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?
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 hephaistosite with a known reference. Hephaistosite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Hephaistosite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Hephaistosite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: bright yellow, yellow-green.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: tabular crystals, crusts, coatings.
Often confused with
Hephaistosite vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Streak differs — Hephaistosite leaves yellow, Calomel leaves white.

How to tell apart: Laurionite is the harder of the two (Mohs 3-3.5 vs. 1.5-2); streak differs — Hephaistosite leaves yellow, Laurionite leaves white.
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
- Tl₂Cl₂Hg
- Mohs hardness
- 1.5-2
- Density
- 7.33 g/cm³
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Tetragonal
- Crystal habit
- Tabular Crystals, Crusts, Coatings
- Cleavage
- None Observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ancient Lead-silver Mine Slags
- Typical price
- $200-1000+ per specimen
Where rockhounds find hephaistosite
Classic worldwide localities
- Laurion, Greece
Field-hunting tip
Look in ancient lead-silver mine slags country — that is the host setting where hephaistosite typically forms. If you start seeing laurionite, fiedlerite, phosgenite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, coatings habit, so train your eye for that shape before scanning the outcrop.



