Lefroy Exploration Limited reported results from recent diamond drill holes on the zero north section and an update to a recently completed step out RC program 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. The Company has not yet established the association between the larger Burns intrusion and the diorite porphyry intrusions intersected at Burns but considers there is a genetic relationship. At Burns, broad high-grade gold mineralisation is hosted within a newly discovered hematite-pyrite-chalcopyrite-magnetite altered diorite porphyry that intrudes high Mg basalt. 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. The copper and gold mineralisation hosted by both the diorite porphyry, basalt and now massive magnetite is considered by the Company to be a new style of 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 in the future. Assay results have been received, collated and reviewed for four (LEFD004, OBURCD025, LEFRD267, LEFR268) of the five diamond holes completed on the zero-north section. Results for LEFRD282 are pending. All samples for each of the holes were submitted for gold and whole rock geochemistry. The whole rock geochemistry will be interrogated once the results are received for LEFRD282. The whole rock data will provide important geochemical information to characterise the three types of porphyries, understand the mineral relationships and provide vectors to gold and copper mineralisation along the Burns corridor. Significant gold and copper results from the four holes are as follows: 6.60m @ 1.14g/t Au & 1.18% Cu from 102m in LEFD004, 12.7m @ 2.53g/t Au & 0.08% Cu from 141.3m in LEFD004, 6.20m @ 1.28g/t Au & 0.29% Cu from 160m in LEFD004, 10m @ 0.25 g/t Au & 0.95% Cu from 77m in OBURCD025, 15m @ 1.61 g/t Au & 0.33% Cu from 218m in OBURCD025, 5m @ 2.90 g/t Au & 0.66% Cu from 228m in OBURCD025, 13m @ 0.90 g/t Au & 0.28% Cu from 263m in LEFRD267, 12.3m @ 0.94g/t Au from 406m in LEFR268, 10m @ 1.19 g/t Au from 265m in OBURCD025. Assessment of the gold, copper and silver results from the four holes highlights multiple zones of gold and or copper mineralisation in the intervals noted from inspection of the core and highlighted in text above. Initial review of the data highlights two steeply dipping zones that are approximately 20m in width with a vertical continuity of 150m. These zones have been further evaluated by diamond drilling on the 40N and 40S sections, with results pending. One zone (western) is a gold copper (and silver) system and includes the mineralisation in LEFR260. The other (eastern) zone is gold only, with a much lower copper and silver content. This eastern zone appears to relate to the more pyrite altered intervals of the porphyry. The Company considers this to be a new style of mineralisation at Burns and provides another style of target. The relationship between the two zones is unclear, but it may represent separate but related mineralisation events. The down dip continuity of both zones is limited by hole LEFR268. However, a new interval of gold only mineralisation (12.3m @ 0.94g/t Au from 406m) was intersected at a deeper interval in this hole, and thismay represent a new and or developing zone. The results from LEFD004 did not replicate the strong mineralisation in LEFR260. The Company considers this to the bias (difference) in the sample size between the RC drilling and the half core HQ diamond core and to the internal variability of the mineral system, noting that in particular the chalcopyrite is a blebby/fracture filled style as opposed to an evenly disseminated style. To further clarify the mineralisation in LEFR260, ten field duplicate samples were selected from the highest-grade interval and analysed for gold by the screen fire assay (SFA) technique. The technique provides detail on the distribution of the gold to either the coarse or fine fraction. They results highlight near 100% reproducibility of the original grade of the interval (10m @16g/t Au) and show a high proportion of gold in the fine fraction. Subsequent panning of an interval in the field highlighted the fine to very fine native gold in the sample, some of which floats on the water, with associated pyrite and magnetite. The assay results from the diamond drill holes on the zero north section and the visuals from July nine hole RC program further highlight and demonstrate the growing scale and multi-stage style of mineralisation in the Burns area. The zero north drilling has provided initial calibration and guidance to develop the July step out RC program that has yielded exciting favourable geology to expand the footprint of the overall system. It has also demonstrated that the basalt can be a host to the magnetite sulphide system with the strong intersection in LEFR292 and, early signals of the same mineralisation style at Smithers. Results are expected for five diamond holes drilled on the 40N and 40S sections over the coming 2 months. Results for the recent RC drilling are not expected until late September. During this extended waiting period exploration will continue at Burns, with a detailed aeromagnetic survey to cover the Burns intrusion (including Burns) commissioned for August 2021.