Location |
NAD 83 |
50° 17' 29.00'' N, 126° 49' 36.00'' W
50.291389, -126.826667
UTM: Easting 654806, Northing 5573289, Zone 9 (North)
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NAD 27 |
50° 17' 29.46'' N, 126° 49' 31.35'' W
50.291516, -126.825374
UTM: Easting 654903, Northing 5573087, Zone 9 (North)
|
NTS |
092L07W |
BCGS |
092L026 |
|
Geological Summary |
THE CLAIM IS UNDERLAIN BY UPPER VANCOUVER GROUP SEDIMENTS AND PYROCLASTIC VOLCANIC ROCKS OF THE LOWER JURASSIC BONANZA GROUP, INTRUDED BY GRANO- DIORITIC ISLAND INTRUSIONS. MINERALIZATION IS STRUCTURALLY CONTROLLED ALONG A SHEARED FAULT ZONE AND ITS SUBSIDIARY SHEARS. SULPHIDES, PREDOM- INANTLY SPHALERITE, OCCUR SPORADICALLY WITHIN THE SHEAR ZONES. THE HIGHEST GRADE MINERALIZATION HAS A STRONG ASSOCIATION WITH CHLORITE.
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