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 — that is 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.



