Dietzeite is a rare calcium iodate chromate mineral exclusively found in the hyper-arid nitrate deposits of the Atacama Desert. Collectors prize it for its vibrant yellow to orange-yellow color and distinct crystal habits, though it is highly sensitive to moisture and should be stored in a dry environment.
Is this dietzeite?
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 dietzeite with a known reference. Dietzeite sits at Mohs 3-3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dietzeite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Dietzeite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow, reddish-orange.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic to acicular crystals, often as crusts or granular aggregates.
Often confused with
Dietzeite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside dietzeite
Minerals reported to co-occur with dietzeite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂(IO₃)₂(CrO₄)
- Mohs hardness
- 3-3.5
- Density
- 3.68 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic to Acicular Crystals, Often as Crusts or Granular Aggregates
- Cleavage
- Distinct On {010}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Arid Saline Deposits
- Typical price
- $50-500 depending on specimen quality
Where rockhounds find dietzeite
Classic worldwide localities
- Atacama Desert, Chile
Field-hunting tip
Look in arid saline deposits country, the host setting where dietzeite typically forms. If you start seeing lautarite, gypsum, halite in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals, often as crusts or granular aggregates habit, so train your eye for that shape before scanning the outcrop.



