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Pronounced Lithium-in-soil Anomalies

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Atlantic Lithium Limited has announced significant lithium-in-soil anomalies from Phase 2 and 3 soil sampling across its Rubino and Agboville licenses in Côte d'Ivoire. At Rubino, Phase 3 results expanded the anomalous zone to approximately 6.0km by 2.5km, showing distinct linear trends. Agboville's Phase 2 results defined a linear anomaly exceeding 5km in length, associated with spodumene pegmatite float. Additional spodumene pegmatite occurrences, with high-grade lithium assays, were discovered in rock float within the Rubino license; one sample (110074) returned 1.36% Li2O. The company has engaged a specialist corporate advisor to explore non-dilutive funding options to accelerate exploration of the Côte d'Ivoire licenses.

Full announcement

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Atlantic Lithium Limited (AIM: ALL, ASX: A11, GSE: ALLGH, "Atlantic Lithium" or the "Company"), the Africa-focused lithium exploration and development company, is pleased to announce the delineation of impressive lithium-in-soil anomalies in results from Phase 2 and Phase 3 soil sampling completed across the Rubino and Agboville exploration licences in Côte d'Ivoire, which are 100%-owned by the Company's wholly-owned subsidiary Khaleesi Resources SARL ("Khaleesi"). Additional spodumene pegmatite occurrences have also been discovered in float from geological mapping completed over the Rubino licence.

Highlights

  • Impressive lithium-in-soil anomalies, extending over several kilometres, identified from Phase 2 and Phase 3 soil sampling completed over the Company's Rubino and Agboville exploration licences in Côte d'Ivoire.
  • At Rubino, new Phase 3 results extend the lithium-in-soil anomalous zone identified from Phase 2 results (reported previously) to cover an increased area of approximately 6.0km by 2.5km, within which there are several distinct linear trends that warrant immediate ground follow-up evaluation.
  • At Agboville, Phase 2 soil sampling results define a pronounced linear anomaly >5km in length as well as other anomalous linear features, one of which is associated with spodumene pegmatite float discovered by the Company's geologists.
  • Additional spodumene pegmatite occurrences, returning high-grade lithium assays, discovered in rock float from geological mapping completed within the Rubino licence.
  • The latest soil sampling and assay results further indicate the prospectivity of the Company's tenure in the mining-friendly jurisdiction of Côte d'Ivoire, which remains significantly underexplored for lithium.
  • The Company is undertaking low-cost exploration of its Rubino and Agboville licences concurrently to the advancement of the Company's flagship Ewoyaa Lithium Project in Ghana to support its objectives of building a pipeline of projects to support long-term growth.
  • A specialist corporate advisor has been engaged to commence a formal process to source funding options that are non-dilutive to the Company's shareholders to accelerate exploration of the Côte d'Ivoire licences.

Commenting, Keith Muller, Chief Executive Officer of Atlantic Lithium, said:

"The latest results from the Company's ongoing exploration programmes across its 100%-owned Rubino and Agboville licences further underscore the prospectivity of its tenure in Côte d'Ivoire.

"Phase 2 and Phase 3 soil sampling results have delineated pronounced lithium-in-soil anomalies extending over several kilometres across the two licences, with several trends warranting further evaluation.

"At Rubino, the anomalous zone reported previously has been expanded by the latest results to an increased area of approximately 6.0km by 2.5km. Meanwhile, at Agboville, a pronounced linear anomaly >5km in length and several other anomalous linear features of interest have been identified.

"Through mapping and rock-chip sampling, the Company has also discovered several new spodumene pegmatite occurrences in rock float, in addition to the previously reported outcrop, within the Rubino licence. Further mapping has now commenced across both licences to support the evaluation of the anomalies identified in the Phase 2 and 3 soil results and to assist in defining follow-up auger drill programmes.

"The Company believes that its licences in Côte d'Ivoire demonstrate significant value potential through lithium exploration. To be undertaken alongside its advancement of its flagship Ewoyaa Lithium Project in Ghana, the Company has, therefore, commenced a formal process to explore funding options, considering minority, project-level investment or partnerships, to accelerate its exploration of the two licences.

"We look forward to providing further updates in due course."

Figures and Tables referred to in this release can be viewed in the PDF version available via this link:

Location

The Agboville exploration licence (PR 0694) covers an area of 397km2 and is located in the departments of Agboville and Adzope in Côte d'Ivoire, while the adjacent Rubino exploration licence (PR 0695) covers an area of 374km2 in the department of Agboville (refer Figure 1). Both licences are 100%-owned by the Company's wholly-owned Ivorian subsidiary, Khaleesi Resources SARL ("Khaleesi"). The town of Agboville is situated only 80km north of Abidjan, the port and commercial capital of Côte d'Ivoire, and the two licences are well-serviced with existing infrastructure, including excellent paved highways and an operating railway linking Burkina Faso's capital city of Ouagadougou and the port of Abidjan.

Figure 1: Location of the Agboville and Rubino licences held by the Company's wholly-owned subsidiary Khaleesi in Côte d'Ivoire and existing operational infrastructure.

Soil Sampling

Soil geochemical sampling was undertaken using 100m by 100m spaced grid over the most prospective areas identified by mapping and rock-chip sampling completed by the Company and also over historical mineral occurrences in both the Rubino and Agboville licence areas.

The soil sampling was completed in two sampling phases in each tenement; Phase 2 consisting of 3,235 sample sites (1,594 sites sampled at Agboville and 1,641 sites sampled at Rubino) and Phase 3 consisting of 1,512 sample sites (442 sites sampled at Agboville and 1,070 sites sampled at Rubino), the extent of which are shown in Figures 2 and 3. The total number of soil samples collected within the Rubino Phase 3 grid increased to 1,070 after the geological team was granted permission to sample a tract of agricultural land that had recently changed ownership (refer announcement of 31 July 2025). The Phase 1 soil sampling programme was a baseline soil programme undertaken along selected sections during reconnaissance mapping, where different sample depths and sieve fractions were tested and the results of which help set the best parameters for subsequent grid soil programmes.

The Company herein reports the results of Phase 3 soil sampling completed at Rubino and Phase 2 and Phase 3 soil sampling conducted at Agboville. The Rubino Phase 2 soil results were reported by the Company in the announcement dated 22 May 2025.

Rubino Licence

Newly-received Phase 3 lithium-in-soil results extend the anomalism 3.5km towards the NE from the previously announced Phase 2 soil grid, delineating a pronounced lithium-in-soil anomalous zone extending NE-SW continuously across the surveyed area, extending over an area of approximately 6.0km by 2.5km (refer Figure 2).

Within the anomalous zone, the results delineate a long NNE-SSW orientated linear anomaly, which could be associated with the interpreted lithological contact between metasediment and granodiorite; a similar lithological contact relationship that is observed in the distribution of anomalies from the Phase 2 soil grid. Similar, but less well defined, NNE-SSW to N-S trending soil anomalies are evident in the Rubino Phase 2 soil grid. These may be related to N-S to NNE-SSW orientated structural features concealed by the laterite cover and could also host pegmatite intrusions at depth. Several of the distinct NNE-SSW, N-S and NE-SW linear trends identified in the anomalous zone from the Phase 2 and Phase 3 soil results warrant immediate ground follow-up and ultimately sub-surface evaluation by the exploration team, as outlined in the 'Next Steps' section below.

Figure 2: Consolidated Rubino Phase 2 and Phase 3 Li (ppm) in soil grid results with spodumene pegmatite discovery sites. Pronounced anomalies are defined by lithium values between 200ppm and a peak value of 806ppm, with values below 85ppm considered a background response and related to the country rock. Refer to Figure 4 for spodumene pegmatite occurrences and associated lithia values.

Agboville Licence

The lithium-in-soil results from the Phase 2 soil grid define a pronounced linear anomaly >5km in length trending NE-SW, which follows the interpreted contact between metasediments to the NW and granodiorite intrusive to the SE (refer Figure 3). Other less well-defined anomalous linear features are developed over the granodiorite, one of which is associated with spodumene pegmatite float discovered by the mapping team, as reported previously (refer announcement of 22 May 2025). The Phase 3 lithium-in-soil geochemical response is more subdued; likely to be related to interpreted metasediment host exhibiting deeper weathering and laterite development and some alluvial cover with rice cultivation invalidating certain survey points.

The NE-SW-orientated lithological contacts in both the Rubino and Agboville licences follow the dominant regional tectonic trend in the Birimian of this part of West Africa, which is NE-SW, and a possible structural displacement across these potentially faulted or sheared contacts could host dilatant zones where pegmatite intrusion could be focused in either the schists of the metasediment or within more competent lithology such as the granodiorite.

Figure 3: Agboville Phase 2 and 3 Li (ppm) in soil grid results. Prominent lithium soil anomalies are defined by values above 200ppm and a peak value of 698ppm, and values below 85ppm considered a background response associated with regional country rock.

Mapping and rock-chip sampling

Additional geological mapping undertaken by the Company's geologists, continued along reconnaissance traverses and in support of soil sampling and in ground truthing Rubino Phase 2 soil anomalies, has discovered several additional spodumene pegmatite occurrences in the Rubino licence as rock float, with spodumene visually observed in hand specimen despite varying degrees of weathering exhibited.

Rock-chip samples were collected during mapping and submitted for assay. The elevated assay values of lithium and other elements from these pegmatite rock-chip samples confirm the Company's visual spodumene observations and the prospectivity of the licences (refer Figure 4 and Table 1). Not all pegmatite samples sent for assay returned anomalous assay results. Spodumene has a propensity to degrade in the tropical weathering environment with the lithium leaching out of the mineral even in weak to moderately weathered pegmatite, so weathered visually observed spodumene will not always have corresponding high lithium values in rock-chip assay results.

Figure 4: Map showing consolidated spodumene pegmatite occurrences within the Rubino licence with associated lithia values from rock-chip assays. Extent of recent Phase 2 and 3 soil sampling grids are also shown.

Table 1: Highlight rock-chip assay results (values >0.2 Li2O%, sorted highest to lowest by Li2O%) from the Rubino licence. Results <0.2 Li2O% are included in Appendix 1 and a geological map of the licences with rock-chip sample locations marked is included in Appendix 2.

Sample IDPermit IDEastingNorthingBe_ppmCs_ppmGa_ppmHf_ppmK_pctLi_ppmLi 2 O_%Nb_ppmSn_ppmTa_ppm
110074PR-695356490665634118.7862.2633.391.531.905963001.3697.60.279.28
110086PR-695356548665612126.4575.5435.041.953.631153001.1491.940.260.51
110075PR-695356485665629121.2268.228.391.072.28094762.11.0377.560.238.36
110032PR-695356506665644216.7992.826.441.124.03214556.70.9853.640.231.41
110087PR-695356577665683119.7946.6330.822.15044093.60.88121.270.252.78
110067PR-695356219665285172.5147.2628.884.563.34423041.50.6535.740.317.77
110085PR-695356419665590131.0386.9932.062.763.6961886.90.41820.272.89
110073PR-69535628166534255.01112.0725.843.793.721415600.3428.250.917.53
110106PR-6953597096669265.0969.9142.533.874.80991344.60.2910.1370.59
110068PR-695356294665308126.483.5221.472.742.87810940.2461.280.136.95

NOTE: Grid references reported in projection UTM, WGS84, Zone 30N.

Figure 5: a) Photograph of a spodumene pegmatite hand specimen (Sample 110074) discovered in the Rubino exploration licence by the Company's geologists. The photograph shows the broken surface of spodumene pegmatite float grab sample with spodumene crystals 10mm to 30mm in length (outlined in red), estimated to be 25-30% of the surface area of the rock sample. b) Photograph of a spodumene pegmatite hand specimen (Sample 100192) discovered in the Agboville exploration licence by the Company's geologists - previously reported (refer announcement of 22 May 2025). The photograph shows the weathered surface of spodumene pegmatite float with spodumene crystals 10mm to 28mm in length (outlined in red), estimated to be 15-20% of the surface area of the rock sample.

NOTE: Visual estimates of mineral abundance should never be considered a proxy or substitute for laboratory analyses where concentrations or grades are the factor of principal economic interest. Visual estimates also potentially provide no information regarding impurities or deleterious physical properties relevant to valuations.

Next Steps

The Company has commenced further mapping across both the Rubino and Agboville licences to continue the evaluation of the anomalies identified in the Phase 2 and 3 soil results. This additional mapping will assist in defining follow-up auger drill programmes to map the source of the anomalies below the laterite at surface, with the intention to define potential reverse circulation and diamond drill targets.

Further, Phase 4 soil sampling across both licences, extending outwards of the Phase 2 and Phase 3 soil sampling programme and across additional prospective areas, is also expected to be planned.

The Company has engaged a specialist corporate advisor to commence a formal process to source funding options to accelerate exploration activities across the Côte d'Ivoire licences. This process is focused on minority, project-level investment or partnerships that offer funding that is non-dilutive to Atlantic Lithium's existing shareholders.

JORC Table 1, Section 1 (Sampling Techniques and Data) and Section 2 (Reporting of Exploration Results) are included in Appendix 4.

Competent Persons

Information in this announcement relating to the exploration results is based on data reviewed by Mr I. Iwan Williams (BSc. Hons Geology), General Manager - Exploration of the Company and reported in accordance with the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (The Joint Ore Reserves Committee Code - JORC 2012 Edition). Mr Williams is a Member of the Australian Institute of Geoscientists (#9088) who has in excess of 30 years' experience in mineral exploration and is a Qualified Person under the AIM Rules and as a Competent Person as defined in the JORC Code. Mr Williams consents to the inclusion of the information in the form and context in which it appears.

For any further information, please contact:

Atlantic Lithium Limited

Keith Muller (Chief Executive Officer)

Amanda Harsas (Finance Director and Company Secretary)

SP Angel Corporate Finance LLP Nominated Adviser Jeff Keating Charlie Bouverat Tel: +44 (0)20 3470 0470Yellow Jersey PR Limited Charles Goodwin Bessie Elliot atlantic@yellowjerseypr.com Tel: +44 (0)20 3004 9512Canaccord Genuity Limited Financial Adviser: Raj Khatri (UK) / Duncan St John, Christian Calabrese (Australia) Corporate Broking: James Asensio Tel: +44 (0) 20 7523 4500

APPENDIX 1

Rock-chip assay results from the Rubino licence.

Sample IDPermit IDEastingNorthingBe_ppmCs_ppmGa_ppmHf_ppmK_pctLi_ppmLi 2 O_%Nb_ppmSn_ppmTa_ppm
110050PR-69437596466684411.5168.7724.650.915.0525100.50.0212.270.31.99
110051PR-69437602566670857.9374.5622.131.15.6341485.30.120.120.45.23
110048PR-6943656626607327.0116.7623.72.813.2535165.70.049.040.81.35
110049PR-6943753146669301.712.8920.230.524.425437.40.014.41.70.27
110108PR-6943691046573230.7214.5214.750.0810340.010.240.20.08
110109PR-6943602496625935.3633.7627.932.944.3094245.60.059.381.11.48
110121PR-6943753146669342.817.4721.560.375.139635.60.014.651.30.44
110122PR-6943759656668444.4443.9428.980.854.2772127.20.0315.50.42.33
110052PR-6953565066656447.436.6829.292.673.7032428.40.0912.411.22.05
110032PR-695356506665644216.7992.826.441.124.03214556.70.9853.640.231.41
110055PR-6953559616654746.4439.6528.392.553.7186345.40.0711.871.21.91
110057PR-6953562506660567.5946.3527.861.93.49813960.0913.140.72.6
110058PR-6953563766662541036.83127.4917.790.634.8659308.50.0738.460.295.71
110053PR-6953556856654064.0175.5921.822.843.51144570.15.191.20.71
110054PR-6953556906653995.6235.9427.32.373.63973540.0810.481.21.5
110110PR-69535606066584715.6493.2926.372.383.3377419.90.0916.610.911.36
110059PR-6953553316657817.4455.7327.562.263.7476401.20.0912.740.82.86
110060PR-695354952663743730.4226.952.443.7513415.60.0911.551.22.02
110061PR-695354774664005168.6567.6927.532.783.8126118.10.03280.215.83
110062PR-6953570716665240.710.360.560.0250.038820.900.470.10.15
110063PR-6953571756664101.0612.986.320.0250.383132.80.014.670.11.81
110064PR-69535723866629010.8533.9128.172.963.67381010.0212.520.245.61
110065PR-6953575156666360.270.221.280.0250.014919.100.090.10.06
110071PR-695356231665295171.0653.5423.983.264.03533.20.1129.710.111.88
110077PR-6953570136650271.773.8928.543.72.852339.10.017.891.70.6
110078PR-69535629466547725.9445.231.381.774.0134313.10.0716.080.52.89
110079PR-6953567626657302.4541.3515.530.0251.4251144.10.037.870.52.46
110080PR-6953567436656590.280.370.980.0250.031120.300.180.050.03
110095PR-69535653366629889.9480.3731.993.462.2682887.40.1961.960.430.47
110096PR-69535606866590874.160.875.730.411.746951.50.013.210.059.2
110072PR-69535622666528389.8640.7828.582.663.1935695.10.1517.840.34.63
110073PR-69535628166534255.01112.0725.843.793.721415600.3428.250.917.53
110067PR-695356219665285172.5147.2628.884.563.34423041.50.6535.740.317.77
110068PR-695356294665308126.483.5221.472.742.87810940.2461.280.136.95
110069PR-695356289665311155.0976.9727.112.971.8366871.10.1968.810.135.85
110070PR-69535627966534177.0177.7424.812.032.6187458.80.122.840.39.85
110074PR-695356490665634118.7862.2633.391.531.905963001.3697.60.279.28
110075PR-695356485665629121.2268.228.391.072.28094762.11.0377.560.238.36
110081PR-6953564866656309.23104.0625.012.893.6619625.40.1310.311.25.15
110082PR-6953564916656330.090.210.170.0250.009633.20.010.090.050.06
110083PR-6953564386655746.2717.328.471.743.0936145.20.0311.220.32.77
110084PR-69535640266568271.4326.8424.851.793.2069159.60.0314.630.48.7
110085PR-695356419665590131.0386.9932.062.763.6961886.90.41820.272.89
110089PR-6953569456654272.351.0218.120.080.0487135.30.030.690.40.72
110090PR-69535644066612854.2459.1826.251.683.1851285.50.0611.570.45.04
110091PR-6953569446661101.4320.6413.630.0250.848560.80.017.660.33.26
110092PR-6953569796660766.56154.8667.230.0254.0247241.10.0546.040.720.8
110093PR-6953569456660742.8658.0927.240.0251.65641030.0217.50.37.61
110094PR-6953569996660934.9395.5949.010.0253.08911880.0429.140.512.66
110102PR-6953579806659703.16.3425.413.684.3631100.10.023.411.50.46
110103PR-695356044665931140.2372.2928.582.123.6513290.0727.90.525.18
110097PR-69535830166638269.144.4529.623.933.97231440.0312.131.54.8
110098PR-6953561256659877.352.8327.642.093.7883287.20.0618.310.57.16
110100PR-69535941266707842.95140.8427.952.53.7014265.50.0613.820.619.2
110101PR-6953594796671623.6912.925.930.291.736686.40.022.460.21.29
110076PR-6953572076643963.157.6825.913.544.2478109.30.023.51.50.43
110119PR-6953490636769403.7113.1622.031.183.769238.70.055.6120.72
110115PR-695349060676940117.1539.826.7913.6034156.30.0316.3433.82
110116PR-695349137676595201.84202.630.42.425.53151560.0332.953.129.52
110111PR-6953603696722511.310.1725.140.470.081511.400.210.70.05
110117PR-69535353567662542.433.6126.342.314.928197.60.0427.852.219.43
110118PR-6953535706766875.2828.122.070.786.1471105.90.023.830.90.83
110120PR-6953551206793185.113.0820.331.437.446244.60.012.681.50.46
110123PR-6953535196821123.599.2124.490.171.4613218.80.0520.541.82.42
110124PR-6953490406799113.4428.2437.511.661.7923235.90.0542.672.17.69
110125PR-6953478116800160.651.94.570.230.186132.90.013.50.50.36
110126PR-695349210672087102.9942.0723.82.476.18893.20.0214.51.211.08
110112PR-6953516206762070.462.465.320.150.203334.70.013.8710.83
110113PR-6953501466788146.6355.0265.790.523.0704235.10.0574.118.213.94
110086PR-695356548665612126.4575.5435.041.953.631153001.1491.940.260.51
110087PR-695356577665683119.7946.6330.822.15044093.60.88121.270.252.78
110104PR-6953581576679680.4711.590.0250.086432.50.010.990.20.49
110107PR-6953599036646893.638.7732.411.672.0914168.90.0417.312.36.48
110106PR-6953597096669265.0969.9142.533.874.80991344.60.2910.1370.59
110105PR-69535970966692250.94129.8325.172.144.5723133.40.036.420.67.96

NOTE: Grid references reported in projection UTM, WGS84, Zone 30N.

APPENDIX 2

Geological map of the Rubino licence with rock-chip sample locations marked. Sample IDs are given where assay values >0.2% Li2O were returned, as reported in Table 1.

APPENDIX 3

Soil assay results (Li ppm >85 ppm, sorted highest to lowest) - Li values greater than 210 ppm are deemed extremely anomalous; values below 85ppm are considered background and are not reported in this announcement (calculated by means of cumulative probability statistics).

Sample_IDEastingNorthingLi (ppm)
100671366827658221698
100797367799659728644
100986368596660404637
101342369266660810429
101084368513660456416
100515367179658107403
101085368423660509377
100697366903658045369
100425367369659051368
101188369260660688366
101622369785661425348
101043368619660627341
101591369592661311339
101042368707660576335
100575367104658275329
100205368426658017327
101005368392660181319
100881368689659634308
101015368499660348307
101017368693660470303
101018368778660410302
101006368477660130301
101016368608660519299
101206369051660467294
100895368545659960293
100949368571660185292
101186369437660577290
101505369219661077290
101004368305660235286
100610366254658679284
101143368332661290278
101658369891661488274
101082368811660746273
101346368936661032265
101263369365660032264
101229369234659637264
101483369112661024263
100514367268658059261
100887368186659957259
100673366645658317249
101192368922660906248
100897368378660070247
101657369970661428245
100391367251658775244
101531369139661238243
101012368746660183242
100645366876657826241
101529369305661131239
101714370172661650239
104074359472666741237
101011368841660132234
101067368414660405232
100608366420658595231
100896368460660017230
101331368830660853229
101344369098660923229
100490367202658332229
100947368750660076227
101867370485662043225
101347368846661073223
101548369498661251221
101589369426661420220
101439370122660378219
100607366508658547219
101341369352660747217
100454367695659565217
100910368201660069216
101121368879659748214
101146368523660572214
100582367694657895213
104023359342666362213
101503369041661192212
101289368991659911211
100579367439658057210
100230367297658387207
101329368995660749207
104178359595667020207
100952368410660292205
100397367257658888204
100898368294660123204
104128359522667189204
104676359892668974204
104272360759666989202
104073359558666699200
100951368488660240199
100544367826659119198
101768370475661930197
101547369580661196197
101461369231661305197
101279369163660638197
103710356795666921197
100605366673658433195
100270369437658201195
100985368674660353195
100424367456659003194
101484369028661077194
101264369374660145193
101066368332660457191
100807367789659620190
101670370073661595189
101580369438661532189
100504368141658679189
100371367517658720188
101039368871660466188
100267369185658363186
101644369975661543185
101530369229661187185
101345369022660976185
101343369185660859185
100474367814658175185
100888368103660008184
100502367971658788184
104175359846666869184
101014368584660297183
101110368946660303183
104538358922668282183
103711356876666867183
100477368066658018182
100999368059660398182
100698366822658102181
100372367432658782181
101763370127662149181
100899368213660176180
100505368226658626180
101109368860660356180
101694370266661710180
100471369997660105179
100879368774659581179
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10375235774166655586

NOTE: Grid references reported in projection UTM, WGS84, Zone 30N.

APPENDIX 4

JORC Table 1, Section 1 - Sampling Techniques and Data

CriteriaJORC Code ExplanationCommentary
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.· Drilling is not being reported in this announcement. · Soil sampling was undertaken on 100m x 100m spaced grid using hand tools, where a 2kg sample is taken from the soil B-horizon at each sample site at a depth of approximately 30cm. Each soil sample is dry sieved to -160 micron at site, homogenised ahead of a 100g representative split being sent for analysis in individually labelled bags. · Soil geochemical analysis is undertaken at Atlantic Lithium's Mankessim facility in Ghana using SciAps Z903 LIBS (Laser induced breakdown spectroscopy) in Geochem mode with analysis undertaken on compressed pellets made from the 100g of -160 micron sieved material received. · 5% QAQC samples were inserted into the soil sample stream in the form of field duplicates, blank samples and appropriate certified reference material. · Rock-chip samples were collected during reconnaissance mapping at the discretion of the geologist, consisting of variably weathered outcrop or float. Approximately 1-2 kg of rock-chip material was sampled and submitted to Intertek Tarkwa for sample prep and forwarded to Intertek Perth for analysis using 4A-Li/MS48. · Visual estimates of spodumene have been reported for the spodumene pegmatite float samples discovered in the Rubino licence.
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).· Drilling is not being reported in this announcement.
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.· Drilling is not being reported in this announcement. · Not applicable to soil sampling programmes. · Recoveries of rock-chip samples is not relevant and results are only used for reconnaissance exploration assessment and will not be used to support mineral resource estimates.
Logging· Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. · Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. · The total length and percentage of the relevant intersections logged.· Drilling is not being reported in this announcement. · All rock-chip samples have been lithologically logged and photographed to a suitable standard to support reconnaissance level exploration. · Visual estimates of spodumene have been reported for the spodumene pegmatite float samples discovered in the Rubino licence. The hand samples have been photographed and the modal abundance of spodumene on the surface estimated visually using a percent abundance estimation chart.
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.· Drilling is not being reported in this announcement. · Intertek have followed standard procedures for sample preparation to produce sub-samples for analysis. Khaleesi Resources personnel followed soil sample preparation procedures to produce a sub-sample for analysis. · Field duplicates of soil samples were collected in the field and submitted for analysis as part of QA/QC.
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.· CP considers laboratory procedures and assaying are appropriate for the type of samples. · Assaying of the rock-chip samples was undertaken by Intertek Perth using their 4A-Li/MS48 analysis technique. The soil samples were assayed in-house at Atlantic Lithium's Mankessim facility using SciAps Z903 LIBS (Laser induced breakdown spectroscopy) set to Geochem mode and after appropriate callibration. · Intertek reported the use of standards and blanks as part of their QA/QC during analysis. Atlantic Lithium use standards as part of their QA/QC during rock-chip analysis. · 5% of soil samples submitted by the Company were standards, blanks and field duplicates. · All QA/QC samples submitted by the Company returned results within acceptable levels of accuracy.
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.· All significant assay results reported by Intertek and Atlantic Lithium have been verified by experienced Company personnel. · All primary data has been uploaded into the Company's data storage and data entry standard procedures checked and verified by two experienced Company personnel. · No adjustments to assay data were undertaken.
Location of data points· Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. · Specification of the grid system used. · Quality and adequacy of topographic control.· Location of soil sampling and rock chip sampling programme is recorded by hand-held GPS devices with +/_3m accuracy and is considered suitable for reconnaissance exploration. · Co-ordinate data is recorded in WGS84 UTM Z30N.
Data spacing and distribution· Data spacing for reporting of Exploration Results. · Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. · Whether sample compositing has been applied.· Soil sample spacing of these results is 100 x 100m. · Not applicable due to reconnaissance nature of this sampling and results are not considered for Mineral Resource classification.
Orientation of data in relation to geological structure· Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. · If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material.· Not applicable. · Drilling is not being reported in this announcement.
Sample security· The measures taken to ensure sample security.· The sample chain of custody is managed by Khaleesi Resources and Atlantic Lithium. The samples are collected in the field by Khaleesi Resources personnel in unique number coded plastic bags and labelled polyweave sacks. All samples are delivered directly to Intertek by Khaleesi Resources personnel. Rock-chip samples are prepared by Intertek in Tarkwa and pulp is securely shipped to Perth by DHL. Soil samples are collected from Intertek Tarkwa by Atlantic Lithium personnel and delivered to the Company's Mankessim facility for analysis.
Audits or reviews· The results of any audits or reviews of sampling techniques and data.· No review of the sampling techniques has been undertaken. The soil assay data will be reviewed internally by the geological team once all the results are received.

JORC Table 1, Section 2 - Reporting of Exploration Results

CriteriaJORC Code ExplanationCommentary
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.· PR 0694 is located in the Department of Agboville and PR 0695 is in the Departments of Agboville and Adzope, Côte d'Ivoire. All permits are owned 100% by Khaleesi Resources SARL, a wholly-owned subsidiary of Atlantic Lithium Limited. · The permits are in good standing and the Company is not aware of any existing or potential impediments which may impact ongoing exploration activities.
Exploration done by other parties· Acknowledgment and appraisal of exploration by other parties.· No systematic modern exploration for lithium-caesium-tantalum pegmatites have been undertaken over the area. No records of other systematic exploration over the tenement areas have been found. · Government 1:200,000 scale geological mapping and historical mineral occurrence evaluations have been undertaken over the area at various times since the 1960s.
Geology· Deposit type, geological setting and style of mineralisation.· Potential for lithium-caesium-tantalum bearing pegmatite mineralisation. The area is underlain by Birimian-aged metasediments with granitic intrusives of the Eburnean orogeny which can host LCT pegmatite deposits similar to those discovered in Ghana and Mali.
Drill hole information· A summary of all information material to the under-standing of the exploration results including a tabulation of the following information for all Material drill holes: · easting and northing of the drill hole collar · elevation or RL (Reduced Level - elevation above sea level in metres) of the drill hole collar · dip and azimuth of the hole · down hole length and interception depth · hole length · If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case.· No drilling is being reported.
Data aggregation methods· In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated. · Where aggregate intercepts incorporate short lengths of high grade results and longer lengths of low grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. · The assumptions used for any reporting of metal equivalent values should be clearly stated.· Not applicable.
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 (e.g. 'down hole length, true width not known').· Not applicable.
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.· Maps are included in the body of the announcement.
Balanced Reporting· 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. · Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.· All meaningful exploration data has been included in the body of this announcement.
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.· Li grid heat map was created using: · MapInfo Discover (Version 2023, Release Build 142) Heatmap · Heatmap settings: Style set at standard; area of influence set to 0 · Grid cell size 25m x 25m
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.· The Company is planning further mapping and soil geochemical sampling programmes to further assess the potential for lithium-bearing pegmatites within the licences. Auger drilling and possibly trenching will be used to define pegmatite targets below laterite cover.

Cleaned text: letterheads, contacts and legal notices removed. View the original announcement ↗ · Company filings. Not investment advice.

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