Sphalerite

Sphalerite specimens for sale

449 for sale · $30–$18,000 USD

2,134 in the gallery

Sphalerite is the zinc sulfide mineral that forms in a variety of crystal habits, from sharp, well-formed tetrahedra to more massive, smoky masses. Its color ranges across black, brown, yellow, and shades in between, often showing a resinous to adamantine luster that makes clean faces glow in reflected light. Crystals can be transparent to translucent and may occur in geodes, sulfide-rich veins, or hydrothermal deposits, frequently replacing or coexisting with other sulfide minerals.

Formula
ZnS
Rarity
Common
Stability
Stable
Collector interest
High Interest
Classification notes
Sulfide mineral; Strunz 2.C (Sphalerite group)

Key characteristics

Crystal system
isometric
Mohs hardness
3.5–4
Specific gravity
3.9–4.1
Luster
adamantine, resinous, submetallic
Transparency
transparent, translucent, opaque
Color
colorless, white, gray, black, brown, red, orange, yellow, green
Streak
white, yellow, brown
Cleavage
perfect
Fracture
conchoidal, uneven
Crystal habit
dodecahedral, druzy, granular, massive, equant
  • Gem mineral
  • Fluorescent: orange, yellow, red
  • Classic / historic

Buy Sphalerite specimens

View all 449

Where Sphalerite is found

Top localities

  1. Elmwood Mine263 specimens
  2. Ballard Mine93 specimens
  3. Picher Field66 specimens
  4. Naica61 specimens
  5. Áliva Mine46 specimens
  6. Eagle Mine42 specimens
  7. Herja Mine36 specimens
  8. Krushev dol Mine35 specimens
  9. Denton Mine32 specimens
  10. Cavnic31 specimens

About Sphalerite

Notable specimens come from classic mining districts in the United States, Bulgaria, Mexico, the United Kingdom, and Peru, where sphalerite can occur with galena, pyrite, and chalcopyrite. Some locales produce color-zoned or highly lustrous crystals that collectors seek for display and study, while massive crystalline masses are valued for their density and brio in a cabinet. Collectors prize sphalerite for its range of hues, its brightness under incident light, and the insight it provides into ore-forming environments.