Lefroy Exploration Limited reported assay results from 4 of the nine-reverse circulation (RC) holes that were completed in July 2021 evaluating the Burns copper (Cu) gold (Au) prospect. Burns is within the Eastern Lefroy tenement package, which is part of the wholly owned greater Lefroy Gold Project (LGP) located 50km southeast of Kalgoorlie. The Burns copper gold prospect is situated outboard of a large interpreted felsic intrusion, termed the Burns Intrusion. The intrusion does not outcrop but features a distinctive annular aeromagnetic and gravity geophysical signature. The Company has not yet established the association between the larger Burns intrusion and the diorite porphyry intrusions intersected at Burns but consider there is a genetic relationship between them. Broad high-grade gold mineralisation is hosted within a newly discovered hematite-pyrite-chalcopyrite-magnetite altered diorite porphyry that intrudes high Mg basalt at Burns. This porphyry, termed the Eastern Porphyry, is open to the north and south. The eastern extent of the Eastern Porphyry is now defined, on multiple drill sections, by foliated basalt (footwall basalt). The copper and gold mineralisation hosted by both the diorite porphyry, basalt and massive magnetite veins is considered by the Company to be a new style of Au-Cu-Ag mineralisation in the area, a land position dominated by Lefroy. The existence of additional mineralisation under Lake Randall is not discounted by the current drilling campaign and additional programs are being planned for CY2021 to expand the system. Four holes (LEFR290, 291, 292, 293) evaluated the northern extension of the Burns system. Hole LEFR290, a 40m step out to the north intersected a 101m downhole interval of altered porphyry including a 10m interval containing intense magnetite-pyrite alteration. The porphyry is open to the north. Hole LEFR 292, an 80m step out from LEFR285 intersected a thick 30m down hole interval of massive magnetite containing up to 20% pyrite alteration in basalt in hole LEFR292. This is one of the largest intersections of magnetite containing coarse pyrite.