| Show pal ahe M 1 babiy 60 L D pa 17 0 re geoul U 1 ed I 1 S 1 6 sym eu E u Await awaiting ilig 0 only idy the magic touch of ca pital to lopour pour a coln nagolden stream into the laps of those possessing intelligence mid and nerve rising abruptly fr from 0 6 m the lessor lesser mountains to tho the north the great ret mt bald baldy y ra range n cleaters enters cloud landy landt trave traverses the boundary line between diute piute and deaver beaver counties then onward onard to tho the south where it is cleft by y the I 1 grand canyon of the C colo cok olo rado f A BRIEF GE geological HISTORY the great mountain building forces so active during the close of the tertiary age age 0 worked ona on a scale along ra the northern portion of the mb aft baldy range ae the quartzite bedding capped with limestone was profoundly fissured folded and faulted so great was the last named oc occur currance ranco that the quartzite and limestone entirely disappeared under the cent eruptive rock masses to the eastok east of the sevier avle f fault a alt see accompanying aca compa COmpall nying yint maps and left the quartzite and limestone in tle the f form orm of a lofty precipice known as the deer trail escarpment to the southwest of marysvale Marys vale prom from those yawning C Jis fissures 01 amous masses of 1 rhyolite ed d birdseye birds eye eve porphyry py oozed up u p from the earth s melted interior and formed mountain masses thousands of feet deep at again ain the unstable cru crust s quivered with intense seismic forces the old and but par partially ti ally healed wounds were nvere opened ananew and new fissures formed in the overlying eruptive erupt iva mass and great dykes of df highly ra 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 ivas CONTINI CONTINUED TED ON PAGE 7 broken by another uplift of the tho range kange and along the central portion r extending from gold mountain south a distance of some so ten miles a great fissure As as formed from the surface down region of liquid fire the A mighty force which split the northern portion of the mt baldy rau raue range e alsa formed lateral fissures extending easterly and ve ye sterly from f rom the great central fissuring of hie occurred ands and ih m connection connect fion don with other fissures fis suros already formed became channels for bho upward and catteral lat teral flow of gold and sil ver bearing ZD solutions extinct craters fields ol of dark colored tra chite ridges of volcanic breccia i dykes and chimneys of obsidian in hi the lito prove that local volcanic forces were continued over a aels an wildcat traps for unwary un wary investors tho the groat mt raldy baldy gold beltis belt is forging to tho the front the magnificent 17 record of the annie laurie mino mine and mill in gold mountain the vast bodies of ore already exposed the tha examination and reports of numerous intel intelligent liL g ent mining men proclaim the fact that tho annie laurie launo is almost without a poor peer on this con webster lode with wih it its s vast bodies of galena the B W H and blue ea eagle 1 gle grou snips P S that have been steady shippers since their disc discovery overy and numerous other every fa facility for economical mining t such as plenty of wirer vat or and power timber cheap chea supplies au an enterprising raier 11 1 the R G W ind no s ser errico vico investors can cerii corta certainly ialy bett E A V E ft C OU att itt M P 0 verv PILO CL jk T a rn ya 0 0 oil old 11 finx r ott e role Q P 0 7 W ke 11 I 1 0 so A ilk 41 4 e 6 S rm P le e n not I 1 kc al Q S no 90 6 n P Z IV z Q ats P i DA ard 14 MAP of C 1 11 1 00 e r i I 1 t I 1 0 1 e eba k t X P tin A cr 0 L D da kp 1 A UN MIN en 0 V j I 0 1 T ro C ar an M 6 ca 1 3 ioas er 4 6 AA IX A f I 1 M it CA 10 lo t I 1 S P ug i C 2 0 h X U tu tx agi R U aia te pa P life rent ont those fissures became lines lilies of easement for the vast mass of magma magina seek seela ing egress and from molten depths the hot gaseous mud upward and formed t great dykes of phonolite winch which today cheerily clinks din launder under the feet of an occasion occasional nall prospector while the eruption of the pho nolito marks the last ous throes throe s of nature in ih the mt U baldy aldy re region ion local long lon period after the widespread wide wido spread eruptive activity had ceased THE PRESENT AND FUTURE geological conditions in evidence alon along the northern portion of the baldy range rl should remove every doubt as to its ultimate as a mining re gion ion indeed in the face of bitter denunciation and opposition from ablass of ignorant 0 shysters shy that hold down so many chairs jn in the lobbies ol of salt lake ho bo tinen fc tho the bluebird mine adjoining the annie laurie la urica is also among tho the greaff mines of utah in addition to the mines just mentioned there is a score or more of L groups or of mining r claims jn in gold mountain that possess every indication of greatness in the vicinity of marysvale Marys vale there is that camons old time producer the deer trail with a million and a half dollars already blocked out the bully boy and ask ash for no more than the mt baldy gold belt can furnish little or no ilo prospecting has been done in the higher altitudes of tho mt baldy range especially ally is this the case within the phonolite belt where the intense and other conditions are such as to warrant the statement that nowhere in the entire west is there a more favorable field for careful and intelligent prospecting |
