Spaltiite is an extremely rare sulfosalt mineral found almost exclusively in the famous Lengenbach Quarry in Switzerland. It is best identified through laboratory analysis of metallic, lead-gray aggregates associated with other complex arsenic-bearing minerals in metamorphosed dolomitic marble.
Is this spaltiite?
4-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 spaltiite with a known reference. Spaltiite sits at Mohs 2.5-3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: lead-gray, black.
- 4Look at form & habitCrystal system: monoclinic. Typical habit: massive, anhedral grains.
Often confused with
Spaltiite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside spaltiite
Minerals reported to co-occur with spaltiite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Tl₂Cu₂As₂S₅
- Mohs hardness
- 2.5-3
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, anhedral grains
- Rarity
- Rare
- Uses
- Collector
- Host rock
- dolomitic marble
Where rockhounds find spaltiite
Classic worldwide localities
- Lengenbach quarry, Im Feld, Binntal, Canton Wallis, Switzerland
Field-hunting tip
Where it forms: dolomitic marble. If you start seeing sartorite, dufrénoysite, realgar in float, you are in the right ground. Typical habit: massive, anhedral grains. Train your eye for that shape before scanning the outcrop.






