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REP00387
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Entry Properties
Last modified
8/24/2016 11:29:18 PM
Creation date
11/26/2007 9:38:44 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981020
IBM Index Class Name
Report
Doc Date
3/14/2000
Doc Name
1999 ANNUAL HYDROLOGY REPORT
Annual Report Year
1999
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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• 1999 AHR McClave & Munger Canyon Mines Page 3 <br />Future Water Inflow <br />As the mine extends farther to the east and then north as shown in Figure 2.1.1 of the <br />permit application, it is possible that water will be encountered. Figure 4.2-3, of the <br />permit application, shows the saturated strata may again be encountered approximately <br />400 feet ahead of the east mains. Mining into the saturated coal bed will produce mine <br />inflows as the coal bed is dewatered. Experience gained by mining in the graben <br />indicates initial flow rates will be much greater than the flow rate after mining. If water is <br />once again encountered, its existence will be documented and detailed in future <br />reports. <br />As shown on Figure 4.2-3, the saturated strata appear to outcrop in the valley formed <br />by the north split of Munger Canyon. Since the strata in the area dip at four percent to <br />the northeast water may be infiltrating the seam along the valley bottom. Any water <br />infiltrating the strata at this location will flow down dip until the aquifer is totally saturated <br />unless there is an area where water may escape. The elevation of the saturated zone <br />would approximate the elevation of the outcrop (5,600 ft) if no water flows out of the <br />strata at a lower elevation. The elevation of the existing faces is approximately 5636 ft. <br />There are no known springs or seeps that would allow escape of the water from the <br />zone of saturation so it can be expected the coal seam will be saturated near the <br />outcrop elevation. <br />• MUNGER CANYON MINE <br />To date there has been no water encountered by this mine; therefore, there has been <br />no effect on the hydrologic regime of the area. The current mine workings are shown on <br />Figure 4. Table I documents that no water was used at the mine this year. <br />PRECIPITATION <br />Based upon Bureau of Land Management records from a rain gage in Ashford Canyon, <br />the 1999 water year experienced 16.02 inches of precipitation compared to average <br />precipitation of 19.03 inches. The rain gage is not located at the mine but about 3.5 <br />miles north at an elevation of 5895 feet compared with 5610 at the portals. The daily <br />rainfall record is detailed on Table 2. The greatest 24 hour precipitation event during <br />the year, 1.08 inches, occurred on May 3`d. Figure 2 presents a graphical comparison <br />of the 1999 total monthly precipitation and the average monthly precipitation for the <br />period 1977 through 1999. <br />EFFECT OF THE MINES ON THE EAST SALT CREEK REGIME <br />Surface Water <br />Due to the limited disturbance of the mines there is little chance any significant effect on <br />the quantity or quality of the surface waters near either mine sites has occurred. As the <br />Division notes in its approval package for the Munger Canyon Mine, the total area that <br />will be disturbed by both mine sites amounts to 0.12 percent of the area of the East Salt <br />Creek drainage basin above the mines. <br />
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