Joteite is a very rare copper-calcium arsenate mineral known primarily from the Jote mine in Chile. It typically forms as delicate, tabular sky-blue to greenish blue crystals within oxidized zones of arsenic-rich copper deposits.
Is this joteite?
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 joteite with a known reference. Joteite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: very pale blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: sky-blue, greenish blue.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Joteite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Conichalcite is the harder of the two (Mohs 4.5 vs. 2-3); streak differs, so Joteite leaves very pale blue, Conichalcite leaves green.

How to tell apart: Austinite is the harder of the two (Mohs 4-4.5 vs. 2-3); streak differs, so Joteite leaves very pale blue, Austinite leaves white; luster reads vitreous on Joteite and subadamantine to silky in aggregates on Austinite.
Often found alongside joteite
Minerals reported to co-occur with joteite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂CuAl(AsO₄)[AsO₃(OH)]₂(OH)₂·5H₂O
- Mohs hardness
- 2-3
- Density
- 3.084 g/cm³
- Colors
- Streak
- Very pale blue
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- Perfect on {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In narrow seams and vugs in the oxidized upper portion of a hydrothermal sulfide vein hosted by volcanoclastic rocks
Where rockhounds find joteite
Classic worldwide localities
- Jote mine, Pampa Larga district, Tierra Amarilla, Copiapó Province, Atacama, Chile
Field-hunting tip
Where it forms: In narrow seams and vugs in the oxidized upper portion of a hydrothermal sulfide vein hosted by volcanoclastic rocks. If you start seeing conichalcite, mansfieldite, pharmacoalumite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.




