Ferrostalderite is a rare member of the tetrahedrite group characterized by its iron-rich composition. It is typically found in rare, complex hydrothermal deposits such as those in the Binn Valley, usually appearing as small, dark tetrahedral crystals.
Is this ferrostalderite?
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 ferrostalderite with a known reference. Ferrostalderite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: tetragonal.
Often confused with
Ferrostalderite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ferrostalderite
Minerals reported to co-occur with ferrostalderite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuFe₂TlAs₂S₆
- Mohs hardness
- 3.5-4
- Density
- 4.528 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed as massive to interstitial sulfosalt accumulations in dolostone by late stage Tl-As-Cu-Fe-rich hydrothermal fluids during upper greenschist to lower amphibolite metamorphism
Where rockhounds find ferrostalderite
Classic worldwide localities
- Lengenbach quarry, Binn Valley, Wallis, Switzerland
Field-hunting tip
Where it forms: Formed as massive to interstitial sulfosalt accumulations in dolostone by late stage Tl-As-Cu-Fe-rich hydrothermal fluids during upper greenschist to lower amphibolite metamorphism. If you start seeing dolomite, realgar, baumhauerite in float, you are in the right ground.






