Wilhelmkleinite is a rare zinc-iron arsenate mineral primarily known from the Tsumeb Mine in Namibia. It typically forms small, blackish green, short-prismatic crystals often associated with other rare secondary minerals in oxidized ore zones.
Is this wilhelmkleinite?
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 wilhelmkleinite with a known reference. Wilhelmkleinite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: green.
- 3Read the lusterHold the specimen under a strong light. Luster: dull, adamantine on fractures.
- 4Match the color rangeCompare against the expected color range: blackish green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: euhedral crystals.
Often confused with
Wilhelmkleinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wilhelmkleinite
Minerals reported to co-occur with wilhelmkleinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- ZnFe³⁺₂(AsO₄)₂(OH)₂
- Mohs hardness
- 4.5
- Density
- 4.34-4.63 g/cm³
- Colors
- Streak
- Green
- Luster
- Dull, adamantine on fractures
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Euhedral crystals
- Cleavage
- On {232}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Very rare from a deep oxidation zone in a dolostone-hosted hydrothermal polymetallic ore deposit
Where rockhounds find wilhelmkleinite
Classic worldwide localities
- Tsumeb, Namibia
Field-hunting tip
Where it forms: Very rare from a deep oxidation zone in a dolostone-hosted hydrothermal polymetallic ore deposit. If you start seeing scorodite, gerdtremmelite, adamite in float, you are in the right ground. Typical habit: euhedral crystals. Train your eye for that shape before scanning the outcrop.




