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Trifecta Gold Ltd. is Drilling Sheeted Quartz Veins at Rye Property, Yukon

Corporate Updates

510 – 1100 Melville St. www.trifectagold.com

Vancouver, B.C. V6E 4A6 [email protected]

Tel: 604.687.2522 TSX-V: TG

Trifecta Gold Ltd. is Drilling Sheeted Quartz Veins at Rye Property, Yukon

• Inaugural drill program underway at Rye Property, Yukon

• Preliminary 2025 rock sampling returned multiple assays greater than 5 g/t gold, including a

highlight assay of 21.1 g/t gold

• First hole intersected a broad area with sheeted vein densities greater than 25 per metre

within hornfels, suggesting close proximity to a gold-bearing fluid source

August 28, 2025 - Trifecta Gold Ltd. (TSX-V: TG) (OTCQB:TRRFF) (“Trifecta” or the “Company”) is

pleased to report that its inaugural drill program at the Rye Property is underway. The Project is situated

14 km from the North Canol Road between two mid-Cretaceous granitic intrusions – the Itsi and Itsi East

plutons – in the eastern portion of Yukon’s Tombstone Gold Belt.

The Company has completed 970 m of diamond drilling in three holes to date, as part of a planned 1500 to

2000 m program (Figure 1). The holes are directed toward zones of densely sheeted quartz -

tourmaline±arsenopyrite veins, located in and around the reduced, mid-Cretaceous Itsi Pluton, where rock

sampling has returned multiple assays in excess of 5 g/t gold and 1000 ppm bismuth, including a highlight

assay of 21.1 g/t gold and 8550 ppm bismuth collected in 2025.

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Figure 1– Map of completed and proposed diamond drill holes at Rye with rock samples greater than 0.5 g/t gold

Hole RY-25-01 was collared approximately 400 m from mapped extent of the Itsi Pluton, within hornfelsed

Road River Formation siliciclastics. The hole targeted an area of intense sheeted veining in outcrop where

specimen samples of individual, one to five centimetre wide, quartz-arsenopyrite veins have yielded up to

6.5 g/t gold and 1565 ppm bismuth. Hole RY-25-01 cut a 224 m wide zone (from surface) of hornfels

hosting an abundance of sheeted quartz -pyrrhotite-chalcopyrite±arsenopyrite±scheelite veins , with

measured vein densities greater than 25 per metre (Figure 2).

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Figure 2 – Three images of drill core from hole RY-25-01, clockwise from left: A) sheeted vein density >25 per

metre comprising quartz-pyrrhotite-chalcopyrite±arsenopyrite±scheelite from 163.45 - 187.45 m; B) detailed view

of a syntaxial quartz-arsenopyrite-scheelite vein at 171.85 m; C) fluorescing scheelite at 94.00 m depth in quartz-

scheelite-pyrrhotite veins

Hole RY-25-02 was collared 360 m southwest of RY-25-01, adjacent to the mapped extent of the Itsi Pluton.

The hole intersected hornfelsed siliciclastics, as well as intervals of granodiorite, commonly exhibiting a

chlorite-rich greisen type of alteration. Sheeted vein density was significantly lower than the first hole,

comprising only minor quartz -sulphide veins in the hornfels and incipient tourmaline-muscovite veins in

the granodiorite.

Hole RY-25-03 is currently in progress, 175 m south of hole RY-25-02. It is directed toward sheeted veins

in hornfels outcrop, developed within an approximately 170 m wide extensional structural corridor. Within

this corridor, specimen samples of individual veins have yielded up to 21.1 g/t gold and 8550 ppm bismuth.

The hole intersected 209 m of hornfels from surface before pr ogressing into intrusive phases of the

underlying Itsi Pluton, which host sheeted quartz±tourmaline±arsenopyrite veins (Figure 3).

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Figure 3 – Drill core from hole RY-25-03, 826 to 976 ft (252 m to 297 m) demonstrating multiple phases of the

reduced Itsi Pluton, as well as moderate sheeted quartz±tourmaline±arsenopyrite veins set within bleached feldspar

halos

Drill hole specifics are listed in the table below:

Hole ID Easting (mE) Northing (mN) Azimuth Dip Total Depth (m)

RY-25-01 443185 6978904 315 -45 318

RY-25-02 443003 6978590 305 -45 287

RY-25-03 442893 6978453 115 -45 In progress

Analytical work was done by ALS Minerals, with sample preparation in Whitehorse, Yukon and assays and

geochemical analyses completed in North Vancouver, British Columbia. All rock samples were analyzed

for gold by fire assay with an atomic absorption spect roscopy (AAS) finish on 30 g samples (Au -AA23),

and 48 other elements by four acid digestion and inductively coupled plasma mass spectroscopy (ME -

MS61L). Overlimit analysis for samples with gold values greater than 10 g/t were analyzed by fire assay

using a gravimetric finish (Au-GRA21).

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Technical information in this news release has been approved by Trifecta’s Vice President, Jackson Morton,

P.Geo., a qualified person as defined under the terms of National Instrument 43-101.

About Rye

The Rye Project is located in eastern Yukon, 14 km south of the North Canol Road, an unpaved,

government-maintained highway. Work in 2024 outlined an intense, 500 x 200 m gold -, bismuth-, and

tellurium-in-soil anomaly overlying the contact zone of a mapped Tombstone Gold Belt reduced intrusion

and surrounding hornfels. Sheeted quartz veining is observed both within the intrusion and surrounding

hornfels and vein specimen samples have yielded up to 21.1 g/t gold and 8550 ppm bismuth.

Tombstone Gold Belt

Extending more than 1000 km from the Fairbanks district in Alaska eastward across the entire width of

Yukon, the Tombstone Gold Belt hosts many large Reduced Intrusion-Related Gold System (RIRGS) mines

such as Fort Knox in Alaska (>10 million oz), Eagle an d Olive in Yukon (>4 million oz) and the past -

producing Brewery Creek Mine, also in Yukon. Since May 2020 over 17 million additional ounces of gold

have been discovered in the Yukon portion of the belt, including Snowline Gold’s Tier 1 Valley discovery,

Sitka Gold’s RC deposit, Banyan Gold’s AurMac deposits and Victoria Gold’s Raven deposit.

Tombstone Gold Belt systems are characterized by sheeted, auriferous quartz veins forming in the carapace

zones of Cretaceous-age plutons. They have a characteristic geochemical signature with a gold -bismuth-

tellurium±tungsten core within a broader gold-arsenic halo. The deposits are found within and surrounding

the reduced intrusions, and typically exhibit a geophysical signature comprising a magnetic low (ie.

reduced) coinciding with at conductivity low. Veining in RIRGS systems is typically zoned with a core of

sheeted veins surrounded by more discrete gold-arsenic veins and more distal silver-lead-zinc veins.

About Trifecta Gold Ltd.

Trifecta is a Canadian -based precious metals exploration company dedicated to increasing shareholder

value through the discovery and development of 100% held gold projects in Yukon and Nevada. Trifecta

has secured an option to acquire a 100% interest in Mt . Hinton, Rye and 9 other highly prospective,

intrusion-related gold projects located in Yukon's Tombstone Gold Belt where over 17 million ounces of

gold have been discovered since May 2020. Initial drilling at the Company's Yuge Gold Project, located in

northern Nevada, has identified multiple broad zones of gold mineralization near historical high -grade

mines. The Company's Eureka Project hosts an 8 x 2.5 kilometre belt of surface showings and anomalous

gold-in-soil that straddle the headwaters of two of the most productive placer creeks in Yukon's southern

Klondike Goldfields. Trifecta's Treble Project covers a large hydrothermal system, located midway between

Western Copper and Gold Corporation's Casino Deposit, the largest copper and gold deposit in the Yukon,

and Rockhaven Resources Ltd.'s Klaza Deposit, a high-grade gold-silver deposit.

ON BEHALF OF THE BOARD

“Richard Drechsler”

President and CEO

For further information concerning Trifecta or its various exploration projects please visit

www.trifectagold.com or contact:

Corporate Information

Trifecta Gold Ltd.

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Richard Drechsler

President and CEO

Tel: (604) 687-2522

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 exploration

and other risk factors beyond its control, and actual results may differ materially from the expected results.

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.