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Plato Gold Acquires 100% Ownership in Good Hope Niobium Project

Mergers & Acquisitions Property Options & Staking

For Immediate Release

Plato Gold Acquires 100% Ownership in

Good Hope Niobium Project

Toronto, August 27, 2019 – Plato Gold Corp. (TSX-V: PGC) (“Plato” or the “Company ”), an

exploration company with a portfolio of properties in Northern Ontario and Santa Cruz, Argentina

is pleased to announce th at the company has met the terms of the KL226 Option Agreement

(“KL226”) and KL37 Option Agreement (“KL37”), as originally announced on May 31, 2017.

“I am very pleased to announce that Plato now has 100% ownership of the Good Hope Niobium

Project” said Anthony J. Cohen, CEO of Plato Gold Corp. “I am also very pleased to announce

our continuing work on the Project with both Dr. Rudy Wahl, the discoverer of the project and Dr.

Roger Mitchell, one of the world’s foremost experts on carbonatite rocks and niobium. With our

World Class team of experts, I am looking forward to further development of the Good Hope

Niobium Project releasing further news of its continuing development when we have completed

important work,” said Cohen.

Dr. Rudy Wahl was the recipient of the Bernie Schnieders Discovery of the Year Award 2014

presented by Don Hoy and Jonie Schnieders to Dr. Wahl at the NWOP A Awards Dinner in

Thunder Bay on April 14, 2015.

In meeting the terms of the KL226 Option Agreement, Plato made a total payment of $106, 600

and issued 7,500,000 common shares. The Optionors for the KL226 Option Agreement are Rudolf

Wahl (45%), Mike Dorval (45%), Roger H. Mitchell (10%).

In meeting the terms of the KL37 Option Agreement, Plato made a total payment of $2,000 and

issued 1,600,000 common shares. The Optionors for the KL37 Option Agreement are Rudolf

Wahl (85%), Leonard Windover (5%), Darren Hutchinson (5%), Ryan Harasym (5%).

As well, exploration expenditures of $400,000 on either or both the KL226 and KL37 properties

were exceeded with a total of $1,113,532 exploration work completed as of June 30, 2019.

The following conditions remains for each of the KL226 and KL37 Option Agreements:

(i) A 3% Net Smelter Return Royalty (the “NSR Royalty”) to Optionors with

provisions that Plato has the right to buy back 50% of the NSR Royalty for

$1,500,000 and that Plato has first right of refusal with respect to bona fide arm’s

length offers to purchase the NSR Royalty from the Optionors.

ii) A 3% Gross Overriding Royalty (the “GOR Royalty”) from the production of

diamonds only to Optionors with provisions that Plato has the right to buy back

50% of the GOR Royalty for $1,500,000 and that Plato has first right of refusal

with respect to bona fide arm’s length offers to purchase the GOR Royalty from the

Optionors.

iii) 1,000,000 common shares to Optionors upon completion of a NI 43-101 compliant

resource exceeding 100 million tonnes of Nb205/P205 and an additional 2,000,000

common shares to Optionors upon a positive bankable feasibility study

iv) 10% of the sale price or option price in cash or shares to Optionors, if the KL226 or

KL37 claims are sold or optioned to a third party.

About Good Hope Niobium Project

As previously announced on May 31, 2017 , the Good Hope Niobium Property consists of a total

of 19 claims, 263 claim units (prior to Mining Lands Administration System claims conversions

in 2018) and 4208 hectares in Killala Lake Area and Cairngorm Lake Area Townships, northwest

of Marathon, Ontario. The Good Hope Property is located approximately 45 kilometers northwest

of Marathon and 28 km north of Highway 17. The property is readily accessible from Trans -

Canada Highway 17 and Dead Horse Road. The Property is also in close proximity to the Hemlo

gold mining camp.

The regional geology around the Good Hope Property consists of alkaline and carbonatite

intrusions formed during Midcontinental rifting within the Trans -Superior Tectonic zone. The

Good Hope Property forms a doughnut around the Prairie Lake Complex. The Prairie Lake

Complex is composed of carbonatite, ijolite and potassic nepheline syenite. The most common

rock types on the Good Hope Property are carbonatite, syenite breccia and ijolite. The Good Hope

Property hosts Niobium mineralization in pyrochlore. The Niobium mineralization differs from

that in Prairie Lake Complex in that it is low in Th and U contents.

The discovery of Niobium mineralization at Good Hope was made by Rudy Wahl in 2010 when

he identified 1.63 % Nb2O5 in a small outcrop on site #28. In 2014, he followed up with mapping

and prospecting in 5 pits that he dug in the area. Subsequent exploration work on the property

includes: grab sampling, chann el sampling, trenching, ground radiometrics survey, airborne

magnetic - radiometrics surveys and mineralogical studies. Mineralogical studies completed in

2014 by Professor Roger H. Mitchell on samples from site #28 shows that the pyrochlore minerals

are ThO2-free and contain very low UO3 so radionuclide problems are low for future extraction.

During the summer of 2015, a detailed prospecting-geological survey was completed on the Good

Hope Property with the objective of finding larger zones of mineralize d, non -radioactive

carbonatite. The first trench, TR -01, revealed a non -radioactive carbonatite at the contact with a

syenite. The carbonatite is at least 5 meters wide by 15 meters long, and observations indicate that

it extends underneath the swamp for an unknown distance. The best result from 26 channel samples

in trench TR -01 is 1.205% Nb 2O5 over 1.10 meters. Trench TR -04 revealed a contact between

ijolite breccia and syenite breccia, both matrix being carbonatite, with a chunk of massive

carbonatite. Again, the carbonatite most likely extends underneath the swamp. The best channel

sampling result for TR-04 is 0.437% Nb2O5 over 0.60 meters. In summary, the 2015 exploration

program was successful in discovering a new type of niobium mineralization which is potentially

a non-radioactive carbonatite intrusion. As the discovery coincide s with a low magnetic/low

topography sector, all the multi square-kilometers low topography, low magnetics area covered by

the Good Hope Property, is considered highly prospective.

Two drill holes were completed in 2016 for a total of 280.7 m on an airborne radiometric anomaly

near the discovery site #28. The assay highlights for drill hole PL -01 include 0.45 % Nb2O5 over

1.0 m and 6.25 % P2O5 over 1.0 m. The assay highlights for drill hole PL-02 include 0.34 % Nb2O5

over 1.0 m and 5.81 % P 2O5 over 1.0 m. The Niobium mineralization in drill core is associated

with carbonatite and syenite carbonatite breccia.

Dr. Selway is a Qualified Person ("QP") as defined by National Instrument 43-101 was responsible

for the technical information contained in the May 31, 2017 news release and has reviewed and

approved its content.

As previously announced on September 19, 2018 , Plato completed 5016 metres of diamond

drilling on the Good Hope Property. The drilling focused on outcropping mineralization at ‘Site

28’ in the northwestern part of the property and encompassed an area of approximately 500m by

500m (see Figure 3). All holes were drilled in a northwesterly direction. The nine completed drill

holes ranged in length from 372 to 672 metres, testing the area to a vertical depth of between 285

and 580 metres (see Press Release dated 6 June 2018 for drill collar information). All holes

intersected zones (up to 27m wide) of massive carbonatite within a brecciated system consisting

of variably fenitized syenite/quartz -syenite intruded by carbonatite dykes and crosscutting

carbonatite veins. Although the brecciated nature of the host rocks makes any orientation or trend

of mineralization difficult to determine, the intersection of massive carbonatite in every drill hole

from surface up to approximately 500m depth suggests that significant potential exists for niobium

mineralization over a large area.

Assays of the drill core samples collected from the program peaked at 0.950% niobium (Nb 2O5)

with 6.20% phosphorus (P2O5) over 1.1m in a sample of massive carbonatite (PGH-18-06, 382.94-

384.04m).

The two most significant intersections from the drilling pro gram were 0.190% Nb2O5 and 2.04%

P2O5 over 93.08m (drill hole PGH -18-06; 354.18-447.26m) and 0.175% Nb 2O5 and 2.03% P2O5

over 89.24m (drill hole PGH-18-10A; 345.0-434.24m).

Dr. Roger Mitchell of Lakehead University is undertaking a petrographic study of core samples

from the recent drill program and has made the following observations:

“The ore mineral of the Good Hope carbonatite, in common with all other niobium producing

carbonatites, is pyrochlore. The high density and coarse grain size of the Good Hope pyrochlores,

along with an association with acid soluble inclusions and host carbonates may be very favourable

for simplifying of ore beneficiation processes.”

“Pyrochlore is a sodium (Na)- and calcium (Ca)- bearing niobium (Nb) oxide with the simplified

composition of (NaCa)Nb 2O7. The majority of the Good Hope pyrochlores are typically of

relatively uniform composition and contain on average about 70 wt.% Nb 2O5 with 1 -2 wt.%

strontium oxide (SrO) and barium oxide (BaO). Minor variations in composition range from these

dominant “normal” Na-Ca-pyrochlores to Na- and Ca-poor (1-4 wt.% Na2O) varieties also with

70 wt.% Nb 2O5. Replacement of both types of pyrochlores by trace amounts of Sr -rich varieties

with 4-6 wt.% SrO, 1-8 wt.% BaO, less than 1 wt.% UO3, and no detectable ThO2 are also present.

Some pyrochlores have been replaced in part by fersmite [CaNb 2O6 with approximately 58 wt.%

Nb2O5] or ferrocolumbite [FeNb2O6] with c. 79 wt.% Nb2O5].”

“The pyrochlores commonly co -exist with the phosp horus (P) bearing mineral apatite

[Ca5(PO4)3(OH,F,Cl)] and appear to form clasts derived from an earlier stage apatite -pyrochlore

cumulate body. These clasts have commonly been disaggregated resulting in the liberation of the

pyrochlores from the apatite i nto the matrix of the diverse later stage carbonate minerals which

make up the carbonatite intrusion.”

“The pyrochlores exhibit a very wide range in size, mainly from 100 microns to 1 mm, with some

crystals being up to 5 mm in maximum dimension. The majority are euhedral, not resorbed and of

relatively uniform composition. Inclusions when present are of apatite, and/or diverse carbonates.”

Dr. Mitchell states that “compared with other carbonatites currently being evaluated for their

niobium potential the Good Hope prospect has significant potential because of favourable

mineralogy and infrastructure”.

Approximately 2150 metres or 40% of all drill core was sampled. A total of 2081 drill core samples

from the program were submitted to Activation Laboratorie s (ActLabs) in Thunder Bay, Ontario

and analyzed for niobium using a fusion XRF method. Samples from holes PGH -18-01 through

PGH-18-03 were also analyzed for a whole rock and trace element ICP analytical package.

Samples from holes PGH-18-04 onwards were submitted for an XRF package designed for coltan

deposits which included Ta, Nb, U, Th, Zr, Fe, P, Sn, Y, and W oxides. An internal Quality Control

Quality Assurance (QAQC) program was implemented with an additional 168 QAQC samples

(blanks, reference standards, and duplicates) also being submitted for analysis.

Laura Giroux, Msc., P.Geo., a Qualified Person as defined by NI 43-101, is responsible for the

technical information contained in the September 19, 2018 news release and has reviewed and

approved its content.

About Plato Gold Corp.

Plato Gold Corp. is a Canadian exploration company listed on the TSX Ve nture Exchange with

projects in Marathon Ontario, Timmins Ontario and Santa Cruz, Argentina.

The Good Hope Niobium Project consists of a total of 254 claims, consisting of 227 Single Cell

Mining Claims and 27 Boundary Cell Mining Claims, and covers an area of approximately 5,100

hectares in Killala Lake Area and Cairngorm Lake Area Townships, near Marathon Ontario. Plato

holds 100% interest in the Good Hope Niobium Property.

The Timmins Ontario project includes 4 properties: Guibord, Harker, Holloway and Marriott in

the Harker/Holloway gold camp located east of Timmins, Ontario. Plato holds 50% interest in the

Guibord property with the remaining 50% held by Osisko Mining Inc. (“Osisko”). Osisko also

holds 80% interest in the Harker property with Plato holding the remaining 20%.

In Argentina, Plato owns a 75% interest in Winnipeg Minerals S.A. (“WMSA”), an Argentina

incorporated company. T he Lolita Property , held by WMSA, is comprised of a number of

contiguous mineral rights totaling 9,672 hectares. Work has advanced on this exploration property

to the point that it is drill-ready or ready to be optioned to a partner.

For additional company information, please visit: www.platogold.com.

NEITHER THE TSX VENTURE EXCHANGE NOR ITS REGULATION PROVIDER (AS THAT

TERM IS DEFINED IN THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS

RESPONSIBILITY FOR THE ADEQUACY OF THIS RELEASE.

For further information, please contact:

Anthony Cohen

President and CEO

Plato Gold Corp.

T: 416-968-0608

F: 416-968-3339

[email protected]

www.platogold.com

Forward Looking Statements

This news release contains “forward-looking statements”, within the meaning of applicable securities laws. These statements include, but are not

limited to, statements regarding the,potential mineralization and resources, exploration results, and future plans and objectives. Generally, these

forward-looking statements can be identified by the use of forward -looking terminology such as “plans”, “expects” or “does not expect”, “is

expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of

such words and phrases or state that certain actions, events or results “may”, “could”, “would”, “might” or “will be taken”, “occur” or “be

achieved”. Forward-looking statements are based on the opinions and estimates of management as of the date such statements are made, and they

are subject to known and unknown risks, uncertainties and other factors that may cause the actual results, use of proceeds, level of activity,

performance or achievements of Plato to be materially different from those expressed or implied by such forward-looking statements, including but

not limited to risks related to: risks related to exploration; actual resource viability, and other risks of the mining industry . Although management

of Plato has attempted to identify important factors that could cause actual results to differ materially from those containe d in forward-looking

statements, there may be other factors that cause results not to be as anticipated, estima ted or intended. There can be no assurance that such

statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in s uch statements.

Accordingly, readers should not place undue reliance on forw ard-looking statements. The Company does not undertake to update any forward -

looking statements that are incorporated by reference herein, whether as a result of new information, future events or otherw ise, except in

accordance with applicable securities laws.