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Visible gold in quartz vein from CL101 at 89.25m downhole. Host rock with minor pyrrhotite and arsenopyrite. Clan Lake Property |
Same sample from CL101 at 89.25m downhole showing visible gold. Clan Lake Property |
visible gold and pyrrhotite in quartz vein from Clan Lake Property |
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Breccia 1: Mineralization in the Ormsby Zone occurs within a hydrothermally altered volcanic breccia. |
Breccia 2: The hydrothermal breccia is variably silicified, carbonate and sulphide altered |
Glacial striae: Very well developed glacial striae mark the metasedimentary rocks at the Ormsby Zone |
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Minerals: Intensely altered Duckfish Granite underlies the BigSky Property with galena and fluorite. |
Pillows: Well formed pillows near West Zone. |
Pillows 1: Intensely stretched pillowed mafic volcanic rocks at the Bruce Lake Zone appear weakly foliated in plan but strongly lineated in section. |
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Pillows 2: Same pillows as shown in Pillows1 reveal hydrothermal brecciation apparent in cores but not selvages. Note garnet development in pillow selvages. |
Teapot 1: Extensive silica-flooding in metasediments occur at the Teapot Zone. |
Teapot 2: Another view of the Teapot Zone with a trench in the middle ground. Area was burned in mid 1990’s when forest fires swept though the area. |
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VG2 NDM236: Visible gold in a pyrrhotit-bearing quartz vein in diamond drillhole NDM236 on the Ormsby Zone.
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ZonedPorph: Zoned plagioclase phenocrysts in porphyritic phase of the Duckfish Granite, BigSky Property.
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Ormsby: View of the Ormsby Zone with the camp and Giauque Lake in the background. |
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