Show SILVER MOUNTAIN 7 the big mining districts ot of utah geologically Con considered eldered what is found within a radius of forty miles of salt lake city tile the cottonwoods Cotton woods west mountain ophir camp floyd and other dis distrusts Di tracts struts TUB THI COTTON cottonwoods WOODS thou those districts commence about fourteen full ail a oath loath of 0 belt lake lily city and TO kra pit noted in the highest portion of the wasatch rugo range bool about to I 1 alloco tt foot above the cr tho the mes c little cottonwood cin can you yoa lit il a gorge fifteen anitila long big canyon splits itoda I 1 lato uto UTI several toyoni or forks forra aad ail Is 1 in antho the mila mein twitty miles long th later aft bof of the woo s cut cat through a gorud tutu giu of ext extending eDding vor with a height cf 2000 gag and nd easterly for ow over ton mate this ihla franits rl ohp out oat or of aad al above a mats dian of tod and orys tallia 0 rocks eastward nl up the ond wo we observe ft a mass of couie costs d la IQ places ra io ia rock cOD talLing 19 with biller sod 1 AD all if my mry overlying lylo lying title graD gridlio lio wo we ob serve or a mass of schist 1400 feet in ID thick 0 dirt dris out east northeast and than by nul gradually north aboia the johiel wo we about BUO ft feet of crystal UDO lido lim hatt than ZO fort or bortni nalla lf sandstone then 40 fiet feel god nil this to io 1600 foot of ni si larian larlan jwo la in this linio lime belt tho bet d boil QI donson amily sonah sta bar ar and nj titola Mort ilog bur vallejo foil fall moon mann north biar kromi emms ca C od oportia ortia mond tearoom of vi alusa Vl usa and dd many liny mothr mines twigged swigged uil swig ged rd we observe Virol nl mountain MonD tAin r duag bif I 1 i a a garmond xia macj s of frd area lid ito oat or of the iho in altti which nj bad ablio thIld ar are bighley iman imp wah copper I 1 ay toiuo mia u it I 1 from the first mu mass ot at bratto la in both blib points point and to site bibid diw of gradito the tb upper pin part of tit clr in ID a north and DI bouth fort fork the pr atno of isi ax boulders the spore of break braung for ng through ui ili I 1 gina ginaine ite bud uj the greally nl mass itself brim ballif tuil lull eore draino that abo mo if i of at A ago iba abo abw 1 on oa ilu code balb of jim tit alio 0 ir acts ol at abo a conti cond uro are clear ir illa grated by b it dumiot cumin friction rn khurt laj nd rl allies law aliro 0 aple ili 9 2 W I 1 at ab ve the place whence i ibo be mae was torn trite abr tho the OVA yon tun up op anal goodfe golch unit lit 1 obory ob tt ory rv tile on the el do of abo ito emma thes wo we bire been two upheavals Dp Leml the iho first from tuo the west throw iu aut tho second tun rise through the ut of cf tact rock fee 0 o winner boil has bu only by fault lug las said aj mm maps to a slight libbl nuat client K vt HILL resti zag the vision roe train from alta alt to the bo amma mine wo we observe min of grafto gr Dito which fact taken tog ulber with the other nu maisco of ind loilo boyone dispute that the 11 cromite under all probability via fo va abola bola of balb dulrich dul the formation lorm xion belong to la the iho raim palm toto age for all 1 that the she aspeti becom of algio and other 1 forand donad la in the ibo belld it almo me of tho the la in loil fail ity fly belong to tho the abio still the abla action to which the rock has bu brn been sab leal veri verifies verities ties the a J of 1 RILL oa the outside of davenport mal the bo silea cand upheaval bee ban rimmed a series nines i I 1 of roas which cintrin Cin tsin Q no DO quartzite but bot ocly daly celil and copper overlying acl binl hi aiono alon 0 so fall of the upheaval abr pirl of hill ia by several dykes ot of a 11 bud ar d 0 nan trap n hardly b oi cu a iha lime jimo tiro tire of those dikes pu pas thin the vial Lity of tho the victoria mouth the upper dyko dyke ratio mod north abia and croaa tho the diedo by the le DayeD dayenport port mace ahalt oa abo cud c f i arld forms a synclinal curve I 1 li i the ridge nd to with has short distance of ib the mini any little anolar fault bulcoa on tho do othorn ank of pla falsely corro ponda with to 00 northern fault which anted tho the abdoo of atad the rock to 1 to a short horl distance dita oc of the break aloot f tor tries idiot the foregoing conclusions jt it to ii that trait ober acter 0 of f the iho cottonwood oros will choa d through the of the try rooks emma hill shows land od g loot land to ia do lomot and port oil I 1 ts with gledic in the lh glad hate la A tho the granito we groob ob orre arte of oLivar galliza sua iron cyri exiles of md and carbon ltd blue of 01 copp r I 1 of oi aarde iro that there wro aro exceptions io ia tazi td on oil amm hill halt the ore oro all fit east aud and west line IQ tho boror or aoi IQ in or belt the deposits appear be tion or moncil on 00 su bode nature his bu etro to IQ oil buo ouo 6 of her culloo h atiq conseco the diffuse diG brout 1 flaa aria so 0 o to ran in imil join to oh oath other As to form to all al a rocilar af itna telo which it r a not CIOL ily by Is olor clog a ob it will bo be seen that tho the oro ora d doss cot occupy ft a real vola ila uro ore but bat that the cuta kraL havo hairs in ia all ant an every open reaco of the i a atan A need rock reacted oa do iho 1110 rimo the iho a cirlO ir bousted DiU of ahmo hmo sod od moll mig bulat bud la in its ibl alacia its akl we flud it kt braat pra at anti aa II 11 oa 00 of the notion to iou to ti ia ill iho 0 flagstaff an I 1 bout i star comes noro abo will wall r rook ook Is ii in ia the line of ct rise fric tare lure apparently talice w out oa by sad boulders show tho the clail of uk ui nora reagents kupcin the same lvery mall all beani of vela vein matter should bo be fat followed up u sett it invariably leabo ic to ore ire and aj way dry iril to As aj I 1 indicated above tb oro ore 9 IQ ii rock of abo districts wad ad beside beide that lo in thi taj grabits gra olto oits an of the be oro ora boli beds shows that th thy 1 wore formed to io the groat up oata 1 by 0 from below ke aa 0 a odo w wt 00 oberto tta tho action of toe igneous rocks rock moro fcc goal trip keep dykes the to lowar w bojia 0 ao flad find in 10 clavio with th chono ova dykes largo of ferrugi una ores some of these byks wm in to bea bo of f olis azaad alrada ally to the sod kod then dui dumpor por k chort ia abo liine ud oil aau 1 I lie oro olto are all 11 II of f a more moio orlgia than ibo dalci but bat all are more or im fall wis with h the same pseudo action hn has removed Ted tho the porphyry and od the iho iamo line with wah ore or me task it is rm abat the tat anallan of ore deposits was iru the second kry ary of alo igneous eruptions the tillo of oc these deposit befog IQ ia moat cur carlos in conformity with tho the coarse of b the iho ill lost the ibo emma mm davenport DaT ul and other bills with mth such aoh dykes nod tk it I 1 TO amy Y suggestive to id sup in indio pio loso aho dyko dyke loitra lu ill the ol of the iho oro ore clop rit more go 0 o as tto tio traced ol at tho the dyko dyke material passing ts ta the north of the emmi emma oro ora deposit dep odit is a deeply marked fult fault which identical fult fault has aten truid ia tho the wn straat the lb illinois tunnel where what in a 1 lovea intal wes u ma by abo north war bur 0 t a lert length ilith or 0 over SOU fa 1 tod slid a share hf took look 30 90 feol feet below the ibo lull to a ext ailua urao the th of tho the wells of uld said fault shows a throw from above down the ibo hanal bidelot log wall of ilo iho fiall fault so no that the abo biblo ca uld d M r of f the iho oro deposit must bo be looked axi le tor for ikler on oa the hong cinelu li nelu itic will wall of goad ij fit bialt sit tho the thrower throw of this hill fall 1 more by a aa o un ard plainly to ID a 6 certain part of the lm lin me nik mine miao tito fault has bu crushed a great aruty of limm limo loBO otone la ia tho the lower list rl of t abo or oro a all oh ambr 4 bat wl fell part I 1 la fillan there with end k ID n time this abl it mass hu bee thit mitt it 16 appears a its first eight ight I 1 tibo ft a floor u ad J Plate 17 I ablo ton depth of cf 23 25 lift la ia the staff 10 foot la in tile iho bou ill atar tr 90 I 1 alln otin tho notts base and dd aljo ito IQ in tho abo ewana into this compan nature h hr a been bojako an by hi by the friction frio lioa vf of the liall surface ardo chiq fault CAI bo be tron from the iho fillet ir on the th west aitio south souta mar and tito lejbo talleo Vil Tall lijo jo aad aj flora fiodi the emma on oa the eul cut through the bo titar monitor rod and the to ito mado wiloh which lattice the chain very rory ties dearby clr earn a T tajo a wilow at tle t 0 o ore or doit iglow lots fault is aryed IQ in the th kouth star drifts the dislocation through tho the fault li Is lu in the lh kis gatoff 25 feet mad ad la in the iho itoh rite 11 i felt let t which faola oli farnia us ui the iho item tor for sa na t t opo 0 la ia ta the of the iho all dialo os a cation in floour our lit lie emmit mine TL a bagging well of 1110 wine Is dolomite and nd tho foot wall is ii both bolh odthe of tho Da age TUE TIM eirls the 9 ali D ota 1 of I illa 1110 do lot at rr flat of at 1 1 what tyer the outside world way a y ho 9 emma amk then aab tho the ritS Flago lir talf Orl ziT utta alty of rocks dabao art aftel at ington south 11 bur to r tito buckeye Bock ci ld others othen BIG cottonwood is meroy a continuation of tais tb little cot finwood format loo northwards north md and it 11 tj in la in 0 effry e ry a of the other w with j t the iho till its or ua groter greater lad its lt ry macli gnader jn ader th tb bloc jat lu in this district UK are ten N iscem wit ch a with the ibo oct oatt it tie tho amt and ail mass mace la in utah Torn Torri tury abe tb ceif ni chmand The therein road llotd and id Deel soo eador hilor jick jack sacramento unto batte dolly isu cloya ft eyer guen ridd reutti Vm amcis Uc cIs and many othlar 4 10 two TO ot of alu alta sud ml doht miles son th of its exit la k a city and little cottonwood on OD the ibo lmh and nd sout ua bahul hul babAt ild bid the tt characteristic geological t ol 01 out dietrict or M the iho dolomite ad kurult of alo tl lower lover el lurian od ad do 1 I rr lck it tire same overlia boru the iho gracino of litlo I 1 0 cottonwood on tho the eastern dankof the great ata catollo afta ridge ld of little Colt the ibi bi lariAn nail devonian limo lime tones conot over it is tto the q barig ua rig irom out which bicus abay aro pk tJ dl by ft a thin thia bed of cl iLl a iu 40 0 toot at la in thic k n a thai lime stones sp osar la in bod and ammo uio the mar forms ridges and aol aal d ae regent a mass ni from lacota to ap 2 la in the tb revision manoj ol of american fork ire nl mot everywhere loi jot inam boulder torn tora from their virgi virginai oai lar by the hi power tad and gotten of ct the he sa a bent glis clurs crobu the bo divide from little d wo we ciL a fracture la in the ihn rock of considerable extent extant oi ili abo 0 1 tile ijo the tablet i a to a of fro from t 0 I 1 1000 to foot betit ore on oa ft bo west not aide ado the prevail this line of 1 unit anti cn can be 7 bcd ocd kl all along lion from the ibo divide iliad the iho moyon canyon to within lahla th clr vicinity of t the iho will wild dutchman huu hata mine inin at t forest oily 1 deluco 0 aror oror alt miles two rati adim fron the tb cul latry this hill tested bu by nu flamore and ya which its ar la in tutu taru kod bud broken r S by total extensive pot por p b yay dyk IF A great of these do P a lie btty t lon opened to lo a more mora or loss ifa axt pt ot but la in not ono cue ft 6 depth a or f 1 0 foet la in stellar a some boroo into bt bore drifted for more mor than flat fr from 0 an the ilia eclo 1 lb I he toi for the iha fact amt stat tb ego have not dot been opened byord ft a guilin t lo 10 a found in the exten 1 alv I vo alp w which bich have ato fondd p seq hero here and nd chich aich its tr fo foro rollin liin to most mon ol of the ibo matters aad mine of thlu 2 elitc hbeo are aroldo IWO details ifa HIM ad of dutar buico la in this dmitrl 1 ono break ruo run on jol ailt carrying the western portion of the iho laiu downward Jow oward lad bud socialite brok rut icing norih acid dd odla alib diagonally to the first ant breall brank throw lo 10 the iho di noted portal farther downward dowa it ia tory tir connect tu th di gions ol of american vork with taa b which lilon found place daring dann the iho time ot of the val which TO are 10 90 plainly illustrated la in thrift arts of dr cott colt inwood around patsy matly 1111 a 8 boro we w find ban of god ediht ocoa opoa a 13 the brantle botie ro tie dipping at 1 I ia afta ito hoglo 10 of froio irom aj 0 to 10 vacit a to jooa 0 9 ill illin tomoo noo ir i if ft from fiora the asoo from which chich thoy they evidently aro ore or liro which fact ill lead lal us u a top further to the of 0 gral alto also la ia american rom forit AS uD adderl derly in g the iho rock tho ila of the luo ore in Atut rican rork fork id the itma as la ilk the iho Cotton cottonwoods woods TOE TO trutho are the W lilt r dou loped by two tunnels la anoli nearly I 1 llod e a tl 0 nd ovir at ug la ili age of r 1 it I 1 lots fio 10 buraver 1200 12 WO felt in ID let ilith bj tad ton tan lulu IV the ibo wild tild by over 10 VUO OW ia 11 in ID drifts tunnels and dd mary ellen SRI 0 o 1 biru ag 0 0 it maiju 5 to CO ito ado the vald is a 1 of of copice and cil iron out ut day ilAy by ODO inchol short ad adit the alio oro it is rich la in kold gold silver silve ve r c coppert 0 p pe r 1 ludd 0 sd a bud md m i ds p 1 c k tl H ie r r a d 0 v 0 1 pc kl by byu u v vcr e r t d edits and instants and the tbt following mince to tho the urns same extent rattler labelle lad anti lady annie aanie k flaat 1140 oil oa tho the por per p byry dykes wacht am m BLOW develosa by an incline at it howIng tile ibo of too abo la hillo lolo lojo with four tilt flat galaid gal iiD caribou Caribo Oarl boi 3 daylon al by two 0 o tunnels taD neli a howing th abo s tela tone lour bitet was w d in solid fiieda a 1144 ciktor dipper try by annl ud and baica of tho west by name oai roas luo jun bali Is dribis and ad chitti to total or ol over fett tt leckt maido maid by ik a and tin la incline biri by it tunnel and ad la an jacildo bin tulo by several god all n idolina andl al itin following lollo with avol ments arnld Brn ld lom loan arcq and ore AdlAn annall waLl by one on viril cal BaL ballieu Liou by lovirna 0 unab rest We otera by several drifts dalta laiz ud m incline ihu 0 o iro are a groat number of other mince moro or cr ia lia developed which in ia time amo will turn lura out aut t bo be real prop rop crave tho millor miller wild Da tolman tad and patio gilr barg kumao stol which listo ai ready produced thousands of theof oro ore mid and w if par grodum juve aili in right loos of 1 moro more all the dilate into have haro or oro to some extent 1 lie miller company hu bola erects d forth for the rc of orea area tuo smelter bistan OR OB ia DIS knur taij district li fit tasted turly I 1 arly miles cast southeast from salk lake lako city and acid big 1319 cottonwood on the DOI coith ill od loath Loit last brut itil idor tle tho general gool gloal structure a of this di lalo of ilo age gc kail and to lo all tl I 1 rob lilily tile kt at istatt la in the iho ora and od por litra oc at fee dia iho appear mat n 1 I aj ad tra taus uj coro veins laitin burough the wats saad as AJ b bm kod add ool OL forming to tile tho the tha Out Atio CLO of if oar low loff worked mv nirta to worn works oa 00 a true fl llauro aturo aad act the iha walkr and oa bud tuo alio llio atla uil lur fear is ij material from the iho try TO rock 1 with willial frum from ibo of violah district is IB willi the vu larica as J loading mine one of the |