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<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 />I <br />I <br />I <br />I <br />I <br />I <br /> <br />The section of canal and natural drainage channel that carries water from the <br />north end of Lake Loveland to Horseshoe Reservoir is known as Dry Creek and <br />is approximately 7,512-feet in length. Features along the canal include the <br />existing 30-foot wide hinged crest gate, the railroad crossing culvert structure <br />(shown in detail on Sheet 1 of 2 in the Map Pocket), the culvert under Hwy 287, <br />the culvert under 29th Street and the double arched culverts under the Monroe <br />Avenue Bridge just upstream from Dry Creek's discharge point at the west edge <br />of Horseshoe Lake. The railroad crossing culvert structure presently limits the <br />SLRC and GLlC's ability to start the runoff season with Lake Loveland in a full <br />condition. Many times the irrigation company has lowered Lake Loveland by <br />moving water to the lower reservoirs in order to accept spring runoff and found <br />that the runoff did not occur as anticipated. This leaves the water level in Lake <br />Loveland lower than desired and results in the need to run pumps out of Boyd <br />Lake to deliver water that could have been delivered by gravity from Lake <br />Loveland. With the capacity of the Dry Creek railroad culvert structure matching <br />the inlet capacity of The Big Barnes Canal, Lake Loveland can start the runoff <br />season full and can safely pass legally decreed and diverted water on to its lower <br />elevation reservoirs without unnecessarily lowering the water surface in Lake <br />Loveland prior to receiving runoff. This will result in resource conservation by <br />eliminating the need to pump water from Boyd Lake that had in the past been <br />repositioned from Lake Loveland prior to runoff seasons. <br /> <br />While considering the capacity of the Dry Creek railroad culvert structure, some <br />discussion should be made regarding the storm capacity of Dry Creek. The <br />main channel of Dry Creek consists of a sandy clean bottom with steep side, <br />eroding side slopes. The channel top width varies between 50-feet to 90-feet. <br />Channel banks vary from 9-feet to 25-feet. The average channel slope is <br />approximately 10.5 ft.lmile or slightly less than 0.002 ft.lft. Storm flows through <br />this section of canal (as identified in the Ayers Dry Creek Study) range up to <br />2,720 cfs during a 100-year storm event with an average depth of 13.6 feet and <br />average velocity of approximately 2.8 ftIsec. During the 1 OO-year storm event, <br />the Monroe Avenue Bridge is overtopped by approximately 662 cfs with a <br /> <br />18 <br />