Lautarite is a rare calcium iodate mineral found primarily in the nitrate deposits of the Atacama Desert. It typically forms colorless to yellowish prismatic crystals that are highly soluble in water, making it a challenging mineral to collect and store in humid environments.
Is this lautarite?
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 lautarite with a known reference. Lautarite sits at Mohs 3.5-4, 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, yellowish, light yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Lautarite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Lautarite leaves white, Dietzeite leaves light yellow.

How to tell apart: Lautarite is noticeably harder (Mohs 3.5-4 vs. 1.5-2); luster reads vitreous on Lautarite and subvitreous, pearly on {010} cleavages, silky if fibrous on Gypsum.
Often found alongside lautarite
Minerals reported to co-occur with lautarite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca(IO₃)₂
- Mohs hardness
- 3.5-4
- Density
- 4.59 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic crystals, massive, granular
- Cleavage
- On {011}, good; {100}, {110}, interrupted
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Coating fractures or embedded in gypsum in the nitrate deposits
Where rockhounds find lautarite
Classic worldwide localities
- Pampa del Pique III, about one km north of Oficina Lautaro, Taltal district, Antofagasta, Chile
Field-hunting tip
Where it forms: Coating fractures or embedded in gypsum in the nitrate deposits. If you start seeing gypsum, brüggenite, dietzeite in float, you are in the right ground. Typical habit: prismatic crystals, massive, granular. Train your eye for that shape before scanning the outcrop.




