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T~.3LE 2 <br />SOZL TYPE DESCRIPTI0~:5 <br />PIKn"VIFi1 QUARRY <br />• Seil Type No. 1 consists of fines from the washing ops rations at the <br />three quarries. This particular soil type was coxbined from all three <br />quarries, and corresponds to mapping unit 35:~f on Figures 1 through 3, <br />Although this is an artificial soil, it can probably be related to the <br />SCS Paunsaugunt Series, as it has a similar parent material, <br />Soil Type No. 2 consists of a mixture of the native and disturbed soil, <br />It corresponds on the maps to the mapping symbol "4S1•P', This is also <br />an artificial type soil, but due to the pxrodominant parent material, <br />can also probably be related to the Paunsaugunt Series, <br />Soil Type A'o, 3 consists of the topsoil overlying the Upper r'anitou <br />Formation, This soil type corresponds to the mapping unit "1TS", <br />Soil Type No, 4 consists of the subsoil over the Upper N,anitou <br />Formation. Soil Type No. 4 corresponds to mapping symbol "2CL". <br />Soil Types Nos, 3 and 4 would most probably be related to the <br />Paunsaugunt Series of the Soil Conservation Service Interpretations. <br />Soil Type No, 6 consists of the subsoil over the residual Pi Fes Peak <br />Granite. The type corresponds to the mapping unit "65C", This soil <br />would correspond to the Kutler-Eroadmoor Complex, <br />• Soil i~pe No, 7 consists of the topsoil over the Harding Formation, <br />The type corresponds to mapping unit "7TS". The Soil Survey Interpretations <br />in the area of the site do not iodic^te a simil:.r interpretation <br />corresponding to soils derived from similar rock types. <br />Soil Type No. 8 consists of subsoil over the Herding Formation, <br />Soil Type No. 8 corresponds to mspping unit "8CL", The Soil Survey <br />Interpretations are lacking in the area of the site for soils <br />weathering from these particular types of rocks. <br />Soil Type Na. 9 consists of the topsoil over the Verdos Alluvium, <br />The type corresponds to mapping unit "9TS". This soil type c:ould <br />correspond to the Jerre-Tecolote Complex as described in the SCS <br />Soil Survey Interpretations, <br />Soil Type No. 10 consists of subsoil ever the Verdos Alluvium. The <br />type corresponds to mapping unit "lOG:v", Phis would gans.•a11y correspond <br />to the Jerre-Tecolote Complex, <br />• <br />P-I-8 <br />