Oxy-chromium-dravite is a rare member of the tourmaline group, distinguished by its intense green color derived from chromium substitution. It typically occurs as prismatic crystals within metamorphic rocks and is highly prized by collectors for its unique chemistry and vivid, saturated hues.
Is this 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 oxy-chromium-dravite with a known reference. Oxy-chromium-dravite sits at Mohs 7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Oxy-chromium-dravite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. 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
Oxy-chromium-dravite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside oxy-chromium-dravite
Minerals reported to co-occur with 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(Cr₃)Mg₆(Si₆O₁₈)(BO₃)₃(OH)₃O
- Mohs hardness
- 7
- Density
- 3.02-3.11 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks
- Typical price
- $50-500 depending on crystal size and clarity
Where rockhounds find oxy-chromium-dravite
Classic worldwide localities
- Sar-e-Sang, Afghanistan
- Urals, Russia
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where oxy-chromium-dravite typically forms. If you start seeing calcite, phlogopite, diopside 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.





