Paraotwayite is a rare nickel hydroxide sulfate mineral that typically appears as bright green to yellow-green platy crusts. It is primarily found in the weathering zones of nickel-rich ultramafic rocks and is a prized target for advanced mineral collectors focusing on supergene species.
Is this paraotwayite?
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 paraotwayite with a known reference. Paraotwayite 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. Paraotwayite leaves a light green streak.
- 3Read the lusterHold the specimen under a strong light. Paraotwayite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, or massive aggregates.
Often confused with
Paraotwayite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paraotwayite
Minerals reported to co-occur with paraotwayite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ni(OH)₂(SO₄)₀.₅
- Mohs hardness
- 3
- Density
- 4.56 g/cm³
- Colors
- Streak
- Light Green
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts, Or Massive Aggregates
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Nickel-rich Weathering Zones of Serpentinites
- Typical price
- $50-300 per specimen
Where rockhounds find paraotwayite
Classic worldwide localities
- Otway Group, Western Australia
- Carr Boyd Rocks, Western Australia
Field-hunting tip
Look in nickel-rich weathering zones of serpentinites country — that is the host setting where paraotwayite typically forms. If you start seeing otwayite, gaspeite, magnesite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts, or massive aggregates habit, so train your eye for that shape before scanning the outcrop.


