Laserfiche WebLink
<br />4 <br /> <br />m <br />I <br />I <br />r <br />I <br />~ <br />I <br />r <br />I <br />I <br />I <br />I <br />t <br />r <br />L <br />I <br />I <br />l <br />~ <br /> <br />TABLE 1. - SUMMARY OF DISCHARGES'IJ <br /> <br />Flooding Source and Location Drainage Peak Discharge <br /> Area (cfs) <br /> (Sq. I 0- year 50-year I 00- year 500-year <br /> Miles) <br />At Confluence with Canyon 45 820 1,280 1,680 2,480 <br />Creek <br />At Confluence with Cascade 75 1,280 1,940 2,590 3,800 <br />Creek <br />At Downstream Corporate Limits not 1,330 2,040 2,720 4,000 <br /> available <br /> <br />NOTES: <br /> <br />(I) <br /> <br />Federal Emergency Management Agency, Flood Insurance Study, City <br />of Ouray, Colorado, Ouray County, July 3, 1985. <br /> <br />Hydraulic Analysis <br />. . <br /> <br />Hydraulic analysis for the model development and for the proposed project were conducted using <br />the U.S. Army Corps of Engineers (US ACE) HEC-2 computer program. The approach taken for <br />these tasks are described below. <br /> <br />Model Development - The original HEC-2 model, used to define the floodplain in the Floodplain <br />Information Report for the Uncompahgre River (Reference I) was not available. Discussions by <br />CWCB personnel with engineers who performed the original work identified that cross section <br />information was digitized by the mapper. However, no records of the model or cross-section data <br />could be found. Research into CWCB files resulted in a blue-print of the original 1"=200', 5' <br />contour interval topographic mapping ("blue-prints"), which was used for the model development, <br />as described below: <br /> <br />A. The location of the original cross sections were identified on the blue-prints using the <br />Floodplain Information Report. Elevations and stations were read and recorded (note: <br />This information was provided by the CWCB and was checked and modified during the <br />course of the work.) <br /> <br />B. Cross section information was plolted on work sheets. The thalweg invert and the <br />floodplain width from the Floodplain Information Report were used to adjust the channel <br />invert and the width of the section at the 100-year water surface elevation. <br />