Tennantite specimens for sale

42 for sale · $340–$9,500 USD

170 in the gallery

Tennantite is a copper arsenic sulfide mineral that forms as a metallic, often dark gray to black to bronze-gray aggregate. It commonly occurs in a crystalline, usually cubic or tetrahedral habit, with a bright metallic to submetallic luster that can show hints of iridescence on fresh surfaces. In well-formed specimens, sharp crystal faces and facets reveal the mineral’s geometric geometry, while massive aggregates display a granular to vein-filling texture. The color ranges from steel gray to almost black, sometimes with a brownish or bronze tinge, and it can accompany other sulfides and sulfosalts in hydrothermal ore deposits. Tennantite often occurs with its polymorphs and related minerals, adding contrast and interest to hand specimens and cabinet displays.

Formula
Cu6(Cu4Hg2)As4S12S
Rarity
Common
Stability
Stable
Collector interest
High Interest
Classification notes
Sulfosalt; copper-arsenide sulfide mineral (IMA/CNMNC), sulfide group

Key characteristics

Crystal system
isometric
Mohs hardness
3–4.5
Specific gravity
4.6–4.7
Luster
metallic, submetallic
Transparency
opaque
Color
gray, black, brown
Streak
black, brown, red
Cleavage
none
Fracture
subconchoidal, uneven
Crystal habit
equant, granular, massive
  • Classic / historic

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Where Tennantite is found

Top localities

  1. Tsumeb10 specimens
  2. Dzhezkazgan mining district6 specimens
  3. Freeland-Lamartine Mine6 specimens
  4. Concepción del Oro4 specimens
  5. Aranzazú Mine3 specimens
  6. Altyn-Tyube dioptase deposit2 specimens
  7. Julcani District2 specimens
  8. Lengenbach Quarry2 specimens
  9. Zacatecas2 specimens
  10. Balmat1 specimen

About Tennantite

Notable specimens come from historic and contemporary mining districts in Namibia, the United States, Mexico, Peru, and Kazakhstan, among others. Classic localities yield well-formed crystals and high luster, making Tennantite a favored specimen for mineral enthusiasts. Collectors value specimens that show clean crystal faces, good transparency in cleavage planes where present, and contrasting matrix or mineral associations that highlight its metallic brilliance. While more commonly encountered in opaque masses, the finest crystals offer a striking aesthetic for display and study alike.