Native vanadium is an extremely rare metallic mineral that almost exclusively occurs as microscopic grains embedded within igneous rocks. Due to its high reactivity with oxygen, authentic native vanadium is rarely found in its pure state and is primarily of interest to advanced mineral collectors or metallurgical researchers.
Is this vanadium?
4-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch vanadium with a known reference. Vanadium sits at Mohs 7, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: steel-gray.
- 4Look at form & habitCrystal system: cubic. Typical habit: massive.
Often confused with
Vanadium vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside vanadium
Minerals reported to co-occur with vanadium. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- V
- Mohs hardness
- 7
- Density
- 6.033 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Massive
- Rarity
- Rare
- Uses
- Industrial, Collector
- Host rock
- In sublimates from high-temperature (550-680° C) volcanic gases at active fumaroles
Where rockhounds find vanadium
2 mapped spotsClassic worldwide localities
- Tungsten Hills, California, USA
- Kola Peninsula, Russia
Field-hunting tip
Where it forms: In sublimates from high-temperature (550-680° C) volcanic gases at active fumaroles. If you start seeing colimaite, shcherbinaite in float, you are in the right ground. Typical habit: massive. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Nevada, Utah. Start trip planning there.



