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3 Aquolls and Aquents, gravelly substratum -- Soils occur through the center of <br /> the eastern portion of the site above the Poudre River floodplain. These are <br /> deep, well drained soils on plains formed in mixed outwash and eolian deposits. <br /> A typical surface layer is brown sandy loam about 10 inches thick underlain by <br /> pale brown calcareous fine sandy loam to 60 inches. Otero Sandy Loam soils <br /> have rapid permeability and moderate available water capacity. Surface runoff is <br /> medium. The hazard of erosion b wind and water is low <br />8 Ascalon loam, 0 to 1 percent slopes - These are deep well drained soils on <br /> terraces. A typical surface layer is brown sandy loam about 10 inches thick <br /> underlain by yellowish brown sandy clay loam about 15 inches thick, with a <br /> substratum of calcareous sandy loam to 60 inches. Ascalon loam soils have <br /> moderate permeability, surface runoff is slow and the erosion hazard is low. <br /> Effective rooting depth is 60 inches or more and available water capacity is high. <br />9 Ascalon loam, 1 to 3 percent slopes - Theses are deep well drained soils on <br /> terraces. A typical surface layer is brown sandy loam about 10 inches thick <br /> underlain by yellowish brown sandy clay loam about 15 inches thick, with a <br /> substratum of calcareous sandy loam to 60 inches. Ascalon loam soils have <br /> moderate permeability, surface runoff is slow and the erosion hazard is low. <br /> Effective rooting depth is 60 inches or more and available water capacity is high. <br />10 Bankard sandy loam, 1 to 3 percent slopes - Deep, somewhat excessively <br /> drained soils on flood plains that occur along the Cache La Poudre River. They <br /> are formed in stratified recent alluvium along streams and rivers. A <br /> representative profile includes a surface layer of brown sandy loam about 4 <br /> inches thick underlain with pale brown, calcareous sand stratified with sandy <br /> loam, loam and fine gravel to 60". The effective rooting depth is 60" or more and <br /> surface runoff is slow. Bankard Sandy Loam soils have moderately rapid <br /> permeability and low available water capacity <br />32 Kim loam, 1 to 3 percent slopes - Kim Loam soils occurs through the northern <br /> portion of the property above the Poudre River floodplain. These are deep, well <br /> drained soils on smooth plains and alluvial fans formed in mixed eolian deposits. <br /> A typical surface layer is brown and pale brown loam about 12 inches thick <br /> underlain by pale brown loam and pale brown fine sandy loam to 60 inches. The <br /> effective rooting depth is 60" or more. Kim loam soils have moderate permeability <br /> and high available water capacity. Surface runoff is medium and erosion hazard <br /> is low. <br />41 Nunn clay loam, 0 to 1 percent slopes This soil type occurs on a small portion <br /> of the site adjacent to the Poudre River. These are deep, well drained soils on <br /> smooth plains and terraces formed in mixed alluvium and eolian deposits. A <br /> typical surface layer is grayish brown clay loam about 14 inches thick underlain <br /> by clay loam and sandy loam to 60 inches. The effective rooting depth is 60" or <br /> more. Kim loam soils have moderately slow permeability and high available <br /> water capacity. Surface runoff is slow and erosion hazard is low. <br />47 Olney fine sandy loam, 1 to 3 percent slopes- This soil type occurs on the <br /> northern portion of the property. Olney Fine Sandy Loams consists of deep, well <br /> drained soils that are formed in mixed outwash deposits. A typical surface layer <br />Riverview Resource <br />Amendment to Permit M1999098 112c <br />Page 12 of 13