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 3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Barlowite leaves a light blue streak.
- 3Read the lusterHold the specimen under a strong light. Barlowite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: deep blue, dark green-blue.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, subparallel aggregates.
Often confused with
Barlowite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Barlowite leaves light blue, Herbertsmithite leaves pale green.

How to tell apart: Streak differs — Barlowite leaves light blue, Paratacamite leaves apple green; luster reads vitreous on Barlowite and adamantine on Paratacamite.
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
- 3
- Density
- 4.15 g/cm³
- Colors
- Streak
- Light Blue
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Subparallel Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Copper Ore Deposits
- Typical price
- $100-500 thumbnail size
Where rockhounds find barlowite
Classic worldwide localities
- Barlow mine, Chile
Field-hunting tip
Look in oxidized copper ore deposits country — that is the host setting where barlowite typically forms. If you start seeing paratacamite, gypsum, atacamite in float, you are in the right ground. Field specimens usually show a tabular crystals, subparallel aggregates habit, so train your eye for that shape before scanning the outcrop.


