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A <br />i <br />Y[LLT yes[: BSlI MIlL. <br />BILL B[LLIS: I'• Blll Ballls with Yrliht ester O~ilneara !n Dmvae, <br />rpnsmtlni tM app licmt•• view polo[ I suppose. <br />1 Mve • ter cornta !o rb. rho vrltlm por!!on o[ tAL rill be <br />wbaittad prior to tM! septaaDer zI a..dun. but they rill not be mDeltbd <br />at thl• point, at tnls tit. <br />By corents an sort of pnanllesd in ear napmta and one is i <br />reuld like to point out !Mt in the LI9 In the rrltten part of 1! mere vu <br />reference made toe 100-toot head OiEEarmea Mtwm !M lover and upper <br />equi[er es dwlinabd m tM dlaires tMt yes Mve up !hare. to ey tinwLd[e <br />there i• no raaund 100-foot difference in the upper and lover aquifer by an <br />eetuQ resurernt. I !oink aayM !ha 100-foo! dlfterann of hwd <ar [[r • 56 <br />N <br />tv report tMt w subeltbd LMt Md • need rp for the upper and lover equl(er <br />b <br />and t! shoved • 100-foot di[brenes es • ruult of a eoapuler tun. But tM! <br />rw not m ¢tuel remrernt, Sn other wrda it ru •lply • run tMt snored <br />Aw •ieilai the heads wn takini into cmaideotim •11 tM aval4Dla <br />hydrmlle mfottatlm !n runnlni • trevlent cal Sbret ion for tM .ode] run. <br />So 1 don`t think then is • 100-foot Mad dl[farenu ruured, !o ry Ivwrbdis <br />m LM cite. <br />secondly. I mould like to wi{eat tMt rybe !Mn M eon eaphaais <br />placed on the (act [list tMre b nyanulee connect tan Mtwen tM upper eM <br />lows aquifers. Our .ode! tuna which wn done to show LM effect of puplr <br />!o deveter in order to hypotMLi<elly eiea the Bahobany oil shale zone and ell 55, <br /> 60 <br />the veils, nypothet leQ wlb In ens lover aqu i[er, ue ltq •I1 the Mareu car <br />data. tMt ie the USOS date foe the wart l<al laatoia end ao [ortn within the <br />strati{nphle nmttvs. W still then wn •bb !o dewGr tM ppae aquifer <br />In LM rdd run. se rlth thb srllabb lntorrtlm I think then b <br />A <br />9 <br />emaldsnbla wSBM [list indleetes tMra b • def lnlM hydraulic connection <br />ThL, Sn emnectim rlth tM eon malysis, mtwl visual mslpL at thaw <br />cone, Snd!<atlty rubble aelullm activity and so forth, adds alein to Lola 55, <br /> 6~ <br />Ides chat LMre is nyaraulic conneetlon. In adOltlon, than la tna actual <br />raaureatmt of tM heed 7n sot of the wlb that snow there is vary sell <br />Head G:f [.rmu in the order of to [eat or leis in sow of the wl4 [or the <br />upper and lover equi Gr. <br />lnothar eoaar:nt mould ba [list there sees to be • eons idenbL eaoun! <br />of espMLLs [or the catastrophic cmdlllm o[ turbulent [lot t( than wn <br />eollepr Ln the love pui[er. I lAint tMt, it is wrt of indicated roar <br />rybe this vu sorthini LMt ova likely to Mppen and would really cause a 56 <br />turbulent tlov and • eorLnilinb of these Mih saline veten of the lover <br />aquifer, or lover sine zone iota tM upper aquifer. But L think that Lhi• <br />rovld be, !E then vets collapse, this wind M on • very local aisle and I <br />cm't torrp Lola Deini transsltbd reedlly as turM len! 4or into !M upper <br />equ i[er. <br />7hosa rwld ba sv eosnenta. Thank You. <br />YILLY !W[: Jerry Daub. <br />JL[BT DADS: i wind like to CMnk yeu [or the oyyortunity to eorent <br />on !M daft [ls w !M Yel( [ldp Corpentlon .ins plan. f teal the BLB <br />aMUld M eoarnded m their efforts. <br />the tint Lwa I ratld lib to eddreu b tM presen! equlEer <br />eosaunieat ton Mtwen the ester Marini Aorixons above the Bahoiany Zone end <br />44, <br />ba low LM MMisny zone. site spat l[ic m the Yolf Bidio Coporat lon•• sodiw 55, <br />lrwa the lover Half o[ tM Manoimy Zone produces the rjorlty of !M valet 6Q~ <br />[or tM ao eallN lover equller. Shia Ms Men publlened In a [weber o[ <br />dlf Grmt pieces. One of which vu In tM Colorado school a[ Blnw' ell shah <br />