Chakana Copper Corp. reported results from two exploration holes drilled in the Estremadoyro breccia pipe and provide an update on drilling in the Mega-Gold target area at the Soledad project, Ancash, Peru. These are the first drill results reported for the southern half of the Soledad project based on a new expanded drill permit that was approved in June 2023 and is part of the ongoing fully funded 3,000 m drill program that started April 5, 2024.

Estremadoyro Breccia Pipe The Estremadoyro breccia pipe is road-accessible and located in the central part of the project at an elevation of 3,860 m within the new drill permit area for the southern half of the Soledad project. The breccia pipe is exposed at the lowest elevation of any breccia tested to date, is strongly mineralized at surface in gold, copper, and silver, and is the closest mapped breccia to the Mega-Gold porphyry target area currently being drilled. Two shallow holes totaling 142.8m were completed to determine the grade of mineralization hosted within the breccia pipe.

Hole SDH24-284 was collared west of the exposed breccia pipe and drilled back to the east, intersecting the breccia at 54.2 m depth and cutting 17.7 m of mineralized breccia. Hole SDH24-285 was collared on the east side of the exposed breccia and drilled steeply to the west. This hole cut 19.45 m of breccia from 14.2 m depth with mineralization extending 2.2 m into the wall rock on the east side, and 1.35 m on the west side.

Chakana's previous drilling on seven breccia pipes on the north half of the project led to an initial inferred resource (see news release dated January 11, 2022) and showed that the breccias are vertically extensive features with additional drilling warranted if the grade profile is considered significant. Based on the mineralized intercepts reported here, additional drilling should be conducted to determine the tonnage potential and grade of this discovery. In addition to the significant grades encountered in drilling, the Estremadoyro breccia has the first identified occurrence of bornite intergrown with chalcopyrite in drilling to date at Soledad.

Bornite has a copper content of 63.3% compared to Chalcopyrite with 34.6%. Another notable difference at Estremadoyro is a low-grade copper halo in the wall rock adjacent to the breccia pipe. Normally the grade drops abruptly at the contact between breccia and wall rock due to the permeability contrast, but in the case of drill hole SDH24-284, a zone of chalcopyrite-pyrite mineralization in wall rock was encountered from 73.00 m to 85.15 m (12.15 m) with a grade of 0.30% copper-equivalent.

This indicates the potential for a greater volume of mineralization surrounding the breccia pipe at depth. Exploration Drill Program Update: Two drill holes have been completed to date at Mega-Gold with the third hole in progress. The Mega-Gold target covers a very large area occupying 2.5 km with anomalous gold and molybdenum in soil overlying pervasive tourmaline-quartz-white mica alteration, overprinted by localized advanced argillic alteration zones and tourmaline breccias.

Within the soil anomaly are distinct Offset (3D) induced polarization chargeability responses. Hole MGDH24-001 was drilled to the northeast to a depth of 353.8 metres. The hole targeted strong soil geochemistry responses up to 0.325 g/t gold and 54 ppm molybdenum.

Both gold and molybdenum are stable in acid oxidizing conditions and useful for drill targeting purposes. The hole also targeted a strong induced polarization chargeability response of >40 millivolts per second, interpreted to indicate the presence of sulfides. Volcanic units of the Calipuy Formation were encountered along the entire extent of the drill hole, consisting predominantly of andesitic tuff, with lessor amounts of porphyritic dacite and volcanic breccia.

The hole is notable for having moderate to intense alteration along its entire length, with deep oxidation to 92 m depth consisting of moderate to intense argillic alteration and up to 70% iron oxides. This alteration is interpreted to be supergene in origin owing to the weathering of a sulfide-rich parent rock. At 113 m depth, moderate to strong quartz-sericite-pyrite alteration occurs and continues to the end of the hole.

Pyrite occurs as disseminations and in association with quartz veins, and quartz- tourmaline veins. Pyrite varies from 3% to 15% to the end of the hole. Molybdenite-pyrite in association with sugary-textured quartz veins occur sporadically from 181 m depth to the end of the hole.

Chalcopyrite-pyrite occurs sporadically in quartz and quartz-tourmaline veins from 228 m depth to the end of the hole. Hole MGDH24-002 was drilled to the south from the same platform as MGDH24-001 to a depth of 453.15 metres. This hole targeted a magnetic body surrounded by strong induced polarization chargeability to the north and south.

The hole cut a similar volcanic rock sequence as MGDH24-001 to a depth of 225.8 where younger granodiorite is in contact with the andesitic tuff. Oxidation from surface to 54.15 m depth is associated with moderate to intense argillic alteration with up to 80% iron oxides. The alteration transitions to quartz-sericite-pyrite beneath the zone of oxidation with pyrite reaching 10% in pyrite veinlets, quartz-pyrite-tourmaline veinlets, and disseminations.

Quartz- pyrite-molybdenite veinlets are noted below 118.8m depth. Tourmaline breccia cuts the andesitic tuff at 167.65 m depth over 9.4 m associated with pyrite and traces of molybdenite. The granodiorite exhibits chlorite alteration overprinted by quartz-sericite-tourmaline-pyrite in veins and zones of replacement with molybdenite and chalcopyrite as disseminations and in quartz-tourmaline veins.

The granodiorite is cut by 105.1 m of tourmaline breccia with highly altered quartz-tourmaline-replaced granodiorite clasts with pyrite and traces of chalcopyrite and molybdenite. Beneath the breccia the granodiorite exhibits zones of strong tourmaline replacement and veining with 0.5-1.0% chalcopyrite in quartz-tourmaline veinlets and disseminations from 399.85-409.05 m depth. Trace chalcopyrite and molybdenite associated with quartz-tourmaline veinlets occurs to the end of the hole.

Hole MGDH24-003 is being drilled from a platform 100 m south of MDGH24-001/002, testing a moderate strength chargeability response adjacent to the same magnetic high. The hole is currently at 137.65 m depth with oxidation to 46.3 m depth and up to 80% iron oxides in argillic alteration. Andesitic tuff occurs from surface to 130.5 m depth, with moderate to strong quartz-sericite- pyrite alteration.

Chalcopyrite is associated with quartz-pyrite-tourmaline veinlets starting at 99.15 m depth and traces of disseminated molybdenite starting at 120.4 m depth. At 130.5 m depth the tuff is cut by a mineralized structure with 70% pyrite and a hydrothermal breccia to the current depth.