Copper Fox Metals Inc. and its wholly owned subsidiary, Desert Fox Copper Inc., are provided a compilation for the recently completed mapping and sampling program on its 100% owned Mineral Mountain copper project located approximately 15 miles east of Florence, Arizona. The updated geological model includes two distinct porphyry targets. Area #1 is underlain by Laramide age Quartz Monzonite and is interpreted to represent the oxidized portion of a porphyry copper-molybdenum deposit as indicated by the zones of disseminated copper-molybdenum mineralization and the positive chargeability anomaly outlined in 1971. The largest zone of disseminated copper mineralization containing the highest concentrations of molybdenum occurs at the intersection of a broad north-northwest trending zone that exhibits late stage re-adjustments by north-south and east-northeast trending structures. Outcrop in Area #2 consists of Precambrian age Pinal Schist, Diabase and Ruin Granite that is interpreted to be underlain by Laramide age Quartz Monzonite. The styles of copper mineralization and low molybdenum concentrations suggest that the source porphyry system is at a deeper level than that seen in Area #1. In November 1971, Marguerite Lake Mines Ltd. under the supervision of Fred. J. Syberg, B.Sc. completed an Induced Polarization and Resistivity survey (six lines) with line spacing of 1,000 feet (ft) (304m), electrode spacing of 800ft (243m), and estimated depth of penetration of 1,600ft (487m) using a dipole-dipole configuration. Based on the results of the geophysical survey, Syberg concluded that the survey identified a chargeability anomaly measuring approximately 6,000ft (1,800m) long by approximately 3,000ft (900m) wide. Area #1 is characterized by disseminated, quartz vein and fracture hosted styles of copper mineralization. Disseminated copper mineralization occurs as three separate northeast trending zones within Area #1 and range in size from 400m by 200m to 1,000m by 345-450m. Both Quartz Vein and Fracture controlled copper mineralization occurs within the zones of disseminated copper mineralization. Molybdenum mineralization (defined as greater than 20 ppm) occurs in three zones within Area #1 that range in size from 800m by 200m to 1,400m by 400-800m and overlaps the disseminated copper mineralization. The Quartz Vein style of copper mineralization contains significant molybdenum concentrations and can exhibit a number of different strike and dip directions over narrow intervals. This style of mineralization exhibits a dominant northeast strike direction and a secondary northwest strike direction. Fracture controlled (1-5 millimeters wide) mineralization is dominantly copper. A number of outcrops exhibit fracture controlled chalcocite mineralization where fractures up to 7 centimeters wide have been observed. This style of mineralization exhibits a dominant northeast and secondary northwest trend with similar dip directions. Fracture density is variable but in specific outcrops, fracture spacing of 1-2 centimeters has been observed. Area #2 consists of Quartz Vein and Fracture controlled copper mineralization hosted in Precambrian Pinal Schist, Diabase and the Ruin Granite that contains significantly lower concentration of molybdenum and variable concentrations of gold and silver. The strike and dip directions for these styles of copper mineralization are similar to that observed in Area #1.