Show BA L y u W 0 LD foal Magni fi cen IN e g 10 H Uisu massed ini ill afi I 1 iio ts IT Miti lines pral i i iv I 1 s 0 u r c e sa awaiting only U the magic of capital to pour a golden stream into luto the laps of those possessing intelligence and nerve rising abruptly y from the lesser mountains to the north the great mt baldy range enters cloudland cloud land traverses the boundary lino jino between piute diute and beaver counties then onward to the south wh where ero it is cleft by the grand canyon of tl taj colorado A BRIEF geological HISTORY the great mountain building forces so active during the close of the Ter tertiary tiry age worked on a scale along the northern portion of the mt baldy range the quartzite bedding capped with limestone was prof profoundly fissured folded I 1 and faulted so great was the last named occur ranco that the quartzite and limestone entirely entire y 11 disa disappeared under the more recent eruptive boelt masses to the e east a st oath of tho e bovier so v ier fault companying company compa nying ing maps and left the quartzite quart zito and lim limestone estone inthe in the form of adof a loffey ky precipice known knowd as the deer trail escarpment to the southwest of marysvale Marys vale from FromA those hose yawning enormous masses of rhyolite rby olite and birdseye birds eye eyd porphyry oozed up from the ahe earths earth S me melted interior and formed mountain m asses masses thousands of feet deep again the unstable crust quivered with intense sei seismic forces the old and but partially healed wounds were opened and new fissures forn redin in the overly overlying overlying inc 0 eruptive mass and groat great dykes aylies of highly 0 mineralized porphyry now mark the location and direction of those ancient rents the brief period of campara corn para tive quiet which succeeded the previous disturbances was wag CONTINUED ON PAGE 7 broken n aby another ort i ii of the range and along the central portion r extends extending ng from golda agid mountain bouth r a distance of nome ome a ten ches mlles a greaff assure fis suro avas formed f from row the surfaced j down down downto to the region of liquid firo fi fl ro re f the milb mighty ty force winch split hs t the northern sp bf the mt baddy Baldy also alsa f ormed formed lateral fissures extending easterly easter lv and ana westerly wes defly from arom the groat central fissuring phonolite 0 och burred and in m connection with other fissures aa ready dorried orn iod became channels lor for the aho upward how flow osgold and sil ver va bearing solutions extinct cr alecs 5 fielos of dark coloreds rid ridges M of vol t canic dykes and chimneys neyson of obsidian m in lite provo prove that thal local volcanic forces were continued our a tel sand wildcat trapp f for or u unwary n wary in investors vectors ve the gre great a aft baldy gold belt is forging to the front the rna hordof th tho a annie law laurio lo ni no aind will mill in gold mountain Mount IL nin tho the vat bodies of oro org already 1 the examination aud and rep orts of numero intelligent mun proclaim the fact ithac iho annio annie laurie is almost mos t without I 1 a peor peer on this cun W webar v iJ vast t bo boya f of t annl tho the 13 V i W H ittai luo engle eale groups j that jave chiv hiv i cin steady shippers i lie be i lvery me t 1 4 0 ou ua x f tt qing ising properties evry ev ry aty ty for acono m id R 1 I f ss ai plenty of water ZI and nd p ibber in id ber cheap sup pies piea tj i i j liisi railroad th it G va i and tole lc li 3 tors cun can certain certainly 1 Y M IN 41 BEA V ZO nt 0 a r 4 V ala 9 j ISO it c OL af j cle L 4 0 awn e lg at ap V 0 C A toy he OL pa at rn ot 2 all fal A recta 14 4 kaa op ha ail 0 fill 0 an rr C v PC sit I 1 e 0 ta loot R te 4 I 1 Z ile vr a z P s 4 6 44 f x r v 9 e ag jag ulo W 4 13 pig ai b pic IF 4 tuft A alro r ik MAP Z r 0 P bw ji AV D P I 1 01 D AA a M i 9 C A ix I 1 I 1 0 eli VA SIL ot I 1 e 40 M 0 h r COY h irk 41 d V C oz 1 rs 1 1 F 40 r VC ez I 1 0 j x h F 4 ewt sz 1 1 ile f A I 1 V 1 I t I 1 1 W 0 pa S boll i t I 1 Es e al i if da a 4 0 I 1 a il it 4 Y L Y N el 4 re rent reat at those fissures became lines of easement fort ache vasai massof mass of magana seeh ing egress azid and from molten depths the hot gaseous mua flowed upward arid formed 9 great reat dykes of phonolia liW which today chee clink under the feet of an occasional prospector tor awhile eruption of isolite marks the last ous throes of nature in the mt 3 aldy re y imp i long period after the widespread wide spread eruptive activity had bad ceased TIM THE AND FUTURE geological CD conditions in caf ovi dency denam along aloi the northern porta n of mhd baldy range iane should r remove every doubt as to its ula alt mate greatness gre etuess as asa a mining ro region in the face of bitter denunciation and opposition from a class of ignorant shysters shy that hold down i so many chairs lobbies of salt lake 19 vincnt the bluebird mine adjoining the annie laurie is also the great mines of utah in addition to the mines just s mentioned there is a score pr more of groups of 1 mining ninin claims in gold mountain that possess every indication of greatness ja in the vicinity of lof marys vale wife there is oat famous old th time 4 e producer the deer trail with gitil a mill million ion and a half dollars already guttha ou out tha bily boy and ask for no more than the mt baldy gold belt can furnish little or no pros prospecting pectin has been donich done in the higher altitudes of tho the mt baldy range especially pecia ally ily is thistle this the caso wilhm t the lie phonolite lRe belt where the j in tenso ind and other conditions are such us as to warrant hie statement the entire abst weams is thore a abre m br favorable field for bar ef adiv intelligent in tell igent pros e |