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2l <br />• Canyon between two wide side canyons. The site is situated on a general southwest-facing slope <br />below a high narrow ridge on which a single dead pinyon is visible. The artifacts generally cluster <br />in three concentrations. Concentration #1 is located on a small bench in the southeast-most comer <br />of the site and measures roughly 7 m in diameter. It consists of roughly 20 tan/gray felsite flakes, <br />mostly secondary and tertiary, and two cores. No ground stone is associated, although two manos <br />lie roughly I S m northeast. Concentration #2 is located on a small flat bench, just below the top of <br />the high ridge, on the northwest edge of the site. Artifacts in this area are largely tools, although <br />three gray felsite tertiary flakes were observed. Tools include two metate fragments, five manos, <br />a flake scraper, two bifaces, two cores, and a battered quartzite cobble. Between these two <br />concentrations is a third concentration, lying on the eroded washed slope. Four manos and two Flake <br />tools were located in this area. Only a couple flakes were scattered outside ofthese concentrations. <br />Soil on this site is a brown sandy loam containing numerous angular sandstone pebbles and cobbles. <br />Deposits are colluvial, residual, and slope-washed. Alluvial erosion and sheetwash are the only <br />disturbances. Vegetation includes oakbrush, pinyon, cactus, low sagebrush, and various grasses. <br />Although erosional cuts on the site indicate no Holocene deposition and thus little potential <br />for buried cultural materials, SLA7374 lies within the LCRHL and is recommended to be <br />contributing to the significance of the district. This site displays a diversity of artifacts as well as <br />a high ground stone to other artifact ratio and may reflect activities related to the procurement and <br />initial processing of pinon nut and acorns. However, because SLA7374 falls within the P3 haul road <br />corridor and had been recommended for cultural resource clearance prior to the creation of the <br />• landscape (McKibbin 1997a), further field work is recommended only if it can be accomplished <br />without delaying the construction of the road (McKibbin 1997a:7). <br />SLA7375 (MM-4780): This prehistoric site was recorded in 1997 during inventory of the <br />realigned P3 haul road. This lithic and ground stone scatter issituated on asoutheast-trending knoll <br />or bend in an otherwise flat, wide, side canyon extending north from Jeff Canyon. Artifacts include <br />five felsite flakes (four of which are tertiary), an endscraper, three sandstone metate fragments, a <br />complete sandstone metate, and a sandstone mano. Deposits are residual and consist of a brown <br />sandy loam containing numerous angular sandstone gravels. No depth to these deposits is present, <br />based on erosional exposures on the site. A trowel test at the datum also revealed a clay which is <br />eroding bedrock immediately below the surface. Vegetation includes pinyon/juniper, oakbrush, <br />cactus, and grasses. <br />Although there is little potential buried cultural material, this site lies within the LCRHL and <br />is recommended to be contributing to the significance ofthe district. The site contains a high ground <br />stone to other artifact ratio and may reflect activities related to the procurement and initial processing <br />of pinon nut and acorns. However, because SLA7375 falls within the P3 haul road corridor and had <br />been recommended for cultural resource clearance prior to the creation of the landscape (McKibbin <br />1997a), further field work is recommended only if it can be accomplished without delaying the <br />construction of the road (McKibbin 1997a:7). <br />• SLA7482 (MM-4706): This prehistoric site was recorded in 1997 during inventory for the <br />proposed railroad spur to the Colorado and Wyoming Railroad tracks. This sparse lithic scatter lies <br />along the south side of the Purgatoire River, in the floodplain north of the mouth of the Lorencito <br />