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LIGHTNING MINERALS LTD Capital/Financing Update 2025

Jan 16, 2025

65212_rns_2025-01-16_7ee436f3-d1fb-4e4f-949c-ed8bc75609b3.pdf

Capital/Financing Update

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Confirmation of Spodumene and Additional Strong Lithium Soil Sampling Results in Brazil Supports Drill Program for Q1 2025

ASX Announcement 1 7 Ja n u a r y 2 0 2 5

Lightning Minerals (L1M or the Company) is pleased to announce the confirmation of spodumene minerals discovered within pegmatites at the Esperança Project in Brazil’s Lithium Valley region of Minas Gerais. Additionally, the highest tenor lithium assays to date from its soil sampling programs at the Caraíbas and Esperança projects, also located in the Lithium Valley have been received. Peak soil assays of up to 429ppm Lithium have been returned at Caraíbas and 320ppm Lithium at Canabrava.

The confirmation of spodumene as the lithium bearing mineral via Raman spectrographic analysis further demonstrates the significance of the recent discovery at Esperança (ASX Announcement 18[th] November 2024) and the upcoming 2,000m drill program. Drill contractor engagement is now being finalised.

HIGHLIGHTS

  • Spodumene Minerals confirmed via Raman Spectroscopy at Esperança project

  • Highest tenor lithium results to date returned from Caraíbas and Canabrava with results up to 429ppm Lithium and 320ppm Lithium respectively

  • Procurement of drilling contractors and logistics progressing well for inaugural drilling campaign of up to 2,000m diamond drilling at Esperança due to begin during Q1 2025

Lightning Minerals Managing Director Alex Biggs said , “Further excellent results across our projects in Brazil provide even greater confidence in the potential prospectivity of both project areas and the region. The past 6-months have been significant for the Company in providing strong drill targets and allowing us to both develop an exploration thesis and drill target priorities. As we move towards our first drill campaign in Brazil el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 at Esperança we look ahead to another busy and productive year that has the potential to deliver significant results and a step change for the Company. I have always believed in being aggressive in our exploration strategy and with the results and targets we have generated so far in Brazil believe in the potential this region holds for us.”.

Spodumene Confirmation through Raman Spectroscopy at Esperança Project

During geological mapping fieldwork conducted in mid-November 2024 field geologists encountered a previously unknown historical artisanal mine within the Esperança project area. Pegmatitic lithologies were present in the walls of the excavations which displayed elongate crystals up to 50cm of suspected spodumene. Selective mineral specimen grab samples were collected and analysed via a SciAps Z-903 handheld LIBS (Laser-Induced Breakdown Spectroscopy) device which returned a qualitative lithium endowment of up to 4.04% Li2O. While the lithium content analyses using the LIBS device was considered positive, the mineral species containing the lithium had not yet been confirmed.

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Selectively sampled mineral specimens were sent to Perth for analyses using a Bruker BRAVO Raman spectrometer. The results confirm the presence of spodumene as the lithium bearing mineral with 5 samples returning positive spectral responses consistent with the mineral data library for spodumene (Table 1 and Figure 2).

Table 1: Raman analyses results for spodumene within selective sampling of mineral specimens at Esperança Project

Sample ID Raman SpectroscopyIdentified Minerals
LMBR0005 Kaolinite
LMBR0006 Albite + Kaolinite
LMBR0007 Kaolinite
LMBR0008 Kaolinite
LMBR0009 Spodumene + Kaolinite
LMBR0010 Albite + Kaolinite
LMBR0011 Albite + Kaolinite
LMBR0012 Muscovite + Albite
LMBR0013 Spodumene + Kaolinite
LMBR0014 Spodumene + Kaolinite
LMBR0015 Spodumene + Kaolinite
LMBR0016 Spodumene + Kaolinite + Wodginite

The Raman test work has also confirmed the high degree of weathering of the mineral specimens, with all but one sample returning spectral response consistent with kaolin for samples that retain a crystal habit. This result suggests the weathering profile of the sampled horizon is high, where precursor minerals have been substantially weathered.

Mineral specimen LMBR0016 contained an accessory opaque mineral which was not readily identified by field geologists. The Raman test work has returned a strong spectral response consistent with Wodginite, which is a Manganese-Tin-Tantalum oxide.

To avoid the highly weathered supergene profile present at the Esperança spodumene occurrence the upcoming proposed drill program will be targeting depths greater than 30m below surface which is the interpreted base of complete oxidation in the local area. Whole rock laboratory sample analysis supports the el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 degree of weathering of the pegmatite samples with lithium content peaking at 0.38% Li2O for sample VLM207. The full suite of analytical data and spatial locations for all whole rock samples is available within (Appendix 1, Table 2, and Figure 4).

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 1: (Left) Photograph of highly weathered spodumene sample LMBR0009, ( Right ) Photograph of highly weathered spodumene sample LMBR0016 showing accessory wodginite in left crystal face (dark mineral)

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Figure 2: (A) Example of Spodumene spectral response of sample LMBR0009, ( B ) Sample LMBR0009 also presents strong Kaolin spectral response which supports weathered interpretation, (C) Example of Spodumene response of sample LMBR0016, (D) Accessory Wodginite mineral in sample LMBR0016

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el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Phase 1 Soil Sampling Campaign Completion – All Projects

Final analytical results for the remaining 1,061 Soil Samples completed across the Caraíbas, Canabrava and Esperança projects are now available. Results are positive with the highest lithium tenor anomalism returned to date occurring at the Caraíbas and Canabrava project areas of 429ppm Lithium and 320ppm Lithium respectively.

Esperança Soil Results

The soil sampling program at Esperança was primarily designed to test for lithium at a tenement scale with collection of 465 samples planned along 400m spaced N-S orientated sample lines. The discovery of a spodumene bearing pegmatites in the northwest corner of the tenement during the beginning of the sampling program resulted in the addition of further 191 samples at a closer line spacing at 100m.

The results for the program are shown in Figure 3. The majority of anomalous results occur within the infilled area in the northwest, with results above 60ppm lithium clustered around the spodumene occurrence, and the target for the Company’s inaugural drill program. An isolated peak result of 144ppm lithium is recorded in sample SOLM1315 which will receive follow up investigation.

Figure 3: Soil sampling (lithium) results at the Esperança project (labelled samples over 100ppm Lithium)

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el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 4: Soil sampling and rock chip sampling locations (lithium) at the Esperança project

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Drill targeting will continue to focus on the spodumene occurrence at Esperança with the thesis that the spodumene bearing pegmatite dips toward to the southeast toward the centre of the tenement.

Caraíbas Soil Results

Soil results for the remaining 213 samples taken at the Caraíbas project show high tenor soil responses for lithium. Sampling proximal to an artisanal mine with known lithium mineral occurrences of lepidolite (ASX Announcement 22 April 2024) has returned elevations up to 429ppm Lithium, with several adjacent samples el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 returning values over 200ppm Lithium which is considered a high response for residual soils of Salinas Formation in the region (Figure 5).

The results are currently being investigated with follow up site visits underway to ascertain if outcropping geology at the sites can explain the magnitude of the lithium response. The results of field investigations will feed into the ongoing drill targeting and prioritisation exercise with a view to potentially developing new high priority targets post completion of the Esperança drilling campaign. This will be targeted at the identified lithium in soil anomaly extending approximately 2km with peak results up to 239ppm Lithium (ASX Announcement 02 December 2024).

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 5: Soil sampling (lithium) results at the Caraíbas project. Previously reported soil results within western most tenement 831424/2013 are shaded

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Canabrava Soil Results

Soil results for 59 infill samples, and 78 new primary samples are now available for the Canabrava project. The infill soil sampling program was designed to follow up previous results where samples on 400m spaced sample lines returned results up to 113ppm Lithium (ASX Announcement 03 October 2024). The infill samples have been collected on a reduced line spacing of 100m and show consistent lithium anomalism el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806 >80ppm which coincides with mapped pegmatites over a 700m strike length (Figure 6). The ability to sample further east into the tenement is truncated by the transition from residual sediments of the Salinas Formation into tertiary depositional sediments which are considered a poor proxy for targeting lithium.

A small 78 sample program was also completed in the south-eastern areas of the Canabrava project in residual Salinas Formation sediments. Results are shown in Figure 7. The two easternmost sample lines have consistent lithium values above 200ppm with a peak result of 320ppm. Infill sampling at this location is being considered as part of the drill targeting and prioritisation exercise.

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 6: Infill Soil sampling (lithium) results at the Canabrava project

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Figure 7: Soil sampling (lithium) results and updated geological mapping at the Canabrava project

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el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Ongoing Works in Brazil

Drill contractor engagement is now underway for the Company’s inaugural 2,000m drill campaign at Esperança due to begin in Q1 2025. Plans are also underway for drilling at Caraíbas which will be targeted at the identified lithium in soil anomaly extending approximately 2km with peak results up to 239ppm Lithium (ASX Announcement 02 December 2024).

Results for the Phase 1 soil sampling campaign have now been returned in full. Further target generation is now underway. Further infill soil programs may be considered where results require further definition prior to moving to drill testing. Prioritisation of the current suite of targets is now being undertaken to ensure the most robust targets and tested via drilling in the first pass.

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 8: Lightning Minerals’ Brazilian tenements in regional context of the Lithium Valley region of Minas Gerais

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el 6 505 Little Collins St Melbourne VIC 3000 Australia | [email protected] | (08) 9429 8806
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Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Figure 9: Local project location of Lightning Minerals’ Brazilian lithium projects

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Approved for release by the Board of Directors

-END-

More information at www.lightningminerals.com.au

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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ABOUT LIGHTNING MINERALS

Lightning Minerals is a mineral exploration company, listed on the Australian Securities Exchange (ASX:L1M) and focused on the exploration of critical minerals and lithium at its tenements across Western Australia. The acquisition of the Caraíbas, Canabrava and Esperança lithium projects in Minas Gerais, Brazil are potentially transformational to the Company’s success in the lithium sector. The Company also owns the Dundas project in the prolific Dundas region of Western Australia, the Dalmas and Hiver lithium projects in Quebec, Canada, another significant and evolving lithium region globally . The Company also holds other projects in Western Australia which include Mt Bartle and Mailman Hill which are prospective for base metals and critic al minerals.

FORWARD LOOKING STATEMENTS

Information included in this release constitutes forward-looking statements. Often, but not always, forward looking statements can generally be identified by the use of forward-looking words such as “may”, “will”, “expect”, “intend”, “plan”, “estimate”, “anticipate”, “continue”, and “guidance”, or other similar words and may include, without limitation, statements regarding plans, strategies and objectives of management, anticipated production or construction commencement dates and expected costs or production outputs.

Forward looking statements inherently involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance and achievements to differ materially from any future results, performance or achievements. Relevant factors may include, but are not limited to, changes in commodity prices, foreign exchange fluctuations and general economic conditions, increased costs and demand for production inputs, the speculative nature of exploration and project development, including the risks of obtaining necessary licences and permits and diminishing quantities or grades of reserves, political and social risks, changes to the regulatory framework within which the Company operates or may in the future operate, environmental conditions including extreme weather conditions, recruitment and retention of personnel, industrial relations issues and litigation. Forward looking statements are based on the Company and its management’s good faith assumptions relating to the financial, market, regulatory and other relevant environments that will exist and affect the Company’s business and operations in the future. The Company does not give any assurance that the assumptions on which forward looking statements are based will prove to be correct, or that the Company’s business or operations will not be affected in any material manner by these or oth er factors not foreseen or foreseeable by the Company or management or beyond the Company’s control.

Although the Company attempts and has attempted to identify factors that would cause actual actions, events or results to dif fer materially from those disclosed in forward looking statements, there may be other factors that could cause actual results, performance, achievements or events not to be as anticipated, estimated or intended, and many events are beyond the reasonable control of the Company. Accordingly, readers are cautioned not to place undue reliance on forward looking statements. Forward looking statements in these materials speak only at the date of issue. Subject to any continuing obligations under applicable law or any relevant stock exchange listing rules, in providing this information the Company does not undertake any obligation to publicly update or revise any of the forward-looking statements or to advise of any change in events, conditions or circumstances on which any such statement is based.

COMPETENT PERSONS STATEMENT

The information contained herein that relates to exploration results is based on information compiled or reviewed by Mr Jarrad Woodland, who is a Competent Person and a member of the Australasian Institute of Mining and Metallurgy. Mr Woodland is a full-time employee of the Company. Mr Woodland has sufficient experience which is relevant to the style of mineralisation and types of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Persons as defined in the 2012 Edition of the ‘Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves’. Mr Woodland consents to the inclusion of his name in the matters based on the information in the form and context in which it appears. Mr Woodland holds options in Lightning Minerals.

REFERENCES TO PREVIOUS ANNOUNCEMENTS

The Company confirms that it is not aware of any new information or data that materially affects the information included in the original market announcements, and that all material assumptions and technical parameters have not materially changed. The Company also confirms that the form and context in which the Competent Person’s findings are presented have not been materially modified from the original market announcement.

Level 11 40 The Esplanade Perth WA 6000 Australia | [email protected] | (08) 9429 8806

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Appendix 1: Brazilian Projects – JORC Code 2012 Table 1 Criteria

The Table below summarises the assessment and reporting criteria used for exploration results for the Exploration Projects and reflects the guidelines in Table 1 of The Australasian Code for the Reporting of Exploration Results, Mineral Resources and Ore Reserves (The JORC 2012 Code).

Section 1 - Sampling Techniques and Data

Criteria JORC Code explanation Commentary
Sampling techniques Nature and quality of sampling (eg cut channels, random chips, or
specific specialised industry standard measurement tools appropriate to
the minerals under investigation, such as down hole gamma sondes, or
handheld XRF instruments, etc). These examples should not be taken as
limiting the broad meaning of sampling.
Include reference to measures taken to ensure sample representivity and
the appropriate calibration of any measurement tools or systems used.
Aspects of the determination of mineralisation that are Material to the
Public Report.
In cases where ‘industry standard’ work has been done this would be
relatively simple (eg ‘reverse circulation drilling was used to obtain 1 m
samples from which 3 kg was pulverised to produce a 30 g charge for fire
assay’). In other cases more explanation may be required, such as where
there is coarse gold that has inherent sampling problems. Unusual
commodities or mineralisation types (eg submarine nodules) may
warrant disclosure of detailed information.

Data in this document relates to Raman Spectroscopy, geochemical soil and rock chip sampling, field visual identification of
minerals, and SciAps Z-903 Handheld LIBS (Laser-Induced Breakdown Spectroscopy)

Mineral samples for VLM207 were collected at the discretion of field geologists targeting spodumene minerals to confirm
the mineral species. The LIB’s test work on these samples relates only to a fraction of the mineral and does not represent
the whole rock lithium content, which is now available and contained within Appendix 1, Table 2 below.

Raman Spectroscopy is a chemical analysis technique which involves illuminating a substance with a laser and analysing the
light that is scattered off the surface of the substance. The scattered light can provide a lot of information about the
substance and its structure, and can be used to identify, characterize, and quantify many chemical components.

Soil sampling is a reconnaissance stage exploration technique which may indicates the geochemical parameters of the
underlying or nearby bedrock geology. Mineralised lithologies of the target commodity may elevate elemental proportions
in the soil and provide vectors toward location the mineralised body.

Soil samples were collected using pick and shovel from depths of approximately 30cm below the surface.

Rockchip samples were collected at the discretion of the field geologist, this method is appropriate given the early stage of
exploration at the Caraíbas Project

Approximately 200g of material from the deepest sample horizon is passed through a 2mm sieve, with the -2mm retained
for assay.

All samples were submitted to SGS Geosol Laboratórios Ltd’ of Belo Horizonte.

Sampling was carried out using Lightning Minerals procedures and QAQC processes as per current industry standard
practice.

Sample site locations are recorded using a Garmin Map 62s handheld device and are reported in projection SIRGAS 2000 /
UTM 23S
Drilling techniques Drill type (eg core, reverse circulation, open-hole hammer, rotary air
blast, auger, Bangka, sonic, etc) and details (eg core diameter, triple or
standard tube, depth of diamond tails, face-sampling bit or other type,
whether core is oriented and if so, by what method, etc).

No drilling is being reported
Drill sample recovery Method of recording and assessing core and chip sample recoveries
and results assessed. Measures taken to maximise sample recovery and
ensure representative nature of the samples.
Whether a relationship exists between sample recovery and grade and
whether sample bias may have occurred due to preferential loss/gain
of fine/coarse material.

No drilling is being reported
Logging Whether core and chip samples have been geologically and
geotechnically logged to a level of detail to support appropriate
Mineral Resource estimation, mining studies and metallurgical studies.

No drilling is being reported

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Whether logging is qualitative or quantitative in nature. Core (or
costean, channel, etc) photography.
The total length andpercentage of the relevant intersections logged.
Sub-sampling techniques
and sample preparation

If core, whether cut or sawn and whether quarter, half or all core
taken.
If non-core, whether riffled, tube sampled, rotary split, etc and whether
sampled wet or dry.
For all sample types, the nature, quality and appropriateness of the
sample preparation technique.
Quality control procedures adopted for all sub-sampling stages to
maximise representivity of samples.
Measures taken to ensure that the sampling is representative of the in
situ material collected, including for instance results for field
duplicate/second-half sampling.
Whether sample sizes are appropriate to the grain size of the material
being sampled.

Soil Samples are collected in the field into small kraft cardboard bags and are 200gm per unit.

Rock chip samples are approximately 1-3kg and are collected into pre numbered calico bags.

Industry standard QAQC practices of field duplicates and the appropriate use of laboratory provided Certified Reference
Material for low level lithium are used for all laboratory sample submissions. Field Duplicates are utilised by the company
at a rate of 1:50 samples.
Quality of assay data and
laboratory tests

The nature, quality and appropriateness of the assaying and laboratory
procedures used and whether the technique is considered partial or
total.
For geophysical tools, spectrometers, handheld XRF instruments, etc,
the parameters used in determining the analysis including instrument
make and model, reading times, calibrations factors applied and their
derivation, etc.
Nature of quality control procedures adopted (eg standards, blanks,
duplicates, external laboratory checks) and whether acceptable levels
of accuracy (ie lack of bias) and precision have been established.

All samples were submitted to SGS Geosol Laboratórios Ltd’ of Belo Horizonte Minas Gerais Brazil.

Analysis procedures are considered appropriate for Lithium and Multi element analysis.

Samples are prepared and analysed using SGS technique PRS80J and are analysed via optical emission spectroscopy analysis
using code ICP90A. Determination by Fusion with Sodium Peroxide - ICP OES.

Soil samples - Elements analysed at ppm limits for include Al, As, B, Ba, Be, Ca, Cd, Co, Cr, Cu, Fe, K, La, Li, Mg, Mn, Mo, Nb,
Ni, P, Pb, Sb, Sc, Sn, Sr, Ta, Ti, V, W, Y, Zn

Rock Chip - Elements analysed at ppm limits include Ag, Al,As, B,Ba, Be,Bi, Ca,Cd, Ce,Co, Cr, Cs, Cu, Dy, Er, Eu, Fe, Ga, Gd,
Ge, Hf, Ho, In, K, La, Li, Lu, Mg, Mn, Mo, Nb, Nd, Ni, P, Pb, Pr, Rb, Sb, Sc, Sm, Sn, Sr, Ta, Tb, Th, Ti, Tl, Tm, U, V, W, Y, Yb, Zn,
Zr

Laboratory CRM material has been utilised at this early stage of exploration works.

A SciAps Z-903 LIBS device was been used for spot sample readings of minerals of interest within sample VLM207. The
device is calibrated each day, and before analysis is begun. QAQC standards are used every 10-15 readings as consistency
checks. Readings times are approximately 3 to 5 seconds and are standard for the device. The device is calibrated to a
lithium profile supplied by SciAps prior to use.

Handheld LIBS is expected to differ from laboratory assay results and can read above theoretical maximum values. They
should not be used to replace assays or indicate whole rock grade which are now available in Appendix 1, Table 2 below.
Verification of sampling
and assaying

The verification of significant intersections by either independent or
alternative company personnel.
The use of twinned holes.
Documentation of primary data, data entry procedures, data
verification, data storage (physical and electronic) protocols.
Discuss any adjustment to assay data.

No verification will be undertaken for these initial samples as they will not be used in any resource estimate.

The samples are to determine the levels of Li and other valuable elements in soil samples.
Location of data points Accuracy and quality of surveys used to locate drill holes (collar and
down-hole surveys), trenches, mine workings and other locations used
in Mineral Resource estimation.
Specification of the grid system used.

Handheld Garmin GPS instruments were used to geo locate each sample location, these instruments are understood to be
accurate within a ±5m in the horizontal and vertical planes.

The level of topographic control offered by a handheld GPS is considered sufficient for early exploration activities.

All samples were collected in the SIRGAS 2000/UTM zone 23S

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Data spacing and
distribution
Orientation of data in
relation to geological
structure
Sample security
Audits or reviews
Quality and adequacy of topographic control.
Data spacing for reporting of Exploration Results.
Whether the data spacing, and distribution is sufficient to establish the
degree of geological and grade continuity appropriate for the Mineral
Resource and Ore Reserve estimation procedure(s) and classifications
applied.
Whether sample compositing has been applied.

The soil and rock chip sample spacing is considered appropriate for the reporting of the exploration results.

No Mineral Resource or Ore Reserve Estimates have been completed.
Whether the orientation of sampling achieves unbiased sampling of
possible structures and the extent to which this is known, considering
the deposit type.
If the relationship between the drilling orientation and the orientation
of key mineralised structures is considered to have introduced a
sampling bias, this should be assessed and reported if material.

The collection of soil and rock chip sampling data was targeted as best possible at this early stage of exploration activities.
The measures taken to ensure sample security.
The chain of custody for sampling procedures and sample analysis was managed by the contract geological consultants
duringcollection
The results of any audits or reviews of sampling techniques and data.
No audits or reviews of sampling techniques have been conducted to date.

Section 2 - Reporting of Exploration Results

Criteria JORC Code explanation Commentary
Mineral tenement and
land tenure status
Type, reference name/number, location and ownership including
agreements or material issues with third parties such as joint ventures,
partnerships, overriding royalties, native title interests, historical sites,
wilderness or national park and environmental settings.
The security of the tenure held at the time of reporting along with any
known impediments to obtaining a licence to operate in the area.




The Esperança, Canabrava, and Caraíbas Projects are located approximately 18km south-south east of the town of Salinas,
Minas Gerais, Brazil.

The Esperança Project area totals ~11.1km2and comprises one exploration licence 301033/2013

The Caraíbas Project area totals ~17.3km2 and comprises 5 granted exploration licences 831.514/2018, 832.041/2011,
831.424/2013, 832.763/2014, and 830.313/2014

The Canabrava Project area totals ~16.7km2and comprises two granted exploration licences 830440/2015 and 830439/2015

The Tenements are considered ingood standingat the time of this report.
Exploration done by other
parties

Acknowledgment and appraisal of exploration by other parties.

The Projects are at a very early stage of exploration and little to no recorded work has been completed by prior explorers.

Recent exploration has included a small reconnaissance explorationprogram by project vendor Bengal Mining.
Geology Deposit type, geological setting and style of mineralisation.
No known mineral deposits occur within project tenure.

Project geology comprises Neoproterozoic age sedimentary rocks of Araçuaí Orogen intruded by pegmatites interpreted to
originate from the fractionation of magmatic fluids from the peraluminous S-type post tectonic granitoids of Araçuaí Orogen.

The target commodityis hardrock lithium within lithium-caesium-tantalumpegmatites.
Drill hole Information A summary of all information material to the understanding of the
exploration results including a tabulation of the following information for all
Material drill holes:
o
easting and northing of the drill hole collar
o
elevation or RL (Reduced Level – elevation above sea
level in metres) of the drill hole collar
o
down hole length and interception depth,
o
hole length.



No drillhole information is reported.

No material information has been excluded from this report, laboratory analytical results have been adequately
communicated and described within the body of this report.

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If the exclusion of this information is justified on the basis that the
information is not Material and this exclusion does not detract from the
understanding of the report, the Competent Person should clearly explain
why this is the case.

Data aggregation
methods
In reporting Exploration Results, weighting averaging techniques, maximum
and/or minimum grade truncations (eg cutting of high grades) and cut-off
grades are usually Material and should be stated.
Where aggregate intercepts incorporate short lengths of high-grade results
and longer lengths of low grade results, the procedure used for such
aggregation should be stated and some typical examples of such
aggregations should be shown in detail.




No levelling of the raw geochemical data was undertaken.

Plan images have been generated using QGIS software.

No metal equivalent values are reported.
Relationship between
mineralisation widths
and intercept lengths
These relationships are particularly important in the reporting of Exploration
Results. If the geometry of the mineralisation with respect to the drill hole
angle is known, its nature should be reported. If it is not known and only the
down hole lengths are reported, there should be a clear statement to this
effect(eg ‘down hole length, true width not known’).





No drillhole information is reported.

There is insufficient data provided by the mapping and geochemical results contained within this report for a relationship
between pegmatite and mineral resources to be reported.
Diagrams Appropriate maps and sections (with scales) and tabulations of intercepts
should be included for any significant discovery being reported These should
include, but not be limited to a plan view of drill hole collar locations and
appropriate sectional views.




Appropriate reporting of results has been included in the body of this announcement; the plans, or lack thereof suitably
represent the nature of the results.
Balanced reporting Where comprehensive reporting of all Exploration Results is not practicable,
representative reporting of both low and high grades and/or widths should
bepracticed to avoid misleading reporting of Exploration Results.



Comprehensive reporting of soil and rock chip geochemical results within the Projects has been included in Appendix 1.
Other substantive
exploration data
Other exploration data, if meaningful and material, should be reported
including (but not limited to): geological observations; geophysical survey
results; geochemical survey results; bulk samples – size and method of
treatment; metallurgical test results; bulk density, groundwater,
geotechnical and rock characteristics; potential deleterious or
contaminating substances.



All meaningful data and relevant information have been included in the body of the report.
Further work The nature and scale of planned further work (e.g., tests for lateral
extensions or depth extensions or large-scale step-out drilling). Diagrams
clearly highlighting the areas of possible extensions, including the main
geological interpretations and future drilling areas, provided this
information is not commercially sensitive.



Follow up infill soil sampling is currently being planned and is expected to begin imminently, however at the time of reporting
the program has not yet begun.

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==> picture [843 x 53] intentionally omitted <==

Appendix 1 - Table 1: Soil Sampling Assays >150ppm lithium

Sample ID Project Easting (UTM 23S) Northing (UTM 23S) Be (ppm) Li (ppm) Nb (ppm) Sn (ppm) Ta (ppm) W (ppm) Y (ppm)
SOLM0143 Caraíbas 800022 8195453 2.5 173 22 25 23 25 33
SOLM0150 Caraíbas 800050 8195109 6 160 20 25 12 25 29
SOLM0178 Caraíbas 800052 8193758 12 154 20 25 12 25 21
SOLM0191 Caraíbas 800450 8195453 2.5 153 41 25 21 25 41
SOLM0196 Caraíbas 800450 8195204 10 239 45 25 5 25 37
SOLM0197 Caraíbas 800432 8195154 9 157 41 25 12 25 30
SOLM0207 Caraíbas 800451 8194703 9 181 49 25 5 25 33
SOLM0279 Caraíbas 800849 8194997 7 160 30 25 5 25 42
SOLM0299 Caraíbas 801252 8194095 7 155 14 25 5 25 12
SOLM0612 Caraíbas 803247 8196163 16 208 12 25 20 25 37
SOLM0613 Caraíbas 803249 8196118 25 277 16 25 26 25 59
SOLM0615 Caraíbas 803254 8196017 11 183 18 25 16 25 95
SOLM0616 Caraíbas 803253 8195966 7 168 5 25 18 25 80
SOLM0618 Caraíbas 803250 8195868 10 156 11 25 17 25 94
SOLM0677 Caraíbas 803687 8195535 12 226 5 25 23 25 45
SOLM0680 Caraíbas 803657 8195379 12 216 5 25 15 25 36
SOLM0688 Caraíbas 803650 8195031 9 159 13 25 27 25 41
SOLM0724 Caraíbas 804053 8195110 9 186 5 25 5 25 45
SOLM0725 Caraíbas 804052 8195165 10 188 5 25 16 25 50
SOLM0726 Caraíbas 804052 8195211 11 229 5 25 5 25 39
SOLM0727 Caraíbas 804051 8195257 13 396 5 25 5 25 36
SOLM0728 Caraíbas 804053 8195308 13 429 5 25 5 25 34
SOLM0729 Caraíbas 804051 8195363 11 227 5 25 13 25 42
SOLM0730 Caraíbas 804047 8195412 17 254 12 25 22 25 71
SOLM0731 Caraíbas 804054 8195464 12 189 10 25 5 25 37
SOLM0732 Caraíbas 804054 8195514 8 202 5 25 10 25 36
SOLM0733 Caraíbas 804056 8195566 12 192 5 25 5 25 32
SOLM0734 Caraíbas 804054 8195612 14 265 12 25 5 25 33
SOLM0735 Caraíbas 804051 8195662 14 286 11 25 5 25 41

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Sample ID Caraíbas Easting (UTM 23S) Northing (UTM 23S) Be (ppm) Li (ppm) Nb (ppm) Sn (ppm) Ta (ppm) W (ppm) Y (ppm)
SOLM0736 Caraíbas 804052 8195717 15 268 10 25 11 25 35
SOLM0737 Canabrava 804051 8195759 11 182 5 25 12 25 28
SOLM1129 Canabrava 800590 8188995 7 160 13 25 5 25 44
SOLM1134 Canabrava 800606 8189255 10 164 18 25 20 25 20
SOLM1149 Canabrava 801382 8189090 8 155 11 25 12 25 38
SOLM1152 Canabrava 801380 8188939 14 175 5 25 23 25 43
SOLM1175 Canabrava 802189 8188919 12 187 5 25 11 25 64
SOLM1186 Canabrava 802568 8188911 10 170 19 25 19 25 54
SOLM1187 Canabrava 802984 8188883 18 228 20 25 17 25 73
SOLM1188 Canabrava 802981 8188932 11 264 11 25 13 25 39
SOLM1189 Canabrava 803000 8188969 13 320 26 25 21 25 62
SOLM1190 Canabrava 802958 8189027 15 238 23 25 17 25 72
SOLM1191 Canabrava 802983 8189078 11 230 5 25 10 25 71
SOLM1192 Canabrava 802982 8189126 8 263 11 25 5 25 47
SOLM1193 Canabrava 802981 8189179 9 231 5 25 13 25 43
SOLM1202 Canabrava 803383 8189221 8 220 5 25 5 25 30
SOLM1203 Canabrava 803384 8189171 14 225 5 25 5 25 42
SOLM1204 Canabrava 803380 8189126 9 213 5 25 5 25 47
SOLM1205 Canabrava 803385 8189076 10 203 11 25 5 25 40
SOLM1206 Canabrava 803386 8189029 15 181 5 25 5 25 41
SOLM1207 Canabrava 803385 8188979 16 223 5 25 5 25 34
SOLM1208 Canabrava 803383 8188927 9 215 5 25 5 25 38
SOLM1209 Caraíbas 803383 8188879 14 168 5 25 5 25 35
SOLM1214 Caraíbas 803748 8194777 11 160 5 25 5 25 37
SOLM1224 Caraíbas 803856 8194770 14 381 5 25 5 25 27

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Appendix 1 - Table 2: Rock Chip Sampling Assays

Sample ID Project Easting (UTM 23S) Northing (UTM 23S) Be (ppm) Li (ppm) Nb (ppm) Sn (ppm) Ta (ppm) W (ppm) Y (ppm)
VLM009 Caraíbas 803852 8194803 13 36 5 11 5 50 5.61
VLM022 Caraíbas 803896 8194826 8 44 12 23 5 50 2.99
VLM029 Caraíbas 803255 8194579 7 15 5 7 5 50 2.41
VLM030 Caraíbas 803234 8194603 8 33 5 2.5 5 50 4.9
VLM032 Caraíbas 803185 8194636 7 11 5 2.5 5 50 11.35
VLM039 Caraíbas 803451 8195112 10 50 5 2.5 5 50 1.27
VLM055 Caraíbas 803227 8195722 31 28 5 2.5 5 50 1.04
VLM072 Caraíbas 794984 8192062 218 5 84 43 88 50 20.79
VLM080 Caraíbas 794614 8192526 227 5 122 15 57 50 2.96
VLM107 Caraíbas 795258 8193586 187 28 97 28 40 50 3.24
VLM122 Canabrava 794653 8192722 161 27 109 47 40 50 1.68
VLM138 Esperança 792121 8187833 51 23 43 11 15 50 7.52
VLM149 Esperança 791982 8187642 12 15 17 7 5 50 2.55
VLM157 Esperança 792170 8187904 29 15 47 2.5 14 50 7.1
VLM163 Esperança 791996 8187840 70 13 89 32 55 50 7.64
VLM165 Esperança 791937 8187715 11 49 29 13 5 50 2.96
VLM176 Esperança 792478 8187543 2.5 39 10 6 5 50 1.83
VLM177 Esperança 792455 8187566 8 233 21 19 5 50 3.5
VLM179 Esperança 792329 8187637 24 49 49 30 18 50 6.57
VLM181 Esperança 792275 8187672 6 34 14 6 5 50 3.14
VLM186 Esperança 792402 8187770 20 38 34 11 12 50 4.65
VLM199 Esperança 793145 8187908 10 30 35 70 5 50 55.42
VLM206 Esperança 792704 8187639 21 434 14 551 23 50 5.58
VLM207 Esperança 792674 8187621 26 1775 43 944 55 50 8.45
VLM208 Esperança 792674 8187624 8 39 18 20 5 50 2.16
VLM209 Esperança 792676 8187623 2.5 37 5 19 5 50 1.91
VLM210 Esperança 792673 8187622 24 265 233 539 46 50 1.47
VLM211 Esperança 792675 8187622 53 29 38 11 5 283 49.46
SRL001 Esperança 792693 8187679 7 153 52 18 5 50 10.47

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Sample ID Project Easting (UTM 23S) Northing (UTM 23S) Be (ppm) Li (ppm) Nb (ppm) Sn (ppm) Ta (ppm) W (ppm) Y (ppm)
SRL002 Esperança 792693 8187679 2.5 39 5 6 5 50 3.55
SRL003 Esperança 792699 8187641 154 1130 69 1141 117 50 9.12
SRL004 Esperança 792699 8187641 22 76 85 88 120 50 12.81
SRL005 Esperança 792254 8187678 22 26 39 16 15 50 10.85
SRL006 Esperança 792449 8187561 166 43 75 25 36 50 25.74
SRL007 Canabrava 794748 8192381 2.5 19 5 7 5 50 4.1
SRL008 Esperança 792536 8187475 31 1325 169 373 30 50 5.67
SRL009 Esperança 792795 8187714 11 34 32 17 5 50 1.48
SRL010 Esperança 792417 8187715 6 51 36 19 5 50 1.51

Appendix 2 - Table 1: Reporting Visual Estimates of Mineralisation

Project Sample ID Geology/Comments
Esperança VLM207 Spodumene mineral species are confirmed for sample VLM207 through laboratory use of a Bruker BRAVO Raman spectrometer. The proportion of
spodumene minerals are reported as visual estimates only and mineral percentages are shown in Appendix 2 Table 2 below.
Whole Rock lithium content is shown in Appendix 1 Table 2 above.

Appendix 2 - Table 2: All Pegmatite Field Descriptions Within the Esperança Project

Sample ID Easting
(UTM 23S)
Northing
(UTM 23S)
Lithology Campaign Primary
Minerals
(Major >30%)
Secondary
Minerals
(Minor >5%
and <30%)
Accessory
Minerals
(Trace <5%)
Boulder
/In-Situ
Comments
VLM009 803852 8194803 Pegmatite 2024 Feldspar Muscovite,
Quartz
Outcrop Large pegmatite, rich muscovite, albite, and quartz
VLM022 803896 8194826 Pegmatite 2024 Muscovite,
Feldspar
Schlorite Outcrop Pegmatite with very rich muscovite, schorlite and
feldspar
VLM029 803255 8194579 Pegmatite 2024 Feldspar Muscovite,
Quartz
Outcrop Artisanal digging, composed quartz, albite and
muscovite, small tunnel
VLM030 803234 8194603 Pegmatite 2024 Feldspar Muscovite,
Quartz
Outcrop Old artisanal digging, pegmatite composed by albite,
quartz and muscovite

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Sample ID Easting
(UTM 23S)
Northing
(UTM 23S)
Lithology Campaign Primary
Minerals
(Major >30%)
Secondary
Minerals
(Minor >5%
and <30%)
Accessory
Minerals
(Trace <5%)
Boulder
/In-Situ
Comments
VLM032 803185 8194636 Pegmatite 2024 Quartz Feldspar Outcrop Old Artisanal digging, composed by core quartz and
edge feldspar
VLM039 803451 8195112 Pegmatite 2024 Quartz Feldspar Outcrop Pegmatite with quartz core and edge feldspar, Old
digging
VLM055 803227 8195722 Pegmatite 2024 Feldspar Muscovite,
Quartz
Outcrop Large block pegmatite with feldspar, muscovite, and
quartz
VLM072 794984 8192062 Pegmatite 2024 Muscovite,
Quartz
Feldspar,
Tourmaline
Float Pegmatite fine, with light green muscovite, quartz,
feldspar and tourmaline
VLM080 794614 8192526 Pegmatite 2024 Feldspar Outcrop Pegmatite, coarse feldspar
VLM107 795258 8193586 Pegmatite 2024 Feldspar,
Quartz
Tourmaline Float Block rolled pegmatite with tourmaline, coarse and fine
VLM122 794653 8192722 Pegmatite 2024 Quartz,
Tourmaline
Muscovite,
Feldspar
Outcrop In drainage subcrop pegmatite fine, composed by
quartz, tourmaline, muscovite, and albite
VLM138 792121 8187833 Pegmatite 2024 Quartz,
Tourmaline
Muscovite,
Feldspar
Outcrop Pegmatite rich tourmaline, quartz, muscovite, and
feldspar
VLM149 791982 8187642 Pegmatite 2024 Feldspar,
Quartz
Tourmaline Outcrop In drainage subcrop pegmatite coarse tourmaline rich
and muscovite
VLM157 792170 8187904 Pegmatite 2024 Feldspar,
Quartz
Tourmaline,
Muscovite
Outcrop Large outcrop pegmatite, composed by tourmaline,
feldspar, quartz and muscovite,
VLM163 791996 8187840 Pegmatite 2024 Feldspar,
Quartz
Muscovite Float Pegmatite composed quartz, albite, and light green
muscovite
VLM165 791937 8187715 Pegmatite 2024 Feldspar Quartz Outcrop Largepegmatite, concordant with foliation
VLM176 792478 8187543 Pegmatite 2024 Quartz,
Tourmaline
Muscovite,
Feldspar
Outcrop Subcrop pegmatite, texture graphic, composed by
quartz, tourmaline, feldspar, and muscovite
VLM177 792455 8187566 Pegmatite 2024 Quartz,
Muscovite
Feldspar Outcrop Old digging in pegmatite, rich quartz, muscovite, and
feldspar.
VLM179 792329 8187637 Pegmatite 2024 Feldspar,
Tourmaline
Quartz,
Muscovite
Outcrop Large outcrop pegmatite, composed by tourmaline,
feldspar, quartz,and muscovite
VLM181 792275 8187672 Pegmatite 2024 Muscovite,
Quartz
Feldspar,
Tourmaline
Outcrop Large coarse and fine pegmatite outcrop, width 5
meters, composed by quartz, muscovite, feldspar, and
tourmaline schorlite

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Sample ID Easting
(UTM 23S)
Northing
(UTM 23S)
Lithology Campaign Primary
Minerals
(Major >30%)
Secondary
Minerals
(Minor >5%
and <30%)
Accessory
Minerals
(Trace <5%)
Boulder
/In-Situ
Comments
VLM186 792402 8187770 Pegmatite 2024 Feldspar,
Tourmaline
Quartz,
Muscovite
Outcrop Large coarse and fine pegmatite outcrop rich
tourmaline, feldspar, quartz and muscovite. Width 20
meters
VLM199 793145 8187908 Pegmatite 2024 Muscovite,
Quartz
Feldspar,
Tourmaline
Outcrop Subcrop pegmatite rich muscovite light green and small
tourmaline
VLM206 792704 8187639 Pegmatite -
Spodumene
2024 Feldspar Quartz,
Muscovite
Spodumene Outcrop Digging, large pegmatite containing crystals of highly
altered spodumene
VLM207 792674 8187621 Pegmatite -
Spodumene
2024 Quartz,
Spodumene
Feldspar,
Muscovite
Outcrop Selective mineral sample selection for analysis from
Artisanal mine in zoned pegmatite. Spodumene
sampled zone(55%quartz and 35% spodumene)
VLM208 792674 8187624 Pegmatite 2024 Feldspar Quartz,
Muscovite,
Tourmaline
Garnet,
Spodumene,
Tantalite
and beryl
Outcrop Artisanal mine in zoned pegmatite. Gallery with quartz
plus spodumene zone (55% quartz and 5% spodumene)
VLM209 792676 8187623 Pegmatite 2024 Feldspar Quartz Float Feldspar - concentrated, minor quartz
VLM210 792673 8187622 Pegmatite 2024 Muscovite Feldspar Float Large light green muscovite concentrate
VLM211 792675 8187622 Pegmatite 2024 Feldspar Columbite,
Tantalite?
Float Dark mineral, possible columbite or tantalite
SRL001 792693 8187679 Pegmatite 2024 Feldspar,
Muscovite
Quartz,
Schorlite
Outcrop Trench in pegmatite that ended in schist. Kf, radial
white mica, qtz, Ox. Mn, schorlite.
SRL002 792693 8187679 Pegmatite 2024 Feldspar,
Muscovite
Quartz,
Schorlite
Outcrop Trench in pegmatite that ended in schist. Kf, radial
white mica, qtz, Ox. Mn, schorlite.
SRL003 792699 8187641 Pegmatite -
Spodumene
2024 Feldspar,
Quartz
Muscovite Spodumene Outcrop Highly weathered spodumene within Feld+Qtz+Musc,
two samples taken
SRL004 792699 8187641 Pegmatite -
Spodumene
2024 Feldspar,
Quartz
Muscovite Spodumene Outcrop Highly weathered spodumene within Feld+Qtz+Musc,
two samples taken
SRL005 792254 8187678 Pegmatite 2024 Feldspar,
Quartz
Tourmaline,
Muscovite
Garnet Outcrop Outcrop of pegmatite in the drainage. kf, ab, qtz,
schorlite, green mus and garnet. Very similar to
Luciano'speg.

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Sample ID Easting
(UTM 23S)
Northing
(UTM 23S)
Lithology Campaign Primary
Minerals
(Major >30%)
Secondary
Minerals
(Minor >5%
and <30%)
Accessory
Minerals
(Trace <5%)
Boulder
/In-Situ
Comments
SRL006 792449 8187561 Pegmatite 2024 Feldspar,
Quartz
Tourmaline,
Muscovite
Garnet Outcrop Old trench that intercepted a robust peg with kf, ab,
qtz, green mus, schorlite and garnet.
SRL007 794748 8192381 Pegmatite 2024 Feldspar,
Quartz
Muscovite,
Schorlite
Pyrolusite? Float Large peg boulder, with ab, qtz, mus, schorlite, Mn
oxide. Moderately weathered.
SRL008 792536 8187475 Pegmatite 2024 Feldspar,
Quartz
Muscovite,
Schorlite
Outcrop Peg outcrop in drainage with ab, kf, qtz, green mica,
shorlite. Thickness 1m and indefinite length.
SRL009 792795 8187714 Pegmatite 2024 Feldspar,
Quartz
Muscovite,
Schorlite
Pyrolusite? Float Attempted artisanal mine that took floats of peg. Kf,
qtz, green mica and Mn oxide.
SRL010 792417 8187715 Pegmatite 2024 Feldspar,
Quartz
Muscovite,
Schorlite
Outcrop Decimeter scale blocks of peg. Kf, ab, qtz, green mica
and schorlite. Coarse and fine texture.