Raberite is an extremely rare thallium-arsenic sulfosalt found primarily in the Allchar deposit of North Macedonia. It typically occurs as small black tabular crystals or in massive form, often associated with other rare thallium-bearing minerals.
Is this raberite?
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 raberite with a known reference. Raberite 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. Raberite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Raberite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: tabular crystals, massive.
Often confused with
Raberite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Raberite leaves black, Lorandite leaves cherry-red.

How to tell apart: Streak differs — Raberite leaves black, Smithite leaves orange-red; luster reads metallic on Raberite and adamantine on Smithite.
Often found alongside raberite
Minerals reported to co-occur with raberite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Tl₅As₂SbS₆
- Mohs hardness
- 2.5
- Density
- 4.86 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Tabular Crystals, Massive
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $100-500 per specimen
Where rockhounds find raberite
Classic worldwide localities
- Allchar, North Macedonia
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where raberite typically forms. If you start seeing lorandite, realgar, orpiment in float, you are in the right ground. Field specimens usually show a tabular crystals, massive habit, so train your eye for that shape before scanning the outcrop.



