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<br />Section II - Understanding the Water Supply <br /> <br />The Gunnison River Basin <br /> <br />The Gunnison River originates where the <br />East and Taylor Rivers join at Almont, <br />Colorado in Gunnison County. From that <br />point, the Gunnison flows 25 miles to Blue <br />Mesa Reservoir, the largest and most <br />upstream of the three reservoirs comprising <br />the Aspinall Unit. Blue Mesa Reservoir <br />releases water into Morrow Point Reservoir <br />which discharges into Crystal Reservoir. <br />From Crystal Reservoir, the Gunnison flows <br />approximately 2 miles to the Gunnison Tunnel <br />(irrigation diversion for the Uncompahgre <br />Project), located just upstream from the Black <br />Canyon of the Gunnison National Monument <br />(Monument). From the Gunnison Tunnel and <br />through the Monument and the Gunnison <br />Gorge, the river tlows for 28.9 miles to the <br />confluence with the North Fork. It then <br />travels 74,9 river miles to its confluence with <br />the Colorado River at Grand Junction. <br /> <br />A TT" Geological S"rvey streamflo'" <br />gaging station is located near the upstream <br />boundary of the Monument (0.4 miles <br />downstream from Gunnison Tunnel). This <br />gage is considered the measurement point <br />when water deliveries under the proposed <br />contract to the Monument are discussed. The <br />area of the Gunnison River watershed is 3,965 <br />square miles at this point. Historical flows <br />have averaged 1,384 cubic feet per second <br />(cfs) and have ranged from 19,000 cfs (1921) <br />to no flow (1936, 1949, and 1950). Another <br />important gaging location is at Whitewater <br />Colorado, located 8 miles upstream from the <br />Colorado River confluence. At this point the <br />Gunnison River drains 7,928 square miles. <br />Average flows are approximately 2,600 cfs <br />and extremes have ranged from 35,700 cfs <br />(1920) to i06 cfs (1934). <br /> <br />Even with the Aspinall Unit, there is <br />considerable variability in Gunnison River <br />flows from year to year because of variable <br />amounts of snowfall during winter months. <br />For example, flows through the Monument <br />averaged 396 cfs during the drought year of <br />1977, and 2,943 cfs during the high water <br />year of 1984. Flows in June 1984 averaged <br />over 8,000 cfs through the Monument. <br />Because of the high natural variability in the <br />water supply, agencies are examining the <br />concept of providing a variable amount of <br />water to the Monument from the Aspinall <br />Unit. <br /> <br />Water Rights <br /> <br />Gunnison River water use began in the <br />19th century with establishment of numerous <br />irrigation water rights by individuals, <br />organizations, and government agencies. A <br />water right is a real property right which <br />allows the holder to use a certain portion of <br />the river's water for beneficial purposes, <br />Beneficial uses include irrigation, drinking <br />water, industrial uses, recreation, and fish and <br />wildlife. <br /> <br />Water is not always physically present to <br />meet the needs of water rights. Water rights <br />are administered by the State Engineer's office <br />in accordance with the date they were <br />recognized in the adjudication system (their <br />seniority). There are more than 5,000 direct <br />diversion decrees that have been perfected and <br />are presently in use on the Gunnison River <br />and its tributaries upstream from Delta. <br />Significant senior diversion rights, established <br />between 1900 and 1910, include the Gunnison <br />Tunnel of the Uncompahgre Project (1,300 <br />cfs) and the Redlands Diversion (750 cfs). <br /> <br />4 <br />