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13 <br />• Interorete' ions of Data <br />ecent Cultural Indicators <br />The recent debris of the drill hole locations is most probably associated <br />xith coal mining activities and hunting in the North Fork of the Gunnison canyon. <br />It is of no cultural significance, and though adverse impact is expected from <br />drilling operations, no further attention is warranted. Likewise, the Hawk's Nest <br />Mine area and the recent debris of the mining waste disposal area cannot be considered <br />to require additional study. <br />Prehistoric Remains <br />Locality #1 is one of the Sew indications of aboriginal presence in the <br />upper portions of the North Folic Valley. Previously recorded sites and isolated <br />finds have been restricted to the wider portions of the valley to the southwest. <br />It is of interest to note that lithic items are confined to a disturbed area, <br />and may be eroding from formerly subsurface strata now exposed by the mad cut. <br />his introduces the possibility that floodplain or neas~floodplain sites in this <br />~rtion of the canyon may be obscured as a result of sediment aggradation. There- <br />fore, the paucity of cultural remains may reflect their subsurface positions rather <br />than their true frequencies, although this irnestigator has heard of no instances <br />of encountering such deposits during excavation in this portion of the canyon. <br />Locality #1 is located on U.S. Steel property beyond pro3ect area boundaries <br />and will not be impacted by proposed Western Slope Carbon activities. <br />An isolated find such as the chert flake designated IF #1, discovered in <br />the mining waste disposal area, can be interpretted only as an indication of limited <br />aboriginal presence in the ir.~mediate area. It is likely that additional isolated <br />artifacts occur throughout the region, and that more extensive remains would occur <br />along the nearby permanent water sources. However, the possibility of different <br />paleoenvi mnmental conditions, as well as the fact that the area is apparently sub- <br />3ect to aeolian deposition, indicate that subsurface deposits may exist. In light <br />of this possibility, disturbe3 areas such as two track roads, the mad cut along the <br />southeast margin of the pm~ect area, and an excavated mad block were examined for <br />cultural evidence. No additional materials were discovered. <br />~ Collection of the isolated Sind has mitigated potentially adverse impact <br />~o the item. However, if subsurface materials exist in the area, impact to such <br />