Trattnerite is a rare hexagonal mineral within the beryl group, primarily distinguished by its magnesium-rich composition. It typically occurs as small prismatic crystals in pegmatitic environments and is primarily sought after by advanced systematic mineral collectors.
Is this trattnerite?
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 trattnerite with a known reference. Trattnerite sits at Mohs 6-7, 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: deep blue, yellowish green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic.
Often confused with
Trattnerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside trattnerite
Minerals reported to co-occur with trattnerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂(Mg₃Si₁₂)O₃₀
- Mohs hardness
- 6-7
- Density
- 2.68 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic
- Cleavage
- Good on {001}, poor on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In small cavities within a Si-rich xenolith in nephelinite volcanic rock
Where rockhounds find trattnerite
Classic worldwide localities
- Stradner Kogel haüyne–nephelinite quarry, near Bad Gleichenberg, eastern Styria, Austria
Field-hunting tip
Where it forms: In small cavities within a Si-rich xenolith in nephelinite volcanic rock. If you start seeing sanidine, plagioclase, quartz in float, you are in the right ground. Typical habit: prismatic. Train your eye for that shape before scanning the outcrop.








