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 2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: lead-gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: lead gray, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: granular, tabular.
Often confused with
Rayite vs. its common look-alikes, and how to tell them apart in the field.


How to tell apart: Streak differs, so Rayite leaves lead-gray, Jamesonite leaves black. grayish.

How to tell apart: Streak differs, so Rayite leaves lead-gray, Bournonite leaves steel-gray to iron-black; luster reads metallic on Rayite and brilliant to dull on Bournonite.
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
- 2.5
- Density
- 6.13 g/cm³
- Streak
- Lead-gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Granular, tabular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a Precambrian polymetallic massive-sulfide deposit interbedded with kyanite-graphite schists, diopside-bearing calc-silicates, and meta-cherts
Where rockhounds find rayite
Classic worldwide localities
- Rajpura-Dariba polymetallic deposit, Udaipur district, Rajasthan, India (type locality)
Field-hunting tip
Where it forms: In a Precambrian polymetallic massive-sulfide deposit interbedded with kyanite-graphite schists, diopside-bearing calc-silicates, and meta-cherts. If you start seeing galena, meneghinite, owyheeite in float, you are in the right ground. Typical habit: granular, tabular. Train your eye for that shape before scanning the outcrop.


