The mineralization is hosted in at least two massive hematite-ilmenite tabular lenses within the Labrieville anorthosite layered complex. The lenses trend NW and dip 25° ENE. These lenses outcrop in a cliff along Lac Lise road and are intercepted at surface and at a depth of 30 metres below surface in the drilling conducted to date. A VTEM survey conducted by the previous land holder delineated a 2.5km conductor. Additional conductors identified on the property have only seen initial exploration with limited surface sampling. One of these conductors, located northwest of the mineralized lenses yielded results which included a grab sample assaying 35.5% TiO₂.