Liebenbergite is a very rare nickel-dominant member of the olivine group. It is primarily identified in nickel-rich geological environments where it forms through the alteration of primary ultramafic minerals.
Is this liebenbergite?
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 liebenbergite with a known reference. Liebenbergite sits at Mohs 6.5-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Liebenbergite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Liebenbergite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-green, brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, massive.
Often confused with
Liebenbergite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside liebenbergite
Minerals reported to co-occur with liebenbergite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni₂SiO₄
- Mohs hardness
- 6.5-7
- Density
- 4.6-4.7 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, Massive
- Cleavage
- Distinct On {010}
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Ultramafic Rocks and Nickel-rich Hydrothermal Deposits
- Typical price
- $100-500 for small analytical-grade specimens
Where rockhounds find liebenbergite
Classic worldwide localities
- Barberton greenstone belt, South Africa
- Bushveld Igneous Complex, South Africa
Field-hunting tip
Look in ultramafic rocks and nickel-rich hydrothermal deposits country — that is the host setting where liebenbergite typically forms. If you start seeing trevorite, bunsenite, millerite in float, you are in the right ground. Field specimens usually show a granular, massive habit, so train your eye for that shape before scanning the outcrop.







