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<br />I <br /> <br />I <br /> <br />In Colorado, the 100-year flood plain is an area of state interest as <br /> <br />defined in H,B, 1041, Lesser floods with higher probabilities of <br /> <br /> <br />occurrence have, therefore. not been considered here. Flood magnitudes <br /> <br />greater than the 100-year flood magnitude can and will occur and plans for <br /> <br />land improvement adjacent to the 100-year flood plain should consider the <br /> <br />probability of flood damage, Flood hydrographs at key locations are shown <br /> <br />in Figures 3 through 6 in the Appendix, <br /> <br />The 100-year flood plain limits and water surface profiles for the reach of <br /> <br /> <br />the Spring Gulch flood plain are shown on the Flood Hazard Area Delineation <br /> <br /> <br />drawings, Sheets 2 through 6 (see Appendix), and the computed 100-year <br /> <br />flood elevations for the various cross section locations are tabulated in <br /> <br /> <br />Table 3 as discussed earlier, A brief description of the significant <br /> <br />flooding aspects for this reach follows: <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The peak flow profiles given in Figure 7, in the Appendix, shows the <br /> <br />discharges developed in the hydrologic portion of this study for the <br /> <br /> <br />100-year flood event and are the discharges used in the hydraulic analysis <br /> <br />portion of the flood hazard area delineation, The discharge values shown <br /> <br /> <br />are those which could occur under fully developed conditions without any <br /> <br /> <br />mitigating measures being considered to control or retard the increased <br /> <br /> <br />rates of runoff. A previous report entitled "Master Plan Of Drainage <br /> <br />Detention for Spring Gulch" has addressed reduced discharge rates <br /> <br /> <br />which are more representative of final design conditions and <br /> <br /> <br />describes the mitigating measures which are to be taken to achieve a <br /> <br /> <br />discharge rate which should not exceed pre-development conditions at <br /> <br /> <br />the downstream edge of Highlands Ranch development, (i,e, D,S, 85), <br /> <br />The downstream terminus of the Spring Gulch Flood Plain (STA 1+00) is <br /> <br />located just upstream of the Army Corps of Engineers Detention Embankment, <br /> <br />As previously mentioned in this report and the Master Plan of Drainage for <br /> <br />Spring Gulch, the backwater elevation at this location was based on a flood <br /> <br />routing of the developed storm through the Corp's outlet structure for this <br /> <br />embankment (see Alternative 2 - Master Plan of Drainage Detention). This <br /> <br /> <br />ponding condition is contained within the Corps property and backs water to <br /> <br />STA 8+00. The Corps of Engineers (CaE) facility is capable of holding <br /> <br /> <br />approximately 16 inches of runoff from the Spring Gulch watershed, The <br /> <br /> <br />limits of P,M,F, ponding are shown on sheets 1 and 2 of 7, The spillway is <br /> <br />located on the north side of the CaE property, <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />The 100-year flood discharges shown in the figures mentioned above are <br /> <br /> <br />conservative in that the highest discharge rate calculated for a subreach <br /> <br /> <br />is used for the entire subreach length, not just for the point for which <br /> <br /> <br />it was calculated, In general, discharge values were selected such that <br /> <br />they increased in step fashion as the flood progressed downstream, <br /> <br />An overtopping of an existing private road 'Old Ranch Road' occurs at STA <br /> <br /> <br />42+00 during the 100-year storm, Flood depth over the top of the road is <br /> <br />approximately 5 feet, It is anticipated that this roadway will cease to <br /> <br /> <br />exist when development begins in the Spring Gulch basin, <br /> <br />I <br /> <br />I <br /> <br />B, FLOOD PLAIN AND FLOODWAY DATA <br /> <br />The only future road crossing scheduled for Spring Gulch at this time is <br /> <br />Westridge Parkway - located at STA 58+00, Backwater conditions have been <br /> <br /> <br />evaluated for this crossing and the following was concluded: The maximum <br /> <br /> <br />allowable backwater elevation will be 5654,5 - this backwater extends <br /> <br /> <br />approximately 1600' upstream to STA 74+00. <br /> <br />I <br /> <br />I <br /> <br />The Spring Gulch flood plain has been characterized as one main reach and <br /> <br />is stationed to readily identify the various points of interest of the <br /> <br /> <br />waterway, The Basin Boundary Map (sheet 1 of 7) in the Appendix of this <br /> <br /> <br />report provides a more exact location of this reach. <br /> <br />In addition to the backwater conditions mentioned above, minor backwater <br /> <br /> <br />conditions exist at 6 check dams located at various points along the Gulch, <br /> <br /> <br />With the exception of these check dams, it was found the lOa-year flood <br /> <br /> <br />event would be confined within the existing natural channel for a major <br /> <br />part of the Gulch. For this reason no cross~sections were found where <br /> <br /> <br />meaningful floodway data could be tabulated (see Table 3 - Appendix), <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />7 <br /> <br />I <br />