Nickelblödite is a rare nickel sulfate member of the blödite group, typically found as an oxidation product of nickel-bearing sulfides. Collectors look for its characteristic pale yellow, vitreous tabular crystals or crusts in arid environments where nickel ores have weathered.
Is this nickelblödite?
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 nickelblödite with a known reference. Nickelblödite sits at Mohs 2.5-3 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Nickelblödite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Nickelblödite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, massive, crusts.
Often confused with
Nickelblödite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside nickelblödite
Minerals reported to co-occur with nickelblödite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₂Ni(SO₄)₂·4H₂O
- Mohs hardness
- 2.5-3
- Density
- 2.36 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Massive, Crusts
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Zones of Nickel-rich Sulfide Deposits
- Typical price
- $50-250 per specimen depending on size and quality
Where rockhounds find nickelblödite
Classic worldwide localities
- Kambalda, Western Australia
- La Rioja, Argentina
Field-hunting tip
Look in oxidized zones of nickel-rich sulfide deposits country — that is the host setting where nickelblödite typically forms. If you start seeing retgersite, morenosite, gypsum in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, crusts habit, so train your eye for that shape before scanning the outcrop.




