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1994-12-29_GENERAL DOCUMENTS - C1980007
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1994-12-29_GENERAL DOCUMENTS - C1980007
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Last modified
2/6/2021 10:59:04 PM
Creation date
11/23/2007 11:13:31 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980007
IBM Index Class Name
General Documents
Doc Date
12/29/1994
Doc Name
Decision Doc Federal Lease
Permit Index Doc Type
Other Permits
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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Upper Cretaceous Mesaverde Formation, which is overlain by the <br /> early Tertiary Wasatch Formation and underlain by the Upper <br /> • Cretaceous Mancos Shale. The lease application is for the Upper <br /> B seam of the Mesaverde Formation; the seam ranges in thickness <br /> from 30 to 20 feet. The combined analysis of the coal seam is 7% <br /> to 8t moisture, 10% to 11% ash, 0.5t to 0. 6% sulfur and 11,000 to <br /> 12, 000 Btu's per pound. The tract contains an estimated 26.5 <br /> million tons of in-place B coal seam reserves. The total minable <br /> reserves are approximately 19 million tons of which 10 million <br /> tons are mie. �uu uwo-BF� <br /> Outcropping on the tract is the Mesaverde Formation and <br /> Quaternary deposits. The Quaternary deposits are an unsorted <br /> mixture of soil and rock formed by various mass-wasting processes <br /> as landslides, earth flows, soil creep and debris avalanches. <br /> They also include river deposits. and slope colluvium as well as <br /> Quaternary unconsolidated deposits derived from the Wasatch <br /> Formation. <br /> The coal bearing sedimentary strata of the Mesaverde Formation is <br /> relatively flat lying with a regional dip of 3.5 degrees to the <br /> north-northeast. Local dips of up to 7.0 degrees are also found. <br /> The USGS Geologic Map C-115 shows that there may be three or four <br /> faults crossing the Jumbo Mountain Tract. There is no surface <br /> evidence of faults due to the colluvial deposits and surficial <br /> cover. The overburden overlying the B seam in the application <br /> area ranges from zero feet at the outcrop to approximately 1,200 <br /> feet. <br /> • The potential for the discovery of conventional resources of oil <br /> and gas under the leased area is very slight. Dry wells have <br /> been drilled to the Dakota Sandstone a few miles to the southwest <br /> and to the northwest of the permit area. There is a possibility <br /> of finding methane in the coal seams. There are no oil and gas <br /> leases located on or near the application area. <br /> B. vegetation <br /> The vegetation of the application lands is comprised of scrub oak <br /> and sagebrush with an understory of grasses. There are stands of <br /> aspen and Engelmann spruce-Douglas fir on the upper north facing <br /> slopes. The grasses and mountain shrubs that have been <br /> identified are western wheatgrass, Indian ricegrass,. oak brush, <br /> serviceberry, chokecherry, sagebrush, mountain brome and <br /> junegrass. <br /> C. Land Use <br /> The topography is characterized as steep north facing slopes on <br /> the southeastern margin of Grand Mesa. The application lands are <br /> approximately one mile south of the North Fork of the Gunnison <br /> River at elevations ranging from 6,600 feet to 8,100 feet above <br /> sea level. The application lands support two principal land <br /> • uses, wildlife use and livestock grazing. <br /> There are no rights-of-way located on the application lands. <br /> Page 6 <br />
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