The property lies within the Dawson Range, an unglaciated portion of the Tintina Gold Belt, west of the Big Creek Fault approximately 15 km northwest of the Freegold Mountain Project and 55 km southeast of the Casino copper-gold-molybdenum deposit.

The Prospector Mountain claims cover a high-level porphyry copper-gold system, the core of which is believed to be hosted within the eastern part of the claim block while peripheral epithermal gold-silver-lead vein targets occur within the western part of the property.

The claims are underlain by Late Cretaceous to early Tertiary Carmacks Suite volcanic rocks that have been intruded by early Tertiary monzonite to quartz monzonite and coeval dykes of the Prospector Mountain Suite. All rocks have been cut by northwest to northeast trending structures that are apparent as recessive topographic lineaments.