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The gold mineralization in the Main Zone occurs in several sub-vertical, northeast-trending lenses measuring between 2 and 35 meters in horizontal thickness.

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The Windfall Lake property occurs within the Urban-Barry Greenstone Belt located in the eastern part of the Abitibi Subprovince.

The Urban-Barry Greenstone Belt has an east-west extent of 135 kilometres and is 4 to 20 kilometres wide.

The Windfall Lake Gold project is located in the province of Quebec, approximately 200 kilometres northeast of Val-d’Or and 115 kilometres east of the town of Lebel-sur-Quévillon and is accessible year-round through a network of well-maintained logging roads (Figure 1).

The property is located north of the 49th parallel and is subject to the provisions of the James Bay and Northern Quebec Agreement executed in 1975.

Osisko Mining is currently the largest stakeholder in the Urban Barry Greenstone Belt with over 40% of the land staked.

At the Windfall Lake deposit, the volcanic stratigraphy trends to the northeast and dips moderately towards the southeast.

Preliminary metallurgical tests indicate a gold recovery of 95.7% using a standard gravity and flotation circuit, followed by cyanidation. Mineral Resource Statement (From SRK Consulting, November 13, 2014).

Reported at a cut-off grade of 3.0 g/t gold, assuming an underground extraction scenario with an assumed gold price of US

At the Windfall Lake deposit, the volcanic stratigraphy trends to the northeast and dips moderately towards the southeast.Preliminary metallurgical tests indicate a gold recovery of 95.7% using a standard gravity and flotation circuit, followed by cyanidation. Mineral Resource Statement (From SRK Consulting, November 13, 2014).Reported at a cut-off grade of 3.0 g/t gold, assuming an underground extraction scenario with an assumed gold price of US$1,200/oz and metallurgical recovery of 96%.The bulk of mineralization averages ~10 g/t over 5 metres, with very high-grade pockets up to 248 g/t over 12.4 metres in some areas.Drill holes in the gold zones demonstrate good grade distribution along the entire mineralized interval.The distribution of the pyrite stockwork is greatly influenced by the geometry of the dikes, specifically for Zone 27 and the Caribou corridor, which are spatially associated with 2- to 30-metre thick northeast-trending porphyry dikes.

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At the Windfall Lake deposit, the volcanic stratigraphy trends to the northeast and dips moderately towards the southeast.

Preliminary metallurgical tests indicate a gold recovery of 95.7% using a standard gravity and flotation circuit, followed by cyanidation. Mineral Resource Statement (From SRK Consulting, November 13, 2014).

Reported at a cut-off grade of 3.0 g/t gold, assuming an underground extraction scenario with an assumed gold price of US$1,200/oz and metallurgical recovery of 96%.

The bulk of mineralization averages ~10 g/t over 5 metres, with very high-grade pockets up to 248 g/t over 12.4 metres in some areas.

Drill holes in the gold zones demonstrate good grade distribution along the entire mineralized interval.

The distribution of the pyrite stockwork is greatly influenced by the geometry of the dikes, specifically for Zone 27 and the Caribou corridor, which are spatially associated with 2- to 30-metre thick northeast-trending porphyry dikes.

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At the Windfall Lake deposit, the volcanic stratigraphy trends to the northeast and dips moderately towards the southeast.

Preliminary metallurgical tests indicate a gold recovery of 95.7% using a standard gravity and flotation circuit, followed by cyanidation. Mineral Resource Statement (From SRK Consulting, November 13, 2014).

Reported at a cut-off grade of 3.0 g/t gold, assuming an underground extraction scenario with an assumed gold price of US$1,200/oz and metallurgical recovery of 96%.

The bulk of mineralization averages ~10 g/t over 5 metres, with very high-grade pockets up to 248 g/t over 12.4 metres in some areas.

,200/oz and metallurgical recovery of 96%.

The bulk of mineralization averages ~10 g/t over 5 metres, with very high-grade pockets up to 248 g/t over 12.4 metres in some areas.

Drill holes in the gold zones demonstrate good grade distribution along the entire mineralized interval.

The distribution of the pyrite stockwork is greatly influenced by the geometry of the dikes, specifically for Zone 27 and the Caribou corridor, which are spatially associated with 2- to 30-metre thick northeast-trending porphyry dikes.

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