| Location |
| NAD 83 |
49° 00' 00.00'' N, 119° 00' 04.00'' W
49, -119.001111
UTM: Easting 353638, Northing 5429385, Zone 11 (North)
|
| NAD 27 |
49° 00' 00.61'' N, 118° 59' 59.86'' W
49.000170, -118.999962
UTM: Easting 353718, Northing 5429183, Zone 11 (North)
|
| NTS |
082E02W, 082E03E |
| BCGS |
082E005 |
|
| Geological Summary |
ACCORDING TO LITTLE (1961), THE PROPERTY IS UNDERLAIN BY (TRIASSIC) METASEDIMENTARY AND META- VOLCANIC ROCKS OF THE ANARCHIST GROUP WHICH ARE LOCALLY INTRUDED BY GRANITIC ROCKS OF THE NELSON BATHOLITH. EOCENE SEDIMENTARY AND ACID VOLCANIC ROCKS OF THE KETTLE RIVER FORMATION OCCUR AS SCATTERED INLIERS AND OUTLIERS. EOCENE VOLCANICS OF THE PENTICTON GROUP CAP THE OLDER UNITS IN THE NORTHERN CLAIM-AREA. QUARTZ VEINS ARE PRESENT IN BOTH THE NELSON AND THE ANARCHIST ROCKS. PYRITE AND GALENA BEARING QUARTZ VEINS IN ANARCHIST GROUP ROCKS HOST PRECIOUS METALS. SEVERAL NORTHEASTERLY TRENDING, STEEPLY, SOUTHERLY DIPPING CONDUCTORS WERE OUTLINED FROM THE ELECTOMAGNETIC SURVEY.
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