Suredaite is a rare lead-tin sulfide mineral typically found in complex polymetallic hydrothermal vein systems. It is generally identified by its metallic lead-gray luster and its close association with other sulfosalt minerals in tin-bearing deposits.
Is this suredaite?
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 suredaite with a known reference. Suredaite 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. Suredaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Suredaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: lead-gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: anhedral to subhedral grains or massive.
Often confused with
Suredaite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Suredaite is noticeably harder (Mohs 3.5-4 vs. 2.5); streak differs, so Suredaite leaves black, Galena leaves lead-gray.

How to tell apart: Suredaite is noticeably harder (Mohs 3.5-4 vs. 2-2.5).

Often found alongside suredaite
Minerals reported to co-occur with suredaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSnS₃
- Mohs hardness
- 3.5-4
- Density
- 4.87 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Anhedral to Subhedral Grains or Massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen
Where rockhounds find suredaite
Classic worldwide localities
- Jujuy Province, Argentina
- Potosi Department, Bolivia
Field-hunting tip
Look in hydrothermal veins country, the host setting where suredaite typically forms. If you start seeing galena, sphalerite, pyrite in float, you are in the right ground. Field specimens usually show a anhedral to subhedral grains or massive habit, so train your eye for that shape before scanning the outcrop.


