New Risk • Apr 14
New minor risk - Share price stability The company's share price has been volatile over the past 3 months. It is more volatile than 75% of Canadian stocks, typically moving 15% a week. This is considered a minor risk. Share price volatility indicates the stock is highly sensitive to market conditions or economic conditions rather than being sensitive to its own business performance, which may also be inconsistent. It also increases the risk of potential losses in the short term as the stock tends to have larger drops in price more frequently than other stocks. Currently, the following risks have been identified for the company: Major Risks Less than 1 year of cash runway based on free cash flow trend (-CA$453k free cash flow). Earnings have declined by 9.1% per year over the past 5 years. Revenue is less than US$1m. Market cap is less than US$10m (CA$6.88m market cap, or US$5.00m). Minor Risk Share price has been volatile over the past 3 months (15% average weekly change). Announcement • Sep 17
Gold Finder Resources Ltd., Annual General Meeting, Nov 14, 2025 Gold Finder Resources Ltd., Annual General Meeting, Nov 14, 2025. Location: british columbia, victoria Canada Announcement • Jun 20
Gold Finder Resources Ltd. Announces That Fieldwork Is Underway At Its 100%-Owned Pipestone Bay Property Gold Finder Resources Ltd. announced that fieldwork is underway at its 100%-owned Pipestone Bay property (the "Property") located approximately 32 kilometres west of the town of Red Lake. Emerald Geological Services conducted a review of all historical exploration on the Property to determine areas where untested targets warrant further exploration. Significant historical work has been conducted in two areas of the Property: the 991 Zone (also known as the NW Pipestone Bay Occurrence) in the eastern part of the Property, and the western part of the Property where there are two known gold occurrences (McIntosh Lake Iron Formation and Stupak-Dynes Group Occurrences). The 991 Zone Previous work has shown that there are at least two styles of gold mineralization at the 991 Zone: 1) High-grade (up to 44.9 g/t Au) hosted in roughly N-S striking quartz veins. 2) Low-grade (in the low 100s of ppb) hosted in altered felsic volcanics which strike roughly east- west and dip north, with a copper association (including 0.23% Cu over 5.5 meters in drilling). To date, only the low-grade gold mineralization has been tested by north-south drilling, which would not have adequately tested the north-south high-grade veins. The mineralized felsic unit hosting the veins remains open to the west-northwest and east-southeast beneath the lake, and IP suggests that mineralization may continue in either direction. There is also potential for nickel and chromium mineralization in the ultramafic unit to the north, as indicated by 2019 grab samples which returned 0.21% Ni and 0.21% Cr. This area hosts both gold and copper mineralization. Anomalous gold (up to 730 ppb) has been discovered in banded iron formation, altered mafic volcanics, and quartz veins, with copper grades up to 3.25% also obtained in altered mafic volcanics. The 2020 airborne magnetic survey suggests that the banded iron formations are strongly folded, with the most prospective area to date being the southwest limb of the fold close to a mafic/intermediate volcanicfelsic volcanic contact. Folded banded iron formations are excellent targets for gold exploration, as they represent structural and chemical traps for gold- bearing fluids. The mafic-felsic volcanic contact may also be an important conduit for gold-bearing fluids. From past records, anomalous gold mineralization has been obtained over a trend of approximately 1 kilometre near this contact. 
