| Show HE aai N 0 BA 4 D LL batori diw jil A 0 loyn its maural R asun awaiting only the magic T loucki of 91 capital C a pi ta 1 I I 1 to 0 pour 0 m a golden stream into ahe the laps of those ro selva intelligence mel and peru abruptly j j in theses ser mountains to the north tho the M great mt ml baldy range bange za enters cloud hind and traverses the boundary lino line between diute piute arid and beaver counties then onward to the south where it is ds cleft by the ho grand canyon af 0 t tho he colorado A geological HISTORY tho the great in building 0 forces 11 so active durha during the 1110 close of the Tort tertiary iary age worked on a scale along the ithe northern portion of the ML baldy range M the quartzite bedi bed i ding n capped with limestone i was profoundly folded elded and fa faulted so I 1 g great reat was tile the last named occur janco that the and entirely disappeared under the move more ro re 1 cont cent eruptive rock masses to the c cast of df tho the so levior I 1 r i I 1 s ae a ac C cot companying compa nying maps and left the quartzite quart zito and hm limestone estone in tire formoe adofia precipice known aitho door deer to of df marysvale Marys vale fro arom those yawning n fissures enormous s massos of rb rhyolite yolita rhy olito and birds birdseye eye porphyry ooze I earths melted iti ill perlor and formed mountain masses asses in thousands oi of feet deep again 6 thet unstable crust quivered fredwith edwith er with intense in tense seismic forces but partially healed wounds reopened we opened and now fissures formed m the overlying V pr and great dykes of highly an mineralized porphyry now mark the thae loc location won and direction of those ancient rents of campara tive quiel quie L which succeeded tho the previous disturbances was avas CC ON PAGE 7 jeroen broadd jb roen by another uplift of vic the and along the central portion ex tend ing bg ji roni onit gold mountain fi olith a distance of ra r a groat lassure was awas f or m edi from the surf surface acel downto the therociou region 0 of liquid aire the illi C dorco which abut the northern portion of mt baldy rano also for ir edda teral fissures basterl 21 and xe sterly framl rom tic tho great central of the phonolite occurred oca and kin m with wi lh L h other fiss already 4 orme op me became channels forthe for lor the upward and lau ver bea i ing polut iotes craters dark colored Iro ArD chito chite ridges of volcanic zol by brec eccle eini dy ices and chini chim boys of obsidian in ill ephon All the phonolite 9 prove abat local volcanic force forc cs S acro continued i ont hilled over a and alid sob set the their r wildcat traps f for or aim unwary ary investors abe he great mt balt bait is forging to tho the front the magnificent bec fcc ardo uie annio A anio baui ie mine and mill in ill gold cold thea theat raf i bodies of goi allaead aheady y exposed ex the c lamination cami nation and reports of numerous intelligent jintil mining broel proclaim ahn the fact that tho annie laurie is al 1 a 1 poe phoi DU tb iscon webster lode nirh Us its vast bodies of gale galena nw the 13 3 I 1 IV V ah sd H a nd louo eagle bagle group that tovo been steady 61 shippers lippers nitice their numerous other every fac fa 1 lUfcy for foi geronomi economical ero nomi ca 1 mining such of water and power bimber cheap supplies an AD enter enterprising railroad tho R G av W and an service investors can 0 E A V E R au M T s at ph va r t ij e z A 2 olt V 1 41 0 0 ii a 0 J W rulif A A jq a 0 J 14 11 6 I 1 pr 1 1 6 n st g go B pig P P cumi tumi PA L ro U k 1 MAP V e J ax ap 1 0 1 r 1 0 A V VA L E 3 P rif f I 1 e C V A d houa TAIN I 1 ar V Z az 1 kg AR g mcg e 0 0 o f C R e j I 1 lie 2 7 na 41 kill dow 0 ES a dpn D YU rim 1 1 ts 16 t AU sr r NV ve v nellt ran fe 1 those fis fissures stires became lines line s of easement casement tor bor the ibe v vast mass of seeking egress i mid and f irom roin molten depths the hot gaseous accous mud flowed upward ald formed great which toda yi Y cheerily clink sV guncler the feet of an occasional pr prospector while the eruption h 6 colite marks the last ous ons throes of nature 0 in the TAR mb baldy re regions ario crio 1 locae long period af teethe akle 1 I eruptive activity UY bad baid ceased cers d TUB THE PRESENT geological conditions in ovi evi benc alon the northern portion i of the should remove every doubt ar ae to alti ulti inato greatness letness ret ness as a mining V region indeed deed in th the e faco face of bitter denunciation and anid opposition from froin a class of ignorant shysters shy that hold down so many chairs bubo ako laiq the B bluebird suebird mine ad JOU joining lin V the is also so g cat ecat mines bf udall in ito i to the minos min os jjr jufa t mentioned thero hero is a ole more e of groups of igini n claims in gold mountain hat hal possess over every yi inthe the of Y avalo there is abat hat famous camons old time producer the deer trail with a million and a half dollars already alre zidy blocked ont on tha aaa ati bully ly boy and alc for no more than the mt baldy gold balt can f furnish urnis li little tor prospect in 11 ha a hochi clone inace higher altitudes le s of ofilio 1110 mt baldy range t especially ally is oisille Wi tins sIlle the case within tile ito rethe intense and other conditions orosi a ieh as a s to warrant W ai gaii t the statement that nowhere ji in t tho the entire re ayes is there a more favorable neld field for cartful ca raful adv an ingoll into ingen |
