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GENERAL34705
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Last modified
8/24/2016 7:56:02 PM
Creation date
11/23/2007 8:01:10 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981018
IBM Index Class Name
General Documents
Doc Date
4/3/1987
Doc Name
MEMO COAL LEASE APPLICATION C-44693 WESTERN FUEL UTAH INC DRAFT ENVIRONMENTAL ANALYSIS & MAXIMIUM EC
From
DIVISION OF LOCAL GOVERNMENT
To
STATE AGENCY REVIEWERS
Permit Index Doc Type
GENERAL CORRESPONDENCE
Media Type
D
Archive
No
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<br />in the valleys and relatively level uplands to 50 percent or more along <br />the sideslopes of major drainages. <br />The area is characterized by mild summers and cold winters, and has a low <br />average annual amount of precipitation. Seasonal temperatures can be <br />extreme, ranging from 108°F in the summer to -33°F in the winter. Average <br />summer temperatures range from 95°F in the daytime to 50°F at night. <br />Average winter temperatures are 29°F. Precipitation averages from 8-1/2 <br />to 9 inches annually, with the majority of it occurring in Late :summer and <br />early fall. Average winter snow accumulation is usually less: than 12 <br />inches and generally does not remain on the ground very long. Southern <br />exposures may remain free of snow for most of the year. Th.e growing <br />season is short, usually less than 100 days, and occurs from late Hay to <br />mid-September. <br />The Cretaceous Hesaverde Group in northwestern Colorado has been divided <br />into two formations: the lower Iles Formation and the upper Williams Fork <br />Formation, which are separated by the Trout Creek Sandstone. The Williams <br />Fork Formation is further divided into Upper and Lower members. The Lower <br />Williams Fork Member contains coal seams A through J, of which the B and D <br />seams are or will be recovered within the Deserado Mine LHU. <br />The dip of the Hesaverde Group within the general area is cont.colled by <br />the asymmetric Red Wash Syncline, which strikes northwest-southeast. Dips <br />vary from 1 degrees to the northeast in the southern part of the LHU, to <br />horizontal at the synclinal axis, to as much as 70 degrees to the <br />southwest on the north flank of the syncline. The coal and sandstone beds <br />outcrop along this steep northern flank. <br />Minerals <br />Coal <br />The coal deposits of the Prairie Dog Lease Tract are located in the <br />Lower White River coal Eield, within the late Cretaceous Hesaverde <br />Group. Coal seams of interest occur within the main coal member of <br />the Williams Fork Formation (seams A thru J). <br />Only coal contained in the B and D seams is of adequate thickness to <br />be considered minable. Exploration in the area indicated the <br />presence of splits and partings in both the B and D seams including a <br />major parting in the D seam. The parting in the D seam reduces the <br />minable seam thickness from 8 to 9 1/2 feet to 3 or 4 feet. The <br />location of the parting in the D seam is a physical boundary which <br />limits the recovery of D seam coal in the area. <br />The thin interburden between the D seam •and B seam (less than 10 feet <br />in some areas) would preclude mining in both the B and overlying D <br />seams. The D seam has a higher clean coal reserve potential than <br />does the B seam. Therefore, mining of the D seam is a priority and 8 <br />seam coal is considered nonrecoverable. <br />Oil and Gas <br />All federal oil and gas minerals have been leased in this area. The <br />tract is covered by two oil and gas leases. The leases are C-37363 <br /> <br />6 <br />
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