Costibite is a rare cobalt antimony sulfide often occurring as a component of hydrothermal veins alongside other cobalt minerals. It typically presents as metallic, tin-white massive aggregates that are difficult to distinguish from cobaltite without X-ray diffraction or chemical analysis.
Is this costibite?
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 costibite with a known reference. Costibite sits at Mohs 6, 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: steel gray.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: inclusions, lamellar.
Often confused with
Costibite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside costibite
Minerals reported to co-occur with costibite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CoSbS
- Mohs hardness
- 6
- Density
- 6.89 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Inclusions, lamellar
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Intimately intergrown with other hydrothermal sulfides (Broken Hill, Australia); in Pb–Zn–Cu–Ag ore deposits remobilized by hydrothermal solutions from later granite emplacement (Bergslagen, Sweden)
Where rockhounds find costibite
Classic worldwide localities
- Consols mine, Broken Hill, New South Wales (type locality), Australia
- Gruvåsen and Getön deposits, Bergslagen metallic province, Sweden
- Sulitjelma, northern Norway
Field-hunting tip
Where it forms: Intimately intergrown with other hydrothermal sulfides (Broken Hill, Australia); in Pb–Zn–Cu–Ag ore deposits remobilized by hydrothermal solutions from later granite emplacement (Bergslagen, Sweden). If you start seeing löllingite, willyamite, dyscrasite in float, you are in the right ground. Typical habit: inclusions, lamellar. Train your eye for that shape before scanning the outcrop.








