Roscan Gold Corporation announced the positive drill results at both Kandiole North and Disse. In Kandiole KN1, the continuity of the mineralized gold envelope has been demonstrated and expended laterally with a number of holes intersecting gold mineralization. In addition, high grade with visible gold was encountered in the fresh rock.

The Reverse Circulation ("RC") and core holes drilling programs have improved and expanded the knowledge of the geometry of the gold-bearing zones. At Kandiole KN1, the gold mineralization envelope has been extended 125 metres depth beyond the current pit limit of 150 metres depth with more consistent gold intercepts from these additional holes. The mineralization remains open to the North and South and to the East directions.

At Disse, the high-grade gold extension continues to grow with high-grade intervals in the fresh rock along several distinct mineralized lodes. From the results of the Western RC fence line, gold mineralization has the potential to continue further toward the West. It should be highlighted that neither Disse nor Kandiole North fresh rock gold mineralization are included in the maiden resource estimation.

Drilling Highlights: Kandiole North DD and RC Holes: 7.62 gpt gold over 10m from drill hole DDKan22-008 from 234.5m Including 66.94 gpt gold over 1m from 238.5m; 1.03 gpt gold over 26m from drill hole DDKan22-009 from 316.5 Including 10.59 gpt gold over 1m from 329.5m; 1.75 gpt gold over 20m from drill hole RCKAN22-0039 from 108m Including 25.21 gpt gold over 1m from 119m. Disse RC Holes: 3.04 gpt gold over 12m from drill hole RCDBS22-0100 from 26m Including 12.22 gpt over 1m from 28m Including 15.91 gpt gold over 1m from 36m; And 3.83 gpt gold over 6m from 90m Including 19.12 gpt gold over 1m from 92m; 5.94 gpt gold over 4m from drill hole RCDBS22-0101 from 78m Including 18.57 gpt over 1m from 79m. The KN1 drilling campaign continues to provide very good grades and increases the dimensions and confidence of the mineralized envelope, which should be captured in the upcoming maiden resources.

Kandiole KN1: The gold mineralization at Kandiole North is located approximately 20km east of the Fekola mine (B2Gold Corp.), but also along a prospective NE-SW structural corridor parallel to the main corridor Siribaya-Mankouke-Seko. Gold mineralization in Kandiole North occurs within the metasediments of the Kofi formation. The N020 main mineralized corridor in KN1 is steeply dipping and expanded over more than 1.5 km, punctuated with several artisanal work pits.

There is a secondary perpendicular mineralized strike steeply north dipping and forming the enlargements at North and South of the drilling zone. The broader geochemical Arsenic and Antimony signatures indicate a strong potential to extend the KN1 gold mineralization. The artisanal work intense suggests a mineralization lengthening toward the North and the South of the main drilling area.

The deep saprolite displays a narrow structural feature and interpreted as trans-tension NE-SW quartz veins within a NE-SW shear corridor developing some perpendicular extension veining (enlargement gold envelope). The host rock is clastic sediment from fine grain shale to coarser greywacke strongly weathered and the quartz veining gold bearing system is associated with disseminated pyrite and arsenopyrite. The KN1 gold mineralization trend appears to be in the same regional structure as Moussala (MO1) gold mineralization.

There are still several other auriferous occurrences in the Kandiole North permits to explore, all located in the major Siribaya-Mankouke-Seko regional structure. Disse: Starting close to the surface, this steeply dipping mineralization at Disse has been identified over 200 meters of strike length, on the Roscan permit in prolongation of the resources zone from the neighbor's property. In the East, several mineralized lenses form a wider zone of 50 meters.

At the West, the fence's RC holes carry thin mineralization intercepts in the extension along the same strike as the main mineralization and which could resume extending toward the West. In such a shear structure, the mineralization can have a pinching and swelling feature. Additional drilling is planned and designed to extend the strike length of this high-grade gold occurrence.