Lefroy Exploration Limited reported results from two RC drill programs 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 on the eastern margin 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 (Figure 2). 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 anew and unique style of Au-Cu-Ag mineralisation in the area, a land position dominated by Lefroy. The existence of additional mineralisation further east and north under Lake Randall is not discounted by the current drilling campaign and will be the subject of more exploration and drilling that is about to commence. Two RC drilling campaigns were completed at Burns during the July to October 2021 period. The July program evaluated extensions immediately peripheral to the established Burns prospect while in October a 17 hole step out program was completed evaluating multiple magnetic anomalies along a 3000m corridor north of Burns. The nine-hole RC drill program (LEFR287-296) was commenced and completed in July 2021 to evaluate both strike extensions to the Eastern Porphyry and strike and down dip extensions to the Cu-Au mineralisation in the western basalt. A total of 2328m of drilling was completed testing 4 targets, including a single hole (LEFR296) testing the Smithers aeromagnetic anomaly. The drilling targeted strike extensions to the Eastern Porphyry (LEFR290) and strike and down dip extensions to the Cu-Au mineralisation in the western basalt. 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 30m down hole interval of massive magnetite containing up to 20% pyrite alteration in basalt. A fence of three 80m spaced holes (LEFR287, 288, 289) were drilled on the 160S section line to evaluate the southern strike extension of the Au-Cu mineralisation in the LEFR273 and the broad downhole intervals of dominantly copper mineralisation in the western basalt intersected in holes LEFR271, and LEFR272 located 80m to the north. A single RC hole was also drilled at Smithers to evaluate this aeromagnetic anomaly approximately 250m to the north of Burns. The hole (LEFR294) was successful in penetrating the 90m downhole interval of palaeochannel cover to intersect diorite porphyry, which is similar to the porphyry at Burns and contains two narrow (3-5m) intervals of pyritic magnetite veining. The hole had to be abandoned at 156m down hole. This hole demonstrates that the Burns system extends to Smithers, a distance of at least 500m. This issue was further evaluated in the October RC drilling campaign. Results for four of the 9 RC holes were reported in the September quarter. Three of the four holes were from the 160S section. The westernmost hole (LEFR289) intersected an impressive 244m downhole interval of copper mineralisation from 20m, hosted by high Mg basalt. This was followed by a further 24m interval of copper mineralized basalt to the end of hole (EOH) at 330m, a combined downhole total of 268m of mineralisation. The mineralisation is open along strike to the south and at depth. The copper mineralisation in LEFR289 is associated with more extensive and elevated magnetite alteration in the high Mg basalt. This Cu dominant zone at Burns is known as the Western Basalt and the mineralisation is open. The final results from the remaining 5 RC holes of that program have been received and validated. These results further support the growing scale of the mineralised system to the north and west. Significant results from those holes include: 11m @ 1.45g/t Au & 0.10% Cu & 0.59g/t Ag from 108m in LEFR290 (Eastern Porphyry) Including 2m @ 5.04g/t Au & 0.13% Cu & 1.0g/t Ag from 114m; 40m @ 0.07g/t Au & 0.14% Cu from 42m in LEFR295 (Western Basalt); 11m @ 0.27g/t Au & 0.29% Cu from 84m in LEFR294 (Smithers); 2m @ 3.96g/t Au from 284m in LEFR291.