Significant Mineral Resource Upgrade at Shaakichiuwaanaan Lithium Project to Underpin Impending PEA
Highlights
- The Mineral Resource Estimate for the Shaakichiuwaanaan Lithium Project (formerly known as Corvette) reaffirmed as the largest lithium pegmatite Mineral Resource in the Americas and the 8th largest globally:
- Consolidated Mineral Resource statement (CV5 CV13 spodumene pegmatites)
80.1 Mt at 1.44% Li2O and 163 ppm Ta2O5 Indicated, and 62.5 Mt at 1.31% Li2O and 147 ppm Ta2O5, Inferred.
- The Company remains on track to provide the market with a Preliminary Economic Assessment for the CV5 Spodumene Pegmatite by the end of September quarter based on the Mineral Resource Estimate announced herein.
- Shaakichiuwaanaan Mineral Resource includes 6.9 km of collective strike length now confirmed to host continuous spodumene pegmatite Mineral Resources (4.6 km at CV5 and 2.3 km at CV13).
- Significant growth potential – both the CV5 and CV13 spodumene pegmatites remain open along strike at both ends, and to depth.
- Cut-off grade sensitivity analysis defines significant tonnage at very high grade, primarily reflecting the Nova and Vega zone discoveries at CV5 and CV13, respectively.
- Mineral Resource Estimate includes only the CV5 and CV13 spodumene pegmatites. It does not include any of the other known spodumene pegmatite clusters on the Property – CV4, CV8, CV9, CV10, CV12, and CV14.
- The Company intends to aggressively advance the remaining infill drilling at CV5 to underpin a maiden ore reserve and Feasibility Study scheduled for Q3-2025.
Darren L. Smith, Vice President of Exploration, comments: “This is a significant update to our Mineral Resource Estimate at Shaakichiuwaanaan, which now includes both the CV5 and CV13 spodumene pegmatites as well as a significant amount of resources now classified as Indicated. This resource update objectively reaffirms the Tier 1 nature of the spodumene pegmatites that define the Shaakichiuwaanaan Project. Further, with both the CV5 and CV13 pegmatites remaining open, as well as multiple spodumene pegmatite clusters on the Property still to be drill tested, significant potential for further resource growth is evident.”
“Exploration success in this industry is never less than a team effort. In this regard, I would like to acknowledge the dedication, work ethic, and contributions from the exploration and development teams, our supporting service providers and consultants, and finally our Chisasibi community workers who have all helped advance Shaakichiuwaanaan through to this key milestone on the path to potential production,” added Mr. Smith.
Ken Brinsden, President, CEO, and Managing Director, comments: “This is a significant accomplishment for our team and a major milestone for the Company as we cement the Shaakichiuwaanaan Lithium Project’s position as one of the most important new hard rock lithium assets globally.”
“The delivery of a substantial maiden Indicated Resource of over 80 million tonnes is a major milestone which will underpin development studies, while the continued growth of the overall resource – in conjunction with the Exploration Target announced separately today – highlights the Tier-1 scale of the mineral system and the enormous potential for further growth. I am immensely proud of our team members and consultants who continue to put a significant focus on safety and quality deliverables as we move forward through the various phases of development”.
“As we advance towards a Preliminary Economic Assessment in the near-term for the Shaakichiuwaanaan Project, and further towards a Feasibility Study scheduled for completion Q3 2025, the Company is firmly positioned as a leading candidate to provide long-term spodumene supply to the North American and European markets,” added Mr. Brinsden.
August 5, 2024 – Vancouver, BC, Canada / August 6, 2024 – Sydney, Australia / Patriot Battery Metals Inc. (the “Company” or “Patriot”) (TSX: PMET) (ASX: PMT) (OTCQX: PMETF) (FSE: R9GA) is pleased to announce an updated consolidated Mineral Resource Estimate (“MRE” or “Consolidated MRE”) for the CV5 and CV13 spodumene pegmatites at its 100%-owned Shaakichiuwaanaan Property (the “Property” or “Project”) – formerly known as Corvette – located in the Eeyou Istchee James Bay region of Quebec. The CV5 Spodumene Pegmatite is situated approximately 13.5 km south of the regional and all‑weather Trans-Taiga Road and powerline infrastructure corridor, and is accessible year-round by all-season road. The CV13 Spodumene Pegmatite is located approximately 3 km west-southwest of CV5.
The updated Consolidated MRE for the Shaakichiuwaanaan Project includes both the CV5 and CV13 spodumene pegmatites for a total of 80.1 Mt at 1.44% Li2O Indicated and 62.5 Mt at 1.31% Li2O Inferred, for 4.88 Mt contained lithium carbonate equivalent (“LCE”) (Table 1, Figure 1, and Figure 2). Presented by resource location/name, this MRE includes 78.6 Mt at 1.43% Li2O Indicated and 43.3 Mt at 1.25% Li2O Inferred at CV5, and 1.5 Mt at 1.62% Li2O Indicated and 19.1 Mt at 1.46% Li2O Inferred at CV13. The cut-off grade is variable depending on the mining method and pegmatite (see footnotes in Table 1 for details). Mineral Resources are not Mineral Reserves as they do not have demonstrated economic viability
The Consolidated MRE for the Shaakichiuwaanaan Project, including that of the CV5 Pegmatite on its own, reaffirms it – by a wide margin – as the largest lithium pegmatite Mineral Resource in the Americas and 8th largest globally (Figure 1, Figure 2, Appendix 2, and Appendix 3). These metrics and context firmly reaffirm and entrench the Project as a Tier 1, world class lithium pegmatite asset.
A primary objective of the drilling completed subsequent to the July 2023 MRE, was to target a significant upgrade from Inferred resources to Indicated resources, which correlates to a more robust Mineral Resource with higher confidence classification. As a result, in addition to the overall size of the MRE increasing compared to the maiden MRE (see news release dated July 30, 2023), a significant amount of the resource has now been classified as Indicated (80.1 Mt at 1.44% Li2O) compared to no Indicated resources being classified in the maiden MRE.
The Consolidated MRE statement for the Shaakichiuwaanaan Project, presented in Table 1, includes only the CV5 and CV13 spodumene pegmatites, which remain open at both ends along strike and to depth along most of their length. Therefore, this Consolidated MRE does not include any of the other known spodumene pegmatite clusters on the Property – CV4, CV8, CV9, CV10, CV12, and CV14 (Figure 3 and Figure 33). Collectively, this highlights a considerable potential for resource growth through continued drill exploration at the Property.
The Mineral Resource statement and relevant disclosure, sensitivity analysis, peer comparison, geological and block model views, and cross-sections are presented in the following figures and tables. A detailed overview of the MRE and Project is presented in the following sections in accordance with ASX Listing Rule 5.8.
Mineral Resource Statement (NI 43-101)
Table 1: NI 43-101 Mineral Resource Statement for the Shaakichiuwaanaan Project.
Pegmatite
Classification
Tonnes
Li2O
(%)
Ta2O5
(ppm)
Contained Li2O
(Mt)
Contained LCE
(Mt)
CV5 CV13
Indicated
80,130,000
1.44
163
1.15
2.85
Inferred
62,470,000
1.31
147
0.82
2.03
- Mineral Resources were prepared in accordance with National Instrument 43-101 – Standards for Disclosure of Mineral Projects (“NI 43-101”) and the CIM Definition Standards (2014). Mineral Resources that are not Mineral Reserves do not have demonstrated economic viability. This estimate of Mineral Resources may be materially affected by environmental, permitting, legal, title, taxation, sociopolitical, marketing, economic, or other relevant issues.
- The independent Competent Person (CP), as defined under JORC, and Qualified Person (QP), as defined by NI 43‑101 for this estimate is Todd McCracken, P.Geo., Director – Mining Geology – Central Canada, BBA Engineering Ltd. The Effective Date of the estimate is June 27, 2024 (through drill hole CV24-526).
- Estimation was completed using a combination of ordinary kriging and inverse distance squared (ID2) in Leapfrog Edge software with dynamic anisotropy search ellipse on specific domains.
- Drill hole composites at 1 m in length. Block size is 10 m x 5 m x 5 m with sub-blocking.
- Both underground and open-pit conceptual mining shapes were applied as constraints to demonstrate reasonable prospects for eventual economic extraction. Cut-off grades for open-pit constrained resources are 0.40% Li2O for both CV5 and CV13, and for underground constrained resources are 0.60% Li2O for CV5 and 0.80% Li2O for CV13. Open-pit and underground Mineral Resource constraints are based on a spodumene concentrate price of US$1,500/tonne (6% basis FOB Bécancour) and an exchange rate of 0.76 USD/CAD.
- Rounding may result in apparent summation differences between tonnes, grade, and contained metal content.
- Tonnage and grade measurements are in metric units.
- Conversion factors used: Li2O = Li x 2.153; LCE (i.e., Li2CO3) = Li2O x 2.473, Ta2O5 = Ta x 1.221.
- Densities for pegmatite blocks (both CV5 CV13) were estimated using a linear regression function (SG = 0.0688x Li2O% + 2.625) derived from the specific gravity (“SG”) field measurements and Li2O grade. Non-pegmatite blocks were assigned a fixed SG based on the field measurement median value of their respective lithology.
Figure 1: MRE tonnage vs grade chart highlighting Shaakichiuwaanaan as the largest lithium pegmatite Mineral Resource in the Americas. See Appendix 2 and 3 for further details.
Figure 2: MRE tonnage vs grade chart highlighting Shaakichiuwaanaan as the 8th largest lithium pegmatite Mineral Resource in the world. See Appendix 2 and 3 for further details.
The Shaakichiuwaanaan MRE covers a collective strike length of approximately 6.9 km, drill hole to drill hole (4.6 km at CV5, and 2.3 km at CV13). Further, the CV5 and CV13 spodumene pegmatites are situated along the same geological trend, separated by approximately 2.9 km, and therefore this corridor is considered highly prospective for lithium pegmatite (Figure 3). This corridor remains to be drill tested; however, current interpretation of the collective dataset over the trend indicates a reasonable potential for connectivity of the pegmatite body(s). As such, given the similar mineralogy, geochemistry, host geological and structural trend, and close proximity to each other ( 3 km), the MREs for the CV5 and CV13 pegmatites have been presented as a consolidated MRE for the Project (Table 1). The MRE is further detailed below with respect to conceptual mining constraint shapes by resource location/name (Table 2).
The Shaakichiuwaanaan database includes 537 diamond drill holes completed over the 2021, 2022, 2023, and 2024 (through the end of April – drill hole CV24-526) programs, for a collective total of 169,526 m, as well as 88 outcrop channels totalling 520 m. The MRE is supported by 344 holes (129,673 m) and 11 outcrop channels (63 m) at CV5, and 132 holes (29,059 m) and 54 outcrop channels (340 m) at CV13.
Table 2: Shaakichiuwaanaan Mineral Resource by Pegmatite and Conceptual Mining Constraint.
Cut-off Grade
Li2O (%)
Conceptual Mining Constraint
Pegmatite
Classification
Tonnes
(Mt)
Li2O
(%)
Ta2O5
(ppm)
Contained Li2O
(Mt)
Contained LCE
(Mt)
0.40
Open-Pit
CV5
Indicated
78.1
1.44
162
1.12
2.78
0.60
Underground
0.5
0.91
169
0.00
0.01
Total
78.6
1.43
162
1.13
2.79
0.40
Open-Pit
CV5
Inferred
29.9
1.34
168
0.40
0.99
0.60
Underground
13.4
1.04
145
0.14
0.35
Total
43.3
1.25
161
0.54
1.34
0.40
Open-Pit
CV13
Indicated
1.5
1.62
195
0.02
0.06
0.80
Underground
0
0
0
0.00
0.00
Total
1.5
1.62
195
0.02
0.06
0.40
Open-Pit
CV13
Inferred
17.7
1.50
118
0.27
0.66
0.80
Underground
1.4
1.05
73
0.01
0.04
Total
19.1
1.46
115
0.28
0.69
All Table 1 footnotes are applicable.
Figure 3: Extent of the Shaakichiuwaanaan MRE with respect to the spodumene pegmatite clusters in the area, highlighting potential for resource growth. CV5 and CV13 remain open along strike and at depth.
Sensitivity Analysis
The sensitivity analysis for the Shaakichiuwaanaan MRE (Table 3 and Figure 4) is presented as the sum of the open-pit and underground constrained and classified resources at the same cut-off. The sensitivity analysis by cut-off grade (“COG”) defines significant tonnage at very high-grade, primarily reflecting the Nova Zone at CV5 and Vega Zone at CV13.
- At a 1.5% Li2O COG for the CV5 Pegmatite, there is a total of 30.4 Mt at 2.09 Li2O Indicated and 13.6 Mt at 1.99 Li2O Inferred.
- At a 1.5% Li2O COG for the CV13 Pegmatite, there is a total of 0.7 Mt at 2.20 Li2O Indicated and 6.6 Mt at 2.47 Li2O Inferred.
Both the Nova and Vega zones have been traced over a significant distance/area with multiple drill hole intercepts (core length) ranging from 2 to 25 m (CV5) and 2 to 10 m (CV13) at >5% Li2O, each within a significantly wider mineralized pegmatite zone of >2% Li2O (Figure 16, Figure 25, and Figure 26). These zones are located approximately 6 km apart, along the same geological trend, and emphasize not only the scale of the entire mineralized system at Shaakichiuwaanaan but also its robustness in mineralized intensity defined to date.
The following Table 3 and Figure 4 outline the corresponding tonnage and lithium grade at various cut-off grades for the Shaakichiuwaanaan MRE. In addition to evaluating sensitivities to cut-off grades, this table can help relate the tonnage and grades at Shaakichiuwaanaan more directly to those calculated for peer deposits, which may have applied different cut-off grades to their resources.
Table 3: Sensitivity Analysis for the Shaakichiuwaanaan MRE.
Figure 4: Shaakichiuwaanaan Mineral Resource grade-tonnage curves for the CV5 and CV13 spodumene pegmatites.
Geological and Block Models
The geological model underpinning the MRE for the CV5 Spodumene Pegmatite interprets a single, steeply dipping (northerly), continuous, principal spodumene pegmatite body ranging in true thickness from 10 m to more than 125 m, extending over a strike length of approximately 4.6 km (drill hole to drill hole), which is flanked by multiple subordinate lenses. At CV5, the pegmatite may extend from surface to depths of more than 450 m in some locations. The CV5 Spodumene Pegmatite, which includes the principal body and all subordinate lenses, remains open along strike at both ends and to depth along a significant portion of its length.
The geological model underpinning the MRE for the CV13 Spodumene Pegmatite interprets a series of flat-lying to moderately dipping (northerly), sub-parallel trending spodumene pegmatite bodies, of which three appear to dominate. The pegmatite ranges in true thickness from 5 m to more than 40 m, and extends over a strike length of approximately 2.3 km. The CV13 Spodumene Pegmatite, which includes all proximal pegmatite lenses, remains open along strike at both ends and to depth along a significant portion of its length.
The geological model of the CV5 Spodumene Pegmatite, which forms the bulk of the Shaakichiuwaanaan MRE, is presented in plan, inclined, and side view in Figure 5 to Figure 11. The MRE block model of the CV5 Spodumene Pegmatite, block classifications, and cross-sections are presented in Figure 12 to Figure 18.
The geological model of the CV13 Spodumene Pegmatite is presented in plan and inclined view in Figure 19 and Figure 20, respectively. The MRE block model of the CV13 Spodumene Pegmatite, block classifications, and cross-sections are presented in Figure 21 to Figure 28.
Figure 5: Plan view of CV5 and CV13 spodumene pegmatite geological models – all lenses. A collective mineralized strike length of 6.9 km, drill hole to drill hole.
Figure 6: Oblique view (looking east-northeast) of CV5 and CV13 spodumene pegmatite geological models – all lenses (not to scale).
CV5 Spodumene Pegmatite
Figure 7: Plan view of CV5 Spodumene Pegmatite geological model – all lenses.
Figure 8: Inclined view of CV5 Spodumene Pegmatite geological model looking down dip (70°) – all lenses (not to scale).
Figure 9: Side view of CV5 geological model looking north (340°) – all lenses – illustrating the scale of the CV5 Spodumene Pegmatite.
Figure 10: Side view of CV5 geological model looking south (160°) – all lenses.
Figure 11: Side view of CV5 geological model looking north (340°) – principal pegmatite only.
Figure 12: Oblique view of the CV5 Spodumene Pegmatite block model (classified material unconstrained) (not to scale).
Figure 13: Oblique view of the CV5 Spodumene Pegmatite block model (classified material unconstrained) overlaid with geological model (semi-transparent light red) (not to scale).
Geologically modelled pegmatite where blocks do not populate, have not reached the threshold confidence for the Inferred Mineral Resource category based on the classification criteria and/or mining constraint shape applied. Additional drilling is required to elevate confidence to the threshold allowing for an inferred classification of grade and tonnage to be assigned, and for these blocks to fall within a conceptual mining constraint shape required to satisfy RPEEE in accordance with NI 43-101.
Figure 14: Oblique view of the CV5 Spodumene Pegmatite block model with respect to applied open-pit and underground conceptual mining constraint shapes (not to scale).
Figure 15: Oblique view of the Indicated (green) and Inferred (blue) block model classifications for the CV5 Spodumene Pegmatite (not to scale).
Figure 16: Select views of classified block model (CV5) highlighting the Nova Zone and continuity of high-grade mineralization along strike (blocks >2% Li2O at top and middle, blocks >3% Li2O at bottom).
Figure 17: Cross-section of the CV5 Spodumene Pegmatite block model with conceptual mining constraint shapes.
Figure 18: Cross-section of the CV5 Spodumene Pegmatite block model (Nova Zone) with conceptual mining constraints shapes.
CV13 Spodumene Pegmatite
Figure 19: Plan view of CV13 Spodumene Pegmatite geological model – all lenses.
Figure 20: Inclined view of CV13 Spodumene Pegmatite geological model looking down dip (25°) – all lenses (not to scale).
Figure 21: Plan view of the CV13 Spodumene Pegmatite block model (classified material unconstrained)
Figure 22: Plan view of the CV13 Spodumene Pegmatite block model (classified material unconstrained) overlaid with geological model (semi-transparent light red).
Figure 23: Oblique view of the CV13 Spodumene Pegmatite block model (classified material unconstrained) with respect to applied open-pit and underground conceptual mining constraint shapes (not to scale).
Figure 24: Plan view of the Indicated (green) and Inferred (blue) block model classifications for the CV13 Spodumene Pegmatite.
Figure 25: Plan view of the CV13 Spodumene Pegmatite block model with >2% Li2O blocks presented.
Figure 26: Plan view of the CV13 Spodumene Pegmatite block model, highlighting the Vega Zone, with >3% Li2O blocks presented.
Figure 27: Cross-section of the CV13 Spodumene Pegmatite block model (Vega Zone), with conceptual open-pit constraint shapes.
Figure 28: Cross-section of the CV13 Spodumene Pegmatite block model (west arm) with conceptual open-pit and underground constraint shapes.
Tantalum
In addition to the lithium as the primary commodity of interest, the CV5 Pegmatite also contains a significant amount of tantalum as a potentially recoverable by-product – 80.1 Mt at 1.44% Li2O and 163 ppm Ta2O5 Indicated, and 62.5 Mt at 1.31% Li2O and 147 ppm Ta2O5 Inferred. Mineralogy completed to date indicates that tantalite is the tantalum-bearing mineral, which may potentially be recoverable from the tailings of the primary lithium recovery process (i.e., potential valorization of waste streams). Additionally, the MRE suggests tantalum grades at the CV5 Pegmatite are generally higher compared to that of the CV13 Pegmatite, although grades at CV13 remain significant (Table 2). The tantalum grades were not used in generating the potential mineable shapes at CV5 and CV13
Tantalum is currently listed as a critical and strategic mineral by the province of Quebec (Canada), Canada, European Union, Australia, Japan, India, South Korea, and the United States. Tantalum is a critical component required for a range of high-tech devices, electronics, and essential niche applications, including in capacitors as it has the highest capacitance of any metal. According to the United States Geological Survey, no tantalum is currently produced in North America or Europe, with a majority of production coming out of the Democratic Republic of Congo and Rwanda.
Next Steps
The Company will continue infill drilling at the CV5 Pegmatite this summer-fall, as well as testing for extensions along strike, up dip, and down dip, where it remains open. The primary focus of the drill program is to support a further increase in MRE confidence from the Inferred category to the Indicated category. This drilling will target Inferred blocks as categorized in the MRE announced herein, with the ultimate objective of delineating a coherent body of Indicated Mineral Resource blocks to underpin a Feasibility Study scheduled for the second half of 2025.
Additionally, the Company will continue its exploratory drill program at CV13, focused on further delineation of the high-grade Vega Zone, as well as various geotechnical, hydrogeological, and geomechanical drilling in support of advancing development studies at CV5.
ASX Listing Rule 5.8
As the Company is listed on both the Canadian Toronto Stock Exchange (the “TSX”) as well as the Australian Securities Exchange (the “ASX”), there are two applicable regulatory bodies resulting in additional disclosure requirements. This Mineral Resource estimate has been completed in accordance with the Canadian National Instrument 43-101 – Standards of Disclosure for Mineral Projects, and the Company will, in accordance with NI 43-101, prepare and file a technical report supporting the Mineral Resource Estimate on SEDAR+ within 45 days of this announcement. Additionally, in accordance with ASX Listing Rule 5.8 and the JORC 2012 reporting guidelines, a summary of the material information used to estimate the Mineral Resource for the Shaakichiuwaanaan Project is detailed below. For additional information, please refer to JORC Table 1, Section 1, 2, and 3, as presented in Appendix 1 of this announcement.
Mineral Title
The Shaakichiuwaanaan Property is located approximately 220 km east of Radisson, QC, and 240 km north-northeast of Nemaska, QC. The northern border of the Property’s primary claim grouping is located within approximately 6 km to the south of the Trans-Taiga Road and powerline infrastructure corridor (Figure 29). The La Grande-4 (LG4) hydroelectric dam complex is located approximately 40 km north-northeast of the Property. The CV5 Spodumene Pegmatite, part of the Shaakichiuwaanaan MRE, is located central to the Property, approximately 13.5 km south of KM270 on the Trans-Taiga Road, and is accessible year-round by all-season road. The CV13 Spodumene Pegmatite is located approximately 3 km west-southwest of CV5.
The Property is comprised of 463 CDC mineral claims that cover an area of approximately 23,710 ha with the primary claim grouping extending dominantly east-west for approximately 51 km as a nearly continuous, single claim block. All claims are registered 100% in the name of Lithium Innova Inc., a wholly owned subsidiary of Patriot Battery Metals Inc.
Figure 29: Shaakichiuwaanaan Property and regional infrastructure.
Geology and Geological Interpretation
The Property overlies a large portion of the Lac Guyer Greenstone Belt, considered part of the larger La Grande River Greenstone Belt, and is dominated by volcanic rocks metamorphosed to amphibolite facies. Rocks of the Guyer Group (amphibolite, iron formation, intermediate to mafic volcanics, peridotite, pyroxenite, komatiite, as well as felsic volcanics) predominantly underly the Property (Figure 32). The amphibolite rocks that trend east-west (generally steeply south dipping) through this region are bordered to the north by the Magin Formation (conglomerate and wacke) and to the south by an assemblage of tonalite, granodiorite, and diorite, in addition to metasediments of the Marbot Group (conglomerate, wacke) in the areas proximal to the CV5 Spodumene Pegmatite. Several regional-scale Proterozoic gabbroic dykes also cut through portions of the Property (Lac Spirt Dykes, Senneterre Dykes). The lithium pegmatites on the Property are hosted predominantly within amphibolite’s, metasediments, and to a lesser extent ultramafic rocks.
Exploration of the Property has outlined three primary mineral exploration trends, crossing dominantly east-west over large portions of the Property – Golden Trend (gold), Maven Trend (copper, gold, silver), and CV Trend (Li-Cs-Ta Pegmatite). The Golden Trend is focused over the northern areas of the Property, the Maven Trend in the southern areas, and the CV Trend “sandwiched” between. Historically, the Golden Trend has received the exploration focus followed by the Maven Trend. However, the identification of the CV Trend and the numerous lithium-tantalum pegmatites discovered to date, represents a previously unknown lithium pegmatite district that was first identified in 2016/2017 by Dahrouge Geological Consulting Ltd. and the Company. The Company’s Vice President of Exploration, Darren L. Smith, M.Sc., P.Geo., was a member of the initial team that identified the potential at Shaakichiuwaanaan, later joining the Company’s Advisory Board in 2018, and as Vice President of Exploration in 2019. Mr. Smith has managed the exploration of the Shaakichiuwaanaan Property since the initial work programs, including drilling of the lithium pegmatites.
At the Property, including CV5 and CV13, lithium mineralization is observed to occur within lithium-cesium-tantalum (“LCT”) pegmatites, which may be exposed at surface as isolated high relief ‘whale-back’ landforms (i.e., outcrops) (Figure 30 and Figure 31). Given the proximity of some lithium pegmatite outcrops to each other at the various clusters, as well as the shallow till cover, it is probable that some of the outcrops may reflect a discontinuous surface exposure of a single, larger pegmatite ‘outcrop’ subsurface. Further, the high number of well-mineralized pegmatites along the trend at these clusters indicates a strong potential for a series of relatively closely spaced/stacked, sub-parallel, and sizable spodumene-bearing pegmatite bodies, with significant lateral and depth extent, to be present.
To date, the LCT pegmatites at the Property have been observed to occur within a corridor of approximately 1 km in width that extends in a general east-west direction across the Property for at least 25 km – the ‘CV Lithium Trend’ – with significant areas of prospective trend that remain to be assessed. The core area of the trend includes the CV5 and CV13 spodumene pegmatites with approximate strike lengths of 4.6 km and 2.3 km, respectively, as defined by drilling to date and which remain open. Further, the CV5 and CV13 spodumene pegmatites are situated along the same geological trend, separated by approximately 2.9 km of highly prospective lithium pegmatite trend (Figure 3). This corridor remains to be drill tested; however, current interpretation of the collective dataset indicates a reasonable potential for connectivity of the pegmatite body(s) that define the CV5 and CV13 pegmatites.
To date, eight (8) distinct lithium pegmatite clusters have been discovered along the CV Lithium Trend at the Property – CV4, CV5, CV8, CV9, CV10, CV12, CV13, and CV14. Each of these clusters includes multiple lithium pegmatite outcrops in close proximity, oriented along the same local trend, and have been grouped to simplify exploration approach and discussion (Figure 33). The Mineral Resource Estimate reported herein is limited to only the CV5 and CV13 spodumene pegmatites (Figure 3).
The pegmatites at the Property, including CV5 and CV13, are very coarse-grained and off-white in appearance, with darker sections commonly composed of mica and smoky quartz, and occasionally tourmaline. Spodumene is the dominant lithium-bearing mineral identified at all the lithium occurrences documented to date. It occurs as typically centimetre to decimetre-scale crystals that may exceed 1.5 m in length and range in colour from cream-white, to light-grey, to light-green. Minor localized lepidolite has been observed in core and in a small number of lithium pegmatite outcrops.
To date, at the CV5 Spodumene Pegmatite, multiple individual spodumene pegmatite dykes have been geologically modelled. However, a vast majority of the Mineral Resource is hosted within a single, large, principal spodumene pegmatite dyke, which is flanked on both sides by multiple, subordinate, sub-parallel trending dykes. The CV5 Spodumene Pegmatite, including the principal dyke, is modelled to extend continuously over a lateral distance of at least 4.6 km and remains open along strike at both ends and to depth along a large portion of its length. The width of the currently known mineralized corridor at CV5 is approximately ~500 m, with spodumene pegmatite intersected at depths of more than 450 m in some locations (vertical depth from surface). The pegmatite dykes at CV5 trend west-southwest (approximately 250°/070° RHR), and therefore dip northerly, which is different than the host amphibolites, metasediments, and ultramafics which dip moderately in a southerly direction.
The principal spodumene pegmatite dyke at CV5 ranges from 10 m to more than 125 m in true width, and may pinch and swell aggressively along strike, as well as up and down dip. It is primarily the thickest at near-surface to moderate depths (225 m), forming a relatively bulbous, elongated shape, which may flair to surface and to depth variably along its length. As drilling has focused over the principal dyke, the immediate CV5 corridor has not been adequately drill tested and it is interpreted that additional subordinate pegmatite lenses are situated proximal, especially in the southcentral areas of the deposit. The pegmatites that define CV5 are relatively undeformed and very competent, although likely have some meaningful structural control.
The geological model underpinning the MRE for the CV13 Spodumene Pegmatite interprets a series of flat-lying to moderately dipping (northerly), sub-parallel trending spodumene pegmatite bodies, of which three appear to dominate. The pegmatite bodies are coincident with the apex of a regional structural flexure whereby the pegmatite manifests a west arm trending ~290° and an east arm trending ~230°. Drilling to date indicates the east arm includes significantly more pegmatite stacking compared to the west, and also carries a significant amount of the overall CV13 Pegmatite tonnage and grade, highlighted by the high-grade Vega Zone.
The CV13 Pegmatite ranges in true thickness from 5 m to more than 40 m and extends continuously over a collective strike length of approximately 2.3 km, along its west and east arms. The CV13 Spodumene Pegmatite, which includes all proximal pegmatite lenses, remains open along strike at both ends and to depth along a significant portion of its length. Spodumene mineralization has been traced more than 400 m down-dip; however, due to the typically shallow dips of the pegmatite bodies, is only ~200 m vertical depth from surface.
Both the CV5 and CV13 spodumene pegmatites display internal fractionation along strike and up/down dip, which is evidenced by variation in mineral abundance including spodumene and tantalite. This is highlighted by the high-grade Nova Zone (CV5) and Vega Zone (CV13), each situated at the base of their respective pegmatite lenses, and traced over a significant distance with multiple drill hole intercepts (core length) ranging from 2 to 25 m (CV5) and 2 to 10 m (CV13) at >5% Li2O, respectively, each within a significantly wider mineralized zone of >2% Li2O (Figure 16 and Figure 26). The Vega Zone is situated approximately 6 km south-west and along geological trend of the Nova Zone. Both zones share several similarities including lithium grades and very coarse decimetre to metre size spodumene crystals. However, both pegmatite zones have distinct orientations whereby the Vega Zone is relatively flat-lying to shallow dipping while the Nova Zone is steeply dipping to vertical.
The CV5 Spodumene Pegmatite (4.6 km in strike length) has currently been delineated to within approximately 1.5 km of the CV4 Spodumene Pegmatite to the east, and to within approximately 2.9 km of the CV13 Spodumene Pegmatite (2.3 km in strike length) to the west (Figure 3). The CV12 Spodumene Pegmatite cluster is situated ~2.4 km northwest along strike of CV13. Collectively, this area of the CV Lithium Pegmatite trend extends nearly 15 km, of which 6.9 km is confirmed by drilling to be continuous spodumene pegmatite hosting defined Mineral Resources, with ~8 km of this highly prospective trend remaining to be drill tested.
The scale of LCT pegmatite present along this local trend (CV12 through CV4), as well as the similar mineralogy and very coarse spodumene crystal size, suggests a deeply rooted and common ‘plumbing’ system and source of the lithium mineralized bodies discovered to date. The area of the CV Lithium Trend, extending from CV12 easterly to CV4, is therefore highly prospective with data collected to date suggesting a reasonable potential for lithium pegmatite to be present throughout this trend, and potentially continuously. Due to a veil of glacial till cover, there is poor outcrop exposure, therefore requiring significant drill testing to confirm continuity.
Figure 30: Principal spodumene pegmatite body outcropping at CV5 with drill hole CF21-001 in forefront (left); typical mineralization from drill core at CV5 (right).
Figure 31: Principal spodumene pegmatite outcrop at CV13 (looking northeast).
Figure 32: Property geology and mineral exploration trends.
Figure 33: Spodumene pegmatite clusters at the Property discovered to date.
Drilling Techniques and Classification Criteria
The Shaakichiuwaanaan Mineral Resource Estimate, including the CV5 and CV13 spodumene pegmatites is supported by 537 diamond drill holes of NQ (predominant) or HQ size, completed over the 2021, 2022, 2023, and 2024 (through the end of April – drill hole CV24-526) programs, for a collective total of 169,526 m, as well as eighty-eight (88) outcrop channels totalling 520 m. This equates to 344 holes (129,673 m) and eleven (11) outcrop channels (63 m) at CV5, and 132 holes (23,059 m) and fifty-four (54) outcrop channels (340 m) at CV13 (Figure 34, Figure 35, and Figure 36).
Each drill hole collar was surveyed with an RTK tool (Topcon GR5 or Trimble Zephyr 3), with some minor exceptions that were surveyed using a handheld GPS (Garmin GPSMAP 64s) only (Table 4). Downhole deviation surveys for each drill hole were completed with a Devico DeviGyro tool (2021 holes), Reflex Gyro Sprint IQ tool (2022, 2023, and 2024 holes), Axis Champ Gyro (2023 holes), or Reflex OMNI Gyro Sprint IQ (2024 holes). Survey shots were continuous at approximate 3-5 m intervals. The use of the gyro tool system negated potential deflection issues arising from minor but common pyrrhotite within the host amphibolite. All collar and downhole deviation data have been validated by the project geologists on site, and by the database lead.
Drill core has not been oriented; however, downhole optical and acoustic televiewer surveys have been completed on multiple holes, at both CV5 and CV13, to assess overall structure. This data guided the current geological models supporting this Mineral Resource Estimate.
At CV5, drill hole collar spacing is dominantly grid based. Several collars are typically completed from the same pad at varied orientations targeting pegmatite pierce points of ~50 to 100 m spacing. The initial drill holes targeting CV5, completed in 2021, assumed a southerly dip to the pegmatite and therefore three (3) of four (4) holes were oriented northerly. However, most holes completed to date are oriented southerly (typically 158°), to cross-cut perpendicular the steeply, northerly dipping pegmatite, apart from drill holes targeting specific structure or areas of the pegmatite.
At CV13, drill hole spacing is a combination of grid based (at ~100 spacing) and fan based. Several collars are typically completed from the same pad at varied orientations targeting pegmatite pierce points of ~50 to 100 m spacing. Due to the varied orientation of the pegmatite bodies along strike at CV13, hole orientations may vary widely.
Drill hole spacing and orientation at the CV5 and CV13 pegmatites is sufficient to support the geological models and resource classifications applied herein.
All drill holes were completed by Fusion Forage Drilling Ltd. of Hawkesbury, ON. Procedures at the drill followed industry best practices with drill core placed in either 4 or 5 ft long, typically flat, square-bottom wooden boxes with the appropriate hole and box ID noted and block depth markers placed in the box. Core recovery typically exceeds 90%. Once full, the box was fibre taped shut with wooden lids at the drill and transported (helicopter and truck) to Mirage Lodge for processing.
Channel sampling followed industry best practices with a 3 to 5 cm wide, saw-cut channel completed across the pegmatite outcrop as practical, perpendicular to the interpreted pegmatite strike. Samples were collected at ~1 m contiguous intervals with the channel bearing noted, and GPS coordinate collected at the start and end points of the channel. Channel samples were transported along the same route as drill core for processing at Mirage Lodge.
Figure 34: Diamond drill hole locations at the CV5 Spodumene Pegmatite, which form the basis of the MRE.
Figure 35: Channel locations at the CV5 Spodumene Pegmatite included in the MRE.
Figure 36: Diamond drill hole and channel locations at the CV13 Spodumene Pegmatite, which form the basis of the MRE.
Sampling and Sub-Sampling Techniques
Core sampling protocols met industry standard practices. Upon receipt at the core shack at Mirage Lodge, all drill core is pieced together, oriented to maximum foliation, metre marked, geotechnically logged (TCR, RQD, ISRM, and Q-Method (since mid-winter 2023)), alteration logged, geologically logged (rock type), and sample logged on an individual sample basis. Wet and dry core box photos are also collected of all core drilled, regardless of perceived mineralization. Specific gravity measurements of entire pegmatite samples were collected at systematic intervals (approximately 1 SG measurement every 4-5 m) using the water immersion method.
Core sampling was guided by rock type as determined during geological logging (i.e., by a geologist). All pegmatite intervals were sampled in their entirety, regardless of whether spodumene mineralization was noted or not (in order to ensure an unbiased sampling approach) in addition to ~1 to 3 m of sampling into the adjacent host rock (dependent on pegmatite interval length) to “bookend” the sampled pegmatite. The minimum individual sample length is typically 0.3-0.5 m and the maximum sample length is typically 2.0 m. Targeted individual pegmatite sample lengths are 1.0 to 1.5 m. All drill core was saw-cut, using an Almonte automatic core saw in 2022, 2023, and 2024 with one half-core collected for assay, and the other half-core remaining in the box for reference.
Channels were geologically logged upon collection on an individual sample basis; however, were not geotechnically logged. Channel recovery was effectively 100%.
The logging of drill core and channels was qualitative by nature, and included estimates of spodumene grain size, inclusions, and model mineral estimates. These logging practices meet or exceed current industry standard practices and are of appropriate detail to support a Mineral Resource estimation and disclosure herein.
All core samples were bagged and sealed individually, and then placed in large supersacs for added security, palleted, and shipped by third party transport, or directly by representatives of the Company, to the designated sample preparation laboratory (Activation Laboratories Ltd. (“Activation Laboratories”) in Ancaster, ON, in 2021, SGS Canada Inc. (“SGS Canada”) in either Lakefield, ON, Val-d’Or, QC, or Radisson, QC, in 2022, 2023, and 2024, being tracked during shipment along with chain of custody documentation. A small number of holes were sent for sample preparation to SGS Canada’s Sudbury, ON, and Burnaby, BC, facilities in 2022. Upon arrival at the laboratory, the samples were cross-referenced with the shipping manifest to confirm all samples were accounted for and had not been tampered with.
Sample Analysis Method and Quality Control
Core samples collected from 2021 drill holes were shipped to Activation Laboratories in Ancaster, ON, for standard sample preparation (code RX1) which included crushing to 80% passing 10 mesh, followed by a 250 g riffle split and pulverizing to 95% passing 105 microns. All 2021 core sample pulps were analyzed, at the same lab, for multi-element (including lithium) by four-acid digestion with ICP-OES finish (package 1F2) and tantalum by INAA (code 5B), with any samples returning >8,000 ppm Li by 1F2 reanalyzed for Li by code 8-4 Acid ICP Assay. Activation Laboratories is a commercial lab with the relevant accreditations (ISO 17025) and is independent of the Company.
Core samples collected from 2022 and 2023 drill holes CV22-015 through CV23-107 were shipped to SGS Canada’s laboratory in either Lakefield, ON (vast majority), Sudbury, ON (CV22-028, 029, 030), or Burnaby, BC (CV22-031, 032, 033, and 034), for standard sample preparation (code PRP89) which included drying at 105°C, crush to 75% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns. Core samples collected from 2023 drill holes CV23-108 through 365 were shipped to SGS Canada’s laboratory in Val-d’Or, QC, for standard sample preparation (code PRP89). Core samples collected from 2024 drill holes were shipped to SGS Canada’s laboratory in either Val-d’Or, QC, or Radisson, QC, for a sample preparation (code PRP90 special) which includes drying at 105°C, crush to 90% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns.
All 2022, 2023, and 2024 (through drill hole CV24-526) core sample pulps were shipped by air to SGS Canada’s laboratory in Burnaby, BC, where the samples were homogenized and subsequently analyzed for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish (codes GE_ICP91A50 and GE_IMS91A50). SGS Canada is a commercial lab with the relevant accreditations (ISO 17025) and is independent of the Company.
A Quality Assurance / Quality Control (QAQC) protocol following industry best practices was incorporated into the drill programs and included systematic insertion of quartz blanks and certified reference materials into sample batches, as well as collection of quarter-core duplicates (through hole CV23-190 only), at a rate of approximately 5% each. Additionally, analysis of pulp-split and coarse-split (through hole CV23-365 only) sample duplicates were completed to assess analytical precision at different stages of the laboratory preparation process, and external (secondary) laboratory pulp-split duplicates were prepared at the primary lab for subsequent check analysis and validation at a secondary lab (SGS Canada in 2021, and ALS Canada in 2022, 2023, and 2024).
Channel samples collected in 2017 were shipped to SGS Canada’s laboratory in Lakefield, ON, for standard preparation. Pulps were analyzed at SGS Canada’s laboratory in either Lakefield, ON, (2017), or Burnaby, BC (2022), for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish. All subsequent channel samples were shipped to Val-d’Or, QC for standard sample preparation with the pulps shipped by air to SGS Canada’s laboratory in Burnaby, BC, where the samples were homogenized and subsequently analyzed for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish (codes GE_ICP91A50 and GE_IMS91A50).
A QAQC protocol following industry best practices was incorporated into the channel programs and included systematic insertion of quartz blanks and certified reference materials into sample batches.
Criteria Used for Classification
The Shaakichiuwaanaan resource classification has been completed in accordance with the NI 43-101, JORC 2012, and CIM Definition Standards for Mineral Resources and Reserves reporting guidelines. All reported Mineral Resources have been constrained by conceptual open-pit or underground mineable shapes to demonstrate reasonable prospects for eventual economic extraction (“RPEEE”).
Blocks were classified as Indicated when:
- Demonstrated geological continuity and minimum thickness of 2 m.
- The drill spacing was 70 m or lower and meeting the minimum estimation criteria parameters.
- Grade continuity at the reported cut-off grade.
Blocks were classified Inferred when drill spacing was between 70 m and 140 m and meeting the minimum estimation criteria parameters. Geological continuity and a minimum thickness of 2 m were also mandatory. There are no measured classified blocks. Pegmatite dykes or extension with lower level of information / confidence were also not classified.
Classification shapes are created around contiguous blocks at the stated criteria with consideration for the selected mining method. The Mineral Resource Estimate appropriately reflect the view of the Competent Person.
Estimation Methodology
Compositing was done every 1.0 m. Unsampled intervals were assigned a grade of 0.0005% Li and 0.25 ppm Ta. Capping was done after compositing. Based on the statistical analysis capping varies by lithological domain.
CV5 Parameters
For the spodumene-rich domain within the CV5 principal pegmatite, no capping was required for Li2O, but Ta2O5 was capped at 3,000 ppm. For the feldspar-rich domain within the CV5 principal pegmatite, a capping of 3.5% Li2O and 1,500 ppm Ta2O5 was applied. For the parallel dykes a capping of 5% Li2O and 1,200 ppm Ta2O5 was applied.
Variography was done both in Leapfrog Edge and Supervisor. For Li2O, a well-structured variogram model was obtained for the CV5 principal pegmatite’s spodumene-rich domain. For the CV5 principal pegmatite, both domains (spodumene-rich and feldspar-rich domains) were estimated using ordinary kriging (OK), using Leapfrog Edge.
For Ta2O5, the spodumene-rich domain and the feldspar-rich domain within CV5 principal pegmatite did not yield well-structured variograms. Therefore, Ta2O5 was estimated using Inverse Distance Squared (ID2).
The remaining pegmatite dykes at CV5 (8) domains did not yield well-structured variograms for either Li2O and Ta2O5 and therefore were estimated using Inverse Distance Squared (ID2), also using Leapfrog Edge.
Three (3) orientated search ellipsoids were used to select data and interpolate Li2O and Ta2O5 grades in successively less restrictive passes. The ellipse sizes and anisotropies were based on the variography, drillhole spacing, and pegmatite geometry. The ellipsoids were 100 m x 50 m x 30 m, 200 m x 100 m x 60 m, and 400 m x 200 m x 120 m. For the first pass interpolation a minimum of five (5) composites and a maximum of twelve (12) composites with a minimum of two (2) holes were needed to interpolate. For the second and third pass a minimum of three (3) composites with a maximum of twelve (12) without a minimum per hole was used. Variable search ellipse orientations (dynamic anisotropy) were used to interpolate for the eight (8) parallel dykes. Spatial anisotropy of the dykes is respected during estimation using Leapfrog Edge’s Variable Orientation tool. The search ellipse follows the trend of the central reference plane of each dyke.
CV13 Parameters
For the CV13 Pegmatite dykes, it was determined that no capping was required for Li2O, but Ta2O5 was capped at 1,500 ppm.
Variography analysis did not yield a well-structured variogram. On CV13, Li2O and Ta2O5 were estimated using ID2 in Leapfrog Edge.
Three (3) orientated search ellipsoids were used to select data and interpolate Li2O and Ta2O5 grades in successively less restrictive passes. The ellipse sizes and anisotropies were based on the variography, drillhole spacing, and pegmatite geometry. The ellipsoids were 80 m x 60 m x 10 m, 160 m x 120 m x 20 m, and 320 m x 240 m x 40 m. For the first pass interpolation a minimum of five (5) composites and a maximum of twelve (12) composites with a minimum of two (2) holes were needed to interpolate. For the second and third pass a minimum of three (3) composites with a maximum of twelve (12) without a minimum per hole was used. Variable search ellipse orientations (dynamic anisotropy) were used to interpolate the dykes. Spatial anisotropy of the dykes is respected during estimation using Leapfrog Edge’s Variable Orientation tool. The search ellipse follows the trend of the central reference plane of each dyke.
Parent cells of 10 m x 5 m x 5 m, subblocked four (4) times in each direction (for minimum subcells of 2.5 m in x, 1.25 m in y, and 1.25 m in z were used. Subblocks are triggered by the geological model. Li2O and Ta2O5 grades are estimated on the parent cells and automatically populated to subblocks.
The CV5 and CV13 block model is rotated around the Z axis (Leapfrog 340°). Hard boundaries between all the pegmatite domains were used for all Li2O and Ta2O5 estimates. For CV5, the Mineral Resource Estimate includes blocks within the pit shell above the cut-off grade of 0.40% Li2O or all blocks within underground mining shapes constructed with a 0.60% cut-off grade. For CV13, the Mineral Resource Estimate includes blocks within the pit shell above the cut-off grade of 0.40% Li2O or all blocks within underground mining shapes constructed with a 0.80% cut-off grade.
Validation of the block model was performed using Swath Plots, nearest neighbours grade estimates, global means comparisons, and by visual inspection in 3D and along plan views and cross-sections.
Cut-off Grade and Basis for Selection
The cut-off grade (“COG”) adopted for the Mineral Resource Estimate is 0.40% Li2O for open-pit resources (CV5 and CV13), 0.60% Li2O for underground resources at CV5, and 0.80% Li2O for underground resources at CV13. It has been determined based on operational cost estimates, primarily through benchmarking, for mining (open-pit and underground methods), tailings management, G, and concentrate transport costs from the mine site to Bécancour, QC, as the base case. Process recovery assumed a Dense Media Separation (DMS) only operation at approximately 70% average recovery into a 5.5% Li2O spodumene concentrate (Figure 37). A spodumene concentrate price of US $1,500 was assumed with USD/CAD exchange rate of 0.76. A royalty of 2% was applied.
Mining Metallurgical Methods and Parameters, and Other Modifying Factors Considered
Mineral Resources that are not Mineral Reserves do not have demonstrated economic viability. This estimate of Mineral Resources may be materially affected by environmental, permitting, legal, title, taxation, sociopolitical, marketing, economic, or other relevant issues.
The extraction scenario constraint retained for the Mineral Resource Estimate at the CV5 Spodumene Pegmatite is mainly open-pit. A pit slope ranging between 45° and 53° was assumed, resulting in a strip ratio of 8.3 (waste to minable resource) at a revenue factor of 1. Underground long hole mining method accounts for approximately 11% of CV5 resources.
The extraction scenario constraint retained for the maiden Mineral Resource Estimate at the CV13 Spodumene Pegmatite is mainly open-pit. A pit slope of 45° was assumed, resulting in a strip ratio of 9.8 (waste to minable resource) at a revenue factor of 1. Underground mining method accounts for approximately 7% of CV13 resources
The metallurgical assumptions are supported by metallurgical test programs completed by SGS Canada at their Lakefield, ON, facility. The testwork included Heavy Liquid Separation (“HLS”) and magnetics, which has produced 6+% Li2O spodumene concentrates at >70% recovery on drill core samples from both the CV5 and CV13 pegmatites. A subsequent Dense Media Separation (“DMS”) test on CV5 Spodumene Pegmatite material returned a spodumene concentrate grading 5.8% Li2O at 79% recovery, strongly indicating potential for a DMS only operation to be applicable. For the Mineral Resource conceptual mining shapes, based on a grade versus recovery curve of the test work completed to date, an average recovery of approximately 70% to produce a 5.5% Li2O spodumene concentrate was used (Figure 37).
Various mandates required for advancing the Project towards economic studies have been initiated, including but not limited to, environmental baseline, metallurgy, geotechnical, geomechanics, hydrogeology, hydrology, stakeholder engagement, geochemical characterization, as well as concentrate transport and logistical studies.
Figure 37: Metallurgical testwork results of global lithium recoveries for HLS and DMS for the CV5 Pegmatite. The estimated recovery of a three-size range DMS concentrator is shown as a recovery curve (generating a 5.5 % Li2O concentrate).
Qualified/Competent Person
The information in this news release that relates the Mineral Resource Estimate for the Shaakichiuwaanaan Project (CV5 and CV13 spodumene pegmatites), as well as other relevant technical information for the Property, is based on, and fairly represents, information compiled by Mr. Todd McCracken, P.Geo., who is a Qualified Person as defined by NI 43-101, and member in good standing with the Ordre des Géologues du Québec and with the Professional Geoscientists of Ontario. Mr. McCracken has reviewed and approved the technical information in this news release.
Mr. McCracken is Director – Mining Geology – Central Canada, of BBA Engineering Ltd. and is independent of the Company. Mr. McCracken does not hold any securities in the Company.
Mr. McCracken has sufficient experience, which is relevant to the style of mineralization, type of deposit under consideration, and to the activities being undertaken to qualify as a Competent Person as described by the JORC Code, 2012. Mr. McCracken consents to the inclusion in this news release of the matters based on his information in the form and context in which it appears.
Table 4: Attributes for drill holes and channels included in the Shaakichiuwaanaan MRE (CV5).
Hole ID
Hole Type
Substrate
Total Depth
(m)
Azimuth
(°)
Dip
(°)
Easting
Northing
Elevation
(m)
Core Size
Pegmatite
CF21-001
DD
Land
229.1
340
-45
570312.0
5930632.4
382.9
NQ
CV5
CF21-002
DD
Land
274.2
340
-45
570417.4
5930652.0
382.9
NQ
CV5
CF21-003
DD
Land
106.1
160
-45
570284.8
5930718.2
377.5
NQ
CV5
CF21-004
DD
Land
148.3
340
-45
569797.9
5930446.4
379.7
NQ
CV5
CV22-015
DD
Ice
176.9
158
-45
570514.7
5930803.9
372.8
NQ
CV5
CV22-016
DD
Ice
252.1
158
-45
570476.4
5930897.7
372.9
NQ
CV5
CV22-017
DD
Ice
344.7
158
-45
571422.5
5931224.6
372.9
NQ
CV5
CV22-018
DD
Ice
149.9
158
-45
570604.1
5930841.2
372.9
NQ
CV5
CV22-019
DD
Ice
230.9
158
-45
570573.7
5930929.8
373.0
NQ
CV5
CV22-020
DD
Ice
203.8
338
-45
571532.0
5931099.6
372.9
NQ
CV5
CV22-021
DD
Ice
246.0
158
-45
571533.1
5931095.7
372.9
NQ
CV5
CV22-022
DD
Ice
184.0
158
-45
570695.2
5930878.2
372.9
NQ
CV5
CV22-023
DD
Ice
285.0
338
-45
571202.6
5930974.2
372.8
NQ
CV5
CV22-024
DD
Ice
156.0
158
-45
570791.5
5930912.6
372.7
NQ
CV5
CV22-025
DD
Ice
153.0
158
-45
570883.9
5930953.5
372.8
NQ
CV5
CV22-026
DD
Ice
156.0
0
-90
571203.1
5930973.7
372.8
NQ
CV5
CV22-027
DD
Ice
150.1
158
-45
570976.2
5930991.9
372.8
NQ
CV5
CV22-028
DD
Ice
291.0
158
-45
570940.9
5931083.5
372.9
NQ
CV5
CV22-029
DD
Ice
165.0
158
-45
571068.2
5931036.9
372.6
NQ
CV5
CV22-030
DD
Ice
258.0
158
-45
570385.1
5930855.6
372.8
NQ
CV5
CV22-031
DD
Ice
231.0
158
-45
570849.7
5931043.2
372.7
NQ
CV5
CV22-033
DD
Land
261.1
158
-45
571349.6
5931146.9
376.3
NQ
CV5
CV22-034
DD
Land
329.8
158
-55
570138.4
5930801.6
380.8
NQ
CV5
CV22-035
DD
Land
281.0
158
-45
571233.8
5931157.5
378.2
NQ
CV5
CV22-036
DD
Land
334.8
158
-45
570041.9
5930778.2
379.9
NQ
CV5
CV22-037
DD
Land
311.0
158
-45
571441.5
5931177.6
377.3
NQ
CV5
CV22-038
DD
Land
316.8
158
-45
569940.4
5930729.6
377.1
NQ
CV5
CV22-039
DD
Land
256.9
158
-45
571398.5
5931163.6
377.0
NQ
CV5
CV22-040
DD
Land
403.8
158
-45
569853.1
5930698.0
375.6
NQ
CV5
CV22-041
DD
Land
295.9
158
-45
571487.3
5931201.3
379.2
NQ
CV5
CV22-042
DD
Land
393.0
158
-65
571487.1
5931201.7
379.1
NQ
CV5
CV22-043
DD
Land
513.6
158
-59
569853.0
5930698.2
375.5
NQ
CV5
CV22-044
DD
Land
414.5
158
-45
571378.4
5931326.0
379.1
NQ
CV5
CV22-045
DD
Land
377.4
158
-45
569764.1
5930673.7
377.3
NQ
CV5
CV22-046
DD
Land
463.9
158
-50
570343.7
5930959.1
383.3
NQ
CV5
CV22-047
DD
Land
554.1
158
-59
571378.5
5931326.2
378.9
NQ
CV5
CV22-048
DD
Land
449.2
158
-45
570257.0
5930903.3
381.1
NQ
CV5
CV22-049
DD
Land
304.8
158
-45
571132.3
5931145.9
376.5
NQ
CV5
CV22-050
DD
Land
339.0
158
-60
571132.6
5931146.4
376.4
NQ
CV5
CV22-051
DD
Land
520.8
158
-58
570158.5
5930876.4
382.2
NQ
CV5
CV22-052
DD
Land
284.8
158
-45
571042.1
5931111.4
375.5
NQ
CV5
CV22-053
DD
Water
218.5
158
-45
570756.9
5930998.2
373.1
NQ
CV5
CV22-054
DD
Land
126.4
158
-58
570014.4
5930567.1
378.9
NQ
CV5
CV22-055
DD
Land
320.0
158
-60
571042.1
5931111.7
375.5
NQ
CV5
CV22-056
DD
Water
241.9
158
-45
570678.6
5930970.9
373.3
NQ
CV5
CV22-057
DD
Land
443.1
158
-45
570014.4
5930566.9
379.0
NQ
CV5
CV22-058
DD
Land
299.0
158
-45
571169.8
5931057.3
376.4
NQ
CV5
CV22-059
DD
Water
352.9
158
-45
570300.2
5930796.4
373.2
NQ
CV5
CV22-060
DD
Land
147.1
158
-45
570148.9
5930635.1
383.4
NQ
CV5
CV22-061
DD
Land
340.9
158
-45
571279.4
5931068.3
378.9
NQ
CV5
CV22-062
DD
Land
220.8
158
-45
570233.0
5930693.9
375.8
NQ
CV5
CV22-063
DD
Land
325.4
158
-45
571580.8
5931234.3
376.5
NQ
CV5
CV22-064
DD
Water
340.7
158
-53
570199.3
5930782.3
373.2
NQ
CV5
CV22-065
DD
Land
242.0
158
-45
570331.7
5930722.3
381.7
NQ
CV5
CV22-066
DD
Land
437.0
158
-48
571560.9
5931295.4
377.0
NQ
CV5
CV22-067
DD
Land
281.1
158
-45
570430.5
5930741.1
380.0
NQ
CV5
CV22-068
DD
Land
233.0
158
-45
569930.0
5930522.4
378.2
NQ
CV5
CV22-069
DD
Land
494.1
158
-65
571560.6
5931295.6
377.0
NQ
CV5
CV22-070
DD
Water
297.4
158
-45
570118.7
5930731.4
373.2
NQ
CV5
CV22-071
DD
Land
377.0
158
-45
569827.9
5930505.3
377.5
NQ
CV5
CV22-072
DD
Water
404.0
158
-45
570080.9
5930689.0
373.2
NQ
CV5
CV22-073
DD
Land
541.9
158
-52
571274.6
5931307.1
381.4
NQ
CV5
CV22-074
DD
Land
398.0
158
-45
569719.7
5930500.1
385.9
NQ
CV5
CV22-075
DD
Water
372.4
158
-45
569987.6
5930639.4
373.7
NQ
CV5
CV22-076
DD
Land
161.0
158
-45
571349.0
5930872.5
377.7
NQ
CV5
CV22-078
DD
Land
163.8
158
-65
571348.8
5930872.4
377.4
NQ
CV5
CV22-079
DD
Land
425.0
158
-45
571661.1
5931296.1
379.5
NQ
CV5
CV22-080
DD
Water
359.0
158
-45
569929.5
5930618.7
374.3
NQ
CV5
CV22-083
DD
Land
440.0
158
-65
571660.9
5931296.4
379.5
NQ
CV5
CV22-086
DD
Water
200.0
158
-45
571400.8
5931070.6
373.6
NQ
CV5
CV22-089
DD
Water
251.0
158
-45
571636.1
5931142.4
373.1
NQ
CV5
CV22-090
DD
Land
416.0
158
-45
571743.8
5931362.1
378.3
NQ
CV5
CV22-093
DD
Land
408.2
158
-65
571743.5
5931362.3
378.3
NQ
CV5
CV22-097
DD
Land
506.1
158
-72
571644.7
5931342.7
378.5
NQ
CV5
CV22-098
DD
Land
374.0
158
-45
570791.5
5931143.5
380.7
NQ
CV5
CV22-100
DD
Land
458.0
158
-45
571472.6
5931356.6
376.6
NQ
CV5
CV22-102
DD
Land
393.2
158
-45
570626.6
5931060.4
378.5
NQ
CV5
CV23-105
DD
Land
452.0
158
-65
571832.1
5931386.7
376.5
NQ
CV5
CV23-106
DD
Land
491.0
158
-65
571929.5
5931439.0
377.8
NQ
CV5
CV23-107
DD
Land
428.2
158
-65
572027.0
5931475.3
374.5
NQ
CV5
CV23-108
DD
Land
461.0
158
-65
572118.4
5931506.1
374.0
NQ
CV5
CV23-109
DD
Land
392.1
158
-45
571832.3
5931386.2
376.5
NQ
CV5
CV23-110
DD
Land
431.0
158
-45
571866.1
5931434.5
375.7
NQ
CV5
CV23-111
DD
Land
356.0
158
-45
572027.2
5931474.7
374.4
NQ
CV5
CV23-112
DD
Land
377.1
158
-45
571929.7
5931438.5
377.8
NQ
CV5
CV23-113
DD
Land
389.0
158
-45
572118.5
5931505.7
374.2
NQ
CV5
CV23-114
DD
Land
500.1
158
-55
571865.9
5931434.7
375.7
NQ
CV5
CV23-115
DD
Land
431.1
158
-45
572056.8
5931529.0
373.0
NQ
CV5
CV23-116
DD
Land
476.0
158
-65
572214.5
5931532.1
373.5
NQ
CV5
CV23-117
DD
Land
566.1
158
-75
571865.9
5931434.7
375.7
NQ
CV5
CV23-118
DD
Land
437.1
158
-45
572214.8
5931531.4
373.4
NQ
CV5
CV23-119
DD
Land
389.0
158
-45
572099.4
5931442.2
373.8
NQ
CV5
CV23-120
DD
Land
443.0
158
-45
572150.2
5931552.7
376.5
NQ
CV5
CV23-121
DD
Land
454.7
158
-48
571782.1
5931402.9
377.0
NQ
CV5
CV23-122
DD
Land
403.9
158
-45
572167.6
5931496.0
375.3
NQ
CV5
CV23-123
DD
Land
386.0
158
-45
571997.7
5931407.9
374.2
NQ
CV5
CV23-124
DD
Land
653.0
158
-45
571955.3
5931497.9
374.4
NQ
CV5
CV23-125
DD
Land
545.0
158
-65
572647.7
5931670.5
382.4
NQ
CV5
CV23-127
DD
Land
548.0
158
-59
571680.9
5931383.8
375.3
NQ
CV5
CV23-128
DD
Land
362.0
158
-45
571212.0
5931077.7
376.5
NQ
CV5
CV23-129
DD
Land
380.0
158
-45
571100.3
5931096.5
375.6
NQ
CV5
CV23-130
DD
Land
377.0
158
-45
571171.8
5931167.6
374.9
NQ
CV5
CV23-131
DD
Ice
454.9
158
-45
571907.3
5931366.9
373.2
NQ
CV5
CV23-132
DD
Land
374.0
158
-49
571068.0
5931148.3
374.7
NQ
CV5
CV23-133
DD
Land
604.8
220
-45
572646.6
5931668.7
382.6
NQ
CV5
CV23-134
DD
Land
331.0
158
-45
571281.9
5931163.8
379.2
NQ
CV5
CV23-135
DD
Land
360.6
158
-60
571171.6
5931167.9
374.9
NQ
CV5
CV23-136
DD
Ice
403.9
158
-45
572240.8
5931603.3
373.1
NQ
CV5
CV23-137
DD
Land
389.0
158
-65
571067.9
5931148.6
374.7
NQ
CV5
CV23-138
DD
Land
359.1
158
-60
571281.9
5931163.8
379.2
NQ
CV5
CV23-139
DD
Ice
565.9
158
-65
572396.1
5931617.8
372.9
NQ
CV5
CV23-140
DD
Ice
545.3
158
-65
572306.4
5931573.2
373.0
NQ
CV5
CV23-141
DD
Land
400.9
158
-65
571781.4
5931403.7
377.9
NQ
CV5
CV23-142
DD
Land
359.0
158
-73
571387.3
5931180.7
377.2
NQ
CV5
CV23-143
DD
Land
530.2
158
-45
572647.9
5931670.0
382.4
NQ
CV5
CV23-145
DD
Land
53.0
0
-90
569657.7
5930878.2
372.7
HQ
CV5
CV23-146
DD
Ice
416.0
158
-45
572306.4
5931573.2
373.0
NQ
CV5
CV23-148
DD
Land
332.0
158
-58
571387.4
5931180.3
377.3
NQ
CV5
CV23-150
DD
Land
302.1
0
-90
571426.9
5931160.9
376.7
NQ
CV5
CV23-151
DD
Ice
486.0
158
-45
572396.1
5931617.8
372.9
NQ
CV5
CV23-153
DD
Land
300.1
0
-90
571785.2
5931397.3
378.6
NQ
CV5
CV23-154
DD
Ice
574.9
158
-65
572487.3
5931652.3
372.9
NQ
CV5
CV23-156
DD
Land
581.3
176
-67
572647.4
5931670.4
382.6
NQ
CV5
CV23-157
DD
Land
278.1
0
-90
570694.6
5931128.2
379.0
NQ
CV5
CV23-159
DD
Land
50.0
0
-90
570520.0
5931135.3
375.6
HQ
CV5
CV23-160A
DD
Land
443.0
158
-45
569567.5
5930470.9
380.4
NQ
CV5
CV23-161
DD
Land
360.0
158
-45
569627.6
5930449.9
384.8
NQ
CV5
CV23-162
DD
Ice
482.0
158
-45
572487.3
5931652.3
372.9
NQ
CV5
CV23-164
DD
Land
200.0
0
-90
570020.1
5930773.5
378.1
NQ
CV5
CV23-165
DD
Land
555.1
165
-60
572647.7
5931669.8
382.4
NQ
CV5
CV23-166A
DD
Land
50.0
0
-90
569353.0
5930256.3
389.1
HQ
CV5
CV23-168A
DD
Ice
388.1
158
-47
571515.8
5931250.9
373.0
NQ
CV5
CV23-169
DD
Land
302.0
0
-90
569733.9
5930466.5
379.2
NQ
CV5
CV23-170
DD
Ice
431.6
158
-45
572461.9
5931596.5
373.0
NQ
CV5
CV23-171
DD
Land
373.4
158
-63
569568.8
5930470.2
380.1
NQ
CV5
CV23-172
DD
Land
404.0
158
-45
569479.9
5930448.2
384.1
NQ
CV5
CV23-173
DD
Ice
516.7
158
-65
572461.9
5931596.5
373.0
NQ
CV5
CV23-174
DD
Land
421.7
0
-90
569992.0
5930469.4
381.0
NQ
CV5
CV23-175
DD
Ice
458.0
158
-57
571316.1
5931230.2
372.9
NQ
CV5
CV23-176
DD
Land
434.0
158
-45
569388.0
5930399.5
386.2
NQ
CV5
CV23-177
DD
Ice
394.7
158
-45
571453.4
5931292.5
373.0
NQ
CV5
CV23-178
DD
Land
473.2
158
-62
569479.8
5930448.6
384.1
NQ
CV5
CV23-179
DD
Ice
437.0
158
-45
572368.8
5931547.6
372.9
NQ
CV5
CV23-180
DD
Land
379.6
150
-60
569387.8
5930400.0
386.2
NQ
CV5
CV23-181
DD
Ice
354.0
158
-46
571316.2
5931230.0
372.9
NQ
CV5
CV23-182
DD
Land
369.0
158
-45
569295.1
5930361.6
389.4
NQ
CV5
CV23-183
DD
Ice
477.1
158
-65
572368.7
5931548.1
372.8
NQ
CV5
CV23-184
DD
Land
417.4
158
-45
569198.6
5930332.0
392.7
NQ
CV5
CV23-185
DD
Ice
425.0
158
-60
571453.3
5931292.7
372.9
NQ
CV5
CV23-187
DD
Land
287.0
158
-45
569698.8
5930420.6
381.0
NQ
CV5
CV23-188
DD
Land
362.0
158
-60
569294.9
5930361.9
389.3
NQ
CV5
CV23-189
DD
Land
287.0
158
-45
571702.0
5931318.4
380.1
NQ
CV5
CV23-190
DD
Land
303.3
338
-45
569596.9
5930277.1
382.2
NQ
CV5
CV23-192
DD
Land
354.0
0
-90
570330.5
5930613.3
383.4
NQ
CV5
CV23-193
DD
Land
250.9
0
-90
569597.2
5930276.2
381.2
NQ
CV5
CV23-194
DD
Land
282.0
0
-90
570802.4
5930731.5
382.1
NQ
CV5
CV23-196
DD
Land
263.0
158
-45
569599.0
5930272.7
381.3
NQ
CV5
CV23-199
DD
Land
261.1
0
-90
570473.2
5930744.8
376.9
NQ
CV5
CV23-201
DD
Land
385.8
158
-45
569015.1
5930242.6
390.3
NQ
CV5
CV23-203
DD
Land
374.0
158
-45
569121.0
5930244.3
396.1
NQ
CV5
CV23-205
DD
Land
353.0
158
-60
569015.0
5930242.8
390.2
NQ
CV5
CV23-206
DD
Land
322.8
158
-60
569120.8
5930244.6
396.1
NQ
CV5
CV23-208
DD
Land
368.0
158
-45
568937.2
5930165.2
391.0
NQ
CV5
CV23-209
DD
Land
434.0
158
-45
569043.4
5930314.1
384.9
NQ
CV5
CV23-211
DD
Land
425.0
158
-60
568937.1
5930165.5
391.0
NQ
CV5
CV23-212
DD
Water
296.0
158
-45
571736.6
5931251.3
372.7
NQ
CV5
CV23-214
DD
Land
502.1
158
-55
569043.3
5930314.3
384.7
NQ
CV5
CV23-217
DD
Land
329.0
158
-45
568751.3
5930093.9
390.0
NQ
CV5
CV23-219
DD
Land
380.1
158
-45
568848.3
5930136.9
394.8
NQ
CV5
CV23-220
DD
Water
275.0
158
-45
571824.6
5931284.7
372.2
NQ
CV5
CV23-222
DD
Land
404.0
158
-65
568751.1
5930094.6
390.1
NQ
CV5
CV23-223
DD
Land
428.0
158
-60
568848.3
5930137.2
394.9
NQ
CV5
CV23-225
DD
Water
452.0
158
-45
571936.0
5931267.6
372.2
NQ
CV5
CV23-226
DD
Land
338.0
158
-45
568706.3
5930070.7
386.7
NQ
CV5
CV23-228
DD
Land
510.0
158
-80
568847.6
5930136.7
394.7
NQ
CV5
CV23-230
DD
Water
311.0
158
-45
570172.3
5930717.7
372.7
NQ
CV5
CV23-231
DD
Land
359.0
158
-65
568706.0
5930071.1
386.6
NQ
CV5
CV23-232
DD
Water
388.9
158
-45
572029.7
5931311.9
373.4
NQ
CV5
CV23-236
DD
Land
383.1
158
-45
568615.9
5930016.6
387.6
NQ
CV5
CV23-240
DD
Land
377.0
158
-45
568637.2
5930099.9
391.5
NQ
CV5
CV23-241
DD
Water
418.9
158
-62
570172.4
5930717.8
372.6
NQ
CV5
CV23-243
DD
Land
395.0
158
-65
568615.8
5930017.1
387.4
NQ
CV5
CV23-244
DD
Water
313.0
158
-45
572125.2
5931345.5
372.9
NQ
CV5
CV23-246
DD
Land
431.0
0
-90
570215.1
5930649.7
382.3
NQ
CV5
CV23-248
DD
Land
466.1
158
-65
568636.9
5930100.4
391.6
NQ
CV5
CV23-251
DD
Water
160.9
158
-45
570938.7
5930950.0
373.2
NQ
CV5
CV23-252
DD
Water
281.0
158
-45
572214.3
5931370.1
372.2
NQ
CV5
CV23-256
DD
Water
296.2
158
-45
571043.3
5930964.1
372.1
NQ
CV5
CV23-259
DD
Land
383.0
158
-45
568550.1
5930065.0
393.5
NQ
CV5
CV23-260
DD
Water
260.0
158
-45
572336.8
5931379.7
372.1
NQ
CV5
CV23-265
DD
Water
277.9
158
-45
571134.0
5931003.5
372.3
NQ
CV5
CV23-268
DD
Land
417.6
158
-65
568550.3
5930064.6
393.4
NQ
CV5
CV23-272A
DD
Water
410.2
158
-45
570328.8
5930856.6
372.8
NQ
CV5
CV23-273
DD
Land
359.0
158
-45
568457.9
5930020.1
392.5
NQ
CV5
CV23-274
DD
Water
226.4
158
-45
571199.9
5930974.4
372.6
NQ
CV5
CV23-279
DD
Water
227.7
158
-45
571250.2
5930988.5
373.1
NQ
CV5
CV23-283
DD
Land
362.0
158
-45
568526.0
5929989.7
387.7
NQ
CV5
CV23-285
DD
Water
469.9
158
-60
570328.4
5930856.8
372.8
NQ
CV5
CV23-287
DD
Water
176.0
158
-45
571336.6
5931031.0
372.8
NQ
CV5
CV23-290
DD
Land
443.0
158
-60
569197.2
5930336.0
392.0
NQ
CV5
CV23-291
DD
Water
169.2
158
-70
571336.7
5931031.4
372.3
NQ
CV5
CV23-292
DD
Land
389.1
158
-65
568457.4
5930020.9
392.5
NQ
CV5
CV23-295
DD
Land
362.9
158
-65
568526.0
5929990.0
387.7
NQ
CV5
CV23-297
DD
Water
194.0
158
-45
571682.5
5931113.0
372.5
NQ
CV5
CV23-298
DD
Water
440.1
158
-64
570449.3
5930831.3
372.7
NQ
CV5
CV23-303
DD
Land
290.9
158
-45
568922.1
5930064.4
395.4
NQ
CV5
CV23-307
DD
Land
357.3
285
-45
569814.2
5930403.6
382.3
NQ
CV5
CV23-308
DD
Water
171.2
158
-46
571479.7
5931087.4
372.9
NQ
CV5
CV23-313
DD
Water
371.0
158
-45
570449.7
5930830.8
372.7
NQ
CV5
CV23-314
DD
Water
359.0
338
-45
571479.2
5931088.9
372.1
NQ
CV5
CV23-317
DD
Land
431.9
338
-45
568922.9
5930067.3
395.1
NQ
CV5
CV23-321
DD
Land
252.1
158
-45
569813.6
5930404.2
381.9
NQ
CV5
CV23-325
DD
Water
238.9
158
-47
571440.8
5931045.2
372.2
NQ
CV5
CV23-327
DD
Water
386.0
158
-45
570541.7
5930871.4
372.7
NQ
CV5
CV23-329
DD
Land
277.8
310
-55
569812.8
5930405.2
381.9
NQ
CV5
CV23-331
DD
Land
423.0
158
-45
568415.4
5929988.0
395.9
NQ
CV5
CV23-335
DD
Water
263.0
158
-76
571440.5
5931063.1
372.7
NQ
CV5
CV23-337
DD
Land
427.9
338
-45
569717.2
5930368.0
382.0
NQ
CV5
CV23-338
DD
Water
176.0
158
-45
570761.8
5930850.3
372.9
NQ
CV5
CV23-340
DD
Water
212.0
158
-60
571760.9
5931197.6
372.9
NQ
CV5
CV23-342
DD
Water
212.0
158
-45
570631.7
5930908.8
372.8
NQ
CV5
CV23-344
DD
Land
530.2
158
-65
568415.3
5929988.4
395.9
NQ
CV5
CV23-347
DD
Land
230.0
158
-45
569717.7
5930367.4
382.0
NQ
CV5
CV23-349
DD
Water
133.9
158
-45
571865.8
5931191.5
373.4
NQ
CV5
CV23-352
DD
Land
227.0
158
-45
569626.0
5930335.2
381.7
NQ
CV5
CV23-354
DD
Land
296.0
158
-45
569536.2
5930296.9
381.9
NQ
CV5
CV23-357
DD
Land
328.8
158
-45
568371.0
5929961.8
392.7
NQ
CV5
CV23-359
DD
Land
251.1
158
-45
569443.3
5930256.2
383.8
NQ
CV5
CV23-362
DD
Land
356.1
338
-45
571560.3
5931009.3
373.3
NQ
CV5
CV23-363
DD
Land
218.0
158
-45
569347.1
5930221.6
389.4
NQ
CV5
CV23-364
DD
Land
401.0
158
-65
568370.8
5929962.2
392.6
NQ
CV5
CV24-366
DD
Land
489.4
158
-52
570954.3
5931181.8
376.3
NQ
CV5
CV24-367
DD
Land
459.2
160
-49
571374.2
5931330.7
378.5
NQ
CV5
CV24-368
DD
Land
493.9
158
-50
569790.2
5930721.4
375.2
NQ
CV5
CV24-370
DD
Land
511.8
158
-48
570073.6
5930820.6
381.2
NQ
CV5
CV24-371
DD
Land
561.9
158
-57
571477.3
5931353.1
374.7
NQ
CV5
CV24-372
DD
Land
487.9
158
-45
570218.9
5930863.1
375.2
NQ
CV5
CV24-373
DD
Land
479.2
160
-45
569832.6
5930629.6
373.0
NQ
CV5
CV24-374
DD
Land
470.0
158
-46
570693.3
5931027.8
373.3
NQ
CV5
CV24-375
DD
Land
302.1
158
-45
569251.7
5930186.6
395.0
NQ
CV5
CV24-376
DD
Land
583.7
158
-60
570036.0
5930779.8
377.9
NQ
CV5
CV24-377
DD
Land
451.9
158
-45
569911.5
5930690.1
374.0
NQ
CV5
CV24-378
DD
Land
493.0
158
-47
571569.3
5931385.6
374.0
NQ
CV5
CV24-379
DD
Land
613.9
158
-60
570693.4
5931028.3
373.3
NQ
CV5
CV24-380
DD
Land
559.9
158
-60
570218.9
5930863.3
374.9
NQ
CV5
CV24-381
DD
Land
302.1
158
-45
569160.9
5930149.9
395.0
NQ
CV5
CV24-382
DD
Land
506.0
158
-56
569911.6
5930690.5
373.9
NQ
CV5
CV24-383A
DD
Land
308.0
158
-45
569003.7
5930137.6
396.3
NQ
CV5
CV24-384
DD
Land
545.9
158
-57
569946.9
5930739.3
376.4
NQ
CV5
CV24-385
DD
Land
382.9
158
-45
569148.4
5930308.3
394.3
NQ
CV5
CV24-386
DD
Land
552.6
158
-58
571388.7
5931175.9
376.5
NQ
CV5
CV24-388
DD
Land
515.0
158
-58
571569.1
5931386.1
374.1
NQ
CV5
CV24-389
DD
Land
388.2
158
-45
569443.3
5930367.7
383.5
NQ
CV5
CV24-390
DD
Land
620.0
158
-45
570392.4
5930967.3
379.2
NQ
CV5
CV24-391
DD
Land
341.0
158
-45
569214.2
5930279.5
396.6
NQ
CV5
CV24-392
DD
Land
633.1
165
-58
571841.1
5931393.0
377.3
NQ
CV5
CV24-393
DD
Land
462.3
158
-75
569003.4
5930138.0
396.2
NQ
CV5
CV24-394
DD
Land
575.2
158
-47
571605.9
5931299.3
377.2
NQ
CV5
CV24-395
DD
Land
296.1
158
-45
569280.1
5930256.9
394.0
NQ
CV5
CV24-398
DD
Land
431.0
158
-45
569409.3
5930473.0
374.9
NQ
CV5
CV24-399
DD
Ice
527.0
158
-60
570600.6
5930984.8
372.1
NQ
CV5
CV24-400
DD
Land
551.0
158
-52
571388.7
5931175.6
376.5
NQ
CV5
CV24-401A
DD
Land
626.1
158
-58
572056.2
5931528.9
373.1
NQ
CV5
CV24-402
DD
Land
444.4
158
-75
569280.1
5930257.5
393.9
NQ
CV5
CV24-403
DD
Land
373.9
158
-45
569031.2
5930205.5
393.6
NQ
CV5
CV24-404
DD
Land
668.2
162
-59
571931.0
5931431.7
377.3
NQ
CV5
CV24-405
DD
Land
439.9
158
-60
571659.0
5931300.4
378.4
NQ
CV5
CV24-407
DD
Land
296.0
158
-45
569066.8
5930115.0
394.7
NQ
CV5
CV24-408
DD
Land
410.0
158
-45
569237.8
5930354.0
389.3
NQ
CV5
CV24-409
DD
Land
356.1
158
-45
569542.0
5930406.0
383.7
NQ
CV5
CV24-410
DD
Ice
609.0
158
-47
570507.2
5930955.1
372.0
NQ
CV5
CV24-413
DD
Ice
431.0
158
-62
570940.7
5931079.8
372.1
NQ
CV5
CV24-414
DD
Land
425.0
158
-45
569516.5
5930473.0
383.8
NQ
CV5
CV24-415A
DD
Land
576.4
158
-45
571679.3
5931388.3
374.3
NQ
CV5
CV24-416
DD
Land
334.8
158
-45
569358.6
5930330.1
389.7
NQ
CV5
CV24-418
DD
Ice
624.4
158
-47
570600.7
5930984.1
372.1
NQ
CV5
CV24-419
DD
Land
595.9
165
-45
572117.8
5931509.9
372.8
NQ
CV5
CV24-422
DD
Land
572.8
158
-58
571955.7
5931504.0
373.3
NQ
CV5
CV24-423A
DD
Land
329.0
158
-75
569358.9
5930329.9
389.6
NQ
CV5
CV24-424
DD
Land
389.0
158
-53
569615.3
5930495.5
378.1
NQ
CV5
CV24-426
DD
Ice
587.0
158
-45
571004.5
5931058.8
371.9
NQ
CV5
CV24-428
DD
Ice
543.1
158
-45
570728.4
5930940.4
372.1
NQ
CV5
CV24-430
DD
Land
361.9
158
-45
569187.9
5930215.3
397.6
NQ
CV5
CV24-431
DD
Land
352.9
338
-60
569800.9
5930431.0
379.5
NQ
CV5
CV24-433
DD
Ice
508.9
158
-48
570881.7
5931098.0
372.1
NQ
CV5
CV24-434
DD
Ice
467.8
158
-60
570507.2
5930955.1
372.0
NQ
CV5
CV24-435
DD
Land
502.9
158
-60
572117.8
5931509.9
372.8
NQ
CV5
CV24-437
DD
Land
433.9
158
-55
571679.2
5931388.7
374.3
NQ
CV5
CV24-438
DD
Ice
408.3
158
-48
571812.0
5931329.7
372.0
NQ
CV5
CV24-440
DD
Land
438.5
158
-75
569187.5
5930215.9
397.5
NQ
CV5
CV24-441
DD
Ice
342.2
158
-65
571004.7
5931058.3
372.0
NQ
CV5
CV24-442
DD
Land
299.1
158
-87
569802.0
5930429.6
379.4
NQ
CV5
CV24-443
DD
Ice
383.2
158
-45
570818.0
5930984.2
372.0
NQ
CV5
CV24-445
DD
Ice
295.3
158
-45
571968.9
5931339.0
371.9
NQ
CV5
CV24-447
DD
Land
308.4
130
-55
571152.3
5931101.1
375.1
NQ
CV5
CV24-448
DD
Land
341.9
158
-75
569802.0
5930430.0
379.4
NQ
CV5
CV24-449
DD
Ice
291.8
158
-62
570881.7
5931098.3
372.0
NQ
CV5
CV24-450
DD
Land
299.0
160
-45
569864.8
5930545.1
373.3
NQ
CV5
CV24-451
DD
Ice
503.0
158
-45
571771.2
5931288.6
372.0
NQ
CV5
CV24-452
DD
Land
505.9
145
-50
571679.5
5931388.0
374.3
HQ
CV5
CV24-455
DD
Ice
379.8
158
-45
570909.9
5931018.4
372.0
NQ
CV5
CV24-456
DD
Land
456.9
200
-55
570174.5
5930836.0
378.3
NQ
CV5
CV24-458
DD
Ice
328.0
152
-62
571968.6
5931339.6
371.9
NQ
CV5
CV24-460
DD
Ice
263.0
158
-45
571650.2
5931198.3
372.0
NQ
CV5
CV24-462
DD
Land
299.5
158
-45
569773.4
5930503.0
377.2
NQ
CV5
CV24-463
DD
Land
337.9
158
-45
570612.9
5930686.0
378.8
NQ
CV5
CV24-465
DD
Ice
325.0
158
-48
571877.8
5931300.2
372.1
NQ
CV5
CV24-466
DD
Ice
530.3
338
-45
571841.0
5931124.0
372.0
NQ
CV5
CV24-467
DD
Ice
539.2
158
-45
570782.1
5931075.0
372.3
NQ
CV5
CV24-468
DD
Ice
461.0
158
-46
571695.3
5931217.0
372.0
NQ
CV5
CV24-469
DD
Land
409.9
40
-60
571572.0
5930953.4
373.2
NQ
CV5
CV24-472
DD
Land
355.9
338
-45
570503.6
5930694.8
379.8
NQ
CV5
CV24-473
DD
Ice
359.0
153
-58
571514.3
5931262.1
371.9
NQ
CV5
CV24-474
DD
Land
223.9
159
-46
569207.2
5930170.9
396.0
NQ
CV5
CV24-475
DD
Ice
280.1
158
-45
572062.4
5931376.6
371.9
NQ
CV5
CV24-476
DD
Land
557.0
154
-55
570170.7
5930834.1
378.4
NQ
CV5
CV24-479
DD
Land
467.1
16
-55
570355.0
5930476.9
379.2
NQ
CV5
CV24-480
DD
Land
560.3
158
-65
571994.4
5931554.1
372.2
NQ
CV5
CV24-481
DD
Land
272.3
157
-46
569311.2
5930294.6
391.0
NQ
CV5
CV24-482
DD
Ice
305.0
158
-55
572062.4
5931376.0
371.9
NQ
CV5
CV24-485
DD
Ice
365.0
150
-45
571515.2
5931261.4
371.9
NQ
CV5
CV24-486
DD
Ice
299.0
156
-45
571551.6
5931169.2
372.0
NQ
CV5
CV24-488
DD
Land
197.0
160
-45
569373.9
5930278.5
390.3
NQ
CV5
CV24-489
DD
Land
356.0
158
-45
570204.3
5930636.1
382.0
NQ
CV5
CV24-490
DD
Ice
314.3
158
-47
572155.1
5931412.9
372.1
NQ
CV5
CV24-493
DD
Land
218.1
160
-45
569649.4
5930384.4
381.0
NQ
CV5
CV24-494
DD
Land
439.9
158
-60
570227.9
5930714.7
374.8
NQ
CV5
CV24-495
DD
Ice
230.3
158
-45
571803.4
5931216.2
372.0
NQ
CV5
CV24-496
DD
Land
509.0
113
-55
571529.1
5931440.2
390.7
NQ
CV5
CV24-500
DD
Land
512.1
158
-65
571932.1
5931649.5
378.7
NQ
CV5
CV24-501A
DD
Land
403.2
155
-49
572023.6
5931471.2
374.6
NQ
CV5
CV24-502
DD
Land
476.5
145
-52
570360.1
5930766.7
374.0
NQ
CV5
CV24-503
DD
Land
533.1
160
-45
570305.6
5930884.3
372.1
NQ
CV5
CV24-504
DD
Land
302.4
158
-45
570181.3
5930561.3
385.0
NQ
CV5
CV24-505
DD
Land
581.0
158
-58
569994.1
5930753.1
376.5
NQ
CV5
CV24-509
DD
Land
425.4
157
-53
570262.4
5930743.7
373.9
NQ
CV5
CV24-512
DD
Land
317.0
158
-46
570054.0
5930596.6
376.9
NQ
CV5
CV24-514
DD
Land
601.3
158
-50
570459.7
5931100.8
378.2
NQ
CV5
CV24-515
DD
Ice
424.4
160
-58
572240.8
5931602.7
371.8
NQ
CV5
CV24-516
DD
Land
517.9
170
-45
572564.5
5931732.2
375.0
NQ
CV5
CV24-517
DD
Land
428.1
152
-56
570402.3
5930773.8
374.1
NQ
CV5
CV24-521
DD
Land
504.1
158
-45
568928.0
5930328.5
377.9
NQ
CV5
CV24-522
DD
Land
260.2
159
-45
570073.4
5930544.4
379.3
NQ
CV5
CV24-526
DD
Land
442.9
158
-45
569994.4
5930752.6
376.4
NQ
CV5
CH22-001
CH
Land
2.1
342
-7
571342.6
5930847.1
378.4
n/a
CV5
CH22-002
CH
Land
3.9
165
-31
571340.7
5930846.3
378.5
n/a
CV5
CH22-003
CH
Land
1.9
346
-6
571377.5
5930850.9
377.9
n/a
CV5
CH22-007
CH
Land
7.3
340
-30
570151.2
5930541.4
385.3
n/a
CV5
CV1-CH01
CH
Land
8.0
0
0
571477.3
5931121.0
373.4
n/a
CV5
CV1-CH02
CH
Land
6.0
0
0
571393.9
5931098.8
381.9
n/a
CV5
CV1-CH03
CH
Land
11.0
0
0
571381.0
5931103.9
382.2
n/a
CV5
CV1-CH04
CH
Land
4.0
0
0
571340.5
5931110.5
381.2
n/a
CV5
CV1-CH05
CH
Land
11.0
0
0
571435.1
5931107.2
380.6
n/a
CV5
CV2-CH01
CH
Land
4.0
338
0
571299.6
5931156.1
379.6
n/a
CV5
CV2-CH02
CH
Land
4.0
355
0
571274.9
5931156.7
380.0
n/a
CV5
(1) Coordinate system NAD83 / UTM zone 18N; (2) DD = diamond drill, CH = channel; (3) DD azimuths and dips presented are those 'planned' and may vary off collar/downhole.
Table 5: Attributes for drill holes and channels included in the Shaakichiuwaanaan MRE (CV13).
Hole ID
Hole Type
Substrate
Total Depth
(m)
Azimuth
(°)
Dip
(°)
Easting
Northing
Elevation
(m)
Core Size
Pegmatite
CV22-077
DD
Land
209.0
200
-45
564974.5
5927821.5
390.9
NQ
CV13
CV22-081
DD
Land
50.0
200
-80
564974.4
5927822.2
390.9
NQ
CV13
CV22-082
DD
Land
186.7
200
-45
565010.2
5927856.7
398.5
NQ
CV13
CV22-084
DD
Land
247.8
200
-80
565010.3
5927857.6
398.5
NQ
CV13
CV22-085
DD
Land
201.1
200
-45
565050.0
5927857.9
399.2
NQ
CV13
CV22-088
DD
Land
185.0
140
-45
565052.8
5927858.4
399.0
NQ
CV13
CV22-091
DD
Land
200.0
135
-45
565249.5
5928035.3
429.6
NQ
CV13
CV22-092
DD
Land
260.0
145
-45
565267.4
5928079.4
434.6
NQ
CV13
CV22-095
DD
Land
58.9
145
-65
565266.9
5928080.0
434.7
NQ
CV13
CV22-096
DD
Land
218.0
140
-45
565731.7
5928451.9
386.0
NQ
CV13
CV22-099
DD
Land
248.1
140
-45
565795.5
5928473.1
382.7
NQ
CV13
CV22-101
DD
Land
245.1
140
-65
565795.1
5928473.5
382.7
NQ
CV13
CV22-103
DD
Land
269.0
200
-45
564406.1
5927962.1
403.8
NQ
CV13
CV22-104
DD
Land
68.0
200
-65
564406.1
5927962.5
403.7
NQ
CV13
CV23-191
DD
Land
308.2
170
-45
565125.9
5928034.9
432.4
NQ
CV13
CV23-195
DD
Land
308.0
0
-90
565125.7
5928035.6
432.3
NQ
CV13
CV23-198
DD
Land
98.0
140
-80
565126.2
5928036.0
432.4
NQ
CV13
CV23-200
DD
Land
250.9
100
-45
565128.0
5928036.2
432.4
NQ
CV13
CV23-202
DD
Land
302.0
220
-45
565054.8
5927953.3
419.4
NQ
CV13
CV23-204
DD
Land
262.9
130
-80
565057.6
5927954.3
419.2
NQ
CV13
CV23-207
DD
Land
278.0
140
-45
565058.1
5927953.0
419.0
NQ
CV13
CV23-210
DD
Land
272.0
210
-55
564875.9
5927914.8
409.7
NQ
CV13
CV23-213
DD
Land
209.0
200
-85
564876.6
5927915.3
409.7
NQ
CV13
CV23-215
DD
Land
215.0
150
-45
564878.4
5927914.4
409.5
NQ
CV13
CV23-216
DD
Land
209.1
200
-75
564841.1
5927978.0
415.4
NQ
CV13
CV23-218
DD
Land
254.1
200
-45
564841.3
5927978.6
415.4
NQ
CV13
CV23-221
DD
Land
218.0
0
-90
564841.4
5927979.0
415.3
NQ
CV13
CV23-224
DD
Land
308.0
200
-45
564748.9
5928008.0
414.1
NQ
CV13
CV23-227
DD
Land
237.5
200
-75
564749.1
5928009.1
414.2
NQ
CV13
CV23-229
DD
Land
254.1
200
-75
564657.3
5928047.4
412.2
NQ
CV13
CV23-233
DD
Land
179.0
200
-75
564561.0
5928082.7
411.1
NQ
CV13
CV23-235
DD
Land
203.2
200
-45
564560.9
5928082.2
411.0
NQ
CV13
CV23-238
DD
Land
176.2
200
-45
564466.0
5928113.6
409.4
NQ
CV13
CV23-242
DD
Land
161.0
200
-75
564466.5
5928114.2
409.4
NQ
CV13
CV23-245A
DD
Land
142.9
200
-45
564339.9
5928050.1
405.0
NQ
CV13
CV23-249
DD
Land
224.0
160
-45
564934.8
5927940.8
417.2
NQ
CV13
CV23-250
DD
Land
116.0
200
-85
564340.5
5928051.4
405.0
NQ
CV13
CV23-253
DD
Land
161.1
200
-45
564619.1
5927947.5
402.2
NQ
CV13
CV23-255
DD
Land
131.2
80
-45
564936.2
5927944.4
417.7
NQ
CV13
CV23-257
DD
Land
161.0
200
-85
564619.4
5927948.4
402.2
NQ
CV13
CV23-258
DD
Land
296.0
0
-90
564935.3
5927944.3
417.6
NQ
CV13
CV23-263
DD
Land
86.0
200
-45
564434.5
5928018.3
401.2
NQ
CV13
CV23-266
DD
Land
127.9
300
-65
565064.9
5928000.9
429.2
NQ
CV13
CV23-269
DD
Land
83.0
200
-85
564434.9
5928019.4
401.6
NQ
CV13
CV23-270
DD
Land
119.0
200
-45
564527.9
5927979.6
404.0
NQ
CV13
CV23-271
DD
Land
149.2
110
-75
565068.5
5927999.1
429.0
NQ
CV13
CV23-276
DD
Land
182.0
140
-45
565180.4
5928160.3
441.7
NQ
CV13
CV23-277
DD
Land
287.0
200
-85
564528.6
5927980.6
404.1
NQ
CV13
CV23-280
DD
Land
209.0
200
-45
565178.1
5928159.7
441.5
NQ
CV13
CV23-282
DD
Land
184.9
70
-45
565181.4
5928163.8
441.8
NQ
CV13
CV23-286
DD
Land
95.0
200
-45
564804.5
5927873.3
402.3
NQ
CV13
CV23-288
DD
Land
314.0
0
-90
565180.8
5928163.4
441.8
NQ
CV13
CV23-293
DD
Land
133.9
140
-45
565325.0
5928117.9
430.8
NQ
CV13
CV23-294
DD
Land
170.2
200
-85
564804.9
5927874.2
402.3
NQ
CV13
CV23-299
DD
Land
113.1
0
-90
565324.1
5928118.8
430.9
NQ
CV13
CV23-300
DD
Land
146.2
200
-45
564715.7
5927915.2
404.2
NQ
CV13
CV23-301
DD
Land
113.0
140
-45
565359.3
5928206.8
435.5
NQ
CV13
CV23-302
DD
Land
125.0
200
-85
564716.3
5927916.3
404.2
NQ
CV13
CV23-305
DD
Land
149.0
200
-60
564373.9
5928148.8
408.0
NQ
CV13
CV23-306
DD
Land
209.0
140
-90
565358.6
5928207.5
435.6
NQ
CV13
CV23-309
DD
Land
79.9
200
-45
564244.9
5928082.6
404.2
NQ
CV13
CV23-311
DD
Land
421.9
140
-45
565394.5
5928309.7
414.3
NQ
CV13
CV23-312
DD
Land
149.0
200
-90
564373.8
5928148.9
408.1
NQ
CV13
CV23-316
DD
Land
164.0
200
-60
564278.9
5928174.3
406.9
NQ
CV13
CV23-318
DD
Land
98.0
200
-90
564245.2
5928083.3
404.0
NQ
CV13
CV23-319
DD
Land
149.1
200
-45
564147.1
5928113.7
400.9
NQ
CV13
CV23-320
DD
Land
176.1
200
-90
564279.1
5928174.7
406.9
NQ
CV13
CV23-322
DD
Land
404.1
140
-90
565393.9
5928310.4
414.9
NQ
CV13
CV23-323
DD
Land
143.0
200
-60
564180.4
5928212.8
411.6
NQ
CV13
CV23-324
DD
Land
197.2
200
-90
564147.4
5928114.3
400.9
NQ
CV13
CV23-328
DD
Land
432.0
200
-45
564057.2
5928154.3
403.9
NQ
CV13
CV23-330
DD
Land
215.1
200
-90
564180.7
5928213.2
412.1
NQ
CV13
CV23-332
DD
Land
427.9
140
-45
565421.2
5928393.4
405.5
NQ
CV13
CV23-336
DD
Land
149.0
200
-60
564091.2
5928247.1
412.0
NQ
CV13
CV23-339
DD
Land
158.1
200
-90
564091.5
5928247.4
412.4
NQ
CV13
CV23-343
DD
Land
194.2
200
-60
564000.8
5928282.3
408.5
NQ
CV13
CV23-346
DD
Land
164.1
200
-90
564057.4
5928154.8
403.8
NQ
CV13
CV23-348
DD
Land
386.0
140
-90
565420.9
5928393.8
405.3
NQ
CV13
CV23-350
DD
Land
104.0
200
-45
563965.0
5928183.6
406.1
NQ
CV13
CV23-351
DD
Land
164.1
200
-90
564000.9
5928282.6
408.4
NQ
CV13
CV23-353
DD
Land
137.9
200
-90
563965.1
5928184.3
406.1
NQ
CV13
CV23-355
DD
Land
245.0
200
-45
563865.2
5928215.9
401.4
NQ
CV13
CV23-356
DD
Land
180.7
200
-60
563906.9
5928314.1
400.8
NQ
CV13
CV23-358
DD
Land
311.2
140
-45
565552.3
5928455.0
394.9
NQ
CV13
CV23-360
DD
Land
140.0
200
-90
563865.5
5928216.7
401.4
NQ
CV13
CV23-361
DD
Land
208.8
200
-90
563907.1
5928314.9
400.7
NQ
CV13
CV23-365
DD
Land
322.9
140
-90
565551.9
5928455.4
394.9
NQ
CV13
CV24-396
DD
Land
357.1
140
-65
565052.7
5928112.1
434.0
NQ
CV13
CV24-397
DD
Land
428.0
140
-45
565424.4
5928248.6
421.7
NQ
CV13
CV24-406
DD
Land
128.0
70
-55
565054.1
5928112.6
434.1
NQ
CV13
CV24-411
DD
Land
356.1
310
-70
565055.0
5928114.7
434.1
NQ
CV13
CV24-412
DD
Land
348.4
140
-90
565423.8
5928249.4
421.5
NQ
CV13
CV24-417
DD
Land
196.9
20
-45
565058.0
5928116.1
434.3
NQ
CV13
CV24-420
DD
Land
305.0
200
-60
564988.6
5928082.2
429.5
NQ
CV13
CV24-421
DD
Land
475.9
140
-45
565433.9
5928165.4
416.5
NQ
CV13
CV24-425
DD
Land
209.0
200
-90
564988.8
5928082.7
429.4
NQ
CV13
CV24-427
DD
Land
331.6
200
-60
564895.7
5928116.7
426.4
NQ
CV13
CV24-429
DD
Land
515.2
140
-65
565433.8
5928165.9
416.3
NQ
CV13
CV24-432
DD
Land
278.0
200
-90
564895.9
5928117.1
426.3
NQ
CV13
CV24-436
DD
Land
220.9
200
-60
564799.1
5928146.2
422.6
NQ
CV13
CV24-439
DD
Land
326.5
140
-45
565515.1
5928210.6
412.7
NQ
CV13
CV24-444
DD
Land
248.0
200
-90
564799.0
5928146.2
422.6
NQ
CV13
CV24-446
DD
Land
286.6
140
-90
565514.5
5928211.3
412.6
NQ
CV13
CV24-453
DD
Land
160.9
140
-45
565199.0
5927986.7
422.8
NQ
CV13
CV24-454
DD
Land
209.0
200
-60
564708.5
5928185.6
421.7
NQ
CV13
CV24-457
DD
Land
143.0
140
-45
565145.6
5927920.0
407.6
NQ
CV13
CV24-461
DD
Land
345.7
140
-45
565434.8
5928491.5
394.0
NQ
CV13
CV24-464
DD
Land
262.9
200
-90
564708.7
5928186.2
421.6
NQ
CV13
CV24-470
DD
Land
281.3
320
-80
565430.9
5928494.3
393.9
NQ
CV13
CV24-471
DD
Land
212.1
200
-60
564613.7
5928220.3
420.4
NQ
CV13
CV24-477
DD
Land
332.1
140
-45
565529.8
5928379.0
399.3
NQ
CV13
CV24-478
DD
Land
248.0
200
-90
564613.9
5928220.6
420.3
NQ
CV13
CV24-483
DD
Land
185.0
200
-60
564518.5
5928253.3
414.9
NQ
CV13
CV24-484
DD
Land
263.2
140
-45
565645.4
5928423.4
392.3
NQ
CV13
CV24-487
DD
Land
308.1
140
-45
565807.6
5928565.2
378.9
NQ
CV13
CV24-491
DD
Land
248.0
200
-90
564518.7
5928253.8
415.0
NQ
CV13
CV24-492
DD
Land
290.4
140
-45
565697.4
5928512.1
385.7
NQ
CV13
CV24-497
DD
Land
230.0
200
-60
564427.0
5928280.4
409.6
NQ
CV13
CV24-498
DD
Land
218.0
140
-45
565467.1
5928559.6
387.9
NQ
CV13
CV24-499
DD
Land
176.2
320
-55
565803.9
5928569.8
379.0
NQ
CV13
CV24-506
DD
Land
218.2
200
-90
564427.3
5928280.9
409.6
NQ
CV13
CV24-507
DD
Land
187.0
0
-90
565466.6
5928560.1
387.7
NQ
CV13
CV24-508
DD
Land
152.0
140
-45
565710.4
5928599.6
382.2
NQ
CV13
CV24-510
DD
Land
239.0
270
-55
565458.5
5928561.1
387.8
NQ
CV13
CV24-511
DD
Land
200.0
200
-60
564329.6
5928311.9
413.2
NQ
CV13
CV24-513
DD
Land
171.2
320
-75
565707.2
5928604.4
381.9
NQ
CV13
CV24-518
DD
Land
199.9
200
-90
564329.8
5928312.3
413.2
NQ
CV13
CV24-519
DD
Land
248.0
140
-45
565599.7
5928537.4
385.4
NQ
CV13
CV24-520
DD
Land
243.7
320
-60
565459.7
5928564.3
387.4
NQ
CV13
CV24-523
DD
Land
203.2
200
-60
564237.2
5928354.7
414.2
NQ
CV13
CV24-524
DD
Land
209.0
20
-60
565464.9
5928560.5
387.7
NQ
CV13
CV24-525
DD
Land
161.0
320
-75
565596.8
5928540.8
385.1
NQ
CV13
CH22-008
CH
Land
3.04
134
-10
565327.4
5927991.9
412.9
n/a
CV13
CH22-009
CH
Land
3.46
314
-20
565327.4
5927991.9
412.9
n/a
CV13
CH22-010
CH
Land
5.24
341
-20
565319.8
5927982.1
412.8
n/a
CV13
CH22-011
CH
Land
1.49
164
-7
565290.2
5927974.0
411.6
n/a
CV13
CH22-012
CH
Land
5.31
344
-18
565290.2
5927974.0
411.6
n/a
CV13
CH22-013
CH
Land
2.47
168
-13
565276.5
5927969.0
409.5
n/a
CV13
CH22-014
CH
Land
2.77
348
-10
565276.5
5927969.0
409.5
n/a
CV13
CH22-015
CH
Land
1.3
151
-20
565261.4
5927948.5
406.3
n/a
CV13
CH22-016
CH
Land
0.8
331
-5
565261.4
5927948.5
406.3
n/a
CV13
CH22-017
CH
Land
13.1
161
-15
565008.4
5927781.9
396.5
n/a
CV13
CH22-018
CH
Land
1.63
7
-5
564999.3
5927781.8
397.9
n/a
CV13
CH22-019
CH
Land
8.87
187
-10
564999.3
5927781.8
397.9
n/a
CV13
CH22-020
CH
Land
3.49
1
-10
564958.2
5927787.0
398.7
n/a
CV13
CH22-021
CH
Land
3.57
181
-10
564958.2
5927787.0
398.7
n/a
CV13
CH22-022
CH
Land
8.42
14
-15
564933.1
5927793.5
397.7
n/a
CV13
CH22-023
CH
Land
2.96
356
-30
564859.2
5927784.0
392.7
n/a
CV13
CH22-024
CH
Land
5.81
176
-10
564859.2
5927784.0
392.7
n/a
CV13
CH22-025
CH
Land
4.93
185
-20
563820.5
5928027.6
401.3
n/a
CV13
CH22-026
CH
Land
9.22
15
-20
563820.5
5928027.6
401.3
n/a
CV13
CH22-027
CH
Land
3.5
2
-10
564543.7
5927827.8
394.5
n/a
CV13
CH22-028
CH
Land
1.63
182
-25
564543.7
5927827.8
394.5
n/a
CV13
CH22-029
CH
Land
3.77
344
-8
564430.7
5927891.8
400.2
n/a
CV13
CH22-030
CH
Land
1.09
164
-25
564430.7
5927891.8
400.2
n/a
CV13
CH22-031
CH
Land
3.14
340
-20
564313.4
5927935.4
402.1
n/a
CV13
CH22-032
CH
Land
1.2
160
-5
564313.4
5927935.4
402.1
n/a
CV13
CH22-033
CH
Land
1.73
349
-15
564317.7
5927922.5
403.6
n/a
CV13
CH22-034
CH
Land
1.46
169
-25
564317.7
5927922.5
403.6
n/a
CV13
CH22-035
CH
Land
1.62
166
-10
564318.2
5927920.4
403.4
n/a
CV13
CH22-036
CH
Land
9.27
340
-10
564229.2
5927961.3
403.6
n/a
CV13
CH22-037
CH
Land
4.82
160
-5
564229.2
5927961.3
403.6
n/a
CV13
CH23-058
CH
Land
6.73
200
-20
564428.8
5927877.0
397.6
n/a
CV13
CH23-059
CH
Land
16.7
185
-25
564395.4
5927899.8
401.0
n/a
CV13
CH23-060
CH
Land
5.11
200
-10
564381.8
5927886.9
398.6
n/a
CV13
CH23-061
CH
Land
13.41
200
-15
564356.1
5927920.0
402.7
n/a
CV13
CH23-062
CH
Land
14.86
180
-15
565813.8
5928472.6
379.6
n/a
CV13
CH23-063
CH
Land
8.47
180
-21
565793.4
5928462.2
380.7
n/a
CV13
CH23-064
CH
Land
13.9
160
-15
565774.8
5928454.4
382.6
n/a
CV13
CH23-065
CH
Land
27.92
180
-15
565757.6
5928430.0
384.6
n/a
CV13
CH23-066
CH
Land
11.93
180
-10
565743.4
5928420.7
386.2
n/a
CV13
CH23-067
CH
Land
4.52
180
-15
565668.3
5928403.0
390.8
n/a
CV13
CH23-068
CH
Land
6.21
148
-18
565459.7
5928331.7
404.0
n/a
CV13
CH23-069
CH
Land
6.77
26
-36
565393.2
5928283.7
418.1
n/a
CV13
CH23-070
CH
Land
3.66
5
-5
565414.5
5928118.5
414.7
n/a
CV13
CH23-071
CH
Land
6.43
160
-25
565358.5
5928074.7
415.8
n/a
CV13
CH24-072
CH
Land
1.71
2
-5
563770.0
5928053.0
394.0
n/a
CV13
CH24-073
CH
Land
6.32
5
-2
563798.0
5928046.0
394.0
n/a
CV13
CH24-074
CH
Land
5.92
192
0
563809.0
5928065.0
398.0
n/a
CV13
CH24-075
CH
Land
9.14
193
0
563872.0
5928036.0
390.0
n/a
CV13
CH24-076
CH
Land
14.98
194
-5
563868.0
5928029.0
397.0
n/a
CV13
CH24-077
CH
Land
1.82
206
-40
563952.0
5928001.0
385.0
n/a
CV13
CH24-078
CH
Land
5.62
183
-19
564022.0
5927996.0
384.0
n/a
CV13
CH24-079
CH
Land
10.98
194
-5
564098.0
5927988.0
401.0
n/a
CV13
CH24-080
CH
Land
8.9
189
0
564206.0
5927971.0
397.0
n/a
CV13
CH24-081
CH
Land
6.4
208
-2
564245.0
5927965.0
396.0
n/a
CV13
(1) Coordinate system NAD83 / UTM zone 18N; (2) DD = diamond drill, CH = channel; (3) DD azimuths and dips presented are those 'planned' and may vary off collar/downhole.
Appendix 1 – JORC Code 2012 Table 1 (ASX Listing Rule 5.8.2)
Section 1 – Sampling Techniques and Data
Criteria
JORC Code explanation
Commentary
Sampling techniques
Nature and quality of sampling (eg cut channels, random chips, or specific specialized industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. Aspects of the determination of mineralization that are Material to the Public Report. In cases where ‘industry standard’ work has been done this would be relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverized to produce a 30 g charge for fire assay’). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralization types (eg submarine nodules) may warrant disclosure of detailed information. Core sampling protocols meet industry standard practices. Core sampling is guided by lithology as determined during geological logging (i.e., by a geologist). All pegmatite intervals are sampled in their entirety (half-core), regardless if spodumene mineralization is noted or not (in order to ensure an unbiased sampling approach) in addition to ~1 to 3 m of sampling into the adjacent host rock (dependent on pegmatite interval length) to “bookend” the sampled pegmatite. The minimum individual core sample length is typically 0.3 to 0.5 m and the maximum sample length is typically 2.0 m. Targeted individual pegmatite sample lengths are 1.0 to 1.5 m. All drill core is oriented to maximum foliation prior to logging and sampling and is cut with a core saw into half-core pieces, with one half-core collected for assay, and the other half-core remaining in the box for reference. Core samples collected from 2021 drill holes were shipped to Activation Laboratories in Ancaster, ON, for standard sample preparation (code RX1) which included crushing to 80% passing 10 mesh, followed by a 250 g riffle split and pulverizing to 95% passing 105 microns. All 2021 core sample pulps were analyzed, at the same lab, for multi-element (including lithium) by four-acid digestion with ICP-OES finish (package 1F2) and tantalum by INAA (code 5B), with any samples returning >8,000 ppm Li by 1F2 reanalyzed for Li by code 8-4 Acid ICP Assay. Core samples collected from 2022 and 2023 drill holes CV22-015 through CV23-107 were shipped to SGS Canada’s laboratory in either Lakefield, ON (vast majority), Sudbury, ON (CV22-028, 029, 030), or Burnaby, BC (CV22-031, 032, 033, and 034), for standard sample preparation (code PRP89) which included drying at 105°C, crush to 75% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns. Core samples collected from 2023 drill holes CV23-108 through 365 were shipped to SGS Canada’s laboratory in Val-d’Or, QC, for standard sample preparation (code PRP89). Core samples collected from 2024 drill holes were shipped to SGS Canada’s laboratory in Val-d’Or, QC, or Radisson, QC, for sample preparation (code PRP90 special) which included drying at 105°C, crush to 90% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns. All drill core sample pulps from 2022, 2023, and 2024 were shipped by air to SGS Canada’s laboratory in Burnaby, BC, where the samples were homogenized and subsequently analyzed for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish (codes GE_ICP91A50 and GE_IMS91A50). Channel sampling followed best industry practices with a 3 to 5 cm wide, saw-cut channel completed across the pegmatite outcrop as practical, perpendicular to the interpreted pegmatite strike. Samples were collected at ~1 m contiguous intervals with the channel bearing noted, and GPS coordinate collected at the start and end points of the channel. All channel samples collected were shipped to SGS Canada’s laboratory in Lakefield, ON, or Val-d’Or, QC, for standard preparation. Pulps were analyzed at SGS Canada’s laboratory in either Lakefield, ON, (2017), or Burnaby, BC (2022, 2023, and 2024), for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish.Drilling techniques
Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc). NQ or HQ size core diamond drilling was completed for all holes. Core was not oriented. However, downhole OTV-ATV surveys were completed to various depths multiple holes to assess overall structure. The quality of the channel sampling allowed the channels to be treated as horizontal drill holes for the purposes of modelling and resource estimation.Drill sample recovery
Method of recording and assessing core and chip sample recoveries and results assessed. Measures taken to maximize sample recovery and ensure representative nature of the samples. Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. All drill core was geotechnically logged following industry standard practices, and include TCR, RQD, ISRM, and Q-Method (since mid-winter 2023). Core recovery is very good and typically exceeds 90%. Channel samples were not geotechnically logged. Channel recovery was effectively 100%.Logging
Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. The total length and percentage of the relevant intersections logged. Upon receipt at the core shack, all drill core is pieced together, oriented to maximum foliation, metre marked, geotechnically logged (including structure), alteration logged, geologically logged, and sample logged on an individual sample basis. Core box photos are also collected of all core drilled, regardless of perceived mineralization. Specific gravity measurements of pegmatite are also collected at systematic intervals for all pegmatite drill core using the water immersion method, as well as select host rock drill core. Channel samples were geologically logged upon collection on an individual sample basis. The logging is qualitative by nature, and includes estimates of spodumene grain size, inclusions, and model mineral estimates. These logging practices meet or exceed current industry standard practices.Sub-sampling techniques and sample preparation
If core, whether cut or sawn and whether quarter, half or all core taken. If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. For all sample types, the nature, quality and appropriateness of the sample preparation technique. Quality control procedures adopted for all sub-sampling stages to maximize representivity of samples. Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling. Whether sample sizes are appropriate to the grain size of the material being sampled. Drill core sampling follows industry best practices. Drill core was saw-cut with half-core sent for geochemical analysis and half-core remaining in the box for reference. The same side of the core was sampled to maintain representativeness. Channels were saw-cut with the full channel being sent for analysis at ~1 m sample intervals. Sample sizes are considered appropriate for the material being assayed. A Quality Assurance / Quality Control (QAQC) protocol following industry best practices was incorporated into the drill programs and included systematic insertion of quartz blanks and certified reference materials into sample batches, as well as collection of quarter-core duplicates (through hole CV23-190 only), at a rate of approximately 5% each. Additionally, analysis of pulp-split and coarse-split (through hole CV23-365 only) sample duplicates were completed to assess analytical precision at different stages of the laboratory preparation process, and external (secondary) laboratory pulp-split duplicates were prepared at the primary lab for subsequent check analysis and validation at a secondary lab (SGS Canada in 2021, and ALS Canada in 2022, 2023, and 2024). All protocols employed are considered appropriate for the sample type and nature of mineralization and are considered the optimal approach for maintaining representativeness in sampling.Quality of assay data and laboratory tests
The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established. Core samples collected from 2021 drill holes were shipped to Activation Laboratories in Ancaster, ON, for standard sample preparation (code RX1) which included crushing to 80% passing 10 mesh, followed by a 250 g riffle split and pulverizing to 95% passing 105 microns. All 2021 core sample pulps were analyzed, at the same lab, for multi-element (including lithium) by four-acid digestion with ICP-OES finish (package 1F2) and tantalum by INAA (code 5B), with any samples returning >8,000 ppm Li by 1F2 reanalyzed for Li by code 8-4 Acid ICP Assay. Core samples collected from 2022 and 2023 drill holes CV22-015 through CV23-107 were shipped to SGS Canada’s laboratory in either Lakefield, ON (vast majority), Sudbury, ON (CV22-028, 029, 030), or Burnaby, BC (CV22-031, 032, 033, and 034), for standard sample preparation (code PRP89) which included drying at 105°C, crush to 75% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns. Core samples collected from 2023 drill holes CV23-108 through 365 were shipped to SGS Canada’s laboratory in Val-d’Or, QC, for standard sample preparation (code PRP89). Core samples collected from 2024 drill holes were shipped to SGS Canada’s laboratory in Val-d’Or, QC, or Radisson, QC, for sample preparation (code PRP90 special) which included drying at 105°C, crush to 90% passing 2 mm, riffle split 250 g, and pulverize 85% passing 75 microns. All drill core sample pulps from 2022, 2023, and 2024 were shipped by air to SGS Canada’s laboratory in Burnaby, BC, where the samples were homogenized and subsequently analyzed for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish (codes GE_ICP91A50 and GE_IMS91A50). All channel samples collected were shipped to SGS Canada’s laboratory in Lakefield, ON, or Val-d’Or, QC, for standard preparation. Pulps were analyzed at SGS Canada’s laboratory in either Lakefield, ON, (2017), or Burnaby, BC (2022, 2023, and 2024), for multi-element (including Li and Ta) using sodium peroxide fusion with ICP-AES/MS finish. The Company relies on both its internal QAQC protocols (systematic use of blanks, certified reference materials, and external checks), as well as the laboratory’s internal QAQC. All protocols employed are considered appropriate for the sample type and nature of mineralization and are considered the optimal approach for maintaining representativeness in sampling.Verification of sampling and assaying
The verification of significant intersections by either independent or alternative company personnel. The use of twinned holes. Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. Discuss any adjustment to assay data. Intervals are reviewed and compiled by the VP Exploration and Project Managers prior to disclosure, including a review of the Company’s internal QAQC sample analytical data. No twinned holes were completed, apart from several holes being recollared with a different core size or due to premature loss of a hole due to conditions. Data capture utilizes MX Deposit software whereby core logging data is entered directly into the software for storage, including direct import of laboratory analytical certificates as they are received. The Company employs various on-site and post QAQC protocols to ensure data integrity and accuracy. Adjustments to data include reporting lithium and tantalum in their oxide forms, as it is reported in elemental form in the assay certificates. Formulas used are Li2O = Li x 2.153, and Ta2O5 = Ta x 1.221.Location of data points
Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. Specification of the grid system used. Quality and adequacy of topographic control. Each drill hole collar and channel end points have been surveyed with a RTK Topcon GR-5 or RTK Trimble Zephyr 3, except for a minor number of channels. The coordinate system used is UTM NAD83 Zone 18. The Company completed a property-wide LiDAR and orthophoto survey in August 2022, which provides high-quality topographic control. The quality and accuracy of the topographic controls are considered adequate for advanced stage exploration and development, including Mineral Resource estimation.Data spacing and distribution
Data spacing for reporting of Exploration Results. Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. Whether sample compositing has been applied. At CV5, drill hole collar spacing is dominantly grid based. Several collars are typically completed from the same pad at varied orientations targeting pegmatite pierce points of ~50 to 100 m spacing. At CV13, drill hole spacing is a combination of grid based (at ~100 spacing) and fan based with multiple holes collared from the same pad. Therefore, collar locations and hole orientations may vary widely, which reflect the varied orientation of the pegmatite body along strike. Based on the nature of the mineralization and continuity in geological modelling, the drill hole spacing is sufficient to support a Mineral Resource Estimate. Core sample lengths typically range from 0.5 to 2.0 m and average ~1.0 to 1.5 m. Sampling is continuous within all pegmatite encountered in the drill hole. Core samples are not composited upon collection or for analysis.Orientation of data in relation to geological structure
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. If the relationship between the drilling orientation and the orientation of key mineralized structures is considered to have introduced a sampling bias, this should be assessed and reported if material. No sampling bias is anticipated based on structure within the mineralized body. The principal mineralized bodies are relatively undeformed and very competent, although have some meaningful structural control. At CV5, the principal mineralized body and adjacent lenses are steeply dipping resulting in oblique angles of intersection with true widths varying based on drill hole angle and orientation of pegmatite at that particular intersection point. i.e., the dip of the mineralized pegmatite body has variations in a vertical sense and along strike, so the true widths are not always apparent until several holes have been drilled (at the appropriate spacing) in any particular drill-fence. At CV13, the principal pegmatite body has a shallow varied strike and northerly dip.Sample security
The measures taken to ensure sample security. Samples were collected by Company staff or its consultants following project specific protocols governing sample collection and handling. Core samples were bagged, placed in large supersacs for added security, palleted, and shipped by third party transport, or directly by representatives of the Company, to the designated sample preparation laboratory (Ancaster, ON, in 2021, Sudbury, ON, Burnaby, BC, and Lakefield, ON, in 2022, Lakefield, ON, in 2023, Val-d’Or, QC, in 2023 and 2024, and Radisson in 2024) being tracked during shipment along with chain of custody documents. Upon arrival at the laboratory, the samples were cross-referenced with the shipping manifest to confirm all samples were accounted for. At the laboratory, sample bags were evaluated for tampering. On several occasions in 2022, SGS Canada shipped samples to a different SGS Canada facility for preparation than was intended by the Company (Sudbury, ON, and Burnaby, BC, in 2022).Audits or reviews
The results of any audits or reviews of sampling techniques and data. A review of the sample procedures for the Company’s 2021 fall drill program (CF21-001 to 004) and 2022 winter drill program (CV22-015 to 034) was completed by an Independent Competent Person and deemed adequate and acceptable to industry best practices (discussed in a technical report titled “NI 43-101 Technical Report on the Corvette Property, Quebec, Canada”, by Alex Knox, M.Sc., P.Geol., Issue Date of June 27th, 2022.) A review of the sample procedures through the Company’s 2023 winter drill program (through CV23-190) was completed by an independent Competent Person with respect to the CV5 Pegmatite’s maiden Mineral Resource Estimate and deemed adequate and acceptable to industry best practices (discussed in a technical report titled " NI 43‑101 Technical Report, Mineral Resource Estimate for the CV5 Pegmatite, Corvette Property" by Todd McCracken, P.Geo., of BBA Engineering Ltd., and Ryan Cunningham, M.Eng., P.Eng., of Primero Group Americas Inc., Effective Date of June 25, 2023, and Issue Date of September 8, 2023. Additionally, the Company continually reviews and evaluates its procedures in order to optimize and ensure compliance at all levels of sample data collection and handling.
Section 2 – Reporting of Exploration Results
Criteria
JORC Code explanation
Commentary
Mineral tenement and land tenure status
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. The Shaakichiuwaanaan Property is comprised of 463 CDC claims located in the James Bay Region of Quebec. All claims are registered 100% in the name of Lithium Innova Inc., a wholly owned subsidiary of Patriot Battery Metals Inc. The northern border of the Property’s primary claim grouping is located within approximately 6 km to the south of the Trans-Taiga Road and powerline infrastructure corridor. The CV5 Spodumene Pegmatite is situated approximately 13.5 km south of the regional and all‑weather Trans-Taiga Road and powerline infrastructure corridor, and is accessible year-round by an all-season road. The CV13 Spodumene Pegmatite is located approximately 3 km west-southwest of CV5. The Company holds 100% interest in the Property subject to various royalty obligations depending on original acquisition agreements. DG Resources Management holds a 2% NSR (no buyback) on 76 claims, D.B.A. Canadian Mining House holds a 2% NSR on 50 claims (half buyback for $2M), Osisko Gold Royalties holds a sliding scale NSR of 1.5-3.5% on precious metals, and 2% on all other products, over 111 claims, and Azimut Exploration holds a 2% NSR on 39 claims. The Property does not overlap any atypically sensitive environmental areas or parks, or historical sites to the knowledge of the Company. There are no known hinderances to operating at the Property, apart from the goose harvesting season (typically mid-April to mid-May) where the communities request helicopter flying not be completed, and potentially wildfires depending on the season, scale, and location. Claim expiry dates range from February 2025 to November 2026.Exploration done by other parties
Acknowledgment and appraisal of exploration by other parties. No core assay results from other parties are disclosed herein. The most recent independent Property review was a technical report titled “NI 43-101 Technical Report, Mineral Resource Estimate for the CV5 Pegmatite, Corvette Property, James Bay Region, Québec, Canada”, by Todd McCracken, P.Geo., of BBA Engineering Ltd., and Ryan Cunningham, M.Eng., P.Eng., of Primero Group Americas Inc., Effective Date of June 25, 2023, and Issue Date of September 8, 2023.Geology
Deposit type, geological setting and style of mineralization. The Property overlies a large portion of the Lac Guyer Greenstone Belt, considered part of the larger La Grande River Greenstone Belt, and is dominated by volcanic rocks metamorphosed to amphibolite facies. Rocks of the Guyer Group (amphibolite, iron formation, intermediate to mafic volcanics, peridotite, pyroxenite, komatiite, as well as felsic volcanics) predominantly underly the Property. The amphibolite rocks that trend east-west (generally steeply south dipping) through this region are bordered to the north by the Magin Formation (conglomerate and wacke) and to the south by an assemblage of tonalite, granodiorite, and diorite, in addition to metasediments of the Marbot Group (conglomerate, wacke) in the areas proximal to the CV5 Spodumene Pegmatite. Several regional-scale Proterozoic gabbroic dykes also cut through portions of the Property (Lac Spirt Dykes, Senneterre Dykes). The lithium pegmatites on the Property are hosted predominantly within amphibolite’s, metasediments, and to a lesser extent ultramafic rocks. The geological setting is prospective for gold, silver, base metals, platinum group elements, and lithium over several different deposit styles including orogenic gold (Au), volcanogenic massive sulfide (Cu, Au, Ag), komatiite-ultramafic (Au, Ag, PGE, Ni, Cu, Co), and pegmatite (Li, Ta). Exploration of the Property has outlined three primary mineral exploration trends crossing dominantly east-west over large portions of the Property – Golden Trend (gold), Maven Trend (copper, gold, silver), and CV Trend (lithium, tantalum). The CV5 and CV13 spodumene pegmatites are situated within the CV Trend. Lithium mineralization at the Property, including at CV5 and CV13 is observed to occur within quartz-feldspar pegmatite, which may be exposed at surface as high relief ‘whale-back’ landforms. The pegmatite is often very coarse-grained and off-white in appearance, with darker sections commonly composed of mica and smoky quartz, and occasional tourmaline. The lithium pegmatites at Property are categorized as LCT Pegmatites. Core assays and ongoing mineralogical studies, coupled with field mineral identification and assays, indicate spodumene as the dominant lithium-bearing mineral on the Property, with no significant petalite, lepidolite, lithium-phosphate minerals, or apatite present. The pegmatites also carry significant tantalum values with tantalite indicated to be the mineral phase.Drill hole Information
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: easting and northing of the drill hole collar elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar dip and azimuth of the hole down hole length and interception depth hole length. If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. Drill hole attribute information is included in a table herein. Pegmatite intersections of 2 m are not typically presented as they are considered insignificant.Data aggregation methods
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (eg cutting of high grades) and cut-off grades are usually Material and should be stated. Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. The assumptions used for any reporting of metal equivalent values should be clearly stated. Length weighted averages were used to calculate grade over width. No specific grade cap or cut-off was used during grade width calculations. The lithium and tantalum length weighted average grade of the entire pegmatite interval is calculated for all pegmatite intervals over 2 m core length, as well as higher grade zones at the discretion of the geologist. Pegmatites have inconsistent mineralization by nature, resulting in some intervals having a small number of poorly mineralized samples included in the calculation. Non-pegmatite internal dilution is limited to typically 3 m where relevant and intervals indicated when assays are reported. No metal equivalents have been reported.Relationship between mineralization widths and intercept lengths
These relationships are particularly important in the reporting of Exploration Results. If the geometry of the mineralization with respect to the drill hole angle is known, its nature should be reported. If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (eg ‘down hole length, true width not known’). At CV5, geological modelling is ongoing on a hole-by-hole basis and as assays are received. However, current interpretation supports a principal, large pegmatite body of near vertical to steeply dipping orientation, flanked by several subordinate pegmatite lenses (collectively, the ‘CV5 Spodumene Pegmatite’). At CV13, geological modelling is ongoing on a hole-by-hole basis and as assays are received. However, current interpretation supports a series of flat-lying to moderately dipping (northerly), sub-parallel trending spodumene pegmatite bodies, of which three appear to dominate (collectively, the ‘CV13 Spodumene Pegmatite’). All reported widths are core length. True widths are not calculated for each hole due to the relatively wide drill spacing at this stage of delineation and the typical irregular nature of pegmatite, as well as the varied drill hole orientations. As such, true widths may vary widely from hole to hole.Diagrams
Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. Please refer to the figures included herein as well as those posted on the Company’s website.Balanced reporting
Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. Please refer to the table(s) included herein as well as those posted on the Company’s website. Results for pegmatite intervals 2 m are not reported as they are considered insignificant.Other substantive exploration data
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. The Company is currently completing site environmental work over the CV5 and CV13 pegmatite area. No endangered flora or fauna have been documented over the Property to date, and several sites have been identified as potentially suitable for mine infrastructure. The Company has completed a bathymetric survey over the shallow glacial lake which overlies a portion of the CV5 Spodumene Pegmatite. The lake depth ranges from 2 m to approximately 18 m, although the majority of the CV5 Spodumene Pegmatite, as delineated to date, is overlain by typically 2 to 10 m of water. The Company has completed preliminary metallurgical testing comprised of HLS and magnetic testing, which has produced 6+% Li2O spodumene concentrates at >70% recovery on both CV5 and CV13 pegmatite material, indicating DMS as a viable primary process approach, and that both CV5 and CV13 could potentially feed the same process plant. A DMS test on CV5 Spodumene Pegmatite material returned a spodumene concentrate grading 5.8% Li2O at 79% recovery, strongly indicating potential for a DMS only operation to be applicable. Various mandates required for advancing the Project towards economic studies have been initiated, including but not limited to, environmental baseline, metallurgy, geomechanics, hydrogeology, hydrology, stakeholder engagement, geochemical characterization, as well as transportation and logistical studies.Further work
The nature and scale of planned further work (eg tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. The Company intends to continue drilling the pegmatites of the Property, focused on completion of the infill drill program at the CV5 Pegmatite as well as testing for extensions along strike, up dip, and down dip where mineralization remains open. The Company also anticipates further drilling at the CV13 Pegmatite and the CV9 Pegmatite.
Section 3 – Estimate and Reporting of Mineral Resources
Criteria
JORC Code explanation
Commentary
Database integrity
Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes. Data validation procedures used. Data capture utilizes MX Deposit database software whereby core logging data is entered directly into the software for storage, including direct import of laboratory analytical certificates as they are received. Collar and downhole deviation surveys are also validated and stored in MX Deposit database software. The Company employs various on-site and post initial QAQC protocols to ensure data integrity and accuracy. Drill hole collar points were validated against LiDAR topographic data. The drill hole database was further validated by the independent Competent Person for the Mineral Resource Estimate, including missing sample intervals, overlapping intervals, and various missing data (survey, collar coordinates, assays, rock type, etc.) All the analytical certificates since the 2023 MRE were validate against the assays present in the database for Li and Ta. No significant errors in the database were discovered. The database is considered validated and of high quality, and therefore sufficient to support the Mineral Resource Estimate.Site visits
Comment on any site visits undertaken by the Competent Person and the outcome of those visits. If no site visits have been undertaken indicate why this is the case. Todd McCracken (Competent Person) of BBA Engineering Ltd., completed site visits to the Property from April 7 to 11, 2023, and June 4 to 7, 2024. Core from various drill holes from CV5 and CV13 from the 2023 and 2024 drill program was viewed and core processing protocols reviewed with site geologists. Drilling was active during the 2023 site visit. Several of the CV5 and CV13 pegmatite outcrops were visited, and various collar locations were visited and GPS coordinates checked against the database. Pulp samples were collected for check analysis from holes selected by the Competent Person. No significant issues were found with the protocols practiced on site. The Competent Person considers the QAQC and procedures adopted by the Company to be of a high standard.
Geological interpretation
Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit. Nature of the data used and of any assumptions made. The effect, if any, of alternative interpretations on Mineral Resource estimation. The use of geology in guiding and controlling Mineral Resource estimation. The factors affecting continuity both of grade and geology. The CV5 and CV13 geological models were built in Leapfrog Geo using MX Deposit database, through an iterative and interpretive process by Project Geologists and VP Exploration, and validated by the Competent Person. The CV5 Pegmatite was geologically modelled as an intrusive for the principal pegmatite body (1), and as a vein for adjacent lenses (8). The CV13 Pegmatite was geological modelled as veins for all of its lenses. A combination of implicit and explicit modelling methods was used, defined by geologically logged drill intersections, channel samples, and outcrop mapping, with external geological controls, including measured contact orientations, cross-sectional polylines, and surface polyline controls to ensure the model follows geological interpretation, validation, and reasonable extensions along trend and dip. The CV5 geological model’s principal pegmatite was further geochemically domain modelled using rock types and assays. The geological interpretation of both the CV5 and CV13 geological models are robust. Alternative interpretations are unlikely to materially alter the Mineral Resource Estimate. Drilling density is the primary factor in assessing the interpreted continuity of both grade and geology. The current drill density is sufficient to support the Mineral Resource Estimate. The controlling factors on mineralization are not fully understood but meaningful structural control is interpreted.Dimensions
The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource. The CV5 portion of the Shaakichiuwaanaan Mineral Resource Estimate includes multiple individual spodumene pegmatite dykes that have been modelled. However, approximately two-thirds of the overall Shaakichiuwaanaan Mineral Resource, and vast majority of the CV5 Mineral Resource component, is hosted within a single, large, principal pegmatite dyke, which is flanked on both sides by multiple, subordinate, sub-parallel trending dykes. The principal dyke at CV5 is geologically modelled to extend continuously over a lateral distance of at least 4.6 km and remains open along strike at both ends and to depth along a large portion of its length. The width of the currently known mineralized corridor at CV5 is approximately 500 m, with spodumene pegmatite intersected as deep as 450 m vertical depth from surface. The pegmatite dykes at CV5 trend south-southwest (approximately 250°/070° RHR), and therefore dip northerly, which is opposite to the host amphibolites, metasediments, and ultramafics which steeply dip southerly. The principal dyke ranges from 10 m to >125 m in true width, and may pinch and swell aggressively along strike, as well as up and down dip. It is primarily the thickest at near-surface to moderate depths (225 m), forming a relatively bulbous, elongated shape, which may flair to surface and to depth variably along its length. The CV13 portion of the Shaakichiuwaanaan Mineral Resource Estimate includes multiple individual spodumene pegmatite dykes that have been modelled, with three appearing to be dominant. The pegmatite bodies are coincident with the apex of a regional structural flexure where the west arm trends ~290° and the east arm at ~230°. Drilling to date indicates the east arm includes significantly more pegmatite stacking compared to the west, and also carries a significant amount of the overall CV13 Pegmatite tonnage and grade, highlighted by the high-grade Vega Zone.Estimation and modelling techniques
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used. The availability of check estimates, previous estimates and/or mine production records and whether the Mineral Resource estimate takes appropriate account of such data. The assumptions made regarding recovery of by-products. Estimation of deleterious elements or other non-grade variables of economic significance (eg sulphur for acid mine drainage characterisation). In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed. Any assumptions behind modelling of selective mining units. Any assumptions about correlation between variables. Description of how the geological interpretation was used to control the resource estimates. Discussion of basis for using or not using grade cutting or capping. The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available. Compositing was done every 1.0 m. Unsampled intervals were assigned a grade of 0.0005% Li and 0.25 ppm Ta. Capping was done after compositing. Based on the statistical analysis capping varies by lithological domain. On CV5, the spodumene-rich domain within the CV5 principal pegmatite, no capping was required for Li2O but Ta2O5 was capped at 3,000 ppm. For the feldspar-rich domain within the CV5 principal pegmatite, a capping of 3.5% Li2O and 1,500 ppm Ta2O5 was applied. For the parallel dykes a capping of 5% Li2O and 1,200 ppm Ta2O5 was applied. For CV13 zones, it was determined that no capping was required for Li2O, but Ta2O5 was capped at 1,500 ppm. Variography was done both in Leapfrog Edge and Supervisor. For Li2O, a well-structured variogram model was obtained for the CV5 principal pegmatite’s spodumene-rich domain. For the CV5 principal pegmatite, both domains (spodumene-rich and feldspar-rich domains) were estimated using ordinary kriging (OK), using Leapfrog Edge. For Ta2O5, the spodumene-rich domain and the feldspar-rich domain within CV5 principal pegmatite did not yield well-structured variograms. Therefore, Ta2O5 was estimated using Inverse Distance Squared (ID2). The remaining pegmatite dykes (8) domains at CV5 did not yield well-structured variograms for either Li2O and Ta2O5 and therefore were estimated using Inverse Distance Squared (ID2), also using Leapfrog Edge. At CV5, three (3) orientated search ellipsoids were used to select data and interpolate Li2O and Ta2O5 grades in successively less restrictive passes. The ellipse sizes and anisotropies were based on the variography, drillhole spacing, and pegmatite geometry. The ellipsoids were 100 m x 50 m x 30 m, 200 m x 100 m x 60 m, and 400 m x 200 m x 120 m. For the first pass interpolation a minimum of five (5) composites and a maximum of twelve (12) composites with a minimum of two (2) holes were needed to interpolate. For the second and third pass a minimum of three (3) composites with a maximum of twelve (12) without a minimum per hole was used. Variable search ellipse orientations (dynamic anisotropy) were used to interpolate for the eight (8) parallel dykes. Spatial anisotropy of the dykes is respected during estimation using Leapfrog Edge’s Variable Orientation tool. The search ellipse follows the trend of the central reference plane of each dyke. At CV13, variography analysis did not yield a well-structured variogram. On CV13, Li2O and Ta2O5 were estimated using Inverse Distance Squared (ID2) in Leapfrog Edge. Three (3) orientated search ellipsoids were used to select data and interpolate Li2O and Ta2O5 grades in successively less restrictive passes. The ellipse sizes and anisotropies were based on the variography, drillhole spacing, and pegmatite geometry. The ellipsoids were 80 m x 60 m x 10 m, 160 m x 120 m x 20 m, and 320 m x 240 m x 40 m. For the first pass interpolation a minimum of five (5) composites and a maximum of twelve (12) composites with a minimum of two (2) holes were needed to interpolate. For the second and third pass a minimum of three (3) composites with a maximum of twelve (12) without a minimum per hole was used. Variable search ellipse orientations (dynamic anisotropy) were used to interpolate the dykes. Spatial anisotropy of the dykes is respected during estimation using Leapfrog Edge’s Variable Orientation tool. The search ellipse follows the trend of the central reference plane of each dyke. Parent cells of 10 m x 5 m x 5 m, subblocked four (4) times in each direction (for minimum subcells of 2.5 m in x, 1.25 m in y, and 1.25 m in z were used. Subblocks are triggered by the geological model. Li2O and Ta2O5 grades are estimated on the parent cells and automatically populated to subblocks. The block model is rotated around the Z axis (Leapfrog 340°). Hard boundaries between all the pegmatite domains were used for all Li2O and Ta2O5 estimates. Validation of the block model was performed using Swath Plots, nearest neighbours grade estimates, global means comparisons, and by visual inspection in 3D and along plan views and cross-sections.
Moisture
Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content. Tonnages are reported on a dry basis.Cut-off parameters
The basis of the adopted cut-off grade(s) or quality parameters applied. Open pit adopted cut-off grade is 0.40% Li2O and determined based on operational cost estimates, primarily through benchmarking and an internal trade-off study, for mining ($5.47/t mined for minable resource, waste or overburden, processing ($14.17/t milled), tailings management ($2.62/t milled), G ($20.41/t milled), and concentrate transport costs ($287/t mine site to Becancour, QC). Process recovery assumed a Dense Media Separation (DMS) only operation at approximately 70% overall recovery based on processing recovery formula of Recovery % = 75% × (1-e^(-1.995(Li2O Feed Grade %) ) )into a 5.5% Li2O spodumene concentrate. A spodumene concentrate price of US $1,500 was assumed with USD/CAD exchange rate of 0.76. A royalty of 2% was applied. Underground adopted cut-off grade for CV5 is 0.60% Li2O and determined based on the same parameters than the open pit with the addition of the underground mining cost estimated at 62.95$/t considering a long hole transverse mining method. Underground adopted cut-off grade for CV13 is 0.80% Li2O and determined based on the same parameters than the open pit with the addition of the underground mining cost estimated at 100$/t considering a mining method that will be aligned with the shallow dip lenses.Mining factors or assumptions
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made. Open-pit mining method is assumed with an overall pit slope ranging from 45° to 53° considering various sectors, single and double bench. No dilution or mining recovery has been considered. Underground mining method considered is long hole for CV5. Stope size considered are vertical 30 m in height, 15 m in width and a minimum of 3 m in thickness. The mining method for CV13 has not been determined but the mining cost used is higher considering the shallow dip of the lenses in CV13. Stope dimensions considered are horizontal considering length of 15 m, 7.5 m in width and a minimum height of 3 m. The Mineral Resources are reported as in-situ tonnes and grade.Metallurgical factors or assumptions
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made. The processing assumptions are based on HLS and magnetic testing, which has produced 6+% Li2O spodumene concentrates at >70% recovery on drill core samples from both the CV5 and CV13 pegmatites and indicate DMS as a viable primary process approach for both CV5 and CV13. This is supported by a subsequent DMS test on CV5 drill core, which returned a spodumene concentrate grading 5.8% Li2O at 79% recovery. For the Mineral Resource conceptual mining shapes, based on a grade versus recovery curve of the test work completed to date, an average recovery of approximately 70% to produce a 5.5% Li2O spodumene concentrate was usedEnvironmental factors or assumptions
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfields project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made. The Project’s CV5 Pegmatite is in the early stages of economic evaluation. A conventional tailings management facility and no material adverse environmental impediments are assumed. No environmental assessment has been completed for the Project. However, a Project Description has been submitted to relevant environmental regulator.Bulk density
Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples. The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc), moisture and differences between rock and alteration zones within the deposit. Discuss assumptions for bulk density estimates used in the evaluation process of the different materials. Density of the pegmatite was estimated using a linear regression function derived from SG field measurements (1 sample every ~4.5 m) and Li2O grade. The regression function (SG= 0.0688 x Li2O% + 2.625) was used for all pegmatite blocks. Non-pegmatite blocks were assigned a fixed SG based on the field measurement median value (diabase = 2.94, amphibolite group = 2.98, metasediment 2.76, wacke = 2.71, ultramafic = 2.95, overburden = 2.00).Classification
The basis for the classification of the Mineral Resources into varying confidence categories. Whether appropriate account has been taken of all relevant factors (ie relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data). Whether the result appropriately reflects the Competent Person’s view of the deposit. The Shaakichiuwaanaan resource classification is in accordance with the JORC 2012 reporting guidelines. All reported Mineral Resources have reasonable prospects for eventual economic extraction. All reported Mineral Resources have been constrained by conceptual open-pit or underground mineable shapes to demonstrate reasonable prospects for eventual economic extraction (“RPEEE”). Blocks were classified as Indicated when 1.) demonstrated geological continuity and minimum thickness of 2 m, 2.) the drill spacing was 70 m or lower and meeting the minimum estimation criteria parameters, and 3.) grade continuity at the reported cut-off grade. Blocks were classified Inferred when drill spacing was between 70 m and 140 m and meeting the minimum estimation criteria parameters. Geological continuity and a minimum thickness of 2 m were also mandatory. There are no measured classified blocks. Pegmatite dykes or extension with lower level of information / confidence were also not classified. Classification shapes are created around contiguous blocks at the stated criteria with consideration for the selected mining method. The classification of the Mineral Resource Estimate is appropriate and reflects the view of Competent Person (Todd McCracken).
Audits or reviews
The results of any audits or reviews of Mineral Resource estimates. The mineral resource estimate has been reviewed internally by BBA Engineering Ltd. as part of its regular internal review process. There has been no external audit of the Mineral Resource Estimate.Discussion of relative accuracy/ confidence
Where appropriate a statement of the relative accuracy and confidence level in the Mineral Resource estimate using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate. The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used. These statements of relative accuracy and confidence of the estimate should be compared with production data, where available. The Competent Person is of the opinion that the Mineral Resource for the CV5 and CV13 spodumene pegmatites (collectively, the Shaakichiuwaanaan Mineral Resource) appropriately consider modifying factors and have been estimated using industry best practices. The accuracy of the estimate within this Mineral Resource is determined by yet not limited to; geological confidence including understanding the geology, deposit geometry, drill spacing. As always, changes in commodity price and exchange rate assumptions will have an impact on the optimal size of the conceptual mining open-pit and underground shapes. Changes in current environmental or legal regulations may affect the operational parameters (cost, mitigation measures). The Mineral Resource Estimate is constrained using open-pit and underground mining shapes to satisfy reasonable prospects for eventual economic extraction.
Appendix 2: Sources for Figure 1 (tonnage vs grade – the Americas) Figure 2
(tonnage vs grade – world)
Company name
Stock Ticker
Project Name
Source
Liontown Resources Ltd.
LTR
Kathleen Valley
ASX announcement dated April 8, 2021
Liontown Resources Ltd.
LTR
Buldania
ASX announcement dated November 8, 2019
Pilbara Minerals Ltd.
PLS
Pilgangoora
ASX announcement dated August 7, 2023
Alita Resources Ltd.
n/a
Bald Hill
Alliance Minerals Assets Limited March 2019 Presentation
Arcadium Lithium Plc
ALTM
Whabouchi
S-K 1300 Technical Report dated September 8, 2023
Arcadium Lithium Plc
ALTM
Galaxy
ASX announcement dated August 11, 2023
Arcadium Lithium Plc
ALTM
Mt Cattlin
ASX announcement dated November 9, 2023
European Lithium Ltd.
EUR
Wolfsberg
ASX announcement dated December 1, 2021
AVZ Minerals Ltd.
AVZ
Manono
ASX announcement dated January 31, 2024
Critical Elements Lithium Corp.
CRE
Rose
TSX Announcement dated August 29, 2023
Atlantic Lithium Ltd..
ALL
Ewoyaa
ASX announcement dated February 1, 2023
IGO Ltd.
IGO
Greenbushes
ASX announcement dated December 31, 2023
Mineral Resources Ltd.
MIN
Wodgina
ASX announcement dated September 22, 2023
Albemarle Corp.
ALB
Kings Mountain
SEC filing dated February 15, 2023
Mineral Resources Ltd.
MIN
Mt Marion
ASX announcement dated February 21, 2024
Sociedad Quimica y Minera de Chile S.A.
SQM
Mt. Holland
Annual Report 2022
Leo Lithium Ltd.
LLL
Goulamina
ASX announcement dated July 1, 2024
Sayona Mining Ltd.
SYA
Authier
ASX announcement dated April 14, 2023
Sayona Mining Ltd.
SYA
NAL
ASX announcement dated April 14, 2023
Sayona Mining Ltd.
SYA
Moblan
ASX announcement dated April 17, 2023
Prospect Resources Ltd.
PSC
Arcadia
ASX announcement dated October 11, 2021
AMG Critical Materials N.V.
AMG
Mibra
Euronext announcement dated April 3, 2017
Sibanye Stillwater Ltd.
SSW
Keliber
JSE announcement dated February 17, 2023
Lithium Ionic Corp
LTH
Bandeira
Press release dated April 24,2024
Frontier Lithium Inc.
FL
PAK + Spark
NI 43-101 technical report dated February 28, 2023
Sigma Lithium Corp.
SGML
Grota do Cirilo
Press release dated January 31,2024
Piedmont Lithium Inc
PLL
Carolina
Press release dated October 21,2021
Sinomine Resource Group Co., Ltd.
002738
Bikita
SZ Announcement dated April 25, 2023
Delta Lithium Ltd.
DLI
Mt Ida
ASX announcement dated October 3, 2023
Delta Lithium Ltd.
DLI
Yinnetharra
ASX announcement dated December 27, 2023
Avalon Advanced Materials Inc.
AVL
Separation Rapids
PR Newswire press release dated August 10, 2023
Andrada Mining Ltd.
ATM
Uis
AIM announcement dated February 6, 2023
Global Lithium Resources Ltd.
GL1
Manna
ASX announcement dated June 12, 2024
Global Lithium Resources Ltd.
GL1
Marble Bar
ASX announcement dated December 15, 2022
Latin Resources Ltd
LRS
Colina
ASX announcement dated May 30, 2024
Essential Metals Ltd.
ESS
Dome North
ASX announcement dated December 20, 2022
Kodal Minerals Plc
KOD
Bougouni
AIM announcement dated January 27, 2020
Savannah Resources Plc
SAV
Mina Do Barroso
AIM announcement dated June 12, 2023
Green Technology Metals Ltd.
GT1
Root
ASX announcement dated October 17, 2023
Green Technology Metals Ltd.
GT1
Seymour
ASX announcement dated November 17, 2023
Rock Tech Lithium Inc.
RCK
Georgia Lake
TSX Announcement dated November 15, 2022
Winsome Resources Ltd.
WR1
Adina
ASX announcement dated May 28, 2024
Cygnus Metals Ltd.
CY5
Pontax
ASX announcement dated August 14, 2023
Core Lithium Ltd
CXO
Finniss
ASX announcement dated April 11, 2024
Appendix 3: MRE details for deposits/projects noted in Figure 1 Figure 2.
Company Name
Project Name
Region
Stage
Category
Tonnage
(Mt)
Grade
(Li2O)
Liontown Resources Ltd.
Kathleen Valley
APAC
Development
Measured
20.0
1.32%
Indicated
109.0
1.37%
Inferred
27.0
1.27%
Liontown Resources Ltd.
Buldania
APAC
Development
Measured
-
-
Indicated
9.1
0.98%
Inferred
5.9
0.95%
Pilbara Minerals Ltd.
Pilgangoora
APAC
Production
Measured
22.1
1.34%
Indicated
315.2
1.15%
Inferred
76.6
1.07%
Alita Resources Ltd.
Bald Hill
APAC
Production
Measured
-
-
Indicated
14.4
1.02%
Inferred
12.1
0.90%
Arcadium Lithium Plc
Whabouchi
Americas
Development
Measured
-
-
Indicated
46.0
1.36%
Inferred
8.3
1.31%
Arcadium Lithium Plc
Galaxy
Americas
Development
Measured
-
-
Indicated
54.3
1.30%
Inferred
55.9
1.29%
Arcadium Lithium Plc
Mt Cattlin
APAC
Production
Measured
0.2
1.00%
Indicated
10.6
1.30%
Inferred
1.3
1.30%
European Lithium Ltd.
Wolfsberg
EMEA
Development
Measured
4.3
1.13%
Indicated
5.4
0.95%
Inferred
3.1
0.90%
AVZ Minerals Ltd.
Manono
EMEA
Development
Measured
132.0
1.65%
Indicated
367.0
1.62%
Inferred
342.0
1.57%
Critical Elements Lithium Corp.
Rose
Americas
Development
Measured
-
-
Indicated
30.6
0.93%
Inferred
2.4
0.78%
Atlantic Lithium Ltd.
Ewoyaa
EMEA
Development
Measured
3.5
1.37%
Indicated
24.5
1.25%
Inferred
7.4
1.16%
Tailson JV
Greenbushes
APAC
Production
Measured
0.7
3.00%
Indicated
397.0
1.50%
Inferred
49.0
1.10%
MARBL JV
Wodgina
APAC
Production
Measured
-
-
Indicated
182.1
1.15%
Inferred
35.3
1.19%
Albemarle Corp.
Kings Mountain
Americas
Development
Measured
-
0.00%
Indicated
46.8
1.37%
Inferred
42.9
1.10%
MinRes / Ganfeng
Mt Marion
APAC
Production
Measured
-
-
Indicated
54.7
1.40%
Inferred
11.4
1.05%
SQM / Wesfarmers
Mt. Holland
APAC
Development
Measured
71.0
1.57%
Indicated
107.0
1.51%
Inferred
8.0
1.44%
Ganfeng
Goulamina
EMEA
Development
Measured
13.1
1.58%
Indicated
94.9
1.42%
Inferred
159.2
1.33%
Sayona Mining Ltd.
Authier
Americas
Development
Measured
6.0
0.98%
Indicated
8.1
1.03%
Inferred
2.9
1.00%
Sayona Mining Ltd.
NAL
Americas
Production
Measured
1.0
1.19%
Indicated
24.0
1.23%
Inferred
33.0
1.23%
Sayona Mining Ltd.
Moblan
Americas
Development
Measured
6.3
1.46%
Indicated
43.6
1.16%
Inferred
21.0
1.02%
Prospect Resources Ltd.
Arcadia
EMEA
Development
Measured
15.8
1.12%
Indicated
45.6
1.06%
Inferred
11.2
0.99%
AMG Critical Materials N.V.
Mibra
Americas
Production
Measured
3.4
1.00%
Indicated
16.9
1.07%
Inferred
4.2
1.03%
Sibanye Stillwater Ltd.
Keliber
EMEA
Development
Measured
10.2
0.96%
Indicated
3.9
1.06%
Inferred
3.3
0.83%
Frontier Lithium Inc.
PAK + Spark
Americas
Development
Measured
1.3
2.14%
Indicated
24.7
1.59%
Inferred
32.5
1.41%
Sigma Lithium Corp.
Grota do Cirilo
Americas
Production
Measured
45.2
1.41%
Indicated
49.1
1.39%
Inferred
14.6
1.37%
Piedmont Lithium Inc
Carolina
Americas
Development
Measured
-
-
Indicated
28.2
1.11%
Inferred
15.9
1.02%
Sinomine Resource Group Co., Ltd.
Bikita
EMEA
Production
Measured
21.7
1.17%
Indicated
12.5
1.09%
Inferred
6.1
1.08%
Delta Lithium Ltd.
Mt Ida
APAC
Development
Measured
-
-
Indicated
7.8
1.30%
Inferred
6.8
1.10%
Avalon Advanced Materials Inc.
Separation Rapids
Americas
Development
Measured
4.3
1.33%
Indicated
5.8
1.36%
Inferred
2.8
1.38%
Andrada Mining Ltd.
Uis
EMEA
Development
Measured
21.0
0.72%
Indicated
17.0
0.73%
Inferred
43.0
0.73%
Global Lithium Resources Ltd.
Manna
APAC
Development
Measured
-
-
Indicated
32.9
1.04%
Inferred
18.7
0.92%
Global Lithium Resources Ltd.
Marble Bar
APAC
Development
Measured
-
-
Indicated
3.8
0.97%
Inferred
14.2
1.01%
Latin Resources Ltd
Colina
Americas
Development
Measured
28.6
1.31%
Indicated
38.6
1.23%
Inferred
3.6
1.10%
Essential Metals Ltd.
Dome North
EMEA
Development
Measured
-
-
Indicated
8.6
1.23%
Inferred
2.6
0.92%
Kodal Minerals Plc
Bougouni
EMEA
Development
Measured
-
-
Indicated
11.6
1.13%
Inferred
20.3
1.02%
Savannah Resources Plc
Mina Do Barroso
EMEA
Development
Measured
6.6
1.10%
Indicated
11.8
1.00%
Inferred
9.6
1.10%
Rock Tech Lithium Inc.
Georgia Lake
Americas
Development
Measured
-
-
Indicated
10.6
0.88%
Inferred
4.2
1.00%
Core Lithium Ltd
Finniss
APAC
Care Maintenance
Measured
6.3
1.41%
Indicated
21.6
1.30%
Inferred
20.3
1.18%
Lithium Ionic Corp.
Bandeira
Americas
Development
Measured
3.3
1.38%
Indicated
20.4
1.33%
Inferred
18.3
1.37%
Delta Lithium Ltd.
Yinnetharra
APAC
Development
Measured
-
-
Indicated
6.7
1.00%
Inferred
19.0
1.00%
Green Technology Metals Ltd.
Root
Americas
Development
Measured
-
-
Indicated
9.4
1.30%
Inferred
5.2
1.03%
Green Technology Metals Ltd.
Seymour
Americas
Development
Measured
-
-
Indicated
6.1
1.25%
Inferred
4.1
0.70%
Winsome Resources Ltd.
Adina
Americas
Development
Measured
-
-
Indicated
61.4
1.14%
Inferred
16.5
1.19%
Cygnus Metals Ltd.
Pontax
Americas
Development
Measured
-
-
Indicated
-
-
Inferred
10.1
1.04%
Shaakichiuwaanaan
Americas
Development
Measured
-
-
Indicated
80.1
1.44%
Inferred
62.5
1.31%
APAC = Asia-Pacific; EMEA = Europe, Middle East, and Africa; Americas = North America, and South America
About Patriot Battery Metals Inc.
Patriot Battery Metals Inc. is a hard-rock lithium exploration company focused on advancing its district-scale 100%-owned Shaakichiuwaanaan Property (formerly known as Corvette) located in the Eeyou Istchee James Bay region of Quebec, Canada, which is accessible year-round by all-season road and is proximal to regional powerline infrastructure. The Shaakichiuwaanaan Mineral Resource1, which includes the CV5 CV13 spodumene pegmatites, totals 80.1 Mt at 1.44% Li2O Indicated, and 62.5 Mt at 1.31% Li2O Inferred, and ranks as the largest lithium pegmatite resource in the Americas, and the 8th largest lithium pegmatite resource in the world. Additionally, the Shaakichiuwaanaan Property hosts multiple other spodumene pegmatite clusters that remain to be drill tested, as well as significant areas of prospective trend that remain to be assessed.
1 Shaakichiuwaanaan (CV5 CV13) Mineral Resource Estimate (80.1 Mt at 1.44% Li2O and 163 ppm Ta2O5 Indicated, and 62.5 Mt at 1.31% Li2O and 147 ppm Ta2O5 ppm Inferred) is reported at a cut-off grade of 0.40% Li2O (open-pit), 0.60% Li2O (underground CV5), and 0.80% Li2O (underground CV13) with an Effective Date of June 27, 2024 (through drill hole CV24-526). Mineral resources are not mineral reserves as they do not have demonstrated economic viability.
For further information, please contact us at info@patriotbatterymetals.com or by calling +1 (604) 279-8709, or visit www.patriotbatterymetals.com. Please also refer to the Company’s continuous disclosure filings, available under its profile at www.sedarplus.ca and www.asx.com.au, for available exploration data.
This news release has been approved by the Board of Directors.
“KEN BRINSDEN”
Kenneth Brinsden, President, CEO, Managing Director
Brad Seward
Vice President, Investor Relations
T: +61 400 199 471
E: bseward@patriotbatterymetals.com
Olivier Caza-Lapointe
Head, Investor Relations – North America
T: +1 (514) 913-5264
E: ocazalapointe@patriotbatterymetals.com
Disclaimer for Forward-Looking Information
This news release contains “forward-looking information” or “forward-looking statements” within the meaning of applicable securities laws and other statements that are not historical facts. Forward-looking statements are included to provide information about management’s current expectations and plans that allows investors and others to have a better understanding of the Company’s business plans and financial performance and condition.
All statements, other than statements of historical fact included in this news release, regarding the Company’s strategy, future operations, technical assessments, prospects, plans and objectives of management are forward-looking statements that involve risks and uncertainties. Forward-looking statements are typically identified by words such as “plan”, “expect”, “estimate”, “intend”, “anticipate”, “believe”, or variations of such words and phrases or statements that certain actions, events or results “may”, “could”, “would”, “might” or “will” be taken, occur or be achieved. Forward-looking statements in this release include, but are not limited to, statements concerning: the timing of the preliminary economic assessment, the timing of a feasibility study, the potential for production, the cost of production and the potential benefits thereof, the significant potential for further resource growth at the Property through continued drill exploration, notably of the potential for connectivity of the pegmatite body of the CV5 and CV13 spodumene pegmatites, the Company’s position as a leading candidate to provide long-term spodumene supply to the North American and European markets, the recoverability of tantalum as a by-product, and the potential for a series of relatively closely spaced/stacked, sub-parallel, and sizable spodumene-bearing pegmatite bodies, with significant lateral and depth extent, to be present near CV5 and CV13 spodumene pegmatites.
Forward-looking information is based upon certain assumptions and other important factors that, if untrue, could cause the actual results, performance or achievements of the Company to be materially different from future results, performance or achievements expressed or implied by such information or statements. There can be no assurance that such information or statements will prove to be accurate. Key assumptions upon which the Company’s forward-looking information is based include, without limitation, that proposed exploration and Mineral Resource Estimate work on the Property will continue as expected, the accuracy of reserve and resource estimates, the classification of resources between inferred and the assumptions on which the reserve and resource estimates are based, long-term demand for spodumene supply, and that exploration and development results continue to support management’s current plans for Property development.
Readers are cautioned that the foregoing list is not exhaustive of all factors and assumptions which may have been used. Forward-looking statements are also subject to risks and uncertainties facing the Company’s business, any of which could have a material adverse effect on the Company’s business, financial condition, results of operations and growth prospects. Some of the risks the Company faces and the uncertainties that could cause actual results to differ materially from those expressed in the forward-looking statements include, among others, the ability to execute on plans relating to the Company’s Project, including the timing thereof. In addition, readers are directed to carefully review the detailed risk discussion in the Company’s most recent Annual Information Form filed on SEDAR+, which discussion is incorporated by reference in this news release, for a fuller understanding of the risks and uncertainties that affect the Company’s business and operations.
Although the Company believes its expectations are based upon reasonable assumptions and has attempted to identify important factors that could cause actual actions, events or results to differ materially from those described in forward-looking statements, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. There can be no assurance that forward-looking information will prove to be accurate, as actual results and future events could differ materially from those anticipated in such information. As such, these risks are not exhaustive; however, they should be considered carefully. If any of these risks or uncertainties materialize, actual results may vary materially from those anticipated in the forward-looking statements found herein. Due to the risks, uncertainties and assumptions inherent in forward-looking statements, readers should not place undue reliance on forward-looking statements.
Forward-looking statements contained herein are presented for the purpose of assisting investors in understanding the Company’s business plans, financial performance and condition and may not be appropriate for other purposes.
The forward-looking statements contained herein are made only as of the date hereof. The Company disclaims any intention or obligation to update or revise any forward-looking statements, whether as a result of new information, future events or otherwise, except to the extent required by applicable law. The Company qualifies all of its forward-looking statements by these cautionary statements.
Link to original news in full length: