Laserfiche WebLink
<br />O ,1',~ ~ t,J <br />U~!)i:.. <br /> <br />Range % <br /> <br />Ave. (%) <br /> <br />Fi:~ed carbon <br />volatiles <br />Water <br />Ash <br />Sulfur <br /> <br />72,34-87.46 <br />6.59-14,19 <br />0,81-1.86 <br />3,50-19.72 <br />0.51-0.76 <br /> <br />83.17 <br />8.70 <br />1. 30 <br />6.83 <br />0.61 <br /> <br />coa12~fthin the Study Area has been mapped but not extensively prospected. <br />Lee -- stated that 2 to 5 feet thick coals had been reported in the <br />Oh-Be-Joyful Valley, but he could not confirm this because the prospect" <br />were inaccessible at the time of his examination. <br /> <br />The potential for economic coal in the Study Area is unknown pending <br />further detailed investigation to determine number, thickness, and <br />rank of the beds. The thinness of the beds within Oh-Be-Joyful, the <br />difficulty of access, the presence of ample reserves outside the Study <br />Area, and the current lack of interest in area coals all are against <br />exploitation of this coal resource at this time. However, anthracite <br />coal can be mined in relatively thin seams because of its high unit <br />value. Adequate data is not yet available to assess the coal resource <br />in the Study Area (see Figure III-II). <br /> <br />3. Oil and Gas <br /> <br />Interest in oil and ':Jas exploration within the Study Area has been <br />indicated. Brooks Exploration, Inc. holds four federal oil and gas <br />lease.;; overlying the Study Area. Conversations with Brooks I personnel <br />in 19"79 indicated th(~ir belief that there is potential for a structural <br />trap for natural gas in the Dakota Sindstone at the crest of the Oh- <br />Be-Joyful anticline. While admittin~ that this possibility was <br />specu.Lative, they eXf,ressed interest in drilling an exploratory hole <br />just east of the Study Area along Oh-Be-Joyful Creek. As of the <br />present date, they have not submitte,:i a drilling application to the <br />U .5. {~eological Survey. <br /> <br />The same high temperatures resulting from igneous intrusions in and <br />near the Study Area, which were responsible for the metallic mineral <br />deposits and anthracitization of coal, also caused the area to have <br />low potential for oil and possibly for natural gas. Baking of the <br />rocks tended to decreas2l~orosity as well as drive off the volatile <br />hydrocarbons. Spencer -- showed this area to be of low oil and gas <br />potential on his map of western C~~7rado. Further discussions with <br />Spencer (u.S. Geological Survey) -- elicited his belief that the <br />western one-third of the study area has no oil or gas potential. He <br /> <br />20/ Lee, W.T., 1912, Coal Fields of the Grand Mesa and West Elk Mountains, <br />Colorado; U,S.G,S. Bull, 510, p. 237, <br /> <br />~/ , . <br />Spencer, C.W., 1980, 'Map Showing Oil and Gas I~tentlal of the <br />San Juan, Gunnison, Grand Mesa, and Uncompahgr< National Forests <br />in Colorado, U.S.G.S. Map prepared for U.S. Fo:est Service/USDA. <br /> <br />?:Y <br /> <br />Spencer, C.W., Personal Communication March 25 <br />March 31, 1981, U.S, GeOlogical Survey, Denvel <br /> <br />1981 and <br />Federal Center. <br /> <br />37 <br />