Rayite is an exceptionally rare lead-silver-thallium sulfosalt mineral found almost exclusively in the unique Allchar deposit in North Macedonia. It typically appears as dark, metallic masses associated with other rare thallium-bearing minerals and arsenic sulfides like realgar and orpiment.
Is this rayite?
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 rayite with a known reference. Rayite 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. Rayite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Rayite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: dark gray, lead-gray, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, anhedral grains.
Often confused with
Rayite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Rayite leaves black, Galena leaves lead-gray.

How to tell apart: Streak differs — Rayite leaves black, Jamesonite leaves gray-black.

How to tell apart: Streak differs — Rayite leaves black, Bournonite leaves steel-gray.
Often found alongside rayite
Minerals reported to co-occur with rayite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₈Ag₂Tl₂Sb₈S₂₁
- Mohs hardness
- 3
- Density
- 5.68 g/cm³
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Anhedral Grains
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Mineral Deposits
- Typical price
- $100-500 thumbnail size
Where rockhounds find rayite
Classic worldwide localities
- Allchar deposit, North Macedonia
Field-hunting tip
Look in hydrothermal mineral deposits country — that is the host setting where rayite typically forms. If you start seeing lorandite, realgar, orpiment in float, you are in the right ground. Field specimens usually show a massive, anhedral grains habit, so train your eye for that shape before scanning the outcrop.




