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just above Highway US 24, plots at about twice the extrapolation <br />of the 100-year discharge relationship along the Fountain Creek <br />main channel. That is an appropriate discharge with the <br />knowledge that Waldo Canyon has a much steeper gradient than <br />Fountain Creek, 90 feet per mile (US Army Corps of Engineers, <br />1974), as compared to the 700 plus feet per mile for Waldo <br />Canyon. , , <br />Diversion/Conveyance Channels <br />The development of the Summit Pit will regairo that changes be <br />made to the existing condition of tho stream channels. It is <br />planned that the channel capacity of the existing c s ag <br />typified in figure Exhibit G-2 Mill be asintay ough the <br />working pit during tho poriad of operat#ow to con normal <br />flood flows. Inspection of the existing channels indicates that <br />the normal flood flows within Waldo Canyon and the East tributary <br />are much less than the design flow as derived by the HEC1 method. <br />This is explained by the fact that the mean annual flows and the <br />more frequent storm flows, up to about the 10-year storm are <br />controlled by snowmelt. The infrequent storms like the 100-year <br />event result from the large thunderstorms which produce the large <br />flows as described in the flood plain information report for <br />Fountain Creek (US Army Corps of Engineers, 1974). <br />CMLRD comments include the recommendation that upland diversions <br />be built to convey flows around the pit operations. This <br />alternative is not feasible in that any upland diversions would <br />have to be cut into the sides of the very steep canyon walls <br />which would cause more disturbance than the present plan to route <br />the existing channels,t~irough the pit area in approximately their <br />current locations. The-.preeerrt plan is to meintafa err <br />appropriate channel cross section through the pit area during <br />operation in accordance with the cross sections as shown in <br />Exhibit G-2. <br />During reclamation. tbo plea is to rip ani blast, as required, a <br />trapezoidal shape chaaa4l in the bedrock a~ depicted is figure <br />Exhibit G-3. The size of the channels, by reach, are listed in <br />Table 2. The channels are relatively wide compared to the depth <br />because of the practical need to have sufficient width in the <br />bottom to work heavy construction equipment to construct the <br />channels in solid rock. As shown in the channel diagram, there <br />is 1 foot of additional depth provided as freeboard. This is <br />standard in channel design. Thn velocities which will occur <br />during th4 d°~ a~ser-ere much higher than clef be perrei.seible <br />in an erodible bed chaaasl. Howevor, ~inae tYwca channels will <br />be cut into solid bedrock, there will be little problem of high <br />velocities in the chenne2. <br />~urtaae Nater Responses: Summit Pit Application page 5 <br />