
An important geological structure enriched in Sillimanite-Microcline extending over 2 kilometers with an average thickness of 125 meters. The known zones totals 5 Mt grading between 20-25% Sillimanite and 8-10% of Microcline of high quality. Numerous Sillimanite-Microcline showings have been identified along the geological structure.
The deposit is free of radioactive minerals and sulphides causing acid mine drainage.
The deposit is located near road and railway infrastructure along a road that can easily be reached via the Municipality of Ste-Anne-Du-Lac.
A quarry operation is planned.

A series of white dolomite deposits with very low iron impurities (Fe). The known deposit consists of an area measuring 600m long by 250 m wide grading more than 85% dolomite.
The deposit is free of radioactive minerals and sulphides causing acid mine drainage.
The deposit is located near road and railway infrastructure along a road that is easily accessible via the Municipality of Ste-Anne-Du-Lac in Québec.