Cualstibite is a rare secondary copper mineral that typically forms as delicate blue platy or tabular crystals. It is most commonly found in the oxidized zones of copper-antimony ore deposits where it is often associated with other rare copper minerals.
Is this cualstibite?
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 cualstibite with a known reference. Cualstibite sits at Mohs ~2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: pale blue.
- 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: hexagonal. Typical habit: massive, microscopic crystals.
Often confused with
Cualstibite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cualstibite
Minerals reported to co-occur with cualstibite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂AlSb(OH)₁₂
- Mohs hardness
- ~2
- Density
- 3.18 g/cm³
- Colors
- Streak
- Pale blue
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Massive, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral from oxidation of a hydrothermal polymetallic barite–fluorite deposit
Where rockhounds find cualstibite
Classic worldwide localities
- Clara mine, near Oberwolfach, Black Forest, Germany
Field-hunting tip
Where it forms: A secondary mineral from oxidation of a hydrothermal polymetallic barite–fluorite deposit. If you start seeing cornwallite, arsenogoyazite, goethite in float, you are in the right ground. Typical habit: massive, microscopic crystals. Train your eye for that shape before scanning the outcrop.








