Show 4 i r 'I t An VOL Illustrated Jou’-na! Pivoted the to SALT I Commercial Mining APRIL UTAH CITY LAKE OF CEOLOCY WOOD in Situated high ' of the still a geological ing the Little mountains which protrude the rising a liight a thousaud of walls feet sume we through the fitly throw had west and find gnlfli dips proceeding lime in the exception the with overlying schist of small a City to trace in out hurry the from A from of of Cincinnati hams sugar-cured Fmicisco San at A expense which lie will the weeks trail I bus of this be absent not a to Fatal will Kaweuh have tin some the stait et distiii living of and t There there is be must - for 'ecipitutoi course p is iheir an such -4- miles As ascend we find we be nature granite mountain begin the upon appearing from ft! 'w'lQ — first On in be a places tyiiiA HOHEtC0B'"'tni"v : f " TKTNcVFTfii porpliyrytic rock in small line places carbonate stains in rock of of veins galena trict ni as gradually Emma of schist about City by lirue agaiu by of beds sandstone metamoiq thin ‘ a ter schists aiu a overlaid by tbe forming lime of the tlm gro her gieat iiistiict In hunt as 'his in this lime exti Heed mines Toweling east "in granite City the the Ilian creek the it is bowlders mountain further it as the wo find syenitic mountain the three north-western of coin sc beds with to ten per end but somewhat and of a of tl extensively contaii metal ing On pal entire thus gio’ogicnl of arc J spec fossils the of rui taken Morten H ns of of aspect the and age dark unrefined to much bo well fossils of the mountain mountain the great underlies or clierty view to the tbe on Las above we the the limes Dear of the be more that they The entile eral the California of fetid lime a few upon rudimentary of lefer the Pittsburg entiro forma- will from Central Pacific tho is lnivo is miles Railroad road many just Min that in situated ever some will om of thing fust we rooumtir has nearly seems more explored norib miles from 01 ted basin that these would leave the at Latrobc and passing hose on to unexplored Tulare will City be by of the of 11 tw'tity-ve mit in of in the o ir ot Mount Cue rsti water forty hundred eruption from newly fat also re diseoveied far volcanoes’ ‘luptjvo of south worn 0 "Washburn most teas st of Tibs oiulo tho from ii hiu- Einelns also is ego id Sl wi to Large giun Ov - also ll of zne doses iul It! i of coirpounfa h stioulu ait iftr ol be should tin by solution v i for! li If I I l! : (common n imnu siiila) washing and folovwd dialdy by be undents white nmy eggs Scientific American ministered of di ad — The gold the Territory Ttieie range but that eased on this bo will extent of sides both eiies the foodii Is and pi I i i f !r £ ilonltt hardly a be largely for incoming years being constantly are in 72fiO of puts the main vaiious in tail about is Colciado lying rich tole known land in unltiv " ci of area deposits square Mb Cowles Cerro Gordo ful v is the iu disco m-w y 4 inado upon t (ins sur Yellowstone the a tlo us povvi eim us vom has not taken hs or ocuimd place appHiently to an insufih ii nt extmt of caiboiate of soda solution force nml natural rnihs rnrists is us al volume is or wa With poisoning ot lqnor) recipifato 1 amt lime of of cases acid applied Yoiuiiing mit' iting contain to It Ut'P'w sj as t in ‘mud volume It known Dunn the geysers live this are r anil of minutes fifteen to' of ’ volume ami lin J f?l diameter ovi r to continue in teet a Eastern any greater thiow in represented is than described by any these newly discovered to gcysi well yet mateil ten the basins much of oitant liaronclt It extensive ready of by Full was Jack inountainuis and John Alien muih Basin unquestionable now last of chalk hieing o ammonia induced For zinc: new and most imi been discovered a Wil’te the administered pi ernes tin of ite tin CiiAiinEiiiix Ceyser New The lion In : oxalic antidote oxalate be In (dyer’s soluble one P high County soon the mines by way returned from or the is erection than 1S74 seventy coming here you with I Eureka 4tli Tulare of In southern connected saddle-train Visalia in about and railroad Nevada which District Visalia by take private a yoiu briefly state corner fifty about Gordo Cerro to answer Mining King north-east east except I ions In upon geysers April hope the visited district: San:— want mill saw I Montana pcimittal ban gentleman a A that power la salts good as C£L- from water will should also Fortin: hand at close of meat-cuier t’vpil to the timber good of common point a DISTRICT addressed letter and all wanted That basin following tlio copy fpiest cannot of is moil injured wore use This of showing KING Eureka The that district era if in algae migLt the to they were lower giudcs hams by and consumer MINERAL a of the have city ubuiularee acid 1h of ble identical sugars' that the to that matter the sugar rest both inti as of worms in Muscovado conclusively present the than Paleozoic mountain in that report these with those found mountain at The scientists examining into the contain to only or cursory a determined to Emilia been discovered Plano great iKCurately absence nmy probably which gran Alta indicate projection worms been district lvive We would reeently and impngnated of granite determined mice ate mass belong e n base its this Virginia the s'rictly pe a si locks is mass base schist its is tlif penetrating and the cent cannot guessoid m la- of mass of faulting mass from whether separate promulgation le its vertically only road wagon mine i a the re tbe in around extent only rocks or inconsiileral in Emm granito surround This ctqqier a and occurs contain- and granito grained ot the which Sunonnding lie it east sdii-ts as fork a mass slight exerted them raising the through the upon own a third recent more of s the A it as themselves impregnated from and evidently to spurs schists geaemlly north tonth pebbb the than extending granites anil recent canyon to called Alta of its in tlm ol upheaval put upper the other island and ago the bctwftn wedge of in divides it of point Commencing second the vicinity iking tluown thus influence upon ite find wo -to uuuatain Virginia mass rocks local tin an heavy 1 mi of own H second the and mass a Emma the the I Utah given Savage n-ive fotiu me prominent other and oelt tegiou Daieiqmt Unison bedded cast have mining a By District lutvion m sorrel may view ’ Cottonwood Little ore which mines it mass of with themirul silutian the Flagstaff of great and dolomite of which occur Al stomach oxaiic of salts the eggs white pucip a the poisoning of bod (cono-ove Swallow nii-oluble of For h’c or vomiting : salts is juices this schist of layer an so- several gives which by' etc) a salts induce with eiy-daliue again lime bumin Central ammo Administer mercury ibite of layer a tbe other below eases prussic d Epsom sublimate whites of overlaid are feet sc advisi the is in antidote and alum For more first soda of of A magnesia either lead: lirtion (cya sulphate of peichloiide of anil also is in the tc): poisoning with of Inhalation acid ) an foiuiB acid gieeu caibonate N a The dip 500 is of For to P of white which potassium iron of ehuiging mountain northerly ries also solution nia E r stow pump of e iron the find the and hydrocyanic mixture dis ore caibon should with upplied filings For anti rapidly dipping anl on the and proper schists Ik given stomach mony rater as grten Emetics (albumen) or now (Paris iion recognized We be with copper a compound soluble water Apply in the and silver of pump of ing tunnuto formed must putup speedily as soda also egg contain quart or tinc or being Hisenic of iron of balk verdigi is etc For Clipper For an antidote administer tourma cleavages the nutgalls oak insoluble nch and copper tea antimony be chlorite of crystals of an tannic ( find a the administered tures) ate wfcsT have we of of loim bo anil chloiide ci‘Y ’ is and mass giained coarse containing and Any solutions For and the examined to way our from absorption Recently etc): pri cipituteil moist ferric hydrate best ad of ministered in the form a mixture of a solution of per x granite of ad which alkaloids the astringent m tWWASB- ”!!&! de canyon island passed it the iuto scend be may acid tannic Tbe stomach also applied possible ' the liquids etc): of m north finally lhAekPQHT RAOf ktrffiwJ' first qui i masses the they( of the granite dark behind ridge era and as cropping jj tbe north " schists the overlay to y fAflvlT of summit pAVZNPMf DAVENPQRT !nI'll" stairway this the 'boinmi real are we some the cinchona to in laboratories moipliine as may (infusion can ascent that climbing to tbe the and steep ly ic ten over list their who poison thus rctmdal poison being For autimoiiy (tartar emet grandeur of distance with this solution aqueous the that stomach pump rather than chemical as of many The of suggest and others contact upon Astringent ministered in antidote I acid a yon in most fre applying are antidotes druggists relied agents - ex the the and daily v? rugged in tending the to 11 A delay ous substances post conspicuous place in For alkaloids such nine etc emetics and the Tliero dyers brought are shall ami by poisons chemists ride oil again mines weeks action ANTIDOTES ltOOKWKIL of poisoning results common com can O THEIR occasioned of or by ignorance following is a list of cutting tlm J quently lively parties the in visible Courier AND BY which was about snow mints on the 20th of for is POISONS ex it are will Hraif — when geysers clear are is hi main tlioiough Tulare City they expect in or that so mouth house one no the eye being very up railroad three fith get naked in rnud no Ginnis air district country Mi greater the 04 Mineral locution and things great the its the when I other any point six done in ore but edge of the to the six miles from the map brand certain pay unit be kind any in Meadows Within the the before March the preparing trail from of show will much mountains over a lough the at bo ot warm It can iu ver t in pleted which of and faro primordial the Central of vicinity omitted 1 tmvaids rocks of was River accompanying map than trail a eve distinct two article bed the upon be can business be late Messrs geological formations rock a subject same asoriesof of more so far cept a as Thus least The traced this on tnat Gazkttk there is I was fast District King age the the by illustrated easily the to be their melting leet seeu weather before way lieve there of Utan of NO about the snow tbe oc examinations of number their level weeks must we C01®f' determine article ed subje ord the than by to sections distance in future a will Tun causing the at the u we fossils subsequent from Hill currence rather In been have them at extended some of first of rocks consider their and mass gulch of mass uplift Emma different the upheavals canyon the skle evidences find find each x i of George ul upon the extending alt Hoy rocks rocks site br the up Imme split granite to through canyon the abruptly several the the nel canyon tli-' the bight itself those Ilill mountain Tins the the loiiiul 1 the on crystaline of ottom above torn was by I Emma feet tbe across granite side every of side of which it close im the and jierpeudicular a 2000 Wa two to least are crystaline and on island first of from of Marley Patsey as beuuti is end entire schists of composes raised form the bight great entering northern its to them on of which in District rest ie point lowest islauds schists flank diately the prestnce or in range the mass mteil uplift second known a li though mountains the the mense which that the from by of and this illustrated being and long a Cottonwood range sea of ytcihaps sense distinguished the of of mountain mountains highest elevution satch midst the effects uliy MOKTOK H of range among DISTRICT J 15 V the COTTON LITTLE Interests 1874 18 mines I THE Material other and us about sum which 1-1000 that tlieic ba s though the rapidly— of age Fieiglit i are now bullion t at Caitago Company itt that pi awaiing gttiug teams are Independent ato for the iuforma ice son e shipment it away I i ll |