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Show F NJINERAUmTIQNfPERSISTS TDWTH HE i Hf I'Wlicf tlmt the rich, surface Idepofcils frorn. which consider ln(s of oro lmvelbeeri thken,6n tlio oloroptabi the Kttk&f'fotf tlio Silyor Wave properties in :Amoricnn! tr&yon, vould be found to perpist to depth, is justified EScnUtrikc in thoHoldon tuhneljiccoi'ding to W. C. HJkjSf itent 6. Keyck. Mr. Brown and Mi-Kcycs, both PH!L ir stockholders tlio ?T-Minlng corapany'..vl8lted KpnerllC8 Sunday,,, which c,orked under a Jtog-jeira KTbr tie" American Leaning Co.. " ' fjrich catena bouiJero,hay6 Hntatfcd from the bed of a K Which makes iU. bed In an KL'tenUflsunro. Co'nsldorablo KTilii) lccn snipped from' sstenuf aults which woro, run &ftrtnatkn to explore tho many Ejt of mineralisation. No Kim exploration of. thoVorma-Eftth;" thoVorma-Eftth;" been done 'fenUl Hfe Ktt'lMilaff company, With Ci Kttin as manngor, acquired' a Ektfet property and tartcd the tficnneU f Euieek. In this, lower tunnel, Efiu'be used "boUi -to explore KlrmtioD and to furnish n'menns Hurting Into the mUKMrteto SSTnpV'tho 'vwIoub oupor-H oupor-H takings, a strike was made ijaMtheBiLsouthweBt .-'flKfure. RlBikH the strike In the lowest Knb doubly Important .Is the. S'ltf'thls' same fissure, 185 &re the Holdcn tunnol.a, largo BtTnilllng ore. from olght to Kj feel wide and averaging ten Kividth, has been oxposcd In No. ifribttlon Trntlstcnt. , .. . Hfeaifsurc.i where ,, Intersected In Hlwer MfOTkliiKs hU a jolnt .In Kiconed ralso fofty-flvo foot abovo Klildw tunnel h4! the same KkW of mineralization, the same Bid.dli as In tho upper adits. Kution to thcao conditions', which MfiJMohetUwyry? HknolbCn Dcrslots to even great-Hth, great-Hth, tho ore fs going BtroiiM--Irt direction, according to Mr. Key. K. Mr. Ferlln now plans to con-Hit con-Hit too raise upward until a con. Hon for ventilation Is made with an Htbtt. At tho same time, drifting H tt'e mineralization to tho south. Ht sbng the atrllcc of Uio fissure C b expedited . Hjr drifting along tlio flssuro a dls-Im dls-Im of twenty feet Into tho Echo Kin, thtneo Into tlio Live Ynnkeo His dls'cnce of 200 foot, tho quart-Hipwphvry quart-Hipwphvry fonnatlon will bo left Htitoluble llmestono ontorcd. Slnco Hi niserillzatlon has been so rich H $ porphyry and tho quartzlto, It I .Hmsoaablo to bcllovo, nccordtng to Hr. Forlln'i theory, that largo bod-Hi bod-Hi depo3lU should bo opened up in H"'atl' limestone. H theory most fuvored now ex HMDS trc ccnocls of tho rich gal. Bu bouldera found In tho creek bed H 't was fonnerly a bedded de-H,!xccrdlns de-H,!xccrdlns to Mr. Browno. Tlie H" tut-west fault displaced tills 4 dropping th0 formation to tho HNtl cf the fault downward a consid-Hru consid-Hru slunco, Kroslon of tho Umo-Hie Umo-Hie bed left at or near tho surface Hi the north of tho fault brought th'o H11 harvest of boulders down Into Bitreara bed. With the geological Ptturod m u result of tlio rccont Pfkt MploTitlon work done from the H"1 tunnel nnd from cstlmnten of r IJIcknoc of tho ah'nle and llnto H1' Wcl r.co overlaid th0 aunrt-H aunrt-H ' u,' north of tlio onst.west P"!!, Mr, Forlln has computed tho ""mm displacement of tho llmo "'from 300 to 400 feet. Ex- o'Mloa i this point will result in H' finiJI,J of this rich' bed, It Is H" Wuourjr Imporlnnt H Ai'Jther recent discovery which Hal?tthen Mr Korlln'n ,hcory ,n re to the BcolnRy of the proporty "'"e mrdo In tho Qlobo tunnel, .'"ch la bfelnt; run by John Cleghorn. H.? turn61' driven to prospect to ,omh ef the east.wost fault, tho toV0rmallon ,rnvo,,!,(,,l by tho snmo ,., ,UothweHt flrguru r.n that In u. lho ore ,,aH bcon opened In li,mlp,ilcCR ,)y 'bo Amorlcnn Lorh- MmPaiy. a bedded doponlt which ? hleh 'n Iron and hIhiwr good In. 'itr! v r' allvcr cnd lead' haB bc0" 'vBtfivi 'n'il('atlon ot tho oxlstcnco 'ftoft . J wero 3l"'1 "I'Parent In Uio J5 of Ul' "rift in a wtnzo sunk ttp- dlH mlnornllatlon can Imj seoii ln- ir-wlllch 0,low ,lmt ",o bod la Hr n '" extent, according to "rowie. A8 HOon (m th. d,p ot tho Wed h dotormincd, Mr. CTeghom will utart en uprnise from a lower tunnol'.on tho Olobo. claim to open up tho IhtcrBectloa.Jof'itnls bed with tbV northoasUaouthwost fhouro, which' Js thought "to bo tho. Mecca of th'o'0nrfch-ing th'o'0nrfch-ing solutions. Tho American Leasing company's water ;ccn(!cntrjatlon mill is "now opl' eratlnif. undor "the Buporvislon of O. E, Adams; nccordlng to Mr. Kcycs, Now that lli'o owi can bo run out throushT'tht Holdou tunnel Into tho mill, h0 operations ol tlr0 mill rthould be.roducedf to" a mlnlmlim cost arid, should bo steady until winter soU In. |