Stranskiite is a rare secondary mineral found almost exclusively in the world-famous Tsumeb Mine in Namibia. It typically appears as striking azure-blue, thin tabular crystals or crystalline crusts associated with other rare zinc and copper arsenates.
Is this stranskiite?
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 stranskiite with a known reference. Stranskiite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: cyanic blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: aggregates, radial.
Often confused with
Stranskiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stranskiite
Minerals reported to co-occur with stranskiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₂Cu(AsO₄)₂
- Mohs hardness
- 4
- Density
- 5.23-5.3 g/cm³
- Colors
- Cyanic blue
- Streak
- Light blue
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Triclinic
- Crystal habit
- Aggregates, radial
- Cleavage
- On {010}, good; on {100}, {001}, {101}, indistinct
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare secondary mineral in the oxidized zone of a dolostone-hosted hydrothermal polymetallic ore deposit
Where rockhounds find stranskiite
Classic worldwide localities
- Tsumeb, Namibia
Field-hunting tip
Where it forms: A very rare secondary mineral in the oxidized zone of a dolostone-hosted hydrothermal polymetallic ore deposit. If you start seeing chalcocite, tennantite, galena in float, you are in the right ground. Typical habit: aggregates, radial. Train your eye for that shape before scanning the outcrop.







