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 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Parasterryite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Parasterryite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray, iron-black.
- 5Look at form & habitCrystal system: orthorhombic. 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
- Ag₄Pb₄Sb₁₀S₂₃
- Mohs hardness
- 3
- Density
- 6.45 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular to Prismatic Crystals
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find parasterryite
Classic worldwide localities
- Wolfsberg, Germany
- Bolivia
- Romania
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where parasterryite typically forms. If you start seeing galena, stibnite, pyrite in float, you are in the right ground. Field specimens usually show a acicular to prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






