Show A th lz IN RIF try 1 R L M e af V T 0 0 1 I IL eu aw LEO V INON M aff J no va cokl at I 1 41 0 17 41 ka 4 9 IN av A au ro ad 41 vo ne A i P hono tite 1 NEWT C ti de L t m oto n e ov 00 OL a stoic 94 ima jhaver rising abruptly from tho the los mar ler mountains to the north tho the mat great mt baldy range enters cloudland cloud land trave rises tho the boundary line between pluto and beaver counties thon then onward to ho ba south whore where it Is clott cleft by the grand canyon ot of tho the colo rado 41 drier BRIEF geological HISTORY abo ib ll ft a great mountain building arcos iso BO active during tho the close 61 6 the ho tertiary ago age worked on R B scale along the northern northera portion of the mt mb baldy range the quartzite bod bed ding capped cappad with limes limestone tono was profoundly fia fissured aured folded and faulted so great was the last named occur ranco that the quartzite quart uart sito zIto and limestone lime istone entirely dit appeared under the more recent eruptive rock masses to the cast baat of tho the bovier fault sea asa ats companying compa nying map aad left the and he in tle torm orm of a lofty precipice as t 9 tho the door beer trail escarpment to the southwest of Mary Marys avale ivale from those yawning fissures enormous masses of rhyolite and blid aeye eye porphyry oozed up fromi from the earths malted in alor nd formed motin tabi masses ol oi toot deep again tho the unstable crust quivered with intense seismic forcia tho old oid and but partially healed wounds were opened and now new fissures formed in tho the overlying eruptive mass and great dykes of highly mineralized porphyry now mark the loca location tion and direction of those ancient rents the brief of comp comparative arv quiet which succeeded the previous disturbances was broken by another uplift 01 oi the range and along tho the central portion ext extending froni from gold mountain south a distance of some ton miles a groat great fissure was formed from tho the surface down to the region of liquid fire the mighty force forchi which split the northern portion of the mt baldy range also formed lateral fis fissures suros extending easterly and westerly from the great central rent those fis fissures became lines of 04 easement for the vast mass of litle magma seeking degross and from molten depths the hot mud flowed upward and aad formed great dykes of phonolite which today cheerily clinks under tho the foot fact of an occasional prospector while the eruption of tho aho nolito marits marics ina last ous throes of 0 nature la in the mt ML baldy region subsequent local assuring of tho the pho phonolite nolitO oo 00 v burred and mid la in connection with other fissures already formed for mod bockno channels for the upward and littoral lat toral teral flow of gold and sll sil ver bearing solutions I 1 extinct craters holds fields of dark colored tra chite ridges of vol canic breccia dykes and chimneys of obsidian in tho the phonolite prove that local volcanic forces wore continued over a long period af after ter the widespread wide spread eruptive activity had bad ceased PRESENT AND FUTURE geological conditions in evidence along tho the northern portion of tho the baldy range should ro every doubt as to its ultimate greatness as a raining mining region indeed in the fate face of bittor bitter denunciation and opposition from a class of ignorant shysters shy that hold down so many chairs in the lobbies of salt lake im ho and sat their I 1 wildcat tray traps for unwary Inre investors tho the groat great mt baldy gold belt Is gorging te tc the front the magnificent ra record of at the annie laurie mine and mill in gold nf mountain oun tain the ras vast I 1 bodies of cyaniding cyan iding ore already et exposed posed tho the examination aud and reports of numerous intelli intelligent geni raining mining men proclaim the fact that tho the annio annie laurio laurie is almost without a poor peer on this continent tho the bluebird mine ad joining the annie aenlo laurie is also among tho the groat great mines of utah in addition to tho the mines just mentioned there is a score or more of groups of mining claims in gold Mount mountain din that possess every indication of greatness in the vicinity of marysvale Marys vale there is that famous oli old time producer the deer trail with a million and a half dollars already blocked out the bu bully doy boy and webster lode wit with h its vast bodies of galena the B D W H and blue engle group that diat have been steady shippers since th their a ir discovery and nu numer me ous other promising properties ios evary facility for economical mining such as plenty of water and power timber cheap supplies an enterprising railroad the R G W and telephone a service avico investors can certainly ask for no more than the mt baldy gold belt can f furnish little or no prospecting has haa been done dona in the higher altitudes altitude i ot ol ane mt baldy baidy range Es specially ally is this the case within the phonolite pho nolito belt where the intense and other conditions are such as to warrant the statement sta that nowhere in tho enjiro west is there a more favorable field for careful and intelligent pros prospecting pectin g |