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Appia reports 65 metres continuous uranium mineralization on Eastside property and REE bearing pegmatite on Loranger

Exploration Programs

500-2 Toronto St.

Toronto ON

M5C 2B6

PH: 416 546-2707

FAX: 416 218-9772

Email: [email protected]

Website: www.appiaenergy.ca

NEWS RELEASE

APPIA SAMPLES OVER 65 METRES OF CONTINUOUS URANIUM MINERALIZATION

AT SURFACE ON THE EASTSIDE PROPERTY AND IDENTIFIES REE-BEARING

PEGMATITE ON THE LORANGER PROPERTY

MR. TOM DRIVAS TO PRESENT AT WALL STREET REPORTER’S “INVESTORS

DISCOVERY DAY” LIVESTREAM BROADCAST

TORONTO, ONTARIO, July 21, 2020 - Appia Energy Corp. (the “Company” or “Appia”) (CSE:API,

OTCQB:APAAF.US, Germany: “A0I.F”, “A0I.MU”, “A0I.BE”) is pleased to announce the exploration

and surface channel sample results from the recently completed exploration activities on the Eastside and

Loranger properties, Athabasca Basin area, northern Saskatchewan.

Highlights include;

- i) a composite sample length of 65.75 metres returning 0.018 wt% U3O8 from within Area 51 of the

Eastside property and

- ii) a 1.0 metre channel sample line returning 0.471 wt% total rare earth oxide (“TREO”) from Area D of

the Loranger property.

EASTSIDE

The Company successfully identified numerous pegmatite dykes (“ dykes”) in outcrops ranging in thickness

from 1 metre to greater than 20 metres width exhibiting elevated radioactivity (>300 counts-per-second

(“cps”)) (see Figure 1). A majority of the dykes could typically be followed for more than 10 metres along

strike-length before being lost underneath overburden. Discrete trends (from 1 metre to 3 metres thick) within

the dykes contained spotty anomalous radioactivity (>1,000 cps) to “off-scale” radioactivity (>9,999 cps).

Two dykes with the most radioactivity rock exposure (Area 51 and Area 7575) were channel sampled and

returned composite sample grades with uranium concentrations exceeding 0.01 wt% U 3O8 (see Figures 1 and

2, and Table 1). Areas 51 and 7575 are on strike with each other but are separated by 1.5 km which is covered

by overburden.

Four separate occurrences of “off-scale” radioactivity were identified along four different dyke trends,

however only one of those was exposed well-enough at surface to be channel sampled (Area 51, Line 3

channel sample). Helicopter reconnaissance identified three large areas (>500 m x >500 m) with many dykes

exposed at surface, however time was limited and those outcrops were not visited.

Mr. James Sykes, Vice-President, Exploration and Development, comments; “We are encouraged by the

surface radiometric and assay results from the Eastside property. The multiple occurrences of “off-scale” and

numerous trends of anomalous radioactivity demonstrate significant potential for surface-hosted uranium

mineralization on the property. The composite U3O8 grades from Eastside are comparable to other world-class

open pit uranium mines, such as the Rössing and Husab uranium mines in Namibia. Based on historic assay

results and those obtained from Line 3 of Area 51, we believe zones with higher uranium grades are possible

on the Property. The property remains underexplored as i) numerous prospective outcrops have yet to be

visited, ii) the currently identified surface trends (i.e. over 1.5 km between Area 51 and Area 7575) would

require overburden to be removed to fully realize the potential of the mineralized strike-lengths, and iii)

diamond drilling has never been conducted on the property to fully realize the depth potential that might

exist”.

Ground reconnaissance prospecting, mapping, and channel sampling was completed on the Eastside property

over four days. A total of 139 channel samples ranging from 0.27 to 1.31 m in length were removed from

outcrops in Area 51 and Area 7575 for a total of 77.69 m and 33.65 m, respectively.

LORANGER

Eight outcrop areas were visited on the Loranger property over a total of 3 days. Similar to the Eastside

property, pegmatite dykes with elevated radioactivity were discovered within outcrops. Of particular interest

was a pegmatite-rich outcrop area (Area D) with anomalous and elevated radioactivity trends observed within

100 to 300 m of a bifurcating and bending conductor. As has been observed on the property in previous

exploration programs, radioactivity levels tend to increase with proximity to graphitic conductors suggesting

the graphitic structural trends remain the primary focus for continued exploration on the property. No

conductive outcrops were exposed on the property.

Area D was channel sampled, with no significant uranium values >0.01 wt% U 3O8 obtained (see Table 1).

The observed radioactivity was emanating from thorium rather than uranium. One sample line (line 7) did

return anomalous rare earth element (“REE”) results of interest; 0.471 wt% TREO over 1.0 m (see Table 2).

The same geological formations at the southern end of the property can be inferred (by airborne magnetic

signatures) to continue over 45 km to the north end of the property within the RCV and gravity low target

areas that were drilled in 2017. Diamond drilling in the RCV area returned 72.9 m at 0.012 wt% U 3O8 (see

news release dated May 24, 2017).

Mr. James Sykes, Vice-President, Exploration and Development, comments; “This field program was

instrumental identifying geological controls that can help vector us towards more uranium mineralization on

the property. Of interest is the new REE discovery on the property which does bear grades similar to those

that have been observed at Appia’s Alces Lake high-grade REE property. Only one sample was taken from

that trend and it remains open along strike in both directions for quite some distance. We plan to follow-up

this area in the future”.

All radioactivity measurements were made with an Exploranium GR-110 hand-held scintillometer. The GR-

110 readings max out at 9,999 cps, therefore any occurrences exhibiting 9,999 cps are considered “off-scale”

because natural radioactivity can exceed 10,000 cps. Background radioactivity on all of the outcrops ranged

from 100 to 200 cps. The reader is cautioned that Appia uses natural gamma-ray readings only as a

preliminary indication of the presence of radioactive materials (uranium-, thorium- and/or potassium-rich

minerals) and that the results may not be used directly to quantify or qualify uranium concentrations within

the rock.

All samples were hand-delivered to and assayed by Saskatchewan Research Council’s Geoanalytical

Laboratory, an ISO/IEC 17025:2005 (CAN-P-4E) certified laboratory in Saskatoon, SK, for multi-element

analysis.

The technical content in this news release was reviewed and approved by Dr. Irvine R. Annesley, P.Geo,

Advisor to the Board of Directors of Appia, and a Qualified Person as defined by National Instrument 43-101.

WALLSTREET REPORTER’S “INVESTORS DISCOVERY DAY” LIVESTREAM

Appia would like to invite the general public to join Mr. Tom Drivas, CEO & President, for a live public

webcast on Tuesday July 21, 2020, starting at 12:30 PM EST, as part of the Wall Street Reporter’s “Investors

Discovery Day” livestream event.

The livestream can be accessed via the link below:

https://www.wallstreetreporter.com/investors-discovery-day-livestream/.

About Appia

Appia is a Canadian publicly-traded company in the uranium and rare earth element sectors. The Company is

currently focusing on delineating high-grade critical rare earth elements (“REE”) and uranium on the Alces

Lake property, as well as prospecting for high-grade uranium in the prolific Athabasca Basin on its Loranger,

North Wollaston, and Eastside properties. The Company holds the surface rights to exploration for 57,048

hectares (140,968 acres) in Saskatchewan.

The Company also has a 100% interest (subject to a 1% Uranium Production Payment Royalty and a 1% Net

Smelter Return Royalty on any precious or base metals payable, provided that the price of uranium is greater

than US$130 per pound) in 12,545 hectares (31,000 acres), with rare earth element and uranium deposits over

five mineralized zones in the Elliot Lake Camp, Ontario. The Camp historically produced over 300 million

pounds of U 3O8 and is the only Canadian camp that has had significant rare earth element (yttrium)

production. The deposits are largely unconstrained along strike and down dip.

Appia’s technical team is directed by James Sykes, who has had direct and indirect involvement with over 550

million lbs. U3O8 being discovered in five deposits in the Athabasca Basin.

Appia has 73.8 million common shares outstanding, 89.1 million shares fully diluted.

For more information, visit the Appia’s website at www.appiaenergy.ca.

Cautionary Note Regarding Forward-Looking Statements : This News Release contains forward-looking statements

which are typically preceded by, followed by or including the words “believes”, “expects”, “anticipates”,

“estimates”, “intends”, “plans” or similar expressions. Forward-looking statements are not guarantees of

future performance as they involve risks, uncertainties and assumptions. We do not intend and do not assume

any obligation to update these forward- looking statements and shareholders are cautioned not to put undue

reliance on such statements.

Neither the Canadian Securities Exchange nor its Market Regulator (as that term is defined in the policies of

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

For further information, please contact:

Tom Drivas , President, CEO and Director: (tel) 416-546-2707, (fax) 416-218-9772 or (email)

[email protected]

James Sykes , VP Exploration & Development, (tel) 306-221-8717, (fax) 416-218-9772 or (email)

[email protected]

Frank van de Water , Chief Financial Officer and Director, (tel) 416-546-2707, (fax) 416-218-9772 or

(email) [email protected]

Figure 1 – Eastside property, Area 51 overview

Figure 2 – Eastside property, Area 7575 overview

Figure 3 – Loranger property overview

Table 1 – Eastside and Loranger properties, U3O8 channel sample results

Project Area Line From (m) To (m) Interval (m) U 3O8 (wt%)

Eastside 51 1 0.00 8.99 8.99 0.021

14.30 15.21 0.91 0.013

Composite Total 9.90 0.020

51 2 0.00 16.15 16.15 0.026

25.42 37.43 12.01 0.028

42.34 51.88 9.54 0.018

Composite Total 37.70 0.025

51 1 all and 2 all 0.00 65.75 65.75 0.018

Composite Total 65.75 0.018

51 3 0.00 0.37 0.37 0.086

Composite Total 0.37 0.086

51 5 2.68 3.47 0.79 0.027

Composite Total 0.79 0.027

51 6 0.64 2.53 1.89 0.026

Composite Total 1.89 0.026

51 7 0.00 2.10 2.10 0.017

Composite Total 2.10 0.017

7575 2 3.32 4.30 0.98 0.010

Composite Total 0.98 0.010

7575 3 3.05 5.91 2.86 0.018

Composite Total 2.86 0.018

7575 4 0.91 1.71 0.80 0.013

5.46 10.15 4.69 0.022

14.69 15.91 1.22 0.012

Composite Total 6.71 0.019

7575 4 all 0.00 17.47 17.47 0.010

Composite Total 17.47 0.010

Loranger D 1 0.00 7.00 7.00 NSR

D 2 0.00 1.00 1.00 NSR

D 3 0.00 1.00 1.00 NSR

D 4 0.00 1.00 1.00 NSR

D 5 0.00 1.00 1.00 NSR

D 6 0.00 1.00 1.00 NSR

D 7 0.00 1.00 1.00 NSR

Cut-off grade = 0.01% U3O8, Cut-off grade for "all" = none

Maximum consecutive internal dilution = 2.0 m

"NSR" = No Significant Results

All Uranium (ppm) results received by SRC from the ICP-MS Total Digestion lab package were converted to

U3O8 (wt%) using a conversion factor of (x1.1792/10000)

Table 2 –Loranger property, REO channel sample results

Area Line Width

(m)

La2O3

(wt%)

CeO2

(wt%)

Pr6O11

(wt%)

Nd2O3

(wt%)

Sm2O3

(wt%)

Eu2O3

(wt%)

Gd2O3

(wt%)

Tb4O7

(wt%)

Dy2O3

(wt%)

Ho2O3

(wt%)

Er2O3

(wt%)

Yb2O3

(wt%)

Lu2O3

(wt%)

Y2O3

(wt%)

ThO2

(wt%)

U3O8

(wt%)

TREO

(wt%)

CREO

(wt%)

D 7 1.0 0.111 0.220 0.024 0.080 0.011 0.000 0.007 0.001 0.003 0.000 0.001 0.001 0.000 0.012 0.092 0.005 0.471 0.108

The REEs Thulium (Tm) and Promethium (Pm) are not reported because they are both extremely scarce in nature, and Pm forms as a product of spontaneous fission of U-238

TREO = Total Rare Earth Oxide = sum of La2O3+CeO2+Pr6O11+Nd2O3+Sm2O3+Eu2O3+Gd2O3+Tb4O7+Dy2O3+Ho2O3+Er2O3+Yb2O3+Lu2O3+Y2O3

CREO = Critical Rare Earth Oxide = sum of Pr6O11+Nd2O3+Eu2O3+Tb4O7+Dy2O3

Highlighting Nd grades associated with high-grade TREO

Highlighting Pr grades associated with high-grade TREO

Highlighting "high-grade" TREO and CREO (i.e. >1.897 wt% TREO)

Light rare earth elements (LREEs = La, Ce, Pr, Nd, Sm)

Heavy rare earth elements (HREEs = Eu, Gd, Tb, Dy, Ho, Er, Yb, Lu, Y)

Radioactive elements (not a rare earth element)

- true thicknesses have not been determined

Note: >1.897 wt% TREO represents >75th percentile for global REO deposit grades of advanced stage-projects (excluding Gakara, Steenkampskraal and Mount Weld CLD deposits). The global REO deposit

information was derived from publicly available information as of January 31, 2018, from individual company websites, SEDAR technical report filings, and the Technology Metals Research Advanced Rare Earth

Projects Index (http://www.techmetalsresearch.com/metrics-indices/tmr-advanced-rare-earth-projects-index/)