Goodman and Seattle Project

• 11,809-hectare consolidated land package
• 40 kilometers northwest of Mayo City, YT
• Accessible by year-round roads via the Silver Trail Highway
• The Goodman Claim block lies south and is contiguous to the claims covering the Eagle Mine
• The Seattle Claim block lies directly north of the Nitra Claim, owned by Banyan, and east of Silver North’s Haldane Project

Geology

The Goodman project is located within the Selwynn Basin, which is a highly mineralized area east of the Tintina Fault. Locally, the geology consists of Upper Proterozoic to Silurian metasediments that are intruded by mid-Cretaceous polyphase quartz monzonite stocks.

The Goodman Project is located along the Potato Hills trend, a mineralized fault system that trends southwest from the Eagle Gold deposit.

The Seattle project is a silver project located in the Keno Hill Geological formations, which is found to host high-grade vein silver deposits. This historical mining district has produced over 200 million ounces of silver.

Lugdush Project

The project is located with the Selwynn Basis, which is a highly mineralized area east of the Tintina Fault.

• 422 claims contiguous and to the south of Sitka Gold’s RC project containing a gold deposit and a recent tungsten discovery
• 80.4km² land package

VIP Project

The VIP project is located within the White Gold District, is on strike with the Coffee Gold deposits (Talamore Mining, formerly owned by Newmont) and is cut by the Coffee Creek fault system.

Numerous soil sampling anomalies, and similar geology to that of the Coffee Gold deposits, indicate the potential for significant gold mineralization.

• 17,538-hectare consolidated land package
• 120 kilometers south of Dawson City
• Accessible by helicopter or barge. An airstrip is available roughly 25 kilometers north of the property
• Nearby projects include Goldcorp’s Coffee deposit, Western Copper & Gold’s Casino deposit, and White Gold’s Golden Saddle deposit
• Contiguous with projects operated by Independence Gold and White Gold

Local geology consists of schistose sedimentary sequences and lesser mafic volcanics, biotite gneisses, and felsic through to ultramafic intrusions of variable size and composition.

Livingstone Project

The Livingstone area is a historical and current placer mining district which is renowned for extremely coarse nuggets. A source for these large nuggets has not yet been identified.

Bedrock mineralization identified to-date includes sulfide-rich quartz veins and sulfide-breccias. Up to 10 g/t Au has been sampled in bedrock.

• Key land position alongside renowned placer mining district of Livingstone and other major placer gold creeks
• 4,640-hectare consolidated land position
• 85 kilometers Northeast of Whitehorse, YT
• Accessible by fixed-wing aircraft using the Livingstone airstrip, winter road, or helicopter
• Numerous 4×4 trails throughout the property from current and historic placer mining activity
• Claim parallel to Big Salmon Fault, which is associated with regional gold emplacement
• Gold mineralization identified in sulphide-rich quartz veins and sulphide breccias
• Seven parallel structures have been identified with potential for gold mineralization

The Livingstone project is located with the Yukon-Tanana Terrane; a composite of crustal blocks including former volcanic island arcs and continental shelf depositional environments. Locally, the claims lie along the contact of an Early Mississippian intrusion and Devonian metaquartzite and schist.

Summit Project

The project displays similarities to many gold occurrences located southeast and northwest of the project area, which includes the Rackla Gold project (ATAC Resources), 3 Aces project (Seabridge Gold), and Banyan’s Hyland project discoveries.

• 1,720-hectare land package
• Located in the Watson Lake mining district, approximately 200 kilometres east of the village of Faro, Yukon
• Alongside the boarder of Yukon and Northwest Territories
• Project is accessible by helicopter and float plane from a base station on Nahanni Range road, approximately 50 kilometres to the southeast.

The project is located within the Selwyn Basin geological province and underlain by Precambrian to Lower Cambrian Hyland Group rocks within a regional northwest plunging anticlinorium.

The property was staked to cover the inferred source of a 99th percentile regional gold-arsenic-antimony stream sediment anomaly taken by the Geological Survey of Canada.