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3:.; <br />i l '.:' <br />Fj.';a <br />Ft ':' <br />F .. <br />J <br />~k <br />J <br />1 <br />t <br />} 1 <br />9 <br />1 <br />i <br />r <br />• I!. ,~ ~I <br />~! <br />~i~ . <br />II . ~ I.!, <br />..p ii <br />~ai~ <br />Is.l ri <br />„G <br />j;; ,, <br />`; <br />~I I.. <br />~I~ <br />! !I <br />1' <br />'; q <br />;~. <br />!:.. <br />. i~ <br />ri <br />„~ <br />~~ ~~~ <br />., <br />~; <br />~;~ <br />~~~ <br />~, <br />~~ <br />,, <br />., ; <br />~. ,, <br />9. ~. <br />~,. <br />~. <br />ii I <br />~, <br />,; <br />,~; <br />~~ <br />Ili <br />4 ORE 80DfES AHD ORES. <br />is frequently found in the western tr.rritory in close proximity to <br />I <br />the shales. <br />The general course of the ore bodies is 11.26° P. with varying dips <br />though wort of the rich bodies have been practically verticnl. <br />T$e width varies from a fert inches u p to 30 or ~0 ft. <br />_Tn nlny places stringers of ore me followed off .into the ,dolomite <br />and it is from these strin};e:•s thnt a roaside:•able toznagc is derived <br />by leaser.^.. <br />All noe is smelting and riilling. <br />A good tre::tweut is effected by ti:e star.lte±•s owing to the large <br />percentage of lime contained in r.:ast of t};r ore. <br />See :?purr's Llonogrnp}•. ao. XXI Pages i1o.153-1F0. <br />• <br />