Barrotite is a rare copper aluminum arsenate, typically intense blue. It is a secondary mineral in sandstone. Associated minerals include chalcophyllite, malachite and cuprite. It was first described from the copper mines of Roua, Alpes-Maritimes, France.
Is this barrotite?
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 barrotite with a known reference. Barrotite 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. Barrotite leaves a pale blue streak.
- 3Read the lusterHold the specimen under a strong light. Barrotite typically shows a vitreous to subadamantine luster.
- 4Match the color rangeCompare against the expected color range: intense blue.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: acicular crystals, radiating clusters.
Often confused with
Barrotite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside barrotite
Minerals reported to co-occur with barrotite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₉Al(HSiO₄)₂[(SO₄)(HAsO₄)₀.₅](OH)₁₂·8H₂O
- Mohs hardness
- 2
- Density
- 2.90 g/cm³
- Colors
- Streak
- Pale Blue
- Luster
- Vitreous to Subadamantine
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Acicular Crystals, Radiating Clusters
- Cleavage
- Perfect Mica-like On {001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
Where rockhounds find barrotite
Classic worldwide localities
- Barrois, France
Field-hunting tip
Look in hydrothermal veins country, the host setting where barrotite typically forms. If you start seeing calcite, smithsonite in float, you are in the right ground. Field specimens usually show a acicular crystals, radiating clusters habit, so train your eye for that shape before scanning the outcrop.



