Show 00 oo ALONG THE MT GOLD BELT BE LT edoo 0 o 1 to WI W oil IIA 4 marcale Ma ea i B i fl u awl W moo ai wimp fill 0 Im if the she missourians Missour ians will push the aldebaran an iho ve of his depar taire lt or mis king received word arom emny the aldebaran A ill ao 10 energetically pushed luring during the f gvinter and instructed him to provide larger quarters qu arlera iw for ahe men to build gild in overy every way provide dor ii the present condition of the alde hinau arau fully autly justifies the efforts clay people to developed dev elope a t manager john Ritan 4 bas u gold the 11 tc of one of dr pierces P P pellets Pelle tg tF with several balver buttons which he be I fl sa safely fely in spill a pill phial and proudly exhibits to intimate friends as ile lubit ablo evidene evidence that aldebaran Aldeba rau acock carries hie real stuff the permanency of the aldebaran Aldeba Alde balan rau contact leonta et is beyond question the lo 10 is ia unusually interesting and is untitled yn tn titled to brief discussion I 1 A glance at tile the map on page seven 1 aboda athe the wilt fault trending easterly and westerly rou alrh Brig brigham harn path park k extending northerly a s another fault line illie now occupied by au extensive purphy ry dyke the faults a intersect caa each h 1 other in the vici mity of cottonwood creek I aud and produced interesting effects to the west of and of lithe creek ds V a great block of quartzite which re mains in almost its ita horizontal position it I 1 is s capped with avith lime which v in turn is capped eappen with rhyolite A eveln ewein ore occurs bithia the tha con tact but unfortunates V a fossil shore 1 I liue on the has cut off tile the ore iu im ithac direction the break in the quartzite extend ian ug northerly lind southerly through h park enabled the cottonwood fault to tilt the quartzite in the i vicinity ot of the he aldebaran aldemar an sharply to the south without wore more than slightly ehg ally disturbing the section to the west of Abe the Park fult this local feature has bas givel to the aldebaran an altri almost ogE vertical coti contact tact of quartzite and limestone lime the latter having been intensely altered by the subsequent intrusion of porphyry within the contact aud and thereby fur ii heat and acid for the bious aud very likely the gold g old with the solutions wore were charged the proposition is this thia the alde ababan contact being branig v vertical er will go lown to the depths and there is no doubt that the same saine which Ae deposited posited ore in the present wor workings icings raoof the contact were even moro more active aud and richer hundreds ot of feet bs be bow further the tunnel reach sa in to the hill the less leas broken la Is ahe quartzite and ore IP ia more aban adsa 40 t tau d The rc is no waa man living no ler how expert a shyster ghyst ar lie way may be b tile the cherew drawn from condit conditions ious in the vicinity of the aldebaran proper berty ty 1 tile the belt far concoct A extel o ake si ie in its westerly w ester ly course it enters the park garft group chenco turns lurus bouth wester y j thence oaut herly and can be traced by where the contact is coveted by the erupt eruptive ivo overflow overl low the aldebaran was ans located some four deurs sigo ago by bya B T I 1 ashby prel ent bupt supt of the property y and nd to ills his admirable credited alj hie b results which have very likely showed those missouri people tho biond to wealth |