Laserfiche WebLink
<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 />HYDROLOGY <br /> <br />11-31 <br /> <br />Where the Chatfield Dam outlet channel empties into the South Platte River, <br />there is a check dam of rocks which drops approximately 6 feet. There- <br />after, the river flows in its natural channel for which the bottom is 160 <br />feet wide on the average. The high bank is approximately 7 feet high. <br /> <br />There is a sewer line encased in concrete across the river bed immediately <br />downstream from the C-470 bridge. The sewer line has been exposed due to <br />river bed and bank erosion. Thereafter, the South Platte River is eroding <br />its banks in places. The river has moved itself appreciably, probably <br />aided by the gravel mining operations. : Between 1964 and 1978, the maximum <br />lateral movement of the meander loops was approximately 900 feet. Vertical <br />degradation of the South Platte River bed was a maximum of six feet during <br />this same period. <br /> <br />The reach between C-470 and Columbine Valley is planned to remain in a <br />semi-natural condition as a floodplain park; however, bank stabilization is <br />a high priority. In this reach there have been two major drops with a <br />total drop of 14 feet. The slope between the drops is about 7.3 feet per <br />mile. The bank full width of the river is 264 feet with an average depth <br />of 6.5 feet, making the width to depth ratio equal to 41. <br /> <br />This bed erosion has been accompanied with bank erosion on both sides of <br />the river. Trees have fallen into the channel and a gravel pit has been <br />breached. <br /> <br />Immediately upstream of Columbine Valley the river bed has aggraded <br />approximately 3 to 4 feet due to the flatter hydraulic slope. <br /> <br />Between Columbine Valley and Union Avenue, the USACE has constructed a <br />stable channel, a channel that has a stable bed, drop structures, and <br /> <br />