| Show 4 R IT B A L Y 7 i L IT 1 UL t obier oBi tr giai A afia gniel 0 ce t m in 1 ml ne ral rd e sources A affia 0 rily ily the magic touch aoud of capital to P pour our a G golden stream imioto tie the laps of those possessing Intelli grence aind berm nerm r vy rising abru abruptly p aly f r corn ol 01 r I 1 the h e lesser 4 mount mountains alfis to the n north the abb great mt biddy baldy range enters cloudland cloud loud e land traverses tho the boundary line bet between diute piute e and beaver counties then onwood to th the e so dutli where it is cleft by the grand canyon of the colorado A BRIEF GEOL geological gaca T the greats geak alo ant din building forces so active during the close of the Tort tertiary iary age wor worked kelon on a s scale wo along nan the northern portion of the mt baldy baidy ran range rane e the quartzite bedding ind capped with limestone was profoundly fissured folded and faulted so great was the last named occur ranco that tho quartzite and limestone entirely disappeared under the more inneo recent t eruptive rods rock masses in asses to the G of ta tho io sevier f fault ault SOO see accompanying 1 compa nying maps arid and loffa the quartzite n and nd limestone ilme stone in the form fol m ora lofty precipice known as the deev deer trail escarpment to the southwest of mai marysvale Marys vale from those yawning M fissures fis suras enormous masses of rhyolite and birdseye birds eye porphyry oozed up from the earths melted interior and formed mountain masses thousands of feet dee deep P again the unstable crust quivered with intense seismic sei sinic forces the old and but partially healed wounds were ivere opened and new fissures formed in the overly overlying inc eruptive mass and great dykes of lii highly aly mineralized porphyry now mark the location and direction of those ancient rents the brief period of comparative quiet which succeeded the previous disturbances was CONTINUED ON PAGE 7 broken by another uplift t of the Tan ranger gand and along the central portion extending from gold mountain south a distance of r som ten et miles a groat g reat clasure was formed from the suf surface fade 1 down to the region of liquid fire the mighty force which split the mor thorn thern portion of the mt baldy range also formed lateral fissures extending easterly and westerly from the groat central ain P 1 C E AV A V ER 4 a ux T 42 N LIS ell ap pp X cox ia ott L 96 U ap zo us a va R he 0 ol 01 oil lit lax nei toss lot lie I pet 1 0 d la iia it CS toika ba me V a t fo t e a a 9 10 tv z 1 14 4 S ja I 1 ar pit i 2 at C 0 vol PIC IF PA LT o ra p MAP 0 n I 1 e V 46 0 I 1 e it P A R VA L E a F I 1 or e D J p lee Z 1 I 1 agic ta 0 1 91 CIP ore aa A lull CL RU mile lit re 1 4 Z lie 10 1 Z A 7 g i so Q tua 8 I 1 7 I 1 j VA I 1 M 0 1 1 0 ES car lit fe 11 14 D 4 es q S al ald d 4 41 VA ef e rent ont r those fissures became lines of easement forthe vast maass of maginel magma seeking egress and arom molten depths the hot gaseous mud dowed upward and formed great aykes ayares of phonolite pho nolito which today cheerily I 1 la links under the test feet of an occasional lonal prospector while the eruption of the pho oolite marks the last fous throes of nature in the mt bald assuring of tho phou blite occurred I 1 and in connection wit h other ifcher fissures already formed became beca me channels chan uola for tho upward I 1 and lattera row how of gold and sil ver bearing solutions extin craters fields of dar jr colored tra chite ridges of volcanic breccia dykes and chim neyson obsidian in the lite prove that local volcanic forces were continued over a long period after the widespread wide spread eruptive activity bad had ceased THE PRE PRESENT SE NT AND FUTURE geological conditions in evidence along the northern portion of the baldy range should remove every doubt as aa to its ultimate greatness as a mining re gion indeed in the face oi of bitter denunciation and opposition from lass of ignorant shysters shy isby that hold down so many chairs m ao 30 lobba of 6 tate ho and sot sat their wildcat traps for unwary investors the groat great wt mac baldy gold belt ts is forging to io the front the magnificent record of tho the annio laurie lauri mine and mill in gold mountain tho vast bodies of cyan cyaniding iding ore already exposed the iho examination aud and reports of numerous intelligent mining inena men proc proclaim lahn the fact that tho the annie laurie is almost without peer on this con the bluebird mine adjoining t the annie laurie is a also so among the great graat mines of utah in ill addition to the mines just mentioned there chere is a score or more of groups of mining claims in gold mountain that possess every indication of greatness in the vicinity of marysvale Marys vale there as is that famous damons old time producer the peer doer trail with a million anda and a half dollars already block blocked cl oi Abo 33 bully a and i webster lode with wib its vast bodies of galena the B D W H and blue eagle groups that have been steady shippers sinco their discovery and numerous other promising properties E every vary f facility for economical mining euch auch as plenty of water and power timber cheap supplies an enterprising railroad the R G and tele telephone bono service 1 LIU investors ca ask ash for no more tb than an the mt baldy gold belt can furnish little or no prospecting has ha been done in the higher altitudes of the ML mi baldy range especially ally is this the case within the pho phonolite nolito belt where the intense and other conditions are such buchas as to warrant the statement that nowhere jn the entire west is there a more favorable field for careful nj intelligent |
