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SOILS CiAP EX1116IT <br />~`V <br />SCALE 1:24,000 <br />1,000 p --.~ <br />1,000 2,000 feet <br />l~ <br /> <br />SOIL LEGEPID <br />Ab <br />Ds <br />6x <br />Cf <br />Cr <br />Cy F <br />Aaberg-Qarishman association <br />Qosler sandy loam <br />Drinkert-tlorset association <br />Coa Lnont-Fluetsch Complex <br />Crespin-Carlstrom clays <br />Cryorthents, steep <br />Eh Fluetsch-Tiagos association <br />GeD Gell<ie sandy loam <br />ilsD t1orset loam <br />Sp Spicerton sandy loam <br />Te Tealson-Rocl: land association <br />Soil in G <br />vel Pit <br />6rinkert-,'1orset association: (3rinkert loam Deep (greater than 40 inches <br />over any restricting material) moderately fine textured soils with a loam <br />surface and clay loam subsoils. It has a moderate available water holding <br />capacity, but, due to the high shrink-swell character of the subsoil, <br />tends to shear roots, retarding plant growth and reducing water intake <br />rate; thus, much of tihe available moisture is lost by evaporation and <br />runoff. <br /> <br />