Vanadium prospectivity
across Australia, the USA, Canada & worldwide.
Mafic-intrusion titanomagnetite and sediment-hosted vanadium, ranked and explained — validated across Australia, the United States and Canada.
Run vanadium on your ground →
Where you can run vanadium.
A certified national model in the countries ticked below — and anywhere else in the world through our global model.
Outside the certified countries, a run returns the prospectivity map, the geology behind it and a per-cell confidence read — how the global model works →
What the model reads for vanadium.
Every vanadium target is scored against the full national evidence stack — mapped geology and rock age, gravity and magnetics, radiometrics, terrain, satellite radar and alteration — the way a geologist reads a map sheet, with a pathfinder-geochemistry signature tuned to this system.
Pathfinder geochemistry the model weighs
Lead signal: Chromium, nickel and cobalt. These are the elements this national model actually reads to rank vanadium ground.
What is vanadium?
Vanadium is a hard, silvery-grey transition metal prized for the strength, toughness and heat resistance it lends to steel and speciality alloys. It seldom forms minerals of its own; instead it substitutes into iron- and titanium-bearing phases, and its principal ore is vanadiferous titanomagnetite — magnetite in which vanadium replaces iron. Secondary vanadate minerals such as vanadinite, descloizite and the uranium-bearing carnotite form in oxidised and sediment-hosted settings. MineDSS models vanadium through two seeded deposit families: mafic-intrusion titanomagnetite systems and sediment-hosted systems. Each leaves a mappable footprint — layered mafic rocks or reduced, metal-rich sediments, characteristic geophysical responses and a distinctive multi-element geochemical halo — which is exactly the pattern a prospectivity model is built to read across large, partly covered terrains.
The deposit model
The two seeded systems form by very different processes. Mafic-intrusion titanomagnetite deposits crystallise from large layered mafic-ultramafic intrusions, where iron-, titanium- and vanadium-rich oxides settle and concentrate into magnetite-rich layers as the magma cools and differentiates; the vanadium is locked inside titanomagnetite rather than in a mineral of its own, and the same intrusions commonly carry chromite, nickel and cobalt. Sediment-hosted deposits form at low temperature, where vanadium that is soluble in oxidising groundwater is fixed in reduced, organic- or sulphide-rich sediments and sandstones, often together with uranium in minerals such as carnotite and roscoelite. MineDSS reads these settings by combining mapped mafic and sedimentary geology and structure, geophysics that resolves dense magnetite-rich bodies and basin architecture, satellite-mapped alteration and weathering, and the pathfinder geochemistry that trails each system, ranking ground by its similarity to known mineralised systems.
Why it matters
Vanadium is a strategic industrial metal and appears on critical-minerals lists in the United States, the European Union and other economies, because both its established steel role and its emerging energy-storage role bear on economic security. World supply is geographically concentrated in a handful of producing countries and is largely recovered as a co-product of iron and steel making, which leaves consuming nations exposed to disruption. Vanadium redox flow batteries add a fast-growing, energy-transition dimension to demand, since they store grid-scale renewable power for hours to days with long service life. Domestic primary production is limited and import reliance is high, so transparent, defensible targeting of prospective ground carries real weight for both explorers and the governments that permit them.
Where it's used
The dominant use of vanadium — around nine-tenths of consumption — is as a metallurgical alloying agent. Small additions of ferrovanadium sharply raise the strength, toughness and hardenability of steel, making it essential to high-strength low-alloy steels used in reinforcing bar, pipelines, structural sections, tools and automotive components, and to titanium alloys for aerospace. Beyond metallurgy, vanadium pentoxide is an important industrial catalyst, notably in sulphuric acid manufacture and other oxidation chemistry, and it colours ceramics and glass. Its capacity to shift cleanly between several oxidation states underpins vanadium redox flow batteries, a long-duration energy-storage technology increasingly deployed to firm renewable generation.
How MineDSS reads it
MineDSS reads a vanadium-focused pathfinder suite qualitatively rather than through fixed weights. The seeded elements are chromium, nickel, cobalt, scandium, uranium, molybdenum and niobium, with chromium, nickel and cobalt carrying the lead signal. Chromium, nickel, cobalt, scandium and niobium trace the mafic-intrusion, titanomagnetite association, while uranium and molybdenum track the redox-controlled sediment-hosted setting in which vanadium concentrates in reduced, organic-rich rocks. This geochemistry is interpreted alongside mapped mafic and sedimentary geology and structure, geophysical expressions of dense magnetite-rich bodies and basin architecture, and satellite indications of altered and weathered ground. No single line is treated as decisive; the model weighs converging evidence so that a coherent, mutually reinforcing pattern is ranked more highly than any isolated anomaly.
Vanadium prospectivity — common questions
Which vanadium deposit types does MineDSS model?
MineDSS models two seeded deposit systems: mafic-intrusion titanomagnetite systems and sediment-hosted systems. The first hosts vanadium inside vanadiferous titanomagnetite within large layered mafic-ultramafic intrusions, the dominant source of primary vanadium worldwide. The second concentrates vanadium at low temperature in reduced, organic-rich shales and in sandstones, where it is often paired with uranium in the vanadate carnotite and the vanadium mica roscoelite. The model does not attempt to represent unrelated deposit styles; it ranks ground by its resemblance to these two well-characterised settings.
How is the model validated, and where is vanadium available?
Every MineDSS model is tested the hard way before it is served: we hide known deposits, rebuild the model without them, then test whether it still finds them, with test ground kept spatially separated so the model cannot memorise nearby points. A model that does not pass our release gates is not offered — for any mineral, in any country. Coverage today for vanadium spans Australia, the United States and Canada. Skill is model-level, never a specific site's measured accuracy, and never a discovery or JORC / NI 43-101 resource claim.
Which pathfinder elements does MineDSS read for vanadium?
The seeded pathfinder suite is chromium, nickel, cobalt, scandium, uranium, molybdenum and niobium, with chromium, nickel and cobalt carrying the lead signal. Chromium, nickel, cobalt, scandium and niobium trace the mafic-intrusion and titanomagnetite association, where vanadium travels with the same oxides and sulphides as those metals, while uranium and molybdenum track the redox-controlled sediment-hosted setting in which vanadium is fixed in reduced rocks. MineDSS interprets this geochemistry qualitatively and alongside mapped geology and structure, geophysics and satellite evidence, rather than applying fixed numeric weights to any one element.
Does a high MineDSS score mean a deposit or a resource estimate?
No. A high score means ground is geologically similar to known mineralised systems and merits closer exploration attention. It is not a discovery, not a JORC or NI 43-101 resource or reserve estimate, and not drilling or investment advice. MineDSS produces model-level prospectivity rankings to help prioritise where to look; confirming whether vanadium is present, and in what quantity and grade, still requires field programmes, drilling and independent assessment by qualified professionals.
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