FALCON GOLD CORP. reported it has entered into two separate arm's-length agreements, pursuant to which the company will acquire a 100-per-cent interest in two battery metals projects in the province of Ontario and Quebec, collectively known as the Timmins West and Outarde Nickel Project northwest of Baie Comeau, Quebec. The first purchase agreement covers 5 mining claims totaling 1,940 hectares within the Kamiskotia Gabbroic Complex (KGC) located 20 km northwest of Timmins, Ontario.

The KGC is a gabbroic to anorthositic intrusive mafic to ultra-mafic body that has documented nickel-copper-cobalt (Ni-Cu-Co) mineralization. An outcrop grab sample in 2004 reported 0.44% Ni, 0.64% Cu and 0.033% Co hosted by 10% pyrrhotite. The Property lies 40 km southwest of the Crawford Ni-Co Project being developed by Canada Nickel.

The KGC property shares many similarities to other well-known complexes such as the Bushveld Complex (South Africa), the Stillwater Complex (USA) and Bell River Dore Lake Complexes (Quebec) (Barrie, 2000). The Timmins West Ni-Cu-Co property has historically been explored for gold. However, it's mafic to ultra-mafic composition within the KGC makes it a prime target for magmatic Ni-Cu-Co mineralization.

The regional government flown magnetic signature of the KGC suggests a possible layer within the KGC that has the potential to a host a pyrrhotite-rich cumulate layer host to Ni-Cu-Co mineralization. An outcrop grab sample in (AFRI 42A12SE2024, sample 185247) taken in 2004 reported 0.44% Ni, 0.645% Cu, 332 ppm Co, 0.053 g/t Au and 3 g/t Ag. This sample was associated with 10% pyrrhotite in a gabbroic mafic outcrop.

Eight (8) additional samples within 15 m of the 185247 also reported anomalous Ni-Cu-Co values. The second purchase agreement comprises of 93 claims covering 5, 138 hectares located 120 km northwest of Baie-Comeau, Quebec. The Outarde Property contains nickel-copper-cobalt style mineralization and was last explored by Falconbridge in 1997.

The property is located at the folded nose of a gabbro-norite suite of mafic rocks, part of the large anorthositic-gabbro pluton of the De La Blache Mafic Plutonic Suite. The gabbro-norite body occupies the entire length of the property (about 30 km) and has only been intermittently explored. Nickel and copper-bearing sulphides are generally located in fracture or shear zones.

Highlights of the best Ni and Cu assays are 1.28% Ni and 1.38% Cu and 700 ppm Co from a grab sample. The property has not been drilled. Recommended work includes a high-resolution airborne magnetic and electromagnetic survey followed by ground truthing of detected anomalies.

Grab samples are selected samples and not necessarily representative of the mineralization hosted on the property.