Tetrahedrite

Tetrahedrite specimens for sale

75 for sale · $80–$9,000 USD

248 in the gallery

Tetrahedrite is a copper antimony sulfosalt mineral that forms metallic, often prismatic to tabular crystals with a brilliant to submetallic lustre. The mineral commonly presents a dark grey to brownish copper colour and can occur as aggregates or intergrown crystals within hydrothermal veins and sulfide-rich deposits. Notable specimens come from classic localities in the USA, Peru, the UK, Romania and Germany, where high-quality, well-formed crystals are found in pockets and vug fillings. The mineral’s structure and habit yield striking, sometimes striated faces that can display a subtle bronzy sheen, making it a favorite for cabinet displays and micromounts.

Formula
Cu6(Cu4Ni2)Sb4S12S
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Sulfosalt mineral (Cu–Sb–S system)

Key characteristics

Crystal system
isometric
Mohs hardness
3.5–4.5
Specific gravity
4.6–5.1
Luster
metallic, submetallic
Transparency
opaque
Color
gray, black, brown
Streak
black, brown, red
Cleavage
none
Fracture
subconchoidal, uneven
Crystal habit
dodecahedral, equant, granular, massive
  • Classic / historic

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Where Tetrahedrite is found

Top localities

  1. Sweet Home Mine65 specimens
  2. Herodsfoot Mine25 specimens
  3. Casapalca Mine12 specimens
  4. Black Pine Mine9 specimens
  5. Cavnic8 specimens
  6. Casapalca7 specimens
  7. Huanzala Mine4 specimens
  8. Kellogg4 specimens
  9. Pachapaqui mining district4 specimens
  10. Beryozovsky4 specimens

About Tetrahedrite

Collectors prize tetrahedrite for its size, crystal form and the range of associated minerals it often accompanies, such as sphalerite, galena and pyrite. Detailed, well-crystallized specimens from famous mines offer a window into hydrothermal ore-forming processes and demonstrate the versatility of sulfosalt chemistry. In hand specimens and prepared slides, tetrahedrite provides visual interest through its metallic lustre, crystallographic geometry and the occasional occurrence of tetrahedral or complex polyhedral shapes that reveal the mineral’s intricate internal arrangement.