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2011-04-08_PERMIT FILE - C1981012A (8)
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2011-04-08_PERMIT FILE - C1981012A (8)
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Last modified
8/24/2016 4:32:28 PM
Creation date
4/12/2011 12:45:03 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981012A
IBM Index Class Name
Permit File
Doc Date
4/8/2011
Section_Exhibit Name
SECTION 2.04 APPLICATION FOR PERMIT FOR SURFACE OR UNDERGROUND MINING ACTIVITIES
Media Type
D
Archive
Yes
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• Spring and Seep Survey <br />In response to Stipulation 7, a preliminary spring/seep <br />suzvey of the New Elk and Golden Eagle permit and adjacent areas <br />was conducted using aerial photographs. Twenty-two potential sites <br />were identified, as shown on Map e, Regional Hydrology. Known <br />springs and seeps previously identified by the USGS were first <br />examined for characteristic features which were then applied to the <br />area of interest. Primary selection criteria included anomalous <br />green vegetation and the presence of deciduous trees along drainage <br />bottoms. Features used for selection of individual sites are <br />summarized in Table 11, Preliminary Spring/Seep Survey Locations. <br />Stcck pond and windmill locations are also plotted on Map 8, <br />Regional Hydrology. <br />In response to Stipulation 8, WFC completed field <br />verification and sampling of springs or seeps on May 9 and 10, <br />. 1984. The area investigated was slightly larger than one mile <br />surrounding the New Elk and Golden Eagle permit boundaries. Twenty <br />springs or seeps were identified. Nine of these fall within one <br />mile of the permit boundaries and were monitored as per permit <br />requirements throughout the 1984 growing season. Parameters <br />measured included pH, flow, conductivity and temperature. The <br />resilts of this inventory are presented in Table 12, Results of <br />Field Spring and Seep Inventory. The locations are shown on Map 8, <br />Regional Hydrology. <br />For the purposes of this discussion no distinction is <br />mad~~ between springs or seeps. It appears however, most of the <br />wate=r encountered was a result of seepage. All of the water, with <br />the exception of No. 14 in Apache Canyon and springs in Santistevan <br />Can•ron, come from seepage from coal or the interfaces between coal <br />and shale or sandstone. No. 14 in Apache Canyon is a developed <br />spr:Lng, while Santistevan Canyon springs <br />• <br />2.04-25(a) (Revised 09/01/89) <br />(Revised 01/04/94) <br />
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