Juggernaut Exploration Ltd. reported results from the 2022 field program on its 100% controlled Bingo property located within the Eskay Rift region of the Golden Triangle, British Columbia. Empire property 100% controlled û high grade metallica zone û fully permitted and drill ready: Grab samples from a massive sulphide vein up to 30 cm wide assayed up to 36,875 gpt Ag, 4.68 gpt Au, 27.6% Cu and 3.27% Zn. Channel samples from the massive sulphide vein assayed 22,694 gpt AG (729.6 oz per tonne), 26.4% Cu, 2.8% Zn.

The vein extends for 40 meters in an east-west direction and remains open. Five separate gently dipping veins assayed between 1 and 16.4 gpt Au, and up to 2470 gpt Ag, 15.45% Cu and 1.58% Zn. These veins are up to 30 cm wide, contain quartz + Fe-carbonate ¦ covellite ¦ sphalerite and are arranged in a traceable set for over 50 meters across strike and remains open.

Mineralization is hosted within a propylitically altered feldspar porphyry unit. The Metallica zone is drill ready and fully permitted, and the Company is planning a maiden drill program for 2023. The Metallica zone is part of the Inca Trend, a high-grade polymetallic mineralized trend that extends for 1.6 by 1.2 kilometer in an area where recent glacial abatement has exposed several extensive new zones of mineralized outcrop which were previously unknown.

Excellent proximity to infrastructure, including highway, railway, high-tension power and the town of Terrace, BC. The Metallica zone is a new discovery in a region of recent glacial retreat exposing mineralized outcrop that has never been seen before. Limited prospecting identified mineralization over an area measuring approximately 250 by 225 meters that remains open.

Multiple outcrop exposures with abundant mineralization were discovered. Mineralization is hosted within a propylitically altered feldspar porphyry unit and is comprised of two distinct types of mineralization: gently dipping, 20û30 cm wide quartz + Fe-carbonate ¦ covellite ¦ sphalerite veins arranged in a traceable set for over 50 meters across strike, and a silver-rich polymetallic massive sulfide vein up to 30 cm wide that extends for 40 meters. Five separate gently dipping veins assayed between 1 and 16.4 grams per tonne gold, and up to 2470 grams per tonne silver, 15.45% copper and 1.58% zinc. The most prominent mineralization observed in outcrop in the Metallica Zone was a solid massive sulphide and sulfosalt vein up to 30 cm wide.

Samples taken across the vein returned assay values of up to 36,875 grams per tonne silver, 4.68 grams per tonne gold, 27.6% copper and 3.27% zinc. Channel cuts from the massive sulphide vein returned values of 22,694 grams per tonne silver (729.6 oz per tonne), 26.4 % copper, 2.8 % zinc and a gold equivalent value of 348 grams per tonne over 0.2 metres. This high-grade vein is hosted in a 75 cm wide altered carbonatized fault with local sulphide bearing stockworks, breccia and parallel, near vertical, quartz-carbonate veins. The structure has been traced over 40 meters to the east and west and remains open in both directions.

The spectacular assay values and sulphide rich mineralization offer a predictive look to mineralization at depth and strong potential for adjacent veins and feeder zones extending from an Eskay Creek style VMS body at depth. The parallel veins also have the same characteristics that have been observed throughout the zone. The Metallica zone is drill ready and fully permitted, and the Company is planning a maiden drill program on the Metallica zone for 2023.

The 100% controlled Empire Property covers 12,480 hectares approximately 70 kilometers northeast of Terrace, BC. It is road-accessible and approximately 15 kilometers from the nearest highway and power line. The Empire property was generated and staked by the J2 Syndicate following a brief reconnaissance exploration program in a highly prospective geological setting which resulted in the discovery of extensive high-grade polymetallic mineralized trends, including the 1.6 by 1.2 kilometer north-south striking Inca Trend host to the Metallica zone.

These trends were discovered in areas where recent glacial abatement has exposed several extensive new zones of mineralized outcrop which were previously unknown.