PMET.TO
Published on 05/12/2025 at 17:02
Representing an increase of ~30% and ~306% in Indicated Resources at CV5 and CV13, respectively
VANCOUVER, BC, May 12, 2025 /CNW/ - May 13, 2025 – Sydney, Australia
Darren L. Smith, Executive and Vice President of Exploration for the Company, comments: "The results of the updated MRE at CV5 have exceeded our expectations with over 100 Mt of Indicated Resources now defined, of which the vast majority resides within only a single pegmatite dyke and includes the high-grade Nova Zone. Additionally, at the CV13 Pegmatite while delineating the high-grade Vega Zone, a total of 6.1 Mt at 1.87% Li2O of Indicated Resources has now been defined, representing a 306% increase in Indicated tonnage and a 16% increase in Indicated grade compared to the August 2024 MRE."
"Collectively, this updated MRE represents a significant increase in resource confidence and an important derisking event for the Project as it advances towards Feasibility on the path to production. Shaakichiuwaanaan continues to demonstrate its Tier-1, world-class nature and robustness as it further positions itself to be a key player in the lithium raw materials industry."
Ken Brinsden, President, CEO, and Managing Director, comments: "This is another significant accomplishment for our team and a key milestone for the Company as we approach the completion of our Feasibility Study on the CV5 Pegmatite, which remains on schedule for CYQ3-2025. It further cements the position of the Shaakichiuwaanaan Project as one of the most important hard rock lithium assets in development globally."
"The delivery of a substantial updated consolidated Indicated Resource of 108 Mt is a major milestone which will underpin our development studies. The continued derisking of the overall resource, while maintaining tonnage and grade, as well as the significant presence of other strategic and critical metals like tantalum, cesium, and now gallium, highlights the Tier-1 scale of the mineral system and the considerable potential for further growth and value creation for shareholders."
"As we advance towards a Feasibility Study, the Company is firmly positioned to be able to provide long-term future spodumene supply and other critical metals to the North American and European markets. The combination of scale, management quality, balance sheet strength, and our high-quality strategic partnerships allows us to remain confident in the success of our strategy," added Mr. Brinsden.
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") located in the Eeyou Istchee James Bay region of Quebec. The CV5 Spodumene Pegmatite is situated approximately 13 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 along geological trend of CV5.
The updated Consolidated MRE for the Project includes both the CV5 and CV13 spodumene pegmatites and totals 108.0 Mt at 1.40% Li2O Indicated and 33.3 Mt at 1.33% Li2O Inferred, for a contained lithium carbonate equivalent ("LCE") of 3.75 Mt Indicated and 1.09 Mt Inferred (Table 1, Figure 1, and Figure 2). Presented by resource location/name, this MRE includes 101.8 Mt at 1.38% Li2O Indicated and 13.9 Mt at 1.21% Li2O Inferred at CV5, and 6.1 Mt at 1.87% Li2O Indicated and 19.4 Mt at 1.42% 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, the third MRE for the Project, continues to reaffirm it as the largest lithium pegmatite Mineral Resource in the Americas and 8th largest globally (Figure 1, Figure 2, Appendix 2 through 4). Additionally, the MRE now ranks as the largest lithium pegmatite Indicated Mineral Resource in the Americas (Figure 3). These metrics and context entrench the Project as a Tier 1, world-class lithium pegmatite asset.
Since the last MRE (August 2024), the focus of drilling at the CV5 Pegmatite has been on infill (targeting ~50 m spaced pegmatite pierce points) to support an upgrade in Mineral Resource confidence from the Inferred category to the Indicated category. The overarching objective of defining the additional Indicated Resources is to underpin the Company's maiden Ore Reserve and Feasibility Study for the CV5 Pegmatite – on schedule for CYQ3-2025 – and which is anticipated to have a production scenario similar to that outlined in the 2024 Preliminary Economic Assessment (see news release dated August 21, 2024)
The Consolidated MRE statement for the Shaakichiuwaanaan Project, presented in Table 1, includes only the CV5 and CV13 spodumene pegmatites, which remain open in multiple directions. Therefore, this Consolidated MRE does not include any of the other known spodumene pegmatite clusters on the Property – CV4, CV8, CV9, CV10, CV12, CV14, and the recently discovered CV15 (Figure 4 and Figure 36). Collectively, this highlights considerable potential for resource growth in lithium, and other critical and strategic metals, which could support a larger or extended mining operation, 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.
Table 1: NI 43-101 Mineral Resource Statement for the Shaakichiuwaanaan Project.
Pegmatite
Classification
Tonnes
(t)
Li2O(%)
Ta2O5(ppm)
Ga(ppm)
Contained LCE(Mt)
CV5 & CV13
Indicated
107,955,000
1.40
166
66
3.75
Inferred
33,280,000
1.33
156
65
1.09
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). The CV5 and CV13 pegmatites are situated along the same geological trend, separated by approximately 2.6 km of prospective trend (Figure 4). As such, given the similar mineralogy, geochemistry, host geological and structural trend, and close proximity to each other, 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).
Table 2: Shaakichiuwaanaan Mineral Resource by Pegmatite and Conceptual Mining Constraint.
Cut-off GradeLi2O (%)
Conceptual Mining Constraint
Pegmatite
Classification
Tonnes
(t)
Li2O(%)
Ta2O5(ppm)
Ga(ppm)
Contained LCE(Mt)
0.40
Open-Pit
CV5
Indicated
97,757,000
1.39
163
66
3.35
0.60
Underground
4,071,000
1.08
186
66
0.11
Total
101,828,000
1.38
164
66
3.46
0.40
Open-Pit
CV5
Inferred
5,745,000
1.16
163
61
0.17
0.60
Underground
8,153,000
1.24
136
60
0.25
Total
13,898,000
1.21
147
60
0.41
0.40
Open-Pit
CV13
Indicated
5,960,000
1.90
200
76
0.28
0.70
Underground
167,000
0.86
131
60
0.00
Total
6,127,000
1.87
198
76
0.28
0.40
Open-Pit
CV13
Inferred
17,920,000
1.45
169
70
0.64
0.70
Underground
1,462,000
1.05
75
55
0.04
Total
19,382,000
1.42
162
69
0.68
All Table 1 footnotes are applicable.
The sensitivity analysis for the Shaakichiuwaanaan MRE (Table 3 and Figure 5) 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.
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 17, Figure 26, and Figure 27). 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 the Property but also its robustness in mineralized intensity defined to date.
The following Table 3 and Figure 5 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.
1.
This table should not be interpreted as a Mineral Resource. The table presents the sum of the open-pit and underground constrained and classified resources at the same cut-off. The data is presented to demonstrate the Mineral Resource tonnage and grade sensitivity to various cut-off grades. The selected cut-off grade for the base case is 0.40% Li2O with the revenue factor 1 pit shell constraint for CV5 and CV13, with a 0.60% Li2O and 0.70% Li2O underground cut-off grade for CV5 and CV13, respectively.
2.
Errors may occur in totals due to rounding.
In addition to lithium as the primary commodity of interest, the CV5 and CV13 pegmatites also contain a significant amount of tantalum as a potentially recoverable by-product – 108.0 Mt at 1.40% Li2O and 166 ppm Ta2O5 Indicated, and 33.3 Mt at 1.33% Li2O and 156 ppm Ta2O5 Inferred. Potential mineable shapes are estimated based on the lithium cut-off grade only. Additionally, domaining of higher-grade tantalum zones within the overall pegmatite have not been incorporated into the MRE.
These tantalum grades are significant and rank Shaakichiuwaanaan as a top five tantalum pegmatite Mineral Resource in the world in terms of grade and tonnage (Figure 6).
Mineralogy completed to date indicates that tantalite is the tantalum-bearing mineral, which may be recoverable from the tailings of the primary lithium recovery process (i.e., potential valorization of waste streams). The Company is currently evaluating the potential for recovery of tantalum through an active mineral processing test program at SGS Canada's Lakefield, ON, facility.
Tantalum is listed as a critical and strategic mineral by the province of Quebec (Canada), Canada, European Union, United Kingdom, 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 significant amounts of tantalum are currently produced in North America or Europe, with a majority of production coming out of the Democratic Republic of Congo, Rwanda, and Brazil.
As part of the Shaakichiuwaanaan MRE update, the Company has included gallium (Ga) – 108.0 Mt at 1.40% Li2O, 166 ppm Ta2O5, and 66 ppm Ga, Indicated, and 33.3 Mt at 1.33% Li2O, 156 ppm Ta2O5, 65 ppm Ga, Inferred. The gallium grades were not used in generating the potential mineable shapes at CV5 and CV13. Potential mineable shapes are estimated based on the lithium cut-off grade only. Additionally, domaining of potentially higher-grade gallium zones within the overall pegmatite have not been incorporated into the MRE.
Although the recovery of gallium from pegmatite has yet to be commercialized, there is a growing interest in lithium pegmatite as a potential source. The vast majority of current gallium production comes from bauxite (aluminum ore) processing, whereby the Ga has substituted for aluminum (Al) and is extracted (at very low overall recovery) out of the spent liquor when concentrations have reached sufficient levels. However, as lithium pegmatites may contain several aluminum rich minerals in abundance (feldspar, muscovite, spodumene), Ga may be present in reasonable concentrations that may encourage extraction in downstream processing. The Company is currently evaluating a metallurgical approach to recover gallium from the lithium waste stream(s).
Gallium is listed as a critical and strategic mineral by the province of Quebec (Canada), Canada, European Union, United Kingdom, Australia, Japan, India, South Korea, and the United States. China dominates global production of gallium and in late 2024 banned all exports of the metal to the United States, thus highlighting security of supply concerns. Gallium is used in various high-tech applications and primarily in the electronics industry as semiconductors.
In news releases dated March 2 and April 9, 2025, the Company announced the discovery of significant cesium mineralization at the CV13 Pegmatite within the Vega and Rigel zones. Initial drill results returned 11.1 m at 4.87% Cs2O, including 7.1 m at 7.39% Cs2O (Vega, CV24-520) and 5.0 m at 13.32% Cs2O, including 2.0 m at 22.90% Cs2O (Rigel, CV23-255).
However, the MRE announced herein does not include cesium. This is in part due to the cesium overlimit analytical results being received after the determined Effective Date of the MRE announced herein (January 6, 2025), the geological modelling still required, as well as the overall ongoing Feasibility Study schedule requiring a frozen and classified block model earlier in the year. The Company anticipates advancing an updated Mineral Resource to include cesium in the CV13 Pegmatite as part of a future MRE update for the Project.
Cesium is listed as a critical and strategic mineral by the province of Quebec (Canada), Canada, Japan, and the United States. Mineral deposits of cesium (pollucite) are extremely rare globally and represent the most fractionated component of LCT pegmatite systems, which are effectively the only primary source of cesium globally. Due to its high-density, low toxicity, biodegradable nature, and recoverability, cesium is used to support the completion of oil and gas wells at high pressure and temperature. Cesium is also used in atomic clocks, GPS, aircraft guidance systems, and telecommunications.
With the updated MRE now completed, including a significant amount of Indicated Resource now estimated at CV5, the Company is focused on completion of the remaining deliverables for the Feasibility Study. The Feasibility Study, which includes only the CV5 Pegmatite (hosting the high-grade Nova Zone), remains on schedule for CYQ3-2025, with the Company recently announcing an update on its progress on March 18, 2025.
With respect to the cesium potential (see news releases dated March 2 and April 9, 2025), with the overlimit analysis now received, the Company is actively refining the geological models for the Vega and Rigel zones. An MRE update is anticipated to follow, which would include cesium, potentially later in 2025. Additionally, the Company will continue its exploratory drill program at CV13, focused on further delineation of the Vega and Rigel cesium zones. Various activities in support of potential development are also being considered.
The geological model underpinning the MRE for CV5 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 and remains open in multiple directions.
The geological model underpinning the MRE for CV13 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, extends over a strike length of approximately 2.5 km, and remains open in several directions.
The geological models of the CV5 and CV13 spodumene pegmatites are presented in plan, inclined, and side view in Figure 7, as well as Figure 8 to Figure 12, and Figure 20 and Figure 21, respectively. The MRE block model, block classifications, and cross-sections for CV5 and CV13 are presented in Figure 13 to Figure 19, and Figure 22 to Figure 29, respectively.
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 reasonable prospects for eventual economic extraction ("RPEEE") in accordance with NI 43-101.
As the Company is listed on both the 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 MRE has been completed in accordance with the Canadian National Instrument 43-101 – Standards of Disclosure for Mineral Projects. 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.
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 30). The La Grande-4 (LG4) hydroelectric dam complex is located approximately 40 km north-northeast of the Property. The CV5 Spodumene Pegmatite is located central to the Property, ~13 km south of KM-270 on the Trans-Taiga Road, and is accessible year-round by all-season road. The CV13 Spodumene Pegmatite is located ~3 km west-southwest of CV5.
The Property is comprised of 463 CDC mineral claims that cover an area of approximately 23,710 ha. All claims are registered 100% in the name of Lithium Innova Inc., a wholly owned subsidiary of Patriot Battery Metals Inc.
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 35). 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 amphibolites, 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.
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 both low and high relief landforms (i.e., outcrops) or present under shallow glacial till cover (Figure 31 and Figure 33). To date, the LCT pegmatites at the Property have been observed to occur within a corridor of generally ~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. To date, nine (9) distinct lithium pegmatite clusters have been reported along the CV Lithium Trend at the Property – CV4, CV5, CV8, CV9, CV10, CV12, CV13, CV14, and CV15.
The MRE reported herein is limited to only the CV5 and CV13 spodumene pegmatites (Figure 4), and represent the core area of the trend. The CV5 and CV13 pegmatites are situated along the same geological trend, with approximate strike lengths of 4.6 km and 2.5 km, respectively – as defined by drilling to date and which remain open – and are separated by a distance of ~2.6 km (Figure 4). The MRE covers ~6.9 km of the ~7.1 km of defined pegmatite trend and remains open.
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 (Figure 32 and Figure 34). 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. Additionally, both CV5 and CV13 host a significant tantalum component (tantalite). A large zone of cesium mineralization (pollucite) has also been identified at the CV13 Pegmatite.
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 at least 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. The pegmatites that define CV5 are relatively undeformed and very competent, although they have 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 2.5 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 in the primary dykes has been traced more than 450 m down-dip (west arm) and over 800 m down-dip (near flat-lying east arm). However, due to the flat-lying to shallow dips of the pegmatite bodies, the mineralization 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 17 and Figure 27). 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 Shaakichiuwaanaan database includes 801 diamond drill holes completed over the 2021, 2022, 2023, and 2024 programs, for a collective total of 234,671 m, as well as outcrop channels totalling 800 m. The Shaakichiuwaanaan MRE, including the host geological models, are supported by 720 diamond drill holes of NQ (predominant) or HQ size, completed over the 2021, 2022, 2023, and 2024 (through the end of 2024 – drill hole CV24-787) programs, for a collective total of 227,703 m, as well 604 m of outcrop channels. This equates to 555 holes (188,695 m) and 179 m of outcrop channels at CV5, and 165 holes (39,008 m) and 425 m of outcrop channels at CV13 (Figure 37, Figure 38, and Figure 39).
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 and Table 5). Downhole deviation surveys for each drill hole were completed with a Devico DeviGyro tool (2021 and 2024 holes), Reflex Gyro Sprint IQ tool (2022, 2023, and 2024 holes), Axis Champ Gyro (2023 and 2024 holes), or Reflex OMNI Gyro Sprint IQ (2024 holes). Survey shots were typically 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 rock units. 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 MRE.
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 depending on the resource classification being targeted. 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 m 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 depending on the resource classification being targeted. Due to the varied orientation of the pegmatite bodies along strike at CV13, hole orientations vary widely with multiple holes often being completed from the same pad.
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 or 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 ~0.5 to 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.
Core sampling protocols meet 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 ("SG") measurements of entire pegmatite samples were collected at systematic intervals (approximately 1 SG measurement every 4-5 m) using the water immersion method. SG measurements are also collected systematically from host rock samples (i.e., non-pegmatite).
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.
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 CV24-787) 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.
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 drill spacing was 70 m or lower, blocks were estimated with at least 2 drill holes, and meeting the minimum estimation criteria parameters. Geological continuity and a minimum thickness of 2 m were mandatory, as well grade continuity demonstrated 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 MRE appropriately reflect the view of the Competent Person.
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.
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), and vein CV_160 were estimated using ordinary kriging (OK), using Leapfrog Edge.
For Ta2O5, a well-structured variogram was obtained for the spodumene-rich domain, the feldspar-rich domain within CV5 principal pegmatite, and vein CV_160. Therefore, Ta2O5 was estimated using ordinary kriging (OK). The remaining pegmatite dykes at CV5 (8) 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. For Li2O, the ellipsoids ranges of the first pass is two (2) x 2nd structure, the second pass is one (1) x 2nd structure and the third pass is one point five (1.5) x 2nd structure. For Ta2O5, the ellipsoids ranges of the first pass is two (2) x 2nd structure, the second pass is one (1) x 2nd structure and the third pass is one point seventy five (1.75) x 2nd structure. For the first pass interpolation a minimum of five (5) composites and a maximum of twelve (15) 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 (15) 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.
For the CV13 Pegmatite dykes, it was determined that no capping was required for Li2O, but Ta2O5 was capped at 3,000 ppm for 3 domains (CV13_100, CV13_101, and CV13_100C) and at 1,200 ppm for the remaining 20 domains. Variography analysis did not yield a well-structured variogram. On CV13, Li2O and Ta2O5 were estimated using ID2 in Leapfrog Edge.
The twenty-three (23) different domains were separated in 3 groups with the same orientation. Different orientated search ellipsoids per group of domains were used to select data and interpolate Li2O and Ta2O5 grades respectively in successively less restrictive passes. The ellipse sizes and anisotropies were based on the variography, drillhole spacing, and pegmatite geometry. The ellipsoid ranges of the first pass is 0.5 x 2nd structure, the second pass is one (1) x 2nd structure and the third pass is two (2) x 2nd structure. For the first and second pass interpolation a minimum of three (3) composites and a maximum of eight (8) composites with a minimum of two (2) holes were needed to interpolate. For the third pass a minimum of two (2) composites with a maximum of eight (8) 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 MRE 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 MRE 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 0.70% 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.
The cut-off grade ("COG") adopted for the MRE is 0.40% Li2O for open-pit resources (CV5 and CV13), 0.60% Li2O for underground resources at CV5, and 0.70% 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&A, 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 40). A long term average SC 6.0 spodumene concentrate price of US $1,500 was assumed with USD/CAD exchange rate of 0.70. A royalty of 2% was applied.
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 MRE 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 7.8 (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 MRE at the CV13 Spodumene Pegmatite is mainly open-pit. A pit slope of 45° was assumed, resulting in a strip ratio of 10 (waste to minable resource) at a revenue factor of 1. Underground mining method accounts for approximately 8.5% 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 magnetic separations, which has produced 6+% Li2O spodumene concentrates at >70% recovery on drill core samples from both the CV5 and CV13 pegmatites. Subsequent HLS as well Dense Media Separation ("DMS") testwork on CV5 material returned a spodumene concentrate grading >5.5% Li2O at >75% recovery, strongly indicating 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 40).
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.
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
Area
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
CV22-032
DD
Land
120.6
158
-45
570138.4
5930800.9
380.6
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
CV22-087
DD
Land
461.0
158
-45
571192.0
5931275.1
380.1
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
CV22-094
DD
Land
320.0
158
-45
571087.1
5931259.2
382.9
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
CV23-126
DD
Land
83.1
158
-47
571680.9
5931383.6
375.3
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
-60
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
CV23-144
DD
Land
25.7
0
-90
570316.3
5930295.9
380.0
HQ
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
CV23-147
DD
Land
185.0
0
-90
571121.4
5931096.9
376.0
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
CV23-152
DD
Land
398.0
158
-47
570714.1
5931114.0
378.8
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
CV23-155
DD
Land
24.9
0
-90
571686.6
5930748.6
379.8
HQ
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
CV23-167
DD
Land
25.5
0
-90
572024.6
5931654.1
374.9
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
158
-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
CV23-186
DD
Land
49.6
0
-90
572596.5
5931710.3
374.2
HQ
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
CV23-197
DD
Land
254.0
158
-45
570803.1
5930728.3
382.0
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
CV23-262
DD
Land
245.1
0
-90
571313.5
5930901.0
377.6
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
CV23-334
DD
Land
70.4
338
-45
569813.6
5930403.6
381.9
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
CV24-369
DD
Land
532.7
158
-62
570253.4
5930912.1
381.3
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
CV24-383
DD
Land
166.0
158
-45
569002.5
5930140.8
396.8
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
CV24-387
DD
Land
627.9
158
-52
570307.0
5931047.4
377.0
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
CV24-401
DD
Land
280.9
158
-58
572052.4
5931534.8
373.7
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
CV24-415
DD
Land
91.6
158
-45
571679.3
5931388.0
374.3
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
160
-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
NQ
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
156
-62
571968.6
5931339.6
371.9
NQ
CV5
CV24-459
DD
Land
314.1
296
-60
571508.9
5930921.8
374.6
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
CV24-501
DD
Land
46.7
155
-49
572024.8
5931469.7
377.9
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
CV24-527
DD
Water
8.6
0
-90
571468.7
5931004.9
372.8
NQ
CV5
CV24-528
DD
Water
108.7
0
-90
571721.4
5930952.2
372.4
NQ
CV5
CV24-530
DD
Water
12.0
0
-90
571443.6
5931037.8
373.0
NQ
CV5
CV24-531
DD
Water
99.4
0
-90
572280.4
5931431.0
379.8
NQ
CV5
CV24-533
DD
Land
51.9
0
-90
568982.8
5930569.5
378.5
HQ
CV5
CV24-534
DD
Land
56.0
0
-90
569493.0
5929975.9
384.3
HQ
CV5
CV24-536
DD
Land
53.0
0
-90
568354.6
5930071.6
397.6
HQ
CV5
CV24-537
DD
Land
30.6
0
-90
570702.3
5931577.7
384.3
HQ
North CV5
CV24-541
DD
Water
13.1
0
-90
571882.6
5931252.9
371.9
NQ
CV5
CV24-542
DD
Water
11.1
0
-90
571235.6
5930959.1
372.9
NQ
CV5
CV24-547
DD
Land
10.3
0
-90
570060.1
5931470.4
390.2
HQ
North CV5
CV24-548
DD
Land
14.8
0
-90
569250.7
5931589.7
375.1
HQ
North CV5
CV24-552
DD
Land
11.9
0
-90
568913.4
5931773.2
379.4
HQ
North CV5
CV24-558
DD
Land
11.0
0
-90
569570.6
5930824.8
370.9
NQ
CV5
CV24-559
DD
Land
558.8
170
-53
572567.1
5931725.4
374.8
NQ
CV5
CV24-562
DD
Land
11.0
0
-90
569602.1
5930842.2
371.3
NQ
CV5
CV24-563
DD
Land
459.2
157
-46
568571.5
5930137.8
390.6
NQ
CV5
CV24-564
DD
Land
317.0
159
-46
568577.9
5929989.5
389.5
NQ
CV5
CV24-567
DD
Land
334.9
160
-45
568868.6
5930091.3
397.2
NQ
CV5
CV24-568
DD
Land
8.4
0
-90
569900.5
5931287.3
382.2
NQ
North CV5
CV24-573
DD
Land
328.9
160
-45
568662.2
5930054.0
387.0
NQ
CV5
CV24-574
DD
Land
502.4
158
-47
572567.8
5931725.4
374.8
NQ
CV5
CV24-576
DD
Land
358.8
160
-45
568902.0
5930133.2
394.3
NQ
CV5
CV24-577
DD
Land
418.5
155
-45
568665.2
5930158.2
388.4
NQ
CV5
CV24-580
DD
Land
100.4
0
-90
568133.9
5932019.0
370.3
PQ
North CV5
CV24-581
DD
Land
301.9
160
-45
568810.4
5930087.1
394.7
NQ
CV5
CV24-585
DD
Land
480.3
180
-45
572566.5
5931726.1
374.8
NQ
CV5
CV24-586
DD
Land
395.9
156
-45
568872.3
5930201.4
390.1
NQ
CV5
CV24-589
DD
Land
468.0
155
-45
568616.1
5930217.1
390.1
NQ
CV5
CV24-591
DD
Land
544.9
160
-50
570294.1
5930963.7
384.3
NQ
CV5
CV24-592
DD
Land
395.1
160
-52
568787.4
5930140.6
392.8
NQ
CV5
CV24-596
DD
Land
551.0
175
-65
572564.2
5931726.1
374.5
NQ
CV5
CV24-597
DD
Land
287.1
157
-56
568963.7
5930244.4
386.5
NQ
CV5
CV24-598
DD
Land
237.0
155
-45
568673.3
5930200.9
389.4
NQ
CV5
CV24-599
DD
Land
257.3
156
-45
568955.3
5930122.4
393.4
NQ
CV5
CV24-600
DD
Land
347.0
156
-45
569049.7
5930158.9
395.9
NQ
CV5
CV24-602
DD
Land
219.0
155
-47
568714.9
5930207.4
388.6
NQ
CV5
CV24-603
DD
Land
422.0
158
-45
569072.2
5930230.8
396.1
NQ
CV5
CV24-604
DD
Water
365.0
0
-90
572400.8
5931363.4
373.1
NQ
CV5
CV24-606
DD
Land
422.0
160
-55
568769.6
5930183.7
386.7
NQ
CV5
CV24-607
DD
Land
236.0
156
-45
569093.9
5930179.0
398.0
NQ
CV5
CV24-609
DD
Land
314.0
160
-46
570437.9
5930996.3
384.9
NQ
CV5
CV24-610
DD
Land
566.0
170
-60
572564.4
5931725.5
374.5
NQ
CV5
CV24-612
DD
Land
125.0
156
-45
569114.5
5930130.7
393.4
NQ
CV5
CV24-613
DD
Water
364.9
156
-62
570030.5
5930662.8
373.4
NQ
CV5
CV24-614
DD
Land
134.0
156
-45
569141.9
5930193.2
399.7
NQ
CV5
CV24-615
DD
Water
409.8
0
-90
572357.9
5931408.6
373.0
NQ
CV5
CV24-616
DD
Land
398.1
156
-45
569100.9
5930296.8
389.9
NQ
CV5
CV24-617
DD
Land
458.0
158
-57
568808.3
5930221.3
383.3
NQ
CV5
CV24-618
DD
Land
131.0
158
-45
569299.9
5930206.2
393.5
NQ
CV5
CV24-620
DD
Land
413.0
160
-60
572214.9
5931531.8
373.1
NQ
CV5
CV24-621
DD
Land
333.1
158
-48
570534.0
5931023.5
377.2
NQ
CV5
CV24-622
DD
Land
107.0
156
-60
569410.4
5930198.9
385.0
NQ
CV5
CV24-623
DD
Land
134.0
160
-45
569488.6
5930274.4
382.5
NQ
CV5
CV24-626
DD
Land
245.5
10
-45
569488.6
5930276.8
383.9
NQ
CV5
CV24-627
DD
Water
394.7
156
-50
570030.9
5930662.0
372.9
NQ
CV5
CV24-628
DD
Land
572.0
156
-54
571747.8
5931540.3
393.5
NQ
CV5
CV24-629
DD
Water
475.8
0
-90
572360.3
5931464.6
371.9
NQ
CV5
CV24-630
DD
Land
539.0
178
-60
572564.5
5931724.9
374.6
NQ
CV5
CV24-631
DD
Land
140.0
158
-50
570577.8
5931046.2
378.7
NQ
CV5
CV24-632
DD
Land
170.0
160
-45
569680.8
5930329.9
381.9
NQ
CV5
CV24-635
DD
Land
412.5
140
-60
572215.2
5931532.2
373.2
NQ
CV5
CV24-636
DD
Land
537.3
155
-50
570159.1
5930879.4
381.2
NQ
CV5
CV24-637
DD
Land
414.8
156
-45
569052.6
5930284.4
389.9
NQ
CV5
CV24-638
DD
Land
314.1
338
-85
569855.8
5930433.4
378.0
NQ
CV5
CV24-639
DD
Land
194.0
355
-60
569682.3
5930336.1
382.1
NQ
CV5
CV24-641
DD
Land
302.0
161
-47
569599.0
5930401.7
382.0
NQ
CV5
CV24-643
DD
Water
394.9
160
-55
570074.0
5930705.6
371.7
NQ
CV5
CV24-644
DD
Land
434.0
158
-60
572151.2
5931550.8
375.9
NQ
CV5
CV24-645
DD
Land
296.0
152
-45
571748.5
5931540.1
393.4
NQ
CV5
CV24-646
DD
Land
251.0
338
-65
569855.6
5930433.6
378.1
NQ
CV5
CV24-648
DD
Land
484.9
180
-48
572564.4
5931724.7
374.6
NQ
CV5
CV24-650
DD
Land
206.2
156
-52
569167.5
5930265.5
397.0
NQ
CV5
CV24-651
DD
Land
289.9
161
-75
569598.8
5930402.1
382.0
NQ
CV5
CV24-652
DD
Water
362.0
158
-82
572424.0
5931416.3
371.9
NQ
CV5
CV24-654
DD
Land
581.1
140
-52
571748.8
5931540.6
393.2
NQ
CV5
CV24-655
DD
Land
197.5
338
-45
569855.4
5930434.1
378.0
NQ
CV5
CV24-657
DD
Land
11.7
0
-90
570732.5
5931935.6
379.3
HQ
North CV5
CV24-659
DD
Land
224.1
156
-55
569231.8
5930246.4
396.9
NQ
CV5
CV24-660
DD
Land
389.3
152
-55
570036.3
5930782.6
377.8
NQ
CV5
CV24-661
DD
Land
283.8
158
-50
569678.9
5930468.7
382.5
NQ
CV5
CV24-662
DD
Land
217.9
156
-45
569856.7
5930430.8
378.1
NQ
CV5
CV24-663
DD
Water
215.0
160
-60
570784.8
5930905.2
371.8
NQ3
CV5
CV24-664
DD
Land
400.9
158
-58
572151.4
5931550.8
375.9
NQ
CV5
CV24-666
DD
Water
467.2
0
-90
572401.4
5931430.2
373.0
NQ
CV5
CV24-667
DD
Land
529.9
179
-58
572564.7
5931725.3
374.6
NQ
CV5
CV24-668
DD
Land
254.0
158
-45
569410.0
5930345.5
389.3
NQ
CV5
CV24-669
DD
Land
281.0
158
-45
569965.3
5930554.4
376.3
NQ
CV5
CV24-671
DD
Land
209.0
160
-45
569762.7
5930394.7
380.1
NQ
CV5
CV24-672
DD
Land
11.7
0
-90
569572.4
5931586.2
376.4
HQ
North CV5
CV24-673
DD
Land
9.2
0
-90
570188.5
5931687.4
384.0
NQ
North CV5
CV24-674
DD
Land
546.0
150
-50
571673.2
5931541.5
396.8
NQ
CV5
CV24-675
DD
Land
490.9
145
-72
572151.5
5931550.8
375.9
NQ
CV5
CV24-676
DD
Land
207.5
145
-65
570036.3
5930783.1
377.8
NQ
CV5
CV24-677
DD
Land
347.0
235
-60
569963.3
5930554.0
376.4
NQ
CV5
CV24-678
DD
Land
299.1
158
-46
569504.8
5930370.1
383.3
NQ
CV5
CV24-679
DD
Water
125.0
340
-60
570814.8
5931002.4
372.0
NQ3
CV5
CV24-680
DD
Land
226.9
158
-45
569841.2
5930331.4
377.6
NQ
CV5
CV24-681
DD
Water
494.0
0
-90
572438.5
5931450.0
372.1
NQ
CV5
CV24-682
DD
Land
362.0
160
-48
570646.9
5931010.2
373.7
NQ
CV5
CV24-683
DD
Land
512.0
163
-56
572564.8
5931726.3
374.6
NQ
CV5
CV24-684
DD
Water
161.0
27
-60
570932.4
5930996.7
371.9
NQ3
CV5
CV24-685
DD
Land
299.0
160
-80
569743.0
5930442.0
379.2
NQ
CV5
CV24-686
DD
Land
209.0
160
-45
570249.5
5930646.4
384.3
NQ
CV5
CV24-687
DD
Land
503.0
134
-62
572151.7
5931551.1
375.9
NQ
CV5
CV24-688
DD
Water
344.1
152
-45
570832.5
5931093.5
371.9
NQ
CV5
CV24-689
DD
Land
167.0
11
-51
569705.4
5930476.0
380.2
NQ3
CV5
CV24-690
DD
Land
115.8
160
-45
569799.1
5930303.3
376.4
NQ
CV5
CV24-691
DD
Water
371.3
158
-46
572275.8
5931522.4
372.9
NQ
CV5
CV24-692
DD
Land
272.1
158
-75
570317.9
5930621.6
383.0
NQ
CV5
CV24-693
DD
Land
344.0
125
-45
570647.6
5931010.5
373.8
NQ
CV5
CV24-694
DD
Land
443.5
160
-48
571672.8
5931541.1
396.8
NQ
CV5
CV24-695
DD
Land
343.9
310
-70
569965.8
5930425.6
377.0
NQ
CV5
CV24-697
DD
Water
322.9
158
-45
570707.1
5930992.2
371.9
NQ
CV5
CV24-698
DD
Water
265.9
160
-59
572263.5
5931404.1
373.0
NQ
CV5
CV24-699
DD
Land
409.7
150
-58
572151.3
5931550.9
375.9
NQ
CV5
CV24-700
DD
Land
302.1
163
-45
569453.6
5930438.9
380.5
NQ
CV5
CV24-701
DD
Land
471.6
157
-59
571947.8
5931540.9
380.7
NQ
CV5
CV24-702
DD
Land
302.2
170
-50
571561.1
5931282.3
374.5
NQ
CV5
CV24-703
DD
Land
450.0
154
-50
571708.1
5931460.6
378.6
NQ
CV5
CV24-704
DD
Land
355.0
200
-50
571097.9
5931094.0
375.2
NQ
CV5
CV24-705
DD
Land
407.2
167
-73
570110.2
5930638.0
377.0
NQ
CV5
CV24-706
DD
Water
203.0
160
-45
571582.3
5931171.8
372.2
NQ
CV5
CV24-707
DD
Water
287.1
162
-48
570707.9
5930989.2
373.5
NQ
CV5
CV24-708
DD
Land
431.0
160
-61
572052.0
5931534.6
372.6
NQ
CV5
CV24-709
DD
Land
320.3
155
-73
571442.8
5931177.7
377.0
NQ
CV5
CV24-710
DD
Water
275.0
185
-55
571586.6
5931171.8
373.0
NQ
CV5
CV24-711
DD
Land
236.5
162
-63
571561.2
5931282.6
374.4
NQ
CV5
CV24-711A
DD
Land
368.0
162
-63
571560.9
5931282.6
374.4
NQ
CV5
CV24-712
DD
Land
371.1
150
-45
571616.1
5931411.0
375.6
NQ
CV5
CV24-713
DD
Water
161.2
175
-50
571509.5
5931133.2
373.0
NQ
CV5
CV24-714
DD
Land
449.1
159
-51
571947.9
5931540.8
380.9
NQ
CV5
CV24-715
DD
Water
317.1
150
-46
570511.7
5930943.5
373.0
NQ
CV5
CV24-716
DD
Water
145.9
158
-45
571371.3
5931036.7
373.0
NQ
CV5
CV24-717
DD
Land
353.0
167
-45
570110.3
5930637.3
377.0
NQ
CV5
CV24-718
DD
Land
425.0
148
-59
572052.2
5931534.7
372.7
NQ
CV5
CV24-719
DD
Land
305.0
158
-53
571132.6
5931145.0
376.3
NQ
CV5
CV24-720
DD
Water
117.9
158
-70
571371.3
5931037.1
372.9
NQ
CV5
CV24-721
DD
Land
402.8
142
-47
571616.4
5931411.0
375.4
NQ
CV5
CV24-722
DD
Water
137.0
158
-45
571097.7
5930963.1
373.0
NQ
CV5
CV24-723
DD
Water
95.1
158
-45
570575.5
5930788.3
373.0
NQ
CV5
CV24-724
DD
Land
356.1
152
-58
572011.7
5931467.0
375.7
NQ
CV5
CV24-725
DD
Land
503.0
155
-65
571311.7
5931087.6
380.0
NQ
CV5
CV24-726
DD
Water
97.8
158
-45
570998.1
5930944.0
373.0
NQ
CV5
CV24-727
DD
Land
446.9
146
-63
572052.3
5931534.8
372.7
NQ
CV5
CV24-728
DD
Water
83.1
158
-45
570667.0
5930827.1
373.0
NQ
CV5
CV24-730
DD
Land
305.0
160
-55
571336.9
5931165.8
375.9
NQ
CV5
CV24-731
DD
Water
101.1
158
-45
570899.1
5930925.1
373.0
NQ
CV5
CV24-732
DD
Water
268.9
158
-58
572212.3
5931385.5
373.0
NQ
CV5
CV24-733
DD
Land
392.2
145
-63
571561.7
5931282.9
374.5
NQ
CV5
CV24-734
DD
Water
122.0
158
-45
570847.3
5930912.0
373.0
NQ
CV5
CV24-735
DD
Land
404.2
155
-51
571653.2
5931324.2
376.8
NQ
CV5
CV24-736
DD
Land
383.1
158
-56
572214.1
5931534.1
373.2
NQ
CV5
CV24-737
DD
Water
415.8
170
-62
572324.5
5931536.8
373.0
NQ
CV5
CV24-738
DD
Water
119.0
160
-45
571292.1
5931011.9
373.0
NQ
CV5
CV24-739
DD
Land
401.0
158
-55
568598.9
5930071.1
388.9
NQ
CV5
CV24-740
DD
Land
536.1
125
-60
571312.4
5931088.5
380.1
NQ
CV5
CV24-741
DD
Land
496.5
170
-64
572051.9
5931534.5
372.6
NQ
CV5
CV24-742
DD
Land
509.8
188
-47
572565.1
5931727.7
373.7
NQ
CV5
CV24-743
DD
Water
85.8
158
-50
571497.3
5931041.6
372.9
NQ
CV5
CV24-744
DD
Water
196.9
158
-45
571570.8
5931124.5
373.0
NQ
CV5
CV24-745
DD
Land
515.2
175
-80
572213.8
5931534.5
373.3
NQ
CV5
CV24-746
DD
Land
369.2
158
-60
571977.8
5931451.6
376.5
NQ
CV5
CV24-748
DD
Water
386.0
155
-58
572324.9
5931538.5
372.1
NQ
CV5
CV24-749
DD
Land
305.0
158
-65
568474.2
5930093.9
399.8
NQ
CV5
CV24-750
DD
Water
443.0
160
-70
571220.1
5930923.9
372.8
NQ
CV5
CV24-751
DD
Land
431.0
150
-85
571286.3
5930893.2
377.4
NQ
CV5
CV24-752
DD
Land
494.1
159
-48
569965.8
5930738.0
376.0
NQ
CV5
CV24-753
DD
Water
345.6
175
-75
572328.8
5931537.4
373.4
NQ
CV5
CV24-755
DD
Land
536.0
194
-51
572564.8
5931727.8
373.6
NQ
CV5
CV24-756
DD
Land
253.9
158
-45
568474.5
5930093.4
399.7
NQ
CV5
CV24-758
DD
Land
506.1
145
-75
572213.9
5931534.8
373.2
NQ
CV5
CV24-759
DD
Land
93.0
158
-45
568479.6
5929966.6
388.9
NQ
CV5
CV24-760
DD
Water
428.0
115
-75
571080.9
5930873.1
373.0
NQ
CV5
CV24-764
DD
Land
77.0
158
-65
568479.8
5929966.0
388.8
NQ
CV5
CV24-765
DD
Water
358.9
0
-90
572445.5
5931369.9
373.4
NQ
CV5
CV24-766
DD
Land
90.0
158
-45
568433.9
5929939.3
391.1
NQ
CV5
CV24-767
DD
Land
326.0
159
-60
569819.4
5930506.5
375.4
NQ
CV5
CV24-769
DD
Land
374.0
170
-68
571579.6
5931234.4
374.9
NQ3
CV5
CV24-772
DD
Water
10.7
0
-90
571335.7
5931245.7
372.9
NQ
CV5
CV24-775
DD
Water
11.0
0
-90
571221.3
5931212.4
372.8
NQ
CV5
CV24-777
DD
Land
101.1
340
-75
568849.3
5930131.6
395.1
NQ3
CV5
CV24-779
DD
Water
13.0
0
-90
571098.5
5931194.9
372.8
NQ
CV5
CV24-780
DD
Land
9.1
0
-90
570917.1
5931288.1
375.9
HQ
CV5
CV24-781
DD
Land
200.1
330
-85
569283.5
5930125.5
388.4
NQ3
CV5
CV24-782
DD
Land
10.2
0
-90
570962.2
5931304.3
376.8
HQ
CV5
CV24-783
DD
Land
416.0
145
-67
571927.4
5931447.3
377.6
NQ3
CV5
CV24-784
DD
Land
32.0
0
-90
569257.8
5930042.2
388.2
HQ
CV5
CV24-785
DD
Land
3.9
0
-90
569751.1
5930197.0
387.0
NQ
CV5
CV24-786
DD
Land
25.3
0
-90
568840.8
5929943.2
389.2
NQ
CV5
CV24-787
DD
Land
18.5
0
-90
569063.2
5930258.1
392.4
NQ
CV5
CH22-001
TR
Land
2.1
342
-7
571342.6
5930847.1
375.9
n/a
CV5
CH22-002
TR
Land
3.9
165
-31
571340.7
5930846.3
374.8
n/a
CV5
CH22-003
TR
Land
1.9
346
-6
571377.5
5930850.9
375.4
n/a
CV5
CH22-007
TR
Land
7.3
340
-30
570151.2
5930541.4
383.0
n/a
CV5
CH24-098
TR
Land
3.6
152
0
570264.5
5930962.7
381.1
n/a
CV5
CH24-099
TR
Land
1.2
158
-10
570452.7
5931063.3
382.7
n/a
CV5
CH24-100
TR
Land
2.4
158
-18
570471.9
5931060.2
381.8
n/a
CV5
CH24-101
TR
Land
7.4
162
-3
570494.4
5931063.5
380.6
n/a
CV5
CH24-102
TR
Land
2.8
350
-44
570518.1
5931074.5
382.4
n/a
CV5
CH24-103
TR
Land
3.0
171
-21
570516.3
5931007.2
374.7
n/a
CV5
CH24-104
TR
Land
2.7
178
-47
570595.3
5931031.6
370.3
n/a
CV5
CH24-105
TR
Land
3.9
165
-14
570602.2
5931034.2
371.2
n/a
CV5
CH24-106
TR
Land
1.9
349
-20
570714.0
5931136.5
377.7
n/a
CV5
CH24-107
TR
Land
1.7
156
-13
570723.0
5931140.3
377.8
n/a
CV5
CH24-108
TR
Land
1.1
340
-7
570782.5
5931153.8
377.4
n/a
CV5
CH24-109
TR
Land
1.8
339
-16
570803.2
5931157.6
377.2
n/a
CV5
CH24-110
TR
Land
2.4
319
-17
570838.9
5931161.7
375.9
n/a
CV5
CH24-111
TR
Land
2.4
333
-16
570850.5
5931166.0
376.6
n/a
CV5
CH24-112
TR
Land
3.5
296
-18
570527.9
5930731.2
371.8
n/a
CV5
CH24-113
TR
Land
1.8
124
-15
570408.9
5930689.8
380.0
n/a
CV5
CH24-114
TR
Land
5.3
141
-34
570404.5
5930706.9
383.3
n/a
CV5
CH24-115
TR
Land
40.5
348
-10
570322.0
5930667.5
390.6
n/a
CV5
CH24-116
TR
Land
7.2
324
-10
570353.6
5930696.3
384.5
n/a
CV5
CH24-117
TR
Land
11.4
160
0
570253.6
5930684.0
380.6
n/a
CV5
CH24-118
TR
Land
6.0
160
-15
570253.0
5930640.6
383.6
n/a
CV5
CH24-119
TR
Land
2.1
158
-10
570234.3
5930627.9
381.5
n/a
CV5
CV1-CH01
TR
Land
8.0
0
0
571477.3
5931121.0
369.9
n/a
CV5
CV1-CH02
TR
Land
6.0
0
0
571393.9
5931098.8
381.9
n/a
CV5
CV1-CH03
TR
Land
11.0
0
0
571381.0
5931103.9
378.0
n/a
CV5
CV1-CH04
TR
Land
4.0
0
0
571340.5
5931110.5
377.7
n/a
CV5
CV1-CH05
TR
Land
11.0
0
0
571435.1
5931107.2
380.6
n/a
CV5
CV2-CH01
TR
Land
4.0
338
0
571299.6
5931156.1
379.6
n/a
CV5
CV2-CH02
TR
Land
4.0
355
0
571274.9
5931156.7
377.7
n/a
CV5
(1) Coordinate system NAD83 / UTM zone 18N; (2) DD = diamond drill, TR = 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
CV24-529
DD
Land
395.0
0
-90
565280
5928735.1
388.119
NQ
CV13
CV24-532
DD
Land
386.4
0
-90
565628.7
5928931.0
402.9
NQ
CV13
CV24-535
DD
Land
440.0
50
-65
565281.6
5928735.1
388.2
NQ
CV13
CV24-538
DD
Land
370.2
130
-60
565631.2
5928931.1
403.7
NQ
CV13
CV24-539
DD
Land
305.0
0
-65
565279.8
5928735.6
388.3
NQ
CV13
CV24-540
DD
Land
314.0
200
-65
565629.2
5928929.5
403.2
NQ
CV13
CV24-543
DD
Land
245.0
310
-65
565279.8
5928735.4
388.2
NQ
CV13
CV24-545
DD
Land
311.0
230
-50
565627.9
5928929.8
403.2
NQ
CV13
CV24-546
DD
Land
385.3
260
-65
565279.3
5928733.5
388.3
NQ
CV13
CV24-549
DD
Land
344.0
0
-70
565629.5
5928932.4
403.4
NQ
CV13
CV24-550
DD
Land
463.8
60
-60
565109.1
5928410.8
418.7
NQ
CV13
CV24-551
DD
Land
329.9
90
-55
565813.6
5928741.7
384.3
NQ
CV13
CV24-554
DD
Land
339.0
10
-60
565812.5
5928743.0
384.4
NQ
CV13
CV24-555
DD
Land
416.0
130
-58
565108.9
5928408.5
419.2
NQ
CV13
CV24-556
DD
Land
263.0
158
-45
565944.2
5928901.8
391.8
NQ
CV13
CV24-561
DD
Land
443.1
0
-65
565107.0
5928411.2
418.7
NQ
CV13
CV24-565
DD
Land
251.1
158
-45
566053.6
5928896.2
388.4
NQ
CV13
CV24-571
DD
Land
236.1
90
-65
565032.3
5928630.7
398.2
NQ
CV13
CV24-572
DD
Land
173.0
158
-45
565954.5
5928688.8
377.6
NQ
CV13
CV24-578
DD
Land
218.0
158
-75
565954.1
5928689.3
377.4
NQ
CV13
CV24-579
DD
Land
215.0
0
-90
565031.7
5928630.6
398.2
NQ
CV13
CV24-582
DD
Land
227.2
10
-65
565031.2
5928632.1
398.3
NQ
CV13
CV24-583
DD
Land
212.0
158
-45
566034.5
5928765.5
379.3
NQ
CV13
CV24-747
DD
Land
281.0
20
-60
565266.8
5928409.4
412.5
NQ
CV13
CV24-754
DD
Land
235.9
280
-65
565288.0
5928612.6
390.0
NQ
CV13
CV24-757
DD
Land
305.3
70
-45
565269.4
5928408.3
412.8
NQ
CV13
CV24-761
DD
Land
227.1
0
-90
565289.2
5928610.8
390.0
NQ
CV13
CV24-762
DD
Land
340.9
120
-45
565268.2
5928406.7
413.2
NQ
CV13
CV24-763
DD
Land
407.4
150
-65
565430.9
5928778.7
389.3
NQ
CV13
CV24-768
DD
Land
284.0
240
-45
565288.4
5928610.3
390.1
NQ
CV13
CV24-770
DD
Land
220.9
0
-90
565129.6
5928730.6
395.0
NQ
CV13
CV24-771
DD
Land
164.3
0
-90
565267.5
5928407.2
413.1
NQ
CV13
CV24-773
DD
Land
200.0
35
-55
565291.6
5928615.0
389.7
NQ
CV13
CH22-008
TR
Land
3.0
134
-10
565327.4
5927991.9
412.9
n/a
CV13
CH22-009
TR
Land
3.5
314
-20
565327.4
5927991.9
412.9
n/a
CV13
CH22-010
TR
Land
5.2
341
-20
565319.8
5927982.1
412.8
n/a
CV13
CH22-011
TR
Land
1.5
164
-7
565290.2
5927974.0
411.6
n/a
CV13
CH22-012
TR
Land
5.3
344
-18
565290.2
5927974.0
411.6
n/a
CV13
CH22-013
TR
Land
2.5
168
-13
565276.5
5927969.0
409.5
n/a
CV13
CH22-014
TR
Land
2.8
348
-10
565276.5
5927969.0
409.5
n/a
CV13
CH22-015
TR
Land
1.3
151
-20
565261.4
5927948.5
406.3
n/a
CV13
CH22-016
TR
Land
0.8
331
-5
565261.4
5927948.5
406.3
n/a
CV13
CH22-017
TR
Land
13.1
161
-15
565008.4
5927781.9
396.5
n/a
CV13
CH22-018
TR
Land
1.6
7
-5
564999.3
5927781.8
397.9
n/a
CV13
CH22-019
TR
Land
8.9
187
-10
564999.3
5927781.8
397.9
n/a
CV13
CH22-020
TR
Land
3.5
1
-10
564958.2
5927787.0
398.7
n/a
CV13
CH22-021
TR
Land
3.6
181
-10
564958.2
5927787.0
398.7
n/a
CV13
CH22-022
TR
Land
8.4
14
-15
564933.1
5927793.5
397.7
n/a
CV13
CH22-023
TR
Land
3.0
356
-30
564859.2
5927784.0
392.7
n/a
CV13
CH22-024
TR
Land
5.8
176
-10
564859.2
5927784.0
392.7
n/a
CV13
CH22-025
TR
Land
4.9
185
-20
563820.5
5928027.6
401.3
n/a
CV13
CH22-026
TR
Land
9.2
15
-20
563820.5
5928027.6
401.3
n/a
CV13
CH22-027
TR
Land
3.5
2
-10
564543.7
5927827.8
394.5
n/a
CV13
CH22-028
TR
Land
1.6
182
-25
564543.7
5927827.8
394.5
n/a
CV13
CH22-029
TR
Land
3.8
344
-8
564430.7
5927891.8
400.2
n/a
CV13
CH22-030
TR
Land
1.1
164
-25
564430.7
5927891.8
400.2
n/a
CV13
CH22-031
TR
Land
3.1
340
-20
564313.4
5927935.4
402.1
n/a
CV13
CH22-032
TR
Land
1.2
160
-5
564313.4
5927935.4
402.1
n/a
CV13
CH22-033
TR
Land
1.7
349
-15
564317.7
5927922.5
403.6
n/a
CV13
CH22-034
TR
Land
1.5
169
-25
564317.7
5927922.5
403.6
n/a
CV13
CH22-035
TR
Land
1.6
166
-10
564318.2
5927920.4
403.4
n/a
CV13
CH22-036
TR
Land
9.3
340
-10
564229.2
5927961.3
403.6
n/a
CV13
CH22-037
TR
Land
4.8
160
-5
564229.2
5927961.3
403.6
n/a
CV13
CH23-058
TR
Land
6.7
200
-20
564428.8
5927877.0
397.6
n/a
CV13
CH23-059
TR
Land
16.7
185
-25
564395.4
5927899.8
401.0
n/a
CV13
CH23-060
TR
Land
5.1
200
-10
564381.8
5927886.9
398.6
n/a
CV13
CH23-061
TR
Land
13.4
200
-15
564356.1
5927920.0
402.7
n/a
CV13
CH23-062
TR
Land
14.9
180
-15
565813.8
5928472.6
379.6
n/a
CV13
CH23-063
TR
Land
8.5
180
-21
565793.4
5928462.2
380.7
n/a
CV13
CH23-064
TR
Land
13.9
160
-15
565774.8
5928454.4
382.6
n/a
CV13
CH23-065
TR
Land
27.9
180
-15
565757.6
5928430.0
384.6
n/a
CV13
CH23-066
TR
Land
11.9
180
-10
565743.4
5928420.7
386.2
n/a
CV13
CH23-067
TR
Land
4.5
180
-15
565668.3
5928403.0
390.8
n/a
CV13
CH23-068
TR
Land
6.2
148
-18
565459.7
5928331.7
404.0
n/a
CV13
CH23-069
TR
Land
6.8
26
-36
565393.2
5928283.7
418.1
n/a
CV13
CH23-070
TR
Land
3.7
5
-5
565414.5
5928118.5
414.7
n/a
CV13
CH23-071
TR
Land
6.4
160
-25
565358.5
5928074.7
415.8
n/a
CV13
CH24-072
TR
Land
1.7
2
-5
563771.9
5928048.3
399.7
n/a
CV13
CH24-073
TR
Land
6.3
5
-2
563799.8
5928042.7
401.2
n/a
CV13
CH24-074
TR
Land
5.9
192
0
563813.3
5928061.1
400.0
n/a
CV13
CH24-075
TR
Land
9.1
193
0
563874.6
5928029.5
394.3
n/a
CV13
CH24-076
TR
Land
15.0
194
-5
563871.0
5928024.7
395.1
n/a
CV13
CH24-077
TR
Land
1.8
206
-40
563957.0
5927996.4
390.2
n/a
CV13
CH24-078
TR
Land
5.6
183
-19
564022.9
5927993.7
394.0
n/a
CV13
CH24-079
TR
Land
11.0
194
-5
564100.6
5927981.6
398.9
n/a
CV13
CH24-080
TR
Land
8.9
189
0
564210.7
5927964.2
399.3
n/a
CV13
CH24-081
TR
Land
6.4
208
-2
564248.0
5927961.9
402.0
n/a
CV13
CH24-082
TR
Land
3.4
195
-30
564462.6
5927864.0
392.8
n/a
CV13
CH24-083
TR
Land
20.1
203
-5
564555.1
5927846.2
392.6
n/a
CV13
CH24-084
TR
Land
7.8
210
-5
564542.6
5927853.1
392.3
n/a
CV13
CH24-085
TR
Land
8.4
211
-5
564524.5
5927840.3
392.3
n/a
CV13
CH24-086
TR
Land
18.8
200
0
564848.3
5927794.0
388.5
n/a
CV13
CH24-087
TR
Land
14.6
142
-5
565392.2
5928063.3
414.6
n/a
CV13
CH24-088
TR
Land
11.3
145
-5
565432.1
5928320.3
405.0
n/a
CV13
CH24-089
TR
Land
1.1
140
-5
565418.1
5928300.1
409.9
n/a
CV13
(1) Coordinate system NAD83 / UTM zone 18N; (2) DD = diamond drill, TR = channel; (3) DD azimuths and dips presented are those 'planned' and may vary off collar/downhole.
Section 1 – Sampling Techniques and Data
Criteria
JORC Code explanation
Commentary
Sampling techniques
Drilling techniques
Drill sample recovery
Logging
Sub-sampling techniques and sample preparation
Quality of assay data and laboratory tests
Verification of sampling and assaying
Location of data points
Data spacing and distribution
Orientation of data in relation to geological structure
Sample security
Audits or reviews
Section 2 – Reporting of Exploration Results
Criteria
JORC Code explanation
Commentary
Mineral tenement and land tenure status
Exploration done by other parties
Geology
Drill hole Information
Data aggregation methods
Relationship between mineralization widths and intercept lengths
Diagrams
Balanced reporting
Other substantive exploration data
Further work
Section 3 – Estimate and Reporting of Mineral Resources
Criteria
JORC Code explanation
Commentary
Database integrity
Site visits
Geological interpretation
Dimensions
Estimation and modelling techniques
Moisture
Cut-off parameters
Mining factors or assumptions
Metallurgical factors or assumptions
Environmental factors or assumptions
Bulk density
Classification
Audits or reviews
Discussion of relative accuracy/ confidence
Company Name
Project Name
Stage
Inclusive of Reserves
Measured
Indicated
Inferred
Information Source(s)
Mt
Li2O (%)
Mt
Li2O (%)
Mt
Li2O (%)
AVZ Minerals Limited 75% / La Congolaise d'Exploitation Minière SA 25%
Manono
Development
Y
132.0
1.7 %
367.0
1.6
324.0
1.6 %
ASX announcement dated January 31, 2024
(IGO Limited & Tianqi Lithium Corporation) 51% / Albemarle Corporation 49%
Greenbushes
Production
Y
1.0
2.6 %
390.0
1.5 %
49.0
1.1 %
ASX announcement dated 20 February 2025
Pilbara Minerals Ltd.
Pilgangoora
Production
Y
16.5
1.3 %
314.4
1.2 %
76.6
1.1 %
Annual Report 2024
Ganfeng Lithium Group Co., Ltd.
Goulamina
Production
Y
13.1
1.6 %
94.9
1.4 %
159.2
1.3 %
ASX announcement dated July 1, 2024
Sociedad Química y Minera de Chile S.A. 50% / Wesfarmers Ltd. 50%
Mt. Holland
Production
Y
74.2
1.4 %
104.0
1.3 %
33.4
1.2 %
Annual Report 2024
Mineral Resources Ltd. 50% / Albemarle Corporation 50%
Wodgina
Production
Y
–
–
162.5
1.1 %
28.9
1.1 %
SEC filing dated February 12, 2025
Liontown Resources Ltd.
Kathleen Valley
Production
Y
19.0
1.3 %
109.0
1.4 %
26.0
1.3 %
ASX announcement dated October 30, 2024
Patriot Battery Metals Inc.
Shaakichiuwaanaan
Development
–
–
–
108.0
1.4 %
33.3
1.3 %
TSX announcement herein
Sigma Lithium Corporation
Grota do Cirilo
Production
Y
45.8
1.4 %
47.4
1.4 %
13.7
1.4 %
Investor Presentation April 2025
Rio Tinto Ltd.
Galaxy
Development
Y
–
–
55.4
1.2 %
55.9
1.3 %
Arcadium 2023 10-K
Sinomine Resource Group Co., Ltd.
Bikita
Production
–
42.2
1.2 %
27.3
1.0 %
43.8
0.9 %
SZ announcement dated April 1, 2024
Sayona Mining Ltd. 60% / Investissement Québec 40%
Moblan
Development
Y
6.0
1.5 %
59.1
1.2 %
28.0
1.1 %
ASX announcement dated August 27, 2024
Albemarle Corporation
Kings Mountain
Development
–
–
–
46.8
1.4 %
42.9
1.1 %
SEC filing dated February 15, 2023
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
NAL
Production
Y
0.9
1.1 %
71.1
1.1 %
15.8
1.1 %
ASX announcement dated August 27, 2024
Winsome Resources Ltd.
Adina
Development
–
–
–
61.4
1.1 %
16.5
1.2 %
ASX announcement dated May 28, 2024
Pilbara Minerals Ltd.
Colina
Development
–
28.6
1.3 %
38.6
1.2 %
3.6
1.1 %
ASX announcement dated May 30, 2024
Frontier Lithium Inc. 92.5% / Mitsubishi Corporation 7.5%
PAK + Spark
Development
–
1.3
2.1 %
24.7
1.6 %
32.5
1.4 %
NI 43-101 technical report dated February 28, 2023
Wildcat Resources Ltd.
Tabba Tabba
Development
–
–
–
70.0
1.0 %
4.1
0.8 %
ASX announcement dated Novemeber 28, 2024
Rio Tinto Ltd. 50% / Investissement Québec 50%
Whabouchi
Development
Y
–
–
46.0
1.4 %
8.3
1.3 %
S-K 1300 Technical Report dated September 8, 2023
Lithium Ionic Corp.
Bandeira
Development
Y
3.3
1.4 %
20.4
1.3 %
18.3
1.4 %
Press release dated April 24,2024
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
Carolina
Development
Y
–
–
28.2
1.1 %
15.9
1.0 %
Press release dated October 21,2021
Critical Elements Lithium Corporation
Rose
Development
Y
–
–
30.6
0.9 %
2.4
0.8 %
TSX announcement dated August 29, 2023
AMG Lithium GmbH
Mibra
Production
-
3.4
1.0 %
16.9
1.1 %
4.2
1.0 %
Euronext announcement dated April 3, 2017
Green Technology Metals Ltd.
Root
Development
-
–
–
10.0
1.3 %
10.1
1.1 %
ASX announcement dated April 3, 2025
Li-FT Power Ltd.
Big East
Development
-
–
–
–
–
16.5
1.1 %
TSXV announcement dated October 1, 2024
SCR-Sibelco NV 60% / Avalon Advanced Materials Inc. 40%
Separation Rapids
Development
-
4.3
1.3 %
8.7
1.4 %
2.3
1.5 %
TSX announcement dated February 27, 2025
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
Authier
Development
Y
6.0
1.0 %
8.1
1.0 %
2.9
1.0 %
ASX announcement dated April 14, 2023
Lithium Ionic Corp.
Baixa Grande
Development
-
1.1
1.2 %
5.4
1.1 %
12.9
1.0 %
Press release dated January 14, 2025
Li-FT Power Ltd.
Fi Main and SW
Development
-
–
–
–
–
13.8
1.0 %
TSXV announcement dated October 1, 2024
Rock Tech Lithium Inc.
Georgia Lake
Development
Y
–
–
10.6
0.9 %
4.2
1.0 %
TSX announcement dated November 15, 2022
Green Technology Metals Ltd.
Seymour
Development
-
–
–
6.1
1.3 %
4.1
0.7 %
ASX announcement dated November 17, 2023
Cygnus Metals Ltd. 51% / Stria Lithium Inc. 49%
Pontax
Development
-
–
–
–
–
10.1
1.0 %
ASX announcement dated August 14, 2023
Note: Mineral resources are presented on a 100% basis and inclusive of reserves where noted. Estimates may have been prepared under different estimation and reporting regimes and may not be directly comparable. Patriot Battery Metals accepts no responsibility for the accuracy of peer mineral resource data as presented. Details on the tonnes, category, grade, and cut-off for mineral resources of each company noted herein are found within the respective information sources provided. Data compiled as of April 11, 2025.
Company Name
Project Name
Stage
Proven
Probable
Information Source(s)
Mt
Li2O (%)
Mt
Li2O (%)
AVZ Minerals Limited 75% / La Congolaise d'Exploitation Minière SA 25%
Manono
Development
65.0
1.6 %
66.6
1.6 %
AVZ FY23 Financial Report
(IGO Limited & Tianqi Lithium Corporation) 51% / Albemarle Corporation 49%
Greenbushes
Production
1.0
2.6 %
171.0
1.9 %
ASX announcement dated 20 February 2025
Pilbara Minerals Ltd.
Pilgangoora
Production
14.0
1.3 %
194.7
1.2 %
Annual Report 2024
Ganfeng Lithium Group Co., Ltd.
Goulamina
Production
8.1
1.6 %
43.9
1.5 %
Leo Lithium Annual Report 2024
Sociedad Química y Minera de Chile S.A. 50% / Wesfarmers Ltd. 50%
Mt. Holland
Production
40.0
1.6 %
45.8
1.4 %
Annual Report 2024
Mineral Resources Ltd. 50% / Albemarle Corporation 50%
Wodgina
Production
–
–
115.8
1.3 %
SEC filing dated February 12, 2025
Liontown Resources Ltd.
Kathleen Valley
Production
3.7
1.2 %
65.5
1.3 %
FY24 Annual Report
Patriot Battery Metals Inc.
Shaakichiuwaanaan
Development
–
–
–
–
Sigma Lithium Corporation
Grota do Cirilo
Production
39.9
1.3 %
36.4
1.3 %
Investor Presentation April 2025
Rio Tinto Ltd.
Galaxy
Development
–
–
37.3
1.3 %
Arcadium 2023 10-K
Sinomine Resource Group Co., Ltd.
Bikita
Production
–
–
–
–
Sayona Mining Ltd. 60% / Investissement Québec 40%
Moblan
Development
–
–
34.5
1.4 %
ASX announcement dated November 19, 2024
Albemarle Corporation
Kings Mountain
Development
–
–
–
–
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
NAL
Production
0.2
1.1 %
19.9
1.1 %
ASX announcement dated November 19, 2024
Winsome Resources Ltd.
Adina
Development
–
–
–
–
Pilbara Minerals Ltd.
Colina
Development
–
–
–
–
Frontier Lithium Inc. 92.5% / Mitsubishi Corporation 7.5%
PAK + Spark
Development
–
–
–
–
Wildcat Resources Ltd.
Tabba Tabba
Development
–
–
–
–
Rio Tinto Ltd. 50% / Investissement Québec 50%
Whabouchi
Development
10.5
1.4 %
27.7
1.3 %
S-K 1300 Technical Report dated September 8, 2023
Lithium Ionic Corp.
Bandeira
Development
2.3
1.2 %
14.9
1.2 %
Bandeira Lithium Project Araçuaí–Itinga NI 43-101 Feasibility Study Technical Report
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
Carolina
Development
–
–
18.3
1.1 %
ASX announcement dated November 19, 2024
Critical Elements Lithium Corporation
Rose
Development
–
–
26.3
0.9 %
TSX announcement dated August 29, 2023
AMG Lithium GmbH
Mibra
Production
–
–
–
–
Green Technology Metals Ltd.
Root
Development
–
–
–
–
Li-FT Power Ltd.
Big East
Development
–
–
–
–
SCR-Sibelco NV 60% / Avalon Advanced Materials Inc. 40%
Separation Rapids
Development
–
–
–
–
Sayona Mining Ltd. (pending merger with Piedmont Lithium Inc.)
Authier
Development
6.2
0.9 %
5.1
1.0 %
ASX announcement dated November 19, 2024
Lithium Ionic Corp.
Baixa Grande
Development
–
–
–
–
Li-FT Power Ltd.
Fi Main and SW
Development
–
–
–
–
Rock Tech Lithium Inc.
Georgia Lake
Development
–
–
7.3
0.8 %
TSX announcement dated November 15, 2022
Green Technology Metals Ltd.
Seymour
Development
–
–
–
–
Cygnus Metals Ltd. 51% / Stria Lithium Inc. 49%
Pontax
Development
–
–
–
–
Note: Mineral reserves are presented on a 100% basis. Estimates may have been prepared under different estimation and reporting regimes and may not be directly comparable. Patriot Battery Metals accepts no responsibility for the accuracy of peer mineral reserve data as presented. Details on the tonnes, category, grade, and cut-off for mineral reserves of each company noted herein are found within the respective information sources provided. Data compiled as of April 11, 2025.
Company Name
Project Name
Stage
Inclusive of Reserves
Measured
Indicated
Inferred
Information Source(s)
Mt
Ta2O5 (ppm)
Mt
Ta2O5 (ppm)
Mt
Ta2O5 (ppm)
Pilbara Minerals Ltd.
Pilgangoora
Production
Y
16.5
144
314
106
76.6
124
Annual Report 2024
AVZ Minerals Limited 75% / La Congolaise d'Exploitation Minière SA 25%
Manono
Development
Y
132.0
44
367
42
342.0
51
ASX announcement dated January 31, 2024
Patriot Battery Metals Inc.
Shaakichiuwaanaan
Development
–
–
–
108
166
33.3
156
TSX announcement herein
Liontown Resources Ltd.
Kathleen Valley
Production
Y
19.0
149
109
131
26.0
118
ASX announcement dated October 30, 2024
Zhejiang Huayou Cobalt Co., Ltd.
Arcadia
Development
Y
15.8
113
46
124
11.2
119
ASX announcement dated October 11, 2021
AMG Lithium GmbH
Mibra
Production
–
3.4
359
17
335
4.2
337
Euronext announcement dated April 3, 2017
Andrada Mining Ltd.
Uis
Production
–
27.3
110
18
105
32.7
89
AIM announcement dated February 6, 2025
Frontier Lithium Inc. 92.5% / Mitsubishi Corporation 7.5%
PAK + Spark
Development
–
1.3
94
25
108
32.5
113
NI 43-101 technical report dated February 28, 2023
Sinomine Resource Group Co., Ltd.
Tanco
Production
–
3.0
1,120
1
960
0.1
790
2024 Annual Report
Delta Lithium Ltd.
Yinnetharra Tantalum
Development
–
–
–
27
95
12.9
117
ASX announcement dated March 31, 2025
Wildcat Resources Ltd.
Tabba Tabba
Development
–
–
–
70
65
4.1
80
ASX announcement dated Novemeber 28, 2024
Critical Elements Lithium Corporation
Rose
Development
Y
–
–
31
118
2.4
129
TSX announcement dated August 29, 2023
Delta Lithium Ltd.
Mt Ida
Development
–
–
–
8
224
6.8
154
ASX announcement dated October 3, 2023
Global Lithium Resources Ltd.
Manna
Development
–
–
–
33
52
18.7
50
ASX announcement dated June 12, 2024
Rio Tinto
Mt Cattlin
Development
Y
0.2
154
10
155
4.8
177
ASX announcement dated November 28, 2025
Green Technology Metals Ltd.
Seymour
Development
–
–
–
6
149
4.1
100
ASX announcement dated November 17, 2023
Note: Mineral resources are presented on a 100% basis and inclusive of reserves where noted. Estimates may have been prepared under different estimation and reporting regimes and may not be directly comparable. Patriot Battery Metals accepts no responsibility for the accuracy of peer mineral resource data as presented. Details on the tonnes, category, grade, and cut-off for mineral resources of each company noted herein are found within the respective information sources provided. Data compiled as of April 11, 2025.
Company Name
Project Name
Stage
Proven
Probable
Information Source(s)
Mt
Ta2O5 (%)
Mt
Ta2O5 (%)
Pilbara Minerals Ltd.
Pilgangoora
Production
14.0
131
194.7
101
Annual Report 2024
AVZ Minerals Limited 75% / La Congolaise d'Exploitation Minière SA 25%
Manono
Development
65.0
–
66.6
–
AVZ FY23 Financial Report
Patriot Battery Metals Inc.
Shaakichiuwaanaan
Development
–
–
–
–
Liontown Resources Ltd.
Kathleen Valley
Production
3.7
176
65.5
120
FY24 Annual Report
Zhejiang Huayou Cobalt Co., Ltd.
Arcadia
Development
11.8
114
30.5
123
ASX announcement dated October 11, 2021
AMG Lithium GmbH
Mibra
Production
–
–
–
–
Andrada Mining Ltd.
Uis
Production
–
–
–
–
Frontier Lithium Inc. 92.5% / Mitsubishi Corporation 7.5%
PAK + Spark
Development
–
–
–
–
Sinomine Resource Group Co., Ltd.
Tanco
Production
–
–
–
–
Delta Lithium Ltd.
Yinnetharra Tantalum
Development
–
–
–
–
Wildcat Resources Ltd.
Tabba Tabba
Development
–
–
–
–
Critical Elements Lithium Corporation
Rose
Development
–
–
26.3
138
TSX announcement dated August 29, 2023
Delta Lithium Ltd.
Mt Ida
Development
–
–
–
–
Global Lithium Resources Ltd.
Manna
Development
–
–
–
–
Rio Tinto
Mt Cattlin
Development
0.1
126
3.6
113
Green Technology Metals Ltd.
Seymour
Development
–
–
–
–
Note: Mineral reserves are presented on a 100% basis. Estimates may have been prepared under different estimation and reporting regimes and may not be directly comparable. Patriot Battery Metals accepts no responsibility for the accuracy of peer mineral reserve data as presented. Details on the tonnes, category, grade, and cut-off for mineral reserves of each company noted herein are found within the respective information sources provided. Data compiled as of April 11, 2025.
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 108.0 Mt at 1.40% Li2O Indicated, and 33.3 Mt at 1.33% Li2O Inferred, and ranks as the largest lithium pegmatite resource in the Americas, and the 8th largest lithium pegmatite resource in the world. Shaakichiuwaanaan also holds significant potential for other critical and strategic metals including tantalum, cesium, and gallium.
A Preliminary Economic Assessment ("PEA") was announced for the CV5 Pegmatite (lithium) on August 21, 2024, and highlights Shaakichiuwaanaan as a potential North American lithium raw materials powerhouse. The PEA outlines the potential for a competitive and globally significant high-grade lithium project targeting up to ~800 ktpa spodumene concentrate using a simple Dense Media Separation ("DMS") only process flowsheet.
1 Shaakichiuwaanaan (CV5 & CV13) Mineral Resource Estimate (108.0 Mt at 1.40% Li2O, 166 ppm Ta2O5 and 66 ppm Ga, Indicated, and 33.3 Mt at 1.33% Li2O, 156 ppm Ta2O5 ppm, and 65 ppm Ga, Inferred) is reported at a cut-off grade of 0.40% Li2O (open-pit), 0.60% Li2O (underground CV5), and 0.70% Li2O (underground CV13) with an Effective Date of January 6, 2025 (through drill hole CV24-787). Mineral resources are not mineral reserves as they do not have demonstrated economic viability.
For further information, please contact us at [email protected] 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
This news release contains "forward-looking statements" within the meaning of applicable securities laws. 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 facts are forward-looking statements that involve risks and uncertainties. Forward-looking statements are typically identified by words or expressions such as "impending", "remains on track", "growth", "potential", "to be", "future", "advances towards", "on the path to", "further", "on schedule", "long-term", "strategy" and similar words or expressions. Forward-looking statements include, but are not limited to, statements concerning: the timing of the feasibility study and an MRE update, the potential for production, the cost of production and the potential benefits thereof, the significant potential for further resource growth in lithium and other critical and strategic metals at the Property through continued drill exploration, the Company's position to provide long-term future spodumene supply and other critical metals to the North American and European markets, and the recoverability of tantalum, cesium, and gallium as by-products.
Forward-looking statements are 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 statements. There can be no assurance that forward-looking 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 MRE 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. If any of the risks or uncertainties mentioned above, which are not exhaustive, materialize, actual results may vary materially from those anticipated in the forward-looking statements. Readers should not place undue reliance on forward-looking statements.
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.
The production target from the PEA referred to in this release was reported by the Company in accordance with ASX Listing Rule 5.16 on August 21, 2024. The Company confirms that, as of the date of this announcement, all material assumptions and technical parameters underpinning the production target in the original announcement continue to apply and have not materially changed.
View original content to download multimedia:https://www.prnewswire.com/news-releases/significant-mineral-resource-upgrade-at-shaakichiuwaanaan-lithium-project-to-underpin-impending-feasibility-study-302452400.html
SOURCE Patriot Battery Metals Inc.
© Canada Newswire, source Canada Newswire English