Sun Metals Corp. announced additional high-grade drill results from the Stardust project that extend the known plunge length of the 421 zone to 425 metres. The 100% owned Stardust project is located in northcentral British Columbia, 250 kilometers northwest of the city of Prince George. Drill hole DDH20-SD-464D returned 12.14% Copper Equivalent (CuEq) over 4.45 metres (m). This drill hole is a 45m step out from hole DDH20-SD-456M and demonstrates that high-grade mineralization continues up plunge to the south from prior drilling, opening up room for ongoing resource growth. This impressive intersection now extends the plunge length of the 421 zone and indicates that the system is open for further expansion. The drill hole returned: 12.14% CuEq over 4.45m grading 5.58% Copper (Cu), 5.99 grams per tonne (g/t) Gold (Au) and 190.5 g/t Silver (Ag), from 614.25m. DDH20-SD-465 tested a fold hinge target within prospective stratigraphy parallel to and east of the 421 zone. This hole identified a major E-W structure and added to understanding of the stratigraphy. It also intersected a complex of dykes that correlate with East Zone mineralization. Trace amounts of copper-gold mineralization were encountered in the drill hole. DDH20-SD-467 tested a lower extension of the Canyon Creek zone and 421 zone. The drilling intersected strong alteration coupled with anomalous geochemistry associated with the projected extension of the Canyon Creek zone. Deeper in the same hole, a 3.35m interval was intersected from a depth of 775.85m with 1.64% CuEq associated with the 421 zone. This intersection is approximately 150m down dip from the intersection in drillhole DDH20-SD-464D. DDH20-SD-468 tested for a lower extension of the Canyon Creek zone and 421 zone, testing the same horizons as drill hole DDH20-SD-467. It intersected a long interval of lower grade mineralization within the historic Canyon Creek zone, over a 46.85 m core length from a depth of 612.00m averaging 0.47% CuEq associated with chalcopyrite and molybdenite veining in intrusive porphyry and clastic sediments. The top 21.00m of that interval intersected 0.73% CuEq in the Canyon Creek zone and also a 1.75m interval from 633.0m grading 1.88% CuEq. At 759.75m downhole a massive sulphide vein with 10.46% CuEq over 0.35m was intersected within the 421 zone. The massive sulphide vein is approximately 225m away from DDH20-SD-464D and demonstrates good continuity of the system at depth.