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proposed <br />provided <br />in "Soil <br />' as Kell <br />:ation. <br />is briefly <br />tics are <br />re prc- <br />ing tests <br />soil treat- <br />discussed. <br />The soil <br />5 the slope <br />er indicates <br />:)soil lost, <br />lost, <br />il lost. <br />D the "Soil <br />:Uional Co- <br />Medium <br />Blue <br />Medium <br />Green <br />Hamel loam <br />Hayden lojun <br />Lake Reaches, sajidy <br />Ncssel loam <br />ShorcK’ood silty clay loam <br />A brief description of each soil is provided. <br />provided to fatiUtate locating the soil types on the detailed sou n. p <br />provided with this report. <br />Hamel loam: <br />_ , • ' 1 ^ 1* I' f'hp p^an color is mcdiiim blue. <br />The map s>inbol for this soil is • foimcd in loaay colluvium over <br />■n-.is is a deep, poorly drained s . ,ev;L on foot slopes <br />loai.ni till. -Ihe soil occurs in M Hie native <br />and 'in long popiar trees. During <br />Kefperiods''of the year thcri is a P^^hed Ka <br />tfe up^rfoifhfitfnl soil has‘'low bearing values. Hiere is <br />a high potential for frost actio^i. <br />^hoyde n loam: <br />The soil was strongly influenced by a , forest Shale and 1ime- <br />ment. The natural vegetation vboulders are common through <br />Ilayden _1 oam - 2 to b^percent siope^ <br />, r iThR and the map color is mcdiiun green.Tlie map synbol for this soil is • o-roas on knolls and hillsides. <br />ti^oi? fs-^-liltaSr^ <br />hill seepage is not uncoiiimon attractive building'sites. <br />or spring thaws, '^e (volume change) is low to mod- <br />Soil strength is adequate. Slirink skcii | modcratelv nenn- <br />erate with changes m moisture content^ ig^'ieft kposed for extended <br />cable. Erosion is a hazard if the soil is leir l.m <br />periods. <br />4' <br />■is <br />Tagc -5- <br />Medium <br />t <br />Green <br />Dark <br />Green <br />jk‘ ^ <br />5 * « 1*1 <br />t -Z*. <br />BroKTi <br />■3 ; : <br />Brown