Makovickyite is a rare sulfosalt mineral primarily found in hydrothermal vein systems associated with other sulfide minerals. It typically appears as lead-gray to tin-white metallic masses and is often identified through specialized analytical techniques like microprobe analysis due to its visual similarity to other complex lead-bismuth sulfosalts.
Is this makovickyite?
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 makovickyite with a known reference. Makovickyite sits at Mohs 3-3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Makovickyite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Makovickyite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, tin-white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains, tabular crystals.
Often confused with
Makovickyite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside makovickyite
Minerals reported to co-occur with makovickyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₁₁Cu₁Pb₁Bi₁₅S₂₈
- Mohs hardness
- 3-3.5
- Density
- 7.35 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains, Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per micro-mount or small specimen
Where rockhounds find makovickyite
Classic worldwide localities
- Sweden
- China
- Russia
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where makovickyite typically forms. If you start seeing galena, bismuthinite, chalcopyrite in float, you are in the right ground. Field specimens usually show a anhedral grains, tabular crystals habit, so train your eye for that shape before scanning the outcrop.






