Stamper Oil & Gas Corp. announced 2023 Redonda Copper Molybdenum drilling program is a successfully complete. Property cleanup and winteriza0on is done, Core Spli2ng completed, Samples into the Lab, and antcipating results in January.

The project comprises 9 claims totalling 2746.46ha and is located 40km northeast of Campbell River, BC. Redonda is easily accessed with year-round regularly scheduled barge service out of Campbell River via Marinelink. Access from Redonda Bay is by 5km of recent upgraded logging road.

Logging is ongoing and assures a well maintained complex of forest service roads across the claims. Work proceeded in 2021 under a Le/er of Support from the Klahoose First Na0on within their Tradi0onal Territory and Free Use Permit, Drill Permit and IP Exemp0on from the Ministry of Energy, Mines and Low Carbon Innova0on (EMLI). The regional se2ng of the Redonda property is part of the Coast Suture Zone between the Wrangellia Terrane and the Coast Plutonic Complex. In the claims area, Early Cretaceous diori0c intrusive rocks of the Coast Plutonic Complex have been intruded by at least three later intrusive units, including a quartz plug, a 60 to 90 meter wide hornblende dike which is locally brecciated over its 650 meter exposed length and several smaller feldspar dikes which cut diori0c rocks near the southwest margin of the hornblende dike.

Higher concentra0ons of copper-molybdenum mineraliza0on are closely associated with the hornblende dike, par0cularly in areas where it has been brecciated. The geological se2ng of the mineraliza0on on the Redonda mineral claims share a number of features similar to those observed at the OK Over copper- molybdenum porphyry deposit located 34 km to the southeast, north of Powell River and the Gambier Copper deposit in Howe Sound. Previous drill core by Teck Corp, supervised by A. Betmanis, P.Eng., from 1979 was located in good shape and visually confirmed the following 1979 intersec0ons: The main metallic mineraliza0on observed on the property is pyrite, chalcopyrite, bornite and molybdenite deposited as dissemina0ons and in fractures and small veinlets.

Mineraliza0on is located in and close to a younger, large hornblende dyke between the quartz and a distance of approximately 350 metres east of the dyke. From recent interpreta0ons of drill hole sec0ons the main mineralized zone forms a V-shaped outcrop with the limbs of the V open for addi0onal explora0on drill tes0ng. Mineraliza0on grades increase in the northeastern part.

The southern and centre of the zone becomes lower grade in copper and molybdenum and more pyri0c. This could be due to mineral zoning as apparent from surface geology and topography. The depth of mineraliza0on is unknown.

The zone appears to plunge steeply to the south, although step-out drilling, and IP surveying would be required to verify this. A significant observa0on made was related to structures referred to as "rusty shears" that may contain and/or control copper mineraliza0on within the felsic intrusive (quartz diorite) host rocks. The importance of this observa0on was not apparent un0l the reference rock samples were saw cut and observed macroscopically.

All quartz diorite rock samples displayed rust-rimmed, feathery and fine-grained chalcopyrite which had par0ally replaced mafic minerals, as well as rusty, weathered fractures. Sample 109684 taken from a road cut contained similar chalcopyrite mineraliza0on but also contained a thin seam of massive chalcopyrite in a fracture within quartz diorite. This suggests that at least some of the rusty seams mapped in outcrops may have contained similar chalcopyrite seams prior to surface weathering.

This feature may have posi0ve metallurgical implica0ons in future work. Field measurements were made of rusty shears in outcrops mapped within a 400 m. x 400 m. area in the southwest quarter of the Redonda GPS grid. The two dominant orienta0ons of rusty shears: N-S striking and steeply-dipping; and E-NE striking and steeply-dipping.

The N-S striking orienta0on is consistent with the interpreta0on of the overall trend of copper-molybdenum mineraliza0on observed in mapping, renching and drilling in previous field programs by Highland Mastodon and Teck. The E-NE striking orienta0on is consistent with the photo lineament study at Redonda; as well as the NE Axis connec0ng Vancouver Island Eocene copper deposits projected by J. Houle, P.Eng from CaMace through Mount Washington. These suggest that the preferred drilling orienta0on at Redonda should be designed to intersect these orienta0ons at the greatest possible angles, with holes bearing 110-120 Az and with inclina0ons of 45-55.

The preliminary modeling by J. Houle, P.Eng of historic trenching and drilling assays suggests that intercepts of increased copper and molybdenum values occur within a 250 m. thick zone or series of sub- parallel sub-zones in a N-NW striking orienta0on, which dip steeply to the west, and plunge gently to the south. This is consistent with elevated soil geochemistry values which appear to be open to the north and terminate to the south. Contoured copper and molybdenum soil geochemistry data also appears to mimic the E-NE structural and lineament orienta0on.

These suggest that the preferred drilling loca0ons at Redonda should be designed using long holes (500 m.) to test the area immediately south and down- plunge of the previous trenching and drilling.