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future directions for flood control system improvements. <br />Fonntain Creek and Tributaries <br />Flows from Fountain Creek and its tributaries run directly into the Arkansas River below Pueblo. <br />Increases in base flow from water transported across the Continental Divide to C;olorado Springs <br />that are dischazged into Fountain Creek following use and treatment by the city ~ias occurred <br />since 1952 with the construction of the Hoosier Tunnel Project. Tlus was followed by the <br />construction of the Homestake VJater Development Program in conj~nction wi~i the City of <br />Aurora in 1965. Finally, the Bureau of Reclamation completed construction of the Fryingpan- <br />Arkansas Project in June 1981. <br />The water rights to the share of water received by Colorado Springs through these projects are <br />fully controlled by the city. These rights continue for any discharge of this, so-c~iled, "trans- <br />mountain water" into Fountain Creek. The city is credited for the dischazge of trans-mountain <br />water into Fountain Creek (and therefore the Arkansas River) through stora.ge of Arkansas River <br />water at Pueblo Dam. This water is stored under a so-called "if and when" aman~ement. Under <br />this arrangement, if storage volume is needed for flood control or when downstream irrigation <br />districts place a demand on the storage volume, the water credited to Colorado Springs is <br />released. At that point, Colorado Springs rights to those waters aze lost. The city also loses <br />rights to waters lost through evaporation, ground percolation and bank losses during transit down <br />Fountain Creek. Colorado Spri.ngs is able to make use of water stored at Pueblo Dam by <br />pumping water back up through the Otero pipeline. <br />The increased base flow down the Fountain Creek and Arkansas River by discharges of trans- <br />mountain water does artificially affect the channel capacity to some degree. Mor~ importantly it <br />may have created a significant imbalance within the creek and river system that fi~rced changes <br />in the system in an attempt to achieve a new equilibrium. This adjustment process may be taking <br />the form of more meandering, increased bank erosion and channel bed degradation in some, <br />reaches and increased aggradation of the channel bed in other reaches. This on-going natural <br />process has negatively impacted upon properties along Fountain Creek in incorporated and <br />unincorporated areas like Colorado Springs, Manitou Springs, Security, Fountain;, Pinon, Pueblo <br />and others. As indicated earlier in this report (see Table 3-3), this process may also Y~e <br />contributing to the accelerated aggradation within the Arkansas River since 1965. <br />Development on Fountain Creek in the City of Manitou Springs has severely encroached upon <br />the floodplain. In the downtown azea, Fountain Creek is reduced to a narrow channel with a <br />conveyance capacity of around 1,000 c.f.s. This equates to approximately the 10-yeaz frequency <br />flood. A reconnaissance report by the Corps of Engineers in May 1995 (revised ~ugust 1996) <br />indicated that flood-warning systems providing 15 minutes to 3 hours advance notice of floodin~ <br />on Fountain Creek do not allow su~cient time for emergency evacuation procedures. The <br />economy of Manitou Springs is highly dependent upon tourism. The tourist seasan coincides <br />with the summer flood season and creating a severe flood management problem. 'The speed at <br />which flows could overflow the nanow channel and create fast moving floodwate.rs several feet <br />Chapter 3- Flood of April ~?9, 1999 <br />Post Flood Assessment Report ~ 28 Draji Revised o9/09/99 <br />