Announcement PDF 28 April 2025 Amendment - Bauloora Drilling and Target Generation (17/04/2025) Legacy Minerals Holdings Limited (ASX: LGM, “LGM”, “the Company”, or “Legacy Minerals”) released an announcement titled “Bauloora Drilling and Target Generation” on 17 April 2025 (Release). The Release referred to stream sediments, rock chip and soil exploration results for which no information was included in the JORC Table 1 as required under Listing Rule 5.7.1. Following is a summary of the material changes made to JORC Table 1 Section 1: Criteria Sampling Techniques JORC Code Explanation Nature and quality of sampling (e.g., cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. Commentary Reporting on stream sediment sampling and rock chip samples. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Aspects of the determination of mineralisation that are Material to the Public Report. In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g., submarine nodules) may warrant disclosure of detailed information. Drilling techniques Drill type (e.g., core, reverse circulation, open‐ hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diametre, triple or standard tube, depth of diamond tails, face sampling bit or other type, whether core is oriented and if so, by what method, etc). Removal of references to diamond drilling Drill sample recovery Method of recording and assessing core and chip sample recoveries and results assessed. As no drilling, removed references to core and drill sample recoveries Measures taken to maximise sample recovery and ensure representative nature of the samples. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. Page 1 of 21 | ABN 43 650 398 897 3/202 Russell Street Bathurst, 2795 www.legacyminerals.com.au ASX: LGM Page 2 of 21 Logging Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Included references to rock chips and removed references to drilling. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevant intersections logged. Sub‐sampling techniques and sample preparation If core, whether cut or sawn and whether quarter, half or all core taken. If non‐core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. Removed references to drilling and drill samples, and reporting quality control procedures for stream sediment sample assays. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Quality control procedures adopted for all subsampling stages to maximise representivity of samples. Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐half sampling. Quality of assay data and laboratory tests The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. Amended reported QAQC procedures. For geophysical tools, spectrometres, handheld XRF instruments, etc, the parametres used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. Location of data points Accuracy and quality of surveys used to locate drill holes (collar and down‐hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. Removal of references to downhole surveys Specification of the grid system used. Quality and adequacy of topographic control. Data spacing for reporting of Exploration Results. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 3 of 21 Data spacing and distribution Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. Whether sample compositing has been applied. Inclusion of reporting on rock chip and stream sediment spacing. Removal of references to drilling Whether sample compositing has been applied. Orientation of data in relation to geological structure Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. Removal of references to drill holes and inclusion of reporting on stream sediment samples. If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. Sample security The measures taken to ensure sample security. Amended reporting on sample security The Company’s amended Release is attached. Approved by the CEO & Managing Director of Legacy Minerals Holdings Limited. For more information: Investors: Chris Byrne CEO & Managing Director chris.byrne@legacyminerals.com.au +61 (0) 499 527 547 Media: Nicholas Read Read Corporate nicholas@readcorporate.com.au +61 (0) 419 929 046 SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM ASX Announcement 17 April 2025 ASX: LGM Amended - Reconnaissance Drilling Defines New Vein Trends at Bauloora Significant alteration at new Prospect areas and recent surface geochemical surveys increase the scale of the Bauloora Project epithermal system. Wide Alteration Zones Highlight Prospective Structural Trends The reconnaissance drill campaign has identified multiple vein trends and broad alteration zones in a number of areas warranting follow-up: • Thunderbolt Prospect (TH001) intersects 200m of argillic alteration from the start to end of the hole (200m), including two wide zones of sericite-silica alteration +/- adularia. The Quarry target drilling aimed to intersect wide epithermal veins mapped on the surface. • In QU001 drilling intercepted minor epithermal veins with wide silicification and hematite alteration towards end-of-hole with elevated Sb (125ppm), As (171ppm) and Mo (11ppm). • Large surface veins were not intercepted, and end-of-hole alteration combined with structural measurements suggests the vein trends may not have been reached. New Sinter Lithology and Veining Identified in Generative Work BLEG Sampling • 92 Regional BLEG samples were taken across the Project area, highlighting previously unrecognised areas of anomalism that require follow-up work. • These anomalous drainages may indicate nearby, previously unrecognised epithermal vein trends to the north, east and south of the known vein field. Soil Sampling • 2,002 soil samples have been collected over the southern vein field area. This is the first time any systematic sampling has been conducted across this area, resulting in the identification of several, new epithermal vein occurrences on the surface. Rock Chip Sampling • 46 rock chip samples were taken from veins that were interpreted to exhibit epithermal-style textures, which occurred across the southern soil sampling grid. Sinter-related lithology identified in undrilled, southern Bauloora area • Petrographic analysis of rock samples has confirmed further sinter-related lithology. o Sinter is a rock primarily composed of silica that is precipitated at or near surface from hot waters at the vents of hot springs and geysers. • These new samples are ~2.5km south of the nearest, previously recognised sinter-related lithology. • This provides strong evidence supporting the preservation of the epithermal system over a significantly larger area of the Bauloora vein field than previously interpreted. Next Stages at the Bauloora Project • These reconnaissance drill results will guide target ranking for the next stages on the Project. • Significant drill intercepts previously intercepted and remaining to be followed up include: • Bluecap - MM008: 13m at 3.6g/t AuEq from 57m, (13m at 1.7g/t Au, 6.7g/t Ag, 0.1% Cu, 4.2% Pb+Zn)i o Incl. 3.7m at 10.5g/t AuEq from 57.44m, (3.7m at 5.6g/t Au, 17.4g/t Ag, 0.3% Cu, 10.5% Pb+Zn) • Ben Hall - BH001: 24m at 0.5g/t Au from 70mi See ‘Endnotes’ on page 18 for references Page 1 of 18 | ABN 43 650 3981897 3/202 Russell Street Bathurst, 2795 www.legacyminerals.com.au ASX: LGM Page 2 of 18 Legacy Minerals Holdings Limited (ASX: LGM, Legacy Minerals or the Company) is pleased to report assay results from new sampling of historic diamond drill core at its Bauloora (EL8994, EL9464) in NSW, Australia. Management comment – Legacy Minerals CEO & Managing Director Christopher Byrne said: “Legacy Minerals is pleased to have completed the latest reconnaissance drilling at Bauloora. It’s encouraging that, while we move further away from known high-grade drill intercepts and surface geochemistry, we continue to see evidence of major structures and broad halo alteration zones. From the drilling results, it appears that two of the Quarry Prospect holes did not intercept the large veins mapped on the surface. The team is incorporating these recently received drilling results to inform our interpreted dip of these veins further and to rank targets for future exploration. In preparation for the next round of exploration, the Company has collected systematic surface geochemical samples across projected southerly extensions of the known vein field. In doing so, the team on the ground collected several rock chip samples of previously unrecognised epithermal veins and confirmed sinter-related lithology in the south. This observation increases the prospectivity of the vein field in the south due to the strong preservation evidence provided through petrological analysis. We look forward to providing further updates at Bauloora as we continue this systematic work with earn-in partners Newmont.” Petrography Rock Chip Samples Figure 1. Petrology Sample 11189 (See Figure 8 for sample location): Interpreted to have formed in a hot spring environment, perhaps as part of the sinter sheet. Similar textures in opaline silica sinter can be observed in the currently forming sinter sheet about the Champagne Pool at Wai-o-tapu, New Zealandii. Sample sent for petrology study only. Cautionary Note – Visual Estimates of Mineralisation: ‘Visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations.’ SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 3 of 18 Daimond Drilling Results On the Bauloora Project, four diamond holes have been completed for a total of 950.2 metres. These tested the Thunderbolt and Quarry Prospects defined by a combination of anomalous soil geochemistry and geophysical signatures. The diamond drill holes have confirmed epithermal-style alteration with veining beneath elevated pathfinder rock chip and soil geochemical results and mapped veins while also suggestive that the main targets at the Quarry may not have been satisfactorily tested. Figure 1: Bauloora Project with recently completed drilling (red border) and previous highlight drilling results over Sb in soil sampling and regional geology interpretation. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 4 of 18 Thunderbolt Prospect At the Thunderbolt Prospect, a single diamond drill hole, for a total of 200m, was completed which tested the 1,300m long zone of elevated epithermal pathfinder elements defined in soil sampling. TH001 intersected strong argillic alteration from 0-200m with increased silica-sericite alteration and anomalous pathfinder elements associated with faults between 0-60m and 105-130mw with no significant gold-silver intercepts reported. The Prospect is interpreted to sit along strike of the Mt Felstead Prospect and as such the size and intensity of the alteration system is encouraging. Figure 2. TH001 cross section (MGA94z55 6177524mN) showing solid geology interpretation. Quarry Prospect At the Quarry Prospect, three diamond drill holes, for a total of 750.2m, were completed which tested the 3km long zone of elevated pathfinder elements defined in soil sampling and mapped epithermal vein on surface. QU001 intersected the strongest silica alteration from approximately 150-270m with hematite increasing from 300 to end of hole at 350m. This suggests that the drill hole may have missed the target veins as the veins may in fact dip in an easterly direction. This presents an obvious follow up opportunity for future testing. QU002 and QU003 intercepted zones of moderate alteration with lesser epithermal veins with no significant intercepts reported. An easterly dip to the Quarry Prospect veins is supported by the lack of alteration and veins intercepted in QU002 and the intersection of a easterly dipping altered and veined zone in QU003. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 5 of 18 Figure 3. QU001 cross section (MGA94z55 6177903mN) showing solid geology interpretation. Figure 4. Bauloora epithermal schematic model showing zone alteration patterns (modified from Buchanan 1981, Morrison et. al 1995). SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Surface Geochemistry BLEG sampling program The regional stream sediment BLEG sampling program has been completed with results highlighting several new catchments along strike to the north and south of the Bauloora vein field. These are new areas not covered by any existing soils, drilling or rock chip results and therefore warrant further investigation. Figure 5. Bauloora Project overview showing BLEG sampling locations and anomalous drainage areas warranting follow up work. Page 6 of 18 | ABN 43 650 398 897 3/202 Russell Street Bathurst, 2795 www.legacyminerals.com.au ASX: LGM Page 7 of 18 Soil and rock chip sampling program The southern extension to the soil sampling program has been completed with 2,002 soil samples collected across 7.5 km2 at 50m x 100m spacing. The soil sampling dataset that was collected in the northern portion of the vein field has been critical in the targeting strategy at the Bauloora Project. The addition of the southern extension will greatly expand and continue this effective strategy. Figure 6. Bauloora Project map with recently completed soil samples and petrology rock chip sample (blue triangle) confirming sinter related lithology While in the field the team collected 46 reconnaissance rock chips from newly identified epithermal vein occurrences. This sampling shows epithermal veins extend a further 2.5km to the south of where the company has previously sampled. Furthermore the identification of sinter related lithology in this southern area is strong evidence for widespread preservation of the epithermal system across the known epithermal vein field. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 8 of 18 Petrology observed rock banding as defined by differences in finely recrystallised quartz texture, and in grainsize, as well as locally having a small proportion of clay. The characteristics of the banded, fine grained quartz are interpreted as indicating deposition of original material as a chemical sediment, e.g. perhaps former opaline or chalcedonic silica, with a small proportion (estimated at ~1%) of fine clastic material. A chemical sedimentary (plus a little admixed clastic material - clay) is interpreted to accord with formation in a hot spring environment, perhaps as part of the sinter sheet. For example, similar textures in opaline silica sinter can be observed in the currently forming sinter sheet about the Champagne Pool at Wai-o-tapu, New Zealand. The observed textures in 11160 and 11189 do not appear to be similar to those formed in chalcedony vein fillings. Future work program Work in the near term will be focussed on ground truthing the newly identified areas of anomalism from the BLEG and soil sampling. In parallel to these activities the understanding gained from the drilling will be incorporated into the targeting strategy and target ranking criteria for the Project which will further refine targets for follow up testing. About the Bauloora Project Legacy Minerals’ Bauloora Project is located in the Lachlan Fold Belt of New South Wales which is host to world-class copper-gold orebodies including the Cadia-Ridgeway, Northparkes, and Cowal Mines. In 2023, Newmont Exploration Pty Ltd entered into a Farm-In and Joint Venture on the Projectiii. It covers a large hydrothermal alteration zone 27km2 in size, within which is an anomalous gold zone currently mapped to 15km2. Rock chip and soil samples collected by the Company from the Project area have highlighted several priority areas of anomalous precious metal values with highly anomalous values of epithermal pathfindersiv. The drilling of the first of these targets resulted in the discovery of the Bluecap Prospect returning 13m at 1.66g/t Au, 6.68g/t Ag, 0.14% Cu and 4.23% Pb+Zn from 57mi. Extensive epithermal alteration exists on the Project, including widespread zones of high-level chalcedonic veins, clay alteration and local sinter formations. The Project has seen very limited exploration drilling and the Company believes the results from work to date support the assessment that there is potential for the discovery of a low-sulphidation epithermal-style gold-silver deposit at the Bauloora Project. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 9 of 18 Figure 7. Regional setting of the Bauloora Project and major deposits in NSWv Approved by the Board of Legacy Minerals Holdings Limited. For more information: Investors: Chris Byrne CEO & Managing Director chris.byrne@legacyminerals.com.au +61 (0) 499 527 547 Media: Nicholas Read Read Corporate nicholas@readcorporate.com.au +61 (0) 419 929 046 DISCLAIMER AND PREVIOUSLY REPORTED INFORMATION Information in this announcement is extracted from reports lodged as market announcements referred to above and available on the Company’s website https://legacyminerals.com.au/. The Company confirms that it is not aware of any new information that materially affects the information included in the original market announcement and that all material assumptions and technical parameters underpinning the estimates in the relevant market announcement continue to apply and have not materially changed. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 10 of 18 This announcement contains certain forward-looking statements. Forward looking statements are only predictions and are subject to risks, uncertainties and assumptions which are outside of the control of Legacy Minerals Holdings Limited (LGM). These risks, uncertainties and assumptions include commodity prices, currency fluctuations, economic and financial market conditions, environmental risks and legislative, fiscal or regulatory developments, political risks, project delay, approvals and cost estimates. Actual values, results or events may be materially different to those contained in this announcement. Given these uncertainties, readers are cautioned not to place reliance on forward-looking statements. Any forward-looking statements in this announcement reflect the views of LGM only at the date of this announcement. Subject to any continuing obligations under applicable laws and ASX Listing Rules, LGM does not undertake any obligation to update or revise any information or any of the forward-looking statements in this announcement to reflect changes in events, conditions or circumstances on which any forward-looking statements is based. COMPETENT PERSON’S STATEMENT The information in this Report that relates to Exploration Targets and Exploration Results is based on information compiled by Thomas Wall, a Competent Person who is a Member of the Australian Institute of Geoscientists. Mr Wall is the Technical Director and a full-time employee of Legacy Minerals Pty Limited, the Company’s wholly-owned subsidiary, and a shareholder of the Company. Mr Wall has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Wall consents to the inclusion of the matters based on this information in the form and context in which it appears in this announcement. SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 11 of 18 About Legacy Minerals Legacy Minerals is an ASX-listed public company that has been exploring gold, copper, and base-metal projects in NSW since 2017. The Company has nine projects that present significant discovery opportunities for shareholders. 0B0B0BAu-Ag Black Range (EL9464, EL9589) 1B1B1BCu-Au Drake (EL6273, EL9616, EL9727, ALA75) Extensive low-sulphidation, epithermal system with limited historical exploration. Epithermal occurrences across 30km of strike. Large caldera (~150km2) with similar geological characteristics to other major pacific rim low-sulphidation deposits. 2B2BCu-Au Rockley (EL8926) 3B3B3B Au-Cu (Pb-Zn) Cobar (EL9511) Helix JV Prospective for porphyry Cu-Au and situated in the Macquarie Arc Ordovician host rocks with historic highgrade copper mines that graded up to 23% Cu. Undrilled targets next door to the Peak Gold Mines. Several priority geophysical anomalies and gold in lag up to 1.55g/t Au. Au-Ag Bauloora (EL8994, EL9464) Newmont JV One of NSW’s largest low-sulphidation, epithermal systems with a 27km2 epithermal vein field. 6B Au Harden (EL9657) Large historical high-grade quartz-vein gold mineralisation. Drilling includes 3.6m at 21.7g/t Au 116m and 2m at 17.17g/t Au from 111m. Au-Cu Fontenoy (EL8995) Earth AI JV Cu-Au Glenlogan (EL9614) S2 Resources JV Large, undrilled magnetic anomaly underneath Silurian cover located 55kms from Cadia Valley. Significant PGE, Au and Cu anomalism defined in soil sampling and drilling. Significant drill intercepts include 120m @ 0.3g/t PGE from 298, and 79m at 0.27% Cu from 1.5m. 4B4B4CCCu-Au Thomson (EL9190, EL9194, EL9728) Prospective for intrusion-related gold and copper systems the Project contains numerous ‘bullseye’ magnetic and gravity anomalies that remain untested. Figure 8. Location of Legacy Minerals’ Projects in NSW, Australia, and major mines and deposits SIGN UP TO LEGACY MINERALS’ INTERACTIVE INVESTOR HUB ASX: LGM Page 12 of 18 Appendix 1 – Drill hole collar details Table 1. Drill hole collar details Hole ID GRS Easting Northing RL (m) Dip Azimuth (True North) Depth (m) QU001 MGA94/55 588559 6177903 419.8 -60.4 80.0 350 QU002 MGA94/55 588292 6178465 455.3 -59.7 75.5 200.2 QU003 MGA94/55 588884 6177458 460.0 -60.0 80.3 200 TH001 MGA94/55 588451 6177525 462.2 -60.6 70.7 200 Appendix 2 – Rock sample vein summaries Reference Easting Northing Estimated Vein % Estimated Sulphide % Preliminary Observations - nature of mineral occurrence, mineral identification and estimated sulphide proportion Figure 1: Sample 11189 588399 6172587 100 0 CC chc Observation codes: qtz – quartz, crb – carbonate, chc – chalcedony, adu – adularia, fl – fluorite, sph – sphalerite, gal – galena, cpy – chalcopyrite, hem – hematite, py – pyrite, CC – crustiform-colloform, Tr – trace. Appendix 3 – JORC Code, 2021 Edition Table 1 Section 1 Sampling Techniques and Data Criteria JORC Code Explanation Commentary Nature and quality of sampling (e.g., cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. Stream sediment sampling was conducted to sample catchments around 5km2. Petrography samples were reconnaissance in nature a biased towards outcrop and alteration. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Sampling Techniques Drilling techniques The purpose of the stream sediment samples was to establish the location and tenor of regionally anomalous weathering drainages. The reconnaissance style of stream sediment sampling and petrography rock chip sampling is appropriate for this type of work. Aspects of the determination of mineralisation that are Material to the Public Report. In cases where ‘industry standard’ work has been done this would be relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g., submarine nodules) may warrant disclosure of detailed information. Stream sediment samples and rock samples weighing up to 1.2 kilograms were taken. Drill type (e.g., core, reverse circulation, open‐hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diametre, triple or standard tube, Not applicable. No drilling completed. Page 12 of 18 | ABN 43 650 398 897 3/202 Russell Street Bathurst, 2795 www.legacyminerals.com.au ASX: LGM Page 13 of 18 depth of diamond tails, face sampling bit or other type, whether core is oriented and if so, by what method, etc). Drill sample recovery Logging Method of recording and assessing core and chip sample recoveries and results assessed. Not applicable. No drilling completed. Measures taken to maximise sample recovery and ensure representative nature of the samples. Not applicable. No drilling completed. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. Not applicable. No drilling completed. Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Geological logging is carried out on all rock chips with lithology, alteration, mineralisation, structure and veining recorded. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. Logging of rock chips records lithology, mineralogy, mineralisation, structures, weathering, colour and other noticeable features. Rock chips are occasionally photographed for reference. The total length and percentage of the relevant intersections logged. Not Applicable. No drilling conducted. If core, whether cut or sawn and whether quarter, half or all core taken. If non‐core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Sub‐sampling techniques and sample preparation Quality control procedures adopted for all subsampling stages to maximise representivity of samples. Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second‐ half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled. The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. Quality of assay data and laboratory tests For geophysical tools, spectrometres, handheld XRF instruments, etc, the parametres used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. Not Applicable. No drilling conducted. Not Applicable. No drilling conducted. Samples were sent by Legacy Minerals Holdings personnel to the Newmont Denver Geochemistry Lab. Samples are dried and produce a homogenous representative sub‐sample for analysis. Laboratory QC procedures for stream sediment sample assays involve the use of internal certified reference material as assay standards. Not appropriate for this stage of exploration. The sample sizes are appropriate to correctly represent the mineralization based on style of mineralisation. All samples were analysed by the Newmont Denver Geochemistry