Arras Minerals Corp. announced assay results from holes Bg23025, Bg23026 and Bg23027 from the ongoing drill program at the Beskauga copper-gold deposit and surrounding area. A 1 km drill step out from main deposit shows continued mineralization: Holes Bg23025 & Bg23026 were drilled 1 kilometer outside of the main mineral resource at Beskauga and returned 500m+ zones of continuous mineralization.

Bg23026: 570.5 m of mineralization grading 0.27% copper-equivalent ("CuEq") - (0.23 g/t gold ("Au"), 0.08 % copper ("Cu"), 0.42 g/t silver ("Ag")) starting at 29.0 m. · Including: 127.0 m grading 0.57 % CuEq - (0.49 g/t Au, 0.17% Cu, 0.77 g/t Ag) starting at 155.0 m depth down-hole. Bg23025: 504.3 m of mineralization grading 0.19% copper-equivalent ("CuEq") - (0.16 g/t gold ("Au"), 0.06 % copper ("Cu"), 0.34 g/t silver ("Ag")) starting at 31.0 m. · Including: 21.0 m grading 0.77 % CuEq - (0.76 g/t Au, 0.17% Cu, 0.70 g/t Ag) starting at 104.0 m depth down-hole. Including: 69.0 m grading 0.45 % CuEq - (0.39 g/t Au, 0.12% Cu, 0.70 g/t Ag) starting at 420.0 m depth down-hole.

Bg23025: Was strategically positioned aimed to test a cluster of historical KGK drill hole samples that tested the top of the bed rock buried by younger sediments and which contained gold values ranging from 0.32 to 1.18 grams per tonne (g/t) Au. Additionally, it targeted a magnetic anomaly associated with potassic-altered Quartz Monzonite. The drill hole encountered quartz monzonite with sporadic K-feldspar vein alteration, along with intermittent argillic (illite) alteration primarily influenced by fault structures.

Within the quartz monzonite, mineralization consists of quartz-pyrite-chalcopyrite veins, occasionally enriched in molybdenite, particularly at greater depths, and sporadically featuring magnetite. The drilling reached a total depth of 535.3 meters.