Zincobriartite is an extremely rare copper-zinc-germanium sulfide mineral known primarily from the Tsumeb Mine. It usually occurs as microscopic inclusions or fine anhedral grains within massive ore samples, making it a target mostly for systematic mineral collectors.
Is this zincobriartite?
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 zincobriartite with a known reference. Zincobriartite 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. Zincobriartite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Zincobriartite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: gray, pinkish-gray.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains.
Often confused with
Zincobriartite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincobriartite
Minerals reported to co-occur with zincobriartite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂(Zn,Ge)(Ga,Ge)S₄
- Mohs hardness
- 4
- Density
- 4.86 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Polymetallic Sulfide Deposits
- Typical price
- $50-300 per small specimen
Where rockhounds find zincobriartite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Look in polymetallic sulfide deposits country, the host setting where zincobriartite typically forms. If you start seeing germanite, tennantite, galena in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.






