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AERO Energy and Fortune BAY Announce Completion of Drilling Program ON the Murmac Uranium Project

Exploration Programs

TSXV: FOR | FWB: 5QN | OTCQB: FTBYF

fortunebaycorp.com

NEWS RELEASE

AERO ENERGY AND FORTUNE BAY ANNOUNCE COMPLETION OF DRILLING PROGRAM

ON THE MURMAC URANIUM PROJECT

HALIFAX, NS July 24, 2024 – Fortune Bay Corp. (TSXV:FOR, FWB:5QN, OTCQB: FTBYF) (“Fortune

Bay” or the “Company”) is pleased to announce completion of the 2024 summer drill program on the

Murmac Uranium Project (“Murmac” or the “Project”), located in northern Saskatchewan near Uranium City.

The program was designed to test regional targets across the Project for high-grade, unconformity-related

basement-hosted deposits typical of the Athabasca Basin. The drilling program was funded by Aero Energy

Limited (TSXV: AERO) (OTC Pink: AAUGF) (FSE: UU3) (“Aero”), and was operated by Fortune Bay, under

an Option Agreement that was executed on December 15, 2023.

Highlights:

• An average of 1,309 counts per second was intersected over 8.7 metres in hole M24-017 in

structured graphitic pelite, with up to 33,600 counts per second (“cps”) (using handheld RS-125

Spectrometer) associated with visible uranium mineralization. This interval is located approximately

70 to 78 metres below surface.

• Hole M24-017 was followed up with three additional holes (M24 -018, -019 and -020), comprising

approximate 50 metre step outs down -dip, along -strike northeast, and along -strike southwest,

respectively. All three holes returned anomalous radioactivity (up to 850 cps) in graphitic rocks

underlying a hematized quartzite hangingwall.

• These results (drill holes M24 -17 to -020) confirm the presence of a larger hydrothermal uranium

mineralizing system along this unexplored, 1.2 kilometre long electromagnetic (“EM”) conductor on

the Howland Corridor.

• Drill holes M24-021, M24-022A and M24-023, tested geophysical (EM and gravity) anomalies H6 ,

A22, and H16 respectively, intersecting compelling hydrothermal alteration and structure associated

with variably graphitic rocks, further confirming the prospectivity of the entire length of the Howland

and Armbruster Corridors for unconformity-related, basement-hosted deposits.

• Following uranium assay and geochemical analysis of d rill core samples , a second phase drilling

program is being planned to follow-up along strike of mineralized drill holes and continue testing of

priority drill targets across the Project.

Dale Verran, CEO for Fortune Bay, commented “ The summer 2024 drilling program at Murmac provides

further confirmation of the potential to deliver a high-grade basement-hosted uranium discovery at Murmac.

The program has significantly enhanced our geological understanding of the unexplored target horizons

and we eagerly await uranium assay and geochemical analyses to assist with vectoring toward a potentially

meaningful discovery. The zone of strong radioactivity intersected in M24-017 was a particular highlight ,

indicative of a strong uranium mineralizing system on this conductor and validates the targeting and

exploration approach. Together with our partners, Aero Energy, we look forward to planning a follow -up

program where larger step-outs from M24-017 are expected to be prioritized, in addition to testing numerous

other high priority targets.”

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Initial Drill Results

A total of eight drill holes were completed at Murmac during June and July, 2024 to test targets documented

in the News Release dated June 4, 2024 along the Pitchvein, Armbruster and Howland Corridors (Figure

1; Table 2) . Drill holes targeted compelling geophysical signature s (electromagnetics and gravity) and

favorable geological/structural settings. Drill target selections also took into account p roximity to historical

uranium occurrences of interest and Fortune Bay’s previous positive drilling results. The completed drill

holes encountered highly favorable geological settings for high -grade basement -hosted deposits

associated with the Athabasca Basin. This included:

• Thick and strongly graphitic target units (up to an estimated ~30 metres in true thickness) often in

contact with quartzites, providing favorable competency/rheological contrast.

• Brittle faulting and brecciation were observed within, or proximal to, the graphitic units and were

typically associated with favorable hydrothermal alteration including abundant hematite, chlorite,

sulphides, and clays.

• Anomalous radioactivity (>300 cps) was intersected in five of the eight holes completed, associated

with cataclastic or mylonitic structured and altered graphitic pelites, as summarized in Table 1.

Table 1: Murmac Drill Hole Radiometric Highlights (Summer 2024)

Hole ID Radioactivity Highlights

From (m) To (m) Length (m) cps Lithology

M24-016A

93.50 93.65 0.15 350 Amphibolite

94.75 95.05 0.30 340 Graphitic pelite

95.70 95.95 0.25 340 Graphitic pelite

235.65 235.80 0.15 340 Psammite

M24-017

81.10 81.70 0.60 432 Hematized quartzite

82.55 83.05 0.50 590 Hematized quartzite

84.00 84.60 0.60 838 Hematized quartzite

85.50 85.80 0.30 317 Hematized quartzite

85.80 94.50 8.70 1,309 Graphitic pelite

incl. 86.10 86.65 0.55 10,608 Graphitic pelite

incl. 86.45 86.55 0.10 33,600 Graphitic pelite

and incl. 87.00 87.40 0.40 2,776 Graphitic pelite

and incl. 92.00 92.20 0.20 7,395 Graphitic pelite

126.80 127.20 0.40 355 Graphitic pelite

M24-018 138.15 142.05 3.90 337 Graphitic pelite

M24-019 100.90 101.10 0.20 650 Graphitic pelite

M24-020 154.85 155.25 0.40 553 Graphitic pelite

Note: Radioactivity values reported are total gamma from NQ2 drill core measured with a Super-SPEC RS-125 handheld spectrometer

reported in counts per second (“cps”). The cps values are averages for the reported drill interval unless otherwise specified .

Measurements of total gamma cps are an indication of the presence of uranium, thorium and/or potassium, but may not directly

correlate with chemical uranium assays. Total gamma cps results are preliminary in nature and may not be used directly to qua ntify

uranium concentrations in the drill core samples. True thicknesses of the drill core intersections are yet to be determined. Results for

M24-017 have been reported previously.

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Figure 1: Murmac 2024 Drill Collar Locations.

Drill Hole Summary

A summary of the drill holes are provided as follows:

M24-016A: The targeted conductor (moderate to strongly graphitic pelite) was intersected between 94.4

and 120.7 m. This step-out hole, approximately 100 metres northeast of positive results in 2022 drill holes

M22-013 and M22-014, and 175 metres southwest of positive historical results from SMDC drilling (CKI-9

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and CKI-10), intersected anomalous radioactivity in graphitic pelite (Figure 2), indicating possible continuity

of mineralization between these two locations.

Figure 2: Hole M24-016A (target P7), 92.8 to 99.3 m. Anomalous radioactivity hosted in structured graphitic

pelite.

M24-017: This hole tested geophysical (EM and gravity) target H15, which occurs at the intersection of the

EM conductor and a property-scale, mineralized cross -fault, beneath Howland Lake. Intermittent

anomalous radioactivity (up to a maximum of 1,800 cps over 0.1 m etre) was intersected in hematized,

faulted hangingwall quartzite. This overlies a structured graphitic pelite averaging 1,309 cps over 8.70

metres, with measurements up to 33,600 cps over 0.1 metre. This intersection (Figure 3), of radioactivity

hosted in previously unexplored (under a shallow lake) graphitic pelite, at a cross-fault location, provides a

compelling validation of the exploration target, justifying down -dip and along strike follow up (sub sequent

three drill holes).

Figure 3: M24-017 (target H15) radioactive intersections (81.00 to 94.50 metres down hole). Hangingwall

quartzite hosts intermittent radioactivity from 81.00 to 85.80 m. Continuous elevated radioactivity is hosted

in the underlying graphitic pelite.

M24-018: Steeper follow up of M22 -017, shows down -dip continuity (approximate 50 metres vertical) in

anomalous radioactivity hosted in graphitic pelite (Figure 4), up to a maximum of 660 cps over 0.1 metre.

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Figure 4: M24-018 (down dip test of target H15) radioactive intersections in graphitic pelite down-dip (~50

m vertically below) of the intersection in M24-017.

M24-019: Approximate 50 metre step out to the northeast from M22-017. Anomalous radioactivity was

hosted in strongly graphitic pelite, confirming presence of active mineralizing system along strike, up to a

maximum of 780 cps over 0.1 metre (Figure 5).

Figure 5: M24-019 radioactive intersections in graphitic pelite along strike 50 m to the NE of M24 -017

(target H15).

M24-020: Approximate 50 metre step out to the southwest from M22-017. Anomalous radioactivity was

hosted in graphitic pelite, confirming presence of active mineralizing system along strike, up to a maximum

of 850 cps over 0.1 metre (Figure 6).

Figure 6: M24-020 radioactive intersections in graphitic pelite along strike 50 m to the SW of M24 -017

(target H15).

M24-021: This hole tested a compelling geophysical (EM and gravity) target (H6) on the Howland Corridor.

While no anomalous radioactivity was intersected, the targeted conductor (strongly graphitic pelite) is

associated with intense hydrothermal alteration and pervasive faulting (Figure 7).

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Figure 7: M24-021 (target H6) strongly graphitic pelite in contact with structured hydrothermally altered

bleached and hematized quartzite.

M24-022A: This hole tested a compelling geophysical (EM and gravity) target (A22) on the southern

Armbruster Corridor. While no anomalous radioactivity was intersected, the targeted conductor (heavily

structured strongly graphitic pelite) also shows hydrothermal alteration with a strongly hematized

hangingwall quartzite overlying the graphitic unit (Figure 8).

Figure 8: M24-022A (target A22) hydrothermal alteration reduction/oxidation front, transitioning from

hematized quartzite to underlying heavily structured strongly graphitic pelite.

M24-023: This hole tested a compelling geophysical (EM and gravity) target (H16) on the Howland

Conductor Corridor, also testing along strike (approximately 600 m SW) of positive results in 2022 drill hole

M22-012. Only two minor intervals (<4 metres) of moderately graphitic pelite were intersected, with no other

notable conductive horizons. This could indicate that M24-023 drilled through a faulted offset and missed

the targeted conductor, drilling through heavily faulted and hematized underlying footwall quartzite.

M24-024 (P4): This hole was designed to test the southwest strike extension of the mineralized graphitic

pelite in M22-013/014 along the Pitchvein Corridor, at the intersection with the same regional cross-cutting

structure tested in M24-017 (target P4). The hole was abandoned at 47.5 metres due to intense brittle

faulting within hematized quartzite and therefore did not reach the targ eted graphitic unit . The intense

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faulting within the hangingwall is encouraging and the target warrants testing to the required depth .

Alternative drill locations will be assessed for a future program.

Table 2: Murmac Drill Hole Summary (Summer 2024)

Hole ID Target ID Easting Northing Azimuth Dip Length (m)

M24-016A P7 630799 6593053 302 -54 258

M24-017 H15 633345 6593642 310 -55 201

M24-018 H15DD 633345 6593642 310 -67 177

M24-019 H15NE 633385 6593691 298 -55 171

M24-020 H15SW 633337 6593593 305 -45 180

M24-021 H6 631386 6589720 315 -50 164.5

M24-022A A22 627965 6585975 305 -55 167.7

M24-023 H16 632955 6592531 320 -55 177

M24-024 P4 630332 6592498 315 -45 47.5*

Notes: Coordinates are reported in UTM NAD83 Zone 12N. Azimuth is true north.

Target prefix A= Armbruster Corridor; H = Howland Corridor; P = Pitchvein Corridor.

*Drill hole M24-024 was abandoned due to intense brittle faulting.

Next Steps

Drill core samples have been collected systematically throughout all zones of radioactivity higher than 300

cps and will be submitted to SRC Geoanalytical Laboratories in Saskatoon for U 3O8 assay and multi -

element characterization. These analytical results will be integrated with the detailed logging information to

prioritize follow-up target areas for future drill testing, in addition to testing of numerous other priority

regional targets. Following on from the Murmac drill program, Aero and Standard Uranium (TSXV: STND;

OTCQBQB: STTDF; FWB: 9SU) plan to test additional targets on the adjacent Sun Dog Project located to

the south of Murmac on the Crackingstone Peninsula.

Technical Disclosure

Preliminary radiometric results represent total gamma from NQ2 drill core measured with a Super -SPEC

RS-125 handheld spectrometer reported in counts per second (“cps”). Measurements are typically collected

over 0.10 to 0.15 metre intervals through areas of anomalous radioactivity (defined as >300 counts per

second, or “cps”). Longer intervals with less variation are shown as length weighted averages for simplicity.

Core is removed from the core box and moved, if necessary, to a location where the instrument reads below

background, and the measurement is collected by placing the sensor against the core at the required

location. The drill cores are subject to comprehensive logging and sampling to characterize mineralization,

alteration and structure. Drill core samples will be submitted to the Saskatchewan Research Council

(“SRC”) Geoanalytical Laboratories (ISO/IEC 17025:2005 accredited) for uranium assay and multi-element

characterization. Reflectance spectrometry will be undertaken on additional core samples to determine the

presence of indicator clay alteration.

Further details regarding the historical uranium occurrences noted in this news release can be found within

the Saskatchewan Mineral Assessment Database (SMAD) and the Saskatchewan Mineral Deposit Index

(SMDI). Fortune Bay has verified the majority of these occurrences through field prospecting and sampling,

however there is a risk that any future confirmation work and exploration may produce results that

substantially differ from the unverified historical results. The Company considers these unverified historical

results relevant to assess the mineralization and economic potential of the property. The historical drill

results obtained by SMDC in drill holes CKI-9 and CKI-10 can be found within the SMAD references 74N07-

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0310 and 74N07 -0311 and have not been verified. Additional historical exploration results (uranium

occurrences related to geochemistry results and scintillometer prospecting) derive from SMAD references

74N07-0290, 74N07-0287 and 74N07-0304.

Qualified Person

The technical and scientific information in this news release has been reviewed and approved by Gareth

Garlick, P.Geo., Technical Director of the Company , who is a Qualified Person as defined by NI 43 -101.

Mr. Garlick is an employee of Fortune Bay and is not independent of the Company under NI 43-101.

About Fortune Bay

Fortune Bay Corp. (TSXV:FOR, FWB:5QN, OTCQB:FTBYF) is an exploration and development company

with 100% ownership in two advanced gold exploration projects in Canada, Saskatchewan (Goldfields

Project) and Mexico, Chiapas (Ixhuatán Project), both with exploration and development potential. The

Company is also advancing seven uranium exploration projects on the northern rim of the Athabasca Basin,

Saskatchewan, which have high-grade potential. The Company has a goal of building a mid-tier exploration

and development Company through the advancement of its existing pr ojects and the strategic acquisition

of new projects to create a pipeline of growth opportunities. The Company’s corporate strategy is driven by

a Board and Management team with a proven track record of discovery, project development and value

creation. Further information on Fortune Bay and its assets can be found on the Company’s website at

www.fortunebaycorp.com or by contacting us as [email protected] or by telephone at 902 -334-

1919.

On behalf of Fortune Bay Corp.

”Dale Verran”

Chief Executive Officer

902-334-1919

Cautionary Statement Regarding Forward-Looking Information

Information set forth in this news release contains forward-looking statements that are based on assumptions as of the date of this

news release. These statements reflect management's current estimates, beliefs, intentions, and expectations. They are not

guarantees of future performance. Words such as “expects”, “aims”, “anticipates”, “targets”, “goals”, “projects”, “intends”, “plans”,

“believes”, “seeks”, “estimates”, “continues”, “may”, variations of such words, and similar expressions and references to future

periods, are intended to identify such forward-looking statements.

Since forward-looking statements are based on assumptions and address future events and conditions, by their very nature they

involve inherent risks and uncertainties. Although these statements are based on information currently available to the Company,

the Company provides no assurance that actual results will meet management’s expectations. Risks, uncertainties and other factors

involved with forward-looking information could cause actual events, results, performance, prospects and opportunities to differ

materially from those expressed or implied by such forward-looking information. Forward looking information in this news release

includes, but is not limited to, the Company’s objectives, goals, intentions or future plans, statements, exploration results, potential

mineralization, timing of the commencement of operations and estimates of market conditions. Factors that could cause actual

results to differ materially from such forward-looking information include, but are not limited to failure to identify targets or

mineralization, delays in obtaining or failures to obtain required governmental, environmental or other project approvals, po litical

risks, inability to fulfill the duty to accommodate First Nations and other indigenous peoples, inability to reach access agreements

with other Project communities, amendments to applicable mining laws, uncertainties relating to the availability and costs of

financing or partnerships needed in the future, changes in equity markets, inflation, changes in exchange rates, fluctuations in

commodity prices, delays in the development of projects, capital and operating costs varying significantly from estimates and the

other risks involved in the mineral exploration and development industry, and those risks set out in the Company’s public documents

filed on SEDAR+. Although the Company believes that the assumptions and factors used in preparing the forward-looking

information in this news release are reasonable, undue reliance should not be placed on such information, which only applies as of

the date of this news release, and no assurance can be given that such events will occur in the disclosed time frames or at all. The

Company disclaims any intention or obligation to update or revise any forward-looking information, whether as a result of new

information, future events or otherwise, other than as required by law. For more information on Fortune Bay, readers should r efer to

Fortune Bay's website at www.fortunebaycorp.com.

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

accepts responsibility for the adequacy or accuracy of this release.