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Creati area , along the Grand 00 -Zlback to the north , Lip <br /> to the <br /> distance of: approxi^ate=y 75 miles . <br /> '�iae'ter area , a Linear - <br /> 71_'-C-1 Presents Contours on the tO- <br /> of the 3011inS sandstone based on drill hole data and the <br /> III-C-2 generalized <br /> dip measured .nt the outcrop . T.xhibiL ! A is - <br /> r <br /> stratigraphic <br /> G.,�� gi se--zion showing the relations' QT the three sandstone <br /> uni. :S to each other and to the ground surface. The west <br /> side o= Huntsman Ridge is controlled by the geologic structure <br /> of the dapping Mesaverde formation , with the three sandstone <br /> units remaining at approximate_; the same depth below the <br /> ground surface throughout the lease area . <br /> C . Ground water recharge , storage , movement <br /> and dischar-le <br /> Recharge to the %lesaverde in the Coal Basin <br /> area occurs principally througil the outcrop area east or <br /> Huntsman Ridge . Recharge will result from percolation of <br /> water '%ertically downward through joint and fracture systems <br /> in the overlying rock near the area of outcrop . exhibit <br /> ll-�-� , Geologic Cross Sect4on Coal ilasin Vicinity , shows <br /> t, '? outcrop area of the three sandstone units , <br /> believed to <br /> De ' .,e primary aquifers in the the Mesaverde Tor^h ation . <br /> Recharge -s mi-hi-nal durin g LdiiitCY ? vih as die <br /> !1 <br /> tJ the r0'en , S^.Q�:p2Cl: CJ:lditiOIIS at t_i e 1g her EieVatiOP_S <br /> Mesaverde outcrops . S-ring thaw brings a period <br /> w:Lere one . <br /> Dr b3D1e maY.�m.um r2Cha ' 'J-:: h saturated soil conGiticns <br /> of <br /> a .d �caa stream ru^ori S,.;?imer and early -all precipitation <br /> 3 <br />