# Galway Metals Intersects Thick Gold-Antimony Mineralization at South Deposit, Including 6.1 g/t Au and 0.7% Sb Over 28.0m *2026-03-31T07:00:00-04:00* Galway Metals Intersects Thick Gold-Antimony Mineralization at South Deposit, Including 6.1 g/t Au and 0.7% Sb Over 28.0m **TORONTO, ON / [ACCESS Newswire](https://www.accessnewswire.com/)/ March 31, 2026 / **Galway Metals Inc. (TSX-V:GWM)(OTCQB:GAYMF) (the "Company" or "Galway")is pleased to report assay results from nine diamond drill holes at the South Deposit within its 100%-owned Clarence Stream high-grade gold project in New Brunswick, Canada. The Clarence Stream Gold Project hosts district-scale potential along an approximately 65-kilometre trend of highly prospective gold showings and anomalies. The Project currently hosts a 2022 Mineral Resource Estimate of 12.4 Mt grading 2.3 g/t Au in the Indicated category (922,000 oz Au) and 16.0 Mt grading 2.6 g/t Au in the Inferred category (1.334 million oz Au), as outlined in the NI 43-101 technical report titled "[Technical Report on the Clarence Stream Mineral Resource Project, New Brunswick, Canada](https://pr.report/k8sc)" dated March 31, 2022, prepared by SLR Consulting Ltd. Rob Hinchcliffe, President and CEO of Galway Metals stated _"We are very encouraged by these initial results from our 2026 drilling program at the South Deposit, which continue to demonstrate strong continuity of thick, high-grade gold mineralization with meaningful antimony values. These intercepts reinforce the robustness of the system within the core of the deposit and highlight the growing importance of antimony as a potential by-product. With an updated Mineral Resource Estimate currently underway for Clarence Stream, and exploration drilling now ramping up with the addition of a fourth rig, we are entering a highly productive phase of drilling. With active drilling on multiple deposits and a large volume of assays pending, we believe the Project is well positioned to deliver consistent news flow and continued advancement throughout 2026."_ **Highlights**([_Plan Map_](https://pr.report/k8sr)) - CS-416 Intersected **6.1 g/t Au and 0.7% Sb over 28.0m, including:** - **21.8 g/t Au and 3.3% Sb over 1.0m** - **40.7 g/t Au and 0.7% Sb over 1.0m** - **22.6 g/t Au and 0.7% Sb over 1.0m** - CS-417 Intersected **3.6 g/t Au and 0.4% Sb over 26.0m, including:** - **12.4 g/t Au and 0.5% Sb over 5.0m** - CS-424: 1.5g/t Au and 0.4% Sb over 3.0m **Thick, High-Grade Gold-Antimony Zones Intersected Within South Deposit Pit Shell** The nine drill holes reported represent the first results from the 2026 drill program at the South Deposit, which hosts the highest-grade resource within the 2022 Mineral Resource Estimate, comprising 333,000 ounces at 2.99 g/t Au (Indicated) and 325,000 ounces at 4.03 g/t Au (Inferred). Drill holes CS-416 and CS-417 were designed as approximately 25-metre spaced infill holes targeting the central portion of the South Deposit to confirm continuity of higher-grade mineralization within the resource pit shell. Both holes intersected thick zones of gold and antimony mineralization, reinforcing the continuity and strength of the mineralization (_see _[_Section 1_](https://pr.report/k8ss)). The remaining seven holes tested both internal grade continuity and mineralization along the pit shell boundaries. All holes intersected gold mineralization with varying levels of antimony. Additional assays remain pending for holes CS-422 and CS-423. The Company currently has assays pending for 8 additional drill holes from the South Deposit, along with 37 holes from the Southwest Deposit and 34 holes from the North Deposit. Several holes from both the Southwest and North Deposits contain visible gold, including hole CL-252 ([_photo_](https://pr.report/k8st)) and hole ND-61 ([photo](https://pr.report/k8su)), and results will be released as assays are received. For a complete list of South Deposit assays reported in this press release, please refer to the [_Assay and Coordinate Table_.](https://pr.report/k8sv) **Geology and Mineralization** Gold-antimony mineralization at Clarence Stream is structurally controlled and associated with quartz veins and quartz stockwork developed within brittle-ductile fault zones hosted in both intrusive and metasedimentary rocks. Mineralization is associated with pyrite, base-metal sulphides, and stibnite, along with anomalous concentrations of bismuth, arsenic, antimony, and tungsten. Alteration within host rocks is typically confined to a few metres surrounding quartz veins and is characterized primarily by sericitization and chloritization. A more detailed description of the Clarence Stream geology and mineralization is available at [www.galwaymetalsinc.com](https://pr.report/k8sl). **Review by Qualified Person** The scientific and technical information contained in this news release has been reviewed and approved by Jesse Fisher, P.Geo., Project Manager for Clarence Stream and a Qualified Person as de