Location |
NAD 83 |
49° 30' 00.00'' N, 115° 58' 04.00'' W
49.5, -115.967778
UTM: Easting 574740, Northing 5483553, Zone 11 (North)
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NAD 27 |
49° 30' 00.10'' N, 115° 58' 00.72'' W
49.500027, -115.966866
UTM: Easting 574808, Northing 5483338, Zone 11 (North)
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NTS |
082G05W, 082G12W |
BCGS |
082G051 |
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Geological Summary |
THE BAR PROPERTY IS UNDERLAIN BY FOLDED AND FAULT- ED PROTEROZOIC AGE ARGILLITE, SILTSTONE AND QUARTZITE OF THE ALDRIDGE AND CRESTON FORMATIONS. QUARTZ VEINS AND SILICIFIED ZONES, RELATED TO THE NORTHEAST TRENDING FAULTS, OCCUR IN IRON-STAINED PHYLLITIC ARGILLITE. A 1984 SOIL GEOCHEMICAL SURVEY INDICATED THAT SOILS ON THE BAR CLAIM ONLY POORLY REFLECT MINERALIZATION IN UNDERLYING BED- ROCK. ROCK SAMPLES TAKEN IN TRENCHES WITHIN STOCK- WORK AND SHEAR ZONES RETURNED LOCALLY ANOMALOUS GOLD (10.8 GRAMS/TONNE) AND SILVER (130 GRAMS/ TONNE) AND LOCALLY HIGH LEAD, COPPER, ZINC AND ARSENIC VALUES.
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