Tarapacáite is a rare potassium chromate mineral primarily found in the hyper-arid regions of Chile. It typically forms small, yellow, tabular crystals or crusts within nitrate-rich evaporite deposits and is highly soluble in water.
Is this tarapacáite?
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 tarapacáite with a known reference. Tarapacáite 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. Tarapacáite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Tarapacáite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive, crusts.
Often confused with
Tarapacáite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tarapacáite
Minerals reported to co-occur with tarapacáite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂CrO₄
- Mohs hardness
- 2
- Density
- 2.71 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Arid Evaporite Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find tarapacáite
Classic worldwide localities
- Tarapacá, Chile
- Atacama Desert, Chile
Field-hunting tip
Look in arid evaporite deposits country — that is the host setting where tarapacáite typically forms. If you start seeing dietzeite, nitratine, gypsum in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, crusts habit, so train your eye for that shape before scanning the outcrop.





