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C-PIT Hydrogeologic Investigations <br />Technical Revision No. 8 <br />2: Site Analysis and Field Activities Mining Permit M-1977-208 <br />occurring in the access road ditch line west of the Canal and south of the B-Pit access bridge. This seepage <br />was routed to the 54-inch RCP discussed below in Section 2.2.3.2. <br />Inspection of the C-Pit highwall on August 22 revealed more seepage than had been observed on July 19. <br />Seepage into C-Pit was evident at the extreme southern comer of the pit, and at multiple locations along the <br />west side. Water was observed dripping from fractures in exposed portions of the Fort Hays Limestone, with <br />sufficient flow volume to accumulate and flow along the floor of the pit, creating a shallow pool of standing <br />water on the west side of C-Pit along the highwall. The previously noted vegetation on and along the base of <br />the highwall continues to thrive. See Photo No. 14 in Appendix C. <br />2.2.3.1 Fort Hays LimestonelBoulder Feeder Canal <br />An unmined portion of the Fort Hays Limestone is currently visible in the west wall of the Boulder Feeder <br />Canal at the northern end of the reach west of C-Pit immediately east of piezometer P-003. See Figure 2 and <br />Photo No. 4 in Appendix C. The bottom grade of the Canal and the limestone bed converge as the Canal <br />drops toward the south, indicating that at least in this northern area a block of residual limestone remains. <br />Presumably, the complete [Wining of all of the limestone in this azea was limited by the presence of the <br />original Feeder Canal as it turns to the north and west away from C-Pit. <br />The likely location of where the relocated Canal converges with and ties into the original canal alignment is <br />just north of the northernmost Brown and Caldwell flow gauging location, as shown on Figure 2. The <br />eastern wall of the Canal at this location appears to transition from a fill slope into the solid bedrock wall of <br />the original canal alignment, as shown by Photos No. 4 and 5 in Appendix C. The remnants of shotcrete, <br />now mostly eroded away, are still visible along the bottom of the fill that makes up the east wall in this <br />location, showing the intent to minimize seepage losses. This is the location of the "earth plug" that was <br />designed to seal off the relocated canal from the original alignment, as shown on the 1981 Plan and Profile <br />drawing in Appendix B. <br />2.2.3.2 B-Pit Drainage and Canal Seepage to D-Pit Pond, Southwest of C-Pit <br />Field inspection on May 3, 2007 confirmed the presence of a 54-inch diameter reinforced concrete pipe <br />(RCP) routing upland reclaimed B-Pit surface water drainage under the Boulder Feeder Canal into the pond <br />located southwest of C-Pit. The 1981 design drawings for the Boulder Feeder Canal Relocation Project <br />indicate that this culvert was designed to receive the drainage from the full extent (north-south) of the east <br />side of the reclaimed B-Pit area (approximately 2700 feet in length). Topographic mapping does not exist for <br />the reclaimed area west of the Canal, but the tributary area to this culvert is estimated to be approximately 25 <br />acres. <br />Field inspections in May and again in August indicated the presence of flowing water and water-born debris <br />at the inlet structure (west end) to this culvert, as well as standing water at the discharge end adjacent to the <br />pond. See Photos No. 15 to 19 in Appendix C. Most notably, the August 22, 2007 inspection indicated that <br />Canal seepage water was welling up in the ditch line on the west side of the canal in the fill section south of <br />the B-Pit bridge and entering the culvert (see Figure 2 and Photo 16). However, there was no evidence of <br />similar seepage through the east face of the embankment holding the Feeder Canal. <br />Comparison of the photos taken of the Southwest pond on May 3, 2007 and August 22, 2007 confirms that <br />' the water surface elevation of the pond has risen several feet during the summer irrigation season. See <br />Photos No. 18 and 19 in Appendix C. This is likely pnmarily due to seepage from the Boulder Feeder Canal <br />entering the pond as surface water via the 54-inch culvert, or as subsurface flow through the embankment <br />that holds the Canal in this area. <br />' 2-6 <br />Use of contents on this sheep is sublet[ to the hmeaeons specdied at the end of this document. <br />\`,BCDENODpmjectslDatalGENlCemex\TR-E1Reporeng\CEMEX Repor10B-31-07 tlw <br />