The Everton Project, located in Northeast Victoria near Wangaratta, is a high-priority exploration opportunity centered on a classic porphyry molybdenum (+/- copper) system. Positioned just south of the prolific Lachlan Fold Belt, the project is anchored by the historical Everton Molybdenum Mine, that operated intermittently from 1917 to 1944, producing around 325 tons of molybdenum (averaging 1.4% MoS₂) from two pipe-like ore bodies mined to shallow depths of about 45 meters.

Recent geological reinterpretation has identified the old mine area as the top of an undrilled porphyry system, with Unidirectional Solidification Textures (USTs) and widespread disseminated molybdenite pointing to a classic molybdenum (+/- copper) porphyry cupola target (“pencil porphyry”) with ready-to-drill prospects that were previously overlooked in earlier exploration.

Geologically, the Everton deposit sits within the Tabberabbera Zone of the Lachlan Fold Belt and is hosted by the Early Devonian Everton Granodiorite, a porphyritic intrusion emplaced into slate and sandstone country rocks. The deposit represents a characteristic porphyry-style system associated with highly fractionated and oxidised I-type granitic intrusions, where molybdenite occurs in disseminations, joints, veins, and distinctive pipe-like bodies formed during late magmatic hydrothermal activity. The Tabberabbera Zone is part of the broader Lachlan Fold Belt, one of Australia’s premier mineral provinces. The recognition of Everton as a porphyry system rather than just a shallow vein deposit fundamentally changes the exploration model and potential, especially given that molybdenum was designated a critical mineral by Australia in December 2023, reflecting growing global demand for this strategically important metal.