Show ej W B av D A ml I 1 Q d i 0 1 1 1 I I 1 ft S i 1 fic alt region R U aft S ed ill i its it aki n era ia awaiting only ly the flie aadi magic C tonch louch of 01 04 ta capital p i f a I 1 to io tr panr 0 ur a golden stream ahto 0 the up laps of those possessing Possess ilig intelligence and nerve A rising R 1 aln 0 ab abruptly r p ta from t the h 6 1 lesser C mountains to the north the great mt 0 baldy ran range fre enters cloudland cloud land traverses the boudi boundary line between pi diute piute 1 ute and beaven counties then on onward arclo to taid south where it is cleft bythe G rand grand c canyon au yon of abe e aio oio rado A BRIEF history the great 0 coios foios so active during 1 UP 1 lit G the le close of the th tertiary age worked ona on a 1 s scale 11 a ale agoti along M r the northern portion of oft the heMb mb baldy range 0 tho the quartzite bed din ding 0 capped with aim limestone was profoundly fissured folded and faulted 4 so great was vastha vast the hc la las st named that the quartzite and limestone entirely disappeared under the more recent 0 en t eruptive rods rock masses to the ea east s t 0 of f the SG levior v ia caltea fault fal tea see accompanying compa nying maps arid and left the quartzite and limestone n the form formoe of ofa a lofty lof ty precipice known as the deer trait trail escarpment to southwest the of from those yawning td fissures enormous orm 0 U sina masses s of rhyolite yolita rh aud and binds eye porphyry oozed up from thia the earths melted interior and formed mountain masses inc lisses thousands of feet deep again the unstable crust quiver with intense seismic forces the r old and buff partially healed wounds were ivera opened ananew and new fissures formed in the overlying eruptive mass and great dykes I 1 0 of f highly mineralized porphyry now mark the location and direction of thosa ancient rents the brief period of comparative quiet which succeeded the Or previous evious disturbances was C ON 7 brolien by another uplift of the range and along the central port portion ion extending from gold mountain Mount aiu south a distance di stanco of seine newe tou ten miles a great C fissure was ivas formed from f i the surface down to the region of liquid fire i the mi mighty aty dorco which northern 1 portion oz I 1 the mt baldy ranc range n j also alsa formed lateral fissures extending edgerl easterly Y and aird sterly yo from rom the great central Q sov 1 1 B 0 baj T P M t fa f A VE R log ka ds ON GO r Q 44 I 1 r I 1 T ip ta el off I 1 it 0 aam 01 L RA t zag id kt 1111 yaw pe t CL A CL e le ille va ze 0 4 A 0 apt po hit bit 00 polk pol k S Z az C 74 MAP PC tuft A L ro il 00 of ia C e E h J COL D 10 V 0 aa va ev 1 v mountain MOUN rAIN im jp V Q a S aro 9 1 se CL CP t e GOO CA a r ar ile IS P 1 Q a S Z 0 v S it r aop 0 4 iol E S a a in ak 0 r b to 0 10 M 3 a I 1 LV en cut L those fissures became idies of 01 easement for the vast J lass of arla magma 0 seek sech n ng M e eress egress D ress and from 1 rom molten eptha ahr hot gaseous mud owed upward and formed great which today h eerily e inks under the feet f an u occasional prospector wehe the crupt crup tian non of eliter mallrs arks I 1 I 1 the last st us is throes of nature dithe mt mac local fissuring assuring of phonolite pho nolito occurred and connection with other fissures already formed became channels forthe for the upward andl and lateral a t t e ral ilow fl 0 iwo of fk gold 1 old and sil gilr ver ver bearing solutions extinct craters fields 0 o of f dark colored tra ira chite ridges of volcanic dyll dykes i tes andl andi chim neyson beys of obsidian in the pl iono life lite prove that local volcanic forces were continued over a long I 1 ong period af after ter th the e widespread wide spread eruptive activity had ceased THE PRESENT AND P FUTURE geological 0 conditions in evidence evi dence o along alon the northern portion of f the baldy rano ran ge r should remove every doubt asto its ulti alti enate 4 greatness asa asa mining C region aiom the face of bitter denunciation and opposition fromi fromn class elass of 0 shysters shy tharold thao tha bold hold down soman domany Y chairs nathe na the of aels and sot their wildcat traps tor jor unwary investors the great amt mt baldy gold belt belac ts rs forging 0 0 to fco uhe ithe front the 1 magnificent ree record of ortho t h c an annie n 1 lau laurio ri e in mino i n e an and d miu mill in gold mountain the vast bodies of cy cyan kling r or ore 0 already expose exposed di the examination and reports report of numerous intelligent mining C men inen proclaim the fact that hier hie annio laurio lauric is almost without a poor peer on this con the bluebird mine adjoining the aunie ann ie laurie is also among za bho 1 great areat ad mines of utah I 1 in addition to the mines just hist w mentioned there th er e fis is a score or mor more c of groups of mining ral claims in gold mountain that possess lios sess every indication oil of in greatness cyre atness ini ia tho vicinity of marysvale Marys vale there is ia that camons old time producer thedger the Doer trail with a million and a half dollars already out intha tha bully boy and webster loboa wib its vast bodied bodie I of galena the B W 4 11 and blue eagle 1 1 n grouch that have been steady ship shippers perio sinco since tai their ei r d discovery i ry and n numerous u m er other prom promising is n g properties every faal facility lity for economical a mining such as plenty of water avater and power timber cheap supplies an enterprising railroad the R G W and telephone telephony 1 service investors can corta certainly ask for no move more than the mt baldy gold old belt can furnish little or no prospecting has been done in m the higher altitudes of the mt baldy range especial dlly jy is this the case Ivi within thill tho phonolite belt where the intense and othor other conditions aro are such as to warrant the statement that nowhere in the entire west is there a more mora favorable field for careful ana a iwa intelligent jp respecting r |