Espadaite is a rare sodium calcium magnesium arsenite, typically colorless. Associated minerals include camanchacaite, anhydrite and gypsum. It was first described from the Torrecillas mine, Iquique Province, Tarapacá Region, Chile.
Is this espadaite?
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 espadaite with a known reference. Espadaite 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: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: colorless.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals.
Often confused with
Espadaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside espadaite
Minerals reported to co-occur with espadaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₄Ca₃Mg₂[AsO₃(OH)]₂[AsO₂(OH)₂]₁₀(H₂O)₆·H₂O
- Mohs hardness
- ~2
- Density
- 2.73 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy crystals
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- granite pegmatites
Where rockhounds find espadaite
Classic worldwide localities
- Torrecillas mine, northern Atacama Desert, Salar Grande, Iquique Province, Tarapacá Region, Chile
Field-hunting tip
Where it forms: granite pegmatites. If you start seeing camanchacaite, anhydrite, gypsum in float, you are in the right ground. Typical habit: platy crystals. Train your eye for that shape before scanning the outcrop.





