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RED MOUNTAIN MINING LIMITED Capital/Financing Update 2025

Jun 26, 2025

65719_rns_2025-06-26_ae67f053-9836-43e9-8881-76c1663ba9ba.pdf

Capital/Financing Update

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ASX ANNOUNCEMENT

27 JUNE 2025

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ASX: RMX

Red Mountain Mining Ltd ACN 119 568 106

Australia and Canada based Gold and Battery metals explorer redmountainmining.com.au

HIGH GRADE ANTIMONY CONFIRMS EXCEPTIONAL ARMIDALE POTENTIAL

HIGHLIGHTS

  • Multiple High-Grade Antimony rock chip samples at Oaky Creek returned including:

  • 28.34% Sb

  • 28.33% Sb

  • o 16.38% Sb

  • High-Grade Antimony assay results have been returned from samples collected up to 500m along strike from historical workings, suggesting potential for a large

orogenic Antimony mineral system

  • Shallow costeaning is planned to expose the bedrock beneath strong soil Antimony anomalies with no visible outcrop

  • RMX also plans to undertake a soil and rock chip sampling campaign over the East Hills Antimony and Horsley Station Gold prospects in the southern portion of the

Armidale Project

  • Gold assays for the Oaky Creek rock samples are pending and expected to be received in July

Red Mountain Mining Limited (“ RMX ” or the “ Company ”) is delighted to report highgrade Antimony rock chip results from Oaky Creek, part of RMX’s 100% owned Armidale Antimony-Gold project (EL9732) in the Southern New England Orogen of New South Wales. Results range up to 28.34% Sb for samples containing quartz-stibnite veining, confirming the high tenor of the mineralisation, and high-grade samples have been collected up to 500m from historical workings, suggesting potential for a large, highgrade, Antimony-bearing orogenic vein system. Similar systems, such as Larvotto’s (ASX: LRV) Hillgrove deposit, also located in the Southern New England Orogen, typically also contain high grade gold mineralisation. RMX has submitted a subset of the Oaky Creek rock chip samples for gold analysis by lead fire assay, with results expected in July.

Extension of Antimony Mineralisation Beyond Historical Workings Confirmed By Antimony Rock Chip Assay Results

During the soil sampling program at Oaky Creek, Red Mountain collected 171 rock chip samples (Refer to ASX Announcement 7 June 2025). Due to sparse outcrop in much of the area covered by the soil survey, the majority of these samples were collected in drainages and close to the Oaky Creek North and Oaky Creek South historical workings (Figure 1).

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Figure 1 compares Antimony rock chip and soil results for Oaky Creek. Two samples of quartz-stibnite veining collected more than 2km apart returned the highest values of 28.34% Sb and 28.33% Sb . One of these samples is float from the Oaky Creek South workings, confirming the tenor of the mineralisation mined historically, while the other is from a creek exposure ~500m NNW of Oaky Creek North (Figure 1, 2 and 3). A total of ten rock chip samples contained over 25,000ppm (2.5%) Sb.

Rock Chip Assays Up to 28.3% Sb Confirm High-Grade Antimony Potential at Oaky Creek

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Figure 1 : Comparison of rock chip and soil antimony results for the Oaky Creek prospect. Note the close spatial relationship between mineralised rock chip samples and the >2ppm Sb soil anomalies at Oaky Creek North (Inset A) and Oaky Creek South (Inset B). Values for rock chip samples that contain over 5000ppm (0.5%) Sb are shown. No rock chips samples were collected within the strong (>50ppm Sb) soil anomalies ~800m SSE of the Oaky Creek North and ~300m NW of the Oaky Creek South historical workings due to a lack of outcropping or float material. Refer to Figure 2 for an overview with location co-ordinates.

The samples were collected from in situ outcropping exposures where possible, but subcrop and float samples were collected where this was not possible. The samples were assayed for antimony and tungsten, using sodium peroxide fusion and ICP-MS finish. Rock chip sample locations, nature (outcrop, subcrop or float) and geochemical results are summarised in Appendix 1.

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Figure 2: A continuation of the Map in Figure 1, showing the broader area and locations of Inset A and Inset B.

Red Mountain interprets that the vein-hosted antimony mineralisation mined at Oaky Creek has a significant inferred strike extent, indicating potential for a large tonnage deposit based on:

  • the identification of outcropping high-tenor antimony mineralisation in a creek exposure ~500m NNW of the historical workings at Oaky Creek North;

  • the spatial correlation between mineralised and anomalous rock chip samples; and

  • elevated Antimony in soils.

Mineralised and anomalous rock chip samples show a strong spatial correlation with anomalous (>2ppm) Sb in soils, although due to paucity of outcropping and float material in parts of the survey area, it was not possible to collect rock chips samples across the full length of the approximately 2km long soil anomaly defined for Oaky Creek North or the approximately 1km long anomaly at Oaky Creek South (Figure 1). Most significantly, no outcrop or float material was found within the two new strong >50ppm Sb soil anomalies that were identified by RMX’s sampling. One of these is located ~800m SSE of Oaky Creek North, while the other lies ~300m NW of Oaky Creek South. Both these anomalies warrant further investigation.

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Figure 3 : TOP: Approximately 5m high mineralised creek exposure ~500m NNW of the Oaky Creek North historical workings. View looking SW. BOTTOM: Stibnite-rich vein material collected from the base of the cliff - sample AAR 126, which returned the second highest assay result of 28.3% Sb.

Further Work Planned By Red Mountain At Oaky Creek

Based on these highly encouraging initial results, RMX will continue to progress the Oaky Creek prospect, with a program of shallow costeaning planned to expose and sample bedrock beneath those parts of the soil antimony anomaly where no outcrop was observed. RMX will also undertake detailed geological mapping of

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the costeans and other exposed geology to better understand the relationship between the Namoi Fault system and orogenic vein-hosted antimony mineralisation, with a goal of generating drill-testable targets at Oaky Creek by late 2025. RMX’s future work plans at Oaky Creek will also be influenced by the rock chip gold results, expected in July.

Two Further Priority Antimony And Gold Targets To Be Tested

In addition to Oaky Creek, RMX’s initial assessment of EL9732 identified two further priority exploration targets[1] , which like Oaky Creek feature evidence of historical mining, likely dating from the early 1900s (Figure 3). Neither the East Hills antimony prospect or the Horsley Station gold prospect have previously been explored systematically, with no soil sampling for gold, antimony or silver previously undertaken at either location.

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Figure 4: Surface geology and known antimony, gold and tungsten mineral occurrences of EL9732 and the surrounding area, showing the location of RMX’s three priority targets of Oaky Creek, East Hills and Horsley Station and the Teatree and Bingarra goldfields.

At the East Hills antimony prospect, several shallow pits and a shaft have been sunk on a stibnite bearing reef striking at 170⁰, approximately parallel to the Cobadah and Peel Faults which lie to the east. Red

1RMX ASX Announcement 2 February 2025. https://investorhub.redmountainmining.com.au/announcements/6794753

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Mountain is planning to collect a total of 88 soil samples over a 500 x 600m grid at 100m line spacing and 50m sample interval (Figure 5) during the second half of 2025.

The Horsley Station gold workings comprise a 10m x 3m x 12m deep open cut mined for gold from a narrow quartz reef striking at 100⁰ and dipping steeply to the north. The prospect lies on the Peel Fault with the host mineralisation including fault slices of serpentinite, which is an analogous setting to the gold deposits of the Bingarra and Teatree goldfields, further north along the Peel Fault (Figure 4). RMX plans to collect a total of 233 soil samples at 50m sample intervals and 100m line spacing to locate gold and antimony (Figure 5).

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Figure 5: RMX planned soils sample locations at the East Hills antimony and Horsley Station gold prospects.

Red Mountain Armidale Antimony-Gold Project Background

Red Mountain’s project lies approximately 100km west of Larvotto’s (ASX: LRV) Hillgrove Project and several of Trigg Minerals’ (ASX: TMG) Antimony Projects and extends for 85km immediately west of the Peel Fault.

The Southern New England Orogen is recognised as Australia’s premier Antimony province (Figure 6). Antimony occurs in hydrothermal quartz veins, breccias and stockworks, often with associated gold and/or tungsten mineralisation.

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----- Start of picture text -----

Red Mountain Mining
Armidale Antimony-Gold
Project
----- End of picture text -----

Figure 6: Known NSW gold and antimony mineral occurrences relative to basement orogenic units. The map clearly demonstrates the prospectivity of the New England Orogen for antimony and gold. The location of the Hillgrove Deposit, Peel Fault and EL9732 are also shown.

The geology of the tenement is dominated by isoclinally folded Carboniferous metasediments of the Tamworth Belt, which is a forearc basinal package related to west-dipping subduction of oceanic crust beneath the Lachlan Orogen. Ultramafic melanges of the Great Serpentinite Belt, which outcrop along the Peel Fault, are considered to be remnants of this oceanic crust. The Peel Fault System has recognised worldclass mineral potential, with over 400 known orogenic gold and base metal mineral occurrences along its over 400km strike extent but is underexplored with less than 200 mostly shallow drillholes over its length, the majority of which are focused on discrete prospects.

Authorised for and on behalf of the Board,

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Mauro Piccini

Company Secretary

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About Red Mountain Mining

Red Mountain Mining Limited (ASX: RMX) is a mineral exploration and development company. Red Mountain has a portfolio of critical minerals including gold, lithium and base metal projects, located in Australia, Canada and USA. Red Mountain is progressing its Armidale Antimony-Gold Project in NSW, Kiabye Gold Project in Western Australia and Fry Lake Gold project, based in Canada. In addition, Red Mountain’s project portfolio includes the Nevada Lithium Projects.

Competent Person Statement

The information in this announcement that relates to Exploration Results and other technical information complies with the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code). It has been compiled and assessed under the supervision of contract geologist Mark Mitchell. Mr Mitchell is a Member of the Australasian Institute of Geoscientists and has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the JORC Code. Mr Mitchell consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears.

Disclaimer

In relying on the above mentioned ASX announcement and pursuant to ASX Listing Rule 5.23.2, the Company confirms that it is not aware of any new information or data that materially affects the information included in the above-mentioned announcement.

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JOIN THE RED MOUNTAIN MINING INVESTOR HUB

Visit https://investorhub.redmountainmining.com.au for access to the Investor Hub

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Appendix 1: Rock chip assay results

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JORC Code, 2012 Edition - Table 1

1.1 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 down hole gamma
sondes, or handheld XRF instruments, etc).
These examples should not be taken as
limiting the broad meaning of sampling.
Include reference to measures taken to
ensure sample representivity and the
appropriate calibration of any
measurement tools or systems used.
Aspects of the determination of
mineralisation that are Material to the
Public Report.
In cases where ‘industry standard’ work has
been done this would be relatively simple
(eg ‘reverse circulation drilling was used to
obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire
assay’). In other cases more explanation
may be required, such as where there is
coarse gold that has inherent sampling
problems. Unusual commodities or
mineralisation types (eg submarine
nodules) may warrant disclosure of detailed
information.

Rock samples were collected from 1kg
grab samples.

Rock chip samples were selective based
on visual appearance and are not used
for resource determination, only to check
if mineralisation is present.

All samples are exploration in nature and
not for resource determination.

Rock & Soil samples have been sent to
Intertek Townsville laboratory with the
soils forwarded on to the Perth
Laboratory. Rock samples were assayed
by sodium peroxide fusion FP6/OM for
Sb and W with an I4CP_MS finish.
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). _
• No drilling reported
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.
• No drilling reported.
Logging Whether core and chip samples have been
geologically and geotechnically logged to a
level of detail to support appropriate
Mineral Resource estimation, mining
• No drilling reported.
• Rock sampling is not used for resource
estimation.

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Criteria JORC Code explanation Commentary
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.
Sub-
sampling
techniques
and sample
preparation
If core, whether cut or sawn and whether
quarter, half or all core taken.
If non-core, whether riffled, tube sampled,
rotary split, etc and whether sampled wet
or dry.
For all sample types, the nature, quality and
appropriateness of the sample preparation
technique.
Quality control procedures adopted for all
sub-sampling stages to maximise
representivity of samples.
Measures taken to ensure that the sampling
is representative of the in situ material
collected, including for instance results for
field duplicate/second-half sampling.
Whether sample sizes are appropriate to
the grain size of the material being
sampled.

Rock chip sampling was biased towards
outcrop that was altered including
samples from old shaft workings.

Rock grab samples were taken raw and
approximately 1kg each.

Grab rock samples are first pass with
size appropriate for initial work and not
intended for grade purposes.
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) andprecision have been established.

Rocks were treated at Intertek and with
standard procedure of drying, crushed,
pulverized (in Nickel crucibles) and sodium
peroxide fused and finished with ICP-MS.

Sodium Peroxide fusion is considered an
appropriate method for antimony.

No duplicate, blank and standards (CRM)
were inserted.
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.
• No drill holes reported.
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.
• All sample taken with GPS readings with site
locations recorded in GDA94 (z56).
• No mineral resource estimation was
conducted.

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Criteria JORC Code explanation JORC Code explanation Commentary Commentary
Specification of the grid system used.
Quality and adequacy of topographic
control.
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.
• Rock sample spacing was biased towards
available outcrop which was limited away from
incised creek exposures.
• Being exploration, any sample results will not
be considered sufficient for any ore
determinations.
• No analytical compositing has been reported.
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.
• Rock samples were collected along outcrop
with strike and dip recorded where available.
• No drilling conducted.
Sample
security
The measures taken to ensure sample
security.
• Samples were managed by field staff,
individually double wrapped and sealed in a 1-
ton bulk which was dropped off in a freight
forwarding yard. Samples arrived at the
laboratorysealed.
Audits or
reviews
The results of any audits or reviews of
sampling techniques and data.
• No audit or reviews of sampling techniques
and data was reported.
1.2 Section 2 Reporting of Exploration Results
(Criteria listed in theprecedingsection also applyto this section.)
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 Exploration licence EL9732 is granted
and 100% wholly owned by Red Mountain
Mining and covers 391km2.
• The licence is predominantly in Freehold
pastoral properties and as such Native Title is
extinguished.
Exploration
done by other
parties
Acknowledgment and appraisal of
exploration by other parties.
• The north-south elongate corridor covered
by the project contains no historical mineral
exploration drilling and has seen limited
previous surface exploration for Antimony
and Gold mineralisation. No soil sampling for
these elements has been undertaken and

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Criteria JORC Code explanation Commentary
rockchip and stream sediment coverage is
limited, leaving the majority of the tenement
untested by systematic exploration and
therefore is considered having significant
potential for discovery
Geology Deposit type, geological setting and style
of mineralisation.
• The project is located in the Southern New
England Orogen. The geology of the
tenement is dominated by isoclinally folded
Carboniferous metasediments of the
Tamworth Belt which is a forearc basin
package related to west-dipping subduction
of oceanic crust beneath the Lachlan Orogen.
Ultramafic melanges of the Great
Serpentinite Belt, which outcrop along the
Peel Fault, are considered to be remnants of
this oceanic crust.
• The style of mineralisation target is
hydrothermal quartz veins, breccia and
stockworks derived from fluids during
regional compression and resulting faulting
providingthe conduits to the fluids.
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:
o easting and northing of the drill hole
collar
o elevation or RL (Reduced Level –
elevation above sea level in metres) of
the drill hole collar
o dip and azimuth of the hole
o down hole length and interception
depth
o hole length.
If the exclusion of this information is
justified on the basis that the information
is not Material and this exclusion does not
detract from the understanding of the
report, the Competent Person should
clearly explain why this is the case.
• No drilling conducted
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
• No aggregated methods are reported

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Criteria JORC Code explanation Commentary
shown in detail.
The assumptions used for any reporting of
metal equivalent values should be clearly
stated.
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’). _
• No relationship is made between
mineralisation width and intercept lengths
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.
• Appropriate location diagram is presented in
the text. The diagram is indicative only as no
assumptions of grade, extent or depth are
made.
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.
• Only pertinent results are given as due to the
relevance of the announcement.
Other
substantive
exploration
data
Other exploration data, if meaningful and
material, should be reported including
(but not limited to): geological
observations; geophysical survey results;
geochemical survey results; bulk samples
– size and method of treatment;
metallurgical test results; bulk density,
groundwater, geotechnical and rock
characteristics; potential deleterious or
contaminating substances.
• There is no other substantive exploration
data provided or withheld as this
announcement deals with this early phase
exploration target.
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 forward work programme depends on
full sample assay results from the laboratory.
If encouraging, then costeaning and drilling
programmes will be implements to
determine the depth and lateral extent of
the stibnite mineralisation.
• Diagrams of the sampling positions have
been provided in the text.

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