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REV05117
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REV05117
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Entry Properties
Last modified
8/25/2016 1:03:29 AM
Creation date
11/21/2007 9:23:03 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Revision
Doc Date
5/17/2001
Doc Name
REVIEW CHECKLIST FOR ANNUAL HYDROLOGY REPORT AND ANNUAL RECLAMATION REPORT
Type & Sequence
TR88
Media Type
D
Archive
No
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<br />' <br />Requirement <br />Require- <br />ment <br />citation Require- <br />ment <br />complied <br />with ? lyes <br />I no) <br /> <br />Comment <br /> Potential aquifers. The post-mining uses of ground water in the <br /> permit area will be irrigation and livestock uses. Only the massive <br /> sandstone aquifers within the upper Williams Fork Formation at <br /> Trapper could reasonably be expected to yield enough high <br /> quality water to serve as a local supply source. These aquifers are <br /> [he Twenty Mile sandstone, 2"d White sandstone, and 3`d White <br /> sandstone. Coal aquifers in the area possess neither the <br /> deliverabili[y nor water quality to be considered for reliable water <br /> supplies. <br /> Twentymile Sandstone. The Twentymile Sandstone is the only <br /> regionally extensive aquifer in the vicinity of the Trapper Mine. It <br /> is several hundred feet deeper than [he deepest mining at Trapper <br /> and has shown no effect from Trapper's mining based on <br /> monitoring data from wells GF-1 and GD-1(2). <br /> 2°' White Sandstone (well P-5) and 3rd White Sandstones <br />GG. Prevention (well P-8). The 2"d and 3`d White Sandstones overlie the <br />of impacts to m <br />stratigraphic sequence being mined at Trapper. The 3 White has <br />ground <br />water that CDMG <br />regulation been cut by Trapper's pits; [he 2"d White crops out down-slope <br />adversel s from the pits. TDS concentrations in both of the White <br />y <br />impact the 4.05.1(2) yes Sandstones have increased over the past several years in the two <br />t <br />i <br />i d Trapper wells (P-5 and P-8) that monitor these aquifers in East <br />n <br />pos <br />m <br />ng an Pyea[t Gulch. <br />land use 4.05.11 <br />within the Suitability for postmining use of water from wells P-5 and P- <br />permit area 8. Prior to mining, high TDS levels caused electroconductivity <br /> values of water in both wells to exceed DMG's guidelines for <br /> irrigation water of I.0 mmhos/cm. Water from both wells, <br /> though, remains suitable for the lower level use of livestock and <br /> wildlife watering based on comparison with water quality <br /> suitability standards for domestic livestock issued by the State of <br /> Wyoming Department of Environmental Quality. (The Wyoming <br /> standards are used for comparison because Colorado has not <br /> issued suitability standards specifically for livestock or wildlife.) <br /> Trapper believes the TDS (and electroconductivity) will <br /> eventually subside, possibly hundreds of years after mining and <br /> reclamation, as discussed under Probable Hydrologic <br /> Consequences, Section 4.8.3 of the mining and reclamation <br /> permit. The suitability of Trapper's ground water for livestock and <br /> wildlife is expected [o continue into the future based on long-term <br /> trends in Trapper's water quality data. <br />Page 6 <br />
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