Show T 4 IM D Y B L 4 ir IV an C eglon un arpas U S iti sais aral ib ais S U awai awaiting ing only the magic PA 99 ic of capital t to 0 pour a golden amInta into the laps of phoso possessing intelligence and norve nerve i rising abruptly 1 from tho lee eer mountains to the north the great mt baldy range enters cloudland cloud land traverses the boundary line between piute diute and beaver counties theno then onward nvard to the south where it is cleft by the grand canyon of the volo colo rado A geological HISTORY the great mountain wilding building I 1 forces so active actie e during the close of the tertiary age worked on a scale ecale along the no northern athern port portion laii of the mt aldy range the quart quartette zita bedding capped with with limes to no was profoundly assured ns folded and faulted so great was the last named mamed that ahat the quartzite and lial limestone estone en entirely disappeared under the more inore recent recant eruptive rock m asselto tho thea ease oas of the soviet fault SW seo accompanying compa nying maps and left the quartzite and li limestone mentone in in 4 the form of a lof lofty y precipice known as the deer trail escarpment to the southwest south west of prom From those aning fissure enormous madeda of rhyll rhyolite ito and ards birdseye birds eye porphyry oozed up tip from the earths melted interior ie gerior bior and formed mountvill monn tain masses thousands of feet feefe deep again the unstable crust quivered with intense tense Ui seismic forces the ephe old and bufa partially healed wounds were opened and now new fissures formed in tho the overlying mass and great dykes of 0 highly corp porphyry hyry now waric mark the be location sud and divio tion of those ancient rents cents the brief periods of gf com cocama ara tiva guieb which succeeded the tha previous aist was CONTINUED 0 PAGE 7 tl roea by another uplift of the range and along tho the central portion tx extending from gold south a 12 dist distance anoe of some ten miles a great frasure was tas formed from the d down downto to the region of liquid firs I 1 ree mighty foree force which split tho northern portion of the MV baldy range also formed lateral fissures Ax extending tending ba easterly casterly and westerly from icv tb great reat ceat central isid IT assuring of the phonolite hon olite occurred aud and in connection connect loii with other fissures already formed became channels for the upward bild catteral lat teral flow osgold of gold and sil ver bearing solutions extinct craters cra tors felds gelds fields of dark colored lored oo trach tra chite Ste ridges of volcanic breccia dykes and chimneys of obsidian in the phonolite prove that local Yol volcanic canie dorcea were continued over a aels aud and sot their wildcat traps araps for unwary ary investors the great mt baldy gold beatts bolac la forging to tho the front tho the magnificent roc ree ord of the annie laurie mine and mill in gold tho bodies of cyan cyaniding iding ore already ekpo expo exposed sod the th and reports of pilm erous intelligent Into lUgent mining jeaa men proclaim the fact that the annie laurie is almost without a peer on this con ww webster lobster lodemah its vast avast bodied of argonti foron galena the B W H Z and blue eargle group that have been steady shippers sine their discovery and numerous other promising prom I 1 ding properties B every very facility bor or economical mining such auch as plenty of water aud and power timber cheap supplies an enterprising railroad the B R G liv and telephone ser vioa investors luv estors c can certainly ee ba AV E PE CO U t A PA L a goo P k AN fa be I 1 ev 6 1 reca P 41 ti 0 I 1 A 41 iam off 0 4 OP 71 km tac t ic bet f V t R 0 F t PC aj 04 4 ap 01 I 1 A a 9 tiff V it C IE W 4 I 1 I 1 A G 40 dro S P aph 5 J ifs is S Is az pit taw DAI ik pa v Z 0 1 R YS VA L E V V F I 1 41 t 21 Z for COL 1 T r ip er P A to 1 e da r t I 1 ul C 0 Z 44 q F it ar T r 0 YI sn P Z e I 1 ta V 1 A e to dr all is NOW r W 1011 if of lip ES C oriba W q 1 6 V VS 4 4 A rent those flos urea became lines of easement for the vast mass masa of magma seek ng g egress and fro from m molten depths the hot bot g ageous thud alf owed upward and formed great dybes of phonolite hinh li wili today cb cheerily eerily tc links clink sk ud brider er the feet of an occasional prospector pro while the eruption of the pho iolite marks tho the last baab otis a throda of nature in the mt ML 87 y region su local long C period after the widespread wide spread eruptive activity had ceased THE PRESENT PRESE NM AND FUTURE geological conditions in evi dence along the northern portion of the B baldy aldy r range ange should remove every ev ery doubt ag aa to its ultimate greatness as mi mining niccy region gion indeed in the face of bit ter denunciation a and aad ad opposition oil from achasa of 1 ignorant i shysters shy that hold down 00 many chairs j lake rna ho 0 0 o the bluebird mine adjoining the annie laurie Js is also among the great atea t raines mines of utah in addition to the mines just mentioned there is a r score or more of groups of mining claims in m gold mountain that possess every indication of greatness in the vicinity of marysvale Marys vale yale there is apt that camons old aime producer the door doer trail with a million and a half dollars already blocked aitho oi atho tho ud and ask for no more than the mt baldy gold belt can caff furnish little or no prospecting has been done in the higher altitudes of the mt baldy range especially ally is this tho the c case as ew within I 1 t n the phonolite belt whore the in intense and other conditions are such as to warrant the statement that nowhere io in the entire west wast is there a no mew favorable field for careful A J |