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, 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.


