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2 • i:i i ': <br />E' ` <br />_ .., t $ozacadxcra t}-savyli tho slide rack. Fsapecfally aouid thin be true, in the early ' '^ <br />~' <br />.all zrhen all of the snow and ice on surface hsd disappeared. Qatar howevery is i " <br />~.; <br />. ...: t this seaaan of the year a aissing but a xmach desired quantity in this section, <br />~~ <br />} <br />ermdatioa is also aided by occasional saowslSdea in wiater sad water spouts in <br />t, <br />;_., er, Rach of +ehich contribute their quota to nature's levelling process. s; <br />i ;I <br />3otsithstsading the great amount of LAas}zR or slide rock present the pros- t! <br />s! <br />-; _, ectox'a lx3vo aucceedeu^ in finding sad locating a aerfee of ors veins that are <br />-\ <br />r: t}weir occurenee Sntesestin;;, intricate and partially demonstrated tfi be reaxtn- <br />relive. dearly every foot of available territory is the basin is located either 4 <br />a lode claim or placer, anG of this a greater nartion i-as been developed suf- '_j <br />_ . _ s;~ <br />iciest to procure iJnitec' States Pat eat. ,early all fissursa.,contain ve1aE, .' ~~!~ <br />s a rustle's a[ fact all fissures examitzed Sn this section were found P121ed with ;' <br />eins, a~.d a great proportion of the veins to be ors veins. ;" <br />j'~, <br />y, <br />The fissures rsn at all pelota of the coswasa, and if viewed from the ~' <br />~i <br />tandpoint of locations and openings upon same would appear to be without system. <br />_ ~~'i <br />f hovevers viewed froFn the standpoint of containing are veins carrying °pay° , <br />III <br />here is a call developed ayutem of Wort}rweat anc south-east fissures. uy nortix- <br />s I <br />cut cad south-cast Ss saaant to include fissures haviry; a course ~.~rithin tho points 3' <br />~i <br />r <br />. f Wort}: 26' an4 5° seat. As auly fissures carryiz~; ore veins will be neationed !' <br />hhe term vein Pill be used in the sense of as ors vein unloss otherwise spsaified i, <br />tt the preseni tSine all veins being ssar'kod t}:at yield pay ors, coma c~ithin y~ <br />the razu;eaf the narth~xest -south-oast system ms above designated. The veiae ~~ <br />~~ <br />r„ost prominent is t}:Ss system are as Yollawe: The :w~ggier-UnSon~->haridan-Alsum- ,?Ei <br />e>s <br />~~ <br />ljar~ oa tka soaat}x~rest side oY basin. The Cirearran-Columbia next north-east. ~' <br />Then in ar8sr namer}, the Gold Bug.-~$fi, Th0 iifg }"J,ephatit-Aswant3no~ Tyre S7ha1e, G <br />-~ <br />'JSrglaAus-_Japan.~Clisaax~ 3daraiz~r Fl'us~a~ Tk'e Zraa _Uaaidantal, Tlae Towbay.-Eel- <br />-,.; ,. ~' <br />I~ 'v <br />wort. fpthzr veins exist t},at might propesly be included, but lima would .i-st per- I <br />1' <br />mit little bayar~d a pasain, aatiae oY their existence. 1' <br />ij~ <br />~~ <br />w.~»-. <br />f' <br />1 <br />