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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 />3758 <br /> <br />Source <br /> <br />T~~~ <br />(tons/yr) <br /> <br />Percent of <br />Total ~ad <br /> <br />TOTAL <br /> <br />13,140 <br />1,131,500 <br />5,110 <br />554,800 <br />1,704,550 <br /> <br />0.8 <br />66.4 <br />0.3 <br />32.5 <br /> <br />Municipal <br />Irrigation <br />Mine Drainage <br />Runoff and Springs <br /> <br />The narrative discussion of the salt budget does not detail <br />the 13,000 tons attributed to municipal use of water. The <br />abandoned mines referred to in the budget, are located in the <br />headwaters of the Uncompahgre and Lake Fork drainages. All but <br />36,000 tons per year of the total yield attributed to irrigated <br />agriculture originate in the Lower Gunnison River Basin. <br /> <br />Mineral springs near Ouray and Ridgeway along the <br />Uncompahgre River account for a small percentage of salt loads <br />contributed by natural sources. Areas drained by the North Fork, <br />the uncompahgre, and the Lower Gunnison are underlain by soluble <br />formations and therefore account for the largest portion of the <br />550,000 tons per year attributed to natural runoff. The <br />headwaters of the Gunnison River, Tbmichi Creek, and Lake Fork <br />are underlain by more resistant rock and therefore yield high <br />quality runoff. <br /> <br />SCS-Final Report on the Lower Gunnison Salinity Control Study <br /> <br />The SCS presents an estimate of salt loading by source for <br />the Gunnison River Basin. Using measurements from the USGS <br />gaging station No. 09152500 - Gunnison River near Grand <br />Junction, the SCS estimated the average annual salt yield since <br /> <br />-26- <br />