Hephaistosite is an extremely rare thallium-mercury chloride mineral found exclusively in the ancient metallurgical slags of Laurion, Greece. It typically occurs as minute, vibrant yellow-green tabular crystals or crusts coating other rare secondary minerals in the slag environment.
Is this hephaistosite?
3-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 hephaistosite with a known reference. Hephaistosite sits at Mohs 1.5-2, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: pale yellow.
- 3Look at form & habitCrystal system: monoclinic. Typical habit: aggregates.
Often confused with
Hephaistosite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside hephaistosite
Minerals reported to co-occur with hephaistosite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- TlPb₂Cl₅
- Mohs hardness
- 1.5-2
- Density
- 5.932 g/cm³
- Colors
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates
- Rarity
- Rare
- Uses
- Collector
- Host rock
- On fragments of altered pyroclastic breccia in a high temperature (400° C) fumarole, most likely formed as a sublimate
Where rockhounds find hephaistosite
Classic worldwide localities
- La Fossa crater, Vulcano, Aeolian Islands, Italy
Field-hunting tip
Where it forms: On fragments of altered pyroclastic breccia in a high temperature (400° C) fumarole, most likely formed as a sublimate. If you start seeing bismuthinite, cotunnite, challacolloite in float, you are in the right ground. Typical habit: aggregates. Train your eye for that shape before scanning the outcrop.






