
THE
MINERAL NAGYAGITE

- Chemistry: AuPb(Sb, Bi)Te2 - 3S6, Gold Lead Antimony Bismuth Iron Tellurium Sulfide
- Class: Sulfides
- Subclass: Sulfosalts and Tellurides
- Uses: As a very minor ore of gold and as mineral specimens.
- Specimens
Nagyagite's chemistry is golden! Nagyagite is one of only a few minerals that are composed of gold. Gold does not often combine with other elements and seems to prefer an existance as elemental, native gold. But there are a few gold minerals and most of those are tellurides, like nagyagite. The two most common and better known gold tellurides are calaverite and sylvanite.
All three minerals are found in relative abundance at a classic gold locality; Sacaramb, Transylvania, Romania.
This is the type locality for nagyagite (from where it was first described).
Sacaramb was formerly named Nagyag, hence the name for nagyagite.
The Sacaramb gold mines are the type localities for several rare and classic gold and silver tellurium minerals such as
PHYSICAL CHARACTERISTICS:
- Color is a dark lead gray to black.
- Luster is metallic.
- Transparency: Crystals are opaque.
- Crystal System: Orthorhombic (pseudotetragonal).
- Crystal Habits include platy to tabular crystals as well as foliated to micaceous masses.
- Cleavage: perfect in one direction (basal).
- Fracture: hackly.
- Hardness is 1 - 1.5
- Specific Gravity is 7.4 - 7.6 (much heavier than average for metallic minerals)
- Streak is dark gray.
- Associated Minerals include
quartz,
krennerite , hessite, native gold calaverite and sylvanite. - Notable Occurrences include the type locality of Sacaramb (formerly Nagyag, hence the name), Transylvania, Romania as well as Kalgoorlie, Western Australia; Washburn Mine, Sunshine and Gold Hill, Boulder County, Colorado; Dorleska Mine, Trinity County and in Shasta and Calaveras Counties, California and Kings Mountain Mine, Gaston County, North Carolina, USA.
- Best Field Indicators are crystal habit, color, softness, locality, associations and density.
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