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Mayo and Associates, LC <br />Figure 1 Maximum extent of Cretaceous Interior Seaway. The Uinta and Piceance <br />Basins are located in eastern Utah and western Colorado, respectively. <br />Modilied after Williams and Stelck,1975. <br /> <br /> <br />,: <br />r, <br />:, <br />~~ <br />~x ~, ~~, <br />~ <br />t <br />t <br />y$ <br />} ~`i <br />ru ~ y <br />1 +t <br />L <br />~Su~aena] Plam Deposits - <br />(MesaverdeGrtiup).:z ~. ~. r ,.: <br />.; <br />:~ - <br />f M ~ ~p f ~~ <br />~: Tyy ~. <br />li <br />-„} <br />S 4, <br />l ~~ ~X ~~\~ <br />~ <br />° O 1 <br />° <br />4 <br />{ ~ 4 ., ~ J <br />~ <br />A <br />,, , x 1S_i <br />C <br />U <br />~ m <br />~° <br />~ <br />~ <br />~ <br />a po <br />.: <br />v „A <br />x ,~S <br />'i ~, ";,` DS <br />Y' <br />v <br />r <br />o ~' <br />v <br />g" ~~~`0 oD Silts[one and Shale <br />'°°~`~ (Marcos Shale) <br />r~'i~ <br />r t~ o <br />; <br />r° <br />`° <br />~ <br />A}",VrAV ~ o <br />° <br />y~~; <br /> <br />0 25 50 Miles <br />I <br />o ao so x,n <br />Figure 2 Schematic diagram of western shoreline of the Cretaceous Interior <br />Seaway. The shoreline locally transgressed and regressed in response to <br />sea level changes and had an overall eastward migration across the Uinta <br />Basin into the Piceance Basin during Cretaceous time, <br />Evaluation of Potential Groundwater Inflows 13 February 24, 2004 <br />Associated with E Seam Mining, <br />West Elk Mine, Somerset, Colorado <br />