This claim group is contiguous to the west side of the Lac Rocher nickel deposit owned by Victory Nickel. The deposit is hosted within a circular mafic-ultramafic iron-nickel-copper intrusion. A PEA for the deposit assumed a base case of 317,730T ore at 1.57%Ni, 0.58%Cu and 0.53%Co.

This early stage property covers part of the Lac-Saint-Jean Anorthosite. The predominant lithology is gabbronorite with or without Fe-Ti-P oxides and coronitic leucronorite. Mineralization in the property area includes titanium, iron, vanadium and phosphate. Eagle Ridge’s property is contiguous to the south side of the Arianne Phosphate Inc. Lac a Paul phosphate project. The Lac a Paul project is fully permitted and has a reserve of 472 Mt @ 6.9% P2O5. The property contiguous to the west side was recently (2018) explored for a massive illmenite outcrop. Rock samples (56) from the neighbouring property to the west with geology similar to Eagle Ridge’s assayed with values between 0.02% and 0.58% V2O5. Davis tube testing yielded substantially higher Vanadium concentration values; up to 1.79 times. Phosphate was found in 57 samples with assays ranging between 0.02 and 10.1%. (GM71591)

This 15 claim property is located 30km ESE of the permitted and shovel ready Dumont Nickel project. The Dumont project has a proven and probable resource of 2.8Mt @ 0.27%Ni and an additional 5.7Mt M+I and Inferred. Eagle Ridge’s property, in 3 separate groups along an E-W line, is situated over similar geology as Dumont’s consisting of a sill of pyroxenite, peridotite, dunite and serpentinite. The east group, consisting of 10 claims is located on either side of the Landrienne Nord showing (0.25% Ni- L279122)owned by others. One surface sample on Eagle Ridge’s east group assayed 0.18% Ni and 0.65% Cr (sample 1980004086). Drill hole 2 (GM64190) samples 63 and 64 assayed 0.08% Ni and 0.12% Ni at a depth of 91.5-96m. (Jan. 2007). No work results have been found for the westerly 5 claims in the group of 15 claims. The east and west groups are about 12 km apart on the same geological horizon.

The eight-claim property is located approximately 90 kms north of Saguenay Quebec. Past work in 2012/13 consisted of stripping and sampling. The host rock for graphite mineralization is quartzo-feldspathic gneiss associated with marble. At this stage of work the Colline Property has very good potential for discovering a high-volume moderate grade graphite deposit as per GM68002. The disseminated flake graphite grades between 2- 6% and appears to be relatively constant from sample to sample. The property is approximately 7.5 kms north of the Saint-Onge Wollastonite deposit (probable 15.3t@36.7% Wollastonite).

This closed mine is covered by two claim units. Historically it was in production in1907-1919 and 1952-1954, producing at least 200T ore. A report in 1953 (GM02343) noted that considering the high quality ore mined, there was no indication of the scope, extension or grade of the ore. Visual examinations of mined ore in 1953 indicated a rough grading of 8-25%.

Work in 1989 revealed a graphite zone consisting of two interlopes with grades greater than 10%. Surveyed conductors indicated an anomalous zone 1,200m by 500m. 2.5km to the west, Lomiko Metals is developing its La Loutre graphite deposit. A 2021 PEA indicated a base case M+I resource of 23.165 Mt @ 4.51% Cg and an inferred resource of 48.82Mt @ 4.01% Cg.