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Prosper Gold Corp. outlines several gold-in-till anomalies and samples high- grade gold at multiple prospects at Golden Sidewalk – Red Lake, ON

Exploration Programs Sampling & Geoscience Results

November 25, 2020 TSXV: PGX

NEWS RELEASE

Prosper Gold Corp. outlines several gold-in-till anomalies and samples high-

grade gold at multiple prospects at Golden Sidewalk – Red Lake, ON

Vancouver, British Columbia – November 25, 20 20 – Prosper Gold Corp. (" Prosper Gold " or the

"Company") (TSXV:PGX) is pleased to report rock and till sampling results from the 2020 exploration

program at the Golden Sidewalk Project (the “Project”) in the Birch-Uchi region of Red Lake. The Golden

Sidewalk is a district scale gold exploration project covering over 16 0 square kilometres of contiguous

mineral claims and mining leases (see the Company's Aug. 10, Sept. 8 , and Sept. 15, 2020 news releases

for details).

Highlights:

- 3 pristine gold grain anomalies outlined in 32 square kilometre reconnaissance till survey

- Channel rock sampling at two discrete zones, results include 1.0 metre grading 15.3 g/t gold

- Rock chip samples up to 16.3 g/t gold at Skinner North prospect, no historical drilling

“High grade gold in surface rock sampling at the Dunkin, KT Vein and Skinner North prospects gives us

confidence in existing targets prior to drilling,” commented Peter Bernier, CEO. “ We are excited by the

identification of three pristine gold grain anomalies near the regional unconformity . All three are in areas

with no historical drill programs and are exciting developments in our regional targeting initiative. The UC

anomaly area is our highest-ranking conceptual target based on available historical data and crews have

infill sampled this target. Results are expected in the coming weeks.”

Till sampling

The 2020 reconnaissance till sampling program at the Golden Sidewalk Project was designed to detect

anomalous gold-in-till near a regional angular unconformity between the Narrow Lake and the Balmer

Assemblages. Such regional unconformities may localize structural corridors for hydrothermal fluid

migration and gold mineralization. Till sampling at 250 m intervals was conducted along lines spaced at 1

km. Three areas with anomalous ly high gold grain counts were detected . A high proportion of the gold

grains are classed as pristine gold. This suggests a nearby bedrock source.

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Figure 1. Map showing anomalies of pristine gold grains from 2020 till sampling survey.

The largest anomaly, the UC, has the highest pristine grain count (samples up to 143 gold grains with 78

pristine grains) directly north of the Narrow Lake / Balmer unconformity. The E-12 anomaly, also to north

of the unconformity, has the highest gold -grain-in-till sample of 149 gold grains (69 pristine grains). The

Balmer anomaly consists of 5 elevated pristine grain samples, coveri ng 1.25km, over the Balmer

Assemblage rocks to the south of the unconformity. The new till sampling results bolster the company’s

high priority geophysical and conceptual targets.

Channel rock sampling

Channel sampling and mapping was completed at the Joe Vein, Dunkin 2 and KT vein to gain insight into

gold mineralization at these area s. Results from the Joe Vein have been previously reported (see the

Company’s Nov. 16, 2020 news release) while the comprehensive channel sampling results for the Dunkin

2 and KT vein are provided below.

Table 1. Channel sampling results at Dunkin 2 and KT vein trenches (center of trenches at 509,176 E /

5,674,473 N, and 507,410 E / 5,679,072 N, respectively. Coordinates within UTM NAD 83 zone 15).

Trench ID Channel

ID

From

(m)

To

(m)

Interval

(m) Gold (g/t) Sample type

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Dunkin 2 A 0 0.8 0.8 0.155 Saw-cut channel

Dunkin 2 A 0.8 1.6 0.8 0.045 Saw-cut channel

Dunkin 2 A 1.6 2.4 0.8 0.351 Saw-cut channel

Dunkin 2 A 2.4 3.2 0.8 0.273 Saw-cut channel

Dunkin 2 A 3.2 4.2 1.0 1.22 Saw-cut channel

Dunkin 2 A 4.2 5.2 1.0 1.14 Saw-cut channel

Dunkin 2 A 5.2 6.2 1.0 10.5 Saw-cut channel

Dunkin 2 B 0 1.0 1.0 15.3 Saw-cut channel

Dunkin 2 B 1.0 2.0 1.0 0.281 Saw-cut channel

Dunkin 2 B 2.0 3.0 1.0 0.245 Saw-cut channel

Dunkin 2 B 3.0 4.0 1.0 0.374 Saw-cut channel

Dunkin 2 C 0 1.2 1.2 0.296 Saw-cut channel

KT Vein A 0 0.4 0.4 0.007 Saw-cut channel

KT Vein A 0.4 0.8 0.4 3.1 Saw-cut channel

KT Vein A 0.8 1.3 0.5 BD Saw-cut channel

KT Vein B 0 0.3 0.3 0.014 Saw-cut channel

KT Vein B 0.3 0.6 0.3 27.2 Saw-cut channel

KT Vein B 0.6 1.2 0.6 0.053 Saw-cut channel

KT Vein C 0 0.4 0.4 0.105 Saw-cut channel

KT Vein C 0.4 0.7 0.3 12.3 Saw-cut channel

KT Vein C 0.7 1.1 0.4 0.071 Saw-cut channel

Figure 2. Plan map of Dunkin 2 Trench

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The Dunkin 2 Trench is described as strongly sheared massive basalts belonging to the Narrow Lake

Assemblage hosting numerous sulphide-bearing quartz veins up to 1 metre in width. Sulphides observed

within quartz veins and in mineralized wallrock consist of pyrite and lesser chalcopyrite. Quartz veins

trending west -southwest have been deformed locally suggesting a relat ively early timing on gold

mineralization in the context of the deformational history of the Birch-Uchi greenstone belt.

Figure 3. Plan map of KT Vein Trench (BD denotes “below detection limit”).

The KT Vein Trench exhibits a quartz vein near the contact between sheared massive basalts belonging to

the Narrow Lake Assemblage and a west-northwest trending felsic dike. Sulphides within the quartz vein

include pyrite and lesser arsenopyrite and chalcopyrite. The west -northwest trend and the undist urbed

nature of the quartz vein suggest timing of the gold mineralization at the KT vein is related to the later D2

deformational event in the Birch-Uchi greenstone belt.

Rock sampling / prospecting

The season’s exploration included prospecting. A highlight of this work is the sampling of high-grade gold

at surface at the historical Skinner North prospect, an area that has seen no drilling to date. The Skinner

North prospect is 2.4 kilometres southwest of the historical Bathurst Mine. All 4 rock samples collected at

Skinner North are sheared and silicified mafic volcanics with fine pyrite and pyrrhotite vein fill. Results of

the sampling are provided below.

Table 2. Rock sampling results from the Skinner North prospect (coordinates within UTM NAD 83

zone 15).

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Area Sample

ID

Easting

(m)

Northing

(m) Gold (g/t) Sample type

Skinner

North 707709 506,233 5,676,570 7.55 Rock - Grab

Skinner

North 707710 506,233 5,676,570 16.3 Rock - Grab

Skinner

North 707711 506,233 5,676,570 11.2 Rock - Grab

Skinner

North 707712 506,233 5,676,570 13.7 Rock - Grab

About the Golden Sidewalk

The 16,400-hectare Golden Sidewalk project is in the western Birch-Uchi Greenstone Belt, approximately

60 km east of Red Lake, Ontario. The vehicle -accessible project straddles 12 kilometres of the Balmer

Assemblage – Narrow Lake Assemblage unconformity, a regional-scale feature that has been the Red Lake

exploration guide, but which has seen limited exploration in the project area. Historical drilling programs

at the Bathurst Mine, Joe Vein, KT vein, Dunkin and Vihonen prospects reported high-grade gold intercepts

which warrant follow-up.

QA/QC Procedures

Channel samples were cut with a cut-off saw across select areas of previously stripped bedrock exposures

at medial widths and depths of 5 cm and 8 cm, respectively. Channel samples were collected and placed in

polyethylene bags, sealed with zip -ties shipped to Activation Laboratories Ltd. (“ActLabs”) in Timmins,

Ontario, where they were crushed and pulverized to 95% passing 105-micron mesh. Samples were analyzed

using ActLabs 1A2 -50 analytical package, whereby 50 g aliquots are subjected to gold fire assay and

finished with Atomic Absorption (“AA”) spectroscopy. Overlimit samples (> 5 g/t gold) were assayed with

ActLabs 1A3-50 fire assay package with a gravimetric finish. Internal laboratory standards were used and

checked upon analysis as a means of quality assurance.

Till samples were collected from below the colluvial soil profile at a medial depth of 50 to 75 centimeters

and placed into 5-gallon plastic pails which were sealed and shipped to Overburden Drilling Management

Ltd. in Nepean, Ontario for processing. The gold grain testing involves extracting an impure preliminary

heavy mineral concentrate from the -2 mm matrix of each sediment sample by tabling, separating any

recovered gold grains from the table concentrate and measuring each grain and classifying it acco rding to

its degree of physical wear.

Rock grab samples were placed into polyethylene bags which were sealed and shipped to SGS Laboratories

in Red Lake, ON, where they were crushed then pulverized to 95% passing 105 -micron mesh with 50 g

aliquots subjected to gold fire assay and subsequent AA finish. Overlimit samples (> 10 g/t gold) were

subjected to 50 g fire assay with a gravimetric finish. Internal laboratory standards were used and checked

upon analysis as a means of quality assurance.

Qualified Person

The scientific and technical information in this news release has been reviewed by Dirk Tempelman-Kluit,

PhD, P.Geo., a Qualified Person under National Instrument 43-101.

For a detailed overview of Prosper Gold please visit www.ProsperGoldCorp.com.

ON BEHALF OF THE BOARD OF DIRECTORS

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Per: “Peter Bernier”

Peter Bernier

President & CEO

For further information, please contact:

Peter Bernier

President & CEO

Prosper Gold Corp.

Cell: (250) 316-6644

Email: [email protected]

Information set forth in this news release may involve forward -looking statements under applicable securities laws. Forward -

looking statements are statements that relate to fu ture, not past, events. In this context, forward -looking statements often address

expected future business and financial performance, and often contain words such as "anticipate", "believe", "plan", "estimat e",

"expect", and "intend", statements that an action or event "may", "might", "could", "should", or "will" be taken or occur, or other

similar expressions. All statements, other than statements of historical fact, included herein including, without limitation,

statements about the planned exploration of the Golden Sidewalk project, are forward-looking statements. By their nature, forward-

looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results,

performance or achievements, or other future even ts, to be materially different from any future results, performance or

achievements expressed or implied by such forward -looking statements. Such factors include, among others, the following risks:

the need for additional financing; operational risks assoc iated with mineral exploration; fluctuations in commodity prices; title

matters; environmental liability claims and insurance; reliance on key personnel; the potential for conflicts of interest amo ng

certain officers, directors or promoters with certain ot her projects; the absence of dividends; competition; dilution; the volatility

of our common share price and volume and the additional risks identified the management discussion and analysis section of ou r

interim and most recent annual financial statement or other reports and filings with the TSX Venture Exchange and applicable

Canadian securities regulations. Forward-looking statements are made based on management's beliefs, estimates and opinions on

the date that statements are made and the Company undertakes no obligation to update forward-looking statements if these beliefs,

estimates and opinions or other circumstances should change, except as required by applicable securities laws. Investors are

cautioned against attributing undue certainty to forward-looking statements.

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

Exchange) accepts responsibility for the adequacy or accuracy of this release.