Maxus Mining Inc. (“Maxus” or the “Company”) (CSE: MAXM | FRA: R7V), is pleased to announce results from the 2025 exploration program (the “Program”)at the Hurley Project (“Hurley” or the “Property”), located in the prolific Bralorne Mining District in British Columbia (Please see Figure 1). The Company engaged Palliser Exploration (“Palliser”) to complete a reconnaissance field program over both blocks of the Property (Please see Figure 1). The field program was focused on evaluating targets that were generated by the Company after a compilation of all available historical assessment reports.
2025 Hurley Exploration Highlights
- The Program confirmed Antimony mineralization highlighted by 9.33% Sb (H038512; quartz vein in talus) and 0.18% Sb (H038531; outcrop; stibnite-mineralized quartz veins).
- The Program confirmed gold mineralization from quartz veins in outcrop samples, highlighted by 11.60 g/t Au (H038576), 2.20 g/t Au (H038578), and 1.99 g/t Au (H038579),
- Desktop compilation of available assessment reports, combined with the Program results demonstrates polymetallic characteristics that support the district-scale exploration potential of the Property.
“These results from Hurley underscore the strength of Maxus’ diversified exploration strategy in British Columbia,” said Scott Walters, Chief Executive Officer of Maxus Mining, “High-grade antimony and gold mineralization identified at surface, combined with compelling historical datasets, demonstrate the potential importance of Hurley within our antimony-focused portfolio and provide a strong technical foundation for follow-up exploration.”
Figure 1: Hurley Project Claims1
2025 Hurley Project Exploration Program
The Company’s technical team reviewed over ten (10) historic assessment reports covering the Property and compiled the results into a central GIS database. This work highlighted favourable geology and targets for potential mineralization at Hurley and outlined several exploration targets across the Property, as well as pathfinder element anomalies in historic soil datasets (Please see Figure 2).2,3
Following the desktop compilation, the Company initiated a field reconnaissance program to evaluate the generated target areas. During the field program, multiple high-grade gold and antimony occurrences associated with mineralized quartz veins hosted in granodiorite were documented.
Several outcrop samples returned significant gold anomalies from mineralized quartz veins in granodiorite, including 11.60 g/t Au (H038576), 2.20 g/t Au (H038578), and 1.99 g/t Au (H038579). These samples are located proximal to areas of historic gold-in-soil anomalies and within the Hurley East claim block (Please see Figure 2).
Antimony mineralization is highlighted by a peak result returning 9.33% Sb from a mineralized quartz vein in talus material (H038512) that is associated with highly anomalous silver (153 g/t Ag) and elevated copper (349 ppm Cu). In addition, an outcrop sample containing stibnite-mineralized quartz veins (H038531) near the Waterloo area returned 0.18% Sb. These occurrences coincide with regional historic soil anomalies of Sb, Zn, and Pb, and further support a broader polymetallic mineralizing system on the Property (Please see Figure 2).
The Hurley 2025 exploration surface sampling results verify the presence of high-grade gold and antimony mineralization on the Property and support the historical geochemical anomalies.
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