Stibnite

Stibnite specimens for sale

104 for sale · $40–$277,000 USD

381 in the gallery

Stibnite is a sulfide mineral composed of antimony and sulfur, typically forming slender, prismatic to acicular crystals that create dramatic, metallic gray to steel-colored displays. Crystals often occur as long, ribbon-like blades or fan-shaped aggregates with a brilliant metallic lustre and a black to dark gray patina when tarnished. The mineral commonly forms in hydrothermal veins and hot springs environments, frequently associated with quartz, realgar, or cinnabar, and it can occur in massive, spheroidal, or radiating habits in sulfide-rich ore deposits. Notable collecting localities include classic European and Asian districts as well as the United States and Mexico, where high-quality, well-formed crystals can be found in primary antimony deposits and hydrothermal vein systems.

Formula
Sb2S3
Rarity
Common
Stability
Stable
Collector interest
High Interest
Classification notes
Sulfide; simple sulfide, stibnite group (Strunz 2.DB.05)

Key characteristics

Crystal system
orthorhombic
Mohs hardness
2
Specific gravity
4.52–4.63
Luster
metallic
Transparency
opaque
Color
gray, black
Streak
gray, black
Cleavage
perfect
Fracture
subconchoidal, uneven
Crystal habit
prismatic, bladed, acicular, radiating, granular, massive
  • Classic / historic

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Where Stibnite is found

Top localities

  1. Wuning Mine62 specimens
  2. Ichinokawa Mine34 specimens
  3. Herja Mine31 specimens
  4. Baia Sprie26 specimens
  5. Xikuangshan Sb Deposit17 specimens
  6. Xikuangshan Mine17 specimens
  7. Wolfsberg8 specimens
  8. Manhattan Mining District5 specimens
  9. Cavnic4 specimens
  10. Banpo Mine3 specimens

About Stibnite

Collectors value stibnite for its striking needle-like crystals that can reach impressive lengths, their sharp terminations, and the contrast of metallic luster against contrasting host minerals. The mineral’s high refractive sheen under reflected light makes it a favorite for display, and specimen quality can range from tapered single blades to complex fan clusters. The association with rich mineral contexts and classic locality specimens adds historical interest for collectors seeking pieces with provenance and distinctive crystalline forms.