Location |
NAD 83 |
50° 37' 29.00'' N, 127° 31' 36.00'' W
50.624722, -127.526667
UTM: Easting 604213, Northing 5609130, Zone 9 (North)
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NAD 27 |
50° 37' 29.48'' N, 127° 31' 31.23'' W
50.624856, -127.525343
UTM: Easting 604310, Northing 5608928, Zone 9 (North)
|
NTS |
092L12E |
BCGS |
092L063 |
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Geological Summary |
THE AREA IS UNDERLAIN BY THE UPPER TRIASSIC TO LOWER JURASSIC AGE VOLCANIC AND SEDIMENTARY SUCCESSION OF THE VANCOUVER AND BONANZA GROUP, AND A DISCONTINUOUS CRETACEOUS AGE SEDIMENTARY COVER. MID-JURASSIC GRANODIORITIC STOCKS (QUATSE STOCK), AND QUARTZ-FELDSPAR PORPHYRY DYKES CUT THE SUCCESSION. HYDROTHERMAL ALTERATION AND MINERAL- IZATION ARE ASSOCIATED WITH PORPHYRY DYKES IN BONANZA TUFFS. THE SUCCESSION DIPS GENTLY TO THE SOUTHWEST. FOUR PROMINANT FRACTURE DIRECTIONS ARE PRESENT ON THE PROPERTY AT 020 DEGREES, 060 DEGREES, 090 DEGREES AND 130 DEGREES. THE DYKES ARE PRESENT ALONG THE 060 DEGREE AND 130 DEGREE FRACTURE DIRECTIONS.
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