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~ Mayo and Associates, LC <br />Figure 1 Maximum extent of Cretaceous Interior Seaway. The Uinta and Piceance Basin <br />aze located in eastern Utah and western Colorado, respectively. Modified after <br />I Williams and Stelck, 1975 ............................................................................... 13 <br />Figure 2 Schematic diagram of western shoreline of the Cretaceous Interior Seaway. <br />The shoreline locally transgressed and regressed in response to sea level <br />changes and had an overall eastwazd migration across the Uinta Basin into the <br />Piceance Basin during Cretaceous time ........................................................... 13 <br />Figure 3 Spatial and temporal variations of selected basal marine shoreface sands of the <br />Mesaverde Group between the Uinta and Piceance Basins, Utah and Colorado, <br />respectively. Modified after A. Papp, Personal Communication .................... 15 <br />Figure 4 Depositional environments and internal structure of sandstone bodies in the <br />upper Mancos Shale and lower Mesaverde Group rocks. Sand is white, coal is <br />black, and siltlshale is gray. Modified after Galloway and Hobday, 1983..... 16 <br />Figure 5 Schematic diagram of water bearing sandstone bodies in the basal sand and <br />I lower sandstone channels of the Mesaverde Group ......................................... 20 <br />Figure 6 Fault related damage zone groundwater inflow in Soldier Creek Mine 1990- <br />1993. Modified after Mayo and Associates, 1996a ........................................ 24 <br />f Figure 7 Generalized stratigraphic column of bedrock formations and coal seams in the <br />vicinity of Energy West and Co-Op mines, Wasatch Plateau, Utah ................ 26 <br />' Figure 8 Map of sandstone channels in the PacificCorp Trail Mountain Mine. Modified <br />after Mayo and Associates, 2001 ..................................................................... 28 <br />Figure 9 Hydrographs of selected in-mine roof drips associated with faults in the Deer <br />• Creek Mine. Modified after Mayo and Associates, 2001 ............................... 30 <br />Figure 10--Locations of mines, faults, and Star Point Sandstone outcrops,-Wasatch - - - -- - - - <br />Plateau, Utah .................................................................................................... 32 <br />Figure 11 Dischazge hydrographs of sandstone channel inflows from the Blind Canyon <br />seam mine roof to the Beaz Cariyon Mine - Co-Op Mine. Modified after Mayo <br />and Associates, 1999a ...................................................................................... 42 <br />Figure 12 Stratigraphic column of bedrock units in the vicinity of West Elk Mine, <br />Somerset, CoIorado .......................................................................................... 50 <br />Figure 13 Map of existing and proposed mine workings, surface and in-mine water <br />sampling locations, faults, and B Seam structure ............................................ 52 <br />Figure 14 Hydrograph of 1996 B East Mains (BEM) fault dischazge from the B East <br />Mains and 24 HG XC 17-21, West Ells Mine .................................................. 53 <br />Figure 15 Hydrograph of 2003 B East Mains fault discharge from 22HG XC 21 E3, <br />West Elk Mine .................................................................................................. 54 <br />Figure 16 Dischazge hydrograph of groundwater flow from the 14SEHG fault, West Elk <br />Mine ................................................................................................................. 55 <br />Figure 17 Map of proposed E Seam workings and E Seam structures and tectonic faults. <br />.......................................................................................................................... 58 <br />~• <br />Evaluation of Potential Groundwater Inflows 3 February 24, 2004 <br />Associated with E Seam Mining, <br />West Elk Mine, Somerset, Colorado <br />