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represented between drill holes 05-01-0007 and OS-01-0006 in the Moffat ores. This <br />fault trends north-northwest across Section 25. Data indicating the extent and throw <br />of this fault have not been collected. <br />Cross Section D-0' <br />Cross section D-D' is shown in Exhibit 2.2-4. It is the southernmost of two east- <br />west trending cross sections that transect the Moffat area. This cross section <br />incorporates data from four drill holes (05-03-0004, 05-03-0005, 05-01-0009, 05-01- <br />0010). These cross sections show the lower coal-bearing member of the Williams <br />Fork Formation from below the Wadge coal to above the Lennox coal. As with the <br />cross sections described above, this section is comprised of interbedded sandstones <br />and shales thought to have been deposited near sea level and containing the Wadge <br />coal (which averages approximately 7 feet thickness), Wadge Rider coal, and Lennox <br />coal (3 feet thick where present). Cross section D-D' shows a portion of the eastern <br />limb of the Twentymile Pork Syncline. Dips are to the west and decrease in that <br />direction. <br />• <br />Cross Section E-E' <br />Cross section E-E' (Exhibit 2.2-5) is located on the West Ridge, down strike from <br />the Moffat ores. It incorporates dots from drill holes 05-01-0012 and 05-01-0013 as <br />well as from surface outcrops and shows an interval of the Williams Fork Formation <br />extending from below the Wadge coal to slightly above the Lennox coal. The <br />stratigraphic interval shown is similar to The same interval shown in cross sections <br />in the Moffat area to the north owing to the general homogeneity of the strata along <br />strike. The section consists of a sequence of interbedded sandstones and shales <br />containing the Wadge, Wadge Rider, and Lennox cools. The Wadge is approximately <br />II feet thick, but contains Ito 2 feet of shaly interburden not shown on the cross <br />section. The Wadge Rider coal is about 2 feet thick. <br />The structure shown on cross section E-E' is strongly influenced by the <br />orientation (Exibit 2.1-I) which is nearly parallel to the fold axis of The Twentymile <br />. Park Syncline and, hence, strike of the bedding. Although located on The western <br />limb of the Twentymile Park Syncline, the structure shown on this cross section <br />2.2-4 <br />