deposited in front of or beyond the <br /> end moraine or the margin of a glacier. The coarser material is deposited nearer <br /> to the ice. <br /> Outwash plain <br /> An extensive lowland area of coarse textured glaciofluvial material. An outwash <br /> plain is commonly smooth; where pitted, it generally is low in relief. <br /> Paleoterrace <br /> An erosional remnant of a terrace that retains the surface form and alluvial <br /> deposits of its origin but was not emplaced by, and commonly does not grade <br /> to, a present-day stream or drainage network. <br /> Pan <br /> A compact, dense layer in a soil that impedes the movement of water and the <br /> growth of roots. For example, hardpan, fragipan, claypan, plowpan, and traffic <br /> pan. <br /> Parent material <br /> The unconsolidated organic and mineral material in which soil forms. <br /> Peat <br /> Unconsolidated material, largely undecomposed organic matter, that has <br /> accumulated under excess moisture. (See Fibric soil material.) <br /> Ped <br /> An individual natural soil aggregate, such as a granule, a prism, or a block. <br /> Pedisediment <br /> A layer of sediment, eroded from the shoulder and backslope of an erosional <br /> slope, that lies on and is being (or was)transported across a gently sloping <br /> erosional surface at the foot of a receding hill or mountain slope. <br /> Pedon <br /> The smallest volume that can be called "a soil."A pedon is three dimensional <br /> and large enough to permit study of all horizons. Its area ranges from about 10 <br /> to 100 square feet (1 square meter to 10 square meters), depending on the <br /> variability of the soil. <br /> 57 <br />