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Trailbreaker Resources Expands Multiple High Grade GOLD Zones at Atsutla with Phase 2 Sampling and Submits Drilling Permit Application FOR 2022

Permits & Approvals

TRAILBREAKER RESOURCES EXPANDS MULTIPLE HIGH GRADE GOLD ZONES AT ATSUTLA WITH

PHASE 2 SAMPLING AND SUBMITS DRILLING PERMIT APPLICATION FOR 2022

November 1st, 2021 – Trailbreaker Resources Ltd. (TBK.V) (“Trailbreaker” or “the Company”) is pleased

to announce the results from the Phase 2 exploration at its 100% -owned Atsutla Gold Project located in

northern British Columbia. Assay results indicate widespread high-grade gold values across all previously

defined zones as well as the expansion of known gold mineralization at the Highlands zone. Assay results

from the Phase 2 program include:

• HIGHLANDS ZONE: Gold values in excess of 100 g/t gold (Au) have been returned from a 750 m

x 600 m area with values as high as 222.05 g/t (6.48 oz/ton) Au at the newly discovered visible

gold showing and 165.4 g/t (4.82 oz/ton) Au with 1,894 g/t (55.25 oz/ton) silver (Ag) from an

area 430 meters to the south.

• NEW – CHRISTMAS CREEK ZONE: High grade mineralization has been discovered 2.0 km east of

the Highlands zone. A 30 cm-wide galena-rich quartz vein in bedrock returned assay values up to

102 g/t Au and 524 g/t Ag.

• WILLIE JACK TREND: The source of the 1.2 km -long Willie Jack gold -in-soil trend has been

confirmed. A series of metasediment -hosted quartz veins along the boundary of the Christmas

Creek batholith have returned assay values up to 9.89 g/t Au from in-situ bedrock and proximal

float. The veins have been traced for at least 700 meters.

• SWAN ZONE: High-grade gold has been discovered at the Swan zone; a 900 m x 700 m Au-Ag-

arsenic (As) -antimony ( Sb)-copper ( Cu)-molybdenum ( Mo)-lead ( Pb) soil anomaly, with soil

samples assaying up to 406 ppb Au. Grab samples from bedrock, proximal float, and talus have

returned grades up to 11.5 g/t Au in bedrock and 175 g/t Ag in float.

Daithi Mac Gearailt, CEO of Trailbreaker, commented: “We have now proved the existence of widespread,

high-grade gold across all explored areas of the Atsutla Gold project. The spatial extent and high-grade

nature of mineralization found at surface at the Highlands and Christmas zones has again exceeded our

expectations. Confirming the bedrock source of the extensive gold-in-soil anomalies at the Willie Jack and

Swan zones has moved this project into the drill planning stage. We are very excited for next season!”

With the addition of recent staking, t he Atsutla Gold Project now covers 37,727 hectares and spans 36

kilometers. The project area is located 70 km south of the Yukon -British Columbia border and 130 km

northwest of the community of Dease Lake, BC.

TSX-V: TBK

APRAF.PK

Frankfurt:KCG1

TRAILBREAKER RESOURCES LTD.

1040 W. Georgia Street, #1500

Vancouver, British Columbia

Canada, V6E 4H1

Telephone: 604 681 1820

Facsimile: 604 681 1864

https://www.TrailbreakerResources.com

https://twitter.com/TrailbreakerLtd.

The 2021 exploration program involved the collection of 2,100 soil samples and 532 prospecting rock grab

samples, as well as geological mapping and an airborne magnetic and radiometric survey. See linked map

for zone and sample locations: Map 1 – Atsutla Gold Highlights.

Highlands zone – Visible gold in an extensive vein system

The Highlands zone is located in the northwestern area of the Atsutla Gold Project. Results from Phase 1

include multiple high-grade grab samples, the highest being 630.04 g/t (18.38 oz/ton) Au with 531.75 g/t

(15.51 oz/ton) Ag . Also, a new visible gold zone was discovered 550 m west of these samples (see

September 13, 2021 news release).

Phase 2 analysis of the visible gold zone yielded values up to 222.1 g/t Au and 55 g/t Ag. More significantly,

prospecting in the vicinity of the visible gold showing revealed an extensive gossanous zone hosting one

or more 20-50 cm-thick quartz veins. This vein system was traced across a 700 m x400 m area and yielded

numerous high-grade gold values from grab samples of bedrock and proximal float (see Map 2 – Highlands

zone).

The vein system was also identified at two other locations at opposite ends of the gossan unit:

• An in-situ quartz vein showing, located 165m north of the initial visible gold discovery, returned

values as high as 112.4 g/t Au and 75 g/t Ag. This vein was traced along a 20-meter strike length,

is 20-40 cm thick, and displays abundant arsenopyrite, pyrite, and galena mineralization

• A zone of in-situ mineralized quartz veining 430 meters south of the visible gold showing returned

values up to 165.4 g/t Au with 1,894 g/t Ag and 125.0 g/t Au with 1,630 g/t Ag.

• In total, these high-grade (>100 g/t Au) vein showings occur across a 750 m x 600 m area.

First-pass prospecting to the northeast of the Highlands zone area yielded a sample assaying 9.9 g/t Au,

located 2.5 km northeast of the visible gold showing.

Christmas Creek zone – New high-grade gold discoveries in bedrock

The Christmas Creek zone is located across the Christmas Creek valley , ~2 km east of the Highlands zone

(see Map 3). To date, very limited exploration has been conducted in this area. Phase 2 prospecting at the

Christmas Creek zone discovered a 30 cm-wide galena-rich quartz vein in bedrock which returned values

up to 102 g/t Au and 524 g/t Ag. A sample of quartz float material 170 meters northwest from the bedrock

samples returned an assay of 50.6 g/t Au and 85 g/t Ag.

Willie Jack trend – Bedrock source of 1.25-kilometer-long Au-As-Ag-Mo-Te soil anomaly confirmed

Phase 2 prospecting has confirmed the source of the extensive gold -in-soil anomaly (termed the Willie

Jack trend) reported in the September 13, 2021 news release . The Willie Jack trend occurs along the

southwestern margin of the early Jurassic Christmas Creek Batholith, where it lies in contact with older,

Permian Kedahda Formation metasediments. The trend is at least 1.25 kilometers long, and falls within a

broader anomalous gold trend of 6.5 kilometers. It is characterized by anomalous Au-As-Ag-Mo-tellurium

(Te) soil sample values, with soil sample assays up to 3,767 ppb (3.77 g/t) Au. Sampling of quartz float and

quartz in metasedimentary bedrock indicate that the anomalous gold-in-soil trend originates from a series

of metasediment-hosted, northwest-trending auriferous quartz veins.

Phase 2 prospecting along this trend involved follow-up on the higher-grade soil samples. Multiple quartz

veins were uncovered, both as in-situ bedrock, and as proximal float. The highest grade returned from the

trend is 9.89 g/t Au, from an in-situ sample of quartz vein material. Rock samples along trend 700 meters

to the southeast returned assay values up to 2.01 g/t Au (see Map 4 – Willie Jack trend). Prospecting an

additional 4.1 km to the southeast has uncovered additional quartz veining, with assay values up to 1.56

g/t Au. A chip sample across siliceous quartzite in this area yielded 0.35 g/t Au over 6.5m.

Swan zone – New high-grade gold discoveries within an intrusive-hosted 900m x 700m Au-As-Ag-Sb-Cu-

Mo-Pb soil anomaly

The Phase 2 program has also led to the discovery of high-grade gold at the Swan zone, located in the

eastern area of the Atsutla claim block. Rock sample assays returned grades up to 11.5 g/t Au and 175 g/t

Ag.

The Swan zone area was staked to cover a historical molybdenum-copper porphyry prospect that was

discovered in the late 1960s and explored periodically since then. Despite collection of more than 500 soil

and surface rock samples , and completion of almost 1,000 meters of shallow diamond drilling, no

geochemical analysis for gold was ever completed before Trailbreaker staked the area.

The initial Phase 1 program at the Swan zone involved the completion of a soil sampling grid adjacent to

the historical drilling on a large gossanous ridge. Assay results from the soil sampling revealed a ~900 m x

700 m Au-As-Ag-Sb-Cu-Mo-Pb soil anomaly, with soil samples assaying up to 406 ppb Au. The core of the

soil anomaly is located ~1.2km east of the historical drilling. The anomaly occurs within a leucogranite -

porphyry unit of the Upper Cretaceous Glundebery Batholith.

Phase 2 involved one day of follow -up work in this area and uncovered sign ificant arsenopyrite

mineralization in bedrock, proximal float, and talus float . Rock samples taken from a mid -slope outcrop

returned grades of 11.5 g/t Au with 16.8 g/t Ag, and 8.39 g/t Au with 55.8 g/t Ag (see Map 5 – Swan

zone). A sample of proximal float 200 m southeast of this outcrop yielded grades of 7.6 g/t Au with 175

g/t Ag. Numerous other samples assayed >1 g/t Au in a 500 m x 200 m area within the soil anomaly.

Airborne survey

An airborne magnetic and radiometric survey has recently been completed at the Atsutla Gold project.

The survey covered the Highlands and Christmas Creek zones, as well as the Willie Jack trend. Trailbreaker

is currently reviewing and compiling the data. Maps and data will be presented in an upcoming news

release.

Drill Permitting

A permit for diamond drilling at the Atsutla Gold project has been submitted to the British Columbia

Ministry of Mines.

Message from the President

“Once again the exploration team has come through and surpassed expectations at the Atsutla project.

With a solid geochemical database and new geophysical data on our hands, we are carefully determining

the next steps for the project. While properly evaluating these high -grade gold showings is our focus, the

majority of the claim block is untouched ground , and one can only imagine what remains to be found at

Atsutla.”

ON BEHALF OF THE BOARD

Daithi Mac Gearailt

President and Chief Executive Officer

OTHER

Sample analysis and assaying for all of Trailbreaker’s projects have been conducted by Bureau Veritas

Mineral Laboratories Canada in Vancouver, BC, which is an ISO-17025 accredited laboratory. Rock samples

were crushed, split and pulverized to a 250 g pulp passing through a 200 mesh screen (prep code PRP70-

250). For gold analysis, a 50 g split underwent fire assay with an ICP-ES finish (FA350-Au). Samples assaying

>10 ppm Au were re-analyzed with a gravimetric finish (FA550-Au). Samples also underwent 37-element

analysis involving aqua regia digestion and ICP-ES/MS analysis (AQ200). Soil samples were sieved to 80

mesh ( prep code SS80) and under went a 37 -element analysis involving aqua regia digestion and ICP-

ES/MS analysis (AQ201).

Rigorous quality assurance procedures are in place regarding sample collection, chain of custody and data

entry. Certified QA/QC standard and blank ref erence samples are routinely inserted into the sample

stream to ensure integrity of the assay process. The reader is cautioned that grab samples are single rock

samples typically, but not exclusively, constrained to mineralization. Grab samples are selective in nature

and collected to determine the presence or absence of metal values. These do not necessarily provide an

accurate representation of the tenor of the targeted zone sampled.

Carl Schulze, P. Geo., Consulting Geologist with Aurora Geosciences Ltd , is a qualified person as defined

by National Instrument 43 -101 for Trailbreaker's BC and Yukon exploration projects, and has reviewed

and approved the technical information in this release.

For new information about the Company’s pro jects, please visit Trailbreaker’s website at

TrailbreakerResources.com and sign up to receive news. For further information , follow Trailbreaker’s

tweets at Twitter.com/TrailbreakerLtd, use the ‘Contact’ section of our website, or contact us at (604) 681-

1820 or at [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 release.

Forward-Looking Statements

Statements contained in this news release that are not histo rical facts are "forward-looking information"

or "forward -looking statements" (collectively, "Forward -Looking Information") within the meaning of

applicable Canadian securities legislation and the United States Private Securities Litigation Reform Act of

1995. Forward-Looking Information includes, but is not limited to, disclosure regarding possible events,

conditions or financial performance that is based on assumptions about future economic conditions and

courses of action; expectations regarding future e xploration and drilling programs and receipt of related

permitting. In certain cases, Forward -Looking Information can be identified by the use of words and

phrases such as "anticipates", "expects", "understanding", "has agreed to" or variations of such words and

phrases or statements that certain actions, events or results "would", "occur" or "be achieved". Although

Trailbreaker has attempted to identify important factors that could affect Trailbreaker and may cause

actual actions, events or results to differ materially from those described in Forward-Looking Information,

there may be other factors that cause actions, events or results not to be as anticipated, estimated or

intended. In making the forward-looking statements in this news release, if any, Trailbreaker has applied

several material assumptions, including the assumption that general business and economic conditions

will not change in a materially adverse manner. There can be no assurance that Forward -Looking

Information will prove to be accurate, as actual results and future events could differ materially from those

anticipated in such statements. Accordingly, readers should not place undue reliance on Forward-Looking

Information. Except as required by law, Trailbreaker does not assume any obl igation to release publicly

any revisions to Forward -Looking Information contained in this news release to reflect events or

circumstances after the date hereof or to reflect the occurrence of unanticipated events.