| Location |
| NAD 83 |
50° 37' 59.00'' N, 127° 40' 06.00'' W
50.633056, -127.668333
UTM: Easting 594176, Northing 5609867, Zone 9 (North)
|
| NAD 27 |
50° 37' 59.49'' N, 127° 40' 01.22'' W
50.633191, -127.667005
UTM: Easting 594273, Northing 5609665, Zone 9 (North)
|
| NTS |
092L12E |
| BCGS |
092L062 |
|
| Geological Summary |
THE UPPER TRIASSIC AND LOWER JURASSIC SEDIMENTARY AND VOLCANIC SUCCESSION OF THE VANCOUVER AND BONANZA GROUPS, RESPECTIVELY, AND THE JURASSIC GRANODIORITIC ISLAND INTRUSIONS UNDERLIE MUCH OF NORTHERN VANCOUVER ISLAND. NORTH OF HOLBERG INLET THE SUCCESSION STRIKES APPROXIMATELY WEST- NORTHWEST AND DIPS GENTLY SOUTHWARD. FROM SOUTH TO NORTH THE FORMATIONS ARE (1) BONANZA VOLCANICS ANDESITIC TUFFS AND FLOWS UNDERLAIN BY (2) PARSON BAY CALCAREOUS SILTSTONE WITH INTERBEDDED SHALES AND ANDESITIC AND CHERTY TUFFS, UNDERLAIN BY (3) QUATSINO LIMESTONE AND (4) KARMUTSEN AMYGDALOIDAL BASALT FLOWS. THE ROCK UNDERLYING THE APPLE 1 CLAIM APPEARS TO BE BONANZA VOLCANICS ANDESITE TUFFS AND GRANODIORITIC ISLAND INTRUSIONS.
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