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• 4. The small water production noted in WSC 06 is most probably coming <br />from the fine grained clastic sequence between the 'C' seam and <br />upper 'B' seam. <br />5. The only open fracture system noted in this sequence of exploratory <br />holes was at a depth of 393 to 395 feet in the WSC U6 at a point 6 <br />feet above the upper 'B' seam, I suggest that this fracture system is <br />the source of the water produced during testing of this hole. <br />This infers that any water production from the llesaverde sequence above or <br />below the 'E' seam will be limited in quantity and highly localized. Such pro- <br />duction should be predictable from surface indications of joints, fracture systems <br />and drainage patterns. <br />• <br />Note: Probably should have map tying surface drainage patterns to in-mine <br />seeps and water-wet areas. <br />• <br />