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Fortune BAY Confirms Near-Surface Uranium Mineralization IN Multiple Drill Holes ON the Murmac Uranium Project

Exploration Programs

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

fortunebaycorp.com

NEWS RELEASE

1969 Upper Water Street, Suite 2001, Purdy’s Wharf Tower II, Halifax, NS B3J 3R7 T 902.422.1421 | F 902.491.4281

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FORTUNE BAY CONFIRMS NEAR-SURFACE URANIUM MINERALIZATION

IN MULTIPLE DRILL HOLES ON THE MURMAC URANIUM PROJECT

HALIFAX, NS December 1 3, 202 2 – Fortune Bay Corp. (TSXV:FOR, FWB:5QN, OTCQX: FTBYF )

(“Fortune Bay” or the “Company”) is pleased to announce analytical results from its maiden exploration

drilling program on the 100% owned Murmac Uranium Project (“Murmac” or the “Project”) , located in

northern Saskatchewan (see Figure 1).

The drilling program was designed to test regional targets across the Project ’s extensive Armbruster,

Howland and Pitchvein Conductor Corridors , which have a combined strike length of approximately 30

kilometres.

Shallow, highly elevated concentrations of uranium were confirmed in six (6) of the fifteen (15) drill holes,

including 0.18% U3O8 and 0.17% U3O8 from individual assay samples.

The uranium is associated with anomalous levels of “pathfinder” elements that are typically associated with

high-grade, basement-hosted deposits in the Athabasca Basin.

Results include shallow intersections derived from between 20 and 150 m etres below su rface within

prospective graphitic units associated with favourable structure and alteration.

Dale Verran, CEO for Fortune Bay, commented “We are pleased to have intersected uranium in our first

drilling campaign at Murmac. The results indicate we are exploring fertile corridors for high-grade uranium

deposits and provide some immediate areas for priority follow-up. The shallow nature of the uranium

encountered, and proximity to infrastructure within a historical uranium mining area, makes for a compelling

exploration scenario. Planning is underway for a drilling program in 2023 to provide follow-up of these

results and continued testing of the corridors on the Project.”

Highlights:

• Drill hole M22-002 (target A6) intersected 0.18% U3O8 from 82.0 to 82.1 metres (approximately 63

metres below surface), with the interval from 82.0 to 82.3 metres averaging 899 ppm U.

• Drill hole M22-012 (target H11) intersected 0.17% U3O8 from 102.2 to 102.3 metres (approximately

72 metres below surface), with the interval from 102.1 to 102.3 metres averaging 646 ppm U.

• Drill hole M22-013 (target P1) intersected intermittent intervals of anomalous uranium, including 347

ppm U from 30.8 to 31.4 metres, 205 ppm U from 35.9 to 36.9 metres, and 448 ppm U from 44.2 to

44.5 metres. These intervals occur over a broad 13 metre zone from approximately 29 to 42 metres

below surface.

• Drill hole M22 -014 (target P1) intersected an average of 241 ppm U over 3.0 m etres from 36.9 to

39.9 metres (approximately 20 metres below surface).

• Drill hole M22-015 (target A10) intersected a maximum of 0.12% U3O8 from 158.2 to 158.3 metres

(approximately 87 metres below surface), with the interval from 158.1 to 158.3 metres averaging

503 ppm U. The interval 161.2 to 161.5 metres averaged 122 ppm U. The interval 163.3 to

163.8 metres averaged 219 ppm U.

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Figure 1: Location of Fortune Bay’s Murmac, Strike and Goldfields Projects.

Analytical Results

A total of 15 drill holes ( 3,168 metres) were completed along the P itchvein, Armbruster, and Howland

Corridors on the Murmac Uranium Project, as announced in the News Release dated August 23, 2022. Drill

hole locations are shown in Figure 2.

Anomalous uranium (>100 ppm) was encountered along all three of the corridors tested. The drill holes

listed in Table 1 intersected shallow , anomalous uranium with pathfinder element enrichment typically

associated with high-grade basement-hosted deposits of the Athabasca Basin. These anomalies are found

in host rocks including thick and strongly graphitic units 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, clays and/or bleaching.

Clay species identification on drill core samples has confirmed the presence of favorable clay alteration

associated with uranium and pathfinder enrichment (Table 1). Chlorite and illite occur as the dominant clay

species with intermittent occurrences of kaolinite. Dravite (an encouraging clay indicator) is present in

M22-012, associated with anomalous uranium at 146.5 metres. Dravite, associated with elevated boron (up

to 1,170 ppm) is present in M22-009, which targeted the intersection of the Armbruster Conductor with a

major cross-cutting fault (Heatherington Fault).

A summary of anomalous uranium encountered is provided in Table 1, with descriptions of pathfinder

element associations and relevant lithological, structural and alteration features.

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Table 1: Summary of anomalous (>100 ppm) uranium intersections.

Target Hole ID From

(m)

To

(m)

U

(ppm)

U3O8

(wt %)

Associated

Pathfinders Description

A6 M22-002

81.2 82.7 206

B, Cu, Pb,

Zn, Ag Foliated and fractured graphitic pelite,

below the contact with overlying quartzite.

Associated with hematization, chlorite

alteration, graphitic shearing and faulting.

incl. 82.0 82.3 899

incl. 82.0 82.1 1,520 0.18

91.0 91.1 208 Pb, Co, As,

Zn, Ag

H1 M22-004 82.9 83.0 209 - Hosted in chlorite-altered graphitic pelite,

proximal to a graphitic fault.

H11 M22-012

102.1 102.3 646 Pb, As, Co,

Cu

Within graphitic pelite in a hematized

graphitic shear / breccia zone. incl. 102.2 102.3 1,150 0.17

146.3 146.5 115 V

Massive hematized gabbro at contact with

underlying hematized pelite with localized

faulting. Clay analysis confirms the

presence of dravite.

P1 M22-013

25.2 26.0 133 V, B, Cu

Anomalous U within graphitic pelite

characterized by patchy hematization,

chloritic shears, pyrite, local quartz

flooding and disseminated sericite.

Bleaching and clay alteration continues

below zone of anomalous U.

Drill hole located approximately 225 m SW

(along strike) of mineralized intersections

from historical core holes, including 1.01%

U3O8 over 2.0 m (56.0 to 58.0 m in drill

hole CKI-9) and 2.19% U3O8 over 0.5 m

(68.0 to 68.5 m in drill hole CKI-10).

30.8 31.4 347 B, V incl. 30.8 30.9 653

35.9 36.9 205 B, V

44.2 44.5 448 B, V

57.4 58.0 135 V

59.0 59.3 110 -

60.0 60.5 104 B, V

64.0 64.2 108 B

67.6 67.9 163 V, Zn

226.2 227.3 121 V, Cu

Apparent association with vuggy texture in

psammite with bleaching, hematization,

chloritization and elevated pyrite content.

P1 M22-014

36.9 39.9 241 V, Cu, Zn,

Co, Ni, Pb

Locally brecciated graphitic pelite with

increased sulphide content and chloritic

shearing. Designed as a follow-up hole

testing the inferred down-dip projection

approximately 25 m from shallow elevated

radioactivity intersected in M22-013.

incl. 39.4 39.7 682

47.8 48.0 360 V, Mo, Co,

Pb

A10 M22-015

158.1 158.3 503 V, Zn, Pb,

As, Cu Graphitic pelite, apparent association

between elevated U and shears and

fractures, with bleaching and

hematization.

incl. 158.2 158.3 886 0.12

161.2 161.5 122 -

163.3 163.8 219 V, B, Cu, As,

Co, Ag, Bi

Notes:

• Uranium and pathfinder element concentrations are shown in parts per million (ppm) as determined through partial digest ICP-OES

or ICP-MS analysis on all samples, as described in the technical disclosure below.

• Uranium content as weight % U3O8 was determined through HCl:HNO3 digestion and ICP-OES analysis on selected samples.

• Thresholds for pathfinder anomalism were assigned based on a combination of statistical analysis of the dataset and appropriate

reference databases. Element abundances were considered elevated at the following thresholds: B>200 ppm, Pb>20 ppm, Ni>80

ppm, Co>25 ppm, As>15 ppm, Cu>40 ppm, V>75 ppm, Mo>5 ppm, Zn>75 ppm, Ag>0.2 ppm and Bi>0.75 ppm.

• True thicknesses of the drill core intersections are yet to be determined.

• Target prefixes A, H and P refer to the Armbruster, Howland and Pitchvein Conductors, respectively.

• Further drill hole details were provided in the News Release dated August 23, 2022.

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Figure 2: Location of the 2022 drill holes completed on the Murmac Uranium Project.

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Technical Disclosure

All drilling was carried out with NQ or NQ2 diameter core. The oriented drill cores have been subjected to

comprehensive logging and sampling to characterize mineralization, alteration and structure. Sample

intervals ranged from 10 to 50 cm. Half -split drill core samples were submitted to the Saskatchewan

Research Council (“SRC”) Geoanalytical Laboratories (ISO/IEC 17025:2005 accredited) for uranium assay

and multi-element characterization. Sample preparation for all samples included drying, jaw crushing to

60% passing -2 mm, and pulverizing to 90% passing -106 microns. Multi -element characterization was

carried out by partial digestion (HNO 3:HCl), using ICP-OES and ICP-MS analytical methods. For selected

samples U 3O8 weight % was determined separately through partial digest (HCl:HNO 3) and ICP -OES

(ISO/IEC 17025 accredited method). Additional analysis for boron content was obtained for all samples

through Na2O2/NaCO3 fusion followed by ICP-OES.

Clay species identification through short-wave infrared (SWIR) spectroscopy was carried out on drill chips

at regular spacing (between 6 and 9 m) down the full length of each drill hole. An Integrated Spectronics

Ltd. Portable Infrared Mineral Analyser (PIMA -II) was used to acqu ire spectral measurements in the

wavelength range from 1250 to 2500 nm. Mineral identification using SWIR spectroscopy is based on both

the position and shape of individual absorption peaks, and the shape of the overall spectrum. These

characteristics were compared to reference spectra (such as SPECMINTM library) provided for a variety of

minerals detectable in the SWIR region of the electromagnetic spectrum.

Qualified Person and Data Quality

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

Verran, M.Sc., P.Geo., Chief Executive Officer of the Company, who is a Qualified Person as defined by

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

101.

Unless otherwise stated, the historical results (scintillometer measurements, geochemical analysis and drill

results) contained within this news release have not been verified and there is a risk that any future

confirmation work and exploration may produce results that substantially differ from the historical results.

The Company considers these results relevant to assess the mineralization and economic potential of the

property. The histo rical drill results obtained by SMDC in drill holes CKI -9 and CKI -10 (Table 1) can be

found within the Saskatchewan Mineral Assessment Database (SMAD) references 74N07 -0310 and

74N07-0311. Assay and scintillometer survey results from SMDC (Figure 2) were captured from tables and

georeferenced figures in these assessment reports.

About Fortune Bay

Fortune Bay Corp. (TSXV:FOR, FWB:5QN, OTCQX: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 the 100% owned Strike and Murmac uranium exploration projects, located near

the Goldfields Project, which have high-grade potential typical of the Athabasca Basin. The Company has

a goal of building a mid-tier exploration and development Company through the advancement of its existing

projects 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.

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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 performanc e. 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. Fortune Bay Corp. (“Fortune Bay” or the “Company”) cautions that all

forward-looking statements are inherently uncertain, and that actual performance may be affected by a number o f material factors,

many of which are beyond Fortune Bay's control. Such factors include, among other things: risks and uncertainties relating to metal

prices, changes in planned work resulting from weather, COVID-19 restrictions, availability of contractors, logistical, technical or other

factors, the possibility that results of work will not fulfill expectations and realize the perceived potential of Fortune Ba y's mineral

properties, uncertainties involved in the interpretation of drilling results and oth er tests, the possibility that required permits may not

be obtained in a timely manner or at all, risk of accidents, equipment breakdowns or other unanticipated difficulties or inte rruptions,

the possibility of cost overruns or unanticipated expenses in wo rk programs, the risk of environmental contamination or damage

resulting from the exploration operations, the need to comply with environmental and governmental regulations and the lack of

availability of necessary capital, which may not be available to Fo rtune Bay, acceptable to it or at all. Fortune Bay is subject to the

specific risks inherent in the mining business as well as general economic and business conditions. Accordingly, actual, and future

events, conditions and results may differ materially fr om the estimates, beliefs, intentions, and expectations expressed or implied in

the forward-looking information. Except as required under applicable securities legislation, Fortune Bay undertakes no obligation to

publicly update or revise forward -looking information. Fortune Bay does not intend, and does not assume any obligation, to update

these forward-looking statements, except as required under applicable securities legislation. For more information on Fortune Bay,

readers should refer 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.