Copper Fox Metals Inc. and its wholly owned subsidiary, Desert Fox Mineral Mountain Co. announced the results of the deep penetrating geophysical survey utilizing Quantec's ORION 3D Swath DCIP configuration on its 100% owned Mineral Mountain project located approximately 16 miles northeast of Florence, Arizona. Highlights of the survey are set out below: A northeast trending open-ended positive (>18mrad) chargeability/resistivity anomaly measuring approximately 3,200 meters (m') long by 1,200 m wide has been identified.

The chargeability/resistivity signature is like that which would be expected in the oxidized/supergene zone above the hypogene zone of a porphyry copper system in Arizona. A 1,200 m long by 900 m wide portion of the larger chargeability/resistivity anomaly comes to surface in an area of the property with quartz vein/veinlet/fracture hosted secondary copper (chrysocolla, malachite, chalcocite) and molybdenum mineralization in sericitic/potassic altered porphyritic quartz monzonite and granodiorite. An additional 80 mineral claims (1,653 acres) have been added to the Project to cover the interpreted extension of the northeast trending open-ended positive chargeability/resistivity anomaly and a mineralized Laramide intrusive.

The porphyry copper footprint at Mineral Mountain is located on the eastern side of the Laramide intrusive and is interpreted to dip to the east and to the north under the PreCambrian rocks consistent with the location of the recently defined chargeability signature. Geophysical Study. Recent investigation of the geophysical characteristics of porphyry copper systems in Arizona shows that the oxidation/supergene processes that affected these porphyry copper systems have altered the petrophysical properties of the mineralization and host rock resulting in lower chargeability and increased resistivity signatures within the oxidation/supergene zone of porphyry copper deposits.

The 2023 geophysical survey has outlined a northeast trending open-ended 3,200 m long by 1,200 mwide chargeability (+18mrad contour) anomaly. Based on the +15mrad chargeability contour, the western, southern, and southeast edges of the anomaly have been defined. The anomaly remains open to the northeast.

The 1,200 m long by900 m wide chargeability/resistivity signature that comes to surface in an area the property that contains abundant mineralized porphyry style quartz veins/veinlets and fractures containing secondary (chrysocolla, Malachite, chalcOCite) copper and molybdenum Mineralization hosted primarily in sericitic and to a lesser degree potassic altered phases of the Laramide age intrusive. The lower chargeability/increased resistivity signature is similar to the recent geophysical model of Laramide age porphyry copper deposits in Arizona. The chargeability and resistivity pseudo sections for L-2000 that crosses the 1,200 m by 900 m chargeability/resistivity anomaly.

The strength of the chargeability signature increases with depth and is interpreted to represent the primary hypogene sulphide zone of a porphyry system. Rationalational Model. The Mineral Mountain project covers a copper-gold-molybdenum porphyry system characterized by a copper-magnetite mineral association that has been subjected to weathering/oxidization/supergene enrichment, a process commonly observed at porphyry copper systems in Arizona.

The 2023 geophysical model for Porphyry copper deposits in the Laramide Copper Province. The 2023 geophysical study has outlined a northeast trending open - 3,200 m long by1,200 m wide chargeability (+18m rad contour) anomaly. Based On the +15mrad chargeable contour, the western, south, and southeast edges of the anomalies have been defined.

The anomaly remain open to the northeast. The anomalies remains open to the northeast.