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Home My WebLink About20090327.tiff• • • • Non -Technical Descriptions Soil Surccy At 618 \VP;LI) COIIN'I'V, COLORAI)O,SOtu'i'IIP;itN PAlt"I' Mop unit; J2 Nunn clay loam, I to 3 percent slopes Ueset//Won ('ate ory: SUI 1 ho Nam soil Is a deep, well drelnnd soil. It is formed on terraces and smooth plains hi mixed eolian and alluvial deposits. The surface Is a clay loam. The underlying material Is clay loam and sandy loam. The soils have moderately slow permeability. T heir available wafer holding capacity Is high. Roots penetrate to 60 inches or more. Runoff is slow and the erosion hazard due to wind is low. Map unit: 32 Wiley -Colby complex, I to 3 petec,nt slopes l)eseripthm Category: SUI This map unit Is on smooth plains. This unit consists of 60 percent Wiley and 30 percent Colby soils. The Wiley soil Is a deep, well drained soil. II formed In calcareous eullan deposits. The surface Is a sill loan. The subsoil Is a silty clay loam. The s ubstratan to a depth of 60 Inches or more Is a silty clay loam. This soil has a moderately slow permeability. The available water holding capacity Is high. Roots penetrate to a depth of 60 inches or more. Runoff Is slow and the erosion hazard due to wind s high. The Colby soil Is a deep, well drained soil. II formed In calcareous eollen deposits. The surface Is a loam. The underlying material to a depth of 60 inches or more Is a silt loam. This soil has a moderate permeability. The available water holding capaclly is high. Roots penetrate to a depth of GO Inches or more. Runoff is slow and the erosion hazard due to wind Is high. Mop unit: 83 Wiley -Colby complex, 3 to 5 percent slopes Description Category: 8O1 This map unit is on smooth plains. This unit consists of 60 percent Wiley and 30 percent iby solla. The s deposits. The surface ley soil Is als a sill loam The subsoitoll.It r calcareous l is a silty clay loam. The a ubstratum to a depth of 60 Inches or more is a silly clay loam. This soil has a moderately slow permeability. The available water holding capacity Is high. fools penetrate to a depth of 60 inches or more. Runoff is slow and the erosion hazard due to wind I s high. The Colby Soli Is a deep, well drained soil. It formed In calcareous eollan deposits. The surface is a loam. The underlying material to a depth of 60 inches or more Is a sill loam. This soil has a moderate permeability. The available water holding capacity Is high. Roots penetrate la a depth of 60 Inches or more. Runoff Is slow and the erosion hazard due to wind is high. Mondry. Frhrnnq' 15, 21101 EXHIBIT • • • • • Non -Technical DeSC111.111011S Soil Survey Area: 618 \VEI,l) COUNTY, t' t)I.t)I(ADors)U'1'11mN J'AWI' Mop curl: .12 Nunn clay loam, I to 3 paeans slopes llesecipllun (.'n(rwary: Sol l ho Nunn soli Is a deep, well drained soil. It Is formed on terraces and smooth plains In mixed eollan and alluvial deposits. The surface Is a clay loam. The underlying material is clay loam end sandy loam. The soils have moderately slow permeability. T heir available water holding capacity Is high. Roots penetrate to 60 itches or mote. Runoff Is slow and the erosion hazard due to wind Is low. Mop f((ril: /'2 Wiley -Colby complex, I to 3 percent slopes Ilene 1pilo Category: SOI This map unit Is on smooth plains. This unit consists of 80 percent Wiley and 30 percent Colby sollS. 1 he Wiley soil is a deep, well drained soil. It formed in calcareous eolian deposits. The surface Is a silt loam. The subsoil Is a silty clay loam, The s ubsiralum to a depth of 60 Inches or more Is a silly clay loam. This soil has a moderately slow permeability. The available water holding capacity is high. Roofs penetrate to a depth of 60 Inches or more. Runoff is slow end the erosion hazard due to wind I s high. The Colby soil Is a deep, well drained soli. It formed In calcareous eotlan deposits The surface is a loam. The underlying material to a depth of 60 Inches or more is a sill learn. This soil has a moderate permeability. The available water holding capacity Is high. Roots penetrate to a depth of 69 inches or more. Runoff Is slow and the erosion hazard due to wind is high. 111r(p u(ril: 83 Wiley -Colby complex, 3 to 5 percent slopes I)esrrlpllpn ('ufegrrry. 801 This map unit Is on smooth plains. This Unit consists of 60 percent Wiley and 30 percent Colby solle. The Wiley soil is a deep, wall drained soil. It formed in calcareous eolian deposits. The surface is a silt loam. The subsoil Is a silty clay loam. The S ubsiralum to a depth of BO inches or more is a silty clay loam. This soil has a moderately slow permeability. The available water holding capacity is high. Roots penetrate to a depth of 00 Inches or more. Runoff is slow and the erosion hazard due to wind I s high. The Colby Coil is a deep, well drained soil. It formed In calcareous action deposits. The surface Is a loam. 'the underlying material to a depth of 00 inches or more Is a silt leant. This soil has a moderate permeability. The available water holding capacity Is high. Roots penetrate to a depth of 60 Inches or more. Runoff Is slow and tire erosion hazard due to wind Is high. Ahmdar, Fe(nnrnr 13, 1001 .... ,,... ....- ...-.nw^'w'.— r.... Y.rrrtt�/r•n�rR�Y'^R '�'�11 1'„gel of 1 Hello