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Western Star Resources Announces 100% Acquisition of the Discovery Property
July 11th, 2025 – TheNewswire - Western Star Resources Inc. (CSE: WSR) (the “Company” or “Western Star”) is pleased to announce that it has entered into an agre
About this update from Western Star Resources, Inc.
[{"type":"text","content":"July 11th, 2025 – TheNewswire - Western Star Resources Inc. (CSE: WSR) (the “Company” or “Western Star”) is pleased to announce that it has entered into an agreement (the “Agreement”) to acquire (the “Acquisition”) the Discovery Property (the “Property”) located approximately 50 km southeast Revelstoke British Columbia. The 1942.10 ha Discovery Property is directly adjacent to the 2797.96 ha Western Star Property. Blake Morgan, CEO and President of Western Star, stated “The 100% acquisition of the Discovery Property has increased our flagship Property by 69.4% in size. The historical 2012 AEROTEM survey, clearly shows an extension of the Western Star Property. With this acquisition now signed we can focus on our planned 2025 drill program. With drill permits in place the team is eager to press ahead. The Discovery Property consists of three known showings: The Glenside Showing is of three quartz and galena veins can be traced from Lardeau Creek to a point about 300 metres distant where they unite in one large vein which can be traced for kilometres. At a point about 150 metres below where the three veins unite, a tunnel is in a distance of 24 metres, on the centre small vein. The Muskateer Showing is on the east side of Ferguson Creek, a southerly flowing tributary of Lardeau Creek. The Muskateer Showing have disseminations and large pockets of massive pyrite and pyrrhotite in phyllite. The Muskateer showing is underlain by folded, deformed and schistose rocks of the middle member of the Jowett Formation. The unit contains deformed argillite and limestone, and brown, grey and greenish tuff and volcanic breccia - some of which contains fragments of limestone. The Copper Mountain Showing was discovered in the early 1900s, traces of copper were located in debris below a cliff of chlorite schist, above an alpine glacier near the head of Surprise Creek. By 1912, a 6.7 metres long adit had been driven into the schist at 1844 metres elevation. The Copper Mountain showing is underlain by folded, deformed and schistose rocks of the Index Formation. The Property is underlain by the Badshot Formation that is composed of a thick Cambrian limestone that is a distinctive marker horizon in the Trout Lake area. It is underlain by Hamill Group quartzite, and it is overlain by a younger assemblage of limestone, calcareous, graphitic and si...