Fabled Copper Corp. announced the first results of 2021 surface field work on it's Muskwa Copper Project comprised of the Neil Property (previously referred to as the North Block) and the Toro Property (previously referred to as the South Block) in Northwestern British Columbia. The Company also holds rights to the Bronson Property.

Sample # D-723002 taken at the lowest elevation of 1,320 meters was composed of quartz veining, breccia and stockwork, with black shale fragments in a white quartz matrix which is mineralized with patches and seams of copper sulphides measuring 5% (bornite ­ chalcopyrite), abundant malachite staining, and returned 8.17% copper over 0.15 meters of exposed veining thru the valley floor rubble. Sample # D- 723260 was taken 87 meters vertically above D-723002 at a vertical elevation of 1,407 meters where the Lady Luck Structure surfaced again. A grab sample of the rubble at the base of the structure returned 20.20% copper, The sample consisted of weathered, dark brassy brown quartz on the surface and mottled white, brassy yellow on a fresh surface.

Moderate malachite, and contained 60% chalcopyrite. At the 1,411-meter elevation, only 4 meters above of that previously described, 2 float samples, D-723259 and D-723258 were taken and reported 2.80 % copper and 1.91% copper respectively. The next mineralized occurrence of the vein structure was at 1,679 meters, 268 meters vertically above, where rubble sample D-723250 returned 3.28% copper.

At 1,715 meters the mineralized structure continued and rubble sample D-723005 assayed 26.10% copper, 36 meters vertically above that which was last sampled. This incredible copper sample consisted of semi-massive sulphides, rusty dark ­ light brown on the surface, minor malachite staining, 95% sulphides, 2% quartz, 3% sheared shale host rock. At the final vertical elevation of 1,764 meters, 24 meters above that last sampled two samples were taken, A grab sample, # D-723003, taken at the base of the mineralized outcropping of the Lady Luck vein structure and returned 16.50% copper.

The sample contained a white quartz carbonate vein with patches of carbonated ribboned with seams and patches of sulphides and iron carbonate, limonite alteration common, vuggy with crystal growth in the cavities, abundant malachite staining, non-magnetic, 6% sulphides, (chalcopyrite ­ bornite). At the same vertical elevation, a composite sample D-723004 was taken over a total of 4.60 meters which returned 14.30% copper. The area sampled consisted of a quartz carbonate vein, with white quartz containing patches of iron carbonate, abundant malachite staining, 7% copper sulphides as semi-massive patches, blebs and disseminated chalcopyrite and bornite.