Duyuru • Jul 02
Trifecta Gold Ltd. Announces Commencement of Drilling At Mt. Hinton, Yukon Trifecta Gold Ltd. announced that drilling is underway at its road accessible Mt. Hinton project, situated within the Keno Hill Mining District of the Tombstone Gold Belt. The Mount Hinton Project is located less than 4 km from Hecla Mining Company's Keno Hill mill. Drilling Underway. A track-mounted drill and ancillary equipment was mobilized to the GC target at Mt. Hinton this past weekend and drilling is now underway. Trifecta plans to drill a minimum of 1,000 m at the GC target to determine the underlying source of a conspicuous resistivity and magnetic anomaly located in the floor of the Granite Creek valley. The extensive system of high-grade precious metal veins on the Mt. Hinton property is theorized to be related to a buried intrusion at the GC target. The shape and amplitude of the resistivity anomaly at the GC target is indicative of intrusive rock, while the magnetic response is comparable to responses derived from Tombstone and Mayo Suite intrusions that host large gold endowments elsewhere in the Yukon. Warrant Exercise. Trifecta announced that 2,852,817 common share purchase warrants (the "Warrants") bearing a strike price of $0.25 per share were exercised prior to their expiry date. The Warrants were issued as part of a Private Placement Financing that closed on June 28, 2024. Total proceeds of $713,204 was received from the exercised warrants. Several Trifecta insiders were among those who exercised Warrants. Trifecta's current shares outstanding is now 47,539,221. Upcoming Event. Trifecta will be participating in the upcoming Yukon Mining Allianc e's annual Invest Yukon Property Tours, taking place July 12-14, 2025, in Dawson City, Yukon. About Mt. Hinton. Mt. Hinton is a road accessible, camp-scale property with over 60 precious metals veins identified to date. The project is underlain by direct extensions of the stratigraphy that hosts Hecla's Keno Hill Mines and, because of this, much of the historical exploration at Mt. Hinton focused on its silver potential. Surprising, historical workers largely overlooked gold potential, despite visible gold that has been found in many of the known veins. Many bonanza grade (>100 g/t gold) assays have been reported from surface grab and chip samples. There are active placer mines on the creeks draining in all directions from the property. Based on metal zonation within the district and the regional magnetic signature at Mt. Hinton, a reduced intrusion on the property is theorized to be the driver for much of the mineralization in the district. Tombstone Gold Belt. Extending more than 1,000 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 and more distal silver -zinc veins. Technical information in this news release has been approved by Trifecta's Vice President, a qualified person as defined under the terms of National Instrument 43-101. Duyuru • Jun 03
Trifecta Gold Ltd., Annual General Meeting, Aug 11, 2025 Trifecta Gold Ltd., Annual General Meeting, Aug 11, 2025. Location: british columbia, vancouver Canada Duyuru • May 16
Trifecta Gold Ltd. announced that it has received CAD 5.320995 million in funding On May 15, 2025, Trifecta Gold Ltd. closed the transaction. The company issued up to 12,790,000 Charity Flow-Through Units at an issue price of CAD 0.38 per unit for the gross proceeds of CAD 4,860,200 and 1,706,648 units at a price of CAD 0.27 per unit for the gross proceeds of CAD 460,794.96 for the aggregate gross proceeds of up to CAD 5,320,994.96. Duyuru • Apr 23
Trifecta Gold Ltd. announced that it expects to receive CAD 5.31075 million in funding Trifecta Gold Ltd. announced a private placement that it will issue up to 12,790,000 Charity Flow-Through Units at an issue price of CAD 0.38 per unit for the gross proceeds of CAD 4,860,200 and 1,668,704 units at a price of CAD 0.27 per unit for the gross proceeds of CAD 450,550.08 for the aggregate gross proceeds of up to CAD 5,310,750.08 on April 22, 2025. Each Charity Flow-Through Unit will consist of one common share and one-half of a common share purchase warrant. Each Unit Warrant will entitle the holder to purchase one common share at a price of CAD 0.40 for a period of 24 months following the closing of the private placement. Each unit will consist of one common share and one-half of a common share purchase warrant, with each whole warrant to entitle the holder to purchase one common share at a price of CAD 0.40 for a period of 24 months following the closing of the private placement. All of the shares issued pursuant to this private placement, including any shares that may be issued pursuant to the exercise of the warrants, will be subject to a hold period in Canada of four months plus one day from closing. The proceeds from this private placement, which is subject to TSX Venture Exchange acceptance. Certain insiders of company may participate in the private placement. Duyuru • Dec 03
Trifecta Gold Ltd. Reports the Results of A 3D Inversion of Airborne Magnetic and Z-Tipper Electromagnetic Data Collected from the Mt. Hinton Project Trifecta Gold Ltd. reported the results of a 3D inversion of airborne magnetic and Z-Tipper Electromagnetic data collected from the Mt. Hinton Project. Mt. Hinton is located immediately to the southeast of Hecla Mining's Keno Hill Mine and Mill Complex within the Tombstone Gold Belt ("TGB") of central and eastern Yukon. Processing of the geophysical data, which was collected earlier this year, has confirmed a large, strong resistivity anomaly at the GC target where granitic boulders were discovered in 2024. The resistivity feature, which extends along a 3 km axis oriented northwest-southeast, is defined by values in excess of 1235 ohm-m at surface and widening in size at depth. In addition, the resistivity anomaly is spatially associated with a parallel magnetic anomaly. These results are highly suggest of a buried intrusion in the floor of Granite Creek that may be the driver of mineralization in the district. Mt. Hinton hosts four major precious metal rich vein trends developed within the Keno Hill Quartzite Formation. Mid- to Late-Cretaceous granitic stocks of the Tombstone and Mayo suites intrude the quartzite sporadically throughout this portion of the TGB. Other in the belt, Tombstone and Mayo Suite stocks are associated with substantial gold endowments deriving from large arrays of sheeted, sulphide-poor quartz veins hosting native gold. Examples include Snowline Gold Corp.'s Valley deposit, and Sitka Gold Corp.'s RC deposit. Gold mineralization at Mt. Hinton is also thought to be related to this intrusive event, but prior to the 2024 exploration campaign no significant amount of intrusive rock had been identified on the property. Mt. Hinton and Mayo Suite intrusions commonly generate a contact metamorphic aureole of hornfels, where iron in the form of pyrite is converted to pyrrhotite and generates a concomitant magnetic response; however, pyrite isabsent in the Mount Hinton quartzites, and as a result, hornfels mineralogy is expected to be dominated by biotite. The shape and amplitude of the resistivity anomaly at the GC targets is highly suggestive of a buried intrusion, while the magnetic response is comparable to responses derived from other Tombstone and Mayo Suite intrusions that host large gold endowments. Combined with the recent discovery of abundant granitic boulders in the valley floor, the Company now considers the GC target to be a high priority drill target. About Mt. Hinton is a road accessible, camp-scale property with over 60 precious metals veins identified to date. The project is underlain by direct extensions of the stratigraphy that hosts Hecla's Keno Hill Mines and, because of this, much of the historical exploration at Mt. Hinton focused on its silver potential. Surprisingly, historical workers largely overlooked gold potential, despite visible gold that has been found in many of the known veins. There are active placer mines on the creeks draining in all directions from the property. Based on metal zonation within the district, the newly identified GC target may represent a reduced intrusion, theorized to be the driver for much of the mineralization in the district. Tombstone Gold Belt: Extending more than 1000 km from the Fairbanks district in Alaska eastward across the entire width of Yukon, the TGB 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, and the past- producing Brewery Creek Mine, and Yukon. 