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j <br />EK r. <br />EXHIBIT 7 o 0 R? Q4 ... ` ,.« .p ROM o 40 <br />>>.?..? ? ?1 <br />Ed, <br />c ?, \ WADGE BOTTOM UCTURE <br />Ei Arm we faW_SOft [or•tass <br />- ? Atm we Ind_wt <br />f . <br />L.Gm we!ral wt tonto?rs 4l• r. ti'.•, - _ - \ ??? I / . - ,' !? ?i.r - .. _ _ 'J: <br />8 rJ <br />yl G <br />- ®e?qe 6ev._300f! I,r / ErY .,aY+ - _ _ <br />AOSMknft -- ' <br />LA <br />RGE NW TRENDING <br />4 <br />° s REGIONAL FAULT " <br />? i - 6 w?m_cdzs_dp ?zzsrn r -\ <br />40' DISPLACEMENT ON FAULT OLD WEST MINE <br />-75 DEGREE T' <br />DIP ANGLE PHOTO POINT (EXHIBIT 8) <br />M. IC#t c"ldm \ j <br />? I - 0 crtr !dt dlRm `? - - -- - - + // '?/??r r I * n <br />• 1 4T <br />T^ ??'*' /; J?_ -'•;,?;!,. 90' DISPLACEMENT ON FAULT <br />ISO <br />c ak„ - R ? a a. _ e t o w ^e - ! - - arwx - Las- <br />1-9W v :mSQ 4;,L cxr <br />PERRY SPRINGS ARE IMMEDIATELY UP-DIP OF THE OLD WEST LW MINE. THE NEW WEST <br />MINE IS DOWN DIP OF THAT AREA. A LARGE NW TRENDING REGIONAL FAULT SEPARATES <br />BOTH MINES FROM A MAJORITY OF ALL THE SPRINGS TO THE SOUTH.