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PROJ00076
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Entry Properties
Last modified
11/19/2009 11:29:57 AM
Creation date
10/5/2006 11:34:10 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153564
Contractor Name
Bauer Lakes Water Company
Contract Type
Loan
Water District
34
County
Montezuma
Bill Number
HB 85-1042
Loan Projects - Doc Type
Feasibility Study
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<br />,1 <br /> <br />-1- <br />\ <br />I~ <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />"'--- <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />~~ <br /> <br />J;I <br />I <br /> <br />3/82 <br /> <br />ll--Sheek-Archuleta--Pramiss. <br /> <br />This map unit is in the southeastern corner and along the eastern boundary <br /> <br />of the survey area. It is mainly on hillsides, canyon sideslopes, ridges <br /> <br />and lllOuntain sideslopes. Slope is 6 to 80 percent. The vegetation on this <br /> <br />unit is mainly ponderosa pine, Douqlas fir~ ROCky Mountain juniper, grasses, <br /> <br />shrubs and forbs. Elevation is 7, )00 to 8,500 feet. The average annual <br /> <br />precipitation is about 15 to 20 inches, the average annual air temperature <br /> <br />is 43 to 47 degrees F, and the avecage frost-free season is 75 to 120 days. <br />i <br /> <br />This unit makes up about 5 percent of the survey area. It is about 40 <br /> <br />percent Sheek and similar soils, 35 percent Archuleta and similar soils, and <br /> <br />15 percent Pramiss and similar soilS. The remaining 15 percent is <br /> <br />components of minor extent. <br /> <br />Sheek and similar soils are on hillsides, .canyon sideslopes and mountain <br /> <br />s~deslopes. These soils are deep and well drained. They formed in <br />\ <br />~ncalcareous colluvium and residuum derived dominantly from sedimentary <br /> <br />rocks. The surface layer is very stony sandy loam. The subsoil is very <br /> <br />stony clay loam. Below this to a depth of 60 inches the soils are very <br /> <br />stony. clay loam. <br /> <br />Archuleta and similar soils are on hillsides, canyon sideslopes and <br /> <br />mountain sideslopes. These soils are shallow and well drained. They formed <br /> <br />in noncalcareous colluvium derived dominantly from sedimentary rocks. The <br /> <br />surface layer is stony and very stony sandy loam. Below this to a depth of <br /> <br />10 to 20 inches the soils are stony clay loam. Weathered shale and <br /> <br />sandstone is at a depth of 10 to 20 inches. <br /> <br />A-I2. <br />
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