Announcement PDF ASX ANNOUNCEMENT Alteration and Quartz–Sulphide Veining Logged 1.25 km from Wilfred Discovery BDRC010C logged a 34 m altered and veined interval from 62 m downhole, including two intervals of stronger quartz–sulphide veining. Assays are pending. Highlights: • A 34 m downhole zone of alteration and quartz veining has been logged in BDRC010C from 62 m to 96 m, approximately 1,250 m north-west of BDRC001 and BDRC002 along the interpreted Gold Ridge corridor, including more strongly developed quartz–sulphide veining from 78 m to 84 m and from 91 m to 96 m, and visually estimated 0.3–0.8% pyrite logged from 78 m to 84 m and from 90 m to 96 m, occurring as disseminations and in veinlets [Competent Person to confirm, including 78–84 m]. These are visual geological observations, not gold assay intersections. • The lithological sequence logged in BDRC010C is similar to that logged in BDRC002 (refer Reference 6). All intervals quoted are downhole widths. • Exploration momentum continues. As at 11 October 2026, ten RC holes (BDRC001–BDRC009 and BDRC010C) had been completed, with 2,252 m drilled in total including BDRC010A, BDRC010B and BDRC010C. The RC rig is now setting up on BDRC011, which is designed to test the interpreted zone at depth, ahead of drilling at Ali and Mag. • Samples from BDRC010C are in transit to the SGS laboratory and will be prioritised for fast turnaround, with assays expected before the end of October 2026. • Samples from BDRC003 to BDRC009 are at the SGS laboratory, with assay results expected from early November 2026, subject to laboratory turnaround and QA/QC review. • Diamond drilling is planned to commence following mobilisation of the Easy Drill rig in mid to late October 2026, targeting down-dip and along-strike extensions of the previously reported mineralisation around BDRC001 and BDRC002. • Dalaroo is advancing plans for an induced polarisation (IP) survey along the approximately 7 km Gold Ridge corridor to help prioritise additional drill targets at Wilfred, Ali and Mag. Cautionary statement: Visual observations of alteration and sulphides are not a substitute for laboratory analysis; assay results are required to determine thepresence and grade of any gold mineralisation. Assay results for BDRC010C are expected before the end of October 2026. 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. Dalaroo Metals Limited (ASX: DAL, OTCQB: DALMF) (“Dalaroo” or “the Company”) reports further geological observations from its maiden RC drilling campaign at the Bondoukou Gold Ridge Project in Côte d’Ivoire. Logging 12 October 2026 2 dalaroometals.com.au | ASX: DAL of BDRC010C has identified a 34 m downhole interval of alteration and quartz veining from 62 m to 96 m, with locally stronger quartz–sulphide veining. The sequence displays similarities to previously reported discovery hole BDRC002 (refer Reference 6). While these geological similarities are encouraging, assays are required to establish whether BDRC010C contains gold mineralisation. With follow-up diamond drilling planned, further RC targets ahead and multiple assay results expected from early November, Dalaroo is progressing a systematic evaluation of the wider Gold Ridge corridor. For further information about Dalaroo, please click here. Management Commentary Dalaroo Chief Executive Officer, John Morgan, commented: “Our first reported high-grade gold intersections at Wilfred established an exciting starting point for exploration at Gold Ridge. We are encouraged that BDRC010C has now encountered alteration, quartz–sulphide veining and a rock sequence comparable to that seen in BDRC002. The immediate priority is to establish, through laboratory assays and follow-up drilling, whether these geological features are associated with further gold mineralisation and how the system is oriented.” “We have a substantial program ahead of us. The diamond rig is planned to mobilise in mid to late October to test extensions of the known high-grade intersections, while additional RC drilling, assays expected from early November and a proposed IP survey will help us assess targets along the approximately 7 km corridor. Oriented diamond core will be especially valuable in developing the structural interpretation and designing the next phase of drilling. Our focus is on building the geological evidence required to assess the scale and continuity of mineralisation.” Refer to the cautionary statement on visual estimates on page 1. BDRC010C Logging Shows Geological Similarities to Discovery Hole BDRC002 Geological logging of BDRC010C shows a lithological sequence similar to that logged in BDRC002. An altered and quartz-veined zone with pyrite logged from 78 m was identified in BDRC010C from 62 m to 96 m. Pyrite is logged over 12 m of this 34 m interval (78–84 m, 90–91 m and 91–96 m), with quartz–sulphide veining strongest from 78 m to 84 m and from 91 m to 96 m. Pyrite is logged as disseminated grains from 90 m to 91 m and as disseminated grains and veinlets from 91 m to 96 m; the occurrence of pyrite from 78 m to 84 m is [Competent Person to confirm]. Pyrite is also logged below this interval. This alteration is seen approximately 1,250 m north- west of BDRC001 and BDRC002 along the interpreted Gold Ridge corridor. A comparison of the geological logs for BDRC002 and BDRC010C shows that the two holes intersected a similar rock sequence at broadly similar depths below collar. Both holes were drilled at −60°, but in opposite directions (BDRC002 towards 225° and BDRC010C towards 045°) and approximately 1.25 km apart, so this depth correspondencedoes notindicate thattheholes intersected the samestructure or that thezones areconnected. Geological similarity does not imply that BDRC010C contains gold mineralisation of a similar grade or width. All depths are downhole. Upper zone: In BDRC002, the upper zone from 63 m to 81 m (refer Reference 6) comprises foliated, strongly silicified volcaniclastic rocks with quartz–sulphide veining, logged with approximately 1% pyrite and 1% vein (visual estimates). BDRC010C intersected a comparable package from 62 m to 96 m, logged as foliated to schistose volcaniclastic rocks and quartz veins with weak to pervasive silicification, with locally 0.3% to 0.8% pyrite and quartz–sulphide veining, most strongly developed from 78 m to 84 m and from 91 m to 96 m. Lower zone: Below the upper zone, both holes pass through basalt (mafic volcanic) before returning to altered, pyrite-bearing rocks. In BDRC002, this lower zone from 109 m to 128 m comprises silicified volcaniclastic rocks with quartz–sulphide veining, logged with 0.5% pyrite and 0.7% to 1% vein (visual estimates). In BDRC010C, 3 dalaroometals.com.au | ASX: DAL pyrite and quartz–sulphide veining are logged from 96 m to 103 m, including 1% pyrite from 96 m to 100 m and 0.3% pyrite from 100 m to 103 m (visual estimates), and volcaniclastic rocks with pervasive chlorite alteration and approximately 0.7% disseminated andveinlet pyritearelogged from115 m to 160 m,with 0.3% disseminated pyrite in basalt from 160 m to 170 m. Volcaniclastic rocks with moderate chlorite alteration and 0.1% to 0.4% predominantly disseminated pyrite are logged from 170 m to the end of hole at 232 m, with strong schistosity from 170 m to 183 m, feldspar (albite and orthoclase) from 183 m to 190 m, and quartz–sulphide veinlets with 0.4% pyrite from 210 m to 228 m. Structure: In both holes, the altered and sulphide-bearing intervals carry a foliation, cleavage or shear fabric, logged as strong in parts. In BDRC002, the gold intercepts coincide with this foliation and quartz–sulphide veining. Sulphide percentages for BDRC010C are visual estimates from RC chip logging. Assay results are required to determine the presence and grade of any gold mineralisation in BDRC010C and are expected before the end of October 2026. Figure 1a. Drill chip trays from hole BDRC010C, 50–100 m (1 m intervals). The red outline marks the altered and quartz-veined zone logged visually from 62 m to 96 m, with pyrite logged from 78 m (78–84 m and 90–96 m); the pyrite occurrence logged for each interval is set out in Table 1. Assays are pending. Figure 1b. Drill chips from hole BDRC010C, 150–232 m, showing strong schistosity (170–183 m), feldspar with pyrite (183–190 m) and pyrite with quartz–sulphide veinlets (210–228 m). Refer to the cautionary statement on visual estimates on page 1. 4 dalaroometals.com.au | ASX: DAL Table 1. Visual estimates of vein and sulphide abundance in BDRC010C, 0–232 m downhole. Refer to the cautionary statement on visual estimates on page 1. From (m) To (m) Lithology Alteration (intensity) Vein type Vein (%) Sulphide Sulphide (%) Occurrence 0 12 Laterite / ferricrete Hematite (strong) – – – – 12 19 Unknown / mixed (quartz vein 13–19 m) Hematite (strong) Quartz 0.4 – – 19 43 Unknown / mixed Limonite / goethite (strong) – – – – 43 62 Unknown / mixed Limonite / goethite (strong) Quartz 0.1 – – 62 78 Volcaniclastic Silicification (weak) Quartz 0.4 – – 78 84 Quartz vein with volcaniclastic Silicification (strong) Quartz– sulphide 1 Pyrite 0.5 Minor Veining 84 88 Quartz vein (milky) Silicification Quartz 1 – – 88 90 Volcaniclastic with quartz vein Silicification (weak) Quartz 0.1 – – 90 91 Volcaniclastic with quartz vein Silicification (strong) Quartz 0.3 Pyrite 0.3 Disseminated 91 96 Quartz vein with volcaniclastic Silicification (pervasive) Quartz– sulphide 1 Pyrite 0.8 Disseminated & Veinlets 96 100 Basalt / mafic volcanic with quartz vein Potassic (strong) Quartz– sulphide 0.7 Pyrite 1 Disseminated & Veinlets 100 103 Volcaniclastic with quartz vein Silicification (moderate) Quartz– sulphide 0.2 Pyrite 0.3 Disseminated 103 115 Basalt / mafic volcanic with quartz vein Chlorite (moderate) Quartz 0.1 – – 115 160 Volcaniclastic Chlorite (pervasive) – – Pyrite 0.7 Disseminated & Veinlets 160 170 Basalt / mafic volcanic with volcaniclastic – – – Pyrite 0.3 Disseminated 170 183 Volcaniclastic (strong schistosity) Chlorite (moderate) – – Pyrite 0.2 Disseminated 183 186 Volcaniclastic with feldspar (albite and orthoclase) Chlorite (moderate) – – Pyrite 0.3 Disseminated 186 190 Volcaniclastic with feldspar (albite and orthoclase) Chlorite (moderate) – – Pyrite 0.3 Disseminated 190 210 Volcaniclastic Chlorite (moderate) – – Pyrite 0.3 Disseminated 210 228 Volcaniclastic with quartz– sulphide veinlets Chlorite (moderate) Quartz– sulphide 0.4 Pyrite 0.4 Disseminated & Veinlets 228 232 Volcaniclastic Chlorite (moderate) – – Pyrite 0.1 Disseminated Notes: Visual estimates are the logging geologist’s estimates of percentage by volume for each logged interval.“–”= not observed. For 170–232 m, the sub- intervals shown are based on the logging geologist’s comments. Pyrite is the only sulphide logged. Vein orientations and true widths cannot be determined from RC chips; all intervals are downhole. Laboratory assay results for BDRC010C are expected before the end of October 2026. Table 1 summarises the visual estimates of veining and sulphide abundance recorded in BDRC010C. Quartz– sulphide veining and pyrite are logged within the altered interval from 78 m to 103 m downhole, with the strongest combined vein and pyrite estimates within the 62–96 m zone recorded from 78–84 m and 91–96 m, and the highest pyrite estimate in the hole (1%, with 0.7% vein) recorded from 96 m to 100 m, immediately below that zone; pyrite is also logged in the lower intervals from 115 m to the end of hole at 232 m, including quartz–sulphide veinlets with 0.4% pyrite from 210 m to 228 m. These observations provide geological context for the logged 5 dalaroometals.com.au | ASX: DAL alteration and veining but are based on visual estimates from RC chips and do not confirm gold mineralisation; laboratory assays are required to determine gold presence and grade. The lithological sequence in BDRC010C is similar to that logged in BDRC002 (Figures 4 and 5). The RC rig is now setting up on the next hole in the program, BDRC011, which will be drilled from the same drill pad as BDRC009 and has been designed as a scissor hole to BDRC010C, drilled in the opposite direction across the interpreted target zone. BDRC011 is intended to test for continuation of the alteration and sulphides logged in BDRC010C at depth, and to help constrain the orientation of the target zone, which may be subvertical. The hole is planned to intersect the target zone between approximately 120 m and 150 m downhole. Figure 2. Dalaroo geologists reviewing RC chip trays at the drill rig. Figure 3. Section B–B′ (045°/225°): BDRC009, BDRC010C (EOH 232 m) and planned scissor hole BDRC011 (225°/−60°, 250 m). BDRC010C: alteration and quartz from 62 m; quartz-veined zone 78–96 m; chlorite alteration, 0.1–0.7% pyrite from 115 m (visual estimates; refer cautionary statement, page 1). Assays pending. True widths unknown. 6 dalaroometals.com.au | ASX: DAL Review of Hole BDRC002 BDRC002 was drilled at the Wilfred target as a scissor pair with BDRC001, at a dip of −60° towards 225° (BDRC001 was drilled towards 045°), to test the quartz reef and its extensions at depth. The hole was ended at 210 m due to dip deviation. BDRC002 returned two previously reported significant intersections (refer Reference 6): • 18 m at 7.31 g/t Au from 63 m (131.6 gram-metres); and • 16 m at 1.46 g/t Au from 113 m (23.4 gram-metres). The 18 m high-grade interval corresponds to a logged unit of strongly silicified volcaniclastic rock with quartz– sulphide veining and pyrite, and the gold intercepts coincide with a strong foliation and quartz–sulphide veining (Figures 4 and 5). All widths are downhole; true widths, geometry and continuity of the mineralisation are not yet known. Follow-up diamond drilling will include a hole from the BDRC002 collar at −70° towards 225° to 250 m, designed to test the mineralised zones below both intercepts, along with step-out holes approximately 80 m north-west and south-east of BDRC002. Figure 4. BDRC002 chip trays showing previously reported assay intercepts (refer Reference 6). BDRC002 18 m @ 7.31 g/t Au from 63 m 16 m @ 1.46 g/t Au from 113 m 7 dalaroometals.com.au | ASX: DAL Figure 5. Close-up of the mineralised zone in BDRC002 with grades associated with corresponding intervals (refer Reference 6). Diamond Drilling to Test Extensions of High-Grade Gold Discovery Following the high-grade results from the first drill section (refer Reference 6), Dalaroo will mobilise a diamond drill rig from Easy Drill to the Bondoukou Gold Ridge Project in mid to late October 2026, with the potential for further diamond rigs from late November 2026. Easy Drill personnel are scheduled to arrive on site during the week of 12 October 2026 for site checks and preparation before mobilising later in the month. The diamond rig will begin with follow-up drilling around BDRC001 and BDRC002, testing the mineralisation down dip and along strike over approximately 160 m of strike length. • RC and diamond drilling: Dalaroo will continue the RC program to complete the orientation drilling and will also use the RC rig for follow-up holes where appropriate. Holes that need structural information, or are not suited to RC drilling, will be drilled with the diamond rig. • Benefits of diamond drilling: Oriented drill core will allow Dalaroo to better understand the structural geology controlling the gold mineralisation at Gold Ridge. Diamond rigs also have a smaller footprint, requiring less clearing at each drill site, and give better control of hole direction. • Follow-up drilling methodology: Follow-up drilling will commence at BDRC002. Drill pad preparation is under way and comprises pegging, clearing and payment of crop compensation, a process that typically requires two to four weeks. Drilling will be scheduled once compensation has been settled. Further drill planning will be undertaken on return of assay results from the initial orientation drilling. As at 11 October 2026, ten RC holes (BDRC001 to BDRC009 and BDRC010C) had been completed and two additional BDRC010 attempts (BDRC010A and BDRC010B) had been abandoned, as part of the initial 24-hole, approximately 4,200 m orientation program (refer Reference 5). The 2,252 m drilled in total includes all three BDRC010 attempts. BDRC010A and BDRC010B were stopped at 174 m and 96 m respectively due to casing failure, and the hole was redrilled from the same drill pad as BDRC010C, which was completed at 232 m, with the RC rig now setting up on BDRC011. Following BDRC011, the RC rig will move to the final drill fence at the Wilfred target, then to the Ali target for approximately 10 to 12 days of drilling, before moving to the final target, Mag, for a further 10 to 12 days. Three earlier holes were ended short of their planned 250 m depth: BDRC002 at 210 m due to dip deviation, and BDRC003 and BDRC004 at 200 m due to excessive water contamination. Drill locations, orientations, depths, drilling methods and sequencing may be adjusted as assay results and geological information become available. 0.01 g/t 0.04 g/t 0.07 g/t 3.21 g/t 5.61 g/t 3.2 g/t 3.05 g/t 5.3 g/t 7.33 g/t 8.05 g/t 10.9 g/t 8.06 g/t 6.7 g/t 13.1 g/t 6.46 g/t 8.96 g/t 1.72 g/t 5.65 g/t 15.9 g/t 6.37 g/t 12 g/t 0.13 g/t 0.15 g/t 0.02 g/t 0.1 g/t 0.04 g/t 0.03 g/t 0.02 g/t 0.03 g/t 0.02 g/t 8 dalaroometals.com.au | ASX: DAL Figure 6. RC rig drilling at the Bondoukou Gold Ridge Project. Figure 7. Soil-gold anomalism along the ~7 km Mag–Wilfred–Ali corridor, with completed Wilfred RC holes (BDRC001–010C; BDRC001/002 assayed), next hole BDRC011 (red), final Wilfred fence PHD003/004, and planned Mag and Ali holes. 9 dalaroometals.com.au | ASX: DAL Assay update: Seasonal rainfall has restricted heavy vehicle access to site, though light vehicle access continues. Samples that became damp before transport to the Company’s Bondoukou office and the SGS laboratory need extra drying before preparation. BDRC003 to BDRC009 samples are at the laboratory, with assays expected fromearly November 2026.BDRC010C samples are in transitand willbeprioritised,with assays expected before the end of October 2026. Both timings are subject to laboratory turnaround and QA/QC review. BDRC010A and BDRC010B, superseded by BDRC010C, had not been logged at release and will be logged, sampled and assayed as a low priority. Dalaroo has since modified on-site sample storage to minimise rainfall exposure before weekly dispatch to the laboratory. Geophysics planning Following the results fromBDRC001 and BDRC002, Dalaroo is finalising arrangements to commence an induced polarisation (IP) and resistivity survey at the Bondoukou Gold Ridge Project. The preliminary survey scope comprises approximately 35.1 line-kilometres of 2D dipole-dipole profiling, using proposed 10-metre electrode spacing and an 800-metre array spread. Final line locations and lengths will be refined using ground magnetic survey results and geological interpretation. The survey is intended to assess subsurface variations in resistivity and chargeability and their spatial relationship to known mineralisation, geological structures and other exploration data. Chargeability responses can be associated with polarisable materials, including disseminated sulphide minerals, which may occur with gold mineralisation. IP is an indirect exploration method and does not detect gold itself; responses can also reflect other geological sources and require careful interpretation. Dalaroo intends to survey the full approximately 7 km Gold Ridge corridor, beginning around known mineralisation and extending outwards along the corridor. Infill surveying would then focus on priority areas identified from the initial results. Inverted resistivity and chargeability sections will be interpreted alongside drilling, geology, geochemistry and magnetic data to refine targets for follow-up drilling. Any anomalies will require geological assessment and drill testing to determine their significance. Figure 8. Proposed IP survey on magnetics: 15 lines (35.1 line-km) across magnetic contact. Priority 1 (red) crosses Wilfred; Priority 2 (maroon) extends to Mag and Ali. 10 dalaroometals.com.au | ASX: DAL Next Steps • Complete BDRC011 and the final Wilfred drill fence, then advance RC drilling at the Ali and Mag targets. • Mobilise the Easy Drill diamond rig in mid to late October 2026 and complete the five-hole, approximately 1,250 m follow-up program at Wilfred (refer Reference 7), testing down dip and along strike of BDRC001 and BDRC002 with oriented core, and assess additional diamond rigs from late November 2026. • Report assay results from BDRC010C, prioritised for fast laboratory turnaround and expected before the end of October 2026, and from BDRC003 to BDRC009, expected from early November 2026, subject to laboratory turnaround and QA/QC review. • Continue the 24-hole orientation program across the Wilfred, Ali and Mag targets. • Integrate the follow-up results into the three-dimensional geological model to define the orientation, true width and continuity of the mineralised zones. • Use the results to plan further step-out drilling along strike and down dip at Wilfred, and assess opportunities for deeper RC or diamond drilling. • Design subsequent drilling with an increasing emphasis on testing mineralisation continuity and geometry to support potential future Mineral Resource definition, subject to encouraging assay results and geological interpretation. Technical Commentary Frank Twum-Berima Bosompem, Exploration Manager – Côte d’Ivoire, commented: “The rock sequence logged in BDRC010C is similar to that in BDRC002. We see a similar foliated, silicified volcaniclastic package with quartz veining from 62 m to 96 m and quartz–sulphide veining from 78 m to 84 m and from 91 m to 96 m, followed by basalt and then a second pyrite-bearing zone below. The structural fabric is a key part of our interpretation. “BDRC011 has been designed as a scissor hole to BDRC010C to test the zone at depth and help constrain its orientation. That information, together with oriented diamond core from the Easy Drill rig, will be important in building a reliable geological model at Wilfred. The team has also improved on-site sample storage, so samples reach the laboratory in better condition during the wet season. We now await assays from BDRC003 to BDRC009, and from BDRC010C, to determine whether the alteration we are logging carries gold.” Refer to the cautionary statement on visual estimates on page 1. References 1. Refer Dalaroo ASX announcement, 9 March 2026: “Bondoukou Goldridge Due Diligence Assay Results”. 2. Refer Dalaroo ASX announcement, 19 March 2026: “Major 2.5 km Gold Drill Target Defined at Gold Ridge Bondoukou Project, Côte d’Ivoire”. 3. Refer Dalaroo ASX announcement, 2 June 2026: “Gold Ridge Soils Define 4.3km Anomaly, Peak 2,188ppb Au”. 4. Refer Dalaroo ASX announcement, 15 June 2026: “Dalaroo Defines ~7km Gold Corridor at Gold Ridge with Peak Soil Assay of 23.26g/t Au”. 5. Refer Dalaroo ASX announcement, 28 September 2026: “Drilling Progresses at Bondoukou Gold Ridge Project Amended”. 6. Refer Dalaroo ASX announcement, 7 October 2026: “Dalaroo Makes High-Grade Gold Discovery at Bondoukou – 18 m at 7.31 g/t Au from Maiden Drilling”. 7. Refer Dalaroo ASX announcement, 9 October 2026: “Dalaroo to Follow Up High-Grade Gold Discovery at Bondoukou – Drilling Planned Around 18 m at 7.31 g/t Au”. 11 dalaroometals.com.au | ASX: DAL This announcement has been authorised for release to the ASX by the Company’s Board of Directors. ENDS For more information: Please visit our website: Dalaroo Metals Website John Morgan Chief Executive Officer T: +61 410 774 319 E: info@dalaroometals.com.au Competent Person’s Statement The information in this announcement that relates to Exploration Results is based on, and fairly represents, information and supporting documentation compiled by Mr John Morgan, a Member of the Australasian Institute of Mining and Metallurgy. Mr Morgan is a full-time employee and Chief Executive Officer of Dalaroo Metals Limited and holds shares and performance rights in the Company. Mr Morgan has sufficient experience relevant to the style of mineralisation and type of deposit under consideration, and to the exploration activities 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 (JORC Code). Mr Morgan consents to the inclusion in this announcement of the matters based on his information in the form and context in which they appear. The Exploration Results addressed in this announcement include preliminary geological observations from the Company’s current RC drilling program, including BDRC010C, and previously reported Exploration Results, including the assay results for BDRC001 and BDRC002, identified in the References section. No new laboratory assay results are reported in this announcement. The geological observations are visual and preliminary in nature, and laboratory assays are required to determine whether gold mineralisation is present and, if so, its grade and significance. JORC Code Table 1 disclosures covering Sections 1 and 2 are provided in Appendix 1 and relate to the current RC drilling program and the preliminary geological observations reported in this announcement. The Company confirms that it is not aware of any new information or data that materially affects the previously reported Exploration Results referenced in this announcement. The Company also confirms that the form and context in which the relevant Competent Person’s findings were presented have not been materially modified from the original market announcements. Forward-Looking Statements This announcement contains forward-looking statements which are based on current expectations, assumptions, estimates and projections. Forward-looking statements are subject to known and unknown risks, uncertainties and other factors that may cause actual results, performance or achievements to differ materially from those expressed or implied. These risks include, but are not limited to, exploration success,geological interpretation, commodityprice fluctuations,regulatory approvals,permitting timelines, operational risks and market conditions. Any statements regarding potential mineralisation, drill targets, grades, scale or development concepts are conceptual in nature and based on early-stage exploration activities, including geological mapping, surface sampling, auger drilling, geochemical analysis, geophysical surveying and early-stage RC drilling. These statements do not constitute, and should not be construed as, a Mineral Resource or Ore Reserve estimate as defined under the JORC Code. Dalaroo Metals Limited undertakes no obligation to update or revise any forward-looking statements, except as required by law. About Dalaroo Metals Dalaroo Metals Limited is an ASX-listed exploration company focused on the discovery and development of high-quality gold and critical minerals projects across Australia and international jurisdictions. The Company’s portfolio includes the Blue LagoonProject in south-west Greenland, prospective for rare earth elements (REE), zirconium and niobium, a rapidly growing portfolio of gold exploration assets in Côte d’Ivoire, including the Bondoukou Gold Ridge Project within the highly endowed Birimian Greenstone Belt of West Africa, and the Lyons River and Watheroo Projects in Western Australia. Dalaroo’s strategy is to systematically advance its projects through modern exploration techniques, resource definition, and strategic partnerships, with a strong focus on value creation for shareholders. The Company is committed to responsible exploration, strong corporate governance and building long- term stakeholder relationships in the regions in which it operates. dalaroometals.com.au | ASX: DAL 13 dalaroometals.com.au | ASX: DAL Appendix 1 – JORC Code, 2012 Edition – Table 1 Table 2. Drill collar details, BDRC003 to BDRC010C. Grid: WGS84 / UTM Zone 30N. Hole ID Easting (m) Northing (m) RL (m) Azimuth (°) Dip (°) Planned depth (m) Depth (m) Status BDRC003 493377 896256 393 45 -60 250 200 Completed BDRC004 493466 896339 387 225 -60 250 200 Completed BDRC005 492943 896399 363 45 -60 220 220 Completed BDRC006 493040 896482 366 46 -60 150 150 Completed BDRC007 493009 896585 367 45 -60 220 220 Completed BDRC008 493046 896631 373 45 -60 150 150 Completed BDRC009 492618 896909 341 45 -60 150 150 Completed BDRC010A 492548 896838 354 45 -60 250 174 Abandoned BDRC010B 492543 896837 350 45 -60 250 96 Abandoned BDRC010C 492550 896847 354 45 -60 250 232 Completed Notes: Collar coordinates and RLs are from handheld GPS (approximately ±5–10 m horizontal accuracy) and all collar points are intended to be picked up by a qualified surveyor at the end of the program. BDRC010A, BDRC010B and BDRC010C were drilled from the same drill pad; the BDRC010A position is the planned collar. BDRC003 and BDRC004 were ended at 200 m due to excessive water. BDRC010A and BDRC010B were stopped due to casing failure. BDRC010C was completed at 232 m. All depths are downhole; true widths are not known. Section 1 – Sampling Techniques and Data Criteria Commentary Sampling techniques Samples comprise reverse circulation (RC) drill cuttings collected over nominal 1 m downhole intervals. Each interval is collected through the drill cyclone and split using a riffle splitter to produce a representative laboratory sample weighing approximately 3 kg. The remainder of each interval is retained at the drill site. Sample condition, including whether samples are dry, moist or wet, is visually monitored during drilling. Drilling t