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<br /> <br />~. <br />~:: <br />;.:, <br />;~ <br />!~ <br />;! <br />~" <br />j ~, <br />'! <br />'' I <br />i <br />~; <br />s <br />I~;' <br />`~ <br />',i <br />;' <br />r <br />.'E <br />'~ <br />I~ <br />I <br />I' i'I <br />I <br />~, <br />I <br />I~ <br />I~~ <br />iii <br />~•i <br />,, <br />~~~ <br />~I~ ~~~ <br />6 <br /> <br /> <br />eRP~Ues. <br />_3eology. <br />There is a good ~o7=~¢allsurvey of the distric~. <br />QuaaT, #`~U. S, G. S. The structsm of theCoiint:ry <br />rock•ia coarse granite. The geological period is <br />Archean. There=aire'mimerons veins tRmning N. S. <br />Diipping to the tYest. The vein filling in the main <br />tunnel is Conglomerate schist and quartz:. The <br />enclosing walls are of granite, <br />P. <br /> <br /> <br />