Brindleyite is a rare nickel-rich member of the serpentine group, often appearing as small, platy, micaceous crystals. It is typically found in association with nickel deposits and is prized primarily by mineral collectors for its scarcity and specific geological occurrence.
Is this brindleyite?
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 brindleyite with a known reference. Brindleyite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Brindleyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Brindleyite typically shows a pearly luster.
- 4Match the color rangeCompare against the expected color range: green, pale green, yellowish green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, micaceous aggregates.
Often confused with
Brindleyite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside brindleyite
Minerals reported to co-occur with brindleyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ni,Mg,Fe)₂(Al,Si)₂O₅(OH)₄
- Mohs hardness
- 2.5
- Density
- 2.7-2.8 g/cm³
- Streak
- White
- Luster
- Pearly
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Micaceous Aggregates
- Cleavage
- Perfect Basal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nickel-bearing Hydrothermal Deposits
- Typical price
- $20-150 thumbnail
Where rockhounds find brindleyite
Classic worldwide localities
- Príbram, Czech Republic
- Kempirsai, Kazakhstan
- New Caledonia
Field-hunting tip
Look in nickel-bearing hydrothermal deposits country — that is the host setting where brindleyite typically forms. If you start seeing goethite, quartz, calcite in float, you are in the right ground. Field specimens usually show a platy crystals, micaceous aggregates habit, so train your eye for that shape before scanning the outcrop.





