Antofagastaite is a rare hydrated sodium-calcium sulfate mineral typically found as delicate, needle-like or fibrous crystal aggregates in arid evaporite settings. Collectors look for these fragile formations within the hyper-arid regions of the Atacama Desert in Chile, where it occurs as a secondary precipitate.
Is this antofagastaite?
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 antofagastaite with a known reference. Antofagastaite 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: white, colorless.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: fibrous, acicular, prismatic.
Often confused with
Antofagastaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside antofagastaite
Minerals reported to co-occur with antofagastaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ca(SO₄)₂·1.5H₂O
- Mohs hardness
- 2
- Density
- 2.42 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Fibrous, acicular, prismatic
- Cleavage
- Distinct on (001) and a second direction visible in thin section
- Rarity
- Rare
- Uses
- Collector
- Host rock
- evaporite deposits
Where rockhounds find antofagastaite
Classic worldwide localities
- Antofagasta, Chile
Field-hunting tip
Where it forms: evaporite deposits. If you start seeing halite, anhydrite, gypsum in float, you are in the right ground. Typical habit: fibrous, acicular, prismatic. Train your eye for that shape before scanning the outcrop.




