My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
GENERAL32987
DRMS
>
Back File Migration
>
General Documents
>
GENERAL32987
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 7:55:13 PM
Creation date
11/23/2007 7:28:57 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981044
IBM Index Class Name
General Documents
Doc Date
3/2/1984
Doc Name
Revised Proposed Decision & Findings of Compliance
Permit Index Doc Type
Findings
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
56
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
~J <br />-44- ~~ u Gnu ~° <br />The Trapper Mine may affect ground water quality through the discharge of <br />spoil waters to the first White sandstone. The first White sandstone is <br />exposed only in the upper portion of the Trapper Mine's highwall. Given the <br />low permeability of this unit, the quality and quantity impacts to the first <br />White sandstone will be confined to the areas adjacent to the underground <br />workings of the Eagle No. 9 Mine, the recharge areas excavated by the Trapper <br />Mine, and the post-mining highwall surface area exposed in the Trapper Mine. <br />Spoil waters would enter this aquifer only through the exposed highwall at the <br />Trapper Mine and only after spoil water levels have reached the exposed <br />highwall section. This impact is expected to be minor. The impacts to the <br />first White sandstone by the Eagle No. 9 Mine are not known. <br />Lenticular and interbedded sandstone and coal aquifers of the Upper Williams <br />Fork Formation may be impacted by the Eagle No. 5 and No. 9 Mines and Trapper <br />Mine. Both the quality and quantity of ground water in these localized <br />aquifers may be impacted. These aquifers are not put to beneficial use, but <br />they may support springs and seeps that have only minor discharge rates. <br />Therefore, the cumulative impacts will be minimal. <br />The Empire Energy and Trapper Mines may impact the quantity of ground water in <br />the Big Bottom alluvium. Both mines may deplete the quantity of water in the <br />alluvium of Big Bottom by reducing discharge of rock aquifers to thfs <br />alluvium. The Trapper Mine will deplete recharge waters of aquifers tributary <br />to the Big Bottom alluvium. The Empire Energy Eagle No. 9 Mine may divert <br />alluvial waters into underground mine workings through affected strata of the <br />Upper Williams Fork Formation. Analyses conducted by Empire Energy <br />Corporation on the impacts of mining in the Eagle No. 9 Mine predict no <br />significant depletions of ground water in the Big Bottom alluvium. The <br />combined impacts of the Eagle No. 9 and Trapper Mines may be significant. <br />The Trapper and Eagle Mines may impact the quality of ground water in the Big <br />Bottom alluvium. The Trapper Mine may impact the quality of water in the Big <br />Bottom alluvium through the discharge of spoils waters. This spoils water <br />discharge will be minor and use of alluvial ground water may not significantly <br />be damaged. The Eagle No. 9 Mine may impact the ground water quality of the <br />Big Bottom alluvium following mining. This mine may discharge mine waters <br />through interconnecting faults, fractures, and affected strata. The greater <br />subcrop area of the affected aquifers over the Eagle No. 9 Mine, and the <br />potential for greater frequency of fracturing over mine workings may result in <br />a more significant impact to the Big Bottom alluvial ground water quality from <br />the Eagle No. 9 Mine than the Trapper Mine. <br />Cumulative Surface Water Impacts <br />The projected surface water effects (7able I) for the Sugarloaf, Foidel Creek, <br />and Empire Energy Mines were added to the projected hydrologic effects from <br />the Kaman Tempo study. For the Foidel Creek Mine, the worst-case mine water <br />discharge was expected to be 1.95 cfs and have a maximum total dissolved <br />solids concentration of 800 mg/l. The long-term effect is to discharge 0.14 <br />cfs of affected ground water (3,200 mg/1) to the Fish Creek drainage. <br />
The URL can be used to link to this page
Your browser does not support the video tag.