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Limited - Results Archaeological Survey Form (Page 3 of 11) <br />Principal Meridian: 6th X NM _ Ute <br />NOTE: Only generalized subdivision ( "quarter quarters ") within each section is needed <br />Township: <br />5N <br />Range: <br />86W <br />Sec.: <br />16 <br />1/4s <br />all <br />Township: <br />5N <br />Range: <br />86W <br />Sec.: <br />10 <br />1/4s <br />SW 1/4 <br />Township: <br />5N <br />Range: <br />86W <br />Sec.: <br />15 <br />1/4s <br />NW 1/4 <br />Township: <br />5N <br />Range: <br />86W <br />Sec.: <br />17 <br />1/4s <br />NE and NW 1/4 <br />Township: 5N <br />Range: 86W <br />Sec.: 18 1/4s NE and NW 1/4 <br />If section(s) is irregular, explain alignment method: Alignment to the section's NW corner <br />16. Total number of acres surveyed: 62.1 <br />17. Comments: A 300 x 300 ft square block was surveyed to include a buffer around the planned <br />borehole pads. and a 100 foot wide corridor (50 feet either side of staked centerline <br />surveyed along the entire length of the proposed new access roads. The existing two -track <br />roads that require upgrades were also surveyed with a 100 foot wide corridor. <br />IV. ENVIRONMENT <br />18. General Topographic Setting: In general, the project area is located in Twentymile Park iust <br />north of Fish Creek northwest of Oak Creek, Routt County, Colorado. The existing road that will <br />be used for access from the west traverses rolling hills and follows a power line for much of its <br />length. The borehole pads are situated on low knobs in the Twentymile Park valley with higher <br />ridges to the west that are part of the Williams Fork Mountains. Fish Creek and Foidal Creek <br />Canyons are located about a mile to the south. <br />Current Land Use: Livestock grazing, power lines, recreation <br />19. Flora: The project area is moderately vegetated with grasses, forbs, and low sagebrush. The <br />western access road traverses areas with less dense vegetation consisting mostly of pasture <br />grasses. <br />20. Soils /Geology: Surface sediments are predominantly alluvial in nature and consist of a dark <br />brown silty loam with a small amount of small gravels and few larqer cobbles. Subsurface <br />geology is composed of sandstone, shale and manor coal beds of the Williams Fork Formation <br />which are sedimentary and igneous rocks from the Early Tertiary and Late Cretaceous Age <br />(Tweto 1979). <br />