Ludjibaite is a rare copper phosphate mineral often found as attractive, bright blue, botryoidal or spherulitic crusts in oxidized copper deposits. It is a dimorph of pseudomalachite and is primarily sought after by advanced collectors for its distinctive color and occurrence in the Katanga copper belt.
Is this ludjibaite?
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 ludjibaite with a known reference. Ludjibaite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue to white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue green.
- 5Look at form & habitCrystal system: triclinic. Typical habit: botryoidal crusts, radiating aggregates, spherulitic.
Often confused with
Ludjibaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ludjibaite
Minerals reported to co-occur with ludjibaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₅(PO₄)₂(OH)₄
- Mohs hardness
- 3.5-4
- Density
- 4.36 g/cm³
- Colors
- Streak
- Pale blue to white
- Luster
- Vitreous
- Transparency
- Translucent to opaque
- Crystal system
- Triclinic
- Crystal habit
- Botryoidal crusts, radiating aggregates, spherulitic
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A rare mineral in the oxidized zone of some copper deposits
Where rockhounds find ludjibaite
Classic worldwide localities
- Ludjiba mine, about 12 km southeast of Kambove, Katanga Province, Congo (Shaba Province, Zaire)
- Lubietová, near Baňská Bystrica (Libethen, near Neusohl), Slovakia
- Käusersteimel mine, near Kausen, Siegerland, Germany
Field-hunting tip
Where it forms: A rare mineral in the oxidized zone of some copper deposits. If you start seeing pseudomalachite, libethenite in float, you are in the right ground. Typical habit: botryoidal crusts, radiating aggregates, spherulitic. Train your eye for that shape before scanning the outcrop.



