Rokmaster Resources Corp. reported the final assay results from the 2022 prospecting programs on it's 100% owned Revel North Properties, extending more than 40 km NW of Revel Ridge. The Revel North Properties consist of three primary mineral claim groups: The Keystone Property, the Downie Gold Property, and the Rift Property, all located north of the Revel Ridge Project.

Work completed in 2022 on the Revel North Properties included prospecting, soil sampling, and channel sampling and was completed concurrently with the summer drill program on the Revel Ridge Project. The 5,276 hectare Keystone Property covers the majority of the Keystone Anticline, a southwest-verging recumbent folded mass of Index Formation carbonate, clastic, and mafic metavolcanic rocks. The Keystone Anticline occurs in the hangingwall of the possible northwestern extension of the Akolkolex Thrust, the regional structure potentially related to the orogenic gold mineralization on the Revel Ridge Project.

Limited work in 2021 on the Keystone Property found a historical trench hosting arsenopyrite mineralization which returned up to 4.5 g/t Au and up to 274 g/t Ag. The Keystone Property was the subject of early-stage prospecting and soil sampling in 2022. The 2022 field program successfully located, sampled, and upgraded undocumented historical adits and trenches hosting replacement-style Zn-Pb-Ag-Au mineralization across the central area of the Keystone Property.

The 3,175 hectare Downie Gold Property was subject to initial reconnaissance prospecting in where encouraging results led to channel samples being collected from the KJ Zone in 2022. The KJ Zone is characterized by broad exposures of massive pyrrhotite-pyrite-galena mineralization associated with discordant stockwork veins and silicification hosted by limestones. Three of the seven continuous channel samples returned significant assay results which are tabulated below and shown on the Downie Gold Property Map.

The 1,277 hectare Rift Property was staked early in 2022 and hosts the Rift Occurrence and related historical exploration work. The Rift Property benefits from being road-accessible from the paved highway 23 which connects the City of Revelstoke to the Mica Hydroelectric Dam, the latter of which is located only 22 kilometers north of the Rift Property. The Rift Occurrence was discovered in 1980 and consists of a number of layers of massive sphalerite, pyrite, pyrrhotite, and galena with traces of chalcopyrite, arsenopyrite, marcasite and hematite which are exposed for approximately 25 metres of strike length in the incised creek gully of Rift Creek, before being lost under cover.

Grab samples collected in 2022 from a stratabound massive sphalerite-galena layer measuring 1.0 metre in thickness hosted by pelitic schist assayed up to 35.25% Zn, 8.60% Pb. Drillhole M-85-2 was completed in 1985 approximately 460 m east of the Rift Occurrence and intersected 22.21% Zn and 4.82% Pb over 1.82 m and may represent the on-strike continuity of the Rift strataform zinc-lead massive sulphide horizon.