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Pure Spodumene Nature of Piedmont Lithium Ore Body

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Pure Spodumene Nature of Piedmont Lithium Ore Body ASX RELEASE | June 18, 2019 | ASX:PLL; NASDAQ:PLL PURE SPODUMENE NATURE OF PIEDMONT LITHIUM ORE BODY XRD analysis confirms pure spodumene nature of Piedmont’s ore body o Absence of petalite and lepidolite in pegmatites expected to lead to high lithium recovery Mineralogy consistent across Piedmont’s Core, Central, and Sunnyside properties Piedmont on-track to release Resource, Metallurgy and Scoping Study updates in the next 60 days Piedmont Lithium Limited (“Piedmont” or “Company”) is pleased to announce the completion of mineralogical analysis on samples of mineralized pegmatites and composite samples from Piedmont’s Core, Central, and Sunnyside Properties. All testwork to date effectively demonstrates that lithium occurs almost exclusively within spodumene in Piedmont’s mineral resource. Table 1: Average XRD Analysis Results from 46 Drill Core and Composite Samples of Piedmont Ore Average Wt. (%) of Mineral Types Sunnyside Core Property Central Property Property Mineralogy Semi- Composite Quantitative Quantitative Quantitative quantitative Variability Samples Samples Sample Samples Samples (19 Samples) (3 Samples) (1 Sample) (13 Samples) (10 Samples) Spodumene 17.8 19.9 16.6 15.9 14.8 - Petalite - - - - - Lepidolite - - - - - Lithium bearing minerals Zinnwaldite - - - - - Holmquistite - - 0.5 - - Non-lithium bearing minerals 82.2 80.1 82.9 84.1 85.2 Total 100.0 100.0 100.0 100.0 100.0 Piedmont has been advised that the relatively pure spodumene character of its ore body is unusual and highly positive, allowing for a simplified flowsheet to produce strong lithium recoveries. Certain hard rock lithium projects are understood to contain multiple lithium-bearing minerals (petalite, lepidolite, zinnwaldite, etc. as well as spodumene). Keith D. Phillips, President and Chief Executive Officer, commented: “As the market’s understanding of lithium processing evolves, it will become increasingly clear that mineralogy and metallurgy are the fundamental building blocks of a successful hard-rock lithium business. Our testwork confirms what we have always suspected – the Carolina Tin-Spodumene Belt is exceptional not only in scale but in terms of mineralogy. When combined with the shallow nature of our ore body and the capital and operating cost advantages of our location, we are excited about the upcoming resource, metallurgical and scoping study updates.” For further information, contact: Keith D. Phillips Anastasios (Taso) Arima President & CEO Executive Director T: +1 973 809 0505 T: +1 347 899 1522 E: [email protected] E: [email protected] PIEDMONT LITHIUM LIMITED +61 8 9322 6322 New York Office Registered Office 50 002 664 4953 +61 8 9322 6558 28 W 44th Street, Suite 810 Level 9, 28 The Esplanade www.piedmontlithium.com [email protected] NEW YORK NY 10036 PERTH WA 6000 The Company has completed mineralogical testing, comprising semi-quantitative and quantitative x-ray diffraction (“XRD”) analysis, on samples of mineralized pegmatites and composite samples from Piedmont’s Core, Central, and Sunnyside Properties. All testwork to date effectively demonstrate that lithium occurs almost exclusively in Piedmont’s mineral resource. 36 samples of mineralized pegmatites were collected from Piedmont’s Core, Central, and Sunnyside Properties. The average results of these samples are shown in Table 1 above with the results of all samples included in Appendix 1. Figure 1 shows the distribution of the mineralized samples across all Piedmont properties. Figure 1. Distribution of XRD Samples from Mineralized Pegmatites from Piedmont Properties 2 Additionally, Piedmont completed semi-quantitative XRD on 10 variability samples from the Core property from composites of core collected during Phase 2 and Phase 3 drill campaigns. These samples were created to simulate a run-of-mine concentrator feed sample in terms of average grade and composition including a distribution of samples across early, middle and late years production. A total mass of 839 kg was collected for these samples. SGS Lakefield is currently completing pre-feasibility level dense medium and locked-cycle flotation tests on the variability samples with results expected in July. The average XRD results of the variability samples are shown in Table 1 above with the results of all samples included in Appendix 1. The data show that the Piedmont ore body does not contain any petalite, lepidolite, or zinnwaldite. These non-spodumene lithium bearing minerals concentrate under different operating conditions than spodumene when processing with dense medium or flotation. Additionally, petalite (4.86% Li2O) and lepidolite (7.70% Li2O) have lower lithium content than spodumene (8.03%). Therefore, Piedmont expects to maintain both high lithium concentrate grades and recoveries at the Company’s planned concentrator in part due to the absence of petalite or other lithium bearing minerals. XRD analysis was also performed on six barren pegmatites and samples of three zones of alteration from waste rock samples. Barren pegmatites were shown to contain no non-spodumene lithium bearing minerals. While certain lithium bearing minerals did appear in the alteration zone samples, these meter-scale alteration zones are of very limited size and it is expected that this altered host rock will largely be segregated from ore during mining operations. Where holmquistite may appear in mine dilution material, it is anticipated this high-iron mineral and other waste rock will be easily separated from mineralized pegmatite by ore sorting or by magnetic separation. The average results of barren and waste rock samples are shown in Table 2 below with all results included in Appendix 1. Table 2: Average XRD Analysis from Barren Pegmatite and Waste Rock Samples Lithium Average Wt. (%) of Mineral Types Bearing Minerals Barren Pegmatite Samples (6 Samples) Waste Rock Samples (3 Samples) Spodumene 0.1 - Petalite - 1.2 Lepidolite - 2.4 Zinnwaldite - - Holmquistite - 26.1 Other minerals 99.9 70.3 Total 100 100 3 About Piedmont Lithium Piedmont Lithium Limited (ASX: PLL; Nasdaq: PLL) holds a 100% interest in the Piedmont Lithium Project (“Project”) located within the world-class Carolina Tin-Spodumene Belt (“TSB”) and along trend to the Hallman Beam and Kings Mountain mines, historically providing most of the western world’s lithium between the 1950s and the 1980s. The TSB has been described as one of the largest lithium provinces in the world and is located approximately 25 miles west of Charlotte, North Carolina. It is a premier location for development of an integrated lithium business based on its favorable geology, proven metallurgy and easy access to infrastructure, power, R&D centers for lithium and battery storage, major high-tech population centers and downstream lithium processing facilities. Forward Looking Statements This announcement may include forward-looking statements. These forward-looking statements are based on Piedmont’s expectations and beliefs concerning future events. Forward looking statements are necessarily subject to risks, uncertainties and other factors, many of which are outside the control of Piedmont, which could cause actual results to differ materially from such statements. Piedmont makes no undertaking to subsequently update or revise the forward-looking statements made in this announcement, to reflect the circumstances or events after the date of that announcement. Cautionary Note to United States Investors Concerning Estimates of Measured, Indicated and Inferred Resources The Project’s Mineral Resource of 16.2Mt @ 1.12% Li2O comprises Indicated Mineral Resources of 8.5Mt @ 1.15% Li2O and Inferred Mineral Resources of 7.7Mt @ 1.09% Li2O. The information contained in this announcement has been prepared in accordance with the requirements of the securities laws in effect in Australia, which differ from the requirements of U.S. securities laws. The terms "mineral resource", "measured mineral resource", "indicated mineral resource" and "inferred mineral resource" are Australian terms defined in accordance with the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (the “JORC Code”). However, these terms are not defined in Industry Guide 7 ("SEC Industry Guide 7") under the U.S. Securities Act of 1933, as amended (the "U.S. Securities Act"), and are normally not permitted to be used in reports and filings with the U.S. Securities and Exchange Commission (“SEC”). Accordingly, information contained herein that describes Piedmont’s mineral deposits may not be comparable to similar information made public by U.S. companies subject to reporting and disclosure requirements under the U.S. federal securities laws and the rules and regulations thereunder. U.S. investors are urged to consider closely the disclosure in Piedmont’s Form 20-F, a copy of which may be obtained from Piedmont or from the EDGAR system on the SEC’s website at http://www.sec.gov/. Competent Persons Statement The information in this announcement that relates to Exploration Results is based on, and fairly represents, information compiled or reviewed by Mr. Lamont Leatherman, a Competent Person who is a Registered Member of the ‘Society for Mining, Metallurgy and Exploration’, a ‘Recognized Professional Organization’ (RPO). Mr. Leatherman is a consultant to the Company. Mr. Leatherman has sufficient experience that is relevant to the style of mineralization and type of deposit under consideration and to the activity being undertaken to qualify
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