Arsiccioite is an extremely rare sulfosalt mineral found in the Apuan Alps of Italy. It occurs as small, black, metallic crystals typically associated with mercury and thallium-bearing minerals in hydrothermal vein systems.
Is this arsiccioite?
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 arsiccioite with a known reference. Arsiccioite sits at Mohs 2-2.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: orange.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic to submetallic.
- 4Match the color rangeCompare against the expected color range: red, internal reflections weak, deep red.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: equant to subhedral crystals.
Often confused with
Arsiccioite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside arsiccioite
Minerals reported to co-occur with arsiccioite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- AgHg₂TlAs₂S₆
- Mohs hardness
- 2-2.5
- Density
- 5.989 g/cm³
- Colors
- Streak
- Orange
- Luster
- Metallic to submetallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Equant to subhedral crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a lens of microcrystalline barite near the contact between schist and pyrite-rich dolostone
Where rockhounds find arsiccioite
Classic worldwide localities
- Apuan Alps, Tuscany, Italy
Field-hunting tip
Where it forms: In a lens of microcrystalline barite near the contact between schist and pyrite-rich dolostone. If you start seeing protochabournéite, cinnabar, laffittite in float, you are in the right ground. Typical habit: equant to subhedral crystals. Train your eye for that shape before scanning the outcrop.








