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<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 />I <br /> <br />Dt~~ " - H\'l'ROLOGY & HYDRAULIC INcORMATION <br /> <br />(Chapters II & III fro;; Floodplain Infonnacion Report) <br /> <br />Ch':'Ylt r< II <br /> <br />STUDY AREA DESCRIPTION <br /> <br />Location <br />The study area is comprised of 2.7 miles of the Lake Fork of the <br />Gunnison and 0.33 miles of its tributary, Henson Creek, both of which <br />are located in the immediate vicinity of Lake City, Colorado. The Lake <br />Fork of the Gunnison has its headwaters in the San Juan Mountains of <br />Southwestern Colorado. After its confluence with its main tributary, <br />Henson Creek near Lake City, it flows northerly for approximately 30 miles <br />to its confluence with the Gunnison River in Blue Mesa Reservoir. The <br />total drainage area for the Lake Fork of the Gunnison is over 350 square <br />miles; its average annual flow is approximately 235 cfs. <br />The study area is located immediately above, within and below the town of <br />Lake City, which is the capital seat of Hinsdale County. The estimated <br />population of Lake City is 500. Most of the drainage area <br />above the study reaches is within the Uncompahgre or Gunnison National <br />Forest and on land administered by the Bureau of Land Management. Plate <br />shows the drainage basin and regional location of the study area. <br />Climate <br />The climate of the drainage area is influenced predominately by the <br />high elevation and rugged topography of the surrounding San Juan Mountains. <br />The climate is typically alpine, characterized by cold winters with heavy <br />snowfall and cool, short summers. <br />The Town of Lake City has an annual average temperature of about 380, <br />with an average January temperature of 180 and an average July temperature <br />of 580. Average annual precipitation in Lake City is 13.4 inches. <br />Climatic conditions in the upper drainage basin will differ significantly <br />from that of Lake City because of differences in elevation and <br />topography. Average annual precipitation in the upper Lake Fork and <br />Henson Creek Basins is 30.6 inches, of which about one-half falls from <br />October through April. The prevailing wind is from the west, but a wide <br />range of surface wind conditions exist as influenced by specific <br />topographic features. The area experiences occasional summer thunder- <br />storms which are primarily localized in individual basins. <br />111-1 <br />