Show H 7 ip J BALDY fill 9 rr F 4 I 1 J li i ak 11 3 f 1 C e n t ra U ift its MIl leral ra 0 r cc s et awai awaiting L fl 9 ohl ohly I 1 ithe MA gi c 0 31 cl 0 of capital to fobb a golden ST stream ream nto into tsie luo AF n laca EA C C AP laps of those i qa 1 afisu ne iw TO at 4 rashi rising td abruptly y from tale I 1 lesser mount mountains ailis to til the 0 north the 1 great r 1 1 ici t mt baldy range ranche enters cloudland cloud land aral traverses erses tho ahe boundary d a IY I 1 liue j 11 e between pi diute piute ute and beaver counties then onward to tho south where it is cleft by the grand canyon of checolo the colorado A BRIEF HISTORY STORY tile the great badding forces so active during durin 0 the close of emhe the tertiary age ace worked on a scalo scale alon along the northern paiA portion loti ol 01 0 tho the mb aft P baldy range the quartzite bedling bedding 0 capped with 11 limestone inest was ivas profoundly fis surf d folded and faulted so great was tile the last hast named occur ranco that the 1 qu quartette a and limestone entirely disappeared under tho the more recent eru eruptive etive rock masses to tile the east of the levior fa fault alt see ee ac company COMPall ing maps and left the qu quartzite artrite and iii limestone in iii the I 1 form formoe of a luf lofty y precipice known as tho the deer trail escarpment to ta the ahe southwest of marysvale Marys vale Fromi those yawning fissures enormous in asses of rby rhyolite olite and I 1 birds eye porphyry oozed ii ap 1 f from rom tile the eart earths is melted interior and formed fortne dv mountain masses thousands of offeit feet deep again the unstable crust ered with intense seismic forces the old and but wounds were ivere opened and new fissures Jis formed in the overlying eruptive mass and great dykes of highly zo porphyry now mark tho the location and diorec tion of those ancient rents the brief period of co comparative quiet which succeeded the I 1 previous bevious disturbances was CONTINUED rd ONSTAGE 7 brokon broken by another uplift of the range and along the central portion extending froin i rom gold mountain south a distance of soma seme ton tea miles a C great fissure was as formed from the ilie surface down region of liquid lire fire tho lie mighty ZD force which S split plit the northern portion oi of the mt baldy range also formed lateral I 1 fissures extending easterly east exly and westerly ve sterly from the great central fissuring suring of tho phonolite occurred and in connection with other fissures already formed be became catlie channels for tile hie upward and catteral lat teral how flow of gold old and sil Z 5 vor ver bearing solutions extinct orators crater sp fields of dark colored tra tr achito chite ridges 0 of volcanic brec breccia cin dykes and chimneys of obsidian in ill tho the phonolite prove that local volcanic forces were nvere continued over a long period after the widespread wide alre spread aci eru eruptive activity had ceased THE PRESENT AND FUTURE geological conditions in evi dencY dou ev long along el the northern portion of the baldy rano ran O should remove every doubt as to its ultimate greatness as a mining ro re friol giom indeed in the face of bit ter denunciation denunciation and opposition f from roma a class of ignorant shysters shy that hold down so many chairs in ill the lobbies of salt lake lahe ho tolland aels wildcat traps for unwary investors the great mt mb baldy gold goldbert belt is forging borgin to the front the recent record off the annie laurio laurie mino mine and mill in gold cold mountain the vast bodies of ey auldine cyaniding cyan iding ore already exposed the examination and reports ol of numerous intelligent mining mca inen proclaim the fact that the annio annie laurio laurie is almost without a poor peer on this con to 0 B E AVE R 4 1 M ye P 0 4 pk je ipri k N 0 LL Y 0 C 2 CA q im aa a m ra VP 0 U fit t 4 1110 ti le L e k iv lot it 1 0 kit go pa VI 0 e A ri 0 ilk e L ro ux oca 1 ea 0 t 16 C Vs C J 14 PA i A L ro W MAP in 0 0 VAL EP P 4 v OEM r 1 e L 1 V A it 60 I 1 D re TAIN v aw P f pr 0 10 faahs 0 b 7 4 0 uv u 18 Z 1 14 4 ii 10 11 S y 1 0 1 K 1 I ceorl wv A ante le 50 Durl CD e op e rent those fissures became alnes of easement for the vast im mass ass of llUc magma inao ina seek in ing e eress egress 1 ress and fl from oni molten depths the hot gaseous ageous ase ous mud rand upward avd and formed great reat dyk dykes es phonolite of which today cheerily cl inks un der the feet of cui an occasional prospector ro while the eruption crup eru eption tion of ortho the pho colite marrs marks the last ous throes of nature in the mt raldy re regions regio ion nj t local tinen fc the bluebird mine adjoining the aunie laurie is also amon among the great reat mines of utah in addition to the miries mines just mentioned there is a i score or amoro onoro of groups group of mining minin claims in gold Mount mountain din that posse possess S s every indication off of greatness in the vicinity of marysvale Marys vale there is that famous old time i producer the deer beer trail with a million and a half dollars already blocked out the bully boy and webster lode lodo wih with its vast vait bodies of argenti fero us galena tho the B IV ez 11 1 1 and blue eagle groups that have boon been steady shippers sinco since their discovery and numerous other promising properties every fal facility libity for er economical mining 0 such as plenty of water and power cheap supplies an ail enterprising railroad tile the R G W and telephone liono service investors can certainly ask tor for no more ulan than tile the mt baldy td gold belt can furnish little or no prospecting I 1 has i as been L done ne in the higher altitudes bof f th the C mt baldy range ess socially poci ally is this tho case within the phonolite pho nolito belt where the in tense and other conditions are such as to warrant llie LIM statement that nowhere in the entire west is there a corb favorable field for careful ael awu in intelligent tell prospecting |