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<br />II <br />I <br /> <br />I <br /> <br />close to the channel. A low dike forms a tail water pond for the Blackmer <br />Lake outlet. <br /> <br />I <br /> <br />Blackmer Lake lies below a loop in the Highline Canal and covers 7.5 acres <br /> <br /> <br />when full. The top of the dam is 22 feet above its tailwater level. A <br /> <br /> <br />3-barrel, 660 cfs siphon spillway goes into operation when the lake level <br /> <br /> <br />rises. The old dam embankment was repaired and modified in 1937. Two small <br /> <br /> <br />tributaries originally joined at Blackmer Lake. The Highline Canal presently <br /> <br /> <br />intercepts low flows from these tributaries. Only the northern tributary <br /> <br /> <br />channel was studied upstream of Blackmer Lake. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Between the Highline Canal and Holly Street, the channel is interrupted by <br /> <br /> <br />three 7-foot high dikes forming private ponds used for the storage of irri- <br /> <br /> <br />gation water, The reach has an unusually heavy growth of weeds, cattails, <br /> <br /> <br />and mature trees. Adjacent homes are out of the flood plain. <br /> <br />I <br /> <br />I <br /> <br />From Holly Street to a line of extension of South El Camino Drive a paved <br /> <br /> <br />road has been built in the bottom of the waterway. Shallow ditches convey <br /> <br /> <br />annual frequency runoff to a 24-inch culvert under Holly Street, but a 10- <br /> <br /> <br />year or larger storm inundates the paved street and the low part of Holly <br /> <br /> <br />Street. The storm in May 1973 partially washed out Holly Street at this <br /> <br /> <br />location. The waterway reach is clear of obstructions. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The last reach of Blackmer Gulch between a line of extension of South El <br /> <br /> <br />Camino Drive and Charlou Drive, an extension of Monaco Street, is steep but <br /> <br /> <br />well covered with prairie grasses. No obstructions exist. An l8-inch <br /> <br /> <br />culvert under Charlou Drive is completely plugged with soil that has been <br /> <br /> <br />eroded and transported by runoff. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Quincy Gulch in Cherry Hills Village. Dry weather flow from Quincy Gulch is <br /> <br /> <br />conveyed in a small, shallow roadside ditch that enters Blackmer Gulch at <br /> <br /> <br />Random Road. Roadside ditches are used to convey low flows for at least <br /> <br /> <br />1,500 feet upstream; however, no well-defined natural channel exists and <br /> <br /> <br />under present conditions 10-year and greater runoff will flow over the area <br /> <br /> <br />in a wide shallow band. From the confluence of Quincy and Blackmer Gulches <br /> <br />I <br /> <br />I <br /> <br />-24- <br /> <br />I <br />