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<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 /> <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 /> <br />I <br /> <br />Colorado Cultural Resource Survey <br />Historical Archaeology Component Form <br />(page 1 of 4) <br /> <br />Use this form in conjunction with the Management Data Form. This form should be completed for <br />each historical site with archaeological potential. <br /> <br />1. State Site Number: 50R1079 <br /> <br />2. Temporary Number: JH.OR.} <br /> <br />Does this form pertain to the site in general? Yes I2J No 0 or <br />a particular feature/structure (please note feature/structure number) <br /> <br />3. Site/Feature Type: Stream bank reinforcement <br /> <br />4. General SitelFeature Description: Site 50R1079 is a stream bank reinforcement structure. <br />known locally as the Upper Skyrocket Diversion Dam. blocking the original route of Skyrocket Creek <br />along the south edge of the drainage immediately upstream of a manmade cut that was made to enable <br />the drainage to take a westward route to the Uncompahgre River. The original route of the creek turned <br />abruptly south at the point of the stream bank reinforcement from a westerly course upstream. The cut <br />through the bedrock formed an extension of the westerly course and enabled the drainage to pass directly <br />past the original south deviation. The new cut through bedrock is 10 to 12 feet wide and 30 to 35 feet <br />deep. The stream bank reinforcement structure blocks the former stream course with large native stone <br />boulders at the bottom and large spruce logs at the top. The original drainage has a grade of about 30 <br />degrees and is in a natural cut about 10 to 15 feet deep. At the structure. the cut is about 10 feet deep <br />and 16 feet wide. The structure fills the former stream bed and ties into the banks on both sides. As <br />such, it is about 20 feet wide across the top. 6 feet thick. and 9 feet high on the north side and 14 feet. high <br />on the south side. The lower portion of the structuro is constructed of boulders and grovel and the upper <br />portion is constructed of four 8 to 12-inch-diameter spruce logs. The uppormost of theso logs has washed <br />about 5 feet to the south and one of the lower logs is broken and slightly out of place. Some large bridge <br />spikos ore in evidonce in the upper logs and somo wire rope is anchored to bedrock. Neither of these <br />appoar to lend support to the reinforcement structure, but do seem to have been part of a support system <br />for the remains of a log and chain link structure about 15 feet downstream in the original stream course. <br />This second structure has boen washed to the east side of the original stream bed. It consists of several <br />sections of 5 to 1O.foot.long sections of 12 to 14.inch.wameter spruce logs that were wired together. <br />Those log sections apparently stood on end llCrosS the creek bod and were hold in place by wire rope <br />anchored to bedrock with iron eyebolts. Wire cyclone fencing was apparently attached to the downstream <br />side. probably to provide additional support, The materials used in the second structure's construction <br />suggest that it may have been placed in the drainage after the 1951 nooding event or more recently. <br /> <br />5. Historic Component date(s) and/or sociopolitical period: 1929-present <br /> <br />Justification: Historic information indicates that the dam was constructed in 1929 <br /> <br />6. Component Function(s) <br /> <br />Original Use: Stream bank reinforcement <br /> <br />Present Use: Stream bank reinforcement <br /> <br />Comments: <br /> <br />7. Ethnic affiliation of occupants: Euroamerican <br /> <br />Justification: Historical records <br />