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ANSON RESOURCES LIMITED Capital/Financing Update 2024

Oct 21, 2024

64435_rns_2024-10-21_91b2cac0-3413-47c4-8283-5fdd1c7945ff.pdf

Capital/Financing Update

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22 October 2024 ASX Announcement

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Anson Completes Second Geotechnical Engineering Survey for Green River Definitive Feasibility Study ASX: ASN Announcement

Highlights:

  • Anson has completed a geotechnical survey for the proposed location for a DLE extraction plant at the Green River Lithium Project for inclusion in a Definitive Feasibility Study,

  • Located in Emery County, which is classified as industrial land,

  • Confirmed subsurface conditions were suitable for the proposed DLE processing plant,

  • The study provided geotechnical data and subsurface conditions to be used in engineering studies to provide construction recommendations for the DLE production plant,

  • Depth of boreholes range from 6.1 to 12.2 m (20 to 40 feet),

  • Depths of the trenches ranged from 1 to 4.58 m (3 to 15 feet),

  • Geophysical surveys were carried out to test the dynamic properties of subsurface materials,

Anson Resources Limited (ASX: ASN ) (“ Anson Resources ” or the “ Company ”) through its 100% owned subsidiary Blackstone Minerals NV LLC is pleased to announce the completion of a second geotechnical engineering study located in Emery County at its Green River Lithium Project, in south-eastern Utah, USA. This engineering study examined soil and rock types, as part of the due diligence being undertaken for the possible location of the proposed Direct Lithium Extraction processing plant or possible site for a stage 2 expansion, on the Company’s privately owned property.

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Figure 1: A photo showing one of the trenches completed for logging and sampling showing shallow bedrock.

Anson Resources Ltd ABN: 46 136 636 005 ASX: ASN OTC: ANSNF

E: [email protected]

Australian Registered Office Level 3, 10 Eagle Street BRISBANE QLD 4000 T: + 61 7 3132 7990

www.ansonresources.com

ASX Announcement 22 October 2024

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The purpose of the report was to collect data on the subsurface conditions at the proposed production facility site regarding the design and construction of preliminary foundation options. The work program consisted of site reconnaissance, subsurface exploration, acquisition of geophysical data and engineering analysis.

Based on the program completed, which consisted of 7 boreholes and 8 trenches (see Table 1 and 2 for locations) and geophysical surveys, it was determined that the proposed site is suitable for the construction of the processing plant’s foundations, see Figure 1. Most of the site is underlain by alluvial deposits sitting on layers of gravel and cobbles. This is underlain by a hard sandstone layer. Bedrock was intersected in the boreholes between 76.5 to 426 cm (2.5 and 14 feet).

The project site generally consists of flatland cut by a winding east-west trending wash which enters from the east travelling down to the west, and hillsides to the south which drain down to the north into the flat areas within the project site. Most of the subject properties were vegetated with sparse native grasses, weeds and desert brush and plants. Elevations at the site ranged between approximately 1,251 m (4,105 feet) along the southern boundary to approximately 1,248 m (4,095 feet) in the northwest area.

The northern two thirds of the subject property was generally flat, with hillsides draining down to the north located along the southern one third of the project site as seen in Figure 2.

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Figure 2: Plan showing the locations of the boreholes, trenches and geophysical lines.

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ASX Announcement 22 October 2024

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The program was carried out by a Professional Engineer and a Professional Geologist licensed in the state of Utah and the field services consisted of

  • 7 boreholes and 8 test pits completed (see Figure 2),

  • Core samples to a maximum depth of 12.2 m (40 feet),

  • Soil samples,

  • Field resistivity measurements,

  • Geophysical surveys were completed to determine dynamic properties of subsurface materials.

SUBSURFACE INVESTIGATION

The borehole drilling and trenching, see Table 1 and 2 for locations, and the geophysical surveys have been completed. 17.8 cm (7 inch) diameter hollow-stem auger boreholes were drilled, and bedrock cored through the annulus using a truck-mounted CME 75 drill rig to depths between 6.1 and 12.2 m (20-40 feet). Standard Penetration Tests (SPT) were carried out on the core and then sent to the laboratory for further engineering test work.

Eight trenches, see Figure 2, were excavated using a Komatsu PC210lc Excavator with a 60 cm (2-foot-wide) bucket to depths between 91 and 457 cm (3 and 15 feet) for test pit observations. Bulk samples of subsurface material were collected for testing of the various rock units intersected.

Geotechnical laboratory tests were conducted on samples collected during the field investigation. The testing was designed to evaluate the engineering characteristics of locations rock units. Test work included:

  • Grain size distribution analysis

  • Atterberg limits (measure of the critical water content of fine-grained soils)

  • 1D consolidation tests

  • Unconfined compression tests

  • Water-soluble chloride and sulphate concentration

  • Electrical resistivity and pH

The bedrock encountered at the subject property is mapped as Cretaceous-aged Cedar Mountain Formation which consists as claystone, shale, mudstone, sandstone and conglomerate. The site is underlain by a very hard sandstone layer present across the entire property at an approximate depth of 4.5 m (15 feet). This is confirmed by the stratigraphy seen in the trenches, see Figure 1. The shallow bedrock appears to gently slope down to the north.

The geotechnical report provides a summary of the analyses, findings and recommendations for possible construction sites:

  • Field logs of soil, rock and groundwater conditions

  • Geotechnical parameters for shallow and deep foundation design

  • Corrosivity evaluation of soils

  • Earth work recommendations

  • Evaluation will provide recommendations for foundation design,

GEOPHYSICAL INVESTIGATION

The geophysical surveys consisted of

  • Multi-Channel Analysis of Surface Waves,

  • “Rippability”.

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ASX Announcement 22 October 2024

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These surveys included one multichannel analysis of surface waves (MASW) site classification survey, one two-dimensional surface wave profile, and three rippability surveys. The data and results for these geophysical surveys will help to further characterize the subsurface materials and potentially estimate the location and configuration of subsurface materials in and around these boreholes

Based on these observations of the Multi-Channel Analysis of Surface Waves it appears that there may be a transition layer or boundary between soft clay soils and stiff soils to rock that has transition strata that ranges from 274 to 396 cm (9 to 13 feet) below ground surface at the west end of the profile to 487 to 670cm (16 to 22 feet) on the eastern end of the profile line, see Figure 3.

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Figure 3: Surface wave model and interpretation.

Rippability measures the degree of difficulty to excavate soils and or bedrock. Measuring seismic P-wave velocities by conducting a seismic refraction survey provides input data to evaluate the rippability of soil or bedrock. It is a function of the site geology, the stratigraphy of the site, and geophysical properties of the soils and rock. The evaluation of rippability is useful to estimate the cost of excavation at specific areas of the subject site.

The depth to bedrock and seismic velocities of the subsurface layers are estimated. The unconsolidated deposits are shown in a pink color and the bedrock layer is shown in blue in the models. The soil/unconsolidated layer ranges in thickness from approximately 152.4 to 304 cm (5 to 10 feet). Figure 4 shows the performance information for a Caterpillar D8 Ripper. According to the D8 Ripper specs, the unconsolidated soil in this area should be rippable to depths indicated and the bedrock material may have marginal rippability.

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Figure 4: Rippability Inversion Model and Interpretation of Line BH05-N.

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ASX Announcement 22 October 2024

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About the Proposed Green River Lithium Production Site

The proposed 20-acre project site is in Emery County and is located on the privately owned land parcel purchased by Anson, see ASX Announcement 9 September 2023. The vacant land with uneven topography is already classified as Industrial Land and is located 1.3 km east of the Green River and just north of the I-70. Flooding is not anticipated as it is located approximately 12m (40 feet) higher in elevation. The vegetation includes sparse native grasses, weeds and desert brush with an approximate elevation of 1250 m (4,100 feet), see Figure 5.

This proposed site has been selected as it provides access to water from the Green River which is essential to the operation of the direct lithium extraction process. The preferred water extraction point is 1,200 m from the production location. In addition, the project site has easy access from the I-70 and also Main Street which passes through Green River City.

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Figure 5: Photograph showing the vegetation of the geotechnical surveyed area.

Geotech ID Easting Northing Depth
(ft)
Rock Unit
(refused in)
BH-1 575011 4314906 20 Claystone
BH-2 575117 4315069 25 Sandstone
BH-3 575183 4315025 28 Sandstone
BH-4 575388 4315037 27 Sandstone
BH-5 575201 4314929 20 Claystone
BH-6 575294 4314935 40 Sandstone
BH-7 575369 4315016 20 Sandstone

Table 1: Borehole locations and rock unit geology.

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ASX Announcement 22 October 2024

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Easting Northing Depth
(ft)
Rock Unit
(refused in)
TP-01 575114 4314950 7 Sandstone
TP-02 575123 4315011 12 Gravels
TP-03 575209 4315043 10 Gravels
TP-04 575388 4315037 3 Conglomerate
TP-05 575242 4314966 8 Sandstone
TP-06 575332 4314935 15 Claystone
TP-07 575639 4315016 13 Shale bedrock
TP-08 575285 4315012 13 Shale

Table 2: Trench locations and rock unit geology.

This announcement has been authorized for release by the Executive Chairman and CEO.

ENDS

For further information please contact:

Bruce Richardson Will Maze Executive Chairman and CEO Head of Investor Relations E: [email protected] E: [email protected] Ph: +61 7 3132 7990 Ph: +61 7 3132 7990 www.ansonresources.com

Follow us on Twitter @anson_ir

Click here to subscribe to news from Anson Resources: https://www.ansonresources.com/contact/

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ASX Announcement 22 October 2024

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About Anson Resources Ltd

Anson Resources (ASX: ASN) is an ASX-listed mineral resources company with a portfolio of minerals projects in key demand-driven commodities. Its core asset is the Paradox Lithium Project in Utah, in the USA. Anson is focused on developing the Paradox Project into a significant lithium producing operation. The Company’s goal is to create long-term shareholder value through the discovery, acquisition and development of natural resources that meet the demand of tomorrow’s new energy and technology markets.

Forward Looking Statements: Statements regarding plans with respect to Anson’s mineral projects are forward-looking statements. There can be no assurance that Anson’s plans for development of its projects will proceed as expected and there can be no assurance that Anson will be able to confirm the presence of mineral deposits, that mineralisation may prove to be economic or that a project will be developed.

Competent Person’s Statement 1: The information in this announcement that relates to exploration results and geology is based on information compiled and/or reviewed by Mr Greg Knox, a member in good standing of the Australasian Institute of Mining and Metallurgy. Mr Knox is a geologist who has sufficient experience which is relevant to the style of mineralisation under consideration and to the activity being undertaken to qualify as a “Competent Person”, as defined in the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves and consents to the inclusion in this report of the matters based on information in the form and context in which they appear. Mr Knox is a director of Anson.

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JORC Code 2012 “Table 1” Report

Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

Criteria JORC Code Explanation Commentary
Sampling techniques Nature and quality of sampling (e.g. cut channels, random chips, or specific
specialized 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 mineralization that are Material to the
Public Report.
Incases where ‘industry standard’ work has been done this wouldbe
relatively simple (e.g. ‘reverse circulation drilling was used to obtain 1 m
samples from which 3 kg was pulverized to produce a 30 g charge for fire
assay’). Inother cases, more explanation maybe required, such aswhere
there is coarse gold that has inherent sampling problems. Unusual
commodities or mineralization types (e.g. submarine nodules) may warrant
disclosure of detailed information.
• The Geotechnical survey was commenced in July 2024 by Geostrata..
• The survey included 7 boreholes and 8 trenches.
• Drill core sampling was carried out with a 7” diameter hollow-stem auger using a
truck-mounted CME 75 drill rig.
• Trenches were dug with a Komatsu PC210lc Excavator with a 2-foot-wide bucket
• Figure 2 in text shows the location of this work.
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.).
• 7” diameter hollow-stem auger boreholes were drilled, and bedrock cored through
the annulus using a truck-mounted CME 75 drill rig.
• Drilling techniques were acceptable for the geotechnical survey.
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.
• Drill core was considered acceptable for geotechnical testing.
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 andpercentage of the relevant intersections logged.
• Drill core and trenches were logged on site by a qualified geotechnical engineer and
geologist.

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Criteria JORC Code Explanation Commentary
Sub-sampling Techniques
and 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
maximize 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.
• Core was transported to Geostrata’s laboratory for further testing to evaluate
engineering properties.
• Disturbed samples were collected by driving a standard 1.4 inch inside diameter
split-spoon sampler.
• Undisturbed samples were collected by driving a 2-inch interior diameter (ID) and
2.5 inch outside diameter (OD) sampler.
• Bucket samples were collected from the trenches.
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 (e.g. standards, blanks,
duplicates, external laboratory checks) and whether acceptable levels
of accuracy (i.e. lack of bias) and precision have been established.
• Laboratory testing included:
Grain size distribution
Attenberg limits
Natural Moisture-Dry Density
Standard Proctor
• MASW survey
24 geophones using 4.5 Hertz vertical geophones
A 10-lb sledgehammer was used to generate seismic energy
Processed using ParkSEIS software
• Rippability
The ASTM Standard D5777 titledStandard Guide for using the seismic refraction
Seismic refraction was used to determine the depth to bedrock and the seismic
velocity ofthe bedrock
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.
• N/A
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 location of data points are shown in Table 1 and 2 and Figure 2 in the Text.
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.
• Data spacing is considered suitable for the geotechnical surveys carried out.

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Criteria JORC Code Explanation Commentary
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 mineralized structures is considered to have introduced a sampling
bias, this should be assessed and reported if material.
• N/A
Sample Security The measures taken to ensure sample security. • Samples were transported to GeoStrata’s laboratory on completion of the survey
program.
Audits or Reviews The results of any audits or reviews of sampling techniques and data • N/A.

Section 2 Reporting of Exploration Results

(Criteria in this section apply to all succeeding sections.)

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 license to operate in the area.
• The Green River Lithium Project is located in southeastern Utah, USA,
consisting of 1,251 placer claims that encompasses a land position of 10,620
hectares.
• Purchased private property consists of a 55-hectare land parcel
• All claims are held 100% by Anson’s U.S. based subsidiary, Blackstone Minerals
NV LLC.
• The claims/leases are in good standing, with payment current to the relevant
governmental agencies.
Exploration Done by
Other Parties
Acknowledgment and appraisal of exploration by other parties. • Anson has completed one geotechnical survey previously on the newly
purchased land parcels.
Geology Deposit type, geological setting and style of mineralization. • The geology of the Paradox Formation indicates a restricted marine basin,
marked by 29 evaporite sequences. Brines that host bromine and lithium
mineralization occur within the saline facies of the Paradox Formation and are
generally hosted in the more permeable dolomite sediments.

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Criteria JORC Code Explanation Commentary
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 meters) 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.
• The borehole and trench co-ordinates and depth are listed in the text.
• All boreholes were drilled at -900with an azimuth of 00.
• The RL for the area is approximately 4,100ft.
Data Aggregation
Methods
In reporting Exploration Results, weighting averaging techniques, maximum
and/or minimum grade
Brine samples taken in holes were averaged (arithmetic average) without 14
Criteria JORC Code explanation Commentary 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.
• N/A
Relationship Between
Mineralization Widths
and Intercept Lengths
These relationships are particularly important in the reporting of
Exploration Results.
If the geometry of the mineralization 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’).
• N/A
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.
• Figures in the text represent the information reported in the 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.
• N/A

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Criteria JORC Code Explanation Commentary
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 available current geotechnical data has been presented.
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 initial Geotechnical Survey is complete for this site.

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