Show vagaries bodies rome maalo abe mirtala of not confining peta it 11 the that makes abe mint aej it shoo d b followed until it his been ploren beyond pera dyan tare abat it 11 tora ething more a blowout or a body of local extent many prospectors find an outcrop of ore on the fid or apex of a hill and bein an tunnel or they will dis bever cever the outcrop of what they assume t b a briz oro body and boing back on abe kill will bedim a shaft they expect to catch aba ore at so many fet bat they alume too at la not often abat tt ey prove absolutely abiol correct it the ore la not it almost invariably inclined inc linea one dav or the other and it prot more to attempt to catch it by interception than it mould to follow it it it is intended to catch it with a tunnel it is almot certain abat a longer tunnel will feleen reckoned upon diw athile tha or 1 lop a a vertical feat or the p and it may dip off ariy come a flat or if 0 local origin dineh out altogether and the came with the outcrops of what go in and develop into verticals br tol lowine tham the miner 11 taking advantage adran tage of abr and ho is vilely to cam oot a little infera nation y the of the ein that may brove valuable tn working if it pream worth working mining in the folding of the earth a crust by mountain and foothill were formed eang elnine and scientific ireba of july jtb Us fissures were opened tl at male veini and brorn arery main lode or mother via literals laterals late rals extend ai the branche of a tre from thee literals laterals late rals are emiller do not extend 0 o deep frequently finch out do not extend for feet alwang extend out eithur side of tl e main iod with both n all alike and can bardy be traced any distance I 1 en ever a vein in the lame cliine to feet and that course i tl e tread of the district it il in values to great depth or to primitive rocks where all it is bt bhatla vein nall lj an a contact to be valuable but a lie ground part cadier in a contact contac than Lleen liere here tl e larger fissure have occurred and the greater have been found to a greater fiona have ocum 1 in goine teina and bratten BC atten 1 the aro 11 s 1 as 1 ten caused ty a foi en naj of t I 1 f ire after the formation f it t a a 1 a inflow of gomeck tl livan n t rail an I 1 rite but ll 11 H any t dac it r s I 1 a 11 tiia w in lace an 1 bit n tl re iular wall |