Barlowite is a rare copper halide mineral first identified in the oxidation zone of copper deposits in Chile. It typically forms deep blue tabular crystals that are highly sought after by mineral collectors for their unique structure and vibrant color.
Is this barlowite?
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 barlowite with a known reference. Barlowite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: sky-blue.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: blue.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Barlowite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside barlowite
Minerals reported to co-occur with barlowite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₄Br(OH)₆F
- Mohs hardness
- 2-2.5
- Density
- 4.21 g/cm³
- Colors
- Streak
- Sky-blue
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals, subparallel aggregates
- Cleavage
- Perfect on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the weathering zone of a copper deposit
Where rockhounds find barlowite
Classic worldwide localities
- Great Australia mine, 2 km south of Cloncurry, northwest Queensland, Australia
Field-hunting tip
Where it forms: A secondary mineral in the weathering zone of a copper deposit. If you start seeing gerhardtite, brochantite, cuprite in float, you are in the right ground. Typical habit: tabular crystals, subparallel aggregates. Train your eye for that shape before scanning the outcrop.







