Hellyerite is a rare nickel carbonate mineral that typically forms as pale blue crusts or small aggregates on serpentinite. It is primarily known from the type locality in the Lord Brassey mine in Tasmania, where it is found associated with other nickel-bearing minerals. Because it is highly sensitive to humidity and can dehydrate, specimens should be stored in controlled conditions to prevent degradation.
Is this hellyerite?
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 hellyerite with a known reference. Hellyerite 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. Hellyerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Hellyerite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: blue, pale blue, greenish-blue.
- 5Look at form & habitCrystal system: trigonal. Typical habit: fine-grained crusts, tabular crystals.
Often confused with
Hellyerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside hellyerite
Minerals reported to co-occur with hellyerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NiCO₃·6H₂O
- Mohs hardness
- 2.5
- Density
- 2.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Fine-grained Crusts, Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Serpentinite
- Typical price
- $50-300 per small specimen
Where rockhounds find hellyerite
Classic worldwide localities
- Lord Brassey mine, Tasmania, Australia
Field-hunting tip
Look in serpentinite country — that is the host setting where hellyerite typically forms. If you start seeing millerite, pentlandite, serpentine in float, you are in the right ground. Field specimens usually show a fine-grained crusts, tabular crystals habit, so train your eye for that shape before scanning the outcrop.




