Parasterryite is a rare sulfosalt mineral found primarily in hydrothermal vein deposits. It is best identified by its metallic, lead-gray acicular crystal habit and its association with other complex lead-antimony sulfides.
Is this parasterryite?
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 parasterryite with a known reference. Parasterryite sits at Mohs 3-4, 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: black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: acicular to prismatic crystals.
Often confused with
Parasterryite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside parasterryite
Minerals reported to co-occur with parasterryite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ag₄Pb₂₀(Sb,As)₂₄S₅₈
- Mohs hardness
- 3-4
- Density
- 5.747 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Acicular to prismatic crystals
- Cleavage
- Poor perpendicular to elongation
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In vugs within hydrothermal barite–quartz veins embedded in barite-pyrite lenses in complexly sheared and metamorphosed sedimentary rocks
Where rockhounds find parasterryite
Classic worldwide localities
- Pollone deposit,Valdicastello Carducci, near Pietrasanta, Apuan Alps, Tuscany, Italy
Field-hunting tip
Where it forms: In vugs within hydrothermal barite–quartz veins embedded in barite-pyrite lenses in complexly sheared and metamorphosed sedimentary rocks. If you start seeing acanthite, famatinite, geocronite-jordanite in float, you are in the right ground. Typical habit: acicular to prismatic crystals. Train your eye for that shape before scanning the outcrop.








