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EMPIRE RESOURCES LIMITED Capital/Financing Update 2022

May 18, 2022

64875_rns_2022-05-18_c00f1fe1-2c90-4673-9b90-c969ecb80527.pdf

Capital/Financing Update

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ASX Release

19 May 2022

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FURTHER MASSIVE SULPHIDES AT SMITHS WELL

HIGHLIGHTS

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  • 22.38m of massive to disseminated pyrrhotite-chalcopyrite-pyrite sulphides intersected from 328.42m downhole (YDD22-04) at Smiths Well

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  • 11.33m of massive to disseminated pyrrhotite-chalcopyrite-pyrite sulphides intersected from 386.12m downhole (YDD22-05) at Smiths Well

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  • Strongly mineralised copper-gold horizon identified in YDD22-03 located below the highly conductive copper-nickel-cobalt horizon at Smiths Well

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Assay results from YDD22-03 returns copper >1%, including

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  • 10m @ 0.65% Cu & 0.10g/t Au from 253m

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  • inc 0.7m @ 1.26% Cu & 0.20g/t Au from 255.3m

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  • and 0.9m @ 1.13% Cu & 0.15g/t Au from 258.7m

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1m @ 1.19% Cu & 0.23g/t Au from 314m

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Diamond drilling continues at Yuinmery Project

Empire Managing Director, Sean Richardson commented:

“Smiths Well continues to impress with further wide intercepts of massive and disseminated sulphides within the modelled DHEM conductor. Assay results have also identified a new copper-gold horizon below the highly conductive copper-nickel-cobalt horizon.

“The diamond drilling program continues at Smiths Well with hole YDD22-07 testing the down dip extents to copper mineralisation at the YT01 prospect. The Company looks forward to updating the market as results from the drilling becomes available.”

www.resourcesempire.com.au [email protected] 159 Stirling Highway, Nedlands WA 6009

t +61 (0) 8 6389 1032

EMPIRE RESOURCES LIMITED ACN 092 471 513 ASX: ERL

ASX Announcement 19 May 2022

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SUMMARY

Empire Resources (ASX:ERL, Empire) advises that it has intersected 22.38m of massive to disseminated pyrrhotite-chalcopyrite-pyrite sulphides from 328.42m in diamond drillhole YDD22-04 and 11.33m of massive to disseminated pyrrhotite-chalcopyrite-pyrite sulphides from 386.12m in diamond drillhole YDD22-05 at the Smiths Well prospect, Yuinmery.

Diamond hole YDD22-04 (Figure 1) was designed to target the strong conductor modelled from downhole electromagnetic (DHEM) surveys completed in March 2022[[1]] . The sulphide intercept is interpreted to be a down plunge extension to the Smiths Well mineralisation, where 30.1m @ 0.60% Cu, 0.17% Ni & 0.034% Co[[2]] was recently intersected in drillhole YDD22-02.

Interval Description
328.42m – 332.25m Massive sulphide (pyrrhotite-pyrite-chalcopyrite)
332.25m – 338.6m Semi-massive sulphide (pyrrhotite-pyrite-chalcopyrite)
338.6m – 350.80m Massive sulphide (pyrrhotite-pyrite-chalcopyrite)

Table 1 – YDD22-04 Visual Sulphide Summary

Diamond hole YDD22-05 (Figure 1) was designed to test the limits of the modelled DHEM conductor approximately 60m down plunge from YDD22-04.

Interval Description
386.12m – 390.40m Massive sulphide (pyrrhotite-pyrite-chalcopyrite)
390.40m – 392.30m Disseminated and vein sulphide (pyrrhotite-pyrite-chalcopyrite)
392.30m – 396.00m Massive sulphide (pyrrhotite-pyrite-chalcopyrite)
396.00m – 397.45m Disseminated and vein sulphide (pyrrhotite-pyrite-chalcopyrite)

Table 2 – YDD22-05 Visual Sulphide Summary

The massive to disseminated intercepts lie within an interpreted mafic sequence comprising coarse grained gabbroic rocks with very coarse grained (glomeroporphyritic) domains and horizons dominated by ferromagnesium minerals and dolerite. Basalt occurs in the footwall of the mineralisation. The highly conductive copper-nickel-cobalt horizon is interpreted to occur in the mafic sequence proximal to the basalt contact.

*Sulphide observations are preliminary in nature and estimates of sulphide minerals are visual only. Visual estimates of sulphide abundance are based on the Company’s sulphide field logging guideline (Table 3). Visual estimates of sulphide mineral abundance should never be considered a proxy or substitute for laboratory analysis. Laboratory analysis is required to determine the widths and grades of visual sulphide estimates.

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YDD22-03 Assay Results

Assay results for YDD22-03 drilled at Smiths Well during the March 2022 quarter have been received from Empire’s preferred commercial laboratory. YDD22-03 intercepted three zones of mineralisation.

Assay results include:

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  • 1.25m @ 0.20% Cu, 0.21% Ni & 0.041% Co from 215.35m

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  • 10m @ 0.65% Cu & 0.10g/t Au from 253m

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  • including 0.7m @ 1.26% Cu & 0.20g/t Au from 255.3m

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  • and 0.9m @ 1.13% Cu & 0.15g/t Au from 258.7m

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  • 2m @ 0.80% Cu & 0.17g/t Au from 313m

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including 1m @ 1.19% Cu & 0.23g/t Au from 314m

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Figure 1 – Smiths Well Long Section

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ASX Announcement 19 May 2022

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The upper copper-nickel-cobalt horizon intercepted at 215.35m is associated with semimassive sulphide, primarily fine pyrrhotite with lesser pyrite and chalcopyrite similar to the highly conductive copper-nickel-cobalt zone. While this interval has copper-nickel-cobalt chemistries similar to the highly conductive zone the relationship between the two is unclear at present.

The strongly mineralised 10m @ 0.65% Cu & 0.10g/t Au from 253m (Figure 2) is considered to be a separate copper-gold horizon located below the highly conductive copper-nickelcobalt horizon. The intersection occurs within a broader 18m wide zone of copper anomalism. Chalcopyrite is the main sulphide mineral present, occurring as net textured and disseminations in quartz-carbonate-sericite-pyrite veins hosted in Gabbro.

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Figure 2 – YDD22-03 (Tray 60), 251.80m – 256.48m: disseminated and vein chalcopyrite in Gabbro

The third mineralised zone from 313m is associated with fine crackle brecciation with silicacarbonate matrix, silicification and aggregates of fine magnetite in a ferromagnesium section of the gabbro. Chalcopyrite is the main sulphide mineral and predominately occurs within the mafic clasts as disseminations or net textured. Mineralisation is likely the result of brittle deformation in the less ductile lithologies.

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Figure 3 – Visible Sulphides in YDD22-04 from 322.71m to 350.59m (Trays 71-82)

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Figure 4 – Visible Sulphides in YDD22-05 from 380.98m to 397.56m (Trays 90 – 93)

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Figure 5 – March 2022 DHEM Conductor & Drill Collars Base Image RTP_Eagcs50nl

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FORWARD PLAN

Samples from YDD22-04 and YDD22-05 have been collected and submitted for laboratory analysis. Assay results from the YDD22-04 and YDD22-05 batch of samples is anticipated to be received during the June Quarter.

Diamond drillhole YDD22-06 at Smiths Well has also been completed, targeting the down dip extents to the modelled DHEM plate conductor and to test for the presence of the new coppergold horizon identified in diamond hole YDD22-03. Logging of YDD22-06 is ongoing.

Drilling continues at Yuinmery with drill hole YDD22-07 at YT01 testing down dip extensions to mineralisation intercepted in diamond drillhole YDD22-01[[2]] .

Samples will be collected and submitted for petrographic analysis to characterise the host geology and sulphide mineralogy. The Company will also investigate petrophysical testing of drill core to assist in optimising geophysical techniques and further refine data processing.

Geophysical surveys, including the use of downhole electromagnetic (DHEM) will continue to be used to plan and target drilling. Geophysical surveys will commence as soon as a geophysical crew is available.

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ASX Announcement 19 May 2022

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This announcement is authorised for release by:

Sean Richardson

Managing Director

For further information on the Company Phone: +61 (0)8 6389 1032 www.resourcesempire.com.au

Additional Information

Further details relating to the information in this release can be found in the following ASX announcements:

  1. ASX:ERL “ Strong DHEM Responses at Smiths Well (Amendment) ” 6 May 2022

  2. ASX:ERL “ Assay Results from Yuinmery Project ” 2 May 2022

Sulphide Mode Percentage Range
Massive >80%
Semi-Massive & Matrix 40-80%
Net-Textured 20-40%
Matrix 20-40%
Heavily Disseminated 10-40%
Disseminated & Blebby 1-10%
Trace <1%

Table 3 – Sulphide Field Logging Guideline

*Visual estimates of sulphide abundance are based on the Company’s sulphide field logging guideline (Table 3). Visual estimates of sulphide mineral abundance should never be considered a proxy or substitute for laboratory analysis. Laboratory analysis is required to determine the widths and grades of visual sulphide estimates.

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Competent Person Statements

The information in this report that relates to Exploration Results is based on information compiled and/or reviewed by Mr Mark Shelverton, who is a Member of the Australian Institute of Geoscientists. Mr Shelverton is a full-time employee of Empire Resources and has sufficient experience that is relevant to the style of mineralisation and type of deposits under consideration and to the activity he is undertaking 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”. Mr Shelverton consents to the inclusion in this presentation of the matters based on this information in the form and context in which they appear.

The information is this release concerning the Mineral Resources for the Just Desserts deposit has been estimated by Mr Peter Ball B.Sc who is a director of DataGeo Geological Consultants and is a member of the Australasian Institute of Mining and Metallurgy (AusIMM). Mr Ball has sufficient experience which is relevant to the style of mineralization and type of deposit under consideration and qualifies as a Competent Person as defined in the 2012 Edition of the “Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves”. Mr Ball consents to the inclusion in this public release of the matters based on his information in the form and context in which it appears.

New Information

Information concerning the current mineral resource estimate relating to the Just Desserts deposit is extracted from the ASX Announcement dated 17 May 2016.

Empire Resources Limited confirms that it is not aware of any new information or data that materially affects the information included in the original market announcement and that all material assumptions and technical parameters underpinning the Resource estimate in the relevant market announcement continue to apply and have not materially changed. Empire Resources Limited confirms that the form and context in which the Competent Persons’ findings are presented have not been materially modified from the original market announcements.

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ASX Announcement 19 May 2022

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About Empire

Empire Resources Limited (ASX:ERL) is a gold and copper focussed exploration and development company. Empire owns four highly prospective projects. The Yuinmery CopperGold Project 470km northeast of Perth in the Youanmi Greenstone Belt, the Barloweerie multielement precious and base metal project, the Nanadie Copper-Gold Project southeast of Meekatharra in the Murchison Region and the Penny’s Gold Project 45km northeast of Kalgoorlie in the prolific Eastern Goldfields Region of Western Australia. Empire’s projects have numerous exploration targets with excellent potential.

Empire has an experienced team of exploration, development and financial professionals who are committed to developing a sustainable and profitable mineral business. Empire seeks to extract value from direct exploration of its existing projects as well as identifying value accretive investment opportunities that complement the Company’s development objectives.

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Empire Resources Project Location

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ASX Announcement 19 May 2022

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Hole ID
East
North
RL
Depth
Az
Dip
Smiths Well YDD22-03
688,835
6,837,272
455
330.5
135
-60
YDD22-04
688,775
6,837,300
455
402.3
135
-60
YDD22-05
688,750
6,837,357
455
426.3
135
-60
YDD22-06
687,250
6,835,625
455
456.3
135
-60
YT01 YDD22-07
687,250
6,835,625
462
350*
180
-60

Table 4 – Diamond Drillhole Summary

  • Planned depth
Prospect Hole ID
Fr.
(m)
To
(m)
Int.
(m)
Cu
(%)
Au
(g/t)
Ni
(%)
Co
(ppm)
S
(%)
Fe
(%)
Smiths Well YDD22-03
213.55
214
0.45
0.20
0.23
296
12.64
29.39
215.35
216.6
1.25
0.20
0.21
412
14.09
27.94
251
263
12
0.54
0.09
0.69
6.56
inc
253
263
10
0.65
0.10
0.77
7.87
inc
255.3
256
0.7
1.26
0.20
1.44
7.61
and
258.7
259.6
0.9
1.13
0.15
1.32
7.89
308.42
309.2
0.78
0.43
0.10
0.58
5.94
311
312
1
0.30
0.11
0.48
8.43
313
315
2
0.80
0.17
0.91
9.43
inc
314
315
1
1.19
0.23
1.30
9.64

Table 5 – Relevant Diamond Drilling Assay Results – Smiths Well

Note. Downhole intervals use a nominal cut off >2,000ppm Cu

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JORC TABLE 1 FOR THE YUINMERY PROJECT

Section 1 Sampling Techniques and Data

Criteria JORC Code Explanation JORC Code Explanation Commentary Commentary
Sampling Nature and quality of sampling (eg Samples collected from diamond core at
techniques cut channels, random chips, or interval lengths from 0.2m-1.2m
specific specialised industry (commonly 1.0m). Lithology, geological
standard measurement tools boundaries, sulphide content, alteration
appropriate to the minerals under and structure are considered in
investigation, such as down hole determining sample intervals.
gamma sondes, or handheld XRF Core selected for sampling is cut in half,
instruments, etc). These examples with one half sent for assay analysis and
should not be taken as limiting the the remaining half retained.
broad meaning of sampling Samples are submitted to Intertek
Include reference to measures taken Laboratories, Maddington for multi-
to ensure sample representivity and element and Au analysis using acid digest
the appropriate calibration of any and aqua regia methods
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 Drill type (e.g. core, reverse Diamond drilling from surface to end of
Techniques circulation, open-hole hammer, hole.
rotary air blast, auger, Bangka, Downhole surveys using Axis Champ
sonic, etc) and details (e.g. core Gyro
diameter, triple or standard tube, Core orientation using orientation tool kit
depth of diamond tails, face- HQ2 diameter core from surface until
sampling bit or other type, whether competent fresh rock encountered, HQ3
core is oriented and if so, by what triple-tube used on occasions
method, etc). NQ2 diamond core is drilled from
competent fresh rock to end of hole
Drill sample Method of recording and assessing Diamond drilling used as the most
recovery core and chip sample recoveries effective drill method in reducing
and results assessed. contamination, preserving geology.
Measures taken to maximise sample Where core loss is encountered it is
recovery and ensure representative marked by the driller on the core block
nature of the samples. and verified by Empire personnel
Whether a relationship exists
between sample recovery and grade
and whether sample bias may have

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occurred due to preferential
loss/gain of fine/coarse material.
Logging Whether core and chip samples All drilling is geologically logged in the
have been geologically and field by a qualified geologist. Lithological
geotechnically logged to a level of and mineralogical data was recorded for
detail to support appropriate Mineral all drill holes using a coding system
Resource estimation, mining studies developed specifically for the Project.
and metallurgical studies. Primary and secondary lithologies are
Whether logging is qualitative or recorded in addition to colour, grain size,
quantitative in nature. Core (or alteration type and intensity, estimates of
costean, channel, etc) photography. mineral quantities.
The total length and percentage of Geological logging is qualitative in nature.
the relevant intersections logged.
Sub-sample If non-core, whether riffled, tube No sub sampling undertaken
techniques and sampled, rotary split, etc and
sample whether sampled wet or dry.
preparation 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.
Quality of The nature, quality and The assaying and laboratory procedures
assay data and appropriateness of the assaying and used are appropriate for the material
laboratory laboratory procedures used and tested.
tests whether the technique is considered Sampling was guided by Empire’s QAQC
partial or total. procedures.
For geophysical tools, Certified analytical standards and blanks
spectrometers, handheld XRF comprise approximately 5% of samples
instruments, etc, the parameters submitted for analysis
used in determining the analysis The laboratory will also carry out its own
including instrument make and internal QAQC checks including
model, reading times, calibrations duplicates taken from the submitted
factors applied and their derivation, samples.
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.
Verification of The verification of significant The drill program was completed under
sampling and intersections by either independent guidance of the listed CP who is a full-
assaying or alternative company personnel. time employee of Empire.
The use of twinned holes. No twin holes were drilled
Documentation ofprimary data, data

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entry procedures, data verification, Geological logs and sampling data were
data storage (physical and recorded into excel spreadsheet
electronic) protocols. templates on a laptop. These files were
Discuss any adjustment to assay compiled and loaded into an Access
data. database.
No adjustment to assay data was carried
out unless noted.
The samples are selected based on the
geological logging.
Location of Accuracy and quality of surveys Collars were initially surveyed by Empire
Data points used to locate drillholes (collar and Resources personnel using a hand-held
down-hole surveys), trenches, mine GPS which has an estimated accuracy of
workings and other locations used in +/- 5m
Mineral Resource estimation. Hole locations are surveyed with a DGPS
Specification of the grid system unit soon thereafter
used. The grid system used for the location of
Quality and adequacy of topographic all drill holes is GDA94 MGA Zone 50
control. Surface elevation is adjusted using points
surveyed by DGPS and reported when
appropriate.
Data spacing Data spacing for reporting of Drill holes were generally spaced at 50m
and Exploration Results. across lines spaced between 75m and
distribution Whether the data spacing and 50m.
distribution is sufficient to establish The hole spacing provided good
the degree of geological and grade coverage along the drill line.
continuity appropriate for the Mineral This drilling is reconnaissance in nature
Resource and Ore Reserve and not of adequate density which to
estimation procedure(s) and generate a Mineral Resource.
classifications applied.
Whether sample compositing has
been applied.
Orientation of Whether the orientation of sampling Holes were drilled approximately
data in relation achieves unbiased sampling of orthogonal to the modelled DHEM
to geological possible structures and the extent to modelled plate
structure which this is known, considering the The direction of sampling is not
deposit type. considered to bias results
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.
Sample The measures taken to ensure Chain of custody is managed by Empire
Security sample security. Resources
Drill core is collected daily from the drill
rig and brought back to the Yuinmery
Station for logging and storage.
Core for sampling is transported by road
to Perth by Empire Resources personnel.
Core is cut and sampled by Empire
Resources personnel in Perth
Samples are delivered by road directly to
the laboratory by Empire Resources
personnel

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Audits or The results of any audits or reviews
reviews of sampling techniques and data.

The program is managed, and data processed by the competent person who is an employee of Empire.

Section 2 Reporting of Exploration Results

Criteria **JORC Code explanation ** **JORC Code explanation ** Commentary Commentary
Mineral Type, reference name/number, The project consists of six granted
tenement and location and ownership including tenements (two mining and four
land tenure agreements or material issues with exploration), for a total area of 106.7 km2
status third parties such as joint ventures,
Mining tenements; M57/265 and M57/636
partnerships, overriding royalties, and exploration tenement; E57/1037 and
native title interests, historical sites, E57/1159 are 100% owned by Empire
wilderness or national park and Exploration tenements are; E57/681 and
environmental settings. E57/1027 are 91.89% owned by Empire
The security of the tenure held at and are subject to a Net Smelter Royalty
the time of reporting along with (NSR) of 1.25%
any known impediments to
obtaining a licence to operate in
_the area. _
Exploration done
Acknowledgment and appraisal of Western Mining Corporation Ltd
by other parties exploration by other parties. commenced base metal exploration in
the area in 1969 and continued until
1981. Soil sampling, ground magnetics,
IP and EM were exploration methods
used to target their vacuum, percussion
and diamond drilling programs.
Esso Australia Ltd explored the area
between 1979 and 1984 using EM, RAB
and diamond drilling in the search for
Golden Grove - Scuddles type base metal
deposits.
Black Hill Minerals Ltd explored part of
the area for base metals between 1986
and 1991. This involved rock chip
sampling and limited percussion drilling.
Meekal Pty Ltd commenced an
exploration program in 1985 by
remapping parts of the syncline and rock
chip sampling. In 1986 Meekal introduced
Arboyne NL into the project who carried
out gold exploration by drilling reverse
circulation holes under old gold workings.
Between 1989 and 1991 RGC Exploration
Pty Ltd explored the area concentrating
on the potential for gold mineralization.
This exploration consisted of geological
mapping, rock chip sampling and some
RAB drilling.
In 1992 Meekal Pty Ltd joint ventured the
project to Giralia Resources NL, who
brought in CRAE as a partner in1993.
CRAE completed a ground EM survey
and drilled three diamond holes in its
search forbasemetals.

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Gindalbie Gold NL then explored the area
for gold between 1995 and 2000. This
work entailed a wide spaced soil
sampling program but although several
anomalous zones were identified no
drilling was undertaken.
Mineral Resources Australia / La Mancha
explored the northern end of the project
area between 2002 and 2010 completing;
extensive soil sampling (Auger),
reconnaissance (RAB / Aircore) drilling
and geophysical surveys (VTEM and
aeromagnetic surveys).
Empire Resources Ltd commenced
exploration in the area during 2006. To
date a number of RAB, RC and diamond
drilling programmes have been
completed as well as aerial, surface and
downhole electromagnetic (EM) surveys.
Geology Deposit type, geological setting The Yuinmery project area covers the
and style of mineralisation. eastern portion of the Archaean Youanmi
greenstone belt with rock types
consisting largely of altered mafic and
ultramafic volcanic and intrusive rocks
with chloritic felsic and intermediate
volcanic units. The volcanic units contain
several intercalated strongly sulphidic
cherty sediments which are host to VMS
copper-gold mineralization. In the project
area these rocks lie on the eastern side of
the regional Youanmi Fault and form the
southern closure of a northerly plunging
syncline.
The volcanic rocks have been intruded by
dolerites, gabbros, pyroxenites and other
ultramafic rocks which probably form part
of the layered Youanmi Gabbro Complex.
Several zones of copper - gold
mineralization have been identified within
the project area by previous surface
sampling and drilling. The volcanogenic
massive sulphide style mineralization is
associated with cherts, felsic volcanic
breccias and tuffs.
Gold mineralisation is interpreted to be
associated with lower order shears
subsidiary to either the Youanmi or
Yuinmery Shear zones. Gold sits in sub-
vertical shears, and forms narrow, steep
plunging high grade shoots at minor
flexures in the shears as quartz-sulphide
lodes.
Drill hole A summary of all information Hole locations are tabulated along with
Information material to the understanding of accompanying collar location diagrams
the exploration results including a within this report
tabulation of the following

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information for all Material
drillholes:
easting and northing of the
drillhole collar
elevation or RL (elevation above
sea level in metres) of the drillhole
collar
dip and azimuth of the hole
down hole length and interception
depth
hole length.
Data aggregation In reporting Exploration Results, Data was compiled using excel
methods weighting averaging techniques, spreadsheets and loaded into an Access
maximum and/or minimum grade database.
truncations (e.g. cutting of high The data was audited using QGIS and
grades) and cut-off grades are Surpac data auditing features.
usually Material and should be A nominal cut-off grade of 2,000ppm Cu
stated. and 100ppb Au have been applied to the
assayresults, unlessnoted.
Relationship If the geometry of the Broad anomalous copper envelopes have
between mineralisation with respect to the been interpreted from the drilling
mineralisation drillhole angle is known, its nature completed. Exact widths and geometry
widths and should be reported. are still to be determined, so all intercepts
intercept lengths If it is not known and only the down are reported as downhole intervals.
hole lengths are reported, there
should be a clear statement to this
_effect. _
Diagrams Appropriate maps and sections Diagrams are included within the report
(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
drillhole collar locations and
_appropriate sectional views. _
Balanced Where comprehensive reporting of All data from the program is provided in
reporting all Exploration Results is not the report
practicable, representative
reporting of both low and high
grades and/or widths should be
practiced to avoid misleading
_reporting of Exploration Results. _
Other Other exploration data, if Not applicable
substantive meaningful and material, should be
exploration data 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. _

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EMPIRE RESOURCES LIMITED ASX: ERL

ASX Announcement 19 May 2022

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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).

A full review of results will be undertaken
prior to planning and execution of future
programs

Reconnaissance drilling programs
planned to test high priority target areas.

Soil and rock sampling programs

Prospect scale mapping

Reinterpretation of geophysical data,
including EM and aeromagnetic /
radiometric data

RC and diamond drilling

Geophysical surveys

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EMPIRE RESOURCES LIMITED ASX: ERL