Westerveldite is a rare nickel-iron arsenide mineral typically found as metallic, massive, or granular aggregates. It is primarily identified through laboratory analysis and is most commonly associated with other nickel-bearing ore minerals in ultramafic intrusive complexes.
Is this westerveldite?
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 westerveldite with a known reference. Westerveldite sits at Mohs >5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: brownish white, gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: irregular grains, microscopic crystals.
Often confused with
Westerveldite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside westerveldite
Minerals reported to co-occur with westerveldite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeAs
- Mohs hardness
- >5
- Density
- 8.13 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Irregular grains, microscopic crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As minute inclusions in maucherite which occurs in chromite-nickeline ores
Where rockhounds find westerveldite
Classic worldwide localities
- La Gallega mine, 3 km west of Ojén, Málaga Province, Spain
- Ilímaussaq intrusion, southern Greenland
- Seinäjoki, Finland
- Birchtree mine, near Thompson, Manitoba, Canada
Field-hunting tip
Where it forms: As minute inclusions in maucherite which occurs in chromite-nickeline ores. If you start seeing maucherite, nickeline, cobaltite in float, you are in the right ground. Typical habit: irregular grains, microscopic crystals. Train your eye for that shape before scanning the outcrop.







