Joteite is a very rare copper-calcium arsenate mineral known primarily from the Jote mine in Chile. It typically forms as delicate, tabular yellow 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 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Joteite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Joteite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, brownish-yellow.
- 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); streak differs — Joteite leaves yellow, Conichalcite leaves light green.

How to tell apart: Austinite is the harder of the two (Mohs 4 vs. 2); streak differs — Joteite leaves yellow, Austinite leaves white.
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)₂(OH)₅·5H₂O
- Mohs hardness
- 2
- Density
- 3.84 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Hydrothermal Zones
- Typical price
- $50-300 per specimen
Where rockhounds find joteite
Classic worldwide localities
- Jote mine, Tierra Amarilla, Chile
Field-hunting tip
Look in oxidized hydrothermal zones country — that is the host setting where joteite typically forms. If you start seeing conichalcite, austinite, guerinite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.
