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- - <br />►-•-•- -•- •- •-•- +-- •-• � -• -� <br />r(1-7 <br />s:: <br />00 • 500 <br />IN FEET <br />�••••••• <br />10% Qq <br />IVA <br />�• • +•�i• +• ++ <br />PI <br />3*11 <br />WAINA F, I Ell I FIA <br />FA'FAF FIN <br />- -- -t - - <br />25' SETBA <br />I <br />t' <br />I' <br />�I <br />fl <br />OWN RSHIP:' <br />UNITED STATES <br />OF AMERI A �r <br />�I <br />I <br />25' SETBACK <br />4 <br />I <br />'1 <br />fit <br />NOTES: <br />OWNERSHIP: <br />UNITED STATES OF AMERICA <br />LEGEND- <br />1 . Property ownership to the east and south is dominated by U.S. Army Corps <br />of Engineers parcels associated with John Martin Reservoir. <br />2. Major Soil Unit Descriptions <br />HoC — Harvey loam. 1 to 9 percent slopes. This units parent material <br />consists of calcareous loamy eolion deposits. Depth to a root restrictive <br />layer is greater than 60 inches. The natural drainage class is well drained <br />and water movement in the most restrictive layer is moderately high. <br />There is no zone of water saturation within a depth of 72 inches. Organic <br />matter content in the surface horizon is about 2 percent. <br />WIB — Wiley silt loam. 0 to 3 percent slopes, Components of this unit are <br />plains soils. The parent material consists of loess. Depth to a root <br />restrictive layer is greater than 60 inches. The natural drainage class is well <br />drained and water movement in the most restrictive layer is moderately <br />high. There is no zone of water saturation within a depth of 72 inches. <br />Organic matter content in the surface horizon is about 1 percent. <br />Cob — Colby silt loam, 1 to 3 percent. The components of this mop unit <br />are found on terraces. The parent material consists of calcareous loess. <br />Depth to a root restrictive layer is greater than 60 inches. The natural <br />drainage class is well drained and water movement in the most restrictive <br />layer is moderately high. There is no zone of water saturation within a <br />depth of 72 inches. Organic matter content in the surface horizon is about <br />1 percent. <br />3. Existing vegetation on the site is typical of the high arid plains. Ground <br />cover is primarily composed of posture grasses such as blue grama. Low <br />growing shrubs such as Skunkbrush Sumac or yucca may also be present, <br />especially in ravines and drainages. <br />SHEET 1 AIIRite Paving and Ready Mix <br />OF 2 1 Lamar Division <br />DATE: July, 2012 <br />SHARP GRAVEL PIT <br />BENT COUNTY. COLORADO <br />0 <br />7 <br />L <br />- - -- Property Line /Proposed Permit /Affected Area Boundary <br />-- - - - - -- Mining Setback Line <br />1 Wiley silt loam, 0 to 3 percent slopes <br />Rocky Ford clay loam, 1 to 3 percent slopes <br />Rocky Ford clay loam, 0 to 1 percent slopes <br />Harvey loam, 1 to 9 percent slopes <br />® Colby silt loam, 1 to 3 percent slopes <br />Coscajo soils and gravelly land <br />Gravel Pits <br />Colby fine sandy loam, 0 to 3 percent slopes <br />EXHIBIT C -1 <br />Existing Conditions Plan Map <br />Property Ownership, Soils & Vegetation <br />BLUE EARTH <br />AM SCHENDERLEIN <br />