Vanadio-oxy-chromium-dravite is an extremely rare member of the tourmaline group characterized by its high vanadium and chromium content, which imparts a vivid green color. It typically occurs in metamorphic environments where vanadium-bearing fluids interact with tourmaline-forming precursors. Collectors prize it for its unique composition and intense, often saturated coloration.
Is this vanadio-oxy-chromium-dravite?
5-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 vanadio-oxy-chromium-dravite with a known reference. Vanadio-oxy-chromium-dravite sits at Mohs 7-7.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Vanadio-oxy-chromium-dravite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Vanadio-oxy-chromium-dravite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: dark green, emerald green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Vanadio-oxy-chromium-dravite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside vanadio-oxy-chromium-dravite
Minerals reported to co-occur with vanadio-oxy-chromium-dravite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(V³⁺,Mg,Cr)₃(Al,Mg,V³⁺)₆(Si₆O₁₈)(BO₃)₃(OH)₃O
- Mohs hardness
- 7-7.5
- Density
- 3.15-3.25 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks
- Typical price
- $50-500 thumbnail
Where rockhounds find vanadio-oxy-chromium-dravite
Classic worldwide localities
- Tanzania
- Russia
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where vanadio-oxy-chromium-dravite typically forms. If you start seeing graphite, quartz, feldspar in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.





