Attikaite is an extremely rare arsenate mineral that occurs as delicate, bright green acicular sprays. It is primarily known from the historic ancient slag dumps of the Lavrion district in Greece. Due to its fragility and rarity, it is highly sought after by advanced micro-mineral collectors.
Is this attikaite?
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 attikaite with a known reference. Attikaite 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. Attikaite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Attikaite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellowish-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tufts of acicular crystals.
Often confused with
Attikaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside attikaite
Minerals reported to co-occur with attikaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₃Cu₂Al₂(AsO₄)₄(OH)₄·12H₂O
- Mohs hardness
- 2
- Density
- 3.32 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tufts of Acicular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Slag Dumps
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find attikaite
Classic worldwide localities
- Lavrion District, Greece
Field-hunting tip
Look in slag dumps country — that is the host setting where attikaite typically forms. If you start seeing lavendulan, jarosite, goethite in float, you are in the right ground. Field specimens usually show a tufts of acicular crystals habit, so train your eye for that shape before scanning the outcrop.





