Show HE ma 0 BALDY 0 o i D I 1 t alt A magilie magnificent dicent WIN region e i 0 fl unsurpassed in its mineral resources awaiting only the magic touch of capital ca 9 ital to pour a golden stream into the laps of those possessing Intelli intelligence b yence and nerve i ait rising abruptly from the lesser er m mountains to the north the 1 greatel great r ga t M Ml L baldy range 6 enters cloudland cloud land traverses the boundary line between diute piute and beaver counties then onward to the south where it is cleft by the grand canyon of the colorado A BRIEF geological HISTORY the greit great mountain building forces I 1 so active during t the close of the tertiary age acre 0 worked on a scale alon along 0 the northern portion of the aft baldy range range the quartzite bedding 0 capped with lit limestone nesto lle was profoundly fissured folded and faulted so great was the last named oc currance that the quartzite and limestone ent entirely rely disappeared under the more recent eruptive rock masses to the vol 11 east of the sevier sevie r fault see ac ab ll 11 i I 1 compall yi maps and left I 1 ef t the A U quartzite and limestone 1 iri A the f form orm of a lofty precipice known as the deer trail es escarpment carp ment to the southwest of marysvale Marys vale from those yawning fissures enormous masses masse s of rhyolite rhyd lite and birdseye birds eye porphyry oozed up from the earths melted interior and formed mountain t masses thousands of feet deep again the unstable crust crusi quivered ered with int intense elise seismic forces the old and but partially healed wounds were ivere opened and new fissures formed in the overlying eruptive mass and great dykes of highly tn mineralized porphyry now mark the location and direction of those ancient rents the brief period of campara tive five quiet which succeeded the previous disturbances was continued on page 7 broken by another uplift of the range aud and along the central portion extell extending dinc from gold mountain south a dis distance talice of some ten miles a M great fissure was formed from the surface down to the region of liquid tire fire the binl mighty aty dorco which split the northern portion of the mac baldy gaii range c also f ormed formed lateral fissures extending basterl easterly Y and westerly fl from flom om the great central rent those fissures became lines of easement casement for foi the vast mass of ina imgana r crina 11 seeking in ecy egress D ress and from molten depths the hot gaseous ageous mud flowed upward and formed great dykes of phonolite which today cheerily clinks under the feet of un an occasional prospector while the eruption of colite marks the last ous throes of nature mature in ill the mt baldy region subsequent loc local al fissuring of the phonolite pho Iloilo nolito lito occurred cur red and in connection with other fissures already formed became channels ls lor for the ilio upward and catteral bastert lat teral ti ilow of gold old and sil ver bearing solutions s IS extinct cra craters tors fields of dark colored tra chite ridges of volcanic breccia ykes dykes 1 I and chimneys of obsidian in the phonolite life prove that local volcanic forces were continued over a long period after tho the widespread wide spread eruptive activity had ceased THE PRESENT AND FUTURE ceolo geological ZD ical conditions in a evidence along n the northern portion of the baldy rall range o should remove every doubt as to its ultimate ra greatness as a mining zi region indeed in the face of bitter denunciation and opposition from a class of ignorant shysters shy that hold down so many chairs in ill the lobbies of salt lake ho bo tol S mid and sot sat their wildcat traps for unwary investors the M great mt mb baldy baidy gold rold belt is forging to the front tile the magnificent 0 record of 0 f the annie laurie la urie mine minean and d mill in ci gold old mountain aln the vast bodies of cyaniding cyan iding oro ore already exposed the exam examination illation and reports of numerous intelligent mining men inen proclaim the fact that the annie laurie is a almost I 1 without a poor peer on this con chient the bluebird mine adjoining the aunie annie laurie lamie is also among 0 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 ever every y indication of greatness gre alness in the vicinity of marysvale Marys vale there is that famous old time producer the deer trail with a mill million conand and a half balf dollars already blocked out the bully boy and IN webster Tebster lode with wih its vast bodies of M aa galena g lena the B W 11 aud and blue eagle groups that have been steady shippers since their discovery and numerous other promising properties every fa facility clity for economical m mining such as plenty of water and power timber irber ti cheap supplies in an enterprising railroad the R G W an and d telephone service investors can certainly C BEA VER colnik M C aa 0 pk ph ilesi 4 1 1 1 V iii e v r tic Q T ip CIP n e e to ra arn M ot TO e act ilip 4 e P I 1 I 1 la 7 1 pis aej it fill 14 3 0 4 dop ile Z et C V 41 00 NV a IL 15 k 0 as e r 1 I dalton W 0 z t MAO e of arz ID Y A R Y sr VA L E ac j e bm 0 xa it t A 6 COL D eft 21 MOUNTAIN S 0 1 sel r A ar z 1 k J I 1 van f too to O r ga mitt gonima f R F pt 1 7 iz s a f 0 11 X 0 1 r 1 1 D ji U ek Z Z AD 4 C A de CY Y r Z z r agite eor eo r P kcf VO V e ask for no more than themi the talo mi mt baldy gold belt can call furnish little or no prospecting n has been done ill in the higher altitudes of the mt ml baldy r range ang in especially ally is this the case within the phonolite bolt where the intense and other conditions are such as to warrant the statement that nowhere in the entire west is there a more favorable neld field for careful andi intelligent prospecting |