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2018-01-31_REPORT - C1981018 (2)
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2018-01-31_REPORT - C1981018 (2)
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Last modified
2/1/2018 9:50:03 AM
Creation date
2/1/2018 8:23:17 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Report
Doc Date
1/31/2018
Doc Name
Annual Hydrology Report
From
Blue Mountain Energy
To
DRMS
Annual Report Year
2016
Permit Index Doc Type
Hydrology Report
Email Name
JDM
DIH
Media Type
D
Archive
No
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13 <br /> <br />3.0 HYDROLOGY AND MINE DEVELOPMENT <br /> <br />This monitoring period from October 1, 2016 to September 30, 2017 provided the hydrologic <br />information necessary to assess the adequacy of monitoring program, the adequacy of the <br />mitigating measures designed to protect the hydrology, and identify and quantify impacts <br />that may have occurred during this period. <br /> <br />3.1 Mining Related Hydrologic Impacts <br /> <br />The only impacts identified to date include: <br /> <br /> Withdrawal of water for the mine from the lagoon adjacent to the White River thus <br />slightly reducing the flow in the White River. BME has legal right to this water. <br /> <br /> Discharge of storm water from pond DP-1 into Scullion Gulch, a White River tributary. <br />Discharges contained lower TSS than typical receiving stream flows during storm <br />events. <br /> <br /> Decline in piezometric level in wells in close proximity to mine workings. Holes that <br />were mined through have turned dry. <br /> <br /> Subsidence in Red Wash resulting in ponding of surface water. The ponds quickly fill <br />with clay and silt with Red Wash maintaining its original channel. <br /> <br /> Subsidence in Scullion Gulch resulted in no surface hydrologic consequences observed <br />to date. Not enough precipitation has occurred to truly test the system. Runoff was <br />rarely observed in the impacted sections of Scullion Gulch prior to mining. <br /> <br /> <br />3.2 Comparison of Projected Impacts with Observed Impacts <br /> <br />The comparisons of the projected impacts (probable hydrologic consequences) with the <br />observed impacts are discussed in the following. <br /> <br />The water withdrawal rate from the lagoon at the White River this reporting year was <br />estimated at 98,013,894 gallons or 301 acre-feet. This compares with a projected <br />withdrawal rate of 552 acre-feet per year at full production. <br /> <br />The decline in piezometric levels in bedrock zones "upper sandstone facies", "siltstone/coal <br />facies", and "lower sandstone facies" was anticipated as probable impacts as the result of
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