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 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Nickelpicromerite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Nickelpicromerite 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: 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
- (K,Ni)₂Mg(SO₄)₂·6H₂O
- Mohs hardness
- 2.5
- Density
- 2.14 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Crusts, Granular, Prismatic Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Secondary Mineral in Mine Dumps and Oxidized Zones
- Typical price
- $20-100 thumbnail
Where rockhounds find nickelpicromerite
Classic worldwide localities
- Schneeberg, Saxony, Germany
- Jachymov, Czech Republic
- Lavrion, Greece
- Broken Hill, Australia
Field-hunting tip
Look in secondary mineral in mine dumps and oxidized zones country, the host setting where nickelpicromerite typically forms. If you start seeing retgersite, morenosite, epsomite in float, you are in the right ground. Field specimens usually show a crusts, granular, prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







