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<br />II - 6 <br /> <br />I <br />I <br />I <br />I <br />I <br />a <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Flow arriving at the area of Highway 36 Bridge over the main channel of South <br />Boulder Creek can potentially spill to the northwest. There are three major and <br />several minor routes which the flow can take: <br /> <br />1. Main Channel. The main channel route conveys flow in a largely riparian <br />cottonwood grove floodplain which has a mixture of open space, agriculture, <br />residential, and commercial uses. As the main channel passes by the <br />Wellman Ditch additional spills to the West Valley occur through a residential <br />area and the golf course (element 237, Drawing 7). Below Arapahoe, the <br />Leggett Canal to the Valmont reservoirs (Hillcrest, Valmont, Leggett) can also <br />carry flood flows (236, Drawing 8). Also, there is another potential spill to <br />the west to Dry Creek Ditch No.2 near the railroad tracks, which has not <br />been evaluated herein due to complex backwater analysis and perceived <br />likely low magnitude. <br /> <br />2. Direct return to South Boulder Creek: Drv Creek No.2. Viele. and the <br />Anderson Ditch. The South Boulder Creek spillage upstream of Highway 36 <br />that flows to the northwest would be joined by flows from Dry Creek Ditch <br />No.2. <br /> <br />There are three modest conveyance systems which will carry an initial <br />portion of the flow across Highway 36 and, for the most part, back to South <br />Boulder Creek just below South Boulder Road. The first 220 cfs would be <br />conveyed in the Dry Creek Ditch No.2 box culvert under Highway 36 (263 <br />and 376, Drawing 10\, and via an irrigation ditch to a spill structure (375\ <br />near South Boulder Road which would shed most of the flow to the New <br />Anderson Ditch, which subsequently could spill to Viele (378). Greater <br />spillage flow from South Boulder Creek, on the order of 500 to 800 cfs, will <br />be intercepted by the Viele drainage system (265 and 1267) adjacent to the <br />Foothills Parkway Interchange and conveyed under Highway 36, and then <br />combine with the spillage from the lower Anderson Ditch and the Dry Creek <br />Ditch No.2, and flow under South Boulder Road to South Boulder Creek. <br /> <br />Greater South Boulder Creek spillage would overtop the Viele system and <br />flow onto the freeway (292). Some portion of this spillage and local <br />drainage flows can be conveyed by the Anderson Ditch to the east to South <br />Boulder Creek, subject to some spillage to the north at several points, the <br />first and most significant of which would occur near the Anderson culvert <br />under the Highway 36 eastbound on ramp (383). <br /> <br />3. West Vallev Overflow. Greater South Boulder Creek spillage (from 700 to <br />1000 cfs) would flow onto Highway 36 (360) and pass by the Anderson <br />Ditch, and then largely overflow the Highway 36 barrier (352 and 1812) and <br />