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L J <br />• <br />u <br />Map Unit GO <br />Soils of this unit appear to occur on north/south <br />lateral moraines of past glaciation. They are g <br />very gravelly with cobbles occurring below 12 inci <br />textures below 24 inches are usually cobbly loam o <br />sandy loams. These textures generally prevail to <br />Soils of this map unit are well drained and have mo <br />rapid permeabilities. These soils have a high <br />hazard to wind and water. <br />Map Unit MS <br />:rending <br />nerally <br />'s. The <br />cobbly <br />Bedrock. <br />erately <br />erosion <br />Soils of this delineation are the result of pas mining <br />operations. Areas where this unit is mapped are E at with <br />varying degrees of volunteer vegetation. Photo 2. eneral- <br />ly, the areas on which this soil delineation oc urs are <br />truncated hills or ridges. <br />These soils are very gravelly ( 358), generally <br />loam or loamy sand textures. wind erosion and water <br />hazard is low because of this gravel content. The v <br />gravel content causes the surface of these soils tc <br />quite warm, and young grass or other flora seedli <br />high mortality rates. <br />.f sandy <br />erosion <br />pry high <br />become <br />iqs have <br />26 <br />