Galway Metals Inc. reported that it has begun drilling on the Oak Bay property that was optioned in July, 2020. Mineralization at Oak Bay and neighbouring Lily Hill consists of arsenopyrite-rich quartz veining in altered, silicified gabbro dykes in contact with sediments, both of which are mineralized - a similar geological setting to the South Zone. The South Zone is located 19 km to the east of Oak Bay and currently hosts the majority of Clarence Stream's gold resource. The zone at Oak Bay has now been drill-delineated with strong consistent intersections over 110m of horizontal distance (strike length). The zone is open in every direction. Most of the assays further down each hole are pending, as are holes 5-8 and 10-13. Highlights for Galway's initial drill program at Oak Bay include: Hole OB-01 intersected 6.0 g/t Au over 3.3m, including 9.3 g/t Au over 1.1m, starting at a vertical depth of 13.8m; Hole OB-02 intersected 2.2 g/t Au over 0.8m, starting at a vertical depth of 18.2m; Hole OB-03 intersected 2.3 g/t Au over 6.65m, including 6.7 g/t Au over 0.6m, starting at a vertical depth of 5.4m; Hole OB-04 intersected 1.6 g/t Au over 4.65m, starting at a vertical depth of 6.2m; Hole OB-09 intersected 3.5 g/t Au over 4.2m, including 8.6 g/t Au over 0.6m, starting at a vertical depth of 31.8m; Hole OB-14 intersected 5.1 g/t Au over 1.15m, starting at vertical depths of 4.2m; Hole OB-15 intersected 4.0 g/t Au over 2.35m, starting at a vertical depth of 3.7m; OB05-07 intersected 5.2 g/t Au over 2.5m, including 11.8 g/t Au over 0.5m, starting at a vertical depth of 13.2m; OB05-03 intersected 1.9 g/t Au over 5.5m, including 8.1 g/t Au over 0.5m, starting at a vertical depth of 50.2m. The 19 km Between Oak Bay and the South Zone is Highly Prospective: Between Oak Bay and the South Zone is a large multi-phase Gabbro Complex. The mineralized gabbro dykes at Oak Bay and the South Zone are thought to have originated from this complex. Galway has not yet drilled the gabbro complex or the 19 km between Oak Bay and the South Zone, except for the 3km trend further north that hosts the Adrian, George Murphy, Richard and Jubilee Zones. The gabbro complex and the area north of it between Oak Bay and the South Zone hosts two of the three highest- grade glacial till anomalies (95 and 86 ppb Au) at Clarence Stream, extensively anomalous gold-in-soil anomalies that extend several km in both NE and NW directions, and boulders and chip samples up to 35.5 and 16.3 g/t Au. Galway plans to follow-up on the initial drill program at Oak Bay, and to drill several of the targets in this highly anomalous 19 km gap, as well as the gabbro complex in 2022. Oak Bay and Lily Hill Host High-Grade Boulders and Chip Samples up to 43.0 g/t Au: The Oak Bay claims are host to widespread boulders with grades up to 18.0 g/t Au, while Lily Hill has chip samples to 43.0 g/t Au. Lily Hill is another optioned property just SE of Oak Bay, containing similar geology; hole LH07-01 (drilled in 2007 by previous operators) intersected 3.7 g/t Au over 3.0m, which has not been followed up since, where a 23.6m Gabbro dyke is entirely mineralized, with the zone in a contact breccia. Strong linear gold soil anomalies at Oak Bay are present grading up to 882 ppb Au, which is in the top 10 of the approximately 50,000 soil samples taken at Clarence Stream, while Lily Hill has soil values to 190 ppb Au. Cordierite alteration is present in the sediments that consist of siltstones and slate. The Sawyer Brook Fault, the main conduit for gold-bearing fluids at Clarence Stream, is located close to the drilling at Oak Bay and Lily Hill. Oak Bay contains a 2km north-south horizontal (strike) length of drill holes with mineralized gabbro along a magnetic high (gabbro is slightly magnetic whereas sediments are not), which continues north 5.0km to the Tower Hill showing that assayed as high as 89.1 g/t along a gabbro-sediment contact. There is a 10 km+ long intrusion flanking the Oak Bay to Tower Hill area to the west; Clarence Stream is thought to be an intrusion-related gold system. All intrusions at Clarence Stream are encircled by one or more of gold-in glacial tills, soils, boulders and/or chip samples, all of which exist along this 10 km+ Oak Bay to Tower Hill trend.