Show APEX AND SQUARE LOCATIONS an exhaustive article bearing on these much mooted questions worth reading k 1 II 11 e apex law and squirt in the V s n 1 s iff r f ban I 1 jail lolli 11 ere appears in arilde on tins subject it at I 1 did not exi let to see in tl at i aper it is evl dently alie effort of a tenderfoot or al one not at all i osted on u at lie Is t liking about lie says tic greiler portion of ins out of lie ilex and side lines 01 its equia equiv ilent I 1 deny his ibid it e remedy of square lo 10 would bo far tonii 11 a lis eist 1 list in tl e lo 10 calion it auld baill 1 ive lines nid I 1 eipl tl e disi alts ts to e aid hirai biot be lessened hen I 1 eddville eid ville was opened opined t t w as boffi found tl i 1 tl 0 ore bodies aers lying oui ir II 11 ere la ri illy no ai ex ind leadville la in tint dai exception to most mining cm is fin aire loc ilione for lint 1 inc ike coun ly t bo acht ibliss ed is ti erule tl at mines ai 4 are folind in a id dai 1 ing sir atas ali it adt fon nations are looked at or prospected hut hie 11 nere not etith c the remedy where deeded they guarnier guar nied b lt I ake s to beg influence to the united and mike square lo callons rule 1 his w 0 miners of utah ind 1 yn HIB cu idt our mines 1 ere no to alie deci and VM do not hive to follow 11 e next county to att del ali for the or jil aith tl in and vicinity h biad any uw sult sIs tl ereio als buteas to have they dia n 1 tapirs nead not apply y old antver opar ie id and other veins or lodes 1 occur ns 1 rocki more or less metamorphosed with a dip from one quarter i itch to tho vertical I 1 ere they occur in one formation they are stratified bed veins en they get down to another forma aton siy quartzite they are contact tins w hen they get dow n to the tonic rocks and syenite they illy become vertical and ire then fissures peri aps all veins at depth become fissures or in other words all other veins mi come aiom tissue e abc not discussing or e orles but stating facts known to exist biow with veins having a dip from the of a root to the of the house which has no dip as dip or pitch can only be reckoned from tl e hoD to tl e vertical an angle of ninety degrees or t a fourth part of a circle lit li t us see 1 ow sq lare locations would apply ou take up a location COO by 1 00 feet discovery and apex in 11 e center strike or co use of vein with tl e claim longi tudin illy and dip a 1 alf or 4 degrees at six hun decd feet in del th tl is vein passes on F ou ow U s vein show a ore assaying ounces silver and 60 per cent ie id it Is in a district wl ere water is abundant and hoisting and pumping machinery are necessary alter tl e first hundred feet a plant of worth of ma cl anery before alie mine can be exploit ed aid made to pay oil er parties own the ground on edtl er side of you but they have no discovery apex or vein aliey have only to sit down lie so many jac kalls until vou pass your ver side line into their ground hat capitalist would invest in this kind of mining he would be compelled to a county of side lines liow ever well benned denned 1 is vein might be here then is your side line remedy f if you are not fortunate enough to locate ide ground to cover your vein n depth ou must purchase if fortun ate enough to fand men alongside of ou who ivill sell at reasonable agures it is of no benefit to the miner himself as he must take up and do assessment work oi dead ground ai order to have something to attract capital in teresta are mutual tie mine owner must have title to 1 is ground in depoli it therefore verti call side lines and sq baie locations would not benefit either the prospector or tl e capitalist lie must locate or purchase ground enough to hold his mine in six hundred feet wide Is enough surface TO HOLD A SUM provided as now ou lave a right to follow it on its dip always at right an g es to its strike or course it is not worth alile to multiply examples or waste words the case is too plain BOW as to tl e apex of a mine about seven years ago more or less the A ing ai d S u called for a definition of the term apex over thirty answers returned from mining experts all more or less definite but differing from eacel oilier in some 11 ey agreed that tte ai ex is wl ere alie vein crops in tho surface but differed s to how the vein should get tl ere or rail er alie proof of its connection with under gro ind workings here a vein crops at the surface between walls j r i s A J kuell bleik or change of dip no dispute would ok cur hut alen is a break or a i er manent change of dip with oil er parallel veins spurs or shoots in the immediate vicinity then comis the ditl culty and even bonese scientific may differ wl ere a whole lull is mineralized and full of g ish veins sl and spurs as to wl ich is tl e main vein and which is alie spur wl ich best conforms to alie general dip of tl e vein and to the strata in which it lies or i is it cl anaed to a fissure vein ind Is it cutting the aliota even IB stratified formation have for short dis ta ices much alie 13 A veini I 1 would neill er ask nor answer such a question in this place it miners and mining men only were supposed to read jui but here are lenty of people who do not under stand 11 aning phrases A true esaura s a vel n tl at cuts foi motions or crosses tl em at various angles J 1 at is lode t of dip strata or strike of for motion ahat is a cleft through for lations and independent of them if it has occurred since secondary forma ions acie del it is probably pio bably due to or earll quake action bieri they are only superficial and of length in strata it would bo safe to say they ire gash veins eliat oc w in the side walls oi aiom one lei vein to another particularly if the continues below the tp parent if emiitt tinker 11 e mining lw it I t it be tl posted like art teller and colt tl ey will not change litts tl athayde worked well since the acquisition of 11 0 1 baates ind i from bpi 0 o tl ingims chai awl net angad by statute x d inifi g them was t eliw of foltting our mine to jail 13 91 |