Kingfisher Metals(TSXV:KFR)

Kingfisher Metals is a discovery-driven team comprised of experienced geologists, backed by a solid management group with decades of corporate and capital markets experience.

Investor website: https://kingfishermetals.com/

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Kingfisher Metals is a discovery-driven team comprised of experienced geologists, backed by a solid management group with decades of corporate and capital markets experience. The team has extensive experience with early-stage exploration in British Columbia, public company management, and capital markets. They focus on responsible and sustainable exploration, working with Indigenous groups and stakeholders to achieve mutually beneficial outcomes with minimal environmental impacts.

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~ $1.8M
Shares outstanding
28,317,230
Fully diluted shares
124,020,855
Mineral resource
Projects With extensive experience in early stage exploration in British Columbia, Kingfisher is focused on exploring untapped district scale properties within the province. Operating in British Columbia provides a safe and predictable environment for exploration and mining. HWY 37 The 849 km2 HWY 37 Project is the largest contiguous project held by a junior in BC’s most prospective mining district – the Golden Triangle. The project is host to numerous porphyry and epithermal target areas ranging from geochemical anomalies through to the discovery stage. The project hosts multiple ages of mineralization including Shaft Creek (Teck), Galore Creek (Teck/Newmont), KSM (Seabridge), Brucejack (Newmont), and Eskay Creek (Skeena) ages. Historical exploration and work done by Kingfisher has prioritized the Mary, Hank, and Williams areas where all three deposits have returned multiple intercepts over 100 gram meter (AuEq) intercepts. The highlight intercept from Williams returned 347 m of 0.33% Cu and 0.39 g/t Au including 190 m of 0.49% Cu and 0.57 g/t Au. Goldrange The 511 km2 district-scale Goldrange Project is located along the same crustal-scale fault network as the Bralorne Mine (Talisker). The project covers a significant deformation zone with highly anomalous Au-As signatures in historic rock, stream, and soil sampling. The project contains numerous zones of high-grade gold mineralization with two drill programs completed to date by Kingfisher (2021 and 2022). Thibert The 124 km2 district-scale Thibert Project straddles the crustal-scale Thibert fault for 25km. The project covers a significant deformation zone with widespread silica-fuchsite alteration, common to orogenic systems. The project is located adjacent to Highway 37 and covers a past and currently producing placer camp with historic production of ~200,000 oz Au. HWY 37 Project The HWY 37 Project covers 849 km² and includes 100% owned tenures (457 km²) and a 4-year option to acquire 100% of the remaining 362km². Since 2023, Kingfisher has assembled a dominant 849 km2 contiguous land position in the heart of BC’s Golden Triangle. The project covers a broad area of favourable stratigraphy and fertile intrusions hosting porphyry copper-gold and epithermal gold-silver mineralization. The project is also located within the Eskay-Rift and hosts Eskay Creek – Equivalent stratigraphy which is prospective for high-grade Au-Ag VMS systems. Historical exploration has outlined Williams, Mary, Hank, and Mess Creek as top priority targets. Location & Infrastructure The 849 km² HWY 37 Project is located in Northwest British Columbia’s Golden Triangle. The property is approximately 125 km north of the town of Stewart and 75 km southwest of the village of Iskut. Port facilities are available at Stewart and Prince Rupert (315 km south), accessible via highways. Both the Stewart-Cassiar Highway (37) and the 287 kV Northwest Transmission Line pass through the eastern portion of the HWY 37 project. The main areas of interest are within 9-15 km of Highway 37 and power. Helicopter staging is available at the Burrage airstrip 4 km to the east, on Highway 37. The project is within the traditional territory of the Tahltan First Nation, with a communications agreement in place. Regional Geology The HWY 37 Project lies within the Stikine terrane of Northwest British Columbia and is predominantly underlain by the Stuhini and Hazelton groups. Mineralization spans porphyry to epithermal deposit types and is related to Late Triassic to Early Jurassic Intrusions which are also responsible for mineralization at the Schaft Ck, Galore Ck, and the Treaty Creek-KSM-Brucejack districts. The northeastern region of the project is underlain by Eskay-equivalent Iskut River Formation, favourable for VMS mineralization.  Targets Williams Porphyry The Williams Cu-Au porphyry deposit (Minfile 104G 434) is highly prospective based on its analogous age to the nearby Mitchell deposits (4.1 Bt, 72.3 M oz Au, 11.9 B Lbs Cu; M&I contained resource)*, and that it is open laterally and at depth. Williams was discovered in 2017 through prospecting and first drilled in 2018 with an initial drill hole returning 377 m of 0.31 g/t Au and 0.28% Cu (HNK-18-001). The deposit drill footprint of 500 m long by 400 m wide and 500-600 m deep is within a 2.2 km long and 1.5 km wide and 1 km deep chargeable body (>25 mV/V) with values up to 212 mV/V identified by the new survey. Intercepts at Williams coincide with potassic-altered monzonite porphyry intrusion that extend to surface with abrupt grade change between intrusive host and the volcanic rocks. The Williams deposit is largely hosted in one structurally focused intrusion within a chargeability anomaly that is prospective to host numerous such bodies. The upper-level porphyry target area includes domains to the north and south of the Williams deposit and are interpreted as structurally-controlled, Williams-like stocks, such as 190 m of 0.49% Cu, and 0.57 g/t Au (HNK-18-13). The deeper target domain spans 1 km wide and includes the peak chargeability values (212 mV/V) where there is potential for more broad, intrusive-hosted stockwork. From regional examples, highest relative copper grades are associated with bornite typically intercepted at deeper levels where higher temperature conditions exist. The geometry of chargeability supports this exploration concept with a marked chargeable high close to surface in volcanic rocks (pyrite>chalcopyrite), a muted mid-level response in mixed intrusions and volcanic rocks (chalcopyrite>pyrite), and a broadening root zone where bornite>chalcopyrite is conceptualized in an intrusive host. Given the grade at Williams and the significant scale of the anomaly, this target area has been elevated to a top priority. Drill Hole From (m) To (m) Interval (m) Au (g/t) Cu (%) Ag (g/t) ----------------------------------------------------------------------------------- HNK-18-001 36.0 413.0 377.0 0.31 0.28 1.75 Including 97.0 182.0 85.0 0.52 0.44 3.16 HNK-18-002 116.0 416.0 300.0 0.22 0.29 2.20 HNK-18-005 148.0 550.8 402.8 0.32 0.28 1.84 Including 148.0 244.0 96.0 0.61 0.43 2.56 HNK-18-007 366.0 603.5 237.5 0.17 0.18 2.01 HNK-18-013 217.3 564.0 346.7 0.39 0.33 2.06 Including 217.3 407.0 189.7 0.57 0.49 2.78 Including 275.0 401.9 126.9 0.69 0.56 3.37 HNK-18-015 393.6 512.0 118.4 0.06 0.14 0.82 HNK-WZ-19-01 233.0 611.5 378.5 0.22 0.28 1.44 Including 272.0 517.0 245.0 0.30 0.38 1.84 Upper Hank Porphyry The upper levels of alteration of the historical epithermal Hank Au-Ag district (Minfile 104G 107) are now considered to be a hybrid alteration expression of an early porphyry and late epithermal system. Evidence of a cryptic early porphyry emplacement is provided by a large ‘advanced argillic’ alteration assemblage of dickite-kaolinite-quartz-pyrite mapped on surface and confirmed by a spectral study. These minerals commonly lie directly above Cu-Au porphyry deposits as part of a ‘lithocap’ or porphyry top. A new 3D IP inversion product from coupled historical and 2024 lines revealed a 1.5 km long by 0.8 km wide and 850 m deep (>35 mV/V) anomaly seated below this porphyry top. The large anomaly at Upper Hank is comparable in size, vertical emplacement level and geometry to the chargeability body at the nearby Williams porphyry deposit and is considered to be highly prospective for a new porphyry discovery. Three target domains exist at the Upper Hank: 1) the projection of at-surface, bed parallel epithermal gold mineralization at the Pit deposit (intermediate sulfidation, e.g., 20 m of 11.63 g/t Au and 13.8 g/t Ag and 63 m of 1.86 g/t Au); 2) disseminated gold-rich or gold-only target from surface in the area of the lithocap above the anomaly (high sulfidation); and 3) intrusive-hosted porphyry Cu-Au in upper-level stocks from ~350 m drill depths below at-surface gold targets. The Upper Hank Porphyry target provides a unique opportunity to drill both high-grade gold targets and porphyry Cu-Au targets with a single hole. Drill Hole From (m) To (m) Interval (m) Au (g/t) Ag (g/t) Cu (%) Pb (%) Zn (%) --------------------------------------------------------------------------------------------------- DDH84-2 4.3 42.5 38.3 0.89 — — — — DDH84-4 2.1 57.9 55.8 1.38 — — — — Including 36.3 44.2 8.0 6.74 12.14 — — — DDH85-04 57.5 91.4 33.9 2.55 — — — — Including 74.0 75.5 1.5 46.66 — — — — DDH85-05 91.5 99.4 7.9 2.27 — — — — DDH85-06 67.0 115.5 47.0 0.58 — — — — DDH85-08 24.5 62.0 37.5 0.54 — — — — DDH85-09 7.0 62.8 55.8 1.47 — — — — Including 42.0 62.8 20.8 3.22 — — — — DDH85-10 7.5 21.0 13.5 2.32 — — — — DDH85-13 5.0 56.4 51.4 0.98 — — — — DDH85-15 82.5 98.0 15.5 1.02 — — — — DDH85-16 26.0 97.0 71.0 0.35 — — — — DDH85-30 7.0 100.0 93.0 0.22 — — — — DDH85-32 6.0 47.5 41.5 2.52 — — — — Inlcuding 25.5 37.0 11.5 8.19 — — — — DDH85-35 17.0 84.4 67.4 0.32 — — — — DDH85-39 26.5 93.0 66.5 0.39 — — — — DDH85-40 8.5 49.7 41.2 0.49 — — — — DDH85-42 0.0 61.0 61.0 0.35 — — — — DDH85-45 35.0 97.5 62.5 1.86 — — — — Including 35.0 66.0 31.0 3.56 — — — — DDH87-1 42.5 69.5 27.0 0.83 — — — — HNK-18-010 114.5 141.6 27.1 8.68 10.87 0.00 0.00 0.02 Including 116.0 136.0 20.0 11.63 13.84 0.01 0.00 0.02 Including 116.0 118.9 2.9 67.27 74.12 0.03 0.02 0.09 DDH90-5 76.5 123.6 47.1 0.57 2.39 0.00 0.00 0.01 DDH88-6 374.5 423.4 48.9 2.83 — — — — Including 374.5 376.4 2.0 67.30 530.44 0.06 0.09 0.10 DDH88-20 40.5 126.5 86.0 0.32 — Lower Hank Porphyry A new 3D IP inversion product from coupled historical and 2024 lines revealed a 1.6 km long by 0.8 km wide and 850 m deep anomaly (>35 mV/V) – the Lower Hank Porphyry target (see ‘Lower Alteration Zone’ Minfile 104G 107). The geometry of the chargeability body aligns with mapped quartz-sericite-pyrite-chlorite (phyllic and propylitic alteration) on surface. The anomaly is focused at shallow levels and broadens at depth, similar to the Williams chargeability anomaly. At the apex of the anomaly, historical holes intercepted high-grade gold, such as hole HNK-17-001 with 95 g/t Au, 1100 g/t Ag over 0.58 m. Deeper drilled extents that correlate with the uppermost levels of the anomaly intersect porphyry-style broad gold, such as hole HNK-17-006 with 0.44 Au Eq. over 341.7 m. Initial drill holes above this anomaly have only intersected volcanic rocks, and have not yet discovered the key porphyry intrusion that hosts mineralization at Williams. An outcrop to the southeast of the historically drilled area contains stockwork and disseminated style mineralization more typical in porphyry type systems (rock here returned 0.37% Cu, 0.44 g/t Au). The top of the Williams porphyry deposit is at the same elevation as Au-Ag-Pb-Zn veins along the Lower Hank Trend. The presence of close vertical emplacement levels for epithermal and porphyry systems indicates a process of telescoping. Although historically a high-grade gold target, the new chargeability anomaly at the Lower Hank Porphyry target represents high potential for porphyry discovery due to: 1) the presence of overlap of epithermal gold veins (telescoping) onto porphyry systems at same elevations, 2) the target is on trend and at the same elevation as the Williams deposit, 3) a transition from structurally-controlled gold at shallow levels into broad, disseminated gold at depth typical of porphyry systems, and 4) potential for rapid grade change into mineralizing porphyry intrusions not yet discovered at this anomaly. Drill Hole From (m) To (m) Interval (m) Au (g/t) Ag (g/t) Cu (%) Pb (%) Zn (%) --------------------------------------------------------------------------------------------------- DDH87-3 22.6 50.9 28.3 2.40 — — — — Including 46.3 47.9 1.5 39.25 332.90 — — — DDH88-11 26.5 84.5 58.0 2.00 — — — — Including 33.5 45.5 12.0 7.23 — — — — DDH88-14 190.0 300.0 110.0 0.43 — — — — DDH88-4 137.0 146.0 9.0 6.19 1.93 0.01 0.03 0.07 And 280.0 323.0 43.0 3.13 31.71 0.03 0.23 0.45 Including 301.4 317.0 15.6 8.18 83.05 0.06 0.61 1.15 Including 307.9 317.0 9.1 13.40 132.36 0.09 1.00 1.57 DDH89-1 29.0 95.1 66.1 0.64 — — — — Including 82.2 90.5 8.4 2.87 — — — — DDH89-10 66.0 111.9 45.9 0.48 3.93 0.01 0.02 0.11 DDH89-11 72.3 121.6 49.3 2.17 28.93 0.02 — 0.42 Including 82.0 89.4 7.4 5.77 35.19 0.02 0.01 0.44 Including 104.5 110.4 5.9 8.74 182.63 0.07 — 1.29 DDH89-3 34.0 115.6 81.6 0.47 5.27 0.01 0.03 — DDH89-4 20.8 84.4 63.6 1.97 — — — — Including 53.7 70.7 17.0 6.56 — — — — DDH89-5 61.5 105.0 43.5 0.84 13.90 0.03 0.09 0.30 Including 94.8 98.4 3.6 7.38 124.26 0.10 0.09 1.32 DDH89-7 10.3 101.2 90.9 0.27 — — — — DDH90-3 93.0 194.0 101.0 0.24 2.77 0.01 0.04 0.08 HNK-17-001 207.6 245.2 37.7 1.87 23.56 0.02 0.09 0.31 Including 241.1 245.2 4.1 14.97 193.85 0.10 0.77 1.97 HNK-17-002 174.0 265.5 91.4 0.53 23.20 0.01 0.09 0.08 Including 223.9 224.5 0.6 54.40 3240.00 0.04 10.60 5.59 HNK-17-005 171.9 257.4 85.5 0.43 4.84 0.01 0.05 0.13 HNK-17-006 74.6 416.4 341.7 0.33 3.86 0.02 0.04 0.12 Including 209.1 213.2 4.1 2.18 72.12 0.12 0.19 3.32 HNK-17-007 63.4 119.0 55.6 0.53 3.54 0.02 0.02 0.40 And 135.0 192.0 57.0 0.73 6.03 0.04 0.23 0.48 Including 185.3 185.9 0.6 45.10 234.00 1.25 1.88 4.41 HNK-17-008 52.7 113.0 60.3 2.12 6.91 0.02 0.11 0.45 Including 111.1 111.9 0.8 133.00 263.00 0.07 1.38 0.69 HNK-17-009 127.0 195.2 68.2 2.40 17.97 0.04 0.00 0.10 Including 133.7 158.6 24.8 5.59 45.94 0.09 0.00 0.10 HNK-17-010 4.8 110.0 105.2 0.36 1.87 0.02 0.03 0.21 HNK-17-012 5.4 160.6 155.3 0.20 1.08 0.02 0.01 0.13 HNK-17-014 121.0 183.0 62.0 0.28 2.19 0.02 0.03 0.28 HNK-18-011 439.7 483.3 43.6 0.39 3.91 0.01 0.01 0.12 DDH87-7 9.8 119.5 109.7 0.36 — — — — DDH87-8 5.2 129.0 123.8 0.34 — — — — DDH88-16 25.5 100.0 74.5 0.43 — — — — DDH88-17 7.5 143.0 135.5 0.16 — Mary & Cliff Porphyry The drill footprint of the Mary area spans 3 km focused along a north-northeast trend defined by the Cliff target, Mary deposit (Minfile 104G 018) and the DM porphyry. Drilling at Mary began in the 1970s from surface mineralization and the first modern 2D induced-polarization survey was completed in 2012 with NWW-trending orientation. Most holes at Mary test relatively shallow depths (300-400 m), but the first deep hole was planned following the first IP survey to drill toward the highest chargeability value that had been defined to date. This hole, BC12-47, intercepted 455 m of 0.11% Cu and 0.28 g/t Au until it cut a late, relatively unaltered monzonite dyke and terminated in volcanic rocks with 39 m of 0.4 g/t Au Eq. A largely untested subvertical chargeability anomaly below Mary swells from ~350 m width near surface to 750 m width at depth (>25 mV/V). The vertical orientation of hole BC12-47 into a structurally controlled system failed to test the porphyry intrusions at depth and failed to cross peak chargeability values. The late intrusion intercepted in the hole is interpreted to have a steep geometry (narrow width) and is not the causative intrusion. The hole failed to reach the core of the chargeability anomaly, located to the south, and did not intercept source intrusions below Mary and failed to explain the source of the deep chargeability anomaly. The chargeability anomaly below Mary is interpreted as a significant untested porphyry target. At the Williams deposit, grade is closely tied to both chargeability and to the location of structurally focused porphyry intrusions. The presence of significant grade in volcanic rocks at depth is interpreted to indicate proximity to the porphyry intrusion body below Mary. Hole BC07-10 provides evidence for such a porphyry target, where 102 m of 0.53 g/t Au and 0.22% Cu in a porphyry host are intersected in peak chargeability values at depth. Along trend ~850 m from Mary, significant lateral and vertical expansion potential at the DM porphyry is also indicated. The DM porphyry is characterized by higher Cu:Au ratios compared to Mary, such as 0.21% Cu and 0.28 g/t Au over 223 m from surface. The chargeability anomaly appears to plunge from the DM porphyry at surface toward Mary, to the SW. Based on the chargeability anomaly, the DM porphyry is interpreted to have significant vertical extent beyond the ~230 m drilled extent. Off the IP section line, the presence of stockwork with 0.42% Cu and 0.97 g/t Au also indicates lateral, or width, potential. The Cliff porphyry lies on the flanks of a new chargeability anomaly 700 m wide and 1 km deep ( > 25 mV/V) identified in the 2024 survey, similar in geometry and calibre to the anomaly centered on the Mary deposit. Alteration patterns, intrusive geometry and quartz stockwork abundance trends indicate a projection of the porphyry system into the slope, to the NE. Only three holes have tested the Cliff porphyry, returning up to 0.11% Cu, 66 ppm Mo over 116. The geometry of the chargeability anomaly indicates a large untested body to the NE, and the presence of high relative Mo, and low relative Au in these initial holes is consistent with the interpretation that the drilled domain is lateral to and flanking a porphyry target into the slope. Drill Hole From (m) To (m) Interval (m) Au (g/t) Cu (%) Ag (g/t) Target Area ------------------------------------------------------------------------------------------------ BC07-05B 15.6 99.2 83.6 0.19 0.08 0.25 Mary BC07-06 0.0 139.8 139.8 0.60 0.23 0.45 Mary Including 108.8 138.1 29.3 0.72 0.40 0.77 Mary BC07-07 18.7 87.0 68.3 0.27 0.18 2.83 Mary BC07-08 0.0 381.0 378.6 0.33 0.12 1.09 Mary Including 51.2 94.5 43.3 0.63 0.23 0.52 Mary BC07-09 84.4 175.8 91.4 0.20 0.05 0.31 Mary BC07-10 3.7 434.3 430.7 0.31 0.12 0.28 Mary Including 239.9 364.9 125.0 0.53 0.22 0.31 Mary BC07-11 12.2 105.8 93.6 0.61 0.15 0.41 Mary BC07-12 3.4 234.4 231.0 0.53 0.21 0.36 Mary Including 55.5 113.4 57.9 0.69 0.27 0.32 Mary BC07-13 6.1 254.8 248.7 0.35 0.11 0.75 Mary BC08-01 33.0 298.0 265.0 0.41 0.16 2.51 Mary Including 159.0 220.0 61.0 0.49 0.26 1.42 Mary BC08-02 78.7 282.9 195.1 0.44 0.18 0.96 Mary BC11-02 16.8 170.0 153.2 0.23 0.10 0.98 Mary BC11-03 21.0 201.3 180.3 0.35 0.14 0.63 Mary BC11-04 3.0 137.2 134.2 0.17 0.05 0.44 Mary BC12-47 9.1 464.0 454.9 0.28 0.11 0.71 Mary Including 190.6 240.5 49.9 0.60 0.24 1.24 Mary BC12-48 4.6 298.2 293.6 0.40 0.08 0.81 Mary Including 7.5 60.7 53.2 0.77 0.09 1.16 Mary BC12-50 10.7 347.0 336.3 0.24 0.09 0.57 Mary Including 32.9 139.4 106.5 0.33 0.16 0.71 Mary BC12-51 8.2 188.9 180.7 0.18 0.11 1.12 Mary BC12-53 150.8 266.5 115.7 0.19 0.12 0.67 Mary BC12-54 2.9 307.0 304.2 0.44 0.15 1.01 Mary Including 122.0 307.0 185.0 0.44 0.21 1.23 Mary BC12-56 13.7 249.9 236.2 0.19 0.08 0.44 Mary BCK-MZ-19-01 15.5 307.0 291.5 0.48 0.14 0.95 Mary dh74-03 78.1 214.3 135.3 0.55 0.23 1.20 Mary dh93-01 48.8 258.2 209.4 0.39 0.16 Mary BC06-01 116.8 197.4 80.6 0.05 0.11 0.66 Cliff M-23-001 264.9 381.0 116.1 0.04 0.11 1.28 Cliff BC06-03 16.0 239.3 223.3 0.28 0.21 2.15 DM Including 104.0 139.0 35.0 0.60 0.40 4.66 DM BC07-01 7.6 103.3 95.7 0.32 0.18 1.20 DM Including 60.3 97.5 37.3 0.49 0.28 2.08 DM BC07-03 45.4 102.7 57.3 0.29 0.19 3.46 DM BC12-49 8.1 134.9 126.8 0.28 0.18 2.09 DM Including 8.1 65.2 57.1 0.44 0.28 3.27 DM M-23-002 79.3 241.0 161.8 0.21 0.01 5.51 Mary M-23-006 9.0 438.0 429.0 0.26 0.04 6.13 Mary ME Porphyry The ME porphyry Cu-Au target (Minfile 104G 042) is situated at the south end of the Mary trend where from-surface, untested chargeability anomalies were identified in a 2024 survey. The area is host to NE-striking porphyry stocks that trend towards the prominent Goat gossan. Mineralization in the area is related to porphyry quartz stockwork with chalcopyrite-pyrite-molybdenite and increasing concentrations of galena, associated with a flanking porphyry position, to the north and northeast away from the IP chargeability anomalies defined in 2024. The ME Target is host to an open-ended soil geochemical anomaly (Cu-Au-Ag-Mo-Pb) that stretches over 3.5 km with grades up to 2900 ppm Cu, 3210 ppb Au, 36,500 ppb Ag, and 750 ppm Mo. Two historical drill holes were completed downslope of the 2024 IP anomalies in 1980. Incomplete assays are available for these holes with reports of grades up to 0.16% Cu. These drill holes were completed prior to the 2019 geochemical soil survey that outlined the broad anomaly. Mapping in 2024 indicates that these drill holes were misoriented, were located laterally far away from the interpreted core, and are too far downslope of the mapped stockwork on surface. Consistent with this, historical drill logs identified widespread sodic alteration, common in deeper flanking positions to Cu-Au porphyry systems.  These holes were located over 500 m from the chargeability targets identified in 2024. Rainbow Ridge Gold Target The gold-rich quartz breccia and stockwork were discovered at Rainbow, or ‘Rainbow North,’ (Minfile 104G 255) in the early 2000s. The first-ever drill hole intersected 0.76 g/t Au over 91.4 m from surface in 2011. Two follow-up drill holes failed to intersect similar mineralization. The outcrop showing is surrounded by broad gossan and anomalous Cu-Au geochemistry. This early-stage discovery has a drill footprint of only ~250 x 50 m. Future drill targets at Rainbow require ground geophysical surveys to target below a widespread mask of glacial till cover rock. Mapping in 2025 identified grade on surface associated with a magnetite-cement breccia. Magnetite can be easy visualized by a ground magnetic survey. Rainbow Ridge Drill Highlights Drill Hole From (m) To (m) Interval (m) Au (g/t) Cu (%) Ag (g/t) -------------------------------------------------------------------------------- RN11-01 3.1 94.5 91.4 0.76 0.05 1.99 Grizzly Au-Cu Porphyry Target The Grizzly target (Minfile 104G 079) is a silica-undersaturated alkalic Cu-Au porphyry with a comparable setting to Galore Creek. Grizzly is situated at the southern extent of the HWY 37 Project in what was formerly known as the LGM tenures. Grizzly is adjacent to the Voigtberg Project held by Galore Creek Mining Corp (Teck/Newmont). Southeast of Grizzly lies the Lucifer Target area that covers a broad area of highly anomalous gold in streams and soils. The Grizzly target is centered on a surface trench of 0.74% Cu and 1.09 g/t Au over 38 m and lies within a 1 km by 1 km Cu-Au-Ag-Mo soil geochemical anomaly that grades up to 2916 ppm Cu,  1100 ppb Au, 5.4 ppm Ag, and 160 ppm Mo. Rock sampling results up to 5.91% Cu and 13 g/t Au at Grizzly were the focus of a small drill program in 2008, with 1442.9 m of diamond drilling. The small program failed to identify the geometry of the porphyry intrusion and drilled exclusively along an east-west azimuth. The NNE axis of mineralization in moderately S-dipping gully defined by rocks was not crossed by the 2008 drill holes. Anomalous intercepts from 2008 include 0.16 g/t Au and 0.10% Cu over 66.6 m (hole GRZ08-11).  The first-ever 3D modelling was completed by Kingfisher in 2024, and it highlighted porphyry mineralization outlined by historical trenching occurs as a ~150 m wide panel that dips moderately to the south on the shoulder of a large magnetic anomaly. Geophysical surveys followed-up on 2008 drilling that identified a chargeability and magnetic anomaly directly below the Grizzly trench showing. The strongest chargeability anomaly remains untested and lies downslope from the Grizzly showing in a region where monzonite to syenite porphyry is mapped on surface. Three large untested magnetic anomalies were identified at depth below the Grizzly showing, the most westerly coincides with a moderate shallow chargeability anomaly. The Grizzly showing appears to be a high-level, Galore Creek-type setting with several untested geophysical anomalies and excellent trench results that have not been crossed by drilling. The LGM/Voigtberg, Galore Creek, and Newmont Lake projects represent the only three areas in the Golden Triangle where ~210-208 Ma silica-undersaturated, alkalic magmatic-volcanic complexes are identified. These rare and Cu-Au-rich systems are marked by the presence of pseudoleucite in both the intrusions and in the overlying volcanic rocks. Although many Galore Creek suite intrusions are identified in the region, only three reflect full vertical preservation that includes the pseudoleucite-bearing volcanic carapace. Galore Creek is the most advanced of these projects with a measured and indicated resource of 1,197 Mt at 0.46% Cu and 0.25 g/t Au*, and the Newmont Lake Project is host to the Burgundy Ridge drill delineated Cu-Au porphyry deposit. The LGM/Voigtberg region represents rare exposure to a Galore Creek-type system, and the only magmatic-volcanic complex where a deposit has not yet been delineated. *The Company notes that mineralization on nearby projects is not indicative of mineralization on the HWY 37 Project Grizzly Drill Highlights Hole ID From (m) To (m) Interval (m) Au (g/t) Cu (%) Ag (g/t) -------------------------------------------------------------------------------- GRZ08-11 70.7 140.4 69.7 0.10 0.35 0.15 Northmore Au-Cu Porphyry Target The Northmore grassroots target area (Minfile 104G 259) includes a soil anomaly that extends 7 km N-S and has a width of 1.5-2.5 km E-W with several sampling gaps in steep gossan slopes. The broad Cu-Au-Ag-Mo multi-element anomaly reflects a region with a mix of outcrop and vegetative cover. Rock samples from the anomaly include up to 8.12% Cu and 1.06 g/t Au. Five shallow widely spaced drill holes totalling 1016 m tested the anomaly focused at the north. Drilling returned anomalous copper grades (~400-800 ppm Cu) over widths of 25 to 100 m. A historical 11 line-km induced polarization-resistivity survey at the northern anomaly, completed in 1991, showed chargeability increasing in the eastern portion of the grid. The Company intends to digitize and invert this paper format data for visualization and targeting work in 3D space. A 352 line-km high resolution aeromagnetic survey from 2006 will also be inverted for use in 3D space and structural interpretation. The broad grassroots Northmore target area is host to Texas Creek, or KSM-type, intrusions as well as syenite interpreted by previous workers to be Galore Creek intrusions. The Company plans to undertake further work to determine whether a KSM or Galore-style exploration model will apply here. Initial work to further refine targets at Northmore will include expanding soil coverage to capture the full extent of anomalism and new geophysical studies. This new data coupled with 3D inversions of historical geophysical datasets will provide insight into the plumbing system and porphyry target areas for additional IP surveys and drill target generation within the large soil anomaly. Mess Creek Grassroots Target The Mess Creek soil and rock anomaly (Minfile 104G 260) extends a minimum of 8 km along the a north south trend with elevated Au-Cu-Mo. In areas, the width of the anomaly measures a minimum of 2 km but sampling along the trend is not sufficient to characterize either the full strike length or width of the anomaly. A total of 24 holes to average depth of 177 m are focused in a 2.3 km N-S by 1 km E-W drill footprint. The drill area intersected anomalous Cu-Au including: 125 m of 0.11 g/t Au and 0.11% Cu (MC07-01), 242 m of 0.16 g/t Au and 0.08% Cu (MC06-02), and 159 m of 0.18 g/t Au and 0.12% Cu (BC-08).   Geophysical coverage at Mess Creek includes 447 line- km of a modern high resolution aeromagnetic survey that encompasses the Mess Creek soil anomaly. The principal Mess Creek soil anomaly is covered by 1970’s era induced-polarization-resistivity data currently in paper format with limited depth penetration. The Company intends to digitize paper format data and to generate inversion products for both IP and magnetic data for 3D visualization and structural interpretation. The Mess Creek area coincides with a trend of Galore Creek intrusions (the Loon Lake stock) and historical work areas document Galore-like alkalic Cu-Au-bearing syenite porphyry intrusions. The Mess Creek target area is also highly prospective for intrusion-related gold systems (e.g., Brucejack or Snip) based on the presence of the regional scale Mess Creek fault system. The Company intends to completely capture the anomaly through expanded soil sample surveys and follow-up with geophysical surveys. These results coupled with 3D visualization techniques to historical geophysical and drill results will inform drill targeting work. Hole ID From (m) To (m) Interval (m) Au (g/t) Cu (%) Ag (g/t) -------------------------------------------------------------------------------- MC06-01 1.5 60.1 58.5 0.21 0.08 0.64 MC06-02 64.0 253.1 189.1 0.15 0.08 1.46 MC06-04 54.1 147.7 93.6 0.12 0.06 0.51 MC07-01 39.9 167.9 128.0 0.11 0.11 0.57 MC07-03 78.8 123.1 44.3 0.08 0.27 4.28 BC-08 9.0 183.0 174.0 0.17 0.11 1.25 Hickman Grassroots Target Area The Hickman grassroots target area (Minfile 104G 470) is an open and relatively new 3.5 km-long Cu-Au-Mo soil anomaly that was delineated in 2019 without follow-up (Figure 3). Surface work identified the presence of potassic-altered porphyry stockwork on surface and rock sampled up to 0.69 g/t Au and 2.5% Cu. The sampled region reflects a comparable geological setting to the Schaft Creek deposit, located ~7 km north of the target. Both the Schaft Creek deposit* and Hickman target lie at the margin of the Late Triassic Hickman batholith (225 to 222 Ma) associated with monzodiorite porphyry phases. No ground geophysical surveys have been completed at Hickman. Eskay-type VMS Grassroots Regions HWY 37 is host to two large regions of Eskay-type stratigraphy in the Eskay rift with potential to host a new precious metal-rich VMS district similar to Eskay Creek. The Eskay Creek historical mine produced 3.3 M oz Au and 160 M oz Ag at 45 g/t Au and 2224 g/t Ag*. Limited historical exploration by Noranda at Table Mountain in the 1990s on the NE HWY 37 Project was carried out despite stream sediment anomalies up to 207 ppb Au. Rock sampling has returned encouraging grades up to 4.7 g/t Au, 22.4 g/t Ag, 1.56% Cu, 1.8% Pb, and 1.7% Sb. Soil sampling coverage is restricted to a small area that is highly anomalous in zinc. Goldrange Project The Goldrange Project covers 51,100 hectares and is 100% owned by Kingfisher Metals. The project covers broad area of high-grade orogenic gold mineralization similar in style to the Bralorne Gold Mine which produced 4.2M oz gold at 17.7 g/t. The project sits ~140km northwest of Bralorne along the same regional fault network host to numerous gold occurrences. The Goldrange Project covers a broad area of highly anomalous gold and arsenic in stream sediment samples with limited historic exploration, hand mining activities dating back to the 1930s and two drill programs – 2021 and 2022 – completed by Kingfisher to date. About Goldrange Location & Infrastructure The Goldrange Project is located in resource-dependent Central British Columbia, near the forestry and mining town of Williams Lake. The project is located within 12km of forest service roads and ~35km from transmission lines that pass through the nearby community of Tatla Lake. The area receives moderate precipitation with a working season of May to October. History & Timeline 1911 Gold discovered at the Argo–Langara showings by early prospectors, accessed by horse trails from Tatlayoko Lake. 1930s Significant exploration and adit development on what is now known as the Cloud Drifter Trend (Argo, Langara, and Standard showings). 1940s – Early 1980s Exploration hiatus, limited to small prospecting campaigns on the Goldrange property. 1983–1984 Homestake Mineral Development Company discovers gold veins in the A Zone, reporting gold grades up to 2.6 oz/t in float and multi-ounce gold in float within “Three Ounce Valley.” 1987 Prospectors discover the HW showings and identify gold veins grading >1 oz/t Au. 1987–1988 Equinox Resources Inc. identifies a large alteration trend on the Argo claims (now the Cloud Drifter Trend) and several new Au–Ag zones. Additional mineralization discovered at the HW showings with values >1 oz/t Au. 1990–1991 Discovery of the Lotus gold prospect with values up to 0.664 oz/t Au, along with the Champagne vein to the north. 1997 Black Horn Gold Mines discovers the Galena, Hunting Lodge, and Milk Can showings on the Nuit claims. 2003 Skeena Resources Ltd. completes reconnaissance prospecting and sampling, returning results of >6 oz/t Au in float near the HW showings. 2003–2020 Exploration hiatus, limited to small-scale sampling programs. 2020 Goldrange property assembled by Kingfisher Metals. 2021 Kingfisher’s first drill program at the Cloud Drifter Trend identifies a significant gold system with anomalous mineralization surrounding high-grade structures. Hole GR21-007 returns 9 metres of 6.88 g/t Au, 13.6 g/t Ag, and 0.28% Cu. 2022 Second diamond drill program at Goldrange follows up 2021 drilling at Cloud Drifter and tests the Langara zone within the Cloud Drifter Trend soil anomaly for the first time. Hole GR22-018 returns 40 metres of 2.86 g/t Au. Regional Geology The Goldrange Project is located within the Coast Belt, adjacent to a major NW-striking structural boundary with the Intermontane Belt to the northeast. In the area of the project, the Coast Belt includes the pre-accretion Stikine terrane (Stuhini and Hazelton groups), post-accretion metamorphic rocks (Triassic to Cretaceous), volcanic rocks (Ottarasko Formation; Lower Cretaceous) and sedimentary rocks (Cloud Drifter Formation; Lower Cretaceous). These rocks are overprinted by mid-Cretaceous fold-and-thrust contractional deformation, which is in turn cut by a Late Cretaceous to Paleocene granodiorite (Bendor suite) and overlain unconformably by Powell Creek Formation (upper Cretaceous) volcanic rocks to the east. Property Geology The Goldrange Project includes both pre- and post-accretion layered rocks (upper Triassic to upper Cretaceous) as well as intrusions of Cretaceous age. Boundaries between layered rocks are either thrust or strike-slip faults. The southern extent of the project is underlain by sedimentary and volcanic rocks of the Mount Moore and Cloud Drifter formations, and a very small domain of the Powell Creek Formation along the southeastern margin of the claims. The southern project is partially bound to the south and north by two northeast-elongate Bendor suite intrusions. The northern Goldrange project is underlain by the Cloud Drifter Formation to the east, and a series of thrust fault-bound panels of volcanic rocks of the Ottarasko Formation and limestone and volcanic rocks of the Stuhini Group. Layered rocks (Triassic to upper Cretaceous) of the Goldrange project have undergone deformation (D1) and metamorphism related to the formation of the East Waddington fold-and-thrust belt, active between 82-87 Ma. Thrust faults carried Triassic and Cretaceous rocks to the northeast along W-dipping thrust faults, which are subparallel to bedding. Beds in the Cloud Drifter Formation include both right-side-up as well as overturned, separated by E- and W-dipping axial planes to overturned, thrust-bounded, isoclinal folds. Metamorphism is syn- to post-kinematic and metamorphic grade increases from northeast to southwest with a series of NW-striking, SW-dipping isograds. Metamorphic grade ranges from sub-greenschist in the Powell Creek Formation to greenschist and amphibolite in the Ottarasko Formation. A second deformation event (D2) is associated with gentle, NW-trending folds. Targets Cloud Drifter Trend Cloud Drifter Trend The 3-km long Cloud Drifter Trend in the southern part of the property has been the focus of the Company’s exploration efforts in 2021 and 2022. The trend is covered by an extensive gold-in-soil anomaly and includes the Cloud Drifter, Standard and Langara zones. In 2022, Kingfisher’s 7,545-metre diamond drill program tested the lower (northern) Cloud Drifter zone, as well as one pad at the Langara zone. This program followed up on the initial 14-hole, 4,925-metre 2021 diamond drill program that tested across the Cloud Drifter zone. The inaugural 2021 drill program targeted high-grade gold vein and breccia in the upper (southern) Cloud Drifter zone. In 2021 drilling, the Pad 400 area returned 6.88 g/t Au over 9 m in GR21-007 and continued to return high-grade intercepts and infill gaps in 2022 drilling. Structural corridors were identified in 2022 breccia and stockwork hosted gold, such as 2.9 g/t Au over 40 m in GR22-018. Gold is structurally controlled and is also focused along contacts of diorite (see Eastern Target Section). 2022 Cloud Drifter Zone Drill Program Highlights
Hole: GR22-016 | From (m): 75.00 | To (m): 77.00 | Interval (m): 2.00 | Au (g/t): 19.54
Hole: GR22-017 | From (m): 82.00 | To (m): 83.00 | Interval (m): 1.00 | Au (g/t): 10.39
Hole: GR22-018 | From (m): 141.00 | To (m): 180.00 | Interval (m): 40.00 | Au (g/t): 2.86
Incl.: From (m): 141.00 | To (m): 150.00 | Interval (m): 9.00 | Au (g/t): 5.56
Incl.: From (m): 161.00 | To (m): 162.00 | Interval (m): 1.00 | Au (g/t): 19.91
Incl.: From (m): 174.00 | To (m): 180.00 | Interval (m): 6.00 | Au (g/t): 5.05
Hole: GR22-019 | From (m): 132.00 | To (m): 133.00 | Interval (m): 1.00 | Au (g/t): 58.88
Hole: GR22-020 | From (m): 85.00 | To (m): 87.00 | Interval (m): 2.00 | Au (g/t): 9.55 2021 Cloud Drifter Zone Drill Program Highlights
Hole: GR21-002 | From (m): 26.00 | To (m): 27.00 | Interval (m): 1.00 | Au (g/t): 5.30
Hole: GR21-007 | From (m): 35.00 | To (m): 43.00 | Interval (m): 8.00 | Au (g/t): 2.16
Incl.: From (m): 41.00 | To (m): 42.00 | Interval (m): 1.00 | Au (g/t): 14.80
and: From (m): 418.00 | To (m): 427.00 | Interval (m): 9.00 | Au (g/t): 6.88
Hole: GR21-014 | From (m): 109.00 | To (m): 111.00 | Interval (m): 2.00 | Au (g/t): 37.82
Incl.: From (m): 110.00 | To (m): 111.00 | Interval (m): 1.00 | Au (g/t): 73.40
Hole: GR21-009 | From (m): 173.00 | To (m): 183.00 | Interval (m): 10.00 | Au (g/t): 1.22
Incl.: From (m): 175.00 | To (m): 179.00 | Interval (m): 4.00 | Au (g/t): 2.62
Hole: GR21-010 | From (m): 10.00 | To (m): 16.00 | Interval (m): 6.00 | Au (g/t): 6.78
Incl.: From (m): 14.00 | To (m): 16.00 | Interval (m): 2.00 | Au (g/t): 18.69
Incl.: From (m): 15.00 | To (m): 16.00 | Interval (m): 1.00 | Au (g/t): 30.20 Kingfisher completed seven line-km of IP surveys over the eastern portion of the Cloud Drifter zone in 2022. The survey highlights two large chargeability anomalies at depth – one below the area of drilling and another below a historical adit at the Standard zone, south of the Cloud Drifter zone. The Langara zone is located in the eastern portion of the Cloud Drifter Trend. In 2022, the first-ever diamond drill holes were completed, with four holes drilled from one pad location. Drilling intersected sulfide breccia, such as in GR22-033 below, and structurally-controlled gold. The Standard zone, in the southern Cloud Drifter Trend, was mined in the 1930s for gold. The Company completed one backpack drillhole in 2020 that returned 10.84 g/t Au over 6.9 m. Day Trip The Day Trip zone was discovered by Kingfisher in 2020, is located approximately 5 km southeast of the Cloud Drifter Trend. In 2022, the Company completed 32 initial rotary air blast (RAB) holes at Day Trip. This initial shallow drilling returned highly anomalous pathfinders in XRF and anomalous gold over an area of 300 x 200 m. Ground geophysical work extended the target area 2 km to the west, where strong chargeability and conductivity anomalies were identified. Lost Fiddle The Lost Fiddle showing was described in previous reports, but the first-ever results were reported by Kingfisher. The prospect is located ~2 km northeast of the Cloud Drifter Trend and hosts similar sulfide-rich vein and breccia. New results from Kingfisher include 42.8 g/t Au over 0.45 m in backpack drill hole and a more than 200 x 200 m soil geochemical anomaly in forest cover. Surface sampling focused on a limited area of historical trenching, the lateral extent of the anomaly is not yet known. Future ground geophysical and soil geochemical surveys are required to delineate the anomaly. Lotus Gold veins were first discovered in the 1990s in a gully exposure within broad forest and till cover at the Lotus prospect. Sampling by Kingfisher returned up to 113.9 g/t Au in outcrop. Future ground geophysical and soil geochemical surveys are required to determine the lateral and vertical extent of the anomaly.
Projects
["HWY 37: The 849 km2 HWY 37 Project is the largest contiguous project held by a junior in BC’s most prospective mining district – the Golden Triangle. The project is host to numerous porphyry and epithermal target areas ranging from geochemical anomalies through to the discovery stage. The project hosts multiple ages of mineralization including Shaft Creek (Teck), Galore Creek (Teck/Newmont), KSM (Seabridge), Brucejack (Newmont), and Eskay Creek (Skeena) ages. Historical exploration and work done by Kingfisher has prioritized the Mary, Hank, and Williams areas where all three deposits have returned multiple intercepts over 100 gram meter (AuEq) intercepts. The highlight intercept from Williams returned 347 m of 0.33% Cu and 0.39 g/t Au including 190 m of 0.49% Cu and 0.57 g/t Au.","Goldrange: The 511 km2 district-scale Goldrange Project is located along the same crustal-scale fault network as the Bralorne Mine (Talisker). The project covers a significant deformation zone with highly anomalous Au-As signatures in historic rock, stream, and soil sampling. The project contains numerous zones of high-grade gold mineralization with two drill programs completed to date by Kingfisher (2021 and 2022).","Thibert: The 124 km2 district-scale Thibert Project straddles the crustal-scale Thibert fault for 25km. The project covers a significant deformation zone with widespread silica-fuchsite alteration, common to orogenic systems. The project is located adjacent to Highway 37 and covers a past and currently producing placer camp with historic production of ~200,000 oz Au.","Ecstall Project: The Ecstall Project covers 28,407 hectares prospective for Cu-Au-Zn-Ag VMS deposits and is 100% owned by Kingfisher Metals with no underlying royalties. The project covers the majority of the highly prospective and underexplored Ecstall Greenstone Belt. A property wide VTEM geophysical survey outlined +40 high quality geophysical targets throughout the property. The Kingfisher team followed up on only one of these targets in 2019 which resulted in the discovery of the high-grade Shiner Zone."]
Leadership
Management Dustin Perry P. Geo. CEO, President, Founder, Director, QP Mr. Perry is an exploration geologist and entrepreneur with +17 years in the mining sector. He has worked on over 50 exploration projects throughout British Columbia, the Yukon and Mexico. He currently sits on the board of several private mining companies and he received a B.Sc Geology from the University of British Columbia. Mr. Perry is a registered professional geologist with Engineers and Geoscientists BC. Tyler Caswell P. Geo. Vice President Exploration Mr. Caswell is a registered professional geologist with over 20 years of experience in mineral exploration, having worked in Peru, Chile, Argentina, Laos, Nunavut, the Yukon, and northern British Columbia. He has focused on exploring for base and precious metals. Most recently, Mr. Caswell served as Vice President of Exploration for NorthWest Copper, where he led discovery teams at the Stardust Project, achieving a drilling result of 2.51% copper, 3.03 g/t gold, and 52.5 g/t silver over 100.0 meters. He was also involved in the Kwanika Project, where they drilled 2.00% copper, 1.21 g/t gold, and 5.3 g/t silver over 235.45 meters. His experience encompasses both producers and junior mining companies, covering brownfield and greenfield exploration programs. He holds a B.Sc. (with distinction) from the University of Victoria. Gayle Febbo M.Sc., P.Geo. Chief Geologist Ms. Febbo is an exploration geologist with over 20 years in the mining sector. She obtained her M.Sc. degree in structural geology (Mineral Deposit Research Unit) from the University of British Columbia. She has spent the majority of her career working in the prolific Golden Triangle on world class projects such as Kerr-Sulphurets-Mitchell (KSM), Brucejack and Galore Creek. She is a registered professional geologist with Engineers and Geoscientists BC. Barry MacNeil CPA, CGA Chief Financial Officer Mr. MacNeil is a member of the Chartered Professional Accountants of BC with more than 30 years of management and accounting experience in public company, private practice, and industry.   Giuseppe (Pino) Perone LLB General Counsel, Corporate Secretary, Director Mr. Perone is a lawyer by background and has extensive corporate experience. His expertise covers securities, corporate commercial, mergers & acquisitions and capital markets related matters as well as regulatory compliance and corporate governance. Mr. Perone serves as an executive and director for various public and private companies in the resources and technology sectors. our Team Board of Directors Dustin Perry P. Geo. CEO, President, Founder, Director, QP Mr. Perry is an exploration geologist and entrepreneur with +17 years in the mining sector. He has worked on over 50 exploration projects throughout British Columbia, the Yukon and Mexico. He currently sits on the board of several private mining companies and he received a B.Sc Geology from the University of British Columbia. Mr. Perry is a registered professional geologist with Engineers and Geoscientists BC. Giuseppe (Pino) Perone LLB General Counsel, Corporate Secretary, Director Mr. Perone is a lawyer by background and has extensive corporate experience. His expertise covers securities, corporate commercial, mergers & acquisitions and capital markets related matters as well as regulatory compliance and corporate governance. Mr. Perone serves as an executive and director for various public and private companies in the resources and technology sectors. Rick Trotman M.Sc. Independent Director Mr. Trotman is a professional geologist with a broad range of experience within the mining industry, having worked in both buy-side and sell-side positions as well as technically focused responsibilities with major mining companies. He was previously with Resource Capital Funds, a leading mining-focused private equity firm and was recently the president and CEO of Barksdale Resources, an exploration company focused on base metals in Arizona. Chris Beltgens MBA, CFA Independent Director Mr. Beltgens has over 15 years of financial experience in the E&P and mining sector in both industry and capital markets. He current sits as a director for a number of private and public junior resource companies. Formerly Partner, Corporate Finance with GMP Securities Europe, where he assisted in raising over $2 Billion in capital for E&P companies. Paul Gruner MBA, CPA, ICD.D Independent Director Mr. Gruner is a senior executive leader with a background in renewable energy, oil & gas, and mining. He brings a wealth of experience in Indigenous business leadership across diverse regions, having previously served as the CEO for Det’on Cho Management LP, the economic arm of the Yellowknives Dene First Nation in the Northwest Territories, and the Tahltan Nation Development Corporation, the economic arm of the Tahltan Nation. Mr. Gruner currently serves as the CEO for Tłı̨chǫ Investment Corporation, which is the economic arm of the Tłı̨chǫ First Nation. His track record speaks volumes about his ability to achieve outstanding business results while collaborating closely with Indigenous stakeholders. He has a dynamic range of experience in strategic leadership, mergers and acquisitions, business development, strategic partnerships, financial management, project management, corporate governance, contract negotiations, capacity building and job creation for citizens, and environmental, social, and corporate governance. Sharon G.K. Singh LLM Independent Director Ms. Singh is a Partner and Co-Head of the Indigenous and Environment practices at McMillan LLP, advising companies on environmental assessment, permitting, regulatory compliance, Indigenous relations, and ESG strategy. She has extensive experience supporting mining, energy, and infrastructure projects from regulatory approvals and Indigenous agreements through to governance frameworks, complemented by experience with an international mining company and board service. Recognized by Lexpert, Chambers Global, and Legal 500 as a leading Canadian lawyer in ESG, Indigenous, environmental, and mining law, she holds a Master of Laws, Bachelor of Laws, and Bachelor of Business (International Trade), and is called to the bar in multiple jurisdictions. Advisors Francis Macdonald B.Sc Mr. Macdonald is an exploration geologist who has spent the majority of his career with Newmont Mining Corp. He has extensive knowledge of exploration and targeting techniques related to VMS deposits and orogenic gold deposits. Currently, Mr. Macdonald is President, CEO and Director of Li-FT Power. Stephanie Sykora PhD. Dr. Stephanie Sykora is a seasoned exploration geologist with over a decade of global experience working with major and junior companies. She has a PhD degree in Geology from the University of Tasmania (CODES), Australia where she studied the giant Lihir (Ladolam) alkalic epithermal gold deposit in Papua New Guinea, under supervision of Professor David Cooke and Dr. David Selley. Dr. Sykora currently works as Chief Geologist at C3 Metals. She has held positions at First Quantum Minerals in South America, Australia, and globally for generative porphyry copper exploration, and at Teck Resources in BC, Canada in porphyry exploration at Highland Valley Copper. Her expertise includes field mapping, technical evaluations, project generation, structural geology, and porphyry-epithermal systems. Dr Sykora has published several articles in peer-reviewed scientific journals as well as various scientific communications for earth sciences. Zach Flood B.Sc Mr. Flood is an experienced geologist who has managed mineral exploration in countries around the world including Mongolia, China, Dem. Rep. Congo, Peru, Argentina, Canada, and the U.S. over the past 15 years. Zach also spent numerous years within the Ivanhoe Group, evaluating early to advanced stage M&A opportunities in the mining sector. Zach is currently the Co-founder, President and Director of Kenorland Minerals Ltd, an established project generator, focussed on exploration in North America. Charlie Greig M.Sc. P.Geo. Mr. Greig is a geologist with 30+ years of experience in the exploration industry. His main area of expertise is in geologic mapping, particularly as it applies to mineral exploration, and he has worked on exploration projects from grass-roots to development. Charlie has mapped, or worked on, a number of projects which have subsequently been put into production, including La India in Mexico (Grayd–Agnico Eagle), Wolverine in Yukon (Atna-Westmin, Yukon Zinc), Alamo Dorado in Mexico (Corner Bay-Pan American Silver), Brucejack Lake (Pretium), and Bisha in Eritrea (Nevsun). He has also worked on a number of advanced exploration projects which are not yet mines, but which have either reached an advanced stage of exploration, are in development, or have had a significant history of mining. These include: Asmara (Emba Derho, Adi Nefas, and Debarwa, for Sunridge Gold), Red Mountain (Lac Minerals, Seabridge), Casino (Western Copper and Gold), and Silbak Premier-Big Missouri (Westmin, Ascot Resources). Charlie’s recent exploration successes include GT Gold’s Saddle South high-grade gold discovery, and the Saddle North Cu-Au Porphyry discovery.

Verified data last updated: 2026-05-15

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