| Property Name |
Sunray
17106.pdf
|
| Location |
| NAD 83 |
49° 29' 29.00'' N, 121° 16' 05.00'' W
49.491389, -121.268056
UTM: Easting 625425, Northing 5483525, Zone 10 (North)
|
| NAD 27 |
49° 29' 29.26'' N, 121° 16' 01.07'' W
49.491462, -121.266964
UTM: Easting 625508, Northing 5483316, Zone 10 (North)
|
| NTS |
092H06W |
| BCGS |
092H044 |
|
| Mining Divisions |
New Westminster |
| Mining Camp |
Coquihalla Gold Belt |
| Title |
1987 Exploration Program 0n Sunray Group of Mineral Claims |
| Report Year |
1988 |
| Number of Pages |
19 |
| Statements of Work |
n/a |
| Affidavit Date |
1987-11-27 |
| Off Confidential |
1988-11-27 |
| Claims |
Sunshine |
| General Work Categories |
Geochemical, Geophysical |
| Operators |
Nicholson, H.
|
| Owners |
Nicholson, H.
|
| Authors |
Nicholson, H.
|
| MINFILE Nos |
|
| Commodities |
Gold |
| Work Done |
| Geochemical |
Soil |
158 sample(s); Scale(s): 1:1500 |
|
Elements Analyzed For |
Gold |
| Geophysical |
Electromagnetic, ground |
VLF; 2.2 km; Scale(s): 1:1500 |
|
| Keywords |
|
| Related Report(s) |
|
| File(s) |
17106.pdf
|
| Geological Summary |
Over 3/4 of the property is underlain by the Coquihalla serpentine belt made up of gabbro, micro-gabbro and serpentinite of uncertain age, which are in the Hozameen fault contact with the Spider Peak Formation massive greenstones and breccia believed to be of Lower Triassic age, and the Ladner Group conglomerate, wacke siltstone and argillite of Lower to Upper Jurassic age. Present work did not determine mineralization or exploration targets.
|
