| Property Name |
Whitewater (Highland Surprise)
17158.pdf
|
| Location |
| NAD 83 |
50° 04' 09.00'' N, 117° 07' 33.00'' W
50.069167, -117.125833
UTM: Easting 490995, Northing 5546329, Zone 11 (North)
|
| NAD 27 |
50° 04' 09.12'' N, 117° 07' 29.53'' W
50.069200, -117.124870
UTM: Easting 491063, Northing 5546113, Zone 11 (North)
|
| NTS |
082K03E |
| BCGS |
082K005 |
|
| Mining Divisions |
Slocan |
| Mining Camp |
Slocan Camp |
| Title |
Geological, Geochemical, Geophysical Report on the Whitewater Project |
| Report Year |
1987 |
| Number of Pages |
278 |
| Statements of Work |
n/a |
| Affidavit Date |
1987-12-15 |
| Off Confidential |
1988-12-15 |
| Claims |
Defender, Grizzly Gold, Grizzly Gold 1, Howard, Lyle 1-3, Mayflower, PD, PT, Plato, Pluto, Revenue, Robin, Tetra, Whitewater 1-3, Wild Swan |
| General Work Categories |
Geochemical, Geological, Geophysical, Physical |
| Operators |
Abermin Corporation
|
| Owners |
Abermin Corporation
|
| Authors |
McArthur, G.F.
|
| MINFILE Nos |
082KSW032,
082KSW037,
082KSW058,
082KSW076,
082KSW077,
082KSW078
|
| Commodities |
Gold, Zinc, Silver, Lead, Copper |
| Work Done |
| Geochemical |
Rock |
365 sample(s); No. of maps: 2; Scale(s): 1:5000 |
|
Elements Analyzed For |
Silver, Gold, Copper, Lead, Zinc |
|
Soil |
251 sample(s); No. of maps: 1; Scale(s): 1:2500 |
|
Elements Analyzed For |
Silver, Gold, Copper, Lead, Zinc |
| Geological |
Geological |
2500.0 ha; No. of maps: 3; Scale(s): 1:2500, 1:5000 |
|
Petrographic |
19 sample(s) |
| Geophysical |
Electromagnetic, ground |
VLF; 54.0 km; No. of maps: 8; Scale(s): 1:2500, 1:5000 |
|
Induced Polarization |
2.5 km; No. of maps: 1; Scale(s): 1:1250 |
|
Magnetic, ground |
54.0 km; No. of maps: 5; Scale(s): 1:2500, 1:5000 |
| Physical |
Line/grid |
71.0 km |
|
Reclamation |
0.0 ha |
|
Road, local access |
7.0 km |
|
| Keywords |
|
| Related Report(s) |
|
| File(s) |
17158.pdf
|
| Geological Summary |
Triassic Kaslo Group greenstones and ultramafic rocks near the Whitewater Fault are cut by a quartz-carbonate shear zone containing sulphide veins consisting of pyrite, chalcopyrite, galena and sphalerite. The regional structural trend is 132 degrees.
|
