Chromium-dravite is a rare chromium-rich variety of the dravite tourmaline group, prized by collectors for its vivid, intense green color caused by chromium substitution. It typically occurs as elongated prismatic crystals within metamorphic rocks associated with ultramafic bodies. Collectors should look for well-defined, transparent to translucent prisms that exhibit distinct green hues, often found alongside chromite or silicate minerals.
Is this 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 chromium-dravite with a known reference. 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. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: emerald green, deep green.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Chromium-dravite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chromium-dravite
Minerals reported to co-occur with chromium-dravite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaMg₃Cr₆(Si₆O₁₈)(BO₃)₃(OH)₃(OH)
- Mohs hardness
- 7-7.5
- Density
- 3.0-3.2 g/cm³
- Colors
- Emerald greenDeep green
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic crystals
- Cleavage
- Indistinct
- Rarity
- Rare
- Uses
- Collector, Lapidary
- Host rock
- metamorphic rocks, specifically chromite-bearing schists and marbles
Where rockhounds find chromium-dravite
Classic worldwide localities
- Outokumpu, Finland
- Zarafshan Range, Tajikistan
- Maku, Iran
- Saranovskii mine, Russia
Field-hunting tip
Where it forms: metamorphic rocks, specifically chromite-bearing schists and marbles. If you start seeing quartz, calcite, chromite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.







