Cardite is a rare zinc arsenate, typically white to pinkish white and pale tan. It is a secondary mineral from a sulfide zone with leached sulfide minerals in a weathered Pb-Zn ore deposit. It is associated with anglesite and pyromorphite. It was first described from the mine dumps of the Block 14 Opencut, Broken Hill, New South Wales, Australia.
Is this cardite?
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 cardite with a known reference. Cardite sits at Mohs 3, 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: white, pinkish white and pale tan.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive.
Often confused with
Cardite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside cardite
Minerals reported to co-occur with cardite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Zn₅.₅(AsO₄)₂(AsO₃OH)(OH)₃·3H₂O
- Mohs hardness
- 3
- Density
- 4.02 g/cm³
- Colors
- WhitePinkish white and pale tan
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular crystals, massive
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral from a sulfide zone with leached sulfide minerals in a weathered Pb-Zn ore deposit
Where rockhounds find cardite
Classic worldwide localities
- Mine dumps of the Block 14 Opencut, New South Wales, Australia
Field-hunting tip
Where it forms: A secondary mineral from a sulfide zone with leached sulfide minerals in a weathered Pb-Zn ore deposit. If you start seeing anglesite, pyromorphite, köttigite in float, you are in the right ground. Typical habit: tabular crystals, massive. Train your eye for that shape before scanning the outcrop.





