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QEOLOCY. ~ ~ '~ <br />There is no good geological survey oY the district, r <br />The country rook ma be ~! <br />Y generally described as gneissic, or <br />banded granite, I'I ' <br />The veins are oY the Yisaure type, as usually understood, ~~ <br />Yollovring the cleavage joints, and in some oases the Yoliation <br />planes oY the gneiss, replacing the country rook on each aide i' ! <br />aY them, <br />The walls oY the veins are usually well deYined, i ~~~ <br />~s <br />The lodes possess a, high degree o3 parallellism in their k~ <br />strike or direction, their course with,but Yew exceptions, I ~f~ <br />being between due east and west on the one hand, and N, ~, and i i,~, <br />S. VP, on the other, The dip oY the lodes is generally at a ~ ~~~~ <br />high angle, but char~aing Yrequently with depth, <br />i j <br />~~~~I <br />a <br />l i <br />~~~ ~I~~ <br />~~~ <br />'~'' <br />i <br />,I <br />i <br />i <br />i ~ti '~~ 1i <br />I" tit <br />i ~I ~ Al <br />,,;.,. <br /> i <br />~,~.:: <br />