Show EASTERN UPLIFT TO CHANGE CHANG MAP Tintic T nt c Standard and Centennial Conditions Identical Says Miner Minert t existing today In n the thet ther r Pr t Stand ad I property are areal areL L 1 al wit with lobe existing In hi the Cen Ceni J 1 i E mine at corresponding i j Is la th i made yesterday ay by 0 F But Busch Bil dJ a well known mining I ai n su urt of or the tho contention cont that i Ig g people e d not y yet st belie begin to the otance ot of th tb geological that the of oft t Anti district exactly i the thi r uplift in tn which have made m in iH he notel OddS p dUc rS of o the thep q p wit l their contributions to the r v ts metallic wealth aggregating 1 Qu U Iny iny years year ago aero said he be such emt r geologists s as George Otis Smith U g P Wart Vann n To Tower er Jr and Professor i 1 FraTs k Emmons of the United l survey In th Issue tsue of ot oft ott t fc CM folio by the govern r point d 11 out the existence of ot the tbt them C m r r uplift u lIft ut f th same fame to j as ab that of the western watern up 1 id d that thaL it due dUO to precisely the aue the thu porphyry intrusions t j 4 the tha fissuring In the lime limer r C ji and d wi U w re the magma permit t 0 he flow t f mineral gase gases an and waters r i the lim in m search of af aff f it h and for tor r tp t 11 purpose of ot exchange L i I deposition dc Is Worthy of Investigation t a S H it j nOl floe rf to conclude from mm I v 1 tact faca at a hald that the east side 1 t i t was worthy worth of thor as us to the existence of ot ofIn Ii i in quantities Aa As long IonS ai 81 ago one Leatham l i v ud tn tIr a 1 considerable lon body bod of ot ott at t w d and started to build F r fo it Iter r at i Ih n But Rut with the failure t it t ventur to bt he carried through the theT T i h for OH an was dropped and aU all these The Tle wl wi m mcH f n of Tintic ltv have failed to toi tolt i lt ue th Ign ns of or nature and the tho in inu 11 u held I n it to hI ther One On can ac no acL L lor fr th Ui r apathy i only by believing they w not of or the sure aure signs of ot r 1 i l 1 existing ther or that they dis dist disa t I tI a the t fd of the most eminent c it J only within the last lut two years of 4 t n ming n f i of r experience have un n m n fl arnst the development of lJ ido J pro i But some of the ther 10 i r 1 the toil tnt i ut nt t are aie engaged In conduct rn in that side aide which are arez z 2 it ig the TI v S tur tor a greater Tintic The Theu 1 u llla a th the Standard the East i 1 l evel i the Provo Prove 1 r t L Lily i nd Ed d other estates are lie being E C i d v th East Tintic De Do Deal Deill Dom al m nt already In the list listi I 1 ii i ready to follow at an early date Il LL j others well on ni the way I Standards Surface Showing i i 1 yr or T the purpose e of ot making an aft intelli r T n between tw the eastern tern and andT T m rn uplifts ot of the th 1 I r I tune mo pei I at the Tintic Standard on C cC c c f K it surface showing and its t u provides the most con COD conis CODIS is exan e on the eastern zone Its Ite how L i is not surpassed ii by that mine nIl u thu th west side not even een by bythe byI I f the Mammoth which is is conceded e lV the ingest surface showing of in i i Tintic The Standard out outi I i I us i an alC a hundred feet In Inand and i i i I knowing the tie ABC A B C iff g gi 1 l r will at once recognize recognise i dS n the a i ants of ot vast ore oodles bodies 1 it ached lid ild t partially i comi n explorations to date i an timed dined shaft Hi 4 4 teet feet deep i I uit ut 9 9 i rd L a t of drifts and crosscuts it t and about feet iii j i to an I cn on tv the A new Tew it cal shaft equipped with m y is now completed to a aT ar T r out feet below tha th present t l vel This ih 13 is to be l sunk to the ther theT I r T J leI led 1 where the mineral zone zoneY zoner Y r furth r explored EXior d L botto lottoR u ut of 1 the inclined shaft so f may r judged at this thiB time is In r tue t e of or the mineral zone Y v i 1 northerly and southerly t Cl i 1 the j ro Crosscuts to the c ard i Id d west on OT that level evel have hae explored rory orv abo about it II 8 feet wide disclosing V nf ot if leached ore bodies or ori orr orr r i ments in la the tho dolomite lime thirty c j i feet tet wide with still an anC anC r C C r 1 v t feet wide vide uncut but showing on ont ont t All of or this is 01 oi the west westi t ll i the property others on the east s B me no fet ft wide remain to be cut cuta O a L own cown on the thu surface Bottom of Leached Zone Near I L rh h ore In small t 3 s h l u been disclosed on this level but bat bate bute I Ie e 3 J i Jt t that depth it shows the action of J 7 ng Ekg Th tact tut however that rich c i 3 lJJ a any is found indicates t i t ot nt depth th bottom of ot the leached r c hag bas been IK arly reached and taken c w uh tn the circumstance that t a I c t there are aTe absolute ab T 1 i u n ual vit jU those thoe existing In m the thel l 1 Eu mint mine same Game depth 1 r 13 3 to the conclusion that C TO tv 3 i feet additional depth b and i as s rich ore bodies will be bec c leered In Tintic flutie Standard as have bave LI en c n fl found in ill the western weste uplift of ot L k limestone V t personal per nal of ot the work 1 2 If c i i by y any i l tun mr r will enable him to tor tor r at OTH ene cr the Immense quantities 1 v of or the eastern astern mineral minerai in a n Tintic H fI tip will realize that by T 4 of nf tl tle e eti ie fissuring and min miner er cr 7 lion ion It Is s a 11 question only of ot rea rca e r v 1 t additional depth d to uncover the theFt theer er Ft r ore bodies s ever known t S w I ic l I confidently predict that within t i t t four months by reason of the thet theL L t tact tant ore disclosures to be made a ar ar ar r rk k l d change chanse in the map of the Tintic L s r t will have taken place |