Agardite-(Ce) is a rare secondary mineral typically found as delicate, needle-like crystals or radiating tufts in the oxidation zones of copper deposits. It is best identified by its vibrant yellowish-green color and habit, though it is often visually indistinguishable from other members of the mixite group without chemical analysis.
Is this agardite-(ce)?
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 agardite-(ce) with a known reference. Agardite-(Ce) 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: greenish to pale yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous to silky.
- 4Match the color rangeCompare against the expected color range: yellow green.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular.
Often confused with
Agardite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside agardite-(ce)
Minerals reported to co-occur with agardite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₆Ce(AsO₄)₃(OH)₆·3H₂O
- Mohs hardness
- ~3
- Density
- 3.70 g/cm³
- Colors
- Streak
- Greenish to pale yellow
- Luster
- Vitreous to silky
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In the oxidation zone of polymetallic sulfide deposits
Where rockhounds find agardite-(ce)
Classic worldwide localities
- Clara mine, near Oberwolfach, central Black Forest, Germany
Field-hunting tip
Where it forms: In the oxidation zone of polymetallic sulfide deposits. If you start seeing barite, quartz, goethite in float, you are in the right ground. Typical habit: acicular. Train your eye for that shape before scanning the outcrop.






