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PERMFILE134772
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PERMFILE134772
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Entry Properties
Last modified
8/24/2016 10:35:28 PM
Creation date
11/26/2007 2:41:30 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981039
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Doc Name
page II.A-1 through II.D-7c
Section_Exhibit Name
II. ENVIRONMENTAL RESOURCES
Media Type
D
Archive
No
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<br />Geology Report <br />Grassy Creek Coal Mine <br />The published source for the basic geology, the regional strati- <br />graphic column and coal sequences, the nomenclature and rock descriptions <br />is "Geology and Mineral Fuels of Parts of Routt and Moffat Counties, Colo- <br />rado, U.S.G.S. Bulletin 1027-D, by Bass, Ebv and Campbell, 1955." Additional <br />information was taken from the private source: Coal Resources of the Long <br />and Teiken Properties for Energy Fuels Corporation by Saunders Associates <br />Inc. Data was also gathered in the field and from drill hole logs. <br />Stratigraphy: <br />Rocks exposed in the Grassy Creek Mine Permit Area are part of a se- <br />quence of beds called the Iles Formation. The Iles with the conformable <br />overlying Williams Fork Formation makes up the Cretaceous Mesaverde group. <br />The Iles rests conformably on the Cretaceous Mancos shale, which does not <br />• crop out in the mine area. The Iles Formation is a sequence of rocks about <br />1,500 feet thick. For the purposes of. this report we have broken the Iles <br />into fouz map units. The lowermost is designated Kil on the Geology Map <br />and is the bottom 600 feet. The Tow Creek sandstone, although not exposed <br />in the mine area, is the basal unit of the Iles Formation. It is a massive, <br />cliff forming light brown sandstone, finegrained, well sorted, tightly cemented <br />and slightly calcareous. It is about 100 feet thick. The next major sand- <br />stone is the "double ledge forming" light gray and white sandstone occurring <br />about 400 feet or more above the base of the Iles. It usually forms two <br />prominent ledges. The No. 1 coal zone represents the basal coal zone of the <br />lower coal group and occurs just above the "double ledge forming" sandstone. <br />A coal zone has been encountered at this level in some of the deeper drill <br />holes. The interval between these two sandstones consists of beds of light-brown, <br />light-gray, and white sandstones interbedded with gray sandy shale. Kil rocks <br />aze exposed in the southeast portion of the permit azea. The top of this <br />map unit is between the No. 1 and No. 2 coals of the Lower Coal group. <br />The next map unit in ascending order is shown on the Geology Map as <br />Kit; it includes rocks between No. 1 and No. 3 coals which enclose the No. <br />II.D-2 <br />
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