
Jamesonite specimens for sale
19 for sale · $80–$12,500 USD
28 in the gallery
Jamesonite is a sulfosalt mineral with a metallic to submetallic luster, typically forming slender, tabular to needle-like crystals or radiating aggregates. Its color ranges from lead-gray to black, often with a silvery sheen on fresh surfaces. The mineral commonly displays a high specific gravity and a relatively brittle feel, with a habit that can include prismatic, bladed, or fibrous intergrowths. Crystallographic form is tetragonal, and crystals may form cohesive masses that are visually striking under reflected light.
- Formula
- Pb4FeSb6S14
- Rarity
- Common
- Stability
- Stable
- Collector interest
- Moderate Interest
- Classification notes
- Sulfosalts; Sulfide minerals (Sulfosalts)
Buy Jamesonite specimens
View all 19Where Jamesonite is found
Top localities
- Herja Mine10 specimens
- Trepča Stari Trg Mine7 specimens
- Yaogangxian Mine4 specimens
- Baia Sprie3 specimens
- San Jose Mine2 specimens
- Boldut Mine1 specimen
- Llallagua1 specimen
- Noche Buena Mine1 specimen
- Oruro (Department)1 specimen
- San Martín Mine1 specimen
About Jamesonite
Notable specimens come from classic localities in Romania, Bolivia, Mexico, Kosovo, and China, where Jamesonite occurs in hydrothermal sulfide veins associated with other sulfide minerals. Collectors prize well-formed crystal faces and sharp, lustrous surfaces, sometimes showing complex intergrowths with related sulfide minerals that enhance the specimen’s overall character. The mineral’s dark metallic appearance, combined with its lustrous sheen and unique crystalline habit, makes it a compelling piece for cabinet displays and mineral studies.
Collectors value Jamesonite for its distinctive morphology and the historical significance of the localities it represents. While not among the rarest sulfides, well-preserved crystals and aesthetically arranged specimens offer strong visual appeal and educational insight into sulfosalt mineralogy and hydrothermal ore-forming environments.





















