he 2011 exploration program consisted of prospecting and rock sampling to confirm the presence of hematite bearing horizons to the north of Lac Connelly.
The first hematite bearing horizon was traced for 2.5 kilometres along a northeast strike, with a minimum width of 30 metres.
The second hematite bearing zone is located 1.5 kilometres to the northwest of the first horizon and was traced for 1.2 kilometres along a northeast strike, and based on preliminary mapping is at least 50 metres wide.
A total of 96 grab and channel samples were collected during two separate site visits to Lac Connelly. On average the samples returned 56.8% Fe203.
Under microscopic examination the rock samples collected consist of coarse grains of hematite and quartz that are not intergrown but rather appear to form separate grains.
There was no drilling at the Lac Connelly property to enable estimation of the DSO (direct shipping ore) potential for a mineral resource.
It is recommended that drilling be initiated in the near term to delimit the actual extents of the iron formation in the Hematite rich DSO zones outlined by the field prospecting and sampling programs.
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