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REV95044
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REV95044
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Entry Properties
Last modified
8/25/2016 3:20:13 AM
Creation date
11/21/2007 11:45:28 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Revision
Doc Date
6/14/2002
Doc Name
Proposed Decision Letter & Form, (Enclosure-Review Check List ARR & AHR)
From
DMG
To
Trapper Mining Inc
Type & Sequence
TR90
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 />/ nol <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 /> the Twenty Mile sandstone, 2"d White sandstone, and 3rd White <br /> sandstone. Coal aquifers in the area possess neither [he <br /> deliverability nor water quality to be considered for reliable water <br /> supplies. <br /> Twentymile Sandstone. The Twen[ymile Sandstone is the only <br /> regionally extensive aquifer in the vicinity of the Trapper Mine. It <br /> is several hundred feet deeper than the 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"d White Sandstone (well P-5) and 3'd White Sandstones <br />W. Prevention <br />of impacts to ,~ m <br />(well P-8). The 2 and 3 White Sandstones overlie the <br />d <br />ground CDMG stratigraphic sequence being minad at Trapper. The 3` <br />White has <br />water that regulation been cut by Trapper's pits; the 2 White crops out down-slope <br />adversely s from the pits. TDS concentrations in both of the White <br />impact the 4.05.1(2) Yes Sandstones have increased over the past several years in the two <br />postmining and Trapper wells (P-5 and P-8) that monitor these aquifers in East <br />land use 4.05.11 Pyeatt Gulch. <br />within the <br />permit area <br />Suitability for postmining use of water from wells P-5 and P- <br /> 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 1.0 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 to continue into the future based on long-term <br /> trends in Trapper's water quality data. <br />Page 5 <br />
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