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G 2007 Suhs~dence an4 Geo'oq c F~tt!d Ohse <br />Box Canyon and South o` DwiCe Rfin~nq a•ea <br />xrtum of sandsame hcdrurk of the Oloo (1-rrk ~lemtxr ul the \lesaverdr Formation IFigure <br />I_I <br />z- t; <br />~. <br />~~ •~,y <br />. <br />~ R <br />• -• _ <br />.'- ~5~. _ <br />i <br />• ~`' -.-vim . <br />~~ -~ _ ;. . <br />`•-a _. <br />• ~ ` .. <br />`~c- <br />. ~ ~ ~i~ a, ~~i <br />t:~i ~ ~S; a!1. <br />~. ~ .~ <br />r ~~~` ` .. ..• ., <br />Fguro t 1 Lon9es[ -.. _. r•~n : aa;acenl to road n drlil Fgure 12 Soutaem end of longest rrack trentl abova <br />pae for MU4ti's 2'~d'1 Yin and 2t-3A Th<s cracks unm~ned ongn~a!~ panel 2t where d term~~na!es m <br />ce!!eved 'v he ih? result nl lateral sp•ead~ng oecause !t Sandstone oed•ock al the Oh!o Greek Pdembor of the <br />~; located above unm~r,ed ~ongwar: panel 21 9.lesaverde Formal!on <br />1 ~cron.l mark, trending roughly parallel to the first (NaU'li 1. appe:nn d+ hr s,(f.ct appn,cinrgeh <br />Icet to the .outhea~t Thi, mark ha, a ma~inunn utdth ul shout ~ inrhr. and .t masunum <br />uh>cn'rd depth of shout 'fret. <br />13atlt crack. appear :rt the narrim'r~t portion of the Ivp of U'cst Flatiron trhrre the ocerhurdcn <br />depth to the 13•tie:un m thi> area !. ahnW ?.I ~Ir feet chi. location i. ott:r the northrat corner of <br />umnmed !ongtcall panel '1 but ~+nhm'_lut (act of rftc unnuned coal hamrr pillar hehteen nunrd <br />InnLtcall panel '(t and unmmrd L+ngttall panel _I. 'fhe narroanr» of the nt.,a top and the <br />Inrauon oter :m unmincd longttall p;mrl ~upEctit~ that the raucr of Ihr crackm~' may hr lateral <br />.prrading due to gravitational tin'rrs tr.c.. hrng cchtrle traltir and or \II)1~' dell pad <br />~unxtructionl, flotteu•r• the pmcinutt to the nursing of h+ngttall panel ZI1, an.l the nnmmrd <br />831-032.7A0 tbngnr Wa:or Engmnea Inc. Page t9 <br />July 2007 <br />