
mineral
Quartz crystal with Pyrite inclusions
Silicon Dioxide (SiO2) with Iron Sulfide (FeS2)
Hardness: 7 (Quartz) / 6-6.5 (Pyrite); Color: White to translucent matrix with metallic gold inclusions; Luster: Vitreous to greasy (Quartz), Metallic (Pyrite); Crystal Structure: Trigonal (Quartz), Cubic (Pyrite); Cleavage: None (Quartz), Poor (Pyrite).
- Hardness
- 7 (Quartz) / 6-6
- Color
- White to translucent matrix with metallic gold inclusions
- Luster
- Vitreous to greasy (Quartz), Metallic (Pyrite)
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Physical properties
Hardness: 7 (Quartz) / 6-6.5 (Pyrite); Color: White to translucent matrix with metallic gold inclusions; Luster: Vitreous to greasy (Quartz), Metallic (Pyrite); Crystal Structure: Trigonal (Quartz), Cubic (Pyrite); Cleavage: None (Quartz), Poor (Pyrite).
Formation & geological history
Formed through hydrothermal processes where mineral-rich hot fluids cool in veins or cavities within host rocks. It can form across various geological ages, often in metamorphic or igneous environments, particularly near tectonic boundaries.
Uses & applications
Used primarily as decorative collector specimens, metaphysical healing stones, and occasionally in jewelry as cabochons or tumbled stones to display the metallic inclusions.
Geological facts
Quartz is one of the most abundant minerals on Earth. When Pyrite is included, it is often called 'Fool\'s Gold' within the crystal. These specimens are prized by collectors for the contrast between the translucent matrix and metallic flakes.
Field identification & locations
Identify by checking for the hardness of quartz (cannot be scratched by a steel nail) and the distinct brassy-yellow metallic glints of pyrite. Commonly found in mountainous regions like the Alps, Andes, or specifically in areas like the Tri-State Mining district in the US.
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