Quatrandorite is a rare sulfosalt mineral primarily found in tin-silver hydrothermal deposits in Bolivia. It is typically identified by its elongated, striated, metallic gray prisms often intergrown with other complex sulfosalts.
Is this quatrandorite?
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 quatrandorite with a known reference. Quatrandorite 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. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: lead-gray, blackish-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: striated prismatic crystals.
Often confused with
Quatrandorite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside quatrandorite
Minerals reported to co-occur with quatrandorite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- AgPbSb₃S₆
- Mohs hardness
- 3-3.5
- Density
- 5.36 g/cm³
- Colors
- Lead-grayBlackish-gray
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Striated prismatic crystals
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector, Scientific study
- Host rock
- hydrothermal veins
Where rockhounds find quatrandorite
Classic worldwide localities
- Oruro, Bolivia
- San Jose Mine, Bolivia
Field-hunting tip
Where it forms: hydrothermal veins. If you start seeing stannite, cassiterite, pyrite in float, you are in the right ground. Typical habit: striated prismatic crystals. Train your eye for that shape before scanning the outcrop.





