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First Nordic Identifies New Multi-Kilometric Gold Anomaly and Returns Highest BoT Drilling Grades to Date at Paubäcken Project

Exploration Programs

First Nordic Identifies New Multi-Kilometric

Gold Anomaly and Returns Highest BoT

Drilling Grades to Date at Paubäcken Project

VANCOUVER, BC

,

June 17, 2024

/CNW/ -

First Nordic Metals Corp.

(the

"Company"

or

"First

Nordic"

) (TSXV: FNM) (OTCQB: FNMCF) (FRA: HEG0) is pleased to report results from its recent

belt-scale glacial till geochemical survey and top-of-bedrock / base-of-till ("BoT") drilling program

targeting orogenic gold mineral systems at its 100%-owned Paubäcken project ("Paubäcken" or "the

Project") located in the Gold Line belt, northern

Sweden

. Paubäcken encompasses approximately 30

kilometers ("km") of first-order structural corridor (strike length) of the Gold Line Belt and is located

30 km south of the Company's resource-stage Barsele project [1]. To date, three multi-kilometric,

distinct structural targets have been identified along / off the property's main corridor (Aida,

Harpsund, and Brokojan).

Highlights:

Discovery of Brokojan target – a large (2.3 km by 1 km) orogenic gold system multi-

element pathfinder till anomaly; together with the adjacent Harpsund target, these two

targets now form a large, semi-continuous southeast-northwest trending anomaly over a

5.5 km strike.

Extension of bedrock anomalism along the Aida structural target by approximately 1 km,

to 1.5 km now tested and confirmed for gold mineralization.

Follow-up exploration programs planned in 2024 to continue to advance targets to drill

testing stage.

Taj Singh

, President and CEO states:

"

The latest results from the district-scale Paubäcken

project are highly encouraging. A brand new multi-kilometric anomaly was discovered which, when

combined with a previously identified Harpsund anomaly, forms a 5.5 km long target area along

the Gold Line belt. To put this in context, the Company's Barsele project resource footprint length is

approximately 3.5 km long. Additionally, on the high-priority Aida target, BoT drilling returned 5.01

g/t gold, the highest value to date, and an additional 1 km of footprint was tested and confirmed as

anomalous for gold mineralization.

We look forward to continuing target delineation BoT drilling

activities across the Paubäcken in 2024 as well as diamond drilling at high-priority areas.

Paubäcken Exploration Program

3,050 regional B-Horizon (below topsoil) till samples were collected covering 1,350 hectares over a

12 km strike length of the northern extent of the first order Gold Line Belt structural corridor, and

1,181 metres ("m") in 71 BoT drill holes were completed along the Aida structural corridor target.

For BoT sampling, two BoT samples from directly above the till bedrock interface and two bedrock

samples within the top of bedrock are collected for all drill holes. All samples are screened with X-

ray fluorescence ("XRF") and analysed using a multi-element suite at MSALABS in Storuman,

Sweden

. For glacial till geochemical sampling, all samples are collected from the glacial till derived

B-Horizon soil layer (subsoil) and screened using handheld XRF for pathfinder elements. Anomalous

areas identified will be tested for gold at an external laboratory.

Surface Till Sample Results

Results from the till sampling program have identified a second large gold pathfinder anomaly

(Figure 2) northwest of the previously identified Harpsund 2.5 km by 1 km Au-As-Cu-Zn-Mo anomaly

(gold-arsenic-copper-zinc-molybdenum) along the same structural corridor. Results from the till

sampling program identified the Brokojan target, defined by a As-Cu-Zn-Mo pathfinder element till

anomaly extending over 2.3 km by 1.0 km. The two targets now form a large, semi-continuous

southeast-northwest trending anomaly over a 5.5 km strike of the Harpsund structural corridor. Both

anomalies are oriented in the prominent ice flow direction. The survey focused on identification of

orogenic gold and VMS (volcanogenic massive sulphide) type mineral systems known to be present

in the Gold Line Belt. All surface till samples were analysed using a portable XRF and follow up

analyses will test the anomalous samples for gold. Both anomalies are coincident with historic ionic

leach gold-in-till anomalies (Figure 3).

Geologic Interpretation of the Brokojan and Harpsund Targets

The geology of the Harpsund target area (Figure 4) consists of a complex sequence of folded and

sheared coarse to fine grained metasedimentary units that have been intruded by a series of felsic

dykes and gabbroic units. The Harpsund structural corridor forms a southwest trending second order

splay structure off the regional north-northwest trending Gold Line belt first order structure. The

Harpsund target lies within the hinge of the second order structural corridor and the Brokojan target

at the intersection of the first and second order structures. All sedimentary units demonstrate a

dominant penetrative fabric and strong schistosity, and folding is isoclinal, indicating a high strain

environment. Gold mineralized quartz veins previously mapped and sampled within the Harpsund

target area are preferentially hosted within felsic dykes due to strong rheological contrast with

surrounding metasediments.

BoT Drilling Results at Aida Target

Results from the BoT drilling program (Figure 5) were positive and extended anomalism along the

Aida structural corridor to >1.5 km, including the highest BoT sample result todate on the Project,

5.01 g/t Au in hole PAU-23-BoT-065. The latest BoT drilling tested portions of the structure to the

north and south of previous BoT and diamond drilling. The Aida structural corridor target lies under

up to

25 m

of glacial till cover and has been identified over 4 km in strike using magnetic geophysical

data. Approximately 2.5 km of the target area remains completely untested, and the Company plans

to continue target delineation BoT drilling activities in 2024.

Results from a sub-parallel structure zone were also positive with multiple bedrock samples

encountered that are anomalous against background. The latest BoT program continues to

demonstrate the size potential of the Aida target and follow up BoT drilling is planned for H2 2024

over the remaining untested 2.5 km strike of the structural corridor to develop targets for follow-up

drill testing. The Aida target lies within 3.5 km of the past producing Svartliden gold mine, owned and

operated by Dragon Mining Ltd ("Dragon"). The Svartliden mill and processing plant is still

operational, and processes concentrate ore from Dragon's operations in

Finland

.

Geologic Interpretation of the Aida Target

The geology of the Aida target consists of a sequence of isoclinal folded and sheared fine to course

grained metasedimentary and metavolcanic units. The Aida structural corridor forms a 4 km long

north-northwest trending second order structure sub-parallel to the regional first order Gold Line belt

structure corridor. All units demonstrate a dominant penetrative fabric and schistosity, and folding is

isoclinal, indicating a high strain environment. Mineralization is mainly hosted within the mafic volcanic

and to a lesser extent coarser grained metagreywacke units that make up the foot wall. No

mineralization is present within the finer grained black shale units that make up the hanging wall

lithology. Mineralization is associated with arsenopyrite and both laminated and non-laminated quartz

veins and has an affiliation to the highest strain zones of the mafic volcanic unit located at the

footwall contact between the metavolcanic host and metagreywacke footwall units.

About the Paub

ä

cken Project

The Paubäcken project consists of three licenses totalling 17,097 ha that cover the central part of an

emerging district in north central

Sweden

known as the "Gold Line belt". The Gold Line belt is host to

several significant gold deposits, including the Company's nearby Barsele project (operated as a

joint venture between the Company and Agnico Eagle Mines Ltd.) as well as the Svartliden mine and

Fäboliden development project (operated by Dragon Mining Ltd). The Svartliden mine was in

production from 2005 to 2015 and a total of 3.18 million tonnes of material grading 4.1 g/t Au was

processed during its operation (

http://www.dragonmining.com/svartliden

). Paubäcken is strategically

positioned between Barsele and Fäboliden, is a few hundred meters northeast of the Svartliden

mine, and features a regional shear zone with multiple untested gold anomalies.

About the Gold Line Belt Geology

The geology of the Gold Line belt consists of an inverted volcano-sedimentary sequence intruded by

small pre- to syn-kinematic granitic intrusions within a broad, anastomosing high strain structural

corridor. Lithologies are regionally metamorphosed to upper greenschist and amphibolite grade

facies, and gold mineralization is associated with intense sericite, carbonate, biotite, and calc-silicate

alteration assemblages and sulphide minerals pyrite, arsenopyrite, and pyrrhotite. The regional Gold

Line structural corridor runs up the axis of the belt with many jogs, splays, and zones of structural

complexity that are potential locations for dilation and deposition of gold bearing fluids. These

lithological sequences are deemed to be highly prospective for orogenic gold deposits.

About First Nordic Metals

First Nordic's flagship is the Barsele gold project, located in

Sweden

and in a joint venture with

senior gold producer Agnico Eagle Mines Ltd. The Barsele project currently hosts a combined open

pit and underground NI 43-101 Indicated Resource of 324,000 ounces gold and an Inferred resource

of 2,086,000 ounces gold [1]. Immediately surrounding the Barsele project, First Nordic is the 100%-

owner of a district-scale license position of close to 100,000 hectares on both the prolific Gold Line

belt and Skellefte VMS belt. Additionally, in northern Finland First Nordic holds the entire

underexplored Oijärvi greenstone belt.

ON BEHALF OF THE BOARD OF DIRECTORS

Taj Singh

, M.Eng, P.Eng, CPA

President & CEO, Director

Qualified Person

Benjamin Gelber

, P. Geo., Chief Technical Director of the Company, is the Qualified Person as

defined in NI 43-101 and takes responsibility for the technical disclosure contained within this

news release.

References

[1] Technical Report and Mineral Resource Estimate for the Barsele Property, 2020, InnovExplo

Follow First Nordic Metals:

Twitter: @fnmetals | Youtube: @firstnordicmetalscorp | LinkedIn: @firstnordicmetals

Facebook: @FirstNordicMetals | Instagram: @firstnordicmetals

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in

policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this

release.

Cautionary Note Regarding Forward-Looking Statements:

This News Release contains forward-looking statements, including but not limited to comments

regarding the timing and content of upcoming work programs, geological interpretations, receipt of

property titles, potential mineral recovery processes, etc. Forward-looking statements address

future events and conditions and therefore involve inherent risks and uncertainties. Actual results

may differ materially from those currently anticipated in such statements and Barsele undertakes no

obligation to update such statements, except as required by law.

APPENDIX

Figure 1: Gold Line Belt project area with regional geology, showing locations of 2023/24 exploration

programs. (CNW Group/First Nordic Metals Corp.)

Figure

1

: Gold Line Belt project area with regional geology, showing locations of 2023/24

exploration programs.

Figure 2: Map of Paubäcken project area showing regional till sampling geochemical results (CNW

Group/First Nordic Metals Corp.)

Figure

2

: Map of Paubäcken project area showing regional till sampling geochemical results

Figure 3: Map of Paubäcken project area showing historic ionic leach gold-in-till results (CNW

Group/First Nordic Metals Corp.)

Figure

3

: Map of Paubäcken project area showing historic ionic leach gold-in-till results

Figure 4: Geological map of the Harpsund structural corridor (CNW Group/First Nordic Metals

Corp.)

Figure

4

: Geological map of the Harpsund structural corridor

Figure 5: Map of the Aida Target area showing BoT drilling results and recent extension of confirmed

gold mineralization (CNW Group/First Nordic Metals Corp.)

Figure

5

: Map of the Aida Target area showing BoT drilling results and recent extension of

confirmed gold mineralization

SOURCE

First Nordic Metals Corp.

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For further information:

For further information contact: Alicia Ford, Business Development

Manager, Phone: 403-604-9646, Email: [email protected]

CO: First Nordic Metals Corp.

CNW 04:00e 17-JUN-24