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the Grand -doDback to the north , up to the <br /> Creep area , along <br /> a r dis`ance of approxi^ately 75 miles . <br /> `Meeker area , 'Li near - <br /> Exhibit II_-C-1 presents contours on the top <br /> of the 3ollins sandstone based on drill hole data and the <br /> III-C-2 generalized <br /> d4 p eacured t -he OUtC'LOp L::hJ' bit <br /> y <br /> stratigraphic <br /> . owing the re_at_onship of the three sandstone <br /> section sh <br /> units to each other and to tilt jrOUild surface . the west <br /> side of Huntsman Ridge is controlled by the geologic s ructure <br /> of the dipping Mesaverde formation , with t^e three sandstone <br /> units renair_ir at appro::imately the same depth below the <br /> ground surface throughout the lease area . <br /> C . <br /> Ground water recharge , storage , movement <br /> and discharge <br /> Recharge to the °lesaverde in the Coal Basin <br /> (• t through the outcrop area east or <br /> area occurs principally <br /> Huntsman Ridge . Recharge will result from percolatica Of <br /> Water :ertiCal1v downward throu2h joint and E racEure systems <br /> in the overlying rock near th= area of outcrop . Exhibit <br /> 1C Cross Secticn , Coal Basin Vicinity , shows <br /> TiI-'-I , GeOlOg <br /> th- outcrop area of the three sandstone units , <br /> believed to <br /> be the primary aquifers in the the Mesaverde ror:natiOn_ . <br /> Recharge _s m-n <br /> i gl OUrino «Tinter =oi?tiis due <br /> to the _rosen , sno�rpack conditiohs at the higher elevations <br /> Snr4 thaw br_ngs a pe:10d <br /> �chere th_ `lesaverde outcrops . o <br /> recharge -arch saturated soil - conditions <br /> Of D_ r_:bable ma-xLmu l <br /> a id oe3'.0 stream rL`=10Li . 5,_Im: er and early .all precipitat3or_ <br />