The Bald Hill property is known for its high-grade antimony deposits, with past drilling outlining a deposit over 700m long to a depth of 400m, averaging widths of over 3 meters and grades of 3% to 4% antimony.
Over 40 drill holes have been completed on the property since discovery in 2008. The deposit consists of at least three antimony-bearing breccias and hydrothermal veins zones trending northwesterly. Mineralization has been defined over 700 meter strike length to a vertical depth of 400 meters and is open in all directions and to depth.
High Grade antimony has been encountered in drilling including the discovery Hole DDH08-03 which intersect ed 4.51m @ 11.7% Sb including 2.29m grading 20.9% Sb. 2010 Trenching ~ 450 meters south of DDH08-03 returned 2.90% Sb over 8.18m, which included 5.79% Sb over 1.75m and 8.47% over 1.53m.
The Bald Hill Property is subject of a NI43-101 Technical Report by JPL Geoservices dated October 2025. (Reference: NATIONAL INSTRUMENT 43-101 TECHNICAL REPORT: BALD HILL ANTIMONY PROJECT SOUTHERN NEW BRUNSWICK, CANADA NTS 21G/09 Prepared for Antimony Resources October 28, 2025. Prepared By John Langton, M.Sc., P. GEO., - JPL GeoServices, Fredericton, New Brunswick, Canada).
While noting that the report does not describe a resource, that report does present the potential for the Bald Hill Project based on work to that date.
The report Details Potential Quantity and Grade of 2,712,947 Metric Tonnes Range Grading 3% Sb to 4% Sb for 81,000 to 108,000 Metric Tonnes of Contained Antimony in the Main Zone and open in all directions and To depth.
The property is located in Queens County, New Brunswick, with excellent access via provincial and regional highways. Since its discovery in 2008, a total of 40 drill holes have been completed on the property. The deposit consists of at least three antimony-bearing breccias and hydrothermal vein zones trending northwesterly. Mineralization has been defined over a 700-meter strike length to a vertical depth of 400 meters and remains open in all directions


The mineralization encountered is described as consisting of massive antimony-bearing stibnite, veins and stibnite bearing breccia. The breccia contains fragments of the enclosing rocks - metasediments and metavolcanics.
On surface the vein/breccia system strikes NNW and dips vertically to steeply to the southwest. The rock unites in the area strike to the northeast with the situation that the stibnite-bearing structures cut across the surrounding units at a very oblique angle. Mineralization is surrounded by alteration consisting of sericite, quartz and carbonate.
The antimony bearing mineralization has been outlined in surface outcroppings over a distance of at least 300 meters to the southeast beyond the original drilling.
The Company plans to conduct further exploration, including up to 6,000 meters of diamond drilling, to expand the known mineralization and potentially define a mineral resource.
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