The Baillargé-Est property is located in the Province of Quebec, in Abitibi, in the township of La Corne on Map 32 C 05 (NTS). The Baillargé-Est project consisting of 35 claims is positioned 38 kilometres north of the town of Val d’Or and at a distance of about 30 kilometres southwest of the village of Barraute. The property also covers about three-quarters of Lake Baillargé. The area thus formed is 1299 hectares.

The project occupies the lower part of the Superior Province, particularly the southern zone of the Sub-Province of Abitibi. The batholite of Preissac‐Lacorne represents the predominant geology and covers an approximate area of 415 Km². The latter, consisting of a syn to late-kinematic plutonic assembly, was set up along the anticline of La Pause in mafic to ultramafic volcanic rocks and sediments which make up the rocks of the Jacola, La Motte‐Vassan, Dubuisson and Caste formations of the Aurora Group.

The main outcrop is named Lac Baillargé‐Est and was discovered in 1955. It is represented by three pegmatites measuring several tens of metres in length and a few metres in width. It has been the subject of 14 surveys, including sampling results of 2.48% Li₂O or 1.15% Li over 2.30m. The best results among the samples collected in 2011 are 0.237% and 0.634% lithium, 5.47%, 1.46% and 2030 ppm molybdenum, 1315 ppm niobium, 193 ppm, 319 ppm and 1125 ppm tantalum (GM 66452). These contain spodumene, beryl, molybdenite, colombo-tantalite, quartz, feldspar, muscovite, cleavelantite and holmquistite.