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Giant Mining Expands Exploration for High Grade Copper-Bearing Breccia Zones at Majuba Hill Copper Project, Nevada

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VANCOUVER, British Columbia - (NewMediaWire) - October 31, 2024 - Giant Mining Corp. (CSE: BFG | OTC: BFGFF | FWB: YW5) ("Giant Mining" or the "Company") is pleased to announce plans to expand the surface exploration to focus on high-grade copper-bearing breccias zones at its Majuba Hill ("Majuba Hill") Copper-Silver Deposit located in Pershing County, Nevada.

High-grade copper was sampled from core hole MHB-30 ("MHB-30") that was clearly associated with magmatic-hydrothermal, copper-bearing breccia zone. The breccia zone returned 218.0 feet (66.4 meters) of 1.35% Cu and 73.4 g/t Ag including 74.0 feet (22.6 meters) of 2.6% Cu and 30.1 g/t Ag.

MHB-30 drilled a prominent breccia zone on the west end of the >0.50% copper zone shown on Figure 1 and drone photo Figure 2.

The Significance of Copper-Bearing Breccia Zones

Copper-bearing breccias are zones in porphyry copper deposits where copper-mineralization is broken into smaller pieces and then those pieces are cemented together by copper-rich minerals. The breccias are formed when magmatic-hydrothermal activity causes mineral-laden fluids to move along faults or fractures in the Earth's crust. These zones are prized in mining for their potential high copper grades, and several deposits have achieved notable commercial success. In larger copper deposits the copper-bearing breccias are a guide that points to where the largest portion of a porphyry copper deposit can be found.

"We are excited to advance our exploration efforts at Majuba Hill," said David Greenway, CEO of Giant Mining. "We look forward to determining the high-grade potential of the copper-bearing breccias, which will further our understanding of the deposit's potential to become a significant domestic supply of copper for the USA and for the benefit of all Giant Mining stakeholders."

Figure 1: Magmatic-Hydrothermal Breccia Corridors and Prominent Breccia Bodies

Majuba Hill Copper-Bearing Breccias

At Majuba Hill the high-grade copper mineralization is commonly found in the tourmaline-matrix type of breccias. Copper occurs as azurite, malachite, chalcocite, cuprite, and traces of chrysocolla found in veins, veinlets, fracture coatings, and replacing phenocrysts in intrusive rhyolite fragments as well as in the tourmaline matrix as shown in Figure 3a. Primary-hypogene copper-mineralization also occurs as intrusive rhyolite fragments with disseminated bornite and chalcopyrite as shown in Figure 3b.

"Recognizing the location and geometry of these breccia zones is a significant step forward for Giant Mining," said Buster Hunsaker, Consulting Geologist to Giant Mining Corp. "By including the geometry and copper mineralization of the breccia zones and their margins, the Company expects to be more successful with the drill holes from the new sites built for the 2024 in-fill and expansion exploration program. It is a testament to the collaborative efforts of the Giant team and the insights provided by Leo Hathaway, Larry Segerstrom, and Dick Sillitoe."