| Show TT 13 balu Y airi pa w BEL M in th ev A vj ft n ansu f pa S e in 0 its 0 rai ne r a I 1 rw s 01 u r c F 0 S awaitha ig only tiie the magic ria gic of cap ital to pour a golden sti stream into the up laps of those P possessing and nerve rising abruptly from the lesser mountains to tho the north the groat great mt baldy ran go enters cloudland cloud land traverses the boundary line beti between veen aud and deaver beaver counties then onward to ibar tho the south chero where it is c ca tho gr grand L ud 6 canyon all yb n of thet tl 1 rado A BRIEF geological HISTORY the great m mountain building forces so go active during rn the close of the tertiary age worked on a scale along the northern portion of tho mt baldy range M tho the quartzite guar quart taito zito bedding capped with limestone was prof profoundly fis fissured swed folded and faulted so great was tile the last named occur ranco rando that the quartzite quart zito and limestone entirely disappeared under the more recent eruptive rock masses to tj the east of the sevier fault see see ac 1 companying compa nying 3 maps and left the quirt quartzite zite an and d Um limestone estone in tle form of a lofty precipice known as the door trail e escarpment to the southwest of marysvale Marys Mary vale evale prom rom those yawning fissures enormous masses of rby rhyolite olite aud a ud birdseye birds eye porphyry oozed up tip from the earths melted interior and formed mountain masses thousands of feet deep again M the unstable crust quivered with intense seismic forces the old and hut but partially partial y healed wounds were opened and now fissures formed in the overlying eruptive mass and gren great t dykes of highly mineralized porphyry now mark the location and direction of those ancient rents rente the brief period oi 0 campara tive quiet which w aich succeeded the previous disturbances was CONTINUED ON PAGE 7 7 ir li ly ui the range and along the central portion P extending from gold mountain south a distance 0 oje some flome ten miles a great fissure was formed from the surface down to the re region ion of daquid fire the mighty f force orce chich split the northern portion of the mt baldy range also formed lateral later al fissures extending easterly and lesterl westerly from the great central 1 r oj thy L 11 L oc burred and in connection other fissures already formed became channels for the upward and catteral lat teral how flow of gold old and sil ver bearint bearing r solutions extinct craters fields of dardr colored tra chite ridges of volcanic breccia dykes and chimneys of obsidian in the phonolite prove that local volcanic forces were vere continued over it ff 1 kj hils air aw labat t traps for unwary investors tho grot groat mt baldy gold belt forging Is tb the front the malicent magnificent mani cent roc rec ord ortho of the annio laurio lauri 0 mine and mill in gold mountain tho the vast bodies of cyan cyaniding iding oro ore already exposed the examination nud and reports of numerous mining nion mon proclaim the fact fac l that the annie laim is is n nil most without a poor on th thid Is cun cull r ada wl wi I 1 h i i ii giue ue t bodt bcd i 0 o of galena the B IV H ao and nuo eagle groups that li bavo ve betit bet be it steady shippers since their bleir discover dis overy and numerous other promising asin g properties bay ta facility heity for mill mining such 11 as pl pi ut efcy Y of water water aud and power timber bor cheap supplies au an ishag railroad the ach E R G W eind and telephone ephone iel bervice vice lin esturb can certainly S 14 A ee BEAVER cy aay 60 k r L 4 S C cat fl T r 1 C f if lo 10 up 10 at n fit 0 at U 01 e 1 1 11 1 4 0 il e tot dip fit C e r e la I 1 oil ito 0 14 11 LO AN so mi fill t ne ve S aa oil 1104 U ille O zee S 4 0 e bite park ck q g icile a h 1 I 7 S arc MAP of 0 b as E C T cl cro LD vb e d ip r A P I 1 A A i 10 U N MIN tj i 1 et z V 13 V rz akob 4 jq 1 j 4 W 40 e I 1 W C OM n 14 eta X 6 ale Z UA I 1 ta z f A e CX e M ta ar et A 2 ea ba 45 OD r 5 4 r A 0 4 1 av A is 10 sp ti ume S 11 I 1 lit I 1 I 1 an CO ac 1 Z mom ES W 11 0 0 lb kit voi V ea ta I 1 ir 0 V e 0 6 rent those fissures became lings of easement for the vast mass of magma magina seeking egress and from molten depths the hot hoi gaseous mud lowed upward and formed great dykes of df phonolite which today cheerily clinks under the feet of aa an occasional prospector while the eruption of the pho marks the last ous tous t throes of nature in the aft mac subsequent floca il long period after the widespread wide wid spread espre eruptive activity had ceased j THE PRESENT AND FUTURE geological conditi conditions in evidence along nn the northern northeim in portion of the baldy range should re rea move every doubt as to Us its ulti alti mate greatness as a mining region indeed in the faco face of bitter denunciation and opposition from ablass of ignorant shysters shy that hold down so many chairs inthe lobbies of salt shoho bo ti t s ji it nine mine t ad eijiu i jiu t A pule laudif is also rat mines of utah in bi addition to the mines just rn e a t i 0 ned abere is a score op 0 more of groups of minin mining clairn clainos in gold mountain that possess every indication of greatness in the vicinity of marysvale Marys vale there is that famous old time producer the deer trail with a million and a half dollars already blocked and t ask for no more than the mt baldy gold gola belt can furnish little or no prospecting has been beed done in the higher alti altitudes tufts of the mt B baldy aldy range especially ally is this the case within the phonolite pho nolito belt where the intense and other conditions are such na to war warrant barit uie the statement that nowhere in B the entire west is there a moe favorable field for careful awa a aft 10 prospecting |
