REG - Power Metal Res. - Fermi Exploration: Summer 2025 Exploration Update
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RNS Number : 3060Y Power Metal Resources PLC 08 September 2025
8 September 2025
Power Metal Resources PLC
("Power Metal" or the "Company")
Uranium Joint Venture
Fermi Exploration: Summer 2025 Exploration Update
Power Metal Resources plc (AIM:POW, OTCQB:POWMF), the London-listed
exploration company with a global project portfolio, is pleased to provide an
update on the completed, in progress, and forthcoming exploration work in the
provinces of Labrador and Northern Saskatchewan in Canada.
The update concerns work undertaken by Power Metal and Fermi Exploration Ltd
("Fermi"). Fermi is the uranium-focused joint venture (the "Joint Venture" or
"JV") comprising Power Metal's portfolio of uranium licences.
HIGHLIGHTS:
· A seven-hole, 2,660 m diamond drilling programme has been completed
on the Drake Lake-Silas Property in Labrador, which intersected a 2.05 m thick
hematite breccia recording 600 ppm Uranium and up to 5,000 Counts Per Second
("CPS").
· A six-hole 1,563 m diamond drilling programme was carried out on the
Perch River Property, testing an inferred shear structure at depth, coincident
with anomalous soil geochemistry and radon results.
· Permit application to conduct Mineral Exploration on the Badger Lake
property is in progress; once approved (expected mid-September), the team will
mobilise to test a gravity geophysics high coincident with electromagnetic
geophysical and geochemical anomalies in the S-Zone.
· A radon and swamp bed sampling programme has been completed on the
Fortin River Property to inform future exploration on that property.
· A drill programme is planned on the East Hawkrock Property, due to
commence in Q1 2026.
Sean Wade, Chief Executive Officer of Power Metal Resources PLC commented:
"Fermi Exploration's summer exploration programmes have delivered strong
technical progress across multiple projects, with encouraging geological and
mineralisation results emerging at Drake Lake-Silas and comprehensive target
testing at Perch River. Alongside this, we continue to advance permitting at
Badger Lake, where drilling is expected to begin in the coming weeks, and
detailed geophysical analysis at East Hawkrock. These developments underscore
the scale and diversity of opportunity within the uranium joint venture
portfolio. With further drilling at new targets planned in the near term, we
look forward to building additional momentum as we continue to advance and
refine this exciting exploration pipeline".
OVERVIEW
Over the summer of 2025, Fermi has advanced several exploration projects
across its Canadian uranium portfolio. At Perch River, in the Athabasca Basin,
Saskatchewan, a series of detailed surveys guided a six-hole drill programme
that successfully mapped key structures and alteration but did not return
significant mineralisation. At Drake Lake-Silas, seven holes were completed,
confirming two zones of mineralisation, including a hematite breccia with
elevated uranium values via pXRF and a massive sulphide zone within a
prospective metasedimentary horizon. Preparations continue at Badger Lake,
where a drilling permit is expected imminently to allow drilling of targets
coincident with strong geophysical and geochemical anomalies.
A combination of wildfire disruption and the geographically challenging
targets has led to the postponement of drilling at East Hawkrock until winter
2026. At Fortin River, the company completed a small combined radon and
lake-sediment sampling programme to follow up on survey results indicating the
presence of a large impact structure. At Reitenbach, fieldwork is underway to
extend and constrain the Nuphar Zone, an area of radon and uranium,
(206/204)Pb isotope in soil anomaly. Fermi is completing further analysis on
the Durrant Lake Property to inform future targeting efforts and is advancing
the Pardoe property through data integration and geophysical inversion
modelling to develop further targets for future exploration.
Perch River
Prior to drilling at Perch River, Fermi completed multiple geophysical surveys
and geochemical sampling to refine targets, including:
Ø FALCON® Airborne Gravity Gradiometry and Magnetic Survey
Ø Xcite Electromagnetic Airborne Survey
Ø Ambient Noise Tomography ("ANT") Ground Survey
Ø Soil, radon, and helium sampling (detailed here:
https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/ryn9qkw
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/ryn9qkw)
)
Drilling at Perch River was designed to test a vertical to sub-vertical shear
structure identified through ANT, directly coincident with highly anomalous
soil geochemistry and radon results. This target ("The Rapids Zone") lies on
the edge of an inferred fault-controlled paleobasin, with complex structural
geology and elevated paleotopography of the unconformity - key features
observed at multiple unconformity-related uranium deposits (1 2 3) (4).
The Rapids Zone lacked significant electromagnetic conductors, though a
moderately conductive body (1.3 mS/m) was detected within the zone and
interpreted as hematite alteration, with the principal drill target at the
Rapids Zone being the vertical to sub-vertical shear structure, mineralisation
contained within, and proximal to it.
While encouraging alteration and the targeted fault structure were
successfully intersected along a 400 m extent of the Rapids Zone, no
significant uranium mineralisation was encountered, and the programme was
concluded after 1,563 m of diamond-drilled NQ core in six drillholes (Table 1)
Fermi is currently awaiting assay results and reviewing geological data to
inform next steps, and will report in full once the results are available.
Drilling was completed by Team Drilling, with technical support from Axiom
Exploration Group and helicopter support from Access Helicopters, the
exploration programme was run out of the Community of Stoney Rapids.
Drake Lake Silas
The drill programme on Drake Lake Silas was designed to test for two main
targets: Iron Oxide Copper Gold ("IOCG") style mineralisation in the centre of
the property, and a potential continuation of economic mineralisation from the
Armstrong Deposit, 550-1,000 m to the northeast. To support this targeting and
build on the previous exploration results, Fermi commissioned a Mobile MT
geophysical survey to help determine the conductivity of the underlying
geology and completed the first Ambient Noise Tomography survey in Labrador,
which informed the drill targeting.
Alongside the drilling, surface mapping and sampling were completed by the
Fermi Technical Team and on-site geologists, primarily to verify the existence
of a mapped granite (and thus a potential source of mineralising fluids) in
the centre of the property, as well as to confirm the presence of historically
mapped carbonate alteration and uraniferous occurrences.
A total of seven NQ (78 mm wide), diamond drill holes, totalling 2,600 m, were
completed (Table 2), and two significant occurrences of mineralisation have
been identified to date:
Drillholes DL25-01 and DL25-02 were drilled to test geology beneath the
historically identified Anomaly 15 and Anomaly 16 targets, respectively, in
the centre of the property. DL25-05 supplemented drilling in this area
following the identification of a radioactive intercept. DL25-03 and DL25-04
were drilled to test for the southwest extension of mineralisation from the
Armstrong deposit; DL25-06 targeted a potential IOCG-style system in the
southeast of the property; and DL25-07 was drilled to test for a lateral
continuation of the mineralisation encountered in DL25-02 and DL25-05. An
eighth hole was planned, but was postponed due to poor weather and a late
start to the programme due to access issues.
In Drillhole DL25-02, at a depth of 496.65 m (circa 277.6 m True Depth "TD"),
a 2.05 m thick hematite breccia recording up to 5,000 Counts Per Second
("CPS") and up to 600 ppm U via handheld pXRF was intersected, within 12 m of
elevated radiation. This narrow intercept lies within an inferred shear
structure, characterised by apparent metasedimentary geology, which cuts
through the basaltic sequence of the property. The unit shallows to the
northeast, where drillhole DL25-05 was collared to intercept it.
In DDH DL25_05, approximately 600 m to the northeast and along strike of
DL25_02, in a target area exhibiting similar geophysics, a massive sulphide
stockwork was encountered between 232.75 m (approximately 126.6 m TD) and
256.5 m (approximately 139.6 m TD); approximately 24 m wide, and localised
4-45 cm wide sulphide lenses from 238.93 m (circa 129.9 m TD) to 247.28 m
(circa 134.6 m TD), composed primarily of massive pyrrhotite, pyrite,
sphalerite, arsenopyrite, and chalcopyrite, were encountered. This
mineralisation occurs within a minor metasedimentary bed within the basalt and
likely represents primary sulphide mineralisation.
Both occurrences appear to be stratigraphically controlled within a
sulphide-rich metasedimentary unit, as indicated by the Mobile MT and ANT
datasets. This unit represents a priority target for follow-up exploration on
the Drake Lake-Silas Property. Further sporadic occurrences of radiation were
present in DL25_02 between 97.8 m (53.2-74.8m TD) and 137.5 m (between 50-1100
CPS), and between 294.8 m (160.5m TD) and 342.1 m (186.2m TD) (between 200-300
CPS). These appear to be related to minor veining and recrystallisation, and
their relationship to the mineralisation described above is currently unclear
No economic mineralisation was encountered in the drill holes along strike
from the Armstrong deposit (DL25_03 and DL25_04). However, the intersected
geology appears to be very similar to the deposit itself(5), with a
carbonate−albite-altered shear zone (which also hosts the mineralisation at
Armstrong) intersected within the metasedimentary rocks at depths of between
182.15 and 211.75m (TD) in DL25_03, and between 206 and 230m (183.6 to 204.6m
TD) in DL25_04. The area remains prospective; however, given the short
timeframe, the early stage of the drilling programme, and the presence of
multiple other targets to be tested, drilling in the northeast of the property
was terminated after the completion of these two initial holes.
Fermi is currently evaluating additional work programmes to enhance future
targeting on the property, including a ground-based induced polarity (IP)
geophysics survey to characterise the sulphide-rich metasedimentary unit
further, and help identify further target locations of the hematite breccia.
In addition, petrographic samples will be analysed to better understand the
detailed geology of the mineralised intercepts and other key intervals,
alongside whole-rock samples for geochemical and Short Wave InfraRed analysis.
Titjaluk Logistics led the Drake Lake exploration programme as the principal
contractor working in partnership with Rally Drilling Services for drilling
operations, Mercator Geological Services for technical expertise, and
Helicopters Canada providing helicopter logistics. The programme was based out
of the town of Postville, Labrador, which is within the Nunatsiavut Land Claim
Area.
Badger Lake
The proposed drillhole locations and target were discussed in the Company
announcement of 18 June 2025;
https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/wk641yx
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/wk641yx)
Fermi is currently awaiting a Saskatchewan Ministry of Environment Crown Land
Work Authorisation to include drilling of up to 30 holes on land, clearing of
trails, clearing of drill pads and clearing of helicopter pads (the "drilling
permit") to facilitate the drill programme. The drilling permit is expected to
be granted by mid-September, with mobilisation to commence shortly thereafter.
The drilling permit has been delayed due to the late issuance of the
duty-to-consult process with Indigenous Communities in the area. Fermi has
engaged all relevant communities and is working collaboratively with them to
advance the permitting process.
To further enhance the targets on the property, Fermi has received inverted
gravity survey data, which outlines a gravity high directly coincident with
the S-Zone. The S-Zone corresponds to a weak electromagnetic anomaly
straddling the unconformity and is overlain by coincident anomalous uranium,
(206/204) lead isotope ratios, cobalt, and nickel results, as discussed in the
previous release.
East Hawkrock
Fermi had intended to, and had received the necessary permits to, facilitate a
drill programme on East Hawkrock in mid-summer 2025. However, due to target
location and access issues caused by regional wildfires, it was elected to
delay the drilling until Q1 2026. To further evaluate the property's geology,
Fermi has engaged an expert geophysicist to conduct a comprehensive analysis
of the electromagnetic, gravity, and magnetic datasets, which will assist the
Fermi Exploration team in defining robust drill targets. Upon the completion
of this work, a full discussion of the targets will be provided.
Preliminary analysis indicates that the majority of the targets are located
beneath shallow lakes. Given the shallow unconformity on the property,
drilling solely from land would be both technically challenging and
potentially limit the scope of the campaign. As such, Fermi intends to conduct
an eight-hole programme between February and April 2026, where drilling can be
completed from the frozen lake surface as well as the land.
Fortin River
On 18 February, the Company released results of the combined electromagnetic
and magnetic survey over the Fortin River Property, which indicated the
presence of an impact crater, as detailed in the following release:
https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/x23987r
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/x23987r)
To support further work and help define if the impact crater may host uranium
mineralisation, Fermi completed a combined radon-in-water and
swamp/lake-bottom sampling programme in June 2025. Preliminary results are in
hand; however, Fermi is awaiting the analysis of the swamp/lake-bottom samples
before proceeding further, given the potential for uranium enrichment from
secondary sources in lake-bottom sediments. Such enrichment could provide a
local, shallow source of radon, rather than indicating potential uranium
mineralisation at depth. Results will be reported in due course
Reitenbach
As announced 21 March 2025, the 2024 sampling work on the Reitenbach Property
(see
https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/rm8povw
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/rm8povw)
) left the combined soil and radon anomaly open to the north of the Nuphar
Target. Constraining the extent of this anomalous area was identified as a key
objective for the 2025 exploration programme.
To advance this work, Fermi has commissioned a small field programme targeting
the northern ('up-ice') extension of the Nuphar anomaly. The aim is to refine
and narrow the prospective area for future work, which may include
ground-based geophysics and/or drilling. Currently, this programme is on hold
due to wildfires in the area, but is expected to be completed by the end of
October 2026.
Other Properties
Geophysical analysis of the West Hawkrock property has failed to indicate the
existence of any conductive lithologies at depth, nor any significant gravity
lows or other targets on the property. In light of the current results, Fermi
has elected to pause further exploration on the West Hawkrock Property.
Fermi is continuing to evaluate the prospectivity of the Durrant Lake
Property, having completed a supplementary HTEM survey on the south of Durrant
Lake in June 2025. Fermi is in receipt of a drill permit on the Durrant Lake
Property, and has both budget and contractors allocated for the potential
drill programme.
Fermi is evaluating the completion of a work programme on the Pardoe Property
(whose acquisition was announced 11 December 2024
https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/xl4jejr
(https://polaris.brighterir.com/public/power_metal_resources/news/rns/story/xl4jejr)
). To support this, Fermi has commissioned Vorticity, a Silicon Valley-based
firm innovating in scientific computing, to integrate and invert the multiple
historical datasets acquired for the property. If the results of this analysis
are positive, Fermi may consider deploying a field programme or conducting
additional geophysical surveys in autumn and winter 2025, to advance the
project to a drilling stage in 2026.
Drillhole Details
Table 1: Drillhole Details on the Perch River Property
DDH Name Easting (NAD83 UTM Zone 13N) Northing (NAD83 UTM Zone 13N) Azimuth° Dip ° Depth (m)
PR25-001 508356.3 6552606 162 -45 377
PR25-002 508356 6552606 - -90 (vertical) 230
PR25-003 508377 6552566 141 -84 203
PR25-004 508830 6552760 317 -60 119
PR25-004A 508214 6552325 318 -70 395
PR25-005 508830 6552760 143 -61 239
Table 2: Drillhole Details on the Drake Lake Silas Property
DDH Name Easting (NAD83 UTM Zone 20N) Northing (NAD83 UTM Zone 20N) Azimuth° Dip ° Depth (m)
DL-25-01 628314 6034013 315 -53 332
DL-25-02 628909 6035268 310 -57 569
DL-25-03 629333 6035875 - -90 (vertical) 314
DL-25-04 629519 6035677 310 -63 281
DL-25-05 628400 6035591 310 -56 320
DL-25-06 629855 6033761 310 -63 401
DL-25-07 628234 6035010 310 -85 443
GLOSSARY
Term Explanation
Albite alteration (carbonate-albite alteration) A chemical change in rocks caused by hot, mineral-rich fluids. These fluids
replace original minerals with albite (a sodium feldspar) and carbonate
minerals. Common around uranium deposits and used as a targeting guide.
ANT (Ambient Noise Tomography) A geophysical imaging method that uses natural background vibrations of the
Earth to map underground structures
Breccia (hematite breccia) A rock made of broken fragments cemented together. In hematite breccia, the
cement is iron oxide. The broken texture can allow metal-rich fluids to flow
and deposit minerals.
Conductive body A rock zone that can carry an electrical current, detected in electromagnetic
surveys. Conductivity often comes from sulphides, graphite, or salty water,
and may point to mineralisation.
Counts Per Second (CPS) A measure of radioactivity recorded by handheld radiation detectors. High CPS
suggests uranium or thorium in the rocks. Quick field tool, but confirmed by
assays.
Data integration and inversion A process of combining multiple exploration datasets (gravity, magnetic, EM,
geochemistry) into 3D computer models. Helps geologists refine drill targets.
Electromagnetic survey (EM) A geophysical survey using EM signals to detect conductive rocks. Conductive
zones can be linked to mineralisation (graphite, sulphides, or water-filled
fractures).
FALCON® Airborne Gravity Gradiometry An airborne survey that measures tiny variations in Earth's gravity. Denser
rocks (like hematite) show up as "gravity highs," while lighter rocks or
alteration zones show as "gravity lows."
Impact crater / impact structure A circular geological feature formed by a meteorite or asteroid collision,
characterised by shocked rocks, brecciation, fracturing, and sometimes central
uplifts or ring structures.
Induced Polarity (IP) survey A geophysical method measuring how well rocks temporarily hold an electrical
charge. Sulphide-rich rocks often give strong IP signals.
IOCG (Iron Oxide Copper Gold) mineralisation A style of deposit containing iron oxides (hematite/magnetite) with copper,
gold, uranium, and other metals. These deposits can be very large and
valuable.
Magnetic survey A survey measuring variations in Earth's magnetic field caused by magnetic
minerals. Helps map rock types and structures linked to mineralisation.
Massive sulphide A solid body of sulphide minerals (pyrite, pyrrhotite, sphalerite,
chalcopyrite). Often forms valuable ore deposits.
Metasedimentary horizon/rocks Sedimentary rocks (sandstone, shale) that have been changed by heat/pressure
(metamorphism).
Mobile MT survey A geophysical method using natural electromagnetic fields to map resistivity
of rocks at depth. Good for imaging deep structures that may control
mineralisation.
Paleotopography The shape of the Earth's surface in ancient times, with reference to the
Athabasca Basin, this was the land surface before the deposition of the
overlying sediments.
Petrographic sample A thin rock slice prepared for microscopic analysis to determine mineral
composition, textures, and alteration, aiding interpretation of rock history
and ore-forming processes.
pXRF (portable X-ray fluorescence) A handheld device that estimates metal content in rocks quickly by shooting
X-rays into themA handheld, energy-dispersive XRF device that rapidly measures
elemental composition of rocks, soils, and sediments in the field, using
characteristic secondary X-ray emissions. Useful in the field, but less
accurate than laboratory assays.
Stockwork A dense network of intersecting mineral-filled veins or veinlets within rock,
formed by repeated fluid flow, often creating significant, bulk-tonnage ore
zones in mineral deposits.
Stratigraphically controlled Mineralisation restricted to a specific rock layer or stratigraphic horizon,
where geological layering dictates the distribution, continuity, and geometry
of the ore body.
SWIR (Short Wave InfraRed analysis) A spectral technique measuring short-wave infrared light absorption in
minerals, used to identify alteration minerals (e.g., clays, carbonates) and
interpret hydrothermal alteration or mineralising fluid pathways.
TD (True Depth) The vertical distance from surface to a geological feature or intercept,
correcting for drillhole angle, ensuring accurate three-dimensional
positioning of mineralisation.
Unconformity A boundary between very old rocks and younger rocks, representing a time gap.
In the Athabasca Basin, unconformities are prime sites for high-grade uranium.
Veining and recrystallisation Mineral deposition within fractures (veining) and re-formation of crystals
under heat or pressure (recrystallisation), both indicating fluid flow and
potential pathways for ore formation.
REFERENCES
1 Jefferson, C.W., Thomas, D.J., Gandhi, S.S.,
Ramaekers, P., Delaney, G., Brisbin, D., Cutts, C., Portella, P. and Olson,
R.A., 2007. Unconformity-associated uranium deposits of the Athabasca Basin,
Saskatchewan and Alberta. Bulletin-geological survey of Canada, 588, p.23.
2 Reid, K.D., Ansdell, K., Jiricka, D., Witt, G. and
Card, C., 2014. Regional setting, geology, and paragenesis of the centennial
unconformity-related uranium deposit, Athabasca Basin, Saskatchewan, Canada.
Economic Geology, 109(3), pp.539-566.
3 Yeo, G., Potter, E., 2010, Review of reducing
mechanism potentially involved in the formation of unconformity-type uranium
deposits and their relevance to exploration. Saskatchewan Geological Survey,
Saskatchewan Ministry of Energy and Resources, Miscellaneous Report 12, 13 p
4 Young, N., Chi, G., Liu, Y. and Song, H., 2023.
Graphite does not function as a direct reducing agent for unconformity-related
uranium mineralization-Evidence from the graphitic metapelite-hosted Gryphon
uranium deposit, northern Saskatchewan, Canada. Ore and Energy Resource
Geology, 15, p.100028.
5 Sparkes, G.W., 2017. Uranium mineralization within
the Central Mineral Belt of Labrador: A summary of the diverse styles,
settings and timing of mineralization. St. John's: Government of Newfoundland
and Labrador, Department of Natural Resources, Geological Survey, Open File
LAB/1684, 198 p.
QUALIFIED PERSON STATEMENT
The technical information contained in this disclosure has been read and
approved by Mr Nick O'Reilly (MSc, DIC, MIMMM QMR, MAusIMM, FGS), who is a
qualified geologist and acts as the Qualified Person under the AIM Rules -
Note for Mining and Oil & Gas Companies. Mr O'Reilly is a Principal
consultant working for Mining Analyst Consulting Ltd which Power Metal
Resources PLC has retained to provide technical support.
The information contained within this announcement is deemed by the Company to
constitute inside information as stipulated under the Market Abuse Regulation
(EU) No. 596/2014 as it forms part of UK domestic law by virtue of the
European Union (Withdrawal) Act 2018. Upon the publication of this
announcement via a Regulatory Information Service, this inside information is
now considered to be in the public domain.For further information please
visit https://www.powermetalresources.com/
(https://www.powermetalresources.com/) or contact:
Power Metal Resources plc
Sean Wade (Chief Executive Officer) +44 (0) 20 3778 1396
SP Angel Corporate Finance LLP (Nomad and Joint Broker)
Ewan Leggat/Jen Clarke +44 (0) 20 3470 0470
Tamesis Partners LLP (Joint Broker)
Richard Greenfield/Charlie Bendon +44 (0) 20 3882 2868
BlytheRay (PR Advisors)
Tim Blythe/Alastair Roberts +44 (0) 20 7138 3204
powermetalresources@blytheray.com
NOTES TO EDITORS
Power Metal Resources plc (AIM: POW, OTCQB: POWMF) is a London-listed
natural resources exploration company and project incubator which finances and
manages global resource projects and is seeking large scale metal discoveries.
The Company has a principal focus on opportunities offering district scale
potential across a global portfolio including precious, base and strategic
metal exploration in North America, Africa, Saudi
Arabia, Oman and Australia.
Project interests range from early-stage greenfield exploration to later-stage
prospects currently subject to drill programmes.
Power Metal will develop projects internally or through strategic joint
ventures until a project becomes ready for disposal through outright sale or
separate listing on a recognised stock exchange thereby crystallising the
value generated from our internal exploration and development work.
Value generated through disposals will be deployed internally to drive the
Company's growth or may be returned to shareholders through share buy backs,
dividends or in-specie distributions of assets.
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