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<br />I <br /> <br />I <br /> <br />the report are designed for the highest velocities modeled and as such can be implemented at any <br />point along the study reach, <br />7. A toe protection detail and typical riprap specification is provided in the report, A potential <br />source of the riprap is identified, Material and placement costs are estimated for different <br />scenarios that offer varying levels of protection, <br /> <br />I <br /> <br />I <br /> <br />Limited Watershed Studv: <br /> <br />I <br /> <br />I. A flood frequency analysis was performed by CWCB using 20 years of streamflow data at the <br />Milner gage on the Elk River. Resulting flows at this location indicate that the 100-year flow is <br />6.190 cfs and the 5~year flow is 4,770 cfs, The peak flow from the 1997 flood event at the Milner <br />gage was estimated to be 5,370 cfs. or between a 10- to 50-year event. <br />2, It is estimated that approximately 41 % of the average basin runoff originates from the Park Range, <br />3, Steamboat Lake controls about 8% of the Elk River drainage basin and is not currently operated as <br />a flood control reservoir. In order to provide flood control, the operation of the reservoir would <br />need to be changed, and it is likely that structural changes to the service spillway andlor <br />emergency spillway would be required, This would negatively impact the recreational and <br />fisheries mission of the reservoir, Resulting flood protection at the lower extremes of Elk River <br />would only be marginally improved, <br />4, Gage information along the Elk River and Willow Creek was used to perform a travel time <br />analysis for determining a relationship between Steamboat Lake releases during the June 1997 <br />flood event and the Elk River discharge at the Milner gage, Our results indicate that the <br />approximate travel time between Steamboat Lake and the Milner gage is around 7 hours. Daily <br />reservoir peak release rate information for Steamboat Lake indicates that between 250 cfs and 280 <br />cfs were released during June I" and June 2", Therefore. it appears that discharge from <br />Steamboat Lake contributed to about 5% of the total peak flow (5370-cfs) at the Milner gage <br />during the 1997 flood event. This flow amount is less than the 400 cfs that the USGS determined <br />had overflowed County Road 42 just upstream of the Milner gage, <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />ICON Engineering Inc. wishes to acknowledge the assistance of the project sponsors and the many <br />interested parties that have provided data and analysis contributing to this report, <br /> <br />I <br /> <br />Submitted by: <br /> <br />I <br /> <br />ICON Engineering, Inc. <br /> <br />By: <br /> <br />By: <br /> <br />Terri Fead, PE <br />Project Manger <br /> <br />I <br /> <br />Penn Gildersleeve. PE <br />Principal ]n Charge <br /> <br />By: <br /> <br />Craig Jacobson, EIT <br />Project Engineer <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />