Polkovicite is a rare germanium-bearing sulfide mineral that typically occurs as small, black metallic grains within complex sulfide ore assemblages. It is primarily identified through specialized mineralogical analysis like microprobe testing due to its visual similarity to other dark sulfide minerals. It is famously associated with the unique germanium-rich mineralization found in the Tsumeb Mine.
Is this polkovicite?
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 polkovicite with a known reference. Polkovicite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Polkovicite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Polkovicite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: cubic. Typical habit: granular to massive.
Often confused with
Polkovicite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside polkovicite
Minerals reported to co-occur with polkovicite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Fe,Zn)₂GeS₄
- Mohs hardness
- 3.5-4
- Density
- 4.49 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Granular to Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Polymetallic Hydrothermal Ore Deposits
- Typical price
- $50-300 per micro-mount or thumbnail specimen
Where rockhounds find polkovicite
Classic worldwide localities
- Tsumeb Mine, Namibia
Field-hunting tip
Look in polymetallic hydrothermal ore deposits country — that is the host setting where polkovicite typically forms. If you start seeing germanite, renierite, tsumebite in float, you are in the right ground. Field specimens usually show a granular to massive habit, so train your eye for that shape before scanning the outcrop.





