Location |
NAD 83 |
51° 32' 00.00'' N, 120° 13' 35.00'' W
51.533333, -120.226389
UTM: Easting 692367, Northing 5712783, Zone 10 (North)
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NAD 27 |
51° 32' 00.19'' N, 120° 13' 31.03'' W
51.533386, -120.225285
UTM: Easting 692449, Northing 5712574, Zone 10 (North)
|
NTS |
092P09E, 092P09W |
BCGS |
092P059 |
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Geological Summary |
THE PROPERTY IS UNDERLAIN BY A NORTH TO NORTHWEST- ERLY TRENDING SEQUENCE OF LIMESTONE, SHALE AND SILICEOUS ARGILLITE OF THE (UPPER TRIASSIC) NICOLA FORMATION AND BASALT OF THE (DEVONIAN TO PERMIAN) FENNELL FORMATION. THE MAJOR, NORTHERLY TRENDING, STRIKE-SLIP(?) LOUIS CREEK FAULT JUXTAPOSES THESE UNITS. MINOR FELSIC DYKES CUT THE ROCKS. A GOLD- ARSENIC SOIL ANOMALY WAS OUTLINED FROM GEOCHEMICAL SAMPLING AND IS ASSOCIATED WITH EASTERLY TRENDING, PYRITIC, QUARTZ AND CALCITE-FILLED FRACTURES IN ALTERED FELSIC DYKES IN THE LOUIS CREEK FAULT ZONE.
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