Announcement PDF ASX ANNOUNCEMENT ASX: DAL | OTCQB: DALMF 02 June 2026 Continuous 4.3km gold-in-soil corridor, peak 2,188 ppb Au, fast-tracks Gold Ridge toward maiden drilling Coherent Gold Anomaly Coincides with 9km Geophysical Corridor, Fold-Limb Structure and Artisanal Gold Workings at Gold Ridge Bondoukou Project, Côte d'Ivoire Highlights • Priority 1 soil geochemistry program identifies a 4.3km-long coherent gold anomaly • Assays pending from an additional ~4.7km of strike, with results expected to materially expand project coverage • Peak soil assay of 2,188ppb Au (2.19 g/t Au) • Multiple contiguous soil anomalies define a robust mineralised corridor • 454 samples returned >20ppb Au, including 27 samples exceeding 200ppb Au • Gold anomaly coincides with interpreted 9km-long geophysical corridor • Anomaly positioned along mapped fold-limb structure identified during recent geological mapping2 • Strong correlation between soil anomaly, artisanal workings, quartz veining and favourable lithological contacts • Results validate Dalaroo's geological and structural model for Gold Ridge mineralisation • 5,000m Auger drilling program designed to test validity and enrichment of anomalous zone • Gold Ridge continues to demonstrate characteristics commonly associated with significant Birimian-hosted gold systems Dalaroo Metals Ltd (ASX: DAL; OTCQB: DALMF) (“Dalaroo” or “the Company”) is pleased to announce significant results from the recently completed Priority 1 soil geochemistry program at the Gold Ridge Prospect within the Bondoukou Gold Project, Côte d'Ivoire. Results from the Priority 1 program have defined a robust and coherent gold-in-soil anomaly extending approximately 4.3km along strike, with peak gold values of up to 2,188ppb Au (2.19g/t Au). The anomaly occurs within a broader interpreted 9km-long geophysical corridor and is spatially associated with mapped artisanal workings, quartz veining, favourable lithological contacts and a major fold-limb structure identified during recent geological mapping2 . Importantly, the newly defined gold anomaly provides strong geochemical confirmation of Dalaroo's geological model for Gold Ridge and significantly strengthens the potential for a large structurally controlled Birimian gold system. To rapidly advance the project toward drilling, Dalaroo has completed the design of a 5,000m auger drilling program that will test the anomaly below the weathered profile and determine whether the gold mineralisation is sourced from in-situ bedrock mineralisation prior to maiden RC drilling. 2 Dalaroo’s CEO John Morgan commented: “The results from Gold Ridge represent a significant milestone for Dalaroo and provide strong validation of our exploration model. Defining a coherent 4.3km gold anomaly associated with a 9km structural corridor, extensive artisanal workings and favourable geology substantially enhances our confidence in the scale potential of the system. Importantly, these results provide a clear pathway to drilling. Our upcoming auger program has been specifically designed to test the bedrock source of the anomaly and rapidly advance the highest-priority targets toward maiden RC drilling. With multiple datasets now converging on the same corridor, we believe Gold Ridge is emerging as a highly compelling gold exploration opportunity within Côte d'Ivoire's prolific Birimian Greenstone Belt.” Major Gold Corridor Confirmed at Gold Ridge The Priority 1 soil geochemistry survey was completed across the southeastern portion of the Gold Ridge Prospect and comprised 2,241 primary soil samples and 120 QA/QC samples collected on a systematic 200m x 50m grid. The program provides comprehensive coverage over the highest-priority target area identified from geological mapping, rock-chip sampling, artisanal workings and structural interpretation1,2,3 . Interpretation of assay results has defined a continuous 4.3km gold anomaly with multiple elevated and high-grade soil responses outlining a coherent mineralised corridor. Peak soil values of up to 2,188ppb Au (2.19g/t Au) highlight the strength of the geochemical signature. The anomaly remains open along strike to the north-west and represents a significant gold exploration target within the broader Gold Ridge Prospect. The strongest gold values occur within a structurally favourable corridor characterised by: • Folded metasedimentary units intersecting major structural trends; • Concentrated artisanal gold workings; • Abundant quartz veining; • Strong hematite, limonite and goethite alteration; and • A major interpreted geophysical corridor extending for approximately 9km. Importantly, the highest gold values occur where these geological, structural and geophysical features overlap, indicating a strong degree of structural control on mineralisation. The close association between elevated soil geochemistry, artisanal workings, quartz veining and favourable structural architecture provides strong support for a bedrock source of mineralisation. The convergence of these independent datasets strengthens the interpretation that the anomaly reflects a coherent bedrock-hosted gold mineralising system. The results significantly enhance the prospectivity of the broader Bondoukou Gold Project and reinforce Gold Ridge as a high-priority drill target. To advance the project toward drilling, the Company has completed planning for a 5,000m auger drilling program designed to test the bedrock source of the anomaly beneath the weathered profile. The program will provide critical information for drill target generation and assist in prioritising areas for maiden RC drilling. For more Information on this release Click Here. 3 Figure 1. Gold Ridge Priority 1 Soil Geochemistry Results Showing 4.3km Gold Anomaly. Gold-in-soil anomaly map highlighting coherent anomalous gold values extending over approximately 4.3km strike length. Peak assay values of up to 2,188ppb Au occur within a broader corridor associated with artisanal workings, quartz veining and interpreted structural controls. The anomaly remains open along strike and coincides with the interpreted 9km magnetic corridor derived from airborne magnetic data. Soil assay anomalies follow topography down the south-western ridgeline. 4 Table 1. Soil assay results greater than 200ppb Au. A total of 454 samples returned values above 20ppb Au, including 27 samples exceeding 200ppb Au Sample ID Easting Northing Rl Au BDS0024 493806 896118 392 487 BDS0032 493526 895833 431 507 BDS0113 493876 896470 366 211 BDS0114 493841 896435 375 301 BDS0119 493665 896258 393 251 BDS0123 493558 896151 390 243 BDS0124 493523 896117 390 259 BDS0207 493806 895833 392 274 BDS0210 493913 895940 398 563 BDS0211 493945 895980 394 327.5 BDS0377 493207 894950 372 249 BDS0563 494516 895404 360 201 BDS0905 495642 895408 399 370 BDS0951 495221 894702 361 264 BDS0952 495254 894736 364 709 BDS0953 495290 894771 365 239 BDS0978 494266 893749 349 258 BDS1002 493487 892969 333 535 BDS1053 495501 894700 377 279 BDS1054 495468 894668 376 426 BDS1056 495397 894597 369 464 BDS1752 495470 891555 333 2188 BDS1952 493733 896612 362 230 BDS2031 493348 896505 380 300 BDS2033 493277 896435 381 204 BDS2100 492920 896648 363 245 BDS2102 492887 896609 362 205 5 Structural and Geological Controls Confirm Exploration Model The newly defined soil anomaly occurs along the contact between metasedimentary and metavolcanic lithologies and directly overlies a major geophysical corridor interpreted from airborne geophysical datasets. Recent geological mapping identified a prominent fold-limb structure coincident with the strongest soil responses and artisanal mining activity2 . The geometry of the anomaly suggests mineralisation is controlled by structural architecture rather than isolated lithological features. This interpretation is supported by: • Extensive artisanal gold workings; • Mapped quartz vein systems; • Fold-related structural controls; • Shear-related deformation; • Strong hydrothermal alteration; • Historical rock-chip assays up to 17.95g/t Au1 . The Company believes these features are characteristic of major structurally controlled Birimian gold systems throughout West Africa. Figure 2. Coherent 4.3km Gold-in-Soil Anomaly Defined Along 9km Structural-Geophysical Corridor at Gold Ridge. Gold-in-soil anomaly map highlighting a robust and continuous 4.3km anomalous corridor with peak assay values of up to 2,188ppb Au. The anomaly is coincident with artisanal gold workings, mapped fold structures, quartz veining and a 9km geophysical trend, demonstrating strong geological and structural controls on mineralisation. The anomaly forms the primary target for the upcoming 5,000m auger drilling program designed to test the bedrock source of mineralisation prior to RC drilling. 6 Auger Drilling Program Designed to Test Bedrock Source Following receipt and interpretation of the soil results, Dalaroo has finalised planning for a 5,000m auger drilling program designed to determine whether the soil anomaly is sourced from in-situ bedrock mineralisation. The program will: • Penetrate transported cover and weathered profiles; • Define the geometry of bedrock geochemical anomalies; • Determine continuity of mineralisation at depth; • Assist prioritisation of drill targets; • Refine locations for maiden RC drilling. The auger drilling program is expected to focus initially on the highest-priority portions of the 4km anomaly where peak soil values coincide with structural intersections and artisanal workings. Auger drilling represents a rapid and cost-effective method of testing whether the surface geochemical anomaly is sourced from in-situ bedrock mineralisation and will provide critical information for targeting maiden RC drilling. Figure 3. Planned Auger Drill Traverses Across Priority Gold-in-Soil Anomaly. Proposed auger drilling traverses designed to test the subsurface expression of the 4.3km gold-in-soil anomaly. The program aims to determine whether anomalous gold values are derived from in-situ bedrock mineralisation and prioritise targets for maiden RC drilling. 7 Gold Ridge Continues to Emerge as a Significant Gold Opportunity The Gold Ridge Prospect is located within the highly endowed Birimian Greenstone Belt of Côte d'Ivoire and is situated approximately 35km northwest of Endeavour Mining's Tanda-Iguela gold system. The Project occupies a favourable structural position within a region known for hosting large, structurally controlled gold deposits. Recent exploration activities, including geological mapping, reconnaissance rock-chip sampling, assessment of artisanal workings and the recently completed soil geochemistry program, have significantly enhanced the Company's understanding of the project and strengthened confidence in the underlying exploration model. The Priority 1 soil geochemistry program has defined a coherent 4.3km gold anomaly with peak values of up to 2,188ppb Au. Importantly, the anomaly is spatially associated with several key features commonly associated with Birimian-hosted gold systems, including: • Regional shear architecture; • Fold-related structural controls; • Widespread quartz veining; • Extensive artisanal gold workings; • Strong hydrothermal alteration; and • Coincident geochemical, geological and geophysical targets. The strongest gold responses occur where multiple independent datasets converge, including favourable lithological contacts, mapped fold structures, artisanal workings and a major interpreted geophysical corridor extending for approximately 9km. The close spatial relationship between these features supports the interpretation that the soil anomaly reflects a significant bedrock-hosted gold system rather than isolated surficial dispersion. The scale and continuity of the anomaly, together with widespread artisanal workings and favourable geological controls, indicate that Gold Ridge remains largely underexplored despite clear evidence of gold mineralisation at surface. The Company believes the results warrant systematic drill testing and further reinforce Gold Ridge as a high-priority target within the broader Bondoukou Gold Project. Regional Setting and Prospectivity The Bondoukou Gold Project is located within the Birimian Greenstone Belt of Côte d’Ivoire, one of the world’s most prospective gold provinces. The Project lies approximately 35km northwest of Endeavour Mining’s Tanda-Iguela gold system and within a region hosting multiple multi-million-ounce gold deposits. Gold mineralisation in the region is commonly associated with: • Regional shear zones • Fold-related structural traps • Quartz veining systems • Volcano-sedimentary contacts • Rheological contrasts between lithologies Extensive artisanal workings developed along interpreted shear zones provide strong evidence for near- surface gold mineralisation across the Project area. 8 Figure 4. Location of Dalaroo Côte d’Ivoire Projects Relative to Major Regional Gold Deposits. Regional geological map showing Dalaroo’s Côte d’Ivoire project portfolio within the Birimian Greenstone Belt relative to major gold deposits and regional structural corridors. Upcoming Catalysts Planned upcoming activities include: • Receipt of Priority 2 soil geochemistry assay results • Final prioritisation of auger drill targets • Commencement of auger drilling program • Definition of maiden RC drill targets • Mobilisation of RC drilling contractor • Maiden RC drilling commencement at Gold Ridge 9 Management Commentary Exploration Manager – West Africa, Frank Twum-Berima Bosompem, commented: "These results provide strong validation of the geological and structural model developed by our exploration team. The anomaly sits exactly where we anticipated mineralisation would occur — along the fold limb and lithological contact within the broader geophysical corridor. The scale, coherence and tenor of the anomaly, together with widespread artisanal workings and quartz veining, significantly increase our confidence in the prospectivity of Gold Ridge. The next step is to use auger drilling to determine the bedrock source of mineralisation and rapidly progress the strongest targets toward RC drilling." References: 1. Refer Dalaroo ASX announcement, 9th of March 2026: “Bondoukou Goldridge Due Diligence Assay Results” 2. Refer Dalaroo ASX announcement, 19th of March 2026: “Major 2.5 km Gold Drill Target Defined at Gold Ridge Bondoukou Project, Côte d’Ivoire” 3. Refer Dalaroo ASX announcement, 12th of May 2026: “Dalaroo Completes Soil Sampling Program at Bondoukou Gold Project” 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 for more information: Dalaroo Metals Website John Morgan Chief Executive Officer T: +61 410 774 319 E: info@dalaroometals.com.au 11 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 Lagoon Project 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 and Bongouanou Gold Projects 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. Competent Persons Statement The information in this report that relates to exploration results is based on information compiled by John Morgan, a Member of the Australasian Institute of Mining and Metallurgy (AusIMM) and the CEO of Dalaroo Metals Ltd. Mr Morgan has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity 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 report of the matters based on this information in the form and context in which it appears. 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, commodity price fluctuations, regulatory approvals, permitting timelines, operational risks and market conditions. Any statements regarding potential mineralisation, exploration targets, grades, scale or development concepts are conceptual in nature and based on early-stage surface sampling only. These statements do not constitute, and should not be construed as, a Mineral Resource or Ore Reserve estimate as defined under the JORC Code. References to peer projects, market pricing, strategic significance or potential future development pathways are provided for contextual purposes only and should not be interpreted as a forecast of future performance or valuation. Dalaroo Metals Limited undertakes no obligation to update or revise any forward-looking statements, except as required by law. The Company confirms that it is not aware of any new information or data that materially affects the information included in the referenced market announcements and that all material assumptions and technical parameters underpinning those announcements continue to apply and have not materially changed. Appendix A 12 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0002 494544 896858 388 56 SOIL WGS84_30N BDS0003 494511 896825 392 77 SOIL WGS84_30N BDS0004 494476 896789 395 22 SOIL WGS84_30N BDS0005 494445 896752 395 54 SOIL WGS84_30N BDS0006 494404 896716 391 48 SOIL WGS84_30N BDS0007 494370 896683 297 34 SOIL WGS84_30N BDS0008 494329 896650 390 67 SOIL WGS84_30N BDS0009 494301 896611 399 59 SOIL WGS84_30N BDS0010 494264 896577 400 75 SOIL WGS84_30N BDS0011 494230 896542 398 65 SOIL WGS84_30N BDS0012 494197 896507 350 24 SOIL WGS84_30N BDS0013 494159 896472 395 70 SOIL WGS84_30N BDS0014 494119 896430 385 82 SOIL WGS84_30N BDS0015 494092 896399 370 73 SOIL WGS84_30N BDS0016 494052 896365 375 57 SOIL WGS84_30N BDS0017 494015 896328 371 94 SOIL WGS84_30N BDS0018 493984 896293 370 170 SOIL WGS84_30N BDS0019 493950 896252 375 113 SOIL WGS84_30N BDS0021 493915 896221 377 96 SOIL WGS84_30N BDS0022 493876 896190 380 175 SOIL WGS84_30N BDS0023 493842 896152 387 170 SOIL WGS84_30N BDS0024 493806 896118 392 487 SOIL WGS84_30N BDS0025 493771 896081 394 59 SOIL WGS84_30N BDS0026 493735 896045 396 102 SOIL WGS84_30N BDS0027 493701 896012 409 95.5 SOIL WGS84_30N BDS0028 493664 895978 420 59 SOIL WGS84_30N BDS0029 493631 895942 426 62 SOIL WGS84_30N BDS0030 493589 895902 413 133 SOIL WGS84_30N BDS0031 493560 895870 417 92 SOIL WGS84_30N BDS0032 493526 895833 431 507 SOIL WGS84_30N BDS0033 493488 895798 433 55 SOIL WGS84_30N BDS0034 493454 895764 438 70 SOIL WGS84_30N BDS0035 493417 895730 448 72 SOIL WGS84_30N BDS0036 493381 895693 441 70 SOIL WGS84_30N BDS0037 493347 895657 429 71 SOIL WGS84_30N BDS0038 493311 895622 417 59 SOIL WGS84_30N BDS0039 493276 895588 420 91 SOIL WGS84_30N BDS0040 493240 895548 425 65 SOIL WGS84_30N BDS0041 493204 895513 423 65 SOIL WGS84_30N BDS0042 493171 895478 397 69 SOIL WGS84_30N BDS0043 493112 895447 396 66 SOIL WGS84_30N BDS0044 493097 895410 379 61 SOIL WGS84_30N BDS0046 493063 895371 376 65 SOIL WGS84_30N BDS0047 493023 895338 383 82 SOIL WGS84_30N BDS0048 492995 895302 386 67 SOIL WGS84_30N BDS0049 492958 895267 381 68 SOIL WGS84_30N BDS0050 492918 895236 389 70 SOIL WGS84_30N BDS0051 492890 895199 371 74.5 SOIL WGS84_30N BDS0052 492854 895162 376 70 SOIL WGS84_30N BDS0053 492816 895127 374 67 SOIL WGS84_30N 13 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0054 492781 895093 375 65 SOIL WGS84_30N BDS0055 492744 895056 371 64 SOIL WGS84_30N BDS0056 492742 895023 371 71 SOIL WGS84_30N BDS0057 492672 894984 370 79 SOIL WGS84_30N BDS0058 492641 894951 366 77 SOIL WGS84_30N BDS0059 492606 894914 363 63 SOIL WGS84_30N BDS0060 492569 894880 361 83 SOIL WGS84_30N BDS0061 492533 894842 361 68 SOIL WGS84_30N BDS0062 492498 894810 362 62 SOIL WGS84_30N BDS0063 492469 894773 355 67 SOIL WGS84_30N BDS0064 492428 894738 353 70 SOIL WGS84_30N BDS0066 492392 894703 351 48 SOIL WGS84_30N BDS0067 492357 894668 355 60 SOIL WGS84_30N BDS0068 492319 894632 352 71 SOIL WGS84_30N BDS0069 492285 894594 353 67 SOIL WGS84_30N BDS0070 492251 894560 353 50.5 SOIL WGS84_30N BDS0071 492217 894526 350 51 SOIL WGS84_30N BDS0072 492179 894488 355 52 SOIL WGS84_30N BDS0073 492143 894454 350 50 SOIL WGS84_30N BDS0074 492109 894421 346 59 SOIL WGS84_30N BDS0075 492074 894386 342 52 SOIL WGS84_30N BDS0076 492040 894350 342 57 SOIL WGS84_30N BDS0077 491998 894316 338 53 SOIL WGS84_30N BDS0078 491967 894280 337 56 SOIL WGS84_30N BDS0079 491933 894244 330 47 SOIL WGS84_30N BDS0080 491896 894208 333 7 SOIL WGS84_30N BDS0081 491861 894178 333 17 SOIL WGS84_30N BDS0082 491786 894105 334 53 SOIL WGS84_30N BDS0083 491756 894068 332 57 SOIL WGS84_30N BDS0084 491719 894032 335 58 SOIL WGS84_30N BDS0086 491687 893996 331 85 SOIL WGS84_30N BDS0087 491649 893961 334 67 SOIL WGS84_30N BDS0088 491613 893926 333 63 SOIL WGS84_30N BDS0089 491577 893887 343 90 SOIL WGS84_30N BDS0090 491543 893856 341 73 SOIL WGS84_30N BDS0091 493275 895304 380 82 SOIL WGS84_30N BDS0092 493304 895334 385 91 SOIL WGS84_30N BDS0093 493347 895374 392 72 SOIL WGS84_30N BDS0094 493382 895410 395 70 SOIL WGS84_30N BDS0095 493415 895444 402 70 SOIL WGS84_30N BDS0096 493452 895478 408 66 SOIL WGS84_30N BDS0097 493487 895513 402 72 SOIL WGS84_30N BDS0098 493523 895550 397 62 SOIL WGS84_30N BDS0099 493560 895558 395 62 SOIL WGS84_30N BDS0100 493595 895623 395 76 SOIL WGS84_30N BDS0102 494265 896859 366 7 SOIL WGS84_30N BDS0103 494230 896824 369 6 SOIL WGS84_30N BDS0104 494196 896788 376 6 SOIL WGS84_30N BDS0105 494160 896754 376 18 SOIL WGS84_30N BDS0106 494126 896722 387 6 SOIL WGS84_30N 14 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0107 494090 896682 385 44 SOIL WGS84_30N BDS0108 494054 896646 389 8.5 SOIL WGS84_30N BDS0109 494018 896611 386 7 SOIL WGS84_30N BDS0110 493983 896576 382 8 SOIL WGS84_30N BDS0111 493948 896540 376 2.5 SOIL WGS84_30N BDS0112 493912 896505 369 2.5 SOIL WGS84_30N BDS0113 493876 896470 366 211 SOIL WGS84_30N BDS0114 493841 896435 375 301 SOIL WGS84_30N BDS0115 493804 896400 379 105 SOIL WGS84_30N BDS0116 493770 896364 402 74 SOIL WGS84_30N BDS0117 493735 896329 408 100 SOIL WGS84_30N BDS0118 493700 896293 403 100 SOIL WGS84_30N BDS0119 493665 896258 393 251 SOIL WGS84_30N BDS0121 493630 896223 388 97 SOIL WGS84_30N BDS0122 493594 896188 388 131 SOIL WGS84_30N BDS0123 493558 896151 390 243 SOIL WGS84_30N BDS0124 493523 896117 390 259 SOIL WGS84_30N BDS0125 493487 896080 389 39 SOIL WGS84_30N BDS0126 493452 896045 390 43 SOIL WGS84_30N BDS0127 493418 896010 389 17 SOIL WGS84_30N BDS0128 493382 895975 388 17 SOIL WGS84_30N BDS0129 493346 895940 397 2.5 SOIL WGS84_30N BDS0130 493311 895904 400 2.5 SOIL WGS84_30N BDS0131 493276 895870 410 2.5 SOIL WGS84_30N BDS0132 493241 895833 411 2.5 SOIL WGS84_30N BDS0133 493205 895798 407 2.5 SOIL WGS84_30N BDS0134 493168 895762 395 2.5 SOIL WGS84_30N BDS0135 493135 895728 394 2.5 SOIL WGS84_30N BDS0136 493099 895692 394 2.5 SOIL WGS84_30N BDS0137 493064 895657 392 37 SOIL WGS84_30N BDS0138 493027 895622 392 2.5 SOIL WGS84_30N BDS0139 492994 895587 383 2.5 SOIL WGS84_30N BDS0140 492957 895550 383 2.5 SOIL WGS84_30N BDS0141 492921 895516 383 2.5 SOIL WGS84_30N BDS0142 492887 895479 379 2.5 SOIL WGS84_30N BDS0143 492852 895445 379 2.5 SOIL WGS84_30N BDS0144 492815 895409 375 2.5 SOIL WGS84_30N BDS0146 492782 895374 374 2.5 SOIL WGS84_30N BDS0147 492745 895338 372 2.5 SOIL WGS84_30N BDS0148 492711 895304 381 2.5 SOIL WGS84_30N BDS0149 492674 895267 377 2.5 SOIL WGS84_30N BDS0150 492639 895233 381 2.5 SOIL WGS84_30N BDS0151 492605 895198 376 2.5 SOIL WGS84_30N BDS0152 492568 895161 374 2.5 SOIL WGS84_30N BDS0153 492534 895127 369 2.5 SOIL WGS84_30N BDS0154 492498 895092 368 2.5 SOIL WGS84_30N BDS0155 492463 895056 367 2.5 SOIL WGS84_30N BDS0156 492427 895020 358 2.5 SOIL WGS84_30N BDS0157 492392 894985 355 2.5 SOIL WGS84_30N BDS0158 492357 894950 353 2.5 SOIL WGS84_30N 15 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0159 492321 894915 349 2.5 SOIL WGS84_30N BDS0160 492284 894878 349 2.5 SOIL WGS84_30N BDS0161 492249 894842 348 2.5 SOIL WGS84_30N BDS0162 492215 894808 346 2.5 SOIL WGS84_30N BDS0163 492179 894772 342 2.5 SOIL WGS84_30N BDS0164 492144 894737 342 2.5 SOIL WGS84_30N BDS0166 492109 894702 341 2.5 SOIL WGS84_30N BDS0167 492072 894664 339 2.5 SOIL WGS84_30N BDS0168 492038 894631 334 2.5 SOIL WGS84_30N BDS0169 492001 894595 336 8 SOIL WGS84_30N BDS0170 491968 894565 334 2.5 SOIL WGS84_30N BDS0171 491934 894528 334 2.5 SOIL WGS84_30N BDS0172 491897 894490 340 2.5 SOIL WGS84_30N BDS0173 491860 894452 338 2.5 SOIL WGS84_30N BDS0174 491825 894419 337 2.5 SOIL WGS84_30N BDS0175 491789 894384 332 2.5 SOIL WGS84_30N BDS0176 491756 894349 334 2.5 SOIL WGS84_30N BDS0177 491719 894313 331 2.5 SOIL WGS84_30N BDS0178 491684 894278 331 2.5 SOIL WGS84_30N BDS0179 491649 894242 330 2.5 SOIL WGS84_30N BDS0180 491614 894207 333 2.5 SOIL WGS84_30N BDS0181 491578 894170 328 2.5 SOIL WGS84_30N BDS0182 491543 894136 337 2.5 SOIL WGS84_30N BDS0183 491508 894100 334 2.5 SOIL WGS84_30N BDS0184 491473 894065 336 2.5 SOIL WGS84_30N BDS0186 491434 894031 337 2.5 SOIL WGS84_30N BDS0187 491401 893996 336 2.5 SOIL WGS84_30N BDS0188 493241 895287 374 11 SOIL WGS84_30N BDS0189 493205 895233 371 15 SOIL WGS84_30N BDS0190 493170 895197 368 11 SOIL WGS84_30N BDS0191 493134 895162 367 8.5 SOIL WGS84_30N BDS0192 493099 895127 367 2.5 SOIL WGS84_30N BDS0193 493062 895091 366 2.5 SOIL WGS84_30N BDS0194 493027 895056 365 2.5 SOIL WGS84_30N BDS0195 492993 895020 363 2.5 SOIL WGS84_30N BDS0196 492958 894985 363 2.5 SOIL WGS84_30N BDS0197 492922 894949 361 2.5 SOIL WGS84_30N BDS0198 492887 894914 360 19 SOIL WGS84_30N BDS0199 492852 894879 360 2.5 SOIL WGS84_30N BDS0200 492816 894844 359 2.5 SOIL WGS84_30N BDS0202 493628 895656 399 17.5 SOIL WGS84_30N BDS0203 493664 895691 404 37 SOIL WGS84_30N BDS0204 493700 895726 396 145.5 SOIL WGS84_30N BDS0205 493735 895761 387 35 SOIL WGS84_30N BDS0206 493770 895797 387 31 SOIL WGS84_30N BDS0207 493806 895833 392 274 SOIL WGS84_30N BDS0208 493841 895867 409 31.5 SOIL WGS84_30N BDS0209 493877 895904 404 10 SOIL WGS84_30N BDS0210 493913 895940 398 563 SOIL WGS84_30N BDS0211 493945 895980 394 327.5 SOIL WGS84_30N 16 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0212 493985 896011 389 61 SOIL WGS84_30N BDS0213 494017 896044 387 17 SOIL WGS84_30N BDS0214 494053 896080 386 20 SOIL WGS84_30N BDS0215 494088 896114 375 51 SOIL WGS84_30N BDS0216 494127 896152 362 20 SOIL WGS84_30N BDS0217 494160 896185 361 7 SOIL WGS84_30N BDS0218 494194 896222 367 2.5 SOIL WGS84_30N BDS0219 494229 896256 376 2.5 SOIL WGS84_30N BDS0221 494266 896292 370 2.5 SOIL WGS84_30N BDS0222 494302 896329 369 2.5 SOIL WGS84_30N BDS0223 494338 896365 374 2.5 SOIL WGS84_30N BDS0224 494369 896400 385 2.5 SOIL WGS84_30N BDS0225 494407 896435 386 2.5 SOIL WGS84_30N BDS0226 494443 896468 391 2.5 SOIL WGS84_30N BDS0227 494480 896507 403 2.5 SOIL WGS84_30N BDS0228 494514 896540 414 2.5 SOIL WGS84_30N BDS0229 494548 896578 416 2.5 SOIL WGS84_30N BDS0230 494584 896608 407 2.5 SOIL WGS84_30N BDS0231 494618 896645 384 2.5 SOIL WGS84_30N BDS0232 494656 896680 382 2.5 SOIL WGS84_30N BDS0233 494688 896718 388 2.5 SOIL WGS84_30N BDS0234 494724 896754 385 2.5 SOIL WGS84_30N BDS0235 494759 896789 381 2.5 SOIL WGS84_30N BDS0236 494797 896823 382 2.5 SOIL WGS84_30N BDS0237 494830 896858 388 2.5 SOIL WGS84_30N BDS0238 492781 894809 357 2.5 SOIL WGS84_30N BDS0239 492745 894773 357 2.5 SOIL WGS84_30N BDS0240 492711 894738 354 2.5 SOIL WGS84_30N BDS0241 492675 894703 353 2.5 SOIL WGS84_30N BDS0242 492639 894666 352 2.5 SOIL WGS84_30N BDS0243 492605 894632 350 2.5 SOIL WGS84_30N BDS0244 492568 894595 348 2.5 SOIL WGS84_30N BDS0246 492533 894562 348 2.5 SOIL WGS84_30N BDS0247 492497 894526 347 2.5 SOIL WGS84_30N BDS0248 492462 894489 347 2.5 SOIL WGS84_30N BDS0249 492428 894454 347 2.5 SOIL WGS84_30N BDS0250 492393 894420 347 2.5 SOIL WGS84_30N BDS0251 492357 894385 346 2.5 SOIL WGS84_30N BDS0252 492322 894350 346 2.5 SOIL WGS84_30N BDS0253 492287 894314 345 2.5 SOIL WGS84_30N BDS0254 492248 894277 343 2.5 SOIL WGS84_30N BDS0255 492214 894243 342 2.5 SOIL WGS84_30N BDS0256 492180 894207 340 2.5 SOIL WGS84_30N BDS0257 492143 894172 339 2.5 SOIL WGS84_30N BDS0258 492108 894137 339 2.5 SOIL WGS84_30N BDS0259 492073 894101 337 2.5 SOIL WGS84_30N BDS0260 492039 894066 336 2.5 SOIL WGS84_30N BDS0261 492004 894032 334 2.5 SOIL WGS84_30N BDS0262 491967 893994 335 2.5 SOIL WGS84_30N BDS0263 491933 893960 328 2.5 SOIL WGS84_30N 17 Sample ID Easting Northing Elevation Au ppb Sample type Utm_Grid BDS0264 491898 893924 327 2.5 SOIL WGS84_30N BDS0266 491862 893890 332 2.5 SOIL WGS84_30N BDS0267 491827 893855 331 2.5 SOIL WGS84_30N BDS0268 491791 893818 331 2.5 SOIL WGS84_30N BDS0269 491754 893782 329 2.5 SOIL WGS84_30N BDS0270 491721 893747 326 2.5 SOIL WGS84_30N BDS0271 491684 893712 325 2.5 SOIL WGS84_30N BDS0272 494933 896674 375 2.5