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Inomin Forms Strategic Alliance on Fleetwood-Seneca Zinc-Copper-Silver- Gold Properties Deal consolidates a high-grade VMS mineral district with several exploration targets

Exploration Programs Partnerships & JV

Inomin Mines Inc. 400 Burrard Street, Suite 1130, Vancouver, BC Canada V6C 3A6

www.inominmines.com

NEWS RELEASE

Inomin Forms Strategic Alliance on Fleetwood-Seneca Zinc-Copper-Silver-

Gold Properties

Deal consolidates a high-grade VMS mineral district with several exploration targets

Vancouver, British Columbia, January 18, 2019 – Inomin Mines Inc. (TSX.V: MINE) ("Inomin”, “MINE”, or the

“Company") reports it has formed a strategic alliance with Turnagain Resources Inc. to co-market the companies’

adjacent Fleetwood and Seneca zinc-copper-silver-gold pr operties as a combined project named Fleetwood-

Seneca. Together the Fleetwood and Seneca properties are a considerably more attractive exploration and

development project as the properties consolidate a significant Volcanogenic Massive Sulphide ( VMS) district in

southwestern British Columbia.

Fleetwood-Seneca host the Seneca zinc-copper-silver-gold deposit, the partially -delineated Fleetwood, 33 and Vent

zones, and several priority exploration targets within a 6 kilometre by 2 kilometre mineral belt.

Any consideration received from a third -party deal, such as an investment or the sale of the Fleetwood -Seneca

project, is to be divided equally between Inomin and Turnagain. The strategic alliance agreement was entered into

December 21, 2018.

“The creation of the Fleetwood-

Seneca strategic alliance consolidates

a proven VMS district with several

polymetallic exploration targets,”

comments John Gomez, President &

CEO of Inomin Mines. “We look

forward to attracting a partner to

advance the exploration and

development of the project.”

Inomin Mines Inc. 400 Burrard Street, Suite 1130, Vancouver, BC Canada V6C 3A6

www.inominmines.com

Fleetwood-Seneca District Mineralization

The Fleetwood-Seneca project is located within a 6 km by 2 km northwest trending volcanic belt hosting extensive

zinc-copper-silver-gold rich VMS mineralization . Exploration in the belt has d iscovered four Kuroko style mineral

zones: Fleetwood, 33, Vent, and the Seneca deposit. These mineralized zones are typical of VMS districts where

deposits commonly occur in clusters.

Seneca Deposit

Within the Fleetwood-Seneca VMS district, most of the exp loration has focused at th e Seneca deposit where (in the

Seneca Pit zone) the mineralization is associated with dominantly felsic fragmental footwall units known as the ore

zone conglomerate. It is a massive sulphide body with a chalcopyrite -pyrite-rich base overlain by a sphalerite -barite-

galena-rich zone.

Drilling at the Seneca deposit has encountered several significant intersections that illustrate the high -grade,

polymetallic nature of portions of the massive sulphide mineralization including the following:

Hole Number Mineralization Zinc Copper Lead Silver Gold Interval

DDH-71-6 Massive 9.15% 1.01% - 84.6 g/t 2.82 g/t 7.3 m

DDH-74-31 Massive 11.28% 0.64% 0.66% 125.1 g/t 0.9 g/t 5.0 m

DDH-83-6 Massive 17.7% 5.11% 0.04% 144.3 g/t 6.96 g/t 1.3 m

Work included 33,000 metres of diamond drilling, underground development and extraction of a bulk sample

that was custom milled at the Britann ia Mine . This ex ploration was not carried out under the supervision of a

qualified p erson, nor has a qualified p erson verified the data ; as all , of the written information and reports are

unavailable. The only relevance herein is strictly as geological information.

An historic estimate of 1.506 million tonnes at a grade of 0.82 g/t gold, 41.13 g/t silver, 0.63% copper, 0.15%

lead, and 3.57% zinc for the Seneca deposit is referenced by Arnold (1996), Hoy (1991) and Chapman (1999),

without specifying any details, referring to an unpublished 1984 report by Wright Engineers.

This report is not available and none of the aforementioned q ualified persons have done enough work to classify this

estimate as current mineral resources or mineral reserves. This estimate ca nnot be considered as reliable since it is

unknown whether or not it was prepared by a qualified person. In addition , resource categories are not mentioned

and assumptions, parameters and methods used to prepare it are not known. There is no known more recent

estimate, and much additional drilling would be needed to verify such an estimate. The only relevance herein is

strictly as geological information. Neither Inomin nor Tur nagain consider this historical estimate as current or as an

indication of what might be found on the Fleetwood -Seneca project claim holdings. A qualified person has not done

sufficient work to classify the historical estimate as a current mineral resource an d is not treating the historical

estimate as a current mineral resource.

Exploration Targets

The stratabound alteration in the Seneca Pit area is along strike from the stockworks in the Fleetwood and Vent

zones indicating a large -scale structural /stratigraphic control o f the hydrothermal activity, as well as a genetic

relationship between the different alteration zones. The 2 and 3 kilometer distances along-strike between the Seneca

deposit and the Vent and Fleetwood zones, respectively, has potential for discovery of additional massive sulphide

bodies, in particular in the following areas:

1. Northeast of the Seneca deposit an 800 m by 80 0 m area has not been drill tested and is bounded by mineralized

intercepts;

2. An EM anomaly has not been drill tested in a 500 m by 500 m area between the Seneca and the Vent zones; and

3. A low intensity magnetic anomaly has not been drill tested in a 500 m section of favourable stratigraphy to the

northwest of the Vent and southeast of the Fleetwood zones.

Inomin Mines Inc. 400 Burrard Street, Suite 1130, Vancouver, BC Canada V6C 3A6

www.inominmines.com

Fleetwood and 33 Zones

The Fleetwood property covers the Fleetwood and 33 zones hosting both stockwork and overlying massive sulphide

mineralization, as well as a large EM anomaly.

The bulk of the exploration drilling done at Fleetwood was by Minnova Inc ., (Minnova became Inmet Mining which

was acquire d by First Quantum Minerals) that discovered the Fleetwood zone in the early 1990s. As part of their

program in 1991, Minnova drilled 41 holes at the Fleetwood zone intersecting significant VMS mineralization including

31.2 metres of stockwork type mineral ization at a depth of 153 metres , grading 2.1% zinc, 0.3 copper, 0.1%

lead, 8.1 g/t silver and 0.1 g/t gold.

At the 33 z one, located 350 metres southwest of Fleetwood, Minnova’s drilling returned 23.3% zinc, 1.8% copper,

1.7% lead, 133 g/t silver and 2.3 g/t gold over 3.2 metres at a depth of 170 metres.

Minnova’s drilling report concluded that further drill testing was warranted at the Fleetwood property.

This exploration was carried out by reputable companies, it was not done under the supervision o f a qualified person

nor has a qualified person verified the data as the written information and reports are unavailable. The only relevance

herein is strictly as geological information.

Exploration Targets

Minnova’s relatively wide spaced drilling at the Fleetwood zone (200 m centres) leaves room for the occurrence of

other mineralized bodies.

Northeast of the Fleetwood zone, field work in 2017 confirmed the presence of anomalous zinc and copper values

(geochemical sampling by Chevron) occurring withi n a prominent 1.75 km x 1 km airborne EM anomaly.

This Fleetwood EM anomaly is located in rocks higher in the volcanic succession and may represent a stacking of

mineralized horizons. A DC IP survey is recommended to further delineate the l arge Fleetwood EM anomaly as

geophysical surveys in the Seneca deposit area demonstrate IP is an effective exploration tool in this environment.

Access and Infrastructure

Located approximately 90 kilometres east of Vancouver, BC., Fleetwood-Seneca benefits from nearby services, good

road access, and excellent infrastructure including an electric powerline on the south end of the project. Additionally,

a railway and tidal-barge access are close to the property.

CEO Comment

“The creation of the Fleetwood-Seneca strategic alliance consolidates a proven VMS district with several polymetallic

exploration targets,” comments John Gomez, President & CEO of Inomin Mines. “We look forward to attracting a

partner to advance the exploration and development of the project.”

Further Information and News

For further information on the Fleetwood-Seneca project visit www.inominmines.com. Subscribe to receive future

MINE announcements by visiting https://bit.ly/2pWsA8i.

About Inomin Mines

Inomin Mines is engaged in the identification, exploration and development of mineral properties. The Company holds

a 100% interest in the Fleetwood zinc -copper VMS project in British Columbia, and the King’s Point gold -copper-zinc

project in Newfoundland under option to Maritime Resources Corp. (TSX.V MAE). Inomin trades on the TSX Venture

Exchange with the symbol MINE. For more information visit www.inominmines.com and join us on Twitter

@InominMines.

Inomin Mines Inc. 400 Burrard Street, Suite 1130, Vancouver, BC Canada V6C 3A6

www.inominmines.com

Inomin Director Bruce Winfield P.Geo, a qualified person as defined by NI 43 -101, has reviewed and approved the

technical information in this news release.

On behalf of the board of Inomin Mines:

Inomin Mines Inc.

Per: “John Gomez”

President and CEO

For more information please contact:

John Gomez

Tel. 604.566.8703

[email protected]

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

Exchange) accepts responsibility for the adequacy or accuracy of this release. This news release may contain assumptions,

estimates, and other forward -looking statements regarding future events. Such forward-looking statements involve inherent risks

and uncertainties and are subject to factors, many of which are beyond the Company's control that may cause actual results or

performance to differ materially from those currently anticipated in such statements.