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Megawatt files NI 43 101 Technical Report for the Tyr Project, NSW and Century South Project, Queensland, Australia

Resource Estimates Technical Reports (NI 43-101)

Megawatt files NI 43 101 Technical Report for the Tyr Project, NSW and Century

South Project, Queensland, Australia

Vancouver, British Columbia--(May 7, 2021) - Megawatt Lithium and Battery Metals Corp.

(CSE:MEGA) (FSE: WR20) (OTC PINK: WALRF) (the "Company" or "Megawatt") is pleased to announce

that it has completed and filed on SEDAR an NI 43 101 Technical Report for the Tyr Silver Project in

New South Wales, Australia and Century South Project in Queensland, Australia. The report has been

prepared by Xplore Resources Pty Ltd (“Xplore Resources”) of Brisbane, Queensland, Australia. The

Qualified Person for the Technical report is Matthew Stephens FAIG.

Highlights:

The Tyr project is located about 20km south-west via sealed road from the town of Tenterfield. The

tenement covers 100 units for an area of 299km2.

The Tyr Project area is located over three (3) main Sub-provinces of New England Orogen;

• Central Block, which is mainly comprised by conglomerate, sandstone and siltstone.

Including some felsic igneous rocks and quartzite units;

• Tablelands Complex, which mainly comprises granite and mineralised related material;

• New England Orogen Granites (dominant lithology of porphyry and basalt).

The Tyr tenement hosts a large number of mineral occurrences according to evidence from historical

mines within the exploration licence area. These activities were mostly focused on silver, lead, zinc,

arsenic and tin. The Tyr exploration area contains a significant amount of silver occurrences which

strikes north-west. Clive group contains major occurrences such as the Ecuador deposit consisting of

4710ppm silver and Torny Mine consisting of 1420ppm silver.

The Tyr project area has over 145 mineral occurrences recorded in the tenement. Those occurrences are

hosted by the Early Permian Bondonga beds form two main clusters:

• the Mole River group in the northern part of the tenement and

• the Clive group in the southern part.

At these two areas, the mineral occurrences are structurally controlled and are related to the

emplacement of the Mole Granite, which is classifies as a I-type Sn-W granite. Metal zonation around

the granite is well developed, with proximal Sn-W, grading outwards from the intrusion to distal

polymetallic Cu-Pb-Zn-Ag mineralisation. Evidence suggests that the Tyr Project Area is underexplored

and there is significant potential for structurally controlled silver rich polymetallic vein/lode systems.

Obvious areas that warrant further exploration include the areas containing the Mole River and Clive

group of mineral occurrences. Both of these areas are strongly mineralised and detailed field mapping

and surface geochemical sampling suck as rock chip and soil sampling, followed

by ground geophysical surveys including IP or even sub-audio magnetics (SAM).

Surface geochemical surveys within the Tyr project area have been completed by most of the past

explorers. The geochemical surveys have included rock chip/grab, stream sediment, panned

concentrate, soil sampling programs and high silver grades have been returned.

Significant silver assays from adits, shaft, and other workings, significant silver assays from surface

samples, and significant assays from drilling samples have all been recorded. The mineral occurrences

are structurally controlled and are associated with joints, faults, shear zones and lithological boundaries

that have controlled emplacement of mineralising fluids.

Despite the large number of mineral occurrences and historical workings and significant silver assays up

to 4,710g/t, there has been little drilling in the Tyr Project area. While past exploration focused almost

exclusively on the historical working, there was little emphasis on

testing the strike potential of the structures and/or lithologies that control mineralisation. Modern

exploration techniques are proposed to fully exploit the potential of the tenement, particularly the

mineralised clusters of historical silver-zinc-lead mines.

The Century South tenement is located approximately 204km NW of the town of Mount Isa, 122km NE

of the town of Mount Isa Camooweal and 61km SW of the town of Mount Isa Gregory.

Generally, the Century South tenement has been sparsely sampled considering its proximity to the

major Zn-Pb massive sulphide deposit of Century Mine. Crucially, the tenement covers land on the exact

same major fault strike as the mine. The major fault complex of the Termite

Range Fault crosscuts the centre of the tenement NW-SE. This faulted area would be the likely source of

mineralisation across the tenement and should be explored and further defined. These constituents

conform to a genetic model alluding to a potential deposit indicative of other massive sulphide deposits

found around the world.

The Grevillea gossan was the subject of an Honours Thesis by Hann (1999), who found that Tl, Pb, Si, and

Fe are surface indicators of mineralisation at the Grevillea deposit. Hann (1999) found there were two

types of gossans present overlying the massive pyrite zone:

• the jarositic limonites and

• the hematite limonites.

There are untested (drilling) surface geochemical anomalies to review.

Enough data from stream sediment, rock chip and soil assays, suggest that elevated levels of zinc and

lead do exist within the tenement area. Recent airborne EM surveys and subsequent exploration drilling

programs conducted by peer companies targeting the mineralised bearing unit of the Riversleigh

Siltstone Formation have yielded promising but ultimately uneconomical levels of Pb and Zn. However,

the results have been auspicious enough to ramp up exploration in the area immediately to the west of

Century South. There are several outcrops visible from satellite imagery that could be easily inspected.

Identifying boundaries this way may be a cost-effective way of defining lithologies. This may be of

benefit as some research suggests; particularly at Grevillea, that the mineralisation in the area is

stratabound.

The thickness of the regolith is substantial in the southern areas, adjacent to Grevillea, west of Century

South. The regolith cover overlaying the mineralisation bearing units can present multiple obstacles.

Deeper penetrating EM methods such as Magneto-Telluric (MT) can be used but at a greater cost.

Ultimately, this factor may be unavoidable as exploration progresses deeper into the bedrock.

Therefore, targeting the more oxidised gossans and obvious outcrops would be the quickest way to gain

preliminary knowledge of the likelihood of mineralisation in the area. A suggested exploration regime of

starting at highlighted areas of magnetic anomalies with elevated stream sediments, may allow more

targeted sampling.

Qualified Person

Mr. Geoffrey Reed (MAusMM (CP)) (MAIG), Consultant for the Company, is a qualified person as defined

by National Instrument 43-101 – Standards of Disclosure or Mineral Projects and has reviewed the

scientific and technical information in this press release.

About MegaWatt Lithium and Battery Metals Corp.

MegaWatt is a British Columbia based company involved in the acquisition and exploration of mineral

properties in Canada. The Company holds a 100% undivided interest, subject to a 1.5% NSR on all base,

rare earth elements and precious metals, in the Cobalt Hill Property, consisting of eight mineral claims

covering an area of approximately 1,727.43 hectares located in the Trail Creek Mining Division in the

Province of British Columbia, Canada.

Additionally, the Company has acquired a 60% interest in a company that indirectly holds a 100%

interest (subject to a 2% NSR) in two prospective silver-zinc projects in Australia, being the Tyr Silver

Project and the Century South Silver-Zinc Project (see press release dated August 13, 2020), an indirect

100% interest (subject to a 1% NSR) in and to certain mining tenements in Northern Territory and New

South Wales, Australia prospective for nickel-cobalt-scandium and rare earths and a 100% interest

(subject to a 2% NSR) in and to the Route 381 Lithium Property, comprised of 40 mineral claims located

in James Bay Territory, north of Matagami in the Province of Quebec, covering 2,126 hectares (see press

release dated February 3, 2021).

Investors can learn more about the Company and team at https://megawattmetals.com.

FOR FURTHER INFORMATION PLEASE CONTACT:

David Thornley-Hall Chief Executive Officer

[email protected]

The CSE does not accept responsibility for the adequacy or accuracy of this release.

This press release includes "forward-looking information" that is subject to a number of assumptions, risks

and uncertainties, many of which are beyond the control of the Company. Forward-looking statements

may include but are not limited to, statements relating to the trading of the Company's common shares on

the Exchange and the Company's use of proceeds and are subject to all of the risks and uncertainties

normally incident to such events. Investors are cautioned that any such statements are not guarantees of

future events and that actual events or developments may differ materially from those projected in the

forward- looking statements. Such forward-looking statements represent management's best judgment

based on information currently available. No securities regulatory authority has either approved or

disapproved of the contents of this news release.