Libero Copper & Gold Corporation announced that a 5,000 metre exploration diamond drill program has commenced at the Big Red project in BC's Golden Triangle west of Telegraph Creek. The first diamond drill pad is approximately 50 metres northwest of the Terry 2020 porphyry copper discovery with the intent of stepping out and confirming mineralization below four reverse circulation ("RC") holes drilled in October 2020 that were limited at depth. Libero has already begun a large soil sampling program and is monitoring the results with a portable XRF at site. The program covers approximately 2.6 square kilometres and to date, 457 samples have been taken. In addition, a 3D IP survey over the Terry discovery has begun, with preliminary results expected within the next two weeks. Big Red is a 26,000-hectare district scale land package with both gold and copper targets, road access, and an airstrip. Big Red is located 45 kilometres southwest of Telegraph Creek along the Barrington Road, 70 kilometres north of Galore Creek, and 120 kilometres west of Red Chris in the Golden Triangle of northwestern British Columbia, Canada. The Golden Triangle is a mining district of prodigious gold and copper mineralization and host to some of Canada's most famous mines (Premier, Red Chris, Snip, Brucejack, Eskay Creek) and porphyry copper deposits (Galore Creek, KSM, Saddle). At Big Red, the Terry porphyry copper target is peripheral to a distinct large magnetic-high feature over the Limpoke Pluton that coincides with a radiometric potassium anomaly, magnetic low, conductivity high, copper, gold, silver and molybdenum anomalies and a mapped Jurassic aged porphyry intrusion. The discovery hole drilled in Terry in October 2020 returned 120 metres of 0.41% copper equivalent from surface to end of hole including 73 metres of 0.49% copper equivalent from surface. The discovery is located just 8 km from road access. Mineralization is associated with a porphyritic dyke swarm hosted in intermediate volcanic rocks. Chalcopyrite mineralization occurs as fine disseminations within the porphyritic dykes and volcanic host rocks, with higher concentrations along the margins. Malachite mineralization is present locally along fractures surfaces.