Kieftite is a rare cobalt antimonide mineral that forms part of the tilasite group, typically found in association with other cobalt minerals. It is identified primarily through laboratory analysis due to its visual similarity to more common metallic sulfides and arsenides.
Is this kieftite?
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 kieftite with a known reference. Kieftite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Kieftite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Kieftite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: anhedral grains and aggregates.
Often confused with
Kieftite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside kieftite
Minerals reported to co-occur with kieftite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CoSb₃
- Mohs hardness
- 3.5
- Density
- 7.35 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Anhedral Grains and Aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and quality
Where rockhounds find kieftite
Classic worldwide localities
- Tunaberg, Sweden
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where kieftite typically forms. If you start seeing skutterudite, cobaltite, chalcopyrite in float, you are in the right ground. Field specimens usually show a anhedral grains and aggregates habit, so train your eye for that shape before scanning the outcrop.




