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Taranis Extends Gold Pit at Depth, Samples 2.04 m of Bonanza-Grade Material 26.6 g/t Gold, 1,246 g/t Silver, 3.1% Lead, 4.3% Zinc & 0.55% Copper

Drill Results Sampling & Geoscience Results

FOR IMMEDIATE RELEASE

Taranis Resources Inc.

14247 West Iliff Avenue

Lakewood, Colorado

80228-5421

www.taranisresources.com

Taranis Extends Gold Pit at Depth, Samples 2.04 m of

Bonanza-Grade Material 26.6 g/t Gold, 1,246 g/t Silver, 3.1%

Lead, 4.3% Zinc & 0.55% Copper

Lakewood, Colorado, November 14, 2017 – Taranis Resources Inc. (“Taranis”) [TSX.V: TRO]

is pleased to update exploration activity related to its 100%-owned Thor mine (MX-5-602).

Taranis has received assay results from a zone located 700m so utheast of the high -grade SIF

gold zone where mining activity was initiated at Thor this summer. Gold Pit channel sampling

was undertaken after Taranis further excavated the zone at depth in A ugust of 2017 , and

extended the highest -grade mineral occurrence known on the Thor project. Mechanical

excavation made another important model-building discovery at Thor in 2017, and this will be

released in a subsequent news release.

2017 Gold Pit Excavation

Contrary to what was previously thought about the Gold Pi t Area, the continued excavation of

the zone at depth showed that the plunge of the mineralization is steeply to the southeast. It was

formerly thought that the mineralization plunged shallowly to the northwest.

A channel sample across the zone at the bottom of the 2017 trench returned the following results,

and a photograph of the outcrop showing the channels sample locations has been posted on

www.taranisresources.com

From

(m)

To

(m)

True

Thickness

(m)

Gold

(g/t)

Silver

(g/t)

Lead

(%)

Zinc

(%)

Copper

(%)

1.53 3.57 2.04 26.6 1,245.7 3.08 4.32 0.55

 Includes 0.64 m of 72.81 g/t Au, 1,716 g/t Ag, 3.6 % Pb, 6.0 % Zn, 0.78% Cu & 0.42%

Sb

Sampling undertaken in 2015 at the top of the currently exposed outcrop (January 14, 2015 )

reported similar, but lower -grade results . These results are duplicated here for the sak e of

comparison, but were all located above the 2017 sampling.

Line From

(m)

To

(m)

Interval

(m)

Gold

(g/t)

Silver

(g/t)

Lead

(%)

Zinc

(%)

1 0.00 1.64 1.64 14.3 254.9 0.99 0.52

2 0.00 2.04 2.04 52.4 1,541.8 1.39 0.08

3 1.16 2.06 0.90 3.9 4.0 0.01 trace

0 0.40 1.35 0.95 4.7 722.9 4.15 4.07

2

Geological mapping of the outcrop appears to show that the zone is widening at depth, and the

high-grade gold and silver is moving onto a structural contact under a quartz -rich zone into the

Sharon Creek Formation.

Comparison and Implications for Gold Pit Zone and SIF / SIF-Extension Zones

The Gold Pit Zone occurs about 700 m southeast of the newly discovered SIF -Extension zone

that was bulk sampled in 2017, and recently yielded high-grade gold including 28.79 g/t gold

over 3.72 meters true thickness. SIF Extension is primarily a coarse -gold in quartz deposit, while

high-grade gold, sil ver and base metals are hosted in the conventional sulphide occurrence at

Gold Pit.

The mineralogy of the two zones differs considerably, but a coherent picture is starting to form

that may indicate that the zones are connected. Both zones occur west of the known Thor deposit

in a complex area of faulting within the Thor Anticline, and both have a unique d ip to the

southwest. All other known areas of mineralization at Thor dip moderately to the northeast and

return lower-grade gold assays. Also, both areas of high-grade gold mineralization lie directly on

the contact between the underlying Sharon Creek formation and the overlying Broadview

Formation. This suggests that the high -grade gold is likely stratifo rm in nature, and has been

subjected to remobilization along the contact by folding and faulting. What is known is that this

receptive contact connects the two areas separated by 700m , and it is possible that the gold

mineralization is contiguous. Further exploration is necessary to prove this concept.

John Gardiner, President and CEO remarks “ Grades and a very unique metal content like tho se

seen at Gold Pit are approaching what defined the unique Eskay Creek Mine in British Columbia

that was mined by Barrick Gold from 1993-2008. Eskay Creek also had a very small footprint

(1.5 M tonnes), and careful exploration is required to define these types of zones . Eskay Creek

produced over 3 M Oz. of gold ( grading 48.4g/t Au) and 160 M Oz. of silver ( grading 2,221g/t

Ag), making it one of the highest -grade mines in Canada. One of the common threads between

Thor and Eskay Creek apart from the metal grades is the volcanogenic massive sulphide model

that has been advocated for both deposits . While the extent o f Gold Pit’s exploration is in its

infancy, we think the potential to extend this bonanza-grade area over distance is very real”.

Quality Control and Analytical Procedures

Samples were analyzed by MS-Analytical in Vancouver, Canada. Fire Assay was completed on a

30g sample for gold content and the remaining analytical data was completed using ICP

analytical methods. Silver content over 100 g/t was determined using gravimetric methods.

All sampling and gold determinations are subject to a rigorous q uality control program that

includes the placement of standards and blanks a minimum of every tenth sample in addition to a

rigorous internal control instituted by MS-Analytical.

Qualified Person - Exploration activities at Thor were overseen by John Gard iner (P. Geol.)

who is a Qualified Person under the meaning of Canadian National Instrument 43-101.

About Taranis Resources Inc.

Taranis is an exploration and mining company focused on the development of its 100% -owned

Thor project in southeast British Columbia. In 2017, Taranis undertook a f ully permitted mining

operation on the property aimed at recovering gold and gaining a better understanding of the

newly discovered gold zones at Thor. Taranis is pursuing two parallel and distinct strategies at

3

Thor: one focused on continuing to mine the deposit in a series of three steps, and the other is the

continued growth and expansion of the existing deposit. P lease visit our website at

www.taranisresources.com for more information.

Taranis currently has 55,951,716 shares issued and outstanding ( 63,376,716 shares on a fully -

diluted basis).

TARANIS RESOURCES INC.

Per: John J. Gardiner (P. Geol.),

President and CEO

For further information contact:

John J. Gardiner

14247 West Iliff Avenue

Lakewood, Colorado

Phone: (303) 716-5922

Cell: (720) 209-3049

[email protected]

NEITHER THE 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 NEWS RELEASE.

This News Release may contain forward looking statements based on assumptions and judgments of management

regarding future events or results that may prove to be inaccurate as a result of factors beyond its control, and

actual results may differ materially from expected results.