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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 />frequency). This relationship produces the following values for peak flows at <br />the following gages: <br /> <br />Manitou: <br />1,075 cfs/mi2 x 103 mi2 = 110,725 cfs <br /> <br />Tejon: . <br />1,075 cfs/mi2 x 392 mi2 = 421,400 cfs <br /> <br />Using a straight-line relationship, with the mean annual flood as the second <br />point, a linear relationship is produced as shown on FiQures 4.8-1 and 4.8-2 <br />using paleohydrologic evidence. <br /> <br />Jarrett (1987) also studied in detail paleohydrologic evidence along Fountain <br />Creek and its tributaries and while little flood flow frequency numerical <br />information was developed, the following conclusions can be reached: <br /> <br />1. Streams above 7,500't show little evidence of large floods in terms of <br />peak unit discharge per square mile. <br /> <br />2. Many individual basins in the elevation range of 6,000 - 7,500' show <br />very high unit di scharges per square mil e but not for the same <br />meteorologic events. This illustrates that the largest floods were <br />caused by intense rainfall which was very localized, possibly due to <br />orographic characteristics and other factors. <br /> <br />3. There is a preference for flood~ on basins facing southeast toward the <br />prevailing flow of moisture. <br /> <br />4.9 HYDROLOGIC SUMMARY AND DESIGN FLOW RECOMMENDATION <br /> <br />Rationale <br /> <br />In consideration of the size of the Fountain Creek drainage basin, its regionally <br />unique geographic position. along the Front Range of Colorado, the site specific <br />basin characteristics, and the lack of consistent, reliable rainfall/runoff <br />information, no one hydrologic method can be depended upon to be uniquely <br />correct. As such, the results of the methodologies described in the previous <br />sections have been compiled on discharge/frequency Figures 4.8-1,4.8-2 and 4.9-1 <br />for the purpose of comparing the estimated IO-year and 100-year flows for each <br />of the hydrologic index locations previously described. This provides a summary <br />of information in a visual format which assists the responsible entity in <br />choosing values and/or a method which is acceptable for the purposes for which <br />those values are to be used. The following paragraphs discuss Figures 4.8-1, <br />4.8-2 and 4.9-1 and interpret the results of the various methods. The final <br />section makes recommendations on design flows to be adopted. <br /> <br />Early in the hydrologic evaluation it was discovered that the U.S. Army Corps of <br />Engineers, authors of the currently adopted flood peak information (used also in <br />the FEMA flood insurance studies), consider that information obsolete and the <br />numbers too high for the reach of Fountain Creek upstream of the confluence. The <br /> <br />4.0-23 <br /> <br />. <br />. <br />. <br />. <br />. <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />i <br /> <br />... <br />C <br />~ <br /> <br />a.: <br />c( <br />IX <br /> <br />... <br />iil <br />j <br />