Wittichenite is a rare copper bismuth sulfide that typically appears as metallic, steel-gray to tin-white massive aggregates. It is best known by advanced collectors for occurring in specific hydrothermal deposit types, particularly in the Black Forest region of Germany.
Is this wittichenite?
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 wittichenite with a known reference. Wittichenite sits at Mohs 2-3, 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: lead gray, bronze, steel gray, tin white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: columnar, massive, nodular.
Often confused with
Wittichenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside wittichenite
Minerals reported to co-occur with wittichenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₃BiS₃
- Mohs hardness
- 2-3
- Density
- 6.01 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Columnar, massive, nodular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In hydrothermal veins with other bismuth minerals (Wittichen, Germany); with Cu-Fe sulfides (Seathwaite Tarn, England); with secondary uranium minerals and selenides of Cu, Pb, and Bi (Kletno, Poland)
Where rockhounds find wittichenite
Classic worldwide localities
- Butte, Silver Bow Co., Montana, USA
- Fairfax quarry, Centreville, Fairfax Co., Virginia, USA
- Bisbee, Cochise Co., Arizona, USA
- Maid of Erin mine, Rainy Hollow district, British Columbia, Canada
- Cobalt, Ontario, Canada
- Schapbachtal, and at the Neuglück, Daniel, and King David mines, near Wittichen, Black Forest, Germany
Field-hunting tip
Where it forms: In hydrothermal veins with other bismuth minerals (Wittichen, Germany); with Cu-Fe sulfides (Seathwaite Tarn, England); with secondary uranium minerals and selenides of Cu, Pb, and Bi (Kletno, Poland). If you start seeing bornite, chalcocite, chalcopyrite in float, you are in the right ground. Typical habit: columnar, massive, nodular. Train your eye for that shape before scanning the outcrop.









