Western Star Resources Inc. announced that it has Drill permits in place until July 05, 2026, for the Western Star Property and have paid a $21,000 Bond. Western Star Property. Revelstoke - Mining District, British Columbia.

2,700 ha (27 Km2) - District Scale. 100% Owned and permitted. CRD - Carbonate Replacement Deposit; precious metals rich.

over 6.2 km Mineralized strike length. limited results to date, by surficial prospecting in well exposed areas. 246.76 g/t silver, 1 to 50.1% lead, 8.22 g/t Au, 3.68% Cu - High Grade Samples.

The Western Star Property hosts twelve MINFILE showings: Black Bear, Lardeau-Goldsmith, Hunter, Wide West, Goodenough, Kitsap, Banner, Daffodil, Royal, Morning Star, Lexington, and Alma. The Alma showing consists of intermittent occurrences of massive bands, streak and lenses of galena-sphalerite in crosscutting quartz-carbonate veins within siderite alteration zones. The Kitsap showing along the northwest trending ridge, early prospectors/miners, have pitted and drifted on the Kitsap showing.

Limestone hosting galena-sphalerites mineralization is encountered. Sericite alteration zone of phyllite is approximately 4 m to the west of contact with limestone, and nearly 30 m wide on the eastern contact with limestone. observed, nor anomalous vein hosted.

The Lardeau-Goldsmith showing is reported to have high silver values a 15-metre adit was driven in 1899. It is inferred that mineralization is similar to nearby showings consisting of pyrite, galena and sphalerite. At the Lexington showing a 3.6-metre-wide quartz vein contains 1.5 metres of massive galena in the footwall which assayed high silver values.

Mineralization in a series of occurrences along strike to the southeast consists of intermittent lenses of galena-spherite in crosscutting fractures and quartz-carbonate veins within Siderite or ankerite alteration zones. The Morning Star contains numerous quartz and calcite stringers is a vein 2.1 metres wide striking 310 to 320 degrees, dipping 62 to 75 degrees east. The vein has been traced by numerous open cuts and trenches.

A crosscut adit was begun in 1914 to cut the vein at a vertical depth of 9 metres and reached 21 metres length. Banner Showing is 32-metre adit in 1900 with the object of cutting the vein at depth. Mineralization consists of intermittent lenses of galENA-sphalerite in Crosscutting fractures and quartz-carbonated veins within siderite or ankerite altered zones.

The Black Bear showing consists of massive pyrite with minor galena-sphalerate veins within siderite in quartz gangue. Float in a boulder train is of siliceous pyritic dolomite with disseminated magnetite and traces of galena and Sphalerite. In 1896, a shaft was sunk 3 metres deep.

The mineralization at the Royal showing consists of galena in two parallel quartz veins. Mineralization in a seriesof occurrences along strike to the southeast includes intermittent lenses of galena-Sphalerite in crosscutting fractures, quartz-carbonate veins withinSiderite or ankerite amendment.