Iquiqueite is an extremely rare chromate-iodate mineral found primarily in the hyper-arid nitrate fields of northern Chile. Collectors prize it for its vibrant yellow fluorescence under short-wave ultraviolet light, although specimens are often quite small and fragile.
Is this iquiqueite?
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 iquiqueite with a known reference. Iquiqueite 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. Iquiqueite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Iquiqueite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Iquiqueite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside iquiqueite
Minerals reported to co-occur with iquiqueite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₃Na₄Mg(CrO₄)₄(IO₃)·H₂O
- Mohs hardness
- 2
- Density
- 2.44 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Platy Crystals, Crusts, Radial Aggregates
- Cleavage
- Good
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nitrate Deposits in Arid Desert Environments
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find iquiqueite
Classic worldwide localities
- Iquique, Tarapacá Region, Chile
Field-hunting tip
Look in nitrate deposits in arid desert environments country, the host setting where iquiqueite typically forms. If you start seeing dietzeite, lautarite, halite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, radial aggregates habit, so train your eye for that shape before scanning the outcrop.



