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11 <br />11 <br />DAUB 8 ASSOCIATES ._ ATE <br />B <br />A <br /> <br />CONSULTING GEOLOGISTS ; <br /> <br />e <br />- ~±~1~~~~•+'`~;,;.w'.Y~+•., ,, <br />198050UTH BROADWAY <br />~~' .si ' „~ ~r^.t <br />' _ <br /> <br />,. <br />1~~:.~1~ <br />TING <br />GEOLOCs <br />ONSUL <br />~ _ <br /> <br />y.Ai~.~^ <br />Ip80 BOUTH BROADWAY <br />•.. <br />r <br />rr . <br />s~e+..~ ~V.'.,'.•••~}~'~ma.?t{r_.. .• <br />~v <br />\ ~ GRA NO JUNCTION. CO B1507~4593 <br />.~~L <br />: ':':.':.. <br />; .. <br />, -.. <br />.r y,~:~ <br />..;.~; e. .J. "' <br />.~` <br />~~~/".. <br />.. ... m.:.•'7ir <br />~~~ <br />'~~e. <br />~S <br />i ~ <br />i <br />~` <br />~ <br />"~~~ ' <br />" GRAND JUNCTION, CO e1503~9597 <br />~_l.l.v...: -.._` <br />•• <br /> <br />~ <br />.. <br />. <br />. <br />. <br />, <br />1]071 ]Ai~098A <br />, <br />. <br />, <br />. <br />:.5 <br />" <br />r t <br />~~ <br />- <br />i <br />_. .~ „ . . <br />. <br />. WOd1 Pn L096. <br />?{s ! Xeedip{ Prjh_ 1 Sent. ! Cotenant! Pj: ! 9elQipj Pij6_ 1 §spt_ Q Co!lent! <br /> •ubJact hme been dlmeuaaed In • ]-12 3.4.2 3 2 *heee two equlfer• ere {caeca lly <br /> <br />vevar premented at the 18th ~ <br />•epereted by the yplaC Mehm{any <br /> Colo redo School of Nine• Oil 8hele some... <br /> Sympoe lum entitled ^Detealed <br /> Lf tholo{ic, Roek Guellty, end DT <br /> Rrdrmim{ic Oete Prom Four Brt 11 I4~1 3-12 3.4.2 3 3 iha appar Mnhojeny zoos i• <br /> Hole• im the Centre] Plceenee probably a 1!!112 semi-contlnln{ <br /> J <br />Creek Be•in, Rio Blanco Coumty layer between the Fro equlfera, <br /> Colorado." which allows •ome communicet Imo <br /> between the twa equifer• thro ujh <br /> •ec on dory poroa ity developed in <br />1-8 1.3.2 1 4 Although the leeched lptg[=!] 1o1pt9a 439!x14414! S!l44i!! amd <br /> 6elmr [he !1441! Meho{any zone trecture• im the ypplj Meho{aey 60~ <br /> eomte ins ei{n ificent qua nt iti am ... zom e. 61 <br /> 44 <br /> the leeched Lome re Pe r• to the <br />44 <br />N entire section from the 3-12 1.4.2 ] 4 Beesuae of Ib hl{h kero pm <br /> diesolutlom eurfece to the top of content, the rock le lame <br />v the R-8 zone Imclutl lnf ell of the brltele; therefore, the upp4C <br /> Meho/any some. Mehojeoy Wane 1• lame •uacept lb la <br /> ten frecturin{ then 1• either the <br /> ioeg eo44l191mj tg! upper or lorer <br />1-9 3.4.1.1 7 13 ... from the drelmmja •reu .j4g_y equifere. <br /> the !caeca .,. <br /> 60 <br /> 9-12 3.4.2 3 5 le some vleee• im the beaiR the <br />1-9 1 4 2 Xeed lnj should Da Blj14lf1 4!!9[ Mehojeoy none 1• ... <br /> §9[432( helor Ground water. <br />3-9 3.d.2 1 1 o! the DSmte evd Cresn River 9-12 1.4.2 4 2 Tht• •eam• that the renter level of <br /> Pormatione. @prelsr. 4!!4!44 46! a roll in the rater beerin6 zones <br /> A§C lod34! 19!999 34 tg! per4g r111 be ht{her than the Q9l9 4( <br /> £9!4[!1 el£alpee C[aeg !lS19 4822! 4g! copf343R{ 1![![. <br /> eju lfe[! fra p[al99tlj 3R <br /> £x!lB43£lf149 !94 £x9!144!44 4Rl. Am t! t• mor •teted Iv the drat[ <br /> 8IS it i• em lecorrect defleitiem. <br />3-9 3.4.2 2 2 7haae equlfer• ere hydrmul lcelly (Qr 60 <br /> connected with ome soother. ih! 3-12 3.4.2 4 6 The preaemea of 43!!4144349 <br /> 4943f9r! £94 hGt g9 £4!l149Eld !! fSlf lral, fault in{ !pd frecturlmi <br /> !eplryte S9!![S?3[!. le confln in{ lsye ra that .., !glCe <br /> tga[a i! my 9bypolpe! of <br /> d39lelutlog fefture9a I[e<ty[19{ <br />3-11 i1{ure 3-2 The toD of the lower aquifer egd teultZpjy glgd differlpfa! !r} <br /> should be extended up lento the }!!! lhgm rgar! there 1! l34or qr <br /> ml ddle of the Naho{emy coma. 3!!1{9341£994 LC9£S4C9lA flR143Bf <br /> !94 411911943x8 19944!9! 1848149 <br />7 R <br />