VANCOUVER - iMetal Resources, Inc. (TSX.V: IMR) (OTC PINK: ADTFF) (FRANKFURT: A7V2) ('iMetal' or the 'Company') is pleased to announce it has entered into an agreement pursuant to which it has been granted the option to acquire the 665 hectare Kerrs Gold Deposit, 90 kilometres east-northeast of Timmins, Ontario, in the Abitibi Greenstone Gold Belt.

The Kerrs Gold Deposit is comprised of a series of gold-bearing pyritized quartz vein replacement breccias enveloped by quartz fuchsite carbonate vein breccias averaging 10 metres in thickness. The deposit hosts an historical resource estimate of 7,041,460 tonnes grading 1.71 g/t gold yielding 386,467 ounces at a 0.5 g/t gold cut-off. Drilling subsequent to the historic estimate appears to have extended the mineralized zone along strike and down dip.

'The Kerrs Gold Deposit is a significant advanced gold asset located in one of the premier mining camps in Canada,' commented iMetal CEO Saf Dhillon. 'The Company leapt at the chance to complement our existing Ontario gold portfolio with the Kerrs Deposit. Once the technical team completes a thorough review of the historical database, iMetal will concentrate on both bringing the historical resource current as well as formulating a development plan to further expanding it.' he continued.

The Kerrs Gold historical resources estimate was disclosed in 'NI 43-101 Resource Estimation on the Kerrs Gold Deposit, Matheson, Ontario' prepared for Sheltered Oak Resources Inc. by Garth Kirkham, P. Geo of Kirkham Geosystems Ltd. and dated June 10, 2011.

Composite length of 2 m was chosen and composites were weighted by length.

Sectional interpretations were wire-framed to create 3-D solids of the zones.

Zones were coded to the composites, and the block model, to constrain the modeling process.

Composites for the mineralized zone were used to interpolate into the blocks for each zone.

Ordinary kriging was used as the interpolator.

Relative elevation modeling was used to guide the ellipse orientation that accounts for the variation in dip due to the synclinal structure.

A minimum of two composites were used for each block and a maximum of two composites were used per drill hole; a maximum of 12 composites were used per hole.

A cutting factor was applied for gold with outlier composites limited to 10 g/t Au based on cumulative frequency plots. A zero cut-off grade was used for the manual polygonal method.

Minesight Software was used to perform the block modeling and estimations.

The Kerrs historic estimate is an inferred resource as defined in National Instrument 43-101. The Company is not aware of any more recent resource estimates, though there was further drilling completed after the historic estimate was released. The Company will need to review the historical drilling and analyses and will need to twin a number of the historic holes to bring the historic estimate current.

The road accessible Kerrs Gold Deposit consists of 36 units totaling approximately 665 hectares and lies 90 kilometres east-northeast of Timmins, Ontario in the Abitibi Greenstone Gold Belt.

The Deposit was discovered by Noranda in the late 1970's early 1980's by following glacial dispersion trains up-ice to the source. Drilling continued into the late 1980's, with further drilling in the early to late-2000's and early 2011's. The drilling database was used to calculate the 2011 historic resource estimate, with further drilling completed subsequent to the release of the estimate. The Kerrs Gold Deposit consists of a series of gold-bearing pyritized quartz vein replacement breccias enveloped by quartz fuchsite carbonate vein breccias averaging approximately 10 metres and alteration envelopes varying up to 40 metres in thickness. Gold is directly related to pyrite content which ranges to 10% and is commonly found as disseminations and crystal aggregates in the sheeted, quartz vein replacement breccias. These breccias, averaging 31% quartz, exhibit reasonable correlation conforming to volcano-stratigraphic contacts as well as moderate to good continuity in grade correlations at the lower and upper boundaries of the vein breccia and alteration envelope assemblages.

The Kerrs Gold Deposit is stratabound, occurring at the contact of a thick, mafic pillow flow sequence overlying an ultramafic, magnetite-rich flow sequence. Quartz feldspar porphyry sills are spatially located above and below the breccia zones. This stratigraphy is synclinally folded with the deposit lying 350 m to 425 m below surface. Drilling has traced the main zone 800 metres and remains open in both directions and at depth.

The Company plans an immediate review of the historical database to define target areas to both significantly expand the historic resource and to test for additional structures. The Company has yet to verify the historical data.

The Kerrs Agreement

iMetal entered into a purchase option agreement (the 'Option Agreement'), dated January 24th, 2022, with Gravel Ridge Resources Ltd. and 1544230 Ontario Inc. (collectively, the 'Vendors') pursuant to which it will be granted the right to acquire the Kerrs Gold Deposit.

About iMetal Resources Inc.

A Canadian based junior exploration company focused on the exploration and development of its portfolio of resource properties in Ontario and Quebec. iMetal is focused on advancing its Gowganda West Project that borders the Juby Project, an advanced exploration-stage gold project located within the Shining Tree Camp area in the southern part of the Abitibi Greenstone Gold Belt about 100 km south-southeast of the Timmins Gold Camp.

Contact:

Saf Dhillon

Tel: 604-484-3031

Email: saf@imetalresources.ca

Web: https://imetalresources.ca

This news release may include forward-looking statements that are subject to risks and uncertainties. All statements within, other than statements of historical fact, are to be considered forward looking. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results or developments may differ materially from those in forward-looking statements. Factors that could cause actual results to differ materially from those in forward-looking statements include results of exploration, variations in results of mineralization, relationships with local communities, market prices, continued availability of capital and financing, and general economic, market or business conditions. There can be no assurances that such statements will prove accurate and, therefore, readers are advised to rely on their own evaluation of such uncertainties. We do not assume any obligation to update any forward-looking statements except as required under the applicable laws.

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