Lefroy Exploration Limited reported results from 3 diamond drill holes on the 40 north (40N) section 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 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 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 currently being planned for current year 2021. A nine-hole diamond drill program commenced on 20 April 2021 to evaluate the Eastern Porphyry over a 200m strike length on 40m spaced drill sections. The first hole of the program (LEFD004) was completed on 3 May 2020. That hole was designed to twin and extend past the high-grade interval found in LEFR260 to confirm structural orientations and determine the width of the Eastern Porphyry on the zero north drill section (0N). That hole was drilled primarily to understand the geological and structural controls of the system but also to provide guidance for the subsequent diamond holes on 0N, 40N and 40s drill sections. The host Eastern Porphyry was intersected in LEFD004 from 117m to 304.5m, a down hole interval of 187.5m. The porphyry is interpreted to have a near vertical dip and an estimated true width of approximately 110m. It is bounded by basalt to the west and east. The results form that hole confirmed (visual & geochemical evidence) three distinct variations of the host diorite porphyry which are interpreted as multi-phase intrusive events.