Iltisite is an extremely rare mercury halide mineral typically found as small, vibrant yellow platy crystals. It is primarily known from its type locality in Austria, where it occurs as a secondary mineral in association with other mercury species. Collectors prize it for its scarcity and distinct crystalline appearance within mercury-rich mineral assemblages.
Is this iltisite?
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 iltisite with a known reference. Iltisite sits at Mohs 2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Iltisite leaves a yellow streak.
- 3Read the lusterHold the specimen under a strong light. Iltisite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange-yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: platy crystals, granular aggregates.
Often confused with
Iltisite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside iltisite
Minerals reported to co-occur with iltisite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Hg₂S(Cl,Br)₂
- Mohs hardness
- 2
- Density
- 6.8 g/cm³
- Colors
- Streak
- Yellow
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Platy Crystals, Granular Aggregates
- Cleavage
- Perfect On {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Limestone
- Typical price
- $100-500 thumbnail
Where rockhounds find iltisite
Classic worldwide localities
- Iltis Valley, near Kalsdorf, Austria
Field-hunting tip
Look in hydrothermal veins in limestone country — that is the host setting where iltisite typically forms. If you start seeing cinnabar, calomel, terlinguaite in float, you are in the right ground. Field specimens usually show a platy crystals, granular aggregates habit, so train your eye for that shape before scanning the outcrop.




