CRITICAL RESOURCES LIMITED — Capital/Financing Update 2019

Aug 22, 2019

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23 August 2019 ASX Announcements Office 152–158 St Georges Terrace Perth WA 6000 Australia

UPDATE ON DRC LITHIUM JOINT VENTURES

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Figure 1: RC drilling samples at the Kanuka Lithium Production Project taken in the DRC in 2018

Force Commodities Ltd ( Force or the Company ) (ASX Code: 4CE) is pleased to provide an update on its lithium joint venture activities in Tanganyika Province in the south east of the Democratic Republic of Congo ( DRC ).

By way of background, during 2017 Force secured an interest in two lithium projects, the KitotoloKatamba Lithium Project and the Kanuka Lithium Production Project and undertook significant exploration at each during 2017 and 2018 involving mapping, rock-chip sampling, trenching, auger drilling and reverse circulation ( RC ) drilling.

Limited exploration has been conducted at each of the Kitotolo-Katamba and Kanuka Lithium Production Projects during calendar year 2019, due to the significant deterioration in the demand for spodumene concentrate and a fall in lithium prices, and as a result of the Company’s focus shifting to advancing its exploration and development activities at the high-grade lead and silver Tshimpala Project in Malawi.

The initial assay results from the Phase 1 RC drilling program at Kitotlo-Katamba have now been received and have confirmed the presence of shallow, low grade lithium mineralisation and further demonstrated the need to complete further deeper drilling. However for the immediate future, the Company is proposing to maintain its focus on advancing the Tshimpala Project towards production and will hold back on further exploration expenditure at its lithium projects in the DRC until a marked improvement in the lithium sector has occurred or until the Company is able to attract additional parties to assist in funding progress at the Kitotolo-Katamba and Kanuka Lithium Projects.

Force Commodities Ltd | Ground Floor, 20 Kings Park Road, West Perth, WA, 6005 | PO Box 1024 West Leederville WA 6007 Ph: +61 8 6426 1421 | F: +61 8 6323 3347 | web:forcecommodities.com.au | ABN 12 145 184 667 | ASX:4CE

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Kanuka Lithium Production Project

In 2018, the Company completed its Phase 1 RC drilling program at the Kanuka Lithium Production Project. A total of 45 RC holes were completed for about 2,700m. The drilling program was designed to rapidly target near surface lithium mineralisation hosted within exposed pegmatites and confirm interpretations from surface geological mapping.

In December 2018 (refer ASX Announcement dated 6 December 2018), the Company confirmed the presence of widespread, shallow , multiple-parallel stacked, high grade lithium mineralised pegmatites as determined by assay from drilling. The drilling showed this mineralisation extended over a strike of at least 1.3km at the Kania Main Pegmatite. This body is located inside the main tin and tantalum open pit mining operation of the Company’s joint venture partner Mining Mineral Resources SPRL ( MMR ) and has a width of up to 300m.

Drilling at the Kalombo Mushwima Prospect, west of the Kania Main pegmatite, showed the existence of a shallow and broad lithium mineralised system having a width of 1.4km, which remains open along strike in all directions.

A number of drill holes reported high grade intersections at depth which were often terminated in mineralisation; indicating the potential for deeper and broader higher-grade lithium mineralisation at depth.

Selected high-grade lithium samples were tested by x-ray diffraction (XRD) methods to determine the specific lithium bearing mineralogy.

The XRD analyses have now been received and show the lithium mineralisation at the Kania Main and Kalombo Mushwima Prospect is predominantly lepidolite, with petalite and spodumene phases.

A summary of the XRD analyses is included in Table 2.

Sample ID	Quartz	Petalite	Muscovite	Chlorite	Albite	Spodumene	Microcline	Lepidolite	Beryl
	%	%	%	%	%	%	%	%	%
A09392	32.21	0.76	10.35	0.07	32.89	0.00	3.25	20.35	0.12
A09474	40.65	0.77	5.02	0.13	31.08	4.46	0.91	16.73	0.23
A09476	39.22	1.33	8.11	0.07	30.24	6.04	0.00	14.65	0.34
A09477	34.28	1.36	7.84	0.07	31.33	0.74	3.61	20.72	0.07
A09562	48.68	1.44	1.56	0.07	29.76	0.17	0.17	18.05	0.10
S554281	26.34	1.52	20.55	0.20	34.10	0.00	0.00	16.91	0.38
S554345	34.79	1.71	13.95	0.13	31.69	0.14	1.14	16.20	0.26
S554511	22.93	17.85	2.46	0.07	49.88	0.00	0.00	6.69	0.12
S554513	23.00	25.81	9.61	0.07	30.12	3.05	0.00	8.13	0.22
S554514	32.64	2.35	10.99	0.03	33.73	0.12	0.00	20.07	0.07
S554562	38.95	2.00	24.17	0.20	16.51	0.20	1.62	15.76	0.60
S554591	30.17	0.84	15.53	0.20	29.16	0.00	1.40	17.71	5.00
S554592	30.49	1.41	9.88	0.13	38.67	0.00	0.00	19.36	0.05
S554924	57.51	0.57	19.47	0.33	1.45	0.71	1.02	18.87	0.08
S554936	28.12	2.14	14.83	0.07	38.31	0.00	0.00	16.24	0.29
S554937	36.43	2.48	11.06	0.07	28.92	0.00	0.00	20.77	0.27
T00331	21.49	2.73	19.90	0.07	39.16	0.18	0.00	16.35	0.13
T00341	41.47	2.23	6.49	1.11	26.02	0.12	0.00	22.01	0.54
T00344	31.61	2.80	23.69	0.20	26.02	0.00	0.00	15.54	0.14
T00398	23.32	2.28	24.58	0.33	33.49	0.35	0.00	15.45	0.19

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Sample ID	Quartz	Petalite	Muscovite	Chlorite	Albite	Spodumene	Microcline	Lepidolite	Beryl
	%	%	%	%	%	%	%	%	%
T00405	20.97	3.66	27.74	0.07	22.89	0.00	0.00	24.41	0.26
T00406	26.16	2.41	5.16	0.07	47.71	0.60	0.00	17.68	0.21
T00417	22.40	3.04	22.82	0.07	34.10	0.00	0.00	17.29	0.28
T00419	20.79	3.18	16.96	0.13	37.59	0.00	0.00	20.81	0.53
T00484	35.51	1.66	19.22	0.13	15.66	0.71	11.50	15.21	0.39
T00485	23.26	2.01	17.77	0.07	37.71	0.84	2.85	15.26	0.23
T00695	39.33	0.89	18.85	0.13	15.30	0.00	5.31	19.94	0.25
T00715	39.55	1.52	7.47	0.07	30.48	0.51	4.19	16.11	0.11
T00899	47.19	0.95	4.68	0.07	15.42	0.00	8.15	23.31	0.24
T00958	20.57	2.08	32.13	1.70	27.71	0.20	0.00	15.35	0.26

Table 1: XRD analyses from selected high-grade lithium samples at Kanuka Lithium Production Project

It is rare for the minerals petalite and spodumene to occur in the same pegmatite because the temperature and pressure of stability affects the presence or absence of each phase. Spodumene is stable in melts of higher pressure and moderate temperature whereas petalite is stable at high temperature and moderate pressure. There is, however, a complicating factor where upon cooling of the melt spodumene sometimes replaces petalite.

The XRD analyses shows a petalite rich, spodumene poor assemblage of lithium bearing phase. Petalite is a high value lithium bearing phase because of its use in ceramics.

Whilst the XRD analyses results are very encouraging given the high value petalite, the Board does not believe further exploration expenditure is warranted in the current market and the Company will continue its discussions with its joint venture partner at Kanuka and determine how best to progress the project.

Kitotolo West Lithium Project.

The Company has elected to relinquish the option it held over the project.

Kitotolo-Katamba Lithium Project

During 2018, the Company completed shallow reverse circulation ( RC ) drilling of 4,272 drill metres with samples taken for routine assay (48 element four acid digest with ICP finish) in South Africa.

Shallow RC drilling was completed to rapidly target near surface lithium mineralisation, extending 1 km northeast from the artisanal Katamba Pit. The target was located in the northeastern quadrant of the Project area and interpreted to occur within a northeast-southwest trending pegmatite corridor.

The Company has received the assay results on the first batch of samples processed from the Phase 1 drilling program. The results from Phase 1 drilling program at Kitotolo-Katamba are set out in full in Appendix 1. The assays results indicate the presence of shallow low grade (0.20% Li2O and 0.39% Li2O) lithium that is hosted in mica schists.

The presence of the lithium mineralisation in the mica schists is considered very positive, given that they are not among the main types of geological accumulation of lithium – such as pegmatites, granites and and brines.

The shallow lithium mineralisation identified in the mica schists, seen to increase at depth in the drill holes is probably due to thin pegmatite stringers occupying a small volume of the total rock volume drilled sampled.

The assay results have confirmed that the drilling program has successfully intersected a number of lithium bearing pegmatite veins with widths of between 7m and 16m. The results also indicate the

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potential for deeper and broader higher-grade lithium mineralisation at depth, with assays from drill holes reporting intersections of lithium mineralisation at depth and ending in mineralisation

Despite the encouraging assays from the Phase 1 drilling program, the Board has determined that raising additional equity capital to further progress exploration activities in the DRC and commence a deeper drilling program will be extremely difficult at the current moment in time and potentially highly dilutive to current shareholders. Furthermore, the Board does not believe that further exploration expenditure of substance at Kitotolo-Katamba is warranted at this point in time. The Company will progress with discussions with its joint venture partner at Kitotolo-Katamba and determine how best to now advance the project given these circumstances.

END

For further information contact:

Jason Brewer Managing Director Force Commodities Limited Tel: +61 (0) 8 6462 1421

Competent Person Statement

The information in this release that relates to sampling techniques and data, exploration results, geological interpretation and Exploration Targets, Mineral Resources or Ore Reserves has been compiled by Jess Oram who is a member of the Australasian Institute of Geoscientists and a Member of the Geological Society of Australia. Mr Oram is engaged by Force Commodities as a non-executive Chairman.

Mr Oram has sufficient experience of relevance to the styles of mineralisation and the types of deposits under consideration, and to the activities undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr Oram consents to the inclusion in this report of the matters based on information in the form and context in which it appears.

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 other 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 differ 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.

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APPENDIX 1

Summary of the Phase 1 RC drilling completed and reported in this ASX release.

Hole_ID	Sample_ID	Li_ppm	Li2O_ppm	Grid_North	Grid_East	Dpth_From	Depth_To
KA18AC007	S555366	226	487	9164545	509064	43	44
KA18AC007	S555367	229	493	9164545	509064	44	45
KA18AC007	S555368	244	525	9164545	509064	45	46
KA18AC007	S555369	253	545	9164545	509064	46	47
KA18AC007	S555370	263	566	9164545	509064	47	48
KA18AC007	S555371	242	521	9164545	509064	48	49
KA18AC007	S555372	254	547	9164545	509064	49	50
KA18AC007	S555373	251	540	9164545	509064	50	51
KA18AC007	S555374	281	605	9164545	509064	51	52
KA18AC007	S555375	255	549	9164545	509064	52	53
KA18AC007	S555376	254	547	9164545	509064	53	54
KA18AC007	S555377	271	583	9164545	509064	54	55
KA18AC007	S555378	275	592	9164545	509064	55	56
KA18AC007	S555379	301	648	9164545	509064	56	57
KA18AC007	S555381	149,5	322	9164545	509064	57	58
KA18AC007	S555382	275	592	9164545	509064	58	59
KA18AC007	S555383	281	605	9164545	509064	59	60
KA18AC009	S555384	48,5	104,5	9164508	509329	0	1
KA18AC009	S555385	66,8	144,0	9164508	509329	1	2
KA18AC009	S555386	92,1	198,5	9164508	509329	2	3
KA18AC009	S555387	162,5	350	9164508	509329	3	4
KA18AC009	S555388	225	484	9164508	509329	4	5
KA18AC009	S555389	172,0	370	9164508	509329	5	6
KA18AC009	S555390	171,0	368	9164508	509329	6	7
KA18AC009	S555391	434	934	9164508	509329	7	8
KA18AC009	S555392	333	717	9164508	509329	8	9
KA18AC009	S555393	470	1010	9164508	509329	9	10
KA18AC009	S555394	402	865	9164508	509329	10	11
KA18AC009	S555395	253	545	9164508	509329	11	12
KA18AC009	S555396	378	814	9164508	509329	12	13
KA18AC009	S555397	446	960	9164508	509329	13	14
KA18AC009	S555398	420	904	9164508	509329	14	15
KA18AC009	S555399	412	887	9164508	509329	15	16
KA18AC009	S555401	620	1335	9164508	509329	16	17
KA18AC009	S555402	540	1160	9164508	509329	17	18
KA18AC009	S555403	550	1185	9164508	509329	18	19
KA18AC009	S555404	690	1485	9164508	509329	19	20
KA18AC009	S555405	960	2070	9164508	509329	20	21
KA18AC009	S555406	720	1550	9164508	509329	21	22
KA18AC009	S555407	770	1660	9164508	509329	22	23
KA18AC009	S555408	780	1680	9164508	509329	23	24
KA18AC009	S555409	650	1400	9164508	509329	24	25
KA18AC009	S555410	870	1875	9164508	509329	25	26
KA18AC009	S555411	830	1785	9164508	509329	26	27
KA18AC009	S555412	840	1810	9164508	509329	27	28
KA18AC009	S555413	790	1700	9164508	509329	28	29
KA18AC009	S555414	860	1850	9164508	509329	29	30

5

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Hole_ID	Sample_ID	Li_ppm	Li2O_ppm	Grid_North	Grid_East	Dpth_From	Depth_To
KA18AC009	S555415	790	1700	9164508	509329	30	31
KA18AC009	S555416	890	1915	9164508	509329	31	32
KA18AC009	S555417	950	2050	9164508	509329	32	33
KA18AC009	S555418	770	1660	9164508	509329	33	34
KA18AC009	S555419	750	1615	9164508	509329	34	35
KA18AC009	S555421	560	1205	9164508	509329	35	36
KA18AC009	S555422	480	1035	9164508	509329	36	37
KA18AC009	S555423	480	1035	9164508	509329	37	38
KA18AC009	S555424	480	1035	9164508	509329	38	39
KA18AC009	S555425	470	1010	9164508	509329	39	40
KA18AC010	S555426	88,1	189,5	9164591	509273	0	1
KA18AC010	S555427	88,5	190,5	9164591	509273	1	2
KA18AC010	S555428	85,0	183,0	9164591	509273	2	3
KA18AC010	S555429	157,5	339	9164591	509273	3	4
KA18AC010	S555430	264	568	9164591	509273	4	5
KA18AC010	S555431	310	667	9164591	509273	5	6
KA18AC010	S555432	290	624	9164591	509273	6	7
KA18AC010	S555433	348	749	9164591	509273	7	8
KA18AC010	S555434	378	814	9164591	509273	8	9
KA18AC010	S555435	421	906	9164591	509273	9	10
KA18AC010	S555436	313	674	9164591	509273	10	11
KA18AC010	S555437	444	956	9164591	509273	11	12
KA18AC010	S555438	530	1140	9164591	509273	12	13
KA18AC010	S555439	530	1140	9164591	509273	13	14
KA18AC010	S555109	750	1615	9164591	509273	14	15
KA18AC010	S555110	NR	NR	9164591	509273	15	16
KA18AC010	S555111	291	626	9164591	509273	16	17
KA18AC010	S555112	560	1205	9164591	509273	17	18
KA18AC010	S555113	490	1055	9164591	509273	18	19
KA18AC010	S555114	520	1120	9164591	509273	19	20
KA18AC010	S555441	480	1035	9164591	509273	20	21
KA18AC010	S555442	321	691	9164591	509273	21	22
KA18AC010	S555443	430	926	9164591	509273	22	23
KA18AC010	S555444	439	945	9164591	509273	23	24
KA18AC010	S555445	440	947	9164591	509273	24	25
KA18AC010	S555446	470	1010	9164591	509273	25	26
KA18AC010	S555447	490	1055	9164591	509273	26	27
KA18AC010	S555448	500	1075	9164591	509273	27	28
KA18AC010	S555449	570	1225	9164591	509273	28	29
KA18AC010	S555450	500	1075	9164591	509273	29	30
KA18AC010	S555451	460	990	9164591	509273	30	31
KA18AC010	S555452	580	1250	9164591	509273	31	32
KA18AC010	S555453	520	1120	9164591	509273	32	33
KA18AC010	S555454	490	1055	9164591	509273	33	34
KA18AC010	S555455	540	1160	9164591	509273	34	35
KA18AC010	S555456	530	1140	9164591	509273	35	36
KA18AC010	S555457	500	1075	9164591	509273	36	37
KA18AC010	S555458	490	1055	9164591	509273	37	38
KA18AC010	S555459	405	872	9164591	509273	38	39
KA18AC010	S555461	366	788	9164591	509273	39	40
KA18AC010	S555462	427	919	9164591	509273	40	41
KA18AC010	S555463	450	969	9164591	509273	41	42

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Hole_ID	Sample_ID	Li_ppm	Li2O_ppm	Grid_North	Grid_East	Dpth_From	Depth_To
KA18AC010	S555464	422	908	9164591	509273	42	43
KA18AC010	S555465	435	936	9164591	509273	43	44
KA18AC010	S555466	384	827	9164591	509273	44	45
KA18AC010	S555467	379	816	9164591	509273	45	46
KA18AC010	S555468	375	807	9164591	509273	46	47
KA18AC010	S555469	334	719	9164591	509273	47	48
KA18AC010	S555470	570	1225	9164591	509273	48	49
KA18AC010	S555471	820	1765	9164591	509273	49	50
KA18AC011	S555472	49,3	106,0	9164675	509216	0	1
KA18AC011	S555473	54,8	118,0	9164675	509216	1	2
KA18AC011	S555474	50,4	108,5	9164675	509216	2	3
KA18AC011	S555475	162,5	350	9164675	509216	3	4
KA18AC011	S555476	54,7	118,0	9164675	509216	4	5
KA18AC011	S555477	194,5	419	9164675	509216	5	6
KA18AC011	S555478	237	510	9164675	509216	6	7
KA18AC011	S555479	234	504	9164675	509216	7	8
KA18AC011	S555481	271	583	9164675	509216	8	9
KA18AC011	S555482	266	573	9164675	509216	9	10
KA18AC011	S555483	251	540	9164675	509216	10	11
KA18AC011	S555484	277	596	9164675	509216	11	12
KA18AC011	S555485	297	639	9164675	509216	12	13
KA18AC011	S555486	267	575	9164675	509216	13	14
KA18AC011	S555487	301	648	9164675	509216	14	15
KA18AC011	S555488	307	661	9164675	509216	15	16
KA18AC011	S555489	298	642	9164675	509216	16	17
KA18AC011	S555490	335	721	9164675	509216	17	18
KA18AC011	S555491	348	749	9164675	509216	18	19
KA18AC011	S555492	359	773	9164675	509216	19	20
KA18AC011	S555493	359	773	9164675	509216	20	21
KA18AC011	S555494	399	859	9164675	509216	21	22
KA18AC011	S555495	362	779	9164675	509216	22	23
KA18AC011	S555496	401	863	9164675	509216	23	24
KA18AC011	S555497	435	936	9164675	509216	24	25
KA18AC011	S555498	427	919	9164675	509216	25	26
KA18AC011	S555499	391	842	9164675	509216	26	27
KA18AC011	S555501	317	682	9164675	509216	27	28
KA18AC011	S555502	415	893	9164675	509216	28	29
KA18AC011	S555503	530	1140	9164675	509216	29	30
KA18AC011	S555504	600	1290	9164675	509216	30	31
KA18AC011	S555505	670	1440	9164675	509216	31	32
KA18AC011	S555506	680	1465	9164675	509216	32	33
KA18AC011	S555507	710	1530	9164675	509216	33	34
KA18AC011	S555508	740	1595	9164675	509216	34	35
KA18AC011	S555509	810	1745	9164675	509216	35	36
KA18AC011	S555510	750	1615	9164675	509216	36	37
KA18AC011	S555511	810	1745	9164675	509216	37	38
KA18AC011	S555512	800	1720	9164675	509216	38	39
KA18AC011	S555513	690	1485	9164675	509216	39	40
KA18AC011	S555514	830	1785	9164675	509216	40	41
KA18AC011	S555115	1820	3920	9164675	509216	41	42
KA18AC011	S555116	1830	3940	9164675	509216	42	43
KA18AC011	S555117	790	1700	9164675	509216	43	44

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Hole_ID	Sample_ID	Li_ppm	Li2O_ppm	Grid_North	Grid_East	Dpth_From	Depth_To
KA18AC011	S555118	420	904	9164675	509216	44	45
KA18AC011	S555119	170,0	366	9164675	509216	45	46
KA18AC011	S555121	313	674	9164675	509216	46	47
KA18AC011	S555122	680	1465	9164675	509216	47	48
KA18AC011	S555123	610	1315	9164675	509216	48	49
KA18AC011	S555515	550	1185	9164675	509216	49	50
KA18AC011	S555516	500	1075	9164675	509216	50	51
KA18AC011	S555517	560	1205	9164675	509216	51	52
KA18AC011	S555518	580	1250	9164675	509216	52	53
KA18AC011	S555519	580	1250	9164675	509216	53	54
KA18AC011	S555521	570	1225	9164675	509216	54	55
KA18AC011	S555522	450	969	9164675	509216	55	56
KA18AC011	S555523	440	947	9164675	509216	56	57
KA18AC011	S555524	520	1120	9164675	509216	57	58
KA18AC011	S555525	440	947	9164675	509216	58	59
KA18AC011	S555526	353	760	9164675	509216	59	60
KA18AC013	S555124	680	1465	9164083	508905	36	37
KA18AC013	S555125	161,5	348	9164083	508905	37	38
KA18AC013	S555126	470	1010	9164083	508905	38	39
KA18AC013	S555127	93,4	201	9164083	508905	39	40
KA18AC013	S555128	150,5	324	9164083	508905	40	41
KA18AC013	S555129	40,5	87,2	9164083	508905	41	42
KA18AC013	S555130	120,0	258	9164083	508905	42	43
KA18AC013	S555131	64,1	138,0	9164083	508905	43	44
KA18AC013	S555132	58,9	127,0	9164083	508905	44	45
KA18AC013	S555133	630	1355	9164083	508905	45	46
KA18AC013	S555134	690	1485	9164083	508905	46	47
KA18AC013	S555135	640	1380	9164083	508905	47	48
KA18AC014	S555136	1280	2760	9164120	508872	12	13
KA18AC014	S555137	1510	3250	9164120	508872	13	14
KA18AC014	S555138	490	1055	9164120	508872	14	15
KA18AC014	S555139	154,5	333	9164120	508872	15	16
KA18AC014	S555141	293	631	9164120	508872	16	17
KA18AC014	S555142	380	818	9164120	508872	17	18
KA18AC014	S555143	700	1505	9164120	508872	18	19
KA18AC014	S555144	357	769	9164120	508872	19	20
KA18AC014	S555145	1280	2760	9164120	508872	20	21
KA18AC014	S555146	780	1680	9164120	508872	21	22
KA18AC014	S555147	434	934	9164120	508872	24	25

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APPENDIX 2 – JORC Code, 2012 Edition – Table 1 Report

Section 1 Sampling Techniques and Data

Criteria	JORC Code explanation	Commentary
Sampling techniques	>Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as downhole 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 (e.g. ‘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 (e.g. submarine nodules) may warrant disclosure of detailed information.	Drilling geology results reported herein relate to Reverse Circulation (RC) drillholes at the Kitotolo-Katamba Lithium Project. A full list of hole collars that includes coordinates, azimuth, dip and depth can be found in Drillhole Information Appendix 1, and significant pegmatite intercepts information is contained tables in the body of the report and as Appendix 2. The azimuth of Force’s drill holes is oriented approximately perpendicular to the interpreted strike of the mineralised trend. Holes are weakly oblique to orthogonal in a dip sense (see cross-sections). • Forces RC drill spoils are collected into two sub-samples: • 1 metre split sample, is homogenized and riffle split at the sample prep facility and then calico-bagged. Usually these weigh 2-3 kg. • 30-40 kg primary sample is collected in polyweave bags and retained until assays have been returned and deemed reliable for reporting purposes.
Drilling techniques	>Drill type (e.g. core, reverse circulation, open- hole hammer, rotary air blast, auger, Bangka, sonic, etc.) and details (e.g. 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.).	RC Drilling technique used by Force and reported herein comprises standard Reverse Circulation (RC) 4 and ¾ inch face sampling hammer (5.5- inchdiameter bit). The rig used is a custom made RC rig and running a 2000 CFM 750 psi compressor. The RC rig was operated by Equity Drilling (DRC),
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.	RC sample recoveries are weighed and recorded by 4CE for each metre. To date sample recoveries have averaged >90%. • Contamination is monitored regularly. Minor issues have been encountered in this program, due to large amounts of ground water. • The cyclone and splitter are regularly cleaned using compressed air, especially in wet intervals. • Drill collars are sealed to prevent sample loss and holes are normally drilled dry to prevent poor recoveries and contamination caused by water ingress. Wet intervals are noted in case of unusual results
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.	Standard sample logging procedures are utilised by 4CE, including logging codes for lithology, minerals, weathering etc. • A chip tray for the entire RC or RAB hole is completed. A sub-sample is sieved from the large RC bags at site into chip trays over the pegmatite interval to assist in geological logging. • Geology of the RC and RAB drill chips were logged on a metre basis with attention to main rock forming minerals within the pegmatite intersections. • Entire drilled interval of RC logged. • Pegmatite sections are also checked under a LW/SW UV light for mineral identification on an ad hoc basis. These only provide indicative qualitative information.

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Section 2 Reporting of Exploration Results

Criteria	JORC Code explanation	Commentary
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.	4CE’s project geologists were supervised by 4CE’s Head of Exploration • All field data is entered into excel spreadsheets (supported by look-up tables) at site and subsequently validated as it is imported into the centralised 4CE database. • Hard copies of survey and sampling data are stored in the local office and electronic data is stored on multiple backup hard drive Samples were assayed for a multi element suite of 48 elements. However, the presented data has been reduced to just Li. In addition Li2O has been reported. It has been calculated from the reported assay result for Li in ppm. The calculation is %Li2O = (ppm Li x 2.153)/10000 and the presented results have been rounded to the second decimal place. No adjustments have been made to reported assay data.
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.	The geological data, including start-point, end-points have been surveyed using handheld GPS devices, giving an accuracy of +/- 3m in open-ground. WGS84 UTM (Zone 35S) No topographic survey has been undertaken. Hand held GPS coordinates have been utilised to locate sampling to date.
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.	Between 300m along strike and between 50 and 200m down-dip across strike. Refer figures in report. This data may be used to support a resource in the future, but only once the drill density has been assessed as sufficient to do so. If not, infill drilling may be required so that confidence is improved sufficiently to do so. Not applicable as no resource estimation. Sampling undertaken to date was of a reconnaissance nature and wide spread along geologic bodies. No sample compositing was used or reported in results
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.	Force’s drilling is oriented perpendicular to the interpreted strike of mineralisation (pegmatite body) as mapped or predicted by the geological model. In some areas the rocks may trend at an angle to the drill traverse. Because of the dip of the hole, drill intersections are apparent thicknesses and overall geological context is needed to estimate true thicknesses. All drill holes are orientated -600and were inclined and drilled orthogonal to the strike of the pegmatite. None-the-less, modern exploration software is easily able to visualize these in 3 dimensions and integrate the drill traces with more recently surveyed drilling by 4CE and, which were oriented approximately perpendicular to the interpreted strike of the mineralised trend. Results to date, indicate drilling was orientated correctly.
Sample security	>The measures taken to ensure sample security.	Rock chip samples were shipped directly from the field by the company in sealed polyweave bags or similar containers using a reputable transport company with shipment tracking capability so that a chain of custody can be maintained. Each bag was sealed with a security strap tag as used by ITRI protocols. The samples were locked in a shed if they were stored overnight at any point during transit, including at the drill site prior to shipping. The laboratory confirmed the integrity of the rice bag seals upon receipt
Audits or reviews	>The results of any audits or reviews of sampling techniques and data.	The sampling techniques and data have been reviewed and the assay results are believed to give a reliable indication of the lithium mineralisation within the samples.

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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 Kitotolo-Katamba licences consist of both Exploitation Permits and Research Permits PE 13247 valid for 30 years and Exploitation Permit PR12453 valid for 5 years with further renewals of 5 years. See above, no other known impediments.
Exploration done by other parties	> Acknowledgment and appraisal of exploration by other parties.	The licence area has been subject to small scale artisanal mining Apart from the mining and test pit excavations, there has been no other exploration licences below alluvial layers and no lithium exploration has taken place.
Geology	> Deposit type, geological setting and style of mineralisation.	The Kitotolo-Katamba Project is an early stage exploration project in terms of Lithium potential. There are high grade lithium occurrences only at this stage. Further exploration programs will be required to determine whether the project has further economic potential. The Project lies within the mid-Proterozoic Kibaran Belt - an intracratonic domain, stretching for over 1,300 km through Katanga and into southwest Uganda. The belt strikes predominantly SW-NE and is truncated by the NS to NNW-SSE trending Western Rift system. The Kibaran comprises a sedimentary and volcanic sequence that has been folded, metamorphosed and intruded by at least four separate phases of granite. The latest granite phase (900 to 950 My ago) is assigned to the Katangan cycle and is associated with widespread vein and pegmatite mineralisation containing tin, Tungsten, Tantalum, Niobium, Lithium and Beryllium. Deposits of this type occur as clusters and are widespread throughout the Kibaran terrain. In the DRC, the Katanga Tin Belt stretches over 500 km from near Kolwezi in the southwest to Kalemie in the northeast comprising numerous occurrences and deposits of which the AVZ (Manono) deposit is currently the largest. The geology of the Manono area is poorly documented and no reliable maps of local geology have been observed for the licence area.
Drill hole Information	> A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: > easting and northing of the drill hole collar > elevation or RL (Reduced Level – elevation above sea level in metres) of the drill hole collar > dip and azimuth of the hole > down hole length and interception depth > hole length. > If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should	Drill hole information is tabled as Appendix 1 in the report.

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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.	All results being reported for RC drill samples are based on 1 metre intervals to provide a 2-3kg sample. No top/lower cut have been applied. At this stage it is considered that an insufficient data set has been collected to allow geostatistical methods of any relevance. Methodology may change as the collected dataset increase Not included in the reported results
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’).	The nature of drillholes with respect to geology is discussed above. Because of the dip of the hole, drill intersections are apparent thicknesses and overall geological context is needed to estimate true thicknesses. Refer to figures in report. All results being reported for pegmatites mineralisation are based on 1m interval lengths. The mineralisation and host rocks are interpreted to dip consistently between 200and 270NW. The geometry of the mineralisation reported is not well understood, as it is under cover and early stage exploration, however the pegmatite is not of uniform thickness and their orientations vary down-dip and along strike. No top/lower cut have been applied.
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.	Refer to this press release body of text
Balanced reporting	>Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results.	Due to the nature of the early stage project status and limited sampling to date, the results should be considered indicative only and not material. All results should be considered in the limited context of the sampling program. The samples collected to date are considered representative of the intersected mineralisation.
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.	No further data available.
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.	Further work may include mapping, soil sampling and bed rock sampling for geochemical anomalies to identify prospective target zones and then small amount of drill testing of higher priority targets. RC/ Diamond drilling is planned to define further shallow mineralisation along strike and down dip. In-fill drilling also planned between current sections to demonstrate grade continuity.

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