Nickelpicromerite is a rare secondary sulfate mineral occurring as efflorescences or crusts in the oxidized zones of nickel-rich ore deposits. It is best identified by its vibrant green color and association with other nickel sulfates in mine workings. Collectors typically seek out well-formed micro-specimens from historic European mining districts.
Is this nickelpicromerite?
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 nickelpicromerite with a known reference. Nickelpicromerite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: light greenish blue.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: crusts, granular, prismatic crystals.
Often confused with
Nickelpicromerite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nickelpicromerite
Minerals reported to co-occur with nickelpicromerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- K₂Ni(SO₄)₂·6H₂O
- Mohs hardness
- 2-2.5
- Density
- 2.20 g/cm³
- Colors
- Light greenish blue
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Crusts, granular, prismatic crystals
- Cleavage
- Distinct on {102̄} (by analogy to picromerite)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the fractures of slightly weathered actinolite-talc schist containing partially vermiculitized biotite and partially altered, nickle-bearing sulfides
Where rockhounds find nickelpicromerite
Classic worldwide localities
- Chelyabinsk area, South Urals, Russia
Field-hunting tip
Where it forms: A secondary mineral in the fractures of slightly weathered actinolite-talc schist containing partially vermiculitized biotite and partially altered, nickle-bearing sulfides. If you start seeing gypsum, goethite in float, you are in the right ground. Typical habit: crusts, granular, prismatic crystals. Train your eye for that shape before scanning the outcrop.





