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<br />I <br /> <br />I <br /> <br />I <br /> <br />This study assumed that all irrigation ditches were full of water and <br /> <br /> <br />that no interception of runoff occurred at any open ditch. It was also <br /> <br /> <br />assumed that no change would occur to the operation, maintenance and <br /> <br />topographic appearance of any ditch in the future totally developed <br /> <br />Basin. <br /> <br />occur at the Dutch Creek Crossing, than was assumed in the other studies. <br /> <br /> <br />This report also shows a reduced area of sheet flow or flood plain over- <br /> <br />flow on the north side of Dutch Creek in Columbine Valley. This may be <br /> <br /> <br />attributable to the larger flow diversion estimated at the Fairway Lane <br /> <br /> <br />crossing in this report, or to the use of more detailed mapping and digit- <br /> <br />ized cross sections in this area resulting in different ground elevations <br /> <br /> <br />at various locations. In all other areas of the Basin, the flood plain <br /> <br /> <br />delineations were found to be consistant between the various studies. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The results of this Flood Hazard Area Delineation study were compared <br /> <br /> <br />with two other previous flood plain information studies: <br /> <br /> <br />- Flood Plain Information Report, Goldsmith Gulch, Dutch Creek, Lilley <br /> <br /> <br />Gulch and Coon Creek, Volume VI, Denver Metropolitan Region, Colorado, <br /> <br /> <br />October 1971, by the U.S. Army, Corps. of Engineers. <br /> <br />- Proposed flood elevation determinations for the Town of Columbine Valley, <br /> <br /> <br />Colorado, National Flood Insurance Program, March 14, 1977, by the <br /> <br />Department of Housing and Urban Development, Federal Insurance Adminis- <br /> <br /> <br />tration. <br /> <br />Flood Plain and Floodway Data <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Differences in flood plain delineations between this report and the other <br />studies primarily are attributable to the following: <br />1. This report used more recent aerial photography. <br />2. Mapping used in this report is more detailed with <br />a 1"-100' horizontal scale and a 2-foot contour interval. <br />3. Different procedures were used in the hydrological investigation <br />for each study which resulted in a variation in streamflow dis- <br />charges. <br />4. Different assumptions were used pertaining to land area develop- <br />ment which also contributed to the variation <br />in streamflow discharges. <br /> <br />The limits of future flooding are outlined on the attached drawings and <br /> <br /> <br />tabulated in Table C-l in Appendix C, Flood Plain and Floodway Reference <br /> <br /> <br />Data. The table lists the potential flood elevations, flooding widths <br /> <br /> <br />and Reference Line elevation at each cross section for the drainage <br /> <br /> <br />reaches studied. The flood profile Thalweg (reference) line and flood <br /> <br /> <br />plain width at any point on the streams is graphically shown on the <br /> <br /> <br />drawings. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Floodways have also been computed for each stream. A floodway repre- <br /> <br /> <br />sents that part of the flood plain which is required to pass a 100-year <br /> <br /> <br />flood event without raising the flood profile more than an acceptable <br /> <br /> <br />amount and which represents hazards to personal safety and welfare. <br /> <br /> <br />In this study, the floodway represents that portion of the flood plain <br /> <br /> <br />where the 100-year flood velocities exceed 2 to 3 feet per second or <br /> <br />I <br /> <br />I <br /> <br />where the water surface profile would not increase more than 0.5 feet <br />after encroachment. Floodway widths, representing the I imj ts of en- <br />croachment into the flood plain at each point in the stream, are tabu- <br /> <br />I <br /> <br />I <br /> <br />The largest variation of the flood plain delineation between this study <br />and the other two seemed to occur in the Town of Columbine Valley. This <br />report shows a more definite flood plain extending along Fairway Lane <br />from the crossing of Dutch Creek eastward to the Platte River, which <br />indicates a larger flow split diversion estimated to <br /> <br />lated in Table C-l of Appendix C. The water surface elevations to be <br />expected after encroachment are also tabulated. <br /> <br />I <br /> <br />Flood Velocities <br /> <br />I <br /> <br />Average flow velocities during a 100-year flood for each creek are pro- <br /> <br />I <br /> <br />11 <br />