Location |
NAD 83 |
51° 22' 00.00'' N, 123° 40' 05.00'' W
51.366667, -123.668056
UTM: Easting 453493, Northing 5690813, Zone 10 (North)
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NAD 27 |
51° 22' 00.32'' N, 123° 40' 00.62'' W
51.366754, -123.666838
UTM: Easting 453577, Northing 5690603, Zone 10 (North)
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NTS |
092O05E |
BCGS |
092O032 |
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Geological Summary |
THE PROPERTY IS UNDERLAIN BY A THICK SEQUENCE OF (CRETACEOUS) ANDESITIES, TUFFS AND MASSIVE FLOW BRECCIAS, CUT BY DIORITE DYKES. MINERALIZATION CONSISTS OF QUARTZ SULPHIDE FISSURE VEINS CARRYING GOLD VALUES THAT ARE DEVELOPED WITHIN THE FAULT STRUCTURE WHICH TRANSECTS THE DYKE SWARM. FOUR HOLES DRILLED FROM THE ADIT; NO MINERALIZATION WAS INTERSECTED NORTH OF THE WEST END OF THE LOWER ADIT. THE EAST AND DOWNWARD EXTENSIONS OF THE SHEAR SYSTEM HAVE NOT BEEN TESTED.
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