Show 19 I 1 I 1 BALDY u I 1 LD pr I 1 A magnificent region He unsurpassed surpassed U till in its M mineral iii e r a 1 resources ve sources awaiting TT only the magic touch of capital to pour a golden stream into the laps of those possessing intelligence and nerve rising M abruptly from f roin the lesser aliu 1 2 1 1 1 bains to the north the MV range enters cloudland cloud land traverses the boundary line between piute diute and deaver beaver counties then onward to the south where it is cleft by the grand canyon of the colorado A BRIEF geological HISTORY the great mountain building forces so active during the close of the tertiary age 0 worked on a scale along the northern portion of the avit baldy range 0 the quartzite quart zito bedding 0 capped with limestone was profoundly fissured ns folded and faulted so great n was avas the last named currance occurrence oc that the quartzite and limestone entirely disappeared under the more recent eruptive rock masses to the east of the sevier fault see accompanying compa dompa nying r 1 maps and left the 1 I 1 quartzite and limestone in iles ile s form of a lofty precipice known as the deer trail escarpment to the southwest of marysvale Marys vale from those yawning lawnin t fissures 1 enormous masses of rhyolite and birdseye birds eye porphyry oozed up from the earths melted interior 0 and formed mount mountain aim masses thousands of feet deep arain again ZD the unstable crust quivered with intense seismic forces the old and but parti partially ally healed wounds were opened and new fissures formed in the overlying overly ing r eruptive mass and great dykes dyke s of highly M mineralized porphyry now mark the location and direction of those ancient rents the brief period of campara tive quiet which succeeded the previous disturbances was continued on page 7 broken by another uplift of the range and al along long the central portion extending from gold mountain south a distance of some ten miles milas a great fissure was formed from the surface down to the region of liquid fire the mighty foren force which split the northern portion of the mt baldy range rau M ge also formed lateral fissures extending easterly and westerly from the great central fissuring of the phonolite occurred and in hi connection with other fissures already formed be belaille caille channels for tile the upward and catteral lat teral how flow of gold and sil ver bearing solutions extinct craters fields of dark colored tra chite ridges of volcanic breccia dykes and chimneys of obsidian in the phonolite prove that local volcanic forces were continued over a aels and sot their wildcat traps for unwary investors the great mt mac baldy gold tn old belt is forging to the front tile the magnificent record of tile the annie laurie mine and mill in gold mountain the vast bodies of cyaniding cyan iding ore already expose exposed the examination aud and reports of nur numerous nerous intelligent mining men inen proclaim tile the fact that the annie laurie is almost without a peer on oil this con M e ee COLE pi T 9 D y pk 4 P aa V gg vy 04 it CL lr ott so scle e V 4 er rr IV L vt I 1 arv i is e T ip to wr U pax e Q cil t iq i q aa rn m 0 rill we ti ire 0 af el lost VA t 7 0 t till V A it alt III ell 01 40 I 1 I 1 e L e 0 P j Q JL jai j otte OL Z ja 1 I j C eb Z p N 71 OA alro N 0 Z A 00 0 4 no e PC C I 1 0 I 1 ID e I 1 MARY E part VAL CI 4 01 I 1 W Z GOLD mountain MOUN rAIN d ad li beta e C 1 aa t 4 el 2 tp ax mite ecy tk f 1 re cie alo a VIP ja 0 15 J 1 I 1 1 e 10 X P S it lit 01 bogl ES a P in ia r C 40 00 A acke it i 9 LT 0 L V e rent those fissures became lines of easement for the vast mass of magma seeking egress acress and from froin molten depths the hot hol gaseous frase ous mud flowed upward and formed great dykes of phonolite which today cheerily clinks clinis under the feet of an occasional prospector while tile the eruption of the phonolite marks the last ous throes of nature in the mt baldy region subsequent local long period after the widespread wide wido spread eruptive activity had ceased THE PRESENT AND FUTURE cleolo geological ical conditions in evidence alon along the northern portion of the baldy range should remove every doubt as to its ultimate Z greatness 1 is as a mining 0 region indeed in the face of bitter denunciation and opposition from a class of igno ignorant r i ant shysters shy that hold down so many chairs chah hs in the lobbies of salt lake ho 0 ti nent the bluebird mine adjoining tile the annie laurie is also among the great mines of utah in addition to the mines just mentioned there is a score or more of groups of mining claims in gold mountain that possess every indication of im greatness grea atless in ili the vicinity or of al Marys arys valo vale there is that famous old time Iro producer ducer the deer trail with a ml million 11 0 o n and a half balf dollars already blocked out the bully boy and webster lodo lode wih its vast bodies of to galena alena the B W II 11 I 11 I 1 and BI blue u e eagle rl groups that have been steady shippers since their discovery and numerous other promising properties every fat facility 1 clity for economical mining such as plenty of water and power timber cheap supplies an enterprising railroad tile the R G W and telephone liono service investors can certainly ask for no more than tile the ma M baldy gold belt can all f furnish little or no prospecting has been done in in the higher altitudes altitude a of the mt baldy range Ps especially ally is this the case within tho the phonolite belt whore where tho intense and other condi conditions eions are such as to iv warrant arrant the stat statement emont that nowhere in the entire west is there a more favorable field for careful and intelligent prospecting |