|
Mineralized Zones: EklandEkland Ridge is one kilometer due south of Lorraine. The NW-trending ridge parallels the Lorraine ridge to the north and shows similar styles of alteration and mineralization. Several holes were drilled on Ekland Ridge in 2004 with some high-grade intersections of copper mineralization cut off by faults. The ridge has very good outcrop exposure and was an area for detailed lithology and alteration mapping in 1996 and 2006 to study and record alteration-mineralization relationships.
Drill Results
| Hole No. |
From (m) |
To (m) |
Intercept (m) |
Cu (%) |
Au (g/t) |
Ag (ppm) |
| 04-85 |
No significant intercepts |
04-86
including
and
and |
23.43
28.6
32.61
34.4 |
26.52
30.47
34.4
37.27 |
3.09
1.87
1.79
2.87 |
0.13
0.15
0.23
0.16 |
0.11
0.02
0.06
1.07 |
-
-
-
-
|
| L96-39 |
3.00 |
11.30 |
8.3 |
2.056 |
0.94 |
18.4 |
| L96-40 |
11.30 |
23.50 |
12.20 |
0.280 |
0.66 |
2.3 |
| L96-41 |
1.50 |
29.80 |
28.30 |
0.278 |
0.00 |
1.8 |
| L96-42 |
1.50 |
17.40 |
15.90 |
0.285 |
0.04 |
1.9 |
| |
