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<br />. <br /> <br />decrease in the value of gas produced. The report is expected to be completed and published in April. <br /> <br />. <br /> <br />NEW COAL REPORTS: The CGS has published two new coal reports. <br /> <br />The first report, published in cooperation with the U.S. Department of Energy, is called "Demonstrated <br />Reserve Base for Coal in Colorado: the Somerset Coal Field" (Open File Report 98-5). The report <br />contains a new estimate of the Demonstrated Reserve Base (ORB) of the Somerset coal field in the <br />Piceance Basin in Gunnison County. The new ORB estimate is 3,180 million tons. The accessible reserve <br />base, which excludes coal restricted by land use or technological considerations, is estimated to be 2,400 <br />million tons. Estimated recoverable reserves are 1,280 million tons, about 40 percent of the ORB. <br /> <br />A second report, prepared in cooperation with the U.S. Geological Survey, also estimates the amount of <br />available coal in the Somerset quadrangle of the Piceance Basin ("Availability of Coal Resources in <br />Colorado: Somerset Quadrangle, West-Central Colorado," Resource Series 36). This report estimates the <br />available coal accessible for mine development under current regulatory, land use and technological <br />constraints. This study indicates that approximately 2,236 million short tons of the total 3,088 million <br />tons (about 75 percent) is available for development. Approximately 75 million tons of coal has been <br />mined in the area, and about 275 million tons o[coal has been lost through mining. Coal loss includes <br />coal unavailable to be mined due to previous mining of adjacent beds or mining of coal within the same <br />bed. The report also contains historical coal production data from the active and historic coal mines of <br />the region. <br /> <br />REPORT OFFERS INSIGHTS INTO MINING STRATEGIES: The CGS has released a new <br />bulletin on "Clastic Dikes Intruding Cretaceous Coals of Western Colorado," Bulletin 53. Studies of <br />clastic dikes are important because they can create severe problems in coal mines that may result in . <br />injury of mine workers and increased cost resulting in mine closure. Clastic dikes are often more <br />permeable than the surrounding coal beds and offer avenues for coal bed methane migration creating a <br />potential for fire and poisonous gas problems at the mine face. <br /> <br />Clastic dikes are formed in certain geological environments soon after the deposition of coal beds. The <br />dikes are composed of sand and other fine-grained material that were injected into the adjacent coal beds <br />effectively replacing the coal beds. Clastic dikes are widespread in western Colorado coal fields and are <br />particularly abundant in southern part ofthe Piceance Basin near the towns of Somerset and Palisade. <br /> <br />SEDGWICK COUNTY RESOURCE POTENTIAL: The CGS has released an evaluation of the <br />mineral and mineral fuel resource potential of the 32,550 acres of state mineral lands located in <br />Sedgwick County as part of its long-term evaluation of 4,000,000 acres of state lands administered by the <br />State Land Board. The CGS divided these lands into 30 individual tracts ranging in size from 480 acres <br />to 7,680 acres for evaluation purposes. This report includes a general summary of the geology and <br />mineral potential of Sedgwick County along with maps of state trust land locations, oil ands gas tests, <br />and industrial mineral prospects. The main body of the report is an evaluation of each individual tract. <br /> <br />NEW REPORT DESCRIBES COLORADO MINING DISTRICTS: The CGS has released a new <br />report on mineral deposits in Colorado, "Alkalic Igneous Rocks of Colorado and their Associated Ore <br />Deposits" (Resource Series 35). The report contains descriptions of the geological setting, geochemistry, <br />economic geology, exploration and production history, and a reference list of the major mining districts <br />in Colorado that are associated with alkalic igneous rocks. <br /> <br />2 <br /> <br />. <br />