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<br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br /> Peak Flow (Cubic Feet per Second) <br />-Index Location Drainage Area 10-Year 50-Year 100-Year SOO-Year <br />Point (Sq. Mi.) Flood Flood Flood Flood <br />1 Near' Somerset gage 531 5,600 8,000 9;200 11,300 <br />2 Near Bowie (below <br /> Hubbard Creek) 626 6,300 9,100 10,400 12,800 <br />3 Near Paonia 734 6,900 9,900 11,300 14,000 <br />4 Above Hotchkiss 851 7,600 10,700 12,200 15,000 <br />5 Below Hotchkiss <br /> (below Leroux Creek) 937 8,100 11,300 12,800 15,700 <br /> <br />Peak flow values for 10-, 50-, 100, and 500- <br />year floods (together with corresponding water <br />surface elevations) at each cross section used in <br />the hydraulic analysis made for this report are <br />shown in Appendix A. <br /> <br />Plate 1 is an index to detailed maps (Plates 2- <br />16) showing the areas that would be inundated <br />by the loo-year flood. As shown on Plates 3, 4, 9, <br />and 12, some areas are subject to sheet flow; <br />that is, broad overland flooding generally less <br />than 2 feet deep on the average and character- <br />ized by unpredictable flow paths. Water surface <br />elevations in sheet flow areas are essentially <br />independent of those along adjacent stream- <br />ways and are affected principally by obstruc- <br />tions and local topography in the area flooded. <br /> <br />Profiles of the 10-, 50-, 100-, and 500-year <br />floods are shown as Plates 17-33. Flood eleva- <br />tions were. computed through use of the Corps <br /> <br />of Engineers step-backwater program HEC-2. <br />Basic cross section input was from field survey <br />data furnished by the Colorado Water Conser- <br />vation Board and Delta and Gunnison Counties. <br />Depth of water in the channel and adjacent <br />flooded areas can be determined from the <br />profiles. <br /> <br />Velocity of flow during a loo-year flood on <br />the North Fork Gunnison River would average <br />about 7-10 feet per second in the channel and <br />2-3 feet per second in overbank areas. Water <br />flowing at 10 feet per second will cause severe <br />erosion of channels, destroy low water cross- <br />ings, and transport large boulders. Streambanks <br />and the fill around bridge abutments may be <br />eroded, and large amounts of sediment trans- <br />ported by water flowing at 5-7 feet per second. <br />Water flowing at about 2 feet per second will <br />deposit sand, silt, and flood borne debris.- <br /> <br />5 <br /> <br />I <br />I FLOOD HAZARD INFORMATION <br />I NORTH FORK GUNNISON RIVER <br /> Hotchkiss to Somerset, Colorado <br />I APPENDIX A <br />I PEAK FLOWS AND STAGES <br /> 10-, 50-, 100-, and 500- Year Floods <br />I (Drainage Area 530 - 940 Sq. Mi.)' <br />I Peak Flow (Cubic Feet per Second) I Stage (Feet)' <br /> Cross Section 10- Year Flood 50-Year Flood 100- Year Flood 500- Year Flood <br />I Number' Location" Flow Stage Flow Stage Flow Stage Flow Stage <br /> 104 33.980 8,100 5262.5 11,300 5262.7 12,800 5263.1 15,700 5263.6 <br />I 106 34.760 8,100 5265.6 11,300 5266.8 12,800 5267.2 15,700 5267.8 <br />108 35.530 8,100 5268.5 11,300 5269.1 12,800 5269.7 15,700 5270.4 <br />110 38.190 7,600 5280.3 10,700 . 5281.3 12,200 5281.5 15,000 5281.8 <br /> 112 39.620 7,600 5288.5 10,700 5289.8 12,200 5290.6 15,000 5292.0 <br />I 112.1 39.710 7,600 5290.5 10,700 5291.9 12,200 5292.2 15,000 5292.5 <br /> 112.2 39.725 7,600 5291.0 10,700 5292.6 12,200 5293.2 15,000 5294.5 <br />I 114 39.760 7,600 5291.4 10,700 5293.1 12,200 5293.8 15,000 5i95.0 <br />116 40.200 7,600 5292.2 10,700 5293.8 12,200 5294.4 15,000 5295.4 <br />118 41.390 7,600 5298.3 10,700 5299.0 12,200 5299.3 15,000 5299.8 <br /> 118.1 41.730 7,600 5300.4 10,700 5301.1 12,200 5301.3 15,000 5301.8 \ <br />I 120 42.070 7,600 5301.7 10,700 5302.7 12,200 5303.2 15,000 5304.0 <br />122 43.080 7,600 5307.3 10,700 5307.9 12,200 5308.2 15,000 5308.7 <br /> 124 43.700 7,600 5309.6 10,700 5310.5 12,200 5310.9 15,000 5311.5 <br />I 126 44.470 7,600 5313.6 10,700 5314.8 12,200 5315.4 15,000 5316.3 <br />128 44.600 7,600 5315.8 10,700 5317.1 12,200 5317.6 15,000 5318.4 <br /> 129 44.634 7,600 5315.9 10,700 5317.2 12,200 5318.0 15,000 5319.0 <br />I 130 44.730 7,600 5316.7 10,700 5318.4 12,200 5319.0 15,000 5320.2 <br />132 46.370 7,600 5325.6 10,700 5326.6 12,200 5327.0 15,000 5327.7 <br /> 134 47.440 7,600 5332.5 10,700 5333.3 12,200 5333.7 15,000 5334.4 <br />I 136 48.620 7,600 5340.1 10,700 5341.0 12,200 5341.3 15,000 . 5341.7 <br />138 49.950 7,600 5349.0 10,700 5349.8 12,200 5350.0 15,000 5350.7 <br /> 140 50.150 7,600 5351.5 10,700 5353.1 12,200 5353.8 15,000 5355.0 <br />I 141 50.160 7,600 5351.6 10,700 5353.5 12,200 5354.5 15,000 5358.4 <br />142 50.210 7,600 5353.4 10,700 5355.0 12,200 5355.7 15,000 5358.5 <br />I 1At upstream and downstream limits of study reach. <br />2National Geodetic Vertical Datum, 1929 adjustment. -- <br /> - <br />'On reportpl'les showing flooded areas (Nos. 2-16) and flood profiles (Nos. 17-33). <br /> "Distance in thousands of feet upstream from mouth. ---._- <br /> --- <br />I 7 <br />