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2020-10-27_GENERAL DOCUMENTS - C1981035
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2020-10-27_GENERAL DOCUMENTS - C1981035
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Last modified
10/29/2020 1:41:04 PM
Creation date
10/29/2020 1:05:13 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981035
IBM Index Class Name
General Documents
Doc Date
10/27/2020
Doc Name Note
For PR10
Doc Name
Proposed Decision and Findings of Compliance
From
DRMS
To
GCC Energy, LLC
Permit Index Doc Type
Findings
Email Name
JHB
THM
Media Type
D
Archive
No
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discharge) and at upstream and downstream locations on Hay Gulch Ditch. <br />(4.05.13 (2)): <br />H. Transfer of Wells <br />There are no wells proposed to be transferred. <br />I. Discharge of Water into an Underground Mine <br />The permittee does not propose to discharge water into the underground workings. <br />J. Stream Buffer Zones <br />There are no surface disturbances proposed with this permit revision. No stream <br />buffer zone delineation is necessary. <br />K. Probable Hydrologic Consequences <br />The probable hydrologic consequence is described in the permit application <br />package and is described here with respect to the entire permit, not just specific to <br />PR10 parcels: <br />Ground Water Effects <br />The ground water -bearing units having the greatest potential to be affected by <br />mining at the King I and 11 Mines are the Hay Gulch alluvium, the Cliff <br />House Sandstone, and the Menefee formation. (GCC has stated that the <br />Point Lookout Sandstone is well beyond the area of influence of the mines <br />because it is approximately 250 feet stratigraphically below the workings. <br />Monitoring data show no impacts from mining at the King I and 11 Mines.). <br />Hay Gulch Alluvium - The Hay Gulch alluvium has been monitored in the <br />Wiltse well, downstream from the west sediment pond at the King I Mine. <br />GCC also monitors alluvial water quality in a well down -gradient of King II. <br />Monitoring data indicate no significant mining impacts to this unit. <br />Cliff House Sandstone - It appears unlikely that the King I and 11 Mines will <br />fill with water after mining is finished. With the exception of one inflow <br />event, the mine workings of the King I Mine have been dry. Both mines <br />appear to underlie the updip, unsaturated portion of the Cliff House <br />Sandstone. Impermeable shale and siltstone of the Menefee formation <br />underlie the workings, and also are unlikely inflow sources for the workings. <br />If the King I Mine or King 1I Mine workings were to eventually fill with water, <br />it seems unlikely the water could be transmitted from the workings to the Cliff <br />13 <br />
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