Otwayite is a rare nickel carbonate mineral that typically appears as bright green, fibrous crusts or micro-crystalline aggregates. It is most commonly found in the oxidized zones of nickel sulfide deposits in Western Australia, often associated with other rare nickel minerals like gaspeite. Due to its scarcity and distinct coloration, it is highly sought after by systematic mineral collectors.
Is this otwayite?
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 otwayite with a known reference. Otwayite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light green.
- 3Read the lusterHold the specimen under a strong light. Luster: silky to waxy.
- 4Match the color rangeCompare against the expected color range: bright green, green.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: aggregates, fibrous.
Often confused with
Otwayite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside otwayite
Minerals reported to co-occur with otwayite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni₂CO₃(OH)₂·H₂O
- Mohs hardness
- 4
- Density
- 3.41 g/cm³
- Colors
- Streak
- Light green
- Luster
- Silky to waxy
- Transparency
- Opaque to translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Aggregates, fibrous
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In veinlets in serpentinite (Otway prospect, Western Australia; Lord Brassey mine, Tasmania, Australia)
Where rockhounds find otwayite
Classic worldwide localities
- Otway Ni prospect, 23 km north of the town of Nullagine, Pilbara region, Western Australia (type locality)
Field-hunting tip
Where it forms: In veinlets in serpentinite (Otway prospect, Western Australia; Lord Brassey mine, Tasmania, Australia). If you start seeing magnesite, pecoraite, gaspéite in float, you are in the right ground. Typical habit: aggregates, fibrous. Train your eye for that shape before scanning the outcrop.






