| Trifecta Gold is Drilling Sheeted Quartz Veins at Rye Property, Yukon accessnewswire.comInaugural 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
 
 
 VANCOUVER, BC /  ACCESS Newswire / August 28, 2025 / Trifecta Gold Ltd.   (TSXV: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.
 
 
  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).
 
 
  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 progressing  into intrusive phases of the underlying  Itsi Pluton, which host  sheeted quartz±tourmaline±arsenopyrite veins  (Figure 3).
 
 
  
 
 
 
 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 spectroscopy (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).
 
 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 and 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.
 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.
 
 SOURCE: Trifecta Gold Ltd.
 
 
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