Liebermannite is an extremely rare high-pressure silicate mineral identified primarily in shocked meteorites. It typically occurs as microscopic inclusions within impact melt veins, often associated with other high-pressure phases like stishovite.
Is this liebermannite?
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 liebermannite with a known reference. Liebermannite 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. Liebermannite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Liebermannite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic crystals.
Often confused with
Liebermannite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside liebermannite
Minerals reported to co-occur with liebermannite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (K,Na,Ba)₁₂(Si,Al,Fe,Mg,Ti)₈O₁₆
- Mohs hardness
- 6-7
- Density
- 4.26 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Impact Melt Veins in Meteorites
- Typical price
- expensive and rarely available for private collection
Where rockhounds find liebermannite
Classic worldwide localities
- Wabar Craters, Saudi Arabia
Field-hunting tip
Look in impact melt veins in meteorites country — that is the host setting where liebermannite typically forms. If you start seeing stishovite, ringwoodite, bridgmanite 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.





