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3.0 INUNDATION EXTENTS <br /> 3.1 Detail of Mapping <br /> The water surface profile from the HEC-RAS hydraulic modeling was exported to ArcGIS, and the <br /> inundation extents were delineated using the 2011 USDA 10-meter DEM. <br /> All bridge crossings in the study reach (with the exception of I-25 over WCR 32) were identified in <br /> aerial photography as small culverts and were therefore assumed to be significantly overtopped. For <br /> this reason, ground surveys were not necessary at the culvert locations. However, a site visit to the <br /> I-25 overpass was conducted to estimate the effective opening and to inspect the embankment <br /> because the 10-meter DEM is not detailed enough to accurately depict roadway embankments. <br /> During the visit a low point in the I-25 profile was identified approximately 1,000 feet north of <br /> WCR 32. Though this local depression was not included in the hydraulic modeling, it was <br /> considered during the delineation of the flood extents. <br /> The inundation maps associated with this report are provided in Appendix F. <br /> 3.2 Description of Inundation Area <br /> The flood from a clear-day piping failure of Highland No. 1 Dam will reach a peak flow rate of 850 <br /> cfs at the breach, and will flow through mostly open farmland along a natural drainage path for <br /> approximately 0.5 miles until reaching the I-25 bridges over WCR 32. Velocities calculated in this <br /> reach average 2 to 3 feet per second,but may achieve speeds up to 5 feet per second. Depths in this <br /> reach are generally less than 2 feet, but can potentially be much greater in the vicinity of the I-25 <br /> embankment (over 6 feet deep). The flow through the overpass opening will be nearly 4 feet deep <br /> with a velocity over 8 feet per second. Slight overtopping of I-25 at the low point in the <br /> embankment 1,000 feet north of WCR 32 is expected,but overtopping can become more severe if <br /> the overpass opening clogs with debris. <br /> After passing I-25, the flood will cross a field and enter a natural drainage channel which it will <br /> follow to Thomas Reservoir. Depths in this reach will range from 1 to 3 feet, and velocities will <br /> often exceed 5 or 6 feet per second due to the narrow channel width. The flood will then enter <br /> Thomas Reservoir where it will be fully contained within the reservoir's surcharge volume. For this <br /> reason, the detailed inundation mapping extent was terminated at the inlet to Thomas Reservoir. <br /> HIGHLAND NO. I DAM -4 - June 15,2012 <br /> INUNDATION MAPPING REPORT <br />