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GEOLOGY. <br />The character of the oount <br />or banded granite intruded b ~ rook consists of e <br />point (aeddle) the y dykes of por gneiaeia <br />to those at Leadvilleerlying quartzites anal men At this <br />thus leaving the have been scored awe similar <br />may. readil granite,. The quartzites y by erosion, <br />at a higher altitude thanothetides sad lime measures <br />oP Buakakin Gulch, even <br />of the property,. <br />a fdasare principal vein is the Kentucky Belle <br />sli htl having a general strike of N, 300 ~•' same being <br />g y to the S, W, varying in vridth from 3 ~° d.ipping <br />with a general average of 4 ft, <br />, to 18 ft, <br />The vein cuts through a dyke, in ell probability <br />quartz porphyry, having an easterly and westerl <br />and width of about 40 ft „ as shown in No,l and <br />tunnels, y strike, <br />No,2 <br />tunnelAt a point about 300 ft, from the mcuth of <br />west side intrusion of gray porphyry comes in from~the <br />the presentadevelopmentsshowsg atth the vein, so far as <br />comprising ell of the vein matter,times•comi <br />°f gray por h r This intruationd <br />P y y seems to have been interrupted by the <br />dyke above mentioned, though the vein appears to be <br />subsequent to both, es it passes through the dyke <br />without any irterraptiott as to strike, width or values, <br />`r <br />