Green River Gold Corp. provided the following information regarding exploration activities at its Kymar Silver Project, which is located in southeast BC, approximately 28 kilometers west of the town of Invermere in the Golden Mining Division. The property is made up of nine mineral tenures, totaling 1,626 hectares, along the southeast flank of Mount Catherine.

The primary objective of the 2023 field reconnaissance program is to focus on the Hot Punch Property situated at the head of Delphine Creek. General site descriptions can be found in the Minfile records for the Hot Punch (L.5100), STAR, and OUTLET mines. Geologically, the region is predominantly composed of Proterozoic clastic sedimentary rocks of the Purcell and Windermere supergroups, alongside lower Paleozoic strata of the Beaverfoot and Mount Forster formations.

Green River's project geologist has visited the Star mine, which is part of the Hot Punch underground mine workings (082KSE034), located just up the slope from the mine prospect, as documented in the Minister of Mines Annual Report from 1949. Mineralization in this area is characterized by fissure veins within sheared dolomite. Historical records in 1921 indicate 3 tonnes of ore was extracted, resulting in the production of 4,821 grams of silver and 1,333 kilograms of lead.

The occurrence is primarily represented by a single caved adit. Tyler Tian, the project geologist, journeyed along the Toby Creek trail for 9 kilometers and proceeded to cross Delphine Creek before entering the designated property. During the exploration, he discovered three camps used by historic miners, along with two adits and a vertical shaft.

A steel rail system was observed near one of the adits. This rail system was constructed on the hillside, starting from the entrance of the adit and extending down to the lower access trail. It is likely that the historic miners utilized this rail system to transport ore from the higher adit to the lower creek bank for shipment preparation.

The current access trails remain in favorable condition, although some sections have been overgrown. Within the vicinity of the site, the rocks belonging to the Kitchener and Dutch Creek formations have undergone additional subdivision and have been reassigned as part of the Van Creek and Gateway formations. The Van Creek Formation corresponds to the Lower Kitchener Formation, whereas the Gateway Formation is equivalent to the lower section of the Dutch Creek Formation.

Moreover, the Mount Nelson Formation has been divided into seven distinct members, namely a lower quartzite, a lower dolomite, a middle dolomite, a purple dolomite, an upper middle dolomite, an upper quartzite, and an upper dolomite (Open File 1990-26). The project geologist gathered samples from four distinct types of bedrock exposures. The bedrock consisted of black argillite, dolomite, schist, and quartzite.

Within these bedrock formations, there are sulfide minerals present, such as Sulfide mineralization consisting of galena, sphalerite, tetrahedrite, chalcopyrite, and small amounts of gold were identified in some of the quartzite layers (Figure 4). A total of twelve rock samples were collected and dispatched to the MSA lab located in Langley, British Columbia. The purpose of sending these samples is to undergo a comprehensive analysis, including a 34-element tracing level diagnosis and a fire assaying test specifically designed to detect gold content.

Each rock will be dried, crushed and pulverized to 85% passing 75 micron, then use then four-acid digestion method with ICP-ES finish. Meanwhile, thirty grams of the representative from each sample will be tested by fire assaying method and use an AA finish. Tyler Tian, the project geologist observes that while the historic miner's camp has deteriorated over time, its size is quite remarkable, measuring 10 meters by 10 meters, suggesting it could have accommodated up to 20 miners.

The abandoned adits and shaft also leave a powerful impression, showcasing the significant mining efforts undertaken in the steep terrain. The presence of historical mining activities, coupled with the occurrence of semi-massive sulphide-bearing quartz veins, indicate the property's considerable potential for mineral exploration. Particularly noteworthy is the potential along the local thrust fault leading to the upper hill area.

Once the assaying lab delivers the results of the assays, Green River will proceed with outlining further phases of exploration.