Stellar AfricaGold Intersects Multiple Gold-Bearing Zones and Confirms Structural Controls at Tichka Est, Morocco - Drilling Resumed on January 30, 2026 (TheNewswire) Vancouver, BC – TheNewswire - February 3rd, 2026 – Stellar AfricaGold Inc. (“Stellar” or the “Company”) (TSX-V: SPX | FSE: 6YP | TGAT: 6YP) is pleased to report additional assay results and an updated interpretation from its ongoing diamond drilling program at the Tichka Est Gold Project, located in the High Atlas Mountains of Morocco. Results received to date confirm the presence of a structurally controlled orogenic gold system, with gold mineralization preferentially hosted within fractured diorite sills and associated carbonate-altered zones linked to secondary shear structures. These results materially advance the Company’s geological understanding of the project and provide a clear framework for follow-up drilling. Assay results for two completed drill holes remain pending and will be released once received and validated. Following a temporary interruption due to unusually severe winter weather, diamond drilling resumed on January 30th, 2026, with at least two additional drill holes planned. Highlights – Diamond Drilling Multiple gold-bearing zones intersected across several drill holes, confirming the presence and continuity of mineralization beyond the initial discovery hole TCK_001 Best new intercept : TCK_006: 6.0m @ 3.81g/t Au from 69 m, highlights the development of higher-grade mineralization within stacked horizons Results support a refined structural model, with gold preferentially concentrated in competent host rocks affected by secondary shearing Drilling resumed on January 30th, 2026, targeting extensions of known mineralization and additional near-surface targets identified through mapping and trenching Gold intercepts from drill hole TCK_001, including 13.0m @ 6.12g/t Au at 0.1g/t Cut-off grade, were reported previously (see Company news release dated January 8, 2026). Updated Composite Drill Intercepts (0.20g/t Au Cut-off) The Company has recalculated composite gold intersections for all drill holes completed to date using a 0.20g/t Au cut-off, a maximum internal dilution of 3.0 metres, and excluding dilution at interval boundaries. This compositing approach better reflects the continuity of mineralization observed within fractured diorite and carbonate-altered zones. Table 1 below summarizes positive composite intercepts (0.2 g/t Au cut-off) from all drill holes completed to date. Table – Summary of Gold Intercepts using 0.2 g/t Au cut-off Hole ID From (m) To (m) Interval (m) Au (g/t) TCK_001 76.0 79.0 3.0 0.47 83.0 87.0 4.0 1.07 89.0 90.0 1.0 0.25 93.0 99.0 6.0 3.48 125.0 137.0 12.0 6.62 TCK_002 73.0 74.0 1.0 0.87 79.0 80.0 1.0 0.35 TCK_003 179.0 182.0 3.0 0.22 104.0 205.0 1.0 0.23 207.0 209.0 2.0 0.22 TCK_004 79.0 80.0 1.0 0.96 85.0 86.0 1.0 0.23 89.0 103.0 4.0 2.45 120.0 121.0 1.0 1.06 TCK_006 0.0 3.0 3.0 0.6 35.0 48.0 13.0 0.5 55.0 57.0 2.0 0.51 69.0 75.0 6.0 3.81 87.0 90.0 3.0 0.47 Notes: Intervals are downhole lengths; true widths are not yet known. Grades are uncut, length-weighted averages. Composite intervals were calculated using a 0.20g/t Au cut-off with a maximum internal dilution of 3.0metres; dilution at interval boundaries is excluded. Geological Interpretation Drilling completed to date indicates that gold mineralization at Tichka Est is preferentially localized within competent lithologies, notably fractured diorite sills and adjacent carbonate units affected by secondary shear structures (cf. TCK_001 and TCK_006). Click Image To View Full Size Figure 1. Cross section of drillhole TCK_001 showing drillhole geology and gold assays. Figure 2. Cross section of drillhole TCK_006 showing drillhole geology and gold assays. Drill hole TCK_003 intersected the Tizgui Shear Zone, characterized by intense brecciation and pervasive calcite veining, but returned limited gold values. This is interpreted to reflect efficient fluid transport along major regional structures, with gold deposition occurring preferentially in zones of elevated fracture density within rigid host rocks rather than within the shear zones themselves. Click Image To View Full Size Figure 3. Cross sections of drillholes TCK_003 showing drillhole geology and gold assays. Drilling and surface observations further indicate that the mineralized diorite bodies occur predominantly as sub-horizontal sills. This geometry promotes the development of laterally extensive fracture networks within competent rocks, enhancing fluid–rock interaction and gold precipitation, particularly where these sills are intersected by secondary shear structures. Overall, this interpretation is consistent with an orogenic gold system and refines the Company’s exploration model by delineating high-priority structural–lithological traps. Next Steps Now that drilling has resumed, the Company plans to : Continue two additional holes on the secondary shear structures interpreted to