Tennantite is a copper arsenic sulfosalt that forms a solid-solution series with tetrahedrite, in which antimony takes the place of arsenic, and the two are very hard to tell apart. It is gray-black to steel-gray and metallic, forming tetrahedral crystals or granular masses in hydrothermal veins and contact metamorphic deposits with other copper, lead, zinc and silver sulfides. It is rarer than tetrahedrite. It was first described from Cornwall, England, in 1819 and named for the English chemist Smithson Tennant.
Is this tennantite?
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 tennantite with a known reference. Tennantite sits at Mohs 3-4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: reddish gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: flint gray, steel gray, iron black, black.
- 5Look at form & habitCrystal system: cubic. Typical habit: tetrahedral crystals; massive, granular to compact.
Often confused with
Tennantite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside tennantite
Minerals reported to co-occur with tennantite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₆[Cu₄(Fe,Zn)₂]As₄S₁₃
- Mohs hardness
- 3-4.5
- Density
- 4.62 g/cm³
- Colors
- Streak
- Reddish gray
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Tetrahedral crystals; massive, granular to compact
- Cleavage
- None
- Uses
- Ore of copper
- Host rock
- Hydrothermal veins and contact metamorphic deposits
Where rockhounds find tennantite
Classic worldwide localities
- Cornwall, England (type locality)
- Tsumeb, Namibia
- Butte, Montana, USA
- Freiberg, Saxony, Germany
- Lengenbach quarry, Binntal, Switzerland
Field-hunting tip
Where it forms: Hydrothermal veins and contact metamorphic deposits. If you start seeing pyrite, calcite, dolomite in float, you are in the right ground. Typical habit: tetrahedral crystals; massive, granular to compact. Train your eye for that shape before scanning the outcrop.









