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2013-04-11_REVISION - C1981018
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2013-04-11_REVISION - C1981018
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Entry Properties
Last modified
8/24/2016 5:19:27 PM
Creation date
4/11/2013 12:57:25 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
Revision
Doc Date
4/11/2013
Doc Name
Letter to SHPO (Emailed) & Attachment
From
DRMS
To
SHPO
Type & Sequence
PR8
Email Name
ZTT
DIH
Media Type
D
Archive
No
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through J. Deserado Mine's zone of interest is the B -Seam located in the Lower Williams Fork <br />Formation of the Mesaverde Group. Although there are several smaller coal seams, the B -Seam <br />is the only mineable in the proposed LBA. It is divided into two separate splits, the Upper and <br />the Lower B -Seam with a parting that ranges from 1 to 3 feet. The estimated coal reserve base is <br />approximately 27 million tons (both splits of the B -Seam) and the estimated mineable reserve is <br />21.3 million tons (lower B- Seam). The majority of mining is projected to occur in the lower B- <br />Seam. <br />The LBA is located in an area identified in the 1997 White River ROD /RMP as acceptable for <br />further consideration for coal leasing and as having high potential for oil and gas occurrence. An <br />isolated 40 acre parcel of Federal oil and gas lease COC73884 encumbers the NWNW, Section <br />21, Township 3 North, Range 101 West, 6th Principal Meridian of the LBA. No producing or <br />abandoned oil and gas wells are within the LBA according to the Colorado Oil and Gas <br />Conservation Commission (COGCC) database. A mining claim for locatable minerals adjoins <br />the LBA on the northern border of the NE Section 20, Township 3 North, Range 101 West 6"' <br />Principal Meridian. <br />Environmental Consequences of the Proposed Action: <br />Direct and Indirect Effects: The Deserado Mine Plan predicts maximum subsidence <br />ranging from 4.2 feet to 7.7 feet in the longwall panels. The amount of subsidence is determined <br />by the depth of overburden and the height of the coal seam mined. Typically, shallow <br />overburden and higher mining height create greater surface expression of subsidence. Results <br />from monitoring of surface subsidence from longwall mining at the Deserado Mine are below the <br />predicted maximum vertical subsidence. Ninety -five to 98 percent of the subsidence resulting <br />from longwall mining occurs during active mining. Long -term subsidence hazards are not <br />expected with longwall mining since such hazards are manifested in a fairly short time. <br />Subsidence above previously mined longwall panels along Rio Blanco County (RBC) roads 65 <br />and 96 and the mine's power line has not interfered with usage of the roads or power line. <br />BME's approved Deserado Mine Plan contains subsidence monitoring and mitigation. Quarterly <br />subsidence reports are submitted to the Division of Reclamation Mining and Safety. Areas and <br />structures that could be affected by subsidence include tributaries to Red Wash, RBC roads 65 <br />and 73, Moffat County (MC) Road 61, clean coal slot storage, rail load out, associated power <br />lines, and coal refuse disposal area. Given the past experience with subsidence at the mine site, <br />subsidence is not expected to adversely affect these areas or structures. <br />Removal of the LBA coal would deplete the underground B -Seam recoverable resources and <br />allow the maximum economic recovery of the underground coal resources in the LBA and the <br />Deserado Mine area. MSHA regulations requires a coal barrier of not less than 300 feet in <br />diameter around oil and gas wells which could limit the recovery of coal resources in the 40 acre <br />parcel of oil and gas lease COC73884. However, it is unlikely mining would occur below the <br />majority of parcel of COC73884 due to the increase in thickness of the partings within the B- <br />Seam. Leasing and developing the coal resources would have little to no effect on the mining <br />claims north of the LBA. <br />Cumulative Effects: Cumulative effects of longwall subsidence would be minimal to the <br />geologic and mineral resources in the Red Wash and Scullion Gulch watersheds. <br />DOI- BLM -CO- 110 - 2012 - 0023 -EA 34 <br />
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