Liebauite is a rare calcium-potassium silicate mineral primarily found in volcanic ejecta and xenoliths within the Eifel region of Germany. It typically forms as small, clear to bluish green tabular crystals that are difficult to distinguish from associated silicate minerals without advanced testing.
Is this liebauite?
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 liebauite with a known reference. Liebauite sits at Mohs 5-6, 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: blue green, greenish blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, granular aggregates.
Often confused with
Liebauite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside liebauite
Minerals reported to co-occur with liebauite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Cu₅Si₉O₂₆
- Mohs hardness
- 5-6
- Density
- 3.62 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular crystals, granular aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In cavities in argillaceous sedimentary xenoliths subjected to very high-grade thermal metamorphism
Where rockhounds find liebauite
Classic worldwide localities
- Sattelberg and Nickenicher Sattel volcanos and the Emmelberg cone, near Kruft, Eifel district, Germany
Field-hunting tip
Where it forms: In cavities in argillaceous sedimentary xenoliths subjected to very high-grade thermal metamorphism. If you start seeing cuprorivaite, tenorite, volborthite in float, you are in the right ground. Typical habit: tabular crystals, granular aggregates. Train your eye for that shape before scanning the outcrop.






