Show rim arl I 1 BAL 11 Y A ia ci cwi LD bal al I 1 incel t R uw H T a rm paoa aisea ll 11 ts M harn 1 eno gir awaits awa I 1 ot I 1 H g only ohly th e magic touch of capital capita to pour par tt a gown golden stream aminto into tiie laps r of those possessing 0 ibid airl iAd wv YVO from mhd lesser mountains to tho the north the t peat great mf alt baldy ran range 0 on ers cloudland cloud land traverses thorbun tha d dary try line between pinto and deaver beaver counti esthen onward to tho south where it is cleft clef t by tho grand canyon of the gol rado ado i A HT ST Y the great mountain in building dorcess for cess active during ahe 0 close j G of the tertiary age work worked edon onti x scale along thu the aj 0 ahern portion of the mt hit baldy range arzan e the quart zite 4 ate bed din ding capped avit with I limestone 01 was a 3 pi profoundly fissel ed fa folded id e and I 1 faulted aulten so gred greab g reab was tl thi las ast named ranco that tl ohp q quartzite quartzite uart zite and a nd limestone entirely entire fly lv d is app appeared oared under the ino more lle i 1 x cent arup to th enst of th the S ovier fault companying compa p nying maps and loft of t the quartzite zite and limestone Jim estone in i n the form of a t lofty pr precipice e capice lano known n asuno e trail ail escarpment E to tho the southwest of marysvale Marys vale from those yawning cr fissures enormous masses of rhyolite 1 and birdseye birds eye porphyry oozed up from afie the eartis earths melted interior and formed mountain masses t thousands hou sands of feet deep again t the io unstable crust quivered 04 with intense seismic seis mic forces the old aud and but partially healed were opened and new fissures formed medin in the overl overlying yina a and great dykes of highly miner mineralized porphyry bowmark now how mark the location and diorec ah tion of choso ancient rents the brief period of live qu quiet iet which succeeded the abo ar brevious or evious disturbances was W N PAGE 7 broken by another uplift of thorance th the range orange and and along the central portion extending from gold mountain south a distance of some ten miles a great fissure was formed from the surface down to the region of liquid fire the mighty force which split the northern portion of the mt baldy ran range rane e also formed later lateral al fissures extending easterly and westerly vv sterly from the groat great central fissuring of the phonolite occurred and in connection with other fissures already formed became channels for the upward and catteral lat teral flow of gold old and sil ve solutions extinct craters fields of dark colored tra chite ridges of volcanic bre breccia accia dykes and chimneys of obsidian in the phonolite prove that local volcanic forces were continued over a j idels and sot their wildcat traps jor for unwary investors the great mt baldy bald gold belt is forging to the front the magnificent record of the annie laurio laurie mine and mill in hi gold mountain the vast bodies of cyaniding cyan iding ore already expose exposed the examination aud and reports of numerous intelligent mining men proclaim the fact that the annie laurie is almost without a peer on this con webster lodo lode with its vasto vast bodies of galena the B W A H and blue eagle groups that have been steady ship shippers pors since their discovery and numerous other promising proper properties tiei E every very faai facility lity for economical minin mining such as plenty of water and power timber cheap supplies an enterprising railroad the E R G W and telephone service investors can certainly 7 0 4 ta e cw df 0 ac L ca I 1 awn fur 04 8 ck ee kit I 1 C ot P T az 0 e a va 4 to A ar n ra T E e J V 0 ate h it a fit lots I 1 4 e ep fl Z lt 7 off ct I 1 10 11 af jile ab A N is S N I 1 S L 44 ell d e ok lot it e a C at ne INC J az 10 s S Y is f p J A alro I 1 ta MAP azmi V of S ei p 1 1 I 1 0 MARYS VAL E ac 4 A f W 1 4 I 1 rini 0 A A 11 aj I 1 vola it M 0 TA ia PV t PT ar vl T CL e A V 0 R del e I 1 4 t V Z Z 0 0 1 I 1 to X U 1 U 10 ev N v G r 00 lit A ml Demy k Y 44 6 L fsr e eo DiSt d e jenec ent those fissures became nes lies of easement for the vast mass ass of magma magina seek effig ig ogress egress and from molten I 1 aptha the hot gaseous mud wed upward ind and formed great I 1 lies es of phonolite which today eerily clinks under the feet an occasional lonal prospector while the eruption of the pho alite lite marks the last s throes of nature in the mt ady idy region subsequent eVent local omi M long period after the widespread wide spread eruptive activity had ceased THE PRESENT SENT AND FUTURE geological conditions in evidence along alona the northern portion of the baldy range should remove every doubt as to its ultimate greatness as a minin mining region indeed in the face of bitter denunciation and opposition from ablass of ignorant shysters shy that hold down so many chairs in the lobbies of salt lahe ho the bluebird mine adjoining tho the annie laurie is also among the great mines of utah in addition to the mines just mentioned there is a score or more of groups of mining claims in gold mountain that possess C very every indication of greatness in the vicinity of marysvale marys vale there s that famous camons old time producer the deer trail with a million mill ion and a half h alf dollars already blocked out the bullyboy bull bully yb boy and j gr j ask for no more than the mt alt baldy gold belt belac can furnish little or no prospecting has been done in the higher altitudes of the mt baldy range E especially s ally is this the case within the phonolite pho nolito bolt where the intense and other condi conditions eions are such as to ivarra warrant nV the statement that nowhere in the entire west is there a more favorable field for careful calef ul ankle intelligent prospecting prospect illg |