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 — 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 — that is 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.


