Mr. Bryson Goodwin reports

Stamper Oil & Gas Corp. has successfully completed its 2023 Redonda copper-molybdenum drilling program. Property cleanup and winterization are done, core splitting is completed, samples have been sent into the lab, and Stamper is anticipating results in January. The company's qualified person is on it, compiled data will drop as soon as interpretation is wrapped up.

Comments from president and chief executive officer Bryson Goodwin:

"I am overjoyed to announce the completion of our Redonda work program! No results yet, but visual inspection of the core reveals extensive mineralization, complete with visible molybdenum crystallization. While grades are TBD, well-executed exploration and strategically placed drilling promises tremendous potential! Last explored in 1979, Redonda impressed with impressive results (see below). If history repeats itself, we should have a very pleasant kickoff to 2024! #Redondacopper #2024Prospects."

About Redonda

The project comprises nine claims totalling 2,746.46 hectares and is located 40 kilometres northeast of Campbell River, B.C. Redonda is easily accessed with year-round regularly scheduled barge service out of Campbell River via Marinelink. Access from Redonda Bay is by five km of recent upgraded logging road. Logging is continuing and assures a well-maintained complex of forest service roads across the claims. Work proceeded in 2021 under a letter of support from the Klahoose First Nation within their traditional territory and free use permit, drill permit and IP exemption from the Ministry of Energy, Mines and Low Carbon Innovation (EMLI).

The regional setting 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 dioritic 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-metre-wide hornblende dike which is locally brecciated over its 650-metre exposed length and several smaller feldspar dikes which cut dioritic rocks near the southwest margin of the hornblende dike. Higher concentrations of copper-molybdenum mineralization are closely associated with the hornblende dike, particularly in areas where it has been brecciated. The geological setting of the mineralization 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, PEng, from 1979 was located in good shape and visually confirmed the 1979 intersections noted herein.

The main metallic mineralization observed on the property is pyrite, chalcopyrite, bornite and molybdenite deposited as disseminations and in fractures and small veinlets. Mineralization is located in and close to a younger, large hornblende dike between the quartz and a distance of approximately 350 metres east of the dike. From recent interpretations of drill hole sections the main mineralized zone forms a V-shaped outcrop with the limbs of the V open for additional exploration drill testing. Mineralization grades increase in the northeastern part. The southern and centre of the zone become lower grade in copper and molybdenum and more pyritic. This could be due to mineral zoning as apparent from surface geology and topography. The depth of mineralization is unknown. The zone appears to plunge steeply to the south, although stepout drilling and induced polarization surveying would be required to verify this.

A significant observation made was related to structures referred to as rusty shears that may contain and/or control copper mineralization within the felsic intrusive (quartz diorite) host rocks. The importance of this observation was not apparent until 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 partially replaced mafic minerals, as well as rusty, weathered fractures. Sample 109684 taken from a road cut contained similar chalcopyrite mineralization 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 positive metallurgical implications in future work.

Field measurements were made of rusty shears in outcrops mapped within a 400 m by 400 m area in the southwest quarter of the Redonda GPS grid. The two dominant orientations of rusty shears: north-south striking and steeply dipping; and east-northeast striking and steeply dipping. The north-south-striking orientation is consistent with the interpretation of the overall trend of copper-molybdenum mineralization observed in mapping, trenching and drilling in previous field programs by Highland Mastodon and Teck. The east-northeast-striking orientation is consistent with the photo lineament study at Redonda; as well as the northeast axis connecting Vancouver Island Eocene copper deposits projected by J. Houle, PEng, from Catface through Mount Washington. These suggest that the preferred drilling orientation at Redonda should be designed to intersect these orientations at the greatest possible angles, with holes bearing 110-120 Az and with inclinations of 45 to 55.

The preliminary modelling by J. Houle, PEng, 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 subparallel subzones in a north-northwest-striking orientation, 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 appear to mimic the east-northeast structural and lineament orientation. These suggest that the preferred drilling locations 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.

J.T. (Jo) Shearer, MSc, PGeo, a qualified person within the meaning of National Instrument 43-101 Standards of Disclosure for Minerals Projects, has reviewed and approved the technical and scientific information presented herein as accurate and has approved this news release.

About Stamper Oil & Gas Corp.

Stamper Oil & Gas is an energy-commodity-focused resource company, seeking to acquire interests in mineral and/or oil and gas resource properties focused on energy creation, storage or delivery. The company is committed to creating sustainable shareholder value by evaluating and developing future prospects into commercially viable assets.

We seek Safe Harbor.