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The trail-clearing crew working at the north end of the claims approximately 2.5 kilometres north of the camp.
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The sampling crew with the concrete drill used to extract a representative, non- weathered sample of the iron-titanium mineralization.
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The sampling crew extracts sample "N3" from the "core" barrel.
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The re-established trail from the camp to Medallion's optioned claims. Geologist Eric Hurtubise is with Project Manager Hector Blake to the right.
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The Quebec Iron & Titanium Lac Allard mine (QIT is owned by Rio Tinto plc), that lies three kilometers to the west of the claims optioned by Medallion.
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The crew illustrates the south boundary of Medallion's claim.
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The QIT ore-loading facilities at the deep-water port of Havre St Pierre, Quebec, which is on the north shore of the Gulf of St Lawrence. Havre St Pierre is 40 kilometres to the south on the claims optioned by Medallion.
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Office tent and cook tent (blue roof) at Camp Medallion. Cook is in his whites.
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Geologists Eric Hurtubise and Sarah-Jeanne Morin at work in the office tent that also serves as a dining hall. Office is equipped with satellite phone fax and Internet.
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Geologist Sarah-Jeanne Morin with an old drill-hole marker (from the 1968 drill campaign).
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Bill Bird at a second old sample pit in the iron-titanium mineralization along traverse "L".
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Bill Bird at a contact between the iron-titanium mineralization, at upper right, and an internal block of anorthosite waste rock. The mineralized rock and the waste are easily differentiated and the contacts between the two are sharp.
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Bill Bird and Hector Blake examine sample "N3."
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An old sample pit in iron-titanium mineralization along traverse "G", which probably provided material for the metallurgical tests conducted in the 1960's.
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Iron-Titanium Mineralization.
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North End of the Mineralized Zone Where U of T Study Samples Were Taken.
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Hector Blake holds the flag at sample site "G1". Two sample holes were drilled at each sample site. The iron-titanium-bearing mineralization crops out throughout the project area as a smooth, rusty-brown rock.
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Bill Bird and Hector Blake at a newly discovered outcrop of iron-titanium mineralization, well north of the area of historical mineralization. This new area of mineralization could add considerable tonnage to the iron-titanium resources.
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A photomicrograph of tan ilmenite (FeTiO3) with white hematite laths (Fe2O3). The dark brown material is made up of the gangue, or waste minerals feldspar and pyroxene. The field of view is approximately 1.35 millimetres.
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The Romaine iron-titanium mineralization intersects Lac Puyjalon at the waterfall and crops out continuously for 3 kilometres to the northeast. Medallion's 23-square-kilometre claim block lies between Lac Puyjalon (right) and the two lakes to the west.
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