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First Atlantic Nickel Has Commenced Drilling at New Alloy MAX Zone Discovery, 7 Km North of Rpm Zone, at the Pipestone Xl Nickel-Cobalt Alloy Project

Exploration Programs

FIRST ATLANTIC NICKEL HAS COMMENCED DRILLING AT NEW ALLOY MAX ZONE

DISCOVERY, 7 KM NORTH OF RPM ZONE, AT THE PIPESTONE XL NICKEL-COBALT

ALLOY PROJECT

GRAND FALLS -WINDSOR, Newfoundland and Labrador - (GlobeNewsWire - April 8, 2026) - First

Atlantic Nickel Corp. (TSXV: FAN) (OTCQB: FANCF) (FSE: P21) ("First Atlantic" or the "Company") is

pleased to announce that drilling has commenced at the Alloy Max Zone, a new large- scale awaruite

(Ni₃Fe) nickel-cobalt alloy discovery located 7 kilometers (km) north of the RPM Zone. The Alloy Max

Zone represents the Company's second major target area within the 30 km Pipestone Ophiolite Complex

at its Pipestone XL Nickel-Cobalt Alloy Project in central Newfoundland. The Alloy Max discovery was

first announced on March 18, 2026 , following the Company's ongoing district -wide surface sampling

program, which identified a new large area of magnetically recoverable nickel -cobalt alloy

mineralization. The initial target area measures approximately 4 km in length and 1.2 km in width.

The initial drill program at Alloy Max is designed to test for awaruite mineralization over a large area

through four drill holes distributed across 2.4 km of strike length and approximately 950 m in width within

the initial 4 km x 1.2 km defined target area. Due to minimal overburden, geologists were able to directly

sample bedrock at the drill pad locations and identif ied visibly disseminated awaruite mineralization in

surface bedrock prior to drilling.

The Company has completed a drill access trail to the Alloy Max Zone from the existing camp and will

now begin construction of a drill access road extending north from Alloy Max through Super Gulp toward

Atlantic Lake, following the geologic 30 km nickel t rend of the Pipestone Ophiolite Complex. As road

construction proceeds northward, the Company plans to conduct direct bedrock sampling through

shallow pits and trenches along the road corridor to evaluate newly identified and historical areas with

elevated DTR nickel values that were previously inaccessible by ground.

HIGHLIGHTS:

1. Drilling Commenced at Alloy Max Zone: Drilling has commenced at the Alloy Max Zone, with four

initial drill pad locations spanning 2.4 km in strike length and testing nickel -cobalt alloy mineralization

across an area approximately 950 m in width. The Alloy Max Zone is located 7 km north of the RPM

Zone within the 30 km Pipestone Ophiolite Complex.

2. Visible Awaruite Discovered in Bedrock Prior to Drilling: Prior to drilling, geologists sampled

bedrock through shallow pits in areas of minimal overburden at the Alloy Max Zone and identified visibly

disseminated awaruite in bedrock at drill pad locations across the 2.4 km strike length and 950 m width

covered by the initial drill holes.

3. Second Large-Scale Nickel-Cobalt Alloy Target Area: Alloy Max, first announced on March 18,

2026, has an initial defined target area of approximately 4 km x 1.2 km. Geological mapping and

geophysics indicate Alloy Max may host a larger mineralized area than the RPM Zone. DTR surface

sampling has returned magnetically recoverable nickel-cobalt alloy grades comparable to surface values

at the RPM Zone, where drill core consistently returned higher DTR grades in drill core.

4. Initial Drill Holes Testing Awaruite Mineralization Across 2.4 km Strike Length: Surface bedrock

samples collected from shallow pits at drill pad locations at the Alloy Max Zone confirmed visible

awaruite mineralization. The 4 drill pad locations span 2.4 km in strike length and 950 m in width. The

program is designed to test for magnetically recoverable awaruite mineralization to establish initial

results and guide further drilling.

5. Drill Access Road North From Alloy Max Toward Atlantic Lake: The Company has completed a

drill access trail to the Alloy Max Zone and will now begin construction of a drill access road extending

north from Alloy Max through Super Gulp toward Atlantic Lake, following the 30 km geologic nickel trend

of the Pipestone Ophiolite Complex. Upon completion, the road will connect to Grand Falls-Windsor and

the Trans-Canada Highway, providing full vehicle access across the entire complex for exploration and

development activities.

6. Bedrock Sampling During Road Construction Along 30 km Trend: Along the corridor between

Alloy Max and Atlantic Lake, the Company has identified areas of interest based on newly identified

DTR nickel surface samples that may indicate additional awaruite nickel-cobalt alloy mineralized zones

previously inaccessible by ground. The Company plans to conduct direct bedrock sampling through

trenching and shallow pits during road construction, which has been designed to closely follow the 30

km nickel trend of the Pipestone Ophiolite Complex.

For further information, questions, or investor inquiries, please contact Rob Guzman at First

Atlantic Nickel by phone at +1-844-592-6337 or via email at [email protected].

Drilling at the Alloy Max Zone is targeting magnetically recoverable awaruite nickel -cobalt alloy

mineralization across a broad area within the initial 4 km x 1.2 km target area, as outlined through the

integration of field geological mapping, surface rock sampling, DTR (magnetic separation and recovery)

analysis, and geophysics. The four initial drill pad locations span 2.4 km of strike length and are

positioned to test an area approximately 950 m wide prospective for nickel-cobalt alloy mineralization.

The objective of the program is to test for the presence and continuity of magnetically recoverable

awaruite nickel-cobalt alloy across the Alloy Max Zone and to generate initial results to guide further

drilling. At the RPM Zone, this exploration model has proven effective, with drill core samples

consistently returning higher DTR nickel grades than weathered surface samples. The Company

anticipates that a similar pattern may occur at Alloy Max, where surface DTR values are comparable to

those recorded at the RPM Zone.

During site preparation at the drill pad locations, minimal overburden allowed geologists to directly

examine and sample bedrock, where visibly disseminated awaruite was encountered at various pad

sites. This observation further supports the presence of aw aruite nickel-cobalt alloy mineralization at

surface across the Alloy Max target area and is consistent with the surface sampling results reported on

March 18, 2026.

Figure 01: Bedrock sample collected beneath shallow overburden at a drill pad location. The sample

confirms the drill target prior to drilling and contains visible disseminated awaruite magnetic nickel cobalt

alloy mineralization.

Figure 02: Map of the Alloy Max and RPM Zone areas showing DTR nickel (%) in surface rock

samples, including Alloy Max drill pad locations and the RPM 2025 drill holes.

Figure 03: Drilling underway at the Alloy Max Zone, testing newly defined targets within the 4 km by 1.2

km wide target area 7 km north of RPM Zone discovery.

PIPESTONE XL DRILL ACCESS ROAD AND EXPLORATION PROGRAM

The Company has completed a drill access trail from the existing camp to the Alloy Max Zone and will

now begin construction of a drill access road extending north from Alloy Max through Super Gulp toward

Atlantic Lake, following the 30 km geologic nickel trend of the Pipestone Ophiolite Complex. Upon

completion, the road will provide full vehicle acc ess from the camp into Grand Falls -Windsor and the

Trans-Canada Highway, which crosses Newfoundland, thereby connecting the entire complex with

ground access for exploration and development activities.

Along this corridor between Alloy Max and Atlantic Lake, the Company has identified areas of interest

based on newly identified DTR nickel surface samples that may indicate additional awaruite nickel -

cobalt alloy mineralized zones. Many of these areas were previously inaccessible by ground. The

Company plans to conduct direct bedrock sampling through trenching and shallow pits during road

construction, which has been designed to closely follow the 30 km nickel trend of the Pipestone Ophiolite

Complex. As construction advances, the Company will systematically explore prospective ground

across the trend, advancing the identification of new nickel -cobalt alloy target areas while building the

access required for long-term project development.

NEWFOUNDLAND JUNIOR EXPLORATION ASSISTANCE

The Company would like to express its gratitude to the Province of Newfoundland and Labrador for

awarding it the maximum grant of $150,000 under the Junior Exploration Assistance (JEA) program.

This funding will support critical mineral exploration at the Company's Pipestone XL Nickel-Cobalt Alloy

Project, a district -scale nickel-cobalt alloy project strategically located in central Newfoundland with

access to key infrastructure, including roads and clean hydro-grid power. Newfoundland and Labrador

is consistently ranked among the world's leading mining jurisdictions.

Newfoundland & Labrador has ranked in the top 10 globally for mining investment attractiveness from

2022 to 2025 according to the Fraser Institute's Annual Survey of Mining Companies; The 2024 survey

states1:

"Only two Canadian jurisdictions ranked in the top 10 for their investment attractiveness:

Saskatchewan (7th) and Newfoundland & Labrador (8th)."

The report further notes:

"Newfoundland & Labrador stands out among all jurisdictions included in the sub- survey, with

86 percent of respondents indicating that they were able to acquire the necessary permits for

exploration in two months or less."

The province combines world- class geology with supportive government policies, well -established

infrastructure, and efficient permitting for mineral exploration and development.

AWARUITE (Ni₃Fe) - EARTH'S RAREST NATURALLY MAGNETIC HIGH- GRADE NICKEL-IRON-

COBALT ALLOY MINERAL

Awaruite (Ni₃Fe) is a naturally occurring nickel-iron-cobalt alloy mineral containing approximately 77%

nickel2 - 2 to 3 times the nickel content of typical sulfide minerals such as pentlandite (~25% Ni) 3.

Awaruite forms during serpentinization, a geological process in which ultramafic peridotite reacts with

water, generating molecular hydrogen gas (H ₂), and liberated nickel (Ni² ⁺) and iron (Fe² ⁺) then react

with this abundant hydrogen to form the alloy. B ecause awaruite already exists in a reduced metallic

state composed entirely of metal elements with no sulfur, it requires no smelting, roasting, or acid

leaching. This offers a direct mine-to-refinery or stainless steel pathway that bypasses the bottleneck of

limited North American smelting capacity.

1 https://www.fraserinstitute.org/sites/default/files/2025-07/annual-survey-of-mining-companies-2024_0.pdf

2 https://www.sciencedirect.com/science/article/abs/pii/S0892687522002667

3 https://fpxnickel.com/projects-overview/what-is-awaruite/

Figure 04: Quote from USGS on Awaruite Deposits4

Awaruite's strong natural magnetic properties - up to 10 times more magnetic than magnetite - enable

recovery through magnetic separator drums commonly used in large- scale open-pit bulk-tonnage iron

ore mines across North America for over a century. DTR is a standard metallurgical test used in iron ore

mining globally to measure the recovery of magnetic minerals, and is a specific method for measuring

awaruite recovery from drill core.

As stated in the August 2025 report "From Rocks to Power" from the Battery Metals Association of

Canada5:

"Awaruite is not a sulfide nor an oxide nickel ore but a high-content native nickel–iron ore. Simple

beneficiation processes after mining could provide 60% Ni concentrate, ready for leaching for

battery cathode purposes and would yield MHP as a by -product. This process would bypass

pyrometallurgy or early hydrometallurgy stages and be among the lowest carbon-intensive nickel

production sites in the global nickel market."

The Battery Metals Association of Canada has also stated in June 20256:

4 https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/mineral-pubs/nickel/mcs-2012-nicke.pdf

5 https://transitionaccelerator.ca/wp-content/uploads/2025/08/From-Rocks-to-Power-Nickel.pdf

6 https://netzeroindustrialpolicy.ca/wp-content/uploads/2025/07/BMAC_TA_EFL_Western_Canadian_Battery_Value_Chain.pdf

"A future nickel metallurgical plant could be designed to produce nickel sulfate or even

precursors to the cathode active material (pCAM) for NMC batteries. Nickel sulfate can be

produced by leaching nickel matte from nickel sulfide concentrates if the fac ility is a

smelter, or it can be easily produced from a hydrometallurgical facility leaching awaruite

concentrates.”

INVESTOR INFORMATION

The Company's common shares trade on the TSX Venture Exchange under the symbol " FAN", the

American OTCQB Exchange under the symbol "FANCF" and on several German exchanges, including

Frankfurt and Tradegate, under the symbol "P21".

Investors can get updates about First Atlantic by signing up to receive news via email and SMS text at

www.fanickel.com.

FOR MORE INFORMATION:

First Atlantic Investor Relations

Robert Guzman

Tel: +1 844 592 6337

[email protected]

DISCLOSURE

Adrian Smith, P.Geo., a director and the Chief Executive Officer of the Company is a qualified person

as defined by NI 43 -101. The qualified person is a member in good standing of the Professional

Engineers and Geoscientists Newfoundland and Labrador (PEGN L) and is a registered professional

geoscientist (P.Geo.). Mr. Smith has reviewed and approved the technical information disclosed herein.

ANALYTICAL METHOD & QA/QC

Representative rock samples were collected in the field from outcrops or subcrop exposures, while

avoiding float material. Sample locations were documented using handheld GPS units. All samples were

securely sealed, labeled and shipped to Activation Laboratories Ltd. (“Actlabs”) in Ancaster, Ontario, an

ISO 17025 certified and accredited laboratory operating independently of First Atlantic.

Each sample was crushed, with a 250 g sub-sample pulverized to 95% passing 200 mesh. A magnetic

separation was then generated by running the pulverized sub- sample through a magnetic separator

which splits the sub-sample into magnetic and non-magnetic fractions. This involves running a 30 g split

of the pulp through a Davis Tube magnetic separator as a slurry using a constant flow rate, a magnetic

field strength of 3,500 Gauss, and a tube angle of 45 degrees to produce magnetic and non -magnetic

fractions.