Nickeltsumcorite is an extremely rare member of the Tsumcorite group, characterized by its distinct yellow color and platy crystal habit. It is found primarily in the oxidation zones of base metal deposits, often associated with other secondary arsenates.
Is this nickeltsumcorite?
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 nickeltsumcorite with a known reference. Nickeltsumcorite sits at Mohs ~4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, brownish yellow, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts, radial aggregates.
Often confused with
Nickeltsumcorite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside nickeltsumcorite
Minerals reported to co-occur with nickeltsumcorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb(Ni,Fe)₂(AsO₄)₂(H₂O,OH)₂
- Mohs hardness
- ~4
- Density
- 5.02 g/cm³
- Streak
- Yellow
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Platy crystals, crusts, radial aggregates
- Cleavage
- Distinct on {001}, by analogy with tsumcorite
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A secondary mineral in the oxidized zone of a hydrothermal deposit containing gersdorffite and galena
Where rockhounds find nickeltsumcorite
Classic worldwide localities
- Tsumeb Mine, Namibia
- Klomnice, Poland
Field-hunting tip
Where it forms: A secondary mineral in the oxidized zone of a hydrothermal deposit containing gersdorffite and galena. If you start seeing annabergite, nickellotharmeyerite, nickelaustinite in float, you are in the right ground. Typical habit: platy crystals, crusts, radial aggregates. Train your eye for that shape before scanning the outcrop.








