
mineral
Milky Quartz with Pyrite inclusions
Silicon Dioxide (SiO2) with Iron Disulfide (FeS2)
AI-generated identification · may be incorrectHardness: Quartz 7 (Mohs), Pyrite 6-6.5; Color: White to translucent with brassy gold metallic flecks; Luster: Vitreous to greasy (quartz) and metallic (pyrite); Crystal Structure: Trigonal (quartz) and Isometric (pyrite); Cleavage: None/Conchoidal.
- Hardness
- Quartz 7 (Mohs), Pyrite 6-6
- Color
- White to translucent with brassy gold metallic flecks
- Luster
- Vitreous to greasy (quartz) and metallic (pyrite)
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Physical properties
Hardness: Quartz 7 (Mohs), Pyrite 6-6.5; Color: White to translucent with brassy gold metallic flecks; Luster: Vitreous to greasy (quartz) and metallic (pyrite); Crystal Structure: Trigonal (quartz) and Isometric (pyrite); Cleavage: None/Conchoidal.
Formation & geological history
Formed in hydrothermal veins and pegmatites through precipitation from hot, mineral-rich fluids escaping from cooling magma deep within the Earth's crust.
Uses & applications
Primarily collected as mineral specimens; Quartz is used in electronics and glass manufacturing, while Pyrite was historically a source of sulfur.
Geological facts
Pyrite is known as 'Fool\'s Gold' because its metallic luster often tricks novice prospectors into thinking they have found real gold; however, it is much harder and more brittle than gold.
Field identification & locations
Identify by quartz's ability to scratch glass and pyrite's brassy color and greenish-black streak. Commonly found in mountainous regions near volcanic or tectonic activity.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
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Granite
Granite (Phaneritic intrusive igneous rock)
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