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section A-A'. Cross section B-B' incorporates data from five drill holes (OS-01-0003, <br />05-01-0005, 05-O1-0006, 05-01-0008, 05-01-0010). This cross section shows the <br />Williams Fork Formation from below the Wolfcreek coal fo above the Lennox and in <br />most respects displays geology quite similar to that shown in A-A'. <br />The Wolfcreek is represented in cross section B-B' by four coals with the second <br />from the top being very shaly, close to a carbonaceous shale. The interburden and <br />interval below the Wolfcreek is composed of interbedded sandstone and shale, with <br />sandstone dominant. Above the Wolfcreek coals shale is more prominent to within 40 <br />feet of the Wadge where a coarsening upward sequence is evident. The Wadge and <br />Wadge Rider coals are continuous from drill hole 05-01-0005 through 05-01-0010 and <br />average approximately 5.5 and 1.5 feet in thickness respectively. The interval above <br />the Wadge is a sequence of interbedded sandstones and shales with sandstone <br />dominant. The Lennox coal contained in this section averages 4 feet in thickness. <br />w <br />The structure shown in cross section B-B' is, like A-A', a brood, open, synclinal <br />fold which is, in part, due to the oblique line of cross section relative to the strike <br />of the bedding. An inferred fault is shown between drill holes 05-01-0003 and 05-01- <br />0005. It trends in a northwestern direction and, at this location, has approximately <br />25 feet of throw. <br />• Cross Section C-C' <br />Cross section C-C' is shown in Exhibit 2.2-3. It trends east-west across the <br />Moffat area and extends westward across Trout Creek. Data from drill holes 05-03- <br />0002, 05-03-0003, OS-01-0007 and 05-01-0006 were used to construct the cross <br />section. The section shown is the Williams Fork Formation from below the Wadge <br />coal to above the Lennox coal. The interval below the Wadge is composed of <br />interbedded sandstones and shale. Examination of data from nearby drill holes, not <br />shown on the cross section, indicate that the Wadge coal rests directly upon <br />sandstone in places and shale in other places. The Wadge coal averages 6.5 feet in <br />thickness and the Wadge Rider coal approximately 2 feet across the section. <br />The interval above the Wadge and Wadge Rider coals consists of interbedded <br />sandstone and shale with sandstone dominant. On the east side of Trout Creek the <br />Lennox coal has been removed by erosion. <br />Cross section C-C' shows a portion of the eastern limb of the Twentymile Pork <br />Syncline. Dips decrease wesiword, toward the fold axis. One inferred fault is <br />2.2-3 <br />