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Power Metals Announces Assays Up To 4.43% Li2O From Paterson Lake Mapping Program

Drill Results

Power Metals Announces Assays Up To 4.43% Li2O From Paterson

Lake Mapping Program

VANCOUVER

,

July 30, 2018

/CNW/ -

Power Metals Corp.

("

Power Metals Corp.

" or the "

Company

") (TSX VENTURE:PWM)

(FRANKFURT:OAA1)(OTC:PWRMF) is pleased to announce that geological mapping at Paterson Lake, 60 km north of

Kenora

, northwestern

Ontario

successfully identified high-grade Lithium (Li) and high-grade Tantalum (Ta) mineralization. The geological mapping program also identified

three target areas for follow up exploration:

Western extension of Marko's Pegmatite

Rhea's Pegmatite

Cook's Pegmatite

Paterson Lake grab sample assay highlights from the western extension of Marko's Pegmatite include (Table 1 and Figure 1 and 2):

Three pure petalite samples (159037, 159201, 159222) with 4.43, 4.17 and 3.90 % Li

2

O

Two petalite dominate samples (159217, 159038) with 3.62 and 3.36 % Li

2

O

Sample 159218 with abundant petalite with 1.57 % Li

2

O

Petalite is an ore mineral of Lithium. Petalite (LiAlSi

4

O

10

) is the high temperature lithium aluminosilicate whereas spodumene (LiAlSi

2

O

6

) is the low

temperature/high pressure lithium aluminosilicate.

In addition to Lithium, the western extension of Marko's pegmatite grab samples are also enriched in extremely high-grade Tantalum (Ta) and

Cesium (Cs) with:

Sample 159219 with 1236 ppm Ta and 2473 ppm Cs

Sample 159221 with 725 ppm Ta and 472 ppm Cs.

Dr. Selway, VP of Exploration, stated "Paterson Lake Property has so many known pegmatites. I am ecstatic that our due diligence mapping has

confirmed the presence of petalite and identified three target areas for exploration follow up. Both the lithium and tantalum grades are extremely

high and this gives us great confidence following up these assays with a drill program. Exploration activities on the Paterson Lake Property are

ongoing."

The western extension of Marko's pegmatite's grab samples were collected between Marko's petalite pegmatite outcrop to the east and the J-

series petalite pegmatite to the west. The grab samples are up to

260 m

west of the historically known Marko's pegmatite outcrop. Historical

mapping has shown that the Marko's pegmatite occurs along the contact between mafic metavolcanics, gabbro and iron formation. Power Metals

grab sampling found the petalite pegmatite samples along strike of Marko's pegmatite along the same lithology contact. Historical mapping has

shown that the Marko's pegmatite has a central core of petalite surrounded by blocky pegmatite which hosts Ta-oxide mineralization.

In 2002, historical drilling indicated that the Marko's pegmatite was

170 m

long and made up of 2 to

12 m

wide boudinaged lenses. The 2002

drilling also intersected North Marko's pegmatite, a 10 to

30 m

wide pegmatite dyke, parallel to Marko's pegmatite with an unknown strike length.

This historical drilling did not test the western extension of the Marko's pegmatite. Since Power Metals Li-rich grab samples are along strike of the

Marko's pegmatite and North Marko's pegmatite, there is an excellent potential for the Marko's pegmatite to extend westward.

Figure 1 Grab sample 159037 of pure petalite from the western extension of Marko's pegmatite, Paterson Lake Property,

Ontario

.

Paterson Lake grab sample assay highlights from Rhea's pegmatite include (Table 1 and Figure 2):

Sample 159021 with 2.31 % Li

2

O and 111 ppm Ta

Sample 159022 with 198 ppm Ta.

Cook's pegmatite has elevated Li values up to 0.34 % Li2O and up to 161 ppm Ta. Rhea's pegmatite and Cook's pegmatite are

312 m

apart along

strike along the contact between mafic metavolcanics, metasediments and mafic tuffs. Rhea's and Cook's pegmatites are along the same contact

between mafic metavolcanics and metasediments as other petalite pegmatites historically mapped by Ontario Geological Survey: Draven, Black

Bear, Ballpeen, Pegmatites # 5, 6, 7, 8, 9, 10 and 11. The exploration potential is excellent that more petalite pegmatites will be found along this

contact on the Paterson Lake Property. The Cook's pegmatite is an enormous pegmatitic granite

420 m

long by

140 m

wide covered by black

lichen. A thorough cleaning of the Cook's pegmatite may result in discovery of lithium mineralization similar to that at Rhea's pegmatite.

Paterson Lake Property occurs within the Separation Rapids Greenstone Belt which is also home to the Big Whopper and Big Mack petalite

pegmatites (Figure 2). Separation Rapids Greenstone Belt is known as the Bird River Greenstone Belt in

Manitoba

which hosts the Tanco

pegmatite.

Power Metals' Paterson Lake property consists of 106 cell claims within the Paterson Lake and Treelined Lake Areas. The Property is

approximately 7 km x 3 km in size. Power Metals optioned the Paterson Lake property in 2017 because the property has multiple known petalite

pegmatite dykes on surface, but yet is still underexplored.

Quality Control

The grab samples were delivered to SGS preparation lab in

Red Lake

by Power Metals' geologist. The samples were then shipped to SGS

analytical lab in

Lakefield, Ontario

which has ISO 17025 certification. Every 20 samples included one external quartz blank and one external lithium

standard. The ore grade Li

2

O% was prepared by sodium peroxide fusion with analysis by ICP-OES with a detection limit of 0.002 % Li

2

O. A

QA/QC review of the standards and blanks for this mapping program indicate that they passed and the assays are accurate and not contaminated.

Paterson Lake

Paterson Lake Property is located in Paterson Lake and Treelined Lake Areas, 60 km north of

Kenora

,

NW Ontario

close to the

Ontario

-

Manitoba

border. Paterson Lake Property is located within the Separation Rapids Greenstone Belt and hosts multiple petalite-bearing pegmatite dykes. The

Property was optioned from Exiro Minerals Corp. in 2017 (Power Metals press release dated

April 20, 2017

). Avalon Advanced Materials

Separation Rapids Lithium Project with 8.12 Mt at 1.37 % Li

2

O measured + indicated resources as of

November 15, 2017

is located 1.2 km from

the Paterson Lake Property. Power Metals has an 80% interest with its 20% working interest partner MGX Minerals Inc.

Table 1 Grab samples from Paterson Lake Property, northwestern Ontario. UTM NAD 83, Zone 15.

Sample

Number

Easting

(m)

Northing

(m)

Li

2

O

(%)

Ta

(ppm)

Cs

(ppm)

west along strike of Marko's pegmatite

159001

393086

5569688

0.096

151

327

159002

393085

5569685

0.204

116

373

159035

392852

5569586

0.233

3.1

935

159037

392864

5569586

4.43

23.1

170

159038

392865

5569592

3.36

157

1742

159039

392866

5569589

0.121

200

1307

159201

393087

5569689

4.17

17.4

39.5

159217

392853

5569581

3.62

74.3

1025

159218

329400

5570239

1.57

1.9

230

159219

392386

5570235

0.245

1236

2473

159221

392901

5569591

0.118

725

472

159222

392900

5569594

3.90

29.7

185

Rhea's Pegmatite

159021

391872

5570163

2.31

111

32.1

159022

391872

5570160

0.018

198

22.9

Cook's pegmatite

159018

329400

5570239

0.221

22.3

195

159043

392275

5570234

0.217

17.4

81.8

159045

392331

5570238

0.275

161

120

159206

392303

5570225

0.337

25.8

170

Figure 2 Paterson Lake Lithium Project geology and pegmatite occurrences map.

Case Lake

Case Lake Property is located in Steele and Case townships, 80 km east of

Cochrane

,

NE Ontario

close to the

Ontario

-

Quebec

border. The Case

Lake pegmatite swarm consists of five spodumene dykes: North, Main, South, East and Northeast Dykes on the Henry Dome. All five of the dykes

contain spodumene mineralization. Power Metals has an 80% interest with its 20% working interest partner MGX Minerals Inc.

Qualified Person

Julie Selway

, Ph.D., P.Geo. supervised the preparation of the scientific and technical disclosure in this news release. Dr. Selway is the VP of

Exploration for Power Metals and the Qualified Person ("QP") as defined by National Instrument 43-101. Dr. Selway is supervising the exploration

program at Case Lake. Dr. Selway completed a Ph.D. on granitic pegmatites in 1999 and worked for 3 years as a pegmatite geoscientist for the

Ontario Geological Survey. Dr. Selway also has twenty-three scientific journal articles on pegmatites. A National Instrument 43-101 report has

been prepared on Case Lake Property and filed on

July 18, 2017

.

About Power Metals Corp.

Power Metals Corp. is a diversified Canadian mining company with a mandate to explore, develop and acquire high quality mining projects. We are

committed to building an arsenal of projects in both lithium and high-growth specialty metals and minerals. We see an unprecedented opportunity to

supply the tremendous growth of the lithium battery and clean-technology industries. Learn more at

www.powermetalscorp.com

ON BEHALF OF THE BOARD,

Johnathan More

, Chairman & Director

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

accepts responsibility for the adequacy or accuracy of the content of this news release.

No securities regulatory authority has either approved or disapproved of the contents of this news release. The securities being offered have not

been, and will not be, registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act"), or any state securities

laws, and may not be offered or sold in the

United States

, or to, or for the account or benefit of, a "U.S. person" (as defined in Regulation S of

the U.S. Securities Act) unless pursuant to an exemption therefrom. This press release is for information purposes only and does not constitute

an offer to sell or a solicitation of an offer to buy any securities of the Company in any jurisdiction.

Cautionary Note Regarding Forward-Looking Information

This press release contains forward-looking information based on current expectations, including the use of funds raised under the Offering.

These statements should not be read as guarantees of future performance or results. Such statements involve known and unknown risks,

uncertainties and other factors that may cause actual results, performance or achievements to be materially different from those implied by such

statements. Although such statements are based on management's reasonable assumptions, Power Metals assumes no responsibility to update

or revise forward-looking information to reflect new events or circumstances unless required by law.

Although the Company believes that the expectations and assumptions on which the forward-looking statements are based are reasonable,

undue reliance should not be placed on the forward-looking statements because the Company can give no assurance that they will prove to be

correct. Since forward-looking statements address future events and conditions, by their very nature they involve inherent risks and

uncertainties. These statements speak only as of the date of this press release. Actual results could differ materially from those currently

anticipated due to several factors and risks including various risk factors discussed in the Company's disclosure documents which can be found

under the Company's profile on

www.sedar.com

.

This press release contains "forward-looking statements" within the meaning of Section 27A of the Securities Act of 1933, as amended, and

Section 21E the Securities Exchange Act of 1934, as amended and such forward-looking statements are made pursuant to the safe harbor

provisions of the Private Securities Litigation Reform Act of 1995. The TSXV has neither reviewed nor approved the contents of this press

release.

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SOURCE

POWER METALS CORP

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For further information:

Power Metals Corp., Johnathan More, 646-661-0409, [email protected]

CO: POWER METALS CORP

CNW 05:00e 30-JUL-18