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Scoria: - 2.04.7 <br />North Fork of the Gunnison River - The North Fork drains an area of approximately 1,250 square <br />• miles, including the entire mine permit and adjacent areas. The headwaters of the North Fork are in <br />the Elk Mountains to the east of the Town of Somerset. The North Fork begins approximately six <br />miles east of Somerset where Anthracite Creek, Coal Creek, Deep Creek, and Muddy Creek join <br />together below Paonia Reservoir. Major tributaries to the North Fork include the following: <br />• Muddy Creek <br />• Deep Creek <br />• Anthracite Creek <br />• Coal Creek <br />• Thompson Creek <br />• Hubbard Creek <br />• Terror Creek <br />• Minnesota Creek <br />• Reynolds Creek <br />• Jay Creek <br />• Cottonwood Creek <br />The North Fork flows to the southwest for approximately 30 miles, where it joins the Gunnison River <br />southwest of the Town of Hotchkiss. The Gunnison River is, in turn, tributary to the Colorado <br />River. Elevations within the North Fork watershed range from approximately 12,000 feet for the <br />mountains to the east and south to 5,000 feet where it joins the Gunnison River. Total average <br />annual discharge of the North Fork is approximately 470,000 acre-feet, corresponding to a discharge <br />rate of approximately 650 cfs (USDA, 1962). The average annual discharge measured over a period of <br />60 years (1934 to 1994) at a USGS gauging station located approximately 2.3 miles east of the Town <br />of Somerset is 330,500 acre-feet, corresponding to a rate of approximately 450 cfs. The Colorado <br />Division of Water Resources has indicated that discharges from Paonia Reservoir will be used to <br />maintain minimum in-stream flows in the North Fork of 60 cfs. Variations in flow in the North Fork <br />are graphically illustrated by Figures 2.04.7-F9A and 2.04-F9B, Surface Water Flow Hydrographs - <br />North Fork of the Gunnison River <br />Perennial Drainages - Within the mine permit and adjacent areas, the only perennial drainage other <br />than the North Fork is Hubbard Creek, which drains an area of approximately 19 square miles <br />including the extreme western portion of the mine permit area. The headwaters of Hubbard Creek <br />are on the south slope of Grand Mesa approximately 12 miles north of the point where Hubbard <br />Creek joins the North Fork Dove Gulch, Sheep Corral Gulch, Freeman Gulch, and a number of <br />smaller unnamed ephemeral drainages are tributary to Hubbard Creek Hubbard Creek flows to the <br />southeast and joins the North Fork between the Towns of Somerset and Bowie near Juanita Junction. <br />Elevations in the Hubbard Creek watershed range from approximately 10,000 feet near its headwaters <br />to 5,800 feet where it joins the North Fork A peak flow, estimated at 600cfs, was documented for <br />Hubbard Creek in 1984. Nonnal flows range from minimal flow up to approximately 80cfs, with high <br />flows in the spring due to snowmen runoff. During much of the year, typical flows are in the range of <br />5 to 20 cfs as illustrated by Figures 2.04.7-F10A and 2.04-F10B, Surface Water Flow Hydrographs - <br />Hubbard Creek <br />Intermittent and Ephemeral Drainages - As previously noted, most of the drainages in the area exhibit <br />an intermittent or ephemeral flow pattern, with flow only in response to snowmen runoff or major <br />thunderstorms. While numerous small ephemeral drainages exist in the area, those intermittent or <br />ephemeral drainages which either carry significant flows or would potentially be impacted by mining <br />• operations are limited to (from east to west) Thompson Creek Hawk's Nest Creek Sanborn Creek <br />Elk Creek, and Bear Creek The following summarizes drainage characteristics for these drainages <br />and seasonal flow variations are graphically illustrated by Figures 2.04.7-F11A through 2.04.7-F11I, <br />Surface Water Flow Hydrographs - Intermittent and Ephemeral Drainages: <br />PR04 2.04-54 Revised August 2000