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~ ~ III IIIIIIIIIIIIIIII <br />STATE Or~ c:uLUxADO <br />MINED LAND RECLAMATION DIVISION <br />Department of Natural Resources <br />1313 Sherman SI., Room 215 <br />Denver, CO 80203 <br />303 866-3567 <br />Fn x: 303 832-8106 <br />DATE: September 18, 1992 <br />TO: Janet Binns <br />FROM: Larry Routten <br />RE: Fruita Hydrology Findings (C-81-015) <br />OF ~~[O <br />r~~~~ <br />f f <br />~ f876 ~ <br />Ray Romer. <br />Governor <br />Michael B. Long. <br />Division Director <br />I reviewed the hydrology information in the Fruita permit <br />application submitted by Greg Lewicki. I also relied on the <br />Division review of the reclamation plan submittal for the Fruita <br />Mine in 1989. That plan was essentially the same as the one we <br />have now, as far as the reclamation plan is concerned. I also <br />relied on baseline information in the old Dorchester application <br />for the Fruita Mine area mines (79-60). Finally, I spoke with Jim <br />Shite, who is a staff hydrologist for the Grand Junction District <br />Office of the BLM. <br />Based on my review of the items above, I wrote the hydrology <br />section and the PHC for the findings document. Some time soon, <br />Steve Wathen or Shawn Smith should amend the Division's CHIA to <br />include the findings on the Fruita Mine. <br />My conversation with the BLM hydrologist centered on the status of <br />Big Salt Wash. In summary, he said Big Salt Wash ran perennially <br />from 1981-1988 (he started monitoring it in 1981) above the Ruby <br />Lee Reservoir diversion. The surface flow has dried up every fall <br />since 1989. The numbers he gave me for the early 1980's indicated <br />peak flows of 28.6 cfs and low flows in the fall of less than 1 <br />cfs. <br />Ruby Lee Reservoir is in disrepair and is not capable of retaining <br />much water in its present state. Water quality just above the <br />diversion (in Big Salt Wash) is typified by specific conductivity <br />readings of around 560 umhos/cm at high flow and 1000-2000 at low <br />flow. <br />