Ralphcannonite is an extremely rare thallium-bearing sulfosalt mineral found almost exclusively in the Allchar deposit of North Macedonia. Collectors typically encounter it as microscopic grains within complex ore assemblages rather than well-formed macroscopic crystals.
Is this ralphcannonite?
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 ralphcannonite with a known reference. Ralphcannonite sits at Mohs 3.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Ralphcannonite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Ralphcannonite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: steel-gray, black.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: anhedral grains.
Often confused with
Ralphcannonite vs. its common look-alikes, and how to tell them apart in the field.


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

How to tell apart: Streak differs, so Ralphcannonite leaves black, Bournonite leaves steel-gray.
Often found alongside ralphcannonite
Minerals reported to co-occur with ralphcannonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- PbSnTl₂S₄
- Mohs hardness
- 3.5
- Density
- 4.74 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Epithermal Deposits
- Typical price
- $200-800 per specimen
Where rockhounds find ralphcannonite
Classic worldwide localities
- Allchar, North Macedonia
Field-hunting tip
Look in hydrothermal epithermal deposits country, the host setting where ralphcannonite typically forms. If you start seeing lorandite, realgar, orpiment in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.




