Stibnite is recognized by its distinct metallic lead-gray color and highly prismatic, deeply striated crystals that often form radiating clusters. It is quite soft and has perfect cleavage, making it a brittle specimen that requires careful handling. It is primarily found in low-temperature hydrothermal veins and is a significant ore for the metal antimony.
Is this stibnite?
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 stibnite with a known reference. Stibnite sits at Mohs 2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: lead-gray.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic, splendent on cleavage surfaces.
- 4Match the color rangeCompare against the expected color range: lead-gray, steel-gray, blackish-gray, bluish lead gray, black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: granular, prismatic, striated.
Often confused with
Stibnite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside stibnite
Minerals reported to co-occur with stibnite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Sb₂S₃
- Mohs hardness
- 2
- Density
- 4.63 g/cm³
- Colors
- Streak
- Lead-gray
- Luster
- Metallic, splendent on cleavage surfaces
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Granular, prismatic, striated
- Cleavage
- Perfect and easy on {010}; imperfect on {100} and {110}
- Rarity
- Common
- Uses
- Collector, Ore of antimony
- Host rock
- Of hydrothermal origin, formed in veins through a wide range of temperatures
Where rockhounds find stibnite
8 mapped spotsClassic worldwide localities
- White Caps mine, Manhattan district, Nye Co., and the Murray mine, Independence Mountains district, Elko Co., Nevada, USA
- San José and other mines, Oruro, Bolivia
- Wolfsberg, Harz Mountains, and near Arnsberg, North Rhine-Westphalia, Germany
- Kremnica (Kremnitz) and Banská Štiavnica (Schemnitz), Slovakia
- Příbram, Czech Republic
- Baia Sprie (Felsőbánya) and Herja (Kisbánya), Baia Mare (Nagybánya) district, Romania
Field-hunting tip
Where it forms: Of hydrothermal origin, formed in veins through a wide range of temperatures. If you start seeing realgar, orpiment, cinnabar in float, you are in the right ground. Typical habit: granular, prismatic, striated. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Idaho, Washington, Arizona. Start trip planning there.










