Christite is a very rare thallium-mercury sulfosalt that typically occurs as tiny, brilliant red tabular crystals. It is primarily found in association with realgar and other thallium minerals in specific gold-bearing hydrothermal deposits. Because of its toxicity and rarity, it is sought after exclusively by advanced mineral collectors.
Is this christite?
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 christite with a known reference. Christite 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. Christite leaves a orange-red streak.
- 3Read the lusterHold the specimen under a strong light. Christite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: red, deep red.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: small tabular crystals.
Often confused with
Christite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside christite
Minerals reported to co-occur with christite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- TlHgAsS₃
- Mohs hardness
- 1.5-2
- Density
- 5.68 g/cm³
- Streak
- Orange-red
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Small Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Sedimentary Deposits
- Typical price
- $100-500 for small thumbnail specimens
Where rockhounds find christite
Classic worldwide localities
- Carlin gold mine, Nevada, USA
- Getchell mine, Nevada, USA
- Allchar, North Macedonia
Field-hunting tip
Look in hydrothermal veins in sedimentary deposits country, the host setting where christite typically forms. If you start seeing realgar, orpiment, lorándite in float, you are in the right ground. Field specimens usually show a small tabular crystals habit, so train your eye for that shape before scanning the outcrop.






