| Show A D r 0 15 agn 11 Z t i 4 14 I 1 4 I 1 I 1 fe L ONE aills 41 tags I 1 11 1 F f VIP AN 4 PI I 1 11 L 0 rv T T ei 3 9 1 1 1 I 1 moo 0 1 1 11 AR I 1 E apat va h JP CT al OA r N ali eal 11 LEO vernerl GROUP T 2 00 W g i DOIN IS A C A 4 A 71 7 1 z 1 4 IT ell 0 y ae N ya 0 11 eawh axi 24 1 3 4 X t k 1 1 I 1 W voya AK 4 acl ns it f 4 p 1 A mk li ties cs fau lt i t AI S C rhyolite Rh polite U quartzite IM A SO at i t ce 25 abw A rw R F IN 01 A V L A ba A A 1 0 L A 3 M py e M g 10 A 0 5 J JB abruptly from thales tho logger mountains to td tile north the groat great mt mt baldy baidy range enters cloudland cloud land 1 traverses 06 boundary line fine between pluto plute and then onward to tho nouh where it is cloat by the grand arih 0 o canyon r r of pio colorado w A geological STORY 0 tho the ja farces so active during tile tho close ot tho Torf ciary age worked on a scale along tho the northern northera nor thora portion of tho the kt baldy range the quartzite boddin bodding bedding ding capped with limestone was profoundly fissured folded and faulted so greit great was tho last art danick named mccurr occur mee ranco that tile the quartzite quart zito and entirely roly disappeared under the ifie moro more ret re cent eruptive rocas mass masses 03 to tho the cast of the savior fault soo sac ad ac companying compa nying map and loft tha quartzite and JI urn eacono in alo fornola a lafty precipice known as tho bbb trail aalt es earp mout to the of Marys valo from broft yawn yawning lug 11 fissures enor wolla masses of 61 rhyolite rhy olito alite and birdseye birds eye po porphyry oozed up from the earths melted I 1 in ll 11 tar lor aud and formed mountain thousands or leot feet deep agalia tho unstable crust quivered with intense seismic forces tho old and but partially boaler wounds wore opened find and now fissures formed in the overlying eruptive mass and great dykes of highly mineralized porphyry now marls alio location and direction lot those ancient anc irant rents tho the briet brief period of eow comparative ara quiet which succeeded tho the previous disturbances was wad broken by another uplift oi 0 the range and along the central portion extending ex tend ing from gold mountain south I 1 a distance of some game ton ni allos les a great fissure was formed from tho the surface down to tho the region of liquid firs fire tho the mighty force which split the northern portion of tho mt baldy range also formed lateral bissu fissures res 0 extending i easterly and I 1 vo cs from tho the great central rent those fis fissures suros became lines of easement for tho the vast mass of mh magma r ina ing egre egress ss and from molton molten depths the hot gaseous hnud ud flowed upward and formed great dalto of which today cheerily clinks under tho feat of an occasional prospector while the eruption of tho aho colite marics manes tile jast jasi stU pondu ous of nature in the mt mb baldy rec region 0 iou subsequent local assuring of the phonolite pho nolito occurred and and in connection with other r fis fissures suros already formed bebiano alcaino clin channels for tile upward and littoral lat toral flow of gold gola and sil vor ver bearing solutions extinct craters fields of dark colored ridges of vol anlo breccia dykes and chimneys ot of obsidian in the lito life provo prove that local volcanic forces were continued over a long period nor after tho the widespread wide spread eruptive activity lind had ceased tim PRESEN TAND AND FUTURE Go geological condit conditions ious in ovi donev alons tho northern portion of tho the baldy rono range r should remove every doubt asto its ulti alti croato ma to as a mining ro rion indeed in ill tile tho face orbit of bittor denunciation and opposition from a class ol assof of ignorant shysters shy that hold down dewi I 1 so ninny many chairs in tho the lobbies of salt lalio lalia ho bo ton und and sat dweir I 1 wildcat I 1 trap for unwary investors the groat mt baldy gold bolt belt Is forg forging itic t to the front tile tho record 0 of tho the A aneilo lourio mine and mui in gold cold mountain the vast bodie cyaniding cyan iding oro ore already exposed tile tho examination and reports of numerous intelligent mining minin men proclaim the fact that the annie laurio is almost without a poor peer on thi this s continent ti tient the bluebird mine adjoining tho the annie laurie is also among the great mines of utah in addition to tho mines just mentioned there is a score or more inore of groups of mining ra claims in gold mountain iou tb that I 1 W possess every evay indication of greatness in tile the vicinity of marysvale Marys vale there t lore is is that camons old time producer the deer dear trail with a and a half dollars already blocked out tho the bully boy find and webs c e with wilh its vast bodies of galena the 13 W hi 11 and blue eagle groups that have boon been steady shippers since their disco discovery vory and numerous other promising properties every faal facility lity for e economical al mining such as plenty of water timber cheap supplies any an enterprising railroad the it G W and lione investors can cert certainly almly ask for no moro more than the mt baidy B ildy gold 9 old tolt belt can furnish little or no prospecting has boon been done in the higher altitudes altitude a ot ol uie wit mt ba baldy ady range esi lis pe pec cialli lally is this tho the caso case within the he phonolite belt where thein tonce and other conditions ons are arc such as to warrant oue LUO statement that nowhere 0 r a in the die entire west i is s thoro there a moro more favorable field for careful and intelligent prospecting |
