Workflow
Epithermal Mineralization
icon
Search documents
Triumph Gold Announces the Acquisition of the Coyote Knoll Silver-Gold Mineral Property - Located in Central Utah
Newsfile· 2025-06-04 08:00
Core Viewpoint - Triumph Gold Corp. has announced the acquisition of the Coyote Knoll Silver-Gold property in central Utah, which is expected to enhance its portfolio due to the property's high-grade mineralization and favorable geological features [1][4]. Acquisition Details - The acquisition cost is $150,000 USD along with the issuance of three million common shares over a period of three years, with an additional payment of three million dollars due before four years from the purchase date [2]. Geological and Mineralization Highlights - Coyote Knoll is located approximately 40 km southwest of the Tintic Mining District, known for its historical significance in mining [10]. - The property has demonstrated high-grade silver mineralization, with drilling results showing 1,350.36 g/t Ag and 3.86 g/t Au over 3.00 meters [6]. - Historical rock samples have returned values up to 6,730.00 g/t Ag and 23.30 g/t Au [6][16]. - Recent surface sampling confirmed mineralization with grab samples returning up to 795 g/t Ag and 1.58 g/t Au [6][20]. Exploration and Historical Context - Coyote Knoll was discovered in 1988, with extensive exploration activities including mapping, trenching, and drilling totaling approximately 2,606.96 meters across 33 drill holes [11]. - The geological setting exhibits similarities to the Tintic Mining District, with potential for both epithermal and carbonate replacement mineralization [19]. - The property has a history of production, including a 12-ton bulk sample in 2012 that returned an average grade of 43.60 oz/ton silver and 0.13 oz/ton gold [6][11]. Future Exploration Plans - The company plans to advance exploration at Coyote Knoll, leveraging the confirmed epithermal silver-gold mineralization and the potential for further discoveries [4].
Headwater Gold Identifies Outcropping High-Grade Veins at its New Doug Target on the Spring Peak Property, Nevada
Thenewswire· 2025-05-28 10:30
Core Viewpoint - Headwater Gold Inc. has identified high-grade epithermal veins at the newly discovered Doug target within its Spring Peak project in Nevada, indicating significant mineral potential in the area [1][4]. Exploration and Discovery - The Doug target is located approximately 9 km north of the Disco Zone and is along the Bear Fault, which is a significant geological structure associated with mineralization [2][11]. - Recent surface exploration has confirmed the presence of outcropping epithermal quartz veins, with notable gold grades of 21.8 g/t, 9.52 g/t, and 7.82 g/t [5][10]. - The Bear Fault corridor is interpreted as a district-scale structure that may host multiple significant mineralized zones, with Headwater controlling over 12 km of strike extent in this area [4][12]. Geological Insights - The vein textures and geochemistry at the Doug target suggest a high-level position within an epithermal system, indicating the potential for preserved high-grade vein targets at depth [5][7]. - Geological mapping is ongoing to understand the relationship between the stockwork zone and major mineralized structures, including the Bear Fault and Aurora Mine vein corridor [11]. Project Expansion - Headwater has expanded its land position by staking 509 new mining claims, bringing the total to over 15 km of continuous strike length along the Bodie–Aurora–Borealis trend, which has historically produced over 4 million ounces of gold [12][13]. - The Spring Peak project is strategically located near existing infrastructure, including a mill and production water wells, enhancing its exploration potential [13]. Future Plans - A systematic program of geological mapping and geochemical sampling is underway, alongside the interpretation of recent geophysical survey results to guide further exploration [13][14].