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Last modified
1/29/2010 10:11:44 AM
Creation date
10/4/2006 8:59:24 PM
Metadata
Fields
Template:
Floodplain Documents
County
Delta
Gunnison
Community
Hotchkiss to Somerset
Stream Name
North Fork Gunnison River
Title
Flood Hazard Information
Date
2/1/1980
Prepared For
Delta County
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Floodplain Report/Masterplan
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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 />FLOOD HAZARD INFORMATION <br /> <br />Dam. From its source to jts mouth near Lazear <br />the stream flows about 30 miles on a southwest~ <br />erly course. Its tributary drainage area (a part of <br />the Colorado River Basin) is situated in west- <br />central Colorado on the western slope of the <br />Rocky Mountains. At Hotchkiss and Somerset, <br />the stream drains 940 and 530 square miles, <br />respectively. Elevation ranges from 5400 feet <br />(NGVD) at Hotchkiss to around 13,000 feet in <br />the highest headwater regions, and stream <br />gradients vary from about 30 feet per mile at <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />l <br />I <br /> <br />Hotchkiss to 60 feet per mile at Somerset. <br />Terrain of the basin is mostly mountainous with <br />some mesa and tableland in the lower portion. <br />Predominant vegetation consists of pine, fir, <br />and spruce in the high portions of the drainage <br />area, while sagebrush and other low-growing <br />shrubs are characteristic in the lower portions. <br />Thick stands of cottonwood occur along the <br />river. A map of the North Fork Gunnison River <br />Drainage Basin and its tril:iutaries within the <br />study limits is shown on page 3. <br /> <br />NORTH FORK GUNNISON RIVER. <br /> <br />Hotchkiss to Somerset, Colorado <br /> <br />CONTENTS <br /> <br />Page <br /> <br />NATURE OF FLOOD PROBLEMS <br /> <br />INTRODUCTION ....... <br />NATURE OF FLOOD PROBLEMS <br />FUTURE FLOODS ....... <br /> <br />General frontal-type rainstorms approaching <br />from the southwest can occur over the North <br />Fork Gunnison River basin from mid-June <br />through December, but records show that they <br />occur most often during September and <br />October. Convective-type cloudburst storms <br />occur frequently during the summer in west- <br />central Colorado. Most of the annual precipita- <br />tion in this region, however, occurs as snow and <br />a deep snowpack usually accumulates in the <br />high areas. Studies show that rapidly melting <br />snow in the spring and early summer constitutes <br />the principal source of flooding along the North <br />Fork Gunnison River. Severe floods result when <br />rapid snowmelt is augmented by rain. The <br />largest flood known in the Gunnison River <br />basin occurred in June 1884. It is probable that <br />flood conditions along the North Fork were also <br />severe that year. <br /> <br />Generally, high flows along the North Fork <br />Gunnison River are contained in-channel, and <br />extensive overbank flooding is infrequent. <br />However, newspaper accounts indicate flood <br />damage. to orchards, roads and road bridges, <br />railroad facilities, homes, and business estab- <br />lishments in 1906, 1907, 1912, 1916, 1917, 1920, <br />and 1927. All flood events occurred in May with <br />damage specifically mentioned in Bowie, <br />Paonia, and Hotchkiss. Serious erosion of <br />farmland, pastureland, and orchards is known <br />to have OCCurred. In descending order of <br />magnitude, the highest recorded flows on the. <br />North Fork occurred in May 1932, June 1957, <br />May 1929, May 1973, May 1928, and May 1974. <br />Peak flows of the larger historical floods on the <br />North Fork Gunnison River in the study area are <br />shown in the following tabulation. <br /> <br />.1 <br />.2 <br />.4 <br /> <br />APPENDIX <br /> <br />A PEAK FLOWS AND STAGES . . . . . . . . . . . . . . . . . . . . . . . . . . 7 <br /> <br />PLATES <br /> <br />PLATES <br /> <br />1 INDEX MAP <br />2-16 FLOODED AREAS <br />17-33 FLOOD PROFILES <br /> <br />PEAK FLOWS OF HISTORICAL FLOODS <br /> <br />INTRODUCTION <br /> <br />Peak Flow (cubic feet per second) <br />Near Paonia CaRe Near Somerset Cage <br /> <br />Date <br /> <br />This report covers the findings of a flood <br />hazard information study of the North Fork <br />Gunnison River from Hotchkiss to Somerset, a <br />distance of 21 miles. Its purpose is to provide a <br />basis for planning to avoid or reduce damage <br />from the use of lands subject to inundation by <br />the 100-year flood. Topographic maps and <br />channel cross sections needed for the report <br />were jointly provided by the Colorado Water <br />Conservation Board and the Commissioners of <br />Delta and Gunnison Counties. Data on past <br /> <br />floods, as well as other information useful in <br />making the study, were obtained from local <br />residents, County Planning Departments, and <br />State and Federal agencies. <br /> <br />Hotchkiss is in Delta County at the junction <br />of State Highway 92 and 133, and Somerset <br />(Gunnison County) is 17 miles northeast from <br />Hotchkiss along Highway J33. The North Fork <br />Gunnison River is formed by the confluence of <br />Muddy and Anthracite Creeks near Paonia <br /> <br />3 May 1928 <br />15 May 1929 <br />12 May 1932 <br />4 Jun 1957 <br />21 May 1973 <br />8 May 1974 <br /> <br />6,450 <br />7,310 <br />8,590 <br /> <br />7,860 <br />6,580 <br />5,130 <br /> <br />'Gage not in operation. <br /> <br />incl1 <br /> <br />1 <br /> <br />:J <br /> <br />2 <br />
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