Triumph Gold Corp. announced results from 896.72 metres of diamond drilling in 3 holes from the Blue Sky Zone(?BSZ?) within the Revenue Deposit at the Freegold Mountain Project (Figure 1), highlighted by 106.50 metres (?m?) of 0.76 grams per ton (?g/t?) gold equivalent1 (?AuEq?) in RVD21-05. The Blue Sky Zone is defined by 12 drill holes: three holes from the 2021 program (Table 1) and nine historical holes. The Blue Sky Zone is a NE-striking, near vertical body of Au-Cu-Ag-Mo mineralization that remains open at depth. The Revenue Deposit is made up of the Blue Sky Zone, WAu Zone, and zones of Cu-Mo-Au porphyry-style mineralization. The Blue Sky Zonehas been expanded 100 metres westwards and towards the surface with a modeled strike length of 210 metres. The zone has an average width of 70 metres and a depth of 480 metres below surface. The 2021 drilling program expanded both the Blue Sky Zone and the WAu Zone and reduced the gap between the two zones to 65 metres. 46% of the 6,615 metres of the 2021 diamond drilling program have been reported to date (PR#21-11). Further updates will be provided when the results for the remainder of the 2021 exploration program are received and interpreted from the Nucleus Deposit, Big Creek South Fault Zone, the Orbit Zone, and regional exploration activities. Detailed Interpretation and Geology; RVD21-05 intercepted the Blue Sky Zone and returned 106.50 metres of 0.76 g/t AuEq from 120.00 metres. This intercept is located 60 metres southwest of RVD18-16, which had an intercept of 110.42 metres grading 1.86 g/t AuEq (PR#18-08). The 2021 program expanded the Blue Sky Zone 100 metres westwards and towards the surface. The updated expression of the Blue Sky Zone is now modeled to be 65 metres from the WAu Zone, suggesting the two zones may be linked in a NE orientation. Mineralization at the Blue Sky Zone is hosted within hydrothermally-altered granodiorite and contains two overlapping mineralization events:; The first and most abundant mineralization event is associated with strong potassic alteration with K-feldspar grading outwards into biotite, suggesting a high-temperature porphyry zone. Sulphide mineralization (chalcopyrite, molybdenite, pyrite and pyrrhotite) is characterized by clots, veinlets, and disseminations. The second phase of mineralization is hosted by epithermal quartz-calcite veins with mineralization of chalcopyrite, molybdenite, galena, sphalerite +/- bismuthinite and visible gold, representing metal enrichment. Porphyry-style mineralization was intercepted south of the modeled Blue Sky Zone. Porphyry-style mineralization consists of local sulphide +/- quartz stockwork veining with broad zones of disseminated sulphide mineralization surrounding vein clusters and local fine grained native gold.